DOCSLIB.ORG

Trilobites from the Dinantian Tn2b-C of the Kastanjelaan-2 Borehole (Maastricht, the Netherlands) C

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Trilobites from the Dinantian Tn2b-C of the Kastanjelaan-2 Borehole (Maastricht, the Netherlands) C 51 Natuurhistorisch Maandblad 71 (3).1982 gedurende de laatste 500.000 jaren Dankbetuiging rous the Brabant Massif has been covered se- zocht de rivier zich een weg, die in veral times by a relatively thin and incomplete De schrijver is zeer erkentelijk voorde hulp, die hij sequence of sediments. These deposits disap- grote lijnen overeenkomt met haar mocht ontvangen van de zijde van Mevr. Th. Ver- peared almost completely as a result of subse- huidige loop. In het begin werden toen boekèt, die het manuscript meermalen moest uit- quent erosion phases. Thick, and more or less zanden en grinden afgezet op het ni- typen, en van Dhr. J.C. Franssen bij het afwerken complete sequences accumulated in the grabens veau van de huidige Pietersberg. Maar der figuren. to the north. This overall sedimentation pattern has been only interrupted during the Late Creta- naarmate de Maas zich verder in haar ceous and Early Tertiary when inversion move- huidige dal insneed werden de sedi- ments caused temporary uplift of the graben area. menten, die vanuit Noord-Frankrijk en Summary During that period the Brabant Massif was de Ardennen werden aangevoerd, op flooded by a shallow sea. lagere niveaus ("terrassen") afgezet. The paleogeographic evolution of the southern The boreholes Heugem and Kastanjelaan in Netherlands and northern Belgium since the Pa- Maastricht have proved that this area was located Pas in de laatste honderduizend jaar leozoic shows the continuous influence on the at the eastern flank of the Brabant Massif. During heeft het Maasdal haar huidige vorm sedimentation pattern of the two principal tectonic the Devono-Carboniferous a narrow graben or verkregen. elements in that area: the Brabant Massif in the depression existed between Vise and Maastricht. south and a complex graben zone to the north. This graben is characterized by rapid local chan- Presumably, during the Devonian and Carbonife- ges in the thickness and fades of the deposits. Trilobites from the Dinantian Tn2b-c of the Kastanjelaan-2 borehole (Maastricht, the Netherlands) C. Brauckmann Fuhlrott-Museum, Auer Schulstrasse 20, 5600 Wuppertal 1, Federal Republic of Germany The trilobites from the 335.10 - 335.25 m interval of the Kastanjelaan-2 Type horizon: The 335.10 - 335.25m level of borehole in the municipality of Maastricht (South Limburg, the Nether- borehole, Dinantian Tn2b-c (see BLESS et al., 1981, p. 348). lands) belong to four different genera: Cummingella maastrichtensis Distribution: Known only from the type loca- Brauckmann nov.sp., Phillipsia (Phillipsia) sp., Piltona? sp. and Archego- lity and the type horizon. nus? nov.sp. The conodonts and corals in this interval suggest a Dinantian Other specimens: Cranidium NHMM Tn2b-c age. 198244 (fig. 1a-b, 3a-c), and perhaps free cheek NHMM 198245 (fig. 5). Derivation of name: After the type locality. Up to present, Carboniferous trilobites ger strata (Tn3a-b) of the Tournai re- from the Netherlands have only been gion. Striking is the difference between Diagnosis: A species of Cummin- regarded by DORSMAN (1945), who the low number of specimens and the gella with the following characteristics. briefly described some fragments from high number of different taxa. Glabella very compact, subquadratic the marine Aegir level (base of Westp- in dorsal view, strongly convex both in halian C; Upper Carboniferous) as Family PHILLIPSIIDAE OEHLERT 1886 longitudinal and transverse section, Griffithides sp. (now probably better Subfamily CUMMINGELLINAE G. & R. scarcely contracted at mid-length; 4 determined as Paladin sp.). Lower HAHN1967 pairs of very shallow glabella furrows; Carboniferous (Dinantian) trilobites Genus Cummingella Reed 1942. anterior border covered by the over- were hitherto completely unknown hanging glabella. Pygidium with 11 Type species: Phillipsia jonesii The more surprising was the discovery rings on the rhachis and 11 pairs of ribs Portlock 1843. of trilobite fragments from several le- on the pleural fields; pleural furrows Diagnosis: G. & R. HAHN(1972), p. vels of the borehole Kastanjelaan-2 in broad (exsag.), reaching the border; 341-342 ("Beziehungen"). the municipality of Maastricht (cf. interpleural furrows passing onto the BLESSef a/., 1981). The better preser- Cummingella maastrichtensis border; anterior band of all ribs dis- ved ones, to be described in this paper, Brauckmann nov.sp. (fig. 1 -4, ?5). tinctly continuing on the border. Stein- are from the 335.10 - 335.25 m level, kern surface of the glabella densely Bollandia n. sp.?; BRAUCKMANN in: BLESSef a/., which is dated as Dinantian Tn2b-c by 1981, p. 352, pi. 15, (fig. 1). granulated, pygidial rhachis (stein- means of conodonts and corals. It kern) with well marked irregular, rather should be noted that in equivalent Holotype: Pygidium (steinkern) NHMM spinous nodes. 