Demy 8vo , 34.2 Pages , 27 Plates . Covers, 5s . ; with Leather Back and Extra Cloth Boards , &y. SYSTEMATIC LISTS ILLUSTRATIVE OF THE Flora, Fauna, Palaeontology, AND OF THE NORTH OF IRELAND. BY MEMBERS OF gjatolifits' ( 0M <3}M. VOL. I. Belfast: PRINTED FOR THE CLUB. V vU PREFACE. N the Annual Report of the Club for the year ending 31st March, 1870, it was stated that “The Committee considered it advisable that the Club should prepare complete lists of the Fauna, Flora, Geology, and Archaeology of Ulster, by publishing an annual contribution to such a work in addition to the ordinary Report.” The purpose thus indicated has been kept steadily in view, the work being inaugurated by Professor Ralph Tate, F.G.S., in a paper issued in 1870, as an appendix to the Report of that year. Owing to the long- continued researches, and the special knowledge required on the part of the authors of the lists, it has not been found possible to publish an appendix every year, nevertheless the series at the present time numbers twenty-one separate papers, extending over 342 pages, illustrated by 27 plates. Thus, though there have been occasional breaks in the regularity of the issue, it has so happened that sometimes several contributions were received and printed in one year, and accordingly the promise has been more than fulfilled. The papers that form the present volume have all appeared as appendices to the Club’s Proceedings, which are printed and dis- tributed annually, but, with a view to their publication in a collected form, the appendices have been separately paged. In these Memoirs, there are given the results of long-continued and laborious research by members of the Club, in the subjects as to 4 which they are most competent. These results are already in the possession of the earlier members ; but it is considered that the time has now arrived when they should be given to those more recently elected, and to the general public. In the treatment of the various subjects, conciseness has been the aim throughout; but the several compilers have arranged their matter in such manner as was considered by each the most suit- able for the elucidation of his subject with brevity. Whatever opinions may be formed as to the style or method of these papers, it is certain that they furnish the fullest, most authentic, and most recent information respecting their different departments. In issuing this, the first volume prepared in accordance with the plan of 1870, it is earnestly hoped that it may not only prove useful to such as are commencing to investigate, but that it may stimulate to further exertion those who have been long engaged in the work. Several branches of local Natural History remain still untouched, and much of our Archaeology requires further elucidation ; and for these purposes additional workers are wanted, and will doubtless be forthcoming. Many volumes such as this are required before the plan can be said to be complete, and it may reasonably be hoped that they will follow in due time. With a more ripened experience on the part of the Club, and a succession of compilers equally painstaking, but having still more extended knowledge, it may be anticipated that the present will be surpassed by future volumes of the series. WILLIAM SWANSTON, F.G.S., F. W. LOCKWOOD, | Hon. Secs. Belfast, November , 1886. TABLE OF CONTENTS. PAGE Appendix I. — A list of the Irish Liassic Fossils, with notes on the new and critical species, by Ralph Tate, Assoc. Lin. Soc., F.G.S., &c. Plate I. ... ... i ,, II. — A list of the Irish Liassic Foraminifera, by Joseph Wright, F.G.S., F.R.G.S.I. 25 ,, ,, — A list of the Fossils of the Estuarine Clays of the Counties of Down and Antrim, by Samuel Alex. Stewart, F.B.S.Edin. ... ... ... 27 ,, III, — A list of the Mosses of the North-east of Ireland, by Samuel Alex. Stewart, F.B.S.Edin. ... ... 41 ,, ,, — A list of the Cretaceous Microzoa of the North-east of Ireland, by Joseph Wright, F.G.S., F.R.G.S.I. Plates II. & III. ... ... ... ... 73 ,, IV. — Recent Foraminifera of Down and Antrim, by Joseph Wright, F.G.S., F.R.G.S.I. Plate IV. ... 101 ,, ,, — Correlation of the Silurian Rocks of County Down, by William Swanston, F.G. S., and Charles Lap- worth, F.G.S. Plates V., VI., VII 107 ,, V. — A list of the Post-Tertiary Foraminifera of the North- east of Ireland, by Joseph Wright, F.G.S. ... 149 ,, ,, — A list of the Mollusca of the Boulder Clay of the North-east of Ireland, by Samuel Alex. Stewart, F.B.S.Edin. ... ... ... ... 165 ,, VI. — A list of Recent Foraminifera from South Donegal, by Joseph Wright, F.G.S. Plate VIII. (in part) ... 178 ,, ,, — Sponge Remains from the Carboniferous Strata of Ben Bulben, near Sligo, by Joseph Wright, F.G.S. 189 6 Appendix 99 59 99 99 99 9 9 99 99 PAGE VI. — Fossil Sponge Spicules from the Carboniferous Strata of Ben Bulben, near Sligo, by H. J. Carter, F.R.S., &c. Plate VIII. (in part) ... ... 190 VII.— Supplement to a list of Mosses of the North-east of Ireland, by Samuel Alex. Stewart, F.B.S.Edin. 196 VIII. — Notes on Irish Coleoptera, by A. H. Haliday, F.L S. 21 1 „ — The Cromlechs of Antrim and Down, by William Gray, M.R.I.A. Plates IX. to XX 225 }s —Notes on the Pre-Historic Monuments at Carrowmore, near Sligo— the Battlefield of Northern Moytura, by Charles Elcock. Plates XXI. to XXIV. ... 249 IX.— Recent Ostracoda of Belfast Lough, by Samuel M. Malcomson, M.D. Plate XXV. ... ... 259 ,, —The Fungi of the North-east of Ireland, by Henry William Lett, M.A., T.C.D 265 1 1 — Foraminifera of “Protector ” Cruise, and from Rockport, Belfast Lough, by Joseph Wright, F.G.S. Plate XXVI 317 „ A list of the Cretaceous Microzoa of Ready Hill, County Derry, by Joseph Wright, F.G.S. Plate xxvii 327 „ —A list of Irish Coleoptera, by Robert Patterson, F.R.S. 335 7 LIST OF PLATES. Plate I. II. III. IV. V. VI. VII. VIII. IX. Irish Liassic Fossils — Tate. Cretaceous Microzoa of North-east of Ireland — Wright. — Recent Foraminifera of Down and Antrim — Wright. Graptolites of County Down — Swanston & Lapworth. Recent Foraminifera of South Donegal — Wright. Fossil Sponge Spicules from Ben Bulben — Carter. Cromlechs, &c., of Antrim, Carnanmore, & Doonan. X.— , ,, Roughfort and Mount Druid. XI — ,, Glegnagh and Cloughnaboghill. XII.- , ,, Cloughanuncher& Ballyvennaght XIII.— ,, Cloughs and Ticloy. XIV.— ,, Broadstone and Finvoy. XV.- ,, Cloughogan and Druid’s Altar. XVI.— of Down, Giant’s Ring and Kempe Stone XVII.— , , Mountstewart and Loughmoney XVIII.— ,, Loughanisland & Slidderyford. XIX.— ,, Cloughmore and Legananny. XX.— ,, Kilkeel and Causeway Water. XXI. — Cromlechs of Carrowmore, Co. Sligo, Dr. Petrie’s, No. 13 and No. 7 — Elcock. XXII. — Cromlechs of Carrowmore, Co. Sligo, Dr. Petrie’s, No. 4 and No. — Elcock. XXIII. — Cromlechs of Carrowmore, Co. Sligo, Dr. Petrie’s, No. 14 and No. — Elcock. XXIV. — Cromlechs of Carrowmore, Co. Sligo, Dr. Petrie’s, No. 37. — Elcock. XXV. — Recent Ostracoda of Belfast Lough — Malcomson. XXVI. — Foraminifera of “ Protector” Cruise, & Rockport — Wright. XXVII.— Cretaceous Foraminifera of Ready Hill — Wright. APPENDIX I . _A_ LIST OF THE SH IASSIC j^OSSILS, WITH NOTES ON THE NEW AND CRITICAL SPECIES, BY RALPH TATE, ASSOC. LIN. SOC., F.G.S., &c. Belfast Naturalists’ Field Club. September, 1870. A LIST OF THE IRISH LIASSIC FOSSILS, WITH NOTES ON THE NEW AND CRITICAL SPECIES, BY RALPH TATE, ASSOC. LIN. SOC., F.G.S., &c. ->■» ♦ ♦ < The only Author, excepting myself, who has enumerated the fossils of the Lias of the Province of Ulster— that division of Ireland in which, only, that forma- tion is developed — is the late General Portlock. The specimens on which he based the list in the “ Survey of Londonderry,” pp. 747 — 769 (1843), now form part of the Collection of the Museum of Prac- tical Geology, London, and that of the Museum of the Irish Geological Survey, Dublin ; these I have carefully examined, and the results arrived at are em- bodied in List I, in the left hand column of which are arranged the specific names quoted by Portlock, and in the right hand those that I have adopted. The sign ! is prefixed to those species, original specimens of which I have examined. Those included in brackets are for the present expunged from the list of Irish Liassic fossils, because from their known distribution, it is ex- tremely probable that these determinations are erroneous ; at any rate their identification requires further confirmation. Some species, examples of which are not now in the Portlockian Collection, have received new names. These are adopted, because there is no doubt that they are the species to which Portlock’s descriptions are applicable, and which, moreover, have occurred to me in the Liassic strata of the North of Ireland. The first column of List I. contains 107 specific names, but by the elimi- nation of synonyms, and the rejection of a few doubtful determinations, the Tate — List of Irish Liassic Fossils. number is reduced to 71. This has been increased during the last few years to 189, all of which species are catalogued in List II. This list cannot be considered complete, inasmuch as additional species have been found time after time, on the occasion of revisiting those sections, which have yielded the greater number of the fossils, and which, consequently, from past experience, will continue to reward a search by an industrious collector. The principal localities in County Antrim are Colin Glen and Cave Hill, near Belfast; Whitehead, Island Magee, and Waterloo, near Lame; Glenarm ; between Garron Point and Red Bay ; Ballintoy. In County Londonderry, Magilligan, Aghanloo, &c., whence Portlock obtained the majority of the species of his catalogue. List No. II. shows the range of each species in the several members of the Lias, as described by me in the Quarterly Journal Geological Society, Vol. xx., p. 103 (1863) ; Vol. xxiii., p. 297 (1867) ; Vol. xxvi. (1870). The Liassic system is represented in the North of Ireland by the forma- tions termed Rhsetic, Lower Lias, and Middle Lias. The Rhaetic series is as fully developed in the immediate neighbourhood of Belfast as in any portion of Great Britain; it is there capable of division into the “ Avicula contorta-shales,” and the White Lias. Not more than 29 species have been satisfactorily identified from this formation ; 24 of these occur in the lower zone, and 13 in the upper, whilst 5 of them pass up into the Lower Lias. The Lower Lias, which I have divided into four zones or palaeontological horizons, has yielded 15 1 species, 2 of which are common to the Middle Lias. The “ Planorbis Zone” has afforded 24 species; two only, Gervillia acuminata , and Mytilus subtilis , are confined to it, whilst the majority do not extend upwards beyond the overlying zone. The “ Angulatus-beds, relatively rich in Gasteropods and Corals, have yielded 120 species, 26 of which pass to the upper zones. The “ Bucklandi-beds” have not been so thoroughly searched as the lower zones, and I can only enumerate 21 species from them, but 5 of these appear to be limited to this horizon. The Ballintoy, or “ Belemnites acutus shales,” have yielded 44 species. They are comparatively rich in peculiar Cephalopods, and 19 species in all are confined to this zone. The Middle Lias at Ballintoy contains sixteen species, two only of which occur in the inferior beds. In the following table are indicated the number of species known and in- ferred that pass from lower to higher zones, and the total number of species in each member, of the Lias, and the per centage number of restricted species in each member. Tate — List of Irish Liassic Fossils. 5 Avicula Shales . . White Lias Avicula Shales White Lias Planorbis Zone Angulatus Zone Bucklandi Limestone Belemnite Shales Ballintoy Marls. Total species known and inferred. Per centage of restricted Species. 24 18 13 4 5 3 4 •- 1 |1 j 29 83 Planorbis Zone . . 24 22 8 7 I \) 1 >• 122 75 Angulatus „ 120 26 17 I ) Bucklandi „ 33 22 I 33 18 Belemnite Shales 44 1 2 44 45 Ballintov Marls 1 - .. 16 16 87-5 The specific names in List No. 2 supersede those which have previously been employed by me. The alterations have been necssitated in some cases on account of erroneous determinations, but, in the majority, because of the preference given to older names and synonymous denominations. CATALOGUE I. Amended List of Species cited by Portlock, from the Irish Lias . CLASS Species of Gen. Portlock’s List. ! Acrodus minimus, Ag. S sp. Portlock t. xiv., fol. 17 ! Gyrolepis Alberti, Ag. ! Gyrolepis tenuistriatus, Ag. ! Saurichthys apicalis, Ag. PICES. Species adopted. Acrodus minimus, Ag. Acrodus Tatei, Moore , MS. Gyrolepis Alberti, Ag. Gyrolepis tenuistriatus, Ag. Saurichthys apicalis, Ag. CLASS CEPHALOPODA. ! Ammonites armatus, Sow. ! Ammonites hastatus, Y dr3 B. ! Ammonites Bucklandi, Sow. ! Ammonites multicostatus, Sow. (pars) ! Ammonites Conybeari, Sow. 1 ! Ammonites striatulus, Sow. ! Ammonites elegans ? Sow. ! Ammonites lseviusculus ? Sow. ! Ammonites subradiatus ? Sow. ! Ammonites intermedius, Portl. ! Ammonites Johnstoni, Sow. Ammonites Lamberti, Sozv. ! Ammonites MacDonnelli, Portl. ! Ammonites planorbis, Sow. S Ammonites Sampsoni, Portl. [Ammonites radians, Rein .] ! Ammonites multicostatus, Sow. (pars) S Ammonites rotiformis, Sow. ! Belemnites abbreviatus, Mill. Ammonites armatus, Sow. Ammonites Bucklandi, Sow. Ammonites Sauzeanus, D’ Orb, Ammonites Conybeari, Sow. Ammonites Buvgnieri, D' Orb. Ammonites Johnstoni, Sow. Ammonites angulatus, Schloth. Ammonites MacDonnelli, Portl. Ammonites planorbis, Sow. ? Ammonites raricostatus, Ziet. Belemnites acutus, Mill. CLASS GASTEROPODA. ! Cerithium carbonarium ? Goldf. ! Dentalium tenue, Portl . ! Melania cf Bronni, Rom. ! Trochus anglicus, Sow. [Trochus fasciatus ? Sow.} Turritella percincta, Portl. ! Turritella tenuicostata, Portl. Cerithium gratum, Terq. Dentalium Portlocki, Tate. Turritella Dunkeri, Terq. Pleurotomaria similis, Sow. ? Pleurotomaria similis, Sow. Cerithium percinctum, Portl. Cerithium tenuicostatum, Portl. Tate — List of Irish Liassic Fossils. 7 CLASS CONCHIFERA. ! Area pulchra ? Sow. ! Astarte elegans, PhU. ! Astarte tetragona, Portl. ! Avicula contorta, Portl. ! Avicula insequivalvis, Sow. ! Avicula modiolaris, Gold/. Avicula substriata, Brown. ! Cardium striatulum, Sow. # ! Cardium tnmeatum, Sow. Corbis ? ovalis, Phil. ! Cucullsea cucullata, Gold/. ! Gryphsea cymbium, Lamk. ! Gryphsea bullata ? Sow. Gryphsea dilatata, Sow. ! Gryphsea MacCullochi, Sow (pars) ! Gryphsea incurva, Sow. [Gryphsea MacCullochi, Sow. pars.] ! Inoceramus cinctus ? Gold/. ! Lysianassa rhombifera, Gold/. ! Lima altemans, Rom. Lima cardiiformis, Sow. ! Lima pectinoides, Sow. ! Lima antiquata, Sow. ! Lima Hermanni, Gold/. ! Lima rustica ? Sow. ! Lima duplicata, Sow. ! Lima gigantea, Sow. ! Lima proboscidea ? Sow. ! Lima punctata, Sow. ! Modiola bipartita ? Sow. Modiola compressa, Goldf. ! Modiola Hillana, Sow. ! id. pars. ! Modiola minima, Sow. ! Modiola alseformis, Sow. ! Modiola oblonga ? Rom. ! . Modiola, nov. spec. ! Modiola scalprum, Sow. ! Nucula antiquata ? Sow. ! Nucula subglobosa ? Rom. ! Nucula variabilis ? Sow ! Nucula rostralis, Gold/. ! Ostrea acuminata, Sow. Cucullsea Hettangiensis, Terq. Astarte Gueuxii, D' Orb. Avicula contorta, Portl. Avicula novemcostse, Brown. Avicula Pattersoni, Tate. ! Avicula papyria, Querist. Cardium Philippianum, Dunk. Cardium Rhseticum, Merian. Lucina limbata ? Terq. 6° P. Cucullsea Grangeri, Tate. Ostrea cymbium, var. obliqua, Lamk. Ostrea MacCullochi, Sow. Ostrea arcuata, Lamk. [Gryphsea vesiculosa, Sow. Cretaceous.] Pema infraliassica, Quenst. Goniomya Sinemuriensis, Oppel. Lima pectinoides, Sow. Lima succincta, Schlotk. Lima succincta, var. , jun. Lima Hettangiensis, Terq. Lima gigantea, Sow. Lima Terquemi, Tate. Lima punctata, Sow. Mytilus rusticus, Terq. ? Mytilus Hillanus, Sow. Mytilus minimus, Sow. Hippodium ponderosum, Sow. Cypricardia compressa, Terq. Myoconcha psilonoti, Quenst. Mytilus Gueuxii, D’Orb. Nucula navis, Piette. Leda tenuistriata, Piette. Ostrea irregularis, Miinst. * 8 Tate — List of Irish Liassic Fossils. Ostrea, nov. spec. Pachyodon concinnus, Sow. Pachyodon crassins cuius, Sow. Pachyodon ovalis, Stutch. Pachyodon hybridus, Sow. Pachyodon imbricatus, Siutch. Panopsea? elongata, Rom. Pecten sublsevis ? Phil. Pecten subulatus ? Munst. Pecten textilis ? Munst. Pecton textorius ? Schloth. Pecten virguliferus ? Phil. Pecten Valoniensis, Defr. Pecten vitreus, Rom. Pecten calvus, Goldf. Pecten cingulatus, Goldf. Pinna cuneata, Phil. Pinna lanceolata, Sow. Pinna mitis ? Phil. Pinna Hertmanni, Ziet. Plicatula spinosa ? Sow. Pholodomya longirostris, Schloth. Pholadomya ventricosa, Goldf. Pholadomya myacites. Pullastra ? Unio Listeri, Sow. Unio Nilssoni, K. <%° D. Unio peregrinus ? Phil. Unio trigonus, Rom. Unio subsequalis. Terquemia, arietes, Quenst. Cardinia concinna, Sow. Cardinia ovalis, Stutch. Cardinia Listeri, Sow, var. hybrida. Cardinia Listeri, Sow., var. imbricata. Anatina longissima, Quenst. » Pecten dextilis, Munst. Pecten textorius, Schloth. Pecten Valoniensis, Defr. Pecten lunularis, Rom. Pinna folium, Y. 6° B. Pinna Harmanni, Ziet. Plicatula spinosa, Sow. Pholodomya Fraasii, Oppel. Pholadomya glabra, Ag. Pleuromya liasina, Schiibl Pleuromya galathea, Ag. Cardinia Listeri, Sow. Cardinia ovalis, Stutch. Unicardium cardioides, Phil. CLASS BRACHIOPODA. Lingula Metensis, Terq. Rhynchonella plicatissima, Qnst. Waldhemia perforata, Piette. ! Lingula Beanii, Sow. Terebratula Mantelliana ? Sow. Terebratula obovata, Sow. ! Terebrata omithocephala, Sow. CLASS ANNELIDA. ! [Serpula lsevis, Goldf. Serpula filiformis, Sow. Cretaceous]. CLASS ECHINODERMATA. ! Pentacrinites basaltiformis ? Extracrinus Briareus, Mill. CATALOGUE ii. As Enumeration op the Liassio Species in the Ibish Sub-divisions. Explanations of Abbreviations. V.C. very common; 6. common; x. not common, or frequency unobserved ; r. rare; V.r. very rare. List of Species, Distribution. Class Reptilia. Ichthyosaurus sp. (femur, teeth), Ichthyosaurus (vertebrae), Class Pices. Acrodus minimus, Ag Acrodus Tatei, Moore Gyrolepis Alberti, Ag Gyrolepis tenuistriatus, Ag. Hybodus minor, Ag Hybodus raricostatus, Ag.. . Hybodus reticulatus, Ag. . . . Saurichthys apiealis, Ag. . . . Class Cephalopoda. Ammonites angulatus, Schloth . Ammonites armatus, Sow Ammonites Birchii, Sow Ammonites Bucklandi, Sow . . . . Ammonites Buvgneiri, D’ Orb . . Ammonites Conybeari, Sow .. .. Ammonites Johnstoni, Sow Ammonites MacDonnelli, Portl.. Ammonites margaritatus, Montf. ,, var. coronatus, Quenst Ammonites Henleyi, Sow Ammonites planorbis, Sow . . . . Ammonites Sauzeanus, D’Orb. Ammonites Turneri, Sow Ammonites raricostatus, Sow . Belemnites acutus, Mill.. .. .. . Belemnites pencillatus, Mill . . Belemnites praematurus, Tate.. . Belemnites umbilicatus, Blainv. Nautilus striatus, Sow Class Gasteropoda. Actaeonina avena, Terq Actaeonina fragilis, Dunk... . Rhaetic. Lower Lias. Midle. Lias. Avicula Shales. White Lias. A. planorbis Zone. — A. angulatus Zone. A. Bucklandi Limestones. Belemnite Shales. Ballintoy Marls. r. X. c. c. c. X. j X. r. r. c. ! ::: r* r. C. r. X. X. X. pc. X. c. V.C. X. r. x. ( I c. X. X. ( ( < X. V.C. c. c. X. i r. c. X. X. C. *Portrush. 10 Tate— List of Irish Liassic Fossils, T ABLE — (continued.) Distribution. Rhsetic. Lower Lias. Midle. Lias. List of Species. i £ cS 3 O V < o5 eS 3 CD 35 •cl £ > o M Actseonina striata, Piette X. ... 1 Cerithium gratum, Terq v.c. Cerithium Semele, D'Orb c. X. On authority of Gen. Portlock. Cerithium percinctum, Portl ... X. Cerithium tenuicostatum, Portl c. Chemnitzia punctata, nov. spec v.r. = Chemnitzia Chemnitzia Berthaudi, Dumortier. . ... v.c. Cryptsenia Brycei, Tate ... r. r. Tylori, Tate. Cryptsenia expansa?, Sow r. Cryptsenia rotellseformis, Dunk.. . . v.r. Den tali um Portlocki, nov. spec Littorina Chapuisi, Terq & Piette... X. v.r. Littorina elegans, Miinst v.c. Littorina liassica, Martin Littorina Strophium, Dumort sp . . r. v.r. Natica Oppelii, Moore X. Pleurotomaria similis, Sow r. r. Pleurotomaria Teetaria, nov. spec . . r. Phasianella Morencyana, Trq. & Pte. c. Pitonillus turbiuatus, Moore. ...... c. Solarium Thomsoni, nov. spec r. Waterloo. Tornatella inermis, Terq X. Tornatella Robinsoni, nov. spec. . . . v.r. Trochus Waltoni, Moore X. Turitella crassilabrata, Trq. & Pte.. v.r. Turitella Dunkeri, Terq r. = Turbo Bur- Turbo solarium, Piette .. X. Class CONCIIIFBRA. Anatina longissima, Quenst X. 1 ? X. toni, Tate , Gar- ron Point. Anatina myacina, nov. spec v.r Anatina prsecursor, Quenst X. Anomia irregularis, Terq X. X. ?' Anomia pellucida, Terq X. X. Anomia striatula, Op X. Area pulla, Terq X. = Astarte den- tilabrum, Etheridge. Astarte Gueuxii, D'Orb X. ? X.? Astarte cingulata, Terq X. 1 Astarte Oppelii, Andler X. =A Saulensis, Axinopsis Ewaldi, Bornem X. X. T. & P., Coll. Geo. Survey, Ireland. = Axinus cloa- Axinopsis concentricus, Moore X. cinus, Quenst. Avicula acuticosta, Terq & Piette . . X. ... 1 Tate — List of Irish Liassic Fossils. ii T ABLE— (continued.) List of Species, Avicula contorta, Portl. Avicula Dunkeri, Terq. . Avicula fallax, Avicula novemcostse, Brown . Avicula Pattersoni, nov. spec.., Avicula papyria, Querist Cardium Philippian um, Dunk. Cardium Rhseticum, Merian. . . Cardinia amygdala, Terq Cardinia Deshayesi, Terq Cardinia cyprina, Ag Cardinia concinna, Sow Cardinia Listeri, Sow Cardinia Listeri, var. hybrida . Cardinia ovalis, Stutch Cardita Heberti, Terq Cardita multicostata, Phil. . . . Ceromya gibbosa, Etheridge . . Cypricardia compressa, Terq. . Cypricardia laevigata, Terq. . . . Cypricardia tetragona, Terq. . Cypricardia cucullata, Gold/. . Cu cull sea Grangeri, nov. spec. . Cucullsea Hettangiensis. Terq . Cucullsea oxynoti, Quenst. Gervillia acuminata, Terq. Distribution. l^bsetic. Lower Lias. Midle. Lias. Goniomya Sinemuriensis, Op. . . . Hippopodium ponderosum, Sow . Hinnites angularis, nov. spec — Leda Bronni, Andler Leda Dewalquei, Terq & Piette Leda Quenstedti, nov. spec Leda Renevieri, Oppel Leda v-scripta, nov. spec Leda tenuistriata, Piette Lima gigantea, Sow Lima Hettangiensis, Terq Lima pectinoides, Sow Lima prsecursor, Quenst Lima punctata, Sow Lima succincta, Ziet Lima Terquemi, Tate Lima Yaloniensis, Def. j c5 a5 m m tab. xiv, fig. 2, .1867. Chemnitzia Tylori , Tate, Quart. Jour, Geol. Soc., Vol. xx, p. 3 1 3 (1867)- Shell turreted, elongated, consisting of ten whorls separated by a deep suture, concave, and ornamented by about twenty very prominent curved smooth ribs ; the sulci faintly striated ; base slightly carinated, smooth or faintly radiated. Total length 3 inch, breadth of last whorl -07 inch. Affinities and Differences. — By its ornamentation closely allied to C. costifera, Piette, and Cerithium Henrici , Martin, but differs from the former apparently in the proportion of its dimensions, and in the less arched outline of the costae ; and from the latter in being only about half the length of that shell, which is pro- vided with only eight whorls. I have no hesitation in referring the shell I had described as C. Tylori to C. Berthaudi , Dumortier, which has priority by some- months. Geological Position. — C. Berthaudi vs, a common shell in the zone of “ A. angulatus” Island Magee, Co. Antrim. The type of the species is unique, and was obtained from the zone of “A. Bucklandi ” at Peronne, Rhone. 7. Solarium Thomsoni, now spec ., Plate I. fig. 9, Shell orbicular, a little wider than high, spire slightly raised, composed of lour whorls, smooth, or ornamented with about 6 raised lines ; last whorl rounded, smooth ; aperture quadrate ; base flat, with fine strice of growth umbilicus narrow and slightly crenulated on its border. Height, ‘075 inch \ diameter, ‘085 inch. Remarks. —S. Thomsoni is allied to S, lenticular e , Terq., but differs in its more embracing whorls and Rotella-like appearance, in its smaller umbilicus, and its more conical form. Geological Position—. Zone of “ A. angulatus , ” Glenarm ; (rare, R. T). The species is dedicated to Professor Wyville Thomson, F. R. S-., President of the Natural History Society, Belfast. 8. Crypt^enia Brycei. Tate, Quart. Jour. GeoL Soc., Vol, xxiii., p, 413 (1867). Plate I. fig. 13. Shell subdiscoid, depressed ; test thin, whorls four, nearly flat or slightly concave ; bluntly carinated ; upper surface of the whorls transversely striated ; base convex, smooth ; callosity large, circumscribed by a sulcus, slightly exca- vated near the columella lip ; siphonal band narrow, rather above than below the keel ; aperture, sub-triangular. Tate — List of Irish Liassic Fossils. 7 Remarks.— C. Brycei is somewhat intermediate between C. caepa , Desk, and C. expansa, Sow. ; it is related to the latter by the concave and carinated whorls, by the band being above the keel, and by the large callus, but differs in its more regularly conoidal form, without the ventricosity of the under sur- face, and by the absence of the raised border to the posterior suture. Geological Position— Zone of “A. angulatus ,” Island Magee; (rare, Gray dr5 Tate) ; Garron Point, Co. Antrim ( R. T). 9. Tornatella Robinsoni, nov. spec., Plate I. fig. 7. Shell ovate-oblong ; spire produced, apex acute ; whorls scalariform, a little obtuse, and with an elevated margin ; the whole surface ornamented with fine longitudinal striae, whilst from the posterior suture fine curved lines pro- ceed to a little beyond the shoulder of the whorl ; aperture ovate, acute ; columella with a single plait. Geological Position. — Zone of ‘ 1 Belemnites acutus , Ballintoy ; very rare (Coll. Belfast Museum). Dedicated to Mr. Hugh Robinson, one of the energetic Secretaries of the Belfast Naturalists’ Field Club. 10. Dentalium Portlocki, nov. spec., Plate I. fig. 15. 1843 Dentalium tenue, Portlock. loc. cit., p. 118 (non Goldfuss, 1841). 1856 Dentalium Andleri, Oppel, Die Juraformation, p. 93 (probably). 1863 Dentalium minimum, pars, Tate, Quart. Jour. Geol. Soc., Vol. xx., p. 3. 1867 Dentalium tenue, Tate, id., Vol. xx., p. 31 1. Remarks. — In 1863, I referred D. tenue, of Portlock, to D. minimum, Strickland, as I then considered the two names synonymous, adopting the latter, because the specific name applied by Portlock was pre-occupied by a Dentalium described by Munster, to which species his shell is not referable ; at a later period I regarded them as distinct, and erroneously gave priority to Portlock’s employment of the specific name. In giving the above denomination to the species described by Portlock, I wish to commemorate the labours of that geologist. The original diagnosis is as follows : — “ The longest ‘4 of an inch, is about -04 of an inch in diameter at the largest end, and tapers to a fine point ; it is very slightly curved.” D. Andleri, Oppel, is probably a synonym to D. Portlocki ; the only character given is, that it is small— “die kleine species but, assuming that the two names refer to the same species, the im- perfect diagnosis of Oppel justifies me in discarding his name. 11. Pleurotomaria Tectaria, nov. spec. Shell turbinated conical, scalariform, spire acute ; whorls six, subquadrate, last whorl with two prominent carinse, separated by a slightly concave area ; surface of whorls strongly longitudinally striated, upper part of each whorl 3 Tate— List of Irish Liassic Fossils. i8 cancellated by very fine oblique striae. Siphonal band very narrow, occupying a slight depression on the upper carina, ornamented with three longitudinal striae. Base imperforate, concentrically striated ; aperture subquadrangular. Dimensions.— Total length, -9 inch ; breadth of last whorl, ’6 inch ; height of last whorl, -4 inch. P. Tectaria cannot be confounded with any Liassic species of the genus, though related to P. subtilis , Deslong. It resembles in figure, several Palaeozoic forms, and especially P. tornatilis , Phil., from the Carboniferous Limestone. Geological Position. — Zone of A. angulatus , between Garron Point and Red Bay, two examples fi?. T. ) ; Island Magee, one example (S. A. Stewart). 12. — Hinnites angularis, nov. spec., Plate I. fig. 2. Shell inequivale, subinaequilateral, thick, left valve convex, transversely oblong; umbo subacute, not extending beyond the hinge line, which is moderately arched; ornamented with crowded radiating ribs, unequal, obtuse, the surface of which is raised into spinous squamae, and alternating irregularly with smaller and similarly ornamented costae; costae of umbonal region without spinous nodulations. Five or six of the radiating costae are much stronger than the others, and somewhat regularly disposed, giving a polygonal outline to the valve. Ears ornamented as the rest of the shell. Right valve ornamented as the other valve. Breadth 2-5 inches, length 2 inches. H. angularis agrees with Lima nodulosa, Terq., in the radiating spiniferous ribs, alternately large and small; but differs in the absence of rugous, serrated concentric stria, and in its greater gibbosity, oblong figure, inequivalve character, and by the polygonal outline given to it by the larger ribs. Geological Position.— Zone of “A. angulatus,” Island. Magee, two ex- amples {R. T.); lowest beds of Lower Lias, Laleston, S. Wales. {P. Etheridge ), Coll. Brit. Museum. 13. — Avicula Pattersoni, nov. spec., Plate I. fig. 10. Shell dfepressed, ovate, transverse, slightly oblique, concentrically striated; anterior margin arched, and superiorly sinuated; hinge line straight; anterior wing very short, acute; posterior wing elongated, acuminated, excavated behind. A. Pattersoni has a general resemblance to Gervillia crenatula, Quenst., which the author states distinctly to possess cardinal pits, and as the type specimen of this species displays a single extended cartilage pit, it cannot be referred to that genus. It has much analogy with A . Deshay esi, Terqm., but is much less oblique, has a smaller anterior wing, and an acute umbo, not being so concave a shell as that species. This species was referred by Portlock to A. Goldfussi. Several specimens from Craig and Gortmore form part of the Portlockian collection. The figured specimen I obtained from the Zone of 11 A. angulatus” at Island Magee. The species is dedicated to my kind friend Robert Patterson, Esq., F.R.S. Tate — List of Irish Liassic Fossils. 19 14. — Lbda v-scripta, nov. spec., Plate I. fig. 5. Shell elliptical; anterior portion rounded, ventricose; posterior elongated, rostrated; ventral margin strongly arched; medial portion of shell ornamented by plications en chevron; the rostral and anterior extremities with oblique plaits. Geological Position. — Zone of “A. angulatus ” Waterloo, Lame. Very rare; {R. T.) 15. — Leda Bronni, Andler , Neues Jarbuch f. Min., p. 642(1858). See Plate I. fig. 1. Nucula palmce , Quenstedt, Jura, t. 13, fig. 42, p. 116, non t. 23, figs. 16.-17., t. 44., fig. 8. (1858). This species resembles L. subovalis of the Middle Lias, from which it is especially distinguished, as pointed out by Andler, in the greater gibbosity of the umbonal region. It is common in the Zone of “ Belemnites acutus ” at Ballintoy, and occurs in the inferior zones. I have recorded it in England from the Zone of “ Ammonites Angulatus ” at Marton, Lincolnshire. 16. — Leda Quenstedti, nov. spec., Plate I. fig. 4. Nuaila inflexa, Quenst., Jura, t. xiii., fig. 41, p. no (1858). This species has been confounded by Quenstedt with L. galathea, d’Orbigny, a moderately common shell in the Middle Lias of England, France, and Germany, from which it is distinguished by its more robust and less inequi- lateral form, and -in the abruptly truncated posterior extremity. Geological Position — Zones of il A. planorbis' ” Garron Point, and (< A. angulatus ,” Island Magee, Co. Antrim {R.T.); Upper part Lower Lias, Ballintoy, Co. Antrim [P. T.) ; and Ofterdingen, Wurtemburg {Quenstedt.) 17. Leda Renevieri, Oppel , Die Juraf., p. 95 (1857). See Plate I. fig 3. Nucula complanata, Quenstedt, Jura, t. 13, fig. 39 ; p. no (1858). The shell represented by fig 3, differs in a few particulars from the ordinary form of Z. tenuistriata, Piette, but may be a young state of that species. Quenstedt’s figure, which I have referred to, evidently represents the same species, which may be the one described by Oppel, in the following terms : Resembles Z. complanata , Goldfuss, but does not attain the same size, and the anterior prolongation is shorter.” Geological Position. — Zone of “ A. Bucklandi, ” Glynn, near Larne (P. T. ) Recorded by Oppel in the Zone of “A. angulatus” and by Quenstedt, from the upper part of the Lower Lias in Swabia. 18. CUCULL;£A Grangeri, nov. spec., Plate I. fig. 12. Cucullcea cucullata, Portlock, Geol. Survey of Derry, p. 120. Shell ovate-rhomboidal, ventricose, rounded in front, and obliquely trun- cated behind, bluntly keeled from the umbo to the posterior angle ; umbones 20 Tate — List of Irish Liassic Fossils. submedial, prominent, broad, high, and incurved. Ornamented with concentric striae, varying in the degree of fineness ; and radiating striae, which are very fine, not distinctly visible without the aid of a magnifier, excepting on the an- terior concave area. The striae merge into impressed circular spaces on the superior margin of the transverse striae, so that the surface, when viewed in certain positions, appears to be regularly punctated. Length, ’35 mch ; breadth, *5. This species is not comparable with any of the Liassic Arcidce', its peculiai ornamentation separates it from C. cucullata, Goldfuss. Geological Position— Upper part of Lower Lias, Ballintoy, Co. Antrim ( Portlock , R. 7, &>c.), where it is very abundant. Dedicated to my esteemed friend the Rev. John Grainger, A.M., the first President of the Belfast Naturalists’ Field Club. 19. Mytilus subtilis, nov. spec., Plate I. fig. 14- Shell elongated, reniform, concentrically plicated and ornamented with closely-set radiating incised lines, which are visible only with the aid of a magnifier ; dorsal margin curved ; ventral margin sinuated ; umbones approxi- mately terminal, prominent, small, incurved. Geologial Position. — Lowermost beds of the Lower Lias, Cave Hill, Belfast ; very rare ( S. A. Stewart). This species has the general form of M. nitidulus, Dunker, but is more cuneiform than that species, which does not possess the radial ornamentation. 20. Myoconcha oxynoti, Quenstedt, Jura, t. 13, fig. 34. A single valve of a narrow cylindrical Myoconcha , forming part of the col- lection in the Belfast Museum, displays the internal characters, but as the ex- terior is unobservable, the shell cannot satisfactorily be referred to any species. Terquem describes a small species from the Lower Lias, and Quenstedt figures the internal cast of another form from the same formation, under the denomina- tion of M. oxynoti. The test of the Ballintoy specimen is very thin, and from the interior sur- face it is judged that the exterior is marked with concentric corrugations and fine lines of growths. The apparent absence of radiating lines removes it from M. inclusa, Terquem, and, as it agrees in shape with M. oxynoti, Quenstedt, I refer it to that problematical species. Breadth, 1-4 inch ; length, *3 inch ; thickness, -i inch. Geological Position. — Zone of “ Belemniies acutus ,” Ballintoy. 21. Myoconcha psilonoti, Quenstedt, Jura, t. 4, fig. 15 (1858). ? Myoconcha scabra, Terquem & Piette, Pal. de l’Est de France ; t. 9, figs. 4-6 (1865). ? Myoconcha scalprum, et M. spaUda (pars) D’Orbigny, Prodromus, Vol. I, p. 218 (1850). Tate— List of Irish Liassic Fossils. 21 1 have no hesitation in referring the specimens named by D’ Orbigny as above, and which I have examined, to M scabra of Terquem & Piette, which I suspect is only the adult state of M. psilonoh. However, the Antrim shell agrees better with the latter. The species was known to Portloclc, in whose collection it is labelled Modiola , now. spec. 22. Astarte Gueuxii, iy Orbigny, Prodromus, Vol. I. p. 216 (1850). A. consobrina , Chapuis & Dewalque, Foss. du. Luxembourg, t. 22, fig- 3> P- 49 (*853)- A. complanata, et A. psilonoti , Quenstedt, Jura, t. 3> fig- I4 (i858)* A. deniUabmm , Etheridge, Quart. Jour. Geol. Soc., Vol. xx., p. 113(1863). This common Astarte I have compared with the type specimens of A. Gueuxii , to which I unhesitatingly refer it. M. Terquem has named specimens of A. dentilabrum, which I sent him, A. consobrina ; so that the synonymic terms may be considered well-established. Though D Orbigny s name has priority of publication, it has not been generally accepted, because of the sup- posed incompleteness of the description, which runs thus : “ Species allied to A. subtetragona , Romer, but less carinated, less compressed, and costulated only in the young state. ” Short as this diagnosis is, yet it is sufficient to its identification, and, conse- quently, the specific name A. Gueuxii should be used. A. Eryx, of the same author, is only a variety of this protean species ; and A. dentilabrum , Etheridge, is founded on an aged form of the same species. The original description of A. dentilabrum is as follows Shell massive, ovate, and deep. Postero- dorsal surface rounded, posterior end slightly truncate, about the position of the annal adductor to the ventral margin ; anterior margin acutely rounded. Umbones small, indistinct, subcentral, slightly curved anteriorly. Lunule slightly excavated, small, oval, and attenuated, occupying half the area between the umbo and the commencement of the antero- ventral margin. Boidei angu- lar ; costse concentrically arranged, and coincident with the contour of the shell. Ventral margin strongly denticulate. The whole of the teeth are inclined in- wards, giving the edge of the shell a bevilled appearance a marked feature in the shell.” 23. Pholadomya Fraasii, Oppel , Juraformation, p. 95. The specific name here adopted was given by Oppel to a shell from the Lower Lias, agreeing in form with P. ambigua , Ziet. , {P. glabra , Ag. ), but possessing from 9 to 12 rather strong ribs, coarsely wrinkled concentrically. Quenstedt has described the same species in much the same words with the name P. prima, which, by the way, is a misnomer, inasmuch as the genus dates farther back than the Lower Lias, and other species besides occur in the lowest beds of the Lias. 22 Tate — List of Irish Liassic Fossils. 24. Ceromya gibbosa, Etheridge , Quart. Jour. Geol. Soc., Vol. xx., p. 112, figs. 3-4 (1863). Isocar dia Elea, D’Orbigny, Prodromus, Vol. 1., p. 218 (1850). s.‘ Shell ventricose, deep, especially at the umbonal region. Umbones small, sub-central, slightly curved or involute, leaving a wide and exposed lunular region, strongly marked by concentric ridges of growth. Anterior side pro- duced, rounded and gaping. Posterior side attenuated, slightly truncate. Ventral margin much produced, giving the shell a nearly circular appearance. Height, 1 7 inch; depth, 1*3 inch; length, 2‘i inches.” — Etheridge. The specific identity of C. gibbosa, Etheridge, with Isocardia Elea , d’Orbigny, results from a comparison of the type specimens ; the diagnosis of the latter is so imperfect as to claim no consideration from palaeontologists. It is as follows: — “ Grosse espece bombee, triangulaire lisse, a crochets contoumes.” Geological Position. — Zone of “A. angulatus,” Island Magee, Co. Antrim; not rare ( Gray, Tate); Cotham, Bristol ! (Napier); “ A . Bucklandi ” Zone, Lyme Regis ! (Coll. Geol. Soc.) ; Lower Lias, Langres, Haute-Mame ! ( D' Orbigny. ) 25. Thracia ^equata, nov. spec. Shell transversely oval, ventricose ; umbones medial, obtuse ; hinge line angulated ; anterior extremity rounded ; posterior extremity moderately ob- liquely truncated ; a very faint keel proceeds from the umbo to the postero- ventral margin, ornamented with furrows and close set fine striae^ coincident with the ventral margin, which is arched. Breadth, '55 inch ; length, ‘4 inch; thickness, '25 inch. It has much the shape of T. lata, Munster, from which it is distinguished especially by its ventricosity and curved front margin. The genus Thracia has not yet been catalogued from English strata, older than the Inferior Oolite, and, indeed, if Myacites ?nactroides , Schlo- theim, of the Lias, be not a Thracia, then the genus has till now been unknown below the Middle Lias. T. rugosa, Dunker, a Lower Lias shell, is considered to be a Pleuromya , and has been re-described as such under the name of P. Dunkeri, by Terquem, so that T. cequata is, at the present time, the oldest British example, if not the oldest-known species of the genus. I take this opportunity to announce the discovery, by Mr. E. Welford, of T. glabra, Agassiz, in the Upper Lias Clay at Eydon, where it was found associated with Leda ovum, Inoceramus dubius, and other species, which serve to fix its stratigraphical position in the Zone of “ Ammonites communis. ” Geological Position. — Zone of “A. angulatus, ” Waterloo, Larne. Speci. men unique. ( R . T. ) 26. Anatina myacina, nov. spec.. Plate I. fig. 16. Shell oblong, elliptical, umbones sub-central, small, ventricose, recurved Tate — List of Irish Liassic Fossils. 23 posteriorly ; anterior margin rounded, posterior produced, obliquely ? trun- cated (the posterior margin is represented in the figure as complete ; the shell is imperfect in this region). An obtuse, ill-defined keel proceeds from the umbo to the lower posterior angle, another to the upper posterior angle, enclosing a broad, deeply-impressed lunular area. Marked by concentric plications and fine stride, and close-set radiating granular lines. Length, 75 inch; breadth, 1 '5 inch ; thickness, •5 inch. Geological Position. — Zone of “A. angulatus ,” Island Magee, Co. Antrim. 27. Discina Holdeni, Tate , Quart. Jour. Geol. Soc., Vol. xxiii., p. 314 (1867). id. Geol. Mag., Vol. vi., p. 6 (1869). Discina sp., Terquem and Piette. Lias Inf. de l’Est de France ; t. xiv., figs. 33-34, P- 1 13 (1865). Shell small, regularly conical, base orbicular, the length and breadth in the proportion of about 5 to 4 » summit central ; test concentrically striated ; colour, black to brownish-black ; yellowish-brown in the young shell. Dimen- sions of an averaged sized specimen : — Diameters, 4*5 and 3*6 millimetres ; height, 2*3 millimetres. D. Holdeni is distinguished from the other Liassic species of the genus by its regularly conical form and central apex ; and from D. reflexa, , Sowerby, with which it has been confounded by the latter character. Geological Position— Ranges from the Zone of “Ammonites angulatus ” to that of “ Ammonites Ibex in England, and throughout the Lower Lias in the East of France. 28. Pollicipes ALATUS, norv. spec. Plate I. fig. 6. The single scutal plate here figured is the one to which Mr. Etheridge (Quart. Jour. Geol. Soc., Vol. xx., p. 114, 1863) applied the M.S. name of F. liassicus ; but, as another species was described by Dunker with a similar denomination, P.liasinus, it appears to me advisable not to adopt Mr. Etheridge’s provisional name. I, therefore, have selected that of P. alatus. Scutum triangular, flat, apex acute with a lateral wing-like extension upon the oceludent side ; basal margin outwardly curved ; the tergal margin inflated. Exterior surface marked with regular raised lines coincident with the basal margin, and which are prolonged on the wing-like projection, and on the enrolled tergal margin. Geological Position. — Zone of “A. angulatus , Island Magee, Co. Antrim. Specimen unique. [P. T. ) 24 Tate— List of Irish Llassic Fossils. The following diagnoses of new species of Corals , type specimens of which were obtained from the Lower Lias in County Antrim , are extracted from Dr. Duncan! s Monograph of British Fossil Corals. Pal. Soc., Vol. xx., 1868. Oppelismilia, Duncan, loc. cit., p. 39. Corallum simple, attached and conical ; epitheca well-marked, and reaches to the calicular margin. Calice shallow, and the septa numerous and close. There are no costse, and there is no columella. Gemmation occurs within the calice; and the bud, which has an epitheca, grows with the parent. The genus includes MontivalticB with calicular gemmation. 29. Oppelismiilia gemmans, Duncan , loc. cit., t. x, figs. 33-34, p. 39- Corallum short, with a broad and flat calice, an oval space at the base, where it was once adherent ; a strong epitheca with circular markings, and there are no costse. Calice flat and shallow, and its margin is sharp. The septa are very numerous and unequal. The bud on the calice has an epitheca, and its septa are faintly dentate. Height of the corallum, 5-ioths inch ; width of the calice, 9-ioths inch. Locality — Waterloo, Larne. {R- T.) 30. Montlivaltia Hibernica, Duncan, loc. cit., t. x, figs. 22-23, p. 39. Corallum discoidal, base flat ; calice convex. Epitheca of the base strongly marked concentrically. Septa numerous, close, unequal, and marked by small papillse, which are very close together, and by flat eminences which are also very close together. There appear to be nearly five cycles of septa, and the largest septa are papillose. Diameter, 4-ioths inch ; height of corallum, i-ioths inch. Locality. — West shore of Island Magee. (R. T.) 31. Montlivaltia papillata, Duncan, loc. cit., t. x., figs. 15-18, p. 36. Corallum cyclolitoid in shape, base slightly concave ; calice convex, with a circular depression in the centre. Epitheca of the base reaching to the cali- cular margin ; it is very thin, and marked with concentrical shallow depressions and elevations, and the costse are seen through it faintly. The calice is nearly circular. The septa are exsert, and the larger have very large dentations or papillse on them. There are 24 septa, which reach the margin of the columel- lary space, and they are strongly papillated. Between two of the longest septa there are three others, one, the central, is longer than the others, which are almost rudimentary ; all are papillate. Diameter— 1 o- 1 2ths inch ; height of corallum, 2-ioths inch. Locality — W est shore of Island Magee ( R.T '.) ; it occurs, also, at Marton near Gainsborough, on the same horizon ; associated with M. Haimei, Chap. & Dew., and Septastrcea Fromenteli, Terq. & Piette, as in the Irish locality. 11 h£B 1886 XPLANATION OF LATE, i.—Leda Bronni : End view and side view, natural size. 2- — Hinnites angular is : Natural size. 3- — Leda Renevieri : Slightly enlarged. 4- — Leda Quenstedti : Natural size. 5. — Leda v-scripta : Natural size, and enlarged. 6. Polhcipes alatus : Interior and exterior faces of a scutal plate, natural size. 7. — Tornatella Robinsoni : Slightly enlarged, and magnified view of upper part of body whorl. 8. — Cerithium tenuicostatum: Left hand figure, enlarged about two diameters ; right hand figure, magnified view of one whorl. 9 . —Solarium Thorns oni : Natural size, and three enlarged views. 10. — Amcula P after soni : Natural size. n.—Chemnitzia punctata : Natural size, and magnified view of a portion of the test. 1 z.—Cucullaa Grangeri: Enlarged about one and a-half diameters. I3- Cryptczma Brycei: Side view, and view of under surface natural size. 14.— Mytilus subtilis: Natural size, and magnified view of a portion of the test. r5* D entcili uni Portlocki : Enlarged two diameters. 16. — Anatina myacina : Natural size. WPvbTTiiss, cLet. As it is intended to issue, from time to time , further Lists of the Fauna, Flora , Fossils , and Antiqui- ties of the North of Ireland, Members are re- quested to preserve this Appendix for binding with those to be issued in the future. APPENDIX II. =0333009 Q0G= -A. LIST OF THE Jrisb frassk Jnrammikm, BY JOSEPH WRIGHT, F.G.S., F.R.G.S.I., Hon. Assoc, of the Belfast Nat. Hist, and Phil. Soc., &c &c. ; AND A LIST OF THE FOSSILS OF THE ESTUAllINE CLAYS, lOF THE COUNTIES OF DOWN AND ANTRIM, BY SAMUEL ALEX. STEWART, Fellow of the Botanical Society of Edinburgh , Hon. Assoc, of the Belfast Nat. Hist, aud Phil. Soc. PUBLISHED BY BELFAST NATURALISTS’ FIELD CLUB. October, 1871. APPENDIX II. ERRATA AND ADDENDA. The paging after page 38 should be as follows Page 37 should be 39, 38 should be 40, 39 should be 41, 40 should be 42. Page 26, line 4. For “ Dr. H. P. Brady” read “ Dr. H. B. Brady.” Convolvulus bidentatus ” read “ Conovulus biden- tatus .” For “ Lcuna divaricata” read “ Lacuna divaricata.” For “ Lacuna palidaul” read “ Lacuna palidula.” For “ scalaria Turtonis *’ read “ Scalaria Turtonis .” For “ Murex erinaceous” read “ Murex erinaceus.” For “ tilus adriaticus var. ovalis” read “ Mytilus adriaticus, VAR. ovalis.” (In some copies only.) For “ Cardiam pygmceum''1 read 6t Cardium pygmceum .” For “ Thracia pubescans” read “ Thracia Pubescens.” For “ Gastrochcenia modiolina ” read “ Gastrochcena mo- diolina. ,, 35. After Terebella conchilegia, add Echinus miliaris, Leske. Very abundant in the Thracia convexa zone of the Belfast Estuarine Clay. Near the upper limit of this zone I found a bed marked by a closely-packed layer of the shells of this urchin. The shells are of large size. The species still lives abundantly in our bay. 29, line 5. For 29, line 18. 29, line 20. 30, line 15. 31, line 4. 32, line 29. 33, line 10. 34, line 36. 35, line 12. Amphidotus cordatus, Pennant. Specimens of this “ heart urchin ” are scattered throughout the Thracia convexa zone in the Belfast bed, but not plentifully. This species occurs on the County Down coast, but I am not aware of its living in Belfast Lough. A sandy bottom is the habitat usually assigned to this urchin, but our fossil specimens must have lived on a bottom entirely muddy. ERRATA CONTINUED. Page 36, line 2. For “ Spiroloculina planatula” read “ Spiroloculina PLANULATA.” ,, 36, line 3. For “ Triloculina Brongnairatii” read “ Triloculina Brongniartii.” „ 36, line 35. For “Quarternary” read “ Quaternary.” ,, 38 line 17. ForLiTToRiNA obtusata, var. ^stuaru” read “ Litto- RINA OBTUSATA, VAR. /ESTUARII.” ,, 38 line 30. For “ Turittella terebra” read “Turritella te- REBRA.” 39 (37), line 16. For “ Murex erinaceous” read “ Murex erina- ceus.” ,, 40 (31), line 3. For “ Ostrea edulis, Minn ,” read “ Ostrea edulis, hinny „ 41 (39), line 16. For “ Thracia pubescans” read “ Thracia pub- escens.” A few typographical errors also appear, which are unnecessary to enumerate, as the correct reading will be apparent. A LIST OF IRISH LIASSIC FORAMIN I FE R A, BY JOSEPH WRIGHT, F.G.S., F.R.G.S.I., Hon. Assoc, of the Belfast Nat. Hist, and Phil. Soc., &c ., &c. Mr. E. Tate, in his valuable paper on the Liassic fossils of Ireland, pub- lished by the Club in 1870, records one species of Foraminifera, Dentalina obliqua, from the locality of Ballintoy, County Antrim. This is, I believe, the first, and, indeed, only notice we have of fossil Foraminifera having been met with in any of our Irish rocks. Shortly after this paper appeared, Mr. W. Gray discovered two or three other Foraminifera in the same beds. On hearing of these discoveries I wsa led carefully to examine these shales at Ballintoy, in the hope of being able to add moie kinds to the few already known from that station ; and through the kindness of several members of the Club, who supplied me liberally with the stone, I am now able to give the names of no less than 20 species. Excepting one spot on Island Magee, where Lingulin a tenera has been met with, the Ballintoy shale is as yet the only Lias known in Ireland in which Foraminifera have been found. The shale at this place is singularly favourable for yielding these lovely little organisms, for on the stone being placed in water, it almost immediately falls down into a fine impalpable 26 Wright — List of Irish Liassic Foraminifera. mud, on passing which through fine muslin the Foraminifera remain behind in the very finest preservation. I cannot conclude these few remarks without expressing my sincere thanks to Dr. H. P. Brady, F.L.S., of Newcastle-on-Tyne, for the very valuable assistance he afforded me in correctly determining the names of the species. Nodosaria raphanus, Linn. sp. Ballintoy. Rare. Nodosaria scalaris, Batsch. sp. Ballintoy. Rare. Nodosaria tetragona, Reuss. Ballintoy. Very common. Nodosaria Boucana, D'Orb. Ballintoy. Rare. Nodosaria humilis, Romer. Ballintoy. Rare. Glandulina laevigata, D'Orb. Ballintoy. Very rare. Lingulina tenera , Bornemann. Ballintoy j Islandmagee. Very common. Dentalina communis, D'Orb. Ballintoy. Common. Dentalina obliqua, Linn. sp. Ballintoy. Very common. Vaginulina legumen, Linn. sp. Ballintoy. Very rare. Vaginulina laevigata, Romer. Ballintoy. Common. Vaginulina striata, D'Orb. Ballintoy. Common. Marginulina raphanus, Linn. sp. Ballintoy. Very Common. Marginulina Lituus, D'Orb. Ballintoy. Rare. Marginulina ensis, Reuss. Ballintoy. Common. Planularia Bronni, Romer. Ballintoy. Rare. Cristellaria crepidula, F. &> M. sp. Ballintoy. Rare. Cristellaria acutauricularis, F. M. sp. Ballintoy. Very common, Frondicularia striatula, Reuss. Ballintoy. Common. Frondicularia augustata, Nilsson. Ballintoy. Common. A LIST OF THE Fossils of the Estuarine Clays of the Counties of Down and Antrim . By SAMUEL ALEX. STEWART, Fellow of the Botanical Society of Edinburgh, Hon. Assoc, of the Belfast Nat. Hist, and Phil. Soc. The term, Estuarine Clay, is intended to signify those deposits, mostly of clay, which have been accumulated in our existing bays and estuaries since the close of the Glacial Period. They are the latest of the long series of geological deposits, and resting, as they most commonly do, on the Boulder Clay, they unite the present to the past. The Estuarine Clay often presents beds of considerable thickness, which have been continuously laid down, and are tenanted by the shells of species that have lived and died on the spot. It is to be regretted that these beds have not received more attention, as they offer perhaps the best means of filling up the gap in geological history between the close of the Glacial Era and the present. These Estuarine Clays are widely spread in Britain, being of consider- able thickness, and covering areas of some extent in such important estuaries as those of the Clyde and of the Mersey. In the North of Ireland we have several of these beds. That at Belfast exceeds twenty feet in thickness, and is spread over an area of at least four or five square miles. It may be seen at Belfast, Sydenham, Holywood, Bangor, and Kilroot. Similar, though apparently less extensive Post-Pliocene accumu- lations, are to be found on the shores of the Loughs of Larne and Strang- ford, and also at Lough Foyle, and near Coleraine. Of the two latter no detailed account has been published, and I have had no opportunity of 28 Stewart— List of Estuarine Clay Fossils. examining them, though I have in my possession some of the shells from the Estuarine Clay of the Bann. In such inlets as those of Loughs Larne and Strangford, into which there are no rivers of any note carrying sedi- ment, these Post-Pliocene clays are indicated by accumulations of small extent, but characterised by the presence of shells, in most part the same as those living in the adjoining waters. A list of the Belfast clay shells was made out by John Grainger, Esq., and published by the British Association in their Report for 1852. A second list by Mr. Grainger, recording all the species known to occur in this bed at that date, was published in the Natural History Review for 1859. By the excavations for the recently constructed floating dock and basin, I have been enabled to examine this clay to a depth of twenty feet over a considerable area. The results are the addition of a goodly number of species to Mr. Grainger’s lists, and the conviction that there is evidence that since the basement portion of that clay was laid down, there have been several oscillations of the sea-level ; these oscillations can be shown by a comparison of the different sets of shells, found at various depths in the clay. The Larne Lough Estuarine Clay may be seen on the shore close to Magheramorne railway station : shells occur in it abundantly, many of the testacea being among our rarer species. This deposit is rich in Fora- minifera , and in the smaller forms of Mollusca, especially univalves. It has been only slightly examined, and would doubtless yield many more fossils if scrutinised as closely as the corresponding bed at Belfast. At Strangford Lough I have seen the Estuarine clay near Newtownards, but have had little opportunity of investigating the bed at that place. Stewart — List of Estuarine Clay Fossils. 29 ANNOTATED LIST OF SPECIES.* Helix nemoralis. Mr. Grainger records the finding of one specimen of this land shell. I met with it two or three times. Helix rotundata. One specimen (Grainger). Zonites nitidulus. Two specimens (Grainger). Melampus bidentatus, Convolvulus bidcntcitus , F. & H. Larne Lough bed, rare. Patella vulgata. One specimen (Grainger). Tectura virginea, Acmcea virginea, F. & H. Very rare. (One young specimen.) Fissurella Gr^ca, Fissurella reticulata , F. & H. Belfast bed, rare. Cyclostrema nitens, Trochus pusillus , F. & H. Plentiful in the Larne Lough deposit. Trochus magus. Of large size, but rare. Trochus cinerareus. Abundant both at Belfast and Larne. Trochus umbilicatus. At Larne Lough, scarce and small. Lacuna crassior. Found by Mr. Grainger in the Estuarine Clay of Bel- fast. I have not myself met with specimens. Lcuna divaricata, Lacuna vincta , F. & H. Occurs in some plenty. Lacuna puteolus. Larne Lough, scarce. Lacuna pallidaul. In the Larne Lough deposits, scarce. Littorina obtusata, Littorina litoralis , F. & H. Frequent. Littorina obtusata, var. iESTUARii. Belfast, rare. Littorinarudis. Scarce. Littorina rudis, var. tenebrosa. Scarce. Littorina litorea. Abundant, especially in the f Scrobicularia bed. Rissoa inconspicua. In great abundance. * I have used the names adopted by Mr. Jeffreys in his Manual of British Conchology. Where the names given by Forbes and Hanley are different, they appear here as synonyms. f See abstract of paper lead by the author on 8th March, in Eighth Annual Report of Belfast Naturalists’ Field Club (1871). 30 Stewart — List of Estuarine Clay Fossils. Rissoa membranacea, Rissoa labiosa, F. & H. Profusely abundant, and of large size. Rissoa viqlacea, Rissoa rufilabrum, F. & H. Not uncommon. Rissoa striata. Larne Lough, in profusion. Rissoa vitrea. In the Belfast deposit, rare. Hydrobia ulv.e, Rissoaulvce, F. & H. Frequent in the Estuarine Clays of Belfast, Larne, and Strangford Loughs. Homalogyra atomus, Skenea nitidissima , F. & H. Abundant in the clay at Magheramorne. Homalogyra rota, Skenea rota , F. & H. With the last species, but rare. Caecum glabrum. Larne Lough, rare. Turitella terebra, Turitella communis , F. & H. Plentiful, [and very large. Scalaria Turton^e, 'scalaria Turtonis, F. & H. Plentiful in the Belfast bed. Aclis supranitida. Belfast bed, very rare. Odostomia minima. This rare little univalve is for the first time recorded as an Irish Shell. One specimen only occurred to me. Odostomia pallida, Odostomia eulimoides, F. & H. Mr. Grainger re- corded this shell from the Belfast deposit. I have found it at Maghera- morne, where it is rather scarce. Odostomia acuta. Belfast and Larne beds, rare. Odostomia indistinct a, Chemnitzia indistincta, F. & H. Rare. Odostomia interstincta. Very rare. Odostomia lactea, Chemnitzia elegantissima , F. & H. Belfast and Larne beds, not uncommon. Eulima bilineata. One specimen found by Mr. Grainger, and recorded as E. subulata. Dr. Grainger is now satisfied that the name I have adopted is right. Natica catena, Natica monilifera , F. & H. Very scarce. Natica Alderi, Natica nitida, F. & H. Commonly diffused through the clay. Aporrhais pes-pelicani. In the greatest abundance. Cerithium reticulatum. Everywhere throughout the deposit in abun- dance. Stewart — List of Estuarine Clay Fossils. 31 Purpura lapillus. A few specimens occurred, but this species may be reckoned among the rare shells of the Estuarine Clay. Buccinum undatum. Very common. Murex erinaceous. Rare at Belfast, rather frequent at Larne. Fusus antiquus. Occurs occasionally, but not at all common. Nassa reticulata. Frequent throughout the Clays. Nassa pygmea. Very common. Mr. Grainger’s N. incrassata belongs, I believe, to this “ segregate.” The distribution of these forms in our local Post-tertiary deposits seems to have been very fluctuating. Nassa incrassata occurs in our Glacial Clays, then disappears from our subsequently deposited Estuarine Clay, and finally reappears as the dominant form in our existing waters. Nassa pygmea , on the other hand, has not been found in our Boulder Clay, but in the Estuarine Clay is abundant, and now again ranks as a rare shell confined to the deep waters outside the bay, Defrancia gracilis, Mangelia gracilis. F. & H. Very rare, one speci- men only. Pleurotoma cost at a, Mangelia costata. F. & H. One specimen, (fide Grainger). Pleurotoma brachystoma, Mangelia brachy stoma. F. & H. Rather rare. Pleurotoma septang.ularis, Mangelia septangularis. F. & H. Very rare. Pleurotoma rufa, Mangelia rufa , F. & H. “ Belfast deposit” (J. Gwyn Jeffreys). By the Belfast deposit, I believe Mr, Jeffreys means our bed of Estuarine Clay. Nevertheless, few discriminate sufficiently between the Estuarine Clay and the raised beaches occurring here. The latter I have excluded from my list. Pleurotoma turricula, Mangelia turricula. F. & H. Rare. Cypr^a Europ^a. Two or three specimens only of our British cowry occurred to me. Cylichna nitidula. In the Belfast bed I found one shell. Utriculus obtusus, Cylichna obtusa. F. & H. In the Larne, and also in the Strangford Lough Estuarine Clay, rare. Utriculus hyalinus, Amphisphyra hyalina , F. & H. Plentiful in the Belfast and in the Larne^beds,but so fragile that specimens can scarcely be secured. 32 Stewart — List of Estuarine Clay Fossils. Acera bullata, Akerct bullata, F. & H. In the Belfast bed abundantly, but restricted to the *zone of Thracia convexci. Plentiful also at Larne, where specimens are of small size, apparently the variety nana. Action tornatilis, Tornatella fasciata , F. & H. Belfast deposit, (fide Grainger). Scaphander lignarius. Rare. Three or four specimens only. Philine aperta. In abundance. Anomia ephippium. This extremely variable shell is distributed through- out the clay in some plenty. Anomia patelliformis. Rare, (Grainger). Ostrea edulis. Shell beds, made up nearly altogether of the common oyster, occurred near the base of the deposit, and again repeated near the upper surface. Ostrea edulis, var. hippopus. Immense shells of this deep-water variety scattered through the clay, mainly in the median portion of the de- posit. Pecten varius. Generally distributed and abundant. Pecten opercularis. Along with the last species, and almost equally abundant. Pecten maximus. Scattered throughout, rather plentifully. Lima hians. Very rare in the Belfast bed, abundant in the corresponding deposit in Larne Lough. Mytilus edulis. Abundant, especially in the basal and superficial por- tions of the clay. Mytilus modiolus, Modiola modiolus , F. & H. Rare at Belfast, plentiful in the Larne bed. Mytilus adriaticus, Modiola tulipa, F. & H. Occurs both at Belfast and Lame, but is rare. tilus adriaticus, var. ovalis. “ Occurred in excavating a channel in Belfast Harbour” (J. G. Jeffreys). Some specimens dug out at the site of the new floating dock appear to belong to this variety. Modiolaria marmorata, Crenelles marmorata, F. & H. Very rare at Bel- fast, frequent at Larne. Nucula nucleus. Very abundant in the Belfast beds ; rare at Larne. Leda minuta, Leda caudata, F. & H. A single valve, (Grainger). * See abstract of paper lead by the author on 8th March, in Eighth Annual Report of Belfast Naturalists’ Field Club (1871). Stewart — List of Estuarine Clay Fossils. 33 Montacuta bidentata. Frequent at Belfast ; occurs in the Larne Lough bed in profusion. Montacuta ferruginosa. In the Belfast bed, rare. Lucina borealis. Belfast bed, rare, but very large and tumid. The normal form occurs abundantly in the Larne Lough deposit. Axinus flexuosus, Lucina flexuosa, F. & H. Abundant and luxuriant. Cyamium minutum, Turtonia minuta , F. & H. Rare in the Belfast Es- tuarine Clay, plentiful in the similar bed at Larne Lough. Cardium echinatum. Occurs in great profusion, and very fine. Cardium exiguum, Cardiam fiygmceum, F. & H. Occurs rather frequently in the Belfast deposit, but generally as single valves. More plentiful at Larne, and often complete. Cardium nodosum. In the Larne Lough bed, very rare. Cardium edule. Very abundant, especially in the upper and lower zones. Some of the shells, if not fully entitled to be considered as belonging to the variety rusticum , certainly approach that estuarine form very closely. Cardium Norvegicum. Very rare. Mr. Grainger found one valve, and two or three valves occurred to me. Cyprina Islandica. Very rare. I found one perfect specimen in the Thracia convexa zone of the Estuarine Clay. Venus lincta, Artemis lincta , F. & H. Occurs occasionally dispersed through the clay, but usually in single valves. Venus Casina. Frequent in the Larne Lough deposit, mostly in single valves. Venus ovata. Frequent at Larne, specimens small. Venus Gallina, Venus striatula, F. & H. Diffused through the beds, form variable. Tapes aureus. Common in the Larne Estuarine bed, not rare in the Belfast bed. Tapes aureus, var. ovata. Not uncommon, occurs both in the Larne and Belfast Estuarine Clays ; attains a much greater size than the typical form. Tapes pullastra. Frequent, especially in the lower zone. Tapes decussata. Shells of this littoral species occupy the lower portion of the clay in great profusion. Many specimens were much above the usual size. 34 Stewart — List of Estuarine Clay Fossils. Lucinopsis undata. Very large, and diffused in immense numbers through the clay, except in the very oldest and very newest portions of the bed. Tellina Balthica, Tellina solidulct , F. & H. Abundant, especially near the upper surface. Tellina tenuis. Near the top, only sparingly, and of small size. Tellina squalida, Tellina incarnata , F. & H. Very rare. The only specimens I have seen were single valves collected by the late Wm. Thompson, Esq., and by Mr. William Darragh, of the Belfast Mu- seum. Psammobia Ferroensis. Single valves frequent, perfect specimens rare. Psammobia vespertina. Mr. Grainger records finding 'a single valve of this species. Mactra subtruncata. Frequent, variable in size and shape. Mactratruncata. Scarce. Lutraria elliptica. Frequent. Lutraria oblonga. One specimen, (fide Grainger). Scrobicularia alba, Syndosmya alba , F. & H. Scattered through the clay in immense numbers. Scrobicularia piperata. Occupies the lower zone of the clay in the greatest profusion, Rare oi absent from the ^higher or more recently deposited portion of the bed. Solecurtis antiquatus, Solecuytis coarctatus , F. & H. A single speci- men, ( fide Grainger). Solen pellucidus. Distributed through the ^median portion of the bed in abundance. Solen ensis. Occurs sparingly. Solen vagina, Solen marginatus, F. & H. Rather frequent. Thracia papyracea, Thracia phaseolina. Frequent ; shells often perfect. The form T. villosiuscula also occurs. Thracia convexa. Perfect specimens of this fine shell are plentiful ; their occurrence made it easy to recognise a well-marked zone of the clay, replete with species that live mostly at a depth of five to ten fathoms. Thracia pubescans. One specimen. (Grainger). Corbula gibba, Corbula nucleus, F. & H. Plentiful, but mostly as single valves. Stewart — List of Estuarine Clay Fossils. 35 Mya arenaria. Frequent, but only in the most recent portion of the bed. Mya truncata. Plentiful throughout ; specimens very fine, and some- times with the siphonal tubes preserved. Mya binghami, Sphcenici Binghami, F. & H. In the Larne Lough de- posit, very rare. Panopea plicata, Saxicava rugosa, young? F. & H. Plentiful at Bel- fast in one narrow zone of the clay bed. Not yet found living on the Irish coasts. Saxicava rugosa. Larne Lough deposit, rare. Saxicava rugosa var. artica. Belfast bed, rare (Grainger). Gastroch^ena dubia, Gastroclicenia modiolinci , F. & H. “ Two portions of the curious flask-like tubes of this species were found in the de- posits” (Grainger). Pholas Candida. Perfect shells imbedded in numbers at the base of the zone of Thracia convexa, and forming a line of demarcation between that zone and the S crobicularia bed. Pholas crispata. In the clay where they had lived in some numbers ; the specimens are very large, many of them being nearly double the usual dimensions of living examples. They occur only at the base of the Thracia convexa bed. Teredo Norvegica. The calcareous tubes of this “ship worm” are not rare in the clay ; complete specimens now in the Belfast Museum were dug up while making sewers in the streets of the town. Creusia verruca. Belfast deposit, (Grainger). Cythere albo-maculata. Belfast bed, rare. Not rare in the Larne Lough deposit. Pectinaria belgica. Belfast deposit, (Grainger.) Serpula triquetra. Belfast Estuarine Clay, on shells. Serpula vermicularis. In the Belfast Clay, rare. Terebella conchilega. Belfast bed, (Grainger.) POLYMORPHINA LACTEA. Bare. Polymorphina gibba, Var. cequalis. Rare. Planorbulina mediterranensis. Very rare. Polystomella crispa. Belfast and Larne bed, very abundant. Quinqueloculina bicornis. Belfast and Larne beds, scarce. Quinqueloculina seminulum. In great abundance. Rotalia beccarii. Extremely abundant, Belfast and Larne Lough . 36 Stewrart — List of Estuarine Clay Fossils. Spiroloculina limbata. Rare. Spiroloculina planatula. Very rare. Triloculina Brongnairtii. Rare. Triloculina trigonula. Common. Truncatulina lobatula. Not common. Verneuilina polystropha? Very rare. In the foregoing list I have given estimates for the several species, approximating as near as possible to the abundance or paucity of speci- mens. These estimates are founded on careful observations, extending over some three years. In preparing them I have derived valuable assist- ance from Dr. Grainger’s previously published lists, and I am confident that they may be relied on as in the main correct. Future excavations, if such be carried on in these beds, may possibly make slight modifications, but I am satisfied that on the whole the estimates here given will remain practically undisturbed. In the table which follows, I have endeavoured to give for the North of Ireland the distribution of these species in Post-tertiary times. Unfortu- nately the unproductiveness of our Glacial beds renders one column rather imperfect. Out of 140 species here recorded, only 29, being 21 per cent., appear as glacial shells in this district. It cannot be doubted but that there existed a much greater community between the two faunas. Species make their appearance in a locality, becoming more and more abundant until they reach their culminating point, from which they recede with more or less rapidity until finally they are replaced by others. Such is the history of many of the shells of our Estuarine Clay, and to make this record as useful and complete as possible, columns are here given, showing those now found living in the waters of our bay, and those 1 lving at present on the coasts of the North of Ireland, distinguishing them from such as have only been found as dead shells. These columns will, it is hoped, prove instructive. It will be seen that many species, now only found dead, existed here during some portion of the Estuarine Clay times in abundance ; and it may be added that during that period some other species, now among the forms dominant in our waters, were either absent or rare. Shells from Raised Beaches, and Quarternary Gravels, are not included in these lists, which have been rigidly restricted to species which certainly occur in the Estuarine Clay. Many Post-pliocene shells are thereby ex- cluded, which have been recorded as from Belfast deposits. It is to be Stewart— List of Estuarine Clay Fossils. 37 hoped that members of the Belfast Naturalists’ Field Club will not overlook the raised beaches that are so numerous in the district : a good catalogue of our raised beach shells would nearly perfect our knowledge of the local Post-pliocene marine fauna. I am very much indebted to J. Gwynn Jeffreys. Esq., F.R.S., for his kindness in identifying for me all critical or doubtful shells ; to Joseph Wright, Esq., F.G.S., who gave much valuable assistance in ascertaining the various forms of Foraminifcra in the Estuarine Clay; and also to Dr. H. B. Brady, F.G.S., F.L.S., who kindly took the trouble to refer these forms to their proper species. To Rev, Dr. Grainger I am also indebted for permission to examine his valuable collections of shells of the Belfast Estuarine Clay. 38 Stewart — List gf Estuarine Clay Fossils. TABLE OF LOCAL DISTRIBUTION List of Species.* Fossil O Gastropoda. Helix nemoralis, Mull Helix rotundata, Linn Zonites nitidulus, Drap Melampus bidentatus, Mont Patella vulgata, Linn Tectura virginea, Mull Fi6surella Graeca, Linn Cyclostrema nitens, Phil Trochus magus, Linn Trochus cinerarius, Linn Trochus umbilicatus, M ont Lacuna crassior, Mont Lacuna divaricata, Fahr Lacuna puteolus, Turt Lacuna pallidula, Da Costa Littorina obtusata, Linn ,, var, aestuaru, jfeff Littorina rudis, Maton “ var, tenebrosa, Mont Littorina litorea, Linn Rissoa inconspicua, Aid Rissoa membranacea Adams Rissoa violacea, Desm Rissoa striata, Adams Rissoa vitrea, Mont Hydrobia ulvae, Penn Homalogyra atomus, Phil Homalogyra, rota, F. & H Caecum glabrum, Mont Turittella terebra, Linn O o Recent Living o X! O l-S Dead Shells o £ U O sM > ccS o C/3 w •a p o 0) d d o C/3 w X bo p o £ bD c d m Living Dead Shells d W C/3 13 m o r> o +J X. X. Solen vagina, Linn X. X. Thracia papyracea Poli X. # 9 X. X. Thracia pubescans. Pult X. X. Thracia convexa, W. Wood • • X. X. X. Corbula gibba, Olivi X. X. X. X, Mva arenaria. Linn X. X. X. Mva truncata, Linn X. X. X. Mya Binghami, Turt X. X. Panopea plicata, Mont X. Saxicava rugosa, Linn X. X. X. X. x# ,, ,. var. arctica, F. &> H. . . X. X. X. Gastrochasna dubia, Penn . ? X. Pholas Candida, I Ann X. X. Pholas crispata, Linn X. X. X. Teredo Norvegica, Speng X. X. Class Crustacea Cv there, alhn-marnlpta, X. X. Crensia verrura T.aar.h. . . . T X. X. Class Annelida V>P‘1r'ir‘ci P/y 7/ X. Stewart — List of Estuarine Clay Fossils. List of Species. Fossil. W o o Eeeent. Living PQ o y Planorbulina Mediterranensis, D'Orb Polystomella crispa, Linn Qumqueloculina bicornis, W. & jf. Quinqueloculina seminulum, Linn Rotalina Beccarii, Linn Spiroculina limbata Spiroculina planulata, Lamk .... Triloculina Brongniartii, D'Orb . Triloculina trigonula, Lamk. Truncatulina, lobatula, W. & J. Verneuilina polystropha ? D'Orb \ X. X. X. X, X. X. X. X. X. x. X. X. X. X, X. X, X. X. X. X. X. X. X. X. X. X, X. X. X. X. X. X. . . X. X. X. * As there is no evidence that any of the Foramanifera were taken alive on our coasts, I have been compelled to enter them in this table as dead shells. No doubt many of them lived here, but further information is required. / . .a. ip if ie n id i ix: III A LIST OF THE Ufomsaf %fjml{r-fet nffttlattir . BY SAMUEL ALEX. STEWART, Fellow of the Botanical Society of Edinburgh ; Hon. Assoc, of the Belfast Nat. Hist, and Phil. Soc. AND A LIST OF ’ Orb., and Dentaline variety. A long thin N. radicula (Linn), passing into Dentalina nodosa, Dy Orb. of his “Memoire- sur la Craie blanche, &c.” (not D. nodosa of D’Orb. “ Models”). Rather frequent. , 24. Nodosaria radicula (Linn.), 3-chambered, thick (near Glandulina discreta, Reuss; G. cylindracea, Alth. ; Marginulina bullata, Reuss.) Only one specimen found. 25. Nodosaria radicula (Linn.), tapering; N. lepida, Reuss (“West- phalia”). Rare. 26. Nodosaria radicula (Linn.), var. (near N. conferta.) Very rare. 27. Nodosaria pyrula, D' Orb. Rare. 28. Nodosaria hispida, D'Orb. Rather rare. 29. Nodosaria raphanus (Linn.); N. Reuss. Rather rare. Wright— List of Irish Cretaceous Microzoa. 83 30. Nodosaria raphanus (Linn.), var. inflata, Reuss. Frequent. 31. Nodosaria RAPHANUS (Linn.), short coarse variety. Abundant. 32. Nodosaria raphanus (Linn.), small; N. obscura, Reuss (“ Elbthal- gebirge ”). Rare. 33. Nodosaria acicula, Lam., slightly Dentaline, and thus passing into Dentalina obliqua (Linn.). Frequent. 34. Nodosaria (Dentalina) limbata, D'Orb. Rare. 35. Dentalina communis, D'Orb., with oblique septa. Frequent. 36. Dentalina communis, D'Orb., var. lorneiana, D'Orb., passing into D. Boueana, D'Orb. Frequent. 37. Dentalina communis, D'Orb., var. irregularis, D'Orb. The nearest figured specimen is Nodosaria monile, V on Hag., in Reuss * ( Kreid. Bohm. t. 8. f. 9 (not f. 7. which, however, Reuss regards as the true “ monile”) ; Dentalina nodosa, D'Orb., “ M6m. Craie blanche ” (not Soldani) is pro- bably the same ; N. irregularis, D'Orb., “For. Fos. Vien.,” is the same with longer chambers; and N. longiscata, D'Orb., has very elongate chambers of the same style. Rare. 38. Dentalina communis, D'Orb., var.; D. Lilli, Reuss (“ Kreid. Lemberg, PI. II. fig. 11). Rather rare. 39. Dentalina communis, D'Orb., exquisitely delicate var. near D. peracuta, Reuss. Rare. 40. Dentalina communis, D'Orb., var. emaciata, Reuss. Very rare. 41. Dentalina pauperata, D'Orb., with straight septa. In great profusion. 42. Dentalina Steenstrupi, Reuss (“Meklenburg ”). Only one specimen found. 43. Dentalina nodosa, D' Orb., var. with flush and short chambers, marked with delicate lines, near D. nodosa, D'Orb. (Soldani) ; D. lineolata, Reuss (“ Bohemia”); D. multilineolata, Reuss (“ Elbthalgebirge”); D. proteus, Reuss (“ Maestricht”) ; D. polyphragma, Reuss (“Westphalia”) ; Nodo- saria subornata, Reuss (“ Dobrutscha” f. 9, 10; the shape being that of f. 5, N. inarticulata, Reuss), and others. Rare. 44. Dentalina marginulinoides, Reuss (“Lemberg,” PI. II. f. 12), sub- septate variety. Rather rare. 84 Wright— List of Irish Cretaceous Microzoa. 45. Dentalina marginulinoides, Reuss, cylindrical variety. Rather rare.. 46. Frondicularia striatula, Reuss (“ Elbthalgebirge,” PL XXI. fig. 2). Frequent. 47. Frondicularia augustata, Nilsson (according to Reuss). A narrow sub-variety of F. striatula. Rare. 48. Frondicularia Verneuiliana, D'Orb., narrow variety. Rather rare. 49. Frondicularia Archiaciana, D'Orb. Frequent. 50. Frondicularia tenuis, Reuss (il Elbthalgebirge,” PI. XXI. f. 3). Rare.. 51. Frondicularia in versa, Reuss. Only one specimen found. 52. Frondicularia elliptica ( Nilsson ). Very rare. 53. Frondicularia mucronata, Reuss (“ Elbthalgebirge”) var. with trifid mucro ; ? F. Goldfussi, Reuss (“ Westphalia”). Rather rare. 54. Flabellina lingula, Von Hagenow, var. Only two specimens found. 55. Flabellina rugosa, D'Orb. Very rare. 56. Flabellina reticulata, Reuss. Frequent. 57. Flabellina pulchra, JD’Orb. Very rare. 58. Flabellina pulchra, N Orb., narrow neat variety, near Fr. obliqua, Von Munster. Very rare. 59. "Flabellina pulchra, D'Orb., a smooth variety with parallel sides ; a narrow form of Fr. obliqua, Alth (“ Lemberg”). Very rare. 60. Flabellina ornata, Reuss (“Kreid. Bohm.,” PI. XXIV. fig. 43) ; near Cristellaria crepidularis, Reuss (“Gault”); ? F. Baudouiniana, D'Orb. Only one specimen found. 61. Lingulina carinata, D'Orb. var.; broad and short. Only two speci- mens found. 62. Marginulina glabra, var. elongata, D'Orb. Abundant. 63. Marginulina bullata, Reuss (“Westphalia” PI. VI. fig. 4). Rather rare. Wright— List of Irish Cretaceous Microzoa. 85 64. Marginulina radicula (Linn.) ; smooth flush Nodosaria radicula with excentric aperture. Only one specimen found. 65. Marginulina seminotata, Reuss (“Westphalia Kreid.,” Pl. V. fig. 6). Very rare. 66. Marginulina raphanus (Linn.)', Nodosaria raphanus with excentric aperture. Only one specimen found. 67. Vaginulina (Marginulina) trilobat a, D'Orb.; Marginulina bacillum, . Reuss. Frequent. 68. Vaginulina (Citharina) harpa, Rom. var. nov., near V. discors, Reuss, and V. arguta, Reuss (“ Gault,” PI. III. fig. 10 and 12). Rare. 69. Vaginulina costulata, Reuss. Only one specimen found. 70. Vaginulina costulata, Romer (Reuss, “ Elbthalgebirge, ” PI. XX. . fig. 24). Variety, thin and slightly curved. Only two specimens found. 71. Planularia, sp. (near Planularia longa), Cornuel. Very rare. 72. Planularia crepidula, D'Orb., becoming Flabellina pulchra, D'Orb „ Very rare. 73. Cristellaria recta, D'Orb. Rather rare. 74. Cristellaria recta, D'Orb. var. hamosa, Reuss (“Elbthalgebirge,” PI. XXIV. flg. 2). Rare. 75. Cristellaria recta, D'Orb. (near C. Bronni, Ro?ner) (Reuss, “Gault,” PI. VII. f. 13). Only one specimen found. 76. Cristellaria rotulata ( Lam. ). In great profusion. 77. Cristellaria navicula, D'Orb. Rare. 78. Cristellaria triangularis, D'Orb. Very rare. 79. Cristellaria (Saracenaria) Italica, Defrance. Very rare. 80. Cristellaria (Saracenaria) Italica, Defrance, a long sub-variety. One specimen found. 81. Polymorphina damyecornis, Reuss, PI. III. figs. 16 and 17. Very rare... 82. Polymorphina horrida, Reuss, PI. III. figs. 14 and 15. Rather rare. 86 Wright— List of Irish Cretaceous Microzoa. 83. POLYMORPHINA fusiformis, Romer. Not unfrequent. 84. POLYMORPHINA regina, B. P. 6° J., var. Very rare. 85. Uvigerina nodosa, D’Orb. Very rare. GLOBIGERINIDA. 86. Globigerina cretacea, D' Orb. In great profusion. 87. Globigerina bulloides, D’Orb. Very rare. 88. Globigerina bulloides, D'Orb ., var. nov., heaped. Very rare. 89. Globigerina marginata ( Reuss). Rare. 90. Pullenia quinqueloba ( Reuss). Rather rare. 91. Textularia gibbosa, D' Orb. Rare. 92. Textularia pupa, Reuss (“Westphalia”). Rather rare. 93. Textularia sagittula, Defrance. Abundant. 94. Textularia trochus, D' Orb. Rare. 95. Textularia turris, D’Orb. Rare. -96. Textularia turris, D’Orb., short and thick varieties. Frequent. 97. Textularia fceda, Reuss. Frequent. 98. Textularia pR/elonga, Reuss. Rather rare. 99. Textularia globulosa, Ehr. In great abundance, but liable to be overlooked from its minute size. 100. Verneuilina triquetra, ( Munster). Rather rare. 101. Gaudryina rugosa, D' Orb. Frequent. 102. Gaudryina pupoides, DOrb. var. pr^elonga (Reuss). Rare. 103. Tritaxia triquetra (Munster). Rather rare. 104. Bulimina Presli, Reuss. Frequent. Wright— List of Irish Cretaceous Microzoa. 87 105. Bulimina ovulum, Reuss. Abundant. 106. Bulimina brevis, jD’Orb. In great abundance. 107. Bulimina intermedia, Reuss. Rather rare. 108. Bulimina regularis, sp. nov. Jones , MS. (near B. marginata, D’Orb.). Only one good example found. 109. ? Bulimina, sp. Very rare. no. Virgulina TEGULATA, Reuss, VAR. In great abundance. in. Bolivina deco rata, sp. nov. Jones , MS. Very abundant. 1 12. Bolivina, sp. Exquisitely delicate form. Only one specimen found. 113. Pleurostomella fusiformis, Reuss (“ Westphalia”). Rare. 1 14. Planorbulina* exsculpta, Reuss (“ Westphalia”). Frequent. 1 15. Planorbulina ammonoides (Reuss). In the greatest profusion. 1 16. Planorbulina ammonoides (Reuss), var. with extra shell-growth, making astral overgrowth on the umbilicus. In great profusion. , 1 17. Planorbulina crenulata (Reuss), (“Gaas,” PI. II. fig. 2). Rather rare. 118. Truncatulina lobatula (W.& J.). Frequent. 1 19. Pulvinulina Micheliniana ( D' Orb.) VAR. Frequent. 120. Rotalia orbicularis {D’Orb.), var. In great profusion. 121. Rotalia vel planorbulina? PI. III. fig. 18. A Rotaline form, like R. orbicularis in shape, but having each chamber symmetrically perforated with a large central aperture on the outside. Only one specimen found. Prof. T. Rupert Jones says:— “This specimen is of great interest, when considered with the few other known open-chambered, Foraminifera. Ehrenberg figures ( ‘ Mikrogeologie, ’ PI. XIX. fig. 8), a Pulvinulina (?) having a symmetrical series of holes, one at the base of each chamber, around the large convex central chamber ; and he figures some Rotalia * Prof. W. K. Parker, F.R.S., has kindly favoured us with his opinion on the Rotaltna and some of the more obscure of the other Foraminifera of this list. G 88 Wright — List of Irish Cretaceous Microzoa. and Planorbulince with less regular holes. M. Vanden Broeck, of Brussels, has lately discovered a Lageniform * porcellanous’ Foraminifer with a regu- larly cribrate or latticed shell. Thus in both divisions of the Foraminifera we have open-chambered shells, analogous to the basket-like structure of the siliceous Polycystina ( Radiolaria ). How far these may be taken as indications of another, or other divisions of the Rhizopods, further research will show.” 122. Fragments of tubular branched forms more or less aculeate near to the so called Dentalina (?) aculeata of D’Orbigny. My friend Professor T. Rupert Jones proposes to distinguish this simple, calcareous, subsegmented, branching, Nodosarian form by the “generic” name Ram u LINA (from “ ramulus,” a little branch) ; the “species” above mentioned, which is common in the French and British chalk standing as Ramulina aculeata {D' Orb.), and our Irish form, which differs from D’Orbigny’s in being smooth, as Ramulina l^evis, gen. et sp. nov. Jones , see PI. III. fig. 19. Rather rare. 123. Ramulina brachiata, sp. nov. Jones , see PI. III. fig. 20. Very rare. Professor T. Rupert Jones says of this form that its nearest known analogue in external form among Protozoa is perhaps Dr. Wyville Thomson’s Coelosphoera tub if ex, a peculiar Sponge from the North Atlantic. Still the fixed position of the tubes and the general aspect of the organism are against the probability of these Microzoa being closely allied. SPONGE SPICULA.* SKELETON-SPICULA. 124. Acerate spiculum, PI. II. figs. 1 and 2. This form is found abundantly . in the Halichondroid sponges both recent and fossil, but it is generally very minute. The same form also prevails to a great extent in the skeletons of many species of Tethea and Geodia , in both of which these spicula are of about the same size and form as those found in the Chalk, and I have no doubt that they are from fossil species of one or the other of these genera. F requent. 125. Attenuato-acuate spiculum ; an abnormal form, PI. II. fig. 3. Very rare. 126. Moniliform attenuato-acuate spiculum, PI. II. fig. 4. Rather frequent. * I am indebted to J. S. Bowerbank, LL.D., F.R.S., for the following report on the Sponge spicula. Wright — List of Irish Cretaceous Microzoa. 89 127. Furcated porrecto-temate moniliform spiculum, PI. II. fig. 5* This is probably an external defensive spiculum from a Sponge closely allied to Tethea. I have seen from our southern Chalk the same form with monili- form shaft and radii, but not so distinctly banded. Rather rare. 128. Equiangular triradiate spiculum, PI. XI. fig. 6. This form occurs as a siliceous form rarely, but abundantly in the calcareous Sponges as skeleton spicula. Rare. 129. Spiculated equiangular triradiate spiculum, PI. II. fig. 7- This occurs as a siliceous form rarely, but abundantly in the calcareous Sponges as internal defensive spicula. * Abundant. CONNECTING-SPICULA. 130. Incipiently expanso-ternate spiculum, probably from a Geodia , PI. II. fig. 8. It is not uncommon in our southern flints. Rare. 131. Expando-ternate spiculum ; closely allied to the last, PI. II. figs. 9 and 10. This form is found in recent Tethea , Geodia , and other genera. Frequent. 132. Expando-ternate spiculum, with cylindrical radii, PI. II. figs. 11 and 12. This form is found in some recent species of Tethea, , but is not a normal condition. Rather rare. 133. Furcated attenuato-patento-ternate spiculum, PI. II. fig. 13. This con- stricted form of an apparently furcated attenuato-patento-ternate spiculum has not yet been found among recent Sponges. It occurs in our southern Chalk flints. Rather jrare. 134. Furcated attenuato-patento-ternate spiculum, PI. II. figs. 14 to 16. This form of spiculum abounds in the expansile dermal system of several of the siliceo -fibrous Sponges, as in that of Dactylocalyx Bowerbankii , Johnson (Proc. Zool. Soc. 1869, PI. III. figs. 6, 7). These spicula vary in form and size to a considerable extent in the same species. In great profusion. 135. Furcated attenuato-patento-ternate spiculum, PI. II. fig. 17 ; from the expansile dermal system of a siliceo-fibrous Sponge. In great profusion. * This rarity of some of our forms of spicula in recent siliceous Sponges is of con- siderable interest, in connection with the fact that all the little organisms in 'the powder from our flints seem to be now silicified, whether they were originally calcareous (as the Foraminifera and Ostracoda) or not. 90 Wright— List of Irish Cretaceous Microzoa. 136. Furcated attenuato-patento-ternate spiculum, PI. II. fig. 18 ; same as the last, but probably from a different species of Sponge. Frequent. 117 Recurvo-temate spiculum, PI. II. fig- >9 5 similar spicula occur in the intermarginal cavities of Tdhea and Geodia, and these are probably from similar positions in the fossil species of these genera. Very rare. 138. Spiculum, PI. HI. fig. 1. This form is quite new to me. It is most probably from the expansile dermal system of a siliceo-fibrous Sponge. Rather rare. 139. Spiculum, PI. HI. figs. 2 and 3. Singular and probably abnormal form of dermal spiculum of a siliceo-fibrous Sponge. Rather rare. 140 Porrecto-ternate spiculum, PI. II. fig. 20. This form of spiculum occurs ’in some species of Tdhea ( Tethea cranium , British). An external defen- sive spiculum. Frequent. 141. Porrecto-ternate spiculum, PI. II. fig. 21. Very rare. 142. Porrecto-ternate spiculum, PI. II. fig. 22 1 same as the last, but probably indicating a different species. Rather rare. H3- Attenuated rectangulate hexradiate spiculum, PI. III. figs. 4 and 5, from a siliceo-fibrous Sponge (see “Mon. Brit. Spongiadae,” Vol. I. PI. VII. fig. 174). In great profusion. SKELETON-FIBRES. 144. Fragments of skeleton-fibres of a siliceo-fibrous Sponge, PI. III. figs. 6 and 7. Very rare. 145. Apparently fragments of skeleton fibre of a siliceo-fibrous Sponge, PI. III. figs. 8 and 9. Abundant. 146. Fragments of skeleton fibre of a siliceo-fibrous Sponge, PI. HI. fig. 10. Rare. Wright— List of Irish Cretaceous Microzoa. 91 The following additional forms were found too late for insertion m the body of the report : — SPONGE SPICULES. 147. Sphero-stellate spiculum, PI. III. % n. Very rare. 148. Recurvo-dentate quaternate spiculum, PI. II. fig. 23. Very rare. 149. Spiculum? PI. III. %. 12. A spherical body ornamented with five delicate projecting limbs, three on the one plane and one at either end. Only one specimen found. 150. Spiculum? PI. III. fig. 13. A spherical body covered with numerous projecting limbs. The few specimens found varied much in size. FORAMINIFERA PERFORATA. GLOBIGERINIDA. 1 5 1. Spiroplecta pr^longa (Reuss). Zoologically the same as Spiroplecta sagittula {Def ranee). Very rare. 92 Wright— List of Irish Cretaceous Microzoa. Table shewing the Geographical Distribution in List of Species. .2 0 •§> s 1 2 '3 s 2 'bp *u 0 3 3 -k White Mountain. 01 Colin Glen. o\ Black Hill. M 0 £ 7 co Squire’s Hill. <3 Cave Hill. 0 White well. 0 •8 V IS £ II £ Woodburn. X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X . X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X : X X X X X X X " X X X X X X X i. ». 3- 4- 5- 6. 7- S. 9- to. IX. 13. *3- *4- *5* x6. »7- x8. jg. 30. 31. 33. 23- 24* 35- 36. OSTRACODA. Cythere virginea, Jones Cythere Harrisiana, Jones (?) Cythere umbonata, Williamson Cythere ? Wrightii, sp. nov. Jones, MS Cythere ? Iernica, sp. nov. Jones , MS Cythere (Cythereis) ornatissima, Reuss Cythere (Cythereis) alata, Bosquet Cythere (Cythereis) spiculata, sp. nov. Jones, MS Cythere (Cythereis) vallata,sp. no v. Jones, MS. Cythere (Cythereis) montuosa, sp. nov. Jones, 3f^". ••••.. ......•• Cythere(Cythereis)cuspidis)sp.nov.y *3 & 4} *J3 0 'rt 13 S 3 22 T3 O O 2 3 £ U m £ u* c n rt O £ F* £ 2 3 4 5 6 7 8 9 10 II 12 Dentalina communis, D’Orb. ; var. Lilli, Reuss Dentalina communis, D'Orb., exquisitely deli- cate variety Dentalina communis, D'Orb. ; var. emaciata, Reuss Dentalina pauperata, D’Orb Dentalina Steenstrupi, Reuss.. . . Dentalina nodosa, D’Orb., var. Dentalina marginulinoides, Reuss. Subsep- tate variety Dentalina marginulinoides, Reuss. Cylindri- cal variety Frondicularia striatula, Reuss Frondicularia angustata, Nilsson Frondicularia Verneuiliana, D’Orb Frondicularia Archiaciana, D’Orb Frondicularia tenuis, Reuss Frondicularia inversa, Reiiss Frondicularia elliptica ( Nilsson ) Frondicularia mucronata, Reuss, var Flabellina lingula. Von Hagenow, var Flabellina rugosa, D’Orb Flabellina reticulata, Reuss Flabellina pulchra, D’Orb Flabellina pulchra, D’Orb. Narrow neat x X X X X variety Flabellina pulchra, D'Orb. Smooth variety with parallel sides Flabellina ornata, Reuss Lingulina carinata, D’Orb., var Marginulina glabra, var. elongata, D’Orb.. .. Marginulina bullata, Reuss Marginulina radicula (Linn.) Marginulina seminotata, Reuss Marginulina raphanus (Linn.) Vaginulina (Marginulina) trilobata, D'Orb. . . Vaginulina (Citharina) harpa, Rom., var. nov. Vaginulina costulata, Reuss Vaginulina costulata, Rom. Variety thin and slightly curved Planularia sp., near Planularia longa, Cornuel. Planularia crepidula, D’Orb., becoming Fla- bellina pulchra, D’Orb Cristellaria recta, D’Orb Cristellaria recta, D'Orb. ; var. hamosa, Reuss. Cristellaria recta, D’Orb., near C. Bronni. . . . Cristellaria rotulata (Lam.) Cristellaria navicula, D’Orb Cristellaria triangularis, D’Orb Cristellaria (Saracenaria) Italica, Dejrance. .. Cristellaria (Saracenaria) Italica, De/rance, long sub-variety Polymorphina damaecornis, Reuss X X X X Whitehead. Blackhead. Wright — List of Irish Cretaceous Microzoa. 95 Forth of Ireland of the Cretaceous Microzoa — ( Continued ). 2 GO c >* d V a Jh u 6 § in a e5 J2 0 s a .0 Xt XI O o 8 Ballytober. 8 rt a> 6 2 V 'S) as s >> a w o c/5 o 13 rTS .(U c/5 Keady Hil 1 i5 16 17 18 19 20 21 22 23 24 25 26 1 27 28 29 30 31 32 33 34 35 36 X 1 X X X 38. X X X X X 39- X X X X X X X 40. i X X X X X X X X X X X X X X X X X X X X X X 41. X 42. X X X X X X X X 43- X X X X X 44. X X X X 45. X X X X X X X X X X X X X 46. X X X X X 47- X X X X X X 48. X X X X X X X 49. X X X X 5°- Si- X 52- X X X X X X X X X X X 53- 54- X 55- X X X X X X X X X X X 56. X 57- X X X 58. X 59- X . . 60. X X X X X X X X X X X X X 62. X 63- 64. X 65- 66. X X X X 67. X X X X 68. 69. X X X 7i- X X 72. X X X X X X 73- X 74- 75* 76. X X X X X X X X X X X X X X X X X X X X X X X X 77- X X 78. X X X X 79- X 80. X X X X x •• 1 •• 8 1. 96 Wright— List of Irish Cretaceous Microzoa. Table showing the Geographical Distribution in thi List of Species. .5 a s rC SP 2 I » Moira. 0 0 S3 M 3 +• White Mountain. Colin Glen. w rt 3 6 K Cm 1 7 00 Squire’s Hill. s l 0 9 0 Whitewell. h Whiteabbey. 3 Woodburn. t 0 A. a 13 £ 13 ! 82. Polymorphina horrida, Reuss X X X X 83. Polymorphina fusiformis, Romer X X X X X X 84. Polymorphina regina, B. P. &> y., var 8-5. Uvigerina nodosa, D’Orb 86. Globigerina cretacea, D'Orb X X X X X X X X X 87. X 88. Globigerina bulloides D’Orb., var. nov., heaped X 89. Globigerina marginata ( Reuss j X X X X X X X X 91. Textularia gibbosa, D'Orb X 92. Textularia pupa, Reuss X X X X 93- Textularia sagittula, Defrance X X X X X X X X X 94- Textularia trochus, D’Orb 95- Textularia turris, D’Orb X X 96. Textularia turris, D’Orb., short and thick variety X X X X X X X X 97- Textularia foeda, Reuss X X X X X X X 98. Textularia prselonga, Reuss X X 99. Textularia globulosa, Ehr X X X X X X X Verneuihna triQuctra ( x X X X IOI. Gaudryina rugosa, D'Orb X X •5 S 102. Gaudryina pupoides, D’Orb. ; var. praelonga, Reuss X 107. Tritaxia triquetra ( Ministry) , X J 104. Bulimina Presli, Reuss X X X X X T 105. Bulimina ovuium, Reziss X X X X X X X X X X X IO6. Bulimina brevis, D’Orb X X X X X X X X X X X X ■ 107. Bulimina intermedia, Reuss X X 108. Bulimina regularis, sp. nov. yones, MS X ? Bulimina sp. x 109 no. Virgulina tegulata, Reuss, var X X X X X X X X X x J Bolivina derorat*^ pny MS* x X X X X X X X 112. Bolivina, sp •• 1J3- Pleurostomella fusiformis, Reuss X X X X X X X .. 114. Planorbulina exsculpta, Reuss X X X X X X X x iiS- Planorbulina ammonoides (Reuss.) X X X X X X X X X X X x 1 116. Planorbulina ammonoides (Reuss), var. with extra shell-growth X X X X X X X X X X X X 117. Planorbulina crenulata (Reuss) X X X X X X X 118. Truncatulina lobatula (W. <5r» J.) X X X X X X 119. Pulvinulina Micheliniana (D’Orb.) X X X X X X X X X X 120. Rotalia orbicularis (D’Orb.), var X X X X X X X X X X 121. Rotalia vel Planorbulina ?, with each chamber symmetrically perforated X 122. Ramulina laevis, gen. et sp. nov. yones X 123. Sponge Spicula, &c. 124. Acerate spiculum. PI. II., figs. 1 & 2 X X X !25- Attenuato-acuate spiculum. PI. II., fig. 3 .. X X X X X X X 126. Moniliform attenuato-acuate spiculum. PI. II., f ]ff. A X X X X I27. f * \ _ Furcated porrecto-temate moniliform spiculum 1 PI. II., fig. 5 X ” ! X X X •• •• 1 Near Gobbins. Wright — List of Irish Cretaceous Microzoa. 97 >rth of Ireland of the Cretaceous Microzoa — (Continued). c 1 0 U CJ £ *5 o\ Ballytober. ■3 Near Mill Bay. a O £ 2 Js * S 18 14 rt u >. 'rt M o c/5 19 § Redhall Glen. 1> o c V o 21 6 01 1 22 in rt h m w> ri C/3 23 £ 5 a V 6 24 § a 25 8v Garron Point. its 'S C V O 27 i £ bi 28 (3 X 1 0 H 29 -T3 cS 4) X u H 30 .£ n pa 31 ^ White Rocks. 2 0 £ Sr § s O J5 33 X bil c 'u a, in 34 $ Slieve Gallion. Ready Hill. X X X X X X X 82. X X X X X X X X X X X 83. X X X X 84. X 85. X X X- X X X X X X X X X X X X X X X X X 86. X 87. X X 88. X X X X X X X X X X X X 89. X X X X X X X X X X X X 90. r X X X X X X 91. X X X X X X X X 92. X X X X X X X X X X X X X X 93- X X 94. X X X X X X X X 95* X X X X X X X X X X X X X X 96. X X X „ X X X X X X X X X X 97- X X X X 98. c X X X X X X X X X X X X X X X X X X X 99. X X X X X X X X X X X X coo. X X X ,101. X X X 102. X X X X X X X X 103. s X X X X X X X X X X X I04. )C X X X X X X X X X X X X X X X * 105. X X X X X X X X X X X X X X X X X I06. X X X X X X I07. X X 108. IO9. K X X X X X X X X X X X X X X X X X no. X X X X X X X X X X X X X X X X in. X X 1 12. X X X X X X X X JI3* X X X X X X X X X X X X X X X X 114. X X X X X X X X X X X X X X X X X X X X X X X nS- X X X X X X X X X X X X X X X X X X X 116. X X X X X X X X X X X X X 117. X X X X X X X X X 118. X X X X X X X X X X X X X 119. X X X X X X X X X X X X X X X X X X X X 120. 121. X X X X X 122. X X 123. X X X X X X X X X X 124. X X X X X X X X X X X X X X 125. X X X X X X X X X X X X X 126. • 1 x X •• X X X X X 127. 98 Wright — List of Irish Cretaceous Microzoa. Table showing the Geographical Distribution in the! .3 *3 .s 0 aS o3 *0 . bS) ’E O 0 C 3 O s T5 > >> 0 (3 *34- 135- 136. i37- 138. 139- 140. 141. 142. 143- 144. 145- 146. 147. 148. 149. 150. 15*. Equiangular triradiate spiculum. PL II., fig. 6 Spiculated equiangular triradiate spiculum. PI. II., fig. 7 . Incipiently expanso-ternate spiculum. PI. II., fig. 8 Expando-ternate spiculum. PI. II., figs. 9&10 Expando-ternate spiculum, with cylindrical radii. PI. II., figs. 11 & 12 Furcated attenuato-patento-ternate spiculum (constricted). Pi. II., fig. 13 Furcated attenuato-patento-ternate spiculum PI. II., figs. 14 to 16 Furcated attenuato-patento-ternate spiculum PI. II., fig. 17 Furcated attenuato-patento-ternate spiculum. PI. II., fig. 18 Recurvo-ternate spiculum. PI. II., fig. 19. Spiculum. nov. PI. III., fig. I Spiculum. PI. III., figs. 2&3 Porrecto-ternate spiculum. PI. II., fig. 20 Porrecto-ternate spiculum. PI. II., fig. 21 Porrecto-ternate spiculum PI. II., fig. 22 Attenuated rectangulate hexradiate spiculum PI. III., figs. 4& s Skeleton fibres. PI. III., figs 6 & 7 .... Skeleton fibres. PI. III., figs. 8 & 9 .... Skeleton fibres. PI. III., fig. 10 Sponge Spicula. Sphero-stellate spiculum. PI. III., fig. 1 1 Recurvo-dentate quaternate spiculum. PI. II., fig. 23 - Spiculum ? Plate III., fig. 12 Spiculum ? Plate III., fig. 13 Foraminifera. Spiroplecta prselonga, ( Reuss ) Whitehead. Near Gobbins. Wright— List of Irish Cretaceous Microzoa. rth of Ireland of the Cretaceous Microzoa— ( Continued). 99 X X X x § Redhall Glen. V o a jj O 21 Jo Waterloo. w Sallagh Braes. B U OS a jy 5 24 £ Carnlough. ■3 Ah a 0 £ rt O 26 ^ Glenariff. a a £ 1) .bp 'jH 3 i-3 28 a -s 1 U ) O H 29 $ Torr Head. m Ballintoy. ^ White Rocks. 0) O a >. c 0 2 <+* 0 & 33 Spring Hill. a .0 O > .0 c/5 35 X >» ■■o and Polystomella striato-punctata , in shore gatherings taken at Grey abbey and Newtownards. Belfast Lough being more convenient for operations than Strangford Lough has been better examined ; the water is shallow throughout, but gets gradually deeper as we near its mouth. From White Head on its northern entrance to Orlock Point on its southern side, the greatest depth is 9 to 10 fms., the deepest parts being near the northern shore ; and this continues also to be the case out- side the lough. Three miles off the Gobbins, a bold headland situated three miles N.E. of White Head, the water attains a depth of 60 to 70 fms., and in the vicinity of the Maiden Lighthouses 70 to 100 fms. Here, however, the bottom is rocky, and yields little or no fine material. The tides all round the coast run with great violence. Too much stress cannot be laid on the necessity Wright — Recent Foraminifera of Down and Antrim. 103 of selecting slack tides for dredging these parts, as otherwise the operations are certain to end in disappointment and failure. A table is appended of the stations from which the various gatherings were taken, with particulars of bathymetrical range, nature of sea bottom, weight of material brought up, and number of species found. As the quantity of material dredged varied greatly at different stations, it appeared desirable to record the weight collected at each place, so as to arrive at a correct estimate of the relative abundance of foraminiferal life at the various places. (1.) To my friend Mr. Henry B. Brady, F.R.S., I am deeply indebted for the kind assistance he has rendered me in the critical examination of the doubtful species ; and likewise to my friend Mr. William Swanston, F.G.S., for the accu- rate and artistic drawings in the plate which accompanies this memoir. The following Foraminifera deserve a passing notice, viz. : — Biloculina ringens, {Lamk.). Generally distributed at various depths. A variety of this species is not uncommon in deep water, small in size, and in contour approaching B. sphcera. Triloculina oblonga, {Montagu). Very abundant in Strangford Lough, where the specimens are large and typical ; in Belfast Lough it is rare, and the specimens usually small. Lituola globigeriniformis, P . and J. Not unfrequent in Belfast Lough and Strangford Lough; and it also occurs plentifully in Cork Harbour and Kinsale Harbour. Lagena sulcata, W. and J. The costae on this species are sharply defined, about every alternate one extending up the neck, round which they are usually somewhat twisted. Lagena costata, {Will.). This species differs from the last in being entosolenian; in full-grown ex- amples the shell is spherical, with the costae slightly raised and very regular, extending to near the neck, where they usually end abruptly, the remainder being smooth, as is also the neck, which is short. The texture of the shell is more glassy than in L. sulcata. Williamson’s figure represents a young speci- (1.) A very ingenious dredge has been constructed by Mr. David Robertson, F.G.S., of Glasgow. It dips deep into the bottom and fills quickly. It has an advantage over the ordi- nary dredges in this respect, as each haul brings up a very uniform quantity of the sea bottom. See notes on the recent Foraminifera and Ostracoda of the Firth of Clyde, by David Robert- son, F.G.S. — Trans. Geol. Soc. of Glasgow, Vol. V., Part I., p. 112. 104 Wright— Recent Foraminifera of Down and Antrim. men; in this state it has no neck, the shell is thin and sufficiently transparent to show the internal tube. Lagena Williamsoni, ( Alcock ). This form differs from Lagena costata , to which it is closely allied, in being smaller in size, less spherical in shape, and the sulci more sharply defined Its chief peculiarity, however, is in the neck, which is short, and formed of two distinct portions — the first directly continuous with the body, and ornamented with two or three rows of hexagonal reticulations; the second a small cylindrical tube, continued from the centre of it. This form is abundant everywhere round our coast, and common in the Estuarine Clay at Magheramome, County Antrim. Lagena striato-punctata, P. and J. A few examples of this Lagena were met with in Strangford Lough; one specimen was also found in Cork Harbour. Abundant in the Estuarine Clay at Magheramome, County Antrim (i). Lagena hispida, Reuse. Ovate, surface covered with numerous blunt spines having a tendency to run into one another in longitudinal rows ; a very rare species, only a few ex- amples having been found. It is new to Britain. Lagena Jeffreysii, Brady. Only one example found ; transverse section round. Mr. H. B. Brady, F.R.S., informs me “that the species is usually slightly quadrate in transverse contour, but sometimes quite round; is always slightly aculeate; theacnlei quite spinous and pointed, very numerous and minute, and the neck commonly with spiral ornamentation. It often has to be washed with hot solution of some al- kali to get the encrusting dirt off, as it seems without this a mere rough form that catches dirt.” Lagena trtgono-marginata, P. and J. A three-sided form of Lagena marginata. Very rare. Lagena oblonga, ( Seguenza ). A three-sided form of Lagena lucida. Very rare. A few examples have been found in the Estuarine Clay at Magheramome, County Antrim. (i.) I am indebted to my friend Prof. T. Rupert Jones, F.R.S., for his opinion on this Lagena and for some of the other Foraminera given in this list. Wright — Recent Foraminifera of Down and Antrim. 105 Vaginulina legumen, (Linn. ). Large and abundant in the deep water of Strangford Lough. Vaginulina linearis, {Montagu). Large and abundant in the deep water in the vicinity of the Maiden Light- houses. TiNOPORUS LUCIDUS, Brady MS. Generally distributed, but usually occurring in a very fragmentary state. Living specimens were found in the deep water in Strangford Lough, as also in the vicinity of the Maiden Lighthouses. This species is abundant in Dog’s Bay, Connemara ; it also occurs in Kinsale Harbour,- and Cork Harbour. A few examples have been met with in the Estuarine Clay, Magheramorne, County Antrim. Discorbina parisiensis, (D'Orb.). This species has not hitherto been recorded as British. It was first found in shore sand near Greyabbey, Strangford Lough; spire depressed, and exhibit- ing in fine state the characteristic dotted lines on the inferior surface. It has since been found in abundance in several of the shallow water gatherings in Belfast Lough, the specimens being usually more conical than those from Grey- abbey (see figs 2 a, 2 b). It has been also found in Kinsale Harbour, and occurs, fossil, in the Estuarine Clay at Magheramorne, County Antrim. Mr. H. B. Brady writes me with reference to this species “ The specimens of Discorbina farisiensis are all very minute, and they vary considerably in contour, some having the thin sharp edge, and low conical figure of D’Orbigny’s Models, whilst others are round-edged and thicker; all have the characteristic stnation of the inferior surface. The latter variety approximates closely to the charac- ters of D. obtusa , and suggests the near relationship of the two forms. It should be observed that D . parisiensis has been obtained of the Rev. A. M. Norman, in dredgings from the North Atlantic, whilst D. obtusa is not only of frequent occurrence in the Arctic Seas, but has been found on our own shores.” EXPLANATION OF PLATE IV. Fig. i . Discorbina parisiensis, (D’Orb. ). I a, upper surface; I b , lower surface; 1 c , edge view, x 60, diam. ; I d, fragment of lower surface, showing- structure, greatly enlarged. Shore sand, Greyabbey, Strangford Lough, County Down. ,, 2. Discorbina parisiensis, (D’Orb. ). 2 a, upper surface; 2 b , lower surface; 2 c, edge view; x 6odiam. Off Grey Point, 6 fms. „ 3. Trochammina gordialis, P. and J. x 60 diam. Off Black Head, 20 fms. „ 4. Tinoporus lucidus, Brady MS. 4 a, upper surface; 4 b , edge -view; x 40 diam. White Knowe, Strangford Lough, 6 fms. ,, 5. Tinoporus lucidus, Brady MS. Encrusting a stem of polyzoan; x 30 diam. Off Maiden Lighthouses, 60 fms. „ 6. Lituola globigeriniformis, P. and J. x 60 diam. Off Maiden Light- houses, 60 fms. ,, 7. Lagena hispida, Reuss. x 60 diam. Off Black Head, 18 fms. ,, 8. Lagena trigono-marginata, P. and J. 8 a, side view; 8 b, end view- showing aperture; x 60 diam. Off White Head, 7 fms. ,, 9. Lagena oblonga, (Seguenza). 9 a, side view; 9 b, end view, showing aperture; x 60 diam. Off White Head, 10 fms. ,, 10. Lagena sulcata , W. and J. x 60 diam. Off Black Head, 18 fms. ,, 11. Lagena costata , (Will.), x 60 diam. Off Black Head, 18 fms. „ 12. Lagena costata, (Will.). A young specimen, x 60 diam. Off Maiden Lighthouses, 60 fms. ,, 13. Lagena costata , (Will.). Bilocular, x 60 diam. Off Orlock Point, 11 fms. „ 14. Lagena Williamsmi, (Alcock). x 60 diam. Off White Knowe, Strang- ford Lough, 6 to 8 fms. „ 15. Lagena Jeffrey sii, Brady, x 60 diam. Off Maiden Lighthouses, 62 fms. 27oc 2#2asl2Vat77z2d 67ul. 2277- 77- (2fy?en2i2j 27. 2J7 StVAHSTOH, DEL WRI GHT-FORAMINIFERA OF DOWN AND ANTRIM ARCHER i SOHS. L/TH I I iii IS. LIST OF LOCALITIES, WITH PARTICULARS OF DEPTH, &c. Localities. Bathymetrical range. A B C D E F G H I J Downhill beach, Co. Derry, 5 miles N.W. of Coleraine Camlough, Co. Antrim, on East, 14 miles N. of Larne Brown's Bay, Islandmagee, Co. Antrim . . Ballyholme Bay, Co. Down, x mile E. of Bangor Ballywalter, Co. Down, 7 miles S. of Donaghadee . . Ballyhalbert, Co. Down, 4 miles S. of Ballywalter Cloghy Bay, Co Down, sj miles S. of Ballyhalbert Ballyhoman Bay, Co. Down, 6 miles E. of Downpatrick .. Tyrella or Dundtum Bay, Co. Down, 6 miles S. of Downpatrick Newcastle beach, Co. Down, between Newcastle and Dundrum.. Between tides ditto ditto ditto ditto ditto' ditto ditto ditto ditto 2 3 4 5 6 7 8 9 10 XI 12 13 14 15 x6 17 18 19 21 22 23 24 25 26 27 28 29 Conswater, between Railway Bridges, brackish Holy wood Bank . . Between Carrickfergus and Kilroot Donaghadee Off Rockport . . . . . . . . . . . . Off Carrickfergus Bangor Bay Ofi Bangor Bay Off Grey Point — Mid-channel Off White Head Off White Head . . Off Orlock Point Off Black Head Off Black Head J Mile off Coalpit Bay 2 Miles N.W. of Copeland Island 2 Miles N.E. of Larne .. 2J Miles N.E. of Donaghadee 2 Miles N.E. of Muck Island ' 2 Miles S. of Maiden Lighthouses 3 Miles S.S.E. of Maiden Lighthouses 2 Miles S.S.E. of Maiden Lighthouses Near Newtownards, Strangford Lough, brackish . . Near Greyabbey, Strangford Lough, slightly brackish Off White Knowe, Strangford Lough . . Off Chapel Island, Strangford Lough Off Bar Rock, Strangford Lough Off Dononeill, Strangford Lough Off Marlpool, Strangford Lough ditto ditto ditto ditto 4 fms 5 fms 4 to s fms 5 fms 6 fms 6 to 7 fins 10 fms 11 fms 15 to 18 fms 20 fms 13 fms 14 fms 22 fms 25 fms 50 fms 60 fms 62 fms 72 fms Between tides ditto 6 to 8 fms 8 to 10 fms 10 to 15 fms 12 fms 20 to 25 fms Sea Bottom. Sand Sand Sand Said S4d Sand ^ Sand . . )' * Sand . . . . . . Sand Sand Mud Fine sand Fine sand . . Fine sand . . Sand and dead shells Coralline . . Sand and dead shells Sand and dead shells Muddy sand and dead shells ... Coralline and mud — two gatherings . . Sand and dead shells Sand Mud, sand, shells, Polyzoa— six gatherings . . Sand Sponges Sand and shells . . ’ Dead shells . . . . Sand and dead shells . . Stones and shells . . . . Sand Sand Sand and Zoophytes— several gatherings . . Sand . . Sand . . . . Mud and sand Sand . . . . . • Sand and shells . . Sand and shells Sand . . Relative quantities of material examined. Number of Species from each locality. 4 oz 33 9 oz 38 1 lb 1 oz 4t 6 oz 3i 6 oz 27 4 oz 42 4 oz 18 9 oz 4i 12 oz 36 4 oz 34 2 lb 4 oz 12 81b 36 81b 26 81b 46 9 oz 49 S oz 66 9 oz 56 3 lb 8 oz 46 3 lb 76 2 lb 66 3 lb 80 8 1b 89 6 lb s oz 92 22 lb 9i 70Z 67 1 lb 9 oz 78 1 oz 21 1 lb 2 oz 38 40Z 3° 8 lb 85 Sib 13 oz 77 11 oz 68 61b 6 3 lb 12 oz 23 81b 85 2 lb 8 oz 73 2 lb 12 oz 54 2 lb 77 5 lb 52 Note. — The first nine gatherings, lettered A to I, have been sent me by Mr. Wm. Gray, M.R.LA., arcomp^ied vritk a note riw^^the^j jfnfs ieft by the Herewith I send you nine samples Foraminiferal sand. All the samples were collected off .lbe surface o However" I wmild not place any value on the rela+:"“ receding tide. Injme cases I : Jwas able to Ufa a ^aner^gathering of the organic Sounder which the sew proportions of sand and organic remains from the respective stations, as the proportion must vary gatherings were made." .tive several if/ TABLE SHEWING THE DISTRIBUTION OP FORAMINIFERA IN THE COUNTIES OF DOWN AND ANTRIM. [ Proceedings Belfast Naturalists ’ Field Club— Appendix , 1876-77.] OS THE SILURIAN ROCKS OF THE COUNTY DOWS. Part I. — Correlation. BY WILLIAM SWANSTON, F.G.S., . # Hon. Assoc, of the Belfast Nat. Hist, and Phil. Soc. -*=§=«* INTRODUCTION. In a paper which I had the honour of reading before the Club in March, 1875, I endeavoured to give some particulars of a series of fossils which I had obtained from the Silurian rocks of the County Down. At that time I had succeeded in procuring them from only one locality — Coalpit Bay, near Donaghadee, — and the results did not exceed fifteen species. Further research in the same locality, and a more extended examination of the district, have been rewarded by a large addition to the list, affording better evidence than has hitherto been available for determining the geological position of the rocks in which they are found. The Silurian rocks of County Down form part of an area which is rudely triangular in form. A line drawn from Grey Point on the shore of Belfast Lough in a south-westerly direction through Holywood, along the valley of the Lagan, by Lisburn and Waringstown, would mark its north-western boundary. The Irish Sea bounds it on the east, and to the south the Carboniferous lime- stone forms the base of the figure by an irregular line running westward from Drogheda. It comprises the greater parts of the Counties of Down, Armagh, Monaghan, Louth, Meath, and Cavan. The district is an agricultural one, its surface of an undulating or hillocky character, possessing few elevations deserving the title of mountains, the granitic areas of Moume, Carlingford, and Ballynahinch being excepted. It is not intended in the present paper to G I08 Swanston— Silurian Rocks of Co. Down. do more than notice the rocks which occupy the north-eastern portion of the area situated wholly in the County Down. PREVIOUS NOTICES OF THE DISTRICT. Perhaps the earliest reference to the rocks of this area is that by Drs. Berger and Conybeare, made in 1816. (i) These pioneers of Irish Geology pointed out the similarity between the County Down rocks and those of South Scotland. On the large geological map compiled by Sir Richard Griffith in 1839 the area is put down as Clay-slate or Greywacke-slate belonging to the Transition series. Dr. Bryce in 1852 stated as follows (2) ' “The County Down con- tained two granitic tracts which seem to have been elevated at different epochs. They are separated from one another, and each is wholly enclosed by a thick band of metamorphic slate, gneissose in its lower part, and passing upwards into flinty and common clay-slate. Superimposed conformably upon these are other slates of less crystalline type, whose aggregate thickness is enormous, and whose upper portions have yielded a few imperfect fossils, which seem to make them referable to the Lower Silurian Group ; but as yet no definite line has been made out to justify a classification.” Sir Roderic Murchison states in 1854 (3) : — “ It is believed that the Schists of Down are of the same age as the Graptolitic Schists of Wigton and Galloway. ” J . Beete Jukes, F. R. S., after referring to the Chair of Kildare, which contains Bala fossils (4), states that “ another great tract of apparently similar beds stretches from the centre of Ire- land, Cavan, &c., to the coast of Down. Among these, however, a portion certainly belongs to the Llandeilo Flags, as near Bellewstown, on the confines of Dublin and Meath, an assemblage of Llandeilo fossils were found. Many years ago it was known to members of the Club that Graptolites occurred in the County Down, and specimens were obtained by them at Tully- garvan, near Saintfield, from the debris of a shaft which was there sunk in the Silurian rocks in search for coals (5); none were, however, sufficiently perfect for identification. (1) . Transactions of the Geological Society of London, Vol. III. (2) . Report of the British Association (1852). (3) . Siluria (1854)— foot note, p. 166. (4) . Manual of Geology (1862), p. 454. (5) . The slightest knowledge of the evidence furnished by these fossils would have saved a vast amount of useless expenditure and misdirected efforts here, and at many other localities throughout the district. The projectors in their search for coals were doubtless imsled by the resemblance of the black Graptolitic bands to the rich carbonaceous shales of the Coal Measures. Swanston — Silurian Rocks of Co. Down. 109 The Geological Survey in its progress northward has almost completed the mapping of this area. The maps of the County Down were published in 1871-72(1). The Silurians are either set down on them in general terms as Lower Silurian, or areas indicated by letters but whose boundaries are often undefined, are assigned to the Bala or Caradoc, and to the Llandeilo. In their examinations of the rocks several fossil localities were discovered which had hitherto been overlooked, and in the “ Explanatory Memoirs ” lists of species were published from time to time (2). The want of precision throughout the foregoing notices is no doubt due to the highly disturbed nature of the strata and comparatively uniform lithological character of the rocks, making the determination of their stratigraphical rela- tions a matter of very great difficulty. This difficulty was much enhanced by the absence, until very recently, of fossil evidence sufficient to allow their correlation with other deposits. LITHOLOGICAL CHARACTER OF THE ROCKS OF THE DISTRICT. Lithologically the rocks consist for the greater part of grey and purple grits — occasionally conglomeritic— pale grey or greenish slates and flags, and a few widely separated bands of black shales. The latter, though forming but a small portion of the entire rocks here exposed, constitute a group which will claim most attention in the following brief notice. In them are found all the fossils which are enumerated in the accompanying table, and it is from a careful study of their fossil contents that we are enabled to arrive at an estimate of their geological position, and that of the barren grits and slates associated with them. The usual dip of the rocks is to the south-east and south, at angles varying from 30° to vertical. Their continuity is much disturbed by faults and contortions, and their upturned edges, where exposed, bear evidence of having suffered much from denundation. Almost the entire rocks of the area are obscured by drift, and with the exception of the coast-line, few good sections can be seen. The grey and purple grits have not as yet yielded any fossil remains, and it is only within the past few months that they have been detected in the grey slates, a notice of which will be given further on. (1) . Geological Survey of Ireland, maps 29, 36, 37, 38, 47, 48 and 49. (2) . Explanatory Memoirs, accompanying maps 37, 38, 29, 48, 49, 50, and 61. 10 Swanston— Silurian Rocks of Co. Down. FOSSIL LOCALITIES. Tieveshilly. — About two miles south of Portaferry, and a short distance east of the bridge on the main road over Carstown Burn, are several quarries formerly worked for roofing- slate. The quarries are low lying, and in winter aie filled with water. In dry seasons, however, the rock can be reached, and proves to be thin fissile slates and flags, varying in colour from almost black to pale greenish gray : the dip is nearly vertical, and they have the usual strike of about N.E. and S. W. The dark bands are very fossiliferous, and many of the fossils are beautifully preserved ; fifteen species have been obtained from this locality, all, with the exception of one crustacean, belonging to the Grap- tolitidse . Coalpit Bay.(i) — This locality is situated on the shore, about three- quarters of a mile south of Donaghadee, and is only accessible when the tide is low. As it is the best exposure of these fossil-bearing rocks, a more detailed account of it is here given. A series of massive grey grits and slates occur to the southward of the little bay, dipping at high angles to the south, and terminating northward in a low escarpment. At their base we find the following rocks, upon which they apparently rest conformably : — I. Massive black slates, with several light-coloured clay bands ; the slates containing, among others, the following characteristic fossils : — Rastrites peregrinus, var. hy- BRIDUS, Lapw. Monograptus Sedgwickii, Portl. „ INTERMEDIUS, var. PROTEUS, Barr. Cephalograptus (Diplograptus) Monograptus tenuis, Portl. ,, lobiferous, M'Coy. Diplograptus Hughesii, Nick. ,, sinuatus, Nick. ,, TAMARISCUS, Nick. COMeta, Geinitz. - - io feet. 2. Dark green mudstones, with several bands, each from two to four inches thick, of buff and light purple clays — unfossiferous — 35 feet. (1). So named from a futile attempt to find coals in the black Graptolitic slates here ex- posed. Swanston— Silurian Rocks of Co. Down. hi 3. Massive black slates and shales rich in fossils ; the following are a few of the most characteristic : — Rastrites peregrinus, Barr. Monograptus gregarius, Lapw. ,, concinnus, Lapw. ,, Sandersoni, Lapw. „ triangulatus, Harkn. ,, spiralis, var. fimbriatus, Nich. Diplograptus folium, His. ,, TAMARISCUS, Nich. ,, VESICULOSUS, Nich. Dimorphograptus elongatus, Lapw. Discinocaris Browniana, Woodw. Dawsonia campanulata, Nich. This area is considerably covered with shingle and sand, and the rocks are intersected by several faults carrying them to the north-east ; their thickness may be set down at about - - - - - 100 feet. 4. A dyke composed of pale grey finely crystalline calcareous rock running easterly (1) .... 6 feet. 5. Pale grey and greenish mudstones, greatly shattered and unfossili- ferous. ...-- about 65 feet. Near the base of these mudstones is a thin band of black shale greatly crushed, in which no fossils have yet been detected, but higher up in the mud- stones a fragment of black shale, about two feet in diameter and several inches thick was found containing well-marked specimens of Dicellograptus Forcham - mcriy Geinitz. 6. Black shales highly indurated and containing numerous flinty bands, and nodules and veins of iron pyrites. The less altered portions are rich in fossils and have yielded the following : — Climacograptus tricornis, Carr. „ ccelatus, Lapw. „ bicornis, var. peltifer, Lapw . Dicellograptus elegans, Carr. Dicranograptus formosus, Hopk. Dicranograptus zic zac ,var. min- nimus, Lapw. Acrotreta Nicholsoni, Dav. Acrothele granulata, Linrs. These shales are too much shattered and crumpled to allow of their thick- ness being exactly estimated. It may, however, be roughly put down at about 50 feet. They form the ridge of a sharp anticlinal, which has for its axis (1). Geological Survey of Ireland — Explanatory memoir to sheets 37, 38, & 39. p. 31. 1 12 Swanston — Silurian Rocks of Co. Down. another series of mudstones somewhat resembling those noted in paragraph 5 of this section. The succeeding rocks in order, still going northward, are a repetition of the mudstones noted in paragraph 5, partially hidden by sand. No rocks are now seen for about 60 feet, and a fault here breaks the continuity of the section, the next beds exposed being — 7. Black fissile shales and slates dipping S. 20 E. at 750. These sud- denly curve over to the opposite direction, and a few feet further north regain their original dip. The section is again lost for several hundred feet, and the next rock ex- posed is massive grey grits and slates, similar to those on the south side of the bay, and having the normal dip of the rocks of the district. Tullygarvan. — This fossil locality is situated about one and a half miles -east of Ballygowan Railway station (Belfast and County Down Railway), in the bed of a small stream which flows eastward through the grounds of Tully- garvan House. The rocks near to the shaft which was sunk in search for coals are of a black carbonaceous character, greatly contorted, and much stained with iron. No fossils have yet been detected in them ; but judging from the few traces obtained from the debris of the sinking, and from the character of their associated mud-stones, they seem to correspond with those in the axis of the anticlinal at Coalpit Bay. Black-slates are exposed further up the stream in several places, yielding in all seven species of Graptolites, referable to the beds described in paragraph 3 of the same locality ; thus pointing to the probability that the rocks here shewn are the westerly extension of those beds. Orlock Point. — On the shore to the north-east of the coastguard station, black and red shales are exposed between tide marks for about 200 yards. They are bounded on the north and south by purple slates, dipping S. 20 E. at angles varying from 40° to vertical. It is impossible, however, to arrive at the order of occurrence of the black and red shales here exposed, as they are much disturbed by minor faults cutting through them in various directions. The con- tinuity of the section is also broken by a dyke of fine grained Elvanite 10 feet wide, running from west to east, almost in the direction of the strike of the rocks. This dyke undoubtedly occupies the line of a more important fault as we find the rocks on the south side of it consist of black flinty shales, while to the north these are replaced by brown and purple arenaceous beds which pass Swanston— Silurian Rocks of Co. Down. 113 up into the prevailing purple and grey slates of the district. Graptolites have been found in the less altered portions of the black shales, they are, however, very indistinct, and onlv two species — Leptograptus flaccidus, Hall, and Dip- lograptus truncatus , Lapw.