ve eS 4 aR TEMES SRSA ene ya oo in a athe Pea skal eee yd 2) HARVARD UNIVERSITY. LIBRARY OF THE MUSEUM OF COMPARATIVE ZOOLOGY. ‘as buchos. Seem ber tf, 1895 Abruary 19,1896. PRA SACTIONS OF THE ROYAL SOCIETY of SOUTH AUSTRALIA. VOL. XIX., for 1894-95. [With Ten Puatszs. | INCLUDING PROCEEDINGS AND REPORTS. EDITED BY PROFESSOR RALPH TATE. $$$ - ISSUED DECEMBER, 1895. bas Adelaide: W. €. RIGBY, 74, KING “WILLIAM STREET. Fd Parcels for transmission to the Royal Society of South Australia, from Europe and America, should be addressed ‘per W. C. Rigby, care Messrs. Thos. Meadows & Co., 35, Milk Street, Cheapside, London,” Ropal Society of South Mustravia. > ae Patron: HER MAJESTY THE QUEEN. EC OE ee [Elected October 1, 1895.] President : WALTER HOWCHIN, F.G.S. Vice-Dresidents : REV. THOS. BLACKBURN, B.A. PROFESSOR R. TATE (Representative Governor). Bon, Treasurer: WALTER RUTT, C.E. Gon, Pecretarics: W. L. CLELAND, M.B. | W. B. POOLE. atlembers of Gouncil: SAMUEL DIXON. PROFESSOR E. H. RENNIE WALTER HOWCHIN, F.G.S. D.Se., FG J. S. LLOYD. W. H. SELWAY, Jon. E. C. STIRLING, M.D., M.A., C.M.G., F.B.S. © ONE aN Tea. PART I. (Issued July, 1895.) PAGE. Parknovse, T. A.: Native See in the Be arounaee’ of Port Darwin 1 freuen, J. G. O.: ve or Little. caeee Orthopters edt tee Callabonna , , 19 GoypDER, G. A.: Batons of ips Craiae Beane upon i Cyanide-process for Gold-extraction : ie igo) BLACKBURN, Rev. T.: Description of New Gace and Species of Australian Coleoptera (X VII.) ? Pager 7! Howcuin, W.: New Facts pearing on the Glacial Reaiiees of Hallett’s Gore oe y, Ea null MouLpeEN, J. C.: Petrographical loncereatons on some South Aus- tralian Rocks ? 70 Tare,2PRor. R.: A SD dniomicne? to a eaters of tie mig: ct Beta tropical South Australia 79 Verco, Dr. J. C.: Descriptions of New Specie a Maeaas iraindes of South Australia (Plates 1-3) : 84 Verco, Dr. J. C.: A Revision of the Recent Gasteropods of ae ' Australia (i. ) 94 Tate, Pror. R., and ae ANT, ah neat of the irate Ter- tiaries of Australia, Part II., Victoria (continued ) 108 PART II. (Issued December, 1895.) DauL, Knut: Treatment after Circumcision in the pay River Tribe, Northern Territory . . 122 SLOANE, THomas G.: Notes on “Cambide ion, Tate pane eee Central Australia ... 124 ETHERIDGE, R., JUN. : Additional Plant Rane from be Leigh Creek Coalfield, Central Australia (Plates 4-6) 138 Treprer, J. G. O.: Notes on Victorian and other Blattavi ea Descriptions of New Species : : 146 SmitTH, Dr. G. ELiior: The oonmnaatiee eistoray of the one tin of Notoryctes typhlops (Plates 7-9) : : ve LGT Howcurs, Waurer: Carboniferous Foraminifera of Weston Aus- tralia, with Descriptions of New Species (Plate 10) coum, LE Howcuin, WALTER: Two New Species of Cretaceous Foraminifera (Plate 10, pars.) ae 198 BLACKBURN, Rev. T.: Description of New Gane and Species of Australian Coleoptera (XVIII. ) * ; 201 1V. PAGE. Abstract of Proceedings . es pe aed ... 259 Annual Report and Balance- sheek oe a re ... 264 Presidential Address... si oe _ a: sad 206 Donations to the Library =e 4 ard 2 Sa IO List of Fellows ae a a se - na )2e80 APPENDICES. Proceedings, Annual Report, and Balance-sheet of the Field Natura- lists’ Section rae 289 Proceedings, Annual tec ae an Balance- avout of atts Astronomia Section... : » ie gee Proceedings, Annual Report sind Palance ated of the Malacologieen Section... es ve ots ee .. 294 REMARKS ON THE NATIVE TONGUES IN THE NEIGHBORHOOD OF PORT DARWIN. By T. A. Parkuouse, formerly Accountant and Paymaster 8.A’ Railways, Port Darwin. [Read November 6, 1894. ] The aborigines in whose country Port Darwin is situate are the Larraki‘a, of whom Mr. Paul Foelsche has given some interesting particulars in a previous paper.* They inhabit a tract of land embracing the seaboard from Shoal Bay to South- port, together with some portion of the country west of that port. At the forty-six mile on the railway line we pass their southern border, and going through a neutral belt of some eight or ten miles, strictly preserved and upon which none trespass without good reason, at near Rum Jungle enter into the terri- tory of the Awarra, whose southern boundary is the Howley. At about Fountain Head commences the country of the Aggra- kundi, extending to the Union and perhaps to near Pine Creek. Beyond Pine Creek to the Katharine are the Addéwen (?) and Mennagi (?). To the east of the Larraki‘a, from Marrakai cattle station on the Adelaide River to Shoal Bay and thence along the seaboard to beyond Escape Cliffs, are the Wulnar ; and east of these again and abutting on the Agegrakundi are the Mary River (! Berigurruk) and Alligator River tribes, the country of the latter extending south as far as the Eveleen. These districts are subdivided among the several families of the tribes. I am of opinion that each family has its own proper name, but I have no evidence that this is the case; nor do I find totems, or that there is any restriction as to food. The laws governing marriage, too, remain to be discovered ; I have little information except that in certain instances, where the indi- viduals were pointed out, a would have been the wife of 6 had a been born a girl, or 6 the wife of c were 6 female . Nimm ngullak—‘‘ Here, boy ;” Néggarik mannagwa—‘ He will come on by-and- Boy you come. T'o you come on by-and-bye. bye.” 6. Argwigam néggellippmerk kwondallippmérk—‘‘ When do you return? These are When you come back ? These fellows are come back. come back.” 7. Adnlamille neggojakk—‘‘ Which way will he come ?” What name come? 8. Dallippmenérk dallipbing — ‘‘ They have come back, and then cleared out They have come back ; they are come out. (broken up camp).” 9, Jeinaminbira barakerk—‘‘ A Chinaman is coming ;” Aragwa barakerk bilira—‘* Which Chinaman coming. Where coming blackfellows ? way are blackfellows coming?” Biramm barakerk—‘“‘ All of them are coming on.” All about coming on. 10. Also, leaning against, as placing a ladder ; thus, gudlamarami is to stand one thing against another, or as one resting his back against a post; Biddla darwin-ng‘idung Him hit, head hide gomulwa gud‘arging—‘ He hit him on his buttocks, his head going down,” making the buttocks come down. figure 4 ‘‘ gud.” cook it, gogérapp, gawapp; I have | crooked, gurnamading-a cooked it, ananng-a gurbaoni _ ery—lI, he, al-, bil--lum; crying bit- copulation, beddijim; he, thisfellow, _ terly, gwilageru billum dual copulate or purpose, be- cut, a, makkamille ngida, kwin-ngida, mogodijji _ cuts (cicatrices), mammétma cough, mamanndillima Dark, dlamaongwa; too dark, ku- country, béinigerrkgwa minngoemilli cousin (?actual kinship), némabor daughter, allmerk; daughter’s hus- band, noaddjak day, to-day, now, illangwa cover me over, menéitchura crocodile, ann-gallaba 1. Arip gogomille—‘ How far do I cut (into a water-melon) ?” Into this fellow cut. dead, baotokk deaf (‘‘no more him hear”), kwaella b‘uéllyidong devil, birauel die (see ill)—I, he will, they, a-, bo-, da- -linnyi difficult (see strong), dankal dirty, gomuntchula dog, little, b‘illimnga; big, mamorol; wild (dingo), bannaminngora door, mialdama dream, gulwao niyani drink? (see eat), gogwe duck, black, kuriminnbirra Ear, banarro eat,® gdgwe, gomogwe; eating—dual are, they are, minnyi, danyl; eaten—he has, thisfellow has, they have, bid-, gar-, dad- -bienni edge (of a knife—see teeth), dlenn- bérrgkwe | egg, gwidammgwa elbow, borumba embrace (short quick hugs), boganar empty, kw‘aotidong; make empty, dakw ‘aot emu, langwirra enough, banuk excrement, munmar eye, lemurra eyelash, madobirma Face, darreminndbirra fallen—thou, he, this fellow has, + no-, ber-, go- -addbing father, nigan; child addressing, naggeding ;> my father, nigann- birra; father’s brother, bipi fight—lI, he, a-, bér- -ramelliddyim find it, genyurup; found (see catch), gare finger, gw‘larrwoa finished, banuk gwilling fire, gwianngwoa; fire gone out, gwiawinng firesticks to produce fire, bollbilli; to use them, willam gillam fish, muddowa flesh, biddloa food, mauma, meiyoma fool, you, and other terms of vitu- peration, dinndidani, dinndaijik, diamy ‘udaijik 2. Kwarrowa mogwe— This fellow wants a drink of water ;” also, Golmorra gwinnyi— Water eat. ‘© Will this fellow drink his grog?” Grog sit dow. 3. Banana mogwe—‘‘ May I eat the bananas?” Bréddema daddbienni—‘‘They have Banana eat. eaten my bread.” Bread they have eaten. 4, Agoldum addbing—‘‘I ran and fell;” Nogoldum noaddbing—‘‘ You ran and fell ;” Ivan from fallen. You Bilajz He has gone, him fallen. hit and has fallen.” beraddbing—‘‘ He has gone and has fallen ;” Biddla ran from fallen. bérraddbing—“‘ He is Him hit, him fallen. 5. Term of endearment, as when an English child throws its arms around its father’s neck, and says, ‘‘ My daddy.” fool, to, z.e., you fool me, noligum; you lie to me, gonélum gwinnyir- am foot, gwiéllkwa footprint, biralpbirra forehead, mudpirrma forget—l, dual, al-, mu- -lerrinn-ga ; I forgot,! kwaélla birw‘a four, gallatillik anndillik fresh (water), kuntltoa frightened, be‘udkhyéllming frog, kulpulwa from, -um . “No more catch him.” 2. Donoerkwi ngigari—‘‘ Go on further.” Further you go. 3. Kwarroa garri—‘‘ Get water.” Water cateh. 4, Kwarrowa an-ngok—‘‘ Give me water ;” An-ngagok Water give. have tobacco given me;” It‘uma an-ngok You givetome I. full (from eating), néddlabokk, yunutpi further,? donoerkwi - Get up—you, he, ngi-, bi- -gidjyi; you are getting up (see stand), neggogiddyi get it, néggildum; I have not got it or brought it (see catch),*® kwaella gaora girl, big, baon-ngugolo ; little, baon- ngilla give to me, to him, an-, bin- -ngok; you give,* nagok tobakkwa—‘‘I am about to Me about to be given tobacco. ana—‘‘ You give yours for mine.’ 10 given to me, you, dual, him—about ( greedy, minnovzel to be, an-, na-, minn-, b‘u- -ngagok | ground, gwialwa give, I will not, barbium growl, to (see adulterer), alennjia, go—I, you, he, a-, ngi-, bi- -gari; allennjiak dual,* mogwiri; this fellow go, | Hair of head, br‘iridlwirra; of face, not to return, goaribing kwiabalma; of body, m‘auerma; going or coming,® néggarikk of abdomen, g‘dulma gone—he, they have, bi-, da- -laji; | half, kwéawirra he has been gone,’ barabilaji hand, gw‘iarrwirra go back—I, you, he, a-, ni-, bi- | hasten, gwillipbikk -géllibum he, she, it, him, her, yaha; his, hers, go round (also turn, as a doorknob), biannage; himself, &c., bimilla gwindari head,* malloma good, padj‘i; very good, patch‘i- | hear—l, he, al-, ba- -leitong milla ; goodbye, mamdok heavy,® m‘tutki goose, bonnamorra; pigmy goose, | here, yenn, yénngwa lidinnda hill, little, gumardéka gulla; big, grass, small, meriedlema; tall, mdot- gologo gwillaga dlema 5. Anannga it‘uma mogwiri—“‘I and you go ;” Ngigari mogwiri—“‘ You go firs‘, we two you. two go. You go, two go. go after ;” Agari bigiddjya bigari—‘‘I will go, let him get up and go away ;” ananng-a I go, him get up, him go. agari m‘ulitudma mulerippma; agari agalimbgwa——‘‘ May I go to the little house, for T go little little house; Igo I urinate. micturition?” Ngigari big‘umm—‘ Go quickly.” Zou go, it is being said. 6. Néggarikk mannagwa—‘‘ He (who has fallen behind) will come on by-and-bye ;” You go towards by-and-bye. Aragwa néggarikk—‘‘ Where are you going?” Adnlamilla Mdell négzarikk—‘‘ Where is Where you go? What name Maell go. Maell going (having departed)?” 7. Dallippbing dalaji—‘‘ They have cleared out, and gone away;” Gallatillikk maram4- They are come out, they are gone. Two two rillikk—‘‘Two have gone away ;” Dagarillikk daragwilling—‘ All have gone away to- have gone. They are gone, they have been entirely. gether ;” Aragwa moléji—‘‘ Which way did we two go?” Arakwa bilaji bilira— Where two gone? Where him gone blackfellows ? ‘* Which way have the blackfellows gone?” 8. Malloma gwillika—‘‘ A big head.” Head big. 9. M‘utma m‘ulit‘udma—“ A little heavy. Heavy little. ~ hit, shot (see stop), biddla I, me, ananng-a; belongs to me, hold him, duppinnyer anagi; myself, anang-amilla horse, nanntoa iguana, kurara hot—I, you, it is, 4-, né-, bér- -rak- | ill, hurt, dying, allinyima; I, you wirra he, they are, a-, ne-, bo-, da- -linyi how much, argugwinnikk inside—you put, this fellow put, house, small, méneliirra, m‘tileribb- no-, go- -gaodta ma; large, kwonaminngwoa; hut | intestines, namannamanerk or wurley, maldurébbma Jabiru bird, daolduba hungry, amunnding, nigar amimnd- | jump on back, baramunnyin lng Kangaroo, l‘un-ngutpa hurt, are you (see ill), nelinnikk; | kills, hurts, wounds — he, this have I hurt you, nawaum fellow, they,” bi-, go-, da- -gilla husband, naow‘a knife, maramari 1. Place in a room or put yourself inside, as, Trautherwa nogoadta—‘‘ Put on your trousers.” Trousers you put inside. 2. Bigilla nimmgololo—‘‘ He is beating the lad ;” Larraba bigilla—‘‘ He has wounded the He kills big boy. Old man he kills. old man.” know, I (see hear), alleitong; I do not know (see see), banbaoning, banmaoning Laugh—I, you, this fellow, they, a-, nel-, gwial-, dal- -lamaoggi; a big mocking laugh,* bokkung gwillagi laughing-jackass bird, l‘anurba lazy,* mumo-ing leg, daonda let me, him (allow), an-, bin- -ngolda lie down, I, anannga nakkgaert liar, kwinnyiram lift it, biddbiddla ; lift this fellow (see stand), g‘ogiddla light of day, lallirirkgwa; of fire, bokulktji; light it,®* bokwinnida lightning, leaurba like, relish, bidjalippmerk; distaste- ful, dukkwa like, affection (see hear), b‘udbaléit- maong; I like you, you like me, al-, nel- -leitmung like, similar, nogzvum listen, inna little, m‘ilit‘il, mtlage, m ‘iilitudma; little fellow,, gumilla lives, he, bimedip lizard, small light, kumungwa ; small darker, lurabella; frill, dad- dlwirra long ago, kwillimigérrgwa, ? allok- wa, ? aragwegum long way, a, dirriwa look out! (see see), gwin-ganna louse, lamilla Make, modlum; this fellow make it, gaodlum; I can make it,’ ana maotbudbing; make it right or proper, *® agg‘aganmidjing 3. Analla gwiallamuggi—‘‘ What do you laugh for?” What for laugh. 4, Illangwa mumo-ing—‘‘ Heis too lazy now.” Now lazy. 5, Erribokwa an-ngok---‘‘Give me a light. Light give me. > 6. Nimmbirra m‘ulit‘idma—‘“ Very little children.” Children small. 7. Kappbirra bimédlum-—‘‘Is he to make me a cap Cap him make. 8. Trautherwa ag‘agannmidjing—‘‘ Make my trousers waist). Trousers me make right. mankind, biaba, birok man, young, ballia; married, mdl- linyu; old, larriba many, binndlka, birammbirra; many people, kwarrabarokk marks, I make, méndirramuggi mate, addressed as, midir moon, laurua more, do some (see another), gal- lagwa mosquito, lamtda mother, algan; my mother, algan- birra; addressed by son, kwoding; by daughter, nemabirra; mother’s brother, tnyi mouth, gwearbaulkwoa, gwerba move farther away, yutkwa, ytit- keri Nail of finger and toe, daalla name, neana 1. Neana adnlamilla—‘t What is your name?” It‘uma Name what is itself ? boy called ? 9 7? right” (tighten them at the native-companion bird, doluba near, ‘ipporo neck, gumudaopgwa night, dark, dlamaongwa no, no more, not any, kwaeélla no (do not want it), kwiaok nose, kwiangwa nosepin, dlemélwira now (to-day), illangwa One, kallaguk open, tdadtman opossum, kw‘aotkita orphan, fatherless, baonari; mother- less, mundalling; either addressed as, bombilla ours, dorennage outside,* nakk, nakkjin Pairs, to place in, kwimitlik palm, an edible, kwillimmba parrot, blue mountain, willrilma enama name néddle — ‘‘ What is your “ou your boy. 2, Tdadman nakkuk mialdama—‘ Open the door ;” Lemurra dadman—“ Look.” Open outside 3. Balallwilwa The middle one throw it away. door. Eye open. winnulma-—‘* Throw it outside ? 12 perhaps, g‘ogndogh plenty, gotuk, baratuk, mamdia pick it up,+ morenjim pregnant, méloa pinch, aragiki _pud. hominis, dubirra, dorkh‘ing ; play, gulamuggi, ilomai, gulomai ; mulieris, dinnda children’s games, as, hide-and- | pull off (see throw),* winntlla seek, agarut; hide, whistle, and | put it down—TI have, anam ‘ai; this spy, dadwiln‘idung; hold with fellow has, gug‘ai; put it up hands and with legs round waist there, gwidjinidaong and fall back, dredbingmung; | put on (see inside),® g‘idta pushing oneanother over, daminaji Quickly, hasten, kwillipbik 4, Arenji ,bigar—‘‘I pick up (the ball) and catch it.” Lpickup him catch. 5. Trauthera winnuulla ‘‘ Pull off my trousers.” Trousers pull off. 6. Aragwa nog‘tidjo— Which way do I put iton?’ Ngigari buminnyi—“‘ You go and Which way you put on? You go him sit down. put it away. quiver, of the limbs in the corrob- | see, baoning, mamann, bannaning, borie, mutmir mamanning; seen him, binnging; Rain, baolmba I have seen,*® 4ragobéoning ready, are you, barabiddji sharp, as scissors, birtinnki ribs, marulma short-fellow—he, this fellow is, bin-, ride, bibiddmi gon- -nopollera river, kwi‘aliggwa | shoulder, daraminndillera; shoulder- rock to and fro, as a baby to sleep, blade, minnikillma sugumedla show me, you, naégalitda run, muddli; towards me, from me, | shut, méittnamilli nogold- -erk, -um; dual run, | sick, vomit, kumenan mogoldariji | silent, be, gaop ; silence ! (emphatic), Say—I, you, he, a-, ne-, bi- -g‘im; | kapp nig‘am* to him, to this fellow, bi-, go- | sinew, vein, déonera -nimbirra; he has said, barag‘tim; | sing, culwagemullam he said, bog‘um; he is, two are | sister, elder, dnmerk ; younger, talking, bin-, man- -g‘fam; a | nullw‘ok general talk,? gégog‘imbirra sit—you, he, dual, ne-, bi-, mo- scratch, mutterum -gw‘inyi; he is, they are sitting, ° sea (?), kunimiddyénderroa bén-, den- -yin season, the wet, gwondreawang sleep—you, he, no-, ber- -ramedjin; 1. Nogoldogol—‘‘ You run there and run back ;” Nakkjin ndgoldo—“‘ Run outsid.e.” Outside you run. 2. “No,” nég‘um binimmbirra neg‘innyi—‘‘ Say ‘No,’ and tell him to sit down ;” No yousay him tell you sit down. Beritt bog‘um—‘‘ He says ‘ Turn.’” ‘Turn,’ he says. 3. Kwaélla baona—‘‘I do not see it ;’ Anyédlde magaono—‘‘Let me see, too Anydlde No more see. Let me dual see Let me bigwaoning—‘‘ Let me have it to see ;’ Anyold gogwaono—“ Let this fellow see ;” Baoning see it. Let me this Fellow see. See mondlkoa—‘‘I see them all about (I see a big mob) ;” Nemang-wa magaono—‘*A revoir ;” all about. To-morrow two see. Arbirra binnging—‘‘ Who sawhim ” Anall 4nnyam—‘‘ What do you look at me for?” Who him saw? What see? Angwaon gwérrip—‘ I fear to see him (the superstition ‘ evil eye ’—‘ him frightened Eyes’ See this fellow into. was the interpretation given me).” 4. ‘* You say a silence.” 5. Gwan mog‘innyi and Gwinn mogw‘inndi—“ Let us two sit here ;” It‘uma anang-a There two sit. Here two sit. You mogwandi—‘ Will you and I live here?” Aragwa nenani—‘‘ Where do you reside?” two sit down. Where you sit down ? 13 you, he has been asleep,® nora-, ban- -medjini slowly, go, manoi smoke, a, kwiigwa; a big smoke, meréidlya; to make asmoke, b‘ud- awillawaéollam smoking, bongbong ; égoma snake, black, daarla; brown, lemir- dla; yellow, lamalla; spotted, kwarilla; a small, kwiungulloa ; a dreaded poisonous, méromor- ludyi © to smoke,’ son, némérk ; son’s son, nédlyo sores, gubengoa spear, Jag, mallag‘irm4; jagged both sides, ménauilidma; stone, dau- inga; reed with point, lierba ; reed without point, g‘wirinnda or griinnda spirit, ghost, portrait, darabdllera spittle, bilirema; I must spit, mera- minnma; to spit phlegm, tokh neg‘am 6. Agol médjim —‘‘T shall go to sleep quickly ;” Nogol medji and Ngigari nogol médji— Irun_ sleep. You run sleep. “ou go you run sleep. “*Go to sleep ;” Mogwiri medjim—‘‘ We two go to sleep ;” Aolmédjimuk—‘‘ I am sleepy ;” Twogo sleep. Alladika belaji berramédjim—‘ He is goin Wife him gone, him sleep. —‘* Where will you sleep ?” I sleep towards. g to live at home for awhile ;” Aragwa medjia here sleep 7. An-ngok gogoma-—.‘‘ Give me a smoke (from your pipe).” Me give smoke. stand, you, negiddyi; standing up,! | kolknari | star, mamudlema steal, guullibik stone, damilla stop—I, you, a-, ne- -g‘do; you, he stay,*?neddh, biddli; leave off (see enough), banuk stretch oneself (see ill), allinnying ; to stretch one’s leg, dh‘uethth‘uel strong, hard, difficult, dankal ; strong fellow, gwillagowang; make it strong, negodpingi | sun, lallirra sweat, kwillikerra sweet, dadbon swim, walaragum | Take it, you, nagukka; he, this | } fellow take it, bin-, go- -nukka; take out,® magdlla, gomodlla, bodlla (or boara, goara) tea, yabarak tears, guloa teeth,* dlenb‘érkgwe tell them—TI do not want to (see say), baragummugegi testicles, gwiyuwunngwa thank you, monkdini that one, yedbirra that side or that way®, yagolak, yagolagwa there,® yagwa, yagbirra, yenn this fellow, amilla this one,’ gwinnbirra this side or this way, * gwinn. gwaonika 1. Kolk agar giddyi—‘‘I stand up ;” Kolk ngigar giddyi—* You stand up.” Um Loo lift. Up you go lift. 2, Neg‘ao—‘‘ Stop (walking or other action) ;” Adnla néddle ngigari—‘‘ Why do yo What you stay? you go. stay there? Be off ;’ Arak biddle—‘‘ Where did it (the ball) stop ?” Where him stay ? 3. Banjollop and millbollom gollop—‘‘ He does not want to take him;” Trautherwa Trousers gogwolla—‘‘ May I take off my trousers?” B‘utpolla padj‘i—‘‘I will take up a good one ;” this fellow take away. Goara This fellow taken, it is gone. it out to throw away.” Him take good. bilaji—‘‘ He has taken it ;”’ Nakk bimukk binnulla—“‘ He has taken Outside him take, him throw away. 4. Dienb‘érrginum allinnyam—‘‘ Toothache.” Tooth all. 5. Yakk golaji—‘‘ This fellow has gone that way ;”’ Gwan That way this yellow has gone. way.” 6. Yan nelaji—‘‘ Have you been there?” There you gone. mogwiri—‘‘ We two go that That way two 40. 7. Gwinnbirra gwinnbirra gwinnbirra gwinn—“ This one, &c., this ” (enumerating). 8. Gwinn This way this fellow gone. long side (of the table).” golaji—‘*‘ Go this way, eh? (having turned off) ;” Gwinn gwillakwa— This This way big. 14 thigh, mukka | tickle, bérribiddbirra thou, it‘uma, adama?® tired, annélling; a cry of weariness three, gallatillik kallaguk or pain, arrgai... throat, mangolma _ to-day, illang-wa ; to - morrow, throwing-stick for spear, bildta; | nemang-wa; day after to-morrow, for reed spear, billilma | nemann kallaguk throw it away, agaribob, binntilma; toe, kwiéllgwa throw it, this fellow away, bo-, go- | together (see pair, to), millik -ara; I have thrown this fellow, tongue, kwiaméddloa both away,!