It\ FIGURES OF REMARKABLE FORMS OP POLYCYSTINS, OR ALLIED ORGANISMS, m THE i$ariiatro^ Ci)alfi Dcjjosit, (CHIEFLY FROM THAT COLLECTED BY DR. DAVY, AND WHICH HE HAD NOTICED IN A LECTURE DELIVERED TO THE AGRICULTURAL SOCIETY OF BARBADOS, IN JULY, 18iC.) DRAWN BY MRS. BURY, AS SEEN IN HER MICROSCOPE, ON SLIDES PREPARED BY CHR. JOHNSON, ESQ, OF LANCASTER, 1860 AND 1861. :>^ i J. (-^ - Itibvarjr of % Pitsciim OP COMPARATIVE ZOOLOGY, AT DARVARD COLIECE, CAMBRIDGE, MASS. JFounticli I)j prtbatc subscrfjjtfon, fn 1861. From the Library of LOUIS AGASSIZ. No. b0 8 h. OP EEMARKABLE SS!U «i« Jfftw ff Ifilwiilt AND ALLIED ORGANISMS, Photographed from the Oriyinal Drawiiii/s hij Mrs. Bury. 12 Photographed quarto Plates, Containing 72 Figures ; with descriptive references to the Works of Professors Johannes Miiller, Ehrenberg, &c. PRICE ONE GUINEA. %n ©geKO ESK! Dr. DAVY, F.R.S, &c. CHR. JOHNSON, Esq. Dr. WALLICH. MISS HUTTON. MISS COOKSON. Mr. HEWSON. MISS MARRIOTT. Dr. GREVILLE, F.K.S., P.L.S., &c. H. C. SORBY, Esq., F.R.S., &c. JOSEPH JORDAN, Esq., PROFESSOR W. C. WILLIAMSON, P.R.S., &c. JOHN MARRIOTT, Esq., PROFESSOR ALLMAN, F.R.S.E., &c. May he had of Mrs. BUBY, Croft Lodge, Windermere; or of Mr. J. QABNETT, Photographer and Publisher, ^c., Windermere. /^./^ ^^^^^UU^ ^^ ' L POLYCYSTINS. PREFACE "But WHA.T ARE PoLYCYSTiNS " is the constant exclamation. — So little is yet known of these curious organisms that Naturalists have not yet decided on their exact place. They belong however, to the sub-kingdom "Protozoa," and Mr. Reay Greene in his "Manual" places them between " Rhizopoda " (of which the type is Amoeba, so commonly found in fresh water as little gelatinous lumps, of the very lowest form of animal life) and Sponges, which form flinty interior skeletons, called Spicules, to support the Spongiose web, and the animal mass of jelly, called Sarcode, with which they are invested. The Fohjcystias are also masses of Sarcode, but they appear to form both internal spicular-like supports radiating from the Nucleus, and also external shells of a network of flint, through the insterstices of which they are said to protrude Pseudopodian threads (perhaps analogous to the Tentacles of Sea-anemones and Star-fishes or arms of Hydra) by means of which they are supposed to imbibe noiu'ishment, and to have some powers of locomotion. A careful observation of the larv4l changes of the Echinoderms, and the Pupae states of other young things, can make one understand how the protean forms of the Polycystins need not all designate distinct species, but that many grotesque diff'erences of shape, and of spinous ornamentation may, in reality belong to the same object, in different stages or under different circumstances of development, such as more or less pressure, abundance or scarcity qf the siliceous material in the surrounding water, &c. Perhaps there may be said to be four classes of form : — 1st., the discoidal or planorbian flattened spheres, variously winged or bordered ; 2nd., the Orbicular, with or without spines ; 3rd., the vase or bellshaped, consisting often of repeated globes growing out of each other, sometimes with a re- duplication of parts, that might seem to indicate a tendency towards increase by fission ; 4ith., the plane or straight-sided forms. Dr. Wallich promises a full history of the structure and mode of development of Polycystins in his forthcoming work, having obtained living specimens in his recent deep-sea soundings : some in association with those wondrous benighted star-fishes from two miles deep. Professor Johannes Miiller fished them up frequently in the Mediterranean, near Cette and St. Tropez; always from great depths, and under very clear pure sea water, but from their great delicacy it was most difficult to obtain really Uving subjects, as even tbe passing through the water, in hauling up the ajiparatus used in dredging them caused death, and when that