=#m/A, His. — could with certainty be made out. In a thin pale grey arenaceous band associated with them occur plant remains, which have been identified as belonging to the genus Buthotrephis , but appar- ently of a species not hitherto figured. Carnalea. — On the shore north of Carnalea Railway Station (Belfast, Holywood and Bangor Railway) just where a small stream flows into the Lough, there is a small exposure of black shales almost vertical. To the south-east they abut against grey slates and grits, and seaward they are covered with shingle and sand. These black shales are rich in fossils, but from the shivery nature of the beds they are usually in a fragmentary state. Among the most characteristic are the following : — Diplograptus truncatus, Lapw. Dicellograptus Forchammeri, „ quadrimucronatus, Hall. Geinitz. Lasiograptus Harknessi, Nick. „ elegans, Carr. Retiolites fibratus, Lapw. Leptograptus flaccidus, Hall. Climacograptus tubuliferus, Lapnv. Crawfordsburn. — Immediately opposite Crawfordsburn House, on the shore near low water mark, grey mudstones and black shales occur, the general strike of which is N. 20 E. In one place, however, the beds are broken sharply across, bent in a direction exactly at right angles to it, and in part inverted. Fossils are few and fragmentary. Ballygrot. — This locality, named from the townland in which it occurs, is near Grey Point, and is also situated on the shore. The rocks consist of a series of pale green mudstones and black shales, which are again followed by a band of grit and an exposure of several hundred feet of black ferruginous shales, containing flinty bands, and which are much threaded with quartz. Faulted against these to the north is a series of purple and grey shales, which are again followed by black shales similar in character to last. Irregularly bedded grits and slates succeed these, and prevail for a considerable distance. No fossils have been detected in the grey or purple shales, but the less altered Swanston— Silurian Rocks of Co. Down. 114 portions of the black ferruginous bands are exceedingly rich, and have yielded a large series, among which are the following : — Diplograptus tricornis, Carr. ,, ANGUSTIFOLIUS, Hall. Glossograptus Hincksii, Nich. CLATHOGRAPTUS CUNEIFORMS, Climacograptus Scharenbergi, Lapw. „ BICORNIS, Hall. ,, ,, var. pel- TIFER, Lapw. „ ,, var. tri- DENTATUS, LapW. ,, CCELATUS, Lapw. ,, PEREXCAVATUS, Lapw. Dicranograptus ramosus, Hall. „ Nicholsoni, Hopk. „ FORMOSUS, Hopk. Dicellograptus Moffatensis, Carr. „ „ van DIVAR1CATUS, Hall. Didymograptus superstis, Lapw , CCENOGRAPTUS GRACILIS, Hall. „ PERTENUIS, Lapw. „ SURCULARIS, Hall. Thamnograptus typus, Hall. CORYNOIDES CALICULARIS, Nick. „ curtus, Lapw. Craigavad. — The fossils noted from this locality were obtained from the railway cutting about three-quarters of a mile east of the station. A very small exposure of black shales occur associated with purple shales and grits. The few fossils obtained point to the similarity between the containing beds and those of Ballygrot, of which they are doubtless the south-westerly exten- sion. The accompanying table gives a list of the fossils which I have collected from the foregoing localities. The total number is seventy-five species and thir- teen named varieties, in all representing twenty-five genera. This is exclusive of many doubtful forms that have been laid aside waiting better specimens to enable their identification ; also, several that are undoubtedly new, but which are either too fragmentary or badly preserved to warrant a diagnosis. The following is a synopsis of those already named, shewing the zoological groups to which they belong : — SUB-KINGDOM. CLASS. Species. Varieties. Ccelenterata. Annulosa. Mollusca. Plant/e. Riiabdophora. Crustacea. Brachiopoda. 68 3 3 1 13 Swanston— Silurian Rocks of Co. Down. 115 It will be noticed from the foregoing that a large proportion of the fossils belongs to one class- namely, the Rhabdophora or Graptolithina. It is not my intention to offer any suggestions as to the conditions which prevailed during the deposition of these fossiliferous black bands, conditions alike favourable to this singular group of organisms, and apparently unsuitable to others. It may be observed, however, that no group affords a better index to the palgeontolo- gist in his endeavours to unravel the sequence of rocks of Silurian age than does the Graptolithina. The number of known species is very large, and it has been ascertained that the vertical range of most of them is very restricted- many, indeed, being confined to zones of but a few inches in thickness. The immense profusion also in which they frequently occur stamps each zone with a character easily recognisable by those who study their form and character. The similarity of the County Down rocks to those in South Scotland was conjectured, as before stated, so early as 1815. This conjecture appears to have been founded more upon the general appearance of the rocks of the two areas than upon any positive evidence that was then obtained from them Subsequent writers did little but repeat these early opinions ; and I am unable to find any evidence adduced tending to prove their identity. The true relationship of the Silurian strata of South Scotland, and their exact position in the geological system, were long a matter of debate, and claimed the attention of many of the best geologists of Britain. To Mr. Charles Lap- worth, of St. Andrews, is, however, due the honour of having finally succeeded in unravelling the many knotty problems which the rocks of that district pre- sented. A brief resume of the conclusions arrived at by that gentleman, as given in a most exhaustive paper read before the Geological Society of Lon- don (1), may here be given, as I trust to be able to prove that they bear with equal force upon the rocks of the area under consideration. The Silurians of South Scotland are best shown in the neighbourhood of the town of Moffat, in Dumfries. The prevailing rocks consist of a vast series of grey and purple greywackes and slates, with occasional bands of conglome- rates, all dipping somewhat uniformly to the N. N. W. at high angles. Exposed in some of the deeper valleys and stream courses is another set of rocks of a totally different character, consisting of black carbonaceous shales and slates, swarming with Graptolites; associated with these beds are pale green and grey unfossiliferous mudstones. These black shales and their associated mudstones, which have been aptly designated the Moffat Series, occupy lenticular or boat- shaped areas in the mass of the barren greywackes, and form extended lines (1.) Quarterly Journal Geol. Soc,, London. Vol. XXXIV., p. 240. H Ii6 Swanston— Silurian Rocks of Co. Down. more or less parallel, and often miles in length. They are found at intervals throughout the northern half of the uplands, from the North Sea to the Irish Channel, and follow the general direction of the strike of the beds. Their well-marked mineralogical character and their peculiar fauna at once distin- guish them from the monotonous greywackes, and afford the geologist data upon which to work out the interrelation of the rocks of the entire series. Without attempting to follow the author in his description of the many sections and diagrams given in elucidation of his subject, I may briefly state that the rocks are found to be arranged in elongated anticlinals, running in a direction from about N.E. to S.W., and that the sub-parallel bands of black graptolitic shales of the Moffat Series form the axes of these anticlinals, and are only seen where denudation has cut sufficiently deep to expose them. The Moffat Series is thus proved to have been one continuous deposit, inferior in position to the prevailing greywackes through which it rises. Where best exposed the Moffat Series naturally falls into three divisions - an Upper, Middle, and Lower — named respectively the Birkhill, Hartfell, and Glenkiln Shales, from the several localities in which each division attains its greatest development. These three divisions possess distinctive lithological features ; but as the entire group is full of perplexing contortions and inversions, and as the continuity of the beds is greatly broken by numerous faults running in different directions, it was impos- sible to work out their sequence from stratigraphical evidence alone. The aid afforded by the contained fossils is, however, most satisfactory, and has enabled the author not only to prove that the divisions must be assigned to different geological periods, but they are each divisible into several distinct zoological zones. The correlation of these various sub-divisions with the typical Silurian area in Wales, and their foreign equivalents, is gone into with great minuteness by the author. I shall content myself by merely giving the conclusions arrived at, and beg to direct those anxious for further details in this department of the subject to the paper itself. The lowest, or Glenkiln Shales, have been referred to the Upper Llandeilo, their nearest representatives in Wales being beds of that age yielding Grapto- lites, in the neighbourhood of Llandridod, Meadow Town, and Aberiddy Bay. Their American and Swedish equivalents bear out this view, and point to a high position for them in the Upper Llandeilo Series. The Hartfell beds have been proved to be the attenuated representatives of the Bala and Caradoc, and the Birkhill Shales correspond with the Coniston mudstones of the Lake Dis- trict, which are of Lower Llandovery age. The accompanying table will give more clearly these Scottish divisions and sub-divisions, and I shall now proceed to give the evidence that has enabled me to append the columns relat- ing to County Down. Table shewing the Divisions and Sub-Divisions of the Moffat Series , and their equivalents in County Down . S_ f/5 s a ^3 O | s. 12 o .. w 1 & Is o do H rf £ 1 is. (L) i — i ™ 03 O hwu a> XI c n 6 ^ £ o - 03 c3 Oh WOP •ITBUnjIg 3IPPIH rP M rv. £ ’E & O ^ Ph p ’a 0 u 1 15 H o PQ j TJ -dy £ O o3 _r P° cf ^ c5 4-J ^ H-> > rf ■§.& o3 G O oS o s u u UU vd CO CO CO d c« _ ;/) in 0) ^ 15 o5 D o3 ^ p 1-0 c n CO CO £3 1u -S (-1 Wq CJ o T3 rtf o Jh Ctf ■ •ireunpg J3AVO'J[ n8 Swanston— Silurian Rocks of Co. Down. As before stated, the section at Coalpit Bay is the best exposure of these fossil-bearing rocks in the district. The lowest are barren mudstones, which form the axis of a sharp anticlinal, and are followed by black flinty shales con- taining II species of Graptolites. The same species, associated with 15 others, are also found at Ballygrot, where a wider area of rock is exposed, thus indi- cating that the rocks of these widely separated localities are but parts of the same bed. This group of 26 species enables us at once to correlate these beds with those of South Scotland ; and it is interesting to find that they agree al- most fossil for fossil with those from the representative localities of Berrybush Burn and Black Linn, which are the upper beds of the Glenkiln Shales. The small exposure in the railway cutting near Craigavad has also yielded fossils of this age, and is doubtless but a south-westerly extension of the Ballygrot Beds. The same may be said of the black shales still farther to the south-west, in a quarry near Cultra, although I have not been able to procure any recognisable fossils from the greatly crushed rocks of this latter locality. The lower Glenkiln Shales, which in South Scotland are comparatively unfossil iferous, may be represented in Ireland by the grey mudstones which form the centre of the anticlinal at Coalpit Bay, and by the series of unfossilife- rous grey and purple shales associated with the black bands at Ballygrot. The next beds in ascending order at Coalpit Bay are the barren mudstones noted in the detailed account of that locality at paragraph 5. The only fossils found associated with them were obtained from a fragment of black shale folded up in their broken strata. This fragment had doubtless been derived from some bed intimately associated with the mudstones, and which may yet be detected in situ among the shattered black bands at their base. The fossils which it has yielded, though few in variety, include Dicellograptus Forchammeri, Geinitz ; Climacograptus, sp. ? and Diplograptus truncatus , Lapw. species highly characteristic of a thin, but persistent, band of shale occurring near the base of the barren mudstones of the Upper Division of the Hartfell Series (1). This circumstance, coupled with the identity in lithological character of the barren beds in the two countries, leaves no doubt but that these Coalpit Bay Mudstones are the representative of that sub-division. This being admitted, it is evident that the rich beds of the Lower Hartfell Series are absent here, having either thinned out or been lost by faulting. The latter view is more probable, as we find them undoubtedly represented by the fossiliferous black- shales of Carnalea, which have yielded ten species of Graptolites, the following six species being peculiar to that sub-division:— Diplograptus truncatus , Lapw.; Diplograptus qua dr im ucronatus, Hall; Lasioqraptus Harknessi, Nich.; Retiolites Swanston— Silurian Rocks of Co. Down. 119 fibratus , Lapw. ; Climacograptus tubuliferus , Lapw. ; and Dicellograptus For- chammeri , Geinitz. The remaining four species are common to the Hartfell, and the underlying Glenkiln Shales. So far as can be judged from the meagre list of fossils obtained at Orlock Point, the beds there exposed also belong to this group. Again returning to the section in Coalpit Bay, we find the mudstones which have just been referred to the Upper Hartfell Series are separated from the next beds in ascending order, by a dyke which runs almost parallel to the strike, and which seems to occupy the line of an east and west fault. The rocks immediately south of this dyke are very rich in fossils, 36 species having been obtained from them, although the area exposed is of but very limited extent. The palaeontological break between these and the preceding beds is most complete, not one of the extensive series of fossils being common to the two rock groups. Not only are the species different, but a marked change also takes place in the generic character of the fauna. All the old types of compound forms such as Ccenograptus, Thamnograptus, Dicellograptus, Dicranograptus, Leptograptus, &c., have disappeared, and their places have been supplied by the simpler genera Monograptus and Rastrites. This extensive series of fossils admits at once of the correlation of the con- taining beds with the Birkhill Shales of the Moffat District, with the lower division of which as exposed at Dobbs Linn they almost exactly correspond, both in lithological character and fossil contents. In these beds also for the first time in the County Down rocks are we enabled to identify the life-zones so ably worked out in the Scottish beds. The zone of Diplograptus aciim- minatus , which is at the base of Birkhill Shales, is found, in part at least, quite close to the dyke above mentioned. The well-marked zone of Diplograptus vesiculosus follows it with a rich assemblage of species, often beautifully pre- served. The succeeding zone of Monograptus gregarius is also easily recog- nised by the immense profusion in which that fossil, associated with Rastrites peregrinus (type) and other forms abound in it. A series of greenish grey mudstones, with thin layers of white clay, sepa- rates the foregoing zones from the next fossil bands. The upper horizon of this barren group is in Scotland taken as the boundary line between the Lower and Upper Birkhills. The only other zone which can with certainty be recognised at Coalpit Bay, is that of Diplograptus (Cephalograptus) cometa, which occurs at the top of the fossil bearing beds. It is just possible that the zone of Mono- graptus spinigerus—Sedgwicki, which follows the latter in Scotland, may be (1). Quartl. Journal Geol. Soc., London. Vol. XXXIV., p. 316. I20 Swanston— Silurian Rocks of Co. Down. represented and in part combined with it, as several of its most characteristic fossils have been detected in its highest bands The top of the Upper Birkhill Shales, marked by the zone of Rastrites maximus , has not yet been detected in Ireland ; did it occur, its peculiar group of fossils would at once make it recognisable. Judging, however, from the fact that these upper beds thin out as they extend westward from the typical Moffat area, and that the zone of R. maximus seems to be absent from Wigtonshire, it is not likely that it will be detected here. The grits and slates already referred to, which immediately overlie these black shales, are similar in lithological character to those of South Scotland. There they are the principal rock which forms the mountainous region known as the Southern Uplands; in County Down, however, though equally de- veloped, their elevation is inconsiderable. As we pass southwards along the promontary of the Ards, these rocks assume in places a more flaggy and slaty character, and are in the neighbourhood of Greyabbey extensively quar- ried and formed into roofing slates. On some of the surfaces exposed at these quarries traces of organisms have been detected-tracks of annelids are abundant, —but the only forms that admit of identification are Crossopodia Scotica, M‘Coy ; Nemertites tenuis , M'Coy; and Nemertites sp. i Still further south, near Portaferry, bands of dark slate occur containing a group of Graptolites strik- ingly different from any we have yet met with in the district. The paleonto- logical break between these and even the highest of the Coalpit Bay zones .s almost complete. An examination shows that of the 14 species obtained from them, only 3 are common to the two localities, and the n which make their appearance for the first time indicate a much higher horizon for the containing beds than those in the northern portion of the county. These latter beds have no exact paleontological representatives in the typical districts of Scotland 0 Wales ; their nearest is, perhaps, the rocks of Upper Middle Silurian age known as the Gala Group, occurring in the neighbourhood of Galashiels (ij The presence, however, of Monographs Riecartonensis and other Upper Sdunan species, and the absence of many of the Upper Moffat forms which occurm that series in South Scotland, points to a higher place in the Silurian Syste than that to which the Gala Group has been assigned. They are mos p ably the exact equivalents of the Hawick rocks of Scotland, *ch in erven between the Gala beds and the Upper Silurian of Riccarton (2); but as (,). Lapworth, on the Lower Silurian Rocks in the neighbourhood of Galashiels. -Trans. Edinburgh Geol. Soc., Vol. II., p. 46. (2). Lapworth, On Scottish Monograptidae-Geo. Mag., 1876. p. 55°. Swanston— Silurian Rocks of the Co. Down. 121 fossils have yet been detected in these beds in Scotland, the evidence depends solely upon the peculiar fauna of the Irish beds. Their representatives in the Lake Disirict are probably the Knock beds exposed near Ambleside, which are considered to be, if not Upper, at least the passage between the Upper and the Middle Silurians (1). If this view of their position be admitted, it is evident that the grey grits and conglomerates which come in between this fossil band and the black shales at Coalpit Bay naturally fall into the place of the Gala Series. The evidence— in the absence of reliable fossils— which they afford tends to support this view. The conglomerates referred to constitute a well-marked zone, and consist of small pebbles of quarts, flakes of black shale, &c., in a grey gritty base. They are well shewn in the quarries at Ballygowan and elsewhere throughout the county, and are identical in character to beds which mark the base of the Gala Group in Scotland. The remaining rocks of this series consist of alternations of coarse grits and slates, void of any peculiar feature upon which to fix a horizon. It is this monotonous character of strata stretching over such vast areas in both Scotland and Ireland, and dipping in the same general direction, that has hitherto baffled all' attempts to unravel their sequence, or define their exact position in the Silurian System. From the above, however, it is clear that they must be considered as of Gala age, the position of which is defined as the top of the Middle Silurian. It will perhaps be difficult to define the boundary line between this Irish Gala group and the Portaferry beds. The fossils in the latter at Tieve- shilly undoubtedly occupy only a black slaty band, the horizon of which in the series has not yet been fixed. The few organisms on the surfaces of the grey slates near Greyabbey afford very little help, but tend to prove that the rocks in which they occur belong to the Gala rather than to the Portaferry series. It is to be hoped that the boundary line between these two sets of rocks may yet be defined ; but the close resemblance between the unfossiliferous beds of both, and the heavy covering of drift by which they are hidden, will render this a work of extreme difficulty. CONCLUSIONS. The Silurian Rocks of County Down are from the foregoing proved to belong to several distinct divisions of the system — 1st. The lowest, exposed at Coalpit Bay, the shales of Ballygrot, Craiga- (1). Harkness and Nicholson on the Strata and their Fossil Contents, between the Barrow- dale Series of the North of England and the Coniston Flags. — Quartl. Jourl. Geol. Soc., London, Vol. XXXIII., p. 461. ,22 Swanston— Silurian Rocks of Co. Down. vad, &c. , are the representatives of the Glenkiln Shales, the equivalents of the Upper Llandeilo of Wales. 2nd. The black shales at Carnalea, and the barren mudstones at Coalpit Bay, represent respectively the Lower and Upper Hartfell Series, the equiva- lents of the Bala or Caradoc. 3rd The black shales of Coalpit Bay, characterised by the zones of D. acum- minatus, D. vesiculosus, M. gregarius, and D. cometa, represent m part both the Lower and Upper Birkhill shales, which are paralleled with the Lower Llandoveries. 4th The grits and conglomerates which immediately succeed the latter are of the same age as the Gala Series, and occupy a high place in the Middle Silurians. 5th. The black shales and associated flags at Tieveshilly, near Portaferry, oc- cupy either the extreme top of the Middle, or the base of the Upper Silurians, and are the highest Silurians yet recognized in the North-east of Ireland. The geographical relation of the area under consideration to that of South Scotland and the general direction of the strike of the rocks in both districts, would naturally lead to the expectation of a certain degree of similarity between their geological characters ; from the foregoing, however, it is clear that not only generally, but in detail, do they correspond in a remarkable degree. While it would, perhaps, be impossible, owing to the imperfect manner in which the fossil bands are exposed, to unravel the sequence of the various beds in County Down from an examination of them alone, the key afforded by the recent re- searches in the Scottish beds has made the subject a matter of ease. We are thus enabled for the first time, with some amount of certainty, to arrive at conclusions regarding the physical geology of the district. The three grapto- litic shale bands and their associated mudstones have been overlaid by the grits and conglomerates so conspicuous in the county; all were folded into vast waves, the crests of which ran in a direction from about north-east to south- west. ' Subsequent denudation completely altered the contour of the district; and judging from the remnants of Carboniferous strata at Castle Espie and C ultra, it seems to have been covered by rocks of that age, and to have been again upheaved and subjected to denuding agencies, which probably left it in almost its present state. The granitic protrusions of the Moume and Ballynahinc Mountains are supposed to have taken place during the Carboniferous epoch, Swanston— Silurian Rocks of Co. Down. 123 they are certainly subsequent to the deposition of the Silurians, which have been forced up and highly metamorphosed by them. The north-western boundary of the Silurian area has been subjected to the greatest amount of upheaval, and as denudation has reduced all to a somewhat uniform elevation, the lowest beds are here consequently most exposed. The Ballygrot beds form the axis of what was the most north-westerly anticlinal, the black shales of Crawfordsburn, Camalea, and Orlock Point possibly represent waves of minor importance; while that at Coalpit Bay seems to have been one of considerable elevation. Southward of this no exposures of the underlying shales are seen in Down ; on the contrary, they and the overlying grits and conglomerates sink into a trough and are covered by higher beds at Portaferry in which the dark fossiliferous shales of Tieveshilly occur. Still further south, near Ardee, m County Louth, the underlying beds again come to the surface, the black Graptolite shales of the Hartfell series being well represented, in association with arenaceous bands containing other fossils of Bala or Caradoc age. The foregoing exposition of the Silurian rocks of the County Down has been very much facilitated by the aid so kindly afforded by Charles Lapworth, Esq., F.G.S., of St. Andrews, who undertook the revision of the Graptolithina of our rocks ; to his acuteness and critical judgment it is owing that our list of species is so extensive, many of the forms would otherwise have escaped detection. The monograph, with figures of the Graptolites of the County Down, which accompanies this paper is the most complete hitherto published in Britain, and I cheerfully acknowledge the obligations under which Irish geologists are placed for this synopsis of a most difficult group of fossils. Through the kindness of William Bullock, Esq., of Donaghadee, I have had access to the fine collection of Coalpit Bay fossils, made by his father the late William Bullock, Esq. In addition to enriching my collection with a number of good specimens, Mr. Bullock has also placed a valuable series from the above locality in the Belfast Museum. The set has been completed, as far as possible, by a selection from my own collection, embracing forms representing the various beds, and including several type specimens, all of which will be available for future reference. \ I -™ ■ ON THE GRAPTOLITES OF COUNTY DOWN. By CHARLES LAPWORTH, F.G.S. The Graptolites discovered by Mr. Swanston in the black carbonaceous shales among the Silurian rocks of County Down constitute a very distinct assemblage, which is identical with that afforded by the Graptolitic bands forming the well- known Moffat Series of the south of Scotland. In Scotland the containing deposits have already furnished sufficient stratigraphical and palaeontological evidences to allow of the determination of their natural divisions and subdivi- sions, and of their precise systematic position in the general succession of Silu- rian deposits. The black shales of County Down, however, are so excessively convoluted and shattered, that as yet it has not been found possible to fix either their total thickness or the characteristics of their component zones. That the general grouping of the beds among them is essentially similar to, if not iden- tical with that of the Moffat Series, may nevertheless be regarded as certain. Exactly as in South Scotland, certain special forms are invariably found in association, while the proportion of the species, and the lithological features of the containing beds, are absolutely identical with those of the corresponding zones of the Moffat Series. It is possible that in the future, local stratigraphi- cal testimony respecting the inter-relations of the various beds may be detected ; but the sequence of the different fossil groups in the South of Scotland is so clear, that beyond demonstrating their identity with those of the Moffat Rocks, this would add but little to our present knowledge. The Coalpit Bay Division of the County Down Silurians has yielded all the Graptolites of the Birkhill shales, with the exception of one special group, viz., that of the Rastrites maximus zone, which lies at the very summit of the Moffat 126 Lapworth— Graptolites of Co. Down. series. This circumstance is very naturally accounted for. The black shale zones of the Moffat series die out one by one, from above, as we pass outward to the north-west, from the typical Moffat area. From this cause the Rastrites maxi- irius is not present in Wigtonshire, and is consequently missing also from the Black shales of the northern part of County Down, which are actually the south-westerly extension of the Wigtonshire Silurians. Should the black shales be detected in the future in the southern districts of the County Down, the maximus zone will probably be found occupying its natural position immediately below the greywackes. The Hartfell shales are as yet less perfectly represented. The Barren Mudstones of the Upper Hartfell are seen in Coalpit Bay ; and a striking proof of the perfect identity of these beds is afforded by the fact that they exhibit the peculiar fossil-bearing seam occasionally visible in the Moffat area. The asso- ciation of fossils, their state of preservation, and the mineralogical character of the seam, are precisely identical with those of this persistent seam in Scotland. The zone at the summit of the Hartfell shales-viz., the zone of Dicellograptus anceps (Nich.) has not yet been discovered. Neither has any trace been found of the prolific zone of Plemograptus linearis. The typical, or Dicranograptus Clingani zone, is indeed the only portion of the Lower Hartfell whose existence in these deposits has been fully established. The upper, or fossiliferous portion of the Glenkiln shales, is present at Ballygrot (Greypoint), and in the section in Coalpit Bay. All its chief charac- teristic fossils have been already collected from these localities. The fossils of the overlying sheet of Greywackes and flagstones are those of the great Greywacke (Gala or Valentian) group of the South of Scotland. They point to a comparatively high place in this group. The association is such as we might expect in the Hawick Rocks, which lie at the summit of the Middle Silurians of the South of Scotland, but which have not hitherto afforded any determinable species of Graptolithina. The forms common to Ireland and Scotland may be seen on an inspection of the table (p. 124), where the range of the Irish species in the typical Scottish series is given. ' The Irish species of Graptolithina, though generally in a fair state of pre- servation, are usually fragmentary ; and the figuring of even the best specimens of the various forms would give a very inadequate idea of their charactenstic appearance. As they are precisely identical in every respect with the Scotch forms, I have thought it best to figure some of the more perfect examples 0 the forms occurring -in the County Down from my own collection, which has Lapworth — GraptoliTes of Co. Down. 127 been almost wholly derived from the equivalent black shales of the Moffat series. Several of these have already been figured by myself in the “ Cata- logue of the Western Scottish Fossils,” issued under the auspices of the British Association (Glasgow, 1876). To such species or varieties as are yet undescribed a brief diagnosis is here appended. Genus I. Rastrites, Barrande. (Grapt. de Boheme. PI. 4-) According to Herr Richter, the thecae in this genus are mere orifices in the periderm of the common canal, and the long isolated and perpendicular tubes are simply ornamental or defensive extensions of the test. (1.) The British specimens which have hitherto come under my notice have afforded no support whatever to this opinion. Mr. W. Carruthers figures a magnificent example of Monograptus spiralis (Geinitz), (2) of which a well-marked example of Rastrites peregrinus (Barr.) seems to form the initial portion, and to be organically connected with it. I have recently examined the specimens from which the figure was taken, and I am inclined to believe that this appearance is owing to the accidental juxta- position of the two forms. 1. Sp. 1. Rastrites peregrinus. Barr, Plate 5> fig* I* The typical form of this well-known species is abundant in the dark shales of Coalpit Bay, a locality which has yielded the only specimens known to me in which the virgula is apparent as a distinct structure. (3). Locality — Coalpit Bay. 2. Var. hybridus. Lapw. Plate 5, fig. 2. This variety is possibly identical with the fragmentary form Rastrites fugax of Barrande. (Grapt. de Boheme. PI. 4. ) Locality — Coalpit Bay. Genus II. Monograptus, Geinitz. Restricted. (Die Graptolithen, p. 32.) 3. Sp. 1. Monograptus triangulatus . Hark. PI. 5? fig* *4* Locality — Coal- pit Bay and Tullygarvan. (1.) Richter. Aus die Thuringe Gebirge, Zeit. der Deutsch Gesellschaft, 1871. (2.) Carruthers. Geological Magazine, 1868. PL 5, fig. 1. (3.) Geological Magazine, 1876. PI. 10, fig. 1. 128 LapWorth — Graptolites of Co. Donw. 4- Sp. 2. Monograptus spiralis. Geinitz. (Leon & Bronn, Jahrbuch, fur. Min. 1842. PI. 10.) PI. 5, fig. 12. This species is usually identified with Prionotus convolutus of Hisinger, but according to Dr. Linnarsson (1.) the latter was originally founded upon a specimen of Rastrites peregrinus (Barr. ). Locality — Tieveshilly. 5- Var .(a), fimbrialus. Nich. PI. 5, fig 17. Locality— Coalpit Bay. 6. Var. (b). communis. Lapw. PI. 5, fig. 16. The two preceding forms are certainly most intimately allied. The latter has an extended range, and varies much in the forms of the polypary and hy- drothecas, and seems to pass into the following form, M. fimbriatus, on the other hand, is very local in its distribution, and constant in its general features. Locality — Coalpit Bay. 7* Var ( c). proteus (?). Barr. PI. 5, fig. 18. It is doubtful if this form is actually identical with Barrande’s species. His figures remind one rather of M. crispus (Lapw.); and the group typified by M. lobiferus (M ‘Coy). Locality— Coalpit Bay. 8. Sp. 3. Monograptus Sedgwicki. Portl. PI. 5, fig. 15. Locality— Coalpit Bay. 9- Sp. 4. Monograptus turriculatus. Barr. PI. 5, fig. 11. As in South Scotland, the majority of the specimens of this species in the beds of County Down are of very diminutive size. Locality — Tieveshilly. 10. Sp. 5. Monograptus crispus. Lapw. PI. 5, fig. 13. Locality — Tieveshilly. 11. Sp. 6. M onograptus exiguus. Nich. PI. 5, fig 9. Locality— Tieveshilly. 12. Sp. 7. Monograptus Barrandei . Suess. PI. 5, fig. 21. Locality — Tieveshilly. 13. Sp. 8. Monograptus runcinatus . Lapw. PI. 5, fig. 7. Locality — Tieveshilly. (1.) Linnarsson. Afdreg ur Gcologiska Foreningensi Stockholm Forhandlingar, 1877. No 40. Band III. No. 12. Lapworth— Graptolites of Co. Down. 129 14. Sp. 9. Monogrciptus lobiferus. M‘Coy. PI. 5, fig. 6. This species occurs in the black shales of Coalpit Bay in a few o^" the com* mon varieties, in all of which the extremity of each theca seems to form a rounded lobe, the aperture being apparently directed partly inward and partly upward against the lower wall of the central portion of the tube. According to Dr. Linnarsson, who has found specimens of this species in the lobiferus schists of Sweden, preserved in relief, the hydrotheca is actually coiled obliquely, and thus the aperture opens outward in a different plane to that of the proximal portion of the theca, which is wholly free. Locality— Coalpit Bay. In the grey schists of Tieveshilly this species appears to be represented by the following form : — is- Var. pandus. Lapw. Var. nov. PI. 6, fig. 3. Polypary simple, monoprionidian, stout, straight ; from four to six inches in length, and with an average diameter of % of an inch in the fully developed portion, inclusive of the projection of the hydrothecse. These are arranged in the proportion of from 24 to 28 to the inch, and are in contact only. They are broad at their origin, and have the superior margin almost horizontal. They narrow rapidly towards their outer extremity, which is bent downwards in the direction of the proximal extremity of the polypary. This form has been frequently noticed by palaeontologists, but its distinct- ness has not hitherto been acknowledged. Barrande (Grapt. de Boheme. PI. 1, figs. 10 to 14) and Geinitz (Die Graptolithen, Taf. Ill, figs. 24, 25, &c.) both refer it to Monogrciptus priodon. (Bronn). From that species, however, it is easily distinguished by the general form of the theca, and the absence of overlap. From Monogrciptus Clingani (Carr.) it differs in the size and shape of the polypary. Locality — Tieveshilly. 16. Sp. 10. Monogrciptus priodon . Bronn. PI. 5, figs. 24a, and 24b. Locality — Tieveshilly. 17. Sp. 11. Monogiaptus Riccartonensis. Lapw. PI. 5, fig. 23. Locality— Tieveshilly. 18. Sp. 12. Monograptus Galaensis . ‘Lapw. PI, 6, fig. 1. Locality — Tieveshilly. 130 Lapworth— Graptolites of Co. Down. The two preceding species are found in association at Tieveshilly. In Scotland the former appears to be restricted to the Riccarton Beds (Wenlock) ; and the latter occurs only in the Gala Group (Llandovery). 19. Sp. 13. Monograptus MlCoyi. Lapw. Sp. nov. PI. 6, fig. 2. Polypary simple, monoprionidian, straight, several inches in length, and with an average width of one-sixth of an inch. Hydrothecae about 30 to the inch, in contact throughout the whole of their extent, inclined at an angle of 450; of the general form of slender quad- rangular tubes, about five times longer than broad ; apertural margin convex, expanded into an oblique, blunt, triangular denticle. (Loc. Builth Bridge, Radnor.) The foregoing diagnosis has been drawn up from M‘Coy’s figure and description of a form from the Silurian Rocks of Wales (Palaeozoic Rocks and Fossils. PI. 1 B, fig 7, and p. 4) ( 1. ) which he erroneously identified with his Graptolithus lotus, originally founded upon a fragment of a Dichograptidian species, from the Skiddaw Slates of the Lake District (Quart. Journal Geol. Society, vol. 4, p, 223). Locality— A single well-preserved fragment only has been obtained from the Llandovery beds of Tieveshilly. 20. Sp. 14. Monograptus Hisingeri. Carr. (See Geo. Mag., 1868. PI. 12, fig. 1.) (a ). Typical form. Locality — Tieveshilly. 21. ( b ). Var. jaculum. Lapw. PI. 5, fig. 20. Localities— Coalpit Bay and Tullygarvan. 22. Sp. 15. Monograptus cyphus. Lapw. PI. 5> fig- 25- Localities Coalpit Bay and Tullygarvan. 23. Sp. 16. Monograptus leptotheca. Lapw, PI. 5> ^2* 22, Locality Some doubtful fragments only of this species have been collected from the black shales of Coalpit Bay. 24. Sp. 17. Monograptus concinnus. Lapw. PI. 5> ^2* I9* Locality Coalpit Bay. (1.) Compare Rbmer in Leon and Bronn, Jahrbuch £ Min., 1855. p. 541. pLte 8, fig. 2. Lapworth— Graptolites of Co. Down. 131 25. Sp. 18. Monograptus gregarius. Lapw. PI. 5, fig. 4. Locality— The characteristic fossil of the central portion of the Birkhill shales. It occurs in myriads in the black shales of Coalpit Bay. 26. Sp. 19. Monograptus argutus. Lapw. PL 5, fig. 5. The accompanying figure, as well as that illustrative of the original description ot this species, was taken from a cast of a compressed example In specimens preserved with their relief the hydrothecse resemble those in Dicellograptus, having a deep excavation in the distal portion of their outer wall, while the aperture opens obliquely outwards, partly overlapping the lateral wall of the common canal. Locality— Coalpit Bay. 27. Sp. 20. Monograptus Sandersoni. Lapw. PI. c, fig 8 Locality Coalpit Bay and Tullygarvan. 28. Sp. 21. Monograptus tenuis. Portlock. PI. 5, fig. IO Localities— Coalpit Bay and Tullygarvan (?) ’ 29. Sp. 22. Monograptus attenuates. Hopk. PI. 5, fig. 3. Locality- Coalpit Bay. y Genus III. Dimorphograptus, provisional genus. Lapworth. (Geo Ma^ 1876, p. 545*) Examples of this genus are found in great profusion both in Ireland and Scotland, and m all we find the characteristic mono-diprionidian polypary. Nevertheless, in the complete absence of specimens preserved in relief, I have grave doubts of the validity of the genus. We meet with occasional examples in which we have a hint of a second series of hydrothecae in the proximal por- tion. It is just possible that in this group the concavo- convexity of the poly- pary general among the diprionidian Graptolites is carried to excess ; and that the partial invisibility of the second series of hydrothecse is due to their lying almost parallel with those of the first series. 30. Sp. 1. Dimorphograptus Swanstoni. Lapw. PI. 6, fig. 5. A most remarkable and very distinct little species. It occurs in admirable preservation in the Coalpit Bay division of the County Down black shales, but has not hitherto been detected in the corresponding zone of the Moffat Series. Geinitz figures an example of this species from the Kissel-scheifer of Central Germany. (Die Versteinerungen, Taf. 1, fig. 25.) Locality— Coalpit Bay. K 132 Lapworth— Graptolites of Co. Down. 31. Sp. 2. Dimorphograptus elongatus. Lapw. PI. 6, fig. 6. Locality Coalpit Bay. Genus IV. Cephalograptus. Hopkinson. (Journal Quekett Micros. Club, 1869.) 32. Sp. 1. Cephalograptus cometa. Geinitz. PI. 6, fig. 4. Locality —Coal- pit Bay. Genus V. Diplograptus. M‘Coy. (Annals and Mag. Nat. His. ). In addition to the diprionidian form of the polypary, the chief charac- teristic of this genus is generally held to be the fact that the central canal is divided longitudinally, by a vertical septum or diaphragm, into two distinct por- tions which do not communicate with each other— at least in the later stages of the growth of the polypary. In one group, however— viz., the sub-genus Glyptograptus (Lapw.)— none of the examples preserved with their relief which have hitherto come under my notice, give evidence of the presence of this dia- phragm; but, on the other hand, the coenosarcal tube appears to be undivided, and to be in organic connection with both series of hydrothecae, as in Retiolites. 33. Sp. 1. Diplograptus acuminatus. Nich. PI. 6, fig. 7. The characteristic fossil of the lowest zone of the Llandoveries of South Scotland. It is as yet unknown in Ireland. 34. Sp. 2. Diplograptus modestus. Lapw. PI. 6, fig. 8. (Catl. Western Scott. Fossils. Plate 2, fig. 33.) Locality— Coalpit Bay. 35. Sp. 3. Diplograptus sinuatus. Nich. PI. 6, fig. 9. Locality— Coalpit Bay. 36. Sp. 4. Diplograptus tricornis. Carr. PI. 6, fig. 10. Localities— Coalpit Bay, Ballygrot, and Craigavad. 37. Sp. 5. Diplograptus angustifolius. Hall. PI. 6, fig. 11. Localities — Coalpit Bay and Ballygrot. 38. Sp. 6. Diplograptus tamariscus. Nich. PI. 6, fig. 12. Locality— Coal- pit Bay. 39. Sp. 7. Diplograptus dentatus. Brongn. PI. 6, fig. 13* Locality Ballygrot. Lapworth— Graptolites of the Co. Down. 133 40. Sp. 8. Diplograptus Hughesi. Nich. PI. 6, fig. 14. Locality— Coalpit Bay. 41. Sp. 9. Diplograptus insutiformis. Nich. PI. 6, fig. 15. Locality — Ballygrot. 42. Sp. 10. Diplograptus folium. His. PI. 6, fig. 16. Locality — Coalpit Bay. 43. Sp. 11. Diplograptus truncatus. Lapw. PI. 6, fig. 17, Diplograptus pristis, var. truncatus. Lapw. (Catl. Western Scott, Fossils. Plate 1, fig. 28.) Polypary diprionidian, sub-fusiform or with parallel margins, one to three inches in length and one-eighth of an inch in maximum diameter; fur- nished proximally with a minute radicle and lateral spines. Virgula invisible. Hydrothecse inclined at an angle of about 45 degrees, linear-tubular, expanding towards the oblique apertural margin and ornamented with minute transverse strise. There are several varieties of this species in the South Scottish rocks, but they agree generally in the foregoing characteristics. Some smaller and wider examples of this form are almost inseparable from Dip. palmem. Forms pre- served in relief show no trace of a longitudinal septum on one of the lateral faces. I formerly referred this species to Diplograptus pristis of Hisinger, but Swedish specimens of the latter show a polypary and hydrothecse of the general type of Diplograptus quadrimucronatus (Hall). 44. Sp. 12. Diplograptus foliactus. Murch. PL 6, fig. 18. Locality — Ballygrot. 45. Sp 13. Diplograptus vesiculosus . Nich. PI. 6, fig. 19. Locality — Coalpit Bay. 46. Sp. 14. Diplograptus quadrimucronatus. Hall. PL 6, fig. 20. In the Scottish examples referred to this species, four rigid spurs are usually given off, one from each of the angles of the prismoid polypary at a normally uniform height corresponding to the position of the sixth or seventh hydrotheca, counting from the initial extremity. In the Irish forms collected by Mr. Swanston the spurs are sometimes i34 Lapworth — Graptolites of Co. Down. regularly disposed in two opposite series, and sometimes irregularly scattered along tlie extent of the outer margin of the polypary. These forms are all certainly allied to Glossograptus , but our present evidences are insufficient to justify their removal to that genus. Locality — Camalea. 47. Sp. 15. Diplograptus Whitfieldi. Hall. PI. 6, fig. 21. The interesting examples furnished with lateral reproductive appendages, figured by Hall in his Graptolites of the Quebec group, Plate B, and assigned by him to the present species, are clearly distinct. It is most probable that they belong to a form of Lasiograptus (?) resembling Lasiograptus bimucronatus , Nich. Locality — Carnalea. 48. Sp. 16. Diplogr aphis (Lasiograptus 1) mucronatus. Hall. PI. 6, fig. 22. In this series the apertural fibres occasionally anastomose; and examples with lateral reproductive appendages are not infrequent in the Moffat Series in Scotland. In Ireland the species is as yet unknown. 49. Sp. 17. Diplograptus ( Hallograptus) bimucronatus. Nich. PI. 6, fig. 23. It is in this species that the lateral reproductive processes are most frequently met with in British Rocks. Few examples of this form occur which appear wholly destitute of them, or of the lateral fibres which support them. Mr. W. Carruthers has suggested that this form, and the very similar Diplograptus mucronatus should be erected into a new genus under the title of Hallograptus , in honour of the eminent palaeontologist, who was the first to figure these forms and to suggest the possible function of their remarkable appendages. Genus VI. Glossograptus. Emmons. 50. Sp. 1. Glossograptus Hincksii. Hopk. PI. 6, fig. 24. The lateral appendages in this species and genus differ from those in Hallograptus , in being rigid blind spurs comparable with those at the proximal extremity of Climacograptus bicornis (Flail). In all the supposed species of this genus, the apertural spines are also remarkably stout and rigid, but they never anastomose as in the older and very closely allied genus Retiograptus of Hall. (Grapt. Quebec Group, Plate 16, figs. 6 to 8). Glossograptus ciliatus , Emmons (American Geol.^vol. 1, plate 1, fig 25); Glossograptus setaceus , Ibid. Fig. Lapworth— Graptolites of Co. Down. 135 20; Diplograptus ciliatus , Ibid. Fig. 19; Diplograptus spinulosus, Hall. Diplograptus fimbriatus , Hopk. (Geol. Mag., 1872. PI. 12, fig. 8.) Diplograptus pinguis, Ibid. Fig. 7 ; all belong to this genus and will pro- bably prove to have been founded on either one or two distinct species : the aspect of the polypary varying to an extraordinary degree according to the direction in which the compression has been effected. Localities- -Coalpit Bay and Ballygrot. Genus VII. Lasiograptus. Lapworth S1* Sp. 1. Lasiograptus Harknessi. Nich. PI. 6, fig. 26. An examination of Nicholson’s type specimen of his Diplograptus Hark- nessi has convinced me that it is identical with my Lasiograptus costatus , which must consequently be suppressed. This species has a great range in the Moffat Series, passing upwards from its very lowest beds into the middle of the Hart- fell Shales. Occasionally a specimen is detected in which the ventral spines are rudimentary and do not anastomose. Locality — Carnalea. 52. Sp. 2. Lasiograptus margaritatus Lapw, PI. 6, fig. 25. Polypary diprionidian, about one inch in length and about one-eighth of an inch in diameter, inclusive of the marginal net-work. Virgula ca- pillary, just visible beyond the distal margin Hydrothecse 25 to 30 to the inch, free, triangular in form, with long-pointed denticles which are developed horizontally outwards as distinct filaments to a distance equal to the width of the central portion of the polypary, where they are split up into several subordinate threads. These are united to those similarly derived from the hydrothecse immediately above and below, and thus originate a continuous series of marginal meshes completely surrounding the polypary. I11 this species the hydrothecse are of the type of those of Diplograptus mucronatus (Hall), and the general aspect of the polypary is essentially similar to that of Diplograptus limucronatus (Nich.). In Lasiograptus Harknessi the thecae resemple those of Climacograptus. Locality— Unknown in Ireland. Genus VIII. Clathrograptus. Lapworth. 53- Sp. 1. Clathrograptus cuneiformis. Lapw. PI. 6, fig. 27. The figure shows merely the skeleton framework of the polypary. In well 36 Lapworth— Graptolites of Co. Down. preserved specimens this skeleton is covered and partially hidden from sight by a thin continuous membrane showing cell-apertures. Locality— Ballygrot. The genus Reiiograptus of Hall included three distinct genera. The title of Reiiograptus is best restricted to the forms to which it was first applied, viz., those of the type Reiiograptus tentaculatus , which combines the generic charac- ters of Glossograptus and Lasiograptus. Clathrograptus embraces the simple diprionidian forms of the type of Reiiograptus Geinitzianus (Hall, non Bar- rande). A third genus remains, which is typified by the extraordinary com- pound species Reiiograptus nucharis , from Lake St. John. Genus IX. Retiolites. Barrande. 54. Sp 1. Retiolites jibratus. Lapw. PI. 6, fig. 28. Polypary simple, diprionidian, one or two inches in length and one-fourth of an inch in breadth; margins parallel, proximal end broadly rounded and destitute of ornament. Virgula stout, straight, distally prolonged, Hydrothecae 24 to 28 to the inch, their position being indicated by broad regularly quadrangular meshes. Epiderm continuous, supported on a skeleton framework of interlacing threads. This form, which is remarkably abundant in the higher zones of the Lower Hartfell of South Scotland, is intimately allied to the forms here united under Retiolites perlatus (Nich. ), but differs from them mainly in the form of the thecal meshes, and in the frequent presence of lateral appendages. Locality— Carnalea. 55. Sp. 2. Retiolites perlatus ? Nich. (Geo. Journal, vol. xxiv.. p. 530.) The original example of this species is too imperfectly preserved to enable us to recognize any specific character beyond the great breadth of the polypary and the extraordinary width of the dermal meshes. In this respect it agrees with certain views of the two following forms which occur in the South of Scotland, but neither of which it is as yet possible to identify with the R. perlatus of the Coniston Mudstones. 56. Var. Daironi. Var. nov. Lapw. PI. 6, fig. 30. Occasionally three or four inches in length. In the characteristic view it resembles a gigantic specimen of Dip. palmeus (Barr.), with a ret.- form covering. In addition to this network this form must have possessed a continuous superficial membrane of sufficient thickness to Lapworth- Graptolites of Co. Down. 137 leave indubitable traces of its presence upon the matrix. Locality — Coalpit Bay. 57. Var. obesus. Lapw. (Rept. Brit. Assoc. 1871.) PI. 6, fig. 29. The special features of this form are the great size and the elegant and cha- racteristic shape of the thecal meshes. The thecse themelves appear almost horizontal. Locality — Unknown in Ireland ; common in the Gala Group of South Scotland, and in the highest seams of the Birkhill shales. Genus X. Climacograptus. Hall. (Grapt. Quebec Group, p, hi.) According to Professor Hall, the polypary in this genus has no central septum, and the hydrothecae are simple openings in the outer test of a single internal coenosarcal canal. By Professor Nicholson, on the other hand, the polypary is believed to be formed, actually or theoretically, of two monoprio- nidian polyparies placed back to back ; their dorsal walls being flattened into a bilaminate median septum, and their virgulse coalescing into a double central virgula. I have verified the accuracy of the latter theory in the species Climacograptus scalaris (His.), in several of its varieties, and in C. Wilsoni. (Lapw.) ; but if the analogy furnished by the structure of Diplograptus as described above, is to guide us, it is not impossible that both these interpreta- tions are correct, each for itself, and that within the limits of Climacograptus , as at present received, are included some forms in which the median septum is con- tinuous from side to side, and others in which the hydrothecas of both series open into one and the same central coenosarcal canal. 58. Sp. 1. Climacograptus scalaris. His. (Non Linnaeus.) (Lethea Suecica, Plate xxxviii.) The form figured by Linnaeus as Graptoliihus scalaris, (1) was a Monograptus allied to M. colonus of Barrande, from the Upper Silurian strata in which the genus Climacograptus is unknown. Examples in my possession procured from the same locality whence Linnaeus obtained his species show the peculiar scala- riform appearance figured by him, with great distinctness. They are also asso- ciated with unrolled examples of a spiralis like Cyrtograptus , as in his original drawing. Linnaeus’ name, scalaris , should be employed for the Monographs, to which he originally applied it; but in the meantime it is perhaps inadvisable to disturb Hisinger’s title for the Swedish Climacograptus. The following forms, 1 Skanska Resa., p. 147. Lapworth— Graptolites of Co. Down. 138 which are usually referred by palaeontologists to this species, all agree in the possession of a tapering polypary, destitute of proximal ornamentation; perpen- dicular, short, square, hydrothecae; and straight, or very gently undulating suture. ^ Var. a. tectus . Barrande. (Grapt. de Boheme. *P| 1, figs. 19 and 20.) Virgula never distally prolonged. Locality— Rare in the Gala Group of South Scotland, unknown as yet in County Down, go. Var. b. normalis. Lapw. PI. 6, fig* 31 • Polypary with sub-parallel margins. Virgula greatly prolonged distally. Locality— Abundant in Coalpit Bay. Var. c. Climacograptus rectangularis. M‘Coy. PI. 6, fig. 32. Virgula prolonged, proximally only, to a considerable length. Polypary tapering. Locality— Unknown in Ireland. Rare in the Birkhill Shales of Moffat. g2< Var. d. Climacograptus caudatus. Lapw. PI. 6, fig. 34. Polypary tapering, several inches in length, with stout virgula prolonged both proximally and distally to a length equal to that of the polypary itself. Locality — Unknown in Ireland. Var. e. Climacograptus tubuliferus. Lapw. PI. 6, fig. 33. Polypary with parallel margins, virgula distally prolonged and expanded into a long flattened plate or vesicle. Locality— Camalea. In Scotland each of the foregoing forms has a definite range in the succession of Silurian deposits. They are all most certainly very intimately allied, but it is possible that we may eventually be forced to look upon them as distinct species. Such of these forms as are known upon the Continent have a corresponding vertical range, and appear to possess similar external features. 64. Sp. 2. Climacograptus Scharenbergi. Lapw. PI. 6, fig. 36. (Catl. West. Scott. Fossils. Plate 2, fig. 36). Polypary diprionidian, about an inch in length and one-twelfth of an inch in average diameter; proximal end ornamented with a short radicle Lapworth — Graptolites of Co. Down. 139 only. Suture deep, zigzag, having each angle prolonged in a short horizontal groove. Virgula distally prolonged. Hydrothecae 28 to 36 in the space of an inch, short, perpendicular, with the distal ex- tremity of each very slightly introverted. The chief characteristic of this species is afforded by its remarkable sutural groove. This is distinctly angulated, running in zig-zag straight lines from side to side. From the outer point of each angulation a short horizontal groove continuous with that of the suture traverses the covering of the coenosarcal tube almost to its outer edge. This form has been frequently figured by palaeontologists, even under its most typical aspect, but always in association with closely allied forms. (1) Its characters are so unique that there can be no hesitation in regarding it as a distinct species. The various forms here referred to C. Scalaris. His. universally abound in Bala and Lower Llandovery rocks. They are unknown apparently in rocks of Llandeilo and Lower Bala age, where their place is taken by the present species, which occurs in Wales, Scotland, and Scandinavia in these ancient formations. The two forms doubtfully overlap for a short period in the Clingaili zone of the Hartfell shales of the Moffat area. Localities-Scot- land— in the Glenkiln and lowest Hartfell beds everywhere. Ireland— Bally- grot, Craigavad, and Coalpit Bay. 65. Sp. 3. Climacograptus bicornis. Hall. Type form. PI. 6, fig. 38a. Locality — Ballygrot. 66. Var. (b.) tridentatus. Lapw. PI. 6, fig. 38c. 67. Var. (c.) peltifer . Lapw. PI. 6, fig. 38b. 68. Sp. 4. Climacograptus ccelatus . Lapw. PI. 6, fig. 39. The figure which illustrates the original description of this species (Quart Journ. Geol. Soc., 1875, PI. 35, fig. 8) is a very bad one. The original diagnosis should be compared with the figure on plate of the present memoir. In the Welsh specimens the hydrothecae are more deeply divided and the” (1) Compare, for example, Boch, Bernerk aug., Graptolitherne, Taf. 1, figs 3 ro „ l8 Scharenburg, Ueber Graptolithen, Taf. 2, figs. 24, 25, &c , &c. Salter Q. J. G. S vol viii ’ pl- 7. fig. 3. Torquist. ‘ '* L 140 Lapworth— Graptolites of Co. Down. interspaces are more oblique than in the Scottish forms. Locality— Coalpit Bay and Ballygrot. 69. Sp. 5. Climacograptus Wtlsoni. Lapw. PI. 6, fig. 40. (Catl. Western Scottish Fossils, 1876. PI. 2, fig. 46.) Polypary two to four inches in length and one eighth of an inch in maximum diameter; proximal end abrupt, furnished with two short horizontal radicular processes. Septum direct. Virgula stout, distally prolonged for a distance nearly equal to the length of the polypary ; and supporting proximally a large elliptical vesicle. Hydrothecae 16 to 20 to the inch ; short, square, perpendicular ; excavation shallow, horizontal. Closely allied to the foregoing and following species— Locality— Unknown in Ireland. 70. Sp. 6. Climacograptus per-excavatus. Lapw. PI. 6, fig. 35. Polypary one and a half inches in length, and about one eighth of an inch in breadth ; margins parallel till close upon the proximal extremity which is broadly rounded off, and ornamented with three short, stiff, proximal spines. Virgula distally prolonged. Hydrothecse 28 to 36 to the inch, with inclined partition walls; excavations wide and deep, occupying more than half the ventral margin of the polypary, and from one-fourth to one third of its trans- verse diameter. Horizon— Glenkiln shales. Localities in Scotland— Craig- michan, Glenkiln, Leadhills. In Ireland— at Ballygrot and Coalpit Bay. A most prolific species, it occurs in great abundance at the localities cited. 71. Sp. 7. Climacograptus innotatus. Nich. PI. 6, fig. 37. Locality— Coalpit Bay. Genus XI. Dicranograptus. Hall. (Grapt. Quebec Group, p. 1 1 2. ) 72. Sp. 1. Dicranograptus ramosus. PI. 7> fig- *• The earlier or Llandeilo examples of this and the following species are re- markably spinose. As we ascend in the series of beds the spines seem to become shorter and less conspicuous. In the highest beds where these species are known they are destitute of spines. Localities— Crawfordsburn, Ballygrot, and Craigavad. Lapworth— GraptoLites of Co. Down. 141 73. Sp. 2. Dicranograptus Nicholsoni. Hopk. PI. 7, fig. 2. Locality — Ballygrot. 74. Sp, 3. Dicranograptus formosus. Hopk. PI. 6, fig. 41. Localities— Coalpit Bay and Craigavad. 75. Sp. 4. Dicranograptus Clingani. Carr. PI. 6, fig. 43. Locality— Not yet detected in Ireland. 76. Sp. 5. Dicranograptus ziczac , Lapw. PI. 6, fig. 420. (Catl. Western Scottish Fossils. Plate 3, fig. 77.) Stem one-eighth of an inch in length, pointed ; branches diverging at an angle of about 120 degrees, about an inch in length, bent into an elegant double curve, and forming a polypary of a vase-like form. Hydrothecse 28 to 30 to the inch, seen in profile on the stem ; invisible upon the branches. Allied to Di- cranograptus furcatus of Hall. (Pal. New York, Yol. L Plate 74, fig. 4. ) Locality — Unknown in Ireland. 77. Var. minimus. Lapw. PI. 6, fig. 42^. Branches half an inch in length, forming a single gentle curve. Locality — Coalpit Bay, Genus XII. Dicellograptus. Hopkinson. (Geol. Mag. 1871. PI. 1, p. 20.) 78. Sp. 1. Dicellograptus elegans. Carr. PI. 7, fig. 8. Localities — Carna- Iea, Craigavad, and Coalpit Bay. 79* Sp. 2; Dicellograptus Forchammeri. Geinitzj PI. 7, fig. 7. Localities — Carnalea, Ballygrot, and Coalpit Bay. 80. Sp. 3. Dicellograptus Moffatensis . Carr. PI. 7, fig. 9. ’Locality — Ballygrot. 81. Var. (a) divaricatus. Hall. PI. 7, fig. 10. Locality — Ballygrot. 82. Sp. 4. Dicellograptus caduceus . Lapw. PI. 7, fig. 3. (Catl. Western Scottish Fossils. PI. 4, fig. 83.) Polypary consisting of two simple monoprionidian branches, which diverge 142 Lapworth— Graptolites of Co. Down. at a small angle, and are so curved that they cross and recross each other distally in the figure of 8. Axillary spine prominent, lateral spines undeveloped. Hydrothecae 24 to 28 to the inch, of the form of those of Dicellograptus elegans , Carr. Sp. Locality — Ballygrot. Genus XIII. Didymograptus. M‘Coy; (Pal. Foss., p. 9.) 83. Sp. 1. Didymograptus super stes. Lapw. PI. 7> figs* *5 a'^- (Catl. Western Scottish Fossils. PI. 3, fig. 74*) Polypary consisting of two simple monoprionidian branches, of great length, attaining a maximum diameter of one-tenth of an inch, within the first three inches of their extent ; broadly curved and including a ventral angle of about 120 degrees. Hydrothecae 24 to the inch, inclined at an angle of 40 degrees, rapidly expanding in the direction of the aper- tural margin, which is deeply concave, and forms a broad triangular denticle. Perfect specimens of this well-marked species are rarely detected ; but the broad and slightly curved branches are numerous both in Scotland and Ireland in the typical Glenkiln Shales. This is in all probability the same species as that figured by Hall as Graptolethus Sagittarius . (Pal. New York. Vol. I., Plate 74, fig. 1.) It is also associated here, as in North America, with a slender species which appears to be the same as Didymograptus serratulus (Hall). Localities— Ballygrot and Craigavad. Genus XIV. Leptograptus'. Lapworth. (Geol. Mag. 1873, p. 558.) 84. Sp. 1. Leptograptus fiaccidus. Hall. PI. 7> fig* I4* Localities — Car- nalea, Orlock Point, and Ballygrot. Genus XV. Ccenograptus. Hall. (Modified.) (Hall, Annual Report, 1867, p. 179.) So far as at present known this genus differs from Pleurograptus (Nich.), in the possession of an initial cross-bar, formed by the persistent sicula. 85. Sp. I. Ccenograptus gi'acilis. Hall. PI. 7> fig- II# Localities Bally- grot and Craigavad. None of the Scottish examples of this species give evidence of having been Lapworth — Graptolites of Co. Down. 143 composed of four branches, as indicated in the American specimen figured by Hall. (Grapt. Quebec Group, p. 14.) 86. Sp. 2. Ccenograptus surcularis. Hall. PI. 7, fig. 12. Locality — Bally- grot. 87. Sp. 3. Ccenograptus pertenuis. Lapw. PI. 7, fig. 13. (Catl. Western Scottish Fossils, 1876. PI. 3, figs. 66, 67.) Polypary consisting of two simple or compound monoprionidian flexuous and extremely slender branches, proceeding in opposite directions from the central portion of a well-marked sicula. Hydrothecae 16 to the inch, of the type of those of Ccenograptus gracilis , The forms C. explanatus , and C. nitidulus figured by myself in the Catl. Western Scott. Fossils may be distinct species, or merely varieties of the pre- sent form. It will consequently be better to defer their description till this point has been satisfactorily determined. Locality — Ballygrot. Genus XVI. Thamnograptus. Hall. 88. Sp. 1. Thamnograptus typus ? Hall. PI. 7, fig. 16. This form has only been procured in small fragments in the dark shales of County Down. It occurs locally in great profusion in the Glenkiln Beds of the South of Scotland. Some comparatively perfect and well preserved examples from these beds lately added to my collection, make it clear that different portions of the polypary are so distinct in their characters, that they have been considered as belonging to distinct species. Rastrites Barrandei of Hall is a true Thamnograptus , and ought probably to be referred to the present form. Localities — Ballygrot and Craigavad. Genus XVII. Dictyonema. Hall. (Palaeontology of New York, Vol. ii., p. 174.) 89. Sp. 1. Dictyonema Moffatensi^. Lapw. PI. 7, fig. 17. Polypary about an inch in length and one-third of an inch in maximum diameter, cupshaped, of an elongate semi-elliptical form; composed of slender, radiating, free, comparatively straight branches, with slightly crenulated margins ; transverse dissepiments distant, scarcely visible ; 144 LaFworth — Cjrai’tolites of Co. Down. Proximal portion of polypary prolonged into, and partially enveloped in a chitonous disc or plate. All the specimens of this species known to me are in a very indifferent state of preservation, and the foregoing characters are all that can be made out with certainty. Locality — Carnalea. \ i- EXPLANATION OF PLATE V. Fig. I . Rcistrites peregrinus , Barr. „ 2. 99 ,, var. hybridus , Lapw. >> 3* Monographs attenuatus , Hopk. „ 4 a. 99 gregarius , Lapw. 4 b, portion enlarged. ,» Sa- 99 argutus, Lapw. 5 b, portion enlarged. tt 6a‘ 99 lobiferfaus , M‘Coy. 6b, portion enlarged. „ 7 a. 99 runcinatus , Lapw. 7 b, portion enlarged. „ 8a. 99 Sanders oni, Lapw. 8b, portion enlarged ; 8c, proximal extremity. „ 9 a. 9 9 exiguus, Nich. 9 b, portion enlarged. ,, io a. tennis, Portl. (proximal extremity). 10c, distal ex- tremity ; 10 b, portion enlarged. „ n. 99 tm riculatus, Barr. , 12. 99 spiralis, Geinitz. » 13- 99 crispus, Lapw. , 14. 99 triangulatus, Harkn. » I5* 99 Sedgwickii, Portl. „ 16. 99 communis, Lapw. » 17. 99 fimbriatus, Nich. » 18. 99 proteus, Barr. » 19. 99 concinnus , Lapw. „ 20. 9 9 Hisingeri, Carr. Var .jaculum, Lapw. „ 21. 99 Barrandei, Suess. „ 22. 99 leptotheca , Lapw. 10 b, portion enlarged. » 23- 99 Riccartonensis , Lapw. ,, 24a. 9 9 priodon. Brown. 2\b, portion enlarged. » 25. 9 9 cyphus, Lapw. EXPLANATION OF PLATE VI. 1. 2. 3a. 4- 5- 6. 7- 8. 9- io. na. 12. 13- 14. 15. 16. 170. 18. 19. 20. 21. 22. 23- 24 a. 25- 26. 27. 28. 29. 3°* Monograplus Galaensis, Lapw. „ M‘Coyi, Lapw. lobiferfus ? M‘Coy. Var. pandus (proximal extremity) 3 b, distal extremity ; 30, the same enlarged. Ceph alog rap tics cometa , Geinitz. Dimorphogrciptus Swans toni , Lapw. „ elongatus, Lapw. Diplograptus acuminatus , Nich. ,, confertus , Nich. „ sinuatus, Nich. „ tricornis, Garr. „ angustifolius, Hall. il£, portion enlarged. „ tamariscus , Nich. }J dentatus , Brogn. ,, Hughesii , Nich. ,, insectiformis , Nich. „ folium , His. „ truncatus, Lapw. 1 7^ portion enlarged. ,, foliaceus , Murch. ,, vesiculosus, Nich. ,, quadtimucronatus , Hall. „ Whitfieldi , Hall. „ mucronatus , Hall. „ bimucronatus, Nich. Glossograptus Hincksi, Hopk. (Ventral aspect); 24^ lateral aspect. Lasiograptus tnargaritalus, Lapw. x. 2. ,, Harknessi , Nich. x. 2. Clathrograptus cuneiformis , Lapw. x. 2. Retiolites fibratus , Lapw. x. 2. „ perlatus ? Nich. Var, obesus, Lapw. x. 2. u Var. Daironi, Lapw. x. 2. 77oc TTeTfasT^aiTjeZdOub 7876- 77 CtypaiducJ J7 17. Ci AHywrM. p£l SWANSTON & LAPWORTH - GRAPTOL1TES OF CO.DOWN 4 savs stt/xsr 147 Fig. 31. Climacograptus sc alar is, His. >> 99 ,, Var. normality Lapw. „ 32. 99 ,, Var. rectangular is, M ‘Coy. >j 33* 99 ,, Var, tubuliferus , Lapw. „ 34- 99 ,, Var. caudatus, Lapw. „ 35«- Climacograptus per-excavatus, Lapw. 35 b, portion enlarged. „ 36a. )« Scharenbergi, Lapw. 3 6b, portion enlarged. » 37 99 innotatus , Nich. „ 38a. 99 bicornis , Hall (typical form). ,, 38^. 99 „ Var. peltifcr. „ 3&. 99 „ Var. tridentatus. V 39. 99 ccelatus , Lapw, „ 40. 99 IVilsoni, Lapw. „ 41. Dicranogt aptus formesus , Hopk. „ 42 a. »> ziczac, Lapw. (typical form). „ 42& >> ,, Var. minimus , Lapw. » 43- » Clmgani, Carr. ivr (Sf.tf >S} EXPLANATION OF PLATE VII. Fig 1. 2. 3- 4- 5- 6. 7- 8. 9- 10. 11. 12. Dicranograptus ramosus , Hall (stem only, older variety). }} Nicholsoni , Hopk. Dicellograptus caduceus , Lapw. „ sextans , Hall. „ anceps, Nich. / t „ Morissi, Hopk. l „ Forchammeri, Geinitz. „ elegans , Carr. }, Moffatensis , Carr. var. divaricatus. Hall. Ccenograptus gracilis , Hall. surcularis , Hall. >> 13 .^pet tenuis, Lapw. „ 14- Leptograptus fiaccidus , Hall. }, 15a. Didymograptus super stes^ Hall. ,, 16. Thamnog raptus typus (?), Hall. ,, 17. Dictyonema Moffatensis , Lapw. , 18. Corynoides calyculans , Nich. 19. „ curtus , Lapw. „ 202. Acrothele sp., A . granulata, Linars. ur. Geol., Stockholm, 1877). „ 21a. Acrotreta Nicholsoni, Dav., Coalpit Bay. 2lc b, from original figure of species (Geo. Mag., 1868, PI. XVI). Discina Portlockii, Geinitz. Various examples. V Dauosonia campanulata , Nich. Various examples. — 153, portion of distal extremity. e( 73 20$ ’ Orb. communis, D' Orb v r r guttifera, D'Orb. ... r obliqua, D' Orb v r vr r Vaginulina, D Orb. legumen, Linn , r v r Marginulina, D' Orb. lituus, D’ Orb r Cristellaria, Lamk. rotulata, Lamk. v r v r v r vr crepidula, F. &> M. v r v r ’ v r Polymorphina, D' Orb. lactea, W. &> J. r r r v r vr r c r gibba, U Orb. c v c r c c r oblonga, Will. r v r v r v r r compressa, D'Orb. v r r r r r r concava, Will. r myristiformis, Will. r v r Uvigerina, D' Orb. angulosa, Will. v r c v r r v r r Orbulina, D'Orb. universa, D' Orb r ... ... r 160 Wright— Foraminifera of North-East of Ireland. TABLE— (Continued). LIST OF SPECIES. Globigerina, jD’ Orb. bulloides, Z>’ Orb. ... inflata, L? Orb Spirillina, Ehrenb. vivipera, Ehrenb. ... Patellina, Will. corrugata, Will Discorbina, P. 6° J. rosacea, D1 Orb globularis, D' Orb. Parisiensis, Orb. Bertheloti, D’ Orb. Planorbulina, D' Orb. Mediterranensis, D' Orb. .. Truncatulina, D'Orb. lobatula, Walker refulgens, Montfort Tinoporus, Montfort. laevis, P. 6° J. lucidus, Brady MS. PULVINULINA, P. 6° J. auricula, F. 6° M. Rotalia, Lamk. Beccarii, Linn nitida, Will. Nonionina, D' Orb. umbilicatula, Montagu depressula, W. &* J. turgida, Will. scapha, F. 6° M. ... Polystomella, Lamk. crispa, Linn. striato-punctata, F. &• M. Raised Beaches. Estuarine Clays. PQ g % § § § J a» I 2 3 4 5 6 7 8 ’ / VC V C ... r v c vr V c ... ... C ... ... r v r ... c r v r v r c r r r ... ... r ... ... r c r v r r c vr c r ... r ... ... v r r r r c r r v c v c r r c c r ... v r v r v r ... ... v r ... •• ... ... v r vr r vr ... r ... ... v r ... c r r v c v c c v c v c VC ... r r •• r r r c v r v r ... c c V c V c c V c V c vc c r r r v r c r v r v r v r vr r r v c c c r v c v c VC c c r V c r r v c c V c Blackstaff Bridge, Strang- ford Lough. Limavady Station, Lough Foyle. Wright— Foraminifera of North-East of Ireland. 161 TABLE SHOWING THE DISTRIBUTION OF THE FORAMINIFERA IN THE BOULDER CLAY DEPOSITS OF THE NORTH EAST OF IRELAND. 4-J c n jA Vh 1j w ■a ! o 1 Falls Park, Belfast. 1 Castle-Espie, Co. Down. | Cherry Valley, Co. Down. Ballyholme Bay, Co. Down. Knock Glen, Co. Down. Woodburn Glen, Carrickfergus. 1 Black Head, Co. Antrim. Gobbins, Islandmagee. Ballyrudder, Co. Antrim. Ballyrudder, Co. Antrim (gravel). I Bovevagh Church, Co. Derry. r 2 3 4 5 6 7 8 9 IO II 12 r r r r VC c vr r r vr ... r c c ... r c vr r r r ... c •• r VC VC ... vr c vr vf vr r ... r r r vr r l r c vr r r ... r r c vr r ... r ... r vr ... j vr r ... vr vr vr v r r vr 1 vr LIST OF SPECIES. Cornuspira, Scultze. involvens, Reuss ... Biloculina, D' Orb. ringens , Lamk. depressa, D' Orb. ... elongata, D' Orb. ... Miliolina, Will. tricarinata, D'Orb.... oblonga, Montagu . . . Brongniartii, D' Orb. seminulum, Linn. ... subrotunda, Montagu Spiroloculina, D’ Orb. limbata, D’ Orb. Haplophragmium, Reuss. canarierisis, D' Orb. Textularia, Defrance. sagittula, Defrance variabilis, Will. diffdrmis, Will. Bulimina, D’ Orb. pupoides, D1 Orb. ... marginata, D’ Orb. ... ovata, D Orb. elegantissima, D' Orb. Virgulina, D' Orb. Schreibersii, Czjzek Bolivina, D’ Orb. punctata, D'Orb. ... plicata, DyOrb. 1 62 Wright— Foraminifera of North-East of Ireland, TABLE— (Continued). LIST OF SPECIES. A in §> 13 § S3 tP i 'u ri <1 W> 1 Q 6 o Q 6 O S3 £ o Q •3 •rj ri U S’ 1 J ri I 4 O 6 S3" o o d jf ri M Q cf 3 U tS ri r^H C/5 U vT O s-T 13 > 0) s > "ri M 2 >> 13 PS Cassidulina, U Orb. laevigata, D’Orb. ... crassa, D'Orb. Lagena, W. and J. sulcata, W. and J. costata, Will. ••• Williamsoni, Alcock laevis, Montagu gracillima, Seguenza globosa, Montagu ... striata, D’Orb. gracilis, Will. ••• semistriata, Will. ... caudata, D’ Orb. . . . marginata, W. and J. var. trigono-marginat; lucida, Will. \an melo, D’ Orb. squamosa, Montagu hexagona, Will. Nodosa ri a, Lamk. scalar's, Batch. Vaginulina, D’Orb. legumen, Linn. Cristellaria, Lamk. crepidula, F. and M. Polymorphina, D’ Orb. lactea, W. and J. ... fusiformis, Rcemer gibba, D’Orb. compressa, D’Orb. Uvigerina, D’ Orb. angulosa, Will. Orbulina, D’Orb. universa, L? Orb. . . . 1 i f 2 ' 3 4 5 6 7 8 9 IO ii 12 .. vr ... vr • • VC r ... ... VC vr vr ... r r r r r ... r 1 vr vr r vr ... c r r r VC r r r c c r vr vr vr r c vr r r ... ... i vr vr r ... r r vr r vr c vr ... ... ... r vr r vr r r r vr r r c c C c ... c c r fe ... vr ... ... ?•] r r vr c c c c r r r r r vr vr c r ... ... ... r vr ... ... ... c c ... vr vr vr c r VC c r vr r^ r ... vr ... c c vr r r r r ... r r ... ... ... ... r ... Wright— Foraminifera of North-East of Ireland. 163 TABLE— (Continued). LIST OF SPECIES. Globigerina, D' Orb. bulloides, D'Orb. ... Patellina, Will. corrugata, Will. Discorbina, P. and J. rosacea, D' Orb. globularis, D' Orb. Planorbulina, D' Orb. Mediterranensis, D ’ Orb. Truncatulina, D'Orb. lobatula, Walker ... Rotalia, Lamk. Beccarii, Linn. nitida, Will. Nonionina, D’ Orb. depressula, W. and J. scapha, F. and M. Polvstomella, Lamk. crispa, Linn. striato-punctata, F. and M. arctica, P. and J. O 7 I 8 r vr i r • r r ... r vc Ballyrudder, Co. Antrim (gravel). Bovevagh Church, Co. Derry. ■ ' ■ I .. ... ... * ■ ''I ' •Xri . ■ - [Proceedings Belfast Naturalists' Field Club — Appendix , 1879-80.] THE MOLLDSCA OF THE BOULDER CLAY OF THE HORTH EAST OF IRELAND. By S. A. STEWART, Fellow of the Botanical Society of Edinburgh. ♦ Amongst the British deposits of the Glacial Period the Boulder Clay is undoubtedly the most important. Though of small magnitude, as compared with beds of greater antiquity, yet it exhibits such remarkable characters as render it unique, and in the entire sedimentary series there are no rocks which can be classed as altogether similar. Attempts have been made to prove a succession of Glacial Epochs in not only Secondary, but also Palaeozoic times ; but if Glacial conditions ever prevailed during those eras, only comparatively faint and questionable evidences remain to us, and the epoch to which the Boulder Clay belongs must still be regarded as the Glacial Epoch. The structure and physical characters of the Boulder Clay, as it occurs in this district, are so distinct that it may be recognised without difficulty, and it has been accurately described by successive writers from the time of Portlock down to the present. It is a stiff, compact, unstratified clay, usually reddish brown, but sometimes blue, very tenacious when moist, and containing numerous boulders, as well as many smaller stones. These boulders and stones have their angles more or less rounded off, their surfaces being in most cases scratched or striated, and such as admit of polishing — especially the limestones — are often beautifully polished. The larger portion of the stones have been derived from local rocks ; but such as are not from the immediate vicinity have been transported from somewhere to the north, sometimes east of north , and often to the west of north. Stewart — Mollusca of the Boulder Clay. i 66 The Molluscan shells occurring in the Boulder Clay are not numerous ; in most cases they are only found by patient searching, and then only m a frag- mentary condition ; but in a few instances they are less rare, and include speci- mens in a perfect state. Astarte sulcata , A. elliptica , A. compressa, and Leda pernula are the prevailing and characteristic forms ; the most widely diffused and the most numerous in examples. Fragments of these shells are to be found almost everywhere, and perfect shells are frequently met with. Leda pygmcea is also remarkable. Though a very small and fragile shell, it is usually found in a perfect state, with the two valves united. The presence of perfect shells of Leda was known long since to General Portlock, and forced him to the same conclusion as arrived at by the Author, that the Boulder Clay is a marine sedimentary deposit. The absence of stratification has led most geologists to the conclusion that the Boulder Clay is an accumulation resulting from land ice, and the occurrence in it of so many marine shells seems to have been either unknown or overlooked. Thefauna ofthe Boulder Clay is not by any means rich, and this is what we might expect from the rigour of the climate of that period. Nevertheless it is a marine fauna ; and there is unquestionable evidence m the case of several of the species that they truly belong to the deposit, and were not drifted into their present position from a distant locality, nor yet are they fossils derived from an older bed. From what has been stated, it will be seen that we must account for the want of stratification in some other way than the land-ice theory, as the presence of even one marine shell unquestionably belonging to the deposit renders that theory invalid. The supposition of a general ice-cap can derive no support from the Boulder Clay. The underlying rocks are very often glaciated, and hear strise which tell of ice that was moving over them from the north, and this is corroborated by the stones contained in the clay, which also tend to show a similar ice movement. We must, therefore, conclude that the clay was rapidly deposited from water-borne ice, and that the ice, with its burthen of clay and stones, was impelled by currents having a more or less southerly direction. On the floor of the sea lived a scanty boreal fauna. Many of the shells were broken into fragments by the ice grounding in the shallow waters, or by t e dropping down of large boulders, and the result that remains is the unstratified till, with its occasional entire shells and more numer,. us fragments The Boulder Clay forms the subsoil over the greater part of our district adding much to the fertility of the land. It is best seen in river banks, because the streams have made sections of the strata, and thereby exposed it to our view. It has, consequently, been often considered as only, or mainly, deposited in sheltered hollows ; but it is found 'that where artificial cuttings have been Stewart— Mollusca of the Boulder Clay. 167 made, as in quarries or roads, they discover the Boulder Clay equally on the hill-side or level plain. The Glacial Drift has been divided by geologists of eminence inth three stages First, the lower Boulder Clay, the most extensive, and displaying the greatest evidence of Arctic conditions ; second, certain sands and gravels deposited under milder conditions of climate ; and third, the upper Boulder Clay, which is said to indicate a recurrence of Arctic conditions. My researches do not lead me to accept this classification. I am unable to separate it into upper and lower, and the gravels said to be interglacial seem to be only local modifications of the deposits of one continuous period, during which Arctic, or semi- Arctic, conditions prevailed over this country without any interval of relaxation. The sands and gravels at Ballyrudder, near Glenarm, which Professor Hull regards as interglacial,* yield abundant specimens of a fauna as Arctic in character as any portion of the Boulder Clay, and are overlaid by an unstratified clay which I cannot distinguish from deposits which are said to be lower Boulder Clay. FOSSIL LOCALITIES. BELFAST WATERWORKS. The Boulder Clay at this locality has yielded a much larger number of Molluscan remains than any other similar deposit in Ireland. Forty-seven different shells are enumerated in the subjoined list, mostly collected in 1842-3 by the late Messrs. James Bryce, F.G.S., and George C. Hyndman, who pub- lished their results in Portlock’s Report on the Geology of Londonderry, PP- 738-9- A further and more complete list of the shells of the Waterworks was given by Mr. Bryce in the “Philosophical Magazine,” vol. 26, pp. 433-5. This deposit of Boulder Clay was proved to be undoubtedly rich in fossils ; but it is not, however, to be inferred that, as compared with other localities, this spot was so excessively rich as would appear from the lists. Mr. Bryce states that about ten thousand cubic yards of the clay were removed during the exca- vations for the lower reservoir, and that the great number of shells obtained was due to the watchfulness of various collectors. In other instances only the surface of a limited section can be examined, and it will be seen that no fair * Hull— Physical Geology and Geography of Ireland, p. 88. 1 68 Stewart— Mollusca of the Boulder Clay. comparison is possible: The four species added by me to the list published by Bryce were obtained by close scrutiny of material collected by the late Mr Hyndman, the deposit being now inaccessible. WOODBURN, COUNTY ANTRIM. A deep bed of Boulder Clay is, for a considerable distance, cut through by the Woodburn River, at rather more than a mile north-west of Carnckfergus. This bed has yielded ten species of shells, and is notable for the occurrence of three species of Leda, many of the specimens being in a perfect state. Trophon laitriceus was also found here. FALLS PARK, BELFAST.. This locality is close to the town, opening to the Falls Road. The clay here would be quite as rich in fossils as that of the Waterworks if sufficient material were available. The beds are exposed only in the low banks of the small stream that flows through the park, and, consequently, the search for fossils can on y be conducted by examining the surfaces of the sections. Seven species have been collected here, all of northern types, including Astarte triangularis . an Trophon Gunneri , which are not recorded from any of the other localities. Fragments of Balani are frequent here, as in all the fossil localities I have examined, except Bovevagh. BANGOR, COUNTY DOWN. The Boulder Clay is seen in a high bank on the shore at Ballyholme, half a mile north-east of Bangor. Six species of the usual northern forms have been found in this spot. The rocks, where denuded of clay, are seen to be finely glaciated. KNOCK, COUNTY DOWN. A small stream (Connswater) has exposed the Boulder Clay in the high banks of Knock Glen, near the Knock railway station. Shells are not plentiful at this plaee ; four species only have been found. Leda minuta and Leda pygmoea are not rare j they usually occur quite perfect. Stewart — Mollusca of the Boulder Clay. 169 CASTLE-ESPIE, COUNTY DOWN. Three miles from Comber, on the shore of Strangford Lough, there is an extensive deposit of Boulder Clay resting on Carboniferous Limestone, which is beautifully polished and striated. Shells are very scarce in the clay. Astarte sulcata and a Leda were the only forms recognised. CRUMLIN RIVER, COUNTY ANTRIM. The Boulder Clay is exposed at several points on the Crumlin River, and this locality is remarkable for the occurrence of a small patch, not much over a square yard in extent, as far as seen, but crowded with shells of Mytilus edulis in a very fragile condition. This bed is exposed on the south bank of the river, at about midway between Crumlin and the shore of Lough Neagh. It was discovered by Mr. E. T. Hardman, F.G.S., who supposed the shells to represent a species of Unio , and the clay to be a lacustrine deposit of Pliocene age.* Mr. W. Swanston, F.G.S., has shownf that the shells are really the tests of the common mussel, and that the clay is truly glacial. No other shells have been found associated with the Mytilus , but Mr. Joseph Wright, F.G.S., has found several species of Foraminifera. BOVEVAGH RIVER, COUNTY DERRY. This bed is situated not far from the village of Dungiven, and was described by Portlock in the Report on the Geology of Londonderry, page 159. It is only remarkable on account of the occurrence, in a very limited exposure of great numbers of Turretella terebra, , a shell that seems to be rare in the Boulder Clay elsewhere in Ireland. BALLYRUDDER, COUNTY ANTRIM. A most interesting glacial bed is to be seen at Ballyrudder, about six miles north of Larne, on the road to Glenarm. This deposit was examined long since by Dr. Jeffreys and the late Mr. George C." Hyndman, who published, in the Report af the British Association for 1859, a list of the shells which they found, at the same time intimating that their search was not exhaustive. It has also been recently mentioned by Mr. T. Mellard Reade, F.G.S., in Vol. XXXV. of * Geol. Mag., Dec. 2. Yol. 3, p. 556. + Geol. Mag., Dec. 2, Vol. 6, No. II. 170 Stewart— Mollusca of the Boulder Clay. the Quarterly Journal of the Geological Society of London. Mr. Reade appre- hended the importance of this bed, and in his communication gives a section and interesting notes. The deposit at this place is well exposed, and differs much from those of the foregoing localities. It consists of gravel, with sub- ordinate layers of sand and clay, the combined thickness of this series being about twenty feet. The gravels are overlaid by a bed of ordinary Boulder Cla y , about ten feet thick. The base is not seen. The gravels can be traced along the road for some fifty or sixty yards, and yield a number of very interesting shells, univalves preponderating. LIST OF THE MOLLUSCA OF THE NORTH-EAST OF IRELAND. I gratefully acknowledge that in compiling this list I received valuable assistance from Dr. J. Gwynn Jeffreys. F.R.S., who, with his usual kindness, undertook the identification of such of my shells as were in any degree doubtful. Rhynchonella psittacea. Chemnitz. Ballyrudder, County Antrim, Jeffreys and Hyndman. Report Brit. Assoc., 1859. Anomia ephippium, Linn. Belfast Waterworks. Bryce. Phil. Mag., Vol. XXVI ., p. 433 : Ballyrudder. Jeffreys and Hyndman. OSTREA EDULE, Linn. Belfast Waterworks. Bryce. Pecten MAXIMUS, Linn. Belfast Waterworks. Bryce. mytilus edulis, Linn. Woodbum, Bangor, Ballyrudder, S. A. S. ; Belfast Waterworks, Bryce ; Ballyrudder, Jeffreys and Hyndman. In great abundance in a bed of stiff blue Boulder Clay on the banks of the Crumlin River. Stewart— Mollusca of the Boulder Clay. 171 Modiolaria marmorata, Forbes. Ballyrudder, County Antrim, S. A. S. Nucula nucleus, Linn . Waterworks, Bryce ; Woodbum, S. A. S. Leda pygm^ea, Munst. Knock, Woodburn, Ballyrudder, S. A. S. This tiny, delicate shell is not uncommon, and almost invariably found in a perfect state. Leda minuta, Muller. Knock, Waterworks, Woodbum, Ballymdder, S. A. S. Similarly to the preceding species, this shell is very often met with in a perfect state. Leda pernula, Muller. Belfast Waterworks, Bryce; Falls Park, Waterworks, Woodburn, S. A. S. My largest specimen attained a breadth of one inch. Pectunculus glycimeris, Linn. Belfast Waterworks, Bryce. Arca pectunculoides, Sacchi. Belfast Waterworks, S. A. S. Arca lactea, Linn. Belfast Waterworks, Bryce. Lucina borealis, Linn. Woodbum, Ballyrudder, S. A. S. Cardium echinatum, Linn. Belfast Waterworks, Bryce. Cardium nodosum, Turton. Belfast Waterworks, Bryce. 172 Stewart — Mollusca of the Boulder Clay. Cardium edule, Linn. Belfast Waterworks, Bryce. Astarte sulcata, Da Costa . Belfast Waterworks, Bryce ; Bangor, Castle-Espie, Knock, Waterworks, Woodburn, Falls Park, S. A. S. This species and the following variety are to be found in almost every Bed of Boulder Clay. Frequently the shells are entire, but more commonly fragmentary. In the deposit at the Waterworks it is especially abundant. Astarte sulcata var . elliptica, Brown. Belfast Waterworks, Bryce ; Ballyrudder Jeffreys and Hyndman; Knock, &c., S. A. S. Astarte compressa, Montagu. Belfast Waterworks, Bryce ; Bangor, Falls Park, Woodburn, S. A. S. Astarte compressa var. globosa, Moller. Ballyrudder, Jeffreys and Hyndman. Astarte triangularis, Montagu. I found one specimen only in the Boulder Clay at the Falls Park. Astarte borealis, Chemnitz. Belfast Waterworks, G. C. Hyndman. Venus gallina, Linn. Belfast Waterworks, Bryce ; Bovevagh, County Derry, S. A. S. Venus ovata, Pennant. Belfast Waterworks, Bryce. Tapes aureus, Gmelin. Belfast Waterworks, Bryce. Tapes decussatus, Linn. Belfast Waterworks, Bryce. Stewart — Mollusca of the Boulder Clay. 173 Tellina balthica, Linn. Belfast Waterworks, Bryce ; Ballyrudder, Jeffreys and Hyndman ; Falls Park; S. A. S. Tellina calcarea, Chemnitz. Belfast Waterworks, G. C. Hyndman; Ballyrudder, Jeffreys and Hyndman. Mactra substruncta, Da Costa. Belfast Waterworks, G. C. Hyndman ; Ballyrudder, Jeffreys and Hynd- man, also S. A. S. Mactra solida vat , truncata, Montagu. Belfast Waterworks, Bryce. Mactra Solida var. elliptica, Brown. Belfast Waterworks, Bryce. Scrobicularia piperata, Bellonius. Belfast Waterworks, Bryce. Mya truncata, Linn. Belfast Waterworks, S. A. S. Saxicava rugosa, Linn. Belfast Waterworks, Bryce. Saxicava rugosa var. arctica, Linn. Falls Park, Waterworks, Woodburn, Ballyrudder, S. A. S. Pholas parva, Pennant . Ballyrudder, County Antrim, where I found one specimen. It is men- tioned by Jeffreys as occurring in the Red crag, which is the only other British deposit in which it is found fossil, so far as I know. Pholas crispata, Linn. Belfast Waterworks, fragments only, Bryce. 174 Stewart — Mollusca of the Boulder Clay* Chiton marmoreus, Fabricius. Ballymdder, S. A. S. Emarginula fissura, Linn. Belfast Waterworks, Bryce. Trochus tumidus, Montagu. Belfast Waterworks, Bryce. Lacuna pallidula, Da Costa. Belfast Waterworks, Bryce. Lacuna divaricata, Babricius. Ballyrudder, S. A. S. Littorina litorea, Linn. Belfast Waterworks, Bryce. Turritella terebra, Linn. Belfast Waterworks, Bryce; Knock and Ballyrudder, S. A. S. ; Bovevagh, Co. Derry, Portlock. This is a rare shell in our Boulder Clay, except at Bovevagh, where I found it abundant in one spot, as recorded by General Portlock. Turritella erosa, Couthouy. Ballyrudder, Co. Antrim, Jeffreys and Hyndman. Natica Montacuti, Forbes. Ballyrudder, Co. Antrim, Jeffreys and Hyndman. Natica affinis, Gmelin. Belfast Waterworks, Bryce : Ballyrudder, S. A. S. Aporrhais pes-pelicani, Linn. Belfast Waterworks, Bryce. Stewart— Moelusca of the Boulder Clay. i75 Purpura lafileus, Linn, Belfast Waterworks, Bryce, Buccinum undatum, Linn , Belfast Waterworks, Bryce ; Ballyrudder, S, A. S, Buccinum undatum var. fusiforme, Belfast Waterworks, Bryce. Buccinum grceanlandicum var, undueatum, Moller, Ballyrudder, County Antrim, Jeffreys and Hyndman. Murex erinaceous, Linn. Belfast Waterworks, Bryce. Trophon clathratus, Linn. Belfast Waterworks, Bryce ; Bangor, S. A. S. ; Ballyrudder, Jeffreys and Hyndman, also S. A. S. Trophon clathratus var. Gunneri, Loven. ■ Falls Park, Belfast, S. A. S. Trophon truncatus, Stromer. Belfast Waterworks, Bryce ; Falls Park, Ballyrudder, S. A. S. Trophon latericeus, Moller . Woodburn, Co, Antrim, S. A. S. Fusus antiquus, Linn, Belfast Waterworks, Bryce. Fusus antiquus Monst . cinctum. Belfast Waterworks, Geo. C. Hyndman, S. A.. S. I have seen two specimens of this form, which seems to me entitled to be considered as a variety rather than as a monstrosity. Fusus gracilis, Da Costa. Belfast Waterworks, Bryce. Stewart— Mollusca of the Boulder Clay. 176 Nassa reticulata, linn . Belfast Waterworks, Bryce. Hassa pygm/ea, Lamarck. Bangor, Co. Down, S. A, S. Nassa incrassata, Stromer. Ballyrudder, Co. Antrim, S. A. S, Pleurotoma turricula, Montagu. Ballyrudder, Co. Antrim, Jeffreys and Hyndman. Pleurotoma decussata, Couthouy . Ballyrudder, Co. Antrim, S. A. S. Pleurotoma exarata, Moller. Ballyrudder, Co. Antrim, S. A. S. Pleurotoma pyramidalis. Stromer. Ballyrudder, Co. Antrim, Jeffreys and Hyndman. Dr. Jeffreys thinks that this was the shell published as Mmgelia. Pingdii in Brit. Assoc. Report, It seems to me nearly certain that the correction is right. Cypbjea europ^a, Montagu. Bangor, Co. Down, S. A. S. 11 FEB 1S86 APPENDIX VI. a oust OF RECENT FORAMINIFERA OBTAINED DURING THE BELFAST NATURALISTS’ FIELD CLUB’S EXCURSION TO SOUTH DONEGAL, August , 1880. BY JOSEPH WEIGHT, F.G.S.; K) SPONGE REMAINS FROM THE CARBONIFEROUS LIMESTONE OF BEN BULBEN, COUNTY SLIGO. BY JOSEPH WRIGHT, F.G.S.; AND FOSSIL SPONGE-SPICULES FROM THE CARBONIFEROUS STRATA OF BEN BULBEN, NEAR SLIGO. BY H. J. CARTER, F.R. S., &c., Reprinted from “ The Annals and Magazine of Natural History ,” for September, 1880. Published by “The Belfast Naturalists’ Field Club,” April, 1882. . . I ' ( Proceedings Belfast Naturalists’ Field Club. — Appendix 1880-1881.) FORAMINIFERA FOUND DURING THE BELFAST NATURALISTS’ FIELD CLUB’S EXCURSION TO SOUTH DONEGAL, 1880. Plate VIII. (upper half), figs. 1-5. 'pj^j’HE objects contemplated by the Club in visiting the Southern Coast of (dJXv^) County Donegal embraced several departments of Natural Science, 'U® especially botany and geology, and as the time was limited it was im- possible to devote much attention to dredging. Three shore gatherings, and four hauls of the dredge were, however, secured, and the present list is the result of an examination of material thus obtained. This list is not given as exhaustive of the locality visited, but simply as a contribution to our knowledge of the Irish rhizopodal fauna. It will also serve to indicate that rich results are likely to reward more systematic investigations in this quarter. Of the shore gatherings, that from Muckros was the only one which yielded a good supply of Microzoa. It was collected in a small sandy bay adjoining the singularly wild and remarkable precipices of Muckros Head. As is usual in the sandy bays open to the Atlantic, along our Western Coast Truncatulina lobatula greatly preponderated over all other forms. Haplo- phragmium globigeriniforme, Lagena costata, and Polymorphina myristiformis were large and abundant at Muckros, and also in the dredgings taken in the open sea, off the headlands of Slieve League, whilst the same forms were rare, and in poor condition in the more sheltered waters of Killybegs Harbour. The four dredgings from Killybegs and Slieve League might, with little disadvan- tage, have been recorded as from two stations. For example, the two gather- ings from Killybegs, one taken in seven fathoms water, inside the harbour, the other in seventeen fathoms, a few hundred yards outside the Lighthouse, were very similar, both in nature of bottom and foraminiferous yield. The material dredged at both places was soft turfy ooze, yielding Microzoa in great profusion, and differing merely in that the one gathered outside the Light- 180 Wright — Foraminifera oj South Donegal . house was somewhat more sandy, and yielded a larger number of species. Bulimina, Bolivina , and Cassidulina were the characteristic genera at both places. The two gatherings taken off Slieve League differed scarcely in any particular. I have taken advantage of the present opportunity to record (under column 8) a list of species found in a dredging taken off Portstewart, by my friend Mr. James Wright, and kindly sent by him to me for examination. I am deeply indebted to my friend Mr. H. B. Brady, F.R.S., who, with his usual kindness, has examined and named the critical species ; as also to my friend Mr. W. Swanston, F.G.S., for the accurate and artistic drawings of the Foraminifera which accompany this memoir. I append a few remarks on one or two of the forms of more special interest. Haplophragmium glomeratum, Brady. (Plate viii, figs, 1, la.) Lituola glomerata, Brady, 1878, Ann. and Mag. Nat. Hist. Ser. 5, vol. 1, p. 433, PI. xx. fig, 1 a, b, c. This simple little Haplophragmium is abundant in Killybegs Harbour. It was also dredged last year by Mr. David Robertson, F.L.S., off the Isle of Skye, being the first record of its occurrence in British waters. The Irish examples are not so coarse in texture as the type specimens from the Arctic seas, figured by Mr. Brady , Ammodiscus Siioneana, Siddall. Trochammina Shoncana, Siddall, 1878, Proc. Chester. Soc. Nat. Sci., part 2, p. 46. A few examples of this pretty little Ammodiscus were found off Killybegs Harbour. It has hitherto been only met with in the Estuary of the Dee, by Mr. J. D. Siddall ; and in Belfast Lough, by Dr. Malcomson. Gaudryina filiformis, Berthelin. (PI. viii. figs, 3, 3 a, Zb.) Gaudryina jiliformis, Berthelin, 1880, Mem. Soc. Geol. France, Ser. 3, Yol. 1. Mem. No. 5, p. 25, pi. 1, fig, 8, a— d. An elongated sandy Gaudryina, with later chambers subquadrate. Often in a fragmentary state, the loose sandy texture of its test making it liable to be easily broken. Well-grown perfect examples are not unfrequent off Killy- begs. It has been found at many stations round our Irish Coasts; also off Skye, by Mr. Robertson. Bulimina bubtereb, Brady , M>S. (PI. viii. figs, 2, 2a.) Bulimina saltires, Brady, 1880, Notes on Reticularian Rhizopoda of the Challenger Expedition— Quart. Journ. Micr. Sol., Vol. xxi, New Series, p. 25. Wright — Forciminifera of South Donegal, 181 Fine examples of this handsome Bulimina are not nnfrequent off Killy- begs Harbour. It has also been found off Skye, by Mr. Robertson, and off the Shetlands, by Mr. Brady. Lagena marginata, Walker 8f Jacob. (PI. viii. figs, 4, 4a.) Serpula ( Lagena ) marginata , Walker & Jacob, 1784. Test. Min. p. 3, pi. 1, 7. Examples similar to Walker & Jacob’s type, having a broad marginal keel of transparent shell substance, are not unfrequent round our coasts. Rare off Killybegs Harbour, seventeen fathoms. Lagena marginata var. Orbignyana, Seguenza. (PI. viii. figs, 5, 5a.) Fissurina Orbignyana, Seguenza, 1862, Foram, Monotal. Mess. p. 66, pi. 2, figs, 25, 26. This well-marked variety, with three keels, is abundant almost everywhere round our coast. It is plentiful in all the Donegal gatherings. Lagena costata, Williamson. Entosolenia costata, 1858, Rec. For. Gr. Br. p. 9, pi. 1, fig, 18 ; Wright, Proc. Belfast Nat. Field Club — app. 1876-7, pi. 4, figs, 11 — 14. I have remarked that, of all our British Lagence, this form appears to flourish best off the exposed parts of our coasts. I imagine this must be due to its strong test enabling it to thrive better in rough water than the other more delicately formed species. Frequent off Slieve League. Fragments of a long, slender, tapering, arenaceous form, consisting of a number of segments, and having its shell-wall frequently composed of closely- fitting sponge spicula, arranged side by side, are not unfrequent off Slieve League, as well as at other stations round our coast. It is, most probably, a Reophax , but as no perfect example has as yet been obtained, its place among the Foraminifera could not be given with any degree of certainty. LIST OF LOCALITIES, WITH PARTICULARS OF DEPTH, &c. l82 Wright — Foraminifera of South Donegal. Wright — Foraminifera of South Donegal , 183 TABLE SHOWING THE DISTRIBUTION OF FORAMINIFERA GA- THERED DURING THE BELFAST NATURALISTS’ FIELD CLUB’S EXCURSION TO SOUTH DONEGAL, 1880. Abbreviations: — vr, very rare; r, rare; c, common; vc, very common. Speciea marked * are new to the British Fauna. Figures in column marked f refer to plate VIII accompanying this paper. LIST OF SPECIES. Reference to plate VIII. I Donegal, — between tides. Ardara, — between tides. Muckros Bay, — between tides. Between Slieve League and Malinbeg, — 24 fms. Off Slieve League, — 34 fms. Killybegs Harbour, — 7 fms. Off Killybegs Harbour, — 17 fms. Off Portstewart, — 15 fms. t 1 2 S 4 5 6 7 8 Cornuspira, Schultze. involvens, Reuss ... r r r r r r foliacea, Philippi ... ... ... ... ... v r ... Biloculina, Z)’ Orb. ringens, Lamk. ... c r r v c c r depressa, D’Orb. c r r r r c elongata, Z)’ Orb. v r ... ... r ... r r ... sphaera, 1)’ Orb. c ... r Miliolina, Will. trigonula, Lamk. ... ... r r r r tricarinata, D' Orb. ... r ... r r r r oblonga, Montagu r ... r r r r Brongniartii, D' Orb r ... ... r r r semin ulum, Linn. r c c c v c v c c subrotunda, Montagu ... r c c c c c v c secans, D, Orb. v r c r v r c bicornis, W. 3. v r c V c c r r c Ferussacii, Z)’ Orb. r r ... v r r r fusca, Brady r c ... ... ... ... ... ... Spiroloculina, I)’ Orb. limbata, Z)’ Orb. ... r r r r r r planulata, Lamk. ... r r r r v r P8AMMATODENDROM, Norman , M.S. arborescens, Norman , M.S., fragment ... ... ... ... v r 184 Wright — Foraminifera of South Donegal, TABLE — Continued. LIST OF LOCALITIES. Reophax, Montfort. fusiformis, Will. scorpiurus, Montfort ... Haplophragmium, Reuss. globigeriniforme, P. Sf J. glomeratum, Brady ... pseudospirale, Will. ... Canariense, D’Orb. ... Ammodiscus, Reuss. incerta, D’ Orb. ... gordialis, J. Sf P. Sboneana, Siddall Trochammina, P. Sf J. squamata, P. Sf J. infiata, Montagu Texttjlaria, Defrance. sagittula, Defrance ... agglutinaus, D’Orb. ... trochus, D’ Orb. difformis, Will. Gaudryina, D'Orh.' *filiformis, Berthelin. ... Verneuilina, D’Orb. polystropba, Reuss Bulimina, D’Orb. pupoides, D’Orh. marginata, D’ Orb. aculeata, D’Orb. ovata, D’Orb. elegantissima, D’Orb. *subteres, Brady Virgulina, D’Orb. Schreibersii, Czjzek .. Bolivina, D’ Orb. dilatata, Reuss punctata, D’Orb. plicata, D’Orb. ^ rg * * i | ri © Is 0 © —between tides. -between tides. rs c © ! © "® h 1 ! £ .: c3 r. w c b - L I © e League, — 34 fms 0 a 2 © *© P3 Donegal,- Ardara,— zn 1 O pi ' S f § ^ © $ > .© m ta O t 1 2 3 4 5 ... ... c v c c Figl ... ... v r y r ... ... ... ... ... y r c c c ... r r v r r r v r ... ... ... r c c c ... r ... ... ... ... ... r - c r r . Figt \ ... ... y r y r y r ... y r r c r c c c y r v r r ... v r • • ••• c r c r r Y I r y r .. Fig: 2 ... Y 1 v 1 . . . Y 1 r r r r 1 ... V 1 r Y 1 .J r r c r r 6 7 8 y r r r r r Y C r Y c ... r r ... r r C r r m4 r r y r r r r r ... ... c c c ... y r ... r r r Y c v c v r v c r ... Y C v c c c Y C r c Y C ... Y C V C r c c .. r r v r c v c ... c Y C c V C : Y r c Y C ! 1 r Killybegs Harbour,— 7 fms. "Off Killybegs Harbour, — 17 fms. Off Portstewart,— 15 fms. 1*5 Wright — Foraminifera of South Donegal. T ABLE — Continued. Ti — © d 03 03 a 03 a LIST OF LOCALITIES. hH hH h-H k o +3 'pH © rs +3 PI © © £ -+3 03 © d © © pS Pi © © £ © rO 1 ve League -24 fms. tH CO l © d t- 1 p d o rO l d o e8 M t, — 15 fms. o © © d © © © rQ l bD © d 43 © rO l d pd Sf PQ m o u M o tween Slie Malinbeg,- © P © .© 5q e3 w 03 bfi © rO Killybegs 17 fms. S £ © 43 03 43 U O P P3 o P ?4 <1 2 s © PQ o 0 O O — — Cassidulina, If Orb. t 1 2 3 4 5 6 7 8 laevigata, If Orb. v r c r r c c crassa, JD ’ Orb. v r v r c r r c r oblonga, I)’ Orb. r r r Bradyi, Norman M.S., broken. v 0* v r Lagena, Walker and Jacob. sulcata, W. Sf J. r r c r r costata, Will. ' Williamsoni, Alcock ... Lyellii, Seguenza ... c r c c c v c c c c y r c r c c c V c laevis, Montagu c c c r c c gracillima, Seguenza c c c globosa, Montagu v r r r r y r r ... striata, If Orb. v r r c V c r striato-punctata, P. Sf J. ... gracilis, Will. 0 r semistriata, Will. hispida, Reuss ... r c r c c c c r aspera, Reuss ... caudata, If Orb. marginata, W. Sf J. ... Fig4 r ... r r r i* r r j* r var. Orbignyana, Seguenza... Fig5 c 1 c c c c c c r n var. trigono-marginata, P. ) v & J- ... .. j ... v r ... ... v r r lucida, Will. ... var. (trigono-) oblonga, Se- ) ... c c c r c c c c guenza ... ... j ... ... r ... pulcbella, Brady v r y r ornata, Will. • •• v r •• lagenoides, Will. r r squamosa, Montagu c c c c Q c * hexagona, Will. ... ... Lingulina, If Orb. ... r c r r r c r c carinata, If Orb., small *tenera, Bornemann (fossil ?)... ... ::: • •• v r v r jg5 Wright — Foraminifera of South Donegal. TABLE— Continued. LIST OF LOCALITIES. Nodosaria, LamJc. scalaris, Batsch. ••• pyrula, D’Orb., and dentalme j variety J Vaginblina, D'Orb. legumen, Linn., small Margikulina, D’ Orb. lituus, I)' Orb., small Cristellaria, LamJc. rotulata, Lamk. crepidula, F. $f M. Pol"v morphina, If Orb. lactea, W. J- gibba, D’Orb. oblonga, Will. compressa, D’Orb. • •• concava, Will ... myristiformis, W ill-, large . communis, D’Orb. Uvigerina, D'Orb. angulosa, Will . Orbulina, D’Orb. universa, D'Orb. Globigerina, D'Orb. bulloides, D'Orb. inflata, D’Orb. ... Spirillina, Ehrenb. vivipara, Ehrenb. ... Patellina, Will. corrugata, Will . Discorbina, P. & J- rosacea, D’Orb. Parisiensis, D’Orb. ... ♦Wrigbtii, Brady Globularis, D'Orb. Bertheloti, D’Orb. 4= pi © 05 I 1 c3 PQ m o u % pi pi . bD 03 $ a ©<* ► t _ bo m g 05 r-* 05 CQ v r v r v r v c v r c v r v r r c v r r c v c v r I r v c GQ GQ 1 Jj 7 \ f sf 1 2 u 5 3 \ 43' u S3 i H < c 52 50 2 e3 £ © m 4 bO J © £ t Is % +=> CO 43 O Pm 3 * ti W C D O 6 7 8 c c v r r r r r r r ... , ... r ... . r r v r v r r v r ... r i r r c r r r s r c r . v r r ... r ... r c r r r ... ... ... c r r v c r v r r r r v r ... 0 c v r r c r c . v : r v r • ..1 v r v c c c c ... r r v r Wright — Foraminifera of South Donegal , 187 TABLE— Continued . LIST OF LOCALITIES. Planorbulina, D' Orb- Mediterraneensis, D’Orb. Truncatulina, D’Orb. lobatula, Walker refulgens, Montfort Tinoporus, Montfort Levis, P. Sf J. lucidus, Brady PULVINTJLINA, P. Sf J. repanda, F.Sf small auricula, F. Sf M. Karsteni, Reuss, small Rotalia, Lamk. Beccarii, Linn. nitida, Will. Operculina, D’Orb. ammonoides, Gron., large Polystomella, Lamk. crispa, Linn. ... striato-punctata, F. Sf M. Nonionina, D’Orb. turgida, Will. depressula, W. Sf J. ... scapha, F. Sf M., small umbilicatula, Montagu stelligera, D’Orb. Reference to plate VIII. Donegal, — between tides. Ardara, — between tides. Muckros Bay, — between tides. Between Slieve League and Malinbeg.— 24 fms. Off Slieve League, — 34 fms. t 1 2 3 4 5 ••• ... ... c c r ••• • •• v c v c V c v c v c ... ... ... ... c v r • • • ... ... ... r v r ... ... v r c c r • •• ... ... r ... ... ... ... r • c r ... ... ... ... ... c v r r .. . ... ... ... v r c r r ... ... ... v r • . • ... c r r ... ... V c v c c r c ... r r r ... ... V c v c c r r ... ... ... ••• I ... ••• ... ... ... ... ... 1 **• ... ... v r ... 1 ••• ... c v c v c r r v r 7 c V c V c c r v c v c r 8 c v c r c r c v r Killybegs Harbour, — 7 fms. Off Killybegs Harbour, — 17 fms. ■ . - 1 * : ■ ( Proceedings Belfast Naturalists ’ Field Club.— Appendix, 1880-1881.) SPONGE REMAINS FROM THE CARBONIFEROUS LIMESTONE OF BEN BULBEN, CO. SLIGO. BY JOSEPH WRIGHT, F.G.S. (Read before the Belfast Naturalists' Field Club , on the 13 th April, 1881.J aFTER referring briefly to the several groups of sponges, and their posi- tion in the animal kingdom, Mr. Wright proceeded to say, that having examined a portion of a pale yellow clay, which had been procured near the summit of Bon Bulben Mountain by Mr. S. A Stewart, he found that it contained an abundance of sponge-spicules, this being the only instance of such remains having been found in Ireland in rocks of Carboniferous age. In company of Mr. Stewart he had visited the spot for the purpose of ascertaining the mode of occurrence of the sponge remains, and to procure a sufficient quantity of the material for his investigations. Ben Bulben is a grand moun- tain, 1,722 feet high, whose stupendous cliffs arrest the attention of the traveller on the way from Bundoran to Sligo. The rock here may truly be called mountain limestone, the entire range, of which Ben Bulben is the most conspicuous, being composed of Carboniferous Limestone from the base to the summit. Nowhere else in Ireland do the Carboniferous rocks attain so great an elevation. Two days were spent on Ben Bulben, an ample supply of the fossiliferous clay obtained, and also many rare fossils met with in the lime- stone. Crinoids were especially abundant, notably the pretty little Pentre. mites Derbiensis. The curiously branched coral, Cladochonus baccilaris, was seen at one spot in great masses in the stone. The clay in question has been under examination, and already has yielded eleven different forms of sponge- spicules. Of these, four belong to the calcareous sponges, two to the Lithi- stidae, and the remaining five to the group of the Hexactinellidae. Three of these last-mentioned are extremely beautiful forms, being spirally ringed spicules apparently referrible to one species of sponge, and new to science. Mr. Wright further mentioned that some of the clay had been submitted to his friend, Mr. James Cooke, of Cork, for chemical analysis, and was found to be 1 9o Carter— Fossil Sponge-Spicules from Ben Bulben. almost purely silicious. Mr. Cooke regards it as disintegrated chert, the disintegrating agent being animal life. The following is Mr. Cooke s analysis i . su e , soluble and insoluble, 97 to 98 per cent. ; alumina, with -^ 0 iron i per cent. ; lime, less than 1 per cent. ; traces of magnesia and man Zese 1-10 per cent. Mr. Cooke finds clear proof of organic matter stiU Listin’- in the clay, and he considers that the sUica was probably bj “olcanic outburst. In the « rotten limestone' » of Cunningham Ayrshire, which seems to resemble our Ben Bulben ®p™g.6"9pl™ f tl Abundant, and yery similar to those found in Sligo. In the Insh as^in the Scotch beds, chert occurs associated with the clays in w i . t to found. Thi is similar to what occurs in our Cretaceous recks, and points to the fact of the silica which forms our flints and chert haying ben, m part at least deriyed from silicious sponges which abounded in ancient seas, the sill being ^deposited in layers, or concentrated round some sponge « otbe organism, and so forming our nodular flints. The paper was lUuutated by a fine series of diagrams representing the various forms o spicules obtained the Sligo mountains, as well as the material in Several examples of recent and fossil sponges were also exhibited of the meeting. Through the kind permission of Mr. H. J. Carter, F R.S., the following paper, “ On fossil sponge-spicules from the Carboniferous strata of Ben Bulbe , has been reprinted from the Annals and Magazine of Natural Histo^ Sep ., 1880 ■ the figures which accompanied it have been reproduced by photo-lith- ography, and are an exact reproduction of the originals. (From the Annals and Magazine of Natokal Hisrour/or Sept, 1880.; ON FOSSIL SPONGE-SPICULES FROM THE CARBONI- FEROUS STRATA OF BEN BULBEN, NEAR SLIGO. BY H. J. CARTER, F.R.S., &c. Plate VIII., (lower half) figs. 1-17. JN the last contribution that Mr. James Thomson made to our pledge > of fossil sponges which existed during the Carboniferous epo h m the neighbourhood of Glasgow (‘Annals,’ 1879, vol. m., p. !«, P'- » described and illustrated Holasterella conferta a genus of sponges, as the name indicates, exclusively composed of stelliform spicule , 3T figure, from tho same locality, had been found and illustrated a yea. ^previous y. M the same time I added (ibid. p. 145) some observations on specimens of Carter — Fossil Sponge-Spicules from Ben Bulben. 1 9 1 limestone belonging to the Carboniferous series which Mr. Thomson had gathered from the western side of Black Head, county Clare, at the southern extremity of the entrance to Galway Bay, in which the siliceous element (often present in great quantity) seemed to indicate that it had been derived from some organisms more or less composed of silica, especially as in other parts, where the limestone is pure, the remains of sponge -spicules in a calcified state are abundantly recognizable, although in none of the specimens sent to me could I find a definite form. Here the matter rested, so far as I myself was concerned ; but Mr. Joseph Wright, F.G.S., who resides at Belfast, having subsequently visited the mountain near Sligo called “ Ben Bulben,” actually ascertained the presence of several forms of sponge-spicules in the limestone of the Carboniferous system there, and kindly forwarded specimens of them to me, together with fragments of the strata in which they are found, for description and illustration. But before I proceed to this, it is desirable that the following extracts from Mr. Wright’s letter, dated Jan. 1, 1880, which accompanied them, should be given, viz. : — “Last summer my friend Mr. S. A. Stewart spent a few days botanizing on Ben Bulben, and, whilst there, observed soft clay bands in the limestone, of which he brought me three different ‘gatherings’ to examine for Fora- minifera, viz. : — 1, containing no organisms ; 2, a few Foraminifera and spi- cules ; and 3, rich in sponge-spicules. “ The last material proved so interesting that we afterwards visited the place in company and brought away a quantity of the clay. It is of a pale yellowish colour, and occurs interstratified with bands of chert, especially at the summit of the mountain, where it is very soft, owing, apparently, to exposure to the weather ; on the other hand, lower down, the same yellow material occurs, but much harder, although lighter, from its open pumice-like structure. At both places we found a great number of fossils belonging to the limestone of the Carboniferous system, viz “ I sent some of the clay to a friend in Cork for analysis ; and he has informed me that it contains 98 per cent, of silica.” After this follow sketches of all the forms of fossil sponge-spicules that Mr. Wright by dexterous manipulation was enabled to extricate from the clay — to which, after carefully looking over all that he found, which were subse- quently forwarded to me, I can add no more specifically, although I have been able to find a few with slightly different forms, which have assisted me in the following descriptions. Of course, as drift-spicules, which these must have been when originally deposited, to say nothing of the subsequent effects of fossilization, &c., they are nearly all fragmentary ; but sufficient of them remains for easy recognition and for restoration, as will be seen by the illus- trations. First and foremost is a sexradiate stellate (PI. XIV. B. fig. 2), which in 192 Garter — Fossil Sponge- Spicules from Ben Bulben. number of rays varies from 6, 12, 18 to 24 (figs. 4-7), according to the amount of division of the extremities of six arms. The stellates vary m size from l-75th to 5-24ths of an inch (fig. 1) in diameter ; and the smallest are not only the most numerous and have the greatest number of rays, but, as the latter often arise from a division of the arm close to the centre, they acquire the appearance of globular little stars ; while, where the arms are a little more extended, they often present the appearance of a “ Maltese cross.” But the most striking feature of this spicule is that, from the smallest to. the largest, each ray is spiriform ; that is, its surface presents a spiral inflation m which the coils are more or less numerous, extending from the base to the apex of the ray (figs. 2 and 3) ; where they are most numerous they, of course, are more transverse, and then appear like separate annulations ; while the most remarkable difference in them is confined to the rays of the largest stellates, where, towards the base, the spiral line of inflation becomes broken up into short portions (fig. 3 b), which look very much, from their alternate arrange- ment in adjoining coils, as if this had been produced by another spiral groove pursuing an opposite direction (that is, across the original inflation). This fossil spicule is incomparably more numerous than the other spicular forms accompanying it ; so that, together with its peculiarities being confined to a stellate form, I am compelled to think that it must have belonged to a species of Holasterella which, if found in situ hereafter (that is, forming the entire sponge), will be like H. conferta ; hence I have much pleasure in naming it Holasterella Wrightii, after its discoverer. The next spicule in frequency appears to have been a hexactinellid, with the sixth or external arm not produced as in the large surface-spicules of the Sarcohexactinellida, in which four arms are extended over the surface laterally, while the fifth, like the shaft of a nail, goes vertically inwards (fig. 8).. With this, and also equally plentiful, are the free ends of “ anchoring -spicules terminated by four much-recurved spines or flukes situated opposite each other, and still attached to a small fragment of the shaft (fig. 9), longer and larger portions of which may be observed in the “chert,” both longitudinally and in transverse sections under fracture, indicating that with the anchoring ends they are the fragmentary remains of what originally were anchoring- or cord-spicules of a Hyalonema or Sarcohexactinellid sponge. Tolerably numerous also are Lithistid spicules, especially one like a tripod, in which the centre is convex and smooth, while the three legs, bending out- wards and downwards, end respectively in expanded concave feet, which seem to show that they were once applied to similar surfaces on adjoining spicules (figs 10 and 11). This in all probability was a surface-spicule like those of Corallistes aculeata (‘ Annals,’ 1880, vol. vi. pi. vii. fig. 45). Fragments of other Lithistid spicules are also present, such as the dendritically branched surface-spicule (fig. 12), and the shafted one of the fully developed or internal structure (fig. 13). Carter — Fossil Sponge- Spicules from Ben Bulben. 193 To these may be added a sausage-shaped spicule like that of some of the Renierce of the present day, also tolerably plentiful (fig. 14) ; and other fusi- form acerate ones (figs. 15 and 16), which being common to many kinds of sponges, cannot in their isolated state, be identified with any in particular. Two fragments represent the arms of a quadriradiate spicule (fig. 17) ; but whether these were equal in length, or one was prolonged into a shaft, there is no evidence to show : if the former, it probably belonged to one of the Pachastrellina ; if the latter, to a zone-spicule of one of the Pachytragida. The most interesting part of this discovery, however, is that the “clay ” of Ben Bulben, in which Mr. Wright found these remains, is apparently identical in every respect with that sent me by Mr. James Thomson, in which he found Holasterella conferta , near Glasgow. In both instances isolated sponge-spicules of different kinds are disseminated through it, which can be obtained by edulc oration with water, and are composed of silica in an opaque or chalcedonic state, rendered more or less irregular by the presence of rhomboidal excava- tions on the surface. Here I might observe that, not only are the sponge-spicules, and the minute fossils of the Carboniferous Limestone which accompany them, silicified and pitted on the surface with the same kind of rhomboidal excavations, but the “chert’’ to which Mr. Wright has alluded appears to be a solid pseudomorph of the limestone ; for its pumice-like worm-eaten character occurring here and there, from partial absorption or decomposition of the material, presents a skeletal rhomboidal structure ; while the same kind of rhomboidal excavations characterize the surface of the weather-worn calcareous fossils in the pure Devonian Limestone of this neighbourhood ; by which I am led to infer that, in the first place, the sponge-spicules become partially or wholly calcified among calcareous material, else why should they now present rhomboidal exca- vations on their surface? that subsequently the siliceous element, being liberated, replaced the calcareous material so as to form the “chert;” and, thirdly, that the rhomboidal excavations on the surface of the spicules and the partial absorption of the spicules themselves, leaving nothing but their moulds, arises from the changes which the siliceous element itself is now undergoing— that is, becoming decomposed and removed, or passing from an amorphous state into clear quartz prisms. The latter, although but slightly the case, comparatively, in the specimens from Ben Bulben, is characteristically so in the specimens to which I have alluded from Black Head, Co. Clare, wherein not only geodic cavities lined with quartz prisms, but perfect prisms themselves are present, imbedded in the amorphous siliceous material composing the rock, ■while all satisfactory traces of sponge-spicule form in these parts is entirely absent, so far as the specimens sent to me indicated. Lastly, I am inclined to think that the “ clay” of Ben Bulben is the “ chert” decomposed, and that the innumerable fragments of sponge-spicules which are present in the latter (for in some parts the chert appears te be almost entirely i94 Carter— Fossil Sponge-Spicules from Ben Bulben. composed of them), rendered still more fragmentary by partial removal so as to leave nothing but their moulds, as before stated, are those which at last come out entire, so far as they go, in the washing of the “ clay.” It is remarkable, too, that by far the most plentiful among Mr. Thomson s collection of spicules from the clay near Glasgow is that of Holasterella conferta i, as it is that of H. Wrightii at Ben Bulben; the “sausage-shaped” spicule (•fig 14) is also analogous to that of the supposed Remend sponge ( Annals, 1879, vol. iii.pl. xxi. fig. 11), and about the same in frequency. In Mr Thomson’s collection were also fragments of Lithistid spicules; and last summer he sent me a section of an entire sponge in Carboniferous Limestone, all calcified withweathered-ont spicules on the surface, but none of it sufficiently defined for useful delineation. The collection also contained some zone-spicules of the Pachytragida ; so that, altogether, the Spongida appear to have been as plentiful and as varied in the Carboniferous age as at any other time. It would be worth while, when the opportunity offers, for some one to look over the weathered surface of the strata in the mountain of Ben Bulben, where fragments, if not entire specimens, of sponges from which the spicules come might be found, after the manner that they have been discovered in the Car- boniferous system in the south-west of , Scotland. 11 u fjttl * JT ^ EXPLANATION OF PLATE VIII. (Upper Half.) Fig. 1. Haplophragmium glomeratum , Brady, magnified 60 diam. Off Killy- begs Harbour, 17 fms. Fig. 2. Bulimina subteres , Brady, magnified 60 diam. Off Killybegs Harbour, 17 fms. Fig. 3. Gaudryina Jiliformis, Berthelin, magnified 60 diam. Off Killybegs Harbour, 17 fms. Fig. 4. Lagena marginata , W. & J., magnified 60 diam. Off Killybegs Harbour, 17 fms. Fig. 5. Lagena marginata , yar. Orbignyana, Seguenza, magnified 60 diam. Off Killybegs Harbour, 17 fms. EXPLANATION OF PLATE VIII. (Lower Half.) Fig. 1. Holasterella Wrightii, spicule of, nat. size. The largest met with (diagram). Fig. 2. The same, restored, to show the perfect form 'with spiral inflation on the arms. Magnified 7 diameters. Fig. 3. The same. Furcate arm, much more magnified, to show — a, the simple spiral inflation, and b, the same when “ broken up.” Scale l-48th to l-1800th inch. Figs. 4, 5, 6, and 7. The same, to show the simple sexradiate and multifid divisions of the arms respectively (diagrams). Fig. 8. Sarcohexactinellid. Fragment of large surface-spicule of unknown species. Fig. 9. The same. Free end of anchoring-spicule. Fig. 10. Lithistid. ? Tripod-like surface-spicule of unknown species. Fig. 11. The same. Lateral view. Fig. 12. The same. Dendritically branched surface-spicule of unknown species. Fig. 13. The same. Form of body-spicule of unknown species. Fig. 14. Reniera ?. Sausage-shaped spicule of unknown species. Fig. 15. Acerate spicule of unknown sponge. Fig. 16. The same. Fig. 17. Quadriradiate fragment of spicule of unknown sponge. U.B. Figs. 3 and 8-17 inclusively are all drawn to the scale of l-48th to l-1800th inch. Proc. Belfast Nat. Reid Club. 1880 -8.1 (App.mdix) PL VIII. WRIGHT- FORAMINIFERA OF SOUTH DONEGAL. CARTER - CARBONIFEROUS SPONGE SPICULES OF BEN BULBEN. ' A s it is intended to issue , from time to time , further Lists of the Fauna , Flora , Fossils , <2/2*2? Anti- quities of the North of Ireland , 'Members are requested to preserve this Appendix for binding with those already issued \ and to be issued in the future. The next part of the Proceedings will contain Draw- ings., Illustrating Papers by Mr. William Gray , <2/2<2? Mr. Charles Elcock , abstracts of which appear in this part. ■ ■ ' ' APPENDIX VII. SUPPLE HyriE! LTT TO A L I ST OF MOSSES OF THE NORTH-EAST OF IRELAND. BY SAMUEL ALEX. STEWART, Fellow of the Botanical Society of Edinburgh. PUBLISHED BY THE BELFAST NATURALISTS’ FIELD CLUB. February , 1884. •a ' (Proceedings Belfast Naturalists' Field Club.— Appendix 1882- 1883 J SUPPLEMENT TO A LIST OF THE MOSSES OF THE NORTH-EAST OF IRELAND. BY SAMUEL ALEX. STEWART, Fellow of the Botanical Society of Edinburgh. fINE years have passed away since the list, to which this is a supple- ment, was published in the Proceedings of the Belfast Naturalists’ Field Club. During that period the world has not failed to move on, nor has botanical knowledge stood still. Stimulated mainly by the Royal Irish Academy, a number of Irish naturalists have been scrutinising nar- rowly the flora of their country. The results of these investigations have been embodied in valuable reports published, or now being published, in the Proceedings of the Academy. These papers, however, have related entirely to the phanerogamic plants, with the exception of that by Dr. D. Moore, on Irish Hepaticse. Meanwhile, with the rolling on of events, we have to de- plore the loss of some who stood in the front rank of the small band of Irish Botanists. Dr. David Moore and Isaac Carroll have been removed by death, and the inexorable fate which so recently overtook our fellow-member, Mr. T. H. Corry, has deprived our Society of one who felt the deepest interest in the objects for which it was established. The wider field of Irish Botany, too, is affected by the premature loss of one who was doing much to enlarge our knowledge of the native flowering plants, and who hoped to take part in the investigation of our Cryptogamic flora also. But while the wheels of fate roll on, bearing away, as we have seen, some of our “best and bravest,” they are bringing up to our ranks valuable acces- sions, and new life. Ever since systematic botany assumed the rank of a science, it has not lacked votaries in Ireland, gifted with acuteness of obser- 198 Stewart — Mosses oj North-East of Ireland (Supplement). vation and enthusiastic love for the study. In the annals of Irish Botany, we find Wade, Templeton, Turner, and others ably leading the van at the close of last century. These were succeeded by such well-known naturalists as Mackay, Taylor, and Hutchins, and these, again, by others who have survived to our own times. So much for the past : indications are not wanting that, in the coming time, there will be those who will carry our knowledge to a still higher point. , . . . As stated in the preface to the list of 1875, the district to which it referred embraced the counties of Down and Antrim, with a small part of Derry It is a matter of regret that, even yet, it is not possible to include the whole of Derry. The fact is, that as far as bryology is concerned, the greater portion of that county is up to the present a terra incognita. The Mourne Mountains, and the southern portion of County Down, hare yielded some novelties to the as yet incomplete, examination of the Rev. H. W. Lett, of Ardmore, and Rev C Herbert Waddell, of Warrenpoint. These gentlemen have kindly- furnished the names of the most interesting species collected by them. A number of their plants remain, which have not yet been diagnosed but it will be seen, on reference to the list which follows, that they have added materi- ally to our Moss-flora, in a very brief period. It is to be hoped that e quickness of observation, and scientific method Mr. Lett and Mr. Wa e have already manifested will be employed to still further elucidate the natural history of a very interesting region. The Museum of the Belfast Natural Historv and Philosophical Society contains a collection of mosses by Mr T Drummond, acquired by the Society in 1831. Some of these plants have been collected in our locality, and a few of them, not previously pub- lished, are now put on record. „„„ The number of Mosses included in the list of 1875 amounted to 238, and the 35 now added bring the number up to 273. Such of the plants as seemed at all doubtful have been submitted to G. A. Holt, Esq., of Manchester, who kindly consented to revise them* Such revision is of the utmost importance ; and the fact that a bryologist of such accuracy has seen the specimens adds much to the value of the records. Rev. John Fergusson, of Forfarshire, has also kindly assisted with advice on some critical plants. Several rare plants have been contribued by J. H. Davies, Esq., of Glenmore ; one of these being Orthotrichum Sprucei, a species not included in any previous list of Irish Mosses. Objections will, no doubt, be made to the arrangement here followed, and perhaps also to the nomenclature. It has, however, seemed desirable not to depart from the classification of the original list, to which this is supplemen- tary. As respects the nomenclature I am not convinced of the value of small genera, based on trivial characters. *Eev. Mr Lett’s specimens have been confirmed by Mr. West, of Bradford. Stewart — Mosses of North-East of Ireland (Supplement). 