° go-, muo- -lomang _ too,® garra thunder, molne; thunderstorm, bierrdwa 9. The softer intonation, ‘‘adama,” is heard in tones of tenderness, as a boy being with another whom he is loth to leave says ‘‘I go,” adding ‘‘adama garra” (you too), wistful that his mate should accompany him. 10. It‘uma binntlma—“ You throw it away.” You him throw. truly, gaodloa whistle, you,® will nég’um, willwill turn it, beritt nog‘um, willwill rogum two, gallatillik white, clean, arkhngarr Up, above, on top, kolkoa whitefellow, arkhngarramilla urinate—I, you, agga-,noar--limmb- who, which one, arbirra; whose, gwa _ arbidénnagi Vent, gum‘ulwa; from it tobladder | why for, why not,°® ‘arbiddla (see carry), biattbirra _ widow, widower, bénnbirria Wait, I, adelaong wife, alladik wake him—yon, negillmi _ wind, minmtnma wash myself, bathe, aramannbitt- wish, want, amalla jium; I wash myself, you yourself, | womankind, muellabirra ara-, ndlo- -mannbiddji; I wash woman, with children, btnbena ; the clothes,” gugumanndub old, g‘umul water,® kwaorrowa work, I’ (see make), agg‘aganmidji wax, in ear, bonorroa wrist, mobirma we, dorendbirra; dual, moanmi//a write (see marks), méndirramuggi what, analla; what name,+ adnla- Yam, pulida milla | yes, I assent, g‘ogogwe, g‘o when, ‘argwigam yesterday, kwodlaogwa where, which way, aragwa | you, (s7g.) it‘ima ; yours, itennage 1. Beritt nogo‘itji beritt n‘egum—‘‘ Turn to the right, turn to the left ;’ Beriddma nongya ? Turn ? right, turn ? left. Turn 2 —‘ Turn over ;” Berittbing gogomang—‘‘ Turn, smoke (reference to forming camp).” 2. Ngigdri nolomannbiddji, gallagewirra gungwa biginnyi platbine gomanndop You go, you wash yourself, another fellow here him sit down plates wash. Lemdlagwa bigdri optigkwa beggaganmiddji—‘‘ You go and wash yourself, the other Lemalagwa himgo ogice him make proper. fellow stay here and wash the plates; Lemalagwa will go to the office and work.” 3. Kunult gdri gwdrroa—‘‘ Fetch cold water ;” Kwaorroa gwilla bidding—‘‘ The water Fresh catch water Water all fall down. has all leaked away ;” Korroa gwaélla negwilling—‘ You have drunk all the water.’ Water no more entirely 4. * Whatisit? WhatdoIdo?” Analla ngigdri—‘‘ What am I to fetch : What for you go ? 5, ** Whistle, you say.” Will barag‘um—‘‘ Somebody whistled. A whistle has been said Arbiddla beg‘ao—‘‘ Why does he not stop ?” Why for stop ¢ fon 15 WULNAR. Most of the words known to me are included in the vocabu- laries compiled by Mr. W. O. Be are therefore not reproduced here. Afternoon, meliter animal, momulydéner Bag, owel big, miyangyer bird, loaga breast, Woman’s, gumunnya brother, younger, uita; nullar; my, nulladbunna Cold, oppogwi cough, mamurrda Dark, dlamungwar day, irning-a Enough, biléiya Fight, wauikattpi finger, téliamunger fire you light, leitonga b‘ukonwa Give me, gunmitja good, nodla Hair of head, lerrmalner; of face, yaber hand, mani husband, lainelonggunya Ill, angeaga insect, moromora elder, AWAR Alligator, bira ankle, ann-gro, annmo ant, little common, bim; yellow, woallum ; red, bom arm, ann-goronng armlet, dAaman Bad, allwarra bandicoot, yok basket, dul before, bulgmarra; you go on before, yaggma bellajin behind—come on, lura kolajin belly, anndoyi belongs to old man, agallawo datt- ulla belt, darabert birth-delivery, bin-ginyan blackfellows, nalmok blood, kuraj bone, annmau boy, little, allil; addressed as, warraba ; big, auwirra breast, woman’s (also milk), d‘utut brother, my, boppa Calf of leg, annbuin 1. Moann yann—‘‘ You come on.” nnett and Mr. A. J. Todd, and Mankind, kumaol _ many, miapunger milk, ngoiyer Navel, lemala No, kwoddlégo; I do not want, litter Open the door, daddmanakwa mo- gwianagwa Pelican, yuropiter pud. hominis, mung-ai Run to me, mokwel; from me, mur- biokwel Silence, you say a, kupp ninnmi sister, younger (see brother), uita ; elder, nelami smoke, lenlatimima stopped, he has, witjunga Thigh, wondga throw it away, linnannmittiger tired, innmdkattaz: tongue, wliyer Wake him, lemorr womankind, mungedmitta RA club, sharp-edged, warawara; blunt, dukkara cold, allal come—you, yann; ye,! biann cough, gulaba crocodile, maimakko cuts (cicatrices), darawumerring Dead, bajum dog, little, ng‘iri Ear, ann-gonnem elbow, annkénmo emu, morin empty, made, addwilling enough, amoge excrement, gudma eye, anndum;_ eyebrow, monndi Father, bibi find it, wado gunya; I have found it, Addnai fire, verk firesticks to produce fire, gwélgma to use them, vagmo food, moiya fool, to, minwalgwinn apndu- foot, ann-goba ; footprint, annborra forehead, annwalma frog, jakkun Girl, baby, allmarramaring; crawl- ing, albupaddma; little, pfotatta give me,” bano go, ya; he has gone, kaiinnye goodbye, mamok good, ammokwao gum, ironbark, yilyil Hair of head, mida, annmar; of face, kéttawerk; of abdomen, tolmida hand, annabi head, annbon hill, giri hungry, uyung* I, me, naak Jabiru, gw‘ael jaw, anndomkok Kangaroo, kupu Lips, tnnduli lizard, kinnimbullo Man, young, dulrgwin; married, bumbiligo ; old, dattpulla micturition, waol moon, karrong mosquito, nael mother, warra; my mother, bulbil Name, what, yemin-gi navel, annlannjérruk no, wado, waggi; not yet, mutto- waggi; no more, amalla nose, annji Opossum, uoda Pregnant, moleru pud. hominis, unnleng, benning ; mulieris, ual 2. Wik bano—‘‘ Give me water.” 1. Lukluk bian—‘‘ Come on, quick.” lannku- 16 2. Wik bilaggin—‘‘ Throw away the water.” AGGRAKUNDI. Arm, ajinn armlet, mamal Bad, yoyo bag, dul belly, margill blood, gulminn boy, baby, innbarro ; little, ambut ; addressed as, tumbitimbi; big, darraggit breast, woman’s (a/so milk), ying brother, boppa bush, the, bunndi Calf of leg, ann-gorro come—you, yann; ye, biann cousin, hawong Quick, hasten, lukluk Shoulder, annmonukk sit, pfaddminninni ; dual sit, gallem galboninni sleep, maiyuol; I want to sleep, maio m‘ai‘i smoke, to, dibbomélwon, dubbomi snake, bellum ; water, gunda; brown, baonobaon sore, bigmi spear, boko, kowonéro; jag, toltol ; jag two sides, méddoballi ; stone. lauk ; reed, darin sun, miral swim, marrimmar Talk, mattgo-inge; tell him, kaji, kaji jai teeth, aliddma testicles, annmueth _ thigh, 4nndarato, annmullok throw it away, laggin; thrown away,” addlaggin throwing-stick, don ; for reed spear, girikk thunder, kéddaduvidma; thunder- storm, duridmin tomahawk, dodol tongue, unnjenn Walk, main; you and I, geironga main water, wik; drink, wik mabel way, that, inndubba what, Abo-in where, umbulla bajim woman, old, imbillalgo ; young, ad- dressed as, allamanduba Yes, yo you (sig.), moann crocodile, genult cry, ra-i cuts (cicatrices), biling Dead, nulgmeung dog, yiri Ear (also toe), adalpi empty, unwilleing eye, mibull eyebrow, marluk Father, awarrago firesticks, to produce fire, gibei food, moiyi foot, amul Girl, anmodalpa ; baby, immalwulk give me, anmo; I give, bano go, yak goodbye, ! mamaok Hair of head, mannmar; of face, keddoark hand, annmoa, abill head, immbun hill, garaui house, small, maiwa I, me, arraman Jaw, adamkill Kangaroo, taning Laugh, gommenn-gommenn; dual, mogabbinn; they, mugga-mug- gamminn lizard, small light, mungbéllma ; small dark, bonjimm Man, young, deinmulva moon, kommil mosquito, kimmiel mother, innarrago mouth, unnyulk Name, naban no, kwaella, wagge nose, agginngelk ; nosepeg, gegung One, udérinn Opossum, dinng-a Plenty, wiomopo pud. hominis, darr, abigelloduk Quick, warri;{come on quickly, allauklauk bian Run to me, marimari Shoulder, abelma sister, mulginn sit, anninni; you sit, méan anninni; dual, manninni sleep, aréiyi, maiyi smoke, I, amitubbimi snake, grass, bann; water, mdbal- lago spear, stone, konddébum; reed, ldimo stop, daonok sun, mawarrik swim, marbirrami Teeth, aiimmerrikk testicles, taiimmell thigh, abell throwing-stick for reed spear, dirik toe (also ear), adalpe Walk,? yiark water, yik way, a long, malwalk what, abbon You (sing.), moan 1. Mamok yawarra—‘‘ Good-bye, I shall come back.” 2. Warri (or waggi) arra yiark—‘‘ I do not want to walk more.” NATIVES OF THE KATHARINE. (Contributed by Mr. E. J. Kemp, of Glenelg). Alligator, dagul All right, Iam, laguit ant, common, cheak; white, karab- lungul apron, man’s _ fringe, woman’s, ungoruk arm, murnuk armlet, willa Back, the, ngolo bag, dilly, miyauk bamboo trumpet, kurnbug bandicoot, yawk barramundi fish, mardbing beard, ngaruk belly, ngoldag; full, wei; empty, gugmarin belt, braak billabong, nglanga blind, tumea blood, kurak bone, unmoa boy, little, megulgul breast, woman’s (a/so milk), gawn brother, unbuba B jolgon ; Camp, numbura catfish, chalo cockatoo, white, ngaruk; blaek, karuk ; tail feathers of black, didjualla come back, goyai crow, yi cry, dollumun Daybreak, ungulara dog, wild (dingo), waruk duck, tilbiuk Kye, undum Father, tchardba fire, wuruk fish, mardigal fly, house, morok foot, undjora Girl, little, ulwan go quickly, ngorra-ngorra go, you, ungan; you and I, negan- neuilo good, nglagamura good-bye, munjungala ground, hard, bawl gumma-gumma hair, bamjuruk hand, barak head, mengalap how are you, ngulawil yigina Jabiru, paundoru Kangaroo, kupu knee, umbart Laugh, yeaumun leg, ungarra leave it, ponga lip, ngalk lizard, yang Man, kingulpoya; old (also woman), tholba-tholba mine, nagulung; this belongs to me, ngagulu warre mosquito, beundo mopoke bird, gogulporuk mountain range, baran ngire moon, deat mother, karung Nails, unbillum night, gullaruk nose, gamul; nose stick, maruk Opossum, wirik Quail, jirik Rain, waak river, unboa, ngugmari Sandfly, ngala sick, I am very, kulwutma sister, dinda smoke, undumugma spear, bogo stone, paat sun, giguil swordfish, chulwul Teeth, nglaidmor tomahawk, mardi tree, laianth turkey, beinuk What is that, guliana whistle, wirdmun woman, old (see man), tholba-tholba Ly, DESCRIPTIONS OF NEW OR LITTLE - KNOWN SPECIES OF BLATTARILZ, GRYLLACRIDA, AND STENOPELMATIDZ COLLECTED AT LAKE CALLABONNA, S.A. By J. G..O. TEepeer, 2-E:8. [Read November 6, 1894. ] The various forms of Orthopterous insects which form the subject of these notes were collected by Mr. A. Zietz during the latter half of 1893, at Lake Callabonna, as bye-work whilst engaged there in the exhumation of Diprotodon and other fossil remains. The specimens referred to form part of the entomologi- cal collection in the South Australian Museum. SECTION BLATTARIA. FAMILY PHYLLODROMIDi. PHYLLODROMIA MAGNA, spec. nov. Ochreous testaceous ; head only slightly prominent, face with a broad blackish band between the bases of the eyes; antenne blackish, basal joints pale ; pronotum slightly wider than long, emarginate in front, with two broad straight black stripes, wider behind (not curved), space between them of the same color as the margins and the elytra; elytra concolorous (wings not observed), veins dark, branches parallel, only divergent at the base; legs pale, concolorous; abdomen above banded with black, ventral seg- ments each with an intramarginal black spot; cerci blackish, banded pale; subgenital lamina broad, rotundate, with a short dark oblique streak on each side, and a blackish dot near the apex. Female. Length of body ... ne i. ee ie lainey Length of elytra bie ae Peis PAN oi Length of pronotum _... oe: ag toner Width of pronotum ... s Setar: ia The single specimen obtained appears to resemble P. Ger- manica, L., but is much larger, the pronotum less transverse, the black stripes of unequal width, and the anterior margin distinctly emarginate ; whilst the branches of the radial vein of the elytra only diverge at the base, being otherwise parallel throughout. 20 The abdomen also is differently marked. This species appears to be the largest hitherto described. PARATEMNOPTERYX ZIETZII, spec. nov. Brown to blackish, paler below, shining; head free, an ill- defined, narrow, curved black bar between the eyes ; ocelliform spots obsolete ; clypeus pale, basal area of the antennz whitish, latter very slender, as long as the body, pale brown. Pronotum elliptical, margins very narrow, disk more or less distinctly exca- vated, anlges rounded, hindmargin straight. Elytra nearly quadrangular veins distinct, raised, scarcely exceeding the first abdominal segment. Wings rudimentary. Legs uniformly pale brown, fore femora crowdedly spinose, all more or less ciliate (tarsi without arolia). Abdomen with dorsal segments finely scabrous along the hind margins, angles not produced, except those of last segment. Ventral segments brown to _ black, shining. Supra-anal lamina longer than wide, subtrigonal, posterior third incurved, apex rounded. Cerci very long, acute. Subgenital lamina very large, cucullate, hindmargin entire, bearing the short, suberect styles; latter black above, pale beneath. Adult males. Male and female larve. Length of body ... 18 -19 mm. 13-15 mm. Length of elytra... 4-5 « — Length of pronotum 4:5- 4:8 “ 3-3°5 ‘ Width of pronotum 6 — 6:5“ 4-5“ There are two full-grown males and three larve, one of them apparently a female. The species is distinguished from P. aus- trale, Sauss., by its larger size, absence of ocelliform spots, much shorter elytra, and the peculiar form of its anal appendages. The larve are much darker, inclining to black. The vertex of the head is paler than the very dark face. FAMILY PERISPHAERID AL. LEPIDOPHORA, gen. nov. Resembling Perisphaeria glomeris, Sauss., in aspect. Body convex, elongate, stout. Anterior angles of dorsal segments pro- duced laterally as a subtrigonal scale overlapping imbricately the respective ventral segments at their base. Supra-anal lamina quadrate, posterior angles produced as short spines. Subgenital lamina subtrigonal, apex produced, forming two conspicuously diverging spines. Styles slender, as long or longer than the lamina. The scale-like appendages along the lateral ventral margin, to which the name refers, are apparently a novel character among 21 the Blattariz, as I have hitherto not observed it myself, and I am unacquainted with any reference thereto either by description or figure in the literature available. Similarly the form assumed by the subgenital lamina is quite unusual. These features justify therefore, I think, the establishment of a new genus for the species, which for the present at least is located among the Peri- spheeridee, to which in general aspect it appears to fit best, but it may require, when better known, to be removed elsewhere. LEPIDOPHORA FURCATA, spec. nov. Black, finely rugulose, wingless. Body much curved. Head concealed, glossy ; vertex and face reddish-piceous ; sides, fore- margin of clypeus, and trophi pale testaceous. Antenne much shorter than the pronotum, slender, reddish. Eyes irregularly reniform or wedge-shaped. Pronotum elliptical, margin narrow, not much reflexed, laterally incrassated, less so in front, arched ; hindmargin concave, angles subacute. Meso- and metanotum similar. Abdomen dorsally almost smooth, hindmargin of seg- ments with minute raised points, straight, rectangular laterally, angles of the seventh segment produced as a short red spine; beneath piceous laterally, disk reddish, penultimate ventral seg- ment narrow, reddish. Legs rather short; internal spines of fore femora short, crowded, very numerous, external ones longer, few, and distant. Coxe pale testaceous, base piceous, remainder reddish. Tarsi long, beneath dilated, whitish. Supra-anal lamina with hindmargin ciliate, pale reddish. Cerci lanceolate acute, longer than the lamina, dark red. Styles reddish. Male. Length of body... sli ape ey 2 Ts Length of pronotum ... ds Sans On Ota us Width of pronotum _... = aes Ss A single male was obtained, but I have since got another from elsewhere. The specific name refers to the peculiar form of the supra-anal appendage. SECTION LOCUSTODEA. FAMILY GRYLLACRID. EONIUS CALLABONNENSIS, spec. nov. Resembling £#. tigrinus, mihi (Trans. Roy. Soc. S.A., XV., 163), paler. Vertex and front of the head pale, clouded darker ; apex of mandibles obliquely truncate, toothed, deep black. Pro- notum with the fore and hindmargin each slightly marked with a blackish band, longer than in the allied species. Elytra ovate, slightly extending beyond the hindmargin of the meta- 22 notum, veins distinct. Wing-lobes rudimentary, concealed by the elytra. Hind femora with six pairs of small spines. Hind tibize with four to six external and six to eight internal spines, all black at the apex. Femora near apex, and all the tibie and tarsi, hirsute, like Z. tigrinus (omitted to state in monograph). Ovipositor very slender and long, nearly straight, acute, apex black. Female. Length of body ... ue ... 396 —37 mm. Length of elytra... fe s3¢.60) BO Oe Length of pronotum ae 4) = Se Length of hind femora... a. LD Oe Length of ovipositor $e .. 43 -48 « The two specimens obtained differ principally from #. tigrinus (independently of color and size) in the black, toothed apex of the mandibles, almost concolorous pronotum, much longer elytra, different arrangement and size of spines, and the more slender ovipositor; from Z. atrofrons and EL. fumatus in much larger size, pale head, and number, &c., of spines. The ova were extracted from both the specimens, and proved to be nearly mature, in the one more so than in the other. One yielded 47, the other 24, a small proportion were only about half-grown. The mature ones were brown, elongate elliptical, 5-5-5 mm. in length, somewhat thicker on one end than the other, each terminating with a circular, smooth, shining, darker lid, the intermediate portion being ornamented with crowded microscopical papilla, arranged in regular diagonals. The small, immature (or male ?) ova are almost cylindrical. Eontus aTrorrons, Tepper (Trans. Roy. Soc. 8.A., XV., p. 164). Two specimens were secured, viz., a nearly mature male nymph (the first example of this sex for the genus) and a female larva. As the species was originally established from a singie female, these not only confirm its validity, but the former supple- ments the generic description, hence a full description becomes necessary. Male (nymph) similar to female, but considerably smaller. Abdominal segments 8 and 9 almost concolorous ; hindmargin of the latter straight, angles lobe-like produced. Supra-anal lamina transverse, divided by four furrows into five unequal parts, the central sulcus produced posteriorly as a dilated rotund- ate lobe, and longer than the basal part. Cerci very short, apex blackish. Subgenital lamina small, subquadrangular, rather longer than wide, simple. Styles minute. Male. Fem. larva. Length of body --2) 2135 mm. 18 mm. Length of pronotum ... 4 “ ori Length of elytra soe) ale, Lae PRES) ah Length of hind femora 10 “* Sk The black face is so conspicuously characteristic of the species that it scarcely can be mistaken for any other yet known. The ovipositor of the female larva is scarcely conspicuous. FAMILY STENOPELMATIDZ. PENTHOPLOPHORA DRIFFIELDI, Zepper (Trans. Roy. Soc. 8.A., XV tp. LES): Of this species fifteen specimens were obtained, viz., six adult and four larval males, and one adult and four larval females, the larvee representing various ages, the youngest being only 9 mm. in length, while the oldest is almost full grown, but presents the ovipositor still in its recurved position, and much abbreviated. This being the first instance of males having been secured, the description is added. Male. Similar to female, somewhat smaller, paler, and the markings less defined. Abdomen with the eighth segment cucullate, hindmargin sinuate, angles and middle slightly pro- duced, rotundate, concave parts with numerous, minute, dark- brown toothlets; the ninth segment only exposed posteriorly, contracted, trigonal, apex broadly rotundate, disk on each side with a conical protuberance surrounded by a depression, its apex formed by a small, blackish, outwardly curved acute spine, from which extends laterally a short blackish ridge. Cerci short, slender, hirsute, pale. Last ventral segment of abdomen trans- verse, hind margin very sinuate, middle much produced with two short, thick, obtuse, blackish spines near apex. Styles short, glabrous, apex blackish. Adult. Larve. Length of body (Male) 30-40 mm. 9 -26 mm. Length of pronotum... 5-6 “« 15-4 * Width of pronotum ... 8-9 «* Zia al Oe oe The considerable difference in length is most probably largely due to unequal contraction after death while immersed in alcohol, through which also the color has been considerably aftected. The dark bands are caused by a pigment, so loosely deposited upon the thin translucent integument, that it becomes detached when one attempts to remove the intestines, no matter how care- fully. This may serve asa hint for recipients of spirit specimens, or fresh ones as well, who may attempt the operation. If the specimens have been preserved in weak spirit, I find it best to 24 immerse them in strong spirit for a sufficient time to harden them; then mount quickly, as most of them when drying rapidly retain their shapes fairly well. These insects, as stated by Mr. A. Zietz, inhabit (singly) bur- rows excavated by themselves in sandy parts of the lake basin. They are perfectly circular in form, about three-quarters of an inch in diameter, twelve to eighteen inches deep, and at the bot- tom somewhat dilated so as to allow the inhabitant to turn round easily. Where the sand is dry, 7.