occurred the Pseudopodia immediately collapsed, the Sarcode substance became flaccid, and little more of the vital economy of the organisms could be observed. The late Professor W. J . Bailey also records some specimens as occurring among his deep-sea soundings in the Sea of Kamschatka; he speaks of their "organic contents" but does not state whether obtained in a living state. In the stomachs of the Salpse, which form so large a portion of the food of the whales, shoals of Polycystins are found, which have in their turn served as food to the Salpte. In a fossil state Polycystins have been found in many parts of the world ; those figured in the accompanying Monograph, are from a sort of chalky earth found in various localities in Barbados, where Sir Robert Schomburgk describes it as having been forced up by volcanic action, through the coral reefs of which the island is formed, from the deep bottom of some ancient ocean, where countless ages ago they may have enjoyed their gift of the power of abstracting pure Silex from the water, and, while in a plastic state, weaving it into their elegant glass corselets, — then laying down their skeletons to form part of that incalculably vast bed of Ocean-deposits, of which some infinitesimally small fraction occasionally comes under the microscopic ken of Man, — to shew us how the minutest and humblest atoms have yet their allotted part in fulfilling the Laws of the Great Creator. Professor Ehrenberg, in a discourse delivered before the Berlin Hoyal Academy of Sciences, says, speaking of these fossils from the rocks of Barbados (which he calls Siliceous PohjgasfricaJ " for these organisms constitute part of a chain which, though in the individual link it be microscopic, yet in the mass is a mighty one, connecting the Life-phenomena of distant ages of the earth, and proving that the dawn of organic nature co-existent with us, reaches farther back in the history of the earth than had hitherto been suspected. The microscopic organisms are very inferior in individual energy to lions and elephants, but in their united influences they are far more important than all these animals." Professor Owen (in his "Palaeontology," I860,) further remarks "if it be ever permitted to man to penetrate the mystery which enshrouds the origin of organic force in the wide-spread mud beds of fresh and salt waters, it will be, most probably, by experiment and observation on the atoms which manifest the simplest conditions of Life." Ch-oft Lodge, January, 18G2. BUIIY'S FIGURES OF POLYCYSTIN^. PLATE I. riG. 1 & 6. — Varieties of Eucyrtidium Acuminatum of Ehren- berg. 5. — Podooyrtis Schombuvgkii. Ehrenberg. 2, 3, 4. — Varieties of the same. 4.— 5.— 6.— PLATE II. ■ Stylodictya Gracilis. Ehrenberg- ■ A Dictyospiris (?) of Ehrenberg, highly developed in in slide Zjg Cambridge, Barbados. ■ Dictyospiris (?) or perhaps Petalospiris (?) May they not possibly be the same organisms in different states of development ? Ceratospiris, Mikrogeologie, PI. XXII, fig. 37, also resembles these shapes which occur in great variety in the Barbados deposits. Ehabdolithes Pipa. spiued stem var. Ehrenberg places Rhabdolithes in the family of Geolithen. Stephanolithes Nodosa. ; also a Geolithen of Ehrenberg. Acanthodesmia of J. Miillcr (Mittelmeeres, p. 30) Ste- phanolithes Spinesoens (?) of Ehrenberg. It occurs in double and single circlets, and with varying num- ber of spines in the Barbados deposits. 2.— 3.- 4. PLATE III. A Polycystinous nucleus, with one spine running through it, and attached at each end to a plain circle of Silex. — (In shde B. VI. Cambridge, Barbados) Lithocircus, Mesocena (?) A similar nucleus with four Acanthometrum shaped spines (see Miiller's Mittelmeeres, &c., PI. X.) attached to it, the hooks of which describe part of a circle. Actiniscus (?) in slide T. Cambridge, Barbado.i. A Hyaline wand, spirally twisted. Rhabdolithes Pipa. var. Ehrenberg. 