199 LIST OF SPECIES. The asterisk denotes that the spocies was not previously recorded for the district. CRYPHiEA HETEROMALLA. Dill. This species is frequent throughout the district, but never abundant. Hookeria ltjcens. Dill. Tollymore Park, and Rostrevor Mountain, County Down. — Rev. C. H. Waddell. Hypnum loreum. Dill. Frequent in the Mourne Mountains. — Rev. C. H. Waddell. Rostrevor Wood : Slieve Comedagh : Slieve Croob (Down) ; fruit abundant : Ballvgallv Head (Antrim).— S. A. S. H. brevirostre. Ehr. Narrowwater Wood, near Newry, fruiting abundantly. — Rev. C. H. Waddell. Fruiting sparingly at upper end of Holywood Glen, in January, 1876.— S. A. S. H. 8CORPIOIDE8. Dill. Rathlin Island (Antrim) ; barren.— S.A.S. * H. sarmentosum. Wahl. Yery rare. Spinkwee River Glen, above Tollymore Park. — Rev. H. W. Lett. H. eugyrium. Schp. [This moss, so rare in Ireland, was found by Rev. Mr. Waddell on Angle- sey Mountain, County Louth. It should be sought for on the Mourne Moun- tains also.] H. RE8UPINATUM. WHs. Ballyholme ; Cregagh Glen (Down) ; Kilroot ; Ballygally Head ; Fair head (Antrim). Frequent in fruit. 11-2. — S. A. S. * H. C UPRE S 8IFORME . Dill. VAR LACUNOSUM. Wife. Warrenpoint, County Down. — Rev. C. H. Waddell. 200 Stewart — Mosses of North’ East of Ireland (Supplement), H. FILICINUM. Dill. Rostrevor Mountain, and near Moira, County Down.-Rev. H. C. Waddell. * H. Sendtneri. Schp. Rare. Rathlin Island. — S. A. S. * H. riparium. Linn. Wet places— rare. Abundant in several places, by the Lagan Canal, above Moira, County Down.— S. A. S. H. UNDULATUM. Dill. Tollymore and Slieve Bignian, Mourne Mountains (Down).— Rev. C. H. Waddell. Rathlin Island (Antrim).— S. A. S. H. MUR ALE. Hedw. Walls near Belfast. — T. Drummond. In the water table, Falls Road, near Andersonstown ; also, on a stone dyke, in old road, at back of Cave Hill. — S. A. S. H. TENELLUM. DicTtS. Old Walls of Dundrum Castle (Down) ; Rathlin (Antrim).— S. A. S. * H. FLAGELLARE. Dicks. Rocky banks of mountain streams. Tollymore, Yellow Water, &c. ; frequent. -Rev. C. H. Waddell. Slieve Donard, Slieve Comedagh, and fre- quent in the Mourne range, but always barren. — S. A. S. * H. speciosum. Brid , Rathlin Island.— S. A. S. Rare and barren. * H. crassinervum.— Tayl. Very rare. Cave Hill, near Belfast.— T. Drummond. Specimen in Belfast Museum Collections ( Musci Scotica). H. MYOSUROiDES. Linn. Widely spread. Warrenpoint and Rostrevor. — Rev. C. H. Waddell. Slieve Donard (Down) ; Ballygally Head, and Glenshesk (Antrim).— S. A. S. H. ALBICANS. Dill. In fruit on sandy warren— Donaghadee, February, 1876.— S. A. S. H. LUTESCENS. Huds. Roetrovor Mountain.— Rev. C. H. Waddell. Upper end of Holjwood Glen, and railway bank, Newtownards.— S. A. S. Stewart — Mosses of North-East of Ireland (Supplement). 201 * Heterocladium heteropterum. Bruch. Very rare. Rocks by stream, Slieve Comedagh, and on rocks in the stream at upper end of Glenmachan Glen (Down). — S. A. S. Barren. * Leskea polycarpa. Ehr. On bases of ash and alder trees — rare. By the Lagan Canal, above first lock, and by the Six-mile River, above Templepatrick. — S. A. S. Climacium dendroides. Linn. Fruiting freely near Lisburn ; October, 1877. — Mr. J. H. Davies. Pterogonium filiforme. Hedw. Tollymore Park. — T. Drummond. * Fissidens osmundioides. Hedw. Wet mountain rocks — rare. On Slieve Croob — sparingly. In several places between Tollymore Park and Donard Lodge. — S. A. S. Fruit, April and May. * F exilis. Hedw. Ditch banks — very rare. Ditch banks near Belfast. — T. Drummond, 1831. In a lane leading from Ballygomartin Road to Black Mountain — S. A. S. It occurs sparingly on the ditch bank at upper end of lane. In fruit, March, 1880. Tetraplodon mnioideb. Hedw. Crocknafeola Plantation, Mourne Mountains. — Rev. C. H. Waddell. Bartramia ithyphylla. Brid. Slieve Donard, and rocks above Bryansford (Down). — S. A. S. Rising to 1600 feet. B. arouata. Licks. One stem in fruit ; November, near Rostrevor. — Rev. 0, H. Waddell. EnTOSTHODOn FA8CICULARE. Dicks. Warrenpoint (Down). — Rev. C. H. Waddell. * E. ericetorum. De Not. Damp rocky places by streams in the mountains — rare. Slieve Donard, at 1500 to 1800 feet.— S. A. S. 202 Stewart— Mosses of North-East of Ireland (Supplement). E. Templetoni. Hook, and Tayl. Mourne Mountains, at Rostrevor. — Rev. 0. H. Waddell. Slieve Donard (Down) ; Rathlin Island (Antrim).— S. A. S. FUNARIA HYGROMETRICA, VAR PATULA. Magheralin (Down). — Rev. 0. H. Waddell. Mnium undulatum. Hedw. Fruiting abundantly in the wood at Narrowwater, County Down.— Rev. C. H. Waddell. M. rostratum. Schrad. Tollymore Park. — Rev. C. H. Waddell. Castlereagh Hill (Down), and Tardree (Antrim). — S. A. S. * Bryum bimum. Schreb. Rare (?) A specimen from Fair head (Antrim) seems to be this, but lacks inflorescence. — S. A. S. B. p allens. Swartz. Mourne Mountains. — Rev. C. H. Waddell. B. PSEUDOTRIQUETRUM. Hedw. Mourne Mountains. — Rev. C. H. Waddell. Rathlin Island. S. A. S. B. carneum. Linn. Magheralin (Down). — Rev. C. H. Waddell. * B. ELONGATUM. Dicks. Very rare. Slate rocks between Slieve Donard and Tollymore (Down). —Rev. H. W. Lett. [Aulocomnion androgynum. Schw. Very rare. In bogs near Ardmore (Lurgan), on weathered stumps of bog- fir._Rov. H. W. Lett. The locality where this rare moss has been found, though in County Armagh, is on the border of our district, and may be hoped for in either Down or Antrim.] [Oligotrichum hercynicum. Ehr. Vory rare. Not found in our district, but collected by Rev. C. H. Waddell from rocks by stream, Anglesey Mountain, County Louth. Probably also on Mourne range.] Stewart — Mosses of North-East of Ireland (Supplement). 203 * Diphyscium foliosum. Linn. Very rare. Slievenamaddy Mountain. — Rev. H. W. Lett. This moss, so rare in Ireland, has been found also on Anglesey Mountain, Louth, just outside our district, by Rev. C. H. Waddell. Zygodon rupestris. Schp. Crevices of rocks on the shore at Portavo, and also, close by, on the old wall of the Donaghadee road (Down). In some plenty on the south-west wall of the Bridge on the Larne road, at Kilroot ; sparingly on rocks in Rathlin Island (Antrim). — S. A. S. * Z. viridissimu3. Dicks. On trunks of trees ; widely diffused in the barren state ; rare in fruit. Rostrevor (Down) ; Shaw’s Bridge, Cave Hill, Kilroot, Magheramorne (fruit) Co. Antrim. — S. A. S. * Orthotrichum calvescens. Wils. Very rare. Two tufts of this moss were collected in the district— I believo in Glenshesk, County Antrim — but as the label has been lost, this species cannot be localised with entire certainty, — S. A. S. 0. LEIOCARPUM. Br. and Schp. On trees, Tollymore (Down).— Rev. H. W. Lett. Base of the Sallagh Braes (Antrim). — S. A. S. * 0. Sprucei. Mont. Very rare. On several trees and bushes by the Lagan Canal, imme- diately above Drum Bridge (County Down). This moss is plentiful in this, its only Irish station, where it was discovered by Mr. J. H. Davies, of Glen- more, in 1878. *0. rivulare. Turner. * Rare. Sparingly on trees, at Drum Bridge (County Down), with the pre- ceding species. Discovered by Mr. J. H. Davies in 1878. Since found in abundance on rocks in Glenavy River (County Antrim), near the junction with Lough Neagh. — S. A. S. 0. Sturmii. Hoppe. On trees Tollymore Park, Co. Down.— Rev. H. W. Lett. Plentiful on stones, in a boggy heath, on Knocklayd Mountain, Co. Antrim, with mature and abundant fruit at latter end of April, 1882. — S. A. S. 204 Stewart— Mosses of North-East of Ireland (Supplement). 0. CTJPULATUM. Eoffm. On stones in Crumlin River, and on the Gobbin Rocks, Co. Antrim.— S. A. S. RACOMITRIUM CANESCEN8. HedlV. Drumcormac, at base of Slieve Gallion, Co. Derry, on the east side.— S. A. S. * R. obtusum. Sm. R. HETEROSTICHUM VAR. gracilescens. Bry. Eur. Amongst Drummond’s mosses, in the Belfast Museum, is a specimen marked by himself “ Racomitrium microcarpon of foreign authors— not of Bry. Brit.” Subsequently it has been marked, by the hand of Dr. Taylor, “ Tn- chostomum microcarpon var. oblongum,” and initialed “ T. T.” . I am in- debted to Rev. John Fergusson for identifying this specimen with the T. obtusum of Smith, afterwards R. obtusum of Lindberg. Drummond’s specimen was collected more than fifty years ago, and the plant does not seem to have been seen on the Mourne range since that time. * R. protensum. A Braun. Very rare. Mourne Mountains.- T. Drummond. Wet rocks in several places between Slieve Donard and Tollymore Park, Co. Down, at 1200 to 1500 feet.— S. A. S. R. ellipticttm. Turner. Mountains above Newcastle, Co. Down; Benbradagh Mountain, above Dungiven, Co. Derry.— S. A. S. Grimmia LEUCOPH2EA. Grev. On schist, Slievnabrock— Mourne Mountains.— Rev. H. W. Lett. G. trichoph v ll a . Grev. Plentiful on a glacial boulder, between the Giant’s Ring and the Lagan, Co. Down.— S. A. S. Barren. G. Schultzii. By id. Plentiful on basaltic rocks— Ballygally Head, Co. Antrim.— S. A. S. G. conferta. Br. and Schp. Var incana. Brean Mountain, Glenshesk ; Bathlin Island, Antrim — S. A. S. Encaeypta streptocarpa. Hedw. On walls, Narrowwater and Tollymore (Down).-Bev. C. H Waddell In great profusion on walls of Clady Bridge, near Dunadry, Co. Antrim.- S. A. S. Always barren. Stewart — Mosses of North-East of Ireland (Supplement). 205 * Tortula hibernica. Mitt. Very rare. To this species Mr. Holt refers a moss from Rathlin Island, It is, however, a poor, drawn out, and barren form. T. latifolia. Br. and Schp. At the bases of trees by the Lagan at Shaw’s Bridge, Drum Bridge, and also on trees by the Six-mile River, above Templepatrick, Down and Antrim. — S. A. S. Barren. * T. PAPILL08A. Wits. On trees, widely spread, but unfruitful, near Lisburn. — J. H. Davies. Greyabbey and Knock, Oo. Down ; Ballygomartin, and between Dunadry and Crumlin, County Antrim.— S. A. S. Barren. T. lasvipila. Brid. Common in Down, Antrim, and Derry ; occurring on trees, walls, and rocks. * T. FALLAX, Hedw ., VAR. BREVIFOLIA. Rare(?) Wet rocks by stream in Cregagh Glen, near Belfast. T. RIGIDULA. Dicks. Limestone rocks and moist banks near Belfast. — T. Drummond. Chalk rocks— Ballysillan, near Belfast; Rathlin (Antrim), Slieve Gallion (Derry).— S. A. S. T. INSULANA. Det Not. Divis Mountain. — Rev. C. H. Waddell. * T. ATRO VIRENS . Sm. Very rare. A very small tuft was found on rocks by the shore, Rathlin Island. — S. A. S. T. aloides. Koch. Walls, Narrowwater, County Down.— Rev. C. H. Waddell. T. stellata. Schreb. On clay, in crevices of slate rocks, Cregagh Glen, near Belfast.— S. A. S. A few capsules only, 12/2/77, and again in January, 1880. Trichostomum homomallum. Hedw. On micaceous rocks on Brean Mountain, above Glenshesk, Co. Antrim. — S. A. S. 206 Stewart— Mosses of North-East of Ireland (Supplement). * T. FLEXICAULE. Schwg. VAR DEN SUM. Schp. Very rare. On peat, Divis Mountain, near Belfast.— Rev. G. H. Waddell. * T. LITTORALE, Mitt. Very rare (?) On rocks by the shore, Rathlin Island, Co. Antrim.— S. A. S. * T. crispulum. Bruch. Var elatum. Schp. Very rare. Sparingly on rocks in Rathlin Island.— S. A. S. (Var. not found elsewhere in Ireland). T. mutabile. Bruch. Abundant on chalk rocks at Whitepark Bay, Ballintoy ; sparingly on Fairhead, Antrim.— S. A. S. No fruit. Pottia Heimii. Br. and Schp. Rocks by the shore, south of Newcastle (Down) ; Rathlin (Antrim).— S. A. S. * P. ASPERULA. Mitt. Very rare. In an old sandpit by the Groomsport Road, close to the Warren, Donaghadee (Down) ; ledges of basaltic rocks at Blackhead (Antrim) ; sparingly in both places. Fruit in January and February.— S. A. S. Referred to the above species with some hesitation. The three Pottias of Mitten are perilously near to each other. * Campylopus Sohwarzii. Schp. Very rare. Tievedocharrah, between Rostrevor and Hilltown, Mourne Mountains. — Rev. H. W. Lett. C flexuosus. Brid. Bencrom, Mourne Mountains.-Rev. H. W. Lett MountamT ^bove Bloody Bridge, Down, and on Knocklayd, Antrim. S. A. S. n June, July, and August. * C. atrovirens. De Not. Splashy, wet places on rocky moors ; rather rare. Kooky Mountain, Mourne range.-Rev. W. H. Lett. Slieye Donard, Down, and Knocklayd, Antrim. — S. A. S. Barren. Dicranum Bonjeanii. Bo Not. Rathlin Island. Sparingly.— S. A. S. * D. Scottianum. Turner. Mourne Mountains.— T. Drummond. Stewart — Mosses of North-East of Ireland (Supplement). 207 * D. rufescens. Turner. Rare. Crown Mountain, near Newry, Co. Down.— Rev. C. H. Waddell. Sandbanks near Belfast.— T. Drummond. Mountain above Glenshesk, Co. Antrim, on mica-schist.— S. A. S. D. cerviculatum. Hedw. Rathlin Island, Glenshesk, and frequent in turf bogs. — S. A. S. D. squarrosum. Schrad. Rostrevor, Co. Down. — Rev. C. H. Waddell. D. crispum. Hedw. Sandstone Rock, Derriaghy.— J. H. Davies. Plentiful on sandy bank between the Botanic Gardens and the Stranmillis Road, Belfast; also, on crumbling mica-schist above Glenshesk, Antrim. — S. A. S. D. pellucidum. Linn. Slieve Donard (Down), Slieve Gallion, and Carndaisy Glen, near Money- more (Derry).— S. A. S. Blindia acuta. Br. and Schp. Wet places on mountains and by rocky streams ; abundant where it occurs. Mourne Mountains. — Rev. C. H. Waddell. Abundant on mountains above Newcastle, Down, and on Knocklayd, Antrim.— S. A. S. * Anodus Donianub. Sm. Very rare. On Greensand rocks, by the stream, at the top of a little fall in Upper Collin Glen, near Belfast. In good fruit on 19th June, 1876.— S. A. S. Not found elsewhere in Ireland. * Rhabdoweissia denticulata. Brid. Crevices of rocks, very rare. Rocks on ascent of Slieve Donard by the Glen River, and between Donard and Tollymore (Down), also sparingly on summit of Slemish (Antrim).— S. A. S. R. fugax. Hedw. Slievenabrock, between Tollymore and Donard, Co. Down.— Rev. H. W. Lett. Weisbia verticillata. Brid. Limestone rocks, Rathlin Island. — S. A. S. 208 Stewart — Mosses of North-East of Ireland (Supplement). W. CRI8PULA. Hedw. Rocks and boulders, between Rostrevor and Hilltown, Co. Down. Rev. H. W. Lett. W. CIRRHATA. Hedw. boulders, on the mountain above Rostrevor Church— October, 1876. S. A. S. Phascum cuspidatum. Schreb. Rathlin Island. — S. A. S. Sphagnum papillosum. Lindb. Wet rocks, not common (?) On rocks on the mountains, above Bloody Bridge (Down), and sparingly on Rathlin (Antrim).— S. A. S. S. subsecundum, Nees ; var contortum, Schultz. Wet rocks ; rare. Plentiful on granite rocks in the mountains, above Newcastle, Co. Down. — S. A. S. Andrea petrgphila. Ehr. Slieve Donard (Down), and on basalt, Cave Hill (Antrim), at 700 feet. Mourne Mountains, near Hilltown.— Rev. H. W. Lett. West side of Bencrom, Mourne Mountains.— Rev. C. H. Waddell. Some fine tufts on — S. A. S. 11 FEB 1886 JJl VS. ir./S X APPEimix viii. I. NOTES ON IRISH COLEOPTERA, BY A. L. HALIDAY, F.L.S. EDITED BY S. A. STEWART, F.B.S., Edin. II. THE CROMLECHS OF ANTRIM AND DOWN, BY WILLIAM GRAY, M.R.I.A. III. NOTES ON THE PRE-HISTORIC MONUMENTS, AT CARROWMORE, NEAR SLIGO : THE BATTLE-FIELD OF THE NORTHERN MOYTURA. BY MR. CHARLES ELCOCK. PUBLISHED BY THE BELFAST NATURALISTS’ FIELD CLUB. January, 1885. I • rjs ■ 1 ( Proceedings Belfast Naturalists' Field Club. — Appendix 1883-1884.^ NOTES ON IRISH COLEOPTERA, By A. L. HALID AY, F.L.S. Edited by S. A. STEWART, Fellow of Botanical Society of Edinburgh. <^HE following list has been prepared from manuscript notes made by the ,, k*® A; L* Hallday» F.L.S. The MS. has been in the possession of the Editor for many years, and as a record of work done by one, who, in his day, ranked amongst the foremost of British entomologists, it has seemed a duty to give it to the public. Mr. Hahday was one of an illustrious band of naturalists whose love for scientific research, and success in the pursuit, conferred distinction on the town of Belfast during the earlier portion of the present century. It is matter for regret that, with respect to the labours of these local pioneers of science, so .I0 *as been upon record, and that their personal history is, in some cases, imperfectly known to their successors. We do know, however, that they were single-minded lovers of Nature, anxious only for a better knowledge of her ways, and careless as to whether their names should, in all cases, be associated with the discoveries they made. . Many of the species in the following enumeration have been noted, as Irish m Curtis’s Illustrations of British Entomology, but the greater part would seem to have remained unpublished. The nomenclature is that of the MS., without alteration, but in such cases as where an insect appears under a different name in Stephens’ British Entomology, the Editor has appended the latter as a synonym. Mr. Haliday had three distinct marks, which, placed against the names of the species m a classified list, constituted his method of recording the localities of his captures The first mark signified “near Belfast” ; the second, “ elsewhere in Ireland ; the third, “ English.” No further details are given. As we are not concerned with the English distribution, the two first only are reproduced tTSe .notes extend t0 Hymenoptera , and other groups, but being, as regards these, incomplete, and lacking localities are consequently omitted. 212 Halidaij.— Notes on Irish Coleoptera. SCABITIDiE. N.B. signifies Near Belfast; E.I., Elsewhere in Ireland. Clivina fossor Dyschirius politus gibbus1 . . minimus Curt. Cychrus rostratus Carabus catenulatus . . nemoralis 111. . . arvensis . . cancellatus . . glabratus . . nitens Pogonopborus (Leistus Freeh . . brunneus2 . . spini labris Helobia brevicollis . . nivalis Deg. Pelophila borealis3 Blethisa multipunctata Elaphras cupreus . . riparius Notiophilus aquaticus . . quadripunctatus . . biguttatus Bembidion paludosum Tachypus striatus . . andrese . . bipunctatus Thous celer . . pygmseus Lopha doris . . pusillus ? . . assimilis Peryphus littoralis . . femoratus . . viridi-ameus . . fuscipes . . atrocseruleus Notaphus bifasciatus Tachys obtusus . . . immunis , . pusillus Lega aenea4 . . fuscifres Ocys currens fulvi bar N.B. E.I l The statement in Cnrt. Brit. Ent. that D. gibbus “r' HaMay’ “ Bf&de°Sr was meant b Payk. was Ogured by Curt's from a specimen in Mr. HaUday’s Cabinet, take on the sandy shore of Lough Ncagli by Mr. ltobert Templeton, on 14th June, 1823. 4 Philocthua, Stephens’ Brit. Ent. Haliday — Notes on Irish Coleoptera. 213 SCAEITID^E. — Continued. N.B. E.I. Blemus paludosus Trechus suturalis . . fulvus . . ruficollis . . minutus, F. aquaticus Marsh. . . Ophonus puncticollis & * . . puhescens * Harpalus ruficornis . . rubripes . . rufimanus . . seneus . . dentatus Badister lacertosus . . humeralis Loricera pilicomis $je. Anchomenus albipes . . prasinus . . oblongus * Agonum picipes % . . pullum ? . . Simpsoni * . . maestum ? . . viduum * . . parumpunctatum . . * . . rotundatum % Synuchus nivalis % Calathus piceus . . frigidus1 * . . melanocephalus . . nubigena. M. * Amara acuminata . . vulgaris * . . eurynota * . . communis * . . familiaris * . . crassa * . . tibialis, wiki * Bradytus apricarius Cyrtonotus piceus * Cbloenius nigricornis * Pristonychus subcyaneus * Stomis pumicatus * Patrobus rufipes * Steropus madidus Poecilus versicolor * . . rutilans * . . cupreus * . . rufifemoratus Omaseus melanarius * 1 Cistelloides , Ml., fuscipes G-mel., flavipes, and obscurus Marsh. Ed. 214 Holiday — Notes on Irish Coleoptera. SCARITIDJE. — Continued.^ . , nigrita . , rufifemoratus . . tetricus1 . . Bulweri Argutor vernalis . . erythropus . . anthracinus2 Platysme nigra Abax striola Dromia melanocepbala « . . . meriodionalis 4maculata . . linearis . . punctatula Lamprias cblorocepbas gyrinid^. Gyrina seneus • • . . natator . . minutus • • 1 dyticidje. Dyticus marginalis . . pnnctulatus Acilius sulcatus Colymbetes fuliginosus . . agilis . . bipunctatus . . obscurus . . Sturmii . . paludosus . . bipustulatus . . cbalonotus . . striatus Laccopbilus minutus Noterus sparsus . . crassicornis Hygrotus confluens . . reticulatus . . inequalis Ilydroporus scitulus3 . . minimus . . pictus . . lineatus 1 This beetle was flrs. discovered and named by Mr. Hallday : it was described by him from specimens taken near Belfast. •» p'-4 * c”tls a°d steph6”B undet Jly groins. Haliday — Notes on Irish Coleoptera. 215 DYTICIDiE. — Continved. N.B. E.I. . . erythrocephalus * . , triguttatus * . . planus * . . nigrita * . . melanocephalus * . . geminus * . . rufifrons . . fluviatilis . . . . Haliplous ferrugineus * . . impressus * . . ruficollis % . . affinis * PARNIDiE. Parnns sericeus # . . auriculatus * HELOPHORIDiE. Octhebius bibemicus1 % . . impressus * . . maritimus Helopborus aquaticus . . granularis * . . griseus . . nubilus . . dorsalis * HYDROPHILIDiE. Limnebius mollis . . truncatellus * . . ater * . . . picinus % Hydrobius fuscipes * . . orbicularis % . . ocbropterus . . . . * . . melanocephalus * . . lividus2 . . bipustulatus * . . minutus . . globulus * . . picipes * 1 The specimen figured for this species in Curt. Brit. Ent. was taken by Mr. Haliday on rushes on the shore of Belfast Bay. 2 H. griseus Herb. ?, Marsh?, Oliv., Curt. Brit. Ent. 216 Haliday— Notes on Irish Coleoptera. SPHJERIDIADiE. Spheridion scarabasoides ... marginatum ... bipustulatum ... lunatum Cercyon littorale ... atomarium ... bemorrhoidale ... melanocepbalum ... ... pygmaeum ... terminatum ... centrimaculatum ... ... quisquilium N.B. E.I. ANIS0T0M1D-3E. Anisotoma ferrugineum1 ... cinnamomeum ... dentipes Clambus armadillus SCAPHIDIAMb Cypba Sericorderus tboracicus Clypeaster cassidiodes Catops rufescens ... sericeus ... agilis2 ... fomicatus Melegetbes rufipes ... aenea Nitidula yaria ... colon ... sordida ... discoidea ... bipustulata ... obsoleta ... silacea Catheretes caricis ... rufilabrum ... urticae SILPHIM. Pbospbuga subrotundata Silpba opaca Oiceoptoma rugosa ... sinuata Necropboras bumater ... vespillo ... vestigater Tbroscus dermestoides l This, and the following species were placed by Curtis, and also by Leiodes. a Cholera agilis , Stephens’ Brit. Ent. * * * * * * * * * * * * * * * * Stephens under Haliday — Notes on Irish Coleoptera. 217 ENGIDJE, Etc. Ips quadripustulatus1 N.B. * E.I. Antberophagus silaceus * Mycetia fumata * Biturus tomentosus * Cryptopbagus lycoperdi * ... fumatus * ... ulicis * ... cellaris * Atomaria ater * ... fuscipes * ... pbeogaster * ... caricis * ... globulus * ... birta2 * ... trichopteryx * Corticaria ferruginea * Latridius rugicollis * ... impressus * ... transyersus * ... ruficollis * Micropeplis porcata * ... tesserula3 * ... stapbylinoides * Byrrbus varius * ... pilula * Semplocaria semistriata * Hister carbonarius * ... cadaverinus * ... unicolor * ... purpurascens * ... 12 striatus * ... seneus * ... nitidulus * Monotoma juglandis4 * Onthophilus striatus * Abreus globusus . . * Stapbylrnus pnbescens * nebulosus * minimus * .. castanopterus * .. brunnipes * ,, erythropterus * ,, seneocepbalus * 1 The mark placed by Mr. Haliday opposite this name has been blotted, and there is some doubt as to what was intended. 2 Atomaria hirta , Curt. Brit. Ent. 3 Discovered and named by Mr. Haliday. The specimen figured by Curtis was taken out of a pond in the County of Down, near Belfast, in Feb., 1827. 4 Synchyta Juglandis , Stephens’ Brit. Ent. 218 Holiday — Notes on Irish Coleoptera. ENGIDJE, Etc .—Continued Philonthus splendens laminatus aeneus ,, decorus politus ,, marginatus ,, aterrimus ,, bipustulatus sanguineolatus ,, opacus , , punctus .. yarius , . fimetarius Cafias xantholoma Bionius cepbalotes ? Gabrius nanus Creophilus maxillosus Othius F fulminans Gyrohypnus cruentatus . . longiceps , , linearis , , punctulatus . . ochraceus Latbrobium fulyipenne , , elongatum . . brunnipes . . quadratum Sunius melanocepbalus Stenus bipunctatus , , oculatus . . flayicomis1 . . pubescens . . boops . . fuscipes . . circularis * * * * * * * * * * * Tacbyporus pusillus . . pubescens . . bypnorum . . abdominalis . . bipustulatus . . marginellus Tacbinus silpboides . . subterraneus * * * * . . pullus . . rufipes . . marginellus Hesperophilus hsemopterus ... . . coelatus Oxytelus rugosus 1 Query fulvicorni*. Haliday — Notes on Irish Coleoptera. 219 ENGIDiE, Etc.— . . carinatus ... • Continued. # o «• N.B. * B.I. . . piceus ... • a * . . laqueatus • a .. * . . depressus * . . sculpturatus ... * . . morsitans1 * Elonium rugosum ... * Bolitobius lumilatus * . . atricapillus * . . cernuus ... ... ... * analis * . . merdarius ... * Callicera vernalis2 * Megarthrus depressus ... ... * . . flavus ... * Aleocbara fuscipes ... * Proteinius brachypterus * Antholobium melanocepbalum * .. tectum * .. grossum3 ... ... * Omalium deplanatum * ,e rivulare * Lesteva caraboides * .. punctulata * .. obscura ... ... * Drusilla canaliculata4 * Pselapbus Herbsteri ... * Falagria sulcata * Tycbus niger * Autalia rivularis ... * .. impressa * Bryaxis j uncorum ... * . . sanguinea ... * Encepbalus complicans ... ... * Anthicus floralis ... * Anaspis lateralis ... .. * . . ruficollis ... * ,, obscura5 ... * Salpingus planirostris * Meloe violacea ... ... ... * 1 Platystephus morsitans , Step, Brit. Ent. 2 Callicerus S pencil. “Taken at Holywood in the shelter of furze bushes; in the first burst of spring I have found it abundant on the fresh grass of sunny banks.” A. L. Haliday, Ourt. Brit. Ent. “ 0. hybridus Hal. MS A single specimen taken at Holywood with the preceding species by Mr. Haliday,” Curt. Brit. Ent. 3 A.piceum , Step. Brit. Ent. 4 Astilbus cannliculalus, Step. Brit. Ent. 5 A. melanopa, Step. Brit. Ent. 220 Holiday— Notes on Irish Coleoptera. ENGIDjE, Etc.- ■Continued. N.B. E.I. Trogosita mauritanica ... ... ... * Atopa cervina ... ... • •• * Cryphon melanurus ... ... * .. marginatus ... ... * .. griseus ... ... • •• * Maltbinus flaveola ... ... * biguttatus ... ... •* * , , brevicollis V * .. minimus * Thelephorus fulyicollis * . . testaceus • • * pallidus * .. bicolor ... ... * , . melanurus * .. setbiops ... ... * Elater nigroaeneus ... * ... testaceus1 * . , niger * ,. riparius2 * .. 4 pustulatus •• * Ctenioceras cupreous * Hemirbipus marginatus3 ... ... * ,, limbatus ... ... * .. segetis ... * ... obscurus * Corynetes quadra ... ... * Anobium rufipes4 ... .. striatum * Ptinus fur * .. crenatus * . . testaceus ... ... * Cis boleti ... * .. nitidus * Hylurgus ater .. ulicis ... * * . . piniperda * Rbizobius litura ... Cacidula pectoralis ... * Coccinella 7 punctata6 * ,. 14 guttata ,, variabilis ... • ^ , . conglobata . * . . 11 notata ... • * ,. 13 punctata . * ,, 22 punctata ... • * 1 Aplotarsus testaceus, Step. Brit. Ent. . 2 This, and the succeeding species stand under Hypnoidus in Stephens’ Brit, n . 3 Cataphagus, Stephens’ Brit. Ent. 4 Death-watch. 5 Lady-hug. Holiday — Notes on Irish Coleoptera. 221 ENGID^, Etc.- ■ Continued. N.B. E.I. • • 18 guttata • •• ... ... ... * 11 punctata ... ... * . . 14 punctata ... * Scymnus discoideus .. * Cassida viridis ... ... , , rubiginosa ... Helodes phellandrii * Timarcha coriaria ... ... Chrysomela margenella1 * • • cochleanac ... -Jjf , , betulae ... ... ■iff # # vitellina ... %- polygoni ... • 0 rapbani ... ... * . , polita . . stapbyloea ... * • • Banksii * Galeruca tanaceti * . , capreae ... ... ... * Haltica testacea2 ... $ # # tabida ... ... • • lutescens ... ... parvula ... ... ... * lurida ... ... ... * ... caerulea ... * • • nemorum3 ... M 4 pustulata ... ... * 9 , erucae mmm ... ... * • 0 oleracea * • 0 atricilla .00 ... ... • 0 fuscipes ... * % 9 lepidii ... ... * t # orbiculata * • • dentipes ... ... ... * |# belxinus ... * • • aurata ... * • 0 rufipes . . * # § transversa ... * • 0 exoleta 9 , nigricollis * , # sordida ... ... • 0 byosciami ... ... ... * 0 0 affinis ... ... ... Lema puncticollis4 ... ... ... * cyanella ... * Leptura laevis ... * 1 Includes Phsedon of Stephens’ Brit Ent. 2 Under Haltica we have here insects of the genera Haltica, Thyamis, Macronema, and Sphxroderma of Stephens’ Brit. Entomology. 3 This minute beetle is the destructive “ Turnip Fly.” 4 Crioceras, Step. Brit. Ent, 222 Holiday — Notes on Irish Coleoptera. ENGIDiE, Etc.- ■ Continued. N.B. E.L . . f emorata • •• ... ... ... 9ft . . elongata ... ... 9ft Cerambyx moscbatus1 ... 9ft Pogonocerus nebulosua ... ... 9ft * . . hispidus ... ... ... ... * Brucbus granarius ... * Apion nigritarse 9jt . . pallipes ... ... . . flavif emoratum2 ... ... ... 'V' 3ft , , vicise ... ... 3(t . . hydiolapatbi ... ... 3ft • • bsematodes ... . . gibbirostre3 ... ... 9|t 3ft . . ervi ... ... ... 3ft • , craccse ... 3ft • , eeneus ... ... ... ... 3ft . . yorax .. ... 3(t Bbyncbites alliarise ... ... •• * . . nanus ... ... * Bampbus? pulicarius . .. ... 3ft Tacbyerges salicis4 ... ... 3ft Orcbestes fagi ... ... 3ft . . f errugineus ... 3ft . . scutellaris ... ... ... Tycbius cinerascens ... Hypera nigrirostris ... ... 3ft . . polygoni . ... ... ... 3ft . • plantaginis ... ... 3ft • • rumicis ... ... 3ft . . punctata ... ... 9ft , • miles ... . . .sk. . . pollux .../ vF 9ft Notaris acridulus ... 3ft Leisoma punctata ... 3ft Hylobius abietis ... ... 9ft Barynotus mercurialis ... ... • • 3ft Alophus ran ... ... 3ft Bagous Latbburii ... ... 3ft Mecinus semicylindricus ... ... 3ft Dorytomus tortrix ... ... ... 3ft . . pectoralis ... 3ft . . maculatus5 ... ... 3ft Antbonomus pomarium ... ... # . . fasciatus ... ... * . . ulmi ... ... ... Balaninus salicivorus ... ... ... $ Cionus scropbulariae ... ... * Orobitis globosus . , ... ... * Sphaerula lytbri ... ... ... ... * 1 Aromia moschata , Curt. Brit. Ent. 2 A. apricans , Step. Brit. Ent. 3 A. carduorum , Curt., and also Step. Brit. Ent, 4 Orchestes salicis. Curt. Brit. Ent. 5 D, fumosus, Step. Brit. Ent, Haliday — Notes on Irish Coleoptera. 223 ENGIDiE, Etc. — Continued. Grypbidius equiseti Rbinonchus pericarpius . . castor . . 4 tuberculatus Nedyus boraginis . . pollmarius , , erysimi . . contractus , . assimilis . . troglodytes Ceuthorrbynchus sulcicollis , . didymus Pacbyrbinus leucogaster Phyllobius argentatus . . parvulus Polydrusus micans * * * * * * * * * * * * * . , oblongus1 Sitona hispidula , , cannia . . lineata . . lineela . . tibialis Stropbosomus coryli Liophlseus nubilus Cossonus Tardii Calandra granaria2 Serica brunnea Anomala horticola3 Melolontba vulgaris4 Typbaeus vulgaris Geotrupes vernalis . . sylvaticus . . stercorarius Apbodius fossor . . fimetarius , , terrestris . . subterraneus . , granarius . . prodromus . . spbacelatus , . contaminatus . . nigripes . . rufescens , . merdarius . . granum . . turpis 1 Nemoicus oblongus , Step. Brit. Ent. 2 Corn Weevil. 3 Anisoplia horticola, Curt Brit. Ent. 4 Cockchafer, I ■ . - (Proceedings Belfast Naturalists' Field Club. — Appendix 1883-1884.,/ THE CROMLECHS OF ANTRIM AND DOWN; By WILLIAM GRAY, M.R.I.A., Ulster Provincial Secretary Royal Historical and Archaeological Association of Ireland. HE gradual decay, and, in too many instances, the complete destruction of our ancient monuments, must be deplored by every Irishman who truly loves his country. The plough, the spade, and the chisel have been employed in removing many of our pre-historic remains, because in this utilitarian age they have been considered impediments to modern improvements. Some have been destroyed by the injudicious zeal of professed archaeologists, and some by the thoughtless frolic of holiday excursionists. The destruction that has already taken place and continues unchecked, suggests the desirability, if not the^absolute necessity, for some protective measures such as may be secured by Parlia- mentary enactment. With this view a Bill has been frequently introduced into the House of Commons by Sir John Lubbock and others ; their laudable efforts have not as yet resulted in legislation on the subject. Let us hope that the enlightened spirit of the age will 226 Gray — Irish Cromlechs . swell the number of Sir John Lubbock’s supporters, and that the time is not far distant when we shall have our ancient monuments under the protection of the Crown, and secure from the decay to which they are now exposed. Anticipating such an event, it is most desirable that we should have some complete catalogue or schedule of the ancient monuments of all kinds at present existing in Ireland. Already certain lists have been prepared— in England, by a Committee of Archaeologists, selected by the Society of Anti- quarians ; in Scotland, by the Society of Antiquarians of Scotland ; and in Ireland, by the Royal Irish Academy. Notwithstanding the efficiency of these organisations, and the ability of the several archaeologists employed, the schedules prepared were very far from complete, especially for Ireland, mainly because there was no systematic effort hitherto made to catalogue the monuments existing in this country. The appeal for contributions to this end, made in the 4th vol. of the Ulster Journal of Archceology, met with no response. Doubtless, descriptions of all the more important structures may be found scattered throughout works of history and archaeology, or in the transactions of learned societies ; but an attempt to tabulate the records thus available would not be so useful as a catalogue compiled from recent personal observation, whereby the present number and condition of our ancient monu- ments could be accurately set forth. The following contribution has been prepared under a con- viction that, with our available organisations and the number of public officials now engaged throughout the country, a complete catalogue of all our Irish ancient monuments could be readily compiled, and the author hopes he may be able to render some assistance in this direction, particularly for the North of Ireland. In an undertaking of this kind it is necessary that the several monuments should be grouped under separate headings, according to their most distinctive characters. This systematic classification of the monuments would facilitate the distribution of the work to be done, and secure a more satisfactory result, Gray — Irish Cromlechs . 227 IRISH CROMLECHS. In the absence of any fixed code of terms, the author, like many other writers on the subject, has to make his own selection, and having undertaken to catalogue “ The Cromlechs of Antrim and Down,” it will be necessary, in the first instance, to settle what is to be understood by the term “ Cromlech.” This is all the more necessary because of the conflict of opinion entertained by archaeologists with reference to the proper application of the term. The opinion that prevails most commonly among the country people is, that the monuments were built by the Druids as altars. An exposition of this erroneous idea is given in the Dublin Penny Journal , 31st May, 1834, page 381, where the writer says : — “ This species of rude altar is very common in many parts of Ireland ; it is called both in the Irish and old British language 1 Crom liagh ’ and ‘ Crom-lecht/ which signify in both a crooked stone, not from any crookedness, but from their inclining posture. They are supposed to have been so formed, in order to allow the blood of the victims slain upon them to run off freely.” O’Curry, in his lectures* refers to these monuments as “ vulgarly called Cromlechs,” and says 4‘ they never were in- tended, and never were used as altars or places of sacrifice of any kind, that they were not in any sense of the word ‘Druidical,’ and that they were in every instance simple sepulchres or tombs, each marking the grave of one or several personages.” Professor Nilsson says— “ They are called in Scania, dos, in Denmark, dyss, in England, cromlech , and in France, dolmen .” | The Rev. H. Rowland, in his work on the Isle of Anglesea,! says : — “ These altars of stone (where stone served to raise them up) were huge, broad, flattish stones, mounted up and laid flat upon * O’Curry’s Lectures on Ancient Irish History. Page 597. f S. Nilsson on the Stone Age. Page 159. f Mona Antiqua Restaurata. Dublin, 1723. Page 47. 228 Gray— Irish Cromlechs . other erect ones, and leaning, with a little declivity in some places, on those pitched supporters, which posture, for some now unaccountable reasons, they seem to have affected, and were and are to this day vulgarly called by the name of ‘ Cromlech,’ either from their bending position, which is gene- rally believed, or rather (that bending posture being not always to be found in everyone of those monuments, nor, indeed, applicable to the idea and notion of ‘ Crom’ in our language) that these first men (I shall adventure to guess) carried the name with them from Babel, as they did several other words, and called it ‘ Caeraem-lech,’ from the Hebrew 1 Caerem-luach, a devoted stone or altar.” In Owen Connellan’s edition of the Four Masters* we have the following note : — “ The name Cromleac signifies the stone of Crom, and they were so called from being used in the worship of Crom, one of the deities of the Irish Druids, said to represent Fate ; or, according to Lanigan and others, the god of fire, or the sun, and sometimes called Crom Dubh, or Black Crom, and Crom Cruach, signifying Crom of the Heap of Stones or Cairns, as quoted by Lanigan from the Tripartite Life of St. Patrick ; and the Idol of Crom Cruach, as stated in Lanigan and O’Flaherty’s Ogygia, quoting from the Four Masters, and also in the Book of Invasions, by the O’Clerys, was destroyed by St. Patrick in the temple of the Druids, on Magh Sleacht, in Brefney, now Fenagh, in Leitrim ; and the last Sunday of summer is still called Domhnach Chrom Duibh, or the Sunday of Black Crom, being sacred to St. Patrick as the anniversary commemorating the destruction of the idol. This is the real origin of the name Cromleac, and not from the stones being in a sloping position, as absurdly stated by some writers, and derived fron the opinions of the common people.” Sir John Lubbock says “ Cromlech is derived from ‘ Crom,’ a circle, and ‘ lech,’ a stone, and Dolmen from 1 daulj a table, and t maen ’ a stone and, with reference to the terms, adds — “They * The Four Masters. By Owen Connellan. Page 271. Gray— Irish Cromlechs . 229 should, therefore, certainly be used as in the text — that is, that the word ‘Cromlech’ should include stone circles , and ‘Dolmen* should be applied to stone chamber si* The terms Cromlech and Dolmen may be almost etymological equivalents, yet the adoption of the term “ Dolmen" would not be sufficiently distinctive for our purpose, because the Conti- nental archaeologists include several kinds of monuments under that denomination. The term is not of Celtic origin, and it does not harmonise with Irish words. Mr. Edward T. Stevens, in “ Flint Chips, ”j describes chambered tumuli under the name of Dolmens. It will be observed that the authors just quoted employ both the terms, “Dolmen” and “ Cromlech,” in a generic rather than in a specific sense, and describe a great variety of monuments under the respective terms. See also “ Essai sur les Dolmens,” by Baron de Bonstetten, of Geneva. Dr. Lukis, who has done good service in exploring the ancient monuments of the Channel Islands, would include all our crom- lechs under the general term “chambered tumuli,” being of opinion that all were at one time of their history covered.! In the first volume of the “Royal Irish Academy Museum Catalogue,” the author, Sir W. Wilde, referring to the chamber found in Phoenix Park, says : — “ This discovery went far to establish the belief that cromlechs were but uncovered tumuli, which originally contained sepulchral remains.” Llewellyn Jewett adopts the theory of Dr. Lukis, and says that researches “ prove beyond doubt that the cromlechs are neither more nor less than sepulchral chambers denuded of their mounds.”§ On this point Mr. Ferguson, a well qualified authority, maintains a contrary opinion, and in his work on Rude Stone Monuments, says “ It seems impossible to believe that the bulk of those we now see were ever hidden by an earthen covering.”|| * Pre-historic Times. By Sir John Lubbock. Page 104. f Flint Chips. A Guide to Pre-historic Archaeology. Page 105. + ^ev> W. C. Lukis, Norwich. Vol. of Pre- Historic Congress. Capt. Oliver, R.A., “ Megalithic Structures of the Channel Islands.” § Grave Mounds and their Contents. Page 51. II Rude Stone Monuments in all Countries. By James Ferguson, D.C.L., F.R.S. London, 187a. Page 44. 230 Gray — Irish Cromlechs. If modern research had demonstrated that all cromlechs were originally only chambers of tumuli, it would still be advisable to use a term expressive of their present condition. For this purpose the author considers the term u Cromlech would be the most appropriate. The original condition of all cromlechs as chambers in tumuli is now incapable of proof, either in Great Britain or the Conti- nent ; it would, therefore, be very unwise to adopt a term that would express and perpetuate what must be only a conjectural idea of the original condition of these monuments. This is a fatal objection to the position taken by Dr. Lukis, in his controversy on the subject with Mr. Du Noyer, in which the former suggests that the terms “Cromlech” and “Dolmen” should be discarded, and the term “Chambered Tumulus” substituted, employing this term in a generic sense.* Mr. Du Noyer, in common with Sir Gardiner Wilkinson and Colonel Meadows Taylor, t adopts the term “ Cromlech,” but limits it very properly to a distinct form of monument, and states his reasons in a most exhaustive and valuable communi- cation, published in the journal of the Kilkenny Archaeological Society.! But the restrictions imposed by Mr. Du Noyer are embai- rassing and confusing, because he would limit the term “Cromlech” to such monumeuts as have been always sub- csrial — a character that is incapable of proof in any case ; and he further perplexes the matter by suggesting that the cromlechs were not in themselves places of sepulchre— an opinion quite untenable. See extract from O’Curry’s lectures quoted above. Besides, the character of the remains and objects found in the chambers of so many Cromlechs proves they were places of sepulchre. , Objections have been urged against the use of the term “ Cromlech,” because of its modern introduction, and because * Journal of Kilkenny Archaeological Society. Vol. V., page 495. f Transactions of the Royal Irish Academy. Vol. XXIV. Part 5. 1865. + Journal of Kilkenny Archaeological Society. Vol V. N.S. Page 474. 231 Gray — Irish Cromlechs. such a term is not known generally among the Irish-speaking people ; but such objections are not feasible, because it is only modern systematic classification that requires special specific terms, and such terms are not commonly employed by the people. The popular terms applied to ancient monuments even of the same class are nearly as varied as the localities in which the monuments occur. It should be noted, however, that in Ireland the prevailing idea involved in local names for crom- lechs is that of a bed or final resting place. If we refer to the ancient Irish manuscripts, we will find that the sepulchral monuments referred to under the generic term “Leacht,” include the group we call “ Cromlechs.’’ Dr. Sullivan, in his introduction to O’Curry’s lectures on the manners and customs of the ancient Irish, says : — “ The word leacht seems to have been a general term applied to stone sepulchral monuments, consisting either of unfashioned stones of every size piled up over a simple grave, or over an Indeilb cloich ' or stone chamber, or of a number of large upright flags, upon which was placed a great block of stone.” The latter kind of leacht is the monument popularly known as a “ Cromlech.” A simple flag marking a grave was called a leac or liace (plural leaca). When a number of persons were buried beside each other, their leaca were placed in a circle around the grave. Similar circles of leaca or upright flags were put around the leachts, formed of piles of stones. Pillar stones, or cairti, were also used to mark graves, and sometimes the name of the dead person was cut in Ogam upon them. The word leacht occurs frequently in topographical names, as, for instance, in Tamleacht) modernised in one case to Tallaght) a place near Dublin, but unchanged in Tamlacht O' Crilly , in the County of Londonderry. Tamleacht may be translated as the leacht of plague, and, so far as I know, consisted of several graves marked by a head and foot stone, or covered over by a mur clocihe or stone mur) and, where there were a number of them in the same place, surrounded by a circle of “ Leaca I* * Manners and Customs of the Ancient Irish. Vol. I., page 331. 232- Gray — Irish Cromlechs. Near Coagh, County Derry, or about five miles east of Cookstown, there is a very fine cromlech, locally known as “ The Tamlacht Stone”— i.e., the plague stone. Here we have the ancient Irish name “ leacht" popularly applied to a genuine cromlech. We may, therefore, reasonably accept the term “Cromlech” as a qualification of the generic Irish term “ Leacht”— and expressive of their usual leaning or bending character, due probably in many cases to the fact that their original constructers were not able to obtain suitable supporters and in other cases, where such supports gave way with time. The qualification “ crom” is, therefore, indicative of a bending with age, and is very significant. What we require is a specific term applicable to the particular group of monuments we wish to describe, and expressive of their present structural condition, without involving any theory as to their original condition or object, and the term Crom lech” meets these requirements fully. The majority of our sepulchral monuments are more or less chambered, but they are separable into groups, each being very distinct in character. Our chambered tumuli are quite distinct from our kistvaens, and both differ so widely from our crom- lechs that they could not be grouped under one head. We have a capital example of the chambered tumulus crown- ing the hill of Carnanmore, East Torr, in the parish of Cul- feightrin, County Antrim. This is the subject of our first illustration, which shows a distinct chamber formed of blocks of stones, roofed by large flags, and all closed or covered over by a great heap of small stones. There is scarcely a feature common to it and a Cromlech. See Sketch No. 1. Farther south in the same county, on the high ground three and a half miles from Carnlough, on the road to Ballymena, we have the subject of our second illustration— Doonan Fort— an example of a tumulus and kistvaen totally unlike what is understood as a cromlech, and which could not be grouped under that head. See Sketch No. 2. Certain chambers of kistvaens may occasionally be found that Gray — Irish Cromlechs . 233 very closely resemble cromlechs. As, for example, the kistvaen at Roughfort, in the parish of Templepatrick, which occurs about three and a half miles south of Doagh, and seven miles north of Belfast, and consists of a series of chambers forming a group forty feet long, the terminal chamber being very large, and covered by a great block of stone. There are about thirty-eight stones in the group, and the block over the large chamber measures 6 ft. X sj ft. X 3 \ ft., or equal to about eight tons. If, in the course of time, this single chamber was left standing alone, it would have all the characters of a cromlech, and might be very fairly described under that head. See Sketch No. 3. The author would define the term “ Cromlech” as an ancient rude stone monument composed of one large block, supported by two or more stones, usually set on end or edge, forming a sub-aerial chamber. Of such monuments the following include all those that occur in the Counties of Antrim and Down, and each of them has been personally examined by the author, and, as far as possible, measured and sketched. CROMLECHS IN COUNTY ANTRIM. The neighbourhood of Ballintoy, on the north coast of County Antrim, possesses many features of very great interest to the Irish archaeologist, particularly the picturesque slopes of Whitepark Bay, to the west of the parish church. The long stretch of sand-dunes that skirt the base of the talus, below the mural cliffs of chalk surrounding the bay, formed the camping ground of early settlers. The evidence in proof of those ancient settlements is furnished by the quantities of stone implements, worked flints, chips and cores, charcoal and pottery, that have been collected here from time to time, and which, from their quantity and variety, indicate long periods of continuous occupation.* * Journal of the Royal Historical and Archaeolgoical Society. 4th Ser., Vol. V., July, 1879. Belfast Naturalists’ Field Club Guide to Belfast, &c., 1873. 234 Gray — Irish Cromlechs. On the slopes of the higher hills, to the south of the public road above the bay, there are no less than three very fair cromlechs, as follows : — 1. MOUNT DRUID CROMLECH. Sketch No. 4. This monument occupies a very commanding site on the hill-side above the rectory, from which the headlands of the Causeway cliffs can be seen. It is known as the ‘‘Druids’ Altar,” and consists of a large block about 6^ ft. long and 5jft. wide, supported on three of the four smaller stones forming the chamber.* This monument comes within Sir John Lubbock’s category of cromlechs, because it is enclosed by two circles of stones, one inside the other. The diameter of the outer circle is about 35 feet, and the stones composing it are about two feet high. Where stone circles occur in connexion with tumuli, they are on the outside. So small a circle as we have here is an indica- tion that, at all events, this cromlech is not a mere chamber of an original tumulus, because a tumulus inside the circles could not very well cover the cromlech. The enclosing stone circle is an unusual feature in connexion with the cromlechs of the North-east of Ireland, and it is to be hoped that where they occur they may be preserved from further destruction. Sketch No. 4, and all the sketches illustrating this paper, have been taken on the spot by the author, who recommends that they should be compared with the respective monuments themselves, or with photographs of the monuments, rather than with such illustrations as are given in the statistical surveys for the Dublin Society, or in the “ Dublin Penny Journal.” 2. GLEGNAGH CROMLECH, BALLINTOY. Sketch No. 5. This small but very perfect cromlech is in the townland of Glegnagh, near a quarry on the hill-side, south of the public * Statistical Survey, County of Antrim, 1812 — Part II., page 582. “Dublin Penny Journal.” Vol. III., page 351. Gray — Irish Cromlechs. 235 road from Ball intoy to the Causeway, and about as far from the road to the south as Whitepark Bay cliffs are to the north side. The sketch is taken from the west side, looking towards the parish church. The islands off the west coast of Scotland can be seen from this monument. The author has found worked flints, flint flakes, and numerous chips of flint very near the cromlech. Stone celts have also been found in the immediate neighbourhood. 3. CLOGHNABOGHIL CROMLECH, BALLINTOY. Sketch No. 6. This is the smallest cromlech in the North-east of Ireland. Its local name, Cloghnaboghil, signifies the stone of the boy. It is situated on the high ground in the townland of Lemnabeg, within half a mile to the west of Glegnagh Cromlech (2), and within sight from the public road. From the open and elevated position of this cromlech there is a very extended prospect seaward, including a considerable portion of the west coast and islands of Scotland. 4. CLOGHANUNCHER CROMLECH, BALLYCASTLE. Sketch No. 7. This cromlech occurs on the heath-covered mountain, in the townland of Ballyvennaght, on the north side of the road from Ballycastle to Cushendun, and near what is known as 4 * * * * * * 11 The Hungry House,” being the house highest on the mountain in that direction. There are three bridges on the county road near “ The Hungry House,” and the cromlech is about a quarter of a mile from the centre bridge, in the direction of East Tor. The chamber, measuring about 5 ft. X 3^ ft., is formed of four upright stones, and is covered by a large stone 9 ft. long and 7ft. 6 in. wide, all the materials being of the Cambrian rocks of the district. There is a very good standing stone, gallaun or menhir, on a hillock near this cromlech, and it can be seen from the county road. 236 Gray- — Irish Cromlechs . 5. BALLYVENAGHT CROMLECH, BALLYCASTLE. Sketch No. 8. This cromlech is about eighty yards north of No. 4. The sketch is taken looking south-west, and shows No. 4 Cromlech in the distance. The top stone measures 13ft. 4 in. by n ft. 6 in., and is about three feet thick. The supporting stones have given way, and are crushed under the ponderous cap stone. The site is a swampy moorland, at the head of the valley of the Cary river. This and the last cromlech are almost overgrown with peat. 6. CLOGHS CROMLECH, CUSHENDALL. Sketch No. 9. In the townland of Cloghs, to the west of Cushendall and about one and a half miles from the village, there is a cromlech with a chamber four feet long and three feet four inches wide, formed of six blocks of stone. The cap stone is turned over from its original position, otherwise the monument is in fair condition. There were other stone monuments in the vicinity, but they have been destroyed. A rude stone circle and avenue occurs on the mountain slope one mile west from the road to Cushendun. It is locally known as “ Ossian’s grave.” The site commands an extensive prospect : from it the Scotch and Irish headlands can be seen, and is well worthy of a visit. 7. TICLOY CROMLECH. Sketch No. 10. In the townland of Ticloy — i.e., The Stone House there are two cromlechs in the same field, the most perfect being the subject of our sketch. The second is shown in the background. The name of the townland is derived from this monument, which still retains the appearance of a stone house. It is well situated on Ticloy hill, above Ticloy water, about five miles to the west of Glenarm, and ten miles east by north of Ballymena. The land is cultivated all round the site, but the farming operations are carefully conducted, so as not to damage the monument in any way. 237 Gray — Irish Cromlechs. The gossip of the neighbourhood tells of a former occupier of the farm who had a dream, in which he was informed that there was some treasure buried beneath the cromlech. It is said he dug for many days, and at last found a crock, and that afterwards he became very wealthy, but refused to give any particulars as to his supposed treasure. Doubtless he did find a crock in the shape of a cinerary urn, and his disappointment at not finding gold prompted his reticence. The ruined condi- tion of the second cromlech is, no doubt, the result of treasure- hunting, and to some extent corroborates the anecdote just related. 8. BROADSTONE CROMLECH, CRAIGS. Sketch No. ii. On a heathy moor, in the townland of Craigs and parish of Finvoy, there is a very remarkable cromlech, known as u The Bedstone.” It is about six and a half miles from Ballymoney in a southerly direction, or about one mile above the rectory of Finvoy. In former times this place was resorted to on Sundays and holidays for picnics, coursing, games, and pastime, and, doubtless, the consequent frolic and thoughtless mirth provoked on those occasions was the cause of the dilapidated condition of this monument at present. Happily there are very few who would wantonly or maliciously destroy our ancient monuments, yet the spirit that animated the ancient Cuitech Fuait, or funeral games, has expired long ago, and the object of their commemoration has been forgotten ; therefore, the young folk of modern times, who entertain no piofound veneration for ancient usages, think lightly of the injury their playfulness may occasion to ancient monuments, although they would not wilfully do them harm. The cromlech, as it now stands, is a restoration ; the cap-stone, measuring 8 ft. 6 in. by ioft., and about 20 in. thick, was thrown down, but was re-erected on its three supporters, as at present, by the people in the neighbour- hood. Adjoining the cromlech proper there are the remains of three or four circular chambers, and the group of stones 238 Gray — Irish Cromlechs. composing the cromlech and chambers is again surrounded by two concentric stone circles, the outer circle being about one hundred feet in diameter, and the inner fifty feet. Very little now remains to mark the outline of the circle. The sepulchral character of this very important monument is proved by the finding of cinerary urns in the round chambers. 9. FINVOY CROMLECH, CRAIGS. Sketch No. 12. Although Broadstone cromlech has been frequently described, the subject of this sketch has been apparently overlooked ; yet it is a very typical example, and occurs in a cultivated field close to the public road, within half-a-mile west of the Broadstone, and one mile east of the Presbyterian Church of Fmvoy. The cap-stone is a flat slab, measuring 8 ft. long by 5 ft. 6 in. wide, over eight upright stones, forming a well-marked oval chamber, the major axis of which runs E.N.E. by W.S.W. Formerly this monument was almost covered with earth, the cap stone alone being exposed. The earth was removed some years ago, and the monument now stands on the natural surface of the ground. During the excavation the chamber was explored, and a cinerary urn was discovered within. 10. CLOUGHOGAN CROMLECH, BALLYGILBERT. Sketch No. 13. On the eastern slope of Bally gilbert hill, above the old road from Larne to Glenarm, there is a cromlech locally known as Cloughogan. It forms part of a boundary hedge near a farm cottage, and has done service for many years as a pigsty and poultry-house. For this purpose the open space between the uprights have been carefully filled in with small stones. The thrifty housewife who made this change, claims the credit of having built the house. Her worthy spouse, however, contends that the Danes built Cloughogan before the memory of man, and that she only built the byre. This cromlech is about eight miles north of Larne, or three and a half miles south of Glenarm, Gray — Irish Cromlechs . 239 on the slope of the hill to the west of the old road from Larne to Glenarm. There are many other antiquarian remains in the same locality, and worked flints are found scattered over the surface of the fields. 11. DRUIDS’ COTTAGE CROMLECH, ISLANDMAGEE. Sketch No. 14. The subject of this sketch may be found at the road-side, on the hill overlooking Larne Lough, from the northern extremity of Islandmagee, opposite the point of the Curran, and about one mile from the ferry. A cottage has been built adjoining the cromlech, so that the latter stands within a few yards of the front windows— a circumstance that has, doubtless, served to preserve the monument up to the present. The cap-stone, which is about six feet long, covers a chamber formed of blocks of stone standing on end, and together form a very fair example of our Irish cromlechs. The folk-lore of the locality refers to this monument when it had a far more imposing appearance, being in early times surrounded by other stones, possibly a complete circle. The building of the cottage and other improvements removed all trace of the circle, and the cromlech now stands alone. Early in the present century a number of gold orna- ments were found in the immediate vicinity of the cromlech,* and worked flints may still be found on the surface of the sloping ground towards the lough. 12. FAIR HEAD CROMLECH, BALLYCASTLE. Away to the east of Ballycastle, above the collieries, on the rocky plateau of Fair Head, there are the remains of a small cromlech. Within living memory this monument was com- plete, and the chamber was the favourite retreat of badgers. Here the country sportsmen came with their dogs to hunt, and the 11 sport” resulted in the overturning of the cap stone and the comparative destruction of the monument. * See Dublin Penny Journal. Vol, J., 1832. Page 209. 240 Qray— -Irish Cromlechs. 13. CLOGHS CROMLECH, CUSHENDALL. Within about a quarter of a mile from No. 6, and farther down the slope of the hill, there was once a very large cromlech. Many of the stones that composed the chamber may still be traced in the fences near the site ; but the great cap stone and others were removed some years ago by an enter- prising workman, who had them blown up by gunpowder to supply material for building the adjoining house ; “ an by the same token,” says our informant, “ no good iver come if him. 14. MOYARGET CROMLECH. This monument stood near the southern, or rather eastern, bank of the Invir, or Inver, Water, now a small stream sepa- rating the parish of Ramoan from the parish of Ballintoy. Like the last, very little of it now remains to indicate its former importance. Twenty-five years ago the standing blocks were known locally as the grey stones. There were originally about six supporting stones about five feet long, the cap stone being about eighteen feet long. The Rev. George Hill, a well- known archaeologist, was one of a party who explored this cromlech in 1840. “A large urn of burnt clay was found about two feet below the surface, placed with the mouth down- wards on a rude pavement, and contained a dark paste, evident y ashes made damp.” This monument may have originally marked the burial-place of a great northern chieftain named Arghad, from whom the two townlands of Upper and Lower Moyarget (Magh- Arghad) may have had their names. 15. TICLOY CROMLECH, No. 2. This cromlech occurs in the same field as No. 7, and has been already sufficiently noticed. In sketch No. 10, the blocks of stone that composed the monument are shown at the foot of the tree in the background. 24! Gray— Irish Cromlechs . 16. DRUMAGORGON CROMLECH. Within about three miles from Antrim to the N.E., in the townland of Drumagorgon, there are the remains of a cromlech, locally known as “ the giant’s grave.” The cap stone, about six feet long, has been overturned, and the monument otherwise dismantled, but not beyond the possibility of restoration. Tradition says that the adjoining hill to the east, known as “ The Standard,” was the scene of a great contest between two rival chiefs, and that one was killed and buried in this cromlech, together with his weapons of war. An enquiring antiquarian, early in this century, wishing to test the accuracy of this story, dug below the cromlech, and discovered such remains as satisfied him that a burial did take place here — a conclusion that was come to at the expense of the cromlech. CROMLECHS IN COUNTY DOWN. 1. GIANT’S RING CROMLECH, DRUMBO. Sketch No. i. Plate XVI. One of the most remarkable of the ancient monuments in the County Down is the well-known Giant’s Ring at Drumbo, about three and a half miles to the west of Belfast. It consists of a circular rampart of earth, enclosing a space of about six hundred feet in diameter, or an area of eight acres. The earthwork is in a very fair state of preservation, owing to the judicious care of the owner, who had the rampart surrounded by a masonry wall, and otherwise well protected. The height of the earthen rampart is sufficient to shut off a view of the surrounding landscape. In section it has a good broad base of about eighty feet, and slopes equally at both sides. The top, at present, is somewhat flat, a form which is apparently due more to weathering than to the original construction. The cromlech stands almost in the centre of the enclosure ; all the stones forming the chamber are in situ , but others are more or less disturbed, and seem to indicate that there was 242 Gray— Irish Cromlechs. originally an avenue leading to the chamber. In former times “the ring” was used as a race course, for which it was admirably suited, the rampart making a “ grand stand.” Under the circumstances, it must be a matter of congratulation that we have so much of the monument preserved. Excavations have been made in the vicinity of the enclosure, and several sepulchral remains have been found. A circular chamber was exposed about seven feet in diameter, formed of blocks of stones covered over with flags. Minor internal divisions of the main chambers contained four cinerary urns and other evidence of ancient burials. Within a short distance of this chamber several other cists of sepulchral character were discovered, all indicating the importance of the central monument in ancient times.* 2. KEMPE STONE CROMLECH, DUNDONALD. Sketch No. 2. The megalithic monument, locally known as the Kempe Stone, is one of the most important in County Down. It occurs on the high ground about a mile to the west of the village of Dundonald, and not far from the main county road from Belfast to Newtownards. The group of stones composing the monu- ment occupy a space of 12 ft. by 8 ft., and stand ten feet high to the east and six feet to the west. The chamber measures five feet long, five feet wide at east end, and three feet wide at the west. This chamber is formed of six blocks of stone ; the eastern blocks are upright, and the side blocks are on edge, eight, and seven feet long respectively ; the cap stone measuring eight feet six inches long, seven feet wide, and on an average three feet six inches thick. The block must weigh about seventeen tons. The top of the cap stone has a quick fall or slope to the west. This feature, so common to our cromlechs, may in this case be due to original construction, as the stones supporting it at the west are smaller than those at the east end, and the cap itself is thinnest at the west end. The present name of the townland is Greengraves. The locality was formerly denominated Bally-clogh-togle (town of the raised or lifted * Ulster Journal of Archaeology. Vol. III., page 357. Gray — Irish Cromlechs . 243 stone). Local tradition states that a stranger warrior has been buried there. Apart from the monument itself, there are scattered all round the vicinity large blocks of stone. Many of them are now built into, or form parts of the boundary hedge. Their distribution and character indicate that they are the remains of some dismantled megalithic monument of very considerable importance. 3. MOUNT STEWART CROMLECH. Sketch No. 3. Within the demesne of Mount Stewart, in the parish of Greyabbey, about five miles from the town of Newtownards, there is a small cromlech-like monument, the remains of a very remarkable cemetery that once existed here. It consisted of a cairn of small stones about thirty feet in diameter and five feet high, and constituted what might be denominated a chambered tumulus* In 1786 the then owner of the estate considered it desirable to drain the field, and the work was undertaken, calculating upon the advantage of having so large a supply of suitable material for filling up the drains. As the workmen employed removed the stones from the cairn, or tumulus, they exposed on the southern portion of the heap a number of cists or stone chambers (between sixty and seventy), formed of stones on edge, and covered by flags. In the north- west corner of most of the chambers there was deposited a cinerary urn, many of them being quite perfect and elaborately decorated with the usual incised patterns, specimens of which are to be seen in private collections, and in the Belfast Natural History Museum. The central chamber was very much larger than the surrounding cists, and constitutes the subject of our sketch. At the side of the cromlech one of the smaller cists, or sepulchral chambers, is preserved. A full description of the exploration of this monument is given in a pamphlet, entitled “ An Historical Essay on the Parish and Congregation of Grey- abbey,” by Dr. S. M. Stephenson, published in Belfast in 1828. * See Ulster Journal of Archaeology. 244 Gray— Irish Cromlechs . 4. LOUGHMONEY CROMLECH. Sketch No. 4. The parish of Saul, so closely identified with the life and labours of St. Patrick, is rich in antiquarian remains, of which the cromlech of Loughmoney is one of the most interesting. It is in a good state of preservation, and stands in a field close to the public road, a few miles east of Downpatrick. The cap stone measures nine feet six inches by five feet three inches, supported by only two stones on edge, each seven feet by three feet, forming a chamber about two feet ten inches wide, and at present open at both ends. 5. LOUGHANISLAND CROMLECH. Sketch No. 5. On the north shore of Loughanisland lake, four miles south of Crossgar and four miles west by north of Downpatrick, near the Buck’s Head Tavern, in the townland of Annadorn, there is a cromlech having a well-defined chamber of four large blocks of stone, with a cap stone measuring eight feet by seven feet. The latter has been turned over a little from its normal position. Some years ago a utilitarian wanting building materials set about demolishing this cromlech by a powder blast. . A splinter of rock fell on and damaged the roof of his dwelling-house— an incident he took to be an omen of bad luck, and quietly gave up the undertaking. 6. SLIDDERY-FORD CROMLECH. Sketch No. 6. Within a mile of Dundrutn, at Sliddery-Ford, on the New- castle road, in the townland of Wateresk, there is a very perfect cromlech. The cap stone, a granite block, measures seven feet six inches by seven feet six inches, or nineteen feet six inches in girth, covers a chamber formed of three blocks of stone, one being six feet high. In Dubourdieu’s statistical survey of County Down, page 271, he describes a circle of twelve standing stones near this cromlech. At present there are but two in the 245 Gray — Irish Cromlechs. locality, at the side of a lane, a little to the south of the cromlech, one of the stones being eleven feet high. The field in which the cromlech stands also contains a souterrain or underground dwelling, and the view from the cromlech overlooks the sand- dunes of Dundrum, which have yielded such a number of worked flints, stone implements, pottery, and other evidences of ancient settlements.* 7. CLOUGHMORE CROMLECH, GOWARD. Sketch No. 7. The cromlech known as Cloughmore, on the mountain side, in the parish of Clonduff and townland of Goward, is one of the largest and best in the county. It is accessible from Hill- town or Rathfriland, being two miles from the former and five from the latter. It consists of a massive cap stone of granite, thirteen feet long, ten feet wide, and five feet thick, weighing probably fifty tons, supported by a group of nine other stones forming several chambers, the principal chamber being nine feet long and three feet six inches wide. One of the front uprights is very slender, and stands seven feet high, the complete monument being fully fourteen feet high. Local authorities state that formerly this cromlech was enclosed by a circle of stone blocks or standing stones. They have been long since removed, and there is no trace of them existing at present. Excavations have been made below the cromlech, and cinerary urns, with other evidence of sepulture, were found within the main chamber. At present the site is protected by a planting of fir trees, and the tenant of the adjoining cottage is the honorary caretaker of the cromlech. 8. LEGANANNY CROMLECH, DRUMGOOLAND. Sketch No. 8. On the craggy southern slopes of Cratlieve mountain, in the parish of Drumgooland and townland of Legananny, the subject of this sketch stands on an exposed site, commanding an exten- * Journal of Royal Historical and Archaeological Society of Ireland. Fourth Series, Vol.V. 246 Gray — Irish Cromlechs . sive prospect to the south and west. The cap stone is shaped like a coffin, fixed north and south, eleven feet four inches long, four feet nine inches wide at the shoulder, and three feet wide at the foot or north end, in which direction it has a slope clearly due to its original construction. It is supported on three upright blocks— two at the south end measuring seven feet and six feet two inches respectively, while the upright at the north end is only four feet five inches high. This upright has been fixed on a bank as if to increase its height, and as all stand now on the bare surface, this northern prop is very unstable, and should be secured. Some years ago an urn was found in the open chamber below the cromlech. Mr. Ferguson, in his work on rude stone monuments,* gives a figure of this cromlech from a drawing by Sir Henry James, of the Ordnance Survey, and refers to it in his argumeut combating Mr. Lukis’ idea that all cromlechs were originally chambered tumuli. 9. KILKEEL CROMLECH. Sketch No. 9. Within a half mile of Kilkeel, in the south of Down, off the road to Newcastle, there occurs a megalithic monument known as the “ Crawtee Stone,” probably from the Irish word emit, meaning hump, which expresses very clearly the shape of the cap stone of granite, nine feet long and eight feet six inches wide, that covers the chamber beneath, measuring about five feet six inches square, and formed of four water-worn boulders of granite, such as were, doubtless, common in this district in pre-historic times. The sketch is taken looking towards the Mourne Mountains. Some years ago, the promoters of some local building speculation debated the advisability of destroying the monument for the materials it would afford. After due deliberation they fortunately abandoned the project, not moved by the laudable desire to preserve our ancient monuments, but they yielded to the dread of unlucky consequences. A similar dread prevents timid folk passing this cromlech alone after dark. * Rude Stone Monuments of all Countries, By J. Ferguson, D.C.L., F.R.S. London, 1872. Page 45. 247 Gray— Irish Cromlechs. 10. CAUSEWAY WATER CROMLECH. Sketch No. io. The Causeway Water is a mountain stream that runs south- west along the eastern boundary of the townland of Kilfeaghan, and crosses the public road from Warrenpoint to Kilkeel, four miles from the latter place. To the west of the river, on the slope of Kurckshee, there is an excellent cromlech on a site that overlooks Carlingford Lough. A block of rounded granite ten feet long, eight feet wide, and five feet thick, weighing probably 30 tons, forms the cap stone over a chamber composed of several granite blocks on end. The site has become a rubbish-heap for ages, and all the loose field stones and other impediments to farming operations have been collected around the cromlech so far as to almost hinder the goats from taking shelter in the chamber as they were wont to do. To the east of the cromlech, and close to the bank of the river, there is another megalithic structure, more like a kistvaen, and the site around has yielded several examples of stone implements. 11. SLIEVENAGRIDDEL CROMLECH. On the topmost peak of Slievnagriddel Mountain, within a few miles to the east of Downpatrick, there are the prostrate remains of a once standing cromlech. The blocks that com- posed it are now resting on the bare rock. The cap stone measures eight feet by six feet, and below it are two slabs that formed the sides of the original chamber. It is said that this cromlech was thrown down by the officials of the Ordnance Survey. 12. SAMSON’S STONE CROMLECH. Near Downpatrick, to the south of the town, there is a large transported block known as Samson’s Stone. This may be the remains of a cromlech such Mr. Du Noyer describes as “earth- fast.’’* The Rev. J. O’Laverty, M.R.I.A., refers to this as a “ ruined cromlech.” See his work on Down and Connor. Vol. *•» page 252. • Kilkenny Archaeological Society. Vol. V. New Series. 248 Gray— Irish Cromlechs . 13. DROMORE CROMLECH. (?) Taken down many years ago to supply stones for a rockery in the Palace Garden. 14. DRUMGREEN CROMLECH. (?) Forty years ago there was a cromlech in the townland of Drumgreen, on the road from Newry to Rathfriland. A large cap stone stood on three supporters. All have been removed to make building materials and road metal. The above list, in the opinion of the author, contains all the known cromlechs of Antrim and Down. If found imperfect, the author will be glad to receive any correction from friendly critics; and such corrections, together with any assistance rendered towards compiling a schedule of the ancient monu- ments of the North of Ireland, will be gratefully acknowledged. Note. — This mark (?) is placed after all the cromlechs that cannot be vouched for upon the author’s personal observation. * PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PLATE IX. COUNTY ANTRIM. Chambered Tumulus, Carnanmore. 1 PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). COUNTY ANTRIM. Kistvean, Roughfort. 3 PL A TE X. Mount Druid Cromlech, Ballintoy. 4 PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PL A TE XI. COUNTY ANTRIM. Glegnagh Cromlech, Ballintoy. 5 C LO U G H N A BOG H I L CROMLECH, BaLLINTOY. 6 PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PL A TE XII. COUNTY ANTRIM. Cloughanuncher Cromlech, Ballycastle. 7 Ballyvennaght Cromlech, Ballycastle. 8 PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB, 1883-84. (APPENDIX). PL A TE XIII. COUNTY ANTRIM. PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PL A TE XIV. COUNTY ANTRIM. Broadstone Cromlech, Craigs. 11 Finvoy Cromlech, Craigs. 12 PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB, 1883-84. (APPENDIX). PLATE XV. COUNTY ANTRIM. Cloughogan Cromlech, Ballygilbert, 13 Druids’ Cottage Cromlech, I s la n d-M ag e e. 14 ■ PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB, 1883-84. (APPENDIX). PL A TE XVI. COUNTY DOWN. PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB, 1883-84. (APPENDIX). PL A TE XVII. COUNTY DOWN. PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB, 7883-84. (APPENDIX). PLATE XVIII. COUNTY DOWN. Slidderyford Cromlech, Dundrum. 6 \ PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PLATE XIX. COUNTY DOWN. Cloughmore Cromlech, Goward. 7 Legananny Cromlech 8 ✓ PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PLATE XX. COUNTY DOWN. Kilkeel Cromlech. 9 Causeway Water Cromlech, Kilfeaghan. 10 ( 'Proceedings Belfast Naturalists' Field Club .—Appendix 1883-1884^ NOTES ON THE PRE-HISTORIC MONUMENTS AT CARROWMORE, NEAR SLIGO : BATTLE-FIELD OF THE NORTHERN MOYTURA. BY CHARLES ELCOCK. FT two and a half miles south-west of Sligo, the it road to Seafield passes through Carrowmore, in parish of Kilmacowen. It lies at the foot of Knock- narea, on the summit of which, at an elevation of 1078 feet above the sea, stands the large tumulus of the celebrated Queen Meave, which has served for many a century as a mark for mariners far out at sea. Carrowmore is slightly elevated above the surrounding country, and the surface is considerably undu- lating. The whole district, and for many miles in a line nearly north and south, inclining a little to the north-west and south- east, is covered with large, irregular, erratic blocks of coarse granite, dropped during the glacial period. Carrowmore may be regarded as classic ground, and the anti- quarian may here revel for days in examining the various rude stone monuments, such as cromleacs, cists, stone circles, tumuli, 250 El cock — Pre- Historic Monuments at Carrowmore . cahirs, and forts which abound upon it. It is the site of the last and desperate battle fought by the Firbolgs,* about the year 30 B.C., just before they fled to Aranmor, where several of their stone cahirs still remain. At Carrowmore they made their last stand on the mainland of Ireland. The name of the Northen Moytura is given to the battle there fought, so as to distinguish it from a previous hardly-contested battle, fought about seven years earlier, on the plain of the Southern Moytura, close to Cong, at the north end of Lough Corrib. The monuments on the latter battle-field, though of a very different character to those at Carrowmore, are equally remark- able and interesting to the antiquary, and form a lasting memento of the fierceness of the struggle which, occupying several days, there took place. They are well described in Wilde’s “ Lough Corrib,” the account being, perhaps, rather too florid for exactness. The monuments on Carrowmore, of which, in 1883, sixty- three could be identified, are clustered together within a roughly oval space of about three-quarters of a mile long by less than half a mile wide. Near the centre of this is a large mound, of which the proper or original name is supposed to be lost. It is now called Listoghil, which I was told on the spot, means rye- fort. But some little investigation kindly undertaken by my friend M. J. Ward, leads him to the conclusion that its deriva- tion is from “ lis”=fort, and “ toghuil” = overthrow, —the Fort of Overthrow,— which possibly may be the “real, original” name, given to mark the spot of the decisive struggle. Listoghil is a large heap of small stones, and for many years served as a quarry for road metal. However, one day when the workmen were carting the stones away, they came upon a huge flat stone resting on several others, “ like a table,” and fear at once stopped any further destruction. It was evident that Listoghil was not a mere mound, but was one of the ancient * For an examination of the question as to whether there was a second battle of Moy- tura fought— which some query— see Jubainville’s “ Cycle Mythologique Irlandais, where the whole matter, with many references, is largely gone into. Elcock — Pre- Historic Monuments at Carrowmore. 251 monuments of which so many lie scattered around it. In 1837 the fort (as it is called) was about one hundred and fifty feet in diameter ; in 1883 it is about one hundred and twenty ; originally, it was probably about fifty feet high. Two stone circles formerly surrounded Listoghil, the outer circle consisting of one hundred and fifty stones. Some of these are still standing. From the top I counted twenty-two stone circles in sight, and six cromleacs, besides the one under my feet. The large stone, u like a table,” which had become exposed, is the cap stone of a large cist, or cromleac. It is a flat lime- stone flag, about nine feet six inches square by one foot six inches thick. The height of the supporting stones I could not determine without excavation, which could not be undertaken. The interior of the cist or chamber is considerably filled up with boulders, which have been thrown in at the entrance to please the rustics by u the thundering noise they make.” The cist was opened “ some years ago ” by “ some distinguished man,” whose name I could not learn. He brought two men with him, and they dug down inside the chamber, and found u burnt human bones, charred wood, and a large stone spear-head,” which were carried off. All trace of them is now lost. I was told by the farmer, in whose fields most of these monuments stand, that burnt bones, “ like horses’ bones,” are still found at Listoghil when a fall of the loose stones occurs. Entrance to the cist cannot now be had without removing the stones lying about. By lying down I got my head inside, and thought I could detect some rudely incised circles on some of the stones, one circle being about ten inches in diameter. These need further investigation. Dr. Petrie’s* number for Listoghil is 51. * Dr. Petrie visited and afterwards described the Carrowmore monuments, and gave numbers to each, so as to identify them afterwards. I have made use of these $ but the route he took in going over the field is very difficult to follow so exactly as to be sure we are correct, and I am not certain whether, in some instances, I may not have mistaken his number. His letter on Carrowmore is dated fi 12. 8. 1837.” See his Life. 252 Elcock — Pre-Historic Monuments at Carrowmore. Walking from Sligo, the first cromleac which meets the eye is one close on the left or east side of the road. It formerly had a stone circle round it, which was cut through when making the road, and several of the stones were broken up to make the wall. Some may be seen in the wall, and one is still in the field, in situ. The cap stone very much resembles the top of a mushroom. It measures about twenty feet m circum- ference, and stands on six stones. One feature of this cromleac arrests the attention almost at the first glance. On the western side it has a sort of projecting porch-like entrance, formed by four stones— a peculiarity which is found on other cromleacs on Carrowmore. Dr. Petrie calls this No. 13. See sketch No. 1. , On the west side of the road, and almost opposite the crom- leac just mentioned, is a short lane leading to a field, near the highest part of which, but not visible from the mam road, ' stands the largest of all the Carrowmore cromleacs. Its Irish name is “Leaba na Ffian,” which means the bed or grave of the warrior— a name which is given to each of the cromleacs in this group. The proverb as to the healing power of time could scarcely meet with stronger proof than that given by this Pagan monument, for the cause of the erection of this cromleac is now so completely forgotten in the neighbourhood, that that which is the result of bitter hatred is now known commonly as “ The Kissing Stone.” Swains and maidens know the reason This cromleac is perfect, and stands from eight to nine feet high. The cap stone rests on three of the six stones under it, and measures about twenty-three feet in circumference, being about ten feet long. A stone circle, nearly forty feet in diameter, still surrounds the cromleac, thirty- two stones, being in situ. The porch-like entrance is here seen also. This is the only cromleac of the group into which we can walk. Dr. Petrie calls this No. 7. See sketch No. 2. < Almost due south of this cromleac, and being but a few yards Elcock — Pre-Historic Monuments at Carrowmore. 253 away, easily seen from it, stands Dr. Petrie’s No. 4. This cromleac is quite perfect, and stands about five feet high. There are five supports for the capstone, which measures about fourteen feet in circumference. It stands near the middle of a field, and formerly had a stone circle around it about forty feet in diameter,, consisting of forty large stones. When Dr. Petrie visited it in 1837, he found twenty-one of these still there. In 1883 these were all gone but one ! On enquiring of the farmer before-mentioned how this was, he told me the twenty-one stones were all there still, but twenty had been buried by the man who held the farm before him, adding— “And he got no good by burying them.” The former tenant feared to destroy the stones, and so dug a large hole at the base of each, and then tipped twenty of them into the holes made, “ and there they are still,” said my informant. He would have tipped over the last stone, but the agent, hearing what he was doing, came and stopped him just in time to save it. On account of the stones being “ still there,” though invisible, I have ventured to name this “ The Cromleac of the Phantom Stones.” Although there are no stones placed as a porch outside the supporting stones, yet the idea of having a special entrance is evident in the con- struction of the entrance. See sketch No. 3. The remains of at least two very fine circles are near this cromleac, one of them containing a ruined cromleac, and the other having been a double circle, the outer circle being formed of very large stones. The chamber of the ruined cromleac was examined about fifty years ago by a gentleman named Walker, who found human remains in it. About a dozen were thus examined, and at least ten of them contained an interment of human remains, and in one instance the cromleac contained an urn, broken. This was found in Dr. Petrie’s No. 17 — a double circle. Crossing the road again, there stands a little way south-west of the farm-house a large heap of stones which have been gathered off the land. Under this heap there is a perfect 25+ Elcock — Pre- Historic Monuments at Carrowmore. cromleac. It was covered when Dr. Petrie visited it. His number for it is 55- This ought to be uncovered by the Board of Works, under whose care these monuments are now placed. Not far from this heap, down in the hollow near the house, stands Dr. Petrie’s No. 53. Nothing but the cromleac is now left, the circle formerly around it having disappeaied through “improvements” many years ago. The cromleac stands very low, and will soon be gone from sight, as it forms a good basis for a stone-heap, such as that at No. 55- It scarcely reached higher than the top of the oats by which it was surrounded when I saw it. See sketch No. 4. In the next field to the south are a great number of circles : one in the east corner is formed of very large stones, and near it on the south-west is a fine large “ giant’s grave,” or stone cist. Half of Listoghil stands in the field, and two cromleacs also. The nearest to us is Dr. Petrie’s No. 52. It is a large cromleac, with a conical cap stone, flat underneath. Query, was it a double cromleac? The porch-like entrance is very marked, unless what looks like a porch may be the supports of a second crom- leac, of which the cap stone is gone. A circle formerly sur- rounded this cromleac, but only one stone is now standing, and this is not in its original place. My informant once saw this stone being moved away, and he put it back as near as he could. There is a gentle incline of earth and stones up to the top of the supports of the cap stone/looking like an inclined plane, up which the cap stone was pushed into position, but I do not think it was formed for that purpose, though I could not learn whether it had been formed by throwing the stones there which were cleared out of the land. See sketch No. 5* Passing by Listoghil on our left, we see below us on the south, Dr. Petrie’s No. 48. This cromleac is perfect, the cap stone being about six feet square, but is nearly level with the ground. At a distance of thirty-eight feet from it stands a Elcock — Pre-Historic Monuments at Carr ow more. 255 large solitary pointed stone, five feet high, the only one left of what must have been a magnificent circle, about eighty feet in diameter. See sketch No. 6. Double circles, with ruined cromleacs, are seen west of this in the same field. Near the pond, at the bottom of the hollow, there is what appears to be a cist of unusual construction. There is a very large flag-like stone, flush with the surface, under which is a hollow space. I pushed my umbrella into it, through an opening on one side, and could swing it about. It was too dark inside to see anything. The peculiar feature is this:— On the top of the flag, and placed round it, resting partly on the flag and partly on the surrounding soil, are a number of large stones, as if put there to keep the flag down and prevent its being raised. What can this be ? I have never seen any similar structure. Just over the wall, in the field at the top of the hill, is seen a very remarkable cashel or fort. It may be called roughly square, the sides being about one hundred and twenty feet long. The circumscribing walls are perhaps ten feet thick, and are made up of earth and massive stones. There are two entrances on opposite sides, north and south. The interior is divided by cross walls at right angles, and there appears to have been a cist or structure of some sort in it. There are a ditch and bank outside the wall. Altogether, it is very difficult to say what this really was, its appearance being so very different to what is usually found in forts, &c., and excavation would be necessary to settle the question whether this was a place of sepulture or not. Can it have been the great Firbolg stronghold ? Dr. Petrie numbers it 46. Leaving the cashel and passing to the east, in the direction of Cloverhill, keeping near the wall, we soon come upon the last of the perfect cromleacs left on Carrowmore. It is Dr. Petrie s No. 37. It stands in the centre of a triple series of circles still there. The cromleac is small, the cap stone being about sixteen feet in circumference, and resting on five stones. 256 Elcock — Pre-Historic Monuments at Carrowmore. The porch is very striking. The smallest circle is forty feet in diameter, and consists of small stones, much covered by the grass, so as to be nearly hidden. The middle arc e is eighty feet in diameter, and is formed of twelve large stones. The outermost circled one hundred and twenty feet in diameter^ and is composed of twelve much larger stones, some of which have been displaced. See sketch No. 7. This list mentions all the cromleacs which are perfect m 1 883 Ruins and traces of others, with single, double, and even triple chambers in them, are numerous, no less than twenty being traceable, though many more formerly stood on Carrow- mThere is one very fine circle not far from No. 37, some of the stones of which stand seven feet above ground. Three or four have slipped from their places owing to the carting away of the gravel from the mound on which the circle stands. There are traces of cists or cromleacs within this circle, and on stamping the ground, it sounds as if hollow. Origina y . ov y stones stood round the edge of this circle, which is seventy to eighty feet in diameter. . , „ A In a field about three hundred yards east of this circ , on the left of the road to Cloverhill, is a stone cist. 1 tops of the stones are level with the ground. Some of the stones are carved with very rude scnbmgs, an one » entrance has on the edge what looks very much like ^Ogham inscription. The drawings of these sculptures in Ferguson “ Rude Stone Monuments” are not correct. At the extreme northern end of the battle-field is st seen the well of very fine water, never known to be dry, at which the Firholgs are said to have drunk on the day of the battle. Its Irish name is “Tober na Ffian,”-the Warrior’s Well. A very short distance north of the Well stands a very remarkable solitary stone. It is called “ Cloch-breac, The Grey [or Speckled] Stone. It is a flagstone standing on Elcock Pre- Historic Monuments at Carrowmore. 257 edge, measuring nearly ten feet above ground, and as wide as high : its thickness is about seven inches. It has a large quad- rangular hole cut through it, large enough for a man to creep through with ease. It forms a “ mearing point ” for the three adjoining parishes. Why it was erected, or when, is quite lost, and I could learn no tradition respecting it. Is it one of the old Pagan oath stones, such as the Maen-an-Thol, in Cornwall, or as “ The Long Stone ” at Minchinhampton, in Gloucester- shire ? . Besides being used for swearing, such stones were used for curing children who had the measles, whooping-cough, &c., by passing the child through the hole ! A superstition which it is hoped is now quite gone. There is yet one more of the antiquities in Carrowmore which must be mentioned, although properly speaking not exactly belonging to the Moytura monuments. This is The Caltragh, a large Pagan burying ground, about a quarter of a mile due east of Cromleac No. 13. It may be seen from the field in which this cromleac stands, and from Listoghil. The Caltragh is an irregularly circular mound, about one hundred and fifty yards in diameter, enclosed by a wall. Some slight excavations made here and therfe many years ago, showed it to be full of human bones. The examination was difficult, owing to the prejudices of the neighbourhood. No burial has ever taken place there within the reach of tradition, and the ground is regarded as under a sort of taboo . Undoubtedly it dates from a very remote antiquity— probably much older than the Carrowmore monuments. The whole of these monuments are included in the Act for the Preservation of Ancient Monuments. There is now little doubt that the stone enclosures known as Druidical Circles, Druid’s Altars, and such like, are invariably sepulchral, with which the Druids had no sort of connection as to worship. The stone circles in all probability mark the burial places of the common soldiers who fell in the battle, and the cromleac in the centre, the grave of the chieftain— the 25s Elcoek — Pre- Historic Monuments at Carrowmore. “great man” who commanded them. Almost invarl*blJ’ wherever^ examined, traces of hnman interments have been found in both. This is borne out by the ancient Irish name for all the Carrowmore monuments-the graves or beds of the WaSuchSof our members who may be in Sligo may count on a dav of exceeding interest and instruction by paying a visit to clrtZl O.t of Brituny, .hero ;> =» coUoouon of such antiquities known to equal it m the wor Works of reference in connection with the subject Ferguson’s Rude Stone Monuments. Dr. Petrie’s Life and Letters. The Book of Fenagh. Dunraven’s Notes on Early Irish Architecture. Jubainville’s Le Cycle Mythologique Irlandais, chaps, vu., viu. Wilde’s Lough Corrib. . Wood-Martin’s History of Sligo.-This book contains the most recent information about Carrowmore. CHARLES ELCOCK. 11 FEB V'se PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB , 1883-84. (APPENDIX). PL A TE XXI. PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB, 1883-84. (APPENDIX). PLA TE XXII. CARROWMORE, CO. SLIGO. The Cromlech of the Phantom Stones, Dr. Petrie's, No. 4. 3 Cromlech, Dr. Petries , No. 4 PROCEEDINGS OF THE BELFAST NATURALISTS’ FIELD CLUB, 1883-84. (APPENDIX). PLATE XXIII. CARROWMORE. CO. SLIGO. Cromlech, Dr. Petrie's, No. 54. 5 Cromlech, Dr. Petrie's, No. 6 PROCEEDINGS OF THE BELFAST NATURALISTS' FIELD CLUB , 1883-84. (APPENDIX). PLA TE XXIV. CARROWMORE, CO. SLIGO. Cromlech, Dr. Petrie s, No. 37. 7 APPRDDlX IX ^ I. RECENT OSTRACODA OF BELFAST LOUGH. BY SAMUEL M. MALC6MSON, M.D. II. the FUNGI OF THE NORTH OF IRELAND. BY HENRY WILLIAM LETT, M.A., Trin. Coll., Dublin. III. FORAMINIFERA OF THE BELFAST NATURALISTS’ FIELD CLUB’S CRUISE OFF BELFAST LOUGH IN THE STEAM-TUG 11 PROTECTOR,” JUNE, 1 885 ; ALSO, FORAMINIFERA FOUND BY DR. MALCOMSON, AT ROCKPORT, BELFAST LOUGH. BY JOSEPH WRIGHT, F.G.S. IV. A LIST OF THE CRETACEOUS FORAMINIFERA OF KEADY HILL, COUNTY DERRY. BY JOSEPH WRIGHT, F.G.S. V. A LIST OF IRISH COLEOPTERA, BY ROBERT PATTERSON, F.R.S. EDITED BY S. A. STEWART, F.B.S., Edin. PUBLISHED BY THE BELFAST NATURALISTS’ FIELD CLUB. January, 1886. ■ ' • ■ ■ . ( Proceedings Belfast Naturalists' Field Club. — Appendix 1884-1885). RECENT OSTRACODA OF BELFAST LOUGH. By SAMUEL M. MALCOMSON, M.D. «S very few Ostracoda have been recorded from the North of Ireland, and as no systematic list of the species inhabiting Belfast Lough and its neighbourhood has ever been made out, I determined some years ago to examine all the material containing them which I could obtain, with a view to supplying this deficiency. When I mentioned my project to Mr. Joseph Wright, F.G.S., he very kindly offered to place at my disposal all the material dredged by himself and Mr. Wm. Swanston, F.G.S., from the examination of which he had compiled the extensive list of Foraminifera published in an appendix to the proceedings of the Belfast Naturalists’ Field Club for 1876-77. To these valuable dredg- ings I have added one gathering of my own, consisting of shore sand from Rockport, County Down, and also the dredgings taken at the Field Club excur- sion in the steam tug “ Protector,” in 1885. Want of time has prevented the examination of Mr. W right’s entire series of dredgings, but those already done seem to give a fairly representative list of the Belfast Lough species, and as Strangford Lough has not yet been systema- tically dredged, I have considered it better not to incorporate the gatherings from that locality in the present list. Altogether, gatherings from twenty- one stations have been examined. Eleven of these situated in the Irish Channel, just outside the mouth of Belfast Lough, were all, except three, in moderately deep water (30 to 72 fathoms). Five of the stations were in Belfast Lough itself, and all in shallow water (4 to 10 fathoms), while the remaining five stations were situated on the beach, and consisted of shore gatherings, taken from the surface of the sand or from rocky pools between tide marks. These gatherings altogether have yielded 100 species of marine Ostracoda, 260 Malcomson. — Recent Ostracoda of Belfast Lough. as well as five fresh water species,* which were found in the shore gatherings, hut these had evidently been carried down by streams, and consequently have not been included in the present paper. Two tables are appended— one giving particulars of depth, locality, nature of sea bottom, quantity of material examined, and number of species found m each gathering; and the other showing the distribution and comparative rarity of each species. I am very deeply indebted to G. S. Brady, M.D., F.L.S, for the great assistance he has rendered me in the identification of many doubtful specimens, and for the valuable information he has given me about some of the more inte- resting species. . . I must also thank my friend, Mr. Joseph Wright, for his kindness m placing his gatherings in my hands, and Mr. David Robertson, F.G.S., of Glasgow, for his help in determining some of the critical species. The following species deserve special notice : — Paracypris polita, G. 0. Sars. Only two or three single valves ^ of this species were found, all of them in one locality- viz., Brown s Bay, Islandmagee, one of the excellent shore gatherings collected for Mr. Wright’s paper by Mr. Gray, M.R.I.A. Bairdia inflata, Norman. This species seems to he fairly common in the Irish Channel, but only one valve was found in Belfast Lough, and that one at White Head, which is almost at the mouth of the Lough. Bairdia obtusata, G. 0. Sars. Only two specimens of this very rare species were found, both in the “ Protector ” dredgmgs. Cythere cribrosa, B. C. and Jt. I have only seen one specimen of this species. It has not been previously found in the recent state, hut occurs fossil in the Post-tertiary deposit at Bridlington, Yorkshire.1 Cythere Cluthse, B. C. and B. Although rare, this species seems to be generally distributed in the deeper water. Recent specimens have no been previously recorded, but fossil ones occur in several post-tertiary deposits* Cythere Dunelmensis, Norman. This species seems to inhabit only a very limited area in Belfast Lough, as it has been found m only tuo gatherings, taken from stations which were close together-™.,' ott ltockport, 4 fathoms, and Rockport shore sand. It is usually found m much deeper water, and is not a littoral species. I think it is probable that the shore sand specimens have been washed up by some curren , * Pot&mocypris fu!va .Brady. Cypris MM ,J t -g Cypridopsis villosa ( jUr{ne ). Candona albicans, Brady , and Candona compressa (Koch). (1.) See Post. Tert. Entom. Scotland, p. 146. (2.) See Post. Tert. Entom. Scotland, p. 153. 261 Malcomson. — Recent Ostracodci of Belfast Lough. although they do not appear much worn ; but as several other species of Ostracoda, as well as Foraminifera, which usually inhabit deeper water, have been found in this locality, I think some such supposition is ren- dered likely. Cythere (?) acerosa, Brady. Although extremely rare, this species seems to be widely distributed in the deeper water outside Belfast Lough, hav- ing been found in no less than five gatherings. Cytheridea suMavescens, Brady. Five or six typical specimens of this extremely rare species have been found. Loj^oconcha cuneiformis, n. sp. Brady JUS. (Plate xxv., figs. 1-2.) Only one specimen, a male, of this species has been found. Carapace of male, as seen from the side, oblong, subrhomboidal, higher in front than behind, greatest height equal to half the length ; anterior extremity broad, marked with a few radiating hair-like lines, well rounded below, and sloping steeply backwards above, where it forms an obtuse angle with the dorsum ; posterior narrow, and obliquely rounded below ; superior margin straight, inferior slightly sinuated in front of the middle, and produced into a thin laminar process behind, which is continued round the posterior border. Outline, as seen from above, cuneate, greatest width in front of the middle, and scarcely equal to height ; acutely pointed in front, somewhat more obtusely behind. Shell pellucid, polished, thickly covered with very fine puncta, and a few distinct elevated papillae. Cytheropteron Montrosiense, B. C. and R. Only a single valve of this species has been found. Bythocythere pavo, n. sp. Brady MS. (Plate xxv., figs. 5-7.) Only six specimens of this species have been seen, all from the dredging off Black Head. It has been previously found by Dr. Brady and the Rev. A. M. Norman, but has not been described. Carapace of female, as seen from the side, oblong, subquadrilateral ; nearly equal in height through- out ; height equal to half the length, extremities rounded ; superior margin straight, inferior slightly sinuated in the middle. Seen from above ovate, greatest width behind the middle, and nearly equal to half the length ; anterior extremity muncronate, posterior evenly rounded. End view triangular, with rounded angles ; height slightly greater than width. Surface of shell thickly covered with fine punctures and large white papillae. Length, 1.100th inch. Dr. Brady informs me that most of his specimens have a slight lateral crest, which mine do nol show. Cytherideis foveolata, Brady. (Plate xxv., figs. 8-12.) This species, which has not been previously found in Britain, seems to be confined to 262 Malcomson. — Recent Ostracoda of Belfast Lough. the deeper water, although the first specimen was in shore sand from Portrush, where it had probably been washed up. Dr. Brady informs me that my specimens differ from the types obtained by him from t e Gulf of St. Lawrence, in being rather stouter, less depressed in front, less distinctly punctated, rather smaller, and in haying the ventral over- lap of the valves in the opposite direction. Paradoxostoma truncatum, n. sp. (Plate xxv., figs. About a dozen specimens of this species have been found in a single locality off Coalpit Bay, hut it has not been seen anywhere else. Carapace, as seen from the side, compressed, irregularly ovate, greatest height m the middle, and equal to rather more than half the length. Anterior margin nearly straight, and sloping upwards almost at right angles to the ante- rior part of the dorsal margin; posterior extremity evenly rounded. Superior margin well arched, sloping somewhat steeply m front ; inferior sinuated in front of the middle. Outline, as seen from above ovate extremities pointed, widest in the middle ; greatest width equal to rather more than one-third the length. Yalves pellucid, white, or slightly ochreous. Length, l-60th inch. Cytherella Scotica, Brady. Only, a single yalve of this species has been TABLE GIVING PARTICULARS OF DEPTHS, &c., OF THE STATIONS. O rd . rO*3 | § •9I t! ® la HOMHHlOfflNffl to 05 tO CO r* TjH CO tH to CO (N » O t)uO CO to CO (N h CO Oi (M CO CO (M CO CO CO to •^d83[ •I 8 00 tH K £ : CO CO CO 05 OS d d I P4.S .<** 2 m „rd l|a 111 4 CD -i d d © d © rd dd j ^ M £ P> 03 'S ‘r3 d d d ■ a d o d Hg d 'g d pj d d d oj d -p lZZ tsj P-i cd o3 i_i -COCOtOi— I CO CO o«©^to g£ £d w odd iS'-rg-rg :'.V^ d.jr r§^ 3 3 s 'o *cd 'o f*3 «h d DQ ° ° 02 02 P © © J® la a © O •5 £ o ES d d o o rd • rd 1 . -+J In^ feD'd , rd P © d © ” rrl 3 d • "■"a •a § d d &*<* a 3 d ^ § d 'd S'g 0*1^3 §H P n 02 *y ^ d 3 :1 mw.m . • ■-■ ‘ OQ^SK -a 02 ta ® m ® O d ® ® © a ©d grdd^ ^ a S a a a a O ® O O £ •a ^ tX I ^ „ 02HEHdHO fig ££ s .a ts ^ -g &&I* 2d » © 2 n d © 0?P sSurSpaap Kioio0jojj ,, •aaXKVHQ HSIHJ SttSdSdSd U oooow •hohot; xsyaaag; «<5 d ,, P p Pt r^ O o HP 5 ftp d a n a-f © cd dT ^op Jg g 60 H a * £ 9 -p> o o © >_, Ppqpq •SOKIHaHXVr) aaoHg U4 EXPLANATION OF PLATE XXY. Fig. 1. Loxoconcha cuneiforms. Fig. 2. ,, Fig. 3. Paradoxostoma truncatum. Fig. 4. ,, Fig. 5. By thocy there pavo. Fig. 6. >> Fig. 7. >> Fig. 8. Cytherideis foveolata. Fig. 9. » Fig. 10. „ Fig. 11. >> Fig. 12. >> Carapace of male, seen from left side Carapace of male, seen from above Carapace of female, seen from left side. Carapace of female, seen from above. Carapace of female, seen from left side. Carapace of female, seen from above. Carapace of female, seen from below. Carapace of female, seen from left side. Carapace of female, seen from above. Carapace of female, seen from below. Carapace of male, seen from left side. Carapace of male seen from above. Proc. Belfast Nat. Field Club. 1884-85. (Appendix.) ' PI. XXV MALCOMSON _ OSTRACODA OF BELFAST LOUGH. /, 3 n M. del et lith I ( Proceedings Belfast Naturalists' Field Club. — Appendix 1884-85.) €fjt jfuttgt of tfye i^ortfj of Irtlaitb* PART i. By HENRY WILLIAM LETT, M.A., Trin. Coll., Dublin The earliest writers who mention any of the Fungi of the North of Ireland appear to be the editors of “ The Antient and Present State of the County of Down: Dublin, 1744.” This book is now generally known as Harris’s County Down, from a Mr. Walter Harris having had the principal share in its compilation. And the next is, Dr. Taylor, of County Cork, who wrote nearly half a century ago. v x Harris’s Down gives “A catalogue of the more rare Plants found spon- taneously growing in the County of Down in May, 1748, by an expert Botanist employed for that purpose, and examined in Dublin by some well skilled in that branch of knowledge.” These plants number exactly forty, and four are Fungi, which are described at p. 183 as follows. “ 28. Fungus Arboreus acetabuli modo cavus, coccineus, marginibus pilosis. Raii Syn. Fungoides coccineum oris pilosis, acetabuli forma. Tournf. Inst. It grows on rotten oaks in Kilwarlin near Hillsborough in June.” There can be no doubt this is Peziza coccinea (Jacq). “ 29. Fungus Pileatus major superne coloris Castanei, lamellis Candidis, caule maculato. Raii Syn. — Chesnut-coloured Mushroom with white Gills and spotted Stalk. Dr. Sherard found this in the County of Down, but has omitted to mention the particular place where.” “ 30. Fungus pulverulentus, Crepitus Lupi dictus major pediculo longiori ventricoso. Raii Hist. — Dusty Mushroom the greater , with a long, tumid foot stalk, found at Moyra and other parts.” This and the next are evidently Puffballs. “31. Fungus pulverulentus, Crepitus Lupi dictus, pediculo longiori sc abro. Dr. Sherard. Dusty Mushroom with a long rough foot stalk, found at War - ingstown." 266 Lett- •2 he Fungi of the North of Ireland. The Dr Sherard whose name occurs twice in connection with these four plants may be regarded as the first Ulster fungologist. Perhaps some more of his observations may be unearthed by future researches. The next worker in this department of the Botany of the district was Templeton, who carried on the collection and study of the Fungi found near Belfast more than eighty years ago, with the result of whose efforts the authors of the “ B.N.F.C. Guide to Belfast, &c.,” were unacquainted. Those efforts are embodied in a paper in the Annals of Natural History , Vol. V., pp 3-6 1840 the title of which is— “ Catalogue of the Species of Fungi obtained in the North of Ireland by John Templeton, Esq., of Cranmore, Belfast,” by “ Thomas Taylor, M D., M.R.I.A., F.L.S ” And to the list is the following preface : — “ Dunkerron, Kenmare, 12th March, 1839.-The following Cata- logue of Fungi, collected by the late Mr. John Templeton in the vicinity of Belfast, is drawn up from drawings and specimens left by him, and whic Mrs Templeton placed in my hands, with a desire that I should carefully ascertain the species and their modern names, with a view to pnbhoa- tion. I have bestowed upon them my best attention, and yet the list is defi- cient by a few of the drawings whose counterparts I have not yet met with in nature, and by a vety few of the specimens, from whose imperfect state no satisfactory conclusions could be drawn. Still, I cannot but. admire the in- dustry and talents of one who, at least equally successful in all the other departments of zoology and botany, displayed so intimate a knowledge of plants difficult of investigation, at least before the termination of the last cen- tury, when the greater part of this collection was already made.-TnoMAS TayloR * * The 226 Species collected by Templeton are inserted in the following Cata- loeue which, for convenience of reference, is arranged according M- °- Cooke’s, Handbook of British Fungi , pp. 901 (London, 1871) whose des°rip- tions are referred to, except where otherwise stated. As I have adopted the classification used in that work, I have not thought it advisable to give titles of the Families and Orders as they occur. , Two forms of Sclerotium (complanatum, Tode. and durum, Pera) collected by Templeton have been omitted, as they are regarded by modern mycologists as immature states. 'Wherever necessary the Synonyms employed by Taylor have been added. . , There are six of Templeton’s species which, owing to being unable to con- sult any of the older writers on British Fungi, I cannot trace to their modern Synonyms, and therefore, for the present, enumerate them here. These are Thelephora aurantiaca, Sow. Peziza aquatica, De Cand. Peziza ly coper dioides , De Cand. Tremella difformis , With. Sphoeria rimosa, Sow. Pers, Demaiilium ciliare, Lett — The Fungi of the North of Ireland. 267 It may here be inquired, what has become of Templeton’s drawings and specimens, and would it be possible to have them placed in the Herbarium of the Museum of Belfast, near the scenes of his varied and many labours for science, and the town close to which he had his home, andr with which his name will be always associated? The Belfast Museum already possesses, through the generosity of Mr. Robert M. Young, a small collection of crypto- gamic plants made by Templeton between the years 1801-1809, which con- tains a few specimens of Fungi, but, as they are not marked with any locali- ties, I regret my inability to recognise them as Irish. However, a more interesting and important discovery has been lately made by Mr. S. A. Stewart, F.B.S.E., who has found amongst Mr. W. Thompson’s papers on the Museum shelves, a number of Fungi collected by that genius of varied talents, some of which I was glad to find were natives of the North, and will be found duly recorded in my list. It would seem that nothing has been done since Mr. Templeton’s time to study the Fungi of our district, except the few species brought together by the author of the Natural History of Ireland. But recently attention has been given to the subject by several students of nature, whose specimens 1 have had the pleasure of inspecting, and a certain public interest has been excited about “Toad stools,” as was evidenced by the attendances at the Fungus Forays of 1883, to Shane’s Castle, County Antrim ; of 1884, to Killymoon, near Cookstown, County Tyrone ; and of 1885, to Rademon, near Crossgar, County Down. The work effected by the B.N.F.C. on those occasions can be esti- mated from the frequent mention of those localities in the accompanying pages. The present list contains 582 species, and is intended as the beginning of a Catalogue which, it is expected, will be continued from time to time. It embraces only a small portion of the Fungi of the North of Ireland, and these from merely a few localities, a large number of the most common species not being recorded in it, a deficiency which time and patience can, and doubtless will, supply. There remain in my possession many specimens and drawings of undecided forms, which I have not been able to clear off in time for this report. In the identification of species, much assistance has been afforded me by W. B. Grove, Esq., B.A., of Manchester, and Greenwood Pirn, Esq., M.A., F.L.S., of Monkstown, County Dublin, who have taken a great deal of trouble with many difficulties that I submitted to their judgment. Mr. Pirn, who has been working for some years on the Fungi of Leinster and Munster, added to his favours by spending two pleasant days with me in September, 1885, when we had the satisfaction of verifying more than 80 species among the woods of Donard Demesne, and Tollymore Park. I hope that the other kind friends who have contributed specimens will continue and extend their observations till the records are completed for all the counties in Ulster. 268 Lett— The Fungi of the North of Ireland. Note.— The plants included in this Part which I did not collect— except Templeton’s in Taylor’s list -have been all examined by me, and in nearly everj instance in a living state.- -H. W. L. 1. Agaricus (Amanita) vaginatus. Bull. Near Belfast, Templeton, Ann. Nat. Hist, Vol. V. Rosstrevor and Narrow Water Woods, County Down, 1883 ; Killymoon, County Tyrone, 1884; and Rademon, County Down, 1885 — H. W. L. 2. Agaricus (Amanita) cecilise. B. and Br. Narrow Water Wood, Co. Down, 1888. Rare.— H. W. L. 3. Agaricus (Amanita) adnatus. Smith. Ardmore Glebe, Co. Armagh, 1884. Very rare.-H. W. L. 4. Agaricus (Amanita) phalloides. Fr. Near Belfast, Templeton (. Ac/aricus hulhosus , Sow.). Ann. Nat. Hist., Yol. Y. Narrow Water Wood, Co. Down, 1888; and Killymoon, Co. Tyrone, 1884.— H. W. L 5. Agaricus (Amanita) mappa. Batsch. Several under trees near the grotto in Tollymore Park, Co. Down, 1885— G. Pirn, and H. W. L. 6. Agaricus (Amanita) muscarius. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Shane’s Castle Park, Co. Antrim ; Wood at the Ferry Hill, near Omeath, Co. Louth, and Raughlan, Co. Armagh, 1883 ; Donard Demesne, Rademon, and Tollymore Park, County Down, 1885. Abundant in fir and birch woods.— H. W. L. 7. Agaricus (Amanita) pantherinus. D.C. Donard Demesne, Co. Down, 1884. Rare.-H. W. L. 8. Agaricus (Amanita) rubescens. P. Warrenpoint, County Down, 1883 ; Killymoon, Co. Tyrone, 1884 ; Donard Demesne, and Tollymore Park, Co. Down, 1885. Abundant in both woods. H. W. L. 9. Agaricus (lepiota) procerus. Scop. Ardmore Glebe, Co. Armagh, and sandhills at N6wcastle, County Down, abundant, 1884 ; Rademon, Co. Down, 1885.— H. W. L. lO. Agaricus (I.epiota) rachodes. Vitt, In a plantation at Raughlan, Co. Armagh, 1883. H. W. L. 269 Lett— The Fungi of the North of Ireland. 11. Agaricus (Lepiota) gracilentus. Krombh. Abundant among the sandhills at Newcastle, Co. Down, 1884.— H.W.L. 12. Agaricus (I.eplota) clypeolarius. Bull. Near Belfast, Templeton, Ann. Nat. Hist. Vol. V. 13. Agaricus (Xiepiota) cristatus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. In the lawn near the Castle of Killymoon, Co. Tyrone, 1884.— H. W. L. 14. Agaricus (Iiepiota) granulosus. Batsch. I have collected this pretty species on the summit of Slieve Donard, which rises to a height of 2,796 feet, and among the sandhills near Newcastle, Co. Down, where it was abundant in the short grass only a few feet above the sea level, 1883. Tollymore Park, Co. Down, 1885.— H. W. L. 15. Agaricus (Xiepiota) granulosus var. carcharias. Pers. In a plantation near Holy wood, Co. Down, 1883— R. L. Praeger ; top of Knockbarragh Hill, Co. Down, 1883.— H. W. L. 16. Agaricus (Armillaria) melleus. Vahl. Shane s Castle, Co. Antrim, and Ardmore Glebe, Co. Armagh, 1883 ; Rademon, Tollymore Park, and Donard Demesne, Co. Down, 1885. Most abundant in late autumn. — H. W. L. 17. Agaricus (Armillaria) mucidus. Fr. Lurgan Demesne, Co. Armagh, aud Killymoon, Co. Tyrone, 1884.— H.W.L. 18. Agaricus (Tricholoma) flavo brunneus. Fr. Maralin, Co. Down, 1884.— C. H. Waddell. 19. Agaricus (Tricholoma) albo brunneus. P. Ardmore Glebe, County Armagh, 1882 ; Donard Lodge, County Down 1885.— H. W. L. 20. Agaricus (Tricholoma) rutilans. Schceff. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Wood at the Ferry Hill, near Omeath, Co. Louth, 1883; Donard Demesne, and Tollymore Park, Co. Down, 1884.— H. W. L. 21. Agaricus (Tricholoma) sculptaturus. Fr. Wood at the Ferry Hill, near Omeath, Co. Louth, 1883.- H. W. L. 270 Lett— The Fungi of the North of Ireland. 22. Agaricus (Tricholoma) columbetta. Ft. Killymoon, County Tyrone, 1884.— H. W. L. 23. Agaricus (Tricholoma) imbricatus. Fr. In fir plantation, Donard Demesne, Co. Down, 1884.— H. W. L. 24. Agaricus (Tricholoma) terreus. Schwff. Killymoon, Co. Tyrone, 1884.— H. W. L. 25. Agaricus (Tricboloma) colossus. Ft. ' A single specimen, in fine condition, under trees at rere of Warrenpoint Church, Co. Down, 1883. H. W. L. 26. Agaricus (Tricboloma) gambosus. Fr. Islandmagee, Co. Antrim, and Ardmore and Derrytrasna, Co. Armagh, 1884. This is very abundant and large every year in the latter localities. - H. W. L. 27. Agaricus (Tricboloma) albus. Fr. Rosstrevor Wood, 1883, and Donard Demesne, 1884, Co. Down.— H.W. L. 28. Agaricus (Tricboloma) grammopodius. Bull. Donard Demesne, Co. Down, 1885.— G. Pim, and H. . L. 29. Agaricus (Tricholoma) militaris. Lasch. A single specimen, in fine condition, at Rademon, County Down, 1885.- H. W. L. 30. Agaricus (Tricboloma) nudus. Fr. Raughlan, County Armagh, 1883. — H. W. L. 31. Agaricus (Clitocybe) nebularis. Batsch. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. In abundant clusters and rings in Shane’s Castle Park, Co. Antrim, 1885. Scarce m Tollymore Park Co Down, 1885.-H W. L. In a very perfect ring, seven yards across, the plants so thick as to be riding on each other, at Glenmore near Lisburn, Co. Antrim, 1885.— J. H. Davies. I went to see this.— H. W. L. 32. Agaricus (Clitocybe) odorus. Bull. Donard Demesne, and Tollymore Park, County Down, 1885. -G. Pun, and H. W. L. 33. Agaricus (Clitocybe) cerussatus. Fr. In a fir wood in Tollymore Park, 1884, and Donard Demesne, 1885, Co. Down.— H. W. L. 271 Lett — The Fungi of the North of Ireland. 34. Agaricus (Clitocybe) dealbatus. P. Killymoon, Co. Tyrone, 1884.— H. W. L. 35. Agaricus (Clitocybe) elixus. Sow. Ardmore Glebe, Co. Armagh, 1882.— H. W. L. 36. Agaricus (Clitocybe) fumosus. P. Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 37. Agaricus (Clitocybe) giganteus. Br. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 38. Agaricus (Clitocybe) maximus. Fr. Near the Yicarage, Warrenpoint, Co. Down, 1883. H. W. L. 39. Agaricus (Clitocybe) geotrupus. Bull. Near the Saw-mill in Tollymore Park, Co. Down, 1884.— H. W. L 40. Agaricus (Clitocybe) inversus. Scop. Under Scotch firs at Raughlan, Co. Armagh, 1884.— H. W. L. 41. Agaricus (Clitocybe) gilvus. Pers. This species is described in Grevillea, No. 65, p. 55, of the new issue of Cooke’s White-spored Hymenocetes. Rademon, Co. Down, 1885.— H. W. L. 42. Agaricus (Clitocybe) flaccidus, var. lobatus. Sow. Derryadd, near Lurgan, Co. Armagh, 1884.— H. W. L. 43. Agaricus (Clitocybe) cyathiformis. Br. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. ; Donard Demesne Co. Down, 1885.— H. W. L. 44. Agaricus (Clitocybe) brumalis. Fr. Roadside, in several places, Derrytrasna, Co. Armagh, 1884.— H. W. L. 45. Agaricus (Clitocybe) fragrans. Sow. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. ; Donard Demesne Co Down, 1885.— G. Pirn, and H. W. L. 46. Agaricus (Clitocybe) ectypus. Fr. Donard Demesne and Tollymore Park, Co. Down, 1885.-G. Pim and H. W. L. * 47. Agaricus (Clitocybe) bellus. Fr. Near Ardmore School, Co. Armagh, 1885 H. W. L. 272 Lett— The Fungi of the North of Ireland. 48. Agaricus (Clitocybe) laccatus. Scop Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. ; Narrow Water Demesne and Donard Demesne, Co. Down, and Shane’s Castle Demesne, Co. Antrim, 1883; Killymoon, Co. Tyrone, 1884; Rademon, County Down, 1885. — H. W. L. 49. Agaricus (Clitocybe) laccatus var. amethystinus. Bot. In a wood at the Ferry Hill, near Omeath, Co. Louth, and Shane’s Castle Demesne, Co. Antrim, 1883. Not common.— H. W. L. 50. Agaricus (Clitocybe) gilvus. Pers. Rademon, Co. Down, 1885. — H. W. L. 51. Agaricus (Pleurotus) corticatus. Fr. Several on decaying “sleepers” of the railway near the sandhills at Newcastle, Co. Down, 1885. I gathered these on the Excursion of the B.N.F.C. in July to the Mourne Mountains. — H. W. L. 52. Agaricus (Pleurotus) dryinus. P. A few specimens on an aged elm tree, Ardmore (Hebe, County Armagh, 1884. — H. W. L. 53. Agaricus (Pleurotus) ulmarius. Bull. A few specimens on a decaying elm, Ardmore Glebe, Co. Armagh, 1884. — H. W. L. 54. Agaricus (Pleurotus) salignus- Fr. Abundant on a dead poplar tree, Derryadd, near Lurgan, Co. Armagh, 1882. This appeared for several years on the same trunk. I have not found it elsewhere. — H. W. L. 55. Agaricus (Pleurotus) acerosus. Fr. On the shady side of a clay bank in Ardmore Glebe garden, Co. Armagh, 1885. -H. W. L, 56. Agaricus (Pleurotus) applicatus. Batsch. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. ; Killymoon, County Tyrone, 1884.— H. W. L. 57. Agaricus (Collybia) radicatus. Relh. In a wood at the Ferry Hill, near Omeath, County Louth, and Lurgan Demesne, Co. Armagh, 1883 ; Tollymore Park, and Donard Demesne, Co. Down, 1884. — H. W. L. Lett — The Fungi of the North of Ireland. 273 58. Agaricus (Collybia) maculatus. A. and S. Shore of Lough Neagh, at Derryadd, near Lurgan, Co. Armagh, 1883. Very rare. — H. W. L. 59. Ag-aricus (Collybia) butyraeeus. Bull. Near Belfast, Templeton, Ann. Nat. Hist , Vol. V. Tollymore Park, Co. Down, 1885.— G. Pirn, and H. W. L, 60. Ag-aricus (Collybia) velutipes. Curt. On elm, poplar, &c., when felled, Oo. Armagh, 1882; Go. Down, 1884; Co. Antrim, 1885. Very common and abundant. — H. W. L. 61. Ag-aricus (Collybia) caulicinalis. Bull. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Ardmore, County Armagh, 1883.— H. W. L. 62. Ag-aricus (Collybia) confluens. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Killymoon, County Tyrone, 1884; Donard Demesne, Co. Down, 1885. — H. W. L. 63. Ag-aricus (Collybia) dryophilus. Bull. Wood at the Ferry Hill, near Omeath, Co. Louth, 1883 ; Killymoon, Co. Tyrone, 1884 ; Donard Demesne, Co. Down, 1885. — H. W. L. 64. Ag-aricus (Collybia) clavus. Bull. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 65. Ag-aricus (Mycena) pelianthinus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 66. Ag-aricus (Mycena) elegans. P. Killymoon, County Tyrone, 1884. — H. W. L. 67. Agaricus (Mycena) purus. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Donard Demesne, County Down, 1885 G. Pirn, and H. W. L. 68. Agaricus (Mycena) lacteus. P. Donard Demesne, Co. Down, 1885.— G. Pirn, and H. W. L. 69. Agaricus (Mycena) galericulatus. Scop. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Rademon, Co. Down, 1885.— H. W. L. 274 Lett— The Fungi of the North of Irelana 70. Agaricus (Mycena) alcalinus. Fr. Tolly more Park, Co. Down, 1885.— G. Pim, and H. W. L. 71. Agaricus (Mycena) tenellus. Schum. Ardmore Glebe, Co. Ai’magh, 1885. — H. Y . L. 72. Agaricus (Mycena) cruentus. Fr. Shane’s Castle Demesne, Co. Antrim, 1888.— H. W. L. 73. Agaricus (Mycena) epipterygius. Scop. Donard Demesne, Tollymore Park, and Rademon, County Down, 1885.— H. W. L. 74. Agaricus (Mycena) pelliculosus. Fr. Bog at Raughlan, Co. Armagh, 1883.— H. W. L. 75. Agaricus (Mycena) roridus. Fr. On dead bramble stem, Ardmore Glebe, Co. Armagh, and Rademon, Co. Down, 1885.— H. W. L. 76. Agaricus (Mycena) stylobates. P. Abundant in Donard Demesne, Co. Down, 1885.— G. Pim, and H. W. L. I 77. Agaricus (Mycena) corticola. Schum. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. On old elm trees, Ardmore Glebe, Co. Armagh, 1883. — H. W. L. 78. Agaricus (Mycena) cohoerens. P. For the description of this species, see Fries’s Epic., 2nd ed., 1874, p. 137 ; also Grevillea, Yol.’ I., p. 174. Near Belfast, Templeton, Ann. Nat. Hist. Yol. Y. 79. Agaricus (Omphalia) pyxidatus. Bull. In short grass, Killymoon, County Tyrone, 1884. H. W. L. 80. Agaricus (Omphalia) umbelliferus. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Common in County Armagh, and among the Mourne Mountains, Co. Down. Near top of Slieve Donard, Co. Down, 1883 ; top of Shan Slieve, Co. Down, 1885.— H. W. L. 81. Agaricus (Omphalia) stellatus. Sow. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 82. Agaricus (Omphalia) griseus. Fr. Donard Demesne, and Rademon, Co. Down, 1885.— H. W. L. 275 Lett — The Fungi of the North of Ireland. 83. Agaricus (Omphalia) fibula. Bull. Narrow Water Demesne, Co. Down, 1883.— H. W. L. 84. Agaricus (Volvaria) bombyclnus. Schceff. I found one specimen, in porfect condition, on a fallen, decayed branch, in Killymoon Demesne, Co. Tyrone, 1884. — H. W. L. 85. Agaricus (Volvaria) speciosus. Fr. A few were growing by the side of the road in Killymoon Demesne, Co. Tyrone, B.N.F.C. Excursion, 1884.— H. W. L. 86. Agaricus (Pluteus) cervinus. Schceff. On the dead stump of a willow tree at Ardmore Globe, County Armagh, 1884.— H. W. L 87. Agaricus (Entoloma) helodes. Fr, On peaty soil, Ardmore Glebe, County Armagh, and Donard Demesne, Co. Down, 1884. —H. W. L. 88. Agaricus (Entoloma) ameides. B. and Br. What Fries calls the “odor peculiaris ” of this plant seems to me to resemble the smell of phosphorus or damp matches. Tollymore Park, County Down, 1885.— G. Pirn, and H. W. L. 89. Agaricus (Entoloma) jubatus. Fr. Ardmore Glebe, Co. Armagh, 1884. — H. W. L. 90. Agaricus (Entoloma) clypeatus. L. Near Belfast, Templeton (. Entoloma fertilis), Ann. Nat. Hist., Yol. Y. 91. Agaricus (Entoloma) rlxodopolius. Fr. Donard Demesne and Tollymore Park, County Down, 1885 G. Pirn, and H. W. L. 92. Agaricus (Entoloma) sinuatus. Fr. Near Belfast, Templeton (Agaricus, Entoloma fertilis, Pers Ann. Nat. Hist., Vol. V. 93. Agaricus (Entoloma) sericeus. Bidl. Narrow Water Demesne, Co. Down, and Ardmore Glebe, Co. Armagn, 1883. -H. W. L. 9 4. Agaricus (Entoloma) nidorosus. Fr. Donard Demesne, and Tollymore Park, Co. Down, 1885.— G. Pirn, and H. W. L. L 276 Lett— The Fungi of the North of Ireland. 9 5. Agaricus (Clitopilus) prunulus. Scop. Shane’s Castle Demesne, Co. Antrim, 1883 — H. W. L. 96. Agaricus (Claudopus) variabilis. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Maralm, Co. Down, 1884. — C. H. Waddell. 97. Agaricus (Jjeptonia) chalybseus. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 98. Agaricus (Wolanea) pascuus. P. Near Belfast, Templeton, Ann Nat. Hist., Vol. Y. 99. Agaricus (TUolanea) rufo-carneus Berk. Among heather in a bog at Derryadd, near Lnrgan, Co. Armagh, 1884 ; Tolly more Park, Co. Down, 1885. -H. W. L. 100. Agaricus (Pholiota) squarrosus. Mull. Near Belfast, Templeton, Ann Nat. Hist., Yol. Y. Holywood, Co. Down, 1883— R. L. Praeger. Ardmore, County Armagh, 1883; Tollymore Park, Co. Down, 1885. — H. W. L. 101. Agaricus (Pholiota) spectabilis. Fr. Near Belfast, Templeton (A. aureus , Bull), Ann. Nat. Hist., Yol. V. On a felled apple tree, Ardmore Glebe, Co. Armagh, 1883. H. W. L. 10Z. Agaricus (Pholiota) aureus. Bull. A plant so named occurs in Dr. Taylor’s List of Templeton’s Fungi, and may for convenience be placed here. Fries, in his Epicrisis, 2nd edition 1874, p. 317, says of it— “Qui fons nominis A. aurei plane diversa tarn a nostro A. aureo quam A. spectabili, lamellis angustis albis mox distinctus, sed affinitatis dubise.” 103. Agaricus (Pholiota) junonius. Fr. In a decaying willow at Raughlan* Co. Armagh, 1884.— H. W. L. 104. Agaricus (Pholiota) mutabilis. Schceff . Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 105. Agaricus (Hebeloma) sinapizans. Fr. Killymoon, Co. Tyrone, 1884 ; Rademon, Co. Down, 1885.— H. W. L. 106. Agaricus (Hebeloma) crustuliniformis. Bull. Tollymoro Park, Co. Down, 1885.— G. Pim, and H. W. L. 277 Lett — The Fungi of the North of Ireland, 107. Agaricus (Hebeloma) fastibilis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Ardmore Glebe, Co. Armagh, 1884,— H. W. L. 108. Agaricus (Hebeloma) flocculentus. Foil. Donard Demesne, Co. Down, 1885. — G. Pirn, and H. W. L. 109. Agaricus (Hebeloma) plumosus. Bolt. Donard Demesne, Co. Down, 1885.— G. Pirn, and H. W. L. 110. Agaricus (Hebeloma) scaber. Mull. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 111. Agaricus (Hebeloma) fibrosus. Sow. Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 112. Agaricus (Hebeloma) rimosus. Bull. On summits of the Sallagh Braes, Co. Antrim, and Killymoon, County Tyrone, 1884. -H. W. L. 113. Agaricus (Hebeloma) geophyllus. Sow. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Donard Demesne, and Tolly more Park, Co. Down, 1885.— G. Pirn, and H. W. L. I14- Agaricus (Hebeloma) calamistratus. Fr. In shady grass by the side of a path in Donard Demesne, Co. Down, 1884.— H. W. L. (See Fries, Epic., 2nd edition, 1874, p. 227.) 115. Agaricus (Flammula) flavidus. Schceff. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 116. Agaricus (Flammula) sapineus. Fr. Donard Demesne, Co. Down, 1885.— G. Pirn, and H. W. L 117. Agaricus (Crepidotus) mollis. Schceff. On decaying wood in Rosstrevor Wood, 1883, and Tollymore Park, Co. Down, 1884.— H. W. L. 118. Agaricus (Naucoria) escharoides. Fr. Ardmore Glebe, Co. Armagh, 1883 ; Killymoon, Co. Tyrone, 1884.— H. W. L. Agaricus (Galera) tener. Schceff. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Abundant in dungy 278 Lett— The Fungi of the North of Ireland. spots among grass on Lough. Neagh shore, at Ardmore Glebe, Co. Armagh, 1884. — H. W. L. 120. Agaricus (Galera) hypnorum. Batsch. In a bog near the Bannfoot, Co. Armagh, 1884 ; Donard Demesne, and Tollymore Park, Co. Down, 1885.— H. W. L. 121. Agaricus (Galera) sphagnorum. Pers. Anglesey Mountain, near Omeath, Co. Louth, 1883 ; Derryinver Bog, Co. Armagh, 1884. — H. W. L. 122. Agaricus (Psalliota) arvensis. Schaff. '. Near Belfast, Templeton {A. Georgii), Ann. Nat. Hist., Yol. Y. Ard- more, Co. Armagh, 1882 ; Tollymore Park, Co. Down, 1885.-H. W. L. 123. Agaricus (Psalliota) arvensis var. villaticus. Brand. Raughlan, and Derryadd, Co. Armagh, 1883.— H. W. L. A specimen weighing oz., and measuring 8 in. high and 10 in. in diameter, was sent to mo °by S. A. Stewart, from a wood by the river near Downpatrick, 19tb August, 1885. (See Fries, Epic., 2nd edition, p. 280.) 124. Agaricus (Psalliota) campestris. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. The Common Meadow Mushroom is common, and in some cases abundant, all through the North of Ireland. — H. W. L. var. pratensis. Vitt. Raughlan, Co. Armagh, 1885.— H. W. L. var. silvicola. Vitt. Derryadd, near Lurgan, Co. Armagh, 1885.— H. W. L. 125. Agaricus (Stropharia) aeruginosus. Curt. Killymoon, Co. Tyrone, Massereene Park, Co. Antrim, 1884 ; Ardmore Glebe, Co. Armagh, Donard Demesne, and Tollymore Park, Co. Down, 1885. — H. W. L. 126. Agaricus (Stropharia) semiglobatus. Batscli. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Ardmore Glebe, Co. Armagh, 1883; Rademon, Co. Down, 1885.— H. W. L. 127. Agaricus (Hypholoma) sublateritius. Fi . Abundant on an old stump near the entrance to Killymoon Demesne from Cookstown, Co. Tyrono, 1884. — H. W. L. 128. Agaricus (Hypholoma) epixanthus. Fr. In a wood at the Ferry Hill, near Omoath, Co. Louth, 1883.— H. W. L. 279 Lett — The Fungi of the North of Ireland, 129. Agraricus (Hypholoma) fascicularis. Hud. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Common and abun- dant everywhere. Ardmore, Co. Armagh, Maralin, Donard Demesne, Tolly- more Park, and Rademon, Co. Down, 1885.— H. W. L. 130. Agraricus (Hypholoma) fascicularis var. robustior. Pers. Ardmore, Co. Armagh, 1885.— H. W. L. (See Fries, Epic., 2nd ed., p. 292.) 131. Agraricus (Hypholoma) lacrymabundus. Fr. Rademon, Co. Down, 1885. — H. W. L. 132. Agraricus (Hypholoma) appendlculatus. Bull. Ardmore Glebe, Co. Armagh, 1884; Rademon, Co. Down, 1885.— H. W.L. 133. Agraricus (Psilocybe) foenisecii. P. Raughlan, 1884, and Ardmore Glebe, Co. Armagh, 1885.— H. W. L. 134. Agraricus (Panaeolus) separatus. L. Near Belfast, Templeton (Ag, semiovotus'), Ann. Nat. Hist., Yol. Y. Shore of Lough Neagh, at Derryadd, near Lurgan, Co. Armagh, 1888 ; Killy - moon, Co. Tyrone, 1884 ; Slieve Donard, Co. Down, 1885.— H. W. L. 135. Agraricus (Panaeolus) fimiputris. Bull'. Ardmore Glebe, Co. Armagh, 1883; Killymoon, Co. Tyrone, 1884.— H. W.L. 136. Agraricus (Psathyrella) hiascens. Fr. In the garden at Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 137. Agraricus (Psathyrella) disseminatus. Fr. hear Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Warrenpoint, County Down, 1883.— H. W. L. 138. Coprinus comatus. Fr. Ardmore, and Raughlan, Co. Armagh, 1883 ; Drumcro, and Rosstrevor, Co. Down, Cookstown, Co. Tyrone, 1884 H. W. L. 139. Coprinus ovatus. Fr. Killymoon, Co. Tyrone, 1884.— II W. L. 140. Coprinus atramentarius. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Derryadd, County Armagh, 1883; Rademon, Co. Down, 1885,— H, W.L, 280 Lett— The Fungi of the North of Ireland. 141. Coprinus fuscesens. Fr. Ardmore Glebe, Go. Armagh, 1884.— H. W. L. 142. Coprinus picaceus. Fr. Derryadd, near Lurgan, 1882, and Ardmore Glebe, Co. Armagh, 1885. "Very rare. — H. W. L. 143. Coprinus niveus. Fr. Derrymacash, Co. Armagh, 1885. Rare.— H. W. L. 144. Coprinus micaceus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Ardmore Slebe, Co. Armagh j Killymoon, Co, Tyrono, 1884 ; Rademon, and Donar o go, Down, 1885. — H. W. L. 145. Coprinus plicatilis. Fr. Ardmore Glebe, Co. Armagh, Killymoon, Go. Tyrone, Donard Lodge, Go. Down, 1884. — H. W. L. 146. Coprinus hemerobius. Fr. Narrow Water Demesne, Go. Down, in old pasture, 1883. Very rare.— H. W. L. 147. Bolbitius boltoni. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 148. Bolbitius fragilis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 149. Bolbitius tener. B. Abundant in grass on Rosstrevor Mountain, Co. Down, fiom 900 feet 1500 feet, 1883.— H. W. L. 150. Cortinarius (Phlegmacium) caper atus. Fr. Shane’s Castle Park, Co. Antrim, 1883. — H. W. L. 151. Cortinarius (Pblegmacium) varius. Fr. Ardmore Globe, Co. Armagh, 1883. — H. W. L. 152. Cortinarius (Pblegmacium) cyanipes. Fr. Donard Demesne, Co. Down, 1885.— G. Pirn, and H. W. L. 153. Cortinarius ’.(Phlegmacium) purpurascens. Fr. Ardmore Glebe, Co. Armagh, and Donard Demesne, Co. Down, 1885.- H. W. L. Lett — The Fungi of the North of Ireland. 281 154. Cortinarius (Phlegmacium) scaurus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 155. Cortinarius (Myxacium) collinitus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 156. Cortinarius (Xnoloma) callisteus. Fr. Donard Demesne, Co. Down, 1885.— G. Pirn, and H. W. L. 157. Cortinarius (Xnoloma) bulliardi. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 158. /Cortinarius (Xnoloma) sublanatus. Fr. Near Belfast, Templeton, Ann. Nat . Hist., Vol. V. 159. Cortinarius (Dermocybe) anomalus. Fr. Tolly more Park, Co. Down, 1885.— G. Pirn, and H. W. L. 160. Cortinarius (Dermocybe) cinnamoneus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Donard Demesne, and Tolly more Park, County Down, 1885 G. Pirn, and H. W. L. 161. Cortinarius’(Telamonia) evernius. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 162. CortinariusKTelamonia^g-entilis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 163. Cortinarius (Hygrocybe) dilutus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 164. Cortinarius (Hygroeybe) acutus. Fr. Bank of the Lagan, near Bolfast, Co. Antrim, B.N.F.C. Excursion, July, 1884. — J. J. Andrew, and H. W. L. 165.1 lepistafpersonata. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Tollymore Park, Co. Down, and in plantation at Glenmore, near Lisburn, Co. Antrim 1885.— H. W. L. 166. Paxillus involutus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Raugklan, and Ard- more Glebe, Co. Armagh, and Killymoon, Co. Tyrone, 1884 ; Rademon, and Donard Demesne, Co, Down, 1885,— H. W. L. 282 Lett— The Fungi of the North of Ireland . 167. Hygropliorus eburneus. Fr. Near Belfast, Templeton, &nn. Nat. Hist., Yol. Y. Tollymore Park, Oo. Down, 1885. — H. W. L. 168. Hygrophorus pratensis. Fr. Near the Ross Monument at Rosstrevor, and in Tollymore Park, Co. Down, 1885. — H. W. L. 169. Hygrophorus virgineus. Fr. Goragh Wood, Co. Armagh, 1888. Abundant in short grass about New- castle, Co. Down, 1884.— H. W. L. 170. Hygrophorus nlveus. Fr. Donard Demesne, Co. Down, 1885.— G. Pirn, and H. W. L. 171. Hygrophorus ovimis. Fr. Near Belfast, Templeton ( H . compresses, Sow.), Ann. Nat. Hist., Yol. V. 172. Hygrophorus ceraceus. Fr. Rosstrevor, 1883, and Donard Demesne, 1884, Co. Down.— H. W. L. 173. Hygrophorus coccineus. Fr. Noar Belfast, Templeton, Ann. Nat. Hist., Yol. V. Among the sandhills at Newcastle, and Donard Demesne, Co. Down, 1885.— H. W. L. 174. Hygrophorus miniatus. Fr. In grass at 1100 feet on Rosstrevor Mountain, Co. Down, 1883 ; at 2204 feet on Shan Slieve, Co. Down, 1885.— H. W. L. 175. Hygrophorus punlceus. Fr. Near Belfast, Templeton, Ann. Nat. Hist. Yol. Y. 176. Hygrophorus obrusseus. Fr. Rosstrevor Wood, Co. Down, 1883 ; Killymoon, Co. Tyrone, 1884.-H. W. L. 177. Hygrophorus conicus. Fr. Ardmore, County Armagh, Killymoon, Co. Tyrone, and sandhills near Newcastle, Co. Down, 1884. — H. W. L. 178. Hygrophorus chlorophanus. Fr. Clonallon, Co. Down, 1883 ; Killymoon, Co Tyrone, 1884 ; Tollymore Park, Co. Dovn, 1885. — H, W. Lt 283 Lett — The Fungi of the North of Ireland. 179. Hygrophorus psittacinus. Fr. Shane s Castle Park, Co. Antrim, 1883 ; Donard Demesne, County Down 1885.— H. W. L. 180. Gomphidius glutinosus. Fi\ Raugklan, Co. Armagh, 1883. Abundant.— H. W. L. 181. Gomphidius viscidus. Fr. Killymoon, Co. Tyrone, and Maralin, Co. Down, 1883 C. II. Waddell. Raughlan, Co. Armagh£ 1884.— H. W. L. 182. Xiactarius tonninosus. Fr. Shane’s Castle Park, Co. Antrim, 1883 ; Tollymore Park, County Down 1885.— H. W. L. 183. Xiactarius cilicioides. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 184:. Xiactarius turpis. Fr. Ardmore Glebe, Co. Armagh, 1884 H. W. L. Rademon, County Down, 1885. — 185. Xiactarius contro versus. Pers. Ardmore Glebe, Co. Armagh, under trees in old pasturage, 1884 ; Tolly- more Park, Co. Down, 1885.— H. W. L. 186. Xiactarius zonarius. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Tollymore Park Co Down, 1885.— H. W. L. ’ 187. Xiactarius blennius. Fr. Narrow Water Demesne, Co. Down, and a wood at the Ferry Hill near Omeath, Co. Louth, 1883 ; Tollymore Park, Co. Down, 1885. H. W. L. 188. Xiactarius hysginus. Fr. Rademon, Co. Down, 1885.— H. W. L. 189. Xiactarius piperatus. Fr. Ardmore Glebe, County Armagh, 1884; Tollymore Park, Co. Down. 1885 — H. W. L. ’ 190. Xiactarius vellereus. Fr. Ardmore Glebe, Co. Armagh, 1885.— H. W. L. 284 Lett— The Fungi of the North of Ireland. 191. lactarius deliciosus. Fr. Knockbarragh Hill, Co. Down, 1883; Killy moon, County ’ Ty™n®> and Raughlan, Co. Armagh, 1884 ; Donard Demesne, Co. Down, 1885.-H. W. xn 192. iiactarius pallidus. Fr. Killymoon, Go. Tyrone, and Raughlan, Co. Armagh, very large, 1884 ; Tollymore Park, Go. Down, 1885.— H. W. L. 193. Lactarius quietus. Fr. Ardmore Glebe, Co. Armagh, 1883; Killymoon, Co. Tyrone, 1884 ; Tolly- more Park, Co. Down, 1885.— H. W. L. 194. Lactarius tlieiogalus. Fr. Knockbarragh Hill, Go. Down, 1888. H. W. L. 195. Iiactarius rufus. Fr. Killymoon, County Tyrone, and Raughlan, Co. Armagh, 1884 ; Donard Demesne, Gounty Down, 1885.— H. W. L. 195. Lactarius glyciosmus. Fr. Raughlan, Co. Armagh, under Scotch firs, 1884.— H. W. L. 197. Lactarius serifluus. Fr. Ardmore Glebe, Go. Armagh, 1882 ; Shane’s Castle Park, Co. Antnm, 1883; Killymoon, Co. Tyrone, 1884; Donard Demesne, Co. Down, 1885.- H. W. L. 198. Lactarius volemum. Fr. Ardmore Glebe, Co. Armagh, abundant, 1883; Rademon, Co. Down 1885. — H. W. L. 19 9. lactarius mitissimus. Fr. Tollymore Park, Co. Down, 1885.-G. Pirn, and H. W. L. 200. lactarius subdulcis. Fr. Ardmore Glebe, Co. Armagh, 1883 ; Killymoon, County Tyrone, 1884— H. W. L. 201. lactarius pargamenus. Sow. (For description see Fries, Epic., 2nd edition, 1874, p. 430.) Nano Water Demesne, Co. Down, 1883.— H. W. L. 202. Russula nigricans. Fr. Killymoon, Co. Tyrone, 1884 ; Rademon, and Tollymore Park, County Down, 1885. Not common. — H. W. L. 285 Lett — The Fungi of the North of Ireland, 203. Russula adusta. Fr. Rademon, Co. Down, 1885. — H. W. L. 20ft. Russula drimeia. Cooke. Raughlan, Co. Armagh, 1884. — H. W. L. 205. Russula virescens. Fr. Rosstrevor Wood, County Down, abundant, 1883 ; Tollymore Park, Co. Down, 1885.— H. W. L. 206. Russula rubra. Fr. Raughlan Island, Co. Armagh, abundant, 1883 ; Killymoon, Co. Tyrone, 1884 ; Rademon, Co. Down, 1885. — H. W. L. 207. Russula heterophylla. Fr. Killymoon, Co. Tyrone, 1884.— H. W. L. 208. Russula emetica. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Raughlan, County Armagh, 1883 ; Killymoon, Co. Tyrone, 1884 ; Tollymore Park, Co. Down, 1885.— H. W. L. 209. Russula fragilis. Fr. Donard Demesne, Co. Down, 1885. — G. Pirn, and H. W. L. 210. Russula Integra. Fr. Ardmore Glebe, Co. Armagh, 1883 ; Donard Demesne, Co. Down, 1885. — H. W. L. 211. Russula alutacea. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 212. Cantharellus cibarius. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Tollymore Park, Co. Down, 1883.— H. W. L. 213. Cantharellus aurantiacus. Fr. Narrow Water Demesne, 1883, Tollymore Park, and Donard Demesne, 1885, Co. Down,— H. W. L. 21ft. Cantharellus lobatus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 286 Lett— The Fungi of the North of Ireland. 215. Marasmius urens. Fr. Donard Demesne, Co. Down, 1885. — H. W. L. 216. Marasmius peronatus. Fr. Rademon, Co. Down, 1885. — H. W. L. 217. Marasmius oreades. Fr. Derrytrasna, Co. Armagh, grass bank along roadside, 1883 ; Newcastle, Co. Down, abundant among the sandhills, 1885. — H. W. L. £>. A. Stewart sent me specimens of this collected many years ago by him in the latter locality. 218. Marasmius erythropus. Fr. Donard Demesne, Co. Down, abundant in upper part of the wood near the granite quarry; and Rademon, Co. Down, 1885. — H. W. L. 219. Marasmius rotula. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Rosstrevor Wood, 1883 ; and Rademon, 1885, Co. Down.— H. W L. 220. Marasmius androsaceus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 221. Xientinus tigrinus. Fr. Ram’s Island, Lough Neagh, 1884. Yery rare.— H. W. L. 222. laentinus flabelliformis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 223. Boletus luteus. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Raughlan, County Armagh ; Killymoon, County Tyrone ; and Donard Demesne, Co. Down, 1884. — H. W. L. 224. Boletus elegans. Schum. Top of Knockbarragh Hill, 905 feet, Co. Down, 1883 ; Crawfordsburn, Co. Down, 1884 ; Tollymore Park, and Donard Demesne, County Down, 1886. Common. — H. W. L. 225. Boletus flavus. With. Donard Demesne, Co. Down, 1883 ; wood at the Ferry Hill, near Omeath, Co. Louth, 1883 ; Killymoon, Co. Tyrone, 1884 ; Rademon, Co. Down, 1885. -H. W.L. 287 Lett— The Fungi of the North of Ireland. 226. Boletus laricinus. Berk. Tollymore Park, 1884, and Donard Demesne, 1885, Co. Down. Not com- mon.— H. W. L. 227. Boletus g-ranulatus. L. Drumcro, near Maralin, County Down, 1884— C. H. Waddell. Donard Demesne, Co. Down, 1884 ; Tollymore Park, Co. Down, 1885.— H. W. L. 228. Boletus bovinus. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Most abundant in heathy places in plantations of larch and Scotch fir, in Donard Demesne, and Tollymore Park, County Down, 1885 H. W. L. 229. Boletus piperatus. Bull. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 230. Boletus chrysenteron. Fr. Tollymore Park, Co. Down, 1885.— G. Pirn, and H. W. L. 231. Boletus subtomentosus. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Tollymore Park, Co Down, 1885.— G. Pirn, and H. W. L. 232. Boletus variecolor. B. and Br. Ardmore Glebe, Co. Armagh, 1884. Rare.— H. W. L. 233. Boletus pachypus. Fr. Killymoon, Co. Tyrone, 1884; Rosstrevor Wood, Donard Demesne, and Tollymore Park, Co. Down, 1885. Common.— H. W. L. 234. Boletus edulis. Bull. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Raughlan, County Armagh, 1883 ; Tollymore Park, and Donard Demesne, County Down, 1884 ; Rademon, Co. Down, 1885. Not common. — H. W. L. 235. Boletus fragrans. Vitt. Ardmore Glebe, Co. Armagh, 1884. Yery rare.— H. W. L. 236. Boletus impolitus. Fr. Ardmore Glebe, Co. Armagh, 1883; Killymoon, Co. Tyrone, 1884; Tolly- more Park, Co. Down, 1885.— H. W. L. 237. Boletus aestivalis. Fr. In several plantations about Warrenpoint, Co. Down, 1883.— H. W. L. 288 Lett— The Fungi of the North of Ireland. 238. Boletus satanas. Lenz. Moira Demesne, and Donard Demesne, Co. Down, 1884. Rare— H. W. L. 239. Boletus luridus. Fr. Gillhall.Co. Down, 1888-0. H. Waddell. Ardmore, Co. Armagh 1883 ; Killymoon, County Tyrone, and Tollymore Park, County Down, 1884. Rare- H. W. L. 240. Boletus scaber. Fr. In a plantation near the Vicarage, Warrenpoint, and Rosstrevor Wood, Co Down, 1883 ; Raughlan, Co. Armagh, 1884 , Donard Demesne, and roily- more Park, Co. Down, 1885. Rather common— H. W. L. 241. Boletus castaneus. Bull. Tollymore Park, Co. Down, 1885— G. Pirn, and H. W. L. 242. Polyporus brumalis. Fr. Raughlan Island, Co. Armagh, 1884.-H. W. L. 243. Polyporus lentus. Berk. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 244. Polyporus'perennis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. Down, 1885.— G. Pim, and H. W. L. Tollymore Park, Co. 245. Polyporus squammosus. Fr. Near Belfast, Templeton, Ann. Nat. Hist. Vol. V Ardmore Glebe, and Raughlan, Co. Armagh, 1883; Killymoon, Co. Tyrone, 1884.-H. W. L. 246. Polyporus varlus. Fr. Tollymore Park, Co. Down, 1884.— C. H. Waddell. 247. Polyporus giganteus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V Rosstrevor Wood, Co. Down, 1883 —0. H. Waddell. Langford Lodge, Co. Antrim, 1883.- H. W. L. 248. Polyporus sallgnus. Fr. On a largo willow, Ardmore Glebe, Co. Armagh, 1884— H. W. L. 249. Polyporus cbloneus. Fr. Killymoon, County Tyrone, 1884.— H. W. L. 289 Lett — The Fungi of the North of Ireland. 250. Polyporus fumosus. Fr. On a rotten stump, near the House, Narrow Water Demesne, Oo. Down, 1883.— H. W. L. 251. Polyporus adustus. Fr. On a gate post, near Derryadd Dispensary, Lurgan, Co. Armagh, 1883. — H. W. L. 252. Polyporus spumous. Fr. Killymoon, Co. Tyrone, 1884 ; Tollymore Park, County Down, 1885.— H. W. L. 253. Polyporus dryadeus. Fr. Shane’s Castle Park, Co. Antrim; and Tollymore Park, County Down ; 1883. -H. W. L. 254. Polyporus betulinus. Fr. Tollymore Park, Co. Down, 1884; Rademon, Co. Down, 1885.— H. W. L. 255. Polyporus pallescens. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Tol. Y. 256. Polyporus fomentarius. Fr. Lurgan Demesne, Co. Armagh, 1883 ; Loughrey, Co. Tyrone, 1884. — H. W. L. Portavoe, Co. Down, 1885. — J. B. A. Hughes. Rademon, County Down, 1885.— H. W. L. 257. Polyporus Iguarius. Fr. Drumcro, near Maralin ; and Gilhall, County Down ; 1883— C. H. Waddell. Ardmore, Co. Armagh, 1884.— H. W. L. 258. Polyporus fraxineus. Fr. On the stump of a large ash tree, Killyglen, near Larne, County Antrim, 1884. — H. W. L. 259. Polyporus annosus. Fr. Bangor, Co. Down, 1836; and Collin Glen, Co. Antrim, 1841.— W. Thomp- son. Narrow Water, 1883 ; Crawfordsburn, 1883 ; Belvoir Park, 1884 ; Donard Demesne, and Tollymore Park, 1885. Common in County Down. — H. W. L. 260. Polyporus radlatus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. Rademon, County Down, 1885. Not common. — H. W L. 2 9o Lett— The Fungi of the North of Ireland. 261. Polyporus fibula. Fr. On the inside of the sash of a window, in the “ prophet’s chamber ” of St. Patrick’s House, Broughshane, Co. Antrim, 1883.— H. W. L. 262. Polyporus velutinus. Fr. Holywood, Co. Down, 1841.— W. Thompson. Ardmore, Co. Armagh, 1883 ; Tollymore Park, Co. Down, 1885— H. W. L. 263. Polyporus versicolor. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Cultra, Co. Down, 1835. W. Thompson. Drumcro, near Maralin, County Down, 1883.— C. H. Waddell. Ardmore, Co. Armagh, 1883. Yery common, and variable.— H. W. L. 264. Polyporus abietinus. Fr. Rosstrevor Wood, Co. Down, 1883.-0. H. Waddell. Raughlan, County Armagh, 1884 ; Tollymore Park, Co. Down, 1885. — H. W. L. 265. Polyporus ferruginosus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 266. Polyporus violaceus. Fr. On a dead Scotch fir at Raughlan, Co. Armagh, 1885.— H. W. L. 267. Polyporus purpureus. Fr. On decayed willow trees ; common throughout the parish of Montiaghs, or Ardmore, Co. Armagh, 1884.— 'H. W. L. 268. Polyporus medulla-panis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. On the insido of the wooden cover of a well, Ardmore Glebe, Co. Armagh, 1883. H. W. L. 269. Polyporus vulgaris. Fr. Killymoon, County Tyrone, 1884. — H. W. L. 270. Polyporus vaporarius. Fr. Ardmore Glebe, Co. Armagh, 1884. — H. W. L. 271. IVIerulius corlum. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 272. Itterulius lacrymans. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Vt 291 Lett — The Fungi of the North of Ireland. 2,73. Fistulina hepatica. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Tollymore Park, Co. Down, 1888. Bare.— H. W. L. 274. Hydnum repandum. L. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Wood at the Ferry Hill, near Omeath, Co. Louth, and Rosstrevor Wood, Co. Down, 1883 ; abun- dant in Donard Demesne, Co. Down, 1884.— H, W. L. 275. Hydnum graveolens. Del. On an oak stump in Tollymore Park, County Down, 1884. Very rare — H. W. L. 276. Zrlex otoliquus. Fr. Warrenpoint, Co. Down, 1883 ; Ardmore Glebe, County Armagh 1884 — H. W. L. 277. Radulum orbicular e. Fr. Rosstrevor Wood, County Down, on dead hazel, 1883.— C. H. Waddell. 278. x Grandinia granulosa. Fr. Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 279. Craterellus cornucopioides. Fr. Rosstrevor Wood, 1883, and Donard Demesne, 1885, Co. Down.— H. W. L. 280. Craterellus sinuosus. Fr. Donard Demesne, Co. Down, 1884.— H. W. L. 281. Thelephora cristata. Fr. On beech leaves near the grotto in Tollymore Park, Co. Down, 1885 G. Pirn, and H. W. L. 282. Thelephora mollissima. P. Rademon, Co. Down, 1885.— H. W. L. 283. Thelephora laciniata. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 284. Thelephora caesla. P. Hillsborough Demesne, County Down, 1883. — H. W. L. 285. Stereum purpureum. Fr. Near Belfast, Templeton ( Thelephora purpurea ), Ann. Nat. Hist., Vol. V. Raughlan, County Armagh, 1884.— H. W. L. 292 Lett- —The Fungi of the North of Ireland. 286. Stereum hirsutum. Fr. Near Belfast, Templeton ( Thelephora hirsute ), Ann. Nat. Hist Vol. V. Ardmore, Co. Armagh, 1882; Killymoon, Co. Tyrone 1884; Maralm, and Eademon, and Donard Demesne, County Down, 1885.-H. W. u. 287. Stereum sanguinolentum. Fi . Donard Demesne, Co. Down, 1885, on stump of larch, and felled Sootch firs. Not common.— H. W. L. 288. Hymenoclisete rublginosa. Lev. Near Belfast, Templeton ( Thelephora rubiginosa), Ann. Nat. Hist., Vol. V. Raughlan, Co. Armagh, 1884; Killymoon, Co. Tyrone, 1884; Rademon, Co. Down, 1885. — H W. L. 289. Corticium evolvens. Fr. Rosstrevor Wood, Co. Down, 1883. H. W. L. 290. Corticium araclmoideum. Berk. Iiolywood House, Co. Down, 1841. — W. Thompson. Killymoon, County Tyrone, 1884:. — H. W. L. 291. Corticium leave. Fr. C ultra, and Bangor, Co. Down, 1S86.-W. Thompson. Caledon Demesne and Killymoon, Co. Tyrone, 1884; Ardmore, Co. Armagh, 1884; Donai Demesne ; and Tollymore Park, County Down ; 1885.-H. W. L. 292. Corticium velutinum. Fr. The Oaks, Co. Derry, 1842.— G. Lyle. Stranmillis, near Belfast, 1885. — S. M. Malcomson. Raughlan, Co. Armagh, 1885.— H. W. L. 293. Corticium coeruleum. Fr. Near Belfast, Templeton ( Thelephora ccerulea ), Ann. Nat. Hist., Vol. 294. Corticium calceum. Fr. Near Belfast, Templeton ( Thelephora calcea), Ann. Nat. Hist., Vol. V. Stranmillis, near Belfast, 1884.— S. M. Malcomson. 29 5. Corticium quercinum. P. On decayed beech, Warrenpoint, Co. Down, 1883.— C. H. Waddell. 296. Corticium nudum. Fr. Bark of laurel, Sydenham, Co. Down, 1883.-W. H. Patterson. Boss- trevor Wood, Co. Down, 1883. — H. W. L. 293 Lett — The Fungi of the North of Ireland, 297. Corticium comfluens. Fr. Near Belfast, Templeton (Thelephora epidermea, Fej's), Ann. Nat. Hist., Vol. V. Ardmore Glebe, Co. Armagh, 1885. — H. W. L. 298. Corticium comedens. Fr. On a decayed oak branch, Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 299. Corticeum lacteum. 0 Fr. Near Belfast, Templeton (Bimantia Candida ), Ann. Nat. Hist., Yol. V. 300. Sparassis iaminosa. On the occasion of the first Fungus Foray in Ireland, to Shane’s Castle, Co. Antrim, 1883, I found an immense Sparassis growing on the stump of an old oak near the ruins. It resembled a huge cauliflower, and was more plaited than .S. crispa, as figured in Cooke’s Handbook, and by Berkeley in Intellectual Observer. If not S. Iaminosa , it comes very near it. — H. W. L. 301. Clavaria fastigiata. D. C. Near Belfast, Templeton ( Clavaria pratensis), Ann. Nat. Hist., Yol. Y. Rademon, C<5. Down, 1885. — H. W. L. 302. Clavaria coralloides. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Yery abundant in Shane’s Castle Park, Co. Antrim, 1883 ; Killymoon, County Tyrone, 1884 ; Donard Demesne, Co. Down, 1885. — H. W. L. 303. Clavaria cinerea. Bull. Very abundant in the woods of Killymoon, Co. Tyrone, 1884. — H. W. L. 304. Clavaria rugosa. Bull. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Shane’s Castle Park, Co. Antrim, abundant, 1883 ; Donard Demesne, Co. Down, 1884. — H. W. L. 305. Clavaria fusiformis. Sow. Near the waterfall, opposite the Ferry at Narrow Water, on County Louth side ; and Ardmore Glebe, Co. Armagh ; 1883. — H. W. L. 306. Clavaria insequalis. Mull. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 307. Clavaria vermiculata. Scop. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Drumcro, near Maralin, Co. Down, 1884 C. H. Waddell. 294 Lett— The Fungi of the North of Ireland. 308. Clavaria fragllis. Holmsk. glieve Donard, Co. Down, at 1100 feet, 1884 ; Donard Demesne, and Rademon, Co. Down, 1885. — H. W. xj. 309. Clavaria pistillaris. L. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 310. Clavaria tuberosa. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 311. Clavaria^cornea. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 312. Typbula erytbropus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 313. Pistillaria micans. Fr. Ardmore Glebe, Co. Armagh, 1883.— H. W. L. 314. Pistillaria puberula. Berk. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 315. Tremella fimbriata. P. Ardmore Glebe, Co. Armagh, 1883.— H. W. L. 316. Tremella foliacea. P. Near Londonderry, 1883.— G. Y. Craig. Ardmore Glebe, Co. Armagh, 1883 ; Rademon, Co. Down, 1885. — H. W. L. 317. Tremella mesenterica. Betz. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Marahn, Co. Down, 1883.— C. H. Waddell. Ardmore Glebe, County Armagh j Killymoon, County Tyrone, 1884 ; Rademon, Co. Down, 1885.— H. W.L. 318. Tremella albida. Hud. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Ardmore, County Armagh, 1883; Killymoon, Co. Tyrone, and Rosstrevor Wood, Co. Down, 1884; Tollymore Park, Co. Down, 1885. — H. W. L. 319. Tremella intumescens. Sow. Portavoe, Co. Down, 1884.— J. B. A. Hughes. Lett — The Fungi of the North of Ireland. 295 320. Hlrneola aurlcula-judae. Berk. On very old and large elder trees inside the ruins of Maghera Church, near Newcastle, 1884 ; and Donard Demesne, Co. Down, 1885.— H. W. L. 321. TCTgematelia encephala. Fr. On a black alder stump, Raughlan, County Armagh, 1884. Yery rare.— H. W. L. 322. Dacrymyees stillatus. Nee. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. Ardmore, County Armagh ; Tollymore Park ; and Donard Demesne, Co. Down ; 1885. Common. — H. W. L. 323. Phallus impudlcus. Linn. Castledawson Demesne, Co. Derry.— S. A. Stewart. Near Holy wood, Co. Down, 1883.— R. L. Praeger. Killymoon, Co. Tyrone, 1883 ; Tollymore Park ; and sandhills near Newcastle, Co. Down ; 1885. Not common.— H. W. L. 324. Bovlsta nlgrescens. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Ardmore Glebe, Co. Armagh, 1882 ; Killymoon, Co. Tyrone, 1883. Rare.— H. W. L. 325. Bovlsta plumbea. P. I found one specimen among the sandhills, near Newcastle, Co. Down, in October, 1884. Rare.— H. W. L. 326. Bycoperdon giganteum. Batsch. Shane’s Castle Park, Co. Antrim, 1883.-H. W. L. This species is not common m the district. I heard of a large specimen found near Belfast, in 1884, that was exhibited in a seedsman’s window in that town ; and in Sep- tember, 1885, one was sent to me weighing 8 lbs., and measuring 3 ft. 10 in. in girth. It grew in Belvoir Park, Co. Down. 327. Iiycoperdon coelatum. Fr. .Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Rademon, and Donard Demesne, County Down, 1885.— H. W. L. 328. Iiycoperdon pusillum. Fr. Killymoon, Co. Tyrone, 1884. Not common.— H. W. L. 329. Iiycoperdon saccatum. Vahl. — Gleb6’ C0* A^Inash, 1883 ’ Moira Demesiie? Co. Down, 1884. 296 Lett-— The Fungi of the North of Ireland. 330. Jjycoperdon gemmatum. Fr. Near tbe Ness Waterfall, Co. Derry, 1842.-W . Thompson. Ranghlan, and Ardmore, Co. Armagh, 1888 ; Kademon, Tollymore Park, and Donard Demesne, County Down, 1885. Common..— H. W. L. 331. tycoperdon pyriforme. Schoeff. Rosstrevor Wood, Co. Down, 1883; Killymoon, Co. Tyrone, and Ardmore Glebe, Co. Armagh, 1884 ; Tollymore Park, Co. Down, 188o. H. W. . 332. Scleroderma vulgare. Fr. Narrow Water Demesne, Co. Down, and Shane’s Castle Park County Antrim, 1888 ; Ardmore, Co. Armagh, Killymoon, Co. Tyrone, and Donard Demesne, Co. Down, 1885. Common.— H. W. L. 333. Scleroderma toovista. Fr* Near Belfast, 1884.— J. J. Andrew. 334. I«y cogala epidendrum. Fr. Ardmore, Co. Armagh, 1883.-H. W. L. By the Lagan’s banks, near Belfast, 1885.— S. M. Malcomson. 335. JEthalium septicum. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 336. Spumaria alba. D. G. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. This enrious plant closely resembles the droppings of some bird lying on moss or grass. Donard Demesne, Co. Down, 188o. — H. W. L. 337. Didymium furfaceum. Fr. Killymoon, County Tyrone, 1884.— H. W. L. 338. Bldymium melanopus. Fr. Donard Demesne, Co. Down, 1884.— H. W. L. 339. Physarum clnerum. Mr. W. B. Grove so named a plant on bark of decayed holly from Ross- trovor Wood, Co. Down, 1885. H. W. L. 340. Dldymlum physaroides. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 341. Angioridium slnuosum. Grev. Near Belfast, Templeton, {Physarum sinuosum ), Ann. Nat. Hist., Vol. V, 297 Lett— ‘The Fungi of the North of Ireland. 342. Craterlum mlnutum. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Maralin, County Down, 1884.— C. II. Waddell. 343. Stemonitis fusca. Roth. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Warrenpoint Co Down, 1883.— 0. H. Waddell. 344. Stemonitis typhoides. D. G. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 345. Stemonitis ovata. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 346. Dictydlum umbilicatum. Schrad, Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 347. Arcyria incarnata. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. Errigle, County Cavan, 1884. — T. H. Moorhead. Ardmore, Co. Armagh, 1883. H. W. L. 348. Arcyria nutans. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 349. Trichia chrysosperma. D. C. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 350. Trichia varia. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 351. Trichia serpula. P. Purdysburn, Co. Down, 1885.— S. M. Malcomson. 352. Perichaena populina. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 353. Iiicea cylindrica. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 354. lilcea fragiformis. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 355. Cyathus striatus. Hoffm. Near Belfast, 1875.— W. Hr Patterson. 298 Lett— The Fungi of the North of Ireland. 356. Crucibulum vulgare. Tul. Near Belfast, Templeton (. Nidularia crucibulum , Pers .), Ann. Nat. Hist. Vol. V. 357. Spbaerobolus stellatus. Tode. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 353. phoma concentricum. l)esm. On leaves of Yucca , Raughlan, Co. Armagh, 1884.-H. W. L. 359. Spbaeropsis taxi. Berk. Near Belfast, Templeton ( Sphceria Taxi, Sow.), Ann. Nat,. Hist., Vol. V. 360. Diplodia ilicis. Curr. Near Belfast, Templeton ( Sphceria ilicis, Schleich ), Ann. Nat. is . Vol. V. 361. Stagonospora pini. This new species was collected at Raughlan, Co. Armagh, r i ttt -r firrwa on “ New or Noteworthy description is given m a paper by VT. B. Giov < sig Fungi,” in Journal of Botany, 1885 Perithecns epiphyUis, t.ctis rotundatis, atris ; sporulis pallide luteolis, singulis ya mis, cy fusoides, utrinque subobtusis, 1 dein 3 septatis, 1 — p x P- foliiswPini Sylvestris. Hibernia, H. W. Lett, August. ’ 362. Septoria castanaecola. Desm. Warrenpoint Vicarage, 1883 ; Tollymore Park, County Down, 1884.- H. W. L. 363. Ascocbyta diantbi. Berk. Ardmore Glebe, Co. Armagh, 1883; Warrenpoint, County Down, 188 . — H. W. L. 364. Asteroma reticulatum. Berk. Ardmore Glebe, Co. Armagh, 1883.— H. W. L. 365. Rabenborstia tiliae. Fr. Near Belfast, Templeton ( Sphceria tillioe, Pers.), Ann. Nat. Hist., Vol.V. 366. Discella carbonacea. Fr. On dead twigs of Golden Willow, in Ardmore Churchyard, Co. Armagh, 1884.- H. W. L. 299 Lett — The Fungi of the North of Ireland. 367. Ceuthospora lauri. Grev. Desertcreat, Co. Tyrone, 1883.— H. W. L. 368. Melanconium bicolor. Nees. Raughlan, Co. Armagh, 1884.— H. W. L. 369. Coryneum disciforme. Kze. Drumcro, near Maralin, County Down, 1883.— C. H. Waddell. 370. Phrag-midium mucronatum. Link. Near Belfast, Templeton (Aregma mucronatum , P.), Ann. Nat. Hist., Vol. V. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Near Strabane, Co. Tyrone, 1883; Ardmore, Co. Armagh, 1884. Common.— H. W. L. 371. Phrag-midium bulbosum. Schl. Near Belfast, Templeton ( Vredo ruborum and Aregma bulbosum ), Ann. Na,t. Hist., Aol. V. Errigle, Co. Cavan, 1884 T. H. Moorhead. Warren- point, Co. Down ; Ardmore, County Armagh ; 1883. H. W. L. 372. Phrag-midium gracile. Grev. Collin Glen, Co. Antrim, 1836.— W. Thompson. Errigle, Co. Cavan.— T. H. Moorhead. Ardmore, Co. Armagh, 1883.— H. *W. L. 373., Phrag-midium obtusum. Link. Uredo spores on Potentilla reptans , near Strabane, 1883 ; and Loughrey Co. Tyrone, 1884.— H. W. L. 374. Triphrag-miunTulmariae. Link. Errigle, Co. Cavan, 1884. — T. H. Moorhead. Ardmore, Co. Armagh, 1883 ; banks of the Lagan, near Belfast, Co. Antrim, 1885. — H. W. L. 375. Puccinia graminis. P. Near Belfast, Templeton ( Uredo rubigo ), Ann. Nat. Hist., y0l. Y. Near Belfast.— W.f Thompson. Errigle, County Cavan, 1884.— T. H. Moorhead. Drumcro, near Maralin, County Down, 1883.— C. H. Waddell. Ardmore, Co. Armagh, 1883. Common.— H. W. L. 376. Puccinia arundinacea. Hedw. Errigle, Co. Cavan, 1884. _T. H. Moorhead. On reeds in Closet River, at Raughlan, County Armagh ; Bog Meadows, near Belfast, 1883.— H. W. L. 377. Puccinia striola. Link. Balmoral, near Belfast, Co. Antrim, 1885.— S. M. Malcomson. 3oo Lett— The Fungi of the North of Ireland. 378. Puccinia coronata. Corda. Banks of the Lagan, near Belfast, 1884.— J. J. Andrew. 379. Puccinia glechomatis. D. C. Ardmore Glebe, Co. Armagh, 1884. H. W. L. 380. Puccinia mentlise. P . Near Belfast, Templeton (Uredo labialarum), Ann. Nat. Hist., Vol. Y. Erricrle, Co. Cavan, 1884.-T. H. Moorhead. Drumcro, near Maralm, County Down, 1883.— C. H. Waddell. Warrenpoint, Co. Down ; and Ardmore, Co, Armagh ; 1883.— 'H. W . L. 331. Puccinia compositarum. Sch. Errigle, Co. Cavan, 1884—T. H. Moorhead. Ardmore, Co. Armagh, 1884 ; Banks of the Lagan, near Belfast.— H. W. L. 382. Puccinia glomerata. Grev. Near Belfast, Templeton ( Uredo senecioms), Ann. Nat. Hist., Vol. V, Warrenpoint, Co. Down; Ardmore, Co. Armagh ; Bog Meadows, near Belfast, Co. Antrim ; 1884. — H. W. L. 383. Puccinia variatoilis. Grev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Clandeboy, and Ballylesson, Co. Down ; Ardmore Glebe, Co. Armagh ; 1884. H. W. L. 384. Puccinia glomerata. Link. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 385. Puccinia umbelliferarum. D. C. Errigle, Co. Cavan, 1884.- T. H. Moorhead. Middletown, Co. Armagh (on Hydrocotyle).— C. H. Waddell. Ardmore, Co. Armagh ; very abundant on Sium latifolium ; 1884. — H. W . L. 386. Puccinia aegopodi. Link. Near Belfast, Templeton ( Sphceria aigopodii), Ann. Nat. Hist., Yol. Y. Ardmore, Co. Armagh, 1883.— H. W. L. 387. Puccinia saniculae. Grev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 388. Puccinia smyrnii. Corda. Ardmore Glebe, Co. Armagh, 1883; Crawfordsburn, County Down, 1884. — H. W. L. 30i Lett — The Fungi of the North of Ireland. 389. Puccinla anemones. P. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 390. Pucclnia violarum. Link. Near Belfast, Templeton ( XJredo violarum , D. G\), Ann. Nat. Hist., Vol. Y. Errigle, Co. Cavan, 1884. — T. H. Moorhead. Ardmore Glebe, Co, Armagh 1884.— H. W. L. 391. Pucclnia lychnidearum. Link. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 392. Puccinla umbilici. Guep. Near Strabane, County Tyrone, 1883.— H. W. L. 393. Puccinia epilobii. D. C. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 394. Puccinia circese. P. Shane’s Castle Park, Co. Antrim, 1883. Rare.— H. W. L. 395. Puccinia fabsc. Link. Warrenpoint, Co. Down, 1883.— H. W. L. 396. Puccinia fallens. Cooke. Near Belfast, Templeton ( XJredo leguminosarum), Ann. Nat. Hist., Yol. V. Warrenpoint, Co. Down ; and Ardmore, County Armagh ; 1883 H. W. L. 397. Pucclnia buxi. D. C. Wolfhill, near Belfast, 1842. — W. Thompson. Errigle, County Cavan, 1884 — T. H. Moorhead. Ardmore Glebe, Co. Armagh, 1885.— H. W. L. 398. Puccinia hieracii. Mart. Crawfordsburn, Co. Down, 1884.-H. W. L. For description see M. C. Cooke’s “ Micro Fungi,” 4th edit., p. 207. 399. Puccinla aeg-ra. Grove . Drumcro, nea* Maralin, Co. Down, 1883.— C. H. Waddell. Warrenpoint Vicarage Garden, 1883. — H. W. L. For description see Journal of Botany. September, 1883. 400. Puccinia malvacearum. Cor. See Grevillea, vol. ii. pp. 47 and 137. Carlingford, County Louth, on mallow ; Ardmore, Co. Armagh, on mallow and hollyhock ; 1883.— H. W. L. 302 Lett— The Fungi of the North of Ireland. 401. Gymnosporanglum juniperi. Lie. I found a specimen of this on grass under fir trees in the Fort Grove, near Moira Rectory, Co. Down, July, 1884. Rare.— H. W. L. 402. Podisoma juniper!. Fr. Near Belfast, Templeton ( Podisoma juniperi -sabince), Ann. Nat. Hist., Yol. V. Wolf hill, Belfast, County Antrim, on upright juniper, 1837.— W. Thompson. 403. Tilietia caries. Tul. Near Belfast, Templeton ( Uredo caries , D. C.), Ann. Nat. Hist., Yol. V. 404. Ustilago carbo. Till. Near Belfast, Templeton ( Uredo segetum, P.), Ann. Nat. Hist., Yol. V. Erriole Co Cayan, 1884.— T. H. Moorhead. Drumoro.near Maralin, County Down, 1883. — 0. H. Waddell. Ardmore, Co. Armagh, 1883. Very common on ears of oats. — H. W. L. 405. Urocystis pompholygodes. Schlecht. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Ardmore Glebe, County Armagh, 1884, on Ranunculus repens and acris. Common.— H. W. L. 406. Uromyces appendiculata. Lev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 407. Uromyces apieulosa. Lev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 408. Uromyces ficariee. Lev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 409. Uromyces intrusa. Lev. Carr’s Glen, near Belfast, Co. Antrim, 1885.— S. M. Malcomson. Collm Glen, Co. Antrim, 1882.— H. W. L. 410. Uromyces concentrica. Lev. Errigle, Co. Cavan, 1884. — T. H. Moorhead. Banks of the Lagan, near Belfast, Co. Antrim, 1885.— S. M. Malcomson. 411. Coleosporium tusilaginis. Lev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Clonallon, Co. Down ; and Ardmore, Co. Armagh ; 1883. Very common.— H. W. L. Lett — The Fungi of the North of Ireland. 303 ♦ 412. Coleosporium petasites. Lev. Clonallon, Co. Down, 1883. — H. W. L. 413. Coleosporium sonchi-arvensis. Lev. Errigle, Co. Cavan, 1884 — T. H. Moorhead. Warrenpoint Vicarage, Co. Down, 1883.— H. W. L. 414. Coleosporium rhinantheacearum. Lev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Fortwilliam, near Moira, Co. Down, 1883,— C. H. Waddell. 415. Melamspora sallcina. Lev. On Salix viminalis , Ardmore, Co. Armagh, 1883. — H. W. L. 416. Melamspora betulina. Desm. Ballyvalley, Co. Down, 1883.— C. H. Waddell. 417. Melamspora euphorbiae. Cast. Errigle, Co. Cavan, 1884. — T. H. Moorhead. Near Newcastle, Co. Down, 1884.— H. W. L. 418. Cystopus candidus. Lev. Near Belfast, Templeton (U redo Candida , P), Ann. Nat. Hist., Vol. V. Errigle, Co. Cavan, 1884. — T. H. Moorhead. Wai*renpoint, Co. Down ; Ard- more, Co. Armagh; 1883. Very common.— H. W. L. 419. Uredo potentillarum. D. C. Errigle, Co Cavan, 1884. — T. H. Moorhead. Loughrey, Co. Tyrone ; side of the Lagan, near Belfast, on “Barren Strawberry” {Potentilla fragarias- trum ) ; 1885.— H. W. L. 420. Uredo hypericorum. J). C. Donard Demesne, Co. Down, 1885 G. Pirn, and H. W. L. 421. Uredo vacciniorum. P. Slieve Donard, Co. Down, 1883.— H. W. L. 422. Uredo blfrons. Grev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 423. Trichobasis petroselini. B. Abundant on Smyrnium olusatri. at Ardmore Glebe, Co. Armagh, 1884. — H. W, If. 304 Lett-— The Fungi of the North of Ireland, 424. Tricbobasis suaveolens. Lev. Errigle, Co. Cavan, 1884.-T. H. Moorhead. Bank of the Lagan, near Bel- fast, 1885.— S. M. Malcomson. Analoist, Co. Armagh; and Warrenpoint, Co. Down ; 1883. Common. — H. W. L. 425. Tricbobasis rumicum. D. C. For description see M. C. Cooke’s “Rust, Smut, and Mildew,” 4th edit, p. 225. Near Belfast, 1884.— J. J. Andrew. 426. Iiecythea lini. Lev. Near Belfast, Templeton ( Uredo Uni, D. C .), Ann. Nat. Hist., Yol. V. Shore of Lough Neagh, at Ardmore Glebe, Co. Armagh, 1883.— H. W. L. 427. Raestelia lacerata. Tul. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Derryloist, Co. Armagh, 1884. -H. W. L. 428. JEcidium epilobii. L). C. Banks of the Lagan, near Belfast, 1885.-S. M. Malcomson. 429. iEcidium euphorbiae. P. Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 430. iEcidium berberidis. P. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 431. JEcidium crassum var. periclymeni. D. G. Errigle, Co, Cavan, 1884— T. H. Moorhead. Near Shaw’s Bridge, on the Lagan, Co. Antrim, 1885.— S. M. Malcomson. 432. iEcidium ranunculacearum. L>. C. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Ardmore, Co. Armagh ; Balmoral, near Belfast, Co. Antrim, 1883. Common.— H. W. L. 433. .Scidium grossulariae. D. C. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. Errigle, County Cavan, 1884.— T. H. Moorhead. Ardmore Glebe, Co. Armagh, 1882. Very common. — H. W. L. 434. JEcidium urticse. D. C. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Ardmore, Co. Armagh, 1885. Not compaon. — H. W. L. Lett — The Fungi of the North of Ireland. 305 435. JEcidium taraxaci. K. et Schn. Errigle, Co. Cavan, 1884. — T. H. Moorhead. Near Belfast, 1884. — J. J. Andrew. Ardmore, Co. Armagh, 1884. — H. W. L. 436. JEcidium compositarum var. tussilaginis. P. Ardmore, Co. Armagh ; Ormeau, and Newcastle, County Down ; 1885. — H.W. L. 437. JEcidium compositarum var. jacobeae. Grev. Errigle, Co. Cavan, 1884. — T, H. Moorhead. Near Belfast, 1884. — J. J. Andrew. 438. JEcidium primulee. D. C. By the side of the Lagan, near Belfast, 1885. — S. M. Malcomson. 439. JEcidium rubellum. P. Banks of the Lagan, near Belfast, 1884.— J. J. Andrew. 440. JEcidium ari. Berk. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 441. JEcidium allii. Grev. Errigle, Co. Cavan, 1884.— T. H. Moorhead. 442. Ceratium hydnoides. A. and S. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 443. Stilbum bicolor. F. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 444. Stilbum vul?are. Tode. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 445. Mystrosporium stemphylium. Corda. On ripe seed vessels of garden Wallflower, Warrenpoint Yicarage, County Down, 1883. (The fig. in Cooke’s Handbook, p. 578, does not appear to belong to this species.) — H. W. L. 446. Cladosporium herbarum. Lk. On dead cabbage loaf, Ardmore, Co. Armagh, 1884. — H. W. L. 306 Lett— The Fungi of the North of Ireland . 447. Cladosporium compactum. Sacc. Mr W. B. Grove considers some specimens on ripe garden pea pods, fiom Warrenpoint Vicarage, Go. Down, 1883, are to be referred to this species.- H. W. L. 448. Aspergillus glaucus. LTc. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Common everywhere on decaying bread, cheese, jam, &c. H. W. L. 449. Aspergillus candidus. Lk. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Ardmore Glebe, County Armagh, 1883. On berries of Tarnus communis , old kid gloves, and fruit stones, 1884. — H. W. L. 450. Peronospora infestans. Mont. Errigle, Co. Cavan, 1884.-T. H. Moorhead. Common everywhere; in some seasons much later than others in making its appearance on the potato crop, as in 1885. — H. W . L. 451. Peronospora nivea. Unq. On hogweed ( JUgopodium podagra ), Warrenpoint, Co. Down, 1883.- H. W. L. 452. Peronospora gangliformis. Berk. On groundsel leaves, Warrenpoint, Co. Down, 1883.— H. W. L. 453. Peronospora Candida. Fekl. Ardmore Glebe, Co. Armagh, 1884.— H. W. L. 454. Polyactis cana. Berk. On a dead strawberry leaf, Ardmore Glebe Garden, Co. Armagh, 1884. H. W. L. 455. Polyactis vera. Berk. Near Belfast, Templeton (. Botrytis vera. Fr.), Ann. Nat. Hist., Vol.V. 456. Stysanus stemonitis. Corda. Tollymore Park, County Down, 1885.— G. Pirn, and H. W. L. 457. Monilia racemosa. Purt. Near Belfast, Templeton, AnD. Nat. Hist., Vol. V. 307 Lett— The Fungi of the North of Ireland. 458. Sepedonium chrysospermum, Lk. Near Belfast, Templeton ( Strachylidium diffusuvi. Fr.), Ann.;Nat, Hist. Vol. Y. On decaying Boleti, especially Boletus pachypus, Gilhall,Co. Down, 1883. — 0. H. Waddell. Donard Demesne, and Tollymore Park, County Down, 1884. Common. — H. W. L. 459. XVXucor mucedo. L. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. On paste, jam, &c. Very common everywhere. — H. W. L. 460. Mucor caninus. P. Near Belfast, Templeton, Ann, Nat. Hist., Vol. Y. 461. Mucor amethysteus. Berk. Ardmore, Co. Armagh, on rotting pears, 1883.— H. W. L. 462. Pilobolus crystallinus. Tode. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 463. Onyg-ena equina. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 464. Microsphaeria berberidis. Lev. Finnebrogue, Co. Down, 1885, on barberry leaves.— H. W. L. 465. Microsphaeria grossulariae. Lev. Drumcro, near Maralin, County Down, 1883.— C. H. Waddell. Ardmore Glebe, Co. Armagh, very abundant in autumn of 1885.— H. W. L. 466. Erysiphe martii. Lk. Errigle, Co. Cavan, 1884.— T. H. Moorhead. Ardmore, Co. Armagh, and Warrenpoint, County Down, 1883.— H. W. L. 467. Erysiphe montagnei. Lev. Ardmore, Co. Armagh, 1884, on burdock ( Arctium lappa ) leaves.— H. W. L. 468. Eurotium herbariorum. Lk. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Ardmore, County Armagh, 1882. Common.— H. W. L. 469. Helvetia crispa. Fr. Drumcro, near Maralin, County Down, 1883.— C. H. Waddell. Ardmore Glebe, Co. Armagh, 1883.— H, W. L. 3o8 Lett— The Fungi of the North of Ireland. 470. Helvella lacunosa. Afz. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 471. Mitrula paludosa. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Slieve Dan.rd.Oo. Down 1885. -S. M. Malcomson. Mountain near Hilltown, o. own, on dead heather ( Colluna vulgaris) in water.-H. W. H. 472. leotia lubrica. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 473. Geoglossum glabrum. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 474. Peziza venosa. P. w T On a gravelled walk, Ardmore Glebe, Oo. Armagh, 1884.— . 475. Peziza badia. P • Warrenpoint Vicarage, Co. Down. 1883 Killymoon, Co. Tyrone, 1884- H. W. L. 476. Peziza cochleata. Buds. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 477. Peziza leporina. Batscli. Killymoon, Connty Tyrone, 1884. Very rare.-H. W L 478. Peziza aurantia. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 479. Peziza vesiculosa. Bull. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. 480. Peziza humosa. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 481. Peziza granulata. Bull. Drnmcro, near Maralin, Connty Down, 1883.-C. H. Waddelh KiUy- moon, Co. Tyrone ; Ardmore, Co. Armagh ; Ormean Park, Co. Down , 1884. Very common. — H. W. L. 309 Lett — The Fungi of the North of Ireland. 482. Pezlza coccinea. Jacq. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. This is mentioned in Harris’s Down as having been found at Kilwarlin, near Hillsborough. Ardmore Glebe Garden, Go. Armagh, 1884. Rare. — H. W. L. 483. Peziza brunnea. A. and S. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Banks of the Lagan, near Belfast, 1885. — S. M. Malcomson. 484. Pezlza trechispora. B. and Br. Near Ardmore Church, Co. Armagh, 1885. Not common. — H. W. L. 485. Peziza scutellata. L. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 486. Pezlza stercorea. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Ardmore, Co. Armagh, 1884.— H. W. L. 487. Peziza virginea. Batsch. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Ardmore, County Armagh, on dead twigs of lime tree, 1884. — H. W. L. 488. Peziza nivea. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 489. Peziza calycina. Schum. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Warrenpoint, Co. Down, 1883, on a fir tree. — H. W. L. 490. Peziza papillaris. Bull. Near Belfast, Templeton ( Peziza papillata. P.), Ann. Nat. Hist., Vol. V. 491. Peziza villosa. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 492. Peziza inflexa. Bolt. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 493. Peziza cinerea. Batsch . Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. Sallagh Braes, near Larne, Co. Antrim, 1884, on rotten wood. — H. W. L. 3 io Lett— The Fungi of the North of Ireland. 494, Peziza fusaroides. Berk. Near Belfast, Templeton (Fusarium tremelloides. Grev.), Ann. Nat. Hist. Vol. V. 495. Helotium aeruginosum. Fr. Shane’s Castle Park, County Antrim, 1883; Killymoon Co. Tyrone, and Rosstrevor Wood, County Down, 1884 ; Tollymore Par , 1885. The stained wood is common; while the fully develope rare, except in the last locality, where I found it in abundance, October, 1885— H. W. L. 496. Helotium calyculus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 497. Helotium citrinum. Fr. Near Belfast, Templeton ( Peziza citrina. Hedw.), Ann. Nat. Hist., Vol. V. 498. Helotium lenticulare. Fr. Near Belfast, Templeton (. Peziza lenticularis. Bull), Ann. Nat. His,, Vol. V. 499. Helotium rluzophilum. Fckl. By the side of the Bloody Burn, Slieve Donard, Co. Down, 1885.-H. W. L. 500. Helotium aciculare. v Near Belfast, Templeton (. Peziza acicularis. Bull), Ann. Nat. Hist., Vo . . 501. Patellaria atrata. Fr. Lurgan Demesne, and Ardmore Glebe, Co. Tyrone, 1884. Common.— H. W. L. Co. Armagh, 1883 ; Killymoon, 502. Patellaria lecideola. Fr. Sallagh Braes, near Larne, Co. Antrim, 1884.— H. W. L. 503. Ascobolus furfaceus. P • Ardmore, Co. Armagh; Killymoon, County Tyrone, 1884. Common. H. W. L. 804. Bulgaria inquinans. Fr. Lurgan Demesne, Co. Armagh, 1883; Killymoon, Co. Tyrone, 1884. Abundant. — H. W. L. Lett— The Fungi of the North of Ireland. 3 1 1 505. Bulgaria sarcoides. Fr. Near Belfast, Templeton (Tremella sarcoides. With.), Ann. Nat. Hist., Vol. Y. Greyabbey, County Down, 1883.— R. L. Praeger. Narrow Water Demesne, 1883 ; Rademon, and Tollymore Park, Co. Down, 1885.—H. W. L. 506. Elaphomyces variegatus. Vitt. Donard Demesne, Co. Down, under beech trees near the Spa Cottage 1885.— H. W. L. 8 ’ 507. Elaphomyces granulatus. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 508. Phacidium coronatum. Fr. Near Belfast, Templeton, Ann. Nat. Hist , Yol. V. 509. Phacidium ilicis. Fr. Warrenpoint and Rosstrevor, Co. Down, 1883 ; Ardmore, Co. Armagh 1883. Common. — H. W L. 510. Heterosphaeria patella. Grev. Loughrey, Co. Tyrone, 1884; Sallagh Braes, near Larne, County Antrim 1884; Ardmore, County Armagh, 1884.— H. W. L. 511. Rhytisraa acerinum. Fr. Near Belfast, Templeton, Ann. Hist., Vol. V. Ardmore, Co. Armagh ; Killymoon, Co. Tyrone ; Maralin, Warrenpoint, Donard Demesne, and Tolly- more Park, Co. Down, 1883. Very common and abundant wherever there are sycamore trees. — H. W. L. 51Z. Hysterium pulicare. P. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 513. Hysterium fraxini. P. Near Belfast, Templeton, Ann. Nat. Hist Vol. V. Killymoon, County lyrone, on ash twigs, 1884.— H. W. L. 514. Hysterium iHypoderma) virgultorum. D. C. Near Belfast, Templeton (. Hysterium rubi. P.), Ann. Nat. Hist., Yol. V. 515. Hysterium (Hypoderma) hederse. De Fot. Arm!!ha?snaraeM Tar C°' Antri“. 1884 1 Ardmore Glebe, County Armagh, 1885. Not common. — H. W. L. 3 1 2 Lett— The Fungi of the N orth of Ireland* 516. Hysterium (Hypoderma) conigenum. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 517. Hysterium CLopliodermium) pinastri. Schratd. Near Belfast, Templeton, Ann. Nat. Hist , Vol. V. 518. Hysterium (lophodermium) juniperinum. D . Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 519. Stegia ilicis. , Errigle, Co. Cavan, 1884.-T. H. Moorhead Ardmore, Co. Annagh 1882; Warrenpoint, Co. Down, 1883; Killymoon, Co. Tyrone, 1884, Donard Demesne, and Tollymore Park, Co. Down, 1884.— H. W,L. 520. Trochlla lauro-cerasl. Fr. Desertcreat, Co. Tyrone, 1883; Tollymore Park, Connty Down, 1884. fl. w. L. 521. Trochila buxi. Capron. Ardmore Glebe, Co. Armagh. I have found this only on dead leaves that have not fallen. — H. W. L. 522. Trocbila craterium. Fr. Ardmore, Co. Armagh, 1885.— H. W. L. 523. Torrubia militaris. Fr. Near Belfast, Templeton (Spharia militaris. Fl. Dan.), Ann. Nat. is., Vol. V. Near Clonallon Church, Co. Down, 1883.— H. W. L. 524. Epicbloe typbina. Berk. Near Belfast, Templeton (Vothidea typhina. P.), Ann. Nat. Hist., o . The Oaks, Co. Derry, 1842, _G. Lyle. Ardmore, County Armagh, 1883- H. W. L. 525. Hypocrea farinosa. B.and Br. Killymoon, County Tyrone, 1884.— H. \V. L. 526. Hypomyces aurantia. dul. Near Belfast, Templeton (Spharia aurantia. P.), Ann. Nat. Hist., Vo . 527. Nectria cinnabarina. Fr. „ Near Belfast, Templeton (Spharia fragiformis), Ann. Nat- Hist, Vo • warrenpoint, and Ormean, Co. Down; Ardmore Glebe Co Armagh , Killy moon, Co. Tyrone, 188t Very common every where—H. W. U. Lett — The Fungi of the North of Ireland. 313 528. Wectria coccinea. Fr. Near Belfast, Templeton, Ann. Nat. Hist., Yol. V. Cave Hill, County Antrim, 1843. — W. Thompson. Errigle, Co. Cavan, 1884 T. H. Moorhead. 529. Nectria cucurbitula. Fr. Ardmore Glebe, Co. Armagh, 1884. — H. W. L. 530. Wectria slnopica. Fr. Rosstrevor Wood, Co. Down, 1883 ; Ardmore Glebe, Co. Armagh, 1883. — H. W. L. 531. Nectria aquifolia. Berlc. Tollymore Park, Co. Down, 1885.— G. Pirn, and H. W. L. 532. Xylaria corniformis. Mont. Crawfordsburn, 1884 ; Tollymore Park, 1885 ; County Down.— H. W. L. 533. Xylaria hypoxylon. Grev. Near Belfast, Templeton, Ann. Nat. Hist. Yol. Y. Waringstown, Ross- trevor Wood, Maralin, Narrow Water Demesne, Rademon, Tollymore Park, Co. Down ; Killymoon, Co. Tyrone, 1884. Very common everywhere. — H. W. L. 534. Xylaria carpophila. Fr. Near Belfast, Templeton ( Sphceria carpophila. P.), Ann. Nat. Hist,, Vol. Y. 535. Ustulina vulgaris. Tul. Falls, Belfast, on a dead Willow , 1842. _W. Thompson. Ram’s Island, Lough Neagh, Co. Antrim ; Raughlan, County Armagh ; 1884.— H. W. L. 536. Hypoxylon coccineum. Bull. Florence Court, Co. Fermanagh, 1840. — W. Thompson. Donard Demesne, and Tollymore Park, Co. Down, 1885.— G. Pirn and H. W. L. 537. Hypoxylon coliaerens. Fr. Tollymore Park, County Down, 1885.— G. Pirn, and H. W. L. 538. Hypoxylon fuscum. Fr. Near Belfast, Templeton ( Sphceria fusca. P.), Ann. Nat. Hist., Vol. Y. Collin Glen, County Antrim, 1844. — W. Thompson. Ardmore Glebe, and Raughlan, Co. Armagh, 1885. — H. W. L. 539. Hypoxylon rubiginosum. Fr. Tollymore Park, County Down, 1 885.— G. Pirn, and H. W. L. 540. Hypoxylon atropurpureum. Fr. Bangor, Co. Down, 1835. — W. Thompson. 3i4 Lett—The Fungi of the North of Ireland. 541. Hypoxylon serpens. Fr. Near Belfast, Templeton ( Sphceria serpens. P.), Ann. Nat. Hist., Vol. V. 542. Eutypa lata. Tul. Ardmore Glebe, Oo. Armagh, 1885.— H. W. L. 543. Eutypa flavo-virens. Tul. Near Belfast, Templeton {, Sphceria flavor irens. Hoffm.) Ann. Nat. Hist., Yol. Y. 544. Dotliidea ulmi. Fr. Ardmore, Oo. Armagh, on fading leaves of Elm. Very common, 1883. - H. W. L. 545. Dotliidea filicina. Fr. Raughlan, Co. Armagh, 1883. — H. W. L. 546. Diatrype quercina. Tul. Ardmore, Co. Armagh, 1883 ; Killymoon, Co. Tyrone, 1884.— H. W. L. 547. Diatrype verrucseformis. Fr. Ranghlan, and Ardmore, Co. Armagh ; Killymoon, Co. Tyrone, 1884.— H. W. L. 548. Diatrype stigma. Fr. Near Belfast, Templeton ( Sphceria stigma. Hoffm.), Ann. Nat. Hist., Vol. Y. 549. Diatrype disciformis. Fr. Near Belfast, Templeton ( Sphceria disciformis. Hoffm.), Ann. Nat. Hist., Yol Y Errigle, Co. Cavan, 1884.— T. H. Moorhead. Ardmore, Co. Armagh, 1884. Drumcro, near Maralin, and Tollymore Park, Co. Down, 1885.— H. W. L. 550. Diatrype bullata. F\. Drumcro, near Maralin, County Down, 1883 — C. H. Waddell. Killy- moon, County Tyrone, 1884. — H. W. L. 551. Diatrype strumella. Fr. Ardmore Glebe garden, Co. Armagh, 1884 — H. W. L. 552. Diatrype nucleata. Carr. Ardmore Glebe garden, Co. Armagh, 1884.— H. W. L. 553. Diatrype ferruginea. Fr. Ardmore Glebe, Co. Armagh, 1883. H. W. L. 315 Lett — The Fungi of the North of Ireland. 554. IHelanconis lanciformis. Tul. Near Belfast, Templeton [Sphceria lanciformis , Fr.), Ann, Nat. Hist. Yol. V. *’ 555. Valsa stellulata. Fr. Ardmore Glebe, Co. Armagh, 1885. — H. W. L. 556. Valsa leucostoma. Fr. Ardmore Glebe, County Armagh, 1885, on dead twigs of Cotoneaster H. W. L. 557. Valsa salicina. Fr. In a garden, at 2, Collin View Terrace, Lisburn Road, Belfast, on dead twigs of Willow , 1884.— H. W. L. 558. Valsa leiphemia. Fr, Rosstrevor Wood, Co. Down, 1883.— H. W. L. 559. Cucurbitaria laburni. De Not. Silverwood, near Lurgan, Co. Armagh ; several large Laburnums dead, and one mass of this fungus, which attacks only old trees ; 1885. — H. W. L. 560. Cucurbitaria elongata. Grev. Desertcreat, Co. Tyrone, 1884, on dead Laburnum.— Li. W. L. 561. Gibbera vaeemii. Fr. Near Belfast, Templeton ( Sphceria vaccinii. Sow.), Ann. Nat. Hist., Yol. V. 562. IVZassaria pupula. Tul. Ardmore, Co. Armagh, on a wooden gate post, December, 1883. — H. W. L. 563. Sphceria aquila. Fr. Near Belfast, Templeton ( Sphceria byssiseda. Tode), Ann. Nat. Hist., Yol. V. 564. Sphceria phceostroma. Mont. Ardmore, Co. Armagh, 1884. — H. W. L. 565. Sphceria spermioides. Hoffm. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 566. Sphceria moriformis. Tode. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 567. Sphceria mammeeformis. P. Ardmore, Co. Armagh, 1884, on rotten Ivy sticks. — H. W. L. 3 1 6 Lett — The Fungi of the North of Ireland . 568. Spliseria pulvis-pyrius. P. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 569. Spheeria scirpicola. D. C. On dead Scirpus lacustris, floating in Lough Neagh, at Raughlan, Oo. Armagh, November, 1883. — H. W. L. 5 70. Sphseria ocellata B. and Br. Near Belfast, Templeton, Ann. Nat. Hist., Yol. Y. 571. Sphseria hertoarumi P» Near Belfast, Templeton ( Gladosporium herbarum. Lk.), Ann. Nat. Hist., Yol. Y. Ardmore, Co. Armagh, 1884.— H. W. L. 572. Sphseria acuta. Moug. Near Belfast, Templeton, Ann. Nat. Hist., Vol. Y. 573. Spliseria pinodes. B. and Blox. Ardmore Glebe, Co. Armagh, 1884 — H. W. L. 574. Spliseria gnomon. Tode. Near Belfast, Templeton, Ann. Nat. Hist., Vol. V. 575. Sphaerella maculseformis. Cooke. Ardmore, Co. Armagh, 1884. — H. W. L. 576. Sphserella punetiformis. B. Near Belfast, Templeton {S phceria punetiformis ), Ann. Nat. Hist., Vol. V. 577. spliserella latebrosa. Cooke. Ardmore, County Armagh, 1884, on -withered Sycamore leaf.-H. W. L. 578. Sphserella osruthii. Fr. Errigle, Co. Cavan, 1884 — T. H. Moorhead. 579. Stigmatea geranii. Fr. Near Belfast, Templeton ( Dolhidea geranii. Fr.), Ann. Nat. Hist., Yol, Y. 580. IDiclisena strobilina» Fr. Raughlan, Co. Armagh, 1884.— H. W. L. 581. Capnodium citri. Waringatown, Co. Down, on Camellia leaves in a greenhouse, 1883.- H. W. L. ( Proceedings Belfast Naturalists' Field Club. — Appendix 1885-1886.) FORAMINIFERA OF THE BELFAST NATURALISTS’ FIELD CLUB’S CRUISE OFF BELFAST LOUGH, IN THE STEAM-TUG “ PROTECTOR,” JUNE, 1885; ALSO, FORAMINIFERA FOUND BY DR. MALCOMSON, AT ROCKPORT, BELFAST LOUGH. BY JOSEPH WRIGHT, F.G.S. Wc N the summer of this year (1885) the members of the Belfast Naturalists’ vjk Field Club engaged the “Protector” for a day’s dredging off Belfast 'Oy Lough. During the cruise a number of dredgings were taken, and materials from the following four places were carefully put aside for future examination, viz. : — No. 1.— Two miles S. (by compass) of Maiden Lighthouses ; sand and shells ; 60 fathoms. No. 2.— Five miles S.S.E. (by compass) of Maiden Lighthouses ; mud, stones, and dead shells ; 60 fathoms. No. 3 — Four miles E. (by compass) of Gobbins ; mud, stones, and dead shells ; 60 fathoms. No. 4.— -Six miles S.S.E. (by compass) of Black Head ; sand and shells; 30 fathoms. The object of the present communication is to give a list of the Forami- nifera found in these gatherings. A few years ago this part of our coast had, on several occasions, been dredged by Mr. William Swanston, F.G.S., and myself, and a list of the Fora- minifera found was given in an appendix to the Club’s Report, 1875. This, 31 8 Wright— For aminif era of Down and Antrim. no doubt, is the reason why so few additions to the Foraminifera of our North-East Coast were obtained from the “Protector” gatherings. . S. M. Malcomson, M.D., had also made a most exhaustive search for Foraminifera in shore sand and rock pools in the vicinity of Rockport, Belfast Lough. At this place he found 87 different species, two of them— viz., Spiroplecta biformis and Placopsilina cenomana — being new to Britain. At my request, Dr. Malcomson very kindly furnished me with a list of the species which ha had found, and also their relative abundance. I have given the record of his discoveries in Column 5 of the table of geographical distribution. For the sake of completeness, I have given in the last column a list of the Foraminifera recorded in my former paper ( loc . cit.)* and at the end of the table the names of three species which had not been met with in either the “Protector” gatherings or at Rockport. The present list, therefore, com- prises all the species that are now known from this part of our coast, f In conclusion, I have to thank Mr. H. B. Brady, F.R.S., for his kind help and advice in the identification of some of the critical species. I am also much indebted to S. M. Malcomson, M.D., for the very accurate and artistic drawings which accompany this memoir. * Recent Foraminifera of Down and [Antrim, Proceedings Belfast Naturalists’ Field Club, app. 1876-7. + Of late years our increased knowledge of Foraminifera has necessitated many changes both in the names of the genera and species, and, in consequence of these altera- tions, a number of the species given in my paper on Foraminifera of Down and Antrim (1876-7) are now known by other names. The following is a list of the species which have been so altered, the names by which they had been recorded being given in italics. I have not , however, thought it necessary to note any changes which may have been made in the generic names, as such will be sufficiently obvious to the reader. Comuspira involvens, Rs. — Cornuspira foliacea, Phil. Haplophragmium pseudo spirale, Will .—Lituola nautiloidea, Lamk. Bolivina dilatata, Rs.= Textularia pygmcea, d’Orb. Lagena lineata, Will .^Lagena caudata , d’Orb. Lagena aspera, Rss. =* Lagena hispida, Rss. Lagena hispida, Rss .—Lagena Jeffrey di, Brady. Lagena laevigata, Rss .=Lagena lucida, Will. Lagena lagenoides, Will .^Lagena yrnata, Will. Marginulina costata, Ba,tsch.= Dent atina, obliquestriata , Rss. Polymorphic gibba, d’Orb., fistulose form ^.Polymorphina Orbignyi , Zbor. Gypsina versicularis, P. and J .=Tinoporus Isevis , P. and J. Gypsina inhserens, Schultze. = Tinoporus lucidus , Brady MS. The following names have been excluded from the present memoir, as they are not now considered good species, viz. Biloculina elongata, d’Orb; Spiroloculina canalieu- lata d’Orb. ; Triloculina Brongniartii, d’Orb. ; Lagena Lyellii, Seg.; Lagena tngono-margi- nata P. and J.; Lagena oblonga, Seg.; Dentalina guttifera, d’Orb.; Textularia vanabilis, Will • and Discorbina ochracea, Will. I have also thought it best to omit the following, as the’ specimens found were not typical, and, in consequence, their identification not as reliable as could have been wished, viz. :-Miliolina agglutinans, d’Orb.; Textularia trochus, d’Orb. ; Lagena distoma, P. and J. ; Lagena gracillima, Seg. ; and Nodosaria raphanus, Linn. Wright— For aminif era of Down and Antrim. 3 1 9 The following notes in reference to some of the species found may be of interest : — XVXlllollna insignis, Brady. (PI. xxvi. fig. 4, a, b.) Miliolina insignis, Brady, 1882, Rep. Foram. H.M.S. Challenger p 165 pi. 4, figs. 8-10. * This species, in contour, resembles Miliolina trigonula, but differs from it in the surface of the shell being marked by closely set, regular, longitudinal costae. Only two specimens were obtained. They were from gatherings taken a few miles apart. The size is small, and the surface ornamentation consists of faint longitudinal lines. New to Britain. IVSiliollna subrotunda, Montagu, sp. var. (PI. xxvi. fig. 5, a, bi) Vermicidum subrotundum, Montagu, 1803, Test. Brit., part 2, p. 521. This variety differs from the typical Miliolina subrotunda in having the peripheral edgo ornamented with somewhat irregular, oblique costze. Fre- quent in shallow water gatherings. Kyperammlna arborescens, Norman , sp. (PI. xxvi. fig. 1.) Psammatodendron arborescens (Norman MS.), Brady, 1881, Deukschr. d. K. Akad. Wiss. Wien, vol. xliii., p. 98, No. 13. Mr. Brady* thus refers to this species : — “ This interesting form was dis- covered by the Rev. A. M. Norman growing on a polyzoan ( Menipea ternata ), dredged during the cruise of the “Valorous ” off Holstenborg, Greenland, at the depth of 20 fathoms, and the name Psammatodendron arborescens was first assigned to it. The original specimen figured in Plate XXVIII. was most kindly lent to me by Mr. Norman when it was the only known example that was even approximately perfect. Quite recently, however, the species has been found in some abundance by Mr. David Robertson, off Cumbrae, on the west coast of Scotland.” A few years ago I found a fragment of it in sand which had been dredged by Mr. James Wright off Portrush, County Antrim. Three other localities, given in the “Challenger” Report, complete the list of places where the species has been found. Mr. Brady, however, adds “It is not improbable that when it is sought for it may turn out a very common species.” It has been found in the four “ Protector ” gatherings, and was abundant in two of them. Ammodlscus Shoneanus. Siddall, sp. Trochammina Shoneana, Siddall, 1878, Proc. Chester Soc. Nat. Sci., part 2 p. 46, figs. 1, 2. This species has been found at only a few places, and, excepting at Rock- port, where a good many specimens were gathered, is very rare where it occurs. It was first found in the Dee (Siddall), afterwards at Rockport, Belfast Lough (Malcomson), Killybegs Harbour, Donegal (Wright), Dublin Bay * Report Forams. H.M.S. Challenger, p. 262. 320 Wright— For aminif era of Down and Antrim. (Balk will and Wright). It has also been recorded from two of the “ Challen- ger ” o-atherings— viz., off Christmas Harbour, Kerguelin Island, 120 fathoms, and Station 238, in the very deepest part of the Pacific, 3950 fathoms * It is indeed remarkable that a species which, in this climate, has been only met with in shallow water and shore gatherings should, in the North Pacific, occur at such a great depth. Placopsilina cenomana, D'Orbigny. (Pl. xxvi. fig. 3, a, b.) Placopsilina cenoviana, d’Orbigny, 1850, Prodr. Paleont., Vol. II., p. 185, No. 758. One large specimen of this rare species was found by Dr. Malcomson at Rockport, between tides. The specimen figured is the only example which has been obtained in Britain. Verneuilina polystropha, Reuss,sp. (Dimorphous form. PI. xxvi. fig. 2.) Bulimina polystropha, Reuss, 1845, Yerstein. Bbhm. Kreid., part 2, p. 109, pl. 22, fig. 53. This species is of frequent occurrence around our coast. An abnormal form, in which the later chambers are arranged in a linear series, with a simple round aperture, is occasionally met with in shallow water gatherings. Mr. Brady considers it a dimorphous form of Verneuilina polystropha. Spiroplecta biformis, Parker and Jones, sp. Textularia agglutinans var. biformis, Parker and Jones, 1864, Phil. Trans., Yol. civ., p. 370, pl. 15, figs. 23, 24. A few years ago this species was found for the first time in British watei by Dr. Malcomson, who obtained several good typical specimens at Rockport. f A few specimens have since been found in Dublin Bay (Balkwill and Wright). Lagena semilineata, Nov. sp. (Pl. xxvi. fig. 7.) Test flask-shaped, with a long, ectosolenian neck, the lower extremity furnished with a short projecting neck ; upper portion of the body of the shel usually smooth ; lower portion ornamented with very numerous, closely-set, longitudinal sulci ; neck marked with longitudinal lines, which occasionally extend a little way down the shell. . . This very elegant form may be readily distinguished from L. semistnata by the ornament on the lower portion being closely-set, longitudinal sulci, instead of the strong costate ribs of the latter species. It has been found at only a few localities, and is rare where it occurs. Lagena bicarinata, Terquem, sp. (Pl. xxvi. fig. 8, a, b.) Fissurina bicarinata , Terquem, 1882, Mbm. Soc. Gbol. France, Ser. 3, Yol. ii., Mom. iii., p. 31, pl. 1, fig. 24, a, b. Professor Williamson, in his Monograph, has figured, under the name of * Eeport Forams. H.M.S. Challenger, p. 335. t Sec woodcut, Trans. Roy. Ir. Academy (Science), Vol. xxviii., p. 333. Wright — Foraminifera of Down and Antrim. 321 Lagena quadrata (pi. 1, figs. 27, 28), two distinct species. Fig. 27 is an oblong form of L. Icevigata, and this variety is known by Williamson’s name ; fig. 28 is L. bicarinata. Both species are often met with around our coast. Xiagena marginata var. insequilaf eralis, Nov. (PI. xxvi. fig. 10, a, b, c ) This curious variety of L. marginata has one side strongly convex, the other side being flattened, or slightly concave ; aperture at the flattened side. Rare. Common in a fossil state in the Estuarine Clay, Limavady Junction. Spirillina margaritifera, Williamson. (PI. xxvi., fig. 12, a — b .) Spirillina margaritifera, Williamson, 1858, Rec. For. Gr. Br. p. 9, pi. vii. figs. 2 — 4. The following is Professor Williamson’s description of this species, the type in brackets being additions of mine : — “ Shell consisting of numerous narrow, somewhat convex, (?) convolutions — the outer one smooth, the inner one obscured by numerous projecting tubercles, arranged in one or two series ; In some parts these are most conspicuous along the centre of the convolution ; in others along the spiral septal line ” [peripheral edge square] . ‘ ‘ Texture hyaline, diam., -£5.” Williamson ( loc . cit.) describes the convolutions of this species as convex. A somewhat similar form, differing only in the convolutions being square, has been found at several localities around our coast, and so closely does his description and illustration agree with these specimens, that I have no hesita- tion in considering them the same. The specimens recorded as Spirillina tuberculata , both by Siddall, in “ Memoir on the Foraminifera of the Estuary of the Dee,” and by Balkwill and myself, in “ Foraminifera of Dublin Bay and Irish Sea,” should, I feel satisfied, be referred to S. margaritifera , and S. tuberculata should be no longer included among the British species. S. mar - garitifera differs from S. tuberculata in the outer convolutions being smooth, the peripheral edge square, and the tubercules being stronger, and not so numerous. 322 Wright — Foraminifera of Down and Antrim . TABLE SHOWING THE DISTRIBUTION OF FORAMINIFERA OFF BELFAST LOUGH. ABBREVIATIONS :-v r, very rare ; r, rare ; c, common; v c, very common; * , previously recorded. LIST OF SPECIES. Biloculina ringens ( Lamk .) ••• depressa, d’ Orb. ••• Spiroloculina linibcitci, d (Jib* ••• planulata {LamTc.) IVIiliolina trigonula {Lamk.) insignis, Brady tricarinata, d’Orb. oblonga ( Montagu ) seminulum (Linn.) tenuis ( Czjzek ) subrotunda {Montagu) ... var. secans (d’Orb.) bicornis (W . Sf J.) Ferussacii {d’ Orb.) ... ••• var. near M. sclerotica, Karrer pulchella (d’Orb.) fusca {Brady) ••• „ n7 Ophthalmidium cannatum, Balkwillcf Wi Cornuspira involvens {Ess.) ... Hyperammina arborescens {Norman) Reophax fusiformis ( IFeV/.) Haplophragmium glomeratum {Brady) globigeriniforme (P. J-) pseudospirale ( Will.) ••• canariense {d’Orb.') ••• 1 i © H 50 f r a W 2 e g S < a p ■s 0 . o m 03 © r ^ • a CM i j i 3 3 5 H 5 A a 0 *" o oa © © 1 o T c . (3 § 5 o i SO j os' P d '1 « o O P o c [3 c m o r-H r a ^ < } s 3 1 A 3 3 3 3 3 © q a ®S OB60 © a Rockport,— Between tides. | Recent Foraminifera of Down and r c c f r f c c c r f f f f ... • •• f r 7 f f r ... vr vr ... ... r r .. r r r vr VC r f f f VC vr r r ... ... c VC VC VC VC vr ... ... ... ... ... vr VC *f c c f c r r r r f ... ... ... ... VC ... ... ... ... ... ... ... ... ... c c c c r ... r f f r c r VC VC r ... ... ... ... ... ... c r r r ... . .. . ... vr vr ... . c c c c ... I ... ... ... .1 c c c c VC 1 Wright — Foraminifera of Down and A ntrim. 323 TABLE — Continued . LIST OF SPECIES. Ammodiscus incertus (d’Orb.) gordialis (J. P.) charoides (J. Sf P.) Shoneanus, Siddall Placopsilina cenomana, d’ Orb. Trochammina squamata, J. Sf P inflata ( Montagu ) macrescens, Brady Textularia sagittula, Defrance gramen, d’ 0)'b. agglutinans, d’Orb. Valvulina fusca ( Will.) ... Verneuilina polystropha ( Rss .) dimorphous form ... Spiroplecta biformis (P. Sf J.) Gaudryina filiformis, Berthelin Bulimina pupoides, d’ Orb. marginata, d’Orb. ovata, d’ Orb. elegantissima, d’Orb. subteres, Brady Virgulina Schreibei’siana, Czjzek Bolivina textilarioides, Rss. punctata, d’Orb. plicata, d’Orb. dilatata, Rss. difformis ( Will.) Cassidullna laevigata, d’Orb crassa, d’Orb. Bag-ena apiculata, Rss lineata ( Will.) lsevis ( Montagu) aspera, Rss. hispida, Rss. striata ( d’Orb .) 2 miles S. of Maiden L.H., 60 fms. 5 miles S.S.E. of Maiden L.H., 60 fms. 4 miles E. of Gobbins, 60 fms. 6 miles S.S.E. of Black Head, 30 fms. Rockport, — Between tides. Recent Foraminifera of Down and Antrim, 1877. vr vr * ... c c c r * ... vr vr vr ... ... ... ... ... r ... ... ... ... ... ... vr f f f c ... * ... ... ... ... c * ... ... ... r * r r r f ... * ... c c c c r ... vr vr vr ... * vr ... ... ... ... r r VC * r ... ... ... vr ... ... ... c r r r r VC * vr r r r VC * r f f vr C * r r r vr c * ... vr ... ... ... ... .. vr ... c * r r r ... ... ... r r r r c * ... r r r r VC * r r r ... c * c c c c c * r c c f r * c f f c * r r r r r * ... ... vr . . . . . • ... r f f f c * r f f r VC * vr * ... ... 7 * ... r r r VC * 324 Wright — Foraminifera of Down and Antrim. TABLE— Continued. LIST OF SPECIES. nov. I'agena gracilis, Will ••• sulcata {W.Jf J •) costata {Will) William sou i ( Alcock ) semistriata, Will. striato -punctata, P. J . squamosa ( Montagu ) me\o {d’ Orb) hexagono {Will.) laevigata {Ess.) ••• var. quadrata ( Will.) marginata {W. J- ) var. inaequilati lagenoides ( Will.) Orbignyana (Seg.) bicarinata ( Terquem ) pulchella, Brady Nodosaria scalans {Batsch) pyrula, d Orb. — (D.) communis [d Urb.) ... (D.) obliqua ( Linn .) ••• tingulina cannata, d Urb. Vaginulina legumen {Linn.) linearis ( Montagu ) •* Cristellaria rotulata, Lam/c. cultrata {Montfort) crepidula {F. M.) ... Polymorphina lactea ( rV. a **.) var. oblonga, Will . gibba (cT Orb.) fistulose form lanceolata, Bss. compressa, d’Orb. rotund ata {Bornemann) ... concava, Will. myriatiformis, Will. «n .J a w S ^ «© P - a: w - ^ ci ^ £ S © '3 r- s * a ° 0 , 03 < © - % ’ 1 . < • ZL 2. a 2 ^ O n CQ 2 i o T a a DO fX a ■O « 03- P s ^ £ < ■O o ■s ^ H 03 © ' a ■*H < j 5 > 3 4 i ; 5 3 4 . • 03 °. a Q ^ o 0 3 CO © l rc P « p 1 <0* r5 h. +3 c « l © c 1 :i 1 ! t f 2 « & O o PS c 1 1 f 1 > 3 •*: 0 t" 3 oo a ,H a s' a *c 0 -S "4 a © © © ..1 ... c .. f c C C vc * .. f vc VC C r * „ C c C c vc * ... r r r r f * | * 7 vc vc c 7 * r vr ... r ... ... r ... r c r c r f r f c * * ... r ... r vr r vr r r ... * .. vr vr ... ... ... r r r ... c c C c vc ... r r ... vr . . . vr * r r ... r * ... vr r 1 r vr r * a .. vr vr vr vr ... r ... vr * ... vr ... r * ... ... ... ... * r r r .. vr vr r vc * ... vr ... r r r r r * ... r r r f f * r r r r ... f r r r f * * r r ... . r ... ... ‘‘ r r ... c ♦ ... vc 5 VC v< J c * • •• •• vr VI ' * Wright — Foraminifera of Down and Antrim . T ABLE — Continued. LIST OF SPECIES. 2 miles S. of Maiden L.H., 60 fms. 5 miles S.S.E. of Maiden L.H., 60 fms. 4 miles E. of Gobbins, 60 fms. 6 miles S.S.E. of Black Head, 30 fms. Rockport, — Between tides. Recent Foraminifera of Down and Antrim, 1877. Uvig-erma angulosa, Will. vr r r r c * G-lobigrerina bulloides, d’Orb. c c c c VC * inflata, d’Orb. f f f f Orfoulisia uni versa, d’Orb. r r r Spirillma vivipara, Ehrenb. c r r 7 vr * Fatellina corrugata, Will. f f f f r * Discorbiraa rosacea (d’Orb.) vr vr ve * globularis {d’Orb.) VC VC VC VC VC * orbicularis {Ter quern) ... -f Bertheloti {d’ Orb.) r r r vr Wrightii, Brady vr r Parisiensis, d’Orb. vr * Plaraorlmlina Mediterranensis, d’Orb. r 7 7 7 r * Truncatulina lobatula {W. J.) ... VC VC VC VC VC * refulgens {Montfort) vr vr * Ungeriana {d’ Orb.) ... 7 Pulvismlina auricula {F. Sf M.) ... vr r r vr r * Karsteni {Rss.) vr vr repanda {F. Sf M.) vr vr vr * Patagonica {d’Orb.) vr vr vr vr vr Rotalia Beccarii {Linn.) ... r f f C VC * nitida, Will. f f f f VC * Gypsina vesicularis {P. Sf J.) vr vr * inhaerens {Schtdtze) vr vr r c * Nonionima turgida ( Will.) ..0 vr * scapha {F. Sf M.) ... ... **. 7 7 * umbilicatula ( Montagu ) vr * pauperata, Balkwill Sf Wright 7 vr vr r f depressula ( W. Sf J.) f f f c VC * stelligera, d’Orb. r r vr vr Polystomella crispa {Linn.) r r r C * striato-punctata {F. # M.) ... f C c VC VC * Operculina ammonoides ( Gronov .)... ... * Jaculella acuta, Brady , off Maiden L.H., 60-72 fms. iagrena semilineata, Nov., Newcastle, between tides, &c. Splrillina margaritifera, Will., Portrush, between tides. EXPLANATION OF PLATE XXVI. Fig 1. Eyperammina arbor escens (Norman), x 30 diam. 2. Verneuilina polystropha (Rs.). dimorphous form, x 75 diam. ’’ 3. piacopsilim cenomam, d’Orb. a, inferior aspect; b, superior aspect, x 40 diam. 4. Miliolim insignis, Brady, a, lateral aspect ; b, oral aspect, x 75 diam. 5. MilMina subrotmda (Montagu), var. a, lateral aspect ; b, oral aspect. x 50 diam. „ 6. Lagena semistriata, Will, x 75 diam. 7. Lagena semilineata, Nov. x 75 diam. 8 LagembicarimtaCTe rquem). «, lateral aspect; b, oral aspect, x 100 diam ” 9. Lagena lamgata {&*■), var. guadrata, Will. «, lateral aspect ; b, oral aspect, x 100 diam. 10. Lagena marginata (W. & J.), var. incequilateralis, Nov. 0, *, lateral aspects ; c, oral aspect, x 100 diam. 11 Polymwphim gibba, d’Orb., fistulose form, x 20 diam. ” 12. Spirmmrnarga,ntifera,m\\. a, lateral aspect ; b, peripheral aspect, x 75 diam. Proc. Belfast. Nat. Field Club. 1884-85. (Appendix.) PI. XXVI. S M Malcoir.son del et.lith. . WRIGHT.. FORAMINIFERA OF BELFAST LOUGH ( \Pi oceeding s Belfast N % t uvci lists' Field Club. — Appendix 1885-1886.) A LIST OF THE CRETACEOUS FORAMINTFERA OF READY HILL, COUNTY DERRY. BY JOSEPH WRIGHT, P.G.S. — $— the year 1874 I published a List of the Cretaceous Microzoa of Ireland. U|\ It was the result of three years’ exploration in the chalk of the Counties of Antrim, Derry, and Down, the only counties in Ireland where rocks of this age occur. The Greensand in Ireland appears to he almost devoid of Microzoa. Only two Foraminifers have as yet been found in it— viz., Orbito- lina concava * and Cristellaria rotulataf I have on one or two occasions examined greensand rocks under the microscope, but failed to find any trace of these organisms in them. With the above two exceptions, all the Microzoa found in the Irish Cretaceous rocks have been obtained from a mealy powder, known as chalk powder, which is of frequent occurrence in cavities in the flints. I do not remember to have ever visited a chalk exposure with flints that did not yield, on searching, at least some of this powder. At some places it was very scarce, at others it was abundant. It may have been merely acci- dental, but flints found in the vicinity of the sea usually contain a much greater quantity of the powder than those found farther inland. The chalk in Ireland is a hard, compact limestone, known as white “ lime- stone,” of the same age as the soft white chalk of the South of England, but very different in character, the hardness of the Irish stone being presumably due to the heat and pressure of the overlying basalt. The flints foimd in it are * Tate, Cretaceous Rocks of Ireland, Quart. Journ., Geol. Soc., 1865. + Wright, Cretaceous Microzoa of Ireland, Rep. andProc., Belfast Nat. Field Club, 1874, aPP» P» 73, 328 Wright— Cretaceous Foraminifera of Ready Hill. of two kinds— (1) Ordinary flints in amorphous masses, and usually lying m bands parallel with the bedding of the chalk, and having the longer ax]B in Jhe plane of the bedding ; (2) Paramoudras (in England known as potstones), usually of an irregular fusiform contour, variable in shape, and having a core ot white limestone passing through them from end to “d ; ^ays^ccurm an upright position, or at right angles to the plane of the bedding, being the reverse of the position in which the other flints are found. Most of the ordinary flints are of a homogenous, silicious structure through- out, others have incorporated with them a white limestone, and some a mea y powder. This material in flints freshly guarded is invariably hard, and in ap- pearance similar to the white limestone in which the flints are imbedded. T is soft powdery chalk seems to have been part of the oose of the Cretaceous sea bottom, which got mixed up or entangled in flints in which siliciflcation had been only partially completed. Thus enclosed in the flinty matrix, it was, no doubt, to a large degree protected from the influences which converted the soft chalk into a hard limestone. On exposure it becomes gradually change into a powdery substance, and in this state the lovely Microsoa, so abundant m chalk, can he readily separated by washing. The' white chalk, as developed in Ireland, has for its base a somewhat pebbly and friable limestone, the joints and partings of which are coloured green by a superficial (glauconite ?) deposit. This bed was formerly well seen at Kilcorig, near Lisburn, and Professor Tate, who studied it at that time, given a good account of it, especially with reference to fossils * This g auco- nitic hand occurs, as above stated, at Kilcorig, on the southern boundary of the Irish Cretaceous series ; and on the north-west it has been found near Moneys more, and high up on the steep face of Benbradagh Mountain. The same line o escarpment is continued across Keady Hill, some nine miles to the north of Benbradagh, and in the limestone quarries at Keady there is a fine exposure o this basement bed of the white chalk. The paleontology of this portion of the chalk is most interesting. Its fossil fauna is much more varied than in any of the beds lying above, and it is much richer in the abundance of specimens whic it yields . When preparing my former paper on the Cretaceous Microzoa of the Nort of Ireland, I was greatly helped in the work by my friend, Mr. William Gray, M B I. A., who kindly procured for me chalk powder from numerous localities throughout the North of Ireland, one of them being Keady Hill. Although the quantity which I received was small, it nevertheless yielded a great variety o Foraminifera, a result to be expected, bearing in mind the great number o Mollusca and Echinoderms that have been collected from this locality ; and 1 was sorry that I had not more material to examine. Some years later I visited the quarries, in company with two members of the Belfast Naturalists Field Club, and collected several pounds weight of the material, which occurs there m Quart. Jour. Geol. Soc., 1865, Wright — Cretaceous Foraminifera of Keady Hill. 329 quantity. The following is a List of the Foraminifera found. Twenty-seven of the species are additions to the Cretaceous Fauna of Ireland, three of which are new to Science. To my friend, Professor T. Rupert Jones, F.R.S., I am deeply indebted for land assistance in helping me in the identification of some of the critical species, and also to my friend, S. M. Malcomson, M.D., for the very accurate and artistic figures which accompany this paper. Species marked * are new to the Cretaceous Fauna of Ireland. FORAMINIFERA (RETICULARIA). LITU0LIDJ3. Hapiostiche clavulina, Ess. Rare. *Tlmrammma papillata, Brady. PI. xxvii. fig, 12. Rare. Ammo discus incertus ( d’Orb .). Rare. Kaplophragmium inflatum, Ess. Very rare. TEXTULARI DJE. Textularia gibbosa, d’Orb. Rare, pupa, Ess. Rare, sagittula, Def ranee. Common eximia, d’Eicliwald, Frequent, turris, d’ Orb. Rare, globulosa, Ehr. Rare. ^ *conulus, Reuss. Rohm. Kreid., pi. xiii. fig. 75 ; near Text, globulosa, , hut more compact. Frequent. Verneuilina triquetra {Munster). Rather rare. *spinulosa, Ess. Frequent. Tritaxi a triquetra {Munster). Rather rare. Spiroplecta praelonga {Ess.). PL xxvii. fig. 3. Rare. Gaudryina rugosa, d’Orb. Frequent. *Jonesiana, sp. Nov. PI. xxvii. figs. 1, 2. Test elongate, tapering, somewhat compressed, quadrilateral ; tri- serial portion, edges cari- nate and faces flat or slightly concave ; biserial portion quadrilateral, the four angles more or less carinate, lateral faces concave, peri- pheral edge square, occasionally keeled from the carinate edge of the triserial portion extending up the shell ; in the specimen figured the keel is not connected with the triserial part. I have pleasure in naming this species after my friend, Professor T. Rupert Jones, F.R.S. Rare. ^Clavulina angularis, d Orb. One specimen. 330 Wright— Cretaceous Foraminifera of Ready Hill Bulimina Presli, Ess. Frequent, affinis, d’ Orb. Frequent, brevis, d’Orb. Frequent, intermedia, Ess. Eare. *Buchiana, d’Orb. Eare. Virgulina tegulata, Ess . Var. Common. *Bolivina obsoleta ( Eley .). Eatber rare. decorata, Jones MS. PI. xxvii. figs. 7, 8. Test elongate, compressed broad at tbe oral end, and tapering to a rounded point at tbe aborai extremity ; surface ornamented with prominent oblong tubercles winch are arranged in oblique rows. Common. Pleurostomella fusiformis, Ess. Eare. LA.GENIDJE. *Eiagena globosa ( Montf. ). Eatber rare. apiculata, Ess. Eare. sulcata ( W. and /.). Eatber rare. * gracilis, Will. One specimen. *XTodosaria (Glandulina) laevigata, d’Orb. Very rare. *(Glandulina) obliquilimbata, sp. Nov., Jones MS. PL xxvii. fig. 5. Test elongate, with oblique limbate sutures. One specimen, glabra, d ’ Orb., and dentaline variety. Eatber rare, radicula ( linn. ). Eatber rare. var., near N. conferta. Very rare, bispida, d’Orb. Eare. (D.) farcimen {Sold.), var. Lorneiana,, d’Orb. Eare. . . exquisitely delicate variety. Eare. (D.) consobrina, d' Orb, var. irregularis, d’ Orb. Eare. . . var. emaciata, Ess. "V ery rare. (D.) soluta, Ess. Very rare. . . var. Lilli, Ess. Eare. (D.) nodosa, d’Orb., var. Eare. (D.) pauperata, d’Orb. Common. (D.) communis, d’Orb. Frequent. acicula , LamJc. Eatber rare. . Zippei, Ess., var. alternata, var. Nov. Jones MS. PL xxvii. fig. This variety bas ribs of normal character, alternating with lines of interrupted costse. Very rare, rapbanus {Linn.). Eatber rare. . . var. inflata, Ess. Frequent. .. short, coarse variety. Common. Wright — Cretaceous Foraminifera of Ready Hill. 33 1 Frondicularia striatula, Ess. Frequent, angustata, Nilsson. Rare. Archiaciana, d'Orb, Rare, elliptica (Nilsson). Very rare, mucronata, Ess., var. Rather rare. *Rhabdogonium excavatum, Ess. One specimen. IVXarg-inulina costata ( Batsch ). Rare. *Reussiana, sp. Nov . Jones MS. PL xxvii. fig. 6. A very fine smooth Marginulina, with the later segments elongated in a linear series. Frequent. *Vaginulina legumen {Linn.). Rare, trilobata, d'Orb. Frequent. *Bronni ( Eoemer ). One specimen, costulata, Ess. Very rare. Cristellaria acutauricularis ( F . and M.). Rare. italica, Def ranee. Specimens very fine. Rather rare, triangularis, d'Orb. Rare, rotulata ( LamJc .). Abundant. *cultrata (Montf.). One specimen. *crepidula {F. and M.). PL xxvii. fig. 4. One very fine specimen, ^simplex, d'Orb. Rare, recta, d' Orb. Rare. *cymboides, d'Orb. Rare, ornata (Ess.). Very rare. Flabellina pulchra, d'Orb. Very rare. . . smooth variety, with parallel sides. Very rare reticulata, Ess. Common. *Polymorphina gibba, d'Orb. Rare. . . fistulose form. Rare, fusiformis, Eoemer. Frequent. . . fistulose form. Rare. ♦cylindrica, Borneman. Frequent, regina, B. P. and J., var. Pl. xxvii. fig. 14. Rare. .. ^fistulose form. Pl. xxvii. fig. 13. One specimen Sagrina nodosa, P. and J. Frequent. Ramulina brachiata, Jones. Rare. Levis, Jones. Rare. *aculeata {d'Orb.). Pl. xxvii. fig. 11. Rare. 332 Wright— Cretaceous Foraminifera of Ready Hill . Globigerina bulloides, d'Orb. Hare. heaped variety. Rather rare, cretacea, d'Orb. Abundant, marginata, Rss. Rare. *aequilateralis, Br. PI. xxvii. fig. 9. Frequent. *Orbulina universa, d'Orb. Rare. ♦Pullenia sphseroides {d'Orb.). Rare, quinqueloba, Rss. Rather rare. Planorbulina exsculpta, Rss. Frequent. crenulata {Rss.). Rather rare. Truncatulina lobatula (W. and J.). Frequent. Planorbulina ammonoides, Rss. Abundant. var., with extra shell growth. Abundant. Pulvinulina Micheliniana, d' Orb. Frequent. Rotalia orbicularis {d'Orb.), var. Abundant. *Beccarii {Linn.). PI. xxvii. fig. 15. Rare. Fig. 1. >> 2. ,, 3. .. 4. 10. 11. 12. 13. 14 15 EXPLANATION OF PLATE XXVII. Gaudryina Jonesiana, Nov. a, lateral aspect ; b, oral aspect ; x, 40 diam. Gaudryina Jonesiana , Nov. a, peripheral aspect ; x, 40 cliam. Spiroplecta prcelong a (Rss.). x, 60 diam. Cristellaria crepidula (F. and M.). a, lateral aspect ; b, oral aspect ; x, 20 diam. . , Xodosaria ( Glandulina ) obliquilimbata , Nov., Jones Mb. a, lateral aspect ; b, oral aspect ; x, 20 diam. . Marginulim Reussiana, Nov., Jones MS. a, lateral aspect; b, oral aspect ; x, 20 diam. . Bolivina decorata, Jones MS. x, 60 diam. en . Bolivina deeorata, Jones MS. a, lateral aspect ; b, oral aspect; x, . GtiUgerina aqmlateraUi, Br. a, lateral aspect; b, oral aspect; x, 60 Nodosaria Zippei, Ess., var. ultimata, Nov., Jones MS. x, 30 diam. Ramulina aculeata (d’Orb.). x, 30 diam. Thurammina papillata, Br. x, 60 diam. ,. Polymorphina regina, B. P. and J„ var. fistulose form, x, 40 dram. Polgmorphina regina, B. P. and J., var. x, «» Rotalia Beccarii (Linn.), a, superior aspect ; b, inferior aspect ; e, oiaJ aspect ; x, 40 diam. Proc. Belfast Nat Field Club. 1884- -65. (Appendix.) PI. XXVII. WRIGHT_ CHALK FORAMINIFERA._ KEADY HILL. S Malcomson, del et lith (■ Proceedings Belfast Naturalists’ Field Club.— Appendix 1884-85.) ' Ebratum.— The following 10 pages should bear the folios 335 to 344 A LIST OP IRISH COLEOPTERA COLLECTED MAINLY BY THE LATE ROBERT PATTERSON, ESQ., F.R.S., IN THE YEAR 1829. fHE following list has been prepared from the manuscript catalogue of a cabinet of Coleoptera now in the possession of the family, and formerly the property of the late Mr. Patterson. The collection referred to was made in the year 1829. Some of the speci- mens were received from other well known naturalists, but by far the greater number were personally collected by Mr: Patterson himself in the North of Ireland. It is fortunate for the purpose of the present compilation that this MS. catalogue was prepared with the accuracy and precision that characterised all Mr. Patterson’s work. Except in a very few instances, the date and locality of every capture has been given ; and where the specimen has been acquired from any other entomologist it is so stated, and also whether such are Irish or English. As we are here only concerned with Irish localities, we do not record those species to which English habitats alone are assigned, nor any of those whose names appear in the manuscript, but are not localised. In connection with the series of local lists issued by the Belfast Naturalists’ Field Club, it is considered that the present may be a useful contribution. It is also rendered of more value by the fact that so few lists of Irish insects have hitherto been published. Further, it may be hoped that this list will be favour- ably received from the fact that it records the early work of some of the pioneers of natural science in the North of Ireland, and founders of the Belfast Natural History Society. Anything connected with the names of Templeton, Drum- mond, Patterson, Haliday, or Hyndman will be of interest to the naturalists of the present day, and still more to those who may succeed them. A review of {Proceedings Belfast Naturalists’ Field Chib. — Appendix 1884-85.) Ebratum. — The following 10 pages should bear the folios 335 to 344 A LIST OF IRISH COLEOPTERA COLLECTED MAINLY BY THE LATE ROBERT PATTERSON, ESQ., F.R.S., IN THE YEAR 1829. fHE following list has been prepared from the manuscript catalogue of a cabinet of Coleoptera now in the possession of the family, and formerly ■ the property of the late Mr. Patterson. The collection referred to was made in the year 1829. Some of the speci- mens were received from other well known naturalists, but by far the greater number were personally collected by Mr: Patterson himself in the North of Ireland. It is fortunate for the purpose of the present compilation that this MS. catalogue was prepared with the accuracy and precision that characterised all Mr. Patterson’s work. Except in a very few instances, the date and locality of every capture has been given ; and where the specimen has been acquired from any other entomologist it is so stated, and also whether such are Irish or English. As we are here only concerned with Irish localities, we do not record those species to which English habitats alone are assigned, nor any of those whose names appear in the manuscript, but are not localised. In connection with the series of local lists issued by the Belfast Naturalists’ Field Club, it is considered that the present may be a useful contribution. It is also rendered of more value by the fact that so few lists of Irish insects have hitherto been published. Further, it may be hoped that this list will be favour- ably received- from the fact that it records the early work of some of the pioneers of natural science in the North of Ireland, and founders of the Belfast Natural History Society. Anything connected with the names of Templeton, Drum- mond, Patterson, Haliday, or Hyndman will be of interest to the naturalists of the present day, and still more to those who may succeed them. A review of Irish Coleoptera — Late R. Patterson , F.R.S. •3*8- the work here summarised should also act as a stimulus to our youthful members. It will he seen how much could he accomplished in a year by one quite young, and fully occupied in business matters. This, too, at a time when hooks ot reference were much less accessible than at present. , „ , The classification of the following catalogue is that of Stephens s Syste- matic List of British Insects. n n w ~ p Abbreviations :-A. H. H.-A. H. Haliday,* F.L.S. ; G. C. H.-Geo. C. Hyndman ; R. T.— Robert Templeton. SCARITIDJE. Clivina fossor. -p ^ Sand pit, Cranmore ; under a stone, Rostrevor Mountain. H. I. Dyscbirius politus. Cranmore. CARABIDJD. Cychrus rostratus. Mourne Mountains. — Mr. Drummond. Carabus catenulatus. Rostrevor Mountain, near the summit. R. i* C‘ T” gw under a stone near M'Swine’s Gun, Horn Head, Co. Donegal-R. T. c. glabratus. Slieve Donard, on the open part of the heatn. Helobia brevicollis. a u t Sand pit, Cranmore ; under stones, Horn Head.— K. l. Xieistus fulvibarbis. Cranmore. HARPALID^. I.oricea pilicornis. Shore of Lough Neagh, near Shane’s Castle. Cbtoeius nigricornis. Irish — from A. H. H. Anchomenus prasinus. Shore of Lough Neagh, near Shane’s Castle. A. albipes. With the preceding species. A. oblongus. Cranmore, among corn. Platynus angusticollis. In the cellar of our house. Aeonum marginatum. , Lough Neagh ; under stones, near the mouth of the Sixmilewater. A. parumpunctatum. Shore of Lough Neagh, near Shane’s Castle. * Note -In Appendix VIII., p. 211. A. L. Haliday should be A. H, Haliday. Irish Coleoptera — Late R. Patter son , F.R.S. Odontcnyx rotundatus. Horn Head, Co. Donegal.-— R. T. Synuchus vivalls. Under stones, Rostrevor Mountain. Calathus melanocephalus. With the preceding. C. cisteiloides. With the two last species. Platyderes erythropus. Cranmore ; Moyntuagh Bogs. Pcecilns cupreus. Among com at Cranmore. P. rufifemoratus. Cranmore. Common. P. versicolor. In Mr. Brownlow’s demesne at Lurgan. Omaseus Bulwerii. Rostrevor Mountain. O. nigrita. Under stones, near Ardglass. O. melanurius. Rostrevor Mountain. Very common. Steropus madidus. Very common. Stomis pumlcatus. Lough Neagh. Patrobus rafipes. Horn Head. — R. T. ; under stones, Rostrevor Mountain. Platysma niger. Tollymore Park ; mountains at Rostrevor. Abax sfriola. Tollymore Park. Amara eurynota. Under stones, near Ardglass. A. communis. Castlewellan ; Moyntuagh Bogs. A. familiarls. Among com at Cranmore. Bradytus apricarius. Under stones, Castlewellan ; among corn, Cranmore ; Moyntuagh Bogs. Harpaius ruficornis, Tollymore Park. 33Sr *5^ Irish Coleoptera — Late R. Patterson, F.R.S. Treciius mimrfcus (aquaticus). Moyntuagh Bogs, under stones. Tachys ofotusus. Cranmore, among corn. PhiloetJies fuscipes 1 Among com at Cranmore. BEMBIDIIDJE. Peryplius femoratus. Castlewellan, under stones p. viridi-seneus. With the preceding. Taciiypus ikndrese. Shore of Lough Neagh. shore of Lough Neagh, near Shane’s Castle T. striatus. Shore of Lough Neagh. T. properans. Among corn at Cranmore. *BeinI>idiiim palsidosum. Shore of Lough Neagh, near Shane’s Castle. elaphrid^, Wotiopliiius aquations. Slieve Donard, under stones. N. toiguttatus. Horn Head, Co. Donegal. — R. T. Elepliras cnpreus. Irish— from Mr. Haliday. E' ^ough^Neagh.at Shane’s Castle, among sand, gravel and short grass, near the water’s edge. BleZT"eStS‘ Given to are by M, HaHday, who had not before see* any indigenous specimens. DYTICIDJE. Haliplns ferrugineus. Irish— from Mr. Haliday. Hygrotus scitulus. • Moyntuagh Bogs, on roots and stems of aquatic plants. S. pictus. With the preceding. EEydroporus dorsalis ? With the two last named species. * The first specimen of this species found in Ireland. Irish Coleoptera — Late R. Patterson , F.R.S. -ffri-Jr1 Tffoteras crassicornis. Moyntuagh Bogs, with, the preceding. Colymbetes fuliginosus. Common in the ponds at Cranmore. C. bipustulatus. In a pond in the fort -field at Moira. Dyficus marginalis. Irish — from G. C. H. D. punctulatus. Common in the ponds at Cranmore. ilcilius sulcatus. Moira, hog hole in the fort-field. GYRINID^E. Gyrinus natator. Cranmore, common in the ponds. LIMNIIDiE. Iiimnius seneus. Irish— from G. C. H. HELEPHQRID^E. Helepliorus nubilus. Cranmore, coming out of rotten wood. HYDROPHILIDjE. Iiimnebius ater. Irish — from A. H. H. Zb. truncatellus. Irish — from A. H. H. SPBLMRIDIID.E. Cercyon sp. ? On roots and stems of aquatic plants in Moyntuagh Bogs. ANISOTOMIDJE. Ortboperus pusillus. Irish— from A. H. H. SILPHID^. Tffecrophorous vespillo. Found in the rabbit warren, at Holywood, in 1827, by James Emerson (Sir James Emerson Tennent). Oiceoptoma rugosa. Irish— from A. H. H. O. sinuata. Shore of Lough Neagh, near Shane’s Castle. Phosphuga subrotundata. Cranmore. V ery common. 3^0 3*3 Irish Coleoptera — Late R. Patterson , Nitldula discoidea. Irish. — from A. H. H. NITIDULIDiE. HJ. obsoleta. Castlewellan. Meligethes viridescens (?) Cranmore, in flowers. M. urticae (?) Cranmore. Atomaria fuscipes. Irish— from A. H. H. ENGID^l. Cryptophagus caricis. Irish — from A. H. H. Byturus tomentosus. Found at Cranmore, under the bark of a decayed beech tree, by R. T. Batridius transversus. Cranmore. DERMESTID-E. Throscus dermestoides. Holy wood, rare — from A. H. H. Byrrhus sericeus. Cranmore. Hister carbonarius. Cranmore. BYRRHID.E. HISTERID2E. H< nitidulus. Irish — from A. H. H. GEOTRUPID^. Geotrupes sylvaticus. County Donegal ; road from Churchhill to Lough Neagh, R. T., and by the edge of Lough Neagh, R. T. Moume Mountains (?) Mr. Drummond. G. stercorarius. Common. Aphodius terrestris. Castlewellan. APHODIIDJE. A. rufipes. Cranmore. A. contaminatus. Rostrevor Mountain. Irish Coleoptera — Late R. Patter son ) F.R.S. MELOLONTHID^E. Serica brunnea. Irish — from A. H. H. Melolontha vulgaris. Cranmore, also an Irish specimen from G. C. H. Anomala borticola. Shane’s Castle. ELATERIDjE. Hemirhipus limbatus. Cranmore. H. marginatus. Irish— from A. H. H. K. obscurus. Cranmore. Slater cupreus (?) Cranmore. E. nig-er (?) Cranmore. CEBRIONEDJE. Atopa cervina. Irish — from A. H. H. CYPHONID^E. Cyphon melanurus. Irish — from A. H. H. C. padi. Cranmore, also an Irish specimen from A. H. H. TELEPHORIDiE. Telephorus pallid us, Cranmore. PTINIDiE. Ptlnus fur. Irish— from A. H. H. P. erenatus. Irish — from A. H. H. Cis sp. (?) Castlewellan. CURCULIONIDJE. Cossonus Tardii. Cranmore. Found during the entire month of June by turning up the under side of an alder, which lay in the farm- yard, and from which the bark Irish Coleoptera — hate R. P atterson, R.R.S. had been stripped. Generally found in clusters of three and four, ranged side by side. They were not found in any other situation, though the adjoining trees were carefully examined by R. T. Ceutorhynclius didymus. Cranmore. Wedyus assimilis (?) Cranmore. Orchestes fagi (calcarU Cranmore. Anthonomus fasciatus. Castle wellan Demesne. Notaris acridulus. Cranmore, among corn. Xiiophleeus nutoilus. Cranmore. Otiorhynchus sulcatus. Cranmore. O. notatus. Moume Mountains.— Mr. Drummond. PUilopedon geminatus. Cranmore. Strophosmus coryli. Rostreyor Mountain, on a hazel. Polydrusus oblongus. Cranmore. Phyllotoius parvulus. Cranmore. Apion hydrolapathi. On a rhodedendron, A. flavipes. Cranmore. at Cranmore. SALPINGIDJE. Salpingus rofooris (ruficollis). Taken under the bark of a holly in Tollymore Park. l.eptura ruficornis. Cranmore. LEPTURIDJE. Irish Coleoptera—Late R. Patterson , R.R. S. CEIOCEEID.E. Bonacia festucae (proteus). On rushes in the Moyntuagh Bogs. GALEEUCIDiE. Galeruca capreae. Cranmore. Haltica exoleta. Cranmore, among corn. H. dentipes (concinna). Cranmore, among corn. CHEYSOMELIDjE. Chrysomela cochleariae. Castlewellan. C. polyg-oni. Cranmore. C. raphani. On Slieve Crooh, about small pools of water. C. polita. Under stones on the beach, near Shane’s Castle. COCCINELLIDJE. Coccinella tredeeimpunetata. Cranmore. BLAPSIDJE. Blaps mortisago. In our shop, crawling up the wall, also in our cellar. 5 4-3 MOEDELLIDJE. Anaspis ruflcollis, Cranmore. CANTHAEIDJE. Proscarabeus violaceus. Near Holy wood. — From A. H. H. TACHYPOEIDiE. Bolitobius atricapillus. Tollymore Park, on a wall. ^4- Irish Coleoptera — Late R. Patterson, F.R.S. Tackinus marginellus. Slieve Donard. T. pullus. Lough Neagh, at Ardmore, found by Miss Jellett. STAPHYLINID2E. Stapliylinus erythropterus. Among com at Cranmore. S, castanopterus. Cranmore, and Squire’s Hill. Quedius tristis. Cranmore, among corn. Plailontlius politus. With the preceding. P. marginatus. With the two preceding species. Ctyroliypnus cruentatus* Castlewellan. Psederus riparius. Tollymore Park. Oxytelus cornutus. Cranmore, among com. STENIDJE. 28 DOT 1886 APPEDDIX I. VOL. II. THE FERNS OF ULSTER BY WILLIAM H. PHILLIPS AND ROBERT LLOYD PRAEGER, B.E., B.A. PUBLISHED BY THE BELFAST NATURALISTS’ FIELD CLUB. January, 1887. ( Proceedings Belfast Naturalists * Field Club. — Appendix 1885-86.) of ^CLsfer. By William H. Phillips and Robert Lloyd Praeger, B.E., B.A. submitting the following list of the species and varieties of our local Ferns to the members of the Belfast Naturalists’ Field Club, we cannot but regret the absence in our district of other observers in this branch of natural science. The study of the varieties of British Ferns is most interesting and fascinating — being half botany, half horticulture, since the finds must be grown in order to be understood and correctly named— and is one which can be carried on with very little trouble or expense. Yet, beyond our own finds, we have been able only to come across a very few stray records. Thus, the counties of Armagh, Donegal, and Cavan are hardly represented at all in our localities for varieties, while the names of Antrim and Down occur in almost every line— those being the counties to which we most easily had access. This, however, only proves the richness of our district in varieties. Ferns there are, if only some one will find them. There is still a great field of discovery among our North of Ireland Filices. Already Ulster has yielded some splendid new varieties — among which we may mention Athyrium Filix-fcemina crispum and Folystichum angulare divisilobum Crawfordia ; and many other treasures lie hidden away in our glens and copses only waiting to be found. At some future time we hope to bring out a supplement to this list, and we trust that then we shall have other names to record as finders of some of these beautiful varieties. The labour is small and the reward great. Nothing is more pleasant than to watch some wild find developing, under one’s care, into an elegant decom- posite or crested form. Again, a great advantage of Fern-hunting, as com- pared with most out-door scientific persuits, is that it can be carried on equally at every season of the year. For botany or entomology, for instance, there is but a short summer season ; but not so among the Ferns ; for while + Phillips and Praeger—The Ferns of Ulster. in summer we can explore the Athyriums and Lastreas and Blechnums in out woods and on our mountain sides, in winter the evergreen fronds of Po y- sliehmn and Seolopendrium peep at ns through the leafless hedges an wave luxuriantly in all our glens, inviting us to take up bag and trowel an go off Fern-hunting. We may add that we shall be very happy to give all the information in onr power concerning this branch of botany to anyone asking it, or to name fronds sent to us, or to receive notes of new localities for SP0°The district to which this list refers is bounded to the southward by the frontier line of Ulster, with the exception of the south-east and south-west corners, where in each case a slight encroachment has been “^e on an adjoining province. In the south-west a detour has been made in order to include the famous botanical region of Ben Bulben, m the extreme northern comer of Co. Sligo ; and on the south-east our line has been rawn so include the Carlingford Mountains, in Co. Louth, which botamcally a less degree geologically, belong to the Mourne Mountains, in Co Do regards the distribution of species In this area, few general observations can be made. Aspleniwn marinum and Adiantum Capillus - Veneris occur y the coast line ; the former being recorded from all our maritime counties, and growing in all suitable situations along our shores ; the latter bein„ to a limited area in Donegal* Polystichum angular* haunts the low districts in the east of the province, and is almost entirely unknown among the barren mountainous districts of Donegal and Fermanagh In he»e latter, however, the Royal Fern, Osmimia regain, occurs most Pl8n“" J' luxuriating in the rich peaty soil that surrounds the numerous lata m those regions. Polysticlium lonchitis and Asplemum vinde are con western counties; Ophioglossum loves the rich pastures of Down and Armagh. As Ulster plants, three of our Ferns are confined to Donega , and it is a very strange thing that these three species, which are found^ly in the bleakest and most northern of all our counties, shoul plants. Ophioglossum lusitanicum is a plant of the “rranemr coaste «md the Canary Isles, whose only other British stations are Kerry and Guernsey The Killamey Fern, Triehomanes radicam, prmcipa y aun s, species, the shadiest rocks in the south and south-west of Ireland and he Maidenhair, Adiantum Capillus- Veneris, makes i\hom\“ TnXd andto and the north of Africa, occurring also on the south coast of England l and the south-west of Ireland. Some of the species, again, seem are Athyrium Filix-fcemina, Polystichum aculeatum, and Lastrea P examples — occurring equally in damp shady woods and glens, though unfortunately their results have not been published ; but the Atliy- riums , Lastreas , and Scolopendriums still remain unarrangod, waiting for some champion to arise to give each one its proper place in the world of Ferns. In the difficult task of naming the varieties, we have obtained much valuable assistance from kind friends on the other side of the channel; among these we would specially mention Colonel Jones, of Bristol, and George B. Wollaston, Esq., of Chislehurst, to both of whom we are deeply indebted, both for naming fronds submitted to them, and for sending us plants and fronds of English forms of our varieties. From the beautiful nature-printed plates of varieties of British Ferns, brought out by Colonel Jones, under the auspices of the British Pterodological Society, we have abstracted our notes on Lastrea Filix-mas and Polystichum angular e proliferum, and have derived much other assistance. To Mr. S. A. Stewart, F.B.S.E., we also owe many thanks for information supplied as to localities for species. As to the distribution of varieties very little can be said. The varieties of Ferns are peculiar, in as much as they generally occur as isolated plants. Occasionally a little colony of some variety is discovered ; but usually a single plant is all that is obtained in any one place. A few of the exceptions to this rule we may mention : — _ P. angulare capitatum has been known to grow in Ballygomartin Glen, near Belfast, for some twenty years ; and in spite of frequent depredations, may still be found there. The Irish Polypody is a striking exception, as it generally occurs in considerable quantity where it occurs at all. The ditches about Ballymenoch, Holy wood, have long yielded examples of P. angu- lare interruptum. On sea-cliffs near Torr Head, in Go. Antrim, this summer, we discovered a large colony of very curious interrupted forms of Athynum Filix-fcemina ; and many other instances might be quoted. But the most noteworthy example occurs on the Mourne Mountains, where two very inter- esting varieties of Blechnum , trinervium and anomalum, occur in hundreds on Phillips and Praeger — The Ferns of Ulster . 7 the hill- sides ; yet we have no record of either of these forms having been found in any other locality in Ulster. In conclusion, we may say a few words as to the times at which the various observers, whose names occur in the following pages, lived and laboured in the cause of science. Mr. Templeton was the great pioneer °.f ."Ulster, botany, and the accuracy and care displayed in his notes have excited the admiration of all who have followed in his wake ; most of his records date between 1780 and 1810. After him came Messrs. Thompson, Whitla, and Hyndman (about 1820 to 1840), each of whom contributed his share towards the knowledge of our local flora. Other names which fre- quently occur in the “Flora of Ulster” (1864), from which we have extracted many notes, are those of Messrs. Ferguson, Millen, and Orr, and that of the author, Dr. Dickie. Following many of the localities in this list will be found the names of Dr. Mackay and Dr. Moore, each of whom did so much good work in the cause of Irish botany. More recent observers, whose names often occur in this list, are Messrs. S. A. Stewart, H. 0. Hart, and R. M. Barrington. After each locality we have given, as far as we were able, the name of the original finder; and where the plant has been since observed there we generally mention it. 1. POLYPODIUM. POLYPODY. 1. P. VU1GARB. Common Polypody. Rocks, walls, trees, and woods — plentiful throughout the district. Ascends to about 1000 feet on the mountains. On summit of Ben Bulben (1721 feet), T. H. Corry. ad pres sum. Craigauntlet, Co. Down, R. LI. P. bifidum. Oastlereagh, Co. Down, W. H. P. and R. LI. P. Holywood hills, Co Down, R. LI. P. denticulatum. Lough Gill, Co. Sligo, Moore’s N.P. Ferns. Knockagh, Co. Antrim, R. LI. P. rotundatum. Near Knockmore, Co. Fermanagh, W. H. P. semilacerum (Irish Polypody ). Co. Antrim. — Redhall Glen, Templeton ; Glenoe and Islandmagee, B. N. F. C. ; east branch of Woodburn glen, T. H. Corry ; Garron Point 8 Phillips and Praeger—The Ferns of Ulster . and Knockagh R LI. P. Near Knockmore, Co. Fermanagh, W. H. P. Island in Lough Erne, Co. Donegal, T. H. Corry Eedhall and Glenoe are two well-known stations for this handsome variety, and at both it grows abundantly and luxuriantly; in the latter place we have measured fronds 14 foot long by 9 inches broad. It is almost confined to Co. Antnm- doubtless the limestone is the attraction there, but why is it so rare m o er limestone tracts ? Beech Pern. 2. P. PHEGOPTERXS. Not common. DamAscIndsa to over 2000 feet in the mountains. At 2400 feet on Slieve Antrif-North branchof Glenarve river, Templeton, «09. On Slievenanee and in Glendun, Rev. S. A. Brenan. Glenariff, W. H. P., R. U. P., Sc By waterfall on Inver river above Glenariff, and by the Camlough and Linford rivers, and on Trostan, R. LI. P. . _ i * n Down. — Two miles south of Slieve Croob, and on Slieve Bmgmn Templeton land later in latter station, Rev. H. W. Lett and R. L . ). mountain, above ToUymore Park, W. Thompson ; (since observed Like™, Rev H W. Lett, W.H.P. and R.L1.P.) Rostrevor, Rev. George Robinson On Slieve Donard and Slieve Commedagh, S. A. Stewart. Luke’ s mountain, W.H.P. Sparingly near Craigauntlet above Holywoo _, and on Slieve Bearnagh, Slieve-na-glough, and ^Thomas mountain, R.L1J-. Louth. — Carlingford mountain, Robt. Browne, 1801, and since by B.N.F.C., Rev H W. Lett, W. H. P. and R. L1.P. Armagh.* — Frequent on rocks on N.E. slope of Slieve Gullion, Rev. H. W. Deny.3 * * 6— Ness Glen, Templeton. By the Owenrigh river, near Banagher, S. A. Stewart. Near Dungiven, B.N.F.C., 1872. _ Donegal. — Lough Eske, Mackey. Near Killybegs A. G. More. Glenah Carradoan, Angterlinn, Croghanmore, Poisoned G1»> mountain, Glenveigh, Alt mountain near Ardara near _ Lough Finn, Milford woods by coast between Slieve-a-tooey and Magheragh, and at 2000 feet on Slieve Snacht West, H. C. Hart. Crockaughnm, Charles "Moore. Tyrone. — Strabane Glen, W. H. P. Fermanagh.— Near Brookeborough, Rev. S. A. Brenan. 3. P. BRVOPTPBIS. Extremely* rare'. ocklayd, CybeleHibernica. Since a single pLnt Of this fern was discovered by Dr. Moore in the above locality near y half a century ago, it has not been observed in the North _o ^Irelan . we very much doubt if it can now be reckoned among our local fer . Phillips and Praeger — The Ferns of Ulster . 9 £P. ROBERTIAHUM is reported to have been found on Oarlingford Mountain, Co. Louth, but this is very unlikely, and requires ample confirmation.] 2. ALLOSORUS. ROCK-BRAKE. 1. A. CRXSPUS. Parsley Pern. Rocky places on mountains. yery rar0> Antrim.— Knocklayd and Carrickfergus Commons, David Moore. South brow of Slievenanee at 1500 feet, Dr. Dickie — since observed in above station by T. EL Corry and Rev. S. A. Brenan. Down.— On Slieve Bingian, Templeton, 1808— and recently, Rev. H. W. Lett and R. LI. P. On Shanslieve, Slieve-na-brock, and north side of Slieve Donard, Rev. H. W. Lett. Near the Eagle Rock, on the road from Hilltown to Kilkeel, Mr. Barcroft. On south side of Slieve Donard, and on the mountain north of Cove mountain, R. LI. P. Louth. — Carlingford mountain, very rare, B.N.F.C., 1878. Derry. — Clontygearagh mountain, David Moore. Donegal.— Very sparingly on Alt mountain near Ardara, H. C. Hart. Fermanagh. — On Cuilcagh mountain near Florencecourt, John M‘Donald. Very rare and scanty in the district, only isolated plants occurring here and there. 3. LASTREA. 1. Xi. THEXiTPTERXS. Marsh Pern. Wet places. y ery rar0. Antrim. — Plentiful about Portmore Park and wood, Templeton, 1794. Banks of Six-mile water near Ballyclare, G. C. Hyndman and F. Whitla. Donegal.— By the river Erne near Ballyshannon, A. G. More. By the same river near Belleek, H. C. Hart. Tyrone.— By a small lake near Caledon Rectory, Rev. G. Armstrong. At Omagh and Gorteen Gap, G. H. Kinahan. Cavan. — Near Belturbet, David Moore. Donegal and Tyrone are the only counties where this fern has been recently found; it is very strange how it has died out at Portmore. IO Phillips and Praeger—The Ferns of Ulster . Mountain Fern. 2. I>. ORBOPTERIS. Banks and mountain pastnres. Not common and xeiylocal. Antrim -At the base of the hill above Carrickfergus, J. Bea Glendun, BNFO 1879— a well-known locality, where it grows in grea pro u . Gb^sk, behind Ballycastle, Dr. O’Connor Glenarm Deerpa* sonth side of Glenariff, at Culraney north of Bnnabay Head, in Glenaan, near Cushendall, R. LI. P. » Down — Tollymore Park, Templeton, 1805-often since recorded from this ^ station. Thomas monntain, W. H. P. In various places about New pi w TT P R LI P &c Luke’s mountain, and near Moneyscalp weft ’of Bryansford, and on the Holywood bills, B. L1.P. Very rare in last locality. Armagh —On Ferry Hill above Narrow Water, R. LI. P. . Deiryv— Bennedy near Dnngiven, David Moore. Cushcape near Dungiv on Ind on Slieve Gallion near Desertmartin, S. A. Stewart. Moyola Park “ cTstledawson, B.N.F.O. Mnllaghmore, H. 0. Hart. L.gnapeiste, Donefal^— Milroy Bay, Newman. Gap of Barnesmore W. Thompson. Ifflybegs, L rL Lough Eske, B. Barrington. Minting^ Charles Moore. Near Black Gap, T. H. Corry. Banks of Eske river, Glen river Lough head river, and Beelan water, at Glenveigh and Bunlinn, and plentiful in glens in Innishowen, H. C. Hart. Near Bnncrana, W. H. P. Tvrone. — Strabane Glen, W. H. P. _ all Leitrim. Sonth side of Glenade mountain, B. Barrington and B. P. Yowell. interrupta. Glendun, Co. Antrim, E. L1.P. revolvens. Newcastle, Co. Down, W. H. P. Male Fern. 3’ ^ow generally admitted that this species as described by Presl includes three distinct forms, which are elevated to the rank of sPec“s ^ Mr. Wollaston. We append the most obvious of their characters brie y as possible under their several heads. fPronds A Propinqua-mas (Wollaston). (Filix-mas abbreviate Moore.) (Fronds ' and pinnae concave, pinnules biserrate, colour dull pale green ; perfect y deciduous, texture soft; indusium embracing spore-cases, persistent, cntifc). Extremely rare. Dry hedge-banks and woods. Near Carngaver, Co. Down, R. LI. P., 1882. B rilix-mas (Presl). (Fronds and pinnae convex, pinnules serrate ' biserrate; colour shiny pale green; texture papery; deciduous; indusium not embracing spore-cases, eventually evanescen , disrupted). Common. Woods, glens, roadsides, & Dr Dickie. Glencolumbkill, B.N.F.C., 1871. Bnncrana T. H Corry. Erris Mountains, Glenveigh, Poisoned Glen, Carradoan, Errlgal, and to the summit of Slieve Snacht West (2200 feet), Ooolcross, and Gap of Mamore, H. C. Hart. Tyrone. — Gorteen Gap, Dr. Kinahan. Fermanagh. — Florencecourt, Hon. J. L. Cole. Knoekmore and Drumbad, S. A. Stewart. Cavan. — Cuilceagh, and Slievenakilla, S. A. Stewart. Sligo. — Annacoona east of Ben Bulbon, R. Barrington and R. P. Yowelh ramosum. In a cave on Slieve Lamagan, Mourne Mountains, R. LI. P. An extraordinary variety, the frond being often four or five times branched. 15. OSMUNDAi Royal Pern. 1. O. REGAIiIS. Very local. Itofr-^shore8 a°t "s' Castle, G. C. Hyndman-extinct there now. Near- Ballinderry, Sefton. Bog at Springmount near Glarryford, J. H. Garrett exterminated about 1855, Rev. H. W. e . Down. — Donard’s Cave in the Mourne Mountains Kirkiston Bog bog no Grevabbev and by a lake S.W. of Castlewellan, Templeton, 1793. By the river above Newcastle, W. Thompson-here it grew abundantly td 1877, when it was completely exterminated, Rev. • • at Bloody Bridge, and in a cave at the same place, C-Dicksom By to Kilbroney River near Mr. at Newcastle, R. LI. P. ArmSX atth: sou* mid 'of Lough Neagh, Templeton-this station is Der^^^ “ Denial —Lough Eske, and Goat Island, Lough £ ^Very^are^in^Inmi^Mven^^^C^Hart. Bally—, H Bingham Shores of Lough Derg, S. A. Stewart. Arran Isles, H C. Hart. Bundoran, W. H. P. ^^^^^-abundant and luxuriant by the streams, s. A. Stewart. Oarrick Lake, W. H. P. 25 Phillips and Praeger — The Ferns of Ulster . Leitrim. — On the Glenade Mountains, W. H. P. Sligo. — Shores of Lough Gill, R. Barrington and R. P. Vowell. interrupta. Carrick Lake, Co. Fermanagh, W. H. P. A very distinct new variety. 16. BOTRYCHIUM. MOONWORT. 1. E. EUWARIA. Common Moonwort. Dry natural pastures. Rather local. Antrim. — Near the second lock on the Lagan Canal, Hannahstown, Knockagh, Black Mountain, and Knocklayd, Templeton. Wolfhill, G. C. Hyndman. Altmore Glen near Cushendall, W. Thompson. Above Colin Glen, S. A. Stewart. Shane’s Castle, Squire’s Hill, and near Randalstown, B.N.F.C. Near Kells, D. Redmond. Cave Hill, C. H. Brett and W. H. P. Carna- neigh, shore at Cushendun, and on Crosslieve near Cushendall, R. LI. P. Down — Scrabo Hill, Templeton, 1806. Carngaver Hill, and on sandhills near Newcastle railway station, S. A. Stewart. Carrowreagh Hill near Craig- auntlet, and Conlig Hill, R. LI. P. Derry. — On Benevenagh, David Moore. Donegal — Culdaff, Dr. Dickie. Templecarn, near Pettigo, Miss Young. Gweedore, P. Mahony. Near Burnfoot, Charles Moore. Leenane, Carra- blagh, west side of Rossgull, Seven Arches, Mullaghmore, and Kildrum, H. C. Hart. Cavan — Lough Sheelin, R. LI. P. Sligo. — Near the summit of Ben Bulben, S. A. Stewart. 17. OPHIOGLOSSUM. ADDER’S TONGUE. 1. O. VU16ATUM. Common Adder’s Tongue. Moist natural pastures. Rather local. Antrim.— By the Lagan near the second lock, Templeton, 1806. On the Knockagh, W. Thompson, and B.N.F.C. 1886. Malone, Dr. Dickie. Wolfhill, W. Millen. Colin Glen and Rathlin Island, S. A. Stewart. Shane’s Castle, 1863, and Cave Hill, 1871, B.N.F.C. Bog Meadows, and Springfield, W. H. P. Plentiful in fields at Cairncastle, R. LI. P. Down.— Grey abbey, 1864, and Mountstewart, 1877, B.N.F.C. Near Cultra House, Robert Patterson— still there. Killinchy, J. Wilson. Crawfords- burn, Mrs. Munster. 26 Phillips and Praeger — The Ferns of Ulster. Armagh.— Ardmore near Lurgan, and abundant in short grass on the shores of Lough Neagh, where it is under water for four winter months, Rev. H. W. Lett. Derry.— Springhill, Garvagh, Somerset, Mountsandal, and sandhills at Magilligan, David Moore. # Donegal.— Kilderry, W. E. Hart. Ballyshannon, Carrablagh, Glinsk, Horn Head, Brown Hall, and very abundant at Leenane, H. G. Hart. Leitrim.— Near the base of Arroo Mountain, Kinlough, R. Barrington and R. P. Vowell. 2. O. X.USITANICUM. Dwarf Adder's Tongue. Dry natural pastures. Extremely rare. Donegal.