¢e., the upper part of the shaft, the grains on its surface are securely fixed by some cement. Around the mouth a mound, an inch or more, raises the entrance by so much above the general surface, and is sloping outwardly. The pellets of excavated soil are carried by the insect toa dis- tance of six to nine inches from the entrance, and disposed there in a regular circle. When a grass stalk is first pushed into the hole, the insect comes up to ascertain the cause of disturbance, and then withdraws, and will not come up again. When dug out, they refuse to fly from their foe, but will resolutely face him, whatever way he turn, standing on the defensive, and move rather towards him than otherwise. bo Or ON SOME IMPORTANT REACTIONS OF DOUBLE CYANIDES BEARING UPON THE CYANIDE PROCESS FOR THE EXTRACTION OF GOLD. By G. A. GoyDEr. [Read December 3, 1894. While endeavoring to find an accurate process for the quanti- tative determination of simple cyanide of potassium in solutions containing also double cyanides, such as the sump liquors obtain- ing in the McArthur-Forrest process for extracting gold, I found that cyanide of potassium was alkaline to phenol phthalein, and that the quantity of alkaline cyanide present could be accurately determined, in the absence of caustic alkalies and alkaline car- bonates, by titrating with acid, using phenol phthalein as indicator. The presence of bicarbonates makes the end reaction more uncertain, but by adopting special precautions accurate results may still be obtained. The double salt zinc potassium cyanide is quite neutral to phenol phthalein. I am further investigating this reaction with the object mentioned above. It appears to be generally believed that such double salts as zinc potassium cyanide in aqueous solution have no solvent action on gold. JI have, however, found by experiment that this double cyanide readily dissolves gold, although the action is slower than that of the simple alkaline cyanides. When a solution of zinc potassium cyanide is shaken with gold-leaf in the presence of oxygen, or air, the gold is dissolved, forming gold potassium cyanide, while zinc is deposited as oxide. A secondary reaction also takes place, involving the formation of the auricyanides of zine and of potassium, the former of which appears to be in- soluble, and of zincate of potash. Copper potassium cyanide also dissolves gold, although the action is still slower than that of the zine double salt. It is hardly necessary to point out that the above reactions may be of considerable importance in the McArthur-Forrest process. In order to determine the total cyanogen in sump liquors I have devised the following modification of Rose & Finkener’s process :—A measured quantity of the liquor is heated on the water bath, or gently boiled, for 20 minutes with excess of oxide of mercury with occasional agitation, filtered and washed. To the filtrate about one gram. of caustic soda is added and excess 26 of sulphuretted hydrogen water to precipitate the mercury. After being well shaken, filtration not being necessary at this point, excess of carbonate of bismuth is added to precipitate the residual sulphuretted hydrogen, well shaken, filtered and washed, and the filtrate titrated with silver nitrate after the addition of a little potassium iodide to sharpen the end reaction which is indicated by a faint permanent opalescence. One molecule of silver nitrate used indicates two molecules of cyanogen present. bo ~J FURTHER NOTES ON AUSTRALIAN COLEOPTERA, WITH DESCRIPTIONS OF NEW GENERA AND SPECIES, By the Rev. T. Buacksury, B.A. [Read April 8, 1895.] OVAL. CARABID. An important and very able memoir by Mr. T. G. Sloane on Australian Carabide appears in the recently published Part (IIL, 1895) of the Proceedings of the Linnean Society of New South Wales. Some of Mr. Sloane’s proposals—e.g., the merging of the Morionides and Trigonotomides in the Feroniides, and of Notonomus and Sarticus in Pterostichus,* while Coxandrus Prosopogmus, &c., are treated as genera—certainly appears to me on first thoughts open to much objection; neither can I acquiesce in Mr. Sloane’s apparent reluctance to regard sexual characters as of classiticatory value (illustrated by his uniting WVurus and Homalosoma on the ground that they do not seem to differ except in respect of sexual tarsal characters). As however the memoir was published in Sydney only a week ago, I have not had time to do more than hastily run my eyes over it and am not justified in seriously criticising it on the strength of so slight an acquaint- ance with its contents, nor should I have discussed it on this occasion if it had not been that Mr. Sloane refers here and there to what I have myself written concerning some Australian Carabide and in at least one instance seems to invite further information from me which this seems a good opportunity to furnish. In dealing with Leptopodus, Chaud., Mr. Sloane refers to my having expressed the opinion that it is scarcely distinct from Simodontus on the strength of its having been formed for the reception of Péerostichus holomelanus, Germ., but thinks that (although he agrees P. holomelanus is a Simodontus, yet) inas- much as M. Chaudoir attributed also other species to Leptopodus some of which stood in need of a new name holome/anus ought to be relegated to Simodontus and Leptopodus retained for other species. I think Mr. Sloane is right in this view of the matter. *T observe that in a footnote Mr. Sloane himself hesitates considerably on this point. 28 Mr. Sloane in a footnote states that Rhytisternus sulcatipes, Blackb., is &. levilaterus, Chaud. I cannot look upon this as more than a guess, inasmuch as M. Chaudoir never really de- scribed levilaterus but only indicated its differences from f. liopleura. Of course it may be sulcatipes but inasmuch as M. Chaudoir says that in levilatera the fifth elytral stria is “‘omnino obliterata,” while in swlcatipes that stria is perfectly traceable throughout the length of the elytra; and as moreover levilatera is said to be from Queensland while I have seen sulcatipes only from Southern Australia, I look upon the identity of the two as far from being established. Discussing the affinities of Cyclothorax Mr. Sloane expresses a doubt whether that genus can be placed in any of the recognised tribes of Carabide. I think however it may be placed in the tribe for which (Proc. L.S., N.S.W., 1892, p. 85) I proposed the name Ambiytelides. Mr. Sloane agrees that, as stated by me Tr. Roy. Soc., §.A., 1894, p. 203, Cyclothorax cinctipennis, Black.—C. (Phorticosomus / lateralis, Cast. Australian coleopterists owe a debt of gratitude to Mr. Sloane for such a memoir as this on which Iam commenting. I sincerely hope that he will be able by degrees to treat all the larger genera of Australian Carabide as he has now treated Homalosoma and Rhytisternus, and that in due course the tribes of Lebtides and Harpalides will be dealt with by him after the manner in which he has dealt with the Feroniides. TRECHUS. T. atriceps, Macl. In Proc. L.8., N.S.W., 1892, p. 97, I men- tioned having seen the type of this species at Sydney and noted that it seemed to be a Thenarotes. Recently Mr. Masters has been good enough to send me an example and [I find that my opinion was correct. It is very close to my Thenarotes discoidalis var. ? minor, but certainly distinct, being much smaller and having the basal part of its prothorax differently sculptured. In 7. atriceps there is a basal punctulate depression extending almost from the central channel to the lateral margin scarcely deepened into a fovea in the middle, while in 7. minor the punctulate space is a distinct (though not sharply defined) fovea separated from the central channel by a considerable unpunctured interval. GYRINIDA. DINEUTES. D. inflatus, sp. nov. Fem. Latissime ovatus ; supra obscure viridis, prothorace elytrisque sat longe intra marginem lateralem vitta sat lata obscure cupreo-aurea (hac postice 29 abbreviata) ornatis; subtus piceo-ferrugineus, pedibus anticis concoloribus, posterioribus 4 paullo dilutioribus; supra fere levis obsolete rugatus, rugis in capite prothoraceque confusis in elytris longitudinaliter dispositis, in elytrorum parte externa paullo magis distinctis substriiformibus; elytris in parte mediana magis quam latera versus convexis, parte cupreo-aurea leviter subimpressa, apicibus singulatim rotun- datis. Long., 6; lat., 4 1. (vix). Easily distinguishable from all the previously described Aus- tralian Gyrinide by its great width, its length being scarcely more than half again its breadth. Victoria. HY DROPHILIDE. PHILHYDRUS. P. eyrensis, sp. nov. Ovalis; nitidus ; piceo-niger, palpis anten- nis tibiis tarsis et capitis prothoracis elytrorumque margini- bus lateralibus rufis vel rufo-testaceis ; supra sat equaliter crebre sat fortiter (elytris quam caput prothoraxque paullo magis fortiter) punctulatus ; elytris puncturis nonnullis (his seriatim dispositis) vix majoribus impressis. Long., 23 1. ; lat., 141. This species is extremely like P. melanocephalus, Fab., and is probably the insect on the authority of which P. melanocephalus has been credited (I believe it is in Dejean’s Cat.) to Australia. But it differs from melanocephalus in its head not being impressed in front of the eyes, in the evidently less strong puncturation of its prothorax and in its palpi being scarcely infuscate at the extreme apex. Hyre’s Peninsula. HYDROCHUS. H. Palmerstoni, sp. nov. Minus elongatus ; sat nitidus ; viridis, elytris brunneis, cupreo-submicantibus ; antennis_ palpis pedibusque sordide testaceis, genubus infuscatis ; capite inter oculos longitudinaliter 3-sulcato; prothorace cordato sat crebre ruguloso-punctulato, indisco minus perspicue 3-areo- lato ; elytris seriatim punctulatis, puncturis basin versus sat parvis postice permagnis foveiformibus. Long., 13, L; lat., 2 1. A remarkable species on account of the peculiar sculpture of its elytra, the seriate punctures being in the basal one-fourth comparatively small and the interstices between the series con- tinuous and well defined, while before the middle the seriate punctures become extremely large round fovez of diameter greater than the width of a puncture and an interstice together in the 30 basal part so as to leave no continuous straight interstices be- tween the fovez. Near Palmerston, N. Terr. ; taken by Mr. Walker. BEROSUS. B. munitipennis, sp. nov. Ovalis; convexus; nitidus; supra pallide testaceus (exemplis nonnullis sparsim fusconotatis), capite prothoraceque rufescentibus ; subtus obscurus, anten- nis palpis pedibusque testaceis ; capite equali, fortiter crebre antice minus crebre) punctulato, prothorace transverso fere ut caput (sed minus crebre quam hujus pars postica) punctu- lato; elytris minus fortiter punctulato-striatis, ad apicem leviter emarginatis, parte emarginata extus ut spina gracilis perlonga producta, interstitiis planis sparsim sat fortiter punctulatis. Long., 241.; lat., 141. Allied to b. externe-spinosus, Fairm., but ditfering from that species, as described, by the much coarser puncturation of its head, its entirely testaceous legs, &c. ; differing from Queensland specimens in my collection (which I have no doubt are Faire- maire’s species) and from all the other described Australian Berosi, also by the very long slender spine into which the external apices of its elytra are produced. S. Australia; taken by Mr. Zietz near Lake Callabonna. NOTOBEROSUS (gen. nov. Hydrophilidarum ). Beroso affinis; differt antennis brevioribus specie 6-articulatis (articuli 3° 4"° que minutissimi cum 5° intime conjunguntur), hoc quam 6° multo latiori; mesosterno haud carinato. The insect for which I propose this name has very singular antenne. Examined under a Coddington lens they appear to consist of six joints, the basal two much like those of a Berosus, the third conical and at its apex much wider than any of the three joints which compose the club. Under a compound micro- scope however the basal part of this apparent third joint seems to consist of two minute joints intimately joimed to each other and the second of them to the large joint that follows. N. Zietzi, sp. nov. Ovalis; nitidus; glaber; supra albido- testaceus, clypeo capiteque in medio et postice plus minusve nigris vel obscure fuscis ; mesosterno metasterno et abdomine nigris ; antennarum clava vix infuscata ; capite prothorace- que (hoc transverso quali) subtiliter crebre punctulatis ; elytris nullo modo striatis, sparsim inzequaliter (hic illic sub- seriatim) punctulatis ; nonnullorum exemplorum (? marium) puncturis raris permagnis juxta suturam positis. Long., 13.1. + Jat. 21. The punctures of the elytra are of several different sizes con- dl fusedly and not closely intermingled; in some specimens (apparently, from the few examples taken, males) a few of these are much larger than the rest and are placed near the suture along its front half. In the male the hind margin of the penultimate ventral segment is widely and sinuously emarginate. S. Australia; taken by Mr. Zietz near Lake Callabonna. NITIDULIDAE. MACROURA. M. Baileyi, Blackb. In Trans. Roy. Soc. 8.A., 1894, p. 204, I stated that this species seemed to be identical with Carpophilus obscurus, Macl., on the authority of a specimen sent to me by Mr. Lea and compared by him with Macleay’s type. I much regret to find that this was an error. I have since received the same species from Mr. Masters as Witedula concolor, Macl., and on investigation I find that the latter name is right and that Mr. Lea’s label must have been a /apsus calami or by some over- sight have been attached to the wrong specimen. I therefore must withdraw my assertion regarding C. obscurus, Macl., and notify that it is Wetedula concolor, Macl., to which it applies. LAMELLICORNES. ONTHOPHAGUS. O. Leat, sp. nov. Robustus; piceus, antennis palpisque testaceis ; nonnullorum exemplorum pedibus rufescentibus; subtus rufo-hirsutus ; clypeo antice late rotundato ; capite creber- rime subtilius transversim, prothorace (hoc subcanaliculato) paullo minus crebre minus subtiliter longitudinaliter, rugu- loso; elytris modice striatis, striis vix manifeste punctulatis; interstitlis sat planis sparsim leviter nec subtiliter punctu- latis; tibiis anticis extus 4-dentatis (processu apicali incluso). Maris; capite postice lamina subtransversa erecta alta armato, hac ad apicem utrinque et in medio acute prominenti ; pro- thorace antice latissime perpendiculariter declivi, superficie perpendiculari areis 3 concavis constituta, supra aream per- pendicularem medianam prothoracis dorso ut lamina horizon- talis profunde bifida producto. Long., 8—91.; lat., 5—541. This fine species is in most respects very much like O. feroz, Har., but differs from it in the shape of the frontal horn of the male which is a transverse lamina (not much wider however than high), rugulose on its face and smooth on its hind surface, soutline (viewed from the front) forming three triangles one on each side with its apex directed outward and one on the top with its apex directed upward; the rugulosity of the prothorax 32 moreover is markedly finer and closer than in ferox and of con- spicuously longitudinal arrangement, the anterior projection of the prothorax is more flatly horizontal with its lobes non- divergent, &c., &c. N.S. Wales; taken near Forest Reefs by Mr. A. M. Lea. APHODIUS. A. callabonnensis, sp. nov. Minus convexus; sat nitidus; piceus vel nigro-piceus, prothoracis lateribus elytris (maculis nonnullis fuscis exceptis) pedibusque (presertim femoribus posterioribus) testaceis ; capite mutico, sparsim sat fortiter punctulato, clypeo antice sinuato-truncato; prothorace ad latera capillis elongatis fimbriato, postice haud marginato, lateribus modice arcuatis, angulis posticis obtusis ; scutello parvo sparsim punctulato; elytris subtiliter striatis, striis seriatim punctulatis, interstitiis suturali 3° 5° que fortiter convexis externis uniseriatim punctulatis; tibiis anticis extus bidentatis (dente apicali incluso); tibiis posticis setis inzequalibus instructis ; tarsorum posticorum articulo primo elongato (quam 2"* 3° que conjuncti paullo longiori), 2° quam 3" longiori. Maris prothorace subtiliter, feminz magis fortiter, sparsim punc- tulato. Long., 241; lat., 14.1. Allied to A. sws, Fab. The fuscous spots on the elytra are one on the fourth interstice immediately in front of the middle and several considerably behind the middle placed in a transverse line and more or less run together. Also resembles A. lindensis, Blackb., differing from it inter alia by its bidentate front tibie, clypeus truncate in front, sides of prothorax not emarginate be- hind, elytral costee more prominent. A. Candezer, Har., also seems (from description) to resemble the present species but belongs to a different section of the genus having its prothorax margined behind. Lake Callabonna ; taken by Mr. Zietz. ATZENIUS. A. Zietzi, sp. nov. Subovatus; nitidus; rufus vel piceo-rufus, nonnullorum exemplorum capite prothoraceque obscuriori- bus ; clypeo antice triangulariter emarginato; capite cras- sissime ruguloso; prothorace inzqualiter nec crebre sat grosse punctulato; elytris fortiter punctulato-striatis, in striis puncturis parvis minus perspicuis, interstitiis sat zequalibus leviter convexis (nullo modo cariniformibus), humeris dente minuto acuto armatis. Long., 2 1; lat., 41. Distinguished by its equal (inter se) and non-cariniform elytral interstices from A. australis, Hope and from all the Australian 33 Atenii that I have described except A. goyderensis (of the Horn expedition); the latter differs from it by its black color and much less coarsely punctulate prothorax. The species described by Sir W. Macleay as Ammuecii (some at least of which seem to be Atenii) all have either cariniform elytral interstices, or very deeply punctulate elytral striz or differ greatly in size from the present species, and are all from parts of Australia very far distant from Lake Callabonna. Lake Callabonna; taken by Mr. Zietz. TROX. T. Crotchi, Har. I have lately received an example from the collection of M. Thomson under this name, which agrees very well with Harold’s description and I have no doubt is correctly named. It is clearly identical with specimens from Central Aus- tralia which I had attributed to 7’. Crotchi and is very close to T. eremita, Blackb., but I think the latter is a good species, as it differs from the type of Crotchz in having the larger tubercles on its elytra less large and of more elongate form also more numerous than the corresponding tubercles in Crotchi and also differs in the external teeth of its front tibize considerably smaller and more obtuse. T. strzeleckensis, sp. nov. Sat late ovatus; opacus ; niger, indumento sordido vestitus; capite minus crebre nec rugulose punctulato, bituberculato ; clypeo antice fortiter angulato ; prothorace quam longiori fere duplo latiori, postice in medio fortiter lobato, ut caput punctulato, supra costis tuberculis- que nitidis sat angustis ineequali, lateribus sat fortiter trilo- batis, angulis posticis obtuse rectis; elytris seriebus 10 tuberculorum elongatorum (his costas fractas simulantibus) inter se equalibus insignibus, tuberculis majoribus vix elevatis nitidissimis per superficiem totam hic illic inter- mixtis, serierum interspatiis seriatim minute granulatis ; tibiis anticis extus dentibus 2 (mediano et apicali) permag- nis armatis ; prosterno postice vix prominulo. Long., 6—7 l.; lat., 4—42 1. The sculpture of the elytra is the strongly distinctive character of this species ; it consists of eight opaque rusty-looking carini- form lines on each elytron which are similar inter se except that the second and fourth are less broken near the base than the rest, each of which is broken into short pieces (about 15 in number), and besides which there are on each elytron a somewhat similar but less defined line close to the suture and two ill-defined ones between the eighth and the lateral margin, a number of scarcely elevated somewhat star-shaped nitid spaces scattered confusedly over the elytra, and a row of very minute granules between each Cc 34 two of the above mentioned broken carine. This insect is perhaps near to 7. Brucki, Har. (which is known to me only by description), but cannot be identical with it since Brucki ++ described “processu prosternali valde tumidulo” whereas the prosternal process of this species is as slightly developed as in any 7'’rox known to me; it is angular behind but scarcely pro- jects beyond the general contour of the prosternum. Lake Callabonna and Strzelecki Creek ; taken by Mr. Zietz. LIPARETRUS. L. distinctus, sp. nov. Sat nitidus ; supra fere glaber ; brunneo- testaceus, nonnullorum exemplorum capite subinfuscato ; hoe cum prothorace crebre subfortiter punctulato ; clypeo antice plus minusve fortiter tridentato vel trisinuato ; pro- thorace fortiter transverso, manifeste canaliculato, antice minus angustato, lateribus sat rotundatis; elytris sat fortiter geminato-striatis, interstitiis sat crebre sat fortiter punctu- latis; pygidio crebre fortiter punctulato; tibis anticis extus dentibus 2 (apicali incluso) elongatis acutis et alio parvo supra medium armatis ; tarsorum posticorum articulis basalibus 2 subeequalibus ; antennis 9-articulatis. Maris segmento 2° ventrali penicilla hirsuta perlonga postice in medio instructo ; femine mutico. Long., 33 1.; lat., 2.1 This is the only described species (of the section having the front of the clypeus tridentate) of uniform testaceous color. Lake Callabonna ; taken by Mr. Zietz. L. melanocephalus, sp. nov. Precedenti valde affinis ; capite, elytrorum basi summa, sternis, segmentis ventralibus (apicali excepto) et tibiis tarsisque posticis atris; tarsorum posticorum articulo 2° quam 1"* manifeste breviori; cetera ut preecedentis (L. distinctz). Maris segmentis ventralibus (apicali excepto) in medio penicilla transversa instructis ; femine muticis. Long., 3 1.; lat., 141. Lake Callabonna; taken by Mr. Zietz. L. aridus, sp. nov. Sat nitidus; supra fere glaber ; testaceus ; capite minus crebre minus subtiliter punctulato; clypeo antice subtruncato (maris quam femine minus late); pro- thorace fortiter transverso, sat sparsim sat subtiliter punc- tulato, haud canaliculato, antice minus angustato, lateribus angulisque posticis rotundatis; elytris leviter geminato- striatis, interstitiis leviter sat crebre punctulatis ; pygidio sparsim leviter (fere obsolete) punctulato; tibiis anticis extus dentibus 2 (apicali incluso) modicis et alio minuto supra medium armatis ; tarsis gracilibus, posticorum articulo 2° quam 1" manifeste longiori ; antennis 9-articulatis. 