1.- 2_. 3. 4.- 5. 6. PLATE IV. • Stephanastrum. Ehrenberg. • Astromma Aristoteles. Ehrenberg. ■ Stylosphiera. Ehrenberg. -Haliomma with four spines. - Lychnocaniuni falciferum. Ehrenberg. ■ Stylosphsera var. (?) with outer web (?) PLATE V. ■ Astromma (?) finely developed with part of outer web adhering between the arms. - Eucyrtidium Mongolfieri. Ehrenberg. 3. — Podocyrtis Mitra. Ehrenberg. 4. — A state of Rhopalocanium (?) 5. — Ptcrocodon Campana. Ehrenberg. 6. — an Astromma partially developed (?) PLATE VI. 1, 2, 3, 4, 5.— Rhopalocanium Ornatum in dift'erent states. 6.— Spicule of (?) PLATE VII. 1 & 2.— Surirella (?) from Cambridge, Barbados. Fig. 1 pos- sibly a young, less developed, form of fig. 2. The slide from which the fig. 2 was drawn was returned to Mr. Johnson, and by him sent to Mr. Ralfs, Pro- fessor W. C. Williamson saw it when in Mrs. Bury's hands (October, 1860), and kindly suggested it might possibly be a Surirella. 3 & 4.— Varieties of Dictyospiris (?) Ehrenberg. 5.— Actiniscus (?) of Ehrenberg and Pritchard ; a triangular net, like a Dictyocha, but with a " solid centre," which centre (or nucleus) gives the idea of being capable of stretching up into a Podooyrtis-like form ; sides of triangle measure .006.5 ; there are nine outer and six inner cells, arranged round a solid-lobed and punc- tured nucleus, which bears one long and two short spines. 6:— A Desmidia-like, but silicious, clear, transparent plate, with waved edges, and a perforated centre. Appears to resemble, in some degree, Lithodesmium undulatum, of Ehrenberg's " Kreidebildung," page 76. Dr. Wallich suggested (from sketch) that it might be a part only of some polycystinous form. 7. — The upper part like Ehrenberg's Podocyrtis Cothurnata, but with a tubulous prolongation of the base. 1,2, PLATE VIII. 3^ & 4. — Varieties of Haliomma. Haliomma Hum- boldtii (?) of Ehrenberg, from Cambridge, Barbados, numerous and variable. Although there are some- times indications of spines radiating from the centre, as in Stylodictya, yet the points round the edge appear to be merely "marginal appendages." — Dia- meters, including spines, from .0077 to .0085. 6. — Muller describes these as stages of growth of the Haliomma, where the outer web is spinning itself over and round the central nucleus, and the siliceous rafters or supports extending like a framework from the nucleus to the exterior covering. Page 21 ';' " Thalassicollen Polycystinen, &c., des Mittelmeeres." & 8. — Spines or Spicules in Barbados deposit. 5, & PLATE IX. riG. 1. — Petalospiris foveolata — var. Elir., Mikrogeologie, Taf. XXXVI, 14. .0075 high, spines included, .0031 did. of ball. 2. — The same without the central spike through it. 3. — A Podocyrtis (?) of Ehreuberg. 4. — A Podocyrtis (?) nearly akin to podocyrtis jEgles. Mik. Taf. XXXV. B. 18.; measures .0106 high, .0052 broad. 5. — A Podocyrtis (?) without the usual surmounting spine. 6. — A Litliomelissa (?) These beautiful little shapes, like crystal tea-pots, or coffee-pots, for some primeval world's Queen Mah, are frequent in the Barbado.s deposit. PLATE X. 1. — Triiusparent cross, with tubular canals running through the arms and united by a central ring, — a structure resembling an object figured in Professor J. W. Bailey's " Microscopic forms in the Sea of Kamschatka," under the name " Spongolitbes orthogona," but which he says he has referred with some hesitation to Spongo- litliis. Measures .01125 high, .008 broad, with a slightly warted or rugose surface. 2.— An Eucy rtidiun form bearing tubular spinous projections, arranged in the pattern of the perforations in Eucyr- ti'Jiuiii elegans ; appears to be enclosed in a transparent egg-shaped sheath or envelope, .00362 long — Litho- botrys adspersa, Ehr. Mik. Taf. XXXVI, fig. 5, has the appearance of a wing or fin extending round the object in a somewhat similar way, and so has Carpo- canium Solitarium, Taf. XXII, fig. 28. This specimen is in Slide No Gi? Springfield, Barbados. 