— On Horn Head and on Carrigan Head, H. C. Hart. . One of our rarest local ferns, whose only known British station— if British it may be called — was Guernsey, till Mr. Hart discovered it on Horn Head in 1878. The same observer has since found it in Co. Kerry. Holywood, Co. Down, November 26th, 1886. W. H. PHILLIPS. R. LLOYD PRAEGER. to Aua >8/ APPENDIX II. VOL. II. THE ESTUARINE CLAYS AT THE HEW ALEXANDRA DOCK, BELFAST, WITH LIST OF FOSSILS BY R. LLOYD PRAEGER, B.E., B.A. PUBLISHED BY THE BELFAST NATURALISTS’ FIELD CLUB. January, 1888, {Proceedings Belfast Naturalists' Field Club. — Appendix 1886-1887.) On The Estuarine Clays AT THE NEW ALEXANDRA DOCK, BELFAST. 4. the construction of the new Alexandra Graving Dock, on the County Down side of the river Lagan, some good sections of our Pose -tertiary Estuarine deposits have been exposed. Being constantly on the ground, I have had a favourable opportunity of observing the different beds over a considerable area, with the organic remains which they contain, and I propose to briefly describe the various strata pierced through in connection with this work, and some of their characteristic fossils. The Pleistocene Clays of the Lagan Estuary have already been closely scrutinised by members of this Club, and in the very complete list compiled by Mr. S. A. Stewart, F.B.S.E.,* containing the results of his own and Mr. (now Eev. Canon) Grainger’s f extensive researches, no fewer than 142 species of fossils are recorded as occurring in these beds. An examination of the deposits exposed in the excavations at the Alexandra Dock has resulted in some additions to this list, and in the present paper I shall notice such species as are noteworthy from their abundance or otherwise in particular beds, or which have not previously been recorded from our North of Ireland Estuarine Clays, and an annotated list is added of all fossils recently observed in the deposits in question. Figure 1 represents a section measured with the spirit-level near the inner entrance of the Dock, and it may be taken as a typical section of the beds exposed. Their relative thickness varied considerably in different parts of the works, but the same sequence was noticeable throughout ; and a similar general relation may be observed, not only where borings or sections have been made * Stewart— “ Fossils of the Estuarine Clays of Down and Antrim,” — Proc. Belfast Naturalists1 Field Club, Vol. 1., Appendix II. t Grainger, in Natural History Review, Vol. VI., for 1859, 30 Praeger — The Estuarine Clays through the strata in the Lagan Estuary, hut in the Quaternary Estaarine deposits in other parts of Ireland, and in England and Scotland. At the Alexandra Dock we hare first several feet of clay and sand, which bed was still in course of formation when the works were commenced, its upper surface being a little above low water mark. Below this is a bed of yellow sand, containing many shells, which probably corresponds in age with the flint-bearing gravels the Kinnegar at Holy wood and the Curran at Larne. Immetotely underlying this is that very distinct deposit, the Estuarine Clay, which at Belfast, Lame, and other points around our coasts, possesses the same peculiar features and yields the same characteristic fossils. Below this is a bed of peat, corresponding with the submerged peat which occurs in so many places on the shores of t British Isles. This rests on fine red glacial sand, the same deposit which occurs at Malone and at the Knock ; which rests in turn on very fine tough red clay- re-assorted Boulder Clay. Underlying this is the Boulder Clay proper, with glacially striated pebbles, which, Anally, overlies the New Bed Sandstone. These last two formations were not exposed at the Dock, but there is no doubt they underlie the red clay, as they do at other points in the immediate vicinity. We have thus an unbroken series of deposits, stretching from the Boulder Clay Period to the present day, and “ offering,” says Mr. Stewart, “ perhaps the bes means of filling up the gap in geological history between the close of the Glacia Epoch and the present day.” . , , . So much for the general section. I now come to a more minute description of the deposits, and shall begin with the section which is shown in Figure 1. This is as follows A M 1 Blackish clay, with sandy layers, of a depth of six to seven feet, the surface between tide marks. Characteristic shells of this deposit are -.-Mya arenana Gardium edule, Tellim Batthica, Mytilm edulis. Mya occurs m beds of thousands, the sheUs all in the position in which they lived, and generally with the siphonal tube preserved. Cardium is also very abundant. This bed yielded two specimens of Helix nemeralis, no doubt washed into it by surface water; and unusually large single valves of Zucma borealis were not unfrequent. 2 Two feet of coarse yellow sand, with abundance of shells, and also tiun layers' of twigs and hazel nuts. The shells are often much worn, and generally occur as single valves, and the deposit has all the appearance of an old sandy beach Pecten opercularis, Zittorina litorea, Mytilm Mis, occurred here abundantly, and fine specimens of Tapes pullastra, Tdeemsatus mi Thracia convexa, which two latter species are not now found living m Belfast Lough- Among the rarer forms which were noticed were :-F,ssurella Grceea Troehm magus. Patella vulgata, Turns amtiqum, Murex erinaeeus, Cypma Ewopcea Anemia patellifmmis, Venus lincta, Cypnrn Islandica. Six species new Estuarine Clays were observed :-Fusm gracilis, Anemia striata, Tapes Venus faseiata, V. exoleta, Area tetragona. Several worn valves of piperata were noticed-this shell will be referred to later on-they had probab y been washed from the underlying beds. at the New Alexandra Dock , Belfast. 31 3. Immediately below the yellow sand, the line of demarcation being remarkably sharp and well defined, is the Estuarine Clay proper. This forma- tion, as Mr. Stewart has shown,* consists at Belfast of two beds which were laid down under widely different circumstances — an upper one, which was deposited in some thirty or forty feet of water at least, and a lower one, which is of a littoral character. The upper bed consists of very fine homogeneous blue clay, and is here about six feet thick. It is remarkably rich in shells, both large and small, many of which do not now exist in our waters, and they are for the most part in a beautiful state of preservation. Thracia convexa, Lucinopsis undata, Car- dium echinatum , Scrobicularia alba , Ostrea hippopus, Acera bullata, are abundant, and characteristic of the deposit. Among many rare fossils obtained from this bed may be mentioned : — Actceon tornatilis, Cyprcea Europcea, Cardium Norvegicum, Tellina tenuis. Not hitherto recorded from the Belfast bed are : — Aclis supranitida , Trochus umbilicatus , JRissoa striata , Melampus bidentatus , Utriculus obtusus, Cardium nodosum ; and the following are new to the deposits : — Capulus Hungarians, Helcion pellucidum, Cylichna cylindracea , Utriculus mammillatus , Anomia aculeata , Echinus sphcera. Beds occur of Ostrea and Eecten maximus , both of which attain a large size ; Scrobicularia piperata is almost unknown. Near the top of the deposit a shell layer occurred, made up almost entirely of Scrobicularia alba and the spines of two Echinoderms — Amphidotus cordatus and Echinus miliaris. It is to be noted that the former, which now occurs around our coasts only in sandy bays, here lived abundantly on a bottom entirely muddy. At the base of the bed just described is a narrow zone in which the boring shells, Pholas crispata and Eholas Candida, occur in profusion ; this layer was also observed by Mr. Stewart on the County Antrim side of the Lagan. The shells are found in a horizontal bed, all in the position in which they lived. P. crispata is of very large size, twice the size which it now attains on the North of Ireland coasts— one specimen measured five inches in breadth by seven and a half in girth. The occurrence of these shells between the overlying deep- water clay and the underlying littoral deposit is of great interest, “and their appearance,” says Mr. Stewart, “is the first intimation of the subsidence then commenced.” 4. We now come to the lower clay, which had a depth of between six and seven feet. It is of a more sandy nature, and has a yellower colour than the upper bed, and is full of the remains of the Grass Wrack, Zostera marina, which furnishes further proof, if such were needed, that this is a shallow water deposit. But the contained fossils testify this conclusively. Scrobicularia piperata is the leading shell of this bed, occurring all through in extraordinary profusion ; an essentially littoral species, which is now quite extinct on our northern coasts. Other characteristic fossils ar e:—Zittorina litorear, Cardium edule, Tapes decussatus. The latter attains by no means so large a size as it does in the bed * Stewart- “Latest fluctuations of the sea-level on our own coasts,” Eighth Annual Report, Belfast Naturalists’ Field Club, 1871. ° 22 Praeger — The. Estuarine Clays of sand above. Shells are far more abundant than in the upper clay, hut the number of species much more limited, and they are many of them in a fragile condition. Eare forms which were noticed here are Scaphander ligmrius , Pleurotoma septangularis , and Eulima bilineatcr, also Philine scabra, Pectenpusio, and Jllactra solida , var. ettiptica , which are new to the Clays. At the base the bed becomes very sandy, and Tellina Palthica is abundant, along with quantities of Cardium edule of small size. The lowest zone consists of grey sand, and is quite unfossiliferous. 5. Immediately underlying the basal sandy layer of the lower clay is the hed of peat before -mentioned, which is now some 27 feet helow high water mark, showing a corresponding subsidence of the land. Of course a far greater subsidence, followed by upheaval, has taken place ; for if the upper clay was deposited in 40 feet of water, the total depression must have amounted to 50 or 60 feet, followed by 30 or 40 feet of subsequent upheaval. The peat is one to two feet thick, very much compressed, and had originally a much greater depth, as is shown by the flat ellipses into which round branches have been pressed. It is full of trunks and boughs of trees, some of which extend upward into the grey sand. Among the vegetable remains, Willow, Hazel, and Alder are easily recognisable. Hazel nuts occur, and the cones of the Scotch Fir. The broad leaves of the Iris are frequent, with remains of rushes and sedges. But the most interesting fossils which the submerged peat yielded were thebones^of laige quadrupeds— a tusk and two portions of the jaw of the Wild Boar, and a rib, vertebra, and leg-bone of the Eed Deer. Wing-cases of insects are of not unfrequent occurrence, and in a tolerable state of preservation. In one place a layer of grey sand occurred in the middle of the peat, rapidly thinmng out m all directions. A sample of this was kindly examined microscopically by Mr. Joseph Wright, F.G.S., but no organic remains were found. That the vegeta- tion which formed this peat flourished on the spot on which it now rests, and was not drifted thither, is proved by the abundance of fine roots which descend several feet into the underlying deposit, which consists of 6 Grey sand, some two to three feet deep, very fine on the top, coarser below. In addition to the roots from the peat, of which the sand is fufl, me only organisms which this bed yielded were Foramimfera ana Ostracoda, oi which Mr. Wright, who has very kindly examined samples of all the deposits a, the Dock for microscopic forms, detected seven species, namely seminulum, Sulimim pupoides, Lagena lavigaU, Jtotalia Beccarn, honvmna depressula. Loxoconcha guttata , Cythere pellucida. 7 The grey sand merges into fine red glacial sand, a deposit winch is largely developed all aronnd Belfast. It is very barren in organic the only fossils detected being two Foraminifera and two Ostracoda : t ySl°” striato -punctata, Rotalia Beccarii, Cythere pellucida, Loxoconcha guUcua^ This sand, which contains occasional clayey layers, had a thickness o four feet, and rested on „ , , iTl not 8. Very fine tough red clay, of glacial age, the base of whxc 33 at the New Alexandra Dock , Belfast. reached in the deepest excavation at the Dock — the foundation of the Rudder Well, over fifty feet below high water mark— although fifteen feet of it had then been passed through. No organic remains were discovered here, but this was probably due to the small sample submitted for examination. As regards the microscopic fossils of these beds, it may be remarked that of the 104 species of Foraminifera recorded from the Post-tertiary deposits of the North-east of Ireland, by Mr. Joseph Wright,* the Alexandra Dock sections yielded forty species, their distribution being as follows : — Estuarine Clay, 40 ; sandy layer overlying peat, 4 ; grey sand under peat, 5 ; red sand, 2. Of twenty species of Ostracoda, all occurred in the blue clay — one in the sandy layer above- mentioned, two in the grey sand, and two in the red sand. One species of each of these orders was found in every deposit throughout— Rotalia Beccarii and Loxoconcha guttata. If we now turn to the section at the outer entrance of the Dock, some 600 feet north of the one just described, some striking differences will be noticed. At the west side of the entrance basin the Estuarine Clay is only four feet thick, and below it is one foot of yellowish clay, which represents the bed of peat. This rests directly upon the fine red sand, the surface of which is here twelve feet higher than at the upper end of the works. At the east side, while making excavations for the inlet culvert, an interesting section was exposed (see Figure 2). Beneath some feet of clay and sand was a bed of coarse blackish sand, with abundance of shells, at the base of which were some two or three inches of almost pure shells. In this layer Littorina litorea was in great abundance, along with Cardium edule , Mytilus edulis, Lucinopsis undata , and Thracia convexa — some littoral and some deep-water forms, it will be noted. This mixture of species is curious, but I think there can be little doubt that the five to twenty fathom shells which occur here in profusion were washed out of the upper clay. The faunas of the two beds (the sand and upper clay) are remarkably similar, considering the very different conditions under which they must have been laid down ; but a closer examination showed me that the deep- water species in the yellow sand were almost confined to its lowest zone, which abounds in the species that especially characterise the upper division of the Estuarine Clay, which lies immediately below it. A fine valve of the rare Cardium Norvegicum occurred here, several examples of Utriculus obtusus, and a single specimen of U. mammillatus, which is new to the Clays. Immediately below the shell layer is the Estuarine Clay, which at this point is only two feet thick. The deposit is very sandy, except at its upper surface, and is replete with species which have lived and died in what was then the sandy bottom of a bay several fathoms deep. Full-sized examples of the large Lutraria elliptica are of constant occurrence, along with large specimens of Mya truncata , and Thracia convexa , Solen vagina , and Tapes pullastra ; of these Mya and Tapes are the only species now found living in the waters of our Lough. A rare and •Wright— “ Post-tertiary Foraminifera of the Xorth-east of Ireland.’’— Proc.Belfast Naturalists’ Field Club, Vol. I., Appendix V. 34 Praeger — The Estuarine Clays interesting specimen which I found here consisted of a large valve of Cyprtna Islandica, to the interior face of which a full-sized Oyster was adhering, its shell fashioned to the shape of the Cyprina , and the other valve was lying close at hand. This tells of a slow rate of accumulation of the deposit. The Cyprina lived and died, and the valves of its shell in time broke asunder. Then the Oyster came and settled in the untenanted house of its predecessor, and it grew and flourished before the slow rain of fine mud buried both m a quiet grave. Pholas crisp at a and P. Candida occur frequently; and a single specimen of Pholas dactylus , new to our Estuarine Clays, was observed. At the base of the bed, where it is quite sandy, there is abundance of Cardtum edule —this stratum evidently corresponds with the lower clay of the first section. Below this we come directly upon the red sand ; there is no trace of the peat bed. The sand is nearly twenty feet in thickness, and rests on the red clay. . It is interesting to compare the sections above described with other sections in the Lagan Estuary which have been examined by local geologists. The beds exposed when Spencer Basin was in course of construction, on the opposite side of the river, which were so thoroughly examined by Mr. Stewart, consisted simply of some twenty feet of Estuarine Clay, which he divides mto three well-defined zones : — 1. Surface clays ; abounding in littoral species. 2. Zone of Thracia convexa ; characterised by shells which live in five to ten fathoms of water. 3. Scrohicularia zone ; in which littoral species again predominate. The physical and palaeontological differences between the two latter were more marked than at Alexandra Dock ; the beds of peat and sand were not exposed. Borings at King Street, in the centre of the town, under the superintendence of Mr. fm. Swanston, F.G.S., showed a depth of no less than twenty-eight feet of Estuarine Clay, at the base of which was a layer containing many twigs and hazel nuts. Next came twenty-four feet of fine running sand, which yielded on examination four species of Eoraminifera, two of these being the two forms obtained in the red sand at the Dock. Beneath this was fifty feet of very fine red Boulder Clay, in which two Foraminifera were found to occur very sparingly, namely Rot alia Beccarii, and Polystomella striato -punctata , the same species which formed the only fossils of the red sand in the Dock sections. The fine clay rested on Boulder Clay, as it usually occurs in our neighbourhood, 100 feet in thickness, and abounding in Foraminifera, underlying which were the sandstones of the New Red. At Sydenham Railway Station a different state of things may he noticed. We have only a couple of feet of Estuarine Clay, replete with the shells of species which live between tide-marks, its upper surface being about three feet above high-water mark, or sixteen feet higher than the top of the Estuarine Clay at the Dock. Then comes a foot of yellow sand, at the base of which is a narrow zone crowded with the crumbling remains of littoral species. This at the New Alexandra Dock , Belfast. 35 rests, at different points, on fine red sand, gravel, or fine red clay ; but before we have reached low-water level, we come upon the coarse Boulder Clay with pebbles, which at this place is therefore some ninety feet higher than in the Lagan Valley a mile to the westward, as shown by the King Street borings. This concludes my brief notice of the Post-pliocene deposits of the Lagan Estuary. The Belfast beds have now been pretty well examined, and our knowledge of them is tolerably complete ; but there is still an ample field for research in the similar clays which are to be found in almost all our loughs and bays ; and it is to be hoped that other members of our Club will devote some of their time and attention to these interesting deposits— the latest page of the great mysterious volume of geological history. The clay at Magheramorne is famous for the profusion of Foraminifera, some of them of great rarity, which it yields,* and its richness in large fossils is apparent from the fact that during one visit— my only visit to it— no less than seventy-one species of fossils were noted, Microzoa excluded. Further examination of this deposit will without doubt result in considerable additions to this number. * See Wright— “ Post- tertiary Forams., N.E. Ireland,” Proceedings Belfast Naturalists’ Field Club, Vol. I., Appendix II. Praeger — Fossils at Alexandra Dock , Belfast. 37 In the following list of 186 species and varieties found at Alexandra Dock, I have employed the term “ top clays ” to designate the clayey and sandy beds which formed the highest and most recent deposit. “ Upper clay ” signifies the upper or deep-water zone of the Estuarine Clay, “Lower clay” the underlying littoral deposit. On account, perhaps, of its less interesting and less varied fauna, the lower clay was not so thoroughly examined as the zone above, and it is probable that some of the species recorded here as from the upper clay alone, occurred also in the lower bed. I have to acknowledge much kind assistance rendered by Mr. S. A. Stewart, E. B.S.E., in the identification of critical species; by Mr. Joseph Wright, F. G.S., who catalogued the Microzoa of the deposits ; and by Professor Cunningham, M.D., of Queen’s College, who identified the vertebrate remains. LIST OF FOSSILS OBSERVED IN THE ESTUARINE CLAYS AT THE ALEXANDRA DOCK, BELFAST. Note. — The nomenclature of the Mollusca is that adopted by J. Gwyn Jeffreys in his Manual of British Conchology. The Foraminifera are named according to H. B. Brady’s Report on the Foraminifera of the “ Challenger ” Expedition ; the Ostracoda in accordance with Dr. G. S. Brady’s Report on the “ Challenger ” Ostracoda. Species marked (*) are additions to the Estuarine Clay fauna of the North of Ireland ; those marked (f) are new to the Belfast deposit. * Cervus elaphus, Linn. A dorsal vertebra, right radius, and posterior right rib of the Red Deer occurred at different spots on the upper surface of the peat bed. * Sus scrofa, Linn. Two portions of the lower jaw of a large Wild Boar, with teeth and both tusks, and at another place a single tusk, were found in a position similar to the Red Deer remains. 38 Praeger — Fossils at Alexandra Dock , Belfast Helix nemoralis, Mull. Two specimens of this land shell occurred in the top clays. Patella vulgata, Linn. Yellow sand, very rare, and much worn. (One specimen, * Helcion pellucidum, Linn. Several young specimens in the upper clay. Grainger). Fissurella Grseca, Linn. Very rare ; a single specimen in the yellow sand. * Capulus Hungaricus, Linn. Upper clay, one specimen. Troclius magus, Linn. In the yellow sand and upper clay, very rare. Troclius cinerareus, Linn. Very frequent, except in the lower clay, where it did not occur. f Trochus umbilicatus, Mont. Upper clay, rare, and of small size. Xiacuna divaricata, Fabr. Very frequent, especially in the upper clay. Xiittorina obtusata, Linn. Frequent throughout. Xiittorina obtusata, var. aestuarii, Jeff. Two examples in the upper clay. Xiittorina rudis, Maton. Frequent in the upper and lower clays. (Scarce, Stewart). Xiittorina rudis, var. tenebrosa, Mont. Upper clay, one specimen. Xiittorina litorea, Linn. Common throughout the deposits. Rissoa inconspicua, Aid. Common, and generally distributed. Now quite extinct in our lough. Rissoa membranacea, Adams. With the last species. Rissoa violacea, Desm. Very frequent in the upper and lower clay, f Rissoa striata, Adams. In the upper clay, not uncommon. Rissoa vitrea, Mont. With the last, but rare. Hydrobia ulvae, Penn. Occurs throughout the deposits ; in abundance in the most recently formed bed. 39 Praeger — Fossils at Alexandra Dock , Belfast. Turritella terebra, Linn. Frequent ; attains a large size in the upper clay. Scalaria Turtonae, Turt. Of constant occurrence in the upper clay. Not now living in Belfast Lough. f Aclis supranitida, S. Wood. In the upper clay, rare. Odostomia lactea, Linn. This elegant little shell is not uncommon in the upper clay and yellow sand. Eulima bilineata, Aid. A single specimen in the lower clay. (One specimen, Grainger). Matte a catena, Da Costa. One small example in the lower clay. Matica Alderi, Forbes. Upper clay, very frequent. Aporrhais pes-pelecani, Linn. Upper and lower clay, and yellow sand, abundant, especially in the first. Cerlthium reticulatum, Da Costa. In the greatest profusion throughout. Purpura lapillus, Linn. In different beds, hut very uncommon. Buccinum undatum, Linn. Plentiful in all but the top clays. Murex erinaceus, Linn. Very uncommon in the deposits, hut of large size. Fusus antiquus, Linn. A few specimens, of large size, occurred. * Fusus gracilis, Da Costa. In the yellow sand, extremely rare. Nassa reticulata, Linn. A common shell in the upper clay and yellow sand. Nassa pygmaea, Lamk. Very abundant in the upper clay, hut does not occur in either the lower clay or top clay. See Mr. Stewart’s note in his list of Estuarine Clay Fossils. Pleurotoma brachystoma, Phil. Two specimens in the upper clay. Pleurotoma septangularis, Mont. I found one specimen in the lower clay. 40 Praeger— Fossils at Alexandra Dock , Belfast Cypraea Europaea, Mont. Our little cowry is extremely rare. The upper clay yielded one specimen, and the yellow sand another. * Cylichna cylindracea, Penn. In the upper clay, very rare. * Vtriculus mammillatus, Phil. A fragment of a shell of this tiny species in the yellow sand made me look for more, and I discovered a perfect specimen in the upper clay. f Utriculus obtusus, Mont. In the upper clay and yellow sand, hut few and far between. Vtriculus byalinus, Turt. One specimen was discovered inside the closed valves o a apes , lower clay. (Plentiful in the Belfast bed, Stewart ). Accra bullata, Mull. . . In profusion in the upper clay, but so fragile that it is well nigh impossible to obtain a perfect specimen. Actaeon tornatilis, Linn. One dilapidated specimen in the upper clay. Scaphander lignarius, Linn. Lower clay, very rare. Philine aperta, Linn. Very frequent in the upper clay and yellow sand. * Philine scabra, Mull. In the lower clay, very rare, f Melampus bidentatus, Mont. Upper clay, very scarce. Anomia ephippium, Linn. Quite abundant in the upper and lower clay and yellow sand, n every variety of shape and size. I obtained one beautiful specimen adhering to the flat valve of a large Pecten maximus , with ridges on both valves as high and regular as those on the Pecten , and measuring four inches m diameter. * Anomia aculeata, Mull. Two or three specimens occurred in the yellow sand. Anomia patelliformis, Linn. Very rare. One specimen was obtained in the yellow sand. (Rare, Grainger) . * Anomia patelliformis, var. striata, F. 8f H. Yellow sand, a single valve. Ostrea edulis, Linn. The Oyster is abundant throughout the deposits. Fine examples occur m numbers in the upper clay, the colours in the interior as vivid as if the animal had inhabited the shell but yesterday. Praeger — Fossils at Alexandra Dock , Belfast. 4i Ostrea edulls, var. hippopus, Lamb. In the upper clay, frequent, and of immense size. One specimen weighed over a pound and three quarters. Pecten varius, Linn. Single valves not uncommon, perfect specimens rare. Pecten opercularls, Linn. Fine examples are scattered plentifully through the upper clay ; in the yellow sand single valves are abundant. Pecten maximus, Linn . In the upper clay, here and there, regular layers of the large shells of this species and of the Ostrea were observed. * Pecten pusio, Linn . One valve of this deformed-looking species was found in the lower clay. A rare shell in our present waters, and not hitherto observed in the Estuarine Clays. Mytilus edulls, Linn. The Mussel is plentiful in the top clays and yellow sand, reaching in the latter its full limit of size. In the upper clay it is unknown, but appears again in the lower clay in a crumbling condition. * Mytilus edulls, var. pellucidus, Penn. Examples of this perhaps not distinct variety are frequent. Mytilus modiolus, Linn. Not at all common. I obtained one perfect specimen and a few fragments in the upper clay. Mytilus Adriaticus, Lamk. Eare ; a few young shells in the upper clay. Nucula nucleus, Linn . Diffused through the upper clay. * Area tetragona, Poli. One complete specimen in the bed of yellow sand. Montacuta bidentata, Mont . This tiny bivalve is scattered plentifully through the upper clay and yellow sand. Montacuta ferruginosa, Mont. In the upper clay, very rare. Iiucina borealis, Linn. In the uppermost deposit at the Dock large specimens of this shell occurred, but only as single valves. Axinus flexuosus, Mont. Generally diffused, and abundant. 42 Praeger — Fossils at Alexandra Dock , Belfast . Cardium ecbinatum, Linn. . , In the deep-water clay fine specimens of this beautiful species are abundant. Worn single valves are common in the overlying yellow sand. Cardium exiguum, Gmel. Diffused through the deposits, hut scarce, and usually as single va ves. + Cardium nodosum, Turt . The upper clay yielded one small valve of this species, so rare as an Estuarine Clay fossil. Cardium edule, Linn. . , In the top clays and yellow sand abundant and large, not uncommon in t upper clay, and in the lower clay very abundant, hut of small size. Cardium edule, var. rusticum, Chemn. Some very oblique valves probably belong to this variety. Cardium Norve&icum, Speng. This fine shell is very rare. A single valve was discovered in the upper clay, and another in the blackish sand of the outer entrance section. (One valve, Grainger'. Two or three valves, Stewart). Cyprina Islandica, Linn • Beyond the complete specimen mentioned in my paper (p. 34), t y evidence of the occurrence of this large shell was the fragments of one great valve, which had been some five inches in breadth, which I found in the yellow sand. (One perfect specimen, Stewart ). Venus lincta, Fult. , Bare ; a few single valves scattered through the top clays an ye ow sa * Venus exoleta, Linn. Very rare ; three single valves occurred m the yellow sand. Venus Gallina, Linn • . Distributed through the upper and lower clays, but of small size. * Venus fasciata, La Costa. A single valve in the yellow sand. Tapes aureusi Gmel. Frequent, and scattered throughout. Tapes aureus, var. ovata, Jeff. Very rare. (Not uncommon, Stewart). Tapes pullastra, Mont. . In the upper clay and yellow sand, where it attams an unusual size. (Frequent, especially in the lower zone, Stewart). Tapes decussatus, Linn . . .. . In the yellow sand very large valves are frequent. In the upper clay uncommon, but large; and in the lower clay it occurs in profusion, hut small. Praeger — Fossils at Alexandra Dock) Belfast. 43 * Tapes virgineus, Linn. Yery rare. I found two worn valves in the yellow sand. Iiucinopsis undata, Penn. In great abundance, and very large, in the upper clay, of which it is one of the most characteristic fossils. Large single valves occur in numbers in the shelly layer at the base of the yellow sand, lying on the upper surface of the clay. Tellina Balthica, Linn. In profusion, but of small size, in the top clays. Abundant and large in the lower clay, particularly in the basal portion. Tellina tenuis, La Costa. Very rare. A few specimens in the newest deposit. Psammobia Ferroensis, Chemn. Single valves occasionally observed. * IVtactrasolida, var. elliptica, Brown. One valve in the lower clay. Mactra subtruncata, La Costa. Yery frequent, but small and of variable form, in the deposits. XiUtraria elliptica, Lamk . Over the greater portion of the excavations young specimens only occurred, but, as previously mentioned, near the outer entrance, where the clay thinned out to a depth of only a couple of feet, full-grown specimens were abundant, covered with a rich golden-brown epidermis, and measuring up to six inches in breadth. Scrobicularia alba, Wood. In extraordinary profusion in the upper clay. Much rarer in both the underlying clay and the yellow sand. Scrobicularia piperata, Bellonius. In countless thousands in the lower clay. Almost entirely absent from the other beds. Solen pellucidus, Penn. Frequent in the deep-water deposit. Solen vagina, Linn. In the upper clay and yellow sand, not uncommon. It is very strange how this species has disappeared from our bay, and how S. siliqua , which is unknown in the Estuarine Clays, has taken its place. Solen ensis, Linn. With the last, but rarer. Thracia papyracea, Poli. Upper clay only, not rare. Fossils at Alexandra Dock , Belfast 44 Praeger— Thracia convexa, W. Wood. Yery characteristic of the upper clay, in which it Common also with Lucinopsis in the shell layer clay. Quite absent from the lower and top clays. is found in abundance, which rests on the upper Corbula gibba, Olivi, Common in the upper clay, frequent in the lower bed. Mya arenaria, Linn. Top clays only, where it is in great abundance. Mya truncata, Linn. . , Plentiful throughout the upper clay, and very large. Single valves m the yellow sand. Fholas Candida. Linn. , With the two following species, this boring shell occurred only m the Pholad zone, between the upper and lower clay, where it was abundant. Pholas crispata, Linn. Perfect specimens, of most unusual dimensions (see p. 31), were observed all over the area of excavation, but only in the zone above-mentioned. * Pholas dactylus, Linn. A single complete specimen in the Pholad layer. Teredo ITorvegica, Speng. . Fragments of the calcareous tubes of this species were found in the upper clay. * Echinus sphsera, Mull. Spines of this large Echinoderm in the upper clay. Echinus miliaris, Leske. This “urchin ” is rather common in the clays, hut is of small size. ■ r. Stewart mentions a thickly -packed layer of the shells of this species near the surface of the upper clay at Spencer Basin.* JLmphidotus cordatus, Fenn. The fragile shells of this “ heart-urchin ” are rather common m the upper elay, and its spines occur in profusion. * Cancer pagurus, Leach. Fragments of a large claw in the yellow sand. * Carcinus maenas, Leach . I twice got remains of this crab in the upper clay. * Portunus depurator, Leach . Top clays, rare. Serpula triquetra, Linn. Yery frequent on shells all through. See Footnote, page 29. Praeger — Fossils at Alexandra Dock, Belfast . 45 Serpula vermicularis, Linn. Not uncommon in the deposits. Cornuspira involvens, Reuss. Frequent in the Estuarine Clay.* t Biloculina ringens, LamJc. Estuarine Clay, rare, t Biloculina depressa', d' Orb. Estuarine Clay, very rare. XVXiliolina oblonga, Montagu. In the blue clay, rare. XVXiliolina seminulum, Linn. Frequent in the blue clay; also occurred, but sparingly, in the grey sands, both above and below the peat bed. (In great abundance, Stewart. Bare, Wright). f XVXiliolina secans, d'Orb. In the blue clay, rare. Miliolina subrotunda, Montagu. Blue clay, rather frequent. (Very rare, Wright). * XVXiliolina sclerotica, Karrer. Blue Clay, frequent. Trochammina squamata, J.*P. Very rare in the Estuarine Clay. Trochammina macrescens, Brady . Estuarine Clay, very scarce. Trochammina indata, Montagu. Estuarine Clay, frequent. Bulimina pupoldes, d'Orb. Common in the Estuarine Clay, rare in the basal sandy portion. Bulimina ovata, d' Orb. Frequent in the blue clay. Bulimina elegantissima, d'Orb. Abundantly distributed through the blue clays. Bulimina marginata, d'Orb. With the last, and equally ^abundant. Virgulina Schreibersiana, Czjzelc. Blue clay, frequent, f Bolivina punctata, d'Orb. Generally diffused through the blue clay. * I reoret that in the case of the Foraminifera and Ostracoda I did not take care to obtain samples of both the upper and lower clays, and have them examined separately, bam pies of the clays were closely scrutinized, but the fossils of both the littoral and deep water beds were grouped together under the head of “ Estuarine Clay,” or “ Blue Clay ” 46 Praeger — Fossils at Alexandra Dock , Belfast. Bolivina plicata, d'Orb. Very frequent in the hlue clay. (Rare, Wright ). * Bolivina difformis, Will. In the hlue clay, rare. Lagena Isevis, Montagu. Estuarine Clay, frequent. * Xiagena Isevis, var. clavata, d Orb. Estuarine Clay, frequent. Xiagena striata, d'Orb. Frequent throughout the hlue clay . f Lagena gracilis, Will. One or two specimens only, in the hlue clay. Xiagena semistriata, Will. Rather more frequent than the last, t lagena hexagona, Will. Blue clay, very scarce. * Xiagena laevigata, Eeuss. A few examples in the grey sand under the peat. * Lagena laevigata, var. lucida, Will. Frequent in the Estuarine Clay. * Xiagena Orbignyana, Seg. Blue clay, very scarce, t Sffodosaria communis, d'Orb. A single specimen in the hlue clay, f K’odosaria scalaris, JBatsch. Very sparingly distributed, f Cristellaria rotulata, Lamk. Blue clay, very rare. Polymorpbina lactea, W. £ J. A few examples in the Estuarine Clay, f Uvigerina angulosa, Will. Not at all common. 4 Globigerina inflata, d'Orb. Very rare, one specimen only. Biscorbina globularis, d'Orb. Not uncommon in the hlue clay. (Very rare, Wright). f Planorbulina Mediterranensis, d'Orb. Blue clay, frequent. Truncatulina lobatula, W. § J. Blue clay, scarce. Praeger — Fossils at Alexandra Dock , Belfast. 47 Rotalia Beccaril, Linn. Abundant in the blue clay, and in the greatest profusion in the basal sandy layer. In the grey sand below the peat it was of frequent occurrence, and in the red glacial sand a few much-worn specimens were observed. f Rotalia nitida, Will. In the Estuarine Clay, very rare. ffonionina depress ala, W. $ J. Common in the blue clay. In the grey sand overlying the peat it was very scarce, but in the grey sand under the peat it again occurred abundantly. Polystomella crispa, Linn. Of frequent occurrence. Polystomella striato-punctata, F. # M. In the Estuarine Clay abundantly ; also in the red sand, where it was extremely rare. Pontocypris mytiloides, Norman . Blue clay, rare. Cythere pellucida, Baird. Abundant in the blue clay and in the sandy layer at its base ; very rare in the red sand. Abundant in the lough at the present time* Cythere crispata, Brady. Plentiful in the blue clay ; very rare in our present waters. Cythere viridis, Muller. In the blue clay, very scarce. (Throughout the deposits, Brady , Crosskey , and Robertson), f Cythere lutea, Muller. Blue clay, not common. Cythere conveia, Baird. Blue clay, very rare. Cythere villosa, G. 0. Sars. Very rare. (Throughout the clays, Brady , Crosskey , and Robertson). Cythere concizma, Jones. Common in the Estuarine Clays. Cythere tutoerculata, G. 0. Sars. Like the last, common. Cythere Dunelmensis, Norman. In the Estuarine Clay, not unfrequent. Extremely rare in our present waters. * For the present distribution of Ostracoda in our waters, see Malcomson, “Recent Ostracoda of Belfast Lough.”— Proc. Belfast Naturalists’ Field Club, Vol. II., Appendix IX + Brady, Crosskey, and Robertson— Monograph of the Post-tertiary Entomostraca of bCOtlanrL r». 109 48 Praeger — Fossils at Alexandra Dock ^Belfast Cytbere antiquata, Baird. Frequent in the blue clay. Cythere Jonesii, Baird . Diffused through the blue clay. Cytbere Whiteii, Baird. Blue clay, rare. Not now found in the lough. * loxoconcba guttata, Norman. Plentiful in the Estuarine Clay. It also occurred sparingly in the sand both above and below the peat bed, and in the red sand was very rare. Loxoconcha impressa, Baird. Not uncommon in the blue clay. Cytberura nigrescens, Baird. In the blue clay, abundant. Cytberura striata, G. 0. Sars. Not at all common. Cytberura undata, G. 0. Sars. Yery scarce in the clays. Paradoxostoma ensiforme, Brady. Blue clay, frequent. * Paradoxostoma Fischeri, G. 0 Sars. Rare in the Estuarine Clay. Yery rare in our present waters. Pinus sylvestris, Linn. Cones and branches of the Scotch Fir occurred in the submerged peat. Quercus Robur, Linn. A few houghs in the peat. Alnus glutinosa, Gaert. Occasional seed vessels in the peat. Salix alba, Linn. Boughs and stumps, which, I believe, belonged to this species, were abundant in the peat. Corylus Avellana, Linn. Hazel nuts were of frequent occurrence in the peat, and were quite plentiful in certain thin layers in the top clay. Iris pseud-acorus, Linn, Leaves and fruit in the peat. Zostera marina, Linn. The Grass -wrack is very abundant in the lower clay* Pteris aquilina, Linn . Rhizomes of the Bracken were not uncommon in the peat bed. Praeger — Fossils at Alexandra Dock} Belfast 49 In order to render this a complete catalogue of the Fossils of the Belfast Clays, I append a list of all species which have heen recorded from these beds by other observers, which did not occur at the Alexandra Dock. These, added to the preceding, bring up the total number of fossils found in the Belfast deposits to 235 species and varieties. Helix rotundata, Linn. One specimen, Grainger. Zonites nitidulus, Drap. Two specimens, Grainger. Tectura virginea, Mull. Very rare (one young specimen), Stewart. lacuna crassior, Mont. Was distributed in some numbers, Grainger, Xiacuna pallidula, Da Costa. Scarce, Stewart. Odostomla pallida, Mont. Was met with sparingly, Grainger. Odostomia acuta, Jeff. Bare, Stewart. Odostomia indistincta, Mont. Bare, Stewart. Odostomia interstincta, Mont. Very rare, Stewart. Defrancia gracilis, Mont. Very rare, one specimen only, Stewart. Pleurotoma costata, Donovan. One specimen, fide Grainger. Pleurotoma rufa, Mont. As a post-glacial or quaternary fossil I have identified P. rufa from only the Belfast deposit.” — J. G. Jeffreys. Pleurotoma turricula, Mont. Bare, Stewart. Cyliclma nitidula, Lov. One shell, Stewart. Xiima Ilians, Gmel. Very rare, Stewart. Praeger— Fossils at Alexandra Dock , Bellas, . Mytilus Adriaticus, van “ Occurred in excavating ovalis, Sowerby. a channel in Belfast Harbour.”-/.*?. Jefrey* IVEodiolaria marmorata, Forbes. Yery rare, Stewart. I«eda minuta, Mull. A single valve, Grainger. Cyamium minutum, Fabr. Eare, Stewart. Tellina squalida, Pult. 7 hompson — Belf. Mus. Coll. Psammobia vespertina, Chemn. A single valve, Grainger. SVIactra truncata, Mont. Scarce, Stewart. IiUtraria oblonga, Gliemn. One large specimen, fide Grainger. Solecurtis antiquatus, Pult. A single specimen, fide Grainger. Thracia pubescens, Pult. One specimen, Grainger. Panopea plicata, Mont. Plentiful in one narrow zone, Stewart. Saxicava rugosa, Linn. Eare, Stewart. Saxicava rugosa, van arctica, F. $ LL. Eare, Grainger. Gastrocbaena dubia, Penn. Yery rare, Grainger. Creusia verruca, Leach. Two or three specimens, Grainger. Pectinaria Belgica, Pall. One specimen, Grainger . Terebella concbilega, Fall. Grainger. Miliolina trigonula, LamJc. Common, Stewart. Eare, Wright. Spiroloculina limbata, d? Orb. Eare, Stewart. Spiroloculina planulata, Lam i. Yery rare, Stewart. Praeger — Fossils at Alexandra Dock , Belfast 51 Textularia sagittula, Lefrance. Rare, Wright. Textularia variabilis, Will. Common, Wright. Verneuilina polystropha, Rems. Very rare, Stewart. Lag’ena gracillima, Seguenza. Rare, Wright. Cytbere albomaculata, Baird. Rare, Stewart. Cytliere pulebella, Brady. Near the surface of the clays, Brady , Crosslcey, ani Robertson .* Cytheridea elongata, Brady. Surface of clays, B., Cl, and R. Iioxocouclia tamarindus, Jones . In the oldest and newest zones of the clays, B , (7. , and R. Xestoleberis depressa, G. 0. Sars. B., C., and R. Xestoleberis aurantia, Baird. B., Cl, and R. Cytberura similis, G. 0. Sars. Lowest zone of the clays, B., C., and R. Cytberura affinis, G. 0. Sars. B., Cl, and R. Cytherura gibba, Mailer. Lowest zone, B., C., and R. Cytberura acuticostata, G. 0. Sars. Uppermost zone of the clays, i?., Cl,: and R. Paradoxostoma variabile, Baird. B. C. and R. * Monog. Post-tert. Entom., Scotland, p. 102. APPEBDXX III. VOL II. THE MARINE SHELLS OF THE NORTH OF IRELAND. BY R. LLOYD PRAEGER, B.E., B.A. PUBLISHED BY THE BELFAST NATURALISTS’ FIELD CLUB. February, 1889. ALKX. MAYNE & BOYD, PRINTERS, BELFAST. {Proceedings Belfast Naturalists’ Field Club . — Appendix 1887-1888.) 'gftcmne g>$?e£ £$ of f$e Ulorff) of gxetanb. (:-=) INTRODUCTION. N compiling the following list of the recent Marine Shells of the North of Ireland, the object of the writer has been to bring together, and present in simple and accessible form, the information which we possess regarding this attractive branch of local zoology. The literature hearing on the subject consists of a number of papers and notes scattered through various publications, some of them not easily obtainable by the enquirer, while the matter which they contain is generally in such a form that it is not easy to discover immediately what shells have been found in our district, and in what localities. Such, too, is the difference of nomencla- ture in the works referred to, that it is a task of some difficulty to compare and correlate the lists of Mollusca which they contain ; and in Thompson’s works, indeed, which were published before the value of systematic nomenclature was appreciated as it is nOw, it is occasionally very troublesome to find what species is intended. In the list which follows, the names adopted by J. Gwyn Jeffreys in his “ British Conchology” — the standard work on the subject— are employed, and where a species is referred to by any of the authors quoted under a different name, such synonym is appended in parenthesis. The sources of information which have been utilised in preparing the present paper are as follows : — I. “A History of British Mollusca,” by Messrs. Forbes and Hanley. This work supplies a few North of Ireland stations for species, other than those taken from Thompson’s work, to be mentioned immediately. j6 Praeger—The Marine Shells II. “ The Natural History of Ireland,” by "William Thompson : vol. IY., 1856 In this work 350 species and varieties of Marine Shells are recorded as Irish, under the names which were in use prior to the publication of Forbes and Hanley’s treatise, of which some 240 are noted from localities ra_ Plater 1 the maiority of these notes are given verbatim in the following pages. Mr. Ihomp- son’s earlier list of Irish Shells, which appears in his “ Report on the Fauna , o Ireland: Division Invertebrate in the British Association Report for 1843, contains many species not to be found in the “ Natural History of Ireland ; but it may be safely assumed that such were intentionally excluded from the latter work, for many Shells had been recorded as native on very insufficient grounds ; and the writer has, therefore, thought it best to be guided by the ‘‘Natural History” alone, as it contains all the notes wmch Mr. Thompson considered thoroughly reliable. n III. The “ Reports of the Belfast Dredging Committee, by George Hyndman, in the Reports of the British Association for 1857, ’58, and 59. The * ii T) nArifoin Station. Depth in Fathoms. Species. 1857 Report. 1. Belfast Bay and Neighbourhood 0-100 205 2. Turbot Bank . . 25-30 192 3. Off Maiden Rocks 70-100 42 1858 Report. 1. 2 Miles off Ballygalley Head 15-25 52 2. Cod Bank, 3m. N. of Muck I. 20 73 3. Lame Lough, l-2|m. from entrance..., 4-5 26 4. Brown’s Bay, Island Magee 1-4 21 5. S. of Maiden Rocks 20 45 6. E. and S.E. of Maiden Rocks 70-90 95 7. Turbot Bank .. . 25-30 129 8. Turbot Bank ... , 25-30 18 9. 2 Miles S.S.E. of Black Head 25 118 10. “ TheRiggs” Bank, S.E. of Donaghade< i 20 63 11. 4 Miles S.S.E. of Black Head 15 79 12. The Sound, Copeland Islands 12 40 of the North of Ireland \ 57 1859 Eeport. An annotated list of additional species and additional localities, and a few corrections. The Stations above are conveniently arranged in four groups, viz : — 1. Belfast Lougb. This signifies the waters lying west of a line drawn from Orlock Point, in Co. Down, to Black Head, in Co. Antrim, and not exceeding 10 fathoms in depth. 2. Entrance of Belfast Lough. Under this head come a number of dred- gings made around the entrance of the Bay, from Donaghadee on the Co. Down shore, northward as far as the great cliff-range of The Gobbins, in Island Magee, Co. Antrim. By far the most important of these, as far as results are concerned, are those made on the Turbot Bank, “a great submarine bank lying a short distance out from the cliffs called The Gobbins, and extending from the Isle of Muck across the entrance of Belfast Bay towards the Copeland Islands.”* On this bank, which lies in from 25 to 30 fathoms of water, a number of rare and interesting species have been obtained, but almost all in a dead state, and it is to be noted that some of the Turbot Bank shells are very doubtfully recent, while a few are certainly fossil. Mr. Hyndman expresses the opinion that the majority of the shells are derived from the deep recess lying near the Maiden Eocks, a few miles to the northward, which will presently be mentioned ; but it would appear probable that some submarine pleistocene deposit in the neigh- bourhood has also contributed to the rich store of Testacea which the Turbot Bank yields. f 3. Larne Lough. Mr. Hyndman’s party made but one haul of the dredge in this lough ; it yielded so little that apparently the scientists never revisited waters that gave so poor a return for their labours. This poverty in shells is the more remarkable when we take into consideration the extreme richness in Mollusca of the Estuarine Clays in that vicinity. 4. Off Lame. This term embraces a large number of stations, from Isle of Muck northward to Bally galley Head, andout eastward to beyond the Maiden Eocks . The latter consist of a group of rocky islets lying some six miles from shore ; on their seaward side the water deepens rapidly, and over a limited area a depth of 90 and 100 fathoms is reached. This abyss, which is very difficult to dredge on account of the rocky nature of the bottom and the strong currents that sweep over it, is the home of many rare species, and those who have successfully faced * Hyndman, 1857 Report. f The question of the origin of the Turbot Bank shells is one of much interest, and has not been satisfactorily settled. The opinion of the compilers of the Naturalists’ Field Club “ G-uide to Belfast and the adjacent Counties,” is worth recording: — “About 200 species of Mollusca have been enumerated from the Turbot Bank, many of them being of extreme rarity; but the majority occurring as dead shells only. It has been suggested that this bank is only a submarine fossil bed, and that a great portion of the shells are really relics of the glacial epoch. It is, however, quite as likely that they are accumulated on this bar by currents, and that they belong to species still living in the vicinity, on rocky bottoms where the dredge has little chance of picking them up.” 5« Praeger — The Marine Shells the troubles attending dredging on such ground, atsncha depth, jmvebeen rewarded with living examples of Argiope cistellula, A. capsula, PropiMtmt ancycloides , and other deep-sea treasures. IY “ Report on the Marine Zoology of Strangford Lough, Co. Down, and corresponding part of the Irish Channel,” by George Dickie, M.D., Professor of Natural History, Queen's College, Belfast, in the British Associa- tion Keport for 1857. A summary of the lists here presented is as follows .- Station. Depth in Fathoms. Species and Varieties. 1. Castle Ward Bay 20 102 15 28 2. Wellstream Bay ... 3. Upper part, ditto 4-8 43 13 4. Bay opposite Killyleagh 6 5 . Centre of Lough ... 15-25 38 6 . Gun Island, Irish Channel ... 7 8 Then follow lists of the Testacea of the open channel opposite the entrance of the Lough, divided into zones according to the distance from s ore. V. “British Conchology by J. Gwyn Jeffreys, F.K.S., l86*-9, This work contains, besides repetitions of many of Thompson s, Diet ^ s and Hyndman’s records, some notes of species obtained by the author, and ako by Mr. WaUer and Mr. Adair, on the North of Ireland coasts ; those notes will found under the respective species. There are earlier works which contain references to Nort ° reJn Mollusm but aU reliable records of any importance are to be found repeate cited above. During the long period that has elapsed since th e pnbb cation of even the latest of these, though a good deal of tod«m^i6e” arine by local scientists, very little has been added to the ^wledge of o« M^e Shells, attention having been chiefly concentrated on ^e “terertmg ^ which the earlier Naturalists had left almost untouched Intod to only additional matter of which I have been able to avail myself s a "" “ couein in the Belfast Museum, has yielded some additional stations for species. of the North of Ireland. 59 Where practicable, I have preferred giving verbatim quotations from the authors quoted, in place of a general summary of their remarks. Of the 404 British species contained in that portion of the Suh -Kingdom Mollusca, as described by Jeffreys, to which the present paper refers {i.e. the classes Brachiopoda , Conchifera, Solenoconchia , and Gasteropoda to the end of Pleurobranchiata ), our district has yielded 291, or very nearly f— 1 1 9 bivalves and 172 univalves — exclusive of such species as are importations or fossils, and which are printed inside brackets. On the whole, the Fauna has a northern aspect, since, of these 291 species, 36 are boreal forms, which live either not at all, or very sparingly, south of Britain, while only 12 are essentially southern, having been taken seldom or never north of the British coasts ; the remaining 243 inhabit seas both north and south of our islands. As is to he expected from geographical considerations, the southern species frequent chiefly the western shores of the province, while the northern forms have been mostly taken on the eastern coast. Of the northern types, Crenella decussata, Leda minuta, Tectura testudinalis , E mar g inula crassa, Trichotropsis borealis , and Trophon truncatus , will serve as examples — they have all been taken alive in our waters ; while the following will serve as representatives of the southern forms which the district yields — Modiolaria costulata, Crenella rhombea , Area lactea , Troehus Duminyi , Natica sordida , Ovula patula. Only one species is, as a British shell, confined to our province — Troehus Duminyi ; it occurs on the western coast, and is a southern shell, its foreign stations being all Mediterranean. The Testacea of the counties of Antrim and Down may he considered as pretty well worked up, though the North of Antrim offers a good field that has been scarcely touched. County Londonderry contains extensive sandy beaches, which yield a large variety of species, that of Magilligan especially ; here the observations have been chiefly made from shore, and dredgings in the deeper water might yield interesting results. I find no record whatever of any dredging in Lough Foyle. From the extensive coast-line of County Donegal, with its magnificent headlands and deep inlets and sandy hays, comes hardly a single note to enrich the list which follows. At Bundoran, indeed, in the extreme southwestern corner of the county, Mrs. Hancock made many finds, which she communicated to Thompson; and here Mr. Waller discovered a new British Troehus , T. Duminyi, whose only British station is still Bundoran ; but beyond these, the conchology of the most northern county of Ireland still remains to be investigated, and will probably amply repay the investigator. Mr. Thompson appears to have placed but light value on the condition (living or dead) of the shells which he found in his dredgings, or thrown up by the tide, and in many instances does not mention this point at all. In the present paper the writer perhaps has erred in the opposite extreme, and has plqced undue importance on this point, but it does appear to him to be of interest and importance to know whether or not a shell has been taken living in the district. It is to be remembered, however, that the fact of a species not having been found living, is by no means positive proof that it no longer 6o Praeger — The Marine Shells inhabits a region. Many bivalves burrow deeply in sand and mud, and flourish out of reach of the naturalist’s dredge. When they die, the shells come up to the surface, and are thus thrown on shore by the waves, or taken by the dredge, in a fresh state. In conclusion, the writer expresses a hope that the following list may prove a reliable foundation for a more complete and extended paper on the Marine Mollusca of the North of Ireland, and that by showing the incomplete- ness of the record, it may encourage other workers to give some of their attention to this interesting subject. of the North of Ireland . 6 1 ANNOTATED LIST OF SPECIES. CLASS BEACHIOPODA. The Brachiopoda are well represented in the district, as out of the six British representatives of the class, four live in our waters. Tereljratula caput-serpentis, Linne. Not uncommon in the deeper water at the entrance to Belfast Lough, and off Lame, from the Copeland Islands to the Maiden Bocks, living in from 12 to 100 fathoms of water— Thompson ( T . aurita ), Hyndman, and others. Dickie obtained it alive at the entrance to Strangford Lough in 12-15 fathoms. Argiope cistellula, Searles Wood. “Living on stones as well as shells in the deeper water ’’—Hyndman, 1859 Beport. Labels in the Belfast Museum Collection show that the Turbot Bank is the place intended. iLrgiope capsula, Jeffreys. Hyndman records this rare species {sub Terebratula capsula ) as found living with the preceding, and Jeffreys, referring to the same station, says “Larne, Co. Antrim (Hyndman and J. G. J.)” The latter author also gives “ off Port- rush (Waller).” Crania anomala, MUller . Off Larne, and at the entrances to Belfast and Strangford Loughs, living in 12-90 fathoms — Thompson ( C . personata ), Hyndman, and Dickie. CLASS CONCHIFERA. ORDER LAMELLIBRAN CHI ATA . Anomia ephippium, Linne. Abundantly distributed throughout our waters, living in from 4 fathoms in Strangford Lough to 90 fathoms near the Maiden Bocks, attached to stones and shells. Different forms of this very variable species are recorded under the names A. squamula, A. cylindrical and A. aculeata. 52 Praeger — The Marine Shells Anomia patelliformis, Linne. General, living in 12-90 fathoms. Thompson has it under A.undulata; he mentions a fine specimen which was obtained adhering to the inside of a quart bottle found in the stomach of a cod-fish ! mr. striata. Frequent, living in from 12 to 25 fathoms ; Hyndman dredged dead shells in up to 100 fathoms {A. striata.) Ostrea edulis, Linne. Gregarious, and widely distributed, from low-water mark to 2o fathoms. Thompson mentions Carrickfergus oysters which he examined, which weighed, before being opened, over 21bs., the animal by itself weighing l^oz. ^ Hynd- man states, on the authority of a Groom sport fisherman, that oysters “ of large size and good quality” have been brought up on the long lines from 45 fathoms ; this depth is the limit assigned by Jeffreys to the species. Pecten pusio, Linne. Living in Belfast, Strangford, and Carlingford Loughs, and in the deeper waters of the Channel, in up to 90 fathoms, its other limit of depth being 10 fathoms. Thompson notes it sub F. sinuosus. Dead valves frequent on the Derry coast — R.L1.P . Pecten varius, Linne. , 10-25 fathoms, attached to old bivalve shells, &c., like the last species. Of general occurrence around the coasts of Donegal, Derry, Antrim, and Down. Pecten opercularis, Linne. _ A common species, and almost universally distributed, living on san m from 7 to 25 fathoms. var. lineata. “Var. lineatus I have dredged in Belfast Bay Thompson. I have it also from this locality — R.L1.P . Pecten septemradiatus, Muller. Recorded with doubt {sub F. Fanicus) by Hyndman in his 1857 Report as from the Turbot Bank, determined by Dr. Dickie. In 1859 Report he records the finding of a second valve, in 80 fathoms, thus confirming Dr. Dickie’s determination. Pecten tigrinus, Muller. Thompson mentions this shell, under the names F. Icevis and F. obsele.us, both of Pennant, as having been found in Belfast and Strangford Loughs. Hyndman dredged it frequently, living in 20-90 fathoms, and Dickie records it from Strangford Lough as living in 12-20 fathoms. Single valves at Port- rush— Miss Richardson ; and Magilligan— R.L1.P. Pecten Test®, Bivona. . , The following note on this rare species occurs in Hyndman’s 1859 Report {sub F. furtivus ):- “Taken alive in 1858 by Mr. Waller and Mr. Hyndman on both the Antrim and Down coasts, along with F. striatus. It was taken again this year, and at once distinguished by Mr. Jeffreys.” of the North of Ireland . 63 Pecten striatus, Muller. “A single specimen dredged in Strangford Lough in 1837 by Mr. Hynd- man and myself ” — Thompson. Hyndman obtained it twice alive off Donagh- adee, in 12 and 20 fathoms respectively, and also in 70-90 fathoms off the Maidens, and dead on the Turbot Bank. Dickie dredged dead valves in Strang- ford Lough. Pecten siznilis, Laskey. No note of its having been taken alive, hut dead valves have been dredged frequently at the mouth of Belfast Lough, in 15-35 fathoms, and Dickie records the same from the entrance of Strangford Lough, 12-15 fathoms. Pecten mazimus, Linne. Common here as elsewhere, living in 7-25 fathoms. “Along the Antrim and Down coasts, where it is commonly called clam, and used as human food, though not so generally esteemed as the scallop ( P . opercular is) ” — Thompson. Xiima subauriculata, Montagu. Dead valves only, in from 4 to 90 fathoms on various parts of the Antrim and Down shores, by the Ordnance Survey collectors, Thompson, Hyndman, and Dickie. Xiima Xioscombii, G. B. Sowerby. “Dredged very sparingly, alive, in the deeper portions of Belfast and Strangford Loughs, on sandy and shelly ground. Single valves of large size obtained in quantity from 23 fathoms at the entrance to the former by Mr. Hyndman. Obtained occasionally in the stomach of haddock taken on the North-East coast ” —Thompson, whose L. fragilis also belongs to this species. Hyndman procured it frequently, both living and dead, in 15-90 iathoms ; Dickie took it alive outside Strangford Lough, in 12-15 fathoms. Xiima Ilians, Gmelin. ‘ ‘ The Ordnance Museum contains upon a card a fresh-looking specimen of this shell, as dredged from 7 fathoms in Belfast Bay” — Thompson (sub L. tenera). Hyndman’s only note of it is a repetition of this record. From a note in Jeffreys’ work, Waller would appear to have taken it some- where on the North-East coast, and the Belfast Museum Collection contains a specimen of Thompson’s labelled “ Belfast Lough.” It is very doubtful if this species can be now reckoned among our indi- genous mollusks ; but it lived in abundance in our waters at no very distant date, for the Estuarine Clay at Magheramorne, on Larne Lough, yields it in the greatest profusion, and it has been found in the similar deposit at Belfast. Pinna rudis, Linne. This fine species, our largest British shell, inhabits the waters off Black Head (25-30 fathoms), where it has been obtained by Hyndman (P. pectinata ) and others. Thompson mentions (sub P. ingens) a wider distribution ; he says of it, “the very few specimens, all taken in deep water, which I have seen from the coasts of Londonderry, Antrim, Down, and Louth, were of large 64 Praeger — The Marine Shells size, and all P. ingens or P. fragilis (Turt. Brit. Biv.),” and he gives Port- rush, Belfast Bay, and 50 fathoms off Island Magee, as localities where examples have been procured. It has been found at the first -mentioned station by Miss Richardson also. Probably the earliest record of this shell in our district is that in a letter from the Rev. Robert Innes, Rector of Magil- ligan, to Dr. Nicholson, Bishop of Derry, dated June 2nd, 1725, in which he describes a large example found in that neighbourhood. General Portlock, of the Geological Survey, writing in 1843*, and commenting on the above, says “ this coast continues a good locality for Pinna fragilis ; to obtain the fish in the valves they must be dredged up from deep water.” Mytiltas edulis, linne. Common on all our shores. Thompson gives some interesting notes as to the rapid growth and increase of this prolific species ; for instance, that on a buoy in Belfast Lougb, cleaned after being 5 years down, “the entire cir- cumference of the base, for a foot of space always under water, was covered a foot thick with full-grown mussels ” ; and that the bottom of the pilot- oa after its being 9 months afloat, yielded quantities of mussels 1^ inches ong. Mr. Incurvata. “ The only bivalve seen on Tory Island, where it is abun- dant, covering the rocks” — Thompson. pellucida. « Common in some parts of Belfast Bay ’’-Thompson (™» M. pellucid**). Cultra, S. A. Stewart-Belf. Mus. CoU. TVIvtilus modiolus, Linne. The “horse-mussel” is common, living in gravelly and muddy localities m 6-90 fathoms. Dickie found it very abundant in Strangford Lough (4-2» fathoms), coming up in quantity in almost every haul of. the dredge (sub Modiola modiolus). var. ovata. “ County Antrim (J .G. J .)”— Jeffreys. Tompson mentions it («» ** Belfast Lough -and Hyndman, under the same name, as living sparingly in “20fathol, while, he obtained dead valvesm i the Turbot^ Banked in 75 fathoms near the Maidens. Strangford Loug e ' . „ „ t d c r. found complete and fresh-looking specimens on the shores of Belfast and La. lingford Loughs. My L^gTSa^off BeMast Lough, and in 70-90 fathoms off Lame -Hyntoan (sub Modiola phamlim); and in 4-20 fathoms in Strangford Lough — Dickie. Tunicata, all round the coast, in depths up to 90 fathoms. Hyndman places it under genus Cremlla, and Thompson and Dickie under MMa. * Beport on the Geology of the County of Londonderry &c., p. 23. of the North of Ireland. 65 Modiolaria costulata, Risso. Found at Bundoran, Co. Donegal, by Mr. Waller— Jeffreys. Modiolaria discors, Linne. “Lame Longb, not nncommon. Donagbadee, 8 to 10 fathoms, Dr. Drum- mond”— Thompson (sub Modiola discrepans). “Living, rare, at the roots of Antennularia and other Zoophytes, in from 10 to 25 fathoms ” — Hyndman, who also obtained it, dead, on the Turbot Bank {sub Grenella discors). Craw- fordsbum, Mr. S. A. Stewart — Belf. Mus. Coll. Crenella rhombea, Berkeley . “Bundoran (Waller)” — Jeffreys (Supplement). Crenella decussata, Montagu. Living in gravelly sand, in 15 to 30 fathoms, off Donaghadee, Black Head, and Lame, and it was one of the few species which Hyndman obtained alive in Lame Lough (4-5 fathoms). Thompson’s only Irish note of the species states that Mr. Hyndman dredged a few odd valves in Strangford Lough ; Dickie took it alive in 18-20 fathoms at the entrance of the latter. Nucula nucleus, Linne. Abundant, living in 5-90 fathoms, in sand and gravel, throughout the North of Ireland. var. radlata, though stated by Thompson {sub N. margaritacea) to be common around the coast, has apparently a more limited distribution in our waters. Nucula nitlda, G. B. Sowerby. Living in mud and sand in from 12 to 20 fathoms, off Donaghadee and Black Head — Hyndman ; and frequent in 4-25 fathoms in Strangford Lough — Dickie. Hyndman also records it, with doubt, from 1-4 fathoms, Brown’s Bay, Island Magee. Dead shells occur on the Turbot Bank. Xfucula tenuis, Montagu. Hyndman records having dredged this species alive in deep water near the Maidens, and specimens labelled as from that locality are in the Belfast Museum. Xieda pygmaea, Munster. “ On the Antrim Coast” — Jeffreys (all said of it). Belfast Lough — Belf. Mus. Coll. It is rare as a British species, inhabiting chiefly the Scandinavian and arctic seas. leda xninuta, Muller. Portrush ; 23 fathoms in Belfast Bay ; and 50 fathoms off South Eock, Co. Down ; all by Mr. Hyndman— Thompson {sub Nucula minuta). In his sub- sequent systematic exploration, Hyndman obtained it occasionally, living in mud, gravel, and sand, in from 12 to 90 fathoms, and more frequently dead, in 1-90 fathoms ( sub L. caudata ). Dickie took it alive in Strangford Lough. Pentunculus glycymeris, Linne. Living in sand and gravel in 10-90 fathoms all round our coast ; and more 66 Praeger — The Marine Shells abundant in a dead state. Hyndman notes that it was dredged by his party in great quantity in 10 to 12 fathoms at Ballygalley, on the Antrim coast, all dead, hut valves united and quite fresh, and that their death was due, m Dr. Dickie’s opinion, to deposits from peat-hogs earned down by rivulets. Thrown up in abundance at Magilligan strand, hut only single valves. Shells of unusual size (2f X 2f inches) may he found at Orlock Point, Co. Down ; they have a rather ancient appearance, and are probably washed in from the Turbot Bank. Thompson cites this species sub F. pilosus. ^rca lactea, Xiwwe. Hyndman dredged dead specimens of this shell on the Turbot Bank (25-30 fathoms) on three occasions. Area tetragona, T <( Portrush in situ— Ordnance Collectors. Magilligan, odd valves W .l. Thompson. Hyndman obtained it dead on the Turbot Bank several times, and records a single living specimen which he dredged in 50 fathoms, embedded in a pebble of black limestone, off the Copeland Islands. Smgle valves fre- quent on the Derry coast— R.L1.P. [Area barbata, linne. ‘ ‘ * This very perfect and new shell on our coasts was found alive, adhering to an oyster from Killinchy in Strangford Lough, by Dr. M‘Gee of Belfast,’ Brown. Never found since ’’—Thompson. It is a common Mediterranean species, which is not admitted as native by any of our conchologists. There must have been some mistake.] X«epton nitidum, Turton. . Dredged alive by Waller on the Turbot Bank, and dead m the same vicimty by Waller and Hyndman— Hyndman, 1858 Report. IVIontacuta substriata, Montagu. This little shell, whose peculiar habitat is the ventral spines of Spatangus purpureas and other Echinoids, is noted by Thompson and Hyndman as living at the entrance of Belfast Lough, in 20 to 30 fathoms, and by Dickie off Strangford Lough, in 12 to 15 fathoms. IVIontacuta bidentata, Montagu. ^ “Bangor, Belfast Bay (one specimen), 1834, Mr. Hyndman and W.T. Bundoran, Mr. Warren ’’—Thompson. Hyndman, and Mr. Wm. Swanston dredged it dead on the Turbot Bank. Cushendall-Belf . Mus. Coll. These appear to he the only records of a species whose decline as a member of the marine fauna must have been rapid, as our pleistocene clays yield it in great profusion. Kontacuta ferruginosa, Montagu. Turbot Bank, dead— Hyndman. The M. ovata mentioned by Thompson is probably this species ; he states that several examples of it were found on the beach at Bundoran by Mrs. Hancock. of the North of Ireland. 67 Iiassea rubra, Montagu. Common between tide marks— Hyndman. Portrusb, and Belfast Bay — Thompson. (Both sub Kellia rubra). Magilligan— Belf. Mus. Coll. Kellia suborbicularis, Montagu. Bundoran— Thompson. Dead, rare, in 10 fathoms in Belfast Bay, and on the Turbot Bank -Hyndman. In Strangford Lough, and in the Irish Channel adjoining, Dickie found it living in 7 to 25 fathoms. Magilligan — Belf. Mus. Coll. Xioripes lacteus, Linne. Eecorded from the Turbot Bank, dead, by Hyndman, 1857 Deport ( sub Lucina leueoma). This record is not confirmed by Jeffreys, and as the species was not obtained again, and is entirely a southern form, it is doubtful if it should be included in our fauna. Xiucina spinifera, Montagu. “At Ded Bay, County Antrim, I found a valve of this species”— Thomp- son. Hyndman dredged it once alive “ on a bank called ‘ The Diggs,’ lying south of the Copelands, about a mile south of Donaghadee, and a mile from shore, in about 20 fathoms,” and several times dead, off Belfast Lough, in 15-30 fathoms. Xiucina borealis, Linne. Commonly dredged in a dead state, in Belfast and Larne Loughs and the deeper waters adjacent, in all depths from 1 to 30 fathoms. Thompson men- tions it {sub L. radula) as found at Ded Bay, and in 6 to 12 fathoms in Belfast and Strangford Loughs, by himself and Mr. Hyndman, but as the latter naturalist, in his subsequent report on the Mollmca of Belfast Bay (1857), notes it only in the column of dead shells, it may be assumed that such alone were found in the locality named. In Strangford Lough Dickie took it frequently alive, in depths ranging from 7 to 25 fathoms. Single valves are commonly thrown ashore on the Derry coast, where also the writer has foimd living specimens. Axinus flexuosus, Montagu. “ Widely distributed, but in sparing numbers ’’—Thompson. I find no note of its having been taken alive. Hyndman dredged dead specimens occasionally in 5-30 fathoms, and Dickie, in Strangford Lough, 4-25 fathoms. Thompson gives Strangford Lough and Bundoran as localities. (Mentioned by the authors quoted sub Lucina Jlexuosa). Cyamium minutum, Fabricius. Abundant, among sea-weeds and stones near low-water mark. Thomp- son states {sub Montacuta purpurea) that the shoals of mullet ( Mugil chelo) consume vast quantities of them when roving over the Zostera banks in spring and summer, and Hyndman (sub Turtonia minuta) estimates that in the stomach of a mullet taken in Larne Lough, there were 35,000 of these little shells, 68 Praeger — The Marine Shells Cardium echinatum, Linne. In the reports of Hyndman and Dickie, the only note of this fine shell having been taken alive is hy the former, who obtained a few living examples in Lame Longh, 4 to 5 fathoms ; while in a dead state it occurred in all the localities dredged, in 4 to 30 fathoms. Thompson says “ dredged from oozy sand in Belfast and Strangford Loughs” hy Hyndman and himself, hut does not state whether living or dead. Dredged alive in 6 fathoms off Bangor— Mr. S. A. Stewart. After northerly gales it is thrown ashore in some numbers on the Co. Down shore of the lough, from Holywood to Craigavad, with the animal quite fresh. Single valves of large size are abundant, and complete specimens frequent, on the sandy beaches of Magilligan and Portrush. Cardium exiguum, Gmelin. . Living in oozy ground in Lame Lough, and in the deeper waters adjoining, in 4 to 90 fathoms; the limit assigned hy Jeffreys is 15 fathoms, so the greater depth quoted would appear to be quite unusual. In and around Belfast Lough it has not been taken alive, and is rare in a dead state. It lives sparingly in Strangford Lough-Dickie, and R.L1.P. Thompson gives Red Bay as an additional station. (Sub G. pygmceum hy Hyndman and Dickie). Portrush, dead— Miss Richardson. Cardium fas datum, Montagu. Frequent, living on gravel and sand in 15 to 20 fathoms. Dead in Strang- ford Lough, on the Turbot Bank, and in up to 90 fathoms of water off Lame. In Thompson’s work it appears as sub C. elongaiwm and C. edulevax. fasciatum. Cardium nodosum, Turton. Belfast and Strangford Loughs— Thompson. Dredged living in 12 fathoms in the Sound between the Copeland Islands, and dead on the Turbot Bank, by Hyndman. More abundant in Strangford Lough and the channel adjoining than elsewhere ; Dickie dredged it frequently there, living in 7-20 fathoms. Cardium eduls, Linne. Gregarious everywhere in sandy hays, at and near low-water mark. Dea shells are dredged on the Turbot Bank, and Hyndman obtained a lirag example in 20 fathoms between the Maidens and the Isle of Muck. “ Attains a very large size in Donegal Bay ’’—Thompson. Cardium minimum, Philippi . Thompson made a new species, C. Loveni, out of specimens of this shell dredged hy Mr. Hyndman from 50 fathoms off the South Rock, Co. Down, and although they subsequently proved to he identical with a species already described and named, to him belongs the credit of having added this pretty shell to the British fauna. Hyndman subsequently records it ( sub C. Suecunm) from the Turbot Bank, and from shallower water (4-5 fathoms) m Lame Lough — in both instances dead. Cardium Tforvegicum, Spengler. “Dredged off Glenarm, in Belfast and Strangford Loughs, sparingly’ of the North of Ireland. 69 Thompson {sub C. favigatum ) ; it is not stated that any of the specimens obtained were alive. Hyndman took it alive only once, which was in 15 fathoms, on a bottom of mud and shells, 4 miles S.S.E. of Black Head, and Mr. Swanston has dredged living examples, of small size, at the entrance of the lough. Dead, it is abundant at various depths in many localities ; large single valves are frequently thrown up on the Co. Down shore of Belfast Lough. Xsocardia cor, Zinne. This large and handsome shell is extremely rare in the North of Ireland, and the authority for its admission to our marine fauna rests almost entirely with Thompson, whose notes of its occurrence I may give in full : — “ The follow- ing note appears in Mr. Templeton’s MS. journal, under October 28th, 1811 : * Beceived a drawing of the Chama cor , from Mr. George Joy, taken by him from a specimen dredged up at Bangor (Belfast Bay).’ The species is known to Mr. J. ft. Clealand to have been dredged near the Copeland Islands, at the entrance of this hay. The Giant’s Causeway is named by Turton as a locality in which it has been found ; hut very rarely. Glassdrummond, Co. Down, P. Doran.” The only other record of its occurrence which I have come across is in Dr. Dickie’s report, who notes it “very rare, dead,” upper part of Wellstream Bay, Strangford Lough, 4-8 fathoms. Jeffreys gives east and south of Ireland alone. Cyprlna Islandica, Zinne. Living throughout our waters, in sand and mud, in 1 -25 fathoms. Thrown up in great numbers on Magilligan strand during northerly gales. From Thompson’s notes it would appear to he much more abundant on the eastern than on the western shores of Ireland. Mr. "W. H. Patterson, M.B.I.A., contributes two curious local names for this species: the one is “yaghan” or “neayghen,” the other “ griggan.” Astarte sulcata, Da Costa. “Dredged off the Co. Antrim coast; in Belfast and Strangford Loughs sparingly, from about 8 to 25 fathoms, on mud and sand” — Thompson ( sub A. Zanmoniensis ). Living in from 10 to 27 fathoms, at the entrance to Belfast Lough, and more abundantly off Larne, in 15-90 fathoms — Hyndman ; and in 7-25 fathoms in Strangford Lough — Dickie. var. Scotica. Antrim coast ; Belfast and Strangford Loughs — Thompson {sub A. Scotica ). Living in 10-20 fathoms off Belfast Lough, and in 70-90 fathoms near the Maidens, and dead on the Turbot Bank — Hyndman. I have specimens dredged near Ardmillan, in Strangford Lough. var. elliptica. Belfast Lough — Belf. Mus. Coll. Astarte compressa, Montagu. Hyndman’s 1859 Report contains a note of a few valves of this species having been found in Turbot Bank sand by Mr. Jeffreys ; hut Jeffreys, in his “ British Conchology,” says, evidently referring to the same specimens, jq Praeger — The Marine Shells “subfossil in 25 fathoms off Lame, Co. Antrim.” As will appear subse- quently, this is by no means the only northern species which has been dredged, if not fossil, at least very doubtfully recent, in that locality. Astarte triangularis, Montagu. Belfast, and Strangford Loughs, dredged by Mr. Hyndman ompson ( sub Goodalia triangularis). Living on the Turbot Bank— Hyndman ; and in Strangford Lough and the channel adjacent— Dickie ; depth 7 to 30 fathoms, sandy ground. Dead valves are abundant on the Turbot Bank. Circe minima, Montagu. Thompson’s only northern locality is Belfast Bay, on the authority of Mr. Hyndman ( Cyprina minima ) . Hyndman obtained it alive twice, in 20 *ataoms> gravelly bottom, his stations being the Cod Bank north of the Isle o i uc , and “The Riggs” bank south of the Copeland Islands, while in a dead state it occurred frequently in depths ranging from 15 to 100 fathoms Dickie procured living examples off the mouth of Strangford Lough, 12-lo fathoms, and dead valves further out to sea. Venus exoleta, Zinne. Belfast, Strangford, and Lame Loughs— Thompson, who does not state the shell was alive in any instance. Though noted by Hyndman and Die e from almost every station (1-30 fathoms), in no case was it taken in a live state. Hyndman remarks (1857 Eeport) that at Cultra single valves are thrown up by the tide, and says, “ probably still living.” At the place in question, fresh-looking specimens with the valves attached are frequent, and I have twice picked up living examples there, and have no doubt that it lives in some quantity in the vicinity. This and the following species are placed under the genus Artemis by the authors quoted. Venus lincta, Fulteney. ^ Eare in a Eve state, the Cod Bank north of Isle of Muck (20 fathoms;, Wellstream Bay in Strangford Lough (15 fathoms), and 12-15 fathoms in t e open channel near the entrance of the latter, being the only stations I can find. More common dead, thrown up on sandy beaches, from Magilligan in Co. Derry to Newcastle in Co. Down. Venus fasciata, J)a Costa. . This beautiful species is of frequent occurrence throughout the district, living on gravelly and sandy ground ; it has been dredged alive off Lame and Belfast Lough, and in Strangford Lough and the open sea adjoining, m depths varying from 7 to 30 fathoms, by Thompson, Hyndman, Dickie, and others. Venus Casina, Zinne. _ Another handsome species, which inhabits our waters, ranging from . fathoms in Strangford Lough to 70 fathoms off the Maiden Light-houses, on gravel, sand, and mud. Dead valves are plentiful on the Turbot Bank and at various depths (6 to 90 fathoms), on the Antrim coast. 7 1 of the North of Ireland . [Venus verrucosa, Linne. “Mr. Hyndman’ s cabinet contains a young shell (V. cancellated) given him as from Magilligan ’ 5 — Thompson; much too slender evidence on which to establish a claim for its admission to our fauna. Its distribution in Ireland is confined to the south and west.] Venus ovata, Pennant. The dredgings of Hyndman and Dickie show that this pretty little shell is one of the most generally distributed of all our bivalve mollusks, as it occurred in almost every haul, generally alive, in from 4 to 90 fathoms. In Strangford Lough it lives in great abundance, and it is one of the very few species which Hyndman found living in Larne Lough. “A rather common species” — Thompson ( Cytherea ovata). Venus gallina, Linne. A common species. “Found alive from low- water mark to 8 and 10 fathoms on the North and North-East sandy coasts. Thrown ashore on the sandy beach of Magilligan in quantity and of large size ’’—Thompson. The V. Pennantii mentioned by this author belongs to the present species. Hynd- man and Dickie found that it lives in from 0 to 25 fathoms in all the waters explored ( sub V. striatula). The V. striolata in Dickie’s paper is apparently a misprint for V. striatula. Tapes aureus, Gmelin. Quoting from an older authority, Thompson says of this species “ ‘ Carriek- fergus Bay (Dr. M ‘Donnell) rare,’ Brown,” and under Turton’s name of Venus cenea , gives Strangford Lough as a locality where he has taken it alive. Hyndman states (1857 Beport) that it is common, living on sandy beaches between tide-marks, but it does not appear to be by any means of such fre- quent occurrence as would appear from this remark. Dickie dredged dead valves in Strangford Lough, and Hyndman on the Turbot Bank. Mr. Swans- ton informs me that it is abundant in Lough Swilly, in Co. Donegal, and Miss Bichardson has sent me complete and fresh specimens from Portrush. Tapes virg-ineus, Linnd. This handsome shell is of very common occurrence, in sandy and nullipore ground, in 4 to 90 fathoms all round our shores. var. Sarniensis. “ Yar. V. Sarniensis , Turt. Brit. Biv., is taken in Belfast Bay’ Thompson (sub Pullastra virginecd). “ Donaghadee, in 8 fathoms (Patterson) ’ ’—Forbes and Hanley. ‘ ‘ Living, rare, off Bangor ’ ’ —Hyndman. var. elongata. “ Larne, Co. Antrim (Hyndman)”— Jeffreys. Belfast Lough — Belf. Mus. Coll. Tapes pullastra, Montagu. Abundant, living between tide-marks. “A common species on sandy beaches ” — Thompson (sub Pullastra vulgaris). Dickie records it living in the unusual depth of 7-20 fathoms in Castle Ward Bay, Strangford Lough. Some valves from Belfast Lough are of unusual size — 2$ inches broad. 72 Praeger — The Marine Shells Jeffreys says the breadth of his largest specimen, found in Skye hy Edward Forbes, is 2i inches, and that 1*7 is the average breadth. var, perforans. Inhabits the forsaken burrows of Pholades , and chinks of rocks. Common — Thompson {sub Pullastra perforans). var. ofolong-a. “ Bundoran, Co. Donegal (J.G-.J.)” Jeffreys. Tapes decussatus, Linne. There is no certain record of this generally common species having been taken alive in our province. Thompson, refeiring to the whole of Ireland, says {sub Pullastra decussata ) “ a common species”, and in his “ Eeport on the Fauna of Ireland ” (1843), he has a cross opposite its name mthe “-North of Ireland” column, but he mentions no northerly locality. Jeffreys simply says “shores of Ireland”. Hyndman’s only note is to the effect that it occurs in the alluvial deposits, and is not now known to be living in Belfast Lough ; neither he nor Dickie found even dead valves in their dredgings. Miss Eichardson has found a specimen with the valves united, at Portrush, but the shell looks old and worn. I have taken it alive at Carlingford, and it is abundant on the coast of Co. Louth, but appears to stop short on the borders of Ulster. Xiucinopsis undata, Pennant. . „ . Dead valves occasionally dredged by Hyndman in 6-90 fathoms m Belfast Lough, and off Lame ; and Mr. Swanston has taken it off White Head with the valves still united. Thompson gives “Belfast Bay” (sub Artemis mtata). Miss Richardson has sent me a fresh and complete specimen from Portrush sands, evidently but recently dead. Like the preceding species, this would appear to he one of those shells which are dying out in the district, as, like 1 , while it is very rare in a live state, it is to be found in profusion an large size in the post-tertiary clays in our estuaries. Tellina crassa, Pennant. Hyndman dredged a single living specimen on the Cod Bank, 3 miles nort of Isle of Muck, 20 fathoms, gravelly bottom. In a dead state it has occurre in various localities, Strangford Lough included, in 10-30 fathoms— Thomp- son, Hyndman, and Dickie. Single valves are thrown up by the tide at Orlock Point, Co. Down, in some quantity— E.L1.P. Tellina BaltHica, Linne. Common between tide-marks on every shore. Sub T. sohdula by the writ quoted above. Tellina tenui*, Pa Costa. A common gregarious species, living in sand about low water mark. M plaice in Belfast Bay feed very much on T. tenuis ” -Thompson. ea valves of both this species aud the preceding dredged on the Turbot Bank, 25-30 fathoms, by Hyndman. Tellina fabula, Gronovius. . , “ Not uncommon on extensive sandy beaches, as Magilligan, W.T. 0 of the North of Ireland 73 from below low water mark to a few fathoms, on sand ” — Thompson. Dickie dredged it living outside Strangford Lough, in 7-15 fathoms: Hyndman records dead specimens only. Tellina squalida, Pulteney. Not a common species anywhere ; rare in our province, and in a dead state only. “Bed Bay, Co. Antrim, Mrs. J. Thomson Tennant ” — Thompson; specimens from this locality are in the Belfast Museum. Dredged by Hynd- man on the Turbot Bank ; in shallow water in Brown’s Bay, Island Magee ; and in 20 fathoms off Black Head ( sub T. incarnata). Tellina donaclna, Linne. Strangford Lough— Thompson ; whether living or dead not specified. Dead in Strangford Lough — Dickie ; and on the Turbot Bank — Hyndman. The latter obtained a single live specimen in 20 fathoms, gravel bottom, on the Cod Bank, north of Isle of Muck. Tellina pusilla, Philippi. “ Dead, valves united, from the Turbot Bank sand” — Hyndman, 1859 Report (sub T. pygmcea). Psammobia telllnella, Lamarck. Living in Belfast and Strangford Loughs, and the waters adjoining, in depths ranging from 7 to 30 fathoms — Thompson, Hyndman, and Dickie. Dead valves were dredged in Larne Lough and other places. Psammobia costulata, Turton. A single valve, found by Jeffreys in Turbot Bank sand which was forwarded to him by Hyndman, is the only trace of this species in our province. Psammobia Ferroensis, Chemnitz. “ Commonly thrown ashore on most sandy beaches. Inhabits below low- water mark ” — Thompson. Hyndman and Dickie never seem to have taken it alive, but in a dead state it occurred in most of their dredgings. Thrown up alive by the tide at Castlerock, Co. Derry, and Cultra, Co. Down — R.L1.P. Psammobia vespertina, Chemnitz. “From Lame Lough, Co. Antrim, a specimen has been sent me” — Thompson. This appears to be the only published note of its occurrence in the North of Ireland. I have before me over a dozen single valves, some of them quite fresh, which were picked up in about twenty minutes’ search on the beach at Cultra, Co. Down ; it evidently lives in some quantity at no great distance from that place. Bonax vittatus, Pa Costa. “ Generally common on extensive sandy beaches. Plentiful close to low water mark at Magilligan, where it is collected by the people for food. Dredged plentifully, but of small size, on pure sand, at a few fathoms’ depth, off Newcastle, Co. Down, Mr. Hyndman and W.T.” — Thompson (sub P. trunculus). The dredgings of Hyndman and Dickie, being generally in 74 Praeger — The Marine Shells deeper water, do not fairly show its distribution : indeed, this common species was only obtained once —in Brown’s Bay, Island Magee (D. anatinus). Portrush, Ballycastle, and a single valve at Ballyholme Bay— B.Ll.P. [Bonax denticulatus, Linne. “ A specimen said to be from Magilbgan is in Mr. Hyndman’s collection Thompson. This is a West Indian species, erroneously introduced into British lists.] Mactra solida, Linne. “ Not generally distributed; Magilligan, Bed Bay, and Lame”— Thomp- son. “A single valve dredged up off Castle Chichester, and odd valves off Bangor Hyndman. Dredged between Bangor and Donaghadee, 6-8 fathoms— Mr. S. A. Stewart (whether living or dead not stated). Portrush, dead, Miss Bichardson. Dead valves are abundant at Magilligan, and are not uncommon on the shore beyond Groomsport, Co. Down— B.Ll.P. var. truncata. “Found near low water mark in sand; brought to Belfast with cockles for sale, and together with Venus aurea, similarly obtained, com- monly called ‘Lady Cockle’; Bed Bay, W.T.”— Thompson. “Bangor Bay, Down (Patterson)”— Forbes and Hanley. “ Living on sandy shores between tide marks ” — Hyndman. Groomsport— Belf. Mus. Coll. var. elliptica. “Belfast and Strangford Loughs; specimens dead in both localities”— Thompson. Dredged frequently by Hyndman, living, in 12 to 30 fathoms ; dead shells common on the Turbot Bank. Dickie took it alive in Strangford Lough and the channel outside. (All sub M. elliptica). Mactra sutotruneata, Da Costa. “ Dredged from 10 to 12 fathoms, on sand, in Strangford Lough, Mr. Hynd- man and W.T.”— Thompson. “Living, few,” in Brown’s Bay, Island Magee, 4 fathoms and less— Hyndman. Groomsport— Belf. Mus. Coll. var. insequivalvis. “Lough Strangford (Adair)”— Jeffreys ; which is the only station assigned by that eminent conchologist to this variety. Mactra stultorum, Linne. Living on sandy beaches near low water mark ; rather local. Bed Bay, Co. Antrim, and Newcastle, Co. Down— Thompson. Being a littoral species, it did not occur in any of Hyndman’s or Dickie’s dredgings. Portrush, and abundant on the Derry coast, and frequently washed up alive on the Co. Down shore from Holywood to Donaghadee — B.Ll.P. var. cinereai Magilligan— Thompson. Under the various species and varieties of the above rather critical genus, x have simply placed the notes on them by the observers named, without com- ment, hut there seems to have been some confusion regarding M. solida var. truncata and M . subtruncata , at least. Contrary to what the notes above might lead one to expect, it is the latter that is by far the more abundant of the two in our district, living in profusion in Belfast Lough and elsewhere, and it is to 75 of the North of Ireland. it that I have always heard the name “ Lady Cockle ” applied. Beyond the records given, I do not know of M. solida var. truncata having been taken in the neighbourhood. £utraria elliptica, Lamarck. Burrowing deeply in sand and mud, at and below low water mark ; common. £ ‘ Like My a arenaria, plentiful in localities on all sides of the coast ’ ’ —Thompson ( sub L. vulgaris). Dredged occasionally (dead) by Hyndman, and alive in 12-15 fathoms by Dickie off Strangford Lough. Newcastle, Ballyholme, Cultra, Bedbay, Ballycastle and Portrush may he mentioned as localities, and on the Derry coast it is very abundant. Bev. Canon Grainger, D.D., informs me that the young shells of this species are called “ aprons” on Magilligan strand. Xiutraria oblonga, Chemnitz. “Magilligan, Mr. Hyndman ’’—Thompson {sub L. Mans). Scrobicularia prismatiea, Montagu. Magilligan, Belfast Bay, and from 50 fathoms off the South Bock, Co. Down — Thompson ( sub Amphidesma prismatiea). “ Living, rare, in 20 fathoms off Black Head”, and frequent in a dead state, 1-27 fathoms— Hyndman ; living both in and outside of Strangford Lough, in 7-20 fathoms — Dickie ( sub Syndosmya prismatiea) . Scrobicularia nifcida, Muller. Near Portaferry in Strangford Lough — Thompson {sub Amphidesma inter- media). Living, rare, in deep water off Belfast Lough, and in 4-5 fathoms in Larne Lough — Hyndman ( 'sub Syndosmya intermedia). Dickie dredged it alive in 15 fathoms in Strangford Lough, and also, in abundance, in 25-26 fathoms in the open channel, 6-7 miles from the bar, on a bottom of fine mud. Scrobicularia alba, Wood. Belfast and Strangford Loughs, sparingly, oozy sand, 8-10 fathoms — Thompson ( sub Amphidesma Boysii). Living in Belfast Lough, in 8 to 12 fathoms— Hyndman ; and in Strangford Lough, in 6 to 20 fathoms— Dickie {sub Syndosmya alba). In a dead state it has been dredged at all depths. Living, common, in 6-8 fathoms ofE Bangor— Mr. S. A. Stewart. var. curia. “ Lough Strangford (Waller) ; Larne, Co. Antrim (J.G.J.)”— Jeffreys. Scrobicularia tenuis, Montagu. “ I have received specimens of this well-marked species from Larne Lough, County of Antrim”— Thompson. Thompson’s specimens from this locality are in the Belfast Museum. It does not appear to have been found since. Scrobicularia piperata, Bellonius. “ This should not perhaps have been noted in the Belfast Bay column, as though not uncommon in a dead state, it has not been found alive to my knowledge ” — Thompson {sub Lutraria compressa) . 1 1 Has not been found living, 76 Praeger — The Marine Shells tut is probably to be found ’’-Hyndman. Like Tapes decmsatm, tbk species appears to stop short on the borders of our province, as it byes in Carlingford Lough (R.Ll.P.), and abounds further southward, while it has never been taken alive further north. Like T. decmsatm, too, it occurs in profusion in our Estuarine Clays, whence are probably derived the odd valves which are found in Belfast Lough and elsewhere. Solecurtus candidus, Renter. . . 1K Dead ; dredged by Hyndman on the Turbot Bank, and by Dickie in 12-15 fathoms outside Strangford Lough. Yery rare. Solecurtus antiquatus, Rulteney. “Bed Bay and Lame Lough, Co. Antrim- Strangford Lough, 8-10 fathoms, soft sand, W.T.”-Thompson (sub Solen antiquatus). Hyndman dredged it several times, in a dead state, off Black Head, m 15 to 30 fathoms. In Strangford Lough, Dickie obtained it in almost every haul of the dredge, hut never alive. (By Hyndman and Dickie sub S. coarctatus). Ceratisolen legumen, Lime. The following from Thompson ( sub Solen legumen) : — “ ‘Plentiful on the East coast from Cork to Belfast’, Brown’s Illust. p. 113, 2nd edit. This re- mark gives quite too extensive an idea of its distribution. Specimens from the extensive sandy coasts of Dublin and Louth only have come under my notice ; if the species be found so far North as Down, it must be only on the more southern part of it”. Newcastle, Co. Down— Belf. Mus. Coll. ; and Mr. Swanston has a fresh and complete specimen, and also a fresh sing e valve, which he found thrown up by the tide at this place. Solen pellucidus, Pennant. A rather common species, living in all our bays and in the deeper waters, on sand and mud, in depths varying from 3 to 25 fathoms. Thompson men- tions that plaice caught on the northeast coast have sometimes their stomachs filled with remains of this shell. Solen ensis, Linnd. Common in sandy bays throughout the province. Solen siliqua, Linne. “ Most common of the genus on our coast generally ’’—Thompson. Dead valves have been dredged in up to 90 fathoms, but the habitat of the species is in sandy bays between tide-marks, where it is abundant. As noted by Hyndman, very fine specimens are to be found at Ballyholme Bay, Co. Down. Solen vagina, Linne. (< < < A specimen has been given me as from Lame Lough ’ ’ Thompson. ' n the Irish coast it is local, inhabiting very extensive sandy beaches, as tiiose of Magilligan, and of the counties of Dublin and Cork (Thompson), xn eig * fathoms, Bangor, County Down, dead (Patterson)”— Forbes and Hanley. “ Dead, off Bangor, Co. Down” is Hyndman’ s only note of it (sub S. margt- natus), and Dickie’ s dredgings never yielded it. This species, which is so rare of the North of Ireland. 77 in our present waters, occurs throughout our later post-tertiary deposits, while S. siliqua, which is not found in. these beds, appears to have now taken its place, being abundant in suitable localities. Pandora insequivalvis, Linne. var. ohtusa. “Dredged off Carrickfergus, Mr. Hyndman; subsequently by Mr. Hyndman and myself in Strangford Lough” — Thompson. Taken aliye off Black Head and Donaghadee, in 15 to 20 fathoms, by Hyndman; and off the entrance of Strangford Lough, in 18-20 fathoms, by Dickie. (All sub P. obtusa). Dead on the Turbot Bank and elsewhere. lyonsia ITorveglca, Chemnitz. This curious shell is rare in the district. “ Dredged in Belfast and Strangford Loughs, in from 6 to 12 fathoms, among seaweed” — Thompson. Living in from 8 to 12 fathoms in Belfast Lough, and dead on the Turbot Bank — Hyndman. Dickie took it alive in 15 to 25 fathoms in Strangford Lough, and dead in shallower water. Off Crawf ordsburn, 6 to 7 fathoms, dead, but fresh and valves united — Mr. S. A. Stewart. Thracia prsetemiis, Pulteney. Thompson says of it ( sub Anatina prcetenuis) — “ ‘Belfast Lough, rare,’ Brown. The latter locality probably a mistake. Magilligan is the only northern locality in which the species has yet been met with by Mr. Hyndman or myself ; it is thrown ashore quite fresh there ”. Dredged by Hyndman in 15, 20 (valves united), and 27 fathoms off Belfast Lough, and in 20 fathoms off Larne, dead in each instance. “Coast of Down (Patterson)” — Forbes and Hanley. (All sub Cochlodesma prcetenue) . I have a valve found by my brother at Magilligan. Thracia papyracea, Poli. ‘"Belfast and Strangford ” — Thompson (sub T. declivis, Thor.). Dredged by Hyndman at various points around the entrance to Belfast Lough, in 20 to 30 fathoms, and by Dickie both in and outside of Strangford Lough, in 7-20 fathoms; in all instances dead ( sub T. phaseolina). Dead, in 6-8 fathoms, off Bangor and Donaghadee — Mr. S. A. Stewart. var. villosiuseula. Dead, in from 1 to 30 fathoms, off Belfast Lough and Island Magee — Hyndman (sub T. villosiuscula). Thracia pubescens, Pulteney. “ Belfast Bay ” — Thompson. On the Turbot Bank, rare, dead— Hyndman. “ The reputed Irish localities are doubtful”— Jeffreys. Thracia eomrexa, W. Wood. “Difficult to procure on account of its habit of burrowing rather deeply in muddy sand” — Jeffreys, which may perhaps account for its not having been taken alive in the province. “In Strangford Lough” — Thompson; speci- mens from thence are in Thompson’s collection in the Belfast Museum. “Hot known to be now living in the Bay ; two specimens have been dredged off Praeger — The Marine Shells Black Head, broken, but with ligament fresh, so that it is probably still living ” — Hyndman. Dickie took it three times in Strangford Lough, but dead in each case. Thracia dictorta, Montagu. “In limestone near Belfast, with Saxicava , Mr. Grainger” — Thompson. The only other note is a repetition by Hyndman of this record. Cortoula gibfoa, Olivi. « Strangford Lough is the best locality known to me for this species, m some parts of which it is common on muddy ground, at a depth of about from 4 to 10 fathoms” — Thompson {sub 0. striata). Living in 12-20 fathoms off Belfast Lough, and in 1-90 fathoms off Larne and the Maidens— Hyndman. The results of Dickie’s explorations in Strangford Lough amply confirm Thompson’s note, as this shell was found in abundance, alive, at every station, 4 to 25 fathoms. Living, common, 8-10 fathoms, Belfast Bay Mr. S. A. Stewart. ftZya arenaria, Linne. A common littoral species, living in abundance in muddy estuaries. 1 fiave seen specimens of unusual size (3x5 inches) dug on the Holy wood Bank for bait, and at Cultra have found small distorted individuals inhabiting the for- saken burrows of Pholades. Locally called “ cockabrillion ” or “ cockle- brillion.” Mya truncata, Linne. With the last, but frequenting more the open sea. aUbreviata was dredged by Hyndman and Jeffreys living in 80 fathoms off the Antrim coast, some 10 miles from land. Kya Bingliami, Turton. A Turbot Bank, living, rare— Hyndman ( sub Sphcenia Binghami). Occa- sionally met with in a dead state. Saxicava rugosa, Linne. Burrowing in limestone and old shells, or free. “ Common around the coast on the North and East ’’-Thompson. Living commonly in from 0 to 30 fathoms in the waters explored by Dickie and Hyndman ; the latter dredge living examples in 70-90 fathoms near the Maiden Bocks. mr. arctica. With the typical form, but not so abundant, and inhabiting rather deeper water (S. arctica). Venerupis Irus, Linne. In Thompson’s collection in the Belfast Museum, there are specimens ot this shell labelled “Bundoran, Co. Donegal” ; in the 4th volume of the “ Natural History of Ireland” there is no mention of its occurrence there. ?bolas dactylus, Linne. Burrowing in sandstone, marl, and hard clay, between high and low water mark, on both sides of Belfast Lough ; Carrickfergus, Greenland, and Cultra may be mentioned as localities where it may be taken alive, of the North of Ireland. 79 Fholas Candida, Linne. The most common of the genus in Belfast Lough, inhabiting the same situations as the last- Dickie dredged dead valves in 7-20 fathoms in Castle "Ward Bay, Strangford Lough. Pholas parva, Tennant. “ Was procured some years ago off the Long Strand, Belfast Bay, by Dr. J. L. Drummond ; subsequently by the Ordnance collectors at Whitehouse Point, in the same bay” — Thompson. Hyndman supplies the additional in'* formation that it was in submerged peat that it occurred in the former locality. Fholas crispata, Linne. “ Belfast Lough, Brown. Inhabiting indurated clay about low water mark, Belfast Bay” — Thompson. “Living in submerged peat at extreme low- water in Bangor Harbour, County Down, and in other places — Hyndman. Castle Chichester, in Triassic marl, but of very small size — Mr. Swanston. It flourishes on the shore at Cultra, near low water mark, in Boulder Clay, Hew Red Sandstone, and Carboniferous Shale ; at this place, from a piece of soft sandstone less than 6 inches square, the writer has taken P. dactylus , P. Candida , P. crispata , and Tapes pullastra var. perforans, all living. Pholadidea papyracea, Turton. “ Two specimens in the Ordnance Museum are labelled “ Portrush”, North of Ireland ” — Thompson ( sub Pholas papyracea ). “ Discovered in the dredg- ings of 1857, embedded in rolled lumps of hard clay, and again in the deep water this season ’ ’ (1858)— Hyndman. Off the Maiden Rocks, 70-90 fathoms, is the station where these specimens, which were living, were obtained. In his 1859 Report, Hyndman again records it “living at the depth of 80 fathoms north of the Maidens, in small pieces of soft sandstone. The smaller speci- mens want the cup-shaped appendage, whether the effect of insufficient space or immature growth.” Hyndman first recorded it as Pholas striata , but sub- sequently corrected it to the present species. “Sandstone at low-water, Castle Chichester near Belfast (Hyndman)”— Jeffreys ; whence it has been obtained subsequently. Low water mark being its usual habitat, it is probable that all the deep water specimens above should go under the following variety, which is essentially a deep water form. var. aborta. “In soft sandstone dredged in 80 f. off the coast of Antrim (J.G.J.)”— Jeffreys. [Teredo Worvegica, Spengler. “ Donaghadee (Co. Down), the animal alive ” —Thompson. “Not known as living in the Bay ” — Hyndman. Probably stray specimens only have been met with here.] 8o Praeger — The Marine Shells CLASS SOLENOCONCHIA. Dentalium entalis, Linne. “On most parts of the Irish coast”— Thompson. The curious ‘ tooth- shell” lives in some profusion on the Antrim and Down coasts, on sand and mud, in depths varying from 5 fathoms in Belfast Lough to 90 fathoms at the Maiden Bocks. CLASS GASTEROPODA. OEDEE CYCLOBEANCHIATA. Chiton fascicularis, Linne. “Generally distributed ’’-Thompson. Living in Strangford Lough- Dickie, and Mr. S. A. Stewart. W. gracilis. “Lough Strangford (Adair). A specimen from the ^last- mentioned locality measures nearly an inch and a half m length, wh „ largest that I have of the typical form (from Unst), is scarcely an inch long — Jeffreys. Chiton Hanleyi, Bean . . ,, “A fine living specimen on a shell, and one on a stone, in 80 fathoms - Hyndman, 1859 Beport. Chiton cancellatus (jMeht), G. B. Sowerby , Jun. « Among oysters from Killinchv, Down, Templeton MSS. Found by M. . Hyndman and myself in different localities on the North-East coast - ■ Thompson (sub 0. albus, Mont.). Belfast Lough-Belf. Mns. Coll. Lit- ing ; not uncommon in deep water” — Hyndman. Chiton cinereus, Linne. “On most parts of the Irish coast ’’-Thompson. Frequent, living m 15-70 fathoms-Hyndman; and commonly in Strangford Lough, 4-20 fathoms— Dickie {sub C. asellus). Carrickfergus— Mr. Swanston. Chiton albus , Linne. Q “North coast of Ireland”— Thompson. “ Strangford Lough — Mr. S. A. Stewart. Belfast Lough— Belf. Mus. Coll. of the North of Ireland . 8 1 Chiton margin at us, Pennant. Among oysters from Killinchy (Temp. MSS.), in the stomach of a haddock taken at Newcastle, Co. Down, and in other localities on the North-East coast — Thompson ( sub C. f uscatus, Brown). Though it is a common species generally, neither Hyndman nor Dickie has any note of it. Belfast Lough— Belf. Mus. Coll. Chiton ruber ( Linne ), Lowe. “ Among oysters from Killinchy, Down, Temp. MSS. Found hy Mr. Hyndman and myself in different localities on the North-East coast” — Thompson. Living in 15-25 fathoms north of Larne — Hyndman ; and in and about Strangford Lough in 7-20 fathoms— Dickie. Belfast Lough — Belf. Mus. Coll. Chiton Isevis ( Pennant ), Montagu. Living, very rare, in Castle Ward Bay, Strangford Lough, 7-20 fathoms — Dickie. Belfast Lough — Belf. Mus. Coll. Chiton marmoreus, Fabricius. ‘ 1 Obtained in Strangford Lough hy Mr. Hyndman and myself. On oysters brought to Belfast market from Carlingford, and Greencastle (Co. Londonderry), W. T.; Bangor, Co. Down, Mr. B. Patterson” — Thompson {sub C. Icevigatus). Strangford Lough — Mr. S. A. Stewart. OEDEE PECTINIBEANCHIATA. Patella vulgata, Linne. Between tide marks, on stones and rocks ; very common here, as elsewhere. Hyndman dredged dead shells in 27 fathoms on the Turbot Bank. He makes a curious statement about the limpet on the authority of Captain White, Harbour Master — that it is found to he good for eating and wholesome on the outer coast of Co. Down, but that in Strangford Lough it is found not to he wholesome, and is avoided hy the people there. There is an interesting paper in the “ Annals of Natural History” for June, 1839, hy the late Mr. Bobert Patterson, F.B.S., on the use of the limpet as food in the North of Ireland, which will well repay perusal. var. depress®,. “Living. Coast of Down, in Mr. Hyndman’ s cabinet” — Hyndman, 1859 Beport ( sub P. athletica). Bangor, Co. Down — Belf. Mus. Coll. Helcion pellucidum, Linne. Of general occurrence round our shores, on the broad fronds of Laminaria digitata, at and near low water mark. Dickie brought up living specimens from as deep as 15 fathoms in Wellstream Bay, Strangford Lough, and Hyndman dredged it dead on the Turbot Bank {Patella pellucida). 82 Praeger — The Marine Shells mr. lsevis. Equally distributed with the typical form, and not separated from it by the authors quoted above. Tectura testudinalis, Muller. On stones at and below low water mark. Newcastle and Bloody Bridge Thompson [sub Lottia testudinalis). Frequent on both sides of Belf ast Lough — Hyndman; and dead specimens were dredged in Strangford Lough by Dickie, and Mr. S. A. Stewart {Acmcea testudinalis). This shell was named by Sowerby Tatella Clealandi in honour of Mr. J . Bose Clealand, of Bathgael House, who procured the first British examples at Bangor, Co. Down ; but as a species it proved to have been previously described and named by Muller, from Danish specimens. On stones near the Twin Islands, Belfast Harbour, of large size — Mr. Swanston. Tectura virginea, Muller. “ Obtained on the shore of Belfast Bay by Mrs. M‘Gee, and found by Mr Hyndman adhering to oysters in Belfast Market in 1831 ’’-Thompson {sub Lottia virginea). Hyndman took it very frequently, living at the entrance to Belfast Lough, and off Larne, in from 10 to 25 fathoms ; and rom Dickie’s dredgings it would appear to live in abundance in Strangford Loug , in 4 to 25 fathoms {sub Acmcea virginea). Dead shells frequent on t e Turbot Bank. Tectura fulva, Muller. Turbot Bank, rare, dead; determined by Dr. Dickie— Hyndman, Beport {sub Filidium fulvum). 1858 Propilidiuzn ancycloides, Forbes. “ Obtained by Mr. Hyndman many years ago on oysters from Strangford Lough”— Thompson {sub Fatella ancycloides). In a dead state it is rather common on the Turbot Bank. The only locality on our shores where it has been certainly taken alive would appear to be the deep water near the Maiden Bocks, where Hyndman procured living specimens several times, in between 70 and 100 fathoms of water! Jeffreys says “on the Antrim Coast m 18-1 fathoms (Hyndman and others),” which looks as if some other observer had taken it at a less depth. Puncturella OToacliina, Linne. “ Mouth of Belfast Bay, 27 fathoms, one dead specimen dredged by Mr. Hyndman ’’—Thompson ; his only Irish note of the species. Hyndman subsequently obtained it on several occasions on the Turbot Bank (the same locality), always dead. Jeffreys says of it-“ Co. Antrim (Hyndman, Waller, and J.G.J.). The specimens, however, from the last-mentioned locality are probably relics of the glacial epoch, and not recent.” It is a species essentially of northern origin, whose most southern station is bear- borough in Yorkshire, while northward it ranges as far as Spitzbergen and North Greenland. of the North of Ireland . 83 Emarginula fissura, Linne. Common off the South Antrim coast, living in depths varying from 5 fathoms in Belfast Lough to 90 fathoms near the Maiden Rocks — Hyndman ; it was not taken alive in Strangford Lough, but was common in a dead state — Dickie ( sub F. reticulata). Thrown up by the tide on sandy beaches at Castlerock and Magilligan, Co. Derry, and Newcastle, Co. Down — R.L1.P. var. elata. Jeffreys records this variety, which is larger, more solid, and much higher than the typical form, as taken by him at “ Larne near Belfast.” Emarglnula rosea, Bell. Hyndman states that this shell was dredged, in a dead state, by Mr. Waller on the Turbot Bank. It is entirely a southern form, inhabiting, as a British species, the Channel Islands and South of England coasts, and its occurrence here as a native would he, to say the least of it, highly improbable. Emarg-inula crassa, J. Sowerby. Very rare, living in 60 fathoms off the Copeland Islands ; dead in shallower water in the same vicinity, and on the Turbot Bank, and in 70-100 fathoms near the Maidens— Hyndman. Dredged alive off the Maidens— Mr. Swanston. It is a species of great beauty and rarity, inhabiting rocky ground in deep water, where it is almost inaccessible to the dredge. Fissurella CS-raeca, Linne. “On all the Irish coasts” — Thompson. Living sparingly in 10 to 25 fathoms at various points of the Antrim and Down coasts — Hyndman, and Dickie ( sub F. reticulata). Portrush — Miss Richardson. Magilligan and Castlerock, Co. Derry, dead — R.L1.P. Capulus Hungarlcus, Linne. “Generally distributed” — Thompson ( C . TTngaricus). Not uncommon, living on stones and oyster shells in 10 to 20 fathoms, off Belfast Lough and Larne. In a dead state it has been dredged by Dickie in Strangford Lough, and by Hyndman in the deepest water off the Maidens (100 fathoms). Rather worn shells are thrown ashore by the tide at Magilligan and New- castle— R.L1.P. Hyndman and Dickie mention it under Lamarck’s generic name of Eileopsis. Locally called “ fool’s cap.” [Haliotis tuberculata, Linne. “ ‘ Dredged near Groomsport, Co. Down, Oct. 1811,’ Templeton, MSS.”— Thompson. The two specimens affirmed to have been there obtained are preserved in the Belfast Museum, on a card which bears the following manuscript note by Mr. Robert Templeton : — “ These are the two haliotes which rank this shell as a native of Ireland. They were got by the late John Templeton, Esq., I believe on the Co. Down shore— R. T.” Jeffreys dis- misses this and other records with very little ceremony— “the Irish localities must have been from hearsay, and are manifestly wrong.” It would appear probable that the Groomsport specimens were actually obtained there, for 8+ Praegev — The Marine Shells Mr. Templeton’s care and accuracy are well known, but they must have been derived from some passing vessel or other extraneous source; this beautiful species inhabits nowhere north of the Channel Islands.] Scissurella crispata, Fleming. A northern species, frequenting, in Britain, chiefly the Orkney and Shetland Islands. “ Mouth of Belfast Bay, 27 fathoms, 2 dead specimens dr-edged by Mr. Hyndman ’’-Thompson. In Hyndman’s Reports, additional specimens are mentioned as having been obtained on the Turbot Bank, and a single fresh shell was taken in 80 fathoms some 6 miles north of the Maidens. Cyclostrema nitens, Philippi. _ Found by Jeffreys in Turbot Bank sand sent to him— Hyndman, 18o8 Report (as Trochus (Margarita) pusillus). Cyclostrema serpuloides, Montagu. In Turbot Bank sand, as last {sub Skenea divisa ) ; and in his 1859 Report Hyndman records having dredged living examples off Larne. [Margarita costulata, Moller. Found by Mr. Waller in Turbot Bank sand— Hyndman. It is an arctic species, whose southern limit is Iceland. Dead specimens have been dredged in several Scotch localities also, which, with those from the Turbot Bank, must be looked on as relics of the great ice age.] Trochus helieinus, Fabricius. “Living, common, on Laminaria digitata, $e.” Hyndman. Assuming that Margarita communis, Mont. = M. vulgaris , Leach, Thompson mentions the loughs of Belfast, Larne, and Strangford as localities. Hyndman dredged dead specimens on the Turbot Bank. var. fasciata. “ Found by Mr. Hyndman in the North of Ireland ~ Jeffreys. Trochus aroenlandicus, Chemnitz. Dredged in a dead state by Hyndman on the Turbot Bank {sub T. {Marga- rita) undulatus). The specimens were determined by Jeffreys, who, how- ever, remarks that they look suspiciously like fossils from a submarine post- tertiary deposit in the locality. It is an arctic species, which descends as far southward as the north of Scotland. [Trochus cinereus, Couthouy. “ Has been dredged by Mr. Waller on the Antrim Coast ; but it is a sub- marine fossil” — Jeffreys. Hyndman also records it, as Margarita cinereal) Trochus magus, Linne. Not uncommon on the coasts of Derry, Antrim, and Down, living chiefly in about 5 to 10 fathoms. Trochus tumidus, Montagu. Belfast and Strangford Loughs, and Donaghadee— Thompson. Hyndman dredged it very frequently, living in depths ranging from 10 to 100 fathoms, of the North of Ireland. 85 and from Dickie’s lists it would appear to live in profusion in Strangford Lough. Trochus cinerareus, Linne. One of our most common species, living on stones and sea-weed between tide-marks and in depths up to 25 fathoms, throughout the province. Hyndman dredged a single living specimen in the great depth of 70-90 fathoms off the Maidens. It is locally called “ silver- shell,” on account of the pearly lustre of the inner layers. The T. littoralis, Brown, for which Thompson, quoting from an older writer, mentions Killough as a station, belongs to the present species, and, according to Jeffreys, can scarcely he considered a variety. Trochus umhilicatus, Montagu. Between tide-marks, among stones and Fuel ; common. Trochus Suminyi, Requien. Our rarest shell, Bundoran in Donegal Bay being its only British habitat. It appears to be of rather rare occurrence there, where it was first discovered some years ago by Edward Waller, an assiduous and distinguished Ulster conchologist. Trochus lineatus, Fa Costa. “This littoral species, found on rocks, stones, &c., is unknown to me further north on the Eastern line of coast than Ballywalter, Co. Down (54^° lat.). Southward it is common ” — Thompson (sub Monodonta crassa). On the western side of the province it flourishes at Bundoran, in just the same latitude — Waller, Jeffreys, and others. Trochus Montacutl, W. Wood. Sparingly hut widely distributed on the Antrim and Down shores. Hynd- man dredged it alive off Ballygalley Head, Waller off Groomsport, and Dickie in Strangford Lough and the open channel adjoining — depths ranging from 12 to 25 fathoms ; in a dead state it occurred frequently, especially on the Turbot Bank (sub T. Montagui). A very elegant scalariform monstrosity was dredged off Larne, as noted by Hyndman and Jeffreys. Trochus striatus, Linne. “Dead, in Turbot Bank sand, Mr. Jeffreys ’’—Hyndman, 1859 Report; specimens from that locality are in the Belfast Museum Collection. In his “British Conchology,” the most northern station which Jeffreys gives is Dublin Bay. It is a southern species, and frequents the Channel Islands and south coasts of England and Ireland. [Trochus exasperatus, Pennant. “Turbot Bank, Dr. Dickie, doubtful”— Hyndman, 1857 Report (sub T. exiguus ). This is the only note of the occurrence of the present species. J effreys regards as doubtful all localities other than those on the South of England coasts and Channel Islands.] 36 Praeger — The Marine Shells Trochus millegranus, Philippi. Of not uncommon occurrence, living in depths varying from 10 fathoms in Belfast Lough to 100 fathoms at the Maiden Rocks ; Dickie includes it in his lists of Strangford Lough shells. Thompson says — “ It inhabits the deeper portions of Belfast and Strangford Loughs, chiefly from 10 to 23 fathoms, in sand ooze, &c. Bundoran, Mrs. Hancock. T. Clelandi, Wood, is considered another variety. It was sent to the Author from Strangford Lough by James Rose Clealand, Esq.” Dredged at Glenarm, Mr. S. A. Stewart. Trochus granulatus, Porn. This handsome shell, the largest British Trochus, is of extreme rarity in our province. “ Two broken specimens dredged up at separate times in Belfast Bay ; hut as there are only two other examples known of its being found so far from its usual southern habitat, these have been no doubt introduced accidentally Hyndman, 1857 Report. “ Fragments in 25 fathoms, 2 miles off Black Head ” — Ibid., 1858 Report. It has been dredged off the Mull of Galloway, and at Sanda Island, opposite the Antrim coast, so its occurence on our shores is not improbable. I find the following marginal note in Mr. Wm. Swanston’s copy of Thompson’s work, opposite the name (T. papillosus, Brown) of this species: “One living and one dead, S.E. of Maidens, 72 fathoms, 11th Sept., 1882— W. S.” The specimens are in Mr. Swanston’s cabinet, and are fine and characteristic examples. Trochus zizyphinus, Linne. A pretty and well-known species, which is distributed throughout our waters, and has been taken alive at all depths. It flourishes most in from about 5 to 25 fathoms. var. X.yonsii. “ The pure white variety has been dredged of all sizes, hut very sparingly, in Belfast Lough by Mr. Hyndman and myself ; on one occasion we found numbers of this variety on the beach at Ardmillan (Strangford Lough), whence they were brought adherent to “wrack ” {Pud) cut for manure about some of the islands”— Thompson. Hyndman took it living in from 20 to 90 fathoms off Larne, and Dickie in Strangford Lough. var. data. “ Deep water on the coast of Antrim (J. G. J.) ” — Jeffreys. Phasianella pulla, Linne. “Littoral in some localities; dredged in from about 6 to 10 fathoms in Belfast Bay, common ’’—Thompson. Living, frequent, near low water mark— Hyndman ; it was dredged by him alive in as deep as 20 fathoms on the Cod Bank off Larne. In a dead state it is abundant in the shell sand of the Turbot Bank, and Dickie records it from Strangford Lough. Xiacuna crassior, Montagu. Frequent, ranging from low water mark to the deepest water at the Maidens. Thompson and Dickie took it in Strangford Lough. Saeima divaricata, Fabricius. A common speeies. “The var. L. vincta is not uncommon ; L. canalis is of the North of Ireland . 87 more so ” — Thompson {sub X. quadrifasciata) . “ Common on laminaria ” — Hyndman (sw£ X. vincta). Abundant in Turbot Bank sand, in a dead state. Xiacuna puteolus, Turton. Apparently rare. Dredged by Hyndman, in a dead state, on the Turbot Bank, and near Ballygalley Head. Strangford Lough — Mr. S. A. Stewart. Bundoran — Belf. Mus. Coll. var. conica. “ Co. Antrim (Hyndman)” — Jeffreys. Xiacuna pallidula, Da Costa. “ Inhabits the laminarian region in Belfast and Strangford Loughs, and chiefly found on the broad fronds of Laminaria digitata ; also on oysters ; occurs hut sparingly ; procured in some quantity at Ballycastle by the Bey. Thomas Hincks ” — Thompson. “Living, common, on Laminaria ” — Hyndman. Magilligan — Belf . Mus. Coll. Xiittorina obtusata, Linne. Abundant on stones and Fuci on all beaches. Hyndman dredged dead shells on the Turbot Bank (X. littoralis). “ Common around the shores” — Thompson (X. Neritoides , Forbes). var. neritiformis. “Captain Brown has given Downpatrick as an Irish locality ” — J effreys . var. fabalis. “ I have found it plentifully at Larne in the North of Ireland. I believe it represents the young males of the ordinary form ” — Jeffreys. Xiittorina neritoides, Linne. On rocks and stones above high water mark; common. Bundoran — Thompson (X. petrcea, Mont.). Xiittorina rudis, Maton. Plentiful on stony beaches everywhere. var. saxatilis. “ North of Ireland ” — Thompson (X. saxatilis). var. jug-osa. “Is common on all quarters of the rocky coasts ’’—Thompson (L. jug os a). var. patula. “ Living, common, on rocky ground a little below high water mark” — Hyndman (X. patula). Is this correct? Jeffreys gives only three stations in Britain — Eddystone, Penzance, and Unst. var. tenebrosa. “Although met with on all sides of the coast, it is local” — Thompson (X. tenebrosa). It is an estuarine form, and occurs on our Zostera hanks. Larne Lough — Hyndman. Fair Head — Belf. Mus. Coll. Xiittorina litorea, Linne. In the greatest abundance on stones and mud hanks. “Abundant round the shores of the Island” — Thompson (X. communis , Turt. Br.). var. turrita. Belfast Lough, Mr. S. A. Stewart — Belf. Mus. Coll. Genus Rissoa, Freminville. Of this large genus of tiny shells, out of the 25 species which Jeffreys in- 88 Praeger — The Marine Shells eludes in the British catalogue, 20 are recorded as occurring in our province. The Rissoa, and that other large genus of small univalves, the Odostomice, will serve as good examples of the richness in the smaller univalves of that inte- resting area of sand and gravel which is known as the Turhot Bank. Thus, of the 20 species of Rissoa found in the district, 18, or all but 2, occur m t e shell-sand from this vicinity, about half of these being inhabitants, of the littoral and laminarian regions, while the other half frequent the coralline and deep-sea zones. As regards Odostomia, to he mentioned presently, we have 24 species, out of 34 British, of which no less than 21 occur in the Turbot Bank sand, and 10 of these have not been obtained elsewhere in our waters. As suggested by Mr. Hyndman, the home of the majority of this large num- ber of species, whose deserted habitations bestrew the Turbot Bank, is pro- bably the profound rocky depths near the Maidens, where they may live, out of reach of the trawl and dredge. Note.— Except where otherwise stated, the shells referred to m the notes on species of Rissoa, were dead. Rissoa striatula, Montagu. Bundoran— Thompson. Frequent on the Turhot Bank— Hyndman. Rissoa cancellata, Fa Costa. . Of frequent occurrence on the Turbot Bauk-Hyndman. Dredged m Strangford Lough, and the open channel adjoining-Diekie. (Both sub It. crenulata). Rissoa calathrus, Forbes $ Manley. Turbot Bank, rare— Hyndman. Rissoa reticulata, Montagu. Common on the Turbot Bank— Thompson, and Hyndman. Common, 7-20 fathoms, Castle Ward Bay, Strangford Lough— Dickie. (All sub R. Beanu). In shell-sand dredged near Ardmillan in the latter lough— R.L1.P. Rissoa cimieoides, Forbes. « Lame, Co. Antrim (J.G.J.) ’’-Jeffreys. The Turbot Bank is probably the locality intended. Specimens in the Belfast Museum Collection are labelled as from Lame. Rissoa punetura, Montagu. Bundoran— Thompson. Common on the Turbot Bank— Hyndman. Rissoa Zetlandiea, Montagu. On the Turbot Bank-Hyndman. Specimens from thence are m the Belfast Museum Collection. Rissoa costata, Adams. ^ a Bundoran— Thompson. On the Turbot Bank, and in about 20 fathoms off Ballygalley Head— Hyndman. Strangford Lough— Dickie, and R.L1.P. Rissoa parva, Fa Costa. “A very common species around the coast” Thompson. It lives in of the North of Ireland. 89 profusion on Zostera and Algos, at low water mark and a few fathoms depth. Dead on the Turbot Bank and elsewhere. var. interrupta, Common around the coast — Thompson (R. interrupta). Rlssoa ineonspicua, Alder. “ One specimen at Bundoran, Mrs. Hancock ” — Thompson. Frequent on the Turbot Bank — Hyndman. Rissoa albella, Loven. Turbot Bank; from Hyndman’s collection — Belf. Mus. Coll. I find no note of it in Hyndman’s Reports. If the determination of the species he correct, the specimens probably belong to the variety Sarsii, which is abun- dant along the west coast of Scotland ; the typical form is confined to Bantry Bay, according to Jeffreys. Rissoa membranacea, Adams. “ Bundoran, Warren. On muddy hanks, within and below low water, it is common and fine in Belfast Bay” — Thompson, who remarks that he is informed that this species lives on the leaves of the “ sleech-grass ” ( Zostera marina), and never, like other Rissoce, on Fuci. A common species, living on Zostera hanks throughout the district. Dead on the Turbot Bank, and in deep water in and outside of Strangford Lough — Hyndman, and Dickie. (R. labiosa by all). Rissoa violacea, Desmarets. Bangor, Belfast Bay — Thompson. “ Living, scarce, on sea-weed between tide-marks” — Hyndman. Dead, common, Castle Ward Bay, Strangford Lough — Dickie. (All sub R. rufilabrum ) . It is one of the two North of Ireland Rissoce. which alone are not recorded from the Turbot Bank. Rissoa striata, Adams. This tiny shell swarms around our shores, on sea- weeds, stones, and mud, between tide-marks. Common also, in a dead state, in up to 30 fathoms of water on the Antrim and Down coasts. Rissoa proxima, Alder. “Magilligan (W.T.) ; Bundoran (Mrs. Hancock) ” — Thompson. Turbot Bank, very rare — Hyndman. It is a rare and critical species, and as it has a southern distribution, and Dublin is the most northern station given by Jeffreys, it is possible that Thompson’s localities belong to the following species. 3£issoa vitrea, Montagu. Turbot Bank, extremely rare — Hyndman. Siissoa fulglda, Adams. “ I have found it sparingly at Larne Lough, near Belfast ” — Jeffreys. Rissoa soluta, Philippi . In Turbot Bank sand, very rare — Hyndman. Specimens from thence are in the Belfast Museum Collection. 90 Praeger — The Marine Shells SUs*oa semistrlata .Montagu. . , „ Matnllifran * ■ X. semistriata has come under my inspection m shell- sand from Ma„illigan and Bundoran ’’—Thompson. On the Turhot Bank, rare Hyndman. pura. Observed in Turbot Bank sand by Mr. Jeff reys-Hyndman (suS var. alba). R1S On" aTsa!sUof "“art ’’-Thompson (*. einyilla) ‘^rnng com- mon, under stones near low water mark ’’-Hyndman. Dead shells in the deeper water. _ m , ,, var. rupestris. “North-East coast, Mr. Hyndman and W. T., not rare —Thompson. Turhot Ban k, rare— Hyndman. [Rissoa Bryerea, Montagu. TTwnrlman ” — 1 “ Among shell-sand from Magilligan, one procured by Mr Hyndman Thompson This is Eimina Bryerea , a West Indian species, stray examples of Inch have been occasionally found at different places in the British Isles.] ...... r. .