3d Maris quam femine statura magis angusta, antennarum flabello magis elongato. lLong., 3 1.; lat., 12—1,4 1. _At once distinguishable (in the group of Liparetri having the antenn 9-jointed, the clypeus more or less rounded or subtrun- cate in front, and the body glabrous, or nearly so, above) by its uniform pale testaceous color. The flabellum of the antenne is nearly white. Lake Callabonna ; taken by Mr. Zietz. COLPOCHILA. C. palpalis, sp. nov. Sat elongata; nitida; supra subglabra, prothorace et elytrorum basi capillis elongatis fimbriatis ; subtus (abdomine pygidioque capillis subtilibus erectis spar- sim vestitis exceptis) dense hirsuta ; albido-testacea, capite (hoc plus minusve infuscato) pedibusque (horum dentibus spinis et carinis plus minusve infuscatis) rufescentibus, pro- thorace pallide brunnescenti; capite fortiter sat crebre rugulose (clypeo, parte postica excepta, subtiliter nec rugu- lose), prothorace subtiliter sparsissime, elytris (his obsolete geminato-striatis) leviter vel vix manifeste, pygidio leviter sparsissime, punctulatis ; antennis 9-articulatis ; prothorace quam longiori fere duplo latiori, antice modice angustato, obsolete canaliculato, basi vix bisinuata, lateribus fortiter rotundatis, angulis anticis acutis posticis rotundatis ; ely- trorum apice haud producto. Maris antennarum flabello quam articuli precedentes 5 conjuncti sat longiori; palporum maxillarium articulo apicali dilatato, quam precedentes 2 conjuncti sat longiori; tibiis anticis (exempli typici) carentibus. Femine antennarum flabello quam articuli preecedentes 5 con- juncti vix longiori; palpis maxillariis normalibus; tibiis anticis extus fortiter 3-dentatis. Long., 10 1.; lat., 541. This insect is very remarkable by reason of the form of the palpi in the male, which are fully as long as the head, the apical joint being dilated and especially elongate; its form is curved and its upper surface is deeply bisulcate, the space between the sulci convex, presenting the appearance of the joint being a husk split open lengthways and revealing an enclosed kernel. It is unfortunate that the only male in the collection has lost its front legs as without examining those organs it seems just possible that the species ought to be regarded as an aberrant member of the Clavipalpides. Its simple claws, however, and mandibles of the Sericoid type point strongly to the probability that the front legs of the male are not of the Clavipalpid type. I have dis- ected a female and failed to find any character to distinguish it rom a female Colpochila, so I feel little doubt that the insect 36 belongs to the Serzcoides and can be separated from Colpochila only by the peculiar palpi of the male. Jt seems undesirable to omit describing this insect in spite of the imperfection of the male type, as it is from a remote inland locality whence more material cannot be expected at any early date ; nor does it seem practicable to found a new genus on it without examining an un- broken male. If the difference from Colpochila prove to be limited to that of the male palpi I doubt whether it can rightly be treated as generically distinct from Colpochila, and, for the present at any rate, it seems best to place it in that genus, of which it has entirely the facies. In my tabulation of Colpochila (Proc. L.8.N.S.W. 1890, pp. 520, &c.) it falls under “ EE” on p. 521, along with C. gigantea, Burm., from which it is very distinct by many characters—znter alia its nearly white color and the antennal flabellum of the male consisting of only three joints. The characters of the palpi in the male of course dis- tinguish it from all the other described species of the genus. Lake Callabonna ; taken by Mr. Zietz. CALLABONICA (gen. nov. /feteronycidarum). Mentum quadratum, tectiforme ; labrum (speciel typice) verti- cale supra clypeum sursum productum; antennz (speciei typice) 8-articulate, flabello 3-articulato, articulis brevibus ; alee obsolete ; cetera ut Heteronycis. It seems impossible to refer the species for which I propose this name to any hitherto characterised genus ; its appendiculate claws aborted wings (which are only about half as long as the elytra) and remarkable mentum taken together render it easy. of identification. The mentum is somewhat of the form known in geometry as a “triangular prism,” being formed of two plane surfaces meeting down the middle line and sloping down from the middle line on either side, the extreme front also being sloped (or obliquely truncate) and representing I presume. the ligula. Unfortunately there is not an example that can be devoted to dissection. The general appearance is that of a very short Heteronyx, with very convex elytra much rounded on their lateral outline. The genus is no doubt near Pseudoheteronyx but differs from it inter alia by the form of its mentum, by its wings not being altogether wanting, and by its longer metasternum (which however is somewhat shorter than in Heteronyx). It also bears some general resemblance to Byrrhomorpha from which however its appendiculate claws at once separate it. It is cer- tainly incapable of flight, and no doubt is found (like Pseudo- heteronyx) under stones. C. propria, sp. nov. Nitida; nigra, antennis palpisque testaceis, pedibus rufescentibus; capite equaliter confertim sat fortiter aii ruguloso, prothorace elytrisque grosse sat crebre sat equaliter (elytris quam prothorax paullo magis crebre), pygidio leviter squamose sat subtiliter, punctulatis ; corpore supra sparsim vix manifeste (capite magis crebre) fulvo-pubescenti, subtus pygidioque pilis erectis minus crebre vestitis ; clypeo antice late leviter emarginato; hunc labro superanti; prothorace quam longiori fere duplo latiori, antice vix angustato, angu- lis anticis acutis productis posticis obtusis, lateribus sat arcuatis; elytris haud striatis; coxis posticis metasterno longitudine sat quali; tibiis anticis extus fortiter acute tridentatis ; tarsorum posticorum articulo 2° quam 1"* duplo longiori. Long., 53 1.; lat., 3—34 1. I do not find any notable sexual difference, but the proportion- ally wider specimen is probably a female. Lake Callabonna; taken by Mr. Zietz. HETERONYX. H. suturalis, sp. nov. Modice elongatus, sat convexus ; postice vix dilatatus; sat nitidus; ferrugineus, elytrorum sutura infuscata ; subtiliter minus crebre pubescens ; capite grosse subcrebre (clypeo magis crebre), prothorace sat sparsim sat fortiter, elytris squamose subtilius sat crebre, pygidio leviter sat grosse, punctulatis ; clypeo antice late levitere marginato, ante oculos minus dilatato, sutura clypeali subtili fere recta ; prothorace quam longiori fere duabus partibus (postice quam antice dimidia parte) latiori, lateribus sat arcuatis, basi leviter bisinuata, angulis anticis sat acutis vix productis posticis rotundato-obtusis ; elytris haud striatis, transversim minus manifeste rugatis ; tibiis anticis extus dentibus 2 (apicali incluso) acutis magnis (alioque parvo supra medium posito) armatis; labro clypeum sat late superanti; antennis 9- articulatis; coxis posticis ad latera quam metasternum manifeste brevioribus, quam segmentum ventrale 2" paullo longioribus; tarsis posticis modice elongatis, articulo 2° quam 1" parum longiori; unguiculis appendiculatis. Long., 34 1.; lat., 1£ 1. This species belongs to my “Group VII.” of Heteronyx (vide P.L.S.N.S.W. 1889, p. 1219) which is tabulated in loc. cit. pp. 662, &c. In the tabulation it falls beside H. vacwus, Blackb., to which it is closely allied, differing however inter alia by its more strongly transverse and more coarsely punctulate prothorax, and the well-marked infuscation of its elytral suture. Lake Callabonna ; taken by Mr. Zietz. HYPHORYCTES (gen. nov. Dynastidarwm ). Mentum hirsutum, sat elongatum, sat convexum, antice rotunda- tum; palpi modici, articulo apicali elongato-ovali; mandibulee 38 externe bidentate (fere ut sodontis),; clypeus antrorsum angustatus, a capite sutura subtili angulata in medio tuber- culo armata divisus; caput haud carina marginatum; pro- thorax equalis ; pedes breves crassissimi, tibiis anticis extus obtuse bidentatis (processu apicali excluso) posterioribus 4 transversim bicarinatis, tarsorui posticorum articulo basali fortiter ad apicem dilatato; processus prosternalis validus hirsutus ; organa stridulationis nulla; maris tarsorum anti- corum unguiculus externus crassus bifidus. I cannot refer the species for which I propose this name to any existing genus, nor is it clear in which of his subtribes of Dynastides Lacordaire would have placed it, as the absence of sexual characters in the head and prothorax would associate it with subtribes in which the basal joint of the hind tarsi is of very different structure. It is generically very close to Pentodon australis, Blackb., but differs from it enter alia by the much more strongly dilated basal joint of its hind tarsi. H. maculatus, sp. nov. Sat elongatus; minus nitidus ; testaceo- rufus, suturis et carinis corporis pedumque fere omnibus et prothoracis utrinque macula laterali infuscatis; capite crebre subfortiter ruguloso, clypeo antice truncato leviter reflexo ; prothorace quam longiori dimidia parte latiori, antice forti- ter angustato, sparsim subtiliter (vix manifeste) punctulato, lateribus (superne visis) parum arcuatis; scutello magno levi ; elytris vix (vel nullo modo) striatis, obsolete seriatim punctulatis; pygidio antice crebre subtiliter postice vix manifeste punctulato. Long., 6—8].; lat., 35—5 1. I have seen several examples of this insect; one of them has the elytra faintly striate with indications of about four obsolete coste and some very faint but distinct punctures ; in the other examples this sculpture is scarcely discernible ; the difference is not sexual. I have no doubt they all appertain to one species. Thursday Island ; also Cape York. NOVAPUS. NV. rugosicollis, Blackb. At the time when I described this species (Proc. Linn. Soc. N.S.W. 1890 p. 305) I was doubtful of the sex of the type but concluded with hesitation that it was a male. Subsequent examination of more recently acquired examples of the genus has satisfied me that it is a female. I have no doubt the male has a large excavation on the prothorax. NV. nitidus, sp. nov. Mas. Brevis; latus; nitidus; subtus sat dense rufo-hirsutus ; piceo-rufus ; capite cornu recurvo acuto armato; prothorace quam longiori fere duplo latiori, antice valde angustato, excavatione permagna a basi ad apicem extensa pernitida fere levi impresso (hujus lateribus sursum 39 obtuse prominentibus), partibus lateralibus sat fortiter sat crebre punctulatis, lateribus fortiter rotundatis, angulis anticis sat acutis posticis obtusis, margine antico fere trun- cato , elytris fere levibus. Long., 103 1.; lat., 6 1. A second example of this insect (in the collection of C. French, Esq.) is larger (long. 12 1.) and has the lateral parts of the pro- thorax a little less closely punctulate, but presents no other difference. The clypeus of this species as of the others of the genus known to me is somewhat narrowly produced forward in the middle, and the apex of the projection is rather strongly re- flexed. This species may be at once distinguished from all the others of the genus that I have seen by its almost levigate elytra which are marked only with a fine sutural stria two or three ob- solete striz (resembling faint wrinkles) and some very faintly impressed and distantly placed punctures. N. Queensland. LV. bidentatus, sp. nov. Mas. Sat brevis; minus latus; sat nitidus ; subtus sat dense rufo-hirsutus ; rufus ; capite cornu vix recurvo acuminato minus elongato armato ; clypeo antice fere equaliter rotundato, margine reflexo sat alte cincto ; prothorace quam longiori vix dimidia parte latiori, antice valde angustato, excavatione permagna a basi ad apicem extensa fere levi impresso (hujus lateribus sursum obtuse prominentibus), partibus lateralibus antice sparsissime punctulatis postice levibus, lateribus rotundatis postice sinuatis, angulis anticis acutis posticis fere (nec acute) rectis, margine antico leviter fere equaliter emarginato prope medium utrinque tuberculo parvo acuto armato; elytris strlis nonnullis leviter impressis, his seriatim (interstitiis confuse) inzequaliter punctulatis. Long., 9 1.; lat., 541. The two small sharp tubercles placed one on either side of the middle of the front margin of the prothorax distinguish this species from all the others yet described of the genus. Central Australia ; McDonnell Ranges. PSEUDORYCTES. P. monstrosus, sp. nov. Mas. Nitidus; rufus, capite elytris pygidioque nigris; capite hirsuto antice perpendiculari, parte perpendiculari planato crasse ruguloso, cetera sparsim punctulato ; antennarum flabello elongato, hujus articulis singulis quam articuli ceteri conjuncti manifeste longioribus; prothorace sparsim minus evidenter punctulato, sparsim hirsuto, spinis 3 perlongis (quam prothoracis latitudo sub- longioribus) sat gracilibus armatis (ex his alio antico sinuato antrorsum et sursum oblique directo, aliis fere erectis utrinque paullo ante medium positis); scutello elytrisque 40 tere leevibus nitidissimis, his stria suturali fortiter impressis ; corpore subtus dense hirsuto ; pygidio fere glabro. Long., 9 1.; lat., 54 1. This extraordinary species is instantly distinguishable from its described congeners by the remarkable armature of its prothorax which consists of three somewhat slender horns of about equal length, each of them about as long as the prothorax is wide. Its black head prothorax and pygidium are also notable. The per- pendicular front of its head viewed from in front is flattened,— not concave as in that of P. mullerianus,—and is almost of semi- circular shape, the chord of the semicircle (which however is slightly arched) forming its upper outline. Gascoigne District, W. Australia; in the collection of Mr. French. P. trifidus, sp. nov. Mas. Latus; sat nitidus ; rufo-brunneus; capite antice perpendiculari, parte perpendiculari concavo ; antennarum flabello elongato ; hujus articulis singulis quam articuli ceteri conjuncti multo longioribus ; prothorace spar- sim subtiliter (parte excavata magis crasse) punctulato, cornubus 3 armatis (his quam prothoracis latitudo fere triplo brevioribus, cornu antico valde trifido, lateralibus crassissi- mis sed apicem versus sat gracilibus); scutello sparsim punctulato; elytris inequaliter striatis, striis crebre sat fortiter punctulatis, interstitiis sparsim ineequaliter punctu- latis ; corpore subtus dense hirsuto ; pygidio crebre (apicem versus sparsissime) punctulato. Long., 12 1.; lat., 7 1. This species is easily recognisable by the armature of its pro- thorax ; the front horn is directed forward over the head and turned upward at the apex which consists of three large triangu- lar teeth (the middle one erect, the lateral ones directed outward on either side); the lateral horns are placed very widely apart and are erect but a little curved (so as to be convergent at their apices), and are extremely thick at their base but in their upper half become slender with almost pointed apices. The striation of the elytra is much better defined than in P. mullerianus, White. Queensland; Darling R. district; in the collection of Mr. G. Masters. HORONOTUS. H., optatus, Shp. I have before me three male specimens for- warded by Mr. French evidently of this species. J should judge from the description of H. variolicollis, Fairm., that it is founded on the same species and must become a synonym. It seems also probable that my Palmerstonia minor is the female (which ap- pears to have been unknown to both Sharp and Fairemaire) of 4] the same species. Whether the Australian species referred by Sharp and Fairemaire to this Indian genus //oronotus are satis- factorily placed there or are better regarded as generically dis- tinct (in which case my name Palmerstonia will stand) I am not in a position to determine positively, as I have not an example of any Indian species for comparison, but it may be noted that according to Burmeister (the author of the genus) and Lacor- daire, one of the generic characters of Horonotus consists in the prothorax being armed with an excavation and also one or more prominences in both sexes. In my Palmerstonia and in the only Australian species attributed to Horonotus of which the female is known (#. duplex, Shp.) the prothorax of the female is quite even; this appears to me to be an important character and to render justifiable the use of a distinctive generic name. SEMANOPTERUS. S. rectangulus, sp. nov. Ovalis; sat latus; nitidus; piceus, capite prothoraceque nigris, antennarum clava rufescenti ; subtus longe sat dense rufo-pilosus; capite transversim rugato tuberculo conico inter oculos armato; prothorace quam longiori plus quam dimidio latiori, minus crebre (in medio obsolete, sed in depressione crasse squamose) punctu- lato, antice angustato, lateribus sat fortiter rotundatis mox ante basin subito fortiter incurvis hine ad basin (superne visis) rectis, angulis anticis sat prominulis posticis acute rectis ; elytris 4 costatis (costa suturali inclusa), interstitiis sat crasse nec crebre nec profunde punctulatis ; tibiis anticis extus fortiter (maris quam feminz magis acute) tridentatis ; segmento ventrali 6° punctulato, postice vitta transversali levi marginato ; processu prosternali angusto carinato. Maris prothorace antice fossa magna rotundata profunda, postice sulco longitudinali in medio dilatato, impresso ; segmento 6° ventrali postice emarginato. Femine prothorace longitudinaliter sulcato, sulco et ante et pone medium dilatato ; segmento ventrali 6° simplici. Long., 7 alate 4 1. It is extremely difficult to arrive at any satisfactory conclusion as to the limits of species in this most perplexing genus; speci- mens taken in company and certainly seeming to be of but one species vary considerably in the puncturation of the upper sur- face (especially in the distinctness of the prothoracic punctures and in the extent to which the punctures of the elytral inter- stices invade the edges of the coste) and even in the width of the prothorax. The insect described above is however easily recognisable by the peculiar outline of the prothorax which is very suddenly and strongly contracted a little in front of the 42 base and thence (viewed from above) quite parallel hindward, the hind angles being sharply rectangular (almost dentiform). The shape of the prosternal process also calls for attention. This in the genus Semanopterus rises perpendicularly behind the coxe and its summit is bent forward so as to project slightly between the coxe towards the head. In the present species it is densely clothed with long sete and is considerably narrower than in some species of the genus; its perpendicular face is strongly convex,—almost cariniform,—and its forward bend is only slight, the bent-forward part being quite narrow and almost evenly continuing the curve and convexity of the perpendicular part. In some species the bent-forward part is much wider flatter and almost at a right angle to the perpendicular part. Alice Springs, Oodnadatta, Leigh’s Creek and Barrow’s Creek. S. persimilis, sp. nov. Ovalis; sat latus ; nitidus; piceo-niger, subtus obscure rufescens longe sat dense rufo-pilosus ; capite crasse squamose ruguloso, tuberculo conico inter oculos armato; prothorace quam longiori dimidio latiori sat crebre sat fortiter (in depressione crasse squamose) punctulato, antice angustato, lateribus sat fortiter rotundatis mox ante basin subito fortiter incurvis hinc ad basin (superne visis) rectis, angulis anticis sat prominulis posticis acute rectis ; elytris 4-costatis (costa suturali inclusa), interstitiis sat crasse nec crebre nec profunde punctulatis; tibiis anticis extus valde fortiter (maris quam feminz etiam magis for- titer) tridentatis ; segmento ventrali 6° punctulato, postice vitta transversali Jevi marginato ; processu prosternali sat angusto carinato, parte summa antrorsum directa minute planata et antrorsum deelivi. Maris prothorace antice fossa magna rotundata profunda, postice sulco longitudinali, impresso ; segmento 6° ventrali postice emarginato. Femine prothorace longitudinaliter sulcato, sulco et ante et pone medium dilatato; segmento ventrali 6° simplici. Long., 7—8 1. ; lat., 4—42 1. This species is very closely allied to S. rectangulus, Blackb., from which it differs by the nearly black color of its upper sur- face, the evidently stronger puncturation of its prothorax, the larger teeth on the external margin of its front tibie, the more confused sculpture of its clypeus and the different shape of its prosternal process. This latter (as in rectangulus) consists of an erect somewhat narrow piece keeled on its hind face rising from the surface of the prosternum behind the coxee and at its summit bent forward slightly towards the head; but whereas in rectangulus this bending forward is the result merely of the top 43 of the process being slightly curved, in persimilis a small flattish lamina appears to jut out (from the top of the process) directed towards the head and also sloping downwards, so that from a certain point of view (7.e. from the side) the top of the process seems to be obliquely truncate with its point furthest from the head subtuberculiform. The process (as in rectangulus) is densely hirsute but in this species the front part of the flattened top is glabrous. This species is distinguished from all the recognisably described Semanopteri (except rectangulus) by the peculiar out- line of its prothorax which (viewed from above) looks as if a small piece had been cut-out on either side close to the base. N. Queensland ; sent by Mr. French. S. dentatus, sp. nov. Late ovalis; minus convexus; nitidus ; piceo-niger, subtus vix rufescens, rufopilosus ; capite crasse squamose nec profunde ruguloso, tuberculo magno armato, pone tuberculum fossa levi impresso; prothorace quam longiori plus quam dimidio latiori, subgrosse minus crebre nec profunde (in depressione et versus angulos anticos crasse squamose) punctulato, antice angustato, margine antico in medio leviter elevato, lateribus sat rotundatis, angulis anticis sat prominulis posticis (superne visis) rectis (haud acute); elytris minus equaliter sat crasse leviter punctulato- striatis, vix manifeste costatis, puncturis striarum et inter- stitiorum nonnihil confusis; tiblis anticis extus fortiter tridentatis ; abdomine sparsim leviter squamose punctulato ; processu. prosternali minus angusto, retrorsum fortiter bidentato. Mas latet. Feminz prothorace antice fossa rotundata, postice sulco longi- tudinali obsoleto, impresso. Long., 11 1; lat., 6 1. (vix). The remarkable form of the prosternal process at once separates this species from its described congeners. The process may be described as rising upwards from the level of the prosternum behind the cox, but instead of rising erectly it inclines forward, and its hinder face bears two large transverse blunt teeth or tubercles (one below the other) and is nearly glabrous. The nitid depression on the head behind the tubercle is also very dis- tinctive. As the apical ventral segment is not emarginate I presume the example before me is a female. The prosternum 2m front of the coxee is somewhat wide, with a strong median keel. N. Queensland. S. carinatus, sp. nov. S. persimili valde affinis ; differt dentibus tibiarum anticarum minoribus, tarsorum posticorum articulo basali ad apicem minus lato, processu prosternali ad sum- mum sat longe horizontali anguste cariniformi, nec tubercu- lato. Long., 7 1.; lat., 41. tt This species is extremely like S. rectangulus, Blackb., and S. persimilis, Blackb., but differs from both by characters that appear to me quite inconsistent with specific identity. The most notable of these is the form of the prosternal process, which at the top is bent forward towards the head in such fashion that its bent-forward portion almost forms a right angle with its erect portion,—but this (7.e., the bent-forward portion) instead of being a small flattish lamina bounded posteriorly by a tubercle (as it is in persimilis) is a narrow keel (its outline viewed from the side being seen however to be slightly concave) ; while in rectangulus the bent-forward portion is scarcely existent being represented merely by the erect portion being slightly curved towards the head at its summit. The prosternum in front of the coxe is in all these three species narrow and roundly cariniform. The puncturation of the prothorax is in this species almost as in rectangulus but the sulcus of the hind part of the prothorax is simple as in persimilis (not dilated in its middle into a fovea as it is in rectangulus). Northern Territory of South Australia ; near Palmerston. N.B.