3. — Eucyrtidium (?) elegans, in an unconstrioted state, .604 long, .0012 broad ; 23 rows of nearly equi-distant perforations ; from Chimborazo, Barbados. 4. — A Podocyrtis (?) Mitra or Papalis, var, (?) the lower part devoid of perforations, and with a thickening of the Silex round the boundary of the plain part, — two spines from the apex. 5. — Podocyrtis Papalis, Ehr. Mik. XXXVI, 23, .00687 high, .00375 broad. In numerous specimens the outline of the base varies considerably, but there always appears to be an internal ring or ledge. PLATE XI. 1. — A magnificent Polycystin, from Cambridge, Barbados. It measures .0214 in height, viz., the ball .0028, and .0186 from the ball to the base, where several more squares appear to have been broken off, — about 18 to 20 rows of squares, like windows ; inside soine of them a very fine internal network is seen ; through others appear a fiiint reflection of the bars on the opposite side of the object : the effect of this, viewed in the Binocular (half-inch objective) , is very striking. 2. — Eucyrtidium Tubulous, Ehr., measures .01 feet long, .0028 broad, from Peak of Tcneriffe, Barbados. Quar- ter-inch objective. 3. — Stylosphsera (?) Ehr., measures .01 high, curiously beset with sharp, spear-like spines, and covered apparently with pointed knobs or warts. Some of the Barbados Polyeystins suggest an idea as if their perforations either may have been, or might have become occupied by these sort of projections, which, when broken off, leave holes, and being hollow, would still permit the protrusion of the so-called Pseudopo- dian threads, which Professor J. Miiller says " one may conjecture (Termuthcn) " to be the means by which the Polyeystins imbibe nourisliment, although their connexion with the Sareode substance of the bodies, requires more clear elucidation. In the Thallassicollen and Polycystena, they can only be traced as far as the skin-like Capsule of the flabby part lying under the flint corselet. 4. — Dictyospiris (?) probably the same object as fig. 2, on plate II ; turned on the reverse side. Ehrenberg calls this " Ruckseite," and the other with the larger openings, " Mouthside ; " from Cambridge, Barbados. 5.— Spongolithis Acicularis, Mik. Taf., XXXVI, fig. 47, a Phvtolitharien of Ehrenberg. 6.— Amphidiscus Verticillatus, Mik. Taf., XXXVI, fig. 45, classed by Ehrenberg as " Phytolitharia," — of plant growth. PLATE XII. 1. — A spinous variety of Eucyrtidium Ampullus, (?) the narrow end prolonged into a tuliulous siiine, — diam. of bulb, .00275. Chimborazo, Barbados. 2.— Podocyrtis(?) wliole height, .0112; breadth, 0055; height of cupola, .0027. Professor J. Midler says, " in all the flask and bell-shaped Polyeystins, the first joint (glied) of the reticulation begins from the top, and the number of the increasing links progresses with growth in a definite ratio." The links of the lower part in this fossil skeleton seem running into each other irregularly, like dropped stitches in a stocking, or bursting bubbles in a gelatinous film while solid- 3. — A further variation of Podocyrtis Schomburgkii, as shewn on plate I, fig. 3. 4.— A modification of fig. 2, on plate I. 4 & 6. — Tlie reticulations progressing further towards the " Ladder" or Lattice-shape. In fig. 6, the inner net is very plainly seen, its reticulations are also square, with quarter-inch objective magnifying power used, about 470 linear. Springfield, Barbados. In another slide is a broken-oft' top of one of these Ladder- Pyramids, with the narrow neck sv^elling out into the surmounting ball nucleus (?) WlNDEEMiRE : fBINIED BY JOHK GABNETT. PLATE 1. PLATE 2. PLATE 3. MCZ i,iA UliA PLATE 4. PLATE 5. PLATE 6. C." PLATE 7. Vf^ wAn'"J'"'-'"-^^c Mfi. USA ««A1«S- PLATE 8. ua:^'--'^ u .-1 1 ' >- ■ ..TY S^RID&E. MA USA PLATE 9. PLATE 10. PLATE U. ©AMS-^^DGE. MA U-SA PLATE 12. ki-SA ^