«■ on the rocks n.r the ttient’e Ceusewey. It * JStt.,,. 4 * Indian shell, and has no claim to he considered British.] HydSmiT'^ "Tzfstem banks and muddy sands in all our hays and estuaries, , f™, Je marks Dead on the Turhot Bank-Hyndman (Xusoa ukce). 5“ “Sehief food of the grey mullet. In winter various sea- birds feed on it. Sar“!lng!”wSughtfrom Tory Island, off the north val bv Mr Hyndman, in 1845, this species was found -Thompson (su Bundoran, Co. Donegal (J.G.J.) ’’-Jeffreys. Specimens from the latter station are in the Belfast Museum. Bundoran by Mrs. Hancoch, in 1840 ”- Thompson ( sub Rissoa albella, Alder) . “ ZlZ^era and Alyoe between tide-mark, Abu. var. tro^hiformis. Larne Lough-Jeffreys. This is the eonvex-spired variety mentioned by Hyndman in his 1859 Eeport. HOmSr=I^-shores of Larne Lough ’’-Hyndman («. jsJJSL »). “ Donegal in Ireland (Warren) ’’-Forbes and 9i of the North of Ireland ’ Hanley [Skenea nitidissima) . Belfast Lough — Belf. Mus. Coll. Has probably been passed over on account of its very minute size ; it would seem to be a common species generally. Homalog-yra rota, Forbes $ Hanley. Tbis rare species has been taken in Donegal by Mr. Warren and Mr. Barlee Forbes & Hanley ( sub Skenea ? rota). It is the smallest known species of British shells, having a length, according to Jeffreys, of only 0*0115 inch, and is rare. Caecum trachea, Montagu. TurDot Bank ; from Hyndman’ s collection — Belf. Mus. Coll. “ Strangford (Waller) ” — Jeffreys (supplement). Caecum g-labrum, Montagu. “ Shell- sand, deep water, Belfast Bay, Mr. Hyndman ’’—Thompson {sub Brochus lavis). Bare, in shell-sand from the Turbot Bank— Hyndman. These refer to the same station, and are the only notes of the occurrence in our district of the species, which J effreys says is common and universal ; its insignificant size may account for this. [Brochus reticulatus of Brown is the young of his B. annulatus , which is an exotic shell. It is said to have been found in Strangford Lough.]. Turritella terebra, Linne. Very common, living in 7 to 25 fathoms throughout our waters. Thompson says Mr. Hyndman observed it living between tide-marks in Carlingford Lough. In Lough Foyle the dead shells of this species constitute a large part of the great shell-banks for which the place ha^long been noted. [Truucafella truncatula, Braparnaud. 11 A specimen agreeing with Montagu’s description of Turbo sub tr uncat a, but not very well with his figure, was found among shell -sand collected at Bundoran by Mrs. Hancock”— Thompson {sub T. Montagui). “ I fear there has been some mistake as to the specimen from this place ’’—Jeffreys. Its British distribution only extends to the south coast of England and the Channel Islands, and its foreign range is entirely southern.] Scalaria Turtouse, Turton. “At Newcastle, Co. Down, this shell has been met with by Dr. Drum- mond ’ ’ —Thompson. This station is given also by Forbes and Hanley, and Jeffreys, on Thompson’s authority. Strangford Lough— Mr. S. A. Stewart. As a pleistocene fossil it is of common occurrence in the Estuarine Clays at Belfast; perhaps the specimens labelled “Belfast Lough” in the Museum Collection were thus derived. Scalaria communis, Lamarck. “Although not yet (so far as I am informed) taken in the Loughs of Strangford or Beliast, it has been procured in the adjacent Lough of Larne ; Bundoran, Mrs. Hancock ’’—Thompson ( sub S. clathrus). Turbot Bank, dead, rare —Hyndman. Magilligan — Belf. Mus, Coll, 92 Praeger — The Marine Shells Scalaria Trevelyana, Leach. “Mr. Hyndman possesses a specimen from Magilligan Thompson, specimen from thence, out of Mr. Thompson’s collection, is in the Belfast Museum. It does not appear to have been taken elsewhere in the province. Scalaria clatbratula, Adams. “ Bundoran, Mrs. Hancock ’’-Thompson ; specimens from thence are in the Belfast Museum. Hyndman dredged dead shells on several occasions, in the vicinity of the Turbot Bank. TAcirsa borealis, Beck. ... “ Dead, in Turbot Bank sand, Mr. Waller, 1857. Described by him m the “Transactions of the Royal Dublin Society,” and provisionally named Turritella Sibernica ’’—Hyndman {sub Scalaria Eschnchti). “ Dredged m 18-20 f. off the coast of Antrim, by Mr. Hyndman, Mr. Waller, and myself. This species has not been found living south of Iceland ’’—Jeffreys.] Aclis unica, Montagu. ir „ n >» “ Bundoran, Mrs. Hancock. Deep water, Belfast Bay, Mr. Hyndman -Thompson ( Chemnitna unica). Turbot Bank, dead, very rare-Hyndman. It is a littoral species. Aclis ascaris, Turton. “Bundoran (Mrs. Hancock, fide Thompson) ’’—Jeffreys. Aclis supranitida, S. Wood. “ It has been collected at Bundoran by Chemnitzia glabra). Hyndman dredged vicinity of the Turbot «ank. Mrs . Hancock ’ ’ —Thompson {sub dead shells occasionally in the Aclis G-ulsonse, Clark. . In Turbot Bank sand, determined by Mr. J effreys— Hyndman ( Jeffreysia Gulsonce). Specimens from the Turbot Bank are in the Belfast Museum. Var. tenuicula. “Lough Strangford (Waller) ’’-Jeffreys. Genus Odostomia, Fleming. This, the largest and perhaps the most complicated genus of British shells, has by no means been worked out in our district. With the assistance of that eminent conchologist, Mr. Jeffreys, Hyndman was enabled to publish very full lists of the Odostomia of the Turbot Bank, and of the 34 British species, no less than 21 are recorded from this vicinity, all in a dead state ; but beyond this, there is a paucity of information concerning them. Then- minute shells are easily overlooked, and it is only with the aid of the micro- scope that the exquisite sculpture which characterises many of the species, may be seen with advantage. In the absence of records of any of the following species having been taken alive, I have omitted noting “dead after each station. Odostomia nivosa, Montagu. u Turbot Bank sand Mr. Jeffreys ’’—Hyndman {sub 0. cylindrica). of the North of Ireland. 93 Odostomia truneatula, Jeffreys. A single specimen found among Turbot Bank sand by Mr. Jeffreys ; and later it was dredged in 25 fatboms off Black Head — Hyndman ; specimens from tbence are in the Belfast Museum. It is a very rare species, and its other British stations are all on the South of England coasts. Odostomia Ssiikisi, Jeffreys. “Bundoran, Co. Donegal, in drift shell sand (Waller) ” — Jeffreys. Odostomia rissoides, Hanley. Found by Jeffreys in Turbot Bank sand— Hyndman. Bundoran— Belf. Mus. Coll. It is a littoral species, and is distributed throughout the British coasts. var. alba. Turbot Bank, Mr. Waller— Hyndman ( sub 0. alba). var. nitida. Found by Jeffreys in Turbot Bank sand— Hyndman ( sub 0. nitida). var. diabia. As last (sub 0. dubia). Odostomia pallida, Montagu. “ A very few individuals of this species have been dredged in Belfast Bay, and taken in the stomach of the grey mullet captured there ; under stones between tide marks. Strangford Lough, on soft sand and ooze” — Thomp- son. Dredged in the vicinity of the Turbot Bank on several occasions — Hyndman ( sub 0. eulimoides). In shell sand dredged near Ardmillan in Strangford Lough— R.L1.P. It is one of the commoner Odostornice, and lives on the ears of Pecten opercularis and P. maximus, in the coralline zone ; the littoral habitat assigned above by Thompson for the species, casts some doubt on the correctness of his determination. Odostomia acuta, Jeffreys. From the Turbot Bank ; determined by Mr. Alder — Hyndman. Odostomia eonspieua, Alder. As last ; like it, it is an inhabitant of the coralline zone (15-50 fathoms). Odostomia uuidentata, Montagu. “ More frequent in the shell sand that has come under my notice than any other species of Odostomia'''’ — Thompson; he mentions Strangford Lough as a locality. Hyndman took it several times on the Turbot Bank, and Dickie off the entrance to Strangford Lough. Twin Islands in Belfast Harbour — Mr. Swanston. Odostomia turrit a, Hanley. Turbot Bank, Mr. Waller— Hyndman [sub 0. unidentata var. turrita). Odostomia plicata, Montagu. “It has been found in Belfast Bay and Strangford Lough by Mr. Hyndman and myself; at Bundoran by Mrs. Hancock” — Thompson. Bare, off Bangor, and on the Turbot Bank— Hyndman. Jeffreys gives no northern stations for the present species, and says that 0. .turrita has been often mistaken for it. Praeger — The Marine Shells Odostomia insculpta, Montagu. Observed by Jeffreys in Turbot Bank sand which was sent to him for examination — Hyndm an . Odostomia otoliqua, Alder. “ Two specimens obtained from shell sand collected at Bundoran by Mrs. Hancock ” — Thompson. Odostomia Warreni, Thompson. “ A specimen from Bundoran, Mrs. Hancock ’’—Thompson (sub Tissoa Warrenii). Turbot Bank, Mr. Waller— Hyndman. In the body of Jeffreys’ “British Conchology” it appears as 0. obliqua var. Warreni, but in the Supplement to that work it is restored to the rank of a species. It was first described by Mr. Thompson in the “ Annals of Natural History,” from specimens found at Portmarnock by Mr. T. W. Warren, an assiduous Irish conchologist, in whose honour Mr. Thompson named it as above. Odostomia decussata, Montagu. This beautiful little shell has been found in Turbot Bank sand by Mr. Jeffreys. Specimens labelled “Co. Antrim” are in the Belfast Museum Collection. Odostomia indistincta, Montagu. Bundoran, Mrs. Hancock— Thompson. On the Turbot Bank on several occasions- Hyndman. In Strangford Lough and the channel adjoining, very rare — Dickie. (All sub Chemnitzia indistincta). Odostomia interstincta, Montagu. It would appear to be of common occurrence in the Turbot bank shell sand (Chemnitzia interstincta), but is not noted elsewhere. A widely distributed and common species generally. Odostomia spiralis, Montagu. “ Very sparingly, in shell sand collected at Magilligan hy Miss Moody Thompson. Common on the Turbot Bank— Hyndman. Entrance to Strang- ford Lough, 12-15 fathoms, very rare— Dickie. Odostomia excavata, Philippi. “Bundoran, Mr. Warren ” —Thompson (sub Eissoa Marveyi). Turbot Bank, Mr. Waller— Hyndman. Mr. Thompson named it It. Sarveyi in honour of Dr. W. H. Harvey, who discovered the first British examples, in Co. Clare ; Dr. Harvey had previously named it Cingula sculpta. Both these proved to be subsequent to Philippi’s name of U. excavata. Odostomia scalaris, Philippi. Found in Turhot Bank sand hy Mr. Jeffreys -Hyndman (Chemnitzia scalaris ). Dickie records it from Strangford Lough, but from a remark in Jeffreys’ work, it would appear that it was the following variety which he obtained there. var. rufescens. Bare, off Groomsport (Waller) ; and dredged on the Turbot of the North of Ireland. 95 Bank— Hyndman {sub Chemnitzia rufescens). “ Lough Strangford (Dickie) ” — Jeffreys. Odostomia rufa, Philippi. var. fulvoclncta. Turbot Bank, rare ; determined by Mr. Alder — Hyndman {Chemnitzia fulvocincta). Bundoran— Belf. Mus. Coll. The Chemnitzia rufa of Hyndman’ s 1858 Report, in Jeffreys’ list of Turbot Bank shells, in all probability belongs to the variety ; the typical form is exclusively southern, while the variety has a northern distribution. Odostomia lactea, Linne. Not uncommon— Thompson. Dredged frequently around the Turbot Bank by Hyndman, and in Strangford Lough and the. open channel adjacent by Dickie (all sub Chemnitzia eleg antissima) . Twin Islands in Belfast Harbour— Mr. Swanston. Bundoran — Belf. Mus. Coll. It is a common but beautiful species, inhabiting the laminarian zone. Odostomia Scillee, Scacchi. Both Waller and Hyndman dredged this shell on the Turbot Bank ( Euli - mella Scillce). Jeffreys, referring to this station, says “ perhaps from a post- glacial deposit.” Specimens from the Turbot Bank are in the Belfast Museum, and look quite as recent as the majority of the shells from that vicinity. Odostomia acicula, Philippi. Found in Turbot Bank sand by Mr. Jeffreys — Hyndman (sub Eulimella acicula). The collection in the Belfast Museum contains specimens from that locality. var. ventrieosa. Turbot Bank, Mr. Waller — Hyndman {subPulimella affinis). var. olbeliscus. “ Dredged by Mr. Waller on the north-east coast of Ireland ” — Jeffreys. Possibly this and the previous note refer to the same specimens. Odostomia nitidissima, Montagu. 11 Specimens from Bundoran have come under my inspection ” — Thompson {Chemnitzia nitidissima). Xanthina rotundata, Leach. This beautiful oceanic species, popularly known as the “blue snail,” is occasionally wafted to our shores by the western winds, during the autumn months. Thompson mentions having obtained a few shells, still containing the animal, on the beach at Groomsport in Co. Down, in the year 1836 {sub I. communis ), but it is very rarely that it is found so far south in the channel. On the north coast of Antrim, and on the coast of Derry, it is of more fre- quent occurrence, and is occasionally washed in in quantity. I am informed that after October gales the strand at Bush-foot is sometimes thickly strewn with it. Portrush, occasionally — Miss Richardson, and R.L1.P. Eulima polita, Linne. About the entrance of Belfast Bay (Ordnance Survey Collectors and Mr. Hyndman), and in Strangford Lough (Mr. Hyndman and W. T.), bottom 9 6 Praeger—The Marine Shells pure sand in each case -Thompson. Hyndman records dead shells only, which appear to he of frequent occurrence in the neighbourhood of t e Turbot Bant. Dickie dredged a few living examples off the entrance to Strangford Lough, in 12-15 fathoms, and dead specimens inside the loug . Off Bangor, in 8 fathoms, living— Mr. Swanston. Uulima disforta, Deshayes. Bundoran, Mrs. Hancock-Thompson. Dead shells are not unfrequent on the Turbot Bank, according to Hyndman. mr. graeills. Dredged by Hyndman on the Turbot Bank, and by Dickie in 12-15 fathoms outside Strangford Lough. rsulima suoulata, Donovan. Stated by Thompson to have been obtained at Bundoran, Co. Donegal, and Dundrum, Co. Down, but there is no doubt that E. bihneata is the species intended.] Sulima Mlineata, Alder. “ Dredged from a sandy bottom, 8-10 fathoms, off Dundrum, Co. Down, Mr. Hyndman and W.T. ; a specimen at Bundoran, Mr. Warren -Tbomp- son (sub E. subulate). Dead shells are common on the Turbot Bank Hyn • man. Living, very rare, in 7-20 fathoms, in Strangford Lough, and dead m the channel adjoining —Dickie. Watica Islandica, Ginelin. Dead; a single young specimen by Mr. Jeffreys "-Hyndman 1859 Report (sub N. helicoides). The locality is not given, but was probably the Turbot Bank. This specimen may have been a quaternary fossil. It is northern species, which in Britain is taken chiefly on the northeast coaste, though it has been found at Cork. It is widely distributed m post-glacial beds. [M, Groenlandica, BecTc. . . , ^ ,, , A shell from the Turbot Bank is in Thompson’s collection m the Belfast Museum. Any specimens occurring there are not recent, hut relics o t e glacial epoch; Jeffreys records it also as dredged on ‘he Turbot Bauk and enters it as a fossil. Its present habitat in Britain is limited to rather deep water off the northeast coasts of England and Scotland.] ^^Stongford Lough and the channel adjoining are the only localities ^ m which this species has been obtained in the North of Ireland. eie ic ie dredged it on several occasions, but only in a dead state, m depths varying from 10 to 25 fathoms; specimens from the same locality are m Thompson s collection in the Belfast Museum. Watica catena, Da Costa. -Fc+hrms One of our commoner shells, living chiefly in sandy bays at a few fathoms depth. “ Living, common, 6-8 fathoms, from Bangor to Donaghauee -Mr. S A.' Stewart. Thrown up alive, and of large size, on MagilUgan Stran , of the North of Ireland. 97 Co. Deny — E. LI. P. Dead shells were dredged in some abundance around Belfast and Strangford Loughs by ILyndman and Dickie, in from 15 to 30 fathoms (JV. moniliferci) . OTatica Alders, Forbes. This very pretty shell is common, living at nearly all depths (4 to 90 fathoms) throughout the waters dredged by ILyndman and Dickie (/V. nitida), and thrown up on sandy beaches throughout the province. OTatiea Montaeuti, Forbes. Thompson records a living specimen dredged in Belfast Bay. Hyndman took it alive off Larne, at different depths up to 90 fathoms, and dredged dead shells in abundance around the entrance to Belfast Lough, in 15 to SO fathoms ( sub N. Montagui). It did not occur in any of Dickie’s dredgings. [Katica clausa, Broderip $ Sowerby. Dredged by Hyndman and Jeffreys on the Turbot Bank. It is a glacial fossil, and now inhabits the circumpolar seas alone.J AdeorMs subearinatus, Montagu. Dredged up from the Turbot Bank by Hyndman, in a dead state, on several occasions ; it is a southern shell, and has not been found elsewhere in our district. Ziamellaria perspieua, Linne. “ Generally distributed ” — Thompson (Sigaretus perspicuus) . Bare, living- on Laminaria, and dredged alive in the unusual depth of 80 fathoms north of the Maidens, and dead in 15-25 fathoms off Ballygalley Head — Hyndman. Very rare, dead, in 15-25 fathoms off the entrance to Strangford Lough — Dickie. Sigaretus tentaculatus, recorded by Thompson as dredged by Mr. Hyndman and himself in Strangford Lough, is the male of the present species ; the typical form is the female. Velutina Isevig-ata, Fennant. A species of frequent occurrence, living on hard ground at all depths. Hyndman took it alive in 12 to 20 fathoms off Belfast Lough, and in 70-90 fathoms near the Maidens ; and in a dead state on the Turbot Bank. Dead, rare, in 6 to 8 fathoms, off Bangor — Mr. S. A. Stewart. It did not occur in Dickie’s dredgings, probably owing to the muddy nature of the bottom in Strangford Lough. Thrown up by the tide at Newcastle, Portrush, and Magilligan — B . LI. P. var. Candida. Jeffreys found this white variety on the coast of Antrim. Tricbotropsis borealis, Broderip $ Sowerby. In Hyndman’s Beports for 1857 and 1858, this species is noted as occur- ring in a dead state in almost every haul of the dredge made around the entrance to Belfast Lough, and on the Turbot Bank especially ; in the 1859 Beport he records having obtained it alive in the latter place. Dead shells also occurred to him in the deepest water at the Maidens. Dickie dredged a 98 praeger—lhe Marine Shells single dead specimen in 12-15 fathoms off the entrance to Strangford Lough. Aporrbais pes-pelecani, Linne. A well-known and common species, locally called “leg-of-mutton she . It lives in about 10 to 25 fathoms, hut is sometimes taken at both less and greater depths. [Cerithium metula, Lov&n. __ In dredged sand from the Turbot Bank— Hyndman, l8o9 Report. Erroneously recorded from the same vicinity in the 1857 Report ; Cerithiopsis pulchella was the species intended. It is a northern form, and its only British station is the Shetland fishing-hanks, where it fives in 45-96 fathoms (Jeffreys) ; the Turbot Bank specimens are manifestly fossil.] Cerithium retieulatum, Da Costa. Very common, living between tide -marks and to a few fathoms depth, everywhere. In a dead state it is common on the Turbot Bank. Cerithium perversum, Linne. “In shell sand, mouth of Belfast Bay, Mr. Hyndman ’’-Thompson (sub Triphoris adversus). Not uncommon in Turbot Bank sand— Hyndman ; very rare, in 12-15 fathoms, off the entrance to Strangford Lough— Dickie (sub C. adversum) ; in all instances dead. Specimens labelled “Bundoran” are in the Belfast Museum Collection. ORDER SIPHONOBRANCHIATA. Cerithiopsis tubereularis, Montagu. “Sandy beach at Magilfigan ; and in stomach of Scaup duck shot in Belfast Bay ’’—Thompson (sub Cerithium tuberculare). Hyndman several times dredged dead shells on the Turbot Bank. Ceritliiopsis pulchella, Jeffreys. Found by Mr. Waller in Turbot Bank sand— Hyndman. It is a rare species. [Ceritliiopsis costulata, Moller. Another of the Turbot Bank fossils ; it was dredged there by Waller and Hyndman (sub STcenea costulata and Cerithium niveum) and specimens from thence are in the Belfast Museum. It inhabits the northern seas, and Shet- land appears to be its most southern station.] Purpura lapillus, Linne. Very common, on rocks and stones, between tide-marks. Locally caned “ white wilk,” or “ dog wilk.” Dead shells occur on the Turbot Bank. Buccinum undatum, Linne. The eommon whelk, or ‘ 1 buckie, as it is locally called, is abundant of the North of Ireland. 99 on all kinds of ground and at all depths, from half-tide down to 100 fathoms, the limit of the British fauna. var. littoralis. Carrickfergus — Belf. Mus. Coll. It is probably common. var. striata. Living in 60 fathoms about 6 miles from the Maidens — Hynd- man. [Buccimim cyaneum, “ fragment only, considered by Mr. Jeffreys to he this species, in Turbot Bank sand, Mr. Waller” — Hyndman, 1858 Report. I have failed to trace this species to a modern synonym ; it is probably some glacial fossil.] IVXurex erinaceus, Linne. Of general occurrence ” — Thompson ( Triton erinaceus). Jeffreys, after giving a list of British stations, remarks “all the specimens procured from the northern coasts were dead and this remark applies to our province, for, though it is of frequent occurrence on the shore, and in depths up to 30 fathoms, I find no note of its having been taken alive.* Troplion murieatus, Montagu. Hyndman dredged it alive on the Cod Bank off Larne (20 fathoms), and also in 25 fathoms off Black Head, hut very sparingly ; and took it rather commonly in a dead state off Donaghadee, and on the Turbot Bank, and in 70-100 fathoms near the Maidens. From Dickie’s Report, dead shells appear to he distributed throughout Strangford Lough and the channel adjacent. J effreys queries these and other northern records, and considers that they are probably referable to T. Barvicensis. The present species has its head- quarters in Lusitanian and Mediterranean waters, and does not range north of Britain. Troplion Barvicensis, Johnston. Hyndman obtained it living with the last in the two stations mentioned, and dead in 8-10 fathoms in Belfast Lough, and on the Turbot Bank. Dickie dredged a few dead specimens in 12-15 fathoms outside Strangford Lough. This is a northern form, ranging to the arctic seas, and not found south of Britain. Troplion truncatus, Strom. “On all parts of the Irish coast ” — Thompson ( sub Fusus Bamffius). Liv- ing in from 6 to 25 fathoms around Belfast Lough, and in much deeper water (70-90 fathoms) off the Maidens, and common in a dead state in from 12 to 100 fathoms — Hyndman. Very rare, dead, in Strangford Lough and the channel adjoining— Dickie. (Both sub T. clathratus.) [Fusus scalariformis, recorded by Hyndman as found in Turbot Bank sand by Mr. Jeffreys, is Troplion clathratus , a characteristic fossil of all glacial and post-glacial beds.] [Fusus decussatus of Brown (Illust. Conch. G. B.) is said to have been discovered by him at Killough, Co. Down. The figures and description are * Since above went to press, the writer has dredged it alive in 3 fathoms off Roekport Belfast Lough. ICO Praeger — The Marine Shells not sufficient for identification. Jeffreys suggests that it may fiave been a plain-coloured variety of Trophon Syracusanus, which is a rather common Mediterranean shell.] Fusus antiquus, Linne. Living commonly around the coast, ranging in depth from between tide- marks in Belfast Lough to 100 fathoms at the Maiden Bocks. Called “ buckie ” along with Buccinum undatum. Specimens of great size from Car- rickfergus are in the Belfast Museum Collection. A curious convoluted mon- strosity is mentioned by Hyndman as dredged off Groomsport by Mr. Samue Yance. var. alba. Carrickfergus— Belf. Mus. Coll. Fusus gracilis, J)a Costa. Frequent, but not so generally distributed as the last. Hyndman (hedged it alive in 60 to 90 fathoms off the Maidens (F. Islandicus). Jeffreys gives its range as 20 to 145 fathoms, but it frequents less depths in our district, as it has been dredged living in abundance in 6-8 fathoms off Bangor by Mr. S A. Stewart, and is sometimes thrown ashore in quantity, with the animal quite fresh, between Holywood and Craigavad, where the greatest depth of water in the vicinity does not exceed 4 or 5 fathoms, and the writer has noticed it living between tide-marks at Cultra. It did not occur to Dickie in Strangford Lough, nor have I observed it on the Derry coast. It is F. corneus of Thompson’s work. Iffassa reticulata, Linne. , . Would appear to be somewhat local. Occasionally found living about Bel- fast Lough in 10 to 20 fathoms; dead on the Turbot Bank-Hyndman. Living between tide-marks at Cultra-E.Ll.P. Not recorded from Strang- ford Lough. I have dead shells from Portrush and Magilligan. 18-assa incrassata, Strom. Abundant throughout the province, living m from 7 to 90 fathoms. A. macula of Thompson’s work. Tffassa pygmeea, Laniard. ■ . Yery rare In Hyndman’s 1858 Eeport it is noted as having been taken alive by Mr. Waller on the Turbot Bank ; in the previous Eeport it had been recorded with doubt from the same vicinity, by Dr. Dickie, but only in a dead state. It is a common shell in our Estuarine Clays, where X. mcmsmia is unknown. rX3"assa hepatica, Montagu. Becordecl from Strangford Lough, on the authority of Turton and Brown ( Monoceros hepaticus). It is a West Indian shell.] tC0A“ratHn*0ytdman’s Beports for 1857 and 1858 {sub Mangelia Eolbolii and Buccinum Eolbolii) as dredged on the Turbot Bank. It is an inhabitan of the arctic seas, and occurs in Britain only as a glacial fossil.] IOI of the North of Ireland. Bsfrancia teres, Forbes. Fragments of this shell were dredged by Hyndman on the Turbot Bank. Befraneia Iieufroyi, Michaud. Dead, but very fresh, in Turbot Bank sand, and a single broken example in 40 fathoms off the Copelands— Hyndman ( Mangelia Leufroyi). Befrancia linearis, Montagu. “ Generally distributed ” — Thompson (Fleur otoma linearis). Frequent on the Turbot Bank — Hyndman ; rare in Strangford Lough and the channel adjoining— Dickie ; in all instances dead {sub Mangelia linearis). Befrancia reticulata, Fenier. “ A single dead specimen of this rare and beautiful shell was found by Mr. Jeffreys in dredging from the deep water north of the Maidens. Hew to the Insh list. It is a southern form ’’—Hyndman, 1859 Beport {sub Mangelia reticulata). As Mangelia scabra , it is recorded in Hyndman’s 1858 Beport as found by Mr. Jeffreys in Turbot Bank sand. Befrancia purpurea, Montagu. “ Of general occurrence ’’—Thompson ( Vleurotoma purpurea). “ Bare, in shell sand”— Hyndman {Mangelia purpurea). Very rare, in 12-25 fathoms off the entrance to Strangford Lough— Dickie. Bangor— Belf. Mus. Coll. Shell sand on beach at Cultra — B.L1.P. Pleurotoma striolata, {Scacchi) Fhilippi. Turbot Bank sand— Hyndman {Mangelia striolata). Pleurotoma attenuata, Montagu. “General, but not abundant ’’—Thompson. “Dead, Turbot Bank sand, Mr. Waller ’’—Hyndman {Mangelia attenuata). Very rare, dead, in 18-20 fathoms 4 to 5 miles from Strangford Bar— Dickie. Bundoran— Belf. Mus Coll. Pleurotoma costata, Donovan . Dead, rare, in 10 fathoms, and not unfrequent on the Turbot Bank— Hyndman {Mangelia costata). Dickie dredged dead shells off the entrance to Strangford Lough, 12-15 fathoms. The variety coarctata, mentioned by Hyndman as obtained near the Turbot Bank, is merely the northern and larger form of the species, Pleurotoiaa brachystoma, Fhilippi. “ Co. Antrim (Waller) ” — Jeffreys ; this is all the information we possess about the occurrence of this shell in the district. Pleurotoma aetoula, Montagu. Dead, rare, in shell sand dredged on the Turbot Bank— Hyndman {Mangelia nebula) . Pleurotoma septangularis, Montagu. “Generally distributed”— Thompson. Living, rare, in 10 fathoms in Belfast Lough, and dead on the Turbot Bank— Hyndman ; and Dickie found a few living examples in Castle Ward Bay, Strangford Lough, 7-20 fathoms (both sub Mangelia septangularis). Bangor — Belf. Mus. Coll. Praegev — -The Marine Shells t 62 Pleurotoma rufa, Montagu. Living, rare, off Groomsport (Waller), and dead on the Turbot Bank- Hyndman ( Mangelia rufa). Dead shells in Strangford Lough— Thompson, Dickie, and R.L1.P.; and in the channel outside— Dickie. var. lactea. “ A small form of this pretty variety, mostly having the upper part of the spire tinged with purplish-brown, was procured by Mr. H} nd- man from Port Ballantrae, Co. Antrim ’’—Jeffreys. var. Ulideana. “Bound the Irish coasts, hut rare ’’-Thompson (sub P. TJlideana) . Pleurotoma turricula, Montagu. _ TJ1 , “Of general occurrence”— Thompson. Living in 2o fathoms off blac Head ; dead, rare, on the Turbot Bank, and off Bally galley Head, and fre- quent’in 5-6 fathoms in Belfast Lough -Hyndman. Dead, rare, m Strang- ford Lough— Dickie (Mangelia turricula). Bangor— Belf. Mus. Co . Crawfordsburn, dead— Mr. Swanston. Cultra, dead— R.L1.P. [Pleurotoma Trevelyana, Turton. mini Dredged in 25 and 27 fathoms in the neighbourhood of the Turbot Bank Hyndman ( Mangelia Trevelliana). Jeffreys considers that the specimens there obtained were glacial fossils. The species is entirely northern.] Marg-inella laevis, Donovan. “MagilUgan, Co. Londonderry, G. C. Hyndman "-Thompson (sub Rato lewis). Cypreea Europsea, Montagu. Generally diffused throughout our waters, living m from about 0 to 20 fathoms. In a dead state it is thrown up on most sandy beaches, and was dredged in up to 100 fathoms depth near the Maidens. The pretty and well- known shells of this, the only British cowry, are locally called “ Johnnjg grots,” which is a corruption of the Scotch name of “ John-o - Groat s buckie.” Bulla diaphana, recorded by Thompson as taken in Strang or Lough, is the young of the present species before the outer Up is formed. TCyprsea moneta. “Specimens of this shell have been frequently found on the shore near Bangor Co. Down. Although not indigenous, its occurrence may be worm noticing, as there is a tradition that a ship engaged in the slave trade was wrecked there, and thus the cowries are accounted for” Hyndman. the money-cowry of South Africa.] Ovula, patula, Pennant. , “ A shell of this species, found some years ago on the sandy beach of Magilligan, County of Londonderry, by Mrs. B. A. Hyndman of Dublin is in the cabinet of Mr. Hyndman, at Belfast "-Thompson. A smgle dead specimen dredged by Mr. Waller on the Turbot Bank-Hyndman These are the only notes of the occurrence of this curious shell m the North of 1 land. The Magilligan specimen is in the Belfast Museum. of the North of Ireland. 103 ORDER PL EUROBR ANCHIATA . Cylichna acuminata, Bruguiere. Mr. Waller obtained a single dead shell of this species on the Turbot Bank, and Hyndman another. These are recorded in Hyndman’s Beports, under , the name Ovula acuminata. Cylichna umbilicata, Montagu. Very rare ; dead shells in Turbot Bank sand — Hyndman. Cylichna eylmdraeea, Pennant. ‘ ‘ Generally distributed” — Thompson {sub Bulla cylindracea). Dredged, in a dead state, on the Turbot Bank, and off Ballygalley Head, by Hyndman, and in Castle Ward Bay, Strangford Lough, by Dickie. Bundoran— Belf . Mus. Coll. [Cylichna striata ( Bulla striata , Brown). “ The late Mr. Thompson of Belfast erroneously noticed this arctic species as found at Bangor, Co. Down, by Mr. Hyndman. It inhabits the eastern coasts of North America, Greenland, and Finmark” — Jeffreys.] Utriculus mammillatus, Philippi. Turbot Bank, dead, Mr. Waller — Hyndman ( Cylichna mammillata), Utriculus truncations, Bruguiere. u Generally distributed ” — Thompson ( Bulla truncata ). Hyndman occa- sionally dredged dead shells on the Turbot Bank ( Cylichna truncata ;), but does not record haying taken it elsewhere. Magilligan— Belf. Mus. Coll. Twin Islands in Belfast Harbour — Mr. Swanston. Utriculus obtusus, Montagu. Generally distributed ” — Thompson ( Bulla obtusa ). Hyndman notes it (sub Cylichna obtusa ) from the Turbot Bank several times, and from off Bally- galley Head, in a dead state. Dead shells dredged in Strangford Lough — Dickie, and E.L1.P. It frequents muddy estuaries chiefly. var. liLaj onkaireaaa. “ From the Turbot Bank, dead; determined by Mr. Jeffreys, in Mr. Hyndman’s cabinet”— Hyndman, 1859 Eeport {sub Cylichna lajonkaireana ) . Utriculus hyaliuus, Turton. “Obtained in shell sand collected at Bundoran by Mrs. Hancock” — Thompson ( sub Bulla hyalina). “Dead, in 80 fathoms, off the Maidens” — Hyndman {sub Amphisphyra hyalina). Acera bullata, Muller. Generally distributed — Thompson ( sub Bulla Altera). It abounds on the Zostera banks of Strangford, Belfast, and Larne Loughs, and in Lough Foyle. Hyndman says he has sometimes seen it swimming in the channel leading to the Quays at Belfast, giving out a purple liquid when touched. 104 Praeger — The Marine Shells var. nana. “ Occurs in Lame Lough” — Jeffreys. ilctseon tornatilis, Linne. Generally distributed — Thompson. Dead, rare, off Bangor, and on the Turbot Bank— Hyndman. Dead, rare, in Castle Ward Bay, Strangford Lough— Dickie. (Sub Tornatella fasciata by all.) Groomsport— Mr. Swanston. Dead, rare, 8-10 fathoms, Belfast Bay— Mr. S. A. Stewart. Port Stewart— Miss Bichar dson. Frequent on the Derry coast, thrown up by the tide, from the Bann to Magilligan Point— B.L1.P. It is a most elegant shell. Bev. Canon Grainger informs me that at Magilligan it is locally known as “beer-barrel.” Bulla, utrieulus, JBroechi. “ Living, very rare. A single specimen from Groomsport many years ago ; none since ’ ’ — Hyndman ; and in his first list of Turbot Bank shells he notes “ a single dead specimen each to Dr. Dickie and G. C. H.” (sub B. Cranchii ). Scaphander lignarius, Linne. “Generally distributed”— Thompson (sub Bulla Lignaria). “Not uncommon, of large size, off Groomsport, living, in 6 or 8 fathoms, and in other places ” — Hyndman; and he dredged dead shells in depths up to 100 fathoms. Living in abundance, and of large size, in 6 to 8 fathoms off Bangor, and from thence to Crawfordsburn — Mr. Swanston, and Mr. S. A. Stewart. Fine living examples dredged in 2 fathoms off Cultra, and it is occasionally thrown up by the tide between Holywood and Craigavad in quantity, with the animal fresh — B.L1.P. Jeffreys states that it usually frequents the coral-line zone (15-50 fathoms) ; the above notes show that in our district it inhabits shallower water. Dead shells at Portrush and M agilligan — B . LI . P . var. alba. Bangor— Belf. Mus. Coll. Philine scabra, Muller. «Has been found at Bundoran (Co. Donegal), by Mrs. Hancock”— Thompson (sub Bulla peetinata) . Bare, dead, on the Turbot Bank Hyndman. PSiiline catena, Montagu. < ‘ Bundoran, Co. Donegal (J.G.J.) ’’-Jeffreys. Specimens from the same station are in Thompson’s collection in the Belfast Museum. Piiilme angulata, Jeffreys. “Lame, Co. Antrim (J.G.J.) Jeffreys. Pbiline quadrata, Searles Wood. “ Dead, in 80 fathoms off the Maidens” — Hyndman, 1859 Beport. PSiiline punctata, Clark. Bundoran in Co. Donegal, where it has been obtained by Airs. Hancock (fide Thompson, sub Bullcea punctata), and J effreys. Pliiline aperta, Linne. « Generally distributed ’’—Thompson (Jlullaa aperta). A rather common species, living in sand and mud at a few fathoms depth. “ Living, common, of the North of Ireland. 105 6-8 fathoms off Bangor” — Mr. S. A. Stewart. Of large size on the Holy- wood Banks —Mr. Swanston. Dead shells on Magilligan strand— R. Ll.P. Aplysia punctata, Cuvier. Living, rather scarce, in 8 or 10 fathoms, off Bangor and Groomsport, and in Castle Chichester Bay ’’—Hyndman (sub A. hybrida). A. nexa of Thompson is the young of this species. Pleurobranclms membranaceus, Montagu. “ Living, scarce, off Groomsport, in 6 or 8 fathoms, and in other places Hyndman. X 1ST 3D IEj 2C- Names of shells which are not admitted as native, owing to their being “P0^0”9’ mistakes, or fossils, or which appear in the foregoing list only as synonyms, are printed, in the case of genera, in parenthesis, and in the case of species, in italics. Acera bullata var. nana (Acirsa) borealis Aclis ascaris G-ulsonae var. tenuicula supranitida unica (Acmaea) testudinalis virginea Aetseon _ tornatilis AdeorMs subcarinatus (AmpUidesma) Boysii intermedia prismatiea (Ampliispliyra) hyalina (Anatina) 103 104 92 92 92 92 92 92 82 82 104 97 75 75 75 103 77 punctata Aporrbais pes-pelecani Area barb at a lactea tetragona Argiope capsula cistellula (Artemis) exoleta lincta undata Astarte compressa Banmoniensis Scotica sulcata var. elliptica var. Scotica triangularis Axinus flexuosus Anemia aculeata cylindrica epbippium _ patelliformis var. striata squamula striata undulata Aplysia hybrida nexa 61 Barleeia 61 rubra 61 (Brochus) 62 annulatus 62 leevis 61 reticulatus 62 Buccinum Q2 cyaneum JTolbolii 105 undatum 105 var. littoralis 105 98 66 66 66 61 61 70 70 72 69 69 69 69 69 69 70 67 90 91 91 91 99 100 98 99 var. striata Bulla Akera Cranchii cylindracea diaphana hyalina Lignaria obtusa pectinata striata truncata utriculus (Bullsea) aperta punctata 99 103 104 103 102 103 104 103 104 103 103 104 104 104 Capulus Hungaricus JJngaricus Cardium echinatum edule var. fasciatum elongatum exiguum fasciatum laevigatum Loveni minimum nodosum Norvegicum pygmeeum Suecieum 83 83 68 68 68 68 68 68 69 68 68 68 68 68 68 Index. 107 Ceratisolen legumen 76 Cerithiopsis costulata 98 pulchella 98 tubercularis 98 Ceritliium adversum 98 metula 98 niveurn 98 reticulatum 98 perversum 98 tuberculare 98 (Chama) cor 69 (Chemnitzia) elegantissima 95 fulvocincta 95 glabra 92 indistincta 94 interstincta 94 nitidissima 95 rufa 95 rufescens 95 scalaris 94 imica 92 Chiton albus, Linne 80 albus , Mont. 80 asellus 80 cancellatus 80 cinereus 80 fascicularis 80 var. gracilis 80 fuscatus 81 Hanleyi 80 Icevigatus 81 lseyis 81 marginatus 81 marmoreus 81 ruber 81 (Cingula) sculpta 94 Circe minima 70 (Cochlodesma) prcetenue 77 Caecum glabrum 91 trachea 91 (Columbella) Rolbolii 100 Corbula gibba 78 striata 78 Crania anomala 61 j personata 61 Crenella decussata 65 discors 65 marmorata 64 rbombea 65 Cyamium mmutum 67 Cyclostrema mtens 84 serpuloides 84 Cylichna acuminata 103 cylindracea 103 LajonJcaireana 103 mammillata 103 obtusa 103 striata 103 truncala 103 umbilicata 103 Cypraea Europsea 102 moneta 102 Cyprina Islandica 69 minima 70 (Cytherea) ovata 71 Defrancia Leufroyi 101 linearis 101 purpurea 101 reticulata 101 teres 101 Sentalium entalis 80 Donaz anatinus 74 denticulatus 74 truncatus 73 vittatus 73 Emarginula crassa 83 fissura 83 var. elata 83 reticulata 83 rosea 83 (Erato) laevis 102 Euliraa bilineata 96 distorta 96 var. gracilis 96 polita 95 subulata 96 (Eulimella) acicula 95 affinis 95 Sc illce, 95 (Euomphalus) nitidissimus 90 Fissurella Grseca 83 reticulata 83 Fusus antiquus 100 var. alba 100 Bamjjius 99 corneus 100 decussatus 99 gracilis 100 Islandicus 100 scalariformis 99 (©oodalia) triangularis 70 (Haliotis) tuberculata 83 Heleion pellucidum 81 var. lsevis 82 Homalog'yra atomus 90 rota 91 Hydrobia ulvse 90 lanthina communis 95 rotundata 95 Zsocardia cor 69 Jeffreysia diaphana 90 Gulsonce 92 Xellia rubra 67 suborbicularis 67 Lacuna canalis 86 crassior 86 divaricata 86 pallidula 87 puteolus 87 var. conica S7 quadrifasciata S7 vincta 86, 87 io8 Index ? 2«amellaria perspicua 97 I«ass8a rubra 67 Xieda caudata 65 minuta 65 pygmsea 65 Saepton uitidum 66 Xsima fray ills 63 Mans 63 Loscombii 63 tenera 63 subauriculata 63 Iiittoriua communis 87 dispar 90 jugosa 87 litorea 87 var. turrita 87 littoralis 87 Neritoides, Forbes 87 neritoides, Linne 87 obtusata 87 var. fabalis 87 var. neritiformis 87 patula 87 petrcea 87 rudis 87 var. jugosa 87 var. patula 87 var. saxatilis 87 var. tenebrosa 87 saxatilis 87 tenebrosa 87 2*oripes lacteus 67 (XiOttia) testudinalis 82 virginea 82 Xmcina borealis 67 Jlexuosa 67 leucoma 67 radula 67 spinifera 67 Xaucmopsis undata 72 Xiutraria compressa 75 elliptica 75 Mans 75 oblonga 75 vulgaris 75 Iiyonsia Norvegica 77 Maetra elliptica 74 solida 74 var. elliptica 74 var. truncata 74 stultorum 74 var. cinerea 74 subtruncata 74 var. insequivalvis 74 (Mangelia) attenuata iOI costata 101 Holbolii 100 Leufroyi 101 linearis 101 nebula 102 purpurea 101 reticulata 101 rufa 102 scabra 101 septangularis 101 striolata 101 Trevelliana 102 turricula 102 (Margarita) cinerea 84 communis 84 costulata 84 pusilla 84 undulata 84 vulgaris 84 Marginella lsevis 102 (Modiola) 65 discrepans marmorata 64 modiolus 64 phaseolina 64 tulipa 64 Modiolaria costulata 65 discors 65 marmorata 64 (Monoceros) hepaticus 100 (Monodonta) crassa 85 Montacuta bidentata 66 ferruginosa 66 ovata 66 purpurea 67 substriata 66 Mures erinaceus 99 Mya arenana 10 Bingbami 78 truncata 78 var. abbreviata 78 Mytilus Adriaticus edulis 64 var. incur vata 64 var. pellucida 64 modiolus 64 var. ovata 64 pellucidus 64 phaseolinus 64 OTassa hepatica 100 incrassata 100 macula 100 pygmsea 100 reticulata 100 Bfatica Alderi 97 catena 96 clausa 97 Grcenlandica 96 helicoides 96 Islandica 96 monilifera 97 Montacuti 97 Montagui 97 nitida 97 sordida 96 TTucula margaritacea 65 minuta 65 nitida 65 nucleus 65 var. radiata 65 tenuis 65 Odostomia acicula 95 var. obeliscus 96 var. ventricosa 95 acuta 93 alba 93 conspicua 93 cylindrica 92 decussata 94 dubia 93 eulimoides 93 excavata 94 indistincta 94 insculpta 94 interstincta 94 lactea 95 Lukisi 93 Index. nitida 93 nitidissima 95 nivosa 92 obliqua 94 var. Warrenii 94 pallida 93 plicata 93 rissoides 93 var. alba 93 var. dubia 93 var. nitida 93 rufa 95 var. fulvocincta 95 scalaris 94 var. rufescens 94 Scillse 95 spiralis 94 truncatula 93 turrita 93 unidentata 93 var. turrita 93 W arreni 94 Ostrea edulis 62 Ovuia acuminata 103 patula 103 Pandora msequivalvis 77 var. obtusa 77 obtusa 77 Patella ancycloides 82 athletica 81 Clealandi 82 pellucida 81 vulgata 81 var. depressa 81 Pecten Danicus 62 furtivus 62 Icevis 62 maxinms 63 obsoletus 62 opercularis 62 var. lineata 62 pusio 62 septemradiatus 62 similis 63 sinuosus 62 striatns 63 Teste 62 tigrinus 62 varius 62 Penlunculiis glycymeris 65 pilosus 66 PSiasianella pulla 86 PMline angulata 104 aperta 104 catena 104 punctata 104 quadrata 1.04 scabra 104 Plaoladidea papyracea 79 var. aborta 79 Plaolas Candida 79 crispata 79 dactylus 78 papyracea - 79 parya 79 striata 79 (Pileopsis) Hungaricus 83 (Pilidium) fulvum 82 Pinna fragilis 64 ingens 63, 64 pectinata 63 rudis 63 Pleuroferanchus membranaceus 105 Pleurotoma attenuata 101 bracbystoma 101 costata 101 var. coarctata 101 linearis 101 nebula 101 purpurea 101 rufa 102 var. lactea 102 var. Ulideana 102 septangularis 101 striolata 101 Trevelyana 102 turricula 102 Ulideana 102 Propilidmm ancycloides 82 PsammoMa costulata 73 Ferroensis 73 tellinella 73 vespertina 73 (Pullastra) decussata 72 perforans 72 109 virginea 71 vulgaris 71 Puneturella Noacbdna 82 Purpura lapillus 98 I&issoa albella, Alder 90 albella, Loven 89 var. Sarsii 89 Beanii 88 Bryerea 90 calathrus 88 cancellata 88 cimicoides 88 cingilla 90 cingillus 90 var. rupestris 90 costata 88 crenulata 88 dispar 90 excavata 94 fulgida 89 Harveyi 94 inconspicua 89 interrupt a 89 labiosa 89 membranacea 89 parya 88 var. interrupta 89 proxima 89 punctura 88 reticulata 88 rubra 90 rufilabrum 89 semistriata 90 var. alba 90 var. pura 90 soluta 89 striata 89 striatula 88 ulvce 90 violacea 89 vitrea 89 Warrenii 94 Zetlandica 88 (Rissoina) Bryerea 90 Saxieava arctica 7S rugosa 78 var. arctica 78 no Index. Sealaria communis elathratula clathrus Eschrichti Trevelyana Turtonse Scaphander lignarius var. alba Scissurella crispata Serobicularia alba var. curta nitida piperata prismatica tenuis (Sigaretus) perspicuus tentaculatus Skeaea costulata depressa divisa nitidissima planorbis var. trocbiformis rota Solecurtus antiquatus candidus coarctatus Bolen antiquatus ensis legumen marginatus pellucidus siliqua vagina (Sphoenia) Binghami (Syadosmya) alba intermedia prismatica Tapes aureus decussatus pullastra var. oblonga var. perforans virgineus 91 92 91 92 92 91 104 104 84 75 75 75 75 75 75 97 97 98 90 84 91 90 90 91 76 76 76 76 76 76 76 76 76 78 75 75 75 var. elongata 71 papillosus 86 var. Sarniensis 71 pusillus 84 Tectura 82 striatus 85 fulva tumidus 84 testudinalis 82 umbilicatus 85 virginea 82 undulatus 84 Tellina 72 zizyphinus 86 Balthica var. elata 86 crassa 72 var. Lyonsii 86 donacina 73 Troplion' 99 fabula 72 Barvicensis incarnata 73 clathratus 99 pusilla 73 muricatus 99 pygmoca 73 Syracusanus 100 solidula 72 truncatus 99 squalida tenuis 73 Truncatella 91 72 Montagui Terei>ratula 61 truncatula 91 aurita (Turbo) 90 capsula 61 dispar caput-serpentis 61 subtruncata 91 (Teredo) JS’orvegica 79 Turritella Hibernica 92 Thracia 77 terebra 91 convexa (Turtonia) declivis distorta papyracea var. villosiuscula 77 78 77 77 minuta 67 71 72 71 72 72 71 phaseolina prsetenuis pubescens villosiuscula (Tornatella) fasciata Tricliotropsis borealis (Triptioris) adversus (Triton) erinaceus Troelms cinerareus cinereus Clelandi Duminyi exasperatus exiguus granulatus Groenlandicus helicinus var. fasciata lineatus littoralis magus Montacuti Montag ui millegranus 77 77 77 77 104 97 98 99 85 84 86 85 85 85 86 84 84 84 85 85 84 85 85 86 Utriculus hyalinus mammilatus obtusus 103 103 103 var. Lajonkaireana 103 truncatulus Velutina laevigata var. Candida Venerupis Irus Venus aurea cancellata Casina exoleta fasciata gallina lincta oznea ovata Bennantii Sarniensis striatula striolata verrucosa 103 97 97 78 74 71 70 70 70 71 70 71 71 71 71 71 71 71 18 JIM 90 10 JUL.9S PROCEEDINGS OF THE Qj&ffaetf Qtafurato0+ jftefb CfuB* APPENDICES, VOL. II, No. 4. 1893-4 i*ML Sen JL i LEPIDOPTERA TAKEN IN THE BELFAST DISTRICT. By CHARLES W. WATTS, F.I.C. LEPIDOPTERA TAKEN IN THE BELFAST DISTRICT. By Charles W. Watts, F.I.C. INTRODUCTION. [Read 20th February , The entomologist living in Belfast has within his reach many places where he can capture his game. For short excursions, the range of hills from the Knockagh to the White Mountain is probably the best ground, including, as it does, wooded glens such as Collin Glen, the chalky slopes of the eastern faces, and the moorland and bogs of the higher parts of the hills. Each of these has its characteristic flora, and, feeding on the plants, we may expect an insect-fauna to correspond. Nearer home than the hills are productive spots like the marshes by the Lagan, and the Bog Meadows, and the lanes and hedgerows produce plenty of common insects, besides some better species among the Micro-lepidoptera. Further afield, but still within a day’s excursion, are Island- magee and the coast just north of Larne, and on the Co. Down side, the shore and the numerous plantations, especially the woods about Helen’s Tower. Inland in both counties we cannot expect great results. The country is more or less cultivated, and on such ground only the commonest species occur, but these sometimes swarm in par- ticular places. Of the more distant localities within the district the Mourne Mountains are undoubtedly the best, and after them, the Glens of Antrim, particularly Glenarm, and the sandhills of Portrush, 1X6 [Appendix B.N.F.C., Ballycastle, and Dundrum. I have no experience of the Antrim hills north of Larne, but they are so similar to the Belfast hills that their fauna is probably very much the same. I will now proceed to describe some of these localities more particularly, and mention some of the insects that occur in each. It will, of course, be understood that I do not imply that these are the only, or the best places for collecting, but that they are the places with which I happen to be familiar, either because they were convenient to the part of the town where I lived, or because they were favourite places for holiday-making. About a quarter of a mile north of the second lock on the Lagan there are some low-lying marshy fields. To the N. and E. the ground rises pretty steeply, and in the N.E. corner is a pond. Along the side of the slope is a disused water-course, which formerly, I believe, supplied the town. It is now filled with water-plants, Spargantum , Ins, and various reeds and grasses. When in flower in June and July these reeds attract numbers of Noctuce , the larvae of which feed on the leaves in the autumn and spring. The most abundant species are Leucania p aliens, impura, comma and lithargyria ; Tapinostola fulva, Noctua umbrosa , baja, c-nigrum, j estiva, rubi, and xantho- grapha , Apamea leucostigma and didyma , the last in great numbers and infinite variety of colour and markings. Earlier in the season several species of the genus T xniocampa may be found feeding at the blossom of the willow at night. Flying over nettles and flowers in the summer, we may net Plusia pulchrina, chrysitis and festucce , Dianthcecia nana and capsincola, whose larvae feed in the seed capsules of Silene and Lychnis. To capture these Noctuce in the summer months, the collector must keep late hours, for they do not settle down to feed till it is really dark, and in these latitudes that is not before half-past ten. From this time until midnight they can be taken off grass and reed flowers by the simple process of enclosing them in a chip-box after examining by the light of a lantern to see whether they are worth taking. They seldom attempt to fly ; at the most, they sometimes drop to the ground or into I«93-94.] 117 the water, as the case may be, for the grasses actually growing in the old water-course are by far the most attractive. The collector must be prepared to get his feet wet, or lose most of his moths. The only scarce Geometer that occurs in the marshes is Phibalapteryx vittata. The larva of this moth feeds on Galium palustre , and the moth is extremely abundant in June, both in these marshes and in the Bog Meadows. It is usually a scarce species in Ireland, so that it may fairly be claimed as a local speciality. Along the rough hedge at the top of the hill we may capture a number of species, mostly common, but Emmelesia decolorata is a good thing, which is abundant here. Only the commonest butterflies can be expected in such a locality, and it is hardly worth visiting in the day-time, except for Micro-lepidoptera, of which a number of common species occur. On the banks of the river I have found the curious larva of the Choerocampa elpenor (Elephant Hawk) feeding on Epilobium hirsutum , and the larva of Smerinthus populi is common on the willows. Epione apiciaria also feeds on the willows along the river, and the moth, which is scarce in Ireland, may be netted while flying at dusk in August. Cataclysta lemnata feeds on Lemna in the pond and ditches, and Hydrocampa stagnata on Potamogeton m the pond. Several species of the genus Scopula are common, and a number of Tortrices and Tinece , but nothing rare has turned up here. Altogether, I have taken 103 species of butter- flies and the large moths in this one field, besides Micro- lepidoptera. Collin Glen is one of the best collecting grounds in the immediate neighbourhood of Belfast. It is at its best in May and June. Later in the year the vegetation gets so rank that it is difficult to collect in the upper glen, which is the best part. The fauna of the upper and lower glens differs considerably, as might be expected from the different character of the ground. In the lower glen the trees are larger and the ground more open, but on the whole the results of collecting, either by day or night, are disappointing. I have tried here the well-known n8 [Appendix B.N.F.C., method of spreading what is called “sugar” on the trees to attract Noctuce, but it has never proved a success. Indeed, the same may be said of every place that I have tried, except the Donard demesne at Newcastle. The cause is probably the dampness of the majority of the otherwise suitable localities, including most of the wooded glens in the district. Two of the less universal butterflies occur here, namely, Par urge egena (Wood Argus) and Epinephele hyberanthus (Ringlet), the former being very common. Euchloe cardamines (Orange-tip) is also common in the glen, and still more so on the mountain just above, where I have taken specimens of a dwarf race. Macro gloss a bombylijormis is common at the top of the glen ; the larva feeds on Scabiosa succisa , and the moth is fond of the flowers of Pedicular is. Of the Bombyces , Spilosoma fuliginosa is common, also Lophopteryx camelina and Thyatira derasa and batis. The Noctuce include Miana arcuosa , Grammesia tn- grammica , Dianthoecia nana , and Plusia bulchrina. and of the Geometrae , which are more abundant, the commonest are Metrocampa margaritaria (Light Emerald), Selenia bi lunar la, Odontopera bidentata , Cabera pusaria and exanthemana, which fly in swarms about dusk, Strenia clathrata, Eupithecia lariciata among the larches in the higher parts, Hypsipetes impluviata among alder, Melanthia bicolor ata and ocellata , Anticlea badiata and nigrofasciaria and. Cidana silaceata, o which the larva feeds on the enchanter’s nightshade. We are on very different ground when we come to explore the hills, and we meet with an entirely different insect fauna. Species which are universal on the lower ground are entirely absent on the heather, and naturally the heath-feeding species do not occur away from the food-plant. Besides the heat species there are several which feed on Vaccinium, on various low plants, on ferns and grasses, and on Salix repens. The last is comparatively scarce on most parts ol the Belfast hills, so that the fauna is poorer than it would be if this favourite food- plant were more abundant. On the steep eastern face of the hills many plants grow which are not to be found off the Chalk, 1893-94] XI9 and this peculiar flora results in a peculiar fauna, many species, particularly among the micros, occurring here, and nowhere else in the district except on similar ground along the Antrim coast. There are no butterflies peculiar to the hills, but Lycoena icarus (Common Blue) and Polyommatus phloeas (Copper) are common on the Chalk. Coznonympha pamphilus is to be found all over the hills, and Euchloe cardamines wherever Cardamine pratensis grows. Of Sphinges , Macroglossa bombyliformis is common, and Zygoena filipendulce on the east of Black Hill. Of the Bombyces, Nemeobhila plantaginis is rather scarce, but Saturnia pavonia (Emperor) is common. The larvae of this moth, and of Bombyx rubi are to be found feeding on heath in the autumn, and the curious cocoon of the Emperor is a familiar object in winter. Several good Noctuce occur, and Celcena Haworthii, Stilbia anomala , Noctua glareosa and f estiva, Agrotis strigula , and Hadena glauca and adusta are all fairly common. Some good varieties of commoner species also occur on the higher ground, Triph(2na comes and Noctua xanthographa being especially remarkable. Of the Geometrce may be mentioned Ematur^a atomaria , Oparabia Jiligrammaria , Larentia ccesiata and salicata , Eupithecia satyr at a, var. callunaria , E. nanata , Phibalaptervx lapidata in marshy places, Cidaria populata , C. testata , and Anaitis plagiata among Hypericum on the east side of Black Mountain. Two species of Plume moths are common on Black Hill, viz., Mimesioptilus bipunctidactylus and pterodactylus , and last autumn I took a specimen of the very rare Platyptilia isodactyla on marshy ground between Divis and Black Hill, where its food-plant grows abundantly. A number of characteristic Tortrices occur, principally among heather. Of these the following are worth mention : — Tortrix viburnana , 7. palleana , Peronea caledoniana , Mixodia Schulziana , Catopiria hypericana , Eupcecilia ciliella , Argyro - lepia Hartmanniana and Xanthoseiia zcegana. 120 [Appendix B.N.F.C., The Knockagh near Carrickfergus is of a similar character, but there are several insects to be found there which do not seem to occur either on the Belfast hills or on Islandmagee. Lycozna minima (Little Blue) occurs about the top of the cliff, this being also the favourite ground for several good species, such as Melanippe tristata, Nemeophilia plantaginis, Ennychia cingulata, Oxyptilus parvtdactylus , and Scopana ingratella) most of which seem peculiar to this hill, at least so far as our district is concerned. The cliffs and slopes of Islandmagee between Black Head and Gobbin Head are very productive. The morning is the best time here, for in the afternoon the sun soon gets behind the hill and the temperature falls rapidly. Of the night-flying insects I know nothing, as the locality is too far for walking back after work, and there is no late train to town. Lyccena minima is exceedingly abundant here in June, and may be seen wherever Anthyllis vulnerana grows. The tiny larva feeds in the woolly flower- heads of this plant, but is very difficult to find. Lycama icarus is common, also Pararge megcera , Vanessa urticm , atalanta , and cardui. Nemeophila plantaginis is commoner here than anywhere else in the district and in some years is exceedingly abundant. Spilosoma fuliginosa occurs, and the larvae of Bombyx quercus) var. callunce may be collected in June, feeding on bramble. Of the other families of Lepidoptera may be mentioned Strenia clathrata) Emmelesia albulata , and Eupithecia con - strictata among the Geometrce ; Scopula jerrugalis , Aciptilia tetradactyla , Homeosoma senecionis , and Phycis subornatella among the Pyralides / and Peronea Schallenana) Penthina gentiana, Sericons littoralis , and Conchylis strammea among the Tortrices. Piutella crucifer arum (the Diamond-back Moth), which has sometimes completely destroyed the crops of turnips and other cruciferous plants in England, is fairly common here, but I have never seen any sign of damage, so it may be hoped that the climate is unfavourable to its multiplication. i893-94*] 121 Glyphipteryx equitella and Fischeriella , tiny black and silver species, are to be found on grass, flying about 4 p.m. in the sunshine ; several species of Argyresthesia and Elachista are also to be found. In all probability much the same species occur at many similar spots along the Antrim coast, and a number of species are recorded from Glenarm, but these places are beyond a single day’s excursion. At Glenariffe I have taken Larentia olivata , which is rare in Ireland, and no doubt the locality would repay investigation, though it is not well suited for night work. On the north coast of Antrim, the sandhills of Ballycastle and Portrush are splendid collecting grounds for those species that frequent such places. At Ballycastle the very local Nyssia zonaria is plentiful at the beginning of April. So far this species is only recorded, in Ireland, from Ballycastle and Achill Island. It occurs also in the Isle of Man and on the coasts of Cheshire and North Wales. I now come to the districts in County Down, and shall confine my remarks to the Mourne Mountains, and more particularly to the immediate neighbourhood of Newcastle, which is the best centre for collecting. To the west of Newcastle there is a fine stretch of sandhills stretching to Dundrum Bay ; at the back of the village are the woods of Donard demesne, perhaps the best woods in our district, and beyond the woods are the mountains. Each of these produces its special insects, which, for the most part, are not to be found in the others. The best part of the sandhills begins about two miles from Newcastle and extends to Dundrum Bay ; they are continued on the opposite side of the bay, but this part is too distant for convenient working. Two butterflies are abundant all over the sandhills, Lycozna icarus and Satyrus semele (Grayling). The western Irish forms of both differ considerably from the English and European types, being in both cases larger and more brightly coloured. In the south of England the male icarus is small and of a rather dull lilac-blue, and the female is brown, slightly tinged with 122 [Appendix B.N.F.C., blue, and with a border of red spots round all the wings. In this district the male is large and very bright blue, approaching the colour of Lycatna adonis , while the female is also blue, though not so bright, and the marginal red spots are very large and bright. Specimens of both forms may be seen in the Museum collection. There is not much to be got on sandhills early in the year ; the real work begins with the flowering of the marram grass in June and July, and is better still when the ragweed is in flower in August. Great numbers of Agrotidce and other Noctuce frequent these flowers. A few come out about 4 p.m. on sunny days, and are then easily collected ; but for one that is out then a hundred are out after dark. The heads of the Senecio are sometimes very large in such situations, and on a single flower-head I have counted fifty or sixty moths at once; but they are very particular in their choice, and while one flower-head is nearly covered with moths, neighbouring and, as far as we can see, exactly similar heads are nearly deserted. Besides the moths there are plenty of earwigs, beetles, and gnats for any that are interested in these orders of insects. A few species are particularly abundant, viz. : — Apamea didyma in infinite variety, Agrotis tritici and Noctua xantho- grapha) also very variable. Five out of six moths belong to one or other of these species, but several others are also common — Miana strigilis , M. bicoloria , M. literosa , Agrotis vestigialis , A. cursoria) A . nigricans , A. prcecox , A. lucernea) and A. suffusa ; Noctua rubi , Triphcena ianthina) and the common yellow underwings ; Phlogophora meticulosa , Hydrcecia lucens) H . micacea) and a number of others. A few Geometrce come also to the flowers, besides a good many Crambi and other Pyralides) and several species of Depressaria . On the heather and bracken of the older parts of the sandhills other species occur, but the only noticeable one is Gnophos obscurata) which is very abundant. Micro-lepidoptera are abundant, and several good species occur, such as Anerastia loietla, Cr ambus W arringtonelius , C. *893*94-] 123 geniculeus , Dictyopteryx Bergmanniana amongst Rosa sfrino- sissima , and many small Gelechidw , which can be obtained by kicking them out of the roots of the bent, where they shelter during the day-time. Insects are abundant in the woods of Donard demesne throughout the season. Lyccena argiolus (Holly Blue) is out in May and Argynnis paphia (Silver-washed Fritillary) in July, but the latter is scarce. No Sphinges seem to occur, and not many Bombyces , but Hylophila prasinana is common, also Hepialus velleda , H. hectus) and Thyatira batis. The latter comes to sugar along with various Noctuce , such as Acronycta rumicis) Hadena adusta) and Caradrina taraxaci , and Aphomia sociella , whose larva feeds on the wax in bee-hives and the nests of wild bees. The Geometrce are well represented, including several un- common species, especially among the fir-feeding kinds. Ellopia prosapiaria is common, also Bupalas piniaria and Boarmia repandata , and the fine banded variety conversaria . Venusia cambrica and Emmelesia teniata are scarce. Several Eupithecice occur, including E. satyrata) castigata , lariciata) and pumilata. The last feeds on the flowers of Ulex) and swarms both in the higher parts of the demense and in the lower valleys. The pretty Melanthia albicillata may be seen settled on tree trunks in July. Thera variata is very abundant, but T. firmata is scarce. Micros are not very abundant, and only Amblyptilia acanthodactyla and Olindia nlmana are worth noting. Collecting on the mountains themselves is rather disap- pointing, especially in the number of specimens obtained. I have sometimes walked several miles without seeing a specimen of any sort, and this on a fine day in summer. Nevertheless, a good many species occur, and I believe that a resident collector could do very good work when he had once found the right spots for insects. This paucity of insects no doubt is due to the poverty of the flora of the Mourne range. There are no truly alpine insects recorded from the district, but then only Slieve Donard rises 124 [Appendix B.N.F.C., appreciably over 2,400 feet, which is the lowest limit of alpine insects, and the upper part of this mountain is too bare and shelterless for Lepidoptera to exist there. The most promising-looking parts for such insects are the actual tops of the few mountains which are crowned with rocks, like Bingian, Bearnagh, and Commedagh. Round these rocks the vegetation is luxuriant, and Salix herbacea grows freely. A few species occurring lower down may be mentioned. Saturnia pavonia is common, and its larva, together with that of Dicra - nura vinula and Pygwra pigra , is common on willow bushes by the streams. Hadena contigua occurs, Anarta myrtilh is common, also Stilbia anomola , Pachnobia rubricosa and Phyto- metva viridaria. The Geometrce include Gnophos obscnvata) Pseudoterpna pruinata , Scodiona belgiana , Larentia ccBsiata , Eupithecia nanata , E. minutata and E. sobrinata — this last feeding on juniper. A few micros may be mentioned : — Phycis fusca occurs in the Happy Valley and also above Donard demesne, Mixodia Schulziana is pretty common, and Pamplusia mercuriana occurs at the top of Slieve Bingian. No doubt further search would result in many additions to this rather meagre list, but there is so large an extent of country to be covered that for anyone living at a distance it would take many years to make anything approaching a complete list of the lepidoptera of the Mournes. In conclusion, I may say that specimens of nearly all the species mentioned are now in the Belfast Museum collection, and that it is much to be hoped that some member of the Club will take up this branch of field work and add to our knowledge of our local Lepidoptera. **93-94] ^5 LIST OF SPECIES. RHOPAEOCERA. Pierls brassioae — Common, rapae — Common. napl — Common. Occurs in the marshes on the Belfast hills up to 900 feet. The specimens are generally strongly marked on upper side, and the under side is sometimes very yellow. Eucbloe cardamines — Common. I have specimens from the Belfast hills expanding only 30 mm. Argynnis papbia — Donard de- mesne and other woods, but not common. Vanessa urticse — Common. atalanta — Not common generally, hut very abundant in 1893. cardui — Common in some years. Pararge egeria — Very abundant in all woods and lanes, from May to October. megaera — Local ; Islandmagee, Newcastle, &c. Satyrus semele — Very abundant on sandhills, Newcastle, &c. ; the [None of the Hesperidce are specimens are large and brightly coloured. Epinepbele janira — Common. Large and well marked ; females, with bipupilled ocellus and extra ocelli, sometimes occur. byperanthus — Common. Coenonympha pampbilus Common. Polyommatus pblaeas — Common. Eycaena i earns — Common. Large; males often very bright blue; females also very blue, with the marginal red spots strongly developed, and occasionally the discoidal spots on both wings are white-ringed. argiolus — - Donard demesne; common. minima — Antrim coast. Very abundant on Islandmagee ; male- often bluer than type, and some times showing the discoidal spots as in L. argiolus. recorded from this district.] SPHINGES. Acberontla atropos — Lisburn, &c. ; scarce. Deillpbila livornica — Two spe- cimens taken at rhododendron flowers in Ormeau Park, Belfast, June, 1888. Cbaerocampa elpenor — Larvae occasionally on Epilobium hirsu- turn about Belfast. Smerlntbus populi — Common. IMCacroglossa stellatarum - Scarce. bombyllformis — Common on Belfast hills. Zygaena filipendulae — Common. SOMBTCES. Hylopbila praslnana — Common. CTudaria mundana — Newcastle, &c. ; scarce. Rucbella jacobaeae— Common. Hemeophila plantaginis — Is- landmagee, very abundant; Bel- fast hills. Arctta caj a— Common. 126 Spilosoma fuliglnosa — Common, mendica — Common; males ap- parently always cream-coloured, lubricipeda - Common, menthastri — Very abundant ; some specimens nearly immacu- late, and ochreous specimens (var. ochracea) are common, sometimes with the wing-rays white. Hepialns humuli— Very abundant, velleda — Very abundant ; var. gallicus also common, bectus — Common. Orgyia anti qua— Larvae scarce. Bombyx rubi — Larvae common on hills. quercus, var. callunee— Larvae common. [Appendix B.N.F.C., Saturnia pavonia — Very common on hills. Sicranura vinula — Common. Xaopbopteryx camelina— Common. Notodonta dictaea — Scarce, dromedarius — Scarce, Belfast, ziczac- Larvae not uncommon on "Willow. Pbalsera bucepbala — Common. Pygaera pigra— Larvae on willow, Mourne Mountains. Thyatira derasa — Collin Glen ; common. batis — Very common. WTOCTUJE. Bryopblla perla — Newcastle. Aconycta psi— Common. rumicis — Donard demesne ; a pale form. Xteucanla conlgera*— Belfast marshes. litbargyria— Common, comma — Common, impura— Very abundant, pallens — Very abundant ; var. rufescens common. Tapinostola fulva — Very abun- dant in marshes near Belfast ; varies from pale bone-colour to dark reddish. Nonagrla arundinis — Local in Co. Down. Hydreecia nictitans — Most, if not all, the specimens from this dis- trict are referable to H lucens. micacea— Common. Xylopbasla rurea — Very abun- dant ; var combusta also common litboxylea— Very abundant, monoglypba — Very abundant ; var. brunnea (Tutt) is common and var. obscura (Tutt) scarce. XTeuronia popularis— Belfast. Cbarceas graminis — Very abun- dant. Xuperina testacea— Belfast ; com- mon. Mamestra brassicee— Common. Apamea basillnea — Common. Apamea opbiogramma — One specimen in a marsh near Belfast. gemina— Common. leucostigma— The type and var. fibrosa are both common in the marshes about Belfast and else- where in the district. didyma— Very abundant. Miana strigilis— The type is scarce, but the darker varieties fairly common. fascluncula — Common ; small grey specimens occur on the hills in August. literosa — Not common, but gener- ally distributed. bicoloria -Very abundant ; var. rufuncula is not uncommon Celeena Haworthii — Common on Belfast hills. Grammesia trigrammica— Common. Stilbia anomola — Common in one place on Black Mountain, Belfast ; also Occurs in the Mourne Moun- tains The specimens are large and dark. Caradrina taraxaci — Common. 4-punctata — Very abundant ; the specimens from this district are generally either ochreous or dark grey. Xtuslna tenebrosa — Belfast scarce. 1*91-94] 127 Agrotls vestlglalis — Sand*hills, Dundrum; abundant, segetum — Common, exclamatlonis — Common, cursoria — Sand-hills ; common, nigricans — Common, trltlci— Sand-hills; very abundant; mostly reddish brown, strigula — Belfast hills, abundant, praecox — Sand-hills, common, lucernea — Sand-hills at Dundrum; dark grey. OToctua glareosa — Belfast hills, abundant, augur — Common, plecta — Common, c-nlgrum — Common, brunnea — Common, festlva — Common, umbrosa — Yery abundant, rubl — Common, baj a — Common. Trlphsena iantblna — Common, comes — Common, pronuba — Common.- Amphlpyra tragopogonls— Common. Mania typica — Common, maura — Common. Taeniocampa gotbica — - Very a- bundant at willows in spring, lncerta — Yery abundant, but not very variable, most of the speci- mens being dark brown, oplzna — Belfast ; both the pale type and var. brunnea (Tutt). stabilis — Yery abundant. Ortbosla lota — Belfast, common. Cerastis vaccinli — Commonat ivy- bloom. spadicea — Common at ivy-bloom. Scopelosoma sateliltia -— Com- mon at ivy-bloom. Xantbia fulvag© — Belfast, scarce. circellaris— Belfast, scarce. Clrrhaedia xerampelina— Belfast and Castlewellan. Calymnla trapezlna — Common. Bianthseda nana — Common in marshes. capsincola — Common, cucuball —Common. Polia chi — Glenarm. Misella oxyacanthae — Common. Agriopis aprilina — Common. Euplexia luclpara — Common. Aplecta nebulosa— Common. Hadena adusta — Donard demesne and Black Mountain ; common, glauca — Belfast hills, common. The specimens belong to var. lappo (Dup.) dentina — Common, trlfolll — Common, oleracea — Common* plsi — Scarce. contlgua — Moume Mountains, scarce. Calocampa exoleta — Belfast, &c.; common. vetusta — Belfast, &c ; common. Cucullia umbratica — Donard de- mesne, scarce. Cronoptera libatrix — Common. Habrostola tripartita — Common. triplasia — Common. Plusia chrysitis — Common, festucae — Common, pulchrina — Common, gamma — Common . ilnarta myrtilli — Mourne Moun- tains, common. Phytometra viridarla — Moume Mountains and Belfast hills ; common. Rlvula sericealis — Common. Zanclognatba grisealis— Common. tarsipeimalls — Common. Pecbypogon barbalis — Common. Hypena proboscidalis — Yery abundant. GEOMSTRJE. Ourapteryx sambucata— Belfast. Epione apiciarla — Belfast, scarce. Rumla luteolata — Yery abundant. Metrocampa margaritaria- Common. Ellopia fasciarla — Donard de- mesne, common. Selenia bllunaria — Common. Odontopera bidentata — Common. Crocallis ellnguaria — Common, 128 [Appendix B.N.F.C., annomoB queroinarla — Tolly- more Park, &c. Phlgalia pedaria— Common; large and pale coloured. Nyssia zonaria — Ballycastle, very abundant. Ampbldasys b etularia— Common. Boarmia pepandata — Common ; rather dark ; var. conversaria , Donard demesne, scarce, gemmaria — Common. Tepbrosla crepuscularla — Don- ard demesne, common ; dark varieties frequently occur. Gnopbos obscurata — Newcastle, abundant ; very dark. Pseudoterpna pruinata— Common. Venusia cambrica — Donard de- mesne, scarce. Addalia dldixniata — Common, blsetata — Common, marginepunctata — Kilkeel, scarce. aversata — Common ; var. spoliata , common. Cabera pusaria — Very abundant; the specimens from this district are rather more sprinkled with black scales than is the case with English specimens, exanthemaria— Very abundant. Macaria liturata — Donard de- mesne. Strenla clat brat a— Common ; the yellow parts of the wings pale, inclining to white. Scodioua belgiaria — Moume Mountains. Ematurga atomaria — Hills, abun- dant. Bupalus piniaria — Donard de- mesne, very abundant. Abraxas grossulariata— Common. Bomaspilis marginata— Common. Hybernia rupicapraria— Common. marginaria — Common ; dusky, ill-marked specimens are frequent. defoliaria— Common. Cbelmatobia brumata— Common. Oparabla dilutata— Common. flllgrammaria — Belfast hills. Earentla dldymata — Very abun- dant. multi stri gar la — Common, gener- ally of an ochreous tint, csesiata — Belfast hills, abundant ; Moume Mountains, scarce, s all c at a~ Belfast hills, common, oil vat a — Glenariffe. viridaria— Common. Emmelesia alcbemillata— Bryansford. alb ul at a — Common ; dark and well marked. decolorata — Belfast, locally abun- dant. tseniata— Donard demense, very rare. Eupitbecla oblongata — Common, satyr ata— Common ; var callun - aria , very abundant on hills ; very variable, some specimens approaching v. Curzoni. castigata — Common ; occasional melanic specimens occur, lndlgata — Belfast, constrictata — Islandmagee, com- mon ; Kilkeel. nanata — Common on hills, vulgata — Common, absyntbiata — Common, minutata — Common, assimllata — Common, lariclata — Collin Glen ; Lame, very abundant, abbreviata— Scarce, sobrinata — Belfast, and Moume Mountains, scarce, pumllata — Common ; very abun- dant on Moume Mountains. Tbera variata — Common. firzuata — Donard demesne, scarce. Hypsipetes trifas data— Common; very abundant in Collin Glen, sordidata — Common. Melantbia bicolorata— Glenarm, Collin Glen, &c., not common, ocellata — Collin Glen, &c. albldllata — Donard demesne, common. Melanippe tristata — Knockagh, abundant ; Moume Mountains, sociata — Common, montanata— Very abundant. I&93-94-J 129 gallafa — Local, not common, fluctuata — Common. Anticlea badiata — Very abundant, nlgrofasciarla -Collin Glen, scarce. Coremia munltata -Local, scarce, deslgnata — Scarce, ferrugata — Common, unidentaria — Common. Campfogramma bilineata — Very abundant. Phibalapteryx lap! data— Belfast Hills. vlttata — Belfast marshes, very abundant. Cldarla miata — Common, truncata— Common, mostly yar. perfuscata. lmmanata — Common, saffumata — Common, silaoeata — Collin Glen, common, testata — Hills, common, populata — Common, fulvata — Common . Pelurga comitata -Common. Eubolia limitata —Very abundant. plumb aria — Very abundant. Anaitis plagiata— Black Mountain, common. Pyralis glauclnalis— Common. farinalls — Common. Sooparia ambigualis —Scarce, cembrsae — Belfast, common, dubitalis — Common, lngrafella — Knockagh, common, trunclcololella — Donard demesne. augustea — Dundrum. ETomopMla noctuella— Common. Berbula cespltalis — Common. Ennycbla clngulata — Knockagh, common. Burrhypara urtlcata— Common. Scapula lutealis— Very abundant, ollvalls — Common, prunalis— Collin Glen, &c. ferrugalls — Islandmagee, scarce. Botys fuscalis— Common. Bbulea sambucalis— Common. Pionea forficalls — Common. Cataclysta lemnata — Common. Hydrocampa stagnata — Common. Chrysocorys festaliella— Belfast. Platyptllla ocbrodactyla— Dunnaneile Island, Strangford Lough. Isodactyla — Belfast Hills, scarce, ffonodactyla — Common. Amblyptilia acanthodactyla— Newcastle and Belfast, scarce. Oxyptilus parvidactyla— Knock- agh, abundant. Mlzneseoptilus bipimctidac- tylus— Black Hill, &c., abun- dant. • pterodactylus — Black Hill, abundant. Pterophorus monodactylus— Common. Aclptilia tetradactyla — Island- magee, scarce. Chllo pbragmitellus — Black Mountain, scarce. Crambu* pratellus— Common, perlellus — Common, warriugtonellus— Sandhills, common. geniculeus— Sandhills, common, culmellus — Very abundant, tristellus — Common, bortuellus — Common. Hozneosoma senecionis New- castle, scarce. Pbycls fusca— Moume Mountains. subornatelia— Islandmagee, rare. Aphomia sociella — Common. TOBTBZCES. Tortrlx cratee gran a— Common, zylosteana — Scarce, rosana — Scarce, dl v er sana — Common. unlfasclana — Belfast Hills, &c., common. eostana — Common, viburnana — Hills, common. 130 [Appendix B.N.F.C., palleana— Black Hill, &c., com- mon. viridana— Common. Peronea Scballeriana — Island- magee. variegana — Common . bastiana — Belfast, scarce, caledoniana — Hills, common. Teras contaminana — Common. DIctyopteryx Boeflinglana— Common. Holmlana — Belfast, scarce. Bergmanniana — Very abundant. Argyrotoxa Conwayana — Com- mon. Penthina sauciana— Common. gentiana — Common. Antitbesia salicella — Belfast, scarce. Hedya ocellana — Common. Spilonota trimaculana — Com- mon. Pardia tripunctana — Common Sericoris littoralis — Islandmagee. cespitana — Common, lacunana- Very abundant IVlixodia Scbulziana— Hills, common. Ortbotsenia antiquana — Belfast. Cnepbasia po lit an a— Donard de- mesne, &c., common, musculana — Common. Sciapbila virgaureana — Com- mon. cbrysantbeana — Common, octomaculana— Bare. Spbaleroptera ictericana— Scarce. Clepsls rusticana- Common. Bactra lanceolana — Very abun- dant. Pboxopteryx myrtillana— Belfast Hills, scarce. lundana — Very abundant. Grapholitba nigromaculana— Mourne Mountains, sub ocellana — Very abundant, trimaculana — Belfast. Penkleriana -Common, nee van a — Common Batodes angustiorana— Belfast. Paedlsca bilunana — Belfast, scarce. corticana— Belfast, common. Eptaippipbora cirsiana — Com- mon. brunnicbeana-Common. Olindia ulmana — Donard demesne, scarce. Pamplusia mercurlana— At top of Slieve Bingian (2400 feet). . Stigmonota perlepidana— Collin Glen, abundant. Blcroramplxa plumbana— Knockagb, abundant. Catoptrla ulicetana — Very abun- dant. bypericana — Belfast Hills, cana — Belfast Hills, citrana — Belfast, scarce. Slmeetbis oxyacantbella — Very abundant. Eupeecilia dubitana — Belfast, scarce. atricapitana — Belfast, scarce, angustana — Common, grlseana — Scarce, cillella— Hills, common. Xantbosetia zoegana — Common. bamana — Common. Argyrolepla Hartmanniana— Belfast Hills, local. Concbylis straminea— Island- magee. Apbelia osseana— Common. TOTE®, Blurnea fagella— Common; always ochreous. Scardla cloacella— Common. Blabopbanes rusticella— Common. Tinea pellionella — Common, pallescentella — Common, lapella — Common, mer della— Common. Jiampronia luzella — Belfast, scarce. XTexnopbora Scbwarziella— Common. Swammerdaraia caesiella Very abundant. pyrella — Common. splnlella— Common . 1893-94*] 131 Hyponomeuta padellus— Common. cag-nag-ellus — Locally common. Prays curtisellus— Common. Plutella crucifer arum— Common. Cerostoma radiatella — Common. costella— Common. Harpipteryx xylostella— Common. Phibalocera quercana— Common. Depressarla costosa— Very abun- dant pallorella — Scarce, utnbellana — Newcastle, scarce, arenella -Common, litur ella —Common, yeatiana — Common, applana — Common, beracleana — Common. Gelecbla ericetella — Common. Bryotropha ter ella— Belfast, desertella — Newcastle sand-hills, p olit ella — Belfast. Xiita artemisiella— Newcastle sand-hills. marmorea —Newcastle sand-hills, very abundant. Teleia vulgella— Scarce. dodecella— Belfast Hills, scarce. Cberlaria Hubnerella— Belfast. Pleurota bicostella— Hills, com- mon. GBcopbora pseudospretella- Common. Endrosis fenestrella — Common. Glypbipteryx tbrasonella — Very abundant in marshes. Haw orthana— Belfast, scarce, equitella — Islandmagee, abun- dant. Flscberiella — Common. Argyrestbesia epbippella— Belfast. nitidella — Common, semltestacella — Belfast, scarce, albistria — Belfast, common, conjugella —Common, mendica — Common, pygmaeella — Scarce. Gracilaria tringipennella— Islandmagee, scarce, syringella — Common. Oruix auglicella — Belfast. betulae — Belfast. Goleopbora albieosta— Belfast, caespititiella— Common. Chauliodus cbaeropbylellus— Belfast. laverna atra — Belfast. Elacbista mouticola — Ballyna- hinch. perplexella — Common, obscurella — Common, rbyucbosporella — Belfast, scarce. rufocinerea — Belfast, scarce, subalbidella— Very abundant, argenteila — Very abundant. Bitbocolletis pomifoliella - Belfast. salicicolella — Belfast, quercifoliella — Belfast, common, alnifoliella — Belfast. 1 A SUPPLEMENT TO THE FLORA OF THE NORTH-EAST OF IRELAND OF STEWART and CORRY. - K ncfj BY S. A. STEWART, F.B.S.Edin., AND R. LLOYD PRAEGER, B.E. Being an Appendix (No. 5 of Vol. 2) to the Proceedings OF THE BELFAST NATURALISTS’ FIELD CLUB For 1894-95. * 4 VUt .( V 1 /i % NOTE. The size of the page in the following paper has been made the same as that of “ Flora of the North-East of Ireland,” in order that the Supplement may be bound with the Work by those who desire it. A SUPPLEMENT TO THE “Flora of the North-East of Ireland” of Stewart and Corry. By S. A. STEWART, F.B.S.Edin., and R. LLOYD PRAEGER, B.E. knowledge of local topographical botanv, an/givitig a general account “f ^ flora of the twelfth district of Oybele Hibermca Since that S' progress has been made ; a godly number of flora, and our knowledge of the distribution of others W a * the noteworthy degree. Since the publicat.on of ifora seveil m^Thf v,,ented ‘° 5 summarizing the more important additions, and others dealing with the hofaS characteristics of certain tracts of country or wHL onrtoi Ine Dotanical within our district. There have ST l°o aFflom in Journals, and Proceedings of Societies Onr Vv r ocai nora all these together, along with a considerable amount of un^hTistTmateriaf and no pains hare been spared to make this Supplement comoW^ ^ l Being a Supplement to the Flora of the North-Fast nf Tiww paper divides itself into two sections (l) Plailtf or Mwes”d — ^ Onoms spine*. Calamintha officinalis. Rom micrantha. Primula veris. Bilans pratensis. [Appendix B.N.F.C., 136 A few varieties have also to he withdrawn, and ^^nhUshed^ transferred to plants different from those under which they w p ’ n wS no recent record could be grr«r a^-^v&,^twSSSft attention here to the more prominent of them, lney m y (11 Plante of which we have reason to doubt the identification 1 ' Leontodon hupidum. Gentuma amarella. . (2) Plants which appear to have been not established in the district, and now missing:— wium sophia^ Planum nigrum. Sinapis nigra. Chenopodium rubrum (3) Plants apparently destroyed through drainage ; these are most y p an s o Lough Neagh basin Carexfongata. Lathy rus palustris. G. Jiliformis. Slum latifolium. 0. paludota. Epipactis palustris. Lastrea thelyp m*. Cephalanthera emifolia. Pilulana globuhfera. (41 Plants apparently lost though building or cultivation Eleocharis uniglumis. Bordeum pratense . Schlerochloa procumbens. Three other plants Hypericum Mrmtum, Adoxa moschalelhna, tarex muricata , have become almost extinct owing to similar causes. (5) Plants not seen recently, but for whose absence no special reason exists ^ Geranium sanguineum. Taxus baccata. Trifolium striatum. Calamagmtu eptgejos. T,,,,,,, aria Poa nemoralis. Arctostaphylos um-ursi. Polypodxum dryoptens. Pyrola secunda. Tohjpella mdifica. We trust that our drawing attention to the above may lead to the rediscovery Mourne Mountains district for cryp ? , valley of the Lower Bann by the present writers; and the e^minatiou of th of Uie he drawn. i894-95-] 137 Irish Naturalist , 1892 to date, papers being : — SOURCES OF INFORMATION. Books — English Botany ; Supplement to Yols. I — IV. By N. E. Brown. 1892 The British Moss Flora, by Dr. Braithwaite, Yols. I. and II., 1880-95. Periodicals — JomnaUf Botmy, 1888 to date. Contains some notes concerning the local Papers and notes, the more important Stewards. A.— Notes on the Flora of the North-East of Ireland, Shoolbred, W. A. — A Botanical Trip to Co. Antrim, 1894. Gr°V189?’ & J‘_The Distribution of the Characese in Ireland, Proceedings of Societies — Boyal Irish Academy. The papers consulted are : — Hart’ C'~^.lants of some of the Mountain Ranges of Ireland, 1884 1 his paper yielded some notes additional to those already extracted from it. Lett, Rev. H. W. -Report on the Mosses, Hepatics, and Lichens oi the Mourne Mountain district, 1890. Hart, H. C.— Range of Flowering Plants and Ferns on the Mountains of Ireland, 1891. Yields very little additional to the iormer paper. Stewart, S A., and R. Lloyd Praeger.— Botany of the Mourne Mountains, 1892. Our increased knowledge of the Co. Down flora is mainly due to this paper, and that by Rev. Mr. Lett. Belfast Naturalists’ Field Club, 1888-9 tiU 1894-5. Papers and notes, including plants found on the Excursions. Praeger.— New or Rare North of Ireland Plants, 1891. Do. —Local Botanical Notes, 1891 and 1892 ; 1893. Botanical Exchange Club Reports , 1888 till 1894. Watson Botanical Exchange Club Reports , 1885—6 till 1893—4. MS. Notes and Lists — Templeton, John Pour -relumes of his MS. “Flora Hibemica,” at present deposited with the Belfast Nat. Hist, and Phil. Society. Contains much original matter concerning local cryptogams, which could not he worked out m time for the present paper. 138 [Appendix B.N.F.C., ; Notes referring to various districts, kindly r supported by specimens when rf Kmwn Robert We are indebted to Mr. James Britten for a transcript of ^af notes contained in the two volumes of MS. n Bntish Muse mentioned in bis review of Flora .WE. Ireland in Journ. Rot. 1888. Leebody, Mrs. ) Knowles , Miss M. G. Lett , Rev. E. W. Waddell , Rev. C. E. Brenan , Rev. S. A. Smith , Rev. W. S. Davies , J. E. To several other observers we are indebted for occasional notes of plants observed by them in new stations, and for specimens sent. ^ 1/ mv David Tbe greater portion of tbe original and duplicate sets renfesenting the flma of Co. Antrim, and of the duplicate set represent- ing the Aot! of Co. Derry, made by Dr. Moore in 1836 and 1837 when in” the Ordnance Survey service, are deposited in the Dublin Science and Art Museum. The duplicate set is unfortunately not localised. _ . . ~ 77 tVip British Herbarium, which includes the Elv.%V.rM.Hiud, was looked into, hut yielded nothing of importance for our purpose. _7 ■ Cravden The British Herbarium contains some of Dr. ff^re“ “nts, buUoo little was found to induce a thorough examination of the collection. _ Grainger, Ben. Canon. A small collection, made chiefly in Antrim, which The additiondoiaourWownMS. notes to this list completes the enumeration. The notes now brought together Jnclu de a mi: mber of the flora of “h^tern largely. K^e S now divided must not be over-estimat , accurately worked out, and in this distribution of the 7arl0U" no otherbin Ireland. Y Some interesting species respect our district is no^ behin j addition to the Irish flora), have been added, such as tares paucijloi ( g tich we are not aware of Bolygonum ItlmLzoviam (in Europe known Saussurea alpina , Orchis pyramtdahs, Ca™* q & of District 12 and to isr.'assis sas separately on a subsequent page. 1894-95*] 139 ADDITIONS TO DISTKICT 12 Ranunculus eircinatus. Drosera intermedia. Trifolium hybridum. Poterium sanguisorba. Rubus Roger sii. nitidus. gratus. erythrinus. Lindleianus. pulcherrimus . silvaticus. micans. Leyanus. echinatus. rudis. scaber. fuscus. rosaceus. hirtus. chamoemorus. Rosa glauca. Arctium minus . Saussurea alpina. Hieracium Leyi. Farrense. rubicundum. argenteum. Sommerfeltii , hibernicum. stenolepis. euprepes. sciaphilum. auratum. Polygonum maculatum. Orchis pyramidalis. Spiranthes Romanzoviana . Sparganium neglectum. Potamogeton undulatus. Garex pauciflora. aquatilis. filiformis. Triticum acutum. Char a contraria. ADDITIONS TO COUNTY DOWN. Ranunculus eircinatus. lepidium campestre. Prosera intermedia. Sagina ciliata. Spergularia rubra. Hypericum quadrangulum. Trifolium hybridum. Rubus suberectus. plicatus. Rogersii. nitidus. Lindleianus. pulcherrimus. silvaticus. mucronatus. Leyanus. rudis. scaber. fuscus. rosaceus. hirtus. Rosa involuta. Epilobium angusti folium. Saxifraga tridactylites . Inula helenium. Saussurea alpina. Hieracium argenteum. hibernicum. sciaphilum. gothicum. auratum. Galeopsis speciosa. Polygonum maculatum. Salix purpurea. Populus tremula. Sparganium neglectum. Potamogeton Zizii. Ruppia rostellata. Eleocharis acicularis. Car ex (Edcri. Bromus racemosus. Triticum acutum. Ohara contraria. 140 [Appendix B.N.F.C. ADDITIONS TO COUNTY ANTRIM. Arabis hirsuta. Geranium perenne. Trifolium hybridum. Poterium sanguisorba. Rubus gratus. Zindleianus. pulcherrimus. echinatus. rosaceus. Rosa glauca. Arctium minus. Hieraeium Jlocculosum. Far rente, rubicundum . Hieraeium stenolepis • euprepes. auratum. Vaccinium oxycoccos. JJtrieularia intermedia. Callitriehe autumnalis. Orchis pyramidalit. Juncus maritimus. Potamogeton undulatus. Car ex pauciflora. aquatilis. filiformis. Schlerochloa ngida. Triticum acutum. ADDITIONS TO COUNTY DERRY. Fapaver rheeas. Meconopsis cambrica. Viola canina. Sagina apetala. Spergularia salina. Ononis arvensis. Trifolium hybridum. Rubus rhamnifolius. gratus. pulcherrimus. Zindleianus. erythrinus. micans. chamoemorus. Myriophyllum spicatum. Galium mollugo. Hieraeium Zeyi. Sommerfeltii. Hieraeium stenolepis. euprepes. Myosotis collina. Veronica polita. Beta maritima. Atnplex erecta. Orchis pyramidalis. Spiranthes Romanzoviana. Carex teretiuscula. stricta. paludosa. rip aria. Trisetum Jlavescens. Ceterach oflcinarum. Chara aspera. contraria. vulgaris. Nitella translucent. As it must ever be, there has been in some cases doubt as to what plants, originally introduced, must now be included m the flora as ! ized, and which may be considered as not permanently esti ibhshed. . T™8*1™! ran settle these points, and we have preferred to err on the side of seventy rather than of leniency as regards admissions to the flora on the plea of naturalization. The number 0/ foreign plants introduced into the country is increasing, along with the increased imports of foreign grain and seed, and no doubt .some of t hardy continental species thus introduced have obtained, or will obto, a p manent footing in the island. The following extraordinary list of imported 1894-95-] X4X plants, collected by Mr. Richard Hanna in 1893 and 1894 in waste ground adjoining the Belfast Distillery, and near Hughes’ Flour Mill, will convey an idea of the number of aliens that are now-a-days showered down on our country : Ranunculus muricatus. T. latipaceum. Sisymbrium repandum. Trigonella coerulea ? S. pannonicum. Lonicera caprifolium. S. columnoe. Valerianella dentata. S. sophia. Anthemis cotula. S. thalianum. Hemizonia sp. Lepidium draba. Serratula tinctoria. L. campestre. Centaurea solstitialis. L. perfoliatum. Carduus crispus. Camelina sativa. Solarium nigrum. Reseda lutea. Echium vulgare. R. suffruticulosa. AmsincTcia lycopsoides. Saponaria baccaria. Salvia vcrticillata. Silene inflata. Stachys annua. S. dichotoma. Marrubium vulgare. Lychnis vespertina. Rlantago arenaria. Geranium phceum. Rumex palustris. G. pratense. Hemerocallis flava. Melilotus arvensis. Setaria viridis. M. parviflora. AZgilops ovata ? Medicago denticulata. IE. caudata. M. falcata ? Echinochloa crus-galli. Trifolium arvense. T. resupinatum. Bromus tectorum. The plants were introduced with foreign grain, Australian, Indian, Russian, and American. A smaller group found by Mrs White- Spunner at Grreenisland, whither they came with food for fowls, is given by R. LI. P. in Irish Naturalist for 1893. Sisymbrium sophia. Thlaspi arvense. Erysimum orientale. Lychnis vespertina. Linum perenne. Melitotus alba. Cichorium intybus. Hyoscyamus nigcr. Linaria sp. Galeopsis speciosa. Other similar lists might be quoted, but the above will serve as examples. During the interval since the publication of the Flora much has been done to extend our knowledge of the Musci and Hepaticce of the district. The workers, indeed, have been few, our notes being derived mainly from Rev. H. W. Lett and Rev. G. H. Waddell, to whose zeal and powers of observation we are indebted for by far the larger portion of the information summarised in the following pages. In 1888 the number of species of mosses known to grow in north-east Ireland 142 [Appendix B.N.F.C., stood at 293, and the hepatics, or scale-mosses, at 73. The present enumeration brings the former up to 301, and the latter to 84. Almost a moiety of the mosses known to occur in the British Islands, and more than a moiety of the scale-mosses, are still desiderata for our district. That in the future our lists will be added to cannot he doubted, especially in the minute and critical species. The publication of Dr. Braith waite’s splendid “ British Moss Flora ” has been a stimulus to present workers, and its completion cannot fail to stimulate and facilitate future researches. A similar Monograph of British Hepaticce would be a boon. That this interesting group of plants is still imperfectly known to us is largely due to the wrant of such help. The publishing of additional species is, however, the smaller portion of the labour of the local botanist. A great amount of work has been done, and much remains to be done, in extending our Knowledge of the range and frequency of the plants already on record. These lists might have been larger had a laxer method of compilation been adopted. Many notes have been held over where satisfactory specimens were not forthcoming, and doubtless some of these excluded records will prove correct hereafter. As regards the few notes of Antrim mosses by Mr. Dixon, they stand on the sufficient authority of that gentleman alone. Extracted from the Templeton MSS. we print at the end a number of localities for hepatics not included in the authenticated list. Many of these are believed to be reliable, while some are manifestly incorrect. No specimens are extant wherewith to test these notes, and their confirmation or otherwise remains for the future. ADDITIONS TO DISTRICT 12. Anisothecium crispum. Polytrichum attenuatum. Tot tula princeps. Grimmia orbicularis. G. Hartmani. Pohlia acuminata. Mnium riparium. Hypnum irriguum. Sphagnum Austini. S. teres. Lejeunea microscopica. Lejeunea Maclcaii. L. patens. Odontoschisma sphagni. Leptoscyphus pyrenaicum. Scapania umbrosa. Plagiochila tridenticulata. Jungermannia pumila. J. crenulata. Nardia sphacelata. Lunularia cruciata. ADDITIONS TO COUNTY DOWN. Polytrichum attenuatum. Mollia verticillata. Grimmia orbicularis. Pohlia acuminata. Bryum proliferum. Hypnum irriguum. H. Kneiffii. H. pulchellum. Sphagnum teres. Lejeunea Mackaii. Odontoschisma sphagni. Cephalozia divaricata. C. connivens. Leptoscyphus interruptus. Scapania umbrosa. S. curta. Jungermannia crenulata. Nardia sphacelata. Lunularia cruciata. Anthoceros punctatus. :894“95-l 143 ADDITIONS TO COUNTY ANTRIM. Oligotriehum incurvum. Pottia Starlcei. Anisothecium crispum. Webei'a sessilis. Grimmia trichophylla. G. Hartmani. Orthotrichum stramineum. Tetraplodon bryoides. Funaria obtusa. Mnium cuspidatum. M. riparium. Hypnum heteropterum. H. Borren. Sphagnum Austini. S. tenellum. S. intermedium. Frullania fragillifolia. Lejeunea microscopica. L. calcar ea. L. patens. L. Mackaii. Pleurozia purpurea. Odontoschisma sphagni. Trichocolea tomentella. Plagiochila tridenticulata. Jungermannia pumila. Nardia hyalina. Cesia crenulata. Lunularia cruciata. The only additions to County Derry are Polytrichum urnigerum, Pottia Heimii , Tortula princeps, Mollia inclinata , Bryum ventricosum and Sphagnum subsecundum var. obesum. Several named varieties are also added to preceding counties. In the systematic list which follows, the authors have personally examined specimens of the greater portion of the plants recorded, and have taken pains to satisfy themselves of the correctness of the remainder. In the case of critical plants, the opinion of an authority has in all cases been obtained and followed. All plants concerning the identity of which there was any doubt, have been omittted; a number of records of Rubi are held over for this reason. The sequence and nomenclature of Flora have been followed throughout for sake of uniformity, except in those critical genera where the greatly extended knowledge w hich now prevails rendered it necessary to introduce the present terminology— thus the Hieracia are arranged and named according to Mr. Hanbury’s list in Journal of Botany , July 1894, and Rev. Moyle Rogers has kindly revised our Rubus list so as to bring it into accordance with the ninth edition of London Catalogue. We have to acknowledge gratefully assistance received in their special departments from Mr. J. G. Baker, Mr. Arthur Bennett, Monsieur Crepin, Messrs H. and J. Groves, Mr. F. J. Hanbury, and Rev. W. Moyle Rogers; to all of whom, as well as the various local botanists who have contributed, our best thanks are due. For the editing of the Phanerogamia , and Cryptogamia as far as the end of Characece, R.L1.P. is responsible; S.A.S. is accountable for the Musei and Hepaticae. \bth May , 1895. 144 [Appendix B.N.F.C., ABBREVIATIONS. Herb. D.M. — Herbarium of Dr. David Moore, now in Dublin Science and Art Museum. Hart R.I.A. — H. C. Hart : Plants of some of the Mountain Ranges of Ireland. Proc. Royal Irish Academy , 1884. The one or two references to Mr. Hart’s subsequent report on the Mountain Plants of Ireland are dis- tinguished by the date 1891. Lett R.I.A. — Rev. H. W. Lett : Report on the Mosses, &c.,of the Moume Moun- tain district, Proc. Royal Irish Academy , 1890. S. & P. — Stewart and Praeger : Report on the Botany of the Moume Mountains, Proc. Royal Irish Academy , 1892. B.N.F.C. — Proceedings of the Belfast Naturalists' Field Club. B. E.C. — Botanical Exchange Club Report. Journ. Bot. — Journal of Botany . I. N.— Irish Naturalist. Shoolbred I.N. — W. A. Shoolbred, “A Botanical Trip to Co. Antrim,” Irish Naturalist, 1894. Groves I.N.— H. & J. Groves, “ The Distribution of the C haracece in Ireland,” Irish Naturalist, 1895. H W.L. — Rev. H. W. Lett, M.A. C. H.W.— Rev. C. H. Waddell, B.D. S.A.S. — Samuel Alexander Stewart. R.L1.P. — R. Lloyd Praeger. «894-95-] 145 PH ANEROGAMI A. RASTUWCUIACEJE. Thalictrum minus L., yar. (3 T. montanum Wallr. 300 — 1600 feet. Down — Pigeon Bock Mountain and Cove Mountain, S. & P. T. flavum L. Antrim — Langford Lodge, E.L1.P. Ranunculus tricbophyllus Chaix. Down — Lough. Leagh (E.L1.P.), B.F.F.C. 1891-2. Ditches below Newtownards, and pool on Conlig Hill, E.L1.P. Antrim — Stoneyford Eeservoir, E.L1.P. R. heterophyllus Fries. Down — Magheralin, C.H.W. Ditches near Crawfordsburn and Helen’s Tower, E.L1.P. “ Moneyreagh Eiver, ” printed in some copies of Flora , should he ‘ ‘ Money caragh Eiver.” R. Baudotii Godr. The plant recorded from Saintfield under this name in Watson B.E.C. Report 1893-94, is transferred to R. peltatus. R. floribundus Bah. Specimens from Clandehoye lower lake have been doubtfully placed under this form by A. Bennett in Watson B.E.C. Report 1891-2. Further investigation is required. R. penicillatus Dum. Antrim— Abundant in Main E. from Eandalstown to Lough Neagh, and in Braid E. at Ballymena, E.L1.P. R. peltatus Fries. Down— Greencastle, Lisnacree, and Lough Island Eeavy, S. & P. Common in the county, var. truncatus Hiern. Down — Ballyagherty near Saintfield, C.H.W. , Watson B.E.C. 1893-4 Lough Mann, C.H.W. R. circinatus Sihth. Down — In the Lagan Canal close to its junction with Lough Neagh, E.L1.P., B.N.F.C. 1892-3. An important extension of range. 146 [Appendix B.N.F.C., R. hederaceus L. 0 — 1000 feet in tlie Moumes, S. 8c P. R. flammula L. Ascends to 1700 feet in the Moumes, S. & P. var. p pseudo-reptans Syme. Down — Near Hilltown, S. & P. R. lingua L. Down— North side of Pollramer Lough, Richd. Hanna. Marshes south of Ballydugan Lake, R.L1.P. Derry — Near Dungiven, Mrs. Leebody. R. aurlcomus L. Down — Rostrevor, S. & P. Glen at Knocknagoney near Holywood, R. L1.P. Antrim — Cushendall, Herb. D.M. Glendun, S. A. Brenan. Stoneyford, Crumlin, Langford Lodge, R.L1.P. Derry — Near Bellarena, Mrs. Leebody. R. acris L. Ascends to 2450 feet in the Moumes, S. & P. var. p R. tomophyllus Jord. Down — Near 'Warrenpoint, S. & P. Perhaps frequent in the district. R. repens L. Ascends to 1300 feet in the Moumes, S. & P. Aquilegia vulgaris L. Down — By the Shimna Riyernear Newcastle, apparently well established, S. & P. It grows here on rough heathy ground, at a distance from any house, and has increased during the last ten years, R.L1.P. NYMPHiEACES. Nympbsea alba L. Down — In almost every lake and pond. Derry — Lakelets near Kilrea, and abundant in Killelagh Lough above Maghera, R.L1.P. PAPAVERACEJE. Papaver hybridum L. Down — Roadside half-way between Killough and Ardglass, R.L1.P., B.N.F.C. 1892-3. i894-95-] 147 P. rhoeas L. Dawn — Ardglass, S.A.S. Derry— Fields near Magilligan railway station, R.L1.P. The plant is still abundant at its old stations, Killough Bay and Lisburn. [P. somniferum L. Down — Abundant in field near Rostrevor, S. & P.] Meconopsis cambrica (Linn.) Vig. Down — Ascends to 1300 feet at Rostrevor, S. & P. It ranges up and down the valley for several hundred feet, being abundant at one spot. Derry— Magilligan braes, S. A. Brenan. Crlaucium flavum Crantz. Down — Mill Bay in Carlingford Lough, Leestone near Kilkeel, and re- found in Templeton’s station “ 5 miles south of Newcastle ” (Glas- drumman), S. & P. FUraAmACKJE. Fumarla capreolata L. var. a F. pallidiflora Jord. Common in Down and Antrim. Derry distribution not yet worked out. var. 8 F. muralis Sonder. Down— Saintfield, C.H.W. ; Watson B.E.C. Report 1893-4. F. officinalis L. Frequent throughout Down and Antrim. CSSITCIFERJE. Cheiranthus cheiri L. May fairly be reckoned as a naturalized plant in certain stations in the district, as ancient buildings at Quoile Castle, Carrickfergus Castle, and Larne. Nasturtium palustre (Willd.) DC. Down — Rostrevor and Narrow- Water, S. & P. Crossgar, R.L1.P. Antrim — Glendun, Sboolbred I.N. Busbfoot, R.L1.P. Barbarea vulgaris R.Br. Down — Frequent in the Mourne district, S. & P. Crawfordsbum, Newtownards, Ballygowan, Downpatrick, R.L1.P. Derry — Kilrea and Bellarena, Mrs. Leebody. 148 [Appendix B.N.F.C-', B. Intermedia Bor. Down — Moygannon, Rostrevor, Killowen, Newcastle, S. & P. Scrabo and Conlig, R.L1.P. Antrim — Stoneyford, R.L1.P. Derry— Kilrea, Mrs. Leebody. [B. prsecox R.Br. Down — Cultivated ground at Struell wells near Downpatrick, R.L1.P., B.N.F.C. 1892-3.] Arabis hirsuta (L.) R.Br. Antrim— Tievebulliagb Mountain, S. A. Brenan. Derry — Still plentiful in sandy fields and on sandhills at Magilligan, Mrs. Leebody, also R.L1.P. In Herb. D.M. is a note recording this plant from Cave Hill, Knockagh, and Torr Head, but we fear some mistake was made, as the plant has never been seen by any other botanist in these well-known places. Cardamine amara L. Down— Abundant at the “Witch Hole” on the Lagan at Glenmore near Lisburn, J. H. Davies; S.A.S., I.N. 1894. Sisymbrium thalianum (L.) Gaud. Antrim — Wall-tops about Larne, Herb. D.M. Cushendun, S. A. Brenan. Derry— Near Derry City, Mrs Leebody. Magilligan and Castlerock, R.L1.P. S. alii aria L. Down — Scarva Glen, H. W. Lett. Antrim — Magheragall near Lisburn, and Altmore Glen, R.L1.P. [Erysimum cbeirantboides L. Antrim — Wheat-field and roadside between Ballinderry and ‘Lisburn, Herb. D.M.] Sinapis alba L. Down — Abundant in fields about Killowen, S. & P. Ardglass (R.L1.P.), B.N.F.C. 1892-3. Draba incana L. Derry — Magilligan sandhills, small and not abundant, Mrs. Leebody, 1890. Abundant and fine on sand-dunes a mile N.E. of Magilligan railway station, R.L1.P., 1894. Still occurs sparingly on Benevenagh cliffs. 894-95.] H9 D. verna L. Down— Ballywalter and Ardglass, Templeton MSS. Saintfield, C.H W Antrim— Roadside near Stoneyford, R.L1.P. Cochlearla danica L. Down-HentiM from Warrenpoint to Greencastle, and at Annalong, Antrim— On limestone rocks, White Park, Herb D M De^eSl:reSetkLlt°dy- °— by Ba“ [Camelina sativa L. Down-Newtownards, E. F. I.inton, 1871, Herb. F. J. Hanbury. An%^an!aE.Ll1pS’ Br0ughshane> Herb- Canon Grainger. Lame Derry— Magilligan, Herb. D.M. Among flax above Garvagh, B.L1.P.] Thlaspl arvense L. Down— Abundant in fields at Killowen, S. & P. Iiepldium campestre (L.) R. Br. Down — Fields at Killowen, S. & P. Antrim— Ram’s Island, H.W.L. I.. Smitbii (L.) Hook. Antrim — Glenravel, R.L1.P. Derry— Kilrea and Garvagh, Mrs. Leebody. Senebiera coronopus (Gaert.) Poir. Down— Rostrevor, Killowen, Kilkeel, Annalong, S. & P. [S. didyma Pers. Down — Killougb, C.H.W. Railway at Dundrum, S.A.S. Antrim — Giant’s Causeway, Miss Knowles. Derry— Portstewart, Mrs. Leebody. Apparently increasing in Ireland, and spreading northward.] Cakile maritima Scop. Antrim— Beach at Ballintoy, R. Brown ; J. Britten, Journ. Bot. 1888, 150 [Appendix B.N.F.C., Raphanus raphanistrum L. Dundonald, Ballykinler Down- Frequent in Monrne district, S. & P. Dundonaia, ua y Dundrum, E.L1.P - -- Anto-wot in " cornfields tough the county, Herb. D.M. Rathlin Island, It. L1.P. Rathlin Island, i a. r . , p ti p Derry — TJpperlands, Kilrea, Garragh, and Bann moutli, R.L . . ». maritimus Sm. and plentiful torn Killough Down— Store near Ballywa > • j [894. Cranfieid coast - to St. John’s Point, S.A.S. , S.A.&., ± .*• guard Station, S. & P- RESEDACE51. Reseda lutea L. Certainly naturalised at Ballycastle, and probably at Magheramome also. VIOLA-CEJE. , eaic T To 1350 feet in the Moumes, S. & P. Vi0laDoClFre4uentmtbe Moume district, S. & P. Near Loughbrickland, H.W.L. Anto-Cmamon on the hills and bogs ; many stations might be given. V. sylvatlca Fries. Ascends to 2796 feet. Hart X.I.A V- -Sbores'of SJ ^nTCi^atord, and Bloody Bridge, Antrbn— Cusbmidm^^boolbred' I.N. Barn’s Island, Busbfoot, BaBy- Derry-Kilrea^Mrs. Leebody. Common about the Bann mouth, E. Ll.P. V. lutea Huds., var. p V. Curtlsll Forst. Down— Margin of Castlewellan Lake, S. & P_ Antrim— Cushendun, Ballycastle, Bushfoot, E.L1.P. SROSERACES. Drosera rotundlfolia L. To 1550 feet in the Moumes, Hart B.I.A. To 1450 feet there, S. & P- 1894-95.] I5I intermedia Hayne. D°™7C® Bridge “T UVame ft^T \Sgy " same place, S. & P. 6 stream’ and m marshes S.W. of The vague record in Irish Flora is thus verified Th;* to have been known to Templeton, who writes (MSS Wm,ld appear Stalk scarcely longer than the hires lansule c™/ i AU Dros«a Iongifolia. m great abundance along with D. rotundifolia and hl tbree salved ; found the head of Kilkeel River, Mourne Mountains, August ^fth^USS noted that we did not find I), analica there or eliww ’ •!' 3.Tt must be another note, after accurately describing D ' analica 1 ? tb° .dlstnct- In common on most of our bogs B Sfnli'n T l ’ Tfmpleto ? wntes - this is watery hog at the head of liikefl °n the B. angllca Huds. ****** Herb. Derrr0tI '°bWland 1°™““’ thrWout northern AnWm^E.uT ’ coirne- K- Br°™; j- Garyagh, and on the Lrgin of I?ear1K:ilrea a“d Mountains, R.L1.P. S 0Ugh 0uske ln th« Sperrin POlYGAlACEa. Polygala vulgaris L. To 2394 feet in the Moumes, S &P Tar' do!: rrra wfe- To 1720 feet in s. & p Down-In the Moumes, but not common, S. & p. BaUygowan R LI P Antrim Common on the north Antrim coast, Shoolbred 1.1V. var. y P. g-randiflora Bah. Derry— Still sparingly on Benevenagh (R.LI.P.) B.JST.F.C. 1892-3. „ ELATIWACEJE, B. nydropiper L. D°™:“l890-Le n0rttend °f L0USh BricUand' =• "-L. ; K-L1.P., The record 11 Near Belfast, Dr Mafppr ” f winv ttj + \ s. to he correct, as shown by a large series of Lf ^0 tu™s °ut unexpectedly the iate Dr. Boswell, now in possession of Mr. F TH^nbur^ tmeh^erbarlum of which have been examined by R LI P hear tfip fr 7' Tb? specimens, mark, Co. Antrim CoU aI fli if label L Lagan Canal near h. tide were, no doubt, intended for' cLribution through Z BotenicAE^h’’ It appears improbable that the plant still survives fn^is 8faf!nEXCha?nge °lub* is now impure, and attempts to refind it have failed ’ ^ b® Water 152 [Appendix B.N.F.C., CARIOPHTIIACSa:. ^SaP°Domi-Bloody Bridge, S. & P. Mountstewart and Hillsborough, B.L1.P Antrim— Portballantrae, B Ll.P.] Silene anglica L. _ « * P Down— By the Annalong Eiver, Hart Jt.I.A. Hdltown, S. & P. Derry Still abundant at Magilligan, Mrs. Leebody, and B.L1.P. S. inflata Smith. _ ^ « v Down— Frequent in the Mourne district, S. & P. Dundonald, Conhg Hill, Ballynahinch, B L1.P. Antrim-Shore of Lough Neagh at Shane’s Castle, Herb. D.M. Basharirin, B.L1.P. S. maritlma With. . , ,AA Down-Abundant on Conlig Hill, some miles from the sea, at 400-500 feet elevation, B.L1.P . S. noctiflora L. Down— At Holywood, but only as a casual ; not seen for some years on Bough Island ; seems to he uncertain in its appearance, B.L1.P. TS. dicbotoma Ehrh. ^ Down— Abundant in several corn-fields between Saintfield and Crossgar. D0WD. BeLond, also C.H.W., 1894. A plant of southern Europe, introduced with seed, apparently not hitherto observed m Ireland.] Lychnis vespertina Sibth. Down— Fields between Downpatrick and Strangford, B.N.F.C. , 1893-4. li. diurna Sibth. , ^ Antrim— Plentiful about Cullybackey, Miss Knowles. Shane s Castle, B.L1.P. Xu ffitbago L. Down — Maggie’s Leap and Killowen, S. & P. Derry— Fields at Bann mouth, B.L1.P. Sacina ape tala L. , Down — Warrenpoint, S. & P. Comber, Saintfield, Tullymurry, an near Pointzpass, B.L1.P. **94-95-] 153 Antrim— Whitehead, R.L1.P. Derry— Walls at Magilligan railway station, R.L1.P. S. cillata Fries. Down — Sandhills at Newcastle, S. & P. S. maritima Don. Newcastle- S- & P' Donaghadee and Mahee 6’ E' Br0W“ ; J‘ Britte“’ J°Urn ' B0L> 1888' S. nodosa (L.) E. Meyer. Do™-d"r^uigtsii7PWater- s- & p- “ Park De^“qU' 3ECrEMLLp!igan and *“ m°Uth> MrS- Leei°dy> Arenaria verna L. Antrim — Glenariff, Shoolbred I.N. Scawt Hill, R.L1.P. A. trinervia L. Down— Rostrevor, and about Tollymore Park, S. & P. Antrim— Glenarm, Herb. D.M. Ram’s Island, H.W.L. Rallycastle and White Park (R.L1.P.), B.N.I.C. , 1892-3. Derry— Dungiven, and near Limavady, Mrs. Leebody. A. serpyllifolia L. Down— Rockport and Downpatrick, R.L1.P. Antrim— Cushendall, Herb. D.M. Near Antrim, D. Redmond head, Cushendall, Bushfoot, R.L1.P. Between White- Stellaria ulig-inosa Murr. Ascends to 2450 feet, S. & P. Cerastium triviale Link. yar. p. c. bolosteoides Fries. Derry— Abundant in meadows on the south side of the Bann below the S^SinatXrfe’ MrS- A - C. tetrandrum Curtis. Down— Rostrevor and Killowen, S. & P. Kirkiston, C.H.W. Rock- port, ix. LI. Jr . AntnE Li1?*1111 Mand’ K’U-P-> 1889-90. Cushendun, [Appendix B.N.F.C., 154 Derry— Benbradagh, Mrs. Leebody. Spergularia rubra (L.) Pers. Down — Abundant on the shores of Lougb Island Heavy , S. & P. 8. salina Presl. Derry— Near Limavady Junction, Mrs. Leebody. Sclerantbus animus L. D0wn —Frequent in the Moume district, S. & P. Derry — Near Kilrea, R.L1.P. MALVACEJE. XVXalva moscliata L. Down— Loughbrickland, H.W.L., I.N., 1893. Tullyveery near Saint- field, C.H.W. Between Dundonald and Comber, and near Tullymurry, R.L1.P. Antrim— Shane’s Castle deer-park, Herb. D.M. M. rotundifolia L. Down— Frequent from Killowen to Seafield, S. & P. Xiaratera arborea L. Antrim— “ On the Shore at Ballantoy and grows also in the Sheep Island about i mile from the Ballantoy shore; Sept., 1797,” R. Brown. Still grows on Sheep Island, S. A. Brenan. Summit of Stackams- kan, an isolated sea-stack at western end of Rathlin Island, R.L1.F., I.N., 1893. We have no doubt that the plant is truly wild in these inaccessible maritime situations. HYPlKICACEiE. Hypericum androssemum L. Antrim - Cully backey, Miss Knowles. Magheragall near Lisburn, Cairncastle, Cushendall, Fair Head, R.L1.P. Derry— Maghera, Kilrea, and Garvagh, R.L1.P. H. perforatum L. Down— Near Newry, H.W.L. Tullymurry, R.L1.P. Antrim — Ram’s Island, R.L1.P. Derry — Eglinton, Mrs. Leebody. Kilrea, R.L1.P. *894-95-] 155 H. quadrang'ulum L. (Ex. p.). yar. p H. macnlatum Bab. Down— By the Lagan Canal two miles above Lisburn, Bichd. Hanna. Abundant by the Lagan Canal close to Lough Neagh, H.W.L. and L.M. W . Near Manno railway station, ft. Ll.P. Antrim— Glenmore near Lisburn ( J . H. Davies), B.N.F.G. 1892-3. H. humifusum L. To 800 feet in the Mournes, S. & P. D0WErJpqUent ^ ^ Mournes’ S‘ & P- Scrabo and Ballynahinch, H. pulchrum L. To 2000 feet in the Mournes, S. & P. H. elodes Huds. To 650 feet in the Mournes, S. & P. D°wn-Several stations near Bryansford, Castlewellan, and Kilkeel, Derry— Ballyamott raee-course, Mrs. Leebody ; S.A.S., I.N. 1894. GERANIACEjE. [Geranium striatum L. Down— Abundant in a lane near Comber, R.L1.P. Antrim— Near Ballinderry, W. D. Donnan.] G‘ sylTa*lcun? f1- R.L1.P. considers that Marino, where this plant grew (but suspiciously near a garden) until some ten years ago, was probably the “Holy wood r station of Flor. JJlst. The localities “ Glenarm deerpark, and glen above Milltown at Cairn- castle, given m Flor. N.E.I. for G. pratense, belong to G. sybaticum. ike range of these two plants in Antrim (and in Ireland) is thus seen to e very limited and well-defined, G. sybaticum being confined to a few square miles m the vicinity of Glenarm, on the east coast of Antrim, wkile G. pratense is found along the north coast from Portrush to Bally- castle, a distance of some twenty miles. *■ JhrfjKAz"4 “ Ireland by TemPlet0n’ «* b7 M°ore> as The Glenarm and Caimcastle stations of Flora are transferred to G. G. perenne Huds. Down— Roadside near Castle Espie, C.H.W. Antrim— Roadside near Whitewell quarries on Cave Hill, W. D. Donnan ■ R.L1.P., B.N.F.G. 1892-3. G. lucidum L. Antrm-Torr Head, Herb. D.M. Glenariff, Shoolbred I.K. Antrim, w b .Smith. Scawt Hill, and lake-shore west of Shane’s Castle, xt.Ll.P. [Appendix B.N.F.C., 156 Erodium cicutarium L’Herit. 0 — 1200 feet. Down — Abundant on the Mourne coast-line; also at Bryansford and Castlewellan, 2 and 4 miles from the sea, S. & P. Holy wood Hills, in fields at 400 feet, R.L1.P. Antrim— Larne, Cushendun, White Park Bay, E.L1.P. Derry— Summit and base of Benevenagh cliffs, B.N.F.C. 1892-3. The plant grows here at an elevation of 800—1200 feet, associated with Silene acaulis , S. maritima , Dryas octopetala, Salix herbacea, and other alpines. E. moschatum L’Herit. Down —Annalong, Hart R.I.A ; and subsequently, S &P Waste ground south of Killough, Bichd. Hanna , S.A.S., I.N. 1894. Eohert Brown, in the MS. referred to in the Introduction, notes tins species as “ growing abundantly at the west end of the suburbs of Londonderry, Sept. 29th, 1795,” and “ near Carrickfergus, July, 1797- _ It has not been found in either of these stations by any recent observer, and it seems probable that A. cicutarium was the plant seen. E. maritimum L’Herit. Down— Abundant at Ballykinler, R.L1.P. Still at KirHston, C.H.W. LIWA CE2E. and at Causeway Radiola linoldes (L.) Gmel. Down— » Water, S. & P. Antrim — Abundant on Bushfoot sandhills, R.L1.P. CEEASTRACEJE. Euonymus europaeus L. Down— Warrenpoint, Annalong, Newcastle, S. & P. Lough Leagh and Castle Espie, C.H.W. Near Ballynahmch, Eichd. Hanna. Near Hillsborough, S.A.S. Clough and Killyleagh, E.L1.P. Antrim-Muckamore Glen (R.L1.P.) B.N.F.C. 1893-4. Cullybackey, Miss Knowles. Basharkin, S. A. Brenan. RBAMTSTACEJE. Rhamnus catharticus L. Antrim— Abundant on the shore of Lough Neagh at the place called the Selchin, Parish of Glenavy, Herb. D.M. Thrs is another L°ugh Neagh record of a shrub that seems now quite lost through drainage. i894-95-J 157 Templeton notes this plant (MSS.) Carrickfergus, June 30th, 1804.” as it was formerly a notable plant, It has not been found there since. *‘in a hedge about 2 miles beyond It may have been planted there, being much used medicinally. R. frangula L. Antrim— Bushy places near the River Main in Shane’s Castle Park, Prof. R. 0. Cunningham ; R.L1.P., B.N.F.C. 1890-1. The only recent record of this species. XiRGUBXXCTOSJE. Ulex europaeus L. Rises in the Mournes to 820 feet, Hart R.I.A. ; to 800 feet, S. & P. ’ TT. Gallii Planch. Upper limit in the Mournes 1600 feet, Hart R.I.A • 1500 feet, S. & P. ; at 1650 feet on Slieve Rearnagh, R.L1.P. Down — Aghaderg parish, H.W.L. Sarotbamnus scoparius L. To 800 feet in the Mournes, S. & P. Ononis repens L. D°W?^TSf^ & P' MarPn o£ Lough Leagh (R.L1.P.), B.N.F.C. 1891-2. Iield at Loughbrickland, H.W.L.8 Derry— Benone at Magilligan, sparingly, Mrs. Leebody. var. p horrida Lange. Down — Sandy shore at Ardglass, C.H.W. O. spinosali. has not been re-found in Co. Down, and was, no doubt a casual, S.A.S. ’ Medicago lupulina L. Down-Common in the Mourne district, S. & P. Conlig, Ballykinler Tullymurry, Killowen, R.L1.P. 3 ’ Antrim Ballycastle, Redbay, Shane’s Castle, Portmore, Whitehead Cave Hill, R.L1.P. ’ [M. sativa L. Down— Fields at Cultra and Craigavad, R.L1.P.] [Melilotus officinalis Willd. Antrim— Glenariif, Shoolbred /.Ah] 158 [Appendix B.N.F.C., 1 VL. arvensis W. Antrim — Still abundant at several places between Kilroot and Larne, as it has been for the last 25 years, and may fairly be considered naturalized here. [IVT. parviflorus Lam. Antrim — Waste ground, Duncrue St., Belfast, R.L1.P.] Trifolium medium L. Antrim— Throughout the county ; many localities might be added. Derry -Railway banks between Coleraine and Castlerock, R.L1.P. T. arvense L. Down — Ballykinler sands, R.L1.P. Antrim — Carrickfergus, Cushendall, Ballycastle, Herb. D.M. T. hybridum L. Frequent in sandy cultivated fields and waste ground, and thoroughly established as a colonist, S.A.S., I.N., 1894. Down and Antrim— Frequent. Derry -Kilrea, and sandy fields at Bann mouth, B.L1.P. [T. resupinatum L. Down— Saintfield, C.H.W.] T. procumbens L. Down — Frequent in Mourne district, S. & P. Shore-line below Holy- wood, and Ballykinler, B.L1.P. Antrim -Cushendall, Herb. D.M. Glenarm, R.L1.P. Derry — Eglinton, Mrs. Leebody. lotus corniculatus L. To 1200 feet in the Moumes, S. & P. var. y 1. crassifolius Pers. Derry— Bosses Bay on the Foyle, Mrs. Leebody. 1. pilosus Beeke. To 1150 feet in the Mournes, S. & P. Down-Magheralin and Saintfield, C.H.W. Loughinisland, B.L1.P. Antrim— Glenariff, Shoolbred l.N. Ballymena, and plentiful at Eacavan, Miss Knowles. Cushendun, S.A. Brenan. Mazetown, and Caim- castle, S.A.S. Basharkin, B.L1.P. Derry— Frequent in North Derry, Mrs. Leebody. Kilrea, Garvag , Maghera, and Coleraine, R.L1.P. i894-95-] iS9 Vlca sylvatica L. Down—Bimka by the sea near Bloody Bridge, but not found elsewhere in Mourne district, S. & P. In a quarry by the railway north of Dundrum, plentiful, R.L1.P. Antrim— A var. with pure white flowers on limestone rocks between Larne and Glynn, Herb. D.M. Upper part of Colin Glen, and by the railway between Lambeg and Dunmurry, J. H. Davies. Glenariff, Sboolbred I.N. Altmore and Culraney, R.L1.P. V. orobus] (L ) DC Not found at Rostrevor (see Mali Syn. ed. II and Ffora N.E.I.) by S & P. Sherard’s plant may have been V. sylvatica, which Templeton found there. The specimens in the Sherardian herbarium at Oxford do not settle the question. V. sepium L A white-flowered variety grows about Glenmore near Lisburn (J. H. Davies) and at Marino (R.L1.P). V. ang-ustlfolia Roth. in Mourne district, S. & P. Kirkiston, C.H.W Killy leagb, R.L1.P. Antrim— Rallycastle and Cusbendun, Herb. D.M. Whitehead and Rasbarkin, R.L1.P. Down — Frequent Greypoint and V. lathyroides L. Down — Ballymacormick Point, R.L1.P. Antrim — Cusbendun, S. A. Brenan. Derry— Still at Magilligan, Mrs. Leebody. Lathyrus macrorrhizus Wimm. To 1,000 feet in the Mournes, S. & P. var. (3. I,, tenuifolius Roth. Down — Rostrevor, S & P. ROSACEiE. Prunus communis L. To 1,000 feet in the Mournes, S. & P. P. insititia L. May fairly be considered as naturalized in the district. P. padus L. Antrim — Refound in Glenshesk, Sboolbred I.N. P. avium L. Derry — Walworth Wood near Londonderry, Mrs Leebody. i6o [Appendix B.N.F.C., P. cerasus L. Down — Crawfordsburn, Clandeboye demesne, and ^Annalong, R.L1.P., B.N.F.C. 1890-1. Near Crossgar and Downpatrick, R.L1.P., B.N.F.C. 1892-3. Antrim — N ear C arnmoney church , plant ed , S . A . S . Bally castle , R.L1.P ., B.N.F.C. 1892-3. Glendun, and Bashar kin, R.L1.P. Derry — Near Draperstown, R.L1.P., B.N.F.C. 1892-3. Not unfrequent, and although no doubt planted in some of its stations, in others appears naturalized. Sanguisorba officinalis L. Down— Refound near Donaghadee, growing abundantly and luxuriantly on a railway bank, J H. Davies ; S.A.S., I.N. 1894. Poterium sanguisorba L. Antrim — Abundant in a meadow at Glenmore near Lisburn, J. H. Davies, I.N. 1892. The late Mr. More inclined to the view that it had been introduced in this station. It has continued abundant during the three years it has been under observation, but is apparently confined to one meadow. The geological formation is New Red Sandstone, but the Chalk is not far away. Agrimonia eupatoria L. Down — Killowen, S. & P. Anadroghal near Lough Neagh, H.W.L. and C.H.W. Near Greypoint, Ballykinler, and Tullymurry, R.L1. P. Antrim — Very frequent. Derry — Kilrea and Magilligan, Mrs. Leebody. A. odorata Mill. Down — Roadside near Steamboat quay, Downpatrick, R.L1.P., B.N.F.C. 1892-3. Antrim — Glendun, Shoolbred I.N. Alchemllla vulgaris L. To 1500 feet in the Moumes, S. & P. var p A. minor Huds. Down — Scrabo Hill, R.L1.P. Antrim — Binnagee near Carnlough, W. D. Donnan. Knockagh and Dunloy, R.L1.P. The recent paper by Rev. E. F. Linton on British forms of Alchemilla vulgaris ( Journ . Bot., April, 1895), and an examination of local specimens kindly made by that botanist, show that the above nomenclature needs revision. What was treated as type in Flora should now be quoted as var. A. alpettns Schmidt ; it is common in our district. The var. A. minor of Flora must now *894-95*3 i6i be called yar. A. filicaulis Buser; it is frequent on the basaltic plateau of Antrim and Derry. . Restricted A. vulgaris L. {—A. pratensis Schmidt) probably occurs in our district also, but has not yet been separated. Potentilla reptans L. Down — Rostreyor, Killowen, and Newcastle, S. & P. Holy wood and Millisle, R.L1.P. Antrim— Carrickfergus Junction, R.L1.P. P. tormentilla Sibtb. var. |3 P. procumbens Sibth. Down — Rostreyor and Newcastle, S. & P. Marino, R.L1 P ; S A S I.N. 1894. Antrim— Glenariff, Glendun, and Glenshesk, Sboolbred I.N. Area in front of Belfast Museum, S.A.S., I.N. 1894. Derry Sandy fields at Bann mouth, and frequent in Kilrea district R.L1.P. P. procumbens x tormentilla (P suberecta Zimmeter). Down— Newtownbreda, 1849, Dr. Mateer ; E. S. Marshall, Journ. Pot 1894, and W. H. Purcbas, ibid . Antrim — Glenshesk {fide Marshall), Shoolhred I.N. Rubus ldaeus L. To 1,400 feet in the Moumes, S. & P. R. suberectus Anders. Down— Margin of Castlewellan Lake, S.A.S., P.JE.C. Peport 1893. This is the plant which is recorded as P. ammobius by S. & P., on the authority of Prof. Babington. Dr. Focke, the describer of the latter species, has examined our plant, and places it under P. suberectus. R. pH cat us W. & N. Down— Aughnadarragh near Saintfield, C.H.W. R. Rogrersil Linton. Down— Old hog in Saintfield demesne, and boggy ground by Aughna- darragh Lake near Saintfield, C.H.W. R. nltldus W. & N. D°W?7~Margin °f Altnadua La1«b S. & P. (as var. hamulosus, which Mr. Rogers remarks appears to be exactly typical nitidus). R. carpinifolius W. & N. Down— Newcastle and Moygannon Glen, S. & P. Loughbrickland, H.W.L. [Appendix B.N.F.C., 162 R. Iiindleianus Lees. Down — Two stations in Aghaderg parish, H.W.L. Antrim — Glenariff and Glendun, Shoolbred I.N. Derry — Ballinderry, S. A. Brenan, Journ. Bot. 1895. R. erythrinus Genev. Derry — Ballinderry, S. A. Brenan, Journ Bot. 1895. R. rhamnifolius W. & N. (Sp. collect.) Down — Between Belfast and Holywood, J. Ball ; W. 0. Focke, Journ. Bot. 1891. Between Ballyvarley and Gilford, H.W.L. Castle- wellan Park, S.A.S. Antrim— Glenariff and Glendun, Shoolbred I.N. Caimcastle, S.A.S. Derry — Magilligan, ,T. Ball; W. 0. Focke, Journ. Bot. 1891. S. A. Brenan’s Ballinderry record in Journ. Bot. 1895 is doubtful. R. nemoralis P. J. Muell. (Genev. non Bab.) Down — By the White water at Donard Lodge, S. & P. (as macro- phyllus var. umbrosus Arr.) var. b. glabratus Bab. Down — By Ghann River, S. & P. (as R. macrophyllus var. glabratus Bab.) R. pulcherrimus Xeum. Down — Lisdalgan near Saintfield, C.H.W. ; S.A.S., I.N. 1894. Ballin- taggart in Aghaderg parish, H.W.L. By Castlewellan Lake, S.A.S. Antrim — Cave Hill, Glenariff, Glendun, and between Cushendall and Knocknacarry, Shoolbred I.N. Derry — Ballinderry, S. A. Brenan, Journ. Bot. 1895. It. Muenteri Marss. Antrim — Colin Glen, J. Ball ; W. 0. Focke, Journ. Bot. 1891. Mr. Rogers considers that this form cannot as yet be included in British lists. R. villicaulls Koehl. Antrim — Glenariff and Glendun, Shoolbred I.N. Derry — Ballinderry, S. A. Brenan, Journ. Bot. 1895. var. b. Selmerl (Lindeb.) Down — Saintfield, C.H.W., I.N. 1894. Between Scarva and Gilford, and at Dromorebreague in Aghaderg parish, H.W.L. Drumeronear Magheralin, C.H.W. *894-95-] 1*3 Antrim— Glendun, Shoolbred l.N. Derry — Ballinderry, S. A. Brenan, Journ. Bot. 1895. R. gratus Focke. Antrim — Glendun, H.W.L. Derry— Ballinderry, S. A. Brenan, Journ. Bot. 1895. R. pubescens Weihe. (Sp. collect.) Down — Carrickmannan near Saintfield, C.H.W. R. silvaticus W. & N. Down— Between Milltown and Clonallen, H.W.L. Saintfield, C.H.W. R. macrophyllus W. & N. Down --White Water, Altnadua Lake, and Tollymore Park, S. & P. Saintfield, C.H.W. Agbaderg parish and Hillsborough, H.W.L. Derry — Ballinderry, S. A. Brenan, Journ. Bot. 1895. var. b. R. Schlechtendalii (Weihe). Down— Moygannon Glen, S. & P. Saintfield, C.H.W. Loughbrick- land, H.W.L. R. micans Gren. and Godr. Derry— Ballinderry, S. A. Brenan, Journ. Bot. 1895. R. pyramidalis Halt. Down— Tollymore Park and Donard Lodge, S. & P. Saintfield. C.H.W. Antrim — Glenariff, Shoolbred l.N. R. leucostachys Scbleicb. Antrim— Cave Hill, near Larne, Glenariff, Shoolbred l.N. Derry— Ballinderry, S A. Brenan, Journ. Bot. 1895. R. mucronatus Blox. Down— Saintfield, C.H.W. R. Gelertii Frider var. h. criniger Linton. Down — Aghaderg glebe at Loughbrickland, H.W.L. R. leyanus Rogers. Down— Saintfield, C.H.W. ; Watson B.E.C. 1898-4 (as B. Brejeri). “Very strong, and differing from the ordinary English plant.”— W. M. Rogers. 