—The species of Semanopterus named previously to those I have described are S. (Philewrus) subcostatus, Cast., S. Ade- laide, subequalis and depressus, Hope, and S. convexiusculus and depresstusculus, Macl. None of them are described sufficiently for confident identification and it is possible that I may have described some of them, especially the first,—the description of which would apply so far as it goes to any Semanopterus. I, however, have species in my collection which seem likely to be Adelaide, subequalis, and convexiusculus and are certainly dis- tinct from those I have described. I should judge from their names that S. depressus and depressiusculus cannot be identical with any of my species unless it be S. dentatus,—but they are both described as having costate elytra, while dentatus is of all the Semanoptert known to me the only one on which no clearly defined elytral costee can be traced. ISCHIOPSOPHA. I. Bowrker, sp. nov. Nitidissimus; lete viridis (vel certo ad- spectu ceruleus), antennis palpisque piceis plus minusve viridi-micantibus, abdominis suturis parte mediana macu- lisque lateralibus certo adspectu nigricantibus ; supra tota creberrime omnium subtillissime coriacea ; capite sparsius subtilius punctulato, clypeo profunde bifido; prothorace (lobo basali excepto) quam longiori (et postice quam antice) duplo latiori, latera versus leviter sparsim (in disco vix manifeste) quam caput multo minus fortiter punctulato, lobo basali magno scutellum fere obtegenti ad apicem emar- + [ey | ginato ; elytris leevibus nisi juxta marginem lateralem trans- versim strigatis, sutura postice carinata et ad apicem spinoso-producta ; pygidio concentrice sat fortiter strigato ; subtus sublevis vel potius obsolete sparsissime punctulata, segmentis ventralibus singulis utrinque spatio crebre oblique strigato ornatis ; processu mesosternali elongato sat horizon- tali. Maris capite elongato, tibiis anticis extus (processu apicali excepto) dente minuto subapicali (et altero submediano haud vel vix manifesto) armatis ; abdomine longitudinaliter concavo. Feminz capite minus elongato, tibiis anticis extus dentibus 3 (apicali incluso) sat fortibus armatis ; abdomine sat eequali- ter convexo, segmento 5° postice puncturis nonnullis sat magnis impressis. Long., 13 1.; lat., 64. I cannot find among the numerous species of IJschiopsopha described (some of them as Lomaptere) as occurring in New Guinea and Malay that this large and magnificent insect has a place. Compared with J. (Lomaptera) pulciripes, Thoms., the present species is larger and of a more robust build,—differently colored, its green tending towards blue whereas that of pulchripes tends towards golden,—its head is very similar except more finely sparsely and faintly punctured, especially in the hinder part,—its prothorax is much more strongly transverse, devoid of transverse strigosity, and very much less strongly punctured (the punctures even close to the lateral margin being very sparse and scarcely so strongly impressed as those halfway between the middle of the prothorax and the lateral margin in pulchripes),—its elytra are practically punctureless (in the female the punctures where most distinct are scarcely so much so as in the middle of the prothorax of pu/chripes, in the male they are still fainter) their sutural apex is more prominent, and their system of submarginal transverse scratches is almost exactly as in Hemipharis insularis, L. and G.,—its legs are very differently colored,—its whole surface under a strong lens is seen to be finely coriaceous or covered evenly with a system of exces- sively close and fine puncturation underlying all the other sculp- ture. The bluish tone of color is more marked in the males than females. N. Queensland ; taken by Captain Edmund Bourke, R.N., and presented to me. ASTREUS. A. Meyricki, Blackb. I see that Herr. van de Pollin Tijdsckr. ent. Xxxvi., p. 67, says that this name has been given to the same species as that which he called A. Badenz. I have already (Proc. L.S., N.S.W., 1894, p. 101) drawn attention to the facts that 46 Herr van de Poll and [ both described some Australian Astrei in 1889, that his descriptions seem to have been published before mine, and that probably his A. Jansonz and my A. Tepperi are names of one and the same species. When writing that note I considered the question whether Meyrick: and Badeni are iden- tical and considered it doubtful, an opinion I still hold. Herr van de Poll gives as the first-named habitat of A. Badeni “Gawler, S.A.,” and adds as a second locality “‘Swan River.” I doubt whether any Astreus is common to these very distant localities, and if the type of A. Ladeni really came from Gawler I should expect to find it different from A. Meyricki which is from N.W. Australia. No doubt the two species are at any rate much like each other, but I notice that A. Badenz as figured has the basal spot of its elytra extending across two interstices while in A. Meyricki it seems to be constantly limited to one interstice,—nor do I find any trace in Meyricki of the fine red line which is depicted across the basal margin of the elytra in Baden. On these grounds I look upon it as quite likely that if the types of the two could be compared other differences would be found. BUBASTES. B. splendens, Blackb. The Coleoptera collected at L. Calla- bonna by Mr. Zietz include what I take to be a second specimen of this insect. It is notably smaller than the type with elytra tending towards violet in color and the puncturation throughout seems to be a trifle less strong but, judging from the extreme variability of its congener 6. inconsistens, Thoms., these differ- ences are unlikely to be specific. CHRYSOBOTHRIS. C. interioris, sp. nov. Obscure znea, hic illic cuprascens, elytro- rum foveis sat lete cupreis; capite antice sat crasse rugu- loso-punctulato et transversim inequali, postice crebre sub- tilius punctulato (in medio levi et canaliculato), oculis minus approximatis ; prothorace quam longiori duabus_ partibus latiori, leviter canaliculato (canali antice obsoleto), crebre subtilius transversim rugato et sat crebre punctulato, antice et postice equaliter angustato, ineequali (presertim utrinque oblique leviter impresso), lateribus (superne visis) in parte mediana rectis vel fere concavis hinc et antice et postice angulatim convergentibus, basi valde trisinuata; elytris crebre subtilius punctulatis, costis discoidalibus 4 et costa abbreviata subscutellari instructis, foveis 3 impressis, lateri- bus denticulatis fere ab humero, apice obtuso ; corpore sub- tus in parte mediana sparsim (latera versus sat crebre) punctulato, puncturis a parte antica retrorsum gradatim 47 minus fortiter impressis; prosterni margine antico late emarginato; segmento apicali ventrali 2-emarginato et 3-spinoso. Long., 62 1.; lat., 23 1. The eyes are wider apart than in most Chrysobothres known to me. The prothorax is of peculiar form (the form probably that M. Thomson calls ‘ subhexagonalis”), approximated however though only feebly by one or two other species in my collection ; the middle part of its sides is slightly concave and at the front and hind apices of this middle part the outline is very distinctly angulated and thence proceeds obliquely to the comparatively narrow front and hind margins respectively, so that the segment is quite decidedly ‘‘ octagonal” (except in so far as its regularity is marred by the trisinuation of the base). Another well-marked character is afforded by the hind outline of the apical ventral segment which is widely emarginate, either side of the emargina- tion being produced in a strong spine, while the longitudinal carina that runs down the segment is produced hindward (dividing the emargination into two) in a third spine very little shorter than the lateral ones. I am unfortunately not able to detail the differences between this species and any other described Australian Chrysobothris as there is not one of those hitherto named that has been recognisably described. I have in my col- lection examples (conjecturally identified) of most of them but it is of no use to compare a new species with an old one unless one is quite certain of the latter. Limiting myself to the char- acters mentioned in the descriptions I may say however that the 3-spinose apex of its abdomen distinguishes this insect from C. subsimilis, Thoms., and amplicollis, Thoms., and that the strong oblique lateral impressions of its prothorax distinguish it from C. Mastersi, Macl., and viridis, Macl. The other species are practically undescribed, although it may be noted that Mr. Saunders’ re-description of C. Australasiw, Hope, seems to imply that the apex of its abdomen is not tri-spinose; their localities however are such as to render extremely improbable their identity with this Central Australian species. The elytral coste of the present insect are very well defined and are placed as in the other Australian species ; the foveze are placed as follows,— one close to the middle of the base, one in front of the middle between the second and third cost, one behind the middle inter- rupting the third costa. The front femora are strongly dentate beneath, the intermediate tibie nearly straight. The basal two ventral segments are shallowly concave longitudinally. Lake Callabonna ; taken by Mr. Zietz. AGRYPNUS. A. Mastersi, Macl. Specimens of Agrypnus taken by Mr. Zietz near Lake Callabonna vary from the type prevalent in N. 48 Queensland to an extent that seems scarcely consistent with specific identity,—the prothorax being very much more finely punctulate and having its sides much more sinuate behind the middle. Nevertheless as that eminent specialist Dr. Candéze has stated his opinion, after examining a long series of Agrypni from various parts of Australia, that he has seen only one species and that it is an extremely variable one, I deem it better to abstain from treating these Central Australian specimens as specifically distinct from J/astersz. LACON. L. Zietzi, sp. nov. Piceus; minus nitidus ; squamulis piliformi- bus griseis vestitus (his in elytrorum interstitiis alternis paullo densioribus), antennis pedibusque rufescentibus ; prothorace quam longiori vix latiori, crebre subfortiter punctulato, canaliculato (canali antice obsoleto), a basi ad apicem gradatim (leviter sinuatim) angustato, basi quam margo anticus duplo latiori, angulis posticis obtusis extus paullo dilatatis; elytris quam prothorax parum latioribus, punctulato-striatis, interstitiis subfortiter punctulatis inter se eequalibus ; sulcis tarsorum nullis. Long., 5 1.; lat., 121. The slightly denser disposition of the vestiture on the alternate interstices of the elytra than on the others,—which is more ap- “parent in some examples than in others,—gives this species a faint appearance of being striped and renders it a little doubtful whether Dr. Candéze would place it in his tabulation (Mém. Liége (2) IX., 1882, pp. 49, &e.) among the unicolorous or the variegated species. Among the former it would stand beside L. princeps, Cand., and crassus, Cand., from which its size and the posterior angles of its prothorax not truncate readily dis- tinguish it,—while among the variegated species it would be at once distinguished by the absence of tarsal sulci. It should be noted that although careful measurement shows the prothorax to be a trifle wider than long, that segment to a casual glance ap- pears longer than wide. Lake Callabonna; taken by Mr. Zietz. MONOCREPIDIUS. M. commodus, sp. nov. Modice angustus ; sat parallelus ; minus nitidus; pube fulva vestitus; totus ferrugineus, antennis pedibusque dilutioribus, scutello elytrorumque basi rufescen- tibus; antennarum articulo 3° quam 2" parum longiori, quam 5" duplo breviori ; prothorace trans angulos posticos quam longiori vix latiori, subtiliter manifeste canaliculato (nonnullorum exemplorum canali antice posticeque abbre- viato), sat crebre minus subtiliter umbilicato-punctulato, angulis posticis divergentibus, bicarinatis (carina interna 49 brevi minus perspicua); elytris ad apicem sat rotundatis nonnullorum exemplorum angulo suturali brevissime acuto), punctulato-striatis, interstitiis leviter convexis crebre sub- aspere punctulatis ; prosterno medio fortiter gibbo, fortius vix crebre punctulato, hoc ad latera haud deplanato, suturis prosternalibus rectis, pronoti margine antico in pro- sternum defiexo; tarsorum lamella sat angusta. Maris antennis prothoracis basin sat longe superantibus ; pro- thorace a basi ad apicem sinuatim angustato. Femine antennis prothoracis basin vix attingentibus ; prothorace ad medium quam trans basin parum angustiori. Long., 63— 73 1.5 lat., 14—22 1. The Australian species of Monocrepidius may be best sub- divided, in my opinion, by the structure of the lateral margin of the pronotum and prosternum which assumes three different forms. In some species (e.g., Australasia, Boisd.) it is strictly lateral ; in others (¢.g., acwminatus, Macl.) it is deflexed in front so that (viewed from directly above) the front part of it passes out of sight and both margins can be seen together in their entirety only by turning the specimen upside down and looking at them on the prosternum, but in other respects it is as in the former group; in a third group of species (¢.g., nigripennis, Cand.) it passes on to the prosternum behind the middle of the segment (so that the greater part of it is invisible when the pronotum is viewed from directly above) and is bordered on the prosternum by a well-defined sulcus (these species mimicking some Hucnemide in their structure. The present species belongs to the second of these groups, and is distinguishable by exceptionally good characters, among which the most noticeable are the remarkably convex—strongly protu- berant—middle part of its prosternum, and the umbilicated punc- tures of its prothorax (inside each of which there appears to be a small granule). Lake Callabonna ; taken by Mr. Zietz. M. inamenus, sp.nov. Modice angustus; sat parallelus ; minus nitidus ; pube fulva vestitus ; supra obscure brunneus, cor- pore subtus ferrugineo, antennis palpis pedibusque testaceis ; capite postice longitudinaliter carinato ; antennarum articulo 3° quam 2"S vix longiori, quam 5* duplo breviori; prothorace trans angulos posticos quam longiori subangustiori, leviter canaliculato (canali antice sat obsoleto), confertissime vix aspere punctulato, angulis posticis parum divergentibus bicarinatis (carina interna sat forti minus abbreviata) ; elytris ad apicem sat rotundatis (angulo suturali brevissime acuto), punctulato-striatis, interstitiis leviter convexis sub- D 50 tiliter transversim rugatis; prosterno medio fortius vix crebre punctulato, hoc ad latera sulcato, suturis prosternali- bus rectis, pronoti margine in prosternum deflexo ; tarsorum lamella angusta. Maris antennis prothoracis basin vix superantibus ; prothorace a basi ad apicem sinuatim angustato. Femine antennis prothoracis basin haud attingentibus; prothorace ad medium quam trans basin parum angustiori. Long,, 5—54 1.; lat., 121. This species belongs to the third of the groups that I have suggested above as convenient subdivisions of Monocrepidius. It is remarkable for the extremely close puncturation of its pro- thorax. It may be noted that the piece of the prosternum in- cluded between the prosternal suture and the margin of the pronotum is (not as in some species acuminate, but) obliquely truncate in front. In Dr. Candéze’s tabulation of Monocrepidius (Mon. II. pp. 191, &c.) the present species would stand beside M. fictus, Cand., from which inter alia its considerably larger size will distinguish it. Lake Callabonna ; taken by Mr. Zietz. APHILEUS. A. ferox, sp. nov. Sat latus ; sat depressus ; fusco-piceus, palpis antennis pedibusque testaceis vel piceo-testaceis ; breviter cinereo-setulosus ; mandibulis elongatis, quam caput (labro excluso) sat longioribus, curvatis, ad apicem acutis (haud bidentatis), pone medium intus dente valde elongato arma- tis; capite sat nitido inter oculos concavo, sat crebre punc- tulato ; prothorace sat nitido, quam longiori tribus partibus latiori, obsolete canaliculato, sat crebre (ad latera fere ut caput, in medio paullo minus crebre) punctulato, trans basin quam trans marginem anticum plus quam dimidia parte latiori, subquadrato (sed lateribus versus apicem summum fortiter convergentibus, versus basin summam fortiter diver- gentibus), lateribus distincte explanatis sed vix manifeste marginatis, angulis posticis divergentibus ; elytris striatis, striis subtilius punctulatis, interstitiis parum convexis obso- lete rugulosis, apice suturali breviter spiniformi. Long. (mands. incl.), 18 1; lat., 54 1. Larger than A. lucanoides and less widely shaped; differs from that species also inter alia by its very distinct mandibles and its more nitid prothorax with much closer puncturation. In the example before me there is a very conspicuous tubercle on the disc of the prothorax a little to the left of the central line, but in all probability this is an individual aberration. N. Queensland ; presented to me by Mr. French. d1 LAIUS. L. eremita, sp. nov. Subopacus ; haud setosus; coccineus, an- tennis nigris, elytrorum maculis binis (his marginem latera- lem nec suturam attingentibus, altera minori basali altera majori subapical1) piceis, pedibus infuscatis ; capite elytrisque (his sat brevibus) creberrime rugulosis vel potius coriaceis ; prothorace valde transverso, inzequali, subnitido, puncturis sat magnis leviter impressis ; oculis fortiter convexis. Maris antennarum articulo 2° valde compresso-dilatato, obovato, ad apicem subtruncato ; capite trans oculos quam prothorax fere latiori. Femina latet. . Hone, tb? 1.5 lat., = 1. A very distinct species owing to the uniform red color of its body with the exception of the two dark spots on the elytra ; its unicolorous black antenne are also characteristic. Central Australia ; near Oodnadatta. PTEROHELEUS. P. fraternus, sp. nov. Late ovalis; sat nitidus ; piceus antennis tarsisque dilutioribus; capite subtiliter obsolete minus crebre punctulato; prothorace fere levigato, quam longiori (et postice quam antice) fere triplo latiori, ad latera late explanato, marginibus lateralibus vix recurvis, angulis an- ticis obtusis sat productis posticis sat acutis, basi sat fortiter trisinuata; elytris subtiliter seriatim punctulatis, vix striatis, ad latera late explanatis, margine explanato ante medium intus dilatato apicem versus angustiori. Long., 7 1.; lat., 43 1. This species in its broad form with wide lateral margins of prothorax and elytra resembles P. picews, Kirby, near which it should be placed in the first group of the genus as subdivided by Sir W. Macleay (P.L.8., N.S.W., 1887, p. 520). Its compara- tively small size will distinguish it from all the other members of that group. Placed beside P. piceus it differs from the latter chiefly by its head and prothorax being even less distinctly punc- tured and its elytral sculpture consisting of mere rows of fine punctures becoming very faint near the apex, the interstices be- tween which are perfectly flat; while the elytra of piceus are distinctly punctulate-striate with distinctly convex interstices. Central Australia ; in my collection ; specimens taken by Mr. Zietz near Lake Callabonna scarcely differ. HELAEUS. H, interioris, Macl. Among the Coleoptera brought from Lake Callabonna by Mr. Zietz are a series of specimens which I attribute to this species, although Sir W. Macleay’s description 52 is not of a kind to justify very great certainty. Unfortunately Sir William in his descriptions of Helaz has relied as a principal character on the number of granules on the elytra and this un- doubtedly appears to be subject to much variety. I am con- vinced that the series before me cannot be regarded as repre- senting more than one species, but there are scarcely two of them in which the elytra are identically granulate. I think them likely to be H/. interioris because, although the description of that species mentions scarcely a character that is really specific, they all have near the suture a row of granules closer and more conspicuous than those in the other rows (and more markedly so than in most other /e/e@i) and this character is mentioned in Sir W. Macleay’s description of H. interioris. The reliable characters of the insect before me seem to consist in its comparatively narrow elongate form and the strongly “turned up” direction of the expanded sides of the elytra. It is quite true that Sir W. Macleay calls the “margin” “a Jittle reflexed” but a comparison of the terms he uses in describing other species points to the conclusion of his intending to signify that the expanded margin in H. interioris is more reflexed than in most other /Helai. EPHIDONIUS. ; E. parvicollis, sp. nov. Ovalis; opacus ; niger ; corpore subtus picescenti ; capite creberrime subtilius subaspere (puncturis * majoribus minoribus que intermixtis) punctulato ; prothorace quam caput dimidia parte latiori quam elytris fere duplo angustiori, quam longiori (et postice quam antice) dimidia parte latiori, postice utrinque sulco obliquo obsolete impresso (his ambobus literam V obscure simulantibus), creberrime subtilissime punctulato (vel potius coriaceo) et puncturis paullo majoribus sparsim impresso, lateribus sat explanatis et leviter recurvis, angulis anticis obtusis posticis acute rectis vix retrorsum directis; elytris quam _ prothorax quadruplo longioribus, costis quinis (sutura inclusa) ornatis, inter costam et costam puncturarum seriebus 4 impressis (serierum interstitiis leviter convexis); labro antice vix emarginato ; maris a femine tibiis haud distinctis. _ deme oils ep, dad. This suebies seems to be near £. Duboulayi, Bates, but differ- ing in several respects,—in its entirely opaque upper surface (Mr. Bates implies that Duboulayi is not more opaque than acuticornis ), its scarcely emarginate labrum, the close punctura- tion of its head, the simple tibie of the male, &c. The elytral coste under a strong lens show the same minute tuberculation continued behind (where the coste become very faint) as Mr. Bates describes in £. Duboulayi. Lake Callabonna ; taken by Mr. Zietz. D3 CISTELIDA. HOMOTRYSIS. H. arida, sp. nov. Fem. Sat elongata; leviter ovata ; minus convexa ; nitida; pilis elongatis erectis sat crebre vestita ; rufobrunnea, capite postice prothoraceque picescentibus, an- tennis palpis pedibus labro (et clypeo antice), rufo-testaceis ; capite (cum prothorace) dupliciter (subtiliter et sat fortiter) sat crebre confuse punctulato ; oculis minus convexis dis- tantibus (spatio intermedio quam antennarum articuli 3' longitudo sat latiori); prothorace quam longiori parum latiori, haud canaliculato (disco utrinque vix impresso), antice modice angustato, lateribus leviter sat sequaliter (superne visis) arcuatis, basi sinuatim truncata, angulis pos- ticis obtuse rectis (superne visis obtusis); scutello punctu- lato, in medio leviter carinato ; elytris sat fortiter striatis, striis punctulatis (puncturis antice magnis quadratis, re- trorsum gradatim obsoletescentibus), interstitiis sat planis fortius minus crebre punctulatis; antennis quam corporis dimidium paullo brevioribus, articulo 3° quam 4*° manifeste longiori ; segmento ventrali apicali zequali, postice rotundato- truncato. lLong., 54 1.; lat., 21. The principal characters of this species,—among its congeners with longish erect pilosity clothing the upper surface,—lie in its feebly convex eyes, exceptionally elongate prothorax, nearly uni- formly colored upper surface, and elytra with both striz (these however only in front) and interstices conspicuously punctulate. Central Australia ; near Oodnadatta. fH. sitiens, sp. nov. Fem. Precedenti affinis ; tota picea, labro antennis pedibusque paullo dilutioribus; capite (clypeo excepto) sparsim subtilius punctulato; prothorace quam longiori fere dimidia parte latiori, ad latera sat fortiter rotundato, minus fortiter punctulato, in disco (exempli typici) haud impresso, antice vix angustato, angulis posticis magis rotundatis; scutello medio nullo modo carinato ; an- tennarum subtiliorum magis elongatarum articulo 3° quam 4"° magis longiori; cetera ut precedentis (H. aride). Long., 5 1.5 lat. 131 Closely allied to H. arida, but differing from it by well defined characters,—especially by its antenne and legs of dark color, the third joint of its antennz longer in proportion to the fourth, its prothorax much more transverse and otherwise dif- ferently shaped, &c. Central Australia ; Hergott Springs. HT, callabonensis, sp. nov. H. arideé aftinis; differt fere ut H. sitvens sed colore et capitis sculptura H. aride haud dis- D4 pari; prothorace minus crebre vix dupliciter punctulato ;. elytrorum versus apicem striis magis perspicue punctulatis. interstitiis manifeste convexis angustatis. Maris tibiis anticis (paullo supra medium) dente valido armatis. Femine tibiis muticis. Long., 44-5 1.; lat., 14-—14 1. This species is closely allied to the preceding two. I should hesitate to consider its differences more than accidental peculiari- ties of an individual if I had seen only a single example, but I have before me several of each sex in all of which the distinctive characters are quite constant. H.arida may be at once dis- tinguished from the other two by its considerably more elongate and less transverse prothorax arched on the sides only feebly. H. sitiens differs from the other two by the dark color of its antenne and legs as well as by the sparseness of the punctures between its eyes and from arida by its more slender antenne with comparatively longer third joint,—while H. callabonensis differs from the other two by the finer punctures of the prothorax being almost absent by the striz of its elytra being quite con- spicuously punctulate to the apex and by its elytral interstices becoming narrower and quite evidently convex near the apex. Central Australia; taken near Lake Callabonna by Mr. Zietz. N.B.—In my tabulation of species of Homotrysis (Tr. Roy. Soc. S.A. 1891 pp. 320-1) the three above described would form a separate section under “ AA” on page 321 (assuming, that is, that the eyes of the male,—as is probably the case,—are not materially different in H. arida and sitiens from those of H. calla- bonensis). The tabulation then will end as follows :—. AA. Interval between eyes in both sexes greater than the width of either eye as seen from above. B. Punctures of elytral strize,—at least in front half of elytra, —well defined, and quite distinct from the much smaller interstitial punctures. C. Head strongly and rather closely punctulate between the eyes. D. Coarser punctures of pro- thorax much confused with fine puncturation.. arida, Blackb. DD. Prothorax almost devoid of fine punctures ... callabonensis, Blackb. CC. Punctures between the eyes very fine and very sparse... sitvens, Blackb. BB. Punctures of elytral strize scarcely defined as distinct from those of the interstices... carbonaria, Germ. D5 NOCAR. NV. debilis, Blackb. This species is identical with Cistela depresstuscula, Macl., an example of which I have to thank Mr. Mr. Masters for. As mine is the more recent name it must sink and the insect must be known as Nocar depressiusculus, Macl. (EDEMERID. ANANCA., This genus is already a receptacle for widely different forms and is only waiting its time to undergo a revision which will probably involve the removal from it of all the Australian species attributed to it. Mr. Champion of the London Entomological Society (who ranks high among the specialists of our day on the Heteromera and to whom I am indebted for much valuable assis- tance in working on the family) has the Australian Wdemeride at present in hand, and I understand is about dealing with them in a memoir which I anticipate with the deepest interest. Under these circumstances it would be out of the question even if I felt competent for the task for me to meddle with it. In the Zietz collection, however, there is a species of @demeride which it seems very inconvenient to omit in my present work of describing the new species of that collection and as it seems quite safe to assume that the species in question is not among those in Mr. Champion’s hands I venture to subjoin a description of it. In describing it the only existing genus to which it can be provision- ally referred is Ananca. It certainly has much resemblance to some of the Australian species that bear the name Ananca but I doubt whether it will stand permanently as really congeneric with any of them. Its very much smaller size at once suggests wide departure from such species as Wdemera puncta, W. S. Macleay, @. australis, Boisd., Nacerdes nigronotata, Bohem., which may be regarded as fair types of the Australian insects that have been attributed to dnanca. These latter species how- ever differ much inter se in the structure of their palpi and tarsi, —so much indeed that the three I have named may possibly be held to represent three distinct genera. The species I describe below could not, in that case, be associated with any of those three. Of them I think nigronotata, Boh., is the one it comes nearest to but it differs from it in notable characters, especially in its much shorter muzzle, in its smaller and much more slender tarsi, in its shorter maxillary palpi the apical joint of which is less securiform, in its shorter legs, and in its prothorax not much narrower than its elytra. Its eyes are much like those of nigronotata and its front tibiz have two apical spines. A, Zietzi, sp. nov. Testaceo-fusca, sternis abdomineque nigri- D6 cantibus exceptis; sat nitida; minus dense pubescens ; antennis quam corporis dimidium brevioribus ; capite crebre distincte, prothorace vix manifeste (hoc quam longiori parum latiori, in medio transversim inequali, lateribus antice sat rotundatis), elytris subtilius sat crebre, punctulatis; his lineis subtiliter elevatis circiter 3 vix distincte instructis. Long., 34—4 1.; lat., 1 1. Lake Callabonna ; taken by Mr. Zietz. CURCULIONID&. TALAURINUS. T. strangulatus, sp. nov. Niger, squamis pallidis plus minusve vestitus et in tuberculis omnibus setis singulis pallidis in- structus ; capite coriaceo vix manifeste punctulato; rostro brevi quam caput paullo angustiori, fortiter concavo, ad apicem emarginato, carinis internis vix distinctis externis crassis minus obliquis bene determinatis obsolete grosse punctulatis ; prothorace quam longiori parum latiori, mox pone marginem anticum profunde transversim sulcato, spar- sim tuberculato, antice quam trans basin paullo latiori, lateribus sat arcuatis ; elytris tuberculis parvis nitidis sub- seriatim instructis, angulis humeralibus tuberculiformibus sed vix antrorsum prominentibus ; tibiis elongatis gracilibus. Maris femoribus anticis sat dilatatis; segmento ventrali apicali pone medium transversim leviter sulcatum, sulci margine postico in medio carina transversa acuta armato. Femina latet. lLong., 7 1.; lat., 3 1. This is a species of narrow subparallel form, its upper surface subopaque (the elytra more so than the prothorax) and bearing small tubercles all of them isolated and separated from each other by distinct intervals many of which are much larger than the area of the individual tubercles. The tubercles of the pro- thorax. are much larger than those of the elytra and resemble small flattish warts while some of those on the elytra (especially towards the sides) are acutely conical granules. The squamosity of the specimen before me is confined to the sides where it forms small patches but probably in a perfectly fresh example it is generally distributed over the surface. I think the following characters in combination will distinguish this species ; rostrum deeply concave with very well developed external ridges; pro- thorax very sparsely tuberculate (much more sparsely than in, e.g., I. tuberculatus, Macl.), and with an extremely strong trans- verse sulcus a little behind the front margin ; shoulders of elytra scarcely projected forward ; apical ventral segment of male bear- ing a feeble transverse impression extending all across it a little D7 behind the middle and limited in the middle part of its hind margin by a sharply defined transverse carina; tarsi long and slender. From certain points of view the elytra appear to be feebly striate and the seriate arrangement of their tubercles is very irregular. Centr al Australia ; Oodnadatta. LONGICORNES. PARANDRA. LP. Frenchi, sp. nov. Nigro-picea, corpore subtus pedibusque plus minusve rufescentibus ; nitida ; capite sat crebre minus fortiter punctulato, inter oculos sat fortiter bituberculato ; prothorace quam longiori dimidia parte latiori, obsolete sub- canaliculato, fere ut caput sed paullo minus crebre punctu- lato, basin versus sat fortiter angustato, lateribus pone medium subangulatis (hine ad basin sinuatim convergenti- bus), margine antico sinuato, angulis omnibas obtusis bene determinatis (anticis dntrorsum, posticis extrorsum, promi- nulis), basi leviter sinuato-emarginata ; elytris quam _pro- thorax parum latioribus, punctulatis (ad basin ut prothorax, retrorsum gradatim magis crebre magis subtiliter); segmento ventrali apicali transverso, granulato (a basi retrorsum gradatim magis fortiter magis crebre), postice late rotundato. Long., 94.1.; lat., 32 1 I cannot identify this insect with any Parandra yet de- scribed. For the sake of precision it will be well to compare it with a previously-named species. Placed beside P. pwncticeps, Shp., it is seen to be a narrower, more parallel, and more convex insect with the puncturation of its head a little finer but not much different, and that of its prothorax and elytra like that of its head (and therefore very different from the same in puncticeps) except that on the prothorax the punctures are a trifle less close and on the elytra they become gradually smaller and closer from the base hindward so that towards the apex of the elytra they differ considerably from those on the head. In P. Frenchi the sides of the prothorax are much more narrowed (and that more sinuately) behind their quasi-angulation than in puncticeps and the lateral margins are wider and better defined while the front angles are decidedly prominent. The large obtuse tubercles between the eyes are wanting in P. puncticeps, and the mandi- bles are very different in the two insects. I am doubtful of the sex of the type of P. Frenchi, but I believe it is a female. Its mandibles are much like those of the Lucanid Lissotus subtuberculatus, Westw., as figured Tr. Ent. Soc., 1885, t. 12, fig. 2. NS. Wales ; in the collection of Mr. French. 58 CATYPNES. C’. planicollis, sp. nov. (Mas.?) Nitidus; minus elongatus ; brunneus, capite obscuriori, elytris apicem versus pedibusque dilutioribus ; capite magno in medio sulcato, fortiter rugu- loso (area utrinque prope sulcum medianum nitida sparsim grosse punctulata excepta), mandibulis sat productis ad apicem hidentatis; prothorace (spinis exclusis) quam longiori fere duplo latiori, supra in disco planato sparsim subtiliter punctulato et foveis 3 grosse rugulosis Impresso (sc. una mediana sublanceiformi, et utrinque ad basin una ovali oblique posita), lateribus late declivibus rugulosis et ad marginem spinis minoribus 2 armatis (his ad apicem retrorsum curvatis) ; elytris sparsim distincte punctulatis et obsolete 3—vel 4—costatis apice suturali breviter spini- formi; antennis quam corpus paullo brevioribus ; pedibus inermibus, abdomine subleevi, sed segmento ventrali apicali (hoc in medio leviter emarginato) sparsim punctulato. Long., 12 1.; lat., 44 1. I feel some nesitation in referring this species to Catypnes owing to discrepancies between the utterly insufficient original diagnosis of Mr. Pascoe and the fuller subsequent one of M. Lacordaire. For example Mr. Pascoe asserts that the eyes are “nearly entire” while M. Lacordaire calls them ‘assez fortement échancrés.” The insect before me, however, agrees very well with M. Lacordaire’s diagnosis ; and therefore it would be un- justifiable (at any rate without examination of the type, which is of course impossible for me) to found a new genus for it. It is fortunately a species which can be distinguished from nearly all the other Australian Prionides by the combination of a very small number of its characters, viz., “sides of the prothorax not denticulate or crenulate but each bearing two well-defined spines, eyes strongly emarginate (almost exactly similar to those of T'oxeutes), antennee shorter than the body with basal joint very much shorter than the third, hind tarsi with basal joint shorter than the third and fourth together, third joint of the tarsi very deeply bilobed and spongiose beneath, legs extremely smooth and nitid without any denticulations, head (at least in the male) taansverse and very large. The present species is readily distinguishable from C. Macleayi, Pasc., by the sides of its prothorax having only two (not three) spines. The prothorax of this insect bears a remarkable resem- blance in outline to that of Zoxveutes arcuatus, Fab., but with its lateral spines very much smaller and (though directed hindward) scarcely arched. Western Victoria ; presented to me by Mr. Jung of Yorketown. 59 TYPHOCESIS. T. adspersa, sp. nov. Brunnea, capite prothoraceque obscuriori- bus, elytris dilutioribus, squamis piliformibus niveis (his in prothorace plus minusve lineatim, in elytris ut macule numerosz minute et fascia linearis vix antemediana, in abdominis segmentis singulis ut fascia apicalis, in partibus ceteris disperse, dispositis) vestita; setis gracilibus erectis vel suberectis sparsim instructa ; capite obscure punctulato ;. prothorace supra sat deplanato, grosse ruguloso (exempli typici disco hic illic quasi ab indumento sculpturam tegenti instructo), lateribus in medio fere parallelis apicem versus rotundato - angustatis pone medium subito fortiter arcu emarginatis (sicut certo adspectu pone medium dens magna videtur); elytris ad basin rectis, basin versus sat crebre fortius rugulose (retrorsum gradatim magis sparsim magis obsolete) punctulatis, lateribus postice gradatim leviter con- vergentibus, apice singulatim rotundato - subacuminato, humeris rotundatis subcallosis. Long., 73 1.; lat., 24 1. The specimen described is evidently a male, its antenne being considerably longer than the body, but they are devoid of the cilize with which in the other species of the genus the basal joints of the male antenne are clothed ; joints 3-7 are armed with a fine spine at their apex. There is a second specimen evidently a female of the same species, as its antennez are scarcely longer than the body, but it differs from the example described in being entirely black, but with exactly similar snow-white scales simi- larly disposed. It differs from the described specimen also in its prothorax being evenly rugulose instead of having some of the rugulosities on the disc obliterated by what looks like (but is not) patches of some extraneous indumentum. The markings on the elytra are almost absolutely the same as those on the elytra of Zygocera pruinosa, Boisd., the post-median fascia however being absent and the anterior fascia running from the suture obliquely hindward instead of forward. N. Queensland ; forwarded by Mr. French. ISCHIOPLITES. I. metutus, Pasc. Mr. French of Melbourne has forwarded to me two examples, which he tells me were taken in N. Queens- land, of an insect that seems to agree perfectly with the descrip- tion of this species. It is possible that a comparison with the type might reveal differences but I can find none to distinguish it from the description, which is a fairly detailed one. ILLENA. This genus is an enigma to the Australian coleopterist. I 60 should feel very thankful if some coleopterist in Berlin would do me the favor of procuring one of Erichson’s types for me to examine (which might perhaps be possible if the specimens in the Museum are fairly numerous), or failing that examine the type and write me a description of it, especially indicating the nature of the armature of the prothorax which in one place Erichson calls “lateribus medio obsolete nodosus ” and in another speaks of as being furnished “lateribus pone medium tuberculo parvo.” Pascoe described a genus WVeissa as resembling what Illena must be, but no doubt distinct from it because furnished with a spine on either side of the prothorax. Subsequently I suggested (P.L.S.N.S.W. 1889, p. 455) that Erichson’s ex- pressions are not consistent enough to warrant this conclusion and expressed the opinion that Weissa and Jllena are probably identical. Subsequently still, Mr. Gahan [Tr. E.S. 1893, p. 196] mentioned his having seen an insect named (by M. Chevrolat) I. exilis, the prothorax of which was spined laterally and added the information that Mr. Walker had found examples of it in Tasmania (Erichson’s locality). Recently my opinion on the matter has been somewhat shaken by the examination of a minute Longicorn (taken in N.S. Wales by Mr. Lea) which seems to agree much better than Wezssa does with Erichson’s descrip- tion of Zllena ; indeed I do not find any character on which this insect could be definitely stated to differ from that description provided the diagnosis of the prothoracic armature be accepted as ‘“lateribus medio obsolete nodosus” rather than the other diagnosis which implies the presence uf defined lateral tuberctes. As regards Mr. Lea’s insect as a species it must be very like, if not identical with, Erichson’s species; and although the great difference in locality would suggest the probability that if Erich- son’s type could be compared it would prove distinct, I deem it better to regard this insect pro tem. as “ Illena exilis, Er.?” and suppose that the species is widely distributed. 