164 [Appendix B.N.F.C., R. radnla Weihe. Down — Aghaderg glebe at Loughbrickland, H.W.L. Antrim — Hedgerows near Larne, Sboolbred I.N. Derry — Ballinderry, S. A. Brenan, Journ. Bot. 1895. R. echinatus Lindl. Antrim— Cave Hill, Glenariff, Glen dun, Sboolbred I.N. R. rudis W. & N. Down — Agbaderg glebe at Loughbrickland, H.W.L. “ Hardly typical,” W. M. Rogers. R. scaber W. & N. Down — Aghaderg glebe at Loughbrickland, H.W.L. S. A. Brenan’s Ballinderry record in Journ. Bot. 1895 is omitted as doubtful. R. fuscus W. & N. Down — Two stations in Aghaderg parish, H.W.L. R. rosacens W. & N. Down — Near Maralin, H.W.L. (“ var. near infecundus ,” W. M. Rogers.) var. b. R. hystrix (W. & N.) Antrim — Glenariff, Shoolbred I.N. R. Koehler! W. & N. Down — Newcastle, S. & P. Antrim Glenariff and Glendun, Shoolbred I.N. var. b. R. pallldus Bab. Down— Tollymore Park, S. & P. Saintfield, C.H.W ; S.A.S., I.N. 1894. Near Scarva and at Loughbrickland, H.W.L. R. hirtus W. & K. var. c. R. Kaltenbachii Metsch. Down — Ballintaggart in Aghaderg parish, H.W.L. R. dumetorum W. & N. Antrim — Cave Hill, and near Larne, Shoolbred I.N. Glendun, S. A. Brenan, Journ. Bot. 1895. var. b. R. diversilolius (Lindl.) Down — Tn Aghaderg parish, H.W.L. R. corylifolius Sm. Ascends to 1400 feet in the Moumes, S. & P. 1894-95*] ^5 a. R. sublustris (Lees.) Common, yar. b. R. conjungrens (Bab.) Antrim — Near Larne, Sboolbred I.N. Many localities might be added. R saxatiMs L. 800-2000 feet in the Mournes, S. & P. Down-Frequent on the Mourne Mountains, S. & P. Antrim— Knockagh, in fine fruit (R.L1.P.), B.N.F.G. 1892-3 Derry— Heathy places near Kilrea, R.L1.P. R. cbamsemorug L. Derry— A small patch on the Derry side of the county boundary on the west side of Dart Mountain, H. O. Hart, Jowl. Sot. 1892 and Hart and Barrington, I.N. 1892. A most interesting confirmation of Prof. Murphy’s record ( Flora Hibernica). S mation Geum Intermedium Ehr. Antrim-Near Muckamore, (K.L1.P.), B.N.F.C. Excursion; I.N. 1893. G. rivale L. Down Decidedly rare in the county Absent from the Mourne district, S. & P. Only obseryed m the glen at Holywood Waterworks, in the Mournes— a remarkable Rosa spimosissima L. To 2000 feet elevation, S. & P. yar. R. cipbiana Sibbald. Derry— Magilhgan, Mrs. Leebody. R. hibernica Sm. var. b. glabra, Baker. Down— Tillysburn, S.A.S. M. Crepin places the Tillysbum plant s: “ un ueu nnhpsnonfo ” rr,. — He considers spinosissima under this variety, adding “ un peu pubescente. U hibernica a hybrid— ft. pimpinellifolia x canina x canina. [R. pomifera Herm. Antrim— Woods in Shane’s Castle Park, S.A.S.] R. involuta Sm. Down— Mountain roads about Hilltown (aggregate), S & P Antrl>rG1™d'm (“form,” W. M. Rogers), S. A. Brenan. Top of Cohn Glen Mora Belfastiemis (A. Sabini). This record was considered doubtful, but a specimen gathered there by S A S in 1894 has been identified by M. Crepin. * 1 66 [Appendix B.N.F.C., var. E. SaUni -Woods. The Braid Valley plant recorded in I.J ., 1894, p. 221 is not R. Sabini ; nor can we be quite sure of the Hilltown plant of S. & . r. mollissima Willd. Down— Near Dundrum, by the Quoile at Downpatrick, and at Ballyna- bincb, S.A.S. Antrim — W aterloo near Lame (E.L1.P.), B.N.F.C 1890-1. Glendun and Glensbesk, Sboolbred I.N. Rasharkin, and between Ballymena and Brougbshane, R.L1.P. Derry — Common near Kilrea weir, R.L1.P. R. tomentosa Smith. To 980 feet in tbe Moumes, S. & P. var. d. scabriuscula Sm. Antrim— Near Cushendall, Sboolbred I.N R. rubiglnosa L. . T n> Down— Hilltown, S.A.S. Near Comber and Downpatrick, K.L1.P. Antrim— Sbane’s Castle, Ram’s Island, Dervock, Rasbarkin, R.L1.P. Derry— Frequent in North Derry, Mrs. Leebody. Portglenone, R.L1.P. E. micrantha Smith. This species must be deleted from our flora. Tbe Cusbendun plant has been finally decided to be R. rubigwosa. R. canina L., var. a. lutetiana (Leman). Down — Comber, S.A.S. Antrim— Common in tbe glens, Sboolbred I.N. Lame and Caimcastle, S.A.S. var. e. dumalis (Becbst.) Antrim— Common in tbe glens, Sboolbred I.N. Crumhn, Ballygilbert north of Caimcastle, and near Belfast, S.A.S. var. j. dumetorum (TbuiR.) Down — Killowen, S.A.S. Antrim — Mazetown, S.A.S. var. n. tomentella (Leman). Antrim— Colin Glen and Crow Glen, S.A.S. var. w. subcristata Baker. Antrim— Glendun, and sandy ground by tbe river in Glensbesk, Sbool- bred I.N. R. glauca Vill. . , Antrim— Near Belfast, and Waterloo near Lame, S.A.S. Determined by M. Crepin. 894-95-] 1 67 R. arvensis Huds. Down-South of Rostrevor, and near Bloody Bridge, S. & P. Between Crossgar and Killyleagh (R.L1.P.), JB.N.F.G. 1891-2. Rademon, Kilmore near Crossgar, and Saintfield, C.H.W. Loughinisland, R.L1.P. Antrim — Near Ballinderry, R.L1.P. var. c. bibracteata (Bast.). Antrim— Hedgerow near Cushendun, Shoolbred I.N. Crataegus oxyacantha L. To 1000 feet in the Mournes, S. & P. Pyrus malus L. Down— Frequent in Mourne district, doubtfully native, S. & P. Antrim — Frequent about Stoneyford, R.L1.P. Derry— Bond’s Glen, Mrs. Leebody. Upperlands and Kilrea, R.L1.P. P. aucuparia Gaert. Antrim '-Ratblin Island, R.L1.P., JB.N.F.G. 1889-90. P. aria (L.) Sm. Antrim — Glendun, 1868, S. A. Brenan (type! S.A.S.). The specimen in Dr. Moore’s Derry collection appears to be F. rupicola . LYTHEACEJE. Peplis portula L. To 1150 feet in the Mournes, S. & P. Down— Throughout the Mourne district, S. & P. Lougbbrickland, H.'W.L. Dundonald, R.L1.P. Derry — Enagb Lough, Mrs. Leebody. OUAGEAGEJE. Epilobium angrustifolium L. To 1500 feet in the Mournes, S. & P. Down — Cliffs of Eagle mountain, and cliffs south of Blue Lough, S. &P. Antrim— Gobbins cliffs (R.L1.P.), JB.N.F.G. 1892-3. Scawt Hill, Carnlough, Parkmore, Altmore, Culraney, Dunseverick, R.L1.P. E. obscurum x palustre. Antrim — Glenariff, Glenshesk, and Giant’s Causeway, Shoolbred l.N. ( teste E. S. Marshall). E. palustre L. To 1150 feet in the Mournes, S. & P. i68 [Appendix B.N.F.C., Down Frequent in the Moume district, S. & P. Sydenham, Dundonald, Conlig, Ballynahinch, and Narrow-water, R.Ll.P. Antrim — Glenarifl, Glendun, Fair Head, Shoolhred I.N. Bog Meadows, Killagan, Lough Naroon, Bushfoot, R.L1.P . j)erry_Kilrea, Bannmouth, and Magilligan, R.Ll.P. Circsea alpina L. Down — Tollymore Park, S. & P. Antrim — Langford Lodge, and still in Glenariff, R.Ll.P. Derry — By the Roe near Limavady, Mrs. Leehody. In addition to its native mountain habitats, it occurs frequently about Belfast as a garden weed— and a troublesome one too— as at Windsor Avenue, Clifton- ville, several gardens at Holywood, and Clandeooye, R.Ll.P. var. P C. intermedia Ehr. Down — As a weed in a garden at Holywood, R.Ll.P. Antrim— Glenariff and Glenshesk, Shoolhred I.N. Glendun, R.Ll.P. HALORAGACEX. XVIyriophyllum spicatum L. Down— Abundant in Clandehoye Lakes, R.Ll.P. Antrim— Abundant in Portmore Lough, R.Ll.P. Derry and Antrim— In Lough Neagh at Toome, abundant in Lough Beg, and thence down the Bann to the sea, R.Ll.P. Hippuris vulgaris L. Down — Altnadua and Moneyscalp, S. & P. Pollramer Lake near Cross- gar C.H.W. Loughinisland and Killinchy, R.Ll.iJ. Antrim -Between Baby castle and 1892-3. Portmore, H.W.L. Bog north of Ballymoney, R.Ll.P. Derry — Bann mouth, R.Ll.P. P O RTUliAC Montia fontana L. To 2450 feet in the Moumes, S. & P. CSASSULACliE, Sedum rhodiola DC. 1000-2000 feet in the Moumes, S. & P Down— Pigeon Rock Mountain, and along the Slieve Muck ridge, b. Antrim — Abundant on the coast north of Torr, R.Ll.P. P. i894-95-] 169 S. telephium L. Down — Dromantine, H.W.L. and C.H.W. gowan, Downpatrick, R.L1.P. Holywood Hills, Bally- Antrim Bally close and Craigbilly, Miss Knowles. Derry — Hear Maghera, R.L1.P. S. anglicum Huds. To 1000 feet in the Mournes, S. & P. SAXirRAGACES. Saxifraga stellaris L. To 2350 feet in the Monrnes, Hart R.l.A. Down— Hot abundant on the Mournes, as stated by Templeton. It is abundant on the H.W. slopes of Donard and Commedagh, but else- where it was seen by S. & P. only sparingly on Cove Mountain and at Hare s (rap. S. hypnoides L. Derry— Benbradagh, Mrs. Leebody. S. tridactylites L. Down— On walls and gravel at Kilmore near Crossgar, and on rocks by the coast at Cloughey Bay, C. H.W. y Derry— Bellarena, Mrs. Leebody. Chrysosplenium opposltifollum L. To 2450 feet in the Mournes, S. & P. Parnassia palustris L. Antrim — Roadside near Drumnasole, Altmore, Kinbane Head, R.L1.P. Derry— Mouth of the Roe, R.L1.P. B.N.F.C. 1890-1. Camlough, UlttBmi£XFE3&JEs Hydrocotyle vulgaris L. To 1500 feet in the Mournes, S. & P. Sanicula europsea L. To 1500 feet in the Mournes, S. & P. Eryngium maritimum L. Do--Yepry abundant from Greencastle Point to Hicholson’s Point, Cicuta virosa L. Down— By the Canal near Goraghwood, R.L1.P. [Appendix B.N.F.C. 170 APlU*Ante^-Rea”*y^Miss Knowles. Still occurs both north and south of Carrickfergus, S.A.S. /T . ^ . , „OT, o a rP»pn• l894-95-] 171 CEnanthe fistulosa L. Antrim— Shores of Lough Beg, and thence to Coleraine occasionally, Derry — Enagh Lough, Mrs. Leebody. Whitehead, and Derry— Coleraine, Mrs. Leebody. Upperlands. R.L1.P. Xilgusticum scotlcum L. Amtrim— Rocks on the shore at Bushfoot, R.L1.P., and recently refound at Garron Point, S. A. Brenan; R.L1.P., B.N.F.C. 1892-3. Derry-Sparingiy at Downhill, and still plentiful between Portrush and Portstewart, Mrs. Leebody. Silaus pratemis (L.) Bess. Has not been refound, and was no doubt a casual. Angelica sylvestris L. To 1500 feet in the Mournes, S. & P. [Peucedanum ostruthium Koch. Antrim— Stoneyford, R.L1.P. Not now on Cave Hill, S.A.S. Derry— Downhill, Mrs. Leebody.] Pastinaca satlva L. Down Holywood and Dundrum, probably casual, R.L1.P. Antrim— By the new path to Cave Hill, casual, S.A.S. Derry Still abundant at Magilligan, and quite naturalized, R.L1.P. Heracleum sphondylium L. To 1,500 feet in the Mournes, S. & P. 172 [Appendix B.N.F.C., Torilis nodosa (Huds.) Gaert. is nodosa (mias.j uwru Down— Abundant near Killowen, S. & P. Whiterock near KiUmcby, C.H.W. Antrim— Rathlin Island, K.L1.P., I.N. 1893. Scandix pecten-veneris I v F r B.KF.C. 1891-2. ' Craigayad, AntaDoTX^M^;PE.U P., 2) ifJ.C. UH4. Carnlough, Dun- severick, Carrick-a-rede, Portballantrae, U.L1.P. Derry — Magilligan, Mrs. Leebody. ChaerophyUum anthriscus Lam. 4. t? n Dow-Killinchy (E.L1.P.), B.N.F C 1890-1. Seashore at Bally- homan Bay, very luxuriant, K.LLf. Antrim— Still on tbe Curran at Larne, R.L1.P. MyrrW. odorata L ^ Near Saintfield and Kearney's “ “M’ H'W'L' ***' wood Hills, “dshurn &o, ^ g A. “e^fn Sontore, Dunadry, ' sioneyford, Torr, Dunseveriek, Giant’s Causeway, R.L1.P. Conium maculatum L. Antrim— At Portmore ; rare inland, K.Bi. P. Mourne district, S. * P. Knock and Downpatrick, R.L1.P. Antrim— Near Antrim, R.L1.P. Derry— Frequent in North Derry, Mrs. Leebody. HSDSKACBJE . Hedera helix L. To 2000 feet in tbe Mournes, S. & P. CAPSIPOtlACSSai Sa“-C‘ ltnaghmore, H.W.L. Near BaUynahinch, and still at Holy wood, R.L1.P. 894-95-] 173 Antrim — Dunadry and Cushendall, R.L1.P. Viburnum opulus L. Down — Rostrevor, Altnadua Lake, and Tolly more Park, S. & P. Tully- murry, R.L1.P. Antrim — Near Slemish, C.H.W. & H.W.L. Clogh, H.W.L. Cully- backey, Miss Knowles. Ballinderry, Glenariff, Rasharkin, R.L1. P. Derry — Glen at Benevenagh, Mrs. Leebody. Kilrea and Garvagh, R.L1.P. Iionicera periclymenum L. To 2,000 feet in the Monrnes, S. & P. Rims.acis.2E. Sherardia arvensis L. Down— Frequent in tbe Mourne district, S. & P. Saintfield, and near Crossgar, C.H.W. Antrim — Rasbarkin, R.L1.P. Derry — Magbera, Kilrea, and Garvagb, R.L1.P. Galium boreal© L. Antrim — Among tbe rocks of Agnew’s Hill 1804, Templeton MSS. Glenariff, Sboolbred I.N. Garron Point, between Ballymena and Brougbsbane, and by tbe river above Bushmills, R.L1.P. G. cruciatum (L.) With. Down — Still plentiful on tbe side of Downpatrick ratb, but no longer to be found at tbe Cathedral. G. moling-© L. Down — Lawn at Rowallen near Saintfield, D. Redmond; S.A.S., I N. 1894. Antrim— Riverside near Cullybackey, S. A. Brenan. Still at Glenarm Park, R.L1.P. Derry — Near Eglinton, Mrs. Leebody; H. C. Hart, Journ. Bot., 1892. VALERIATJACEJE. Valeriana officinalis L. var. a Mikanii (Wats.) Down — At 1500 feet on Slieve Muck, S. & P. Antrim — Common in tbe Glens ; tbe only form observed, Sboobred l.N. Sparingly by Lagan River at Mazetown, S.A.S. 174 [Appendix B.N.F.C., var. P V. sambucifolia Mikan. Down -Moume Park and Tullybranagan, S. & P. Maxwell’s Court near Comber, S.A.S. Antrim— Plentiful by tbe Lagan at Mazetown, S.A.S. Valerian ella olitoria (L.) Moencb. Down— Frequent in the Moume district, S. & P. Saint field, C.H.W. Antrim— Ballymena and Ballyclare, Miss Knowles. Larne, Scawt Hill and abundant on cbalk rocks on Garron Point, forming a close turf with Saxifraga hypnoides and Hieraeium anglicum , R.L1.P. V. carinata Lois. Down — Is increasing steadily at Dundonald, R.L1.P. V. dentata Willd. Down— Maggie’s Leap, Lisnacree, and abundant about Killowen and Seafieldf S. & P. Killmchy (E.L1.P.), B.N.F.C. 1890-1, and margins of Lough. Leagh (R.L1.P.), B.N.F.C. 1891-2. DIPSACACEX. Scabiosa suecisa L. To 1900 feet in tbe Moumes, S. & P. S. arvensis L. X)0Wn — Frequent in tbe Mourne district, S. & P. Antrim — About Ballymena, Miss Knowles. Derry — Dungiven and Kilrea, Mrs. Leebody. Ballynabincb, B..L1.P. COMPOSITE. Eupatorium cannabinum L. Antrim-Lambeg, Templeton MSS. Barn’s Island, Altmore, and Turr Head, R.L1.P. Derry — Cliffs at Downbill, B.L1.P. Petasites vulgaris L. Down— Very rare in tbe Moume district, S. & P. It is not generally common in tbe county, tbougb abundant in Antrim. p. fragrans L. Quite naturalized, and spreading tbrougbout tbe district. L. To 1900 feet in tbe Mournes, S. & P. Tussilago farfara >894-95-] 175 Erigeron acris L. The late Mr. A. G. More has informed us that this plant has been found on sandhills north of Newcastle ; this is almost the same station as given in Flora , hut is an interesting confirmation. Solidago virgaurea L. To 2449 feet in the Mournes, S. & P. var. p. augustifolia Koch. Down — By the Bann above Hilltown, and abundant by the river in Tollymore Park, S. & P. var. y S. cambrica Huds. Not now in 'lolly more Park, S. & P. ; must be deleted from our flora. Xnula Selenium L. Down — Near Ballynahinch and Saul, R.Ll.P. Antrim — Antrim, Carnlough, Portballantrae, Dunseveriek, R.Ll.P. Derry — Waste ground north of Kilrea, B.L1.P. Filago germanica (Huds.) L. To 500 feet in the Mournes, S. & P. Down— Frequent in the Mourne district, S. &P. Loughinisland, R.Ll.P. Antrim — Portrush, Bushfoot, Killagan, R.Ll.P. Derry — Kilrea, Mrs. Leebody. F. minima (Fries ) Huds. To 500 feet in the Mournes, S. & P. Crnaphalium sylvaticum L. To 800 feet in the Mournes, S. & P. Down — Frequent in Mourne district, S. & P. Ballygowan, R.Ll.P. Antrim — Glenariff, Shoolbred I.N. Near Ballymena, Miss Knowles. Scawt Hill, Culraney, Portrush, R.Ll.P. Derry — Bellarena (R.Ll.P.), B.N.F.C. 1892-3. Kilrea and TJpperlands, R.Ll.P. ** Antennaria dioica (L.) R. Br. Down— Kilbroney River, Slieve Muck, Slieve Meel-beg, S. ] 179 C. paludosa (L.) Moench. Down— Ballymacormick Point, a few feet above sea-level, R.L1.P. Antrim— Stoneyford, Shane’s Castle, and abundant in tbe 2-lens along- the coast, R.L1.P. Derry By the Roe, Mrs. Leebody. Kilrea and Garvagh, R.L1.P. Hieracium anglicum Fr. 200-2000 feet in the Mournes, S. & P. Down — The most abundant hawkweed in the Mournes, S. & P. Antrim— Fair Head and Giant’s Causeway, Shoolbred I.N. Rocks north of Ballycastle, S.A.S. var. b. acutlfolium Backh. Down— Luke s Mountain at 1000 feet, and bv the Shimna River above Tollymore Park, S. & P. var. d. longlbracteatum Hanb. A ntrim — Garron Point and Glenariff, W. A. Shoolbred; S.A S I.JY. H. lricum Fr. Derry— Basaltic cliffs, Downhill, R.L1.P. H. flocculosum Backh. Down— By Spinkwee River at 800 feet (not 1500 feet, as given in S^Tp an<^ ^ Same stream on shady rocks in Tollymore Park, Antrim— Sallagh Braes, S.A.S. H. heyi Hanb. Antrim— Benevenagh, W. A. Shoolbred; S.A.S., J.iV. 1894 (as H bifidum Tausch). v H. Schmldtii Tausch. Down — Granite cliffs of Bencrom, S. & P. The Antrim and Derry localities, published in Flora for R. pallidum , have been mostly transferred to H. euprepes ; the remainder are doubtful. H. lasiophyllum Koch. The Ballycastle record has been transferred' to R anglicum. H. Farrense Hanb. Antrim— Sallagh Braes, S.A.S.; R.L1.P., B.N.F.C. 1892-3. H. rubicundum Hanb. Antrim— Sallagh Braes, S.A.S.; R.L1.P., B.N.F.C. 1892-3. i8o [Appendix B.N.F.C., H. argenteum Fr. 100-1700 feet in the Mournes, S. & P. Down — Cove Mountain, Bencrom, Slieve Donard, and Tollymore Park, S. & P. The H. argenteum of Flora is transferred to H. hibernicum. H. Sommerfeltii Lindeh. Derry — Benevenagh, S.A.S. H. hibernicum Hanh. Down— Mountain stream in the Monrne Mountains near Rostrevor, H. 0. Hart. Journ. Hot. 1886 (as H. argenteum Fr.). Befound on rooks at Broughnamaddy (the same station), S. & P. H. stenolepis Lindeh. Antrim-Cave Hill, R.L1.P., and plentiful on Knockagh and Sallagh Braes, S.A.S. ; R.L1.P., B.JS.F.C. 1890-1. Garron Pomt, W. A. Shoolhred ; S.A.S., I.N. 1894. Glenarifi, Shoolhred I.N. Derry — Benevenagh, Shoolhred I. N. H. murorum L. pt. Down — Very rare in the Mournes ; found only hy the Bann, S. & P- Antrim— Garron Point, Shoolhred I.N. var. m. pacHypkyllum Purchas. Antrim— Basaltic cliffs of Knockagh and Sallagh Braes, S.A.S. ; W. H. Purchas, Journ. Bot. 1895. H. euprepes Hanh. Antrim— Cave Hill, Dr. Mateer, 1845, Herb. Hanbury Sallagh Braes S.A.S. ; R.L1.P., B.N.F.C. 1892-3. Bank at Milltown near Kea Bay, W. A. Shoolhred ; S.A.S., I.N. 1894. Derry — Benevenagh, S.A.S. H. caesium Fr. Antrim — Glenariff (S.A.S.), B.N.F.C. 1889-90. H. vulg-atum Fr. Down — Blue Lough, Hare’s Gap, Slieve Muck North, S. & P- H. sciapMlum Uecht. Down — Saintfield, D. Eedmond. i894-95-] 181 H. g-othicum (Fr. pt.) Backh. (E. Friesii Hartm.). Antrim — Riverbanks in Glendun, Shoolbred I.JSf. yar. Stewartii Hanb. 350-950 feet, S. & P. Down— Several spots by tbe Bann above Hilltown, and Tollymore Park, S. & P. (as H. Friesii, Hartm.). It tbe course of tbe Bann for about three miles. sparingly in grows along H. corymbosum Fr. Antrim — Riverbanks in Glendun, Shoolbred IN. H. auratum Fries. 150-1500 feet in the Mournes, S. & P. D0WS_&Tpe m°St abundant acciPitrine Hawkweed in tbe Mournes, Antrim— Lough Neagh shore at Cranfield, S A S Cushendun, R.L1.P.; R.L1.P., B.N.F.C. 1892-3. in Glendun, Shoolbred I.N. H. crocatum Fr. and sea-cliffs at Several places Down— By tbe Sbimna River, and on Pigeon Rock Mountain, S. & P. Antrim— Milltown near Redbay, and Glendun, Shoolbred I.N. H. boreale Fr. Down— Abundant by tbe Sbimna River above Tollymore Park, S & P (as FL. commutatum , Beck.). CAMPAXiTU:L.a.CEiE. lobelia Bortmanna L. 330-1350 feet in the Mournes, S. & P. There is no lake at 1500 feet, the elevation given by Hart, It. I. A. Down — Lough Sbannagb and Altnadua Lake, S. & P. Antrim— Abundant in a kkeiet on summit of Binnagee near Carnlough, at 1000 feet, R.L1.P., B.N.F.C. 1890-1. Jaslone montana L. To 1500 feet in tbe Mournes, S. & P. Campanula rapuneuloi&es L. Down— Fields near Rostrevor and north of Newcastle, S. & P. Antrim— In a sandpit near Brougbsbane, R.L1.P. Derry— Common in a field near Kilrea, R.L1.P. na^p2e5iStatWndy laDd ^ Ne™stle for 0TCr 20 7“®, is C. rotunditolia L. To 2450 feet on tbe Mournes, Hart U.I.A. i82 [Appendix B.N.F.C., ERICACBJE. 7 . • /r \ Dr. Diclde’s Slieve Donard plant was Arctostaphylos uva-ursi (L.) bpreng. no doubt Vaccimum mtis-xdcea , b. « r. Erica tetralix L. To 2055 feet on the Moumes, S. & P. E. cinerea L. To 2440 feet on the Moumes, S. & P. Vaccinlum vitis-ideea L. 1500-2796 feet on the Moumes, S. & P. 200-2000 feet in Derry. Down— On most of tbe Moume summits, S. & P. t s£- s * R.L1.P. extensive bogs above Dunloy and Rasbarkin, R.LI. • Derry-Bog on margin of Lougb Ouske in tbe Sperrin Mountains, R.L1.P., P.N.F.C. 1892-3. Fyrola media Swartz. Down— Still abundant on Conlig Hill. Antrim-Near Cairn Hill and Irish Hill, , W. Macmillan. Rocky thicket between. Kilrea and Garvagb, Miss Knowles. D°own-Between the Barbican gate and the sawmill in Tollymore Park, H.W.L. p. minor L. Down- H. Antrim — Refound in Ulenariff, S- A. Brenan. to /Jn T Thmiffb carefully searched for at Errigal Banks by Mrs. P. secmda L. inougn careiu y ^ not been s k vz.'t&szrJ&s P. secunda. i894-95-3 m not 183 AQVXFO&IACEJE. Hex aqulfolium L. To 1050 feet in the Mournes, Hart R.I.a. O&EACEJE. Praxlnus excelsior L. To 1000 feet in the Mournes, S. & P. CEXTIAWACEJE. Erythreea eentaurlum (Curt.) Pera. var. b. capltata (Koch). Antrim— Sand-banks near Giant’s Causeway, Shoolbred I.N. Gentiam amarellaL. The specimen which apparently represents this species Dr. Moore s Derry herbarium is G. campestris. G. amarella has i been iound m the district by any recent botanist. G< campestris L. Down— Spelga Mountain near Rostrevor, and by the Causeway water, S. & P. Ballykmler, and still on the Kinnegar at Holywood, R LI P Many “ "** * Derry— Eskers south of Kilrea, R.L1.P. Menyanthes trlfollata L. To 1600 feet in the Mournes, S. & P. COWVOIVULArr. a Convolvulus arvensls L. ^rAr^JPTfS’o^66?’ Newcastle> S- & P. Killough Bay (RXLP.) B.N.F.G. 1892-3. Abundant on the coast near Millisle, R O P^168 Queens Island* Newtown ards, Ballydugan Lake, Antrim— Along the railway from Belfast to Lame, where it has come ahSdaSy’R^ tich m obtamed on the Curran, where the plant grows pUykeUy’ Mrs< Leebody- Bann mouth and Limavady Junction, BOBAGXHrACE.2:* Cynoglossum officinale L. Down— Abundant on shore at Killowen, rising to 500 feet on the adjoin- ing stony slopes of Spelga Mountain, S. & P. 184 [Appendix B.N.F.C., CBOTnt"nLLs' at White Park Bay, away from any houses, W. J. Knowles.] Ancbusa sempervirens L. Herb. D.M. Cullybaeiey, probably Escaped, Miss Knowles. Oldstone near Antrim, W. S. Smith. Queen’s Island, Knock- Symphytum officinale L. Down— Near Hilltown and Newcastle, b. & t'. nagoney, Ballynahinch, R.L1.P. Antrim— Portrush, Dunseverick, and about Portballantrae, R.L1. . Derry — Magilligan, Mrs. Leebody. KHrea, R.L1.P. _ tllhPT.n,um L Rev. G. Robinson’s station is among the woods close to S‘ tUl ^ClandXye House where the plant grows abundantly, and appears quite naturalized, though it probably originated m the garden there, R.L1.P. ISchium vulgar e L. c « p Abundant in a field near Wood House, Rostrevor, b. & r. Kirkiston, O.H.W. On the railway at Ballymacarrett Junction, Antrim— Magberamorne, probably casual, R.L1.P. Mertensia maritima (L.) Don. rl asSJBTSr ft? Derry— Between Portrush and Portstewart, Mrs. Leebody. This last is the locality mentioned by Sampson ( Statistical Survey of the Co unty ‘ism, ^hen he speaks of the ^r £t ” -growmg^on ^interesting confirmation of an old record not mentioned in Flora. ™dSneear' Saltwater Bridge, Belfast, Dr. I. L. Drummond 1820 ; Belfast Museum Herb. This station is long since built over, and become part of the city. Myosotis palustris With. . __ « * p Down— Near Rostrevor and Newcastle, rare in the Moumes, b. « • Ballynahinch and Lougbinisland, R.L1.P. *894-950 185 Antrim — Bush River and Crumlin Waterfoot, R.L1.P. The Slieve Donard station of Flora belongs to M. repens. var. b. strig-ulosa Reichb. Antrim— Cushendun, Shoolbred I.N. M. repens Don. To 1000 feet in the Mournes, S. & P. Down-Abuudant on the flanks of the mountains and low grounds of Mourne, S. & P. Crossgar, R.L1.P. Derry— Near Upperlands, R.L1.P. M. collina Hoffm. Down — Kirkiston, C.H.W. Antrim— Gravelly banks at mouth of Sixmile River, R.L1.P., B.N.F.C. 1892- 3. Derry— Portstewart, Miss Davies, B.N.F.C. 1889-90. SOIAK'ACEiE. Solanum dulcamara L. D own — Glasdr umm an near Annalong, S.& P. Hedges between Killouffh and Ardglass, C.H.W. Grey Point and Ballynahinch, R.L1.P. Antrim— Bally castle, R. Welch. Near Ballymena, Miss Knowles.* Derry— Dungiven, and by the Foyle, Mrs. Leebody. Hyoscyamus nigrer L. Down— Plentifu! on distillery rubbish at Comber, imported with seed, o.A.b., I.N. 1894. Antrim— A few plants at Glenmore near Lisburn in 1890, but not found since, J . H. Davies. Carnlough, casual, Rev. J. Hall. Still about Ballycastle, R.L1.P. OEOMffCIMUs Orobancbe rubra Sm. Antrim— “ Gathered near BaRycastle, Oct. 1797,” R. Brown (as O. major), Kmbane Head, R.L1.P. ' Derry— Castlerock, R.U.P. [O. minor Sm. Down— Abundant in a field by the sea at Craigavad, 1892, H. C. Marshall ; R.L1.P., B.N.F.C. 1892-3. Also in 1893, H. C. Marshall. No doubt introduced with seed, along with the Lucerne on which it grows, but in view of the spread of this species in Ireland, its behaviour should be watched.] 1 86 [Appendix B.N.F.C., I,atlir»a^ sq^t ngar Brouglishane, on Plum, S. A. Brenan. Derry — Bellarena, Mrs. Leebody. SCSOPBV1ASIACEZ. waste ground at Downpatrick, R.L1.P. Antrim-Shore of Lougb Neagh in Glenayy Parish, Herb. D. M. Derry— Dungiven and Limavady, Mrs. Leebody. ^ tCat ptotfn’ow Sliced in the North of England, hut apparently not previously noticed in Ireland.] Digitalis purpurea L. To 1400 feet in the Moumes, S. & P. June, 1884, S. & P. 1,1 ^Down-Crossgar, Killyleagh, Loughinisland, Killinchy, Antrim-Kam’e Island, Broughshane Dnnloy, Dervock, BaUycastle, R.L1.P. Near Doagh, Rev. W. S. Smith. The Killowen record under this name belongs to L. repent. Castlewellan Lake, S.A.S. Mnnre’s note Denrv^tm^“m^hedcSy” UcertILlyIn error; the above i. the only station we know of. «. t 100-1400 feet in the Mournes, S. & P* Melampyrum pratense L. 100 14UU i The Mourne — * Tollymore Park, where the type grows abundantly. *894-95-3 i87 Antrim— Shane’s Castle, W. D. l'onnan. Runabay Head, Camlough, rocks near Lough Naroon, and heath above Rasharkin, R.L1.P. Derry— Bog near Portglenone, Miss Knowles. Wood near Kilrea, R. LI. P. var. b. latlfolium Syme. Antrim— In the glens, Shoolbred I.N. var. c. BE. montanum Johnst. 1400-2394 feet in the Mournes, S. & P. Down — Many places in the Mournes, S. & P. Antrim— In the glens, Shoolbred I.N. On Knocklayd at 1500 feet, R.L1.P. M. sylvaticum L. Antrim— Glenoe, 1837, Herb. D.M. Thompson’s Tollymore Park plant was no doubt a form of M. pratense , S. & P. Mimulus luteus L. Down — Edge of Clandeboye Lake, R.L1.P. Thoroughly naturalized in the district. Rhinanthus crista-galll L. To 1000 feet in the Mournes, S. & P. 1690 feet in Antrim (summit of Knocklayd), R.L1.P. Bartsia odontites Huds. var. b. serotina fReichb.) Antrim— Giant’s Causeway, Shoolbred I.N. Euphrasia officinalis L. To 2300 feet in the Mournes, S. & P. var. b. E. gracilis, Fries. Down — By Bloody Bridge River, S.A.S. Antrim— Between Bally earth and Ballintoy, Shoolbred I.N. Basalt debris on Knockagh, S.A.S. Veronica scutellata L. Down— A number of stations in the Mournes, S. & P. Magheralin, C.H.W. Dundonald, Conlig, Downpatrick, R.L1.P. Antrim— Refound on Rathlin, R.L1.P., B.N.F.C. 1889-90. Ballycastle, Killagan, above Lisburn, and near Soawt Hill, R.L1.P. Derry — Enagh Lough, Mrs. Leebody. Kilrea, R.L1.P. V. anagallis L. Down— Lisnacree, Harrow- water, White Water, S. & P. Ballynahinch, C.H.W. Newtownards and Killinchy, R.L1.P. Antrim— Lisburn, Stoneyford, Doagh, Crumlin, Shane’s Castle, R.L1.P. Derry— Bellarena, Mrs. Leebody, Coleraine, R.L1.P. 1 88 [Appendix B.N.F.C., V. montana L. Down— Saintfield, C.H.W. Downpatrick, R.L1.P. A ntr im — Glendun , S. A. Brenan. Shaw’s Bridge, Langford Lodge, Bushmills, R.L1.P. Derry— Bellarena and Prehen, Mrs. Leehody. Kilrea, R.L1.P. V. serpyllifolia L. To 1000 feet in the Mournes, S. & P. V. polita Fr. Down — Frequent in Mourne district, S. & P. C ultra, B-Ll.r. Antrim — Bushmills, S.A.S., /.AT. 1894. Derry— Coleraine, Mrs. Leehody. Kilrea and Castlerock, R.L1.P. V. Buxbaumii Ten. Down— Rostrevor, Killowen, Greencastle, S . & 1\ Kilmore near Crossgar, H.W.L. Milhsle, R.L1. Antrim— Ballymena and Glenariff, Miss Knowles. R.L1.P., l.N. 1893. Dundrum, P. Rathlin C.H.W. Island, V. bederifolia L. Down — Killowen, S. & P. Saul and Newcastle, C.H.W. W. D. Donnan. _ „ . Antrim — Rathlin Island, R.L1.P., I.N. 1893. Stoneyford magee, R.L1. P. Craigavad, and Island- LA.BIA.TJE. [Mentha viridis L. Down— Stream by roadside at Saul, C.H.W.] [1VI. rotundifolia L. Down— River-side near Ballynahinch, Richd. Hanna, and between Newtownards and Comber, R.L1. P.J Near Saul Chapel, [m. alopecuroides Hull. Down— Stream by roadside at Saul, L.il. w ., Watson B.E.G. 1893.] M. piperita Huds. . . , Down Plentiful by the old road between Ballynahinch Richd. Hanna. M. sativa L. var. p. M. rubra Huds. Down — Saintfield, C.H.W. and Drumaness, i894-95-] 189 var. paludosa (Sole). r erry— Limavady Junction, Mrs. Leebody ; S.A.S., I.N. 1894. M. pulegium L. Antrim — Abundant in a damp meadow near the north end of Lough Beg, Miss Knowles and R. Ll.P. Not now to be found at foot of Tullybranagan Mountain, Down ( Ir. Flor ), S. & P. > \ h Iiycopus europaeus L. Down— Annalong, and Narrow-water demesne, S. & P. Near Crossgar, C.H.W. Portavoe and Killinchy, R.L1.P. By Ballyward Lake, S.A.S. Derry— TJpperlands, Kilrea, and near Portglenone, R.L1.P. Origanum vulgare L. Down — Walls of Teraplepatrick graveyard, Richd. Hanna. Derry— Eglinton, Mrs. Leebody. Thymus serpyllum L. To 2050 feet in the Mournes, Ilart E.I.A. To 2000 feet, S. & P. Scutellaria galericulata L. Down— By canal south of Scarva, H.W.L. and C.H.W. Loughin- island, R.L1.P. Antrim— Glenmore near Lisburn, J. H. Davies. Cushendun, S. A. Brenan. Roadside near Rasharkin, Miss Knowles. Langford Lodge, R. LI. P. Nepeta cataria L. Down— Abundant by a roadside at Cloughey Bay, C.H.W. Lamium amplexicaule L. Down — Kilbroney, Killowen, Knockshee, G-reencastle, Annalong, S. & P. Killough Bay (R.L1.P.), B.N.F.C. 1892-3. Rough Island, Bally- water, Ballykinler, R.L1.P. Antrim — Stoneyford, Broughshane, B.L1.P. Derry — Dungiven, Mrs. Leebody. Zi. intermedium Fries. Throughout Down and Antrim. Numerous further stations might be quoted. 190 [Appendix B.N.F.C., L. hybridum Yillars. Down — Killowen, and Grlasdrumman near Annalong, S. & P. Antrim — Camlough, R.L1. P. Im, album L. Down — Kilmore near Crossgar, C.H.W. Lougiibrickland, H.'W.L. Narrow- water, R.L1.P. Antrim — Broughshane, S. A. Brenan. Magheramome, R.L1.P. Galeopsis speciosa MilL Down— Annalong, Hart R.I.A. Field at Six-road-ends near Conlig, S.A.S., I.N. 1894. Antrim — Frequent in sandy cornfields in tlie neighbourhood of Cushen- da.11, July, 1836, Herb. D. M. Still at Cushendall, R.L1.P., B.R.F.C. 1890-91. Glenariff, Ardclinis, and Cushendun, R.L1.P., B.N.F.C. 1892-3. Breckagh in parish of Skerry, S. A. Brenan. Derry -Eglinton, and near Enagh Lough, Mrs. Leehody. Half way between Kilrea and Maghera, R.L1.P. Stacbys betonica (L.) Benth. Derry— Refound at Kilrea by Mrs. Leebody; S.A.S., l.N. 1894. It grows here in some abundance in several pasture fields between the weir and the bridge, R.L1.P. S. sylvatica x palustrls. Down— Struell wells near Downpatrick, R.L1.P. Antrim — Islandmagee, Herb. D. M. Roadside bank near Belfast, S.A.S., B.E.C. Report 1889. Camlough, and Magheragall near Lisburn, RXLP. Hybrids nearer palustris than sylvatica are the prevailing forms in the district. The only station we know for true 8. ambigua Smith is that of b.A.^.. given above, which is near Glenville, on the road from Hannahstown to Woodburne. S. arvensis L. , Down— In some abundance from Newcastle to Kilkeel, and very abun- dant at Killowen, S. & P. Fields by shore south of K-iUough, and between Castlewellan and the Factory, S.A.S. Saul, R.L1.P. Antrim — Broughshane, and west base of Knocklayd, R.L1.P. ta aiDa xj. Down— Near Warrenpoint, S. & P. Ballynahinch, and Ballykinler, R.L1.P. i894-95-] I91 Antrim — Near Moira, 1837, Herb. D. M. Brown’s Bay on Islandmagee, (R.L1.P.) B.A/.F.C. 1892-3. Cushendun, S. A. Brenan. Bally- castle and Bushmills, It. LLP. Teucrlum scorodonla L. To 1400 feet in the Moumes, S. & P. VISBE1TACE2, [Verbena officinalis L. Down — Roadside about a mile from Pointzpass on the way to Lough - brickland, H.W.L. ; R.L1.P., B.1SI.F. C. 1892-93. ; and still there, H.W.L.] ZiBETTlSUXiARZACfiJE. Pingulcula vulgaris L. To 2000 feet in the Moumes, S. & P. P. lusitanica L. 0-1600 in the Mournes, S. & P. Down — A number of stations in the Mournes, S. & P. Antrim — On moist banks near the Giant’s Causeway, Herb. D. M. Glendun, S. A. Brenan. Margins of Lough Naroon, Miss Knowles and R.L1.P. Cushendall, R.L1.P. Derry — “ Gathered on a bog by the roadside about half way between Londonderry and Newtownlimavady, Aug. 6th, 1795,” R. Brown. Bran Lough above Maghera, R.L1.P. Utricular! a vulgaris L. Down — Altnadua Lake, and site of Money scalp Lake, S. & P. Brown Bog near Loughbrickland, H.W.L. Lake near Helen’s Tower, R.L1.P. Antrim— Very fine in clayey holes below the Asylum, Belfast, 1837, Herb. D.M. Portmore, R.L1.P. Derry — Lakelets near Kilrea, R.L1.P. U. intermedia Hayne. Antrim — On a large peat-bog near Rasharkin, D.M. ; Cybele Hibernica. Abundant and fine in a boggy pool about a mile west of Lough Naroon, R.L1.P. 6 U. minor L. Down— Anahilt bog, and bog near the head of Kilkeel River [still there, S. & P.], Templeton MSS. Altnadua Lake, S. & P. Near Crossgar, C.H.W. Pollramer Lake, S.A.S. Ballydugan Lake, R.L1.P. ! 192 [Appendix B.N.F.C., Antrim — In marshes along the shore of Lough Beg, and near Trostan mountain, 1837, Herb. D.M. Bog north of Ballymoney, R.L1.P. Derry — Bogs near Maghera, and Garvagh, It. LLP. PBIMULACES. Kottonia palustris L. “ Everogue’s Bridge,” the original station for this plant, is Crossgar, where it still grows abundantly, R.L1.P., B.N.F.C. 1890-1. Primula vulgaris L. To 1500 feet in the Moumes, S. & P. [P. veris L. Antrim — Pare, only found in Glenarm Park, 1837, Herb. D. M. Lambeg, in old pastures, H.W.L.] Hot refound by S. & P. at Rostrevor, the only station in which the authors of Flora considered it might be native. “ Must be removed from the list of native plants,” S.A.S., /.A. 1894, in which opinion R.L1.P. agrees. To show how this plant may be introduced to wild-looking habitats, we may quote the following note by R.L1.P. : — “Abundant in an old pasture at Cherryvalley near Crumlin. On enquiry it transpired that the stream that waters this meadow passes through a stack-yard in which was stored hay that grew on the lawn at Cherryvalley, where cowslips had been formerly planted, and hence the plant spread to the present station. The cowslips appeared in the meadow the year after the lawn had been cropped for hay.” Ziysimacbla vulgaris L. Down — Lakeside at Portavoe, and still at Lough Leagh, R.L1.P. Xi. nummularia L. Down — Kilmore near Crossgar, C.H.W. Antrim— Lough Neagh shore at Langford Lodge, R.L1.P. Anagallis arvensis L. var. (3. A. coerulea Schreb. Antrim— Bank near the gate of Belfast Botanic Garden, J. J. Andrew; R. L1.P., B.N.F.C. 1890-1. A. tenella L. To 1600 feet in the Moumes, S. & P. Down — Frequent in Moume district, S. & P. Antrim — Throughout the county, R.L1.P. Centunculus minimus L. Down— Abundant on drained site at Ballymartin Lake, near Annalong, S. &P. *94-95*] 193 Samolus valerandi L. Down — Narrow- water demesne and mouth of White Water, S. & P. Antrim— Shores of Lough Beg, Miss Knowles. Portrush and Dunluce, R.L1.P. PLUIYEBAGINACE.ZE. Statice bahusiensis Fr. Down — Many places on both sides of Strangford Lough, R.L1.P. Antrim — Abundant at upper end of Larne Lough, R.L1.P. PIi ANT AGIN ACEJE. Plantago lanceolata L. To 1150 feet in the Moumes, S. & P. P. major L. var. P. intermedia Lilib. Antrim— Plentiful on shore of Lough Neagh at Crumlin waterfoot, S. A.S. Iiittorella lacustris L. To 1350 feet in the Mournes, S. & P. ; there is no lake at 1500 feet, the elevation given by H. 0. Hart, It. I. A. CHENOPODZACEJC. Salsola kali L. Antrim — Bushfoot, White Park Bay, It. Ll.P. Derry— Benone, Mrs. Leehody. Chenopodium bonus-benricus L. Antrim— Bailee, Miss Knowles. Cullybackey, S. A. Brenan. Clough and Broughshane, H.W.L. Magheragall near Lisburn, It. Ll.P. Derry — Kilrea, Mrs. Leehody. Beta maritima L. Down— Dunnyneile Island near Killyleagh (R.L1.P.), B.N.F C. 1891-2. Portavoe and Millisle, R.L1.P.; S.A.S., 7.2V. 1894. Newry, R.L1.P. Antrim — Maritime rocks from White Park to Derrygregor Head, 1836, Herb. D.M. Refound on Rathlin Island, R.L1.P., B.JSf.F.C. 1889-90. White Park Bay and Kinbane Head, R.L1.P. ; S.A.S., I.N. 1894. Derry — Downhill, Mrs. Leehody. Atriplex erecta Huds. Down — Newcastle, S. & P. Derry — Bellarena, Mrs. Leehody. I 1 94 [Appendix B.N.F,C. A. deltoidea var. p. A. salina Bab. Derry — Shore near Bellarena, Mrs. Leebody. A. farinosa Dum. Down— Shore south of Millisle, and still at Groomsport and Newcastle, R.L1.P. Antrim — Redbay, Cushendun, and Bushfoot, R.L1.P., B.N.F.C. 1892-3. Foraff, Miss Knowles. A. portulacoides L. Down— Plentiful on sea-shore close to railway bank half a mile north of Dundrum, Richd. Hanna. This is its most northerly station in Ireland. In its other habitat in our district, near Warrenpoint, it is abundant, and extends from Newry southwards. POLYGON ACE A!. Humes sanguineus L. The type is extremely rare. R.L1.P. has observed it for some years by the roadside between Bally castle and the sea, which is the only station we know of. R. hydrolapathum Huds. Down — Loughinisland (R.L1.P.), £ “<-<«. a*. ».». Derry Eglinton, Mrs. Leebody. Bann mouth, R.L1.P. C. murlcata L. Ant1ho™Mpir„*y " Springfield Bead and the Forth River above Clowney Bridge, Richd. Hanna ; S.A.S., I.N. 1894. C. teretluscula Good. C. panlculata L. Antrim— Grange of Killagan, and Parish of Aghagallon Herb D M IN- 1893 • ***' M”d> m Derry— Kilrea, Mrs. Leebody. C. canescens L. Down— Camgaver, R.L1.P. Antrim— Killagan, and bogs above Dunloy and Rasharkin R LI P Derry— Hear Kilrea, Mrs. Leebody. 206 [Appendix B.N.F.C., C.leporina L. . Down — Sparingly on the lower grounds of Moume distnet; abundant around Lough Island Heavy, S. & P. Aghaderg, H.W.L Victoria Park, W. D. Donnan. Conlig, Killinchy, Downpatrick, R.Lil.r. Antrim— Bailee and Cullybackey, Miss Knowles. Killagan and Dunloy, R.L1.P. Derry — Kilrea, Mrs. Leebody. C. stricta Good. Antrim— Side of Lough Neagh at Shane’s Castle, Herb. D.M. Abundant and luxuriant on several spots around Portmore Lough, and islet on Antrim side of Lough Beg, R.L1.P.; S.A.S., IN 1894. Frequent where the Bann leaves Lough Beg, and agam half-way to Portgle- none, and abundant on the river edge for half-a-mile at Portglenone House, R.L1.P. Derry — Side of the Bann near Coleraine, Herb. D.M. [Still there, below the town, R.L1P.] Side of the Bann below Toome, R.L1.P. ; S.A.S., I.N. 1894. By the Bann at Kilrea, Mrs. Leebody. This plant, for which in Flora only Templeton’s notes could be quoted, is thus abundantly restored to its place in our flora. C. acuta L. Antrim — Banks of the River Main, near Ballandraid, Herb. D.M. C. rigida Good. Dr. Dickie’s record, “Summit of Slieve Donard,” was certainly an error, S. & P. C. aquatilis Wahl. var. elatior Bab. Antrim— Ditch by the Main River in Shane’s Castle Park, R.Ll.P., Journ. Bot. 1892. See also A. Bennett in I.N. 1892. C. Goodenovli Gay. To 1450 feet in the Moumes, Hart R.I.A. ; to 1400 feet, S. & P. C. pallescens L. Down— Tollymore Park, S. & P. Dundrum and Saintfield, C.H.W. Aghaderg, H.W.L. Derry — Kilrea, R.Ll.P. C. limosa L. Down— Plentiful in a wet marsh on Saul Camp ground at Downpatrick, R.Ll.P., B.N.F.G. 1892-3. Antrim — Bog east of Killagan railway station, margins of Lough Naroon, and still frequent on wet bogs above Rasharkin, R.Ll.P. i394-95-] 207 Derry— Margins of Lough Ouske in the Sperrin Mountains, R LI P Journ. Bot. 1892. C. strig-osa Huds. Antrim— Near Muckamore, B.N.F.C. ; I.N. 1893. C. pendula Huds. Antrim— Glenariff, Shoolbred I.N. Langford Lodge, H.W.L. Wood- burn Glen, R.L1.P. C. preecox Jacq. Antrim— Rathlin Island, R.L1.P., B.N.F.C. 1889-90. Derry— Near Bellarena, Mrs. Leebody. Kilrea, R.L1.P. C. pilulifera L. Antrim— Glenariff, Shoolbred I.N. C. giauca Scop. To 2510 feet in the Mournes, S. & P. C. CEderi, auct. plur. Down— Augbnadarragh Lake, C.H.W. ; Watson B.E.C. 1893-4. By Pollramer Lake, S.A.S. 3 C. extensa Good. Down— By the (Juoile below Downpatrick, R.L1.P. Derry — Coleraine, Mrs. Leebody. Bann mouth, R.L1.P. C. Hornschuchiana Hoppe. To 1700 feet in the Mournes, S. & P. Down— Between Dunny Water Bridge and Annalong, Hart It. I. A. Frequent on the Mournes, S. & P. Camgaver, R.L1.P. Antrim — Glensbesk, bogs above Agnew’s Hill, and bead of Glenariff, Herb. D.M. Bogs above Dunloy and Rasharkin, R.L1.P. Derry— Killelagb Lough above Magbera, and near Kilrea, R.L1.P. C. dlstans L. Down — South of Rostrevor, S. & P. Antrim— Below Cushendall, Herb. D.M. Derry— Near Portstewart, Mrs. Leebody. Bann mouth, R.L1.P. C. binervis Sm. To 2394 feet on the Mournes, S. & P. C. laevigata Sm. Down— Between Dunny Water Bridge and Annalong, Hart R.I.A. Moume Park, S. & P. Kilmore near Crossgar, C.H.W., Watson B.E.C. 1893-4. Derry— Dungiven, Mrs. Leebody. 208 [Appendix B.N.F.C., C. filiformis L. Antrim — A fine specimen is in Herb. D.M., labelled “ At S el chin neu deer park, side of Lough Neagh, July, 1832.” This plant, whicl is included among the “ Plants erroneously recorded ” in Flora, musi therefore be restored to its place in our flora, though it is feared it h now extinct, through drainage, along with C. elongata, which grew at the same place. C. hirta L. Down — White Water, S. & P. Aghaderg and Tullylish, H.W.L Cultra, R.L1.P. Antrim — Shane’s Castle, W. D. Donnan. Glenarm, R.L1.P. Derry — Maghera, Mrs. Leebody. Bellarena, W. Kennedy. Kilrea R.L1.P. C. rostrata Stokes. To 1150 feet in the Mournes, Hart R.I.A.; also S. & P. var. p. robusta Sonder. Down — Brown Bog near Loughbrickland, H.W.L. C. vesicaria L. Down — Pollramer Lake, C.H.W. Brown Bog near Loughbrickland H.W.L. Antrim — Cushendall, and abundant by the Bann at Portglenone House and at its outflow from Lough Beg, R.L1.P. Derry — By the Bann at Kilrea, Mrs. Leebody. C. paludosa Good. Derry — Side of the River Bann below Coleraine, Herb. D.M. C. riparia Curt. Antrim — Still at Portmore, by the Tunny drain, R.L1.P. Derry - Abundant in several spots on south bank of Bann, between Cole raine and the sea, R.L1.P. GRAITCINEJE. Anthoxantbum odorafum L. To 2394 feet in the Mournes, S. & P. Alopecurus pratensis L. Down — Donaghadee, S.A.S., J.W. 1894. Antrim— Stranmillis, Ballygomartin, and roadside beyond Ligonie S.A.S. ITardus atrlcta L. To 2449 feet in the Mournes, S. wlthout access; the place is now close-cropped Arrostis canlna L. To 2300 feet on the Mournes S & P s- & p- Antrim— Mazetown, Castle Hpton, and Crumlin Waterfoot, S.A.S. A. vu^aris^ With. g var^ (3. A. pumila Lightf. 1200 -1600 feet in the Down— Slieve Bingian and Eagle Mountain, S. & P. Antrim— Ballycastle, R.L1.P. Den-y-Wenagh, E.L1P., B.N.F.C. 1892-3. Near Maghera and Ailrea, sand-dunes at Bann mouth, and fields at Magilligan, R.L1.P. A. alba L. To 2055 feet on the Mournes, S. & P. Holcus lanatus L. To 1350 feet on the Mournes, S. & P. H. mollis L. Down— A tall (4 feet) slender form at White Water, S. & P. Castle- wellan Park, S.A.S. Derry— Limavady, Mrs. Leehody. Kilrea, R.L1.P. 210 [Appendix B.N.F.C., Aira flexuosa L. To 2790 feet on the Moumes, Hart JR. I. A., also S. & P. Down— Common on the Mournes, S. & P. Hills above Dundonald, S.A.S. Antrim — Above Dunloy and Rasharkin, R.L1.P. Derry — Benevenagb and Benbradagb, S.A.S. Garvagh, R.L1.P. A. prsecox L. To 1662 feet on the Moumes, S. & P. Trlsetum flavescens (L.) Beauv. Down— Killyleagh (R.L1.P.), B.Jf.F.G. 1891-2. Marino, Cultra, New townards, R.L1.P. Antrim— Plenty near Antrim and Ballinderry, Herb. D.M. Lisburn Park, Greenisland, Carrickfergus, R.L1.P. Derry — On a wall at Garvagb, R. Ll.P . [Avena fatua L. Antrim — Rubbish heaps at Springfield, Belfast,' with other casuals, S.A.S.] [A. strigosa Schreb. Antrim — Frequent near Clogb Mills, Herb. D.M.] A. pubescens L. Down— Shore at Craigavad, R.L1.P. W. D. Donnan. station). Antrim— Cliffs of Cave Hill, and in Parkmore wood, S.A.S. S.A.S., I.N. 1894. Holywood, Not found by S. & P. at Newcastle (Templeton’s Trlodla decumbens Beauv. Derry— Moume district frequent, S. & P. Near Lough Shark, H.W.L. and C.H.W. Antrim— Glenariff, Sboolbred I.N. Cusbendun, Dunloy, R.L1.P. Derry— Magbera, Kilrea, Garvagb, Bann mouth, R.L1.P. Koehlerla crlstata (L.) Pers. Antrim— Dry, sandy ground at Cushendall, Herb. D.M. Still at Giant si Causeway, and still on Islandmagee, growing 3 feet high at the Rocking-stone, R.L1.P. Melica uniflora Retz. Down — Frequent in Mourne district, S. & P. Downpatrick, R.L1.P. UUWU ^ — 7 - T1 T3 Antrim— Glenariff, H.W.L. Camlougb and Shane s Castle, R.Ll.t7. Derry — Garvagb, Mrs. Leebody. Kilrea, R.L1.P. I 1 894-95-] 2 1 1 Molinia cserulea Schreb. To 2449 feet on the Moumes, S. & P. Antrim— Bogs at Killagan and above Dunloy, R.L1.P. Poa annua L. To 2450 feet on the Moumes, S. & P. P. pratensis L. To 1350 feet on the Mournes, S. & P. We could not find it on summit of Slieve Donard, whence it is recorded with a ? by Dickie (Flor. TTlat.)t and apparently copied from this work (but without the ? ) into Gybele Hibernica and Mr. Hart’s Report, R.I.A. 1891 • and we believe this note to be a mistake. Glycerla fluitans (L.) R.Br. To 1150 feet in the Mournes, S. & P. Scblerochloa dlstans (L.) Bab. Down — Warrenpoint, S. & P. S. rlgida (L.) Link. Down— Walls by the sea at Ardglass and Killough, R.L1.P., B NFC 1892-93. Antrim — Wall top at Magheramorne railway station, R.L1.P. S. lollacea (Huds.) Woods. Down— White Water, and near Newcastle, S. & P. By Ballyduean Lake, R.L1.P. Antrim— Redbay, Cushendun, and still at Ballycastle and 01derfleet,R.Ll.P. Briza media L. Down — Narrow- water, S. & P. Newcastle, C.H.W. Killinchy, R.L1.P. Catabrosa aquatica Beauv. D own — Saintfield, D. Redmond. Antrim — Dervock, R.L1.P. Derry— Lignapeiste Glen, Mrs. Leebody. Near Upperlands and Maghera, Miss Knowles. Near Garvagh, R.L1.P. Festuca sciuroides Roth. Down— Near Warrenpoint, S. & P. Rostrevor, H.W.L. Downpatrick, and still at Holywood, R.L1.P. Antrim — Randalstown, W. D. Donnan. F. ovina L. Type ascends to 1500 feet, and viviparous form ranges from 200 to 2796 feet on the Moumes, S. & P. var. p. P. tenuifolia Sibth. Down— Cliffs of Slieve Muck, at 1600 feet, S.A.S. 212 [Appendix B.N.F.C., var. y. F. duriuscula L. Antrim— Frequent in meadows throughout the Co. of Ant™, especially along the shores of L. Neagh, Herb. D.M. Glenanff, Shoolbred I.X. Knockagh, R.L1.P. F. rubra L. To 1600 feet in the Mouraes, S. & P. T. sylvatica Till. Down— Abundant and luxuriant by tbe Sbimna and Spinkwee Rivers in Tollymore Park, S. & P. F. glgantea Till. Down — Moygannon Glen, Moume Park, Tollymore Park, S. & P. Holywood Waterworks, R.L1.P. Antrim — Orumlin "W aterfoot, S.A.S. Massereene Park, R.L1.P. Derry — Magilligan, Mrs. Leebody. F. arundinacea Scbreb. Down— Tollymore Park, S. & P. .1 Dundrum, R.L1.P. Antrim— Templepatrick and Knockagh, |S. A. S. Island at north end of Lough Beg, Mrs. Leebody. Busbfoot, R.L1.P. Derry — TTpperlands,*Kilrea, and Magilligan, ^_R. LI. P. Bromus sterllls L. Down-Abundant from Eillowen to Seafield, and sparingly at Warren- point, S. & P. '^Killowen church at Killyleagb, (R.L1.P.), B.Jv.r- 0. 1891-2. Antrim— Roadside between '.Ballycastle and tbe sea, R.L1.P. For “ railway bank ” at Marino in Flora read “ railway bridge. B. racemosus L. Down — Holywood, R.L1.P. Antrim — White well, R.L1.P. [B. secalinuB Bab. Antrim— Waste ground at Duncrue Street, Belfast, and hedge-bank at Magheragall near .Lisburn, R.L1.P.] Triticum caninum L. p Down— Shore a mile south of Newcastle, and near Kilkeel, b. & Sandy shore at Groomsport, S.A.S. 1 894-95-] 2I3 T. acutum DC. Down-Gravelly shore of Ballyhornan Bay, S.A.S. Antrim— Sandy shore, Red Bay, Shoolbred I.N. T. junceum L. Down— Kilkeel and Greencastle, S. & P. Antrim— Ballycastle, R.L1.P. [Hordeum murlnum L. Antrim— Garron Point, 1861, H.W.L.] Xiepturus filiformis Trin. Down-Between Warrenpoint and Narrow-water, H.W.L. Antrim— Shores at Larne Lough plentifully, Herb. D.M. [Lolium temulentum L. Antrim— Near Larne, Herb. D.M. Derry— Near Limavady, Mrs. Leebody.] CRYPTOGAMIA. EQUISBTACEJD. Equisetum pratense Ehr. Grainger. Glen on north side of Garron Point, R.lu? b' Catl Shoolbred I.N. Old waU at Kilrea, Mrs. Athyrtum fiilx-foemlna (L.) Koth. To 2449 feet on the Mournes, S. & P. Asplenlum adlantum-nigrum L. To 1000 feet on the Mournes, S & P ?n throhgiout the district-a long list of further localities migni oe given. far. p. A. acuttm Bory.H The Beneyenagh plant of Flora, though a very Sh»t A' “(lantum;n'9™m, cannot be correctly pkced here' Sherard s MourneJMovmtam plant (Herb. Oxon. and Ran Synopsis) Iw tanen ,pll‘.niu6e’*form of Athyrium JiUx~fTTD ^ntrim White Park Bay and Giant’s Causeway, K.L1.F. Derry By the Roe above Limavady, Mrs. Leebody. As marinum L. Derry — Benevenagh Cliffs, Shoolbred I.N. . t Growing on trap-rock on Benevenagh, R.L1.P., A. rn j^ -p G 1892-3, and the same at Fair Head, R.L1.P. CeteXwn-NeTa“g [5ft 1889-90. Maryfield near Holywood, D w Patterson. Ringdufferin, J. Wilson Larchfield near r esacurry, J. H. Davies. Ardilea House near Dundrum, R.L1.P. Antrim— Glemnore near Lisburn, J. H. Davies. Bridge in Glendun, S. A. Brenan. Derrv— Wall at Prehen near Londonderry, Mrs. Bernard. The prevailing form in the district is var. cremtum Milde; the type is apparently rare. Blecbnum splcant Both. To 2449 feet on the Moumes, S. ft P. Pterls aquiltna L. To 1450 feet on the Moumes, Hart 1 ; 1400 feet on the Mournes, S. & P. • 77 „ t a oVippt of small fronds in Mr. Hanbury s labelled “Morne Mns., Co. Down Ireland.” There iTno date or collectors name. The sheet has no history, and comes from some old herbarium. B unilateral® Wffld. To 1750 feet on the Moumes, Hart Jt.I.A. ; 150- 1500 feet on the Mournes, b. & r. Down— Some additional Mourne Mountain localities are given y S. &P. Osmu Down_West gide of giieve Bingian, and by the Causeway water; still at Bloody Bum and sea-cliffs south of Newcastle; apparently extinct by the Glen River, S. & P. 1894-95-] 217 Antrim— Island of Rathlin, sparingly, and on boggy ground along the side of Portmore Lough, Herb. D.M. Hear Whitehall at Brough - shane, S. A. Brenan. Still lingers by Lough Neagh at Shane’s Castle, R.L1.P. ; S.A.S., I.N. 1894. Derry— By Lough Bran above Maghera, R.L1.P. Bog two miles east of Kilrea, R.L1.P. Botrycliium lunaria (L.) Sw. Down— Bloody Bridge, S. & P. Conlig Hill, R.L1.P. Tonaghmore Hill near Saintfield, D. Redmond. Antrim— Rathlin Island, R.L1.P., B.N.F.C. 1889-90. Glenariff, S. A. Brenan. Summit of Binnagee near Carnlough, R.L1.P. Ophioglossum vulgratum L. Down — Rostrevor, S. & P. Saintfield, C.H.W. Loughbrickland, H.W.L. Clandeboye demesne, R.L1.P. Antrim— Glenmore near Lisburn, J. H. Davies. Glenballyemon, S. A. Brenan. Langford Lodge and Binnagee, R.L1.P. Derry — Kilrea, Mrs. Leehody. MARSXLEiiCliJE. Pilularia globulifera L. Antrim — Drain, side of Portmore Lough, Herb. D.M. lycopodsacbje. Xsoetes laeustris L. 1100-1350 feet [not 1500] in the Mournes, S. & P Descends to less than 50 feet in Antrim (Lough Neagh, D.M.). Down — Blue Lough and Lough Shannagh, S. & P. Antrim— Shore of Lough Neagh near Toome Bridge and Selchin, and at Lady Bay in parish of Glenavy, Herb. D.M. Craigfad Lough above Carnlough, R.L1.P. b Lycopodium clavatum L. Down— One plant on Slieve Donard at 2450 feet, S. & P. Slieve Com- medagh, H.W.L. Antrim— Skerry, Herb. D.M. Evish Mountain near Parkmore, and Glenleslie near Clogh, H.W.L. Summit of Knocklayd, R.L1.P. Derry — Crockmore above Draperstown, R.L1.P., Journ. Bot. 1892. L. alpinum L. 1900-2796 feet on the Mournes, S. & P. Down — On most of the Mourne summits, S. & P. / 2l8 [Appendix B.N.F.C., Antrim— Near Retreat, S. A. Brenan. Cloughcor above Glenariff, H W L. Summit of Trostan, and of Little Trosk above Camlough, R.L1.P. I,, selago L. To 2796 feet on tbe Moumes, S. & P. Selaglnella spinosa Beauv. To 2020 feet on tbe Moumes, Hart E.I.A. 0-2000 feet on tbe Moumes, S. & P. Down — Common on tbe Moumes, S. & P. CHARACEJE. Chara fragilis Desv. Down— Co. Down [Lougbinisland], S.A.S. ; H. & J. Groves Journ. Bot. 1890. Warrenpoint town reservoir, S. & P. Ballyward Lake and Castlewellan Lake, S.A.S. Bull’s Eye near Downpatrick, Clande- boye lakes, Conlig Hill, and Ballygowan quarries, R.L1.P. Antrim — Lougb Neagb, D. Moore ; Groves I.N. Bogbole above Carn- lougb, R.L1.P. var. barb at a Gant. Down— Holywood Hills, R.L1.P. : Groves I.N. South side of Tardree Hill, Herb. Canon Grainger. Clandeboye lower lake, and near Craigauntlet, R.L1.P. Antrim — Lougb Beg [Portmore Lougb], W . Thompson ; Groves I.N. var. Hedwigii Kuetz. Down — Holywood Hills, R.L1.P. ; Groves I.N . var. delicatula Braun. Antrim — Ram’s Island, H.W.L. C. aspera Willd. Down — Money Lake, R.L1.P. Antrim— Rathlin, Hb. D. Moore ; Groves I.N. Lougb Beg, R.L1.P. 5 Groves I.N. (abundant at north end of tbe lake, R.L1.P.). m Lougb Neagb near Shane’s Castle, R.L1.P. Derry— Lougb Beg, R.L1.P. ; Groves I.N. var. lacustrls H. & J. G. Antrim— Lougb Neagb, Crumlin, S.A.S. ; Groves I.N. var. subin ermls Kuetz. Antrim— Rathlin Island, D. Moore; Groves I.N. Ram’s Island, H.W.L. Derry — River Bann [below Coleraine], R.L1.P. ; Groves I.N. i894-9S-] 219 C. eontrarla Kuetz. Down— Clandeboye Lake, R.Ll.P., B.N.F.C. 1892-3. Derry— Brackish pools at Limavady Junction, R.Ll.P. and W D Donnan ; R.L1.P., B.N.F.C. 1890-1. C. hisplda L. Down— Downpatrick, R.L1.P. ; Groves I. If. It grows here in Money Lake and m the Bull’s Eye, R.L1.P. r)errLeebodBann’ Coleraine’ D’ Moore J Groves I.If. Magilligan, Mrs. var. rudls Braun. Down— Money Lake, R.L1.P. C. vulgaris L. Down— Downpatrick, and Clandehoye Lakes, R.L1.P. Antrim— In Lough Neagh south of Shane’s Castle, R.L1.P. Derry— Magilligan, Mrs. Leehody ; Groves I.If. var. longlbracteata Kuetz. Down— —Co. Down [Victoria Park], S.A.S. ; H. & J. Groves, Journ. Bot. 1890. Blackstaff Bridge near Kirkcubbin, R.L1.P. Antrim— Springfield, W. M. Hind ; Groves I.If. Iffltella translucens A g. Down— Pool on Conlig Hill, W. D. Donnan. Very abundant in a small lake in Llandeboye demesne, R.L1.P. Antrim Lissanorn Castle, D. Moore ; Groves I.If. Derry— Kilrea, D. Moore; Groves I.If. (still there, R.L1.P.). Enagh Lough, Mrs. Leebody. Killelagh Lough above Maghera, R.Ll.P. Down-Tollymore Park, Burren River, Lough Island Reavy, and by Bann. above Hilltown, S. & P. Money Lake and Ballygowan quarries, R.Ll.P. Antmn— Ram’s Island, H.W.L. Six-mile River at Templepatrick, Derry— Kilrea, W. Thompson; Groves I.If. Racecourse bog near Londonderry, Mrs. Leebody. Killelagh Lough above Maghera, xt.JLl.P. 220 [Appendix B.N.F.C., M U S C I . AITDKS^ACEJE. Andresea crassinervis Bruch. Down — Eagle Mountain, C.H.W. ; Lett R.I.A. A.rupestrls (L.) Both. Down — Summit of Slieve Bignian, H.W.L. var. falcata Schimper. Down — Bocky Mountain near Hilltown, C.H.W. var. liamata Lindb. Down — Slieve Commedagh and Slieve Dermot, H.W.L. POL7TRZCHACEJB. Oligotrichum lncurvum (Huds.) Lindh. Down — I 'evil’s Brewing Pan at Mourne Mountains, Templeton MSS. Antrim — Gravelly heath above Cave Hill Deerpark, C.H.W. Polyfrichum urnigrerum Linn. Derry— Garvagh, S. A. Brenan; H.W.L. P. attenuatum Menz. Down — Drumsallagh, Aghaderg, H.W.L. 1889. Saintfield demesne, C.H.W. & H.W.L. DSCHAlVACEiE. Pleurldium axillare (Dicks.) Lindh. Down— Abundant in stubble fields, and by the lake shore at Loughbrick- land, H.W.L. P. subulatum (Huds.) Baben. Down — Warrenpoint, C.H.W. Scarva, H.W.L. Antrim — Glendun, S. A. Brenan ; H.W.L. Ditriehum bomomallum (Hedw.) Hampe. Antrim— Glenariff, H.W.L. i894-95*] 221 Anlsotheclum crispum (Schreb.) Lindb. var. 0. elatum. Antrim Cushendall, H. N. Dixon, Journ. Bot. 1891. Seems to be tbe only Irish locality for this variety. A. rubrum (Huds.) Lindb. Down— Deer’s Meadow and Rocky Mountain, Lett R.l.A. A. rufescens (Dicks.) Lindb. Down— Abundant on shores of Loughbrickland, H.W.L. A. squarrosum (Starke) Lindb. Antrim— Slievenanee and Glenballyemon, H.W.L. Campylopus fleznosus (L.) Brid. Antrim— Cloughcor near Glenariff, H.W.L. C. setlfollus Wilson. Down— Pigeon Rock Mountain, Lett R.l.A. Blcranowelssia clrrata (L.) Lindb. Antrim— On thorn bushes in Cave Hill Deerpark, C.H.W Dicranum majus Sm. Derry— Lignapeiste Glen, Mrs. Leebody. D. Bonjeanl De Not. Down — Slieve Dermot, Lett R.l.A. Antrim — Parkmore, H.W.L. D. fuscescens Turner. Down— Shanlieve, C.H.W. ; Lett R.l.A. Scottll Turner. Down — Hen Mountain, Lett R.l.A. Dlcbodontlum pelluddum (L.) Schimp. Antrim Cushendall, H. N. Dixon, Journ. Bot. 1891. D. flavescens (Dicks.) Lindb. Antrim— Ballycastle, H. N. Dixon, Journ. Bot. 1891. 222 [Appendix B.N.F.C., TOETU1ACESI. Pott la Helmii (Hedw.) Fuem. Antrim — Giant’s Causeway, H. N. Dixon, Journ. Bot. 1891. Derry — Between Portstewart and Bann mouth, H.W.L. P. Starke! (Hedw.) C. Muell. Antrim- Ditch-bank at Ballysillan limestone quarries, S.A.S. Tor tula ericcefolia (Neck.) Lindb. Down— Old quarry at Maralin, H.W.L. Antrim— Ditch-bank at Ballysillan limestone quarry, S.A.S. T. paplllosa Wils. Down— Drumsallagh, Aghaderg, H.W.L. Ti princeps De Not. Antrim -Gleuarm Deerpark, D.M. ; Brit. Most Flora. Derry — Benevenagh, S.A.S.; Brit. Most Flora. Mollia microstoma Lindb. Down— Near Warrenpoint, C.H.W. ; Lett R.I.A. Antrim— Ballycastle, H. N. Dixon, Journ. Bot. 1891. XVI. aeruginosa (Sm.) Lindb. Antrim-Parkmore and Glenballyemon, H.W.L. Drumnasole, S. A. Brenan; H.W.L. M. verticillata (L.) Lindb. Down— Wall of bridge in Tollymore Park, C.H.W. ; Antrim— Glenarm, H. N. Dixon, Journ. Bot. 1891. H.W.L. M. crispula (Bruch) Lindb. Antrim— Ballycastle, in fruit, H. N. Dixon, Journ. Bot. 1891. M. lit or alls (Mitt.) Braith. „ , 1Qn1 Antr i m — Cushendall and Ballycastle, H. N.|Dixon, Journ. Bot. 1891. M. bracbydontia Lindb. Down — Kinehalla, H.W.L. 1VX. tenuirostris (Hook. & Tayl.). Down — Several stations in Mourne Mountains, H.W.L. i*94-95-3 223 M. lnclinata (Hed.) Lindb. Antrim — Portrush, H.W.L. Derry — Portstewart, H.W.L. B*. tortuosa (L.) Schrank. Antrim— Drumnasole, S. A. Brenan ; H.W.L. Barbula curvirostris (Ehr.) Lindb. Down— Cove Mountain, Lett R.I.A. B. spadlcea Mill. Down— Tollymore Park, Lett R.I.A. B.rlgldula (Hed.) Mitt. Antrim — Fairliead, H. W.L. B. cylindrlca (Tayl.) Schimp. Antn^7?891ballyem°n’ H'W,L- Custendl>11. H. N. Dixon, Journ. B. ung-uiculata (Huds.) var. y. apiculata Hedw. Down— Wall of Agbaderg Glebe, H.W.L. Eeersia contorta (Wulf.) Lindb. Antrim— Rocksat upper end of Colin Glen, J H. Davies. Glenballyemon, H.W.L. Glendun, S. A Brenan; H.W.L. WEBER ACE JE. Webera sessllls (Schmid.) Lindb. Antrim— Slemish Mountain, H.W.L. m Fl°ra t0 be barf®n- This was an error, as Mr. Lett finds it fruiting freely from early summer till late in autumn. GXIMMZACEE. Grimmia funalls (Schwaeg.). Down— Sliere Dermot, Lett R.I.A. orbicularis Bruch. Down— Top of stone fence onfSpelga M ountain, H.W.L. ; Brit. Moss Flora This is the only locality in the North of Ireland known to us. 224 [Appendix B.N.F.C-, G. trichopliylla Grey. Down— Fofanny, and Butter Mountain, Lett B.I.A. Bryansiord, C.H.W., Brit. Moss Flora. Antrim — Basalt rocks at summit of Bally gaily Head, S.A.S. G. Hartman! Schimp. Antrim— Fairhead, H. N. Dixon, Journ. Bot. 1891. G. Donii Sm. Down— Granite blocks between Slieve Martin and Kilbroney bog, Lett R.I.A. G. ovata was hastily inserted as an addendum when the Flora was at Press. This must be deleted, as it was subsequently ascertained to be an erroneous determination. G. obtusa (Sm.) . Lindb. Down — Shanslieve, Slieve Donard and Slieve Bingian, Lett; Brit. Moss Flora. G. affinis (Scbleicb.) Lindb. var. p. grracilescens Lindb. Down— Shanslieve, Lett ; Brit. Moss Flora. G. patens (Dicks.) Br. et Schimp. Antrim- -The Craig rocks, Rasharkin, H.W.L. By inadvertance 2700 was printed in Flora for 1200 feet, the highest elevation known to us. ORTHOTRICACEJE. Orthotrichum Sturmii. The Lough Neagh locality of Flora must be transferred to 0. striatum. Ortbotrlchum diaphanum Schrad. Down — Donard demesne and Loughbrickland, H.W.L. 0> cupulatum Hoft'ni. Antrim — Glenarm, H. N. Dixon, Journ. Bot. 1891. O. stramlneum Homsch. Antrim— Fairhead, D.M.; herb. Carrington, fide G. A. Holt. O. rlvulare Sm. Antrim— Ram’s Island, J. H. Davies. s 894-95.] 225 O. pulchellum Sm. Down — On apple trees at Ravernet, J. H. Davies. Antrim — Barkmore, H.W.L. Weissia Bruchli (Hornsch.) Lindb. Antrim — Glenariff, S.A.S. Glendun, S. A. Brenan; H."W.L. W. vittata (Mitt.) Braith. Antrim— Glenshesk, 1880, and Glenariff, 1889, S.A.S.; Brit. Moss Flora. SPIACHITAGE^;. Tetraplodon bryoides (Mitt.) Braith. Antrim— Glenariff, S. A. Brenan. Funaria obtusa (Dicks.) Lindb. Antrim — Sallagh Braes, C.H.W. P. attenuata (Dicks.) Lindb. Down — Wet rocks near Donaghadee, J. H. Davies. Antrim — Islandmagee, J. H. Davies. Derry — Benbradagh Mountain, Mrs. Leebody. It is to be regretted that the name of Templeton, our pioneer botanist, which was associated with this plant by Smith in 1813, has to be replaced by a prior term. J * P. calcarea Wahlenb. Antrim— Near Carrick-a-rede, H. N. Dixon, Journ. Bot. 1891. BUTACSJE. Beptobryum pyriforme (L.) Wils. Down— Abundant on flower-pots at Aghaderg, H.W.L. Poblla acuminata Hornsch. Down— Wet rocks at Blackstairs, Slieve Donard, and on Spaltha Moun- tain, Lett R.I.A . P. nutans (Schreb.) Lindb. var, longlseta Brid. Down— County Down [Cotton Moss], S.A.S. ; Brit. Moss Flora. 226 [Appendix B.N.F.C., P. annotina (L.) Lindb. Down — Shanlieve, S.A.S Slieve Bingian, Lett R.I.A. P. albicans (Wabl.) Lindb. Down — Wayside well near Fofanny, Lett R.I.A. Plaglobryum Zierii (Dicks.) Lindb. Antrim — Sallagb Braes, C.H.W. Bryum inelinatum (Swaitz) Bland. The station in Victoria Park assigned to this species was an error, the plant having subsequently been decided to be B. intermedium. Bryum Mildei Juratz. Antrim— Slemish Mountain, Moore ; Brit. Moss Flora. B.alpinum Huds. Down— White Eiver Glen, Lett R.I.A. Fruiting very sparingly in Moume Mountains, S.A.S., July, 1888. Antrim — Rasharkin bog, H.W.L. & C.H.W. B. pallens Swartz. Down — Slieve Donard, Lett R.I.A. Antrim — Parkmore, H.W.L. B. ventricosum Dicks. Down — Leitrim near Hilltown, and frequent in the Mourne Mountains, Lett R.I.A. Antrim— Near Parkmore, H.W.L. By the stream in Glenshesk, in fine fruit, J. H. Davies. Derry — Lignapeiste Glen, Mrs Leebody. B. proliferum (L.) Sibth. (B. roseum Dill.). Down— Newcastle, C.H.W. BARTRAMZACEiE. Bartramla pomiformis (L.) Hedw. Antrim — Drumnasole, S. A. Brenan ; H.W.L. B. norvegica (Gunn.) Lindb. Antrim — Fruiting in Glenariff, H.W.L. B. fontana (L.) Swartz var. p. falcata Brid. Antrim — Rasharkin, H.W.L. & C.H.W. *894-95-] 2 27 1TCITXACEJ&. Gymnocybe palustris (L.) Fries. Antrim— Glendun, S. A. Brenan ; H.W.L. Aulacomnium and Sphcerocephalus must give way to the prior name of Fries. Mnlum rlparlum Mitt. Antrim — A few barren stems intermixed with other mosses in wet bog at Glenariff, H.W.L. The only Irish locality known at present. AX. cuspidatum (L.J Neck. Antrim — Wet ditch at Hightown, Carnmoney, G.H.W. M. pseudopunctatum Bruch & Schimp. Antrim — Parkmore, H.W.L. HYPWACE51. X*eskea polycarpa Ehr. Down — Loughbrickland, H.W.L. Anomodon vltlculosus (L.) Hook. & Tayl. Antrim — Fruiting at Drumnasole, S. A. Brenan ; H.W.L. Hypaum filiclnum Linn. Antrim — Glendun, S. A. Brenan; H.W.L. H. confervoides Bridel. Derry— Sandy warren at Portstewart, S.A.S., 1884. The only Irish station. H. lrrigruum Wils. Down — Rocky stream in Drumbo Glen, S.A.S. Doubtfully mentioned in excluded list of Flora. H. rlparium Linn. Down — Shore of Loughbrickland, H.W.L. Antrim — By the Lagan near Glenmore, J. H. Davies. Pond by railway line north of Kilroot, S.A.S. Parkmore, H.W.L. H. stellatum Schreher. Down — Stormount Glen, and marsh on Conlig Hill, S.A.S. 228 [Appendix B.N.F.C., Antrim— Glendun, S. A. Brenan ; H.W.L. Abundant in Rasharkin bog, H.W.L. X. fluitans Linn. Antrim— Parkmore and Lurgethan, H.W.L. Glendun, S. A. Brenan; H.W.L. H. Xneiffii Br. & Schimp. Down — Near shore of Lough Neagh at Kilmore, C.H.W. Loughbrick- land, H.W.L. H. revolvens Swartz. Down— Slieve Dermot, Lett R.I.A. Antrim — Glenballyemon, H.W.L. Derry — Marshes in Portstewart sandhills, S.A.S. X. scorpioides Linn. Down— Margin of Bally ward Lake and of Pollramer Lake, and in fruit in a marsh on Conlig Hill, S.A.S. Antrim— Glenariff and Glendun, H.W.L. H. ocliraceum Turner. Antrim — Glenariff, H.W.L. H. sarmentosnm Wahl. Down — Shanslieve, Lett R.I.A. X. Swartzii Turner. Antrim — Glendun, S. A. Brenan ; H.W.L. X. speciosum Brid. Antrim— Knockagh, C.H.W. X. crassinervum Tayl. Antrim— Knockagh, and on wall at Carnmoney, and on limestone blocks in Cave Hill Deerpark, C.H.W. Glenariff, H.W.L. X. piliferum Schreb. Down — Tollymore Park, C.H.W. Antrim — Glendun, S. A. Brenan ;\H.W.L. X. tenellum Dicks. Down — Greenhouse at Aghaderg Glebe, H.W.L. Wall of bridge in Tollymore Park, Lett R.I.A. «*94-95-] 229 Antrim — Walls about Code Glebe, Carnmoney, C.H.W. Parkaore H.W.L. Drumnasole, S. A. Brenan ; H.W.L. B. flagellare Dicks. Down— Rocks by the river at Tollymore Park, Templeton (spec, in herb. Belf. Mus.). Slieve Donard, Slieve Commedagh, and frequent in the Moume range, but always barren, S.A.S., Suppl. to Mosses of N.E. Ireland. Tollymore, Yellow Water, &c., frequent, C.H.W. Common throughout the Mourne range, Lett R.I.A. Antrim — Glenariff, H.W.L. Localities for this species were published in Supplement to Mosses of North- East Ireland , but accidentally omitted from Flora. B. heteropterum (Bruch). Down — Slieve Bingian and Slieve Meel Beg, Lett R.I.A. Rostrevor Mountain, C.H.W. Antrim — Slemish Mountain, H.W.L. & C.H.W. In following Moore and giving R. atrovirens Turner as a synonym for UR. heteropteronf the authors of the Flora were in error, as Mr. Lett has pointed out to us. Moore’s second synonym, R. catenulatum , is likewise erroneous., B. cupresslforme Linn. var. lacunosum Wils. Down— Slievenabrock, Lett R.I.A. B. resupinatum Wils. Down— Slieve Donard, H.W.L. B. Patlentlse Lindb. Down — Saintfield, C.H.W. Antrim— Glendun, S. A. Brenan; H.W.L. Carnmoney and Hydepark, widely distributed, C.H.W. B. Borrerl Spruce. Down — Saintfield, C.H.W. Sandy bank at Knocknagoney, S.A.S. Antrim — Slemish and Sallagh Braes, C.H.W. B. pnlehellum Dicks. Down — Tollymore Park, C.H.W. Antrim— Glenariff, C.H.W. & H.W.L. B. nxtdulatnm Linn. Antrim — Parkmore, H.W.L. Derry — Benbradagh Mountain, Mrs. Leebody. 230 [Appendix B.N.F.C. H.sylvaticum Linn. Down — Slieve Donard, Lett R.I.A. H. dentlculatum Linn. Down — Chimney Rock Mountain, Lett R.I.A. In a small glen close to Dundonald station, S.A.S. SP1A6NACE3:, Sphagnum Austlni Sulliv. Antrim — Evish Mountain near Parkmore, H.W.L., 1889. Mr. Lett, who was the first to find this plant in Ireland, has subsequently (1892) met with it in King’s County. S. papillosum Lindh. Down — Common in Moume Mountains, Lett R.I. A. Antrim-Parkmore, H.W.L. Glendun, S. A. Brenan; H.W.L. S.tenellum Ehr. Antrim — Glendun, S. A. Brenan; H.W.L. g, snbsecandnm Nees & Von Es. Antrim — Crockalough near Parkmore, H.W.L. var. obesum Wilson. Derry— Racecourse bog at Ballyamot, Mrs. Leebody. S. rigldum Nees & Von Es. var. p. compactum DC. Antrim— Parkmore, Crockalough, and Rasharkin hog, H. W .L. Glendun, S. A. Brenan ; H.W.L. S. teres Angst. Down — Hen Mountain, Lett R.I.A. The only Irish station known at present. S. acutifollum Ehr. Antrim — Glendun, S. A. Brenan; H.W.L. A number of varieties of this polymorphic species occur. S. Intermedium Hoffin. Antrim — Parkmore, H.W.L. *894-95-3 231 S. cuspidatum Ehr. Down — Rostrevor Mountain, C.H.W. ; Lett R.I.A. Antrim — Parkmore and Glenballyemon, H.W.L. var. plumosum Nees & Hsch. Antrim— Glendun, S. A.. Brenan; H.W.L. HEPATIC^. JUJTCBBMAirwIACEJE. Prullanla fragillfolia Tayl. Antr™~ “LThe Craigs,” Rasharkin, H.W.L. & C.H.W. Glenariff, Xiejeunea hamatlfolla Hook. Antrim — Glenariff, C.H.W. Xu calcarea Libert. Antrim— Glenariff, H.W.L. and C.H.W. Xu ovata (Dioks.) Tayl. Antrim — Glenariff, C.H.W. Xu mioroscoplca Tayl. Antrim — Glenariff, C.H.W. Xu patens Lindb. Antrim— On NecJcera crispa at Sallagh Braes, H.W.L Mackali (Hook.) Spreng. Down— On an old yew tree in Tollymore Park, C.H W • Lett R I. A ^ 18°9’ T6mplet0n- 'GobM* Porella rlrularls Nees. Down — Saintfield, C.H.W. Plenrozia purpurea (Ligbtf.) Dum. Antrim— Rasharkin bog, H.W.L. & C.H.W. Evish Mountain, H.W.L. [Appendix B.N.F.C., 232 Trichocolea tomentella (Ehr.). Down— By a rivulet in Belvoir Park, Templeton. Antrim — Glendun, S. A. Brenan; H.W.L. X.epldozla setacea (Web.) Dum. Down— Hen Mountain, Lett R.I.A. Tollymore Park, H.W.L. Antrim— Glendun, S. A. Brenan ; H.W.L. Kasharkin bog, H.W.L. Bazzanla trllotoata (L.) Gray. Down— Tollymore Park, Templeton. Odontoschlsma sphagni (Dicks.). Down— Tollymore Park and Cock Mountain, C.H.W. ; Lett R.I.A. Antrim— Clougbcor near Parkmore, H.W.L. Cephalozla divaricata (Sm.). Down— Hen Mountain and bog between Hilltown and Kathfnland, Lett R.I.A. Tollymore Park, C.H.W. Antrim — Parkmore, H.W.L. This was probably the plant noted by Templeton as C. byssacea , occurring at Lambeg, Cranmore, etc. C. connirens (Dicks.) Spruce. Down — Slievenamady, Lett R.I.A. Kantia tricbomanis (Linn.). Down— Bog near Ballynahinch, H.W .L. Antrim — Glendun, S. A. Brenan ; H.W.L. Parkmore and Lurgethan, H.W.L. Seapania nemorosa (L.) Dum. Down— Saintfield, frequent, C.H.W. Antrim— Glendun, S. A. Brenan ; H.W.L. Lurgethan, H.W.L. S.resupinata (L.) Dum. Antrim — Fairhead and Glendun, in company with Taylor, Hooker, and Stokes, Templeton. S. nmbrosa (Schrad.) Dum. Down — Hen Mountain, H.W.L. 8. curta (Mart.) Dum. Down— Bally varley bog, Aghaderg, H.W.L. 1 894-95 *3 233 Chlloscyphus polyanthos (L.) Corda. Down— Aghaderg Glebe and Ballyvarley bog, H.W.L. Antrim— Slemisb, Templeton. Glendun, S. A. Brenan ; H.W.L. Xieptoscyphus lnterruptus Nees var. p. pyrenalcum Spruce. Down— Roadside wall south of Rostrevor quay, H.W.L, Plaglocblla splnulosa (Dicks.) Dum. Antrim Gobbin cliffs, C. H . W. Drumnasole and Rasharkin bog, H.W.L. P. trldentlculata (Tayl.). Antrim— Drumnasole, S. A. Brenan; H.W.L. Jungrermannla rlparla Tayl. Down — Cove Mountain, Lett K.I.A. AntrS1~C1olin/^len} C.H. W. Drumnasole and Glendun, S. A. Brenan ; H. W .L. Glenariff and Rasharkin bog, H.W.L. T. crezralata Sm. var. gracilllma Sm. I)ow^^<^ymore park and Slieve Commedagh, Lett R.I.A. Aghaderg, J. p ami la With. Antrim— Glendun, S. A. Brenan ; H.W.L. Slievenanee, H.W.L. J. sphserocarpa Hook. Antrim— Colin Glen, 1818, Templeton. Parkmore, H.W.L. V.barbata Schreb. (Coll.). Antrim— Rasharkin bog and Slemish Mountain, H.W.L. Given by Mr. Lett as J . barbata var. quinquedentata, but Schreber’s species seems inseparable from quinquedentata Hudson. IflTardia spbaoelafa Giesecke. Down— Slieve Donard, J. J. Andrew ; H.W.L. Iff. hyallna (Lyall) Carring. Down — Cove Mountain and Hen Mountain, H.W.L. Antrim — Parkmore, H.W.L. Cesla crenulata (Gottsche) Carring. Antrim — Shady rocks on north-east side of Slemish, H.W.L. & C.H.W. 234 [Appendix B.N.F.C., Pellla calycina (Tayl.). Down— Aghaderg, H.W.L. Antrim— Drumnasole, S. A. Brenan ; H.W.L. Parkmore, H.W.L. Aneura pingals (L.) Dum. Derry — Portstewart, S.A.S. A. multlfida (Dill.) Gray. Down — Loughbrickland, H.W.L. Antrim — Seymour Hill, Templeton. MARCHAirTXACBJE. Preissia commutata Nees. Down — Scarya demesne, H.W.L. Antrim— Parkmore, H.W.L. Glendun, S. A. Brenan; H.W.L. 3bunularia cruclata (Linn.) Dum. Down — Drumcro, C.H.W. Agliaderg, H.W.L. Antrim— Moss hole at Seymour Hill, Templeton, 1806. East end of Belfast Botanic Gardens, H.W.L. *ICCXACE.ffi. XUccla fluitans Linn. Down — Abundant in a drain at Meenan bog, Loughbrickland, H.W.L. ANTBOCEROTACZ2:. Anthoceros punctatus Linn. Down — Clover and stubble fields in Parish of Aghaderg, H.W.L. Antrim — Belfast Botanic Gardens and river bank in Glendun, H.W.L. 1894-95*] 235 ERRONEOUS OR DOUBTFUL HEPATICS. SS.Tii",E“ *“ “-’I" "■>"». “* >“• 1- Porella thuja. On the rock at the waterfall in Woodburn Glen, 3lst March, Cephalozia curvifolia. Rock crevices on Bingian Mountain. C. byssacea. Lambeg, Cranmore, and Birky moss. Sarpanthus scutatus, Glen below Rockport. Plagiochila, tridentieulata. Common on the rocks of the Cave Hill. Mylm AnnaMlt bog and summit of Divis. [Perhaps the same plant Jungermannia cuneifolia. Near top of Divis. J. pumila. Common on bare ground about Belfast. 7. barbata Common in the recumbent state on the rocks about the Cave Hill : also on Divis Mountain, and in Ness Glen. ’ J. exsecta. With the next species on Holy wood Warren. 7 excisa. Divis and Black Mountain, and on Holywood Warren. J‘ inCiSh»„ vLAmbegA ™°°r Jalfwa7 tween Holywood and Bangor, and rocky bank above the Manyburn at Purdysburn racecourse. Nardia compressa. Near Belfast. Hnfp l\e«fT?S°ln^ llst ^emPleton’8 nomenclature, which was that current in his time, has been replaced by names now adopted. 236 [Appendix B.N.F.C., ADDENDA ET CORRIGENDA. p. 135. Add Grimmia ovata to the list of plants to be withdrawn from Flora. n 139 Sparg atrium neglectum was recorded prematurely ; on referring the specimen to the describer of that form, it was named by him S ramosum var. microcarpum , and is recorded under that name in the body of the Supplement, p. 201. . , pp 142-3. A number of specimens of cryptogams have been examined and verified since the first portion of the manuscript went to press, and the following have to be placed to lists of additions in the Introduction. DISTRICT 12. Hypnum confervoides. Bryum Mildei. H. Jlagellare. COUNTY DOWN. Hypnum Jlagellare. COUNTY ANTRIM. Tortula princeps. Bartramia norvegica. Hypnum Jlagellare. COUNTY DERRY. Hypnum confervoides. Funaria attenuata. H revohens. Aneura pinguxs. A BIBLIOGRAPHY OF IRISH GLACIAL AND POST-GLACIAL GEOLOGY BY R. LLOYD PRAEGER, B.E. Being an Appendix (No. 6 op Vol. 2) to the Proceedings of the BELFAST NATURALISTS’ FIELD CLUB For 1895-96. A BIBLIOGRAPHY OF IRISH GLACIAL AND POST-GLACIAL GEOLOGY. THE following list of books, papers, and notes bearing on the glacial and post-glacial geology of Ireland bad but a small beginning. It originated in a few dozen references to records of post-glacial fossils in the North-east of Ireland, thrown together for my own convenience. This list was added to by degrees, accumulating according to the manner of a snowball, each paper giving references to a number of others. Eventually, it appeared to me that if the list could be extended, completed, and published, it might prove a saving of time and labour to other workers ; and in this thought I had especially in my mind the energetic members of the Geological Section of the Belfast Naturalists’ Field Club, who have not convenient access to many of the journals, &c., quoted below, and on whom Prof. Cole recently urged1 the importance of getting together their local geological literature. In order to complete the list, systematic work was necessary, and sets of Periodicals and Proceedings of Societies which might contain references to Irish geology had. to be carefully gone through. This portion of the work proved more extensive and tedious than ;was expected, and indeed had I known how much time it would involve, it is doubtful if the present effort would have seen the light. But in spite of time and care, I am well aware that my list must contain many omissions, though it is hoped that none of them are serious ones. Geologists working at any branch of the subjects included in the present com- pilation, or at the geology of any particular district, are nearlv sure, among the scattered records of Irish geology, to unearth some references which, in my necessarily hurried work, have escaped notice. To them I would appeal to favour me with a note of such references, in order that, by the publication of a supplement, the present attempt may justify its title, and become a complete guide to the literature of Irish glacial and post-glacial geology. As to the scope of the present list. Although believed to be of Pliocene, not Pleistocene age, the so-called “ manure gravels ” of Wexford have been included. They are the only marine Tertiary beds in Ireland, and are moreover of late Pliocene age, possessing a fauna distinctly related to that of the incoming glacial period ; when to these is added the fact that the literature relating to the Wexford beds is .much mixed up with that of the succeeding series, the advantage and convenience of this inclusion will be apparent. In view of recent papers in the Irish Naturalist on caves, and Dr. Scharff’s bibliography of that subject, references to caves have been included, even if these references had no distinctly geological bearing ; for much cave-exploration remains to be carried out in Ireland, as to both their past and present fauna ; and a list of localities is therefore a desideratum. In dealing with the human period, a difficulty constantly presented itself as to 1 Irish Naturalist, IV., 49. 1895. 240 [Appendix B.N.F.C., how far papers on the remains of pre-historic man were admissible in a geological bibliography. Thus, while a flint implement found in the stratified marine gravels of Antrim, or a bronze celt in a stalagmitic deposit, are objects of distinct geological interest, the same cannot be said of a cinerary urn found in a kist, or a flint arrow-head which the urn may have contained. But it is difficult to draw the line, for geology and archaeology not only meet, but overlap. The rule which I have endeavoured to follow is to admit papers which describe the mode of occurrence or stratigraphical position of human relics, and to omit papers dealing with objects artificially buried, or merely with the affinities or ornament of objects found. Thus sand-hill sites, crannogs, cave-deposits, and flint implement gravels are included ; but papers 04 such subj ects shade imperceptably into others which are purely ethnographical in their bearing. In the way of existing bibliographies there was very little to assist me. The only papers giving even a tolerably complete bibliography of any part of the subjects included in the present paper, or of any district, were Dr. V. Ball s list of papers on Irish fossil mammals (39)* and Mr. Hardman’s list of papers on North of Ireland geology (251). The shorter lists of papers given by Adams (5, 6), Close (129), Cole (136), Gray (232), Hull (297), M'Henry (492), and Scharff (607), were of course consulted. I made a point of verifying every reference by consultation of the original publication, where possible; the few papers (4 out of the 767 which have a place in the list) which I was not able to consult are distinguished by an asterisk .. Subjoined are particulars relating to Proceedings of Societies and to Journals systematically examined for references to the subject included in the list, the contracted titles used in the list being added in parenthesis : — ACADEMIES' PROCEEDINGS , $c. British Association for the Advancement of Science : Reports , years 1 — 64, 1831-1894. (Brit. Assoc. Reports .) Geological Society of London : Quarterly Journal, I. — LI., 1845-1895. ( Q.J.G.S .) Geologists’ Association, London : Proceedings , I.— XIV. pt. 5, 1859-1895. ( Proc . Geol. Assoc.) Anthropological Institute : Journal, I. — XXV. pt. 2, 1871-1895. (Journ. Anthrop. Inst.) Geological Survey of Ireland : Memoirs , 120 parts, 1858-1891. 8vo. Royal Irish Academy : Proceedings, I.— X., 1836-1870; 2nd s. {Science), I.— IY., 1869-1888; 2nd s. {Polite Literature and Antiquities), I.— II., 1870-1888; 3rd s., I.— III. pt. 4, 1887-1895. 8vo. (Proc. R I. A.) Transactions , I. — XXX. pt. 17, 1785-1895. 4to. {Trans. R.l.A ) Royal Dublin Society : Journal, I. — VII., 1856-1878. 8vo. (Journ. R.D.S.) Scientific Proceedings, n.s., I. — VIII. pt. 4, 1878-1895. 8vo. {Sci. Proc. R.D.S.) * The numbers refer_to the index numbers in the general list. 895-96.] -24I SeimtTr°am. 'Tes.)*’ ^ S" L_V' pt' U> 18”-1895- 4to. (Sci. Geological Society of Dublin : Journal, I.— X., 1833-1864. (Jomn. G.S.D.) E°Tof DubUn)°?CAL S°CIETY 0F lKELAND (previously Geological Society Jmrt.6ls7L)lli' (XI _XVIIL °f whole aeries), 1864-1889. (Journ. Dublin Natural History Society : Proceeding s, I.-VI., 1849-1870. (Proc. Dublin Nat. EM. See.) Belfast Naturalists’ Field Club : Reports, 1 10, 1863-4 — 1872-3. [Ann. Reports B.N.F C) Annm^SeporUm^Proceedings, 2nd s„ I.-IV. pt. 2, 1873-4-1894-5. Belfast Natural History and Philosophical Society: Proceedings, 11 yols., 1871-2— 1881-2. Reports and Proceedings, 13 vols., 1882-3—1894-5. {Proc. B.N.H. 4 Cork Historical and Archeological Society • Jour7 y;r™;.) 1892-1894 ; 3ndn-3j- 1895- <** Kilkenny Archeological Society : Transactions, I.-II., 1849-1853. (Trans. Kilk. Arch. Soc ) Proofings and Transactions, UI., 1854-1855. (Proc. and Trans. Kilk. Kilkenny and South-East of Ireland Archaeological Society - (Previously Kilkenny Archaeological Society.) JOUrlrckntc.f~yL’ 1856‘1867- Kilk. t S.E. Ireland Historical and Archeological Association of Ireland : (Previously Kilkenny & S.E. Ireland Arch. Soc.) Journal, 3rd s., I., 1868-1869. {Journ. U. § A. A. I.) Koyal Historical and Archeological Association of Ireland- (Previously Hist. & Arch. Assoc, of Ireland.) Journal, 4th s., I.— IX., 1870-1889. {Journ. R.H. $ A.A.I.) Koyal Society of Antiquaries of Ireland : (Previously R. Hist. & Arch. Assoc, of Ireland.) Fr°CeRhS.SA 7) PaPerS’ 5th S,/ L’ 1890-1891* (Proc. and Papers Journal, 5th s., II.— V., 1892-1895. {Journ. R.S.A.I.) J 0 TJRN ALS, $c. Geological Magazine : Decade 1, vol. I. to decade 4, vol. II., 1864-1895. {Geol. Mag.) 242 [Appendix B.N.F.C., Geologist , The : From 1858 to 1864. Glacialists' Magazine : I.—III. pt. 3, 1893-1895. Geological Record : From 1874 to 1884. Annals of British Geology : From 1890 to 1894. Natural History Review : I. VII., 1854-1860; andn.s., I.— V., 1861-1865. [Nat. Hist. Review .) Dublin Quarterly Journal of Science: I.—VL, 1861-1866. (. Dublin Q.J.S.) Dublin Philosophical Journal and Scientific Review : j 1825-1826. ( Dublin Phil. Journ. $ Scient. Review.) Irish Naturalist : I.— IY., 1892-1895. [l.N.) Ulster Journal of Archeology : I.— IX., 1863-1862. New Issue, I., 1894-95. [Ulst. Jour n. Arch.) About a hundred books on geology, archeology, topography, &c., which contained, or might have contained, references to the subjects in hand, were likewise looked through. Occasional references were also made to the following ACADEMIES' PROCEEDINGS , $c: — Royal Society of London : Philosophical Transactions. [Phil. Trans.) Geological Survey of Great Britain : Memoirs. Paljeontographical Society : (. Publications .) Geological Society of London : Proceedings. ( Proc . Geol. Soc. London.) Zoological Society of London : Proceedings. [Proc. Zool. Soc. London.) Society of Antiquaries of London: Proceedings. [Proc* Soc. Ant. London.) Manchester Geological Society: Proceedings. [Proc. Manchester Geol. Soc.) 1895-96.] 243 Literary and Philosophical Society of Manchester : Proceedings. ( Proc . Lit. $ Phil. Soc. Manchester .) Liverpool Geological Society : Proceedings. {Proc. Vpool Oeol. Soc.) Geological and Polytechnic Society of the West Riding of York- shire : Proceedings. (Proc. Geol. $ Polytechnic Soc. of W. Riding of Yorks.) Society of Antiquaries of Scotland : Proceedings. (Proc. Soc. Ant. Scotland.) Edinburgh Geological Society : Transactions. (Trans. Edinb. Geol. Soc.) Royal Physical Society of Edinburgh : Proceedings. (Proc. R. Phys. Soc. Edinb.) Geological Society of Glasgow : Proceedings. (Proc. Geol. Soc. Glasgow.) Natural History Society of Glasgow : Proceedings. {Proc. Nat. Hist. Soc. Glasgow.) Royal Dublin Society : Proceedings .* {Proc. R.D.S.) Waterford and South-East of Ireland Archaeological Society : Journal. (Journ. Waterford $ S.E. Ireland Arch. Soc.) Museum d’Histoire Naturellb (Paris) : Annales. Sooiete de Speleologie (Paris) : Spelunga : Bulletin. JOURNALS , $c.— Academy. Annales des Sciences Naturelles. Annals and Magazine of Natural History. (Ann. $ Mag. Nat. Hist.) Annals of Philosophy. Archceologia. Archmologieal Journal. Dublin Evening Telegraph. Dublin Penny Journal. Edinburgh Journal of Science. Edinburgh New Philosophical Magazine. (Edinb. New Phil. Mag.) Farmers ’ Gazette. Irish Penny Magazine. Magazine of Natural History (Mag. of Nat. Hist.) * Not to be confounded with the Scientific Proceedings issued by this Sooiety. •244 [Appendix B.N.F.€., Natural Science. Nature. Philosophical Magazine. {Phil. Mag.) Popular Science Review. Science Gossip. Zoologist. {Zool.) It onlv remains to add a few particulars concerning the list which follows. Brackets are used to show all editorial additions— the subject of papers which have no printed title, the names of authors of papers published anonymously, and all editorial comments, &c. . . , When the title of a paper does not sufficiently express its scope, a bnet note of its contents is added. ..... A hook or paper is not included in the list if it merely quotes from another without any original expression of opinion — such, for instance, are the references to Irish glacial geology in certain general text-books of geology. Announcements of exhibits or donations, accounts of excursions, or other officially supplied items in the Proceedings of Societies, are entered under the name of the Society publishing them. When the date of the reading of a paper before a Society diners from its date of publication, the former is usually -given in brackets in addition to the latter. The Volumes of Proceedings of Societies are usually published in parts, and the publication of a volume frequently extends over several years. In bound volumes there is frequently no means of discovering the date of publication of any particular paper, owing to the destruction of the covers or temporary title-pages of the parts ^ In such cases the date given without brackets is the date on the title-page of the volume ; the collective date of the volume being usually added in brackets immediately after the number of the volume. In addition to the contracted titles already given, the following contractions are used : — descr.=description ; ref.=reference ; locs.=localities , glac. glacial ; post-glac.=post-glacial ; geol.=geology. The list includes papers published up till the end of the year 189o. [895-96.] 245 LIST OF PAPERS, &c. A. (M.). “s°.f n- »■ Adams (A. Iieith). Rep°rt on the Exploration of the Shandon Cave. Trans. It I. A . ^ 3' 1876‘ [FUU 01 **>*■ -d Observations on the Remains of Mammals found in a Fossil State in Ireland. Journ. R.G.S.I. , IV., 246—248. 1877. Monographof the British Fossil Elephants. Palceontographical Soc., 1877-81. [Irish localities.] ’ On the Recent and Extinct Irish Mammals. Sci. Proc R D S ns II., 45-86, plates 1-5. (read 1878). 1880. ' ' Report on the History of Irish Fossil Mammals. Proc.R.I.A. (2) III. [Science), 89 — 100. 1878. [“Abridgement of the Report.”] 679, 680). Haugiiton, W. Boyd Dawkins, and John Uvans. First Report of the Committee appointed for the Purpose of exploring the Caves of the South of Ireland. Brit. Assoc. Report for 1880 209-2ll. 1880 [Consists of a report from R. and a letter from R. Day on Carngower.l See Ussher (678, Adams (A. Leith) S. IO 11 12 Second Report do. do. do. Brit. Assoc. Report for 1881 218—221. 1882. [Report from R. J. Ussher.] Adams (A. Leith), G. I, Kinahan, and R. J. Ussher. Explorations in the Bone Cave of Ballynamintra, near Cappagh, Countv Waterford. Sci. Trans. R.B.S., n.s. I., 177—266, plates 11— 14. 1881. [Full descr. of deposits and fossils.] Agassiz (Louis). On Glaciers, and the evidence of their having once existed in Scotland, Ireland, and England. Proc. Geol. Soc. Bond. Ill ii S27 — 332. 1840-41. [Brief ref. to Irish striated rocks]. ’ The Glacial Theory and its recent Progress. Edinb. New Phil. Journ XXXIII., 217 — 288. 1842. [Brief ref. to Irish erratics, p. 223.] Ainsworth (W.). An Account of the Caves of Ballybunian, Co. Kerry, with some mineralogical Details. 96 pp. 8vo. Dublin, 1834. [Descr.] 246 [Appendix B.N.F.C., 13 14 15 16 17 Allman (G. J-). , , Notice of erratic blocks of greenstone, occurring in tte neighbourhood of Bandon, County Cork. (Abstract.) Journ. G.S.D ,111., 242. 1847. Andrews (Mary K..). A Denudation at Cultra, Co. Down. LM, II., 16-J8» 1893; and Proc. B.N.F. C., (2) III., 629-632, plate (for 1892-93), 1893. [Post-glac. denudation.] Andrews (Thomas). . . , ... On some Caves in the Island of Rathlin and the adjoining Coast of the County of Antrim. Brit. Assoc. Report for 1834, 660. 1835. [Short abstract : general descr.] On the Composition of an Inflanimable Gas Issuing from. below the Silt-Bed of Belfast. Proc. B.N.H. 4 F.S. for 18/3-74,93—94. 1874. Audrows (^X^a)s On Oyster Deposits. Journ. R.G.S.I. , II., 13—15. (read 1867). 1871. [Those of Kenmare river are quite recent.] [For discussion on this paper see same vol., p. 132.] \ Philosphical Survey of the South of Ireland . . (1788), see Campbell (755). A Tour through Ireland (1780), see luckombe (760 18 19 20 21 22 Excursions through Ireland [1818], see Cromwell (754). Fossil Deer of Ireland. Dublin Phil. Journ. % Scimt.Pevim, , I., «*— 486. 1 825 ; reprinted in Annals of Philosophy , n.s. XI., 3U5 tu-. 1826. [Edit, notes, and extracts from Maunsell (503) and Dai. (266).] Kingston Cave. Dublin Penny Journ., II., No. 61 , 65—66. Aug. 31, 1833. [Discovery and descr. of Mitchelstown cave.] Stalactite Cavern at Mitchelstown. Dublin Penny Journ., III., No, 130, 201— 208, maps. Dec. 27,1834. [Ed. note: letter from Dr. Nichol : anon, letter: paper by Dr. Apjohn, reprinted (28).] Remarkable Discovery of Fossil Remains. Farmer's Gazette, V., 487, Nov. 28, 1846. Reprinted in Zool., V., 1593 — 1595, 1847, undei the title “ Discovery of the Bones of Deer and Cattle at Lougn Gur.” [Descr. of Lough Gur find by an eye-witness.J Ancient Lake -habitations of Switzerland and Ireland. _ Gist. Journ. Arch., YIL, 179—194. 1859. [Descr. of several Irish crannogs.J 1895-96.] 247 23 Anon. Human Remains. Geologist for 1862, 353. [Human body in gravel below 11 feet of bog, Earl of Moira’s estate, Co. Down]. 24 [Skeleton and horns of Irish deer in “ soil ” at bottom of pond, Fethard, Co. Tipperary]. Dublin Evng . Telegraph, Nov. 6, 1884. Findf, ^L?Hheads’ &c* [Note.] Troc. $ Papers R.S.A.I., (5)1., (1890-91), 485. 1892. [At Cappagh Bog, Adare, Co. Limerick.] General Guide to the Science and Art Museum, Dublin. 8vo. Dublin, 1892. [Preface by Y. Ball.] [List with Iocs, of Fossil Mammals of Ireland, pp. 28 — 25.] Antisell (T.). Irish Geology, in a series of chapters, containing an outline of the science of Geology, and a description of the various rocks dis- tributed on the surface of the Island, with some remarks on the climate. 84 pp. 12mo. Dublin, 1846. [Chap XI., Tertiary system.] L r 3 Apjohn (J.). On the newly discovered Cave situate between Cahir and Mitchelstown Journ. G.8.D. , I. (1833-38), 103-111 (read 1834), 1838- reprinted with lllustr. in Dublin Penny Journ., III. No 130 Dec. 27, 1834 (see 20.) Archer (F.). Notes on the Worked Flints of the Raised Beaches of the N.E. Coast of Ireland. Proc. Vpool Geol. Soc., IV. Hi. (1880-81), 209—216. 1881. [Good descr., Larne, Kilroot, &c.] Atkinson (George IS.). Kitchen Middens in the Estuary of Cork Harbour. Journ. R.R. OTlrUSh-] ^ 51 Excumon to Gobbing 6th Ann. Report (for 1868-69), 13. 1869. 52 53 Excursion to Larne. 1th Ann. Report (for 1869-70;, 23 1870 [Curran gravels and implements.] ' E“ P’Hnt-flak^&e J *** SeP°H (f°r 187°-71)> 16- 1871. 54 55 56 57 58 59 60 _“n ^ <** >5. 23- [Refifi«° thfLf^fS and “am“»th remains.! Proe., (2) I 166—167 (for 1875-76). 1876. K ' ’ Excursion to Killyleagh, &c. Proc., (2) I., 245 (for 1876-77). 1878 [Glac. beds of Strangford Lough.] V ° C‘ Excursion to Greenore Proc., (2) I., 332 (for 1878-79). 1879 [Kaised beach, implements, striae.] ' Excursion to Toome. Proc., (2) I., 401-402 (for 1879-80). 1881 [Diatomaceous earth, implements.] EXCU[Irish eTk ®r0mere- Froc-' W IT > 9 (for 1880.81). 1882. 250 [Appendix B.N.F.C., 62 6ft 61 II., 13 (for 1880.81). 1832. [Flint implements.] "Excursion to Woodbum. Proc., (2) II., 94-95 (for 1881-82). 1883. [Boulder clay.] 63 Excursion to Ballycastle Free [Ice-action at F airhead. Sandhill sites at White rarn y j Excursion to Larne. Pm., (2) 11. 107-108 (for 1881-2). 1883. [Raised beach, estuanne clay, implements.] 65 “ Excursion to Cultra. Proc., (2) II., 225-226 (for 1883-84). 1884. [Boulder clay with erratics. Implements.] Excursion to Ram’s Island. Proc., (2) II., 229 (for 1883-84). 1884. [Boulder clay with erratics.] Excursion to Toome. Proc (2) H„ 416 (for 1886-86). 1886. [Boulder clay, marl, peat.] Excursion to Mourne Mountains. Free., (2) II., 420 (for 1885-86). 1886. [Glaciation of the range. J 66 67 68 69 70 71 72 73 7ft 75 Excursion to Greyabbcy. Proc., (2) II., 428 (for 1885-86). 1886. [Butterlump stone, a large erratic.] Excursion to Knockagb. Proc., (2) II., 508 (for 1886-87). 1887. [Sea-cayes at 600 feet]. “Excursion to Portaferry, 4c. Proc (2) III., 18 (for 1887-88). 1888. [Raised beach, Bally quintm.] TRef to Stoneyford boulder clay.] Proc., (2) III., 91 (for 1888- 89). 1889! ^ Excursion to Scrabo. Proc., (2) III., 169-170 (for 1889-90). 1890. [Boulder clay.] Excursion to Mourne Mountains. Proc., (2) III., 181 (for 1889-90). 1890. [Ice- moulding on Moolieve.] Excursion to Kilroot. Proc., (2) 111 257-261 (for 1890-91). 1891. [Raised beaches, Kilroot and Whitehead.] i895-96*] 251 76 Belfast Naturalists’ Field Club 77 78 79 80 81 82 83 84 m-276 189^>. «»i. {im 189I-92>- 1892- ““ ‘[Ca^Sa'rite JR" « m- 362 (*» <2) m ’ 466 (fM 1892'93)- 1893- ExCUrpi0n.t? KiUough Ac. Proc., (2) III., 494 (for 1892-93) 1893 [Glacial section north side Xillough Bay.] V '' 1S93, Excursion to Portaferry, &c. Proc., (2) IV., 21 (for 1893-94) iscu [Glaciation at Bally quintin.] ' Excursion to Dundrum, &c. Proc., (2) IV 183 (fir 1894 om icqk [Raised beach of Newcastle sand-hills ] }‘ Excureion to Templepatrick (Geol. Section). /.IV, IV., 343 1895 [Boulder clay, erratic.] ’ - See Kendall (368). 85 Bell (Alfred). The Paleontology of the Post-glacial Drifts of Iceland. Geol. Ma9„ a., 447 453. 1873. [General descr. and lists of fossils.] y 1883- [Portlock’s glacial nrst Ee^f the Committee . . upon the •< Manure ” Gravels [GeSdes'cr.] Report for 1887, 299-211. 1888. Second Keport do . do. do. Brit. As, oc. Xeport for fossil’s.] [Wexford, Ellin ey, Bray ; details, 86 87 88 89 [Appendix B.N.F.C., 252 90 BXrtHddFinal Report do. do do for 1890, 410—424. 1891. [General descr. and fossil lists, Pliocene, glac., and post-glac. beds, Wexford to Portrusb.] 91 — Notes upon the Marine Accumulations in Largo Bay, Fife, and Portrusb, Co. Antrim. Proc. B. Phyc.Soc. Bdmb., X. ... (for 1889-90), 290— 297. 1891. [Lists of fossils.] Notes on the Correlation of the later and Lost-Pliocene Tertian* on either side of the Irish Sea with a Reference to the Fauna of the St. Erth Yalley, Cornwall. Proc. R.I.A., { 3) II., 620 64... 1893. [Correlations and fossil lists.] Bell (Robert G.). Notes on Pliocene Beds. Geol Mag., (3) IY., 554-558. 188/. [Ref. to Wexford reversed Fusus, p. 557.] 94 Benn (Edward). -cr ib [ Contemporaneity of Man and Megaceros in Ireland.] Proc. Kilk. L Arch. Soc., I. (1866-57), 155—159. I808. 92 S3 95 Observations on Irish Crannogs. Journ. Kilk. Arch. Soc., III. (1860-61), 86— 90. 1861. [Animal remains, &c.J 96 97 98 On flint implements found in the County of Antrim. Proc. Kilk. Arch. Soc., V. ii., 294-300. 1865. [Ref . to mode of occurrence.] Birmingham (John). ’ The Drift of West Galway and the Eastern Parts of Mayo. J°^rn- The VIII. ,28 38 (1858), Ul-lU (1859). 8 0 ; also .Bn . Assoc. Report for 18o7, Sections, 64— 60. 1858 [abstractj. [Sequence of beds, &c.] 1864. 99 100 [Remarks on Bears’ bones.] Journ. G.S.D., X. (1862-64;, 174. [From Co. Limerick.] On the Animal Inhabitants of Ancient Proc. i R.I.A , VIIL, 472—476. 1861-64 ; and Dublin Q.J.S., IV., 149— 1DZ. ieo*. [Bos and Megaceros chiefly.] Boate (Gerard), Thomas hlolineux, and others A Natural History of Ireland in three parts. 4to. Dublin, 1755. T Letter of Francis Nevii to the Bishop of Clogher on the Magnery find of elephant’s teeth (522), and Dr. thereon (509), with plate, reprinted from Phil. Trans. XXIX.). Dh^ourse concerning the -large Horns frequently Winder ground in Ireland . . . by Thomas Molyneux (508), with plate, (reprinted from Phil. Trans. XIX. ).J Bogs, Report of Commission on. See Commissioners (143). 895-96.] 253 XOl Boulger (G. S.). Msh Cave Exploration. Nature , XII., 212. 1875. TShort letter on Shandon caye.] *102 Cave Hunting in Ireland [abstract]. Proc. West London Scient. Assoc., I., 29—31. 1875. [Shan don cave.] 103 The first Irish Cave Exploration [abstract]. Proc. Geol. Assoc., IV., No. 8, 524 526. 1876. [Shandon. Descr. and animal remains.] 104 ®rady (Geor^e Stewardson), Henry William Crosskey, and David Robertson. Monograph of the Post-tertiary Entomostraca of Scotland, including species from England and Ireland .Palceontographical Soc., XXVIII., 18.74; [Lists of species from Woodburn boulder clay, Portrush raised beach, and Belfast estuarine clay.] 105 106 Brash (Richard Rolt). ; The Antiquities of Cloyne. Journ. KilJc. Arch. Soc.. 253 — 266. 1859. [Descr. of caves, p. 258.] Srenan (Edward). II. (1858-59), Notice of the Discovery of extinct Elephant and other Animal Eemains, occurring in a Fossil State under Limestone, at Shandon, near Dungarvan, County of Waterford. Journ. P.P.S., II., 344—350 plates 10 — 13. 1859 ; and Nat. Hist. Review, VI., 494 — 500. ] 859^ 107 Brownrigg (W. B.) and Theodore Cooke. Geological Description of the District extending from Dungarvan to Annestown, County of Waterford. Journ. GS.JD.JX. 8 12 (read 1860). 1862. [Ref. to caves.] 108 Bryce (James). On the Evidences of diluvial Action in the North of Ireland. Journ G.S.D., I (1833-38), 33-44 (read 1833). 1838. [Glacial beds* transported blocks.] 109 On some Caverns containing Bones, near the Giant’s Causeway. Brit Assoc. Report for 1834, 658-660. 1885. [Descr., list of animals.] HO Notice of a Tertiary Deposit lately discovered in the neighbourhood of Belfast. Phil. Mag., XXVI., 433—436. 1845. [Waterworks boulder clay : descr. and list of fossils.] 111 Bryce (James) and George C. Hyradman. Notice of an elevated Deposit of Marine Shells, of the Newer Pleiocene Epoch, lately discovered near Belfast. [Appendix to Portlock’s Geology of Londonderry $c. (572) pp. 738 — 740]. 1843. f Descr • list of fossils.] 112 Bulck (Rer. George Raphael). On Flint workshop sites at Glenhue, County Antrim. Journ. R H & A.A.I., (4) VI. i. (1883), 120-126. 1884. [Surface finds.]' 254 [Appendix B.N.F.C., 113 Suick (Rev. George Raphael . On a particular kind of Flint Knife common in the County of Antrim, Ireland. Proc. Soc. Ant. Scotland, XXII., 51— 61. 1888. [Kef. to sand-hill sites.] 114 Fresh Facts about Prehistoric Pottery. Proc. <$■ Papers P.S.A.I. , (5) I. (1890-91), 433-44-2, 4 plates. 1892. [Ref. to mode of occur- rence, &c.] 115 The Crannog of Moylarg. Journ. P.S.A.I., (5) III., 27 — 43, 5 plates. 1893. Second Paper, ibid., IV., 315 — 331, 2 plates. 1894. [Full descr.] 116 Burnside (William Smyth). [Memorandum on crannog finds]. Proc. P.I.A., V. ('1850-53). 214 — 215 (read 1851). 1853. 117 Busk (George). Report on the Animal Remains [of Brixham Cave]. Phil. Trans., CLXIIL, 499-572. 1873. [Ref. to Irish bears’ skulls, p. 543.] C. (J.) see Coleman (140,141). 118 Campbell (J. F.). On the Glaciation of Ireland. Q.T.G.S., XXIX., 198 — 225. 1873. Abstract in Geol. Mag.,X., 127. 1873. [Full paper: general glaciation, &c.j Campbell (Thomas) see 754. 119 Cane fRobert)i The Gigantic Irish Fossil Deer. Journ. Kilk. Arch. Soc., I., 164 — 166. 1850. Carpenter (G. H.) see 755. 120 Carte (Alexander). Description of the Fossil Bones discovered by Mr. Brenan at Shan don, near Dungarvan. Journ. P.D.S., II., 351 — 357. 1859 ; andiVa(. Hist. Review, VI., 501 — 507. 1859. 121 [Remarks on deer remains]. Journ. G.S.D., X. (1862-64), 166 (read 1863). 1864. [From Cos. Limerick and Dublin.] 122i On the Remains of the Reindeer which have been found fossil in Ireland. Journ. G.S.D., X. (1862-64), 103-107 (read 1863). 1864 ; and Dublin Q.J.S., IV., 103—107, plate 3. 1864. On the former Existence of the Polar Bear in Ireland, as is probably shown to he the fact by some Remains recently discovered at Lough Gur, County of Limerick. Journ. G.S.D., X. (1862-64), 114 — 119, plate 7. 1864. [For discussion see pp. 173—174] ; and Dublin Q.J.S., IV., 143-148. 1864. Notice of discovery of American Reindeer at Ashbourne, Co. Dublin. Journ , G.S.D., X. (1862-64), 71 (read 1862). 1864. 124 895-96.] 255 125 126 127 128 120 130 Carte (Alexander). On some indented Bones of the Cervus Megaceros, found near Lough Our, County of Limerick. Journ. R.G.S.I., I., 151-154, plate 7 I867* [Lor discussion see pp. 177—179] ; and a 308-312’ Plate 6. 1866. [Indentations produced by rubbing when in situ.] Charnock (R. S.). [Presented and described a greenstone celt from Toome, found with many implements and a canoe, 10—12 feet below bed of Lough -Neagh.] Froc. Soc. Ant. London for 1861-64, (2) ii., 119. Clarke (Dr. ). On certain Alterations of Level on the Sea Coast of part of the County WaJerford’ and the cause thereof. Brit. Assoc. Report for 1857, Sections, 65. 1858. [Raised beach up to 60 feet.] Close (Rev. Maxwell H.). Notes on the General Glaciation of the Rocks in the Neighbourhood of Oubhn. Journ. R.G.S.I., L, 3—13, plate 1 (read 1864). 1867. L, °r discussion seepp. 91—93] ; and Dublin Q.J.S., Y., 177—187, plate 5. 1865. [Important paper.] On the General Glaciation of Ireland. Journ. R.G.S.I., I., 207—242, plate 8 (read 1866). 1867. [For discussion see pp. 283 — 284], [Important paper.] 131 132 On the General Glaciation of Ireland [a letter]. Geol. Mag., IV., 234— 235, plate 1. 1867. [Explanation of map showing striae over all Ireland.] On some Corries and their Rock-basins in Kerry. Journ. R.G S II , 236—248, plate 22 (read 1869). 1871. The Elevated Shell-bearing Gravels near Dublin. Journ. R.G S I , tip 36 “40 (read 1873)- 1877 J and Geol Mag., (2) I., 193-197. 1874. [Descr. : lists of shells.] 133 The Physical Geology of the Neighbourhood of Dublin. Sci. Froc. R.D.S., n.s. I., 133 — 161. 1878 ; also Journ. R.G.S.I., V., 49 — 77 (read 1878). 1880; and Guide to the County of Dublin, 1878, pp. 19—47. [Descr. of glac. and post-glac. beds.] See Close (756), Cusack (152), Kinahan (760). 134 Cody (Patrick). [Note on discovery of skull of Megaceros 8 feet below peat in a stratum of cockle-shells at Toryhill, Co. Kilkenny.] Trans. KiVk. Arch Soc., I. Hi. (for 1851), 388. 1852, 135 Colby (Lt.-Col. Thomas). Ordnance Survey of the County of Londonderry. 4to. Dublin, 1835. [Section 1., sub-section 2, deals with “ detritus”.] 2 '6 [Appendix B.N.F.C., 136 Cole (Grenville Arthur James;. County Dublin, Past and Present. V., From Past to Present. I.N., I., 90—95. 1892. [General descr. of glac. geology.] 137 TExhib. Ailsa Craig rock, from Killiney and Greystones.] Dublin Micro. Club, in I.N., II., 172. 1893. 138 139 Glacial Drift of the Irish Channel. Nature, XLVII.,464. 1893. [Ailsa Craig rock at Killiney and Greenore.] Excursion to the Counties of Dublin and Wicklow. Proc. Geol. Assoc., XIII. (1893-94), 168—177. 1895. [Refs, to glac. geol.] 140 C[oleman] (J[ames]). Cork County and the Ice Age. Journ. Cork Hist. § Arch. Soc., I., 192. 1892. [Glaciation.] 141 - — Islands of Oyster Shells, [note]. Journ. fork Hist. § Arch. Soc., II., 59. 1893. [Kitchen-middens in Cork Harbour.] 142 Coleman (James). Additional Irish Caves. I.N., IV., 94. 1895. [In Cork and Kerry.] 143 Commissioners appointed to inquire into the nature and extent of the several Bogs in Ireland, and the practicability of draining and cultivating them : 1st, 2nd, 3rd, and 4th Reports. Folio. 1810-14. [Many maps and sections.] 144 Conwell (Eugene A.). On a Fossil Mussel-shell found in Drift in Ireland. Brit. Assoc. Report for 1869, Sections, 87. 1870. [A fresh shell from base of an esker near Trim.] Cooke (Theodore), see Brownrigg (107). 145 Cork Naturalists’ Tield Club. [Excursion to “The Ovens” cave.] I.N. , III., 241. 1894. 146 Cox (Robert). Megaceros Hibernicus [a letter]. Geol. Mag., VI., 523. 1869. [Skull and antlers from bog at Schiule, Co. Limerick.] 147 Croker (Thomas Crofton). Researches in the South of Ireland. 4to. London, 1824. [Caves at Cloyne : cave at Castlemartyr with skeleton covered with gold plates, pp. 251—253.] Cromwell (T. HE.), see 757. Crosskey (Henry William;, see Brady, &c. (104). 148 Cruise (Richard J.). Explanatory Memoir to accompany sheets 89 and 90 of the Maps of the Geological Survey of Ireland, illustrating parts of the counties of Longford, Westmeath, and Meath. 8vo. 1872. [Glac. & post- glac. 24 — 26.] 1895-96.] 257 149 150 151 Cruise (Richard j). Do' , Jj?- ' Cslieets 66 and 67 do. illustrating parts of the counties o± oligo, Leitrim, Roscommon, and Mayo. 8vo. 1878. TO lac & post-glac. 6 : caves 13 : sections 28— 32. J L Do. do. sheet 58 do. illustrating parts of the counties of Armagh, Fermanagh, and Monaghan. 8vo. 1886. 1 Glac & post-glac. 11.] L Do. do. sheet 46 Fermanagh, Monaghan, post-glac. 14—15,] do. do. 8vo. 1886. Armagh. Phys. geogr. 5—7 [Tyrone, : glac. & 152 153 154 155 156 See Hull (304, 305, 307, 309), Kinahan Leonard (470), Wilkinson (716, 717). (427, 429), Cusack (XVI. p.). A History 1110 County and City of Cork. 8vo. Dublin and Cork, “LVfc 419~ 453 : The Geology of Co. Cork, contributed by Rev. M. H. Close. [Glac. & post-glac. geology, caves, &c.] Cuvier (Baron Creorg'es). Sur ies Os Fossiles de Ruminans, trouves dans les Terrains meubles. Article 11., | 1 : De 1 elan fossile d’lrlande. Annales du Museum dEisioire Nuturelle XII., 340-357. 1808. Reprinted in Recherches sur les Ossemens fossiles de Quadruples . . ” IV., Art II., pt. i. 4to. Paris, 1812. Dawkins (W. Boyd). °n ‘^Distribution of the British Post-glacial Mammals. Q.J.O.S., XXV., 192-217. 1869. [Eef. to Irish records.] Cave Hunting. &c. 335.] 8 vo. London, 1874. [Short ref. to Shandon cave, Early Man in Britain. 8vo. London, 1880. [General ref.] 157 The British Pleistocene Mammalia. Part A: A Preliminary Treatise on the Relation of the Pleistocene Mammalia to those now living m Europe Palaontographical Soc., XXXII. 1878. [Brief ref. to Ireland.] L See Mams (7, 8). 158 Day (Robert). [Flint Implements from Toome, Co. Antrim.] Journ. Kilk. Arch Soc., Y. 226—228. 1865. 159 [Communication on presenting flint-flakes from near Belfast 1 PM . A.A.I., (3) I. (1868-69), 147—148. 1873. Journ. 258 [Appendix B.N.F.C., 160 Day (Robert). Supplemental Notes on some of the Antiquities discovered in Lough Gur. Journ. Cork Hist. # Arch. Soc ., (2) I., 303 — 305. 1895. [Ref. to animal remains.] 161 On some Prehistoric Remains from Lough Erne. Hist. Journ. Arch., n.s. I., 47 — 55. 1895. [Implements, canoes, &c.] See Adams (7). 162 Deneley (Thomas). [Extracts from his Journal.] Journ . Kilk. Arch. Soc., V. Hi., 441. 1866. [Irish elk finds. j 163 Denny (Henryu On the Claims of the Gigantic Irish Deer to be considered as contem- porary with Man. Troc. Geol. $ Polytechnic Soc. of IV. Riding of Yorks., III. (1845-59), 400—440 (read 1855). 1859. [Full paper.] 164 Observations on the Distribution of the extinct Bears of Britain, with especial reference to a supposed new Species of Fossil Bear from Ireland. Proc. Geol. Polytechnic Soc. of W. Riding of Yorks., IY. (1859-68), 338— 358, plate 10 (read 1864). 1869. [Brenan’s Shandon specimens ] 165 Dickie (George). [On “a recent deposit of wood, shells, &c.,” at Newcastle, Co. Down.] Read before B.N.H. & P.S., 24 Febr., 1858. [For contents see Praeger, 581, p. 240. At this time the Proceedings of this Society were issued at intervals in leaflet form, without consecu- tive paging, &c.] 166 Dickson (John Mitchell). Crannog-hunting in Co. Down. Hist. Journ. Arch., n.s. I., 290. 1895. [Localities.] 167 Dixon (Robert V.). On the Occurrence of an Ancient Paved Road, under deep bog, in the neighbourhood of Omagh, County of Tyrone [a letter]. Journ. G.S.D., IX., 343—344 (read 1861). 1862. 168 Donovan ( ). [Remarks on Kitchen- middens.] Journ. R.G.S.I. , I. (1864-67), 189 (read 1866). 1867. 169 Drummond (James !■.). On Fossil Infusoria found in the County Down, Ireland. Magatine of Nat. Hist., n.s. III., 353 — 355. 1839. [At Lough Island Reavy : descr. of deposit, &c.] 170 Dunne (Right Hon. Major-G-en. F. P,), [Letter on crannogs and implements in Lough Annagh, borders of King’s and Queen’s Cos.] Journ. H. $ A. A. I., (3) I. (1868-69), 154. 1873. 1895-96.] 259 171 Du BToyer (George Victor). Remarks on the Geological Sections exposed by the Cuttings of the Dublin and Drogheda Railway. Journ. G.S.D., III., 255—260. 1S47. [Remarks on glacial beds.] 172 On the Geology of the Lake District of Killarney. Journ. G.S.R., YII., 97 — 115 (read 1856). 1857. [Ref. to drift beds.] 173 Explanations to accompanying sheet 101 of the maps of the Geological Survey of Ireland, illustrating parts of the counties of Meath, Dublin, and Kildare. 8vo. 1860. [Form of ground 5 — 7 : glac. beds 24.] L 6 8 17£ Do. do. sheet 111 do. do., illustrating part of the counties of Dublin, Kildare, and Meath. 8vo. 1860. [Glac. geol. 23—24.] 175 Do. do. sheet 193 do. do., illustrating part of the Counties of Cork and Kerry. 8vo. 1861. [Glac. beds 18—20.] 176 Drift at Donald’s Hill, Ireland. Geologist for 1861, 116— 117. 1861. [Co. Derry : deers’ horns, &c., under drift on denuded surface of Chalk.] 177 On the Evidence of Glacial Action over the South of Ireland during the Drift Period ; and of a subsequent slight Elevation, followed by a depression of the Land, to its present Level. Geologist for 1862, 242—254, plates 13—14. 1862. 17S Explanation to accompany sheets 167, 168, 178, and 179 of the maps, and sheet 13 of the longitudinal sections of the Geological Survey of Ireland, illustrating parts of the counties of Waterford, Wexford, Kilkenny, and Tipperary. 8vo. 1865. [ Glac. and post- glac. 15—17, 80.] 179 On the Discovery of the Head and Antlers, with some of the Bones, of the Megaceros Hibernieus, near Kilsheer, County of Meath. Journ. R.G.S.I., I. (1863-66), 247—248 (read 1866). 1867. [Descr. & additional records of mammalian bones.] 180 On Worked Flints from Carrickfergus and Larne [abstract]. Q.J.G.S. , XXIV. , 495. 1868. [Found in gravel up to 20 feet, and subsoil clay up to 600 feet.] 181 On Flint Flakes from Carrickfergus and Larne (abridged). Q.J.G.S., XXV. , 48 — 50. 1869. [Distribution and mode of occurrence.] 182 [The Glacial period and its influence on the flora] [a letter]. 6th Ann. Report R.N.F.C. (for 1868-69), 31—33. 1869. 26o [Appendix B.N.F.C., 183 Du Woyer (George Victor). On the Flint flakes of Antrim and Down [a letter], Journ. R.G.S.I, II., 169— 171, plate 13. (Read 1869). 1871. [Distribution.] See Jukes (334 to 345, 351), O'Kelly (533). 184 Du Woyer (George Victor) and J. Beete Jukes. Explanations to accompany sheets 100 and 1 10 of the maps of the Geological Surrey of Ireland, illustrating parts of Westmeath, Meath, Kildare, and King’s Counties. 8vo. 1860. [Glac. & post-glac. 19 — 21] 185 Edgeworth (Richard Eovell). A further Account of Discoveries in the Turf Bogs of Ireland. Archceoloffia, VII., Ill — 112 (read 1 783). 1786. [Iron, wooden, and textile articles under 15 feet of hog near Mullingar.] 186 Egan (F. W.). Explanatory Memoir to accompany sheet 48 of the maps of the Geological Survey of Ireland, illustrating parts of the counties of Down and Armagh. 8vo. 1872. [Glac. & post-glac. 88 — 42. Deer remains.] 187 188 189 190 191 Do. do. sheet 47 do. do., including the country around Armagh. 8vo. 1873. [Form of ground 7 — 8 ; glac. and post- glac. 50 — 65 : Megaceros.'] Do. do. sheet 59 do. do., including the districts of N e wto wnhamilton, Keady, and Castleblayney. 8vo. 1877. [Phys. geogr. 7 — 9 ; glac. & post-glac. 24 — 25 ; striae 30 — 31.] Do. do. sheet 27 do. do., including . . . [parts of] Londonderry . . . Tyrone, and . . . Antrim. 8vo. 1881. [Phys. geogr. 7 — 9 ; glac. & post-glac. 35 — 40 ; striae 43—44.] Do. do. Antrim. sheet 19 do. do. 8vo. 1882. [Cos. Derry and Phys. geogr. 5 — 7 ; glac. and post-glac. 16 — 22.] Do. do. Antrim. sheet 13 do. do. 8vo. 1884. [Cos. Derry & Phys. geogr. 5—7 ; glac. and post-glac. 11 — 14.] See Hull (307), Kinahan (433), Nolan (538, 529), Symes (649), Traill (667), Wilkinson (718). 192 Egan (F. W.), J. R. Kilroe, and W. F. Mitchell. Explanatory Memoir to accompany sheet 24 of the maps of the Geological Survey of Ireland, comprising portions of the counties of Donegal and Tyrone. 8vo. 1888. [Phys. geogr. 7 — 12; glac. and post-glac. 38—45.] 193 Enniskillen (Earl of). [Remarks on crannogs.] Proc. R.I.A. , V. (1850-68), 214 — 216 (read 1851). 1853. 1895-96.] 2.6 I 194 195 196 197 193 199 200 201 202 203 - 204 - Evans (John). On some Discoveries of Stone Implements in Lough Neagh Ireland Tj XLI> 397“i08’ plate 18- 1867-68- “n Address, Sertion C. Brit Assoc. Report for 1878, 519-527 [Kef. to absence ©f palseolithic implements, &c.] 1879, See Adams (7, 8). F. (J.). Ancient Iron Fetters. TJlst. Journ. Arch., VI., 168 160 185« [Stone crannog submerged in Port Lough near Londonderry.] ' Pirth (Wiiuam a.) and William Swanston. t0 the.Piat0“ace°us Deposits at Lough Mourne and in 1887-8U8T f8rtS n- 113— 114, 1859; IY., 194, 1859. Bank fossils.] (3) II., [Turbot British Conchology. 5 vols., 8vo. London, 1862-69. [Turbot Bank glac. fossils, I., xciT-xcTiii. Vols. II.-V. contain numerous ie±s. to Irish fossils, chiefly from Stewart’s, Hyndman’s, & Grainger s papers. Supplement in Y. has many refs, to Walpole’s Killiney fossils & Bell’s Portrush fossils.] 319 Jennings (Francis). On some Geological Phenomena in the vicinity of Cork. Brit. Assoc. ment]f°r lg44. [Submerged peat, sea encroach- 320 Jukes (Joseph Beete). Annual Address [to Geol. Soc. Dublin], L uwnuj . O UUI H . O (read 1854). 1856. [Ref to glac. deposits.] J~ourn. G.S.D., YI., 61 10S 272 [Appendix B.N.F.C., 321 Jukes (Joseph Beete). Annual Address [to Geol. Soc. Dublin]. Journ. G.S.D. , VI., 252 — 283. (read 1855). 1856. [Review of papers read.] 322 [ ] Explanations to accompany sheets 147 and 167 of the Maps of the Geological Survey of Ireland, illustrating parts of the counties of Kilkenny, Carlow, and "Wexford. 8vo. 1861. [Glac. & post- glac. 56 — 59.] 323 Manual of Geology. 2nd ed. Edinburgh, 1862. [Irish glac. & post- glac. beds, 674 — 686; Irish Pleist. mammals 695 — 696.] 324 On the Mode of Formation of some of the liiver- valleys in the south of Ireland. Q.J.G.S., XVIII., 378—403, plate 20. 1862 ; and Journ. G.S.D., X. (1862-64), 72-73 (read 1862). 1864 [abstract]. [Refs, to glac. & post-glac. geology.] 325 ■ On certain Markings on the Bones of a Megaceros lately found in Ireland. Brit. Assoc. Report for 1863, Sections, 81. 1864. [Co. Longford.] 326 On some Indentations on Bones of a Cervus Megaceros found in June, 1863, underneath a bog near Legan, Co. Longford. Journ. G.S.D. , X. (1862-64), 127—137, plates 12—14 (read 1863). 1864. [For discussion see pp. 168 — 171] ; and Dublin Q.J.S., IV., 209 — 219, plates 11 — 14. 1864. 327 Explanation of sheets 187, 195, and 196 of the Maps, and part of sheet 5 of the sections, of the Geological Survey of Ireland, illustrating part of the County of Cork. 8vo. 1864. [Glac. 9, 68 — 60.] 328 Explanation to accompany sheet 192 and part of sheet 199 of the Maps of the Geological Survey of Ireland, illustrating parts of the counties of Cork and Kerry. 8vo. 1864. [Glac. 45 — 46.] 329 [Remarks on bears in Ireland.] Journ. G.S.D., X. (1862-64), 173, 1864. 330 [Remarks on striations at Ross Hill, Co. Galway.] Journ. R.G.S.I., I. (1864-67), 90 (made 1864). 1867. 331 [Remarks on indented bones of Megaceros. ] Journ. R.G.S.I., I. (1864-67), 177—178 (made 1865.) 1867. [From Legans, Co. Longford.] [Remarks on Kitchen- middens,] Journ. R.G.S.J., I. (1864-67), 188 — 189 (made 1866). 1867. 332 [S95-96.] 27 3 333 334 335 Jukes (Joseph Seete). 0n “^trf S* Ration in “ Mand. zZZltiont p. 1] (,'ead 1866)' 187L £S«al sss&sj ao9>’ <«•- [Jukes (Joseph Beete) and George Victor Bu Woyer], ,«i ®5,s?ni’!10ns to accompany Quarter Sheet 46 N.W. [sheet 6 ], °f the Maps of the Geological Survey of Ireland Svo 1858 [Tipperary, Kilkenny. Glac. and post-glac. 7-8, 24.] Explanations to accompany sheet 184 do. of the County of Kerry. 8vo. 1859 post-glac. 34—36.1 do., illustrating part [Glac. 17 — 18; glac. & do., illustrating parts of 1861. [Glac. 34—35.] 336 [ ] Do. do. sheets 185 and 186 do the Counties of Kerry and Cork. 8vo. 337 [ ] toe ^Counties ifublirf and Meath. sections 62 ; glac. & post-glac. 66 — 68.] ^ * ’ 338 [ -J toe county of ^ork.^ 29 ^ of D°' of Kerry, “l861. J/iheCotty [Gf c. & apart P engraved sectton, ‘sheet Na’lfi rffte^So^orf post-gla™' 48— 49f]‘he C°Untj °f Ken7' 8™' 1S68, [Glac- * lliiplanations to accompany sheets 121 and 130 of the maps of the Gcologieal Survey of Ireland, illustrating a portion of the counties gL“l7a“ blm- 8V0- 1869- [«1“- 11; glac. & post- [,WynnerePh V’ WOyer’ J' O'Kelly, and A. B. Data and Descriptions to accompany Quarter Sheet 35 N.E., [sheet rK^™h|“T 0flhn Geo!°gical sm'vey Of Ireland. 8vo. 1858. [Kildaie, King s and Queen’s cos. Glac. & post-glac. 17—18 1 339 340 341 342 343 274 [Appendix B.N.F.C., 3^'S: [Jukes (Joseph Beete), G. V, Du TJoyer, and A. B. Wynne.] Do. do. Quarter Sheet 45 S.W. [sheet 166], do. do. Svo. 1858. [Limerick, Cork, Tipperary. Glac. 23.] 345 [ ] _ , , Do do. Quarter Sheet 45 S.E. [sheet 166], do. do. 8vo. 1858. [Tipperary, Waterford. Cave 4 : glac. and post- glac. 22 — 23, 27.] 346 [Jukes (Joseph Beete) and Frederick J. Foot.] Explanations to accompany sheet 162 of the maps of the Geological Survey of Ireland, illustrating part of the County of Kerry. 8vo. 1859. [Glac. 16.] 3^7 [ ] Do do. sheets 150 and 151 do. do., illustrating part of the County of Kerry. Svo. 1859. [Glac. and post- glac. 16.] 348 [Jukes (Joseph Beete) and G. H. Kinahan.] do. sheet 128 (formerly quarter sheet 35 S.E.) Do. __ ^ ^ ^ 35 S.E.) do. do., illustrating parts of the County of Kildare and Queen s County. 8vo. 1859. [Glac. and post-glac. 13, 28—30.] 349 [ ] , . , Do. do. sheets 163, 174 and part of 175 do. do., illustrat- ing parts of the Counties of Limerick, Kerry, and Cork. 8vo 1861. [Glac. & post-glac. 31.] [ Do. do. sheets 200, 203, 204, and 205, and part of 199 do. do., illustrating part of the County of Cork. 8vo. 1861. [Glac., Chalk flints 17 ; glac. & post-glac. 19—20.] 351 [Jukes (Joseph Beete,) CL H. Kinahan, and G. V. Du Woyer.] Do. do. sheet 137 (formerly quarter sheet 40 N.E.) do. do. 8 vo. 1859. [Kilkenny, Carlow, Queen’s Co., Kildare Denudation 5-8 ; sections 25—48 ; glac. and post-glac. 49— 51.J 352, [Jukes (Joseph Beete), G. H. Kinahan, and J. O Kelly.] Do. do. sheets 197 and 198, and the south-east part of 191 do. do., illustrating part of the Counties of Cork and Kerry. 8 vo. 1860. [Glac. & post-glac. 28—29.] 353 [Jukes (Joseph Beete), G. H. Kinahan, and A. B. Wynne.] Do. do. sheet 144 do. do., illustrating parts of the Counties of Limerick, Tipperary, and Clare. 8vo. I860. [Uiae. & post-glac. 34—36 : Megaceros.] 354 [Jukes (Joseph Beete), and J. O’Kelly.] Do do. sheet 154 do. do., illustrating part of the Counties of Limerick and Tipperary. Svo. 1861. [Glac. post-glac. 27.] 355 [Jukes (Joseph Beete), and A. B. Do. do. sheet 164 do. Counties of Cork and Limerick. 20 — 21 : Megaceros.'] Wynne.] do., illustrating parts of the Svo. 1859. [Glac. & post-glac. 895-96.] 275 316 [Jukes (Joseph Beete), and A, S, Wynne.] D°’ d,°‘ s.keet 135 do. do., illustrating parts of the and of King’s and Queen’s Counties. 8vo. I860. [Glac. & post-glac. 80—32.] 357 [ ] D0‘ n' *• Shecet^18? and 189 do. do., illustrating parts of gkc°20— 1 21 ]f C°rk and Waterford- 8vo* 1861 • [Glac. & post- 358 [ ] D°' Of n Sh?tS l7n&Xld VJ d0- d0-’ illustrating parts of the Counties of Cork, Waterford, and a small portion of Tipperary. 8vo. 1861. [Glac. & post-glac. 28 — 29.] [Jukes (Joseph Beete), A. i. Wynne, and C3-. H. Einahan.] Do. do. sheets 182, 183, 190, and parts of 172 and 191 do. do., illustrating the part of the County of Kerry, containing the I romontory of Iveragh and Dunkerron. 8to. 1861 [Form of ground 5—8 ; glac. & post-glac. 31-34.] [Jukes (Joseph Beete), A. B. Wynne, and J. O’Kelly.] D°’ 133 — 165, map, &o. (read 1854). 1856. [Full descr., &c.] 366 Kendall (Percy r.). Glacial Geology, Old and New. Geol. May., (3) IX., 491—500 1892. [Ref. to Irish beds.] 367 On the Glacial Geology of the Isle of Man. Yn Hoar Manninaqh the Journal of the Isle of Man Natural History and Antiquarian Society, I 397-438, plate, maps. 1894. [Refs, to Ireland, pp. 12, 38, plate.] [Appendix B.N.F.C., 363 369 370 371 372 373 374 375 376 377 276 Kendall (Percy F.). Erratic Blocks of England, Wales, and Ireland. Twenty-third Report of the Committee [Advance copy] Brit. Assoc. Peport for 1895. [Report from B.N.F.C. on N. of Ireland erratics.] Kllroe (Tames R.). Explanatory Memoir to accompany sheet 55 of the Maps of the Geological Survey of Ireland, comprising parts of the counties of Sligo and Leitrim. 8vo. 1885. [Glac. & post-glac. 26 — 28.] Directions of the Ice Flow in the North of Ireland, as determined by the Observations of the Geological Survey. Q.J.G.S., XLIV., 827—833. 1888; and Sci. Proc. P.D.S., n.s. VI., 259—262 (read 1888). 1888-90. See Rgan (192), Hull (306, 307), Symes (650, 654), Wilkinson (718 to 721). Kinahan ^George Henry). Explanation to accompany sheet 124 and that part of sheet 125 that lies on the west of Lough Derg of the maps of the Geological Survey of Ireland, illustrating parts of the counties of Galway and Clare. 8vo. 1863. [Caves 7 ; glac. & post-glac., Megaceros , 47.] On Crannogs in Lough Rea. Proc. B.I.A., VIII. (1861-64), 412 — 427 (read 1863). 1864. [Co. Galway, descr. & finds.] On the Eskers of the Central Plain of Ireland. Journ. G.S.D., X., 109—112 (read 1863). 1864 ; and Dublin Q.J.S., IV., 109—112. 1864. [Classification : marine origin, &c.] [Irish Drifts — a letter.] Geol Mag ., II., 91 — 9S. 1865. [Classifica- tion.] On Pre-glacial (?) Drift in Oueen’ s couuty . Geol . Mag., II., 442—444. 1865. [“ Stratified drift” under “ boulder clay.”] Explanation to accompany sheets 115 and 116 of the maps, and sheets 17 and 18 of the sections of the Geological Survey of Ireland, illustrating a portion of the counties of Clare, Galway, and Tipperary. 8vo. 1865. [Caves, crannogs 7 — 9, 36 — 38 ; glac. & post-glac., marl shells, 13 — 15, 26 — 36; strise 27.] Primary and Secondary Strise [a letter.] Geol. Mag., II., 525. 1865. [Co. Galway.] Notes on some of the Drift of Ireland. Journ. E.G.S.I., I., 191 — 207 (read 1866). 1867 ; and Dublin Q.J.S., VI., 249— 265. 1865. [Full paper : classification of drift.] 378 i?95 379 380 381 382 383 384 335 386 - 387 - 388 - 389 - 390 - 391 - 392 - •96.} !// Kinahan (George Henry). Pr“C ** [a IettarJ On tie Formation of the “Bock-basin” of Lough Corrib, county re 7a7‘ 1 Gml' Mag'\ IIL> 489-«5, plates 18-19. 1866. L-ttei. to glac. & post-glac. geology.] Notes on the Crannogs of Ballin Lough. Proc. S.I.A., JX. (1864- 66), 172-176 (read 1864). 1866. [Co. Galway: descr. and finds.] Explanation to accompany sheet 105, with that portion of sheet 114 1 r Trtho °f Gal"’ay Bar. of *0 maps of the Geological 41-5j,°s“-560- 1869' [6k°- &BOS‘-«k0” "*Us, 00Xr“l!“oltofei8b79Re°eilt A“Um'akti0M' ** Notes on a Crannoge in Lough Naneevin. Proc. R.I.A., X. (1866- finds ] ’ ^ 1866)* 187°- CCo-Galway. Descr. and [Observations ^exploration of Crannogs.] Journ. R.H. $ JEolian Drift or Blowing Sand, Ireland. Geol. Mag.. VIII., 155—158 1«71. [Descr. and origin of sand deposits ] Middle Gravels (?), Ireland. Geol. Mag., IX., 265—268 1872 [Eskers, “ Middle ” gravels, Wexford gravels.] Supplementary Notes on some of the Drift of Ireland. Journ. P.G.S.I., III., 9—15 (read 1871). 1873. [General.] Glacialoid or Be-arranged Glacial Drift. Geol. Mag. , (2) I. , 1 1 1 — 1 1 7 169—174. 1874. [Post-glacial sea ; Esker sea.] ’ On the °ngm of the Lagoon called The Fleet, Dorsetshire. Geol. Mag., (2) I., 49—50. 1874. [Comparison with Irish lagoons.] 0n thaXs! D“° ^ Asar, Esker, or Kaims. Geol. Mag., (2) II., 86—87. 1875 [Characters ; marine origin.] 278 [Appendix B.N.F.C., 393 39ft 395 396 397 398 399 ftOO ftOl 402 403 40ft 405 Xinahan (George Henry). The erroneous Nomenclature of the Drift [a letter]. Geol Mag., (2) II., 328—331. 1875. [Ref. to Irish beds.] Boulder Clay in Ireland [a letter], Geol. Mag., (2) II., 568 — 569. 1875. [The Irish succession.] Valleys and their Relation to Fissures, Fractures, and Faults. 8vo. London, 1875. [Many refs, to glac. & post-glac. geology.] On a Prehistoric Road, Duncan’s Flow, Bally albanagh, Co. Antrim Journ. Anthrop. Imt.,V., 106-110. 1876. [Under 6 feet of hog.] Irish Tide Heights and Raised Beaches. Geol. Mag., (2) III., 78 — 82. 1876. [Table of tide heights ; heights of tides and of raised beaches.] An Outlier of Glaeialoid or Re-arranged Glacial Drift on Stratified Gravel (Esker Period), Mourne Demesne, Co. Down. Journ. R.G.S.I., IV., 122-123. 1877. Irish Drift. Subgroup— Meteoric Drift. Journ. R.G.S.I. , (2) IV., 115— 121 (read 1876). 1877. The Estuary of the River Slaney, Co. Wexford. Journ. R.G.S I., IV., 60—69 (read 1875). 1877. [Peat under deep mud.] The Drifting Power of Tidal Currents versus that of Wind waves. Proc. R.I.A., (2) II. (Science), 448 — 458. 1875—77. [Examples from Irish coasts.] Hummocky Moraine Drift. Nature, XV., 379. 1877. [Oughterard, Co. Galway.] On. the Chesil Beach, Dorsetshire, and Cahore Shingle Beach, County Wexford. Q.J.G.S. , XXXIII., 29—41, plate 2. 1877. Irish Drifts. Subgroups : Aqueous and Glacial Drifts. Journ. R.G.S.I., IV., 210—218 (read 1876). 1877. Manual of the Geology of Ireland. 8vo. London, 1878. [Section Hi., ch. XIV— XVII. deal with glac. & post-glac. geology.] Irish Drifts. Trans. Manchester Geol. Soc., XIV. (1876-78), 190 205 (read 1877). 1878. [Classification.] 406 i895-96-] 279 *407 Kinahan (George Henry). Irish Drifts. Land and Water , Jan. 19, 1878. 408 409 410 411 412 413 414 413 416 417 *418 419 Explanatory Memoir to accompany sheets 169, 170, 180, and 181 of the map of the Geological Survey of Ireland, in the County of Wexford. 8vo. 1879. [LagoonsS — 6; glac. &post-glac. 12—14, 28—51.] Sea-beaches, especially those of Wexford and Wicklow. Proc. P.I.A (2) II. {Science), 191— 208, plates 4— 7. 1879. [Formation and travel.] On the Arklow Beach and Fivers. Sci. Proc. P.D.S., n.s. II., 250— 258, plates 16 — 18. 1880. [Travelling of beaches.] [Remarks on Young’s paper on wrought timber found in boulder clay (749).] Journ. P.H. $ A.A.I., (4) V. in. (1881), 449— 450. 1882. [An effect of weathering.] Explanatory Memoir to accompany sheets 168 and 159 of the maps of the Geological Survey of Ireland, including the district around Enniscorthy, co. Wexford. 8vo. 1882. [Form of ground 7 8 • glac. & post-glac. 19— 37.] Notes on Cervus megaceros (Megaceros hibernicus). Trans. Edinb . Geol. Soc. IV. in. (for 1882-83), 343—345. 1883. [Distribution, &c.] Glacial Moraines on Mount Leinster, Counties Wexford and Carlow. Sci. Proc. B.D.S., n.s. III., 334—335, plates 27—29. 1882 ; and Journ. P.G.S.L, VI., 186—187, plates 4—6 (read 1882). 1886. Notes on the Classification of the Boulder Clays and their associated Gravels. Sci. Proc. R.D.S., n.s. IV., i., 207—210. 1885 ; and Journ , P.G.S.L, VI., 270—278 (read 1884). 1886. Deal Timber in the Lake Basins and Peat Bogs of North-east Donegal. Sci. Proc. B.P.S., n.s. V., 629—635. 1886-87. Gravel Terraces ; Valleys of the Mourne, Strule, and Foyle, Counties Tyrone and Donegal. Sci. Proc. B.P.S., n.s. V., 636—638. 1886-87. [Description.] [ ] [Nanahik, Pseudonym]. The Morrogh of Wicklow. Land and Water , XXIII., 45. 1887. [Formed by tides and winds.] Large Irish Boulders [a letter]. Geol. Mag., (3) V., 189. 1888. [Dimensions of large erratics.] 28o [Appendix B.N.F.C., 420 Kinahan (George Henry). Economic Geology of Ireland. [Being vol. VIII. of Journ. H.G.H.I.'] 8vo. Dublin, 1889. [Ref. to clays, &c.] 421 Kitchen Middens in co. Donegal. I.N. , III., 138. 1891. [General note.] 422 The Recent Irish Glaciers. /JV., III., 236 — 240. 1894, [Effects of heavy snow-drifts against crumbling cliffs.] 423 Kitchen Middens, co. Donegal. I.N., IV., 21. 1895. [Short note.] See Adams (9), Foot (206), Hull (307), Jukes (348 to 353, 359), Kinahan (760), Trench (668), Ussher (681, 681). 424 [Kinahan (George Henry) and J. Beete Jukes).] Explanations to accompany sheet 143 of the maps of the Geological Survey of Ireland, illustrating part of the Counties of Clare and Limerick. 