61 NEW FACTS BEARING ON THE GLACIAL FEATURES OL ALL ETT’S Cove. By W. Howcuiy, F.G:S. [Read April 3, 1895. ] A scientific investigator in looking for one thing often unex- pectedly stumbles on another which proves of greater interest than the primary object of his search. Eighteen years ago Pro- fessor Tate went to Hallett’s Cove to look for shells. He was disappointed in the objects of his visit, but discovered the ice- polished surfaces on the cliffs which remain to this day the finest examples of their kind in any part cf Australia. The announce- ment then made of glacial action at sea level in the latitude of Adelaide was met with incredulity not only from the public, but also from many scientific men, who without seeing the evidences prejudged the conclusions from a distance. Competent judges, however, when taken over the ground, without exception, con- firmed the discoverer’s diagnosis; and the interest with which this locality has come to be regarded by the geological world has rapidly increased, and Hallett’s Cove must now be ranked as classic ground in Australian geology. The meeting of the Australian Association for the Advance- ment of Science, in Adelaide in September, 1893, presented the opportunity for a large number of scientific men from the other colonies of verifying the evidences, and through the generosity of the President of the Association, what was called by Sir James Hector “the largest scientific excursion ever held in the Southern Hemisphere” made a pilgrimage to the spot. The evidence of ice action was taken by all present without a doubt and as over- whelming in its conclusiveness. There was the polished and grooved pavement extending at intervals for two miles along the top of the cliffs, and occurs alike on the basset edges of the purple shales as well as on the harder quartzites. There was also noted a limited quantity of morainic material, with scratched stones, resting on the glaciated platform, together with larger transported blocks at the southern end of the Cove. There was no difference of opinion on the main facts. The discussion among the geological experts was directed almost exclusively to the question of the age when this extensive glaciation occurred. Some defended the view that the glacial features did not pass under the Miocene escarpment, which at this point overlies the Archean 62 shales and reaches in its talus within a few yards of the edge of the cliffs. This view supposes that the morainic matter was marginal, and that instead of passing beneath the Miocenes was banked up against the face of these beds. If this could be demonstrated it would follow that the glaciation had taken place after the Miocene deposits had been laid down, and, hypothet- ically, synchronous with the great glacial age of the Northern Hemisphere in Pleistocene times. Other of the visitors held this hypothesis to be improbable, (1) on the grounds that the geological interval was too brief to account for the enormous change in the physical features of the country which must be assumed in the extinct glacial valley, and that the direction of flow, which was opposed to the present lines of drainage. (2) It was considered that the soft clays and sands of Miocene age must have been swept away by the erosive force of an ice sheet that had the mechanical energy to plane down metamorphic shales and quartzites. The question was considered of so much interest that the Council of the Association determined to set aside the sum of £20 as a fund to be devoted to works of exploration, and by this means demonstrate whether the glacial features were Pre- miocene or Post-miocene. Professor Tate and the writer of the present paper were entrusted with the duty of carrying out the explorations for this object. Valuable aid was given by Prof. T. W. E. David, the General Secretary of the Glacial Research Committee, who in December last visited Adelaide with the express purpose of assisting in the investigations. Mr. L. Birks, B.Sc., of Adelaide, was also present throughout the examination and rendered important help. The first practical step was to obtain permission of the pro- prietor of the ground, Walter Reynell, Esq., J.P., to carry out the necessary operations. Mr. Reynell not only readily gave his permission, but supplied several workmen and tools to do the pick-and-shovel work. Three days were spent on the ground. The first was devoted to a general survey of the features under the guidance of Prof. Tate. The second and third days were spent in working up the details and in mapping the boundaries of the glacial deposits on the north side of Field River. Prof. Tate was unfortunately called away by urgent business and was unable to remain for the last two days’ work. EXPLORATION. The point to be determined was—On what do the Miocene beds of the locality rest? Do they lie immediately on the de- nuded edges of the Archean metamorphic shales? Or are the 63 Miocene and Archean formations separated by a wedge of glacial till? The first trial was made near the northern limits of the glacial area and at a point where the base of the Miocenes is distinctly marked by a shelf of calciferous and fossiliferous sand- stone. Beneath this hard shelf of rock was a softer bed of doubtful character. A tunnel was cut for a foot or two into this underlying bed, which proved to be an arenaceous clay of a greyish color, and was seen to pass beneath the Miocene beds in an undisturbed condition. This was the first important item of evidence. We had found a bed which could not be classified either with the Archzans beneath or the Miocenes above. To expose the beds still further a trench was cut in a vertical line with the tunnel, but lower down the escarpment. The same beds as seen in the tunnel were proved in this cutting, unaltered in character, but alternating in color from red to blue or grey, and intercalated with sand bands. No junction was proved at this spot between the stratified glacial beds and the underlying Archeeans, as a considerable talus blinded the latter. A little to the south of these trials is a well-marked valley which runs due east for half a mile. This valley is excavated in a thick deposit of glacial till, carrying numerous scratched stones and erratics. One large block of coarse-grained granite measured three feet long by two feet wide. Near the western outlet of this valley the Archzeans have been exposed by denudation and exhibit polished and scratched surfaces, covered by a bare and sloping bank of morainic matter. Scratched stones were plenti- ful in this clay. Work was begun at this spot to establish the conjunction of the glacial deposits with the Miocene base, but after a short trial it was discontinued, as a thick talus of Miocene debris was found covering the face near the point of junction. A third spot was selected about midway between the valley just referred to and Black Point, where the Miocene ledge ap- proaches nearest to the edge of the cliffs. The Archzans were seen to outcrop at the base of the hill, but without glaciated surface, whilst the Miocene ledge occupied the crest of the hill. A distance of about a dozen yards separated the two points. On laying bare the Archean surface, the purple shales exhibited a highly glaciated face, having a steep inclination landwards, and the glacial clay was seen to be in direct contact with the polished surface. The trench was continued, vertically, until the uni- formity of deposit between the Miocene base and glaciated pave- ment was demonstrated, the lithology of the beds agreeing en- tirely with those exposed in the first trench. The results ob- tained were considered the quod erat demonstrandum of the in- vestigations and rendered any further exploratory work needless. 64 THe GuactaAL Beps. These are strongly marked off from the Archeans, on which they rest by a horizontal, or approximately horizontal stratifica- tion, as well as essentially distinct lithological character. They are also distinguishable from the overlying Miocenes in possess- ing a thinly-bedded or laminated structure, the clays are more tenacious, they frequently contain striated stones and erratics, and are separated from the Miocenes by a strongly-marked divisional plane. The line of division between the two forma- tions gives evidence of unconformability in the eroded surface of the till and the presence of water-worn boulders, which often occupy the line of junction. The glacial deposits thin out to the north, about half-a-mile from Black Point, where they are about 20 ft. thick, beyond which point they have not as yet been proved. They maintain an approximately uniform thickness on the top of the cliffs, but suddenly thicken within the limits of the Cove, attaining a maxi- mum thickness in “Trig Hill,” as measured by the aneroid, of 112 ft. The hill just mentioned is central to the amphitheatre of the Cove, and was a convenient point from which to take the trigonometrical readings. The glacial beds were traced from this height uninterruptedly (except where covered by blown sand) down to low-water mark. On the southern half of the Bay a steep escarpment rises to a height of 90 ft. facing the sea, and is composed throughout of boulder clay with erratics. The same beds are continued on the south side of Field River at a similar height, the river occupying a valley of erosion that has been cut through the glacial beds. How far these deposits extend seawards, and below sea level, are problems that remain to be solyed. As so little money was spent on the late explora- tions, perhaps the Council of the Association for the Advance- ment of Science may think fit to make another grant, that the thickness of the beds at sea level may be tested. LITHOLOGY OF THE BeEps. The beds which have been laid down within the glaciated area may be roughly classified as mudstones, friable sandstones, and conglomerates. The two trenches that were cut passed through the upper series of beds, and exposed alternating beds of reddish and grey clays, with soft sandstones of a yellowish color. These beds are distinctly stratified, and the materials uniformally fine, no stones, indeed, of any kind were met with in the trenches. A little further to the south, where the beds thicken, a dark- colored mudstone, with sandy layers and inclusions, is met with, and is highly charged with facetted and scratched erratics. This can be noticed ina thin layer on the top of the Black Point 65 Cliffs, but is best seen in the basal portions of the amphitheatre of the Cove, as well as in the escarpment on the southern side of the Bay, and upon the beach between tide marks. The mud- stones, where they have not been exposed to the weather, are very compact and tough, and split into thin bands and cubical fragments. Thin layers of sand occur in the mudstones, and it is along the lines of these sandy partings that the rock usually splits. The sand grains are rounded, and exhibit the effects of considerable attrition, but the sand-beds are but slightly consoli- dated in mass, and do not, as a rule, split on lines of bedding. The conglomerates are best seen on the beach at low water, where they stand up as weathered bosses, excavated from the surrounding clays by the action of the waves. On this floor of marine denudation numerous joints are seen to run irregularly through the glacial till, and are rendered conspicuous from their being filled with a dark-colored ferruginous material. BOULDERS. If any confirmation were needed that we are face to face with glacial phenomena at Hallett’s Cove, it is found in the innumer- able, subangular, facetted, and scratched erratics which occur abundantly at the lower levels of the Hallett’s Cove beds. As already stated, no stones of any kind were met with in the two experimental trenches cut through the beds on the northern side of the area. This may have arisen from the shallowness of the trenches and the small extent of rock exposed. The boulder till is first seen on the northern boundary of the area in the banks of the east and west valley, and on the top of the cliffs a little to the south of the principal polished face of rock. From the latter position a goodly number of striated stones have been obtained. From that point, southwards, they become con- spicuous in all exposed surfaces, and can be found from the size of small pebbles, up to large masses many tons in weight. Several huge erratics occur on the beach, near the centre of the Bay, whilst on the south side of the Field River they cover the beach within tide marks, and are of great variety, as well as innumerable. It is a common feature to observe a layer of boulders at the junction of the glacial beds with the overlying Miocene, and in some instances these boulders are included in the lower part of the Miocenes themselves. They have the facies of glaciated stones, and in one or two instances I could detect the strie distinctly preserved on their surfaces, although the wash they have been subjected to at the time of the encroachment of the Miocene Sea has no doubt obliterated the surface features from many of them. A large enclosure of metamorphic shale, in the same position, measuring twelve feet in length, has attracted E 66 the attention of scientific visitors to the Cove. There is now no doubt that this immense fragment has been transported and placed in its present position by the agency of ice. One of the striated pebbles placed on exhibit is of interest, as taken by the writer from near the top of the “Trig.” Hill, 112 feet above sea level. Many of the erratics have no doubt been derived from the Archeans of the neighbourhood, but there are a great many that are unrepresented by any rock now known in situ for many miles, and proves that the ice must have been more than of local extent. I fear that we have too little data at present to locate these travelled stones with regard to their source. To do this effectively would involve careful petrological examinations—a promising field of research that is awaiting some competent student in this department. SUPERFICIAL AREA OF THE GLACIAL DEPosITs. Fortunately two little streams cut the glacial beds through their entire easternly extension, one on the north side of Black Point, and the other to the south of that landmark, so that the area of this fragment of glacial action can be mapped with ap- proximate exactness. By following up the beds of these streams it was found that the glacial deposits extended about half a mile from the coast line, passing not only up the main, but the lateral valleys, and thinning out as the higher altitudes were reached. In the most southernly of these two streams the limit of the beds was reached near the old sheds, well known as the usual camping place for picnicers in visiting the locality. In restoring the glacial area we must imagine the outline of the Cove in preglacial times to be that of a comb or saucer-shaped depression on the flanks of the Archean hills. The ice sheet, moving from south to north, filled this lateral depression and passed over the minor heights on its northern and southern limits. A depression of this kind on the flanks of a glacier would supply the most favorable condi- tions for the accumulation of a ground moraine, and its contents would also be subsequently protected from the erosive forces by the wall of hard rock with which it was nearly surrounded. The deposition of the Miocene beds over the same area in later times would still further help in preserving this remarkable outlier, the Tertiary beds acting asa protective cover that has remained to the present day. THE AGE OF GLACIATION is a most interesting, although difficult, question to solve. The beds in question rest upon rocks of Archzean age, the most ancient of the sedimentary series, and are capped by Miocenes, one of the newest of the geological formations. They may, therefore, be 67 of any age between these geological landmarks. But the time limitations are here so enormously distant from each other that they serve little purpose in fixing the date of the intermediate deposits. We can only fall back on analogies, and establish a synchronism, if possible, with the glacial deposits of other localities that offer the nearest resemblances to the beds in ques- tion. As the glaciation must have taken place before the Miocene beds were deposited, it is out of the question to refer this refrigeration of the Australian climate to the so-called Glacial Period of the Northern Hemisphere, which took place in Post-Tertiary times. In conversation with Sir James Hector, on the occasion of his visit to the spot, he suggested the possibility of the glaciation being of Cretaceous age, and stated that there were enormous glacial deposits of this age in New Zealand. I am not aware that any indications of glacial action have been observed with regard to the Cretaceous beds of this continent, There are, however, abundant evidences of a glacial period of great intensity which occurred in South-Eastern Australia during Permian, or Permo-Carboniferous times. Near Bacchus Marsh and Derrinal, in Victoria, there are glacial beds (sometimes seen to rest on polished and grooved pavements) that can be traced over hundreds of square miles, and must be several thousand feet in thickness. Having recently visited the Bacchus Marsh District, I have been able to place on exhibit, for comparison with the Hallett’s Cove material, a series of specimens from the Victorian beds. The close resemblance between these two sets of exhibits will be appreciated by all. The Bacchus Marsh beds appear to have suffered more disturbance than the Hallett’s Cove beds, as they dip almost uniformly at about 42° They con- sist of alternating beds of mudstones, thickly studded with glaciated boulders, sandstones, grits, and conglomerates. Many of the beds exhibit fine laminz along the lines of stratification, and at other spots are locally much distorted, as though ploughed up before the ice. In lithological features they closely resemble the Hallett’s Cove mudstones, sands, and conglomerates, but are more highly indurated, and in this respect have more the facies of rocks of Upper Paleozoic age. The sandstones particularly are often highly siliceous, and in one case, in the Wirribee Creek, there occurs a band of hard quartzite (a specimen of which is on the table). The age of these glacial beds of Victoria has been determined by the remains of Gangamopteris, a fossil fern char- acteristic of Permo-Carboniferous age, which occurs in consider- able numbers at one or two horizons intercalated with beds of glacial origin. The importance of these glacial conditions in Permian times is accentuated by the fact that deposits which seem to require ice action to account for their existence, are 68 found of this age in such remote places as Great Britain, India South Africa, and Australia. It is possible that further search in the Hallett’s Cove beds may bring to light some fossil remains that will definitely fix the date of their deposition, but at present analogy seems to point most strongly to the conclusion that the Bacchus Marsh and the Hallett’s Cove formations belong to the same geological age. The Victorian beds rest on Silurian, or on granite, and, like the Hallett’s Cove beds, are capped by Tertiaries. THe InmMAN VALLEY SHALE. Since the late important discoveries at Hallett’s Cove, it has occurred to me that there may possibly be some relationship be- tween the glacial beds of the latter and the mudstones which occur in an isolated patch in the Inman Valley, The peculiarity of this formation attracted the attention of Mr. Brown, the Government Geologist, who thought it might be an outlier of the Jurassic rocks of the Leigh’s Creek district, and under his ad- vice the Government has bored through nearly a thousand feet of these beds prospecting for coal without reaching the bed rock. Evidences of glacial action are not wanting in this district. Granite boulders of great size can be traced from the Bluff, as a radiating centre, up the Inman Valley for miles. As far back as 1859 Mr. A. R. C. Selwyn reported as follows :—‘‘At one point in the bed of the Inman I observed a smooth striated and grooved rock surface, presenting every indication of glacial action.” Al- though this spot has, unfortunately, not been rediscovered, it is not likely that so good a field geologist as Mr. Selwyn should have been deceived in his observations. Mr. H. Y. L. Brown in his report (1892) describes these undetermined deposits in the follow- ing terms :—‘“ This formation consists of a jointed shale, varying in color from a bluish-green to black, and interstratified with them there are undulatory beds of sandstone and quartzose sand- stone, and occasionally limestone of irregular thickness. The upper portion of this shale, which in some places exhibits a con- cretionary structure, has become decomposed into clay, and con- tains water-worn pebbles and boulders of granite, quartzite, sandstone, ironstone, &c. Some of the boulders of granite are of great size, and in character resemble the granite of Victor Harbor.” I think from the evidences before us it is not impro- bable that these anomalous beds of the Inman Valley may prove to be of the same character and age as the Hallett’s Cove and Bacchus Marsh glacial formations. THE SOURCE OF THE ICE. A word may be said, in conclusion, as to the probable source from whence the ice originated. In view of the extremely low 69 latitude of Hallett’s Cove, which agrees with North Africa and the southern shores of the Mediterranean in the opposite hemis- phere, we might have fallen back on the iceberg theory if the features had been reconcilable with such an hypothesis. This, however, is inadmissable. berg ice could not possibly polish and groove hard rocks over extensive areas, whilst maintaining definite lines of erosion and striz, such as occur at Hallett’s Cove. The polished floor near the coast is indeed a huge roche moutonnée in the form of a ridge, with an elevation of about 20 ft., presenting uniform lines of glaciation on all sides. I am led to think that only terrestrial ice of great thickness and operating through a long period could produce effects such as have been referred to. Again, as far as can be judged at present, the morainic matter has been gathered from local, or at least South Australian, sources. Moreover, most of the beds are distinctly stratified (which could scarcely be expected of iceberg debris), and in their deposition show thin, alternating beds of different lithological character indicating the presence of water operating under quiet conditions. Lastly, in the absence of organic remains the proof is wanting that the Hallett’s Cove beds are of marine origin, for whilst many of the clay bands are eminently adapted for the preservation of such, no fossils have hitherto been discovered in them. The land plants of the Bacchus Marsh beds seem to point to fresh-water conditions in analogous formations in the adjoining colony, and I should anticipate a greater probability of finding similar remains in the Hallett’s Cove beds than a marine fauna. There seems to be only two suppositions which could offer adequate conditions for the glaciation of Southern Australia. Hither a much higher altitude of the land, with the main moun- tain systems restored to the height they possessed before suffer- ing the waste undergone during the enormous period separating Paleozoic times from the present ; or the extension of the Ant- arctic Continent and ice-cap into lower latitudes, with the physi- cal contour of the land such as to deflect the Antarctic currents to our shores, so that Southern Australia would be climatically much nearer the Southern Pole than it is to-day. Either of these factors—or, perhaps, both conjointly—may have supplied the efficient cause of that refrigeration of climate in South Aus- tralia, the evidences of which we have discussed to-night. 70 PETROGRAPHICAL OBSERVATIONS UPON SOME SOUTH AUSTRALIAN ROCKS. By J. Cottetr Mouupen, Associate Royal School Mines, London. Communicated by J. East, F.G.S. [Read May 7, 1895.] Through the kindness of Mr. J. J. Hast, F.G.S., Registrar of the School of Mines and Industries, Adelaide, I have been enabled to examine a small series of rocks, chiefly South Aus- tralian, from the collection of that Institution, and the following observations on them may prove of interest. In each case, thin sections for examination under the micro- scope were cut, and the component minerals of the rock, its nature, structure, and texture were examined. The sections number 20 in all, and some possess many points of interest. The contributions to the Petrography of South Australia have, in the past, been very meagre—the harvest indeed is rich but the reapers few—and the few notes herewith appended will, I hope, merely serve to point out the great desirability of such work being actively pushed forward in the near future. I wish it to be quite understood at the outset that these rocks have been named on petrographical grounds, combined with a microscopic examination of the hand specimens. I have, un- fortunately, at present, no opportunity of studying these examples in the field, and knowing what a terrible stumbling- block in geology the nomenclature of rocks is, one may easily conceive that some of the names may have to be slightly modi- fied after an examination of the rocks im situ. Even under such circumstances the names to be applied to them is greatly a matter of individual opinion. The localities of the rocks are mostly well known and authen- ticated—some, indeed, were personally collected by Mr. East— and these circumstances render it the more desirable that reliable information should be forthcoming concerning them. In some cases the specific gravity of the rocks was taken by means of a Walker’s balance. I. OutvenE Basatt, Mount Eden, Auckland, N.Z. The rock consists of plagioclase, olivene, and magnetite in grains, with a fair amount of augite. The olivene is fresh, gives the usual splendid polarisation-colors, and has the usual irregular (i cracks. The plagioclase is in lath-shaped crystals in the base. The olivene crystals are corroded by the magma. The felspar microliths in the base show the flow-structure well. The augite encloses some dark grains, undetermined. The whole mass is rather scoriaceous in character, so the specific gravity was not determined. It is quite a typical olivene basalt. II. Oxnivenrt Basatt, Mount Gambier, S.A. The minerals composing this rock are—Olivene in rounded grains, cracked and a good deal corroded by the magma ; they are fresh and clear. Augite of a brownish-green color, fresh and giving good polarisation colors ; it is allotriomorphic. Plagioclase Jelspar in lath-shaped clear crystals in the ground mass. Mag- netite is plentiful in the usual black grains scattered throughout the mass. The sp. gr. of the rock =2:°73, which is rather low due perhaps to the presence of cavities and gas-holes. It isa fine grained typical rock, and shows flow-structure. III. Oxrivene Basatt, Kangaroo Island. This exceedingly interesting rock consists of plagioclase felspar, both as porphyritic crystals and as the usual laths in the base. The former at times show most beautiful zoning and inclusions, with the usual lamellar twinning of plagioclase. Augite is plentiful. It is, curiously enough for a basalt, quite clear and colorless, and well-twinned in some crystals, while others exhibit good “ hour-glass” structure. Owing to its being colorless and having such a high refractive index, it is not always easily to be distinguished from some of the olivene present. Olivene occurs as fresh and clear grains corroded by the magma, while magnetite is abundant in the usual black grains. Felspar and augite are the most abundant constituents, then olivene, and lastly magnetite. The rock is typically ophitic in structure, and there is a good deal of glass of a dirty brown-green color in the base, which is quite isotropic. The rock is a very basic one in character, as may be guessed from the mineral com- ponents, and it has a sp. gr. of 2°88. The rock is not holocrys- talline, but it has otherwise rather the character of a dolerite (ophitic), but I have called it a basalt since I have no informa- tion as to its field occurrence, but since the specimen was labelled ‘‘Columnar Diorite,” I presume it must exist as a lava flow. If, however, it occurs as a dyke-rock, dolerite might per- haps be applied to it as a name rather than basalt. This seems to have been the rock noted by Dr. Chas. Chewings.* The most important and perhaps also the most valuable feature of this *“ Beitrage zur Kenntnis der Geologie Siid und Central Australiens” (Petrographischer Anhang.), Heidelberg, 1894. 72 rock is that it is gold-bearing. The hand specimen in my pos- session shows a small speck of metallic gold imbedded in it. I do not know whether I am correct in so saying, but I believe this this to be the first recorded occurrence of gold in a volcanic rock for South Australia. Whether it really occurs as an original constituent or not it would be impossible to conjecture from the evidence at my disposal, but the field-occurrence is at least well worth an investigation. Supposing that it is not an original con- stituent, it is easy to understand how a lava flow in passing over auriferous sands or gravels might catch up and include some of the gold, as has been the case with the zircons occurring in the basalts of the Eifel District in Europe. On the other hand, if the basalt occurs as a dyke-rock,* the dyke may have inter- sected an auriferous quartz reef and caught up some particles of gold or-auriferous quartz. The quartz, in the presence of such basic materials as compose this rock, would be corroded and finally dissolved away, leaving the gold as an included speck. It is curious that the speck should occur in such a small hand speci- men as J have, the dimensions of which are not greater than about 24” x 14” x 2” The rock is fine-grained and compact. Another point of some interest is that, although it is a basalt, still the magnetite in it is not large in amount, and most of the minerals composing it are colorless, or nearly so. On one edge of the specimen and in one or two other places there are some reddish-brown clear minerals of high refractive index, which appear to be either garnet or zircon. As they do not appear in section it is very difficult to say which. The specimens of this mineral are not large, but are quite easily seen by the unaided eye. IV. AxinitE AMPHIBOLITE, Rosetta Head, S.A. This is a very much altered rock, which consists mainly of hornblende and a perfectly colorless awgite, the former largely pre- dominating. Some biotite is present in minute crystals, with quartz and chlorite as accessories. It has been much altered, as evidenced by the chlorite, &c. The one great point of interest in this rock is the presence of a considerable amount of the mineral axinite as a rock-forming constituent, which occurs not only as allotriomorphic grains but also as idiomorphic crystals, which in section give most perfect lozenge or hatchet-shaped sections. In one part of the hand specimen there is a small druse or cavity, * This rock was observed at Kingscote by Prof. Tate in 1881 and in the Freestone Range in 1883 ; it was reported a diorite intrusive in mica-schist in Trans. Roy. Soc., S.A., vol. vi., p. 122, 1883, and in the accompanying geological map its course is laid down, though by inadvertence was not prolonged to the sea-cliff at Kingscote.—[EDITOR. ] 73 wherein there are some of the most beautiful and characteristic sharp-edged triclinic crystals of axinite of a brown-violet color, and whose edges, where broken, exhibit the curious serrated fracture of that mineral. These crystals are, roughly, from 2” to }” across. In the section they are very pleochroic. Many of them show cleavage cracks parallel to 010 (xc P&) and the polarisation-tints are not high. If it occurs, as I imagine, in contact with the granite, which forms Rosetta Head, it can easily be understood that the conditions would be favorable to the occurrence of axinite. Jam not aware that axinite has before been recorded for South Australia, though Liversidge [‘‘ Minerals of New South Wales,” p. 183] has recorded it for that colony. The zircons seen in the section of this rock are very good. Taking it on the whole, axinite-amphibolite seems the most suitable name for it. The augite is frayed and bent in places. V. Eprpote Rock, Wooltana, Far North Ranges. Epidote of a greenish-yellow color and with high refractive index, for the greater part, composes this rock, which is exceed- ingly compact, fine-grained, and has a sp. gr. of 3:18. It seems rather altered and does not show much pleochroism. The hand specimen on one side shows some of the characteristic pistachio-green epidote. Magnetite in irregular grains is scattered throughout the mass There is a mineral, probably secondary quartz, filling up interstitial spaces. In mass it is of a very dark-green color and heavy. In the section the epidote appears to be quite granular, and it makes up by far the larger part of the rock, which seems to present no particular feature of interest. VI. ALTERED AMPHIBOLITE (with Epidote), Hale River, lat. 23° This is composed chiefly of hornblende, with the usual 120° cleavage cracks ; some of the hornblende is twined. It contains also a good deal of hornblende altered to chlorite and epidote. The epidote fills up the cracks. A little secondary augite is present. Some parts of the section appear greatly clouded. Its polari- sation-colors are most beautifully bright and the whole mass is greatly altered. The sp. gr. =3:10. It is holocrystalline and the texture inclines to coarse. It is an amphibolite which has undergone change. VII. Atrerep Diorirse, Hale River, lat. 23° 40’ S. This rock is a diorite, which has been somewhat altered. It is composed of hornblende, showing splendid cleavage cracks inter- 74 secting at about 120°. Some of this mineral has undergone chloritic change. Plagioclase polysynthetically twinned and altered ; epzdote in fair grains as an alteration product ; secondary colorless awgite, sparingly ; secondary quartz, which is very clear and contains liquid enclosures; and apatite which is rather abundant in grains. Some sphene is also present as an accessory. It has a sp. gr. of 3:03. The whole rock has been a good deal crushed and indicates a tendency to become schistose. . VIII. Aucen Gneiss, Florence River “Ruby” Field, Central Australia. This gneiss is composed of a good deal of biotite, which is very pleochroic ; plagioclastic felspar, beautifully twinned and clear, the twin lamelle show intense strain and bending, and in fact the whole rock has been much strained and shorn; quartz, forming a mosaic with felspar ; mzcrocline containing apatite (?) as needle-like inclusions; garnets of a clear pink color, surrounded by bzotite and some greenish alteration products; epidote(?) with high polarisation colors. The garnets are isotropic. Some of the felspar contain some ramifying masses of calcite as a secondary infilling. A little rutile is present as an accessory constituent. The rock has a sp. gr. of 2°75 and has a perfectly gneissose structure. Zirconsin small crystals are present, as is often the case in these rocks. It is an augen-gneiss with garnet. IX. GARNETIFEROUS GNEISs, from same locality as No. VIII. The minerals present are as follows:—Plagioclase felspar, showing splendid lamellar twinning ; one piece shows both the albite and pericline types combined; it is fairly clear. Ortho- clase felspar is present ; quartz in plenty, also as an inclusion in the garnets present ; biotite in plenty; garnets of a beautiful pink color are abundant in the slide and hand specimen, they are irregularly cracked across and are full of cavities and inclusions, are quite isotropic and show no anomalous optical characters. Rutile is present as an accessory mineral ; crystals of light yellow and of a dark red are present, both as simple prismatic forms and as geniculate twins. The geniculation angle of one of the latter was found to be 114° 30’ (this angle is given by Rosenbusch as 114° 25’). In some cases the rutile occurs as an inclusion in biotite, while in one case it occurs in garnet. Apatite occurs, both as fairly large prisms in felspar and as long needle-like forms ; zircon is moderately abundant as an accessory in small colorless crystals with dark borders, due to the high index of refraction. The whole rock is typically metamorphic, has a sp. gr. of 2°83 and is rather coarse-grained. 75 X. SyenitE Porpuyry,* Yardea, Gawler Ranges. This rock, which has been a good deal altered, is composed of a felsitic ground-mass of a brown color, in which occur porphyri- tic crystals of felspar, greatly altered and clouded. This felspar polarises in low tints, and much resembles soda-orthoclase. Augite is present as a porphyritic constituent, the crystals of which have been much altered, with separation of brown iron- oxide, especially along the cleavage cracks. There is a blue mineral, with high refractive index and quite unaltered, present in the ground-mass in tiny granules, which I have not been able to determine (corundum ?). Agatite is present as an accessory. The felspars show secondary growth very well. The rock has a sp. gr. of 2°63, is very hard and compact, and tends to break with a splintery and rather conchoidal fracture; it may be an anorthoclase syenite porphyry. XJ. Biotire Granite (from an erratic boulder), Hallett’s Cove, S.A. This rock is a coarse-grained granite. The hand specimen is a small one and rather weathered. It consists of felspar, ortho- clase, with a little plagioclase, cracked, clouded, and altered ; quartz in plenty, containing liquid cavities ; biotite, a good deal altered and darkened. The texture is coarse and the structure typically granitic. XII. Coarse MuscovirE Granite (Pegmatite), Mount Gawler, near Port Lincoln, S.A. This is a much decomposed rock of a very coarse texture. The felspar has nearly all passed to kaolin, the plates of musco- vite are turning silvery-white, and losing their transparency and elasticity. The quartz is abundant and, of course, unaltered As this rock was so decomposed and presented no particular features of interest, no section was cut, but the foregoing notes were made from an examination of the rock specimen itself. It is an exceedingly acidic rock. XIII. Brorire Granite (red), Murray Bridge, S.A. This granite, which is coarse-grained, consists of orthoclase and mcrocline, the latter showing microperthitic structure; plagio- clase well-twinned in lamelle ; quartz in large grains, which ap- pear smoky in the hand specimen and in the section are seen to be full of beautiful liquid cavities with moving bubbles. Biotite is present in fair amount. Apatite occurs as an accessory con- * Vide ‘‘ Report on the Geological Character of Country passed over from Port Augusta to Eucla,” H. Y. L. Brown, Adelaide, 1885. No quartz at all observable in my sections.—J.C M. 76 stituent; a basal section of this mineral shows the common hexagonal outline, the sides of which measure about 3,” in length. Quartz and felspar are intergrown, forming micrographic struc- ture. It shows no special characters beyond those noted, and is a typical granite, having a sp. gr. of 2°63. XIV. Granite (Grey), Monarto, near Murray Bridge, S.A. The section shows orthoclase in zoned crystals, mzcrocline with . the common “cross-hatching” well shown between crossed nicols. Some plagioclase felspar is likewise present. Quartz is fairly abundant and in some parts is intergrown with orthoclase, giving micrographic structure. Both biotite and muscovite are abundant and are intergrown. The biotite shows some pleo- chroic haloes around included crystals of zircon. Zircons are also present as inclusions in felspar and quartz, while apatite also occurs in some of the felspars. The hand specimen shows the rock to be fine grained and compact ; the structure as seen from the slide is typically granitic. XV.(A) Biotrre GRANITE (with Microcline and Sphene), Palmer, S.A. (Collected by the author.) This rock is a reddish granite and has a sp. gr. of 2°63. It consists of orthoclase, which has so intergrown with quartz in places as to give micrographic structure; microcline with very good cross-hatching visible between crossed nicols ; quartz is abundant and contains liquid enclosures. The felspars are clouded and altered somewhat. Avotite is in plenty and some of the pieces show pleochroic haloes around included crystals of zircon. As accessory minerals are present—zircon in moderate sized prisms ; apatite in prisms and larger sections; sphene and- ilmenite are pretty conspicuous, occurring sometimes together. The structure is quite granitic and the texture moderately fine. The plagioclase is, as usual, at once seen by reason of its prominent lamellar twinning. ie Si sae selipung pur seseysog Ay ‘pp ‘8 F "‘SLNAWASUAASIC, ""a/) ” ” O19 IF 0 OT 9ST SUOIZAIIOSGNG ,, 00 8st “ ws oe "+ Kgato0g [eAoY WoIy sZUBIDD ,, Ot 9T I = ct paemaoj JYSNoIg souryeg OJ, 2 ~8s 5: "SLUIHOAY “umd ‘C6-F68 UVAA AHL WOK SLENAWASHAYUSIGQT ANV SLdIgOayY CD LIPS PPL LL LS LIS IFS eeryvvvvvvswry srry ‘VIIVULSAV HLOOS JO ALAIOOS I1VAOU AHL AO NOILOUS SLSTIVHOLVN CATA ASTRONOMICAL SECTION OF THE Hoval Society of South Australia. THIRD ANNUAL REPORT. Since presenting the last Annual Report this Society has endeavored to forward the object for which it was founded, viz., the encouragement of a popular interest in the science of astronomy. The roll of membership has kept up, and is (notwithstanding unavoidable removals) slightly over that of last year. During the past twelve months five general meetings have been held, and the Committee met six times for the transaction of business. In the early part of the session a new departure was made by the introduction of a question box, the contents of which have provoked discussion on a variety of subjects, as “The effects of the tides on the earth’s rotation,” ‘‘ Non-luminous bodies in space,” “The methods by which terrestrial gravity is ascertained,” “ The latest method for determinating difference in longitude,” ‘“ The refractor and reflector telescopes,” ‘“‘The best method of con- structing a planisphere,” “The motion of the stars in the line of sight as measured by the spectroscope,” ‘‘ Method of determining the right ascension and declination of stars,” ‘‘ On the changes of gravity at different altitudes,” ‘‘ The dividing powers of the re- fractor telescope,” ‘‘ The way of deducing the progressional motion of the perigree from the time of perihelion passage and the longi- tude as given in the Nautical Almanac,” ‘‘ Why the moon ap- pears larger on the horizon than when at its highest altitude,” and “* Why stars scintillate and the planets do not.” In November last Mr. J. W. H. Hullett gave a paper on the ‘“‘ Determination of the Orbits of Comets and their Elements.” The astronomical notes have been published monthly and a copy sent to every member. Adopted at annual meeting held at Adelaide Observatory 24th September, 1895. C. Topp, President. W. E. Cueesman, Hon. Secretary. ‘tomnsved 7, “UOH ‘NVINSWUHHO “Ol “AN ‘COST “EG “Idag ‘quopisald “GdOk 0 SHLIGHTH9O “CHOld ‘qooIt0d pUNOF pue poyIpuy 665 8 & 66% hal nee nee ea “ puey UL VOURTe ,, Il me vine ey sie yueg Sssurarg ,, jehoy oy} 09 aaro pred suorydraosqng ,, el 9 — | a ( eae oe: ci agi uae nse ‘* qseleqUy ,, 0 0m —" ce yood-pavuyy pue pavogyprtq 45, 9g GEL oo” ae ay gy oy ‘* SUOTydIZOSqng ,, Loa O. & “hk ao es a eeeisOg ay “eo ; ‘ : ; ¥ oh , an we ; ah a ‘ an 4 ; Ro ie : 5 : i: > ee) r ‘ 4. 4 ‘ e > Pe es ‘ f ‘> ie! " ; ; te. 7 eu & i 5 m } j - 1 > 1 a & eo Ps ‘ % é Z bE a ¢ > 3 y t cs f ™~ ‘ , : 7 5 , 7 ‘~ < ; ‘ as : vs - AD ‘ si y 7. ON 6 i + - er. iz . : ‘ " rd - ; - i ae . ‘ VF Aas ’ 4 a ~ * : i 7" : i mF n° ri i 4 ee J aS , ms [ eae ir. 9 ; an) + * , - " yard ‘ ‘ t y oy, i 7 x > A ; f ; be % Ls nye 3 i fo SIN sate Se ene ce ee a ates ewe Had) Se ek Wy RDN EO ae cere Hele ae Vol. XIX. Plate VII. 7) Bie Yond y 4 Tt , rf : i Dan ? 5 ra F ; if id z : a yy a ba) | pecine AME 8 eile Sat ce a) . i] ’ - : oe Ag = = : . - 7 . - 7 ~ at * ‘ ws va', . \ pipe fe ; @ . : d A 3 o . " . \ 4 ‘ “ x ; " 7 Py 4 ‘ j - de . “* A . - ‘ ' “a s . . ce | . i rT 24 < A 1 re, i es ‘ 2 ag . ‘ * fi ~ ' 5 ‘ 4 a ee as ; Ma 4 LS . , * > . * ' : a ‘ ‘ € a “ * ~ : . a s a; 4 : a s ge ae ss —— : , ‘ ? . 4 be . : 5 7 ~ - , = 4 * ‘ if ~ > oe e "7 * te ; ‘ y - . . ~ t ~ _ - ' “ i i * ’ . a ’ ‘ : 2 ’ : i & « 1 . hh 5 6 —— 4 y * . ? 7 i - = é : 7 = ~3 “ 7 ’ : - a , - « - 7 i be hs - a x q ' ® . Aan f a é ace ° 1 . ¥ < 7 7 } . od ra z e' 2 u me ™ 4 J e e tem 4% -~ a « ‘ te é a .@ . 2 , é a “3 . ' ¥ . - Pp . - - * ~ - oe - - ; * ae Sed a i “ ay Se pa . ' : uN * 7 " af - : ® , t i PASS as . af A a! —— ¥, Ay P : t) 4 ¢ f =3 , : A . cae Ff a ‘ any on \* ‘ (viv ) ae . — ’ ’ L's \ “ he Vie ¥ ' ? - va PY F : - wy & pea, OD ped 4 o id r Se é Z A ) 7 ra Y § : (ey , 2 j _ ad bart Vn ‘a 5 — ~~: pty J : wane > CO nt ee ae na a a a ee aS ewnemat a ee he ¥? zm ™ ~ Vol: XIX, Plate VEIL he tri ttrthees Cp 1 ij hi i n i: j al (y és ‘ik i is ya ©, * Aone % a \ r - d ws i .% ¥ ° Pala =. eS oir oak wath HE sean ars le eed ches aera 4 He at me raindance a ee apa 4 E vy ' ? 7, : 7 e a @ 7 \ Vol. XIX. Plate IX, Hig HOE 4 Ves Ey ees Beatecseae sh = OL at hte ne La 2 ‘ y 7.) ‘ : ’ 3 ; \ =: ‘ ie} C > pre ‘-.- 4 v ‘ # a * ty H ‘ { ‘ is a : t * 4 er - ;. Fe ; i ‘ r i f . “ . er : . \ ~ “= " = ’ 5 ; ‘ ‘ ‘ = +s . : 4 « q . ’ ‘ i x ‘ ae r é - er : = ‘ a . . is i] Ba) t - "re = oo . ‘ P " 1 7 3 Vol. XIX. Plate xX, as, ” n B: 2S Bn oe « . wi bl dae gokart waste _ = SL at ase as Re OF THE i ROYAL SOIBTY of SOUTH AUSTRALIA [ | NAA A AAEM oe eS VO. XX, Part I. 2 : [With Turee Pratzs, | ISSUED JULY, 1895. EDITED BY PROFESSOR RALPH TATE. Adelaide : W. C. RIGBY, 74, KING WILLIAM STREET. ~ Parcels for transmission to the Royai Society of South _ Australia, from Europe and America, should be addressed # per W. C. Rigby, care Messrs. Thos. Meadows & Co., 35, Milk Street, Cheapside, London.”’ ae se sececes eee —~<— rai Seda aes sree ee CONTENTS — PAGE. 2 ae PaRrKuHovusE, T. A.: Native Tongues in the Neighbourhood of Port Darwin | - Tupeer, J. -G. O. : New or Little-known Orthoptera from Lake Callabonna petig ‘Goyprr, G. A. : Reactions of Double Cyanide, bearing upon the Cyanide-process for Gold-extraction _- Brackpurn, Rev. T.: Description of New Genera and Species of - Australian Coleoptera (xvii.) uae ¥ - Howcury, W.:. New Facts bearing on the Glacial Features of -, Hallett’s Cove - _ Movpen, J. C. : Petrographical Observations on some South Aus- tralian Rocks _... Re ars : ‘Tarr, Pror. R.: A Supplement to a Census of the Flora of Extra- - tropical South Australia ; -VERCO, Dr. J. C.: Descriptions of New Species of Marine Mollusca : of South Australia (Plates 1-3) fs A Revision of the Recent Gasteropods of South Rig Australia (i.) no Tats, Pror. R., and Dennant, J.: Correlation of the Marine Ter- 3 _tiaries of Australia, Part II., Victoria (continued ) 19 61 84 108 T FTRANSACTIONS. a ; OF THE —____—_+—__-- VOL: XIX... Part. IT. al 3 Pier! Savin Pein | a ae 4 EP ae s o ay INCLUDING PROCEEDINGS AND REPORTS. | EDITED BY PROFESSOR RALPH TATE. se Sauer Adelaide : ~ W. ©. RIGBY, 74, KING WILLIAM STREET. ; || Parcels for transmission. to the Royal Society of South 1 \ustralia, from Europe and America, should be addressed «per W.>c! Rigby, ‘care Messrs. Thos. Meadows & Co., ee 35, Milk Street, Cheapside, London.” VARDON & PRITCHARD, PRINTERS, GRESHAM STREET ‘y r wt DEN CUMOA Si de [Uke ils UTA a ey j AS TAR ak a ey AN ae i i) Yay | ay At oy i i ea With a ae me ins i BAD Ma 0, HUI AA 3 2044