8vo. 1860. [Glac. & post-glac., Megaceros , 8 — 9, 33-34.] 425 [Kinahan (George Henry), J. Beete Jukes, and F. J. Foot.] Do. do. sheet 15*2 do. do., illustrating part of the Counties of Kerry and Limerick. 8vo. 1860. [Glac. & post- glac. 26—27.] 426 [Kinahan (George Henry) and F. J. Foot.] Do. do. sheet 142 do. do., illustrating parts of the Counties of Clare, Kerry, and Limerick. 8vo. 1860. [Glac. & post-glac. 39—40.] 427 Kinahan (George Henry), H. Leonard and R. J. Cruise. Explanatory Memoir to accompany sheets 104 and 113 with the adjoining portions of sheets 103 and 122 (Kilkieran and Aran sheets) do. do., illustrating a portion of the County of Galway. 8vo. 1871. [Glac. & post-glac., sea-cliffs (Aran) 31 — 37 ; glac. & post-glac. (mainland), kitchen-middens 69—74 ; table of striae 75-85.] 428 Kinahan (George Henry), and Joseph Nolan. Explanation to accompany sheet 95 do. do. ... illustrating parts of the counties of Galway and Mayo. 8vo. 1870. [Lough Corrib islands 30—36 ; L. Mask islands 45 ; glac. & post- glac. 45— 52 : table of striae 53— 58. J 429 Kinahan (George Henry), J. Nolan, H. Leonard, and R. J. Cruise. Explanatory Memoir to accompany sheets 93 and 94, with the adjoining portion of sheets 83, 84, and 103 do. do., illustrating the geological structure of the district around Clifden, Connemara. 8vo. 1878. [Drift bar 13 ; denudation 44 — 47 ; glac. & post-glac. 143 — 144 ; table of striae 145 — 160.] 430 [Kinahan (George Henry,) J. O’Kelly, and J. Beete Jukes.] Explanation to accompany sheet 153 do. do., illustrating parts of the Counties of Limerick and Cork. 8vo. 1861. [Glac. & post-glac. 28.] 1895-96.] 28i 431 432 433 do. 1876. do. [Glac. Klnahan (George Henry) and R. c?. Symes swtta *ie?ha»oiSSraf® H.eaJJnafd. Symes’ s- B- Wilkinson, D°' ^StntS 73 and 74 1858‘ ^Naraes Kingr (Prof. William). Xing (Eight Bee. Dr. William,, archbishop of Dublin deposits.] (17U8-9), 69-64. 1710. __ [Post-glac. Knowles (William James). w"ii‘2i ‘ZiiTi. “mg';.;1 S"**’ A»™r o«am, Z&’Z.’Xsz, ia 435 436 437 438 439 440 441 282 [Appendix B.N.F.C., 442 Knowles (William James). On Prehistoric Remains at Portste wart. Proc. B.N.F.C., (2) I., 100 (for 1874-75). 1875. [Sand-hill finds.] 443 A Glimpse of Prehistoric Times in the North of Ireland. Brit. Assoc. Report for 187 4, Sections , 155—156. 1875. [Implements, bones.] 444 Additional Remarks on the Find of Prehistoric objects at Portstewart. Brit. Assoc. Report for 1876, Sections , 166. 1877 ; and Journ. Anthrop. Inst., VI., 485 — 487. 1877. [Implements, &c.] 445 Flint Implements and Associated remains found near Ballintoy, Co. Antrim. Journ. Anthrop. Inst., VII., 202 — 205. 1878. 446 Flint Factories at Poitstewart and elsewhere in the North of Ireland. Brit. Assoc. Report for 1878, 579—580. 1879. [Implements, hones, shells.] 447 Report of the Committee .... for the purpose of conducting Excavations at Portrush and elsewhere in the North of Ireland. Brit. Assoc. Report for 1879, 171—175. 1879. [Implements, animal remains.] 448 Portstewart and other Flint Factories in the North of Ireland. Journ. Anthrop. Inst., IX., 320 — 328. 1880. 449 Flint Implements from the Valley of the Bann. Brit. Assoc. Report for 1879, 389—390. 1879 ; and Journ. Anthrop. Inst., X., 150 — 153. 1881. [In marl under peat.] 450 Prehistoric Implements found in the Sandhills of Dundrum, Co. Down. Proc. R.I.A., (2) II. ( Polite lit. and Antiquities ), 103—113. 1881. 451 On Basalt apparently overlying Post-Glacial Beds, Co. Antrim. Brit. Assoc. Report for 1883, 497. 1884. [Short abstract.] 452 On the Antiquity of Man in Ireland. Brit. Assoc. Report for 1883, 562. 1884. [Pre-palseolithic implements in N. E. Ireland.] 453 Flint Implements from the Raised Beach at Larne and other parts of the North-east coast of Ireland. Proc. R.I.A. (2) II. ( Polite Lit. and Antiquities), 209—213, plates 14 — 15. 1884. [Pre- palseolithic.] 454 Flint Implements from the North-east of Ireland. Proc. R.I.A. , (2) II. ( Polite Lit. and Antiquities ), 436 — 444, plates 22—23. 1886. [From boulder clay, Co, Antrim, etc.] 895-96.] 455 456 457 458 459 460 461 462 463 - 464 - 465 - 466 -i 467 463 283 Knowles (William James). Whitepark Bay, Co. Antrim. Journ. R H & A A T u\ vtt __ (1885), 104 125, plate 9. 1887. [Ref. The Prehistoric Sites at Portstewart, County Londonderry. Journ. tSkf ’ ( ) L 221-287’ 4 P'atea’ 1887’ [Fun Tbe the°rNodrtf nfterfT ?e BaiSed Beach at elsewhere in 1886 87? 1887 (2) 639-fi« (*» Rep?.j“.??i?ilrei89. °\z North-east °f “• l'Flri cL?o?T 2* ‘ a® P^ehist“rirc .Remains from the Sandhills of the lZ °mfand-- Frr- £-Li-> 173-189, plates 10—13 [Descr., implements, bones.] _ -«25? plates 22-24. ts91. [Descr., ^men^boMS.1]’ 612 _IrishPisr ra- “*-«* On the Occurrence of Flint Flakes in the Ballyrudder Gravels. Proc. gmJt.f’ IIL’ 41°‘“414 (for 1891-92)- 1892. [In glacial Prehistoric Pottery from the Sandhills, and its Antiquity. Journ. X.S.A.I., (6) IT., 243-255. 1895. Kitchen Middens of Antrim. /.IV., IV., 80. 1895. [Bones of Great ^ Kit0hen Midden3 of Donegal. /.IV, IV., 80. 1895. [Short note.] Third Report on the Prehistoric Remains from the Sandhills of the [?nlLfre“'4W- ^ ^ ^ Xientaigne (John). [Remarks gg^g“t^Poraneity^of Megaceros and man.] Journ. G.S.D., Leonard (Hugh). **.V, 284 [Appendix B.N.F.C., 469 Leonard (Hugh). , Explanatory Memoir to accompany sheets 68 and 69 of the Maps of tne Geological Survey of Ireland, illustrating parts of the Counties of Cavan, Leitrim, and Roscommon. 8vo. 1878. [Roches mou- tonnees 11 ; glac. Sc post-glac. 21 22.] 311). 470 471 472 See Kinahan (427, 429,432) . Leonard (W. B.), see Hull (308, 310, Leonard (W. B.), and B. J. Cruise. Explanatory Memoir to accompany sheets 78, . <9, and 80 of the Maps of the Geological Survey of Ireland, including portion of the Counties of Roscommon, Leitrim, Longford, Cavan, and Meath. [Glac. & post-glac. 40.] Leslie (David). . _ . , „ , • y On Remains of Megaceros hibernicus in gypsum in Ireland. Geologist for 1864, 165-166, plate 11. [Co. Monaghan.] Lett (Rev. Henry -William). /n,TT Records of a Former Level of Lough Neagh. ProcB.N.F.C., (2) ., X17 ns (for 1881-82). 1883. [Submerged hog and forest, bordered by submerged cliff.] 473 474 47S 476 477 478 479 480 Ancient Canoe found near Loughbrickland, Co. Down. Arch., n.s. I., 153 — 154. 1895. Tilsit Journ. Lewis (Henry Carvill). . . T i -1 Papers and Notes on the Glacial Geology of Great Bntian and Ireland. 8vo. London and New York, 1894. [Ireland, pp. 83-166.] ^A Topographical Dictionary of Ireland. 2 vols., 4to. 1837. [Mega- ceros at Dromore, Co. Down, I., 578.] Lockwood (Frederick W.). 1882-83). 1884. [The Crannogs of Lough Mourne.] [Abstract.] Journ. R.H. § A. Ad., (4) YI. i. (1883), 177. 1884. removing shoals.] Luhbock (Sir John). Prehistoric Times .... 8vo. London, 5th edition. 1890. [General ref. to Ireland.] Luckombe (Philip)i see 761, 1895-96-] 285 481 Xiydekker (Richard). Catalogue of the Fossil Mammalia in the British Museum, in 5 parts. 8vo. London, 1885-87. [Contains Irish localities, as in II., 82 — 89, Gervus giganteus .] Catalogue of Fossil Mammals, Birds, Reptiles, and Amphibians in the Science and Art Museum [Dublin]. 8vo. Dublin, 1891. [Many Irish specimens, localities and references.] Zi[ynch] (J. p.). Lough Gur. Journ. Cork Hist, and Arch. Soc . (2) [., 241—258, 289 302. 1895. [Descr. and ref. to animal remains.] MacAdam (James). On the Cuttings of the Belfast and Ballymena Railway. Journ. G.S.D., IV., 36 41. 1848. [Refs, to Boulder clay and gravels ] Observations on the Neighbourhood of Belfast, with a Description of the Cuttings on the Belfast and Co. Down Railway. Journ. G.S.D., IV., 250 265, plate 1. 1850. [Chiefly glac. & post- glac.] Supplementary Observations on the neighbourhood of Belfast. Journ. G.S.D., IV., 265—268. 1850. [List of fossils of estuarine clays, chiefly by Grainger.] On the Fossiliferous Beds of the Counties of Antrim and Down. Brit Assoc. Report for 1852, Sections, 53 — 55. 1353. [Post-glacial beds.] L MacAlister (Alexander), see Plunkett (562). M‘Clay (James I.,). Some Notes on the Geology of Londonderry made during Holiday Rambles in that County. Proc. Vpool Geol. Soc., III. in (1876- 77), 236-241. 1877. [Ref. to glac. geology.] M‘BonaM (John), see Hist. &. Arch. Assoc, of Ireland (286). M‘Rvoy (D.). [Ancient road, human bones, and utensils found near Urlingford, Kilkenny.] Trans. Kilk. Arch. Soc., III. (1854.65), 131—132. 1856. M‘Henry (Alexander). Report on the Explorations at White Park Bay, Ballintoy. Proc. B.I.A., (2) II. {Polite Lit. and Antiquities ), 463—464. 1888. [Descr., implements, animal remains.] Crannog of Lough na Cranagh, Fair Head, Co. Antrim. Proc. R.I.A., (2) II. {Polite Lit. and Antiquities), (1879-SS), 462. 1888’ [Descr.] Sketch of the Geology of Co. Antrim. Proc. Geol. Assoc., XIV, i29— H7, plate 5, map. 1895. [Short descr. of glac. & post- glac. beds.] or 482 483 484 485 486 487 488 489 490 491 492 See Hull (307, 309), Symes (649, 651, 652, 655). [Appendix B.N.F.C., 2 86 493 M‘Henry (Alexander), and W. W. Watts. Guide to the Collections of Rocks and Fossils belonging to the Geologi- cal Survey of Ireland, arranged in Room III. E. of the Museum of Science and Art, Dublin. 8vo. Dublin. 1895. [General descr. of glac. & post-glac. beds, by provinces ; lists of fossils.] 494 M‘Intosh (!>.). On the precise Mode of Accumulation and Derivation of the Moel Tryfan Shelly Deposits, &c. Q.J. G.S., XXXVII., 351 — 369. 1881. [Ref. to Irish high-level beds.] 49 5 M‘Skimin (Samuel). History of Carrickfergus. 8vo. Belfast, 1811. [Submerged peat with calcified nuts, p. 110 (p. 225 of 2nd edition, 1823.).] 496 Mahony (James A.). On the Natural History of Donegal, with some account of its Archaeology. Proc. Nat. Hist. Soc. of Glasgow , III. (1875-78), 152 — 162 (read 1877). 1878. [Glac. & post-glac. beds.] 497 On the Shell Mounds of the North of Ireland. Proc. Nat. Hist. Soc. of Glasgow, V. (1880-83), 7—11 (read 1880). 1884.. [Shells, bones, pottery, sandhills of Donegal and Ballintoy.] 49S Mallet (Robert). [Annual] Address [to Geol. Soc. of Dublin.] Journ. G,S.D., III., 168 — 178. 1846. [Review of papers read.] 499 [Annual] Address [to Geol. Soc. of Dublin.] Journ. G.S.D., III., 215 — 235. 1847. [Review of papers read.] 500 On certain molecular changes occurring in the structure of recent shells. Journ. G.S.D., III., 301—302. 1848. [Sparry infil- tration, shore at Carrickfergus.] See also 763. 501 Mantell (Gideon Algernon). On the Remains of Man and Works of Art embedded in Rocks and Strata, as illustrative of the connection between Archaeology and Geology. Archeological Journal, VII., 327 — 346. 1850. [Con- temporaneity of Man and Megaceros.~\ 502 Medals of Creation. 2 vols., 8vo. London, [1853]. [Calcified nuts from submerged peat, Carrickfergus, I., 71.] 503 Maunsell (Archdeacon William Wray). [Letters to R.D.S. on presentation of Elk’s hones.] Proc. P.D.S. , LX., 169—170, 211—212, 1824; LXI., 93-97, 1825. [Localities, &c.] 504 Milligan (Seaton Forrest). Crannogs in County Cavan. Journ. R.H. A. A. I., (4) YII t. (1885), 148—152. 1887. See Belfast N.H, & F.S. (44), 1895-96-] 28; 505 Mitchell (W. F,)i Explanatory Memoir to accompany sheet 62 and the northern portion of sheet 73 of the Maps of the Geological Survey of Ireland. 8vo. 1879. [Mayo : glac. & post-glac. 19—21.] 506 Do. do. sheet 129 do. do., illustrating the district of Baltinglass and Dunlavin in the County of Wicklow. 8vo. 1884. [Glac. & post-glac. 24—27.] See Egan (192), Hull (306, 307)i 507 Molloy (Kyran), [Letter on a timber structure below 4 feet of bog.] Journ. R.E. § A. A. I., (4) I. i ., 279. 1870. [Clonmacnoise, King’ s Co.] SOS Molyneux (Thomas). A Discourse concerning the Large Horns frequently found under Ground in Ireland, Concluding from them that the Great American Deer call’d a Moose was formerly common in that Island .... Phil. Trans., XIX. (1695-97), 489 — 512, plate. 1098. [Reprinted m Boate, Molyneux, &c., “Nat. Hist, of Ireland” (100).] 509 Remarks upon the aforesaid Letter [see Wevile (533)] and Teeth Phil. Trans., XXIX. (1714-16), 370—384, plate. 1717. 510 A Journey to Kilkenny. From MS. notes of Thomas Molyneux. Edited by Rev. James Graves. Journ. Kilk. Arch. Soc., III., 1860-61), 296 — 303. 1861. [Descr. of Dunmore Cave.] See Boate (lOO). 511 Moore (Rev. Canon Courtenay). The Mitchelstown Caves. Journ. Cork Hist. & Arch. Soc., Ill 1—5 1894. [Descr., map.] 512 Moore (Joseph Scott). On the Discovery of a Stone Hatchet at Kilbride, County of Wicklow. Journ. R.G.S.I. , I., 250—252 (read 1866). 1867. [Under a large boulder.] L 513 On the Growth of Turf Bogs of fibrous character. Journ. R G S 1 II. (1867-70), 171—174. 1871. 51ft On the Discovery of a Cache at Ballinatona, near Blesington. Journ. R.G.S.I., II., 174—176 (read 1869). 1871. [Under 6 feet of bog.] 515 Moran (John). Mammoth’s Tooth recently found in the drift gravels at Larne Harbour Proc B.N.H. Sf P.S. for 1888-89. 35-37. 1889. [In raised beach. Descr. of beds.] 288 [Appendix B.N.F.C., 516 Morant (George). [On Crannogs in Ballyhoo Lake, near Carrickmacross, Co. Monaghan.] Joui'n. Kilk. Sf S.E. of Ireland Arch. Soc., YI. ' 1 867), 8 — 10. 1871. 517 [Ancient floor under bog near Carrickmacross, Co. Monaghan.] Journ. R.H. # A.A.I., (3) I. (1868-69), 269-270. 1873. 518 Moss (Richard J.). Report on the Exploration of Ballybetagh Bog. Proc. It.l.A. , (2) II* (Science), 547—552. 1875-77. [Descr., list of hones.] 519 Mudge (Capt. William). Description of an ancient Structure dug out of Drumkelin Bog, in the Parish of Inver, County of Donegal, in the year 1833. Archaz- ologia, XXVI., 361—367 (read 1833). 1836. [Wooden house under 16 feet of hog.] 520 Mulvany (William T.). Collection of antiquities presented to the Royal Irish Academy. Proc. R.l.A. , V. (1850-53), appendix V., 1853. [Some skulls, &c. in- cluded.] 521 Murray (William). On some timber found at a considerable depth below the surface in the Co. of Tyrone. Journ. G.S.D. , III., 75. 1844. [Measured section ; wood at 57 feet depth, in clays, &c.] TTanahik ( Pseudonym ) see Kinahan (418). 522 Revile (Francis). A Letter to the Right Reverend St. George, Lord Bishop of Clogher, o-iving an account of some large Teeth lately dugg up in the North of Ireland. . . . Phil. Trans., XXIX.' (1714-16), 367— 370. 1717. Reprinted in Boate, Molyneux, &c., “Nat. Hist, of Ireland” (100). [Elephant’s teeth at Maghery, borders of Cavan and Monaghan.] 123 Newman (Edward). Further Notes on the Bones of Extinct Deer found in Ireland. Zool., V., 1629-1633. 1847. [Editorial comments following letters by Owen (550) and Richardson (597, 598), on the Lough Gur find.] 524 Sfficliol (A.). [Letter describing Michelstown Cave.] Dublin Penny Journal, III., 202—203. Dec. 27, 1834. 525 KTolan (Josepli). Explanatory Memoir to accompany sheet 70 of the Maps of the Geological Survey of Ireland, including the country around Dundalk and Carrickmacross. 8vo. 1877. [Armagh, Monaghan, Louth. Caves 10 ; glac. & post-glac. 33 — 34 ] Do. do. sheet 34 do. do. 8vo. 1878. Phys. geogr. 7 — 9 ; glac. & post-glac. 21 — 23.] 526 [Tyrone. 1895-96.] 289 §27 528 §29 §30. §31 §32 §33 § 34 §33 §36 §37 §38 Nolan, (Joseph). ^°* n d°'. sheet 26 do. do., comprising portions of the Counties Tyrone and Londonderry. 8vo. 1884. P [Phys geogr 7— 9 ; glac. & post-glac. 21— 24.] L J 6 s See Hull (307, 309), Kinahan (428, 429, 432, 433). Nolan (Joseph) and p. w. Egan. I)o' m do’ ®keet 18 do. do. 8 VO. 1884. [Derry and J^rone- Ph^- geogr. 7—10 ; glac. & post-glac. 23-24.] 7 Do. do. sheet 12 and part of sheet 6 do. do including the country around Limavady. 8vo. 1885. [Phys. geo-? & — 9 ; glac. & post-glac. 24 — 29.] L ^ ° 0 * ©’Callaghan (C. Cr.). Hitherto unnoticed Orannogs in Lough Bridgid, Oo. Clare. Free and Papers S.8.A.I., (5) I. (1890-91), 487 1892. [Q’2£eISy (J.)]. Explanations to accompany sheet 127 ol the Maps of the Geological 8yo y!8°62 ref’ ‘““S a of the Queen’s County eyo. 1862. [Olac. & post-glac. 26—27.] J Do. do. sheet 117 and 118. do. do illustrati™ * portion of the Kings’s and Queen’s Counties, and the Countief of &4r 8to- l866- ***■ ***■#»■*- See *430)?°S’ a°9>’ ,Ukes <343> 3«2- 3*4, 360), SCinahan C°Woyler.l A- *• Wynne, and ©. v. Sc D°' Cnnnttof T'Slleet 165 C d°i do., illustrating part of the County of Tipperary. 8vo. 1860. [Glac. & post-glac. 21 22.1 ©’Siaverty (Bev. James). Relan«At’v!l2y2-12?toni85?d BmnZe m>t- Jmrn ■ Oldham (Thomas). On the more recent Geological Deposits of Ireland. Journ. G.S.D., shells]71’ 1844’ tGood generai descr. ; list of Howth glac. °“ “to gHciS.]5^ •*"-■***•. HI., 60-61. 1844. On the Occurrence of Marine Shells in the Gravels of Ireland Brit Amo- Xeportfor 1844, Sections, 67. 1846. [In many localities.] Some further remarks on the more recent Geological Deposits of Ireland. Journ. G.S.D. , III 130—139 ixak Ft • r shells from Dublin glac. beds, fe.] ^ [LlStS °f 290 [Appendix B.N.F.C., 539 540 541 542 543 544 545 546 547 548 549 550 551 Oldham (Thomas). On the supposed existence of Moraines in Glenmalur, Co. of Wicklow. Journ. G.S.D., III., 197—199. 1846. [Believes them to be tidal bars.] On a remarkable group of the remains of deer found near Kiltiernan. Journ. G.S.D., III., 252-253. 1847. [Many Megaceros skulls.] On the “drift” deposits of the County of Wicklow [abstract]. Journ. G.S.D. , III., 302—303. 1848. [General.] [Annual] Address [to Geol. Soc. Dublin.] Journ. G.S.D., III., 273 — 300. 1848. [Review of papers read.] On the Geology of Howtb [abstract]. Journ. G.S»D., IV., 154 156. 1849. [Ref. to glac. beds.] O’Reilly (J. P-). , Notes on Litbotbamnion met with in deep cuttings at the mouth of the river Liffey. Proc. R.I.A., (3) III., 223-224. 1893. [Section 24 ft. through post -glac. beds.] Ormstoy (M. H.). On a Polished and Striated Surface in the Limestone of Ross Hill, Co. Galway. Journ. R.G.S.I., I., 18 — 20 (read 1864). 1867. [Dor discussion see p. 90] ; and Dublin Q.J.S., V., 201 — 204. I860. Ouseley (Ralph). . An Account of the Moving of a Bog, and the Formation of a Lake, in the County of Galway. Trans. R.I.A., II., 3 — 5, plate 1. 1788. Owen (Richard). , Report on the British Fossil Mammalia, Part II., Ungulata. Brit. Assoc. Report for 1843, 208—241. 1844. [Ref. to Irish remains.] [ 1 , Description and illustrated catalogue of the Fossil organic remains of Mammalia and Aves contained in the Museum of the Royal College of Surgeons of England. 4to. 1845. [Irish localities, as at pp. 255—261, Megaceros Hibernicus.'] History of British Fossil Mammals and Birds. 8vo. London, 1846. [Irish refs.] [Letter on Lough Gur find.] Farmer's Gazette, V., 523. Dec., 1846, reprinted in Zool, , V., 1620-1622. 1847. See also Ball (38). P, The Cave 1832. of Dunmore. Dublin Penny Journal , I., no. 10. [General descr.] Sept. 1, S95-96.] 291 552 Palliser (C. W.). On a submarine bog recently discovered in Wexford Harbour [a letter! J°urn. G.S.D., IX., 344 (read 1861.) 1862. [14 feet of blue mud over 6 feet of peat, over 2 feet of mud, over marl : discussion.] §53 Parkinson (James). Organic Remains of a former World. 3 vole., 4to. London, 1804- 1811. [Irish Elk, HI., 313—318.] 554 Patrickson (Major S.). Description of a limestone District on the N.E. shore of Carlingford Lough, and of littoral Deposits of Shells and Limestone, &c. J°urn. G.S.D., I. (1833-38), 180-182. 1837. [Raised beach.] 555 Patterson (William Hugh). On a newly discovered Site for Worked Flints in the County of Down. Journ. R.S.A.I., (5) II., 154—155, plate. 1892. [Flakes, ox and and deer remains at Sydenham.] 556 Notice of a Pre-Historic Site at Ballykinler, Dundrum Bay, County of Down. Journ. R.S.A.I., (5) III., 80-81. 1893. [Flints, pottery, bones.] 557 Shell-mounds at Rosapenna, North Donegal. I.N., III., 49—51 plate 3. 1894 ; and Proc. B.N.H. § P.S.for 1893-94, 35. 1894. [Short abstract.] [Shells and bones.] See Belfast N.H. & P.S. (44). 558 Percy (Rev. Dr.), Bishop of Dromore. Extract of a letter from, to the Rev. Dr. Lort, on some large Fossil Horns. Archwologia, VII., 158 — 159. 1785. [Megaceros horns, size only.] 550 Petrie (George). Account of a human, body in a singular costume found in a high state of preservation in a bog on the lands of Gallagh, in the county of Galway. Dublin Phil. Journ. $ Scient. Review , I., 433—435. 1825. [Near bottom of bog 10 feet deep ; clad in skins.] 560 Phayer (J. R.). [Exhibited drawing of antler of Irish Elk found at Rathard, Tory Hill, Kilkenny.] Journ. Kilh. Arch. Soc., I., 33. 1849. 561 Pike (William). [Presented quern, &c. from crannog at Roughan Island near Dun- gannon.] Proc. R.I.A. , I., 457 (read 1840). 1841. 562 Plunkett (Thomas). On the Exploration of the Knockninny Cave. With an Account of the Animal Remains, by Rev. Prof. Haughton and Prof. Macalister. Proc. R.I.A. , (2) II. (Science), 455—483. 1876-77. [Descr. ; implements : bones.] 292 [Appendix B.N.F.C., 563 Plunkett (Thomas). A Detailed Account of the Exploration of Knockmore Caves in Fermanagh. Journ. R.G.S.I., IV., 131 — 140 (read 1876). 1877. [General account.] 564 On the Exploration of some Caves in the Limestone Hills of Fermanagh. Brit. Assoc. Report for 1877, Sections , 76. 1878. [Human and animal remains.] 565 Report of the Committee . . . appointed for the Purpose of exploring the Fermanagh Caves. Brit. Assoc. Report for 1878, 183 — 185. 1879. [General account of six caves.] 566 On an Ancient Settlement found about 21 feet beneath the surface of the peat in the Coal-bog near Boho, Co. Fermanagh. Brit. Assoc. Report for 1880, 623. 1880 ; and Proc. R.I.A. , (2) II. ( Polite Lit. $ Antiq.f 66—70, plate 2. 1880. [Crannog under peat and lacustrine marl.] 567 Porte (George). Remarks on the Recent Discovery of Remains of the Cervus Megaceros at Ballybetagh. Proc. R.I.A., (2) II. (Science), 738 — 741. 1875-77. [Age and condition of the bones.] 568 Porter (Rev. Thomas H.). On the Deposits of Gravel in the Neighbourhood of Dublin. Proc. R.I.A. , II., 37— 40. 1840-41. [Caused by a deluge.] 569 Portioek (General Joseph E.). On the Study of Geological Phenomena in Ireland. Journ. G.S.D., I., 1—15. 1833. [Post-glac. beds 14-15.] 570 On the Shelly Gravel underlying Dundalk. Journ. G.S.J). , I., 246 — 248 (read 1834). 1837. [Recent marine deposits.] 571 Address delivered at the 8th Annual Meeting of the Geol. Soc. Dublin. Journ. G.S.D., II., 1—34. 1839. [Review of papers read.] §72 Report on the Geology of the County of Londonderry . . . 8vo. Dublin, 1843. [Ch. I. Review of works of preceding writers. Ch. VI., Tertiary — calcareous clays (with list of fossils, Portrush raised beach, by J. Smith). Ch. IX. p. 473, mammalian remains. Ch. XIII., Detritus. Appendix : addendum to Ch. VI., with Bryce and Hyndman’ s paper and list of fossils, Belfast W ater- work boulder clay (111).] 573 [Annual] Address [to Geol. Soc., Dublin.] Journ. G.S.D. , IV., 167 — 244. 1850. [Review of papers read.] 574 Rudimentary Treatise on Geology. 2nd ed. 8vo. Dublin, 1862. [Lough Foyle raised beach 57 : Bumthollet river- terraces 59.] 895-96.] 293 §75 Portlock (General Joseph £.)• Notice of Scratches upon the Rocks of Bantry Bay, and of some intrusions of Igneous Rocks among the Schists, and consequent disturbance of the strata. Journ. G.S.P. , V. (1850-53) 111— 112 (read 1850). 1853. [Boulder clay and striated rocks!] §76 Praeger (Robert lloyd). On the Estuarine Clays at the new Alexandra Dock, Belfast. Proc B.N.F.C., (2) II., Appendix for 1886-87, 29—62 1887* [Glac. & post-glac. beds : list of fossils.] §77 Report of a Committee of Investigation on the Gravels and associated beds of the Curran at Larne, Co. Antrim. Proc. B.N.F.C. (2) 198—210, 2 plates (for 1889-90). 1890. [Descr. and lists of fossils.] §78 A Contribution to the Post-tertiary Fauna of Ulster. Proc. B N F C ^v^pII^tC218 Af°+ *889"99)’ 189°* [List of some estuarine clay shells, Derry, Antrim, and Down.j 579 On the Skull of an Irish Elk found at Belfast. Proc B N F r (9\ HL, 416-417 (for 1891-92). 1892. [In peat' below 30 fee of marine clay.] §80 [Exhibited bones of Irish Elk.] Proc. B.N.F.C (2) III 422—42*? at°BeRasV] ^ ' 1892’ ^ rom §ravel below peat beiow marine clay §81 582 Report on the Estuarine Clays of the North-east of Ireland. Proc. P.I.A., (3) II., 212—289. 1892. [Full descr. and lists of fossils, Londonderry to Dundalk.] §83 §84 §85 The Irish Post-glacial Estuarine Deposits. I.N., I., 138—141. 1892 [General descr.] Report of the sub -committee appointed to investigate the Gravels of Ballyrudder, County Antrim. Proc. B.N.F.C.. (2) III 518— 525 (for 1892-93). 1893. [Glac. gravels. Descr. and lists of fossils.] The Raised Beaches of Inishowen. [Descr. and lists of fossils.] I.N., IV., 278—285. 1895. The Mourne Mountains. Proc. Geol. Assoc., XIV., 148—152. 1895 [Ref. to glac & post-glac. beds.] See Belfast N,H, & P.S, (43), Sollas (626, 628, 629), 294 [Appendix B.N.F.C., 586 Reade (T. Mellard). Notes on the Scenery and Geology of Ireland. Proc. V pool. Geol. Soc ., IY. i. (1878-79), 64—89. 1879. [Irish coast, Down to Clare via Donegal.] 587 588 589 590 591 On a section of Boulder-clay and Gravels near Ballygalley Head, and an Inquiry as to the proper Classification of the lush Diilt. Q. J.G.S., XXXV., 679 — 681. 1879. [Descr.: fossils.] A Problem for Irish Geologists in post-glacial Geology. Journ. R. G.8.I. , V., 173 -176. 1880 ; and Sei. Proc R.B.S., n.s. 11., 255—258, plate 19. 1880. [Correlation of English and Irish beds.] On the Delations of the Glacial Deposits of the Clyde and Forth to those of the North-west of England and North of Iceland. Trans. Geol Soc. Glasgow, YI. «». (1878-9, ’79-80), 264-276 (read 1880). 1882. [Descr. of beds, Antrim, Mayo, &c.J Glacial Geology, Old and New. Geol. Mag., (3) IX., S10— 321. 1892. [Kefs, to Irish Beds.] The Dublin and Wicklow Shelly-drift. Proc. L’pool Geol. Soc., VII. «. (1893-94), 183-206. 1894. [Descr. and fossils, high and low level beds, Howth and Glenasmole to Bray. Many lllustr.] 592 Excursion to Belfast, Whitsuntide, 1893. VII. ii. (1893-94), 226—227. 1894. Down and Antrim.] Proc. IS pool Geol. Soc., [Glac. & post-glac. beds, 593 594 The High and Low-level Shelly Drifts around Dublin and Bray. I.N., III., 117—121, 150—153. 1894. [General descr.] beeves (Rev. William) [afterwards Bishop of Down and Connor and Dromore]. „ [Supplementary observations on Wilde’s paper on certain Crannog L Pfn Ulster (694).] Free. VII. (1857-61), 153-159 (read 1859). 1862. [Descr. of additional crannogs.] 595 596 597 An Account of the Crannoge of Inishrush and its a^cie1^t-^cup1a.go Proc. R.I.A., VII. (1857-61), 212-217 (read 1859). 1862. [Near Portglenone, Co. Derry.] Reid (Clement). The Origin of Megaceros- M arl. [Plants from marl, &c.] I.N., IV., 131—132. 1895. Richardson (H. D.>. The Extinct Gigantic Deer [a letter] . Farmer ’ s 1846. Keprinted in Zool., V., 1623-1628. find.] Gazette , V., 538 — 539. 1847. [Lough Gur IS95-96.] 295 598 599 600 601 602 603 604 605 606 607 60S 609 Richardson (H. D.). [Letter on Lough Gur find.] Zool ., V., 1628-1629. 1847. Facts concerning the Natural History, &c. of the Gigantic Irish Deer (GervusMegacerosHibernicus). 54pp. 8vo. Dublin, M'Glashan, 184 6. [Age, distribution, &c.] F urther^Particulars of the Giant Deer of Ireland. Zool., V., 1685-1686. Robertson (David) see Brady (104). Robertson (J. G.). Cave of Dunmore. [Read before the Kilkenny Lit. and Scient. Institution, 31 March, 1864.] Hat. Hist. Review I., 1G9 174 1854. [Descr.: animal remains.] On the Cave of Dunmore. [Read before the Kilkenny Lit. and ?8 Apri1’ 1854-1 Nat. Hlst- Review, I., 174 — 176. 18o4. [Further particulars.] Rowan (Eev. A. b.). Limestone Boulders of Corkaguiny, County of Kerry. Journ. G.S D V. (1850-53), 201—203 (read 1852). 1853. [Erratic blocks'.] Rudler (P. W.). J The Geology of Belfast. Academy, VI., 134-186. 1874 TRefto glac. geol.] ' L Ryland (Eev. E, R.) see 763. Savape (John) see (764). Seharff (Robert Francis). The 1oqq'GL??i-1ii;Britisl1 1Fa-,una 0 letterJ- Nat. Science, III., 400. 1893. [Irish mammals.] ’ 011 tr35(TTfin 47qthe/s1Sh and Fresh water Fauna. Proc. R.I.A., [6) HI., 479—485. 1894. [Geol. considerations.] Some Notes on the Irish Caves. I.N., IV., 57—59,. 1895 rRe- P™,ted felling a : Bulletin de la Societe de Speleo logic, I i ' 1895. List of caves.] y * Cave^at^BaUymote, Co. Sligo. I.H., IV., 94. 1895. [Short note. ^yVekk^l/?, 5SB)!um' “Ub,ini MdM- See ^non (26), Scott (Robert H.). Catalogue of the more remarkable instances of the finding of mam- DubHn UPS T Qrel?ndn [7In Keport of Co^> Geol. SoC P^b \o^32n?> Se?slon-] Jom. G.S.B., X. (1862-64), 143— 161. 1864. Reprinted under the title “Catalogue of the Mammalian fossils which have been hitherto discovered in Ireland/ m Lublin Q.J.S., V., 49-56. 1866; and under ^ a ^8mrat“ne]m GmL ^ VI1’ 413-^20' 1*-»- [Much 296 [Appendix B.N.F.C., 610 Scouler (John).| Remarks on the Natural History of the Fossil Elk. Journ. G.S.P., I., 197—210 (read 1836). 1837. 611 Notice of Animals which have disappeared from Ireland during the period of authentic History. Journ. G.S.D., I. (1833-38), 224 — 231 (read 1836). 18S8. 612 On certain elevated Hills of Gravel containing Marine Shells, in the Vicinity of Dublin. Journ. G.S.D., I. (1833-38), 266 — 276. 1838; reprinted in Proc. Geol. Soc. Lond ., II. (1836-37), 435 — 487. 1838. [Howth, Bray, Glenismaule ; lists of shells from two former.] 613 Anniversary Address [to Geol. Soc. Dublin]. Journ. G.S.l )., III. 10 — 22. 1844. [Review of Papers read.] 614 Sexagenarian (A) [ Pseudonym ]. Animal Remains— Gigantic Deer [a letter]. Farmer's Gazette , V., 566. Jan., 1847. [Dunshaughlin find.] 615 Seymour (Henry J.). [Exhibited Foraminifera from Portmarnock raised beach, Dublin Micro. Club, 28 March, 1895.] I.N., IV., 134. 1895. 616 Sigerson (George). Discovery of Fish -remains in the Alluvial Clay of the River Foyle, with Observations on the Existence and Disappearance of an Upper Lough Foyle, and on the former Insulation of Derry and of Inishowen. Proc. P.I.A. , (2) I. (Science), 212 — 224. 1872. [Probably Cod, in clay underlying peat.] 617 On Changes in the Physical Geography of Ireland. Proc. P.I.A. , (2) II. (Science), 6— 22. 1875-77. [Ancient records.] 61S Simpson (W. J.). On Worked Flints found on a Raised Beach at Portrush. Proc. P.I.A., (3) I., 76—77. 1888. 619 Smith (Charles). Ancient and Present State of the County and City of Waterford. 8vo. 1746. [Rib of Elephant dug up near Whitechurch, p. 81 (p. 58 of 1774 ed.) : see also Harkness (264).] 620 — - History of Cork. 2 vols., 8vo. Dublin, 1750. [Submerged peat at Youghal, &c. I., 109-112 (I., 74—76 of 1893-94 ed.)] 621 Smith (Bavid). Outlines of the Rocks of Antrim. 8vo. Belfast, 1868. [Gen. descr. and four sections at Belfast docks, 115 — 125.] 1895-96.] 297 €22 Smith (James). Researches in Newer Pliocene and Post-tertiary Geology. 8vo 1862 [Irish refs Elevated marine beds 1G ; Howth and Brav beds 18 • catalogue of glac. shells, Britain and Ireland, 46—56.] ‘ ’ See Portlock (572). Smith (Rev. w.). On Deposits of Diatomaceous Earth found on the shores of Lou ^oial (pw Sollas (William Johnston). _A M^Mke ^ ***» A CIi£Fs of KHiney Bay. J.IF , III 13 is _ 1894. [Detailed descr., with fossil lists by Prater.]’ ' ThS ^ deposits.] ; 895' general account of glac. Sollas (William Johnston) and R. sioyd Praeger. JNotes on Glacial Deposits in Ireland. I. The Brav River T v ttt 161 166, 194 198. 1894. [Descr. ohe»£ts 623 624 625 626 627 €23 629 1895. 630 Do* rn d°' t IL r fill-o’ -the- Grange. I.N., IV., 321— 39q [Descr.: lists of fossils.] ’ °"y- Stanley (P.) [? Thomas.] CB^52tu3ami0867a r£*'] Review’ Y > Proceed^, i0/ L66‘ A858- [Rogs and underlying beds.] y 631 Stanley (Thomas). On the Faults sometimes found in the Drift Gravel of Ireland TA letter.] Journ. G.S.D., IX., 6-7 (read I860). 1862; 632 Dublin QJ.S., I., 123—124. ’’l861. 633 [On Rough Armagh Crannog, King’s Co.— a letter.] A L‘ (3) I. (1868-69), 156—157. 1873. J Journ. B. § A. Staples (James H.). The fheirf'’ Sippnd’ .f'^ed Flkts t0 be found in the Gravel in 298 [Appendix B.N.F.C., 634 Stewart (Samuel Alexander). [Earth movements in Glacial period.] 6 th Ann. Report B.N.F.C. (for 1868-69), 33—35. 1869. [Reply to Du Noyer’s letter (182).] 635 The latest Fluctuations of the Sea-level on our own Coasts. 8th Ann. Report B.N.F.C. (for 1870-71), 55—57. 1871. [As shown hy submerged peat and estuarine clays.] A List of the Fossils of the Estuarine Clays of Down and Antrim. 8 th Ann. Report B.N.F.C. (for 1870-71), Appendix , 27—40. 1871. [From deposits of Belfast, Larne, and Strangford Loughs. Table of shells, glacial, est. clay, and present day.] Mollusca of the Boulder Clay of the North-east of Ireland. Proc B.N.F.C., (2) I., Appendix for 1879-80, 165—176. 1881. [Descr. and list of fossils, Down, Antrim, and Derry.] The Boulder Clay of the North-east of Ireland. Proc. B.N.F.C., (2) II., 51—62 (for 1881-82). 1882. [General.] 636 637 638 639 Stirrup (Mark). The Raised Beaches of County Antrim, their Molluscan Fauna, and flint Implements. Proc. Lit. and Phil. Soc. Ma)ichester, X\ 1. (for 1876-77), 51—56. 1877. [Descr.: lists of shells, &c.] 640 Stoney (George Johnstone). On the recent Formation of Gravel-beds resembling Middle Drift. Brit. Assoc. Report for 1870, Sections, 86 — 87. 1871. [Grey- stones, Co. Wicklow, caused hy denudation of surface of lower boulder clay.] 641 642 Swanston (William). On supposed fossiliferous Pliocene Clays overlying Basalt, _ near the Shore of Lough Neagh. Geol. Mag., (2) VI., 62 65. 1879 , and Proc. B.N.F.C., (2) I., 348—350 (for 1878-79). 1879. [Abstract.] [Are boulder clay with Mytilus.'] Mr. Howarth on Irish Glacial Drifts [a letter]. Geol. Mag., (2) X., 190—191. 1883. [Correction re Bovevagh, Co. Derry.] Report of the Committee appointed to investigate the Lame Gravels, and determine the Position in them of the Flint Flakes and Cores for which they are noted. Proc. B.N.F.C., (2) II., 519 630 (for 1886-87). 1887. [Raised beach overlying clays : detailed account.] 644 A Fossiliferous Ironstone Nodule. Proc. B.N.F.C., (2) III., 401— 402 (for 1891-92). 1892. [From boulder clay, Stoneyford, Co. Antrim.] See Firth (197). i895-96-] 299 645 646 647 64S Symes (Richard Glascott). Explanatory Memoir to accompany sheet 75 of the Maps of the StS?1 illustrating a portion of the county post-dac' if U . ? I [Form of «™und- wes, 7-9 ; glac. & post glac. 33— 34 , eskers, crannogs, deer remains.] do. 8vo. Do. do. sheets 41, 53, and 64 country around Ballina . glac. 22 — 26 ; table of striae.] Do* do- sheet 20 do. do. Fhys geogr. 6—6, glac. & post-glac. 19 — 2i • glaciation 22.] D°' iso?0' rnsieets, 31 (in part) and 32 139J [Donegal and Fermanagh chiefly, glac. & post-glac. 21_23 ; glaciation 25.’] do., including the 1879. [Glac.&post- 8vo. 1886. [Co. Antrim, list of raised beach fossils, do. do. 8 vo. Phys. geogr. 7—9 ; 649 650 653. 652 653 654 655 T. W. Egan, and Alexander See Xinahan (431, 432), (Richard Glascott), MvHenry. ’ Explanatory Memofr to accompany sheets 7 and 8 of the maps of the geological burvey of Ireland. 8vo. 1888. [Antrim and Derrv Glac. & post-glac. 38-39 ; sections 50-58.] L 5 ’ Symes (Richard Glascott), and James R. Xilroe. ° do d° dn 5r and t]ie south. western portion of sheet 42 Mp feTK “,r '[Si {yyt Symes (Richard Glascott) and Alexander ltt‘Henry. o. do. sheet 14 do do Rvn l cor* r r< a . • SymJ%B n«-10: glac- & yM'He “V °IaSOOtt ’' Willia» A. Traill, and Alexander D°' do d°' do *°’ 51- «2. and northern portion of 62 8vo mi’ ™ ludrng the country around Belmullft . , . . 19-231]81' ^May°' GlaC' & r,ost-Slac- list of glac. fossils Symes (Richard Glascott) and S. B. Wilkinson. °' p do* sheet 44 do. do., including portions of counties gl“g16^™i7a]d CaVan' 8T°- 1S86' [Glac- & P«t- STo°S ,RlohardtG^SrU’’,S- B‘ Wllkinson- a"d J.K. Kilroe. ’ sheet 65 do. do., including the country around rPWcCUriy’ ? th? counties of Sligo and Mayo. 8y05 1881 [Phys. geogr. 5-6 ; glac. & post-glac 16 — 17.7 ymes (Richard Glascott), S. B. Wilkinson, and A. M‘Henrv D°‘ in ldd* Iheet 63 and northern half of 74 do do ' ofta^ %\rfslorTANeWV°Vt -o' ’ County 15-17 ] ’ [PhyS’ ge0gr' 7~9 : SIac- * Post-glac. 300 [Appendix B.N.F.C., 656 Symonds (Eev. W. S.). _ , , 10-- Notes of a Geologist in Ireland during August and September 1857. Geologist for 1858, 292-296, 330-335, 377-385. |Bn«f refs, to glac. & post-glac. geology.] €57 Taylor (J. E.). _ , . . , „ . An Editor’s Holiday in the West of Ireland. Hardmehe s Science Gossip for 1878. 228-231. 1878. [Brief ref. to glaciation of Connemara.] Tennant (W.). On the traces of an Irish lake-dwelling found by Capt. L Estrange m the county of Cavan. Brit. Assoc. Report for 1866, Sections , <9. 1867. Thompson (Sydney Mary). A Plea for Irish Glaciology. I.N. , III., 30- €58 €59 -34. 1894. [General.] €60 €61 662 €63 Report of the Geological Committee [for 1893-94]. Proc. B.N.P.C., (2) IV., 114—127 (for 1893-94). 1894. [Glacial geology. Sections, erratics, lists of fossils.] Report of the Geological Committee [for 1894-95]. Proc. B.N.F.G., (2) IV., 229—235 (for 1894-95). 1895. [Erratics, &c ] Thompson (William). Report on the Fauna of Ireland; Div. Vertebrata. Brit. Assoc. Report for 1840, 353—409. 1841. [Refs, to extinct species.] [Exhibited horn of Cervus Alces , from bog in Tyrone.] Proc. Zool. Soc. London , V., 53 — 54. 1837. 664 „ The Natural History of Ireland. Vol. IV. 1856. [Extinct Mammals 33—36 ; a few post-glac. fossils also among Mollusca.] 665 Tighe (William). Statistical Observations relative to the County of Kilkenny, made m the Years 1800 and 1801. 8vo. Dublin, 1802. \Megaceros 88 — 89 ; Dunmore cave 107 — 109.] €66 Traill (William A.). On the Occurrence of Lower Boulder Clay or Till, with Shells, in the Counties of Down and Mayo, Ireland. Brit. Assoc. Report }or 1875, Sections , 83—84. 1876. [South of Mourne Mountains, and at Ballycastle in Mayo.] See Symes (652). 667 Traill (William A), and F. W. Egan. Explanatory Memoir to accompany sheets 49, 50, and part of 61 of the maps of the Geological Survey of Ireland, including the country around Downpatrick, &c., county of Down. 8vo. 1871. [Form of ground 8—14 ; glac. & post-glac., marl shells, Megaceros , 18 — 20, 59—61 ; strim 62—65 ; worked flints 67.] 895-96.] 30i 668 Trench (H. B.) and G, H. Xinahan. Notes on a Crannoge in Lough Nahinch. Proc. R.I.A., IX. (1864-66), 176 — 179 (read 1864). 1866. [Border of Tipperary and Queen’s Co. Descr. and finds.] 669 Trouton ( ) [Skull of Red Deer fished out of R. Boyne.] Proc. Publin Nat. Hist. Soc., 1. (1849-55), 70 (read 1855). 1860 ; and Nat. Hist. Review II., Proc., 36. 1855. 670 Ussher (Robert J.). On the Caves and Kitchen-midden at Carrigagower, Co. Cork. Geol. Mag., (2) VII., 512—514. 1880. [Bones, implements.] 671 Report on the Caves and Kitchen- middens near Cappagh, Co. Water- ford. Brit. Assoc. Report for 1881, 218—221. 1882. [Imple- ments ; animal remains.] 672 [The Submarine Crannog of Ardmore — a letter.] Journ, R.H. $• A.A.I., (4) V. i. (1879), 144-145. 1882. 673 [First] Report of the Committee appointed for the Purpose of carrying out Explorations in the Caves of Carboniferous Limestone in the South of Ireland. Brit. Assoc. Report for 1882, 240—241. 1883. [General.] 674 [Second] Report of the Committee appointed for the purpose of carrying out Explorations in Caves in the Carboniferous Limestone in the South of Ireland. Brit. Assoc. Report for 1883, 132 — 133. 1884. [Short narrative.] 675 A Description of objects found in the Kitchen-middens of Raths. Journ. R.H. § A.A.I., (4) VII. ii. (1886), 362—368, 3 plates. 1887. [Ref. to extinct mammals.] 676 Notes on the Irish Caves. I.N., IV., 92—94. 1895. CListof caves, &c.] 677 The Ardmore Crannog. Journ ., Waterford $• S.E. of Ireland Arch. Soc., I., 198 — 201, plate. 1895. [Crannog below sea-level.] See Adams (8,9). 678 Bssher (Robert T.) and A. leith Adams. On the Discovery of a Bone Cave near Cappagh, Co. Waterford. Brit. Assoc. Report for 1879, 338 — 339. 1879. [Implements and animal remains.] Notes on the Discovery in Ireland of a Bone Cave, containing Remains of the Irish Elk, apparently co-existent with Man. Set. Proc. R.D.S., n.s. II., 234—236. 1880; and Journ. R.G.S.I., V 170—172. 1880. 679 302 [Appendix B.N.F.C., 680 Ussher (Robert J.) A, Leith Adams, and G. H. Kinahan. Abstract of Report on the Exploration of Ballynamintra Cave, Cappagh, near Dungarvan. Proc. E.I.A. , (2) IT. ( Polite Lit. and Antiquities ), 78 — 78. 1881. [Descr. of deposits, bones imple- ments, &c.] 681 Ussher (Robert J.) and G. H. Kinahan. On a Submarine Crannog discovered by R. J. TJssher at Ardmore, Co. Waterford. Proc. R.I.A. , (2) II. ( Polite Lit. and Antiquities ), 61—65, plate 1. 1880. [In peat below raised beach. Bones and implements.] 682 Wakefield (Edward). Account of Ireland, Statistical and Political. 2 rols., 4to. London, 1812. [I., ch. iv., 92—112, bogs. Crannog near Roscrea, &c.] 683 Wakeman (G. W.). On the Remains of Animals, &c. at Dunshaughlin. Proc. Lublin Nat. Hist. Soc ., I. (1849-55), 69—70 (read 1865). 1860 ; and Nat. Hist. Review , II., Proc., 99 — 100. 1855. 684 [Presentation of two skulls of oxen, from bog at Dunshaughlin, Co. Meath.] Proc. Lublin Nat. Hist. Soc., I. (1849-55), 69 (read 1854). 1860 ; and Nat. Hist. Revieiv, II., 16. 1855. 685 Wakeman (W. P.). Remarks upon three hitherto unnoticed Crannogs in Drumgay Lake, near Enniskillen. Journ. R.H. £ A.A.I., I. i., 232—235. 1870. 686 Further Remarks upon the hitherto unnoticed Crannogs in Drumgay Lake, near Enniskillen. Journ. R.H. A.A.I. , (4) I. i., 305 — 314, plate. 1870. [Chiefly descr. of objects found.] 687 The Cave of Knockmore, near Derrygonelly, County of Fermanagh ; with remarks on the Character of the primitive scorings and early Christian symbols inscribed on its sides. Proc. R.I.A., X, (1866-70), 229—232 (read 1868). 1870. 688 On the inscribed Cavern of Lough Nacloyduff, Parish of Bohoe, County of Fermanagh. Proc. R.I.A., X., (1866-70), 327—329 (read 1868). 1870. [Cave.] 689 On the Cavern called “ Gillie’s Hole ” at Knockmore, Co. Fermanagh. Proc. R.I.A. , X. (1866-70), 395—397 (read 1869). 1870. [Brief descr. Inscribed stones.] 690 — Remarks on the Crannog at Bally doolough, County of Fermanagh. Journ. R.H. $ A.A.I., (4) I. ii., 360—371, plate. 1871. [Objects found chiefly.] 691 [On iron tools, &c. from Cornagall Crannog, Co. Cavan.] Journ. R.H. $ A.A.I., I. ii., 4C1— 466, plate. 1871. [Refs, to other crannogs.] IS95-96.] 3°3 692 Wakemaa (W. F.). The Crannogs in Lough Eyes, Co. Fermanagh. Journ. R.H. <$• A. A. I., I. ii., 563 — 564, 2 plates. 1871. [Descr.] 693 On certain recent Discoveries of ancient Crannog Structures, chiefly in the County Fermanagh. Journ . R.IJ. A. A. I., (4) V. ii. (1880), 324-339. 1882. [On the Crannog and Antiquities of Lisnacroghera, near Broughshane, Co. Antrim.] Journ. It.H. $ A.A.T., (4) VI. ii., 375— 4C6. 695 — The Crannogs of Drumdarragh, otherwise Trillick, and Lankill, Co. Fermanagh. Journ. R.E. A.A.I., (4) YII. ii. (1886), 372 — 389, 6 plates. 1887. 696 On the Crannog and Antiquities of Lisnacroghera, near Broughshane, Co. Antrim. Second Notice. Journ. R.E. # A. A. I., (4) IX. (1889), 96 — 106. 1890. Third Notice, Proc. $ Papers R. S.A.T., (5) I. (1890-91), 542 — 545, 3 plates. 1892. Fourth Notice, ibid, 673 — 675, 4 plates. 1892. [Chiefly descr. of objects found.] 697 — - Arehaeologia Hibernica. A handbook of Irish Antiquities, Pagan and Christian. 8vo. Dublin and London, 1891. [Causeways, crannogs, stone implements, &c.] 698 Walker (Adam). A Leter to Charles Morton, M.D., Sec. R.S., Containing an account of the Cavern of Dunmore Park, near Kilkenny, in Ireland. Rhil. Trans., LXIII. i., 16-19. 1773. 699 Waller (Edward). On the Discovery in Ireland of a new British Shell. Journ. R.D.S., I., 386—388. 1856. [ Columbella Holbollii, Turbot Bank, Co. Antrim.] 700 — On the Discovery in Ireland of New Shells. Journ. R.D.S., II., 29 — 34, plate 1. 1858. [Glac. fossils from Turbot Bank.] Warren (J. X..), see Hull (310, 311). Watts (W. W.), see M'Henry (493). 701 Wauchope (Admiral R.) Remarks on the Flint Implements found at Amiens and Abbeville, in connection with the Glacial Theory. 8vo. Penrith, lS6l! [Reviewed in Geologist , 1861, 272. Stone hatchet buried in Megaceros skull, Lough Gur. See also 684.] Stone Weapon in a Fossil Deer’s Skull. Geologist for 1861, 381—382. [At Lough Gur, and in Co. Carlow.] 702 304 [Appendix B.N.F.C,, 703 Weaver (Thomas). On the fossil elk of Ireland. Phil. Trans., CXV., 429 — 435. 1825 ; and Annals of Philosophy, n.s. IX., 463 — 465. 1825. [Dundrum, Co. Down. Marl shells, &c.] 70S: Welch (Robert J.). Kitchen Middens in Co. Donegal. I.N. , III., 243. 1894. [Short note.] 705 W[estropp] (T. J.). A “Find” in Coolasluasty Lough, Co. Clare. Journ. R.S.A.I., (5) V., 179. 1895. [Planks, skulls, &c.] 706 Westropp (W. K.). Sketch of the Physical Geology of North Clare. Journ. P.G.S. I. ,111., 75 — 79 (read 1872). 1874. [Ref. to glac. geology.] White (Rev. P.) see 765. 707 Wilde (William R.). On the animal remains and antiquities recently found at Dunshaughlin, in the County of Meath. Proc. R.I.A. , I., 420 — 426. 1840. [Heaps of hones in bog.] 708 Descriptive Catalogue of the Antiquities of Stone, Earthen, and Vegetable Materials in the Museum of the Royal Irish Academy. 8 vo. Dublin, 1857. 709 On the ancient and modern races of Oxen in Ireland. Proc. E.I.A. , VII. (1857-61), 64—75 (read 1858). 1862; and Nat. Hist. Review V., Proc., 276 — 287. 1858. 73.0 Upon the unmanufactured animal Remains belonging to the Academy. Proc. R.I.A., VII., 181—212 (read 1859). 1857-61 ; and Nat. Hist. Review VII., 41—72. 1860. [Catalogue, extinct and other animals.] 712. A Descriptive Catalogue of the Antiquities of Animal Materials and Bronze in the Museum of the Royal Irish Academy. 8vo. Dublin, 1861. 712 [On three Crannogs in Leitrim, Longford, and Antrim.] Proc. R.I.A., VII. (1857-61), 147—153 (read 1859). 1862. [At Lough Rinn, Castle Forbes, and Toome.] 713 A Descriptive Catalogue of the Antiquities of Gold in the Museum of the Royal Irish Academy. 8vo. Dublin, 1862. 714 [Remarks on indented bones of Megaceros.~\ Journ. G.S.D., X. (1862- 64), 169—170. 1864. Description of a Crannoge in the County of Cavan. Proc. R.I.A., VIII. (1861-64), 274-278 (read 1863). 1864; and Dublin Q.J.S., III., 279-284. 1863. 715 1895-96.] 305 716 717 713 719 720 Wilt?1655)! (SydnSy Bl)’ see Kigali (432, 433), Symes (653 Wilkinson (Sydney B.) and R. J. Cruise. Explanatory Memoir to accompany sheets 76 and 77 of the Maps of the Geological Survey of Ireland, including the country around ToSi rf. ' * , m the counties of Roscommon and Mayo. Svo. 1874. [Form of ground 5—7 ; glac. & post-glac. 21.] "Do‘ q d°*. , sll®.et 56 do. do., including the country around bwanlmbar, Florencecourt, and Dowra. 8vo. 1886. [Leitrim, Cavan, Fermanagh. Glac. & post-glac. 14— 15.] Wilkinson (Sydney B.), F W. Bg-an, and J. r. snroe. Do. do. sheet 25 do. do. 8vo. 1887. [Donegal and Tyrone. Phys. geogr. 5—7 ; glac. & post-glac. 17, 19, 21.] Wilkinson (Sydney B.) and J. R, SCilroe. 'Do* tit d0V sheet 57 do. do., including parts of Fermanagh, Monaghan, and Cavan. 8vo. 1881. [Glac. & post-glac. if— 16 ; stnse 18.] 0 Do. do. sheet 45 Enniskillen . . 721 do. do., including the country around 8vo. 1882. [Glac. & post-glac. 17—18.] 722 723 724 725 726 727 D n d 7. s*ieet3'> do. do., including the district around Umagh, Imtona, and Irvmestown. Svo. 1886. [Fermanagh, lyrone. Phys. geogr. 5-7 ; glac. & post.glac. 19—20.] Williams (William). On “ Cervus Megaceros .” Brit. Assoc. Report for 1878, 537 [Ballv- hetagh find : age of Megaceros. ] On an Attempt to elucidate the History of the Cervus Megaceros. commonly called the Irish Elk. Sci. Proc. R.D.S ns IT 105 111. 1880. [Age and cause of extinction.] * On the Occurrence of Megaceros Hibernicas , Owen, in the Ancient Lacustrine Deposits of Ireland, with Remarks on the Probable Age of these Reds. Geol. Mag., (2) VIII., 354—363. 1881 [Descr. of Ballybetagh ; age of Megaceros ; climate.] Williams (W. ^Eattieu). Notes on the Glaciation of Ireland and the Tradition of Lough Lurgan Brit. Assoc. Report for 1878, 528-529. 1879. [Geographical features caused by glaciation.] Windele (John). Historical and Descriptive Notices of the City of Cork and its vicinity ’ ' ; non8/!?* C°?’ 184°- [Refs, to caves, pp. 188 (Carriga- crump), 220 (Ovens).] v & On an Ancient Cemetery at Ballymacus, County of Cork ICilk. Arch. Soc., II. ii. (1853), 230—239. 1854. Castlemartyr cave and elk teeth.] Trans. [Ref. to 3°6 [Appendix B.N.F.C., 728 Wood (Searles V.), jun. Observations on the Sequence of the Glacial Beds. Geol. Mag., \ II., 17_22, Gl— 68. 1870. [Ref. to Wexford beds, pp. 17 — 18.] 729 Further Remarks on the Sequence of the Glacial Beds. Geol. Mag., VIII., 406— 412. 1871. [Ref. to Wexford beds.] 730 Wood-Martin (Lt.-Col. W. G.). The Lake -dwellings of Ireland . . . 8vo. Dublin and London, 1886. [Much information.] 731 Description of a Crannog Site in the County of Meath. Proc. R.I.A., (2) II. (. Polite Lit. $■ Antiquities) (1879-88), 480—484 (read 1866). 1888. 732 Pagan Ireland : an Archaeological Sketch. 8vo. Dublin, 1895. See also 766. 733 Wright (Edward Perceval). Notes of a visit to Mitchelstown Caves. Brit. Assoc. Report for 1857, Sections, 108—109. 1858. [Abstract]; and Nat. Hist. Review IV., 231— 241. 1857. [Present fauna.] 734 Wright (Joseph). Post- Tertiary Foraminifera of the North-east of Ireland. Proc. B.N. PC., (2) I., 428—429 (for 1879-80), 1881 [abstract]; and do. (2) I., Appendix for 1879-80, 149—163. 1881. [Of boulder clays, estuarine clays, and raised beaches.] 735 The Occurrence of Boulder Clay on Divis. Proc. B.N.F.C. , (2) IV. 215—216 (for 1894-95). 1895. [Marine clay at 1300—1400 feet, Co. Antrim.] 736 Wynne (Arthur B.). Explanations to accompany sheet 126 (and the portion of 125 lying to the east of the Shannon) of the Maps of the Geological Survey of Ireland, illustrating parts of Tipperary and the King’s and Queen’s Counties. 8vo. 1862. [Glac. & post-glac. 9, 13 — 14; detailed descr. 14 — 36.] 737 Irish Drift Fossils. Geologist for 1862, 428—429. [ Mytilus in gravel- pit south of Sligo.] 738 — On the Geology of part of Sligo. Brit. Assoc. Report for 1862, Sections, 96—97. 1863. [Abstract]; also Journ. G.S.D., X., 31—41 (read 1863). 1864; and Dublin Q.J.S., III., 171—179. 1863. [Ref. to shelly drift and mammalian remains.] 739 On Denudation with Reference to the Configuration of the Ground. Geol. Mag., IV., 3—11, plates 1—2. 1867. [Ref. to submerged peat, Youghal Bay.] 1895-96.] 30-7 740 Wynne (Arthur s>). On Disturbance of the Level of the Land near Youghal, on the South Coast of Ireland. Q.J.G.S., XXIV., 4-8. 1868. [Glac. & post-glac. beds ; shells.] 741 On the Disturbance of the Level of the Land near Youghal. [A letter.] Geol Mag., V., 484 — 485. 1868. [Answer to criticisms by Greenwood.] 742 Explanatory Memoir to accompany sheets 42 and 43 of the Maps of the Geological Survey of Ireland, comprising portions of the Counties of Sligo and Leitrim. 8vo. 1885. [Glac. & post. -glac, 27 — 28 ; caves 28 ; strise 30.] 743 Note on Submerged Peat Mosses and Trees in certain Lakes in Connaught. Sci. Froc. R.F.S., n.s. V., 499—503. 1886-87; and Journ. R.G.S.I. , VII., 186—190. 1887= See Jukes (343 to 345, 355 to 360), Xinahan (434), O’Xelly (533). 744 Wynne (Very Rev. G. R.), Traces of Ancient Dwellings in the Sandhills of West Kerry. [Note.] Journ. R.S.A.I. , (5) III., 78—80. 1893. [Bones, &c.] Young (Arthur), see 767. 745 Young (Robert). On the Eskers of the Central Plain of Ireland. Brit. Assoc, Report for 1852, Sections, 63 — 64. 1853. [Submergence theory.] 746 The recent Elevation of the Land in the Vicinity of Belfast. [Abstract.] 4 th Ann. Report B.N.F.C. (for 1866-67), 20—22. 1867. [General descr.] 747 The Boulder Clay of the Belfast District. [Abstract.] 8th Ann. Report B.N.F.C. (for 1870 — 71), 32 — 35. 1871. [General.] 743 — Some Remarks on the recent Changes of coast Level at Ballyholme Bay, Co. Down. Froc. B.N.H. $ F.S. for 1871-72, 89—40. 1873. [Boulder clay, peat, raised beach.] 743 [Wrought logs in boulder-clay near Belfast.] Journ. R.H. & A. A. I. , (4) V. it. (1880), 307—308. 1882. 750 — - Some Notes on the Upper Boulder Clay near Belfast. [Abstract 1 Froc. B.N.H. F.S. for 1889 90, 57. 1890. Notes on the Geology of the Excavations for the Main Drainage Works [Belfast]. [Abstract.] Froc. B.N.H. $ F.S. for 1890-91, 89. 1892. 751 308 [Appendix B.N.F.C,, 752 Young (Robert Magill). Brief Antiquarian Notes at Bushfoot and Ballymagarry [Co. Antrim]. Proc. B.N.H. % P.S. for 1892-93, 37—34. 1894. [Ref. to Bushfoot sandhill finds.] 753 On a Recent Find of Irish Elk Bones, &c., in Belfast. Proc. B.N.H. # P.S. for 1893-94, 76—78. 1894; and I.N., III., 81— 82. 1894. [In cuttings in Belfast streets.] See Belfast N.H. & P.S. (44). ADDENDA. 754 [Campbell (Thomas).] A Philosophical Survey of the South of Ireland, in a series of Letters to John Watkinson, M.D. 8vo. Dublin, 1778. [Dunmore cave, p. 106.] 755 Carpenter (George Herbert). Animals found in the Mitchelstown Cave. I.N., III., 25 — 35, plate 1. 1896; reprinted (in part) in Spelling a : Bulletin de la Societe de Speleologie, I. i. Paris, 1895. [Present fauna.] 756 Close (Rev. Maxwell H.). On the Geology of the Neighbourhood of Dublin as affecting its Sanitary Conditions. [Read Oct. 3rd, 1884, at Congress of the Sanitary Institute of Great Britain, held at Dublin. 8 pp. Authors’s copy, headed “Excerptfrom vol.YI. of the Transactions ” &c.] [Descr. of beds underlying the city.] 757 [Cromwell (Thomas Kitson).] Excursions through Ireland. 3 vols. 12mo., no date. [1818.] [Dun- more cave, II., p. 58.] 753 Foot (Frederick J.). Natural History Notes on the Mammalia of the West coast of Clare. Proc. Dublin Nat. Hist. Soc ., III. (1859-62), 104 — 106. 1863. [Caves.] 750 Hardman (Edward T.). The Limestone Caves of Sligo. [Appendix A. (pp. 375—378) of Wood-Martin’s “ History of Sligo,” I. 8vo. Dublin, 1882. [Localities.] 760 Rinahan (George Henry) and M, H. Close. The Glaciation of Iar-Connaught and its neighbourhood. 8vo. Dublin, 1872. [Important paper.] 761 [Luckombe (Philip).] A Tour through Ireland, wherein the present state of that Kingdom is considered .... 12mo. Dublin, 1780. [Caves. Cork and Kerry, pp. 130— 131, 134, 190, 282.] &S95-96*] 3°9 762 763 764 765 766 Mallet (Robert). On some Stalagmites from the Care of Dunmore, County of Kilkenny. Journ. G.S.D., III. in., 262 — 263. 1846. [Short abstract.] Ryland (Rev. R. H.). The History, Topography, and Antiquities of the County and City of Waterford. 8vo. London, 1 824. [Refs, to caves.] Savage (John). Picturesque Ireland .... 4to. New York, no date. [Bursting of a bog at Dunmore, North Galway, p. 264.] White (Rev. P.). History of Clare .... 8vo. Dublin, 1893. TCave at Kil- tannon, p. 2.] Wood-Martin (Lt.-Col. W. G.)> History of Sligo, County and Town. [Vol. III]. 1688 to present time. 8vo. Dublin, 1892. [Ch. XXI Y., Geology, &c.; boulder clay, bogs, raised beaches, crannogs, caves.] See Hardman (759). 767 Young (Arthur). A Tour in Ireland .... made in the Years 1776, 1777, and 1778 and . . . 1779. 4to. London, 1780. TMitchelstown cave, 380 — 381 (I., 464 — 465 of Hutton’s ed., 1892).] 3io [Appendix B.N.F.C.j INDEX. Note. — It must be understood that the following indexes, being compiled from the titles of the papers, and from the brief indication of their contents appended, are not exhaustive. They are intended as a rough guide to the papers, &c., dealing with any particular group of beds, or with any particular district. By consulting the papers indicated under any group, and also the papers indicated in the “general” list at the head of the section (A or B), a tolerably complete list will be obtained of papers dealing with the group in question ; but for a complete list of references the Bibliography itself must be looked through. SECTION A.— GEOLOGICAL INDEX. Group 1 — General. (Papers referring to various formations.) 3 4 5 27 3* 33 34 39 45 85 90 9* i33 i35 136 148 149 150 I51 152 178 184 186 187 188 189 190 191 192 200 201 202 205 206 207 208 209 217 240 *44 *57 *59 260 270 283 284 288 *95 *97 300 3CI 3°4 3°5 306 307 308 3°9 310 311 322 323 3*4 333 334 335 337 340 241 34* *43 345 347 348 349 35° 35* 35* 353 354 355 356 357 358 359 360 361 369 371 376 380 382 395 405 408 412 420 4*4 425 426 427 428 429 431 43* 433 434 439 469 470 485 486 49* 493 496 5°5 506 5^5 526 5*7 528 5*9 53i 53* 533 535 57* 585 586 592 609 645 646 647 648 649 650 651 652 653 654 655 656 657 716 717 718 719 720 721 736 742 Group 2 — Pliocene. (Chiefly W exford gravels.) 87 88 89 90 93 *54 *57 258 263 316 387 641 728 7 29 Group 3- -Glaciation, Strips. 10 35 58 63 68 74 82 1 18 128 129 130 *3* i39 140 177 188 189 203 228 *39 *59 281 289 294 *97 301 3°7 3°9 31© 33° 37° 376 377 382 427 428 429 431 43* 433 436 469 474 536 545 575 624 646 647 648 651 653 657 659 660 667 719 7*5 742 760 I S 94- 95-] 31 1 Group 4 — Glacial Deposits, Erratics. i r 13 47 48 5i 56 57 62 65 66 67 69 72 73 76 77 78 81 84 87 88 89 97 108 1 10 1 1 1 *32 137 138 x39 171 172 173 i74 i75 176 2I3 214 222 224 242 243 246 250 253 254 ^55 258 272 290 291 293 302 314 320 327 328 336 338 339 344 345 35° 365 366 368 373 374 375 378 387 388 389 392 393 394 398 399 402 404 406 407 4H 4i5 419 435 437 441 462 474 484 488 494 537 538 539 54i 542 568 575 583 587 589 590 59i 593 603 604 612 620 622 625 626 627 628 629 631 637 638 641 642 644 659 660 661 666 706 728 729 735 73/ 738 74° 745 747 748 75° 757 760 766 Group i 5— Post-glacial in General, V 389 399 440 487 544 569 57° 576 588 621 635 734 75i 756 766 Group 6— -Submerged Peat, Bogs, Marl. 16 21 23 25 36 37 40 42 5° 59 67 H3 165 169 i*S 197 205 207 21 1 218 245 286 3°8 3i9 364 376 382 400 416 483 495 502 5i3 5H 518 5*9 521 546 552 559 566 579 596 620 623 630 682 724 739 74° 743 748 764 Group 7— •Post- ■glacial Clays. 64 220 221 400 55i 576 577 578 581 582 616 636 643 Group 8 — Kaised Beaches. 29 5° 52 58 64 7i 75 83 9i 165 180 221 222 237 252 273 292 295 3°4 3i5 397 453 457 515 554 574 6 77 584 615 618 639 643 732 748 Group 9 '—Caves and Cave-Deposits. 2 7 8 9 12 15 19 20 28 55 79 IOI 102 *°3 i°5 106 107 109 120 142 H5 H7 149 152 I55 198 *99 202 231 256 267 296 37i 376 438 510 51 1 524 525 55i 562 563 564 565 601 602 607 608 645 665 670 671 673 674 676 678 679 680 687 688 689 726 727 732 733 742 754 755 756 757 758 759 76 1 762 763 765 766 767 312 [Appendix B.N.'F.d., Group 150 — Vertebrate Fossils. 2 3 4 5 6 9 18 21 23 24 25 26 3i 36 37 38 39 40 4i 56 60 94 98 99 100 IOI 102 103 106 109 1 17 H9 120 121 122 123 124 I25 i34 146 153 i54 *56 157 l6o 162 163 164 176 179 186 187 198 202 206 2I5 216 219 222 223 226 235 248 256 262 264 266 267 268 269 276 277 278 279 280 285 286 287 300 301 308 323 325 326 329 33i 353 355 364 37i 4i3 424 434 467 47i 475 481 482 483 489 501 5°3 508 509 5i5 518 520 522 523 540 547 548 549 55° 553 558 559 560 562 564 567 576 579 580 596 597 598 599 600 601 602 605 608 609 610 61 1 614 616 619 645 662 663 664 665 667 669 678 679 680 683 684 701 702 703 705 709 710 714 722 723 724 727 738 753 Group 11- -Invertebrate Fossils. 31 33 47 85 86 87 88 89 90 91 92 93 104 1 10 1 1 1 132 144 169 197 205 207 210 220 221 222 243 252 260 263 295 297 3°4 308 312 3*3 3H 316 3i7 318 365 367 376 382 437 486 487 493 500 535 537 538 572 576 577 578 583 SH 59i 612 615 622 623 626 628 629 636 637 639 641 642 643 647 652 660 664 666 699 700 734 735 737 738 Group 12 — Prehistoric Settlements. (Crannogs, kitchen-middens, sandhill sites, &c., and associated remains.) 1 -17 22 30 63 95 ”5 1 16 141 166 167 168 170 i93 196 225 230 234 261 265 271 274 275 282 332 363 372 376 379 381 384 385 396 421 423 427 442 444 446 447 448 450 455 456 459 460 464 465 466 468 476 477 478 489 490 491 497 5°4- 5°7 5i4 516 Sl7 5J9 53° 555 556 557 566 594 595 632 645 658 668 6 JQ 671 672 675 6 77 681 682 685 686 690 691 692 693 694 695 697 698 704 705 707 712 715 730 73 1 732 744 749 752 766 Group 13 — Prehistoric Implements, , Utensils, &c. 29 42 46 48 49 52 53 54 58 59 61 64 65 80 96 1 12 “3 114 126 156 158 159 161 180 181 183 185 194 1 95 212 227 229 23r 232 233 235 236 237 238 273 441 443 445 449 452 453 454 457 458 461 462 463 473 479 489 512 534 561 562 618 633 639 643 667 678 679 680 698 701 702 708 71 1 7i3 732 1895-96.] .313 Group 14— Denudation, Deposition, Formation of Sea -beaches and Lagoons. 14 205 319 351 383 39o 391 397 398 401 4o3 408 409 410 411 4*7 4l8 422 427 429 574 640 739 Group 15— Elevation, Subsidence, Submergence. 70 127 177 247 303 416 472 546 606 617 634 635 672 677 681 740 741 743 746 748 Group 16— Climate of Past Epochs. 182 210 213 605 SECTION B— GEOGRAPHICAL INDEX. 1 — General or Indefinite. (Papers dealing with many localities, or with general considerations.) 3 4 5 6 10 11 18 22 26 27 34 36 37 39 4i 85 88 90 92 94 95 99 100 108 1 *4 1 16 118 119 122 129 140 *43 *53 *54 1 56 *57 162 163 164 168 1 77 182 *93 1 95 210 2*3 214 217 218 222 223 227 230 231 232 238 240 241 242 244 246 249 250 2 53 255 264 266 268 269 281 283 284 285 287 288 290 291 292 293 294 296 297 303 318 320 321 323 324 329 332 333 361 362 364 366 367 368 37° 373 374 378 383 385 386 387 388 389 39° 391 392 393 394 395 397 399 401 404 405 406 407 409 4*3 4*5 419 420 422 439 443 446 447 448 452 453 454 457 458 459 460 461 463 466 467 472 474 479 480 481 482 493 494 498 499 5°* 5°3 508 5*3 520 523 534 535 537 538 542 547 548 549 553 558 569 57* 573 574 581 582 586 587 588 589 59° 594 596 599 600 605 606 607 609 610 611 613 617 622 625 634 635 638 656 659 660 661 662 664 673 674 675 676 682 693 697 708 709 710 711 713 7*4 723 724 725 73 0 732 739 743 745 3^4 2— Co. Antrim. [Appendix B.N.F.C., 15 16 29 3i 43 45 46 47 49 50 51 52 53 54 56 59 62 63 64 66 67 70 75 76 77 80 83 91 96 104 109 no hi 112 1 13 ”5 126 158 159 180 181 183 190 191 194 197 212 220 221 224 226 228 229 232 233 234 235 236 237 251 254 25 7 258 273 295 310 312 313 3i4 317 396 411 441 445 447 449 451 453 454 455 457 462 464 476 477 478 484 485 486 487 490 491 492 495 497 500 502 5 1 5 572 577 578 579 580 583 587 592 604 618 621 623 624 635 636 637 639 641 643 644 647 649 651 694 696 699 700 712 734 735 746 747 749 750 751 752 753 3- ■Co. Armagh. 150 151 186 187 188 189 194 251 257 525 4- -Co. Carlow. 259 305 322 35i 4H 702 5- -Co. Cavan. 248 251 261 469 470 504 5°9 522 653 658 691 715 7i7 719 6- -Co. Clare. 199 202 205 206 353 37i 376 424 426 434 OO CO 530 705 706 7 58 765 7 —Co. Cork. 1 7 13 17 3° i°5 140 141 142 H5 H7 152 i75 262 265 319 327 328 336 338 340 344 349 35° 352 355 357 358 430 575 620 670 726 727 739 740 741 761 8- -Co. Donegal. 44 192 239 251 270 271 272 306 307 309 416 4*7 421 423 433 440 465 496 497 5i9 557 584 616 648 704 718 9- -Co. Down. 14 23 45 48 57 60 61 65 68 69 71 72 73 74 78 81 82 165 166 169 183 186 197 229 232 251 275 301 31° 311 398 450 473 475 485 486 487 554 555 556 576 578 585 592 633 635 636 637 666 667 703 734 74* 895-96.3 3i5 10 — Co. Dublin. 32 216 33 260 121 290 124 298 128 299 132 300 133 3°4 136 337 *37 342 138 365 139 437 171 518 i73 54° 174 543 544 756 567 568 59i 593 612 615 622 626 627 629 722 723 724 11— Co. Fermanagh. 42 55 79 150 X5X 161 251 2 77 278 279 562 563 564 565 566 648 653 684 685 686 687 688 689 690 692 693 695 717 719 720 721 12 —Co. Galway, 97 202 207 208 251 33° 371 372 376 377 379 380 381 382 384 764 402 427 428 429 431 432 468 532 545 546 559 657 760 13 -Co. Kerry. 12 35 131 143 172 *75 201 211 289 328 335 336 339 341 346 347 349 352 359 425 426 603 744 761 14- -Co. Kildare. 173 174 184 300 343 348 35i 15- -Co. Kilkenny. i34 178 198 200 209 256 267 286 322 334 35i 489 510 55x 560 601 602 665 698 754 755 762 16 — King’s Co. 170 184 208 245 343 356 5°7 532 632 736 17- -Co. Leitrim. H9 251 369 469 470 653 712 7i7 742 18— ■Co. Limerick. 21 25 40 98 121 123 125 146 160 215 219 280 344 349 353 354 355 424 425 426 43° 434 483 55° 597 598 701 702 19— Co ». Londonderry. 86 1 3 5 176 189 190 191 196 247 251 272 274 3i5 433 44° 442 444 446 448 449 456 488 527 528 529 572 578 595 616 624 637 642 649 734 20 — Co. Longford. 40 148 203 204 208 251 325 326 33i 43i 47° 712 3 1 6 21 — Co. Louth. 58 138 251 304 308 525 570 22— Co. Mayo. [Appendix B.N.F.C. 97 * 149 242 243 25* 428 431 432 595 645 1 646, 650 65* 654 65^ 666 716 760 23 — Co. Meath. 144 148 171 *73 *74 179 184 251 304 308 337 470 614 669 683 684 707 731 24 — Co. Monaghan. 150 1 5 1 188 248 25* 308 471 509 516 5*7 522 525 7*9 25— Queen’s Co. 170 200 276 343 348 35* 356 375 53* 532 668 736 26— Co. Roscommon. 149 207 208 25* 363 43* 469 470 7 16 27 — Co. Sligo. 149 242 251 369 608 650 654 737 738 742 759 766 28— Co. Tipperary. 19 20 24 28 178 200 209 334 344 345 353 354 356 358 360 376 434 5** 524 532 533 668 682 733 736 755 767 29— Co. Tyrone. 151 167 189 192 251 257 4*7 433 521 52& 527 528 561 663 718 720 721 30 — Co. Waterford. 2 7 8 9 IOI 102 103 106 107 120 127 *55 *78 252 282 345 357 358 619 671 672 677 678 679 680 681 7 63 31— Co. Westmeath. 38 148 184 185 208 225 251 630 631 32 — Co. Wexford." 87 88 89 90 178 259 263 305 316 322 400 403 408 409 412 414 552 728 729 3S_Co. Wicklow. 33 128 *37 *39 259 300 302 305 342 409 410 418 435 436 506 5 12 5*4 536 539 541 591 593 622 628 640 I A APPENDICES VII. and VIII. (Vol. II.) TO PROCEEDINGS OF BELFAST NATURALISTS’ FIELD CLUB, Belfast : PRINTED AT THE “ BELFAST NEWS-LETTER ” OFFICE, 55, 57, & 59 Donegall Street. [Proc. B.N.F.O. 1905-1906.] SHOWING DISTRIBUTION OF ERRATICS A SUMMARY 1905- 1906.J OF RECENT GLACIAL INVESTIGATIONS BY THE BELFAST NATURALISTS’ FIELD CLUB. COMPILED BY madame rodolphe christen (Miss Sidney m. Thompson). Bern, an Appendix (No. 7 of Vol. II.) to the Proceedings of the Belfast Naturalists' Field Club, for 1905-6 . G 820 rB.N.F.G. APPENDIX. SUMMARY OF RECENT GLACIAL INVESTIGATIONS BY THE BELFAST NATURALISTS’ FIELD CLUB. Compiled by Madame Rodolphe Christen (Miss Sydney M. Thompson). Fully a dozen years have elapsed since a circular was sent to our Club by Mr. Percy F. Kendall, M.Sc., Secretary of the British Association Erratic Blocks Committee, requesting the Club to co-operate by examining the glacial phenomena of our district, with especial reference to the distribution of erratics in the drift. A ready response was given by the Club, and a geological section formed for the express purpose of conducting the inquiries, and a collection of Irish rocks commenced, to assist in identifying the parent locality from which the erratics had travelled, specimens of Scotch rocks likely to occur being presented by Mr. Kendall. A room was acquired at the Museum where meetings could be held and collections and instruments stored. The patient accumulation of a multitude of details on many points was willingly undertaken by many members of the Club, as well as by the little group specially appointed; and erratics from outlying districts were received from time to time, invaluable assistance being also given by Mr. S. A. Stewart, A.L.S., F.B.S.E., and Mr. Joseph Wright, F.G.S., whose works on the Mollusca1 and Microzoa2 of our boulder clays rank amongst the classics of British glacial literature. 1. Mollusca of the Boulder clay of the N.E. of Ireland. Proc. B.N.F.C. (2) I. Appendix for 1879-80, p. 165. 2. Post-tertiary Foraminifera of the N.E. of Ireland. Proc. B.N.F.C. (2) I. 1879-80, p. 428. 1505-1906.. 321 The work was commenced on the 12th of August, 1892 when Miss Mary K. Andrews, Mr. Stewart, and the writer visited a fine section of boulder clay 25 feet in depth, exposed (in making subway) at Greenland Railway Station. A short description of the work may be of interest, as all sub- sequent examinations were similarly conducted, sometimes by solitary workers, sometimes by the whole geological section, but usually by two or three members, amongst whom I must .gratefully single out Miss Andrews and Mr. Robert Bell, whose unwearying toil made this summary a possibility. Boulder clay usually contains innumerable stones of all sizes embedded irregularly throughout its mass. Of these 100 or more stones were selected at random, broken and counted to give the percentage of erratics, an erratic being defined as “any stone found m a glacial deposit that is not resting on its parent rock, no matter how short 1 distance it may have travelled ” lhe subjacent rock at Greenisland being Trias, every stone not of Tnassic origin was an erratic, and it was surprising and interesting to note what a varied assortment occurred, varying in size from chalk boulders, five feet long, down to tiny pebbles of far-travelled rocks from Scotland, Ailsa Craig, North Antrim Derry, and Tyrone, and large, beautifully-scored, and polished blocks of Silurian slate, hailing from either Scotland or the County Down. Shells were looked for, and bags of the clay col- Jected to be submitted to Mr. Wright for microscopical examina- tion. This is the most troublesome and tedious process con- nected with our researches, involving hours of monotonous labour on Mr. Wright’s part, with only occasional assistance from Miss Smythe, as sometimes several pounds of stiff clay \.h^u washed, dried, and floated, yield one tiny foraminifer too small to be visible to the naked eye ! Fossils found in the clays were carefully collected, and photographs of the section taken by Miss Andrews for future reference. Specimens of well-known rocks were listed in the field, other fragments being brought to the Museum, to be num- bered, mounted, labelled, and submitted to Mr. Stewart Mr J St. J. Phillips, A.R.I.B.A., or Mr. Seymour to ascertain theh 822 [B.N.F.C. place of origin. Unknown erratics were from time to time for- warded to Dublin to Mr. A. M'Henry, M.R.I.A., of the Geo- logical Survey of Ireland, whose unrivalled acquaintance with Irish rocks was always generously placed at our service ; to Professor Grenville A. J. Cole, M.R.I.A., F.G.S. (to whose warm sympathy and kindly help our geological section owes so much), to Professor W. W. Watts, F.R.S., and others, whose special knowledge made them able to identify the rarer erratics, and I gladly acknowledge the great assistance thus kindly given. Immense aid was also obtained from the fine Bibliography of Irish Glacial Geology3 expressly compiled for this purpose by Mr. R. Lloyd Praeger, B.E., M.R.I.A. We have more than a hundred different erratics in our Club collection; n of these are unquestionably Scotch, io others may be of Scotch or Northern Irish origin, the remaining 86 being Irish. An erratic of Ballachulish slate is our most northerly specimen, others from the Clyde Area. Cantyre, and fragments of fossiliferous Silurian rocks from Girvan carry us southward to Ailsa Craig, whose unique riebeckite rock is so widely distributed in our boulder clays. Passing to Ireland, we find fragments from the primary rocks of North Antrim, Derry, and Tyrone, others from Cultra, Castle Espie, the Coasts of Down, and from, Armagh, joining the icy procession until we reach in the pretty pink eurite found near Annalong our most southerly parent rock. A remarkable change has come over geological thought with regard to the glacial period in the dozen years that have elapsed since our section commenced its work ; gradually the controversy as to1 the origin of our drifts has died away, as the conception of a vast ice sheet from, various confluent sources moving over our islands, grinding solid rocks, picking up and transporting fragments of every material met in its progress, transforming the surface of the country by erosion and deposi- tion, became widely accepted. The issues to be studied were 3. A Bibliography of Irish Glacial and Post-glacial Geology. By R- Lloyd Praeger, B.E., B.N.F.C. Proc. 1895-6. 1905-1906.] 323 also vastly simplified, resolving themselves chiefly into the transport of erratics as indications of the directions of ice-flows • t e presence or absence of marine organisms' remaining an important factor m differentiating between ice-sheets of inland and transmarine origin. Let us pass in imagination backwards over an unknown but vast number of centuries to a period when Arctic conditions p e vailed over Northern Europe, and mighty confluent fields of ice slowly travelled onward, traversing the North Channel, the yde, and the Irish Sea, grinding out deep troughs in the sea floor where such an obstacle as Rathlin Island obstructed the lower layers, enveloping it, Ailsa Craig, and the Isle of Man, overflowing eastward into England, and entering Ireland west- ward over the noble promontory of Fair Head, the first in our list of localities recorded in this summary. The iceworn summit of Fair Head is strewn with erratics rom many points of the compass, and strolling further south we observe many large blocks resting on the cliffs that encircle urlough Bay Noticing one of schist we ponder on its origin. Was it torn from a bed of similar rock on the shore many hundred feet below, or was it borne on ice ao miles across the over TtTr r rr!CS “ Cantyre’ wh°Se fragment* are shattered either d Glancing at the tiny handful of pebbles g thered at random, over Fair Head, which include a. small rounded fragment of Ailsa Craig, which lies due east, one from a point near Torr Head to the S.E., a bit of chert, old red cong omerate, and a peculiar smooth-looking green felsite from Scotland or North Antrim, we see the significance of studying the distribution of erratics and the important deductions to be drawn from their presence on these Ballycastle headlands Our summary includes 36 localities, and we will follow the course of the intrusive ice southwards, first considering the dis- tribution of erratics from Ailsa Craig which are much worn indrcating severe ice action, even some specimens dredged by Mr. Welch 40 fathoms deep off Rathlin were ground completely smooth. It occurred at 26 out of our 36 localities, has been found round our shores by Mr. Welch at Portrush in sandhills 324 [B.N.F.C. by Miss Andrews at Portstewart and at Kilkeel, by Mr. H. J. Seymour, F.G.S., away down at Waterford and Youghal, and by Messrs. W. B. Wright, B.A., and H. B. Muff, B.A., F.G.S., at Whiting Bay and other Coik localities.4 Its absence from io of our localities is worth analysing, as in some cases this seems to tally with other circumstances sug- gesting a special period for these deposits. Although none was found at No. II., a drift-filled valley on Fair Head, fragments occur as loose drift half a mile away. Gleno, VI., Cave Hill, XV., and Divis, XIX., are small deposits of very local rocks ; Wolf hill, XVIII., and Dungannon, XXX., have not been fully investigated, and Killough, XXXIII., and Bloody Bridge, XXXV., have special features suggesting that they may be the product of later local glaciations. Although none was found in Castle Espie, XXVIII., boulder clay, fragments are frequent as loose erratics on the shore of Strangford Lough, XXIX., and Mr. J. O. Campbell found an isolated morsel on Spinkwee moun- tain in the Moume range. In spite of careful search, Mr. Bell never found any west of the Bann until this year, when he picked up a solitary piece on the shore of Lough Neagh, near Moyola River. Passing southward to No. III., the esker ridges about Killagan and Glarryford, we have another very important sign of an unsuspected iceflow to1 the N.N.W., in the frequent occur- rence of Templepa, trick rhyolite, the latter place lying some five and twenty miles S.S.E. W^e found rhyolites also at Bally- mena, IV., near Cookstown Junction. IX., in boulder clay at Macedon, on the western shores of Strangford Lough, and away down at' Newry, XXXIV. Turning for a moment from, the rhyolite fragments m Killagan eskers, let us read an extract from Mr. Maxwell Close’s 4. See Geology of Cork and Cork Harbour, Drift Memoir. Geol. Surv., 1905, p. 105, etc. Also Proc. Hoy. Dub. Soc., Vol. X., Part 2, p. 269 (1904). Pre-Glacial Raised Beach. W. B. Wright, B.A., and H. B. Muff, B.A., F.G.S. 1905-1906.' 325 famous paper on the Glaciation of Ireland,5 6 dealing with that neighbourhood:— “About 3y2 miles from Ballymoney, on the new road to Coleraine, at Seccaun Quarry, smoothings and stnations, N.W. by W., were found by me on basalt. It was impossible to say in which direction the grinding agent moved along the lines. . . . Near Cullybackey at the distance of about of a mile on the road to Ballyconnelly Cross-roads, stnations may be seen at a basalt quarry, N.N.W. Also on the same rock at the very cross-roads, r mile S.W. of Cullybacky a good example. These are parallel to the others, but it must be confessed they rather look as if the grinding move- ment were towards the N.N.W. This, however, I suppose, must be impossible.” Writing to Mr. Close some three years ago, I mentioned our discovering rhyolites at Ballymena and Killagan, to which he replied : — “I am interested and pleased to know what you tell me of the northward movement of frag- ments of Templepatrick rhyolite, which confirms my reading of those striations to which you refer.” This is the second time that our glacial researches have proved the remarkable acute- ness of Mr. Close s reading of glacial striae,^ Passing Ballymena, IV., we reach at Kilwaughter, V., and Gleno, VI., our only two localities where drift rests directly upon chalk, the former at an altitude of 500 feet,, yielding only 3 Ailsa and 2 Bauxite erratics amongst a crowd of dolerite, basalt, and cretaceous fragments. Gleno at 300 feet being a totally different deposit, crowded at its. base with Liassic frag- ments, its upper portion stratified, with unusually angular stones. Probably the basalt along this easterly coast has been stripped off the chalk by the impact of ice, as well as over Islandmagee, where magnificently glaciated surfaces of lime- stone are sometimes exposed in the quarry opposite Maghera- morne ferry, and our members are familiar with the ice-ground 5. Notes on the General Glaciation of Ireland. By the Rev. Maxwell Close. Journ. Roy. Geol. Soc. Irel., Vol. I., Part 3, p 215 6. Note on “ Glacial Geology of Kerry/’ by Miss Sydney M. Thompson. The Irish Naturalist, Vol. VIII., No. 3, p. 61, 1899. 326 [B.N.F.C. layers of basalt capped by boulder clay in the less-exposed face of the great Magheramorne Quarry. At Cloughfin, immediately north of Black Head, we have boulder clay resting on Trias about 50 feet above the open sea, and, as might be expected, we have a very varied series of erratics, including slate from Ballachulish, felsite from the Clyde, Cushendun, and Torr rocks, Ailsa rock, syenite from Slieve Gallion, ironstone nodules from Lough Neagh, granite from Slieve Croob, and three fragments of the porphyry dyke at Bloody Bridge, near Newcastle, nearly 50 miles south of Cloughfin. Just inside the mouth of Belfast Lough, near Whitehead, we find an interesting difference in the list of erratics at Cloghanport ; this deposit is only 4 or 5 miles from Cloughfin, but is much more limited in range. No rocks from south or west occur, Ailsa, Torr Head, and Cushendun furnishing the most distant boulders. Amongst the 339 erratics listed, 24 were from Ailsa Craig. We may group Ballyholme, near Bangor, with these two' seaside localities, and note abundant pebbles of Ailsa and eight undoubtedly Scotch rocks, including a Silurian shale from Girvan, containing a fossil trilobite. Retracing our steps inland to a group about Lough Neagh, with Drumsough IX. (near Cookstown Junction) and Cranfield Point, X., on its north, the glacial gravels of Antrim,, XI., and Glenavy and Crumlin, XVII., on its eastern shore, we still find erratics from Cantyre, the Clyde, Cushendun, and Slieve Gallion, adding granites from Pomeroy in Co. Tyrone, as we descend eastward to Woodburn Glens, XII., anl arrive at Greenisland, where our survey first commenced its labours with such a surprising list of travelled rocks. Once more we ascend the basaltic plateau, search- ing, at Mr. Wright’s request, for the highest attainable boulder clays, visiting the great quarry behind Carnmoney Church, and extracting with difficulty the boulders un- usually firmly bedded in the clay. Here we came upon chert, carboniferous limestones, and shales that have probably travelled 40 miles across the plateau from the Ballycastle coal- 1905-1906.] 327 fields. Subsequently we ascended the Cave Hill, and found a small deposit in the hollow behind M'Art’s Fort, more than a thousand feet above the sea, containing erratics of flint and several foraminifera, but the loftiest record fell to Mr. Stewart, who discovered fossiliferous boulder clay between 1,300 and 1,400 feet on Divis Mountain!7 8 In the recent geological survey memoir of the drifts around Belfast, published in 1904, we are told of Lake Belfast, 8 a vast expanse of fresh water, formed during the waning of the glacial period by flood waters from melting ice in the Lagan Valley dammed back by a barrier of ice that still existed across the head of our present Lough. The waters of this lake escaped y the Dundonald Valley, emptying themselves into Strangford 3 „ The Sravel PJt at Longhurst, XXVI., Neill’s Hill, XXI Morrison’s Sandpit, XXIII., and other deposits of Dun- onald Valley, XXIV., all belong to this late glacial period Possibly these southerly floods bore along much floating ice winch may partially explain the occurrence of many rocks from he Mourne districts in the Belfast drifts, in the Dundonald sands and gravels, and along the wave-worn boulder clays of Strangford Lough, where they are mingled with granites from omeroy, Slieve Gallion, and Slieve Croob, rhyolite from Tard- ree an eurite from Annalong, one unique specimen embedded in boulder clay at Castle Espie, XXVIII., being identified by . enry as a primary conglomerate occurring in Cavan, Monaghan, and Armagh, We found Castle Espie limestone as an erratic southward as far as Killough, where our geological sec mn eld a pleasant Christmastide excursion in 1897. This Killough deposit of stiff boulder clay and conglomerate, partially urne to calcrete, occurs close to Silurian rocks, whose splendid g aciation disappears below the waves; yet no microzoa were found in the clay from this section, although the spray is 7. The O« ot Boulder Clay on Divis. Proc. B.N.F.C. (2), IV.. p. 8. The G-O3p°%tte60ountry Around Belfast. Mem. Geol. Surv. Irel. 328 [E.N.F.C. actually beating upon its face. Is it, perhaps, the deposit of more recent inland glaciers during the waning of the “West British ice,” believed by Mr. Lamplugh to- have reached its maximum earlier, and to have shrunk more rapidly than the Hibernian ice? Loose erratics at the foot of these clay cliffs included carboniferous limestone from Armagh, which lies almost due west, with sundry rocks from Slieve Croob and Slieve Gallion, confirming Mr. Close’s observation of N.W. by westerly glacial movements in the Comber and Killyleagh districts. The geological survey memoir just alluded to mentions certain striae running east and west in this district,9 although the chief grinding movement seems to have been from N.N.W. to S.S.E. Mr. Kilroe believes these E. and W. striae to denote an earlier ice movement from the east, but the absence of microza in Killough section seems to' me almost a conclusive proof that it was not deposited by transmarine ice. I referred before to the importance of examining drift deposits for marine organisms, and microzoa formed our chief reliance owing to the remarkable scarcity of shells in our N.E. drifts ; they only occurred sparsely at 9 of our 36 localities. I once visited the celebrated glacial cliffs of Killiney, near Dub- lin, with Mr. Praeger, and easily collected more shell fragments in an hour than in seven years work round Belfast; a useful warning against conclusions drawn only from a single district. The presence of stones bored by marine plants or animals is another test used to1 distinguish submarine deposits. Of these we only found two, one at Cloghanport and one at Greenisland. The relative proportion of underlying rocks and erratics was another point recorded. Glacialists are well aware that in many drift deposits none of the subjacent rock occurs, although it may be found further on in the line of movement ; also that in Eskers, which usually rest on boulder clay (frequently pass- ing imperceptibly into it at their upper ends) erratics are usually carried further afield than in those contained in the boulder 9. Opus cit., p. 97. 1905-1906.] 329 clays upon which the Esher rests. Hence the value of these records. At Greenland we counted 300 boulders, each 100 taken at random, from a different level in the section : all were erratics, and the proportion in which they occured varied in a definite ratio for each level— 100 at Castle Espie, similarly pro\ed to be all erratic boulders. In the Black Mountain deposit, discovered by Mr. Bell, the only place I have seen in our district with distinct upper and lower boulder clays (the latter being so1 hard that hammer and chisel were required to extract ita stones), 270 out of 274 were erratics; at Cloghanport 331 out of 339, with percentages at other localities varying down to 17 per cent, at Carnmoney and Bloody Bridge, XXXV. The latter has been considered a, moraine deposit, and contained only a few travelled rocks, including a fragment of the porphyry dyke on the shore, 100 feet beneath, but no chalk nor flints were found in it. Another point noted in our schedules is the frequent oc- currence of some erratics and rarity of others. Of 107 varieties we found 26 at Dromore, XXXI., 27 at Ballyholme, 28 at Cloughfin, 33 at Newry, and 44 different rocks — almost 40 per cent, of the total list of rock varieties in the brickfields round Belfast, 10 out of 44 being isolated records of erratics, not as yet found elsewhere, showing the value of patient, persistent investigation, such as Mr. Bell devoted to them. Glacialists who may wish to study the matter more fully are referred to the tables accompanying this summary, and can examine our valu- able list and collection of erratics at the Museum and the manuscript schedules with detailed descriptions of localities investigated. When commencing work, we were frequently assured that we would, never find erratics north of their place of origin. Our experience does not at all bear out this assertion, which postulates a simple, southward ice-flow, and omits to reckon, with radiating local systems of glaciation that may have per- sisted over high ground prior to, and long after, the great central plain of Ireland and the Irish Sea were free from solid ice. A scrutiny of the tables giving the compass direction of 330 [B.N.F.C. parent localities of definitely-recognised erratics shows a sur- prisingly frequent mixture of southern rocks, even in our most northerly districts. In the drift memoir already referred to (p. 87) Mr. W. B. Wright suggests that our records of Mourne granite may be really due to the presence of a closely similar Arran rock found by him in drift on the basaltic plateau. Our Mourne erratics, however, include various dykes identified by Mr. M‘Henry as Tertiary intrusions in the Mourne range, one of the most distinctive being a pink eurite which he locates near Annalong. This we found in many brickfields round Belfast, in several places in Dundonald Valley, and on the shores of Strangford Lough. Our S.S.W. record is a large composite block of grit and Slieve Croob granite, weighing about 9 tons, discovered by Miss Andrews and Mr. Stewart on Rough Island, near the northern extremity of Strangford Lough, 18 miles distant from its home. In connection with this question of drift from the south, which suggests, a gradual amelioration of the local climate, I must not omit referring to an ox skull and vertebra and frag- ments of wood found by Mr. Bell in apparently undisturbed boulder clay at Springfield brickyard in 1895, an inch and half of horn protruded from the clay seven feet below the surface. The fragments were submitted to Professor Haddon, F.R.S., and Mr. E. T. Newton, of Jermyn Street Museum.10 Mr. Stewart and I subsequently visited the spot with Mr. Bell, and collected a bag of clay from the point where the bones were found, which was examined by Mr. Wright, but did not yield any marine organisms. When we recall the faunal conditions of Arctic regions in the present day, where the ice age still prevails, there seems no inherent impossibility in the coeval existence of animal life and many local icefields. Mr. Maxwell Close, Professor King, and many other geologists believed that the West of Ireland was relatively higher during the glacial 10. Proc. B.N.F.C. Report of Geol. Section. Miss Sydney M. Thompson (1895-6). p. 304. 1905-1905. 331 with°thphan f4 1PreSe.nt’ and lts western shores conterminous recen dred°° T °f SOundin^ belief sanctioned by whose m ^ °Ur WeStern C°aSt °n 3 muddy Pbteau, on Jr Art many D°negal b0ulders close *> ‘he edge of bv tf T A P°St-glacial Nation followed, indicated e el esker^d8 ^ ” Sh°reS’ wMe ^cial and . . ke” disappear beneath the waves of to-day. May we imagine these traces of land-ice and land-bogs to be com temporaneous during that post-glacial elevation, which some geologists consider was sufficiently great to connect Ireland with England and permitted the re-peopling of our island by animals from the less severely glaciated sister land ? In compiling this summary of the Club’s recent glacial work, I have felt strongly the lack of more thorough famfliarity with Similar work m other countries than is possible for those residing at a distance from great scientific libraries. When our work commenced in r893, Ailsa erratics had been found for the first time m Ireland by Professor Cole, and we can still recall the warm interest excited by our first schedule handed in at the British Association meeting at Oxford in 1894, when its frequent occurrence m our drifts was mentioned. Ours was the first report ever received from Ireland by that Committee during its exist- ence of fully 20 years. Our Club’s Annual Proceedings have also furnished the Geological Survey with many useful data for eir drift memoir, showing the value of careful local records, and the patient accumulation of details only possible to residents in a oca lty. The corresponding assistance rendered to local work- ers by such a memoir, which correlates our own observations with a wide experience of drift deposits in other parts of our islands is also inestimable. We have proved the ubiquitousness of Ailsa rock, and the frequent occurrence of other Scotch erratics, whose presence at Belfast was noted by Messrs. Bryce and Hyndman in 184 r.a We have established the unexpected occurrence of rocks many miles north of their parent locality, and traced many trains of 11. Beport on the Geology of Londonderry. Tyrone, and Fermaua-h By J. E. Portlock, F.R.S. Appendix, p. 738. 882 [B.N.F.C. -erratics across the land ; but some field work is still needed to connect distant records with our own neighbourhood. Let us compare the north-westerly occurrence of Temple- patrick rhyolite (see ante , p.824 ) and frequent chalk and flint from Malin to Inishowen Head, recorded by Mr. Close and Mr. Harte,12 in conjunction with evidences of an ice-movement northwards of Inishowen Peninsula. Professor Carvill Lewis, when visiting Ireland in 1885 to compare British with American glaciation, wrote13:— “My ideas concerning glaciation have now been completely revolutionised. I came to Ireland, expecting to find it glaciated from the north. I find instead a complicated system of ice streams. A Scotch sheet invaded the eastern corner of Ireland, going down to Belfast. The ice-sheet of the interior radiated off in all directions.” Again, when driving from Buncrana towards Malin, he describes “evidences of a great stream of ice moving north and east out of this valley. Slieve Snaght and the adjoining hills, together with this water- shed, formed a great snowfield. Did the whole ice-sheet of Ireland move out on this watershed, or did it only drain a local snowfield? The watershed is 500 feet high.” Mr. Close’s N.N.W. ice-stream was moving to meet this one at Malin on the other side of the same watershed. Coupling these facts with the rarity of Ailsa rock west of the Bann and the proximity of the great Sperrin range of mountains, where Mr. Kilroe has recorded evidence of a glacial movement south-eastward,14 seems to suggest a Sperrin ice-stream meeting the Scottish ice and a lobe diverging N.-west, bearing rhyolites and Ailsa with it. To ascertain the truth of this purely speculative hypothesis by in- vestigating deposits between Killagan and Malin Head should be a fascinating bit of work. Although the main mass of the intruding ice moved southward, pressing on the Mourne moun- tains as it received fresh streams from the heights to the west of 12. On the Post-Tertiary Geology of Co. Donegal. By William Harte. Journ. Roy. Geol. Soc. Ireland.. II., 30-67 (read 1867), 1871. 13. Glacial Geology of Great Britain and Ireland. By the late Henry Carvill Lewis, M.A., F.G.S. Longmans, Green & Co. (1894), p. 118. 14. Directions of Iceflow in the North of Ireland. T.I.G.S., XLIV., 827- 833 (1888). 1905-1906. j 383 Lough Neagh, passing down the centre of Ireland, sending off side-currents into Carlingford Bay and north of Howth on its ^’a,mr stream Probably reached Galway as suggested in Mr. Kilroe’s paper, a supposition interestingly supported by the discovery by Mr. J. O. Campbell during our Club’s visit in 1896 of an Antrim flint on one of the Aran Islands in Galway Bay Mr. Kilroe informs me that Antrim, flints have a good distribu- tion westward, and he recently found one in coarse sandy alluvium m Co.. Limerick, which must have travelled west in ice and down the Shannon valley, probably in river drift In response to my mention of the N.N.W. rhyolite erratics he wntes 1 - ~t’AU I have seen of the drifts since my original paper on the Ulster ice-flow has confirmed me in the opinion that there must have been an overwhelming flow . . . from Scotland over Ulster, and that this was followed by a flow northward and southward from Hall’s axis of Irish distribution perhaps N. by W . in Antrim, northward through Co Derry and N.N.E. through Donegal. I should not say that this northerly flow or any part of it constituted part of the over- whelming Scottish ice, though materials carried westward by the latter may have been subsequently carried northward and southward from the region indicated by Hall, extending from South Antrim to Galway.” Our own observations incline me to question whether the Scottish ice swept westward over Donegal as Mr. Kilroe indicates, but these points are purely personal speculations to be refuted or confirmed by further investigation. In conclusion I cannot speak too warmly of the fascination of erratic-hunting, and the triumphant joy of bringing home a handful of unfamiliar fragments ; of many pleasant days spent m the open-air along the shore or on breezy hillsides, till the icefields of the past became living realities to us, and we almost seemed to share in their irresistible onward movement. Neither can I conclude without a grateful reference to the many un- dying friendships cemented by mutual tastes and mutual toil and study that will ever cluster round the memory of our pleasant Field Club Excursions ! !3! VI XIV XLV XXXIV \ \ \ I XVI SIX XXIX XXII XXXV XXV xm X V 1 1 XLII Will XXXVI XXVIII Fair Head Bally voy and Cnlhame (Ballycastle) Killagan and Olarryford . . I '.l I I \ 1 1 ICl III Kilwaughtcr (Larne) Cranllold Point, N. shore, Lough Neagh Antrim Gravels, near Antrim Station Woodburn Glens, Carrlckfergus Greenisland Station Qnarry behind Caramoney Church Cave Hill (McArt’s Fort) Ballyholme, Bangor Crumlin and Glenavy, E. shore of Lough Neag Wolfhill and Llgoniel, Belfast Dlvis Mountain . . Black Mountain Brickfields round Belfast Neill’s Hill Mori Ison 's Sand Pit, Dundonnld Station Ballyoran and Carrowreagh Colin Glen Longhurst, Dunmurry Island Hill and Rough Island. N -W. shore Lough Castle Espie W. shore of Strangford Lough Dungannon Dromore Armagh Tyrone Down Armagh 1,300 to 1,4( 600 30-220 Sea level 39 Sea level Sea level 90 100 Sea level and Trias Basalt Trias Carboniferous Silurian Carboniferous Silurian s and g b e, s and g Derived Fossils. Cret Carb, Lias, Cret Cret Cret Sil, Carb, Lias, Cret Cret Lias Carb (Castle Espie) Relative Proportion of Shells Shells For and Ostra None For (May, 1906) For (very rare) Abbreviations Types of Drift— Is d— loose, stoney drift ; b c— boulder clay ; s— sand; g— gravel. Compass direction In which the parent rock of erratics Ilea, taken from tho localities whore such erratics were fouud. W.N.W.j N.W. N, N.W. N. N.N-E. 1 1 N.E. E.N.E. E. E.8.E. |„ S.S E. S. S.S w. s.w, W.8.W, Ino, 8 1 8 1 1 1 J 1 'g ’• :: 3 *2 2 3 1 2 1 I? 1 2 1 7 12 1 8 2 18 *i 2 9 81 *8 1 i 8 \l ;i 17 18 20 1 6 3 g 1 1 :: 3 22 28 •i 6 2 1 :: 1 "i 26 20 2 1 1 27 'l ‘3 2 -1. 1\ 29 *3 * 2 1 'i ‘i 32 1 :: 3 10 *i *2 84 1 ■■ ‘i 30 I- 2 1 14 26 os 10 47 3 2 11 8 14 1 2 Shells.— frag— fragmentary, Microzoa.— For-foraminifera ; Ostra— Ostracoda. Blanks indicating that the drifts of that locality have not yet been examined. “ None "—that drifts were examined and none found The relative proportion of erratics was ascertained from boulders of all sizes taken at random and counted. The Compass direction is only given for erratics, whose parent rock is definitely ascertained, excluding rocks found in situ in more than one locality. 1905-1906.] THE CARNMONEY CHALCEDONY: Its Occurrence and Origin. (With a General Note on the Formation of “Secondary’ Siliceous Minerals in Volcanic Lavas). By JAMES STRACHAN. Being an Appendix (No. 8 of Vol. II.) to the Proceedings of the Belfast Naturalists' Field Club, for 1905-6. H 886 [B.N.F.O. THE CARNMONEY CHALCEDONY, ITS OCCURRENCE AND ORIGIN, (WITH A GENERAL NOTE ON THE FORMATION OF “SECONDARY” SILICEOUS MINERALS IN VOLCANIC LAVAS). BY JAMES STRACHAN. i. Carnmoney Hill, with its steep escarpment sloping sharply towards the Belfast Lough, is a prominent and picturesque feature in the landscape of the country lying to the North of Belfast. The attention of the geologist is attracted both by the peculiar shape and the comparatively isolated position of this Hill, which represents the site of an ancient volcano, from whose throat, in Tertiary times, poured forth part of the Upper Basaltic Lava. On the south side of the hill, the denuded ‘neck’ or ‘plug’ of this old volcano may be traced, cutting through the Lower Basalt, the Cretaceous, and old<_r strata. The Upper Basalt and part of the Lower have been re- moved by denudation, leaving the plugged-up vent, which is almost one quarter of a mile in diameter. The material of the neck is a vesicular lava similar in appearance to that of the doleritic dykes found in various parts of Co*. Antrim. In a recent Survey Memoir, the following petrological analysis of this rock is given: — “Under the microscope the rock is a fairly coarsely crystalline dolerite, containing much magnetite in the form of opaque, black, and unaltered crystals. The chief constituents are pale brownish augites and fresh plagioclase laths (labradorite) intergrown, ophitically with one another. There occurs also here and there in the sections a more com- pact or finely crystalline material of similar composition, but with a large proportion of glass. It is chiefly in this part that the mineral ‘hullite’ occurs as a brownish or greenish-brown translucent substance, somewhat like palagonite in appearance, 1905-1906 J 837 1 in the rock Th ^ g irregularlyshaP^ vesicles “ the rock. The central greenish (chloritic) part is usually almost isotropic, and is surrounded by a zone of yellowish brown material, with a fibrous structure and a radial arrange- ment of the component parts.” ° Professor Hull remarked that olivine was also present in the tock but according to Professor Cole it is by no means an abundant constituent of the mass. There is no doubt, how- ever, think, that m some places the rock approaches the nature of an olmne-dolerite, and, that in such portions of the wen60 1 'C m ale °f m°re C°mm0n occurrence than P ely siliceous ones. To this analysis must also be added iron pyrites, which appears to be distributed in a very irregular ashion th roughout the rock. On the whole, it is not a common onstituent, but occasional fragments of the rock may be found ■containing at least five per cent, of the bright, brass-yellow f rys als. In the mam, we may freely accept Professor Cole’s description and nomenclature of the rock as a basaltic-andesite ■or allied to the pyroxene-andesites. Although coarser in crystalline structure, the basaltic-andesite of Carnmoney is nearly related to many of the Scottish andesites, which are compact rocks made up chiefly of labradorite, with a smaller proportion of augite, and without olivine ; from these lavas are obtained the finest of the chalcedonies, known as ‘Scotch pebbles.’ 2. The Chalcedony of Carnmoney occurs in large cracks, or veins, in the rock. These are sometimes as much as twelve inches in width, and from this, the cavities thin away into a mere hair’s-breadth. These veins have apparently been formed during the consolidation of the lava, for the vein-sides are coated, m all degrees of thickness from a mere film to one inch with the mineral hullitc, which has been described by Professor Cole as “the altered and hydrated glass of the original basaltic ground-mass. ’ As the hot magma hardened, the cooling and crystallisation of the minerals caused mechanical contracdon to lake place, resulting in the formation of large cracks into which 888 [B.N.F.C. the still fluent portion of the lava was secreted, coating the walls of such cavities with ‘hullite.’ This mineral must now be con- sidered for a little, because its presence plays an important part in the structural arrangement of the Chalcedony, and perhaps in the deposition of the silica, in that form. Hullite is a black pitch or waxy-like substance, passing in colour to yellow-brown and red-brown. It is soft (H— 2 to 3) and extremely brittle, breaking with a smooth, slightly conchoidal fracture. In thin sections the black specimens show a greenish colour, but a good deal of the hullite in the cavities and veins is more yellow- ish-brown and reddish-brown in colour. This mineral has been described as mammillated and ‘minutely stalactitic, but ‘minutely reniform* or ‘minutely spherical’ would be a better description, because the ‘stalactites’ of hullite, like those of chalcedony, have a fibrous structure, and seem to be ‘animated by a kind of crystalline spinal energy.’ Very rarely these spherical forms are slightly translucent, and by reflected light appear to' glow with a fiery amber colour. The thicker deposits of hullite, coating the sides of the veins in which the chalcedony occurs, are often cracked and fractured, representing on a minute scale the larger cracks or veins of the mother-rock. These small cracks are filled up in the same fashion as the large veins, with chalcedony and other minerals. In chemical composition hullite varies, but it might be described as a basic mineral, composed of aluminium, iron, magnesium, and calcium silicates, containing about 39 per cent, of silica, and about 13 per cent, of ‘water of hydration.’ It has been placed minera- logically as ‘near delessite,’ but might be said to occupy a posi- tion between celadonite and chlorophseite, so far as chemical composition is concerned. All of these minerals, however, vary in their composition, and by some mineralogists are not regarded as definite species. The old-fashioned name of ‘green earth seems to> be the best title for minerals of this class, although several are not ‘green,’ and a number not ‘earthy.’ Fifteen years previous to Professor Cole’s investigation of hullite, the latter was carefully examined, for the first time, by E. T. Hard- man and Professor Hull. Hardman came to the conclusion 1905-1906.] 339 the th T t SeC° 7 mmera1, and dassed k as a member of e chlorito-ferruginous group or green earths. As far back as the year 1837, however, Dr. Scouler described it as a ‘pitch- stone, ^ or volcanic glass, and in 1843 General Portlock called 1 an obsidian. It is of interest to trace the history of geo- ogical opinion concerning hullite from these earliest references to those of the present day. In the years 1837-1843, it was regarded as a volcanic glass, which had been exuded into the “ lava, cooled. About the year 1868 this opinion UtP^Id bl'1G- V' du N°yer> but ten years later Hardman departed entirely from this view, as we have already stated escribing it as a secondary mineral of the green earth variety.’ n 1879, as Professor Cole has pointed out, Dr. Heddle, of St Andrews, supported Hardman in his claim for the retention of ! aa a definite mineral species. It is here worthy of notice, that Heddle’s views concerning the origin of such green earths underwent a complete change; in 1871 he re garded such minerals as contemporaneous with the last stages of coohng in the early history of the lavas in which they are nd whereas in his “Mineralogy of Scotland,” written at a tion r, Ti f’ u* d6SCribeS the same minerals as decomposi- tion products of the weathering lava. In the same year (1879) “ ,au t’ of BeIfast, took up this idea, that hullite was a thart Ty ,mmera1’ and accounted for its origin by supposing that it was deposited, along with chalcedony and other siliceouf necT ‘ S’ n h0t aIkaHne Spri^s wbicb arose in the volcanic The h ?n§n,arer V C31liC f0rces had sPent their vigour.’ The hot alkaline water acted on the rock sides and penetrated ground of the rock, dissolving mineral matter from the mass, and ^-depositing it in the gas-vesicles and veins. In 188; hullite was again examined, on this occasion by Lacroix, who also determined it to be a secondary mineral related to the decomposition-products of olivine. Latterly, in 1895, Professor Cole reviewed the opinions of Hardman, Hull, Heddle, and Lacroix, and, setting aside the idea that hullite is a ‘secondary mineral at all, described it as ‘a basic glass that has become soft and gummy ’ by alteration.5 840 [B.N.F.C. 3. In considering the above interpretations of observed facts, we may class the theories for the origin of hullite into three distinct groups. These are : — (1) . The Igneous Theory (supported by Scouler, Portlock, and Du Noyer), that hullite is a glassy substance like ‘pitchstone’ or ‘obsidian/ and was probably formed during the last stages of the rock’s solidifying. (2) . The Mineral Theory (upheld by Hardman, Heddle, Gault, and Lacroix) that hullite is a ‘secondary mineral’ of the green earth group, and was probably formed during the decomposition of the rock, per- meated by meteoric waters in the ordinary course of rock-weathering, or by hot alkaline waters of telluric origin, under special circumstances. (3) . The Altered-Glass Theory (presented by Professor Cole) that hullite is ‘the altered and hydrated glass of the original basaltic ground-mass,’ or ‘a basic glass that has become soft and “gummy” by altera- tion;’ it was formed in the first place by igneous fusion, but has suffered subsequent transforming changes. There is no' doubt whatever that Professor Cole is correct in his surmise as to the identity of the hullite lining the cavities of the rock, with the material of the ground-mass, but, with all due respect to' his fine treatment of the subject, I am inclined to1 doubt that hullite was in the first place simply a volcanic glass ; I believe that this substance was not only hydrous in its composition from the first, but that it has not undergone any extensive alteration since that time. In its original condition,, and as still found in certain portions of the rock, the hullite might be more accurately described as a hydrous, waxy sub- stance, intermediate in its nature between a volcanic glass and a green earth. Professor Cole compares the alteration of the original hullite to its present form, to the alteration of basaltic glass into a green “serpentinous” material ; but, where the hullite is altered, I believe that the change is mostly a physical one, and only to a small extent chemical. The resemblance of 1905-1906 ] 341 hullite to a chloritic mineral I regard as an original structure. It is closely related to the green earths, celadonite and chlorophseite, which form the 'skin’ of many agates, and which originated in quite a different manner from the “serpentinous” green earths; the latter are decomposition-products, and the former are contemporaneous formations of the lava. Professor Cole compares the coating of hullite in the vesicles to 'lava- stalactites’ on a small scale, 'the glassy matrix of the lava having oozed out under pressure into any cavities it could find;’ but these 'stalacites’ and spherical crusts of hullite possess a fibrous structure similar to the reniform or spherical growths of haematite and chalcedony, and I believe that the hullite was formed, to a great extent, under the guidance of active crystal- line forces.. The highly vesicular nature of the rock suggests the probability that that much water was present in the hot magma, and that the formation of the hullite was not purely an igneous action, but rather intermediate between igneous, and hydro-thermal. 4- The extensive literature concerning hullite has rendered Carnmoney Neck historic in the annals of mineralogical geology, but of the chalcedony and other minerals found in the cavities of the rock, very little has been said or written. The Survey Memoir, for example, merely mentions the fact that 'a good deal of chalcedony occurs throughout the mass, and occasionally fills the vesicles.’ Gault investigated the 'chalcedony and other siliceous minerals’ generally, but did not give any detailed de- scription of the type-vein containing them. The typical vein at Carnmoney consists of three distinct layers, or groups of layers, more or less intergrown, and representing three con- secutive stages in the deposition of the mineral matter filling the vein. These are: — (1). The Hullite Layer, consisting of hullite in varying degrees of thickness from, a mere film to a crust, which is never more than an inch in measurement! The usual thickness of this mineral is one-sixteenth to one-eighth of an inch. The hullite coats the rock-sides, and was the first substance deposited in the vein. 342 [B.N.F.C. (2). The Zeolitic and Calcitic Layer, deposited im- mediately on the surface of the hullite, consists of a thin layer, occasionally of fibrous zeolites, but gener- ally composed of calcite. The usual thickness of this layer is about one-sixteenth to one-eighth of an inch, and it is mostly much weathered. The zeolitic parts of this layer appear to consist chiefly of natrolite, and occasionally this passes into analcime. Small crystals of chabazite are also to be found in this portion of the vein. The zeolites and calcite are rarely found together, but when they occur thus, the former have been deposited upon the latter. The thin layer of calcite frequently develops sporadic crystals of that mineral to % of an inch in length. {3). The Chalcedonic Layer, coating the second layer, and sometimes entirely filling the central portion of the vein. After a single layer of chalcedony had been deposited, the large sporadic crystals of calcite again appeared here and there on its surface. These crystals in turn became enveloped by a second, and by succeeding layers of the chalcedony, and the finest examples of spherical crystalline growth may be found in the latter. In such in- stances, there is often in the chalcedony immediately investing the calcite crystals, a zone of white, opaque, jaspery material, containing calcareous and zeolitic matter. The Carnmoney chalcedony exhibits all the typical structures of that mineral. In colour it varies from bluish- white to bluish-grey, the latter being more translucent than the whiter varieties. A beautiful translucent specimen, with typical reniform structure, was found to have a specific gravity of 2.582. A section through the reniform chalcedony shows very well its fibrous and spherically-crystalline arrangement. The chalcedony is almost entirely composed of these ‘radiate- 1905-1906 j 343 acicular fibres, but it also contains a small quantity of amorphous silica, perhaps opal. The fibrous structure becomes very apparent when a polished section is etched with hydro- fluoric acid. In, many instances the chalcedony passes into crystallised quartz, which has sometimes an amethystine colour. Small groups of crystallised iron, pyrites occur sparingly on the surface of the chalcedony in some of the veins. Between the first and second layers of the chalcedony a very thin crust of a green earth, resembling chlorophseite, is sometimes found. The banded arrangement of the chalcedony, layer upon layer, parallel to the vein-sides, is often varied by onyx-layers of milk-opal and wax-opal, perfectly level and apparently formed under the influence of gravity. A variety of cacholong, com- posed of opal, with an admixture of zeolitic and chalcedonic- quartz fibres:, is also found in the onyx-structures of the veins. Gault has pointed out that one kind of opal found at Cam- money becomes very strongly phosphorescent when it is pressed against a revolving grindstone. Tribe-luminescence appears to be a marked characteristic of both chalcedony and opal. This phenomena is often observed by those who are accustomed to polish agates and other siliceous stones. 5- Mineralogical opinion on the mode of formation, or origin, of the various chalcedonies found in volcanic lavas is much divided, and on the whole, rather indefinite. One hundred years ago the early mineralogists regarded the chalcedony as a contemporaneous product of the lava, in which it is found. To-day the general opinion, expressed in well- known text-books on geology and mineralogy, is that the chalcedony found in the cavities of volcanic lavas is a decomposition-product of the weathering and decomposing rock. For example, let us take the common variety of banded chal- cedony known as ‘agate’ or ‘Scotch pebble.’ * In the old days Jameson described agate as contemporaneous with the lava in which it is found embedded. In more recent times Heddle, who studied agate very carefully, came to the conclusion that it was purely a decomposition product formed in the ordinary course of rock-weathering. This view has been stronglv upheld 844 [B.N.F.C. during the last twenty years by J. G. Goodchild, and to-day we find a similar opinion in the fine text-book by Professor Miers. Other writers, still pointing to rock-decomposition as the source of this ‘secondary silica/ regard it as more or less a product of ‘solfataric’ action formed soon after the solidifica- tion of the lava.. But even the standard text-books of geology are strangely indefinite in their remarks on this subject. The Carnmoney chalcedony is a very near relation to- the agates found in the Scottish andesitic lavas, and bearing this in mind, we may express modern opinion as divided into two classes of theories concerning the origin of chalcedony in lavas. These are : — (1) . The Hydro-thermal or Solfataric Theory. This theory was applied to the Carnmoney chalcedony by Mr. Gault, who supposed that, long after the volcano' has spent its forces, hot alkaline water was poured into the veins and per- colated through the mass of the rock. These hot springs dis- solved silica and other substances out of the rock-mass, and re-deposited them in the cavities and veins. He thus accounted for the origin, not only of the chalcedony, but also' of the hul- lite and other minerals. Gault seems to have considered that a common origin must be sought to- account for the formation of all the minerals found in the veins. (2) . The Epigenetic Theory. The theorists of this class hold that the chalcedony is a decomposition-product formed during the weathering of the mother rock. Rain-water falls upon the ground, and passing through the soil, which contains decaying vegetable matter, becomes charged with carbonic acid gas, and humic acid, which gives rise to carbonic acid. The dilute solutions of carbonic acid slowly percolate through the rock-mass, attacking the silicates, and become charged with carbonates of the alkalies and alkaline earths, and free silica. Labradorite, for example, loses sodium and calcium, which are removed as carbonates, and silica as silicic acid, leaving silicate of alumina behind in the form of clay. The calcium carbonate and silica are deposited in such cavities or veins as occur in the 1905-1906.] 345 rock, and the sodium carbonate is supposed to attack fresh silicates, setting free more silica. Both of the above theories, it will be observed, depend upon the decomposition of the mother-rock for the supply of mineral matter deposited in the veins and vesicles. In the first case, the action of the hot alkaline waters, aided by carbonic and hydro-sulphuric acids, is supposed to have been a com- paratively rapid one; while, in the second theory, the decom- position of the rock and deposition of the mineral matter in the cavities by the action of cold, slightly alkaline water, aided by carbonic and humic acids, is supposed to have extended over extremely long periods of time. G. Bischof calculated that it would require no less a time than 1,296,000 years to deposit one pound weight of amethystine quartz in this fashion. 6. It has been frequently pointed out that trap-rocks and lavas containing nodules and veins of chalcedony are for the most part much decomposed. In some cases they are com- pletely weathered into a. saponaceous green, earth, from which the chalcedony may be dug out without trouble. Some geolo- gists go- so far as to1 say that the beauty of the chalcedonic con- cretions is in direct proportion to the amount of decomposi- tion suffered by the mother-rock. I have not found this to be the case as a. general rule. Agate and chalcedony in the un- altered rock are more difficult to get at, but such specimens are almost invariably much better than pieces from, the weathered rock. Indeed, where the rock is very much decomposed, the chalcedony has also1 suffered changes, being cracked, stained, and devitrified. This is the case at Carnmoney, for the finest specimens found there are extracted from the portions, of the rock that have suffered the least from weathering influences. Many of the veins, in this rock have suffered so much from percolating surface-waters that the zeolitic or calcitic layer has been entirely removed, and the chalcedony lost much of its native translucency. When such veins are broken open the chalcedony usually drops out because of the clear space be- tween it and the rock-sides, and it is often found to be much weathered. 346 [B.N.F.C. On, the whole, I feel convinced that such deposits of chalcedony in volcanic lavas, and this one at Carnmoney in particular, are contemporaneous formations of the rock, and that they were formed during the last stages of the lava’s cool- ing and drying. Furthermore, I am, constrained to believe that the zeolitic or calcitic layer, and the siliceous contents of these veins and cavities, owe their origin, not to the decomposition of the mother-rock, but to the final process of its construction. In all probability the water present in the hot lava pjayed an important part in the formation of these minerals. We may look upon this process of vein-filling in lavas as an example of the thorough economy so often exhibited in Nature. During the consolidation of the lava contraction took place, and the cracks or veins were formed. These were points of weakness in the rock — real wounds — and Nature immediately set about their healing. The residual magma — the very life-blood of the lava we might call it — was secreted into- these rents, impelled more or less by physical forces, but, nevertheless, continually guided within itself by active crystalline- energy. The hullite, calcite, zeolites, and chalcedony were deposited each in its order, and when the rock was cold and dry these minerals stood each in its place, and each ready to play its own part as a necessary portion of the solid earth. There is an unbroken sequence in the mineral matter from the main constituents of the lava to- the chalcedony in the centre of the veins. Professor Cole has shewn that the hullite plays the part of a true ground- mass in the intercrystalline spaces of the rock. Lacroix ob- served that the hullite has included in its formation minute crystals of felspar and magnetite ; also- small crystals of calcite. The calcite and zeolites follow upon the hullite, and finally the chalcedony, which in its growth has included crystals of calcite, and zeolitic matter. 7. That the calcitic or zeolitic layer of the veins is often much weathered I have already mentioned, and very often, its former presence can only be inferred from the hollow pseudo- morphous cavities in the chalcedony. This calcite has in some cases been re-deposited in other portions of the veins, and 1905-1906.] 547 occasionally minute tufts of zeolites may be found in similar positions. There is no> doubt that cold, surface-waters, charged with carbonic acid, can remove calcium carbonate from the rock, and dissolve existing crystals of calcite, carrying away, in the form, of bi-carbonate, considerable amounts of that mineral, and re-depositing it in other places. The formation of zeolites- from felspar and from existing zeolites takes place in a similar manner, but tO' a much less extent ‘ and the formation of chalcedony in this fashion appears to' be a very rare occur- rence. There is also- no doubt that these reactions, resulting in the growth of calcite, hydrated silicates, and various forms of silica, would go on at a much faster rate, and to a much greater extent, if the cold meteoric waters were replaced by hot alkaline waters of telluric origin. These actions have their place in nature ; but when we consider the molten magma from which certain lavas have been formed, containing water under immense pressure, and at a temperature far exceeding that of any solfataric water, we come to the conclusion that the residual waters of such magmas contained large quantities of silica, silicates, and carbonates in solution. As the temperature fell, the dissolved mineral matter would be secreted and deposited in the veins and cavities, in a definite sequence, according to the nature of the dissolved elements. It is natural that such secondary minerals should bear some chemical relation to the primary rock-forming minerals, because both are formed from the same magma. The rock-forming minerals of the Carnmoney basaltic andesite are augite, labradorite felspar and magnetite. Augite is composed mainly of calcium, magnesium, aluminium, and iron silicates, the silica amounting to 47-48 per cent. In the hullite we find hydrous silicates of the same elements, iron being the preponderating element. When the water of hydration is omitted from the analysis the silica amounts to almost 46 per cent. The primary augite and magnetite have thus a second- ary counterpart in the hullite. Labradorite is composed of aluminium, calcium, and sodium silicates ] the silica amounting^ t°‘ 5 2_53 Per cent. In natrolite (the most common zeolite in 848 [B.N.F.C. this rock) we have a hydrous silicate of aluminium and sodium. When the water of hydration is omitted from the analysis the silica amounts to 52 per cent. The natrolite occasionally passes into analcime, which is a more acid, hydrous silicate of aluminium and sodium. In these zeolites the aluminium and sodium silicates of the felspar have a secondary representation, and the calcium silicate of that primary mineral has its second- ary counterpart in the calcite and the free silica of the chalcedony. 8. From this point of view it is evident that we cannot draw the line very finely between the terms primary and second- ary, if we regard the former as applied to minerals of igneous origin, and the latter as applied to minerals of aqueous (hydro- thermal) origin. In the formation of such rocks, and the mineral contents of their veins, there is an unbroken sequence of action from igneous to hydro-thermal, and it is possible that a mineral might be formed by a process which is neither a purely igneous one nor purely an aqueous action. We see this in the case of hullite, which, from one point of view, has been described as a basic volcanic glass of igneous origin, and from another as a hydrous green earth of aqueous origin. There is a certain amount of truth in each aspect, and the truth in both cannot be reconciled by regarding the hullite, on the one hand, as a volcanic glass altered to1 a green earth material, or, on the other, as a member of the green earth family derived by solution and decomposition from the primary minerals in the rock. It is more likely that from the beginning the hullite was by nature both a volcanic glass and a green earth. Mineralogists do not seem to have made a clear enough distinction between the two great sources of ‘secondary’ minerals in lavas — t of the Irish Liassic Fossils— late, 1 Plate ... ... ••• / Eighth Annual Report-1870-71, containing Appendix II., Lurt of Irish. Liassic Foraminifera— Wright ; and List of the lossils of the Estuarine Clays of Antrim and Down— Stewart ... ip Ninth Annual Report — 1871-72 Proceedings — Series II., VvLV, Part I., 1873-4, containing' Appendix III.” List of Mosses of North-East of Ireland — Stewart ; and List of Cretaceous Microzoa of North of Ireland— Wright, 2 Hates Series II.,Vol. I., Part II., 1874-75 ” „ III., 1875-76 ••• IV., 1876-77, containing Appendix IV., Recent Foraminifera of Down and Antrim Wright, 1 Plate , and Silurian Rocks of County Down— Swanston and L,ap- WSeries Il^Volf I. , Parts V.' and Vl.','l877.78 a„d ’78-''79 (in one)' ” Part VII. ,1879-80, containing Appendix V., List’of Post-tertiary Foraminifera of North-East of Ireknd— Wright; and List of Mollusca of lioulder Clay of North-East of Ireland— Stewart ... ••• vj" Series II., Vol. 11.. Part I., 188t 81 containing Appendix \ I., ” List of Foraminifera of South Donegal— VV right ; Sponge Remains from Carb. Limestone, County Sligo— Wright, and Fossil Sponge -spicules, County Shgo—L’arter, 1 llate Series II., Vol. II., Part 11., 1881 82 ... ,J }> III., 1882 83, containing Appendix V II., ” Supplemental List of Mosses of the North-East of Ireland— SSeTiai\l , Vol. II., Part IV., 1883-84, containing Appendix ” VIII Notes on Irish Coleoptera— Haliday ; Cromlechs of Antrim and Down-dray, 12 Plates; and Pre-hrstonc Monuments near Sligo — Eleock, 4 Plates ... ... ••• „ Series II., Viol. II., Part V., 1884-85, contain^ Appendix IX., Ostracoda of Belfast Lough-Malcomson ; Furfgi of North of Ireland— Lett ; Foraminifera of “ 1 roteidor Wright; Cretaceous Foraminifera of Ke&dy Hill— Wright , Trish Coleoptera — Patterson ••• . ••• ■;* ' Series II., Vol II.. Part VI., 1885-86, containing Appendix ” X The Ferns of Ulster— Phillips and Praeger ... „ Series II., Vol. II., Part VII. , 1886-87, containing Appendix II. Notes on the Sections exposed at the Alexandra Dock Belfast, with. List of Fossils, 1 Plate— Praeger Series II., Vol. III., Parr I., 1887-88, containing Appendix ” nx. Marine Shells of the North of Ireland Praeger Series II., Vol. III., Part II., 1888-89 ... ••• ••• ” e > , „ hi. ^ 1889-90, containing Report of Larne Gravels Committee, 2 Plates „ Series II., Vol. III., Part IV., 1M0-91 . ••• ;;; ” ” Vl! 1892-93 2/6 V- 1/- 2/6 1/- 2 1- 1/6 v- • 1/- 3/- 3/* 2/- 2/- Index Series II., Vol. IV . Vol. V. Part L , 1893-94, containing Appendix IV. V. VI. 11., 1894-95, 111., 1895-96. IV. 5 1896-97, V., 1897-98, VI., 1898-99, VII i 1899-1900, 1900-01, in one Parts I. & II., 1901-02, 1902-03 „ Part III., 1903-04 „ IV., 1904-05 ... .... ••• V. 1905-06, with Appendices VII. ” ’ and VIII. 2/- 2/- V- 2/- 1/- 1/- 2/* 6d 2 /- 2/- 2/- 1/- ifc 2/- 2/- 1/- V-