198243 (fig. 2a-b, 4a-c). strata in Belgium only different trilobite Description: Glabella (paratype Type location: Borehole Kastanjelaan-2 in taxa have been found yet, while com- the municipality of Maastricht (South Limburg, the NHMM 198244; other parts of the cra- parable species occur in slightly youn- Netherlands). nidium are not preserved). Lateral Natuurhistorisch Maandblad 71(3).1982 52 ribs; pleural furrows broad (exsag.), not deeply incised, reaching the con- T 0 vex, rather narrow and indistinctly marked border; interpleural furrows (= rib furrows) of all ribs weak, but pas- sing onto.the border; anterior bands of the ribs continuing on the border, breadth of the anterior and posterior 4mm bands of the ribs nearly the same (ex- sag.); steinkern of the rhachis with well marked, rather spinous irregular no- Figure 1. Cummingella maastrichtensis Brauckmann nov. sp. Reconstruction of paratype glabella, des. Lengths: pygidium 7.6 mm; rha- NHMM 198244. a: dorsal view, b: lateral view. chis 6.8 mm. Breadths: pygidium 10.6 mm; rhachis 4.2 mm. Remarks: Perhaps also to this spe- cies belongs an isolated free cheek (NHMM 198245; fig. 5) of nearly cum- mingelloid outline, which shows a sculpture very similar to that of the gla- bella described above. Unfortunately the poor preservation does not allow an exact identification. Discussion: Among the characte- ristic features of C. maastrichtensis the most important ones are (1) the very strong convexity of the overhan- ging glabella, in which this species Figure 2. Cummingella maastrichtensis Brauckmann nov. sp. Reconstruction of holotype pygidium, shows' quite un-cummingelloid, but NHMM 198243. a: dorsal view, b: lateral view (same scale as fig. 1). bollandoid tendencies, and (2) the prominent sculpture both on the gla- bella and on the pygidial rhachis, which is also very uncommon in Cum- view (fig. 1b, 3b): Scarcely curved then falling down steeply to the very mingella. Both features led to the pre- (nearly plain and horizontal) in poste- short (sag.), convex post-axial part of liminary determination as "Bollandia rior half, but frontal lobe strongly bent the pleural fields; rings moderately n. sp.?", based on the at that time un- down, distinctly overlapping the ante- prominent, with steep posterior slope; completely prepared specimens. But rior border. Very strongly arched in an- pleural field slightly inclined backward, mainly the configuration of the glabella terior view (fig. 3c). Dorsal view nearly plain beside the rhachis, but be- furrows and the outline and structure of (fig. 1a, 3a): Subquadratic, scarcely coming more convex against the pos- the pygidium (anterior bands of the ribs contracted at mid-length, frontal lobe terior border; ribs moderately promi- continuing on the border!) show that nearly truncate in outline. 4 pairs of nent; border convex. Posterior this species belongs to Cummingella. very shallow glabellar furrows; S1 and view (fig. 4c): Rhachis equally ar- There is no other known species within S2 beginning at the dorsal .furrow, ched; inner half of pleural fields direc- Cummingella with shows this kind of strongly curved backward (S1 perhaps ted horizontally, outer half strongly combination of characteristics. Most not reaching the occipital furrow, but bent downward to the convex border; closely related to C. maastrichtensis is the poor preservation does not allow a dorsal furrows only weakly incised. a still undescribed taxon from the definitive conclusion), S3 and S4 not Dorsal view (fig. 2a, 4a): Slightly Tn3a-b, collected in several speci- connected with the dorsal furrows, elongate; rhachis broader than one mens in the Tournai region (SW Bel- very weak, directed more transversely pleural field, nearly parabolic in outli- gium), which will be described in detail than S1 and S2. The whole surface of ne, long, with 11 rings; anterior 7-8 in one of the next parts of the mono- the steinkern is distinctly granulated. rings rather prominent, posterior ones graph on the trilobites of the Belgian Length 6.0 mm. Breadth at mid-length more indistinct, but visible; axial fur- Lower Carboniferous by G. & R. Hahn 4.0 mm. rows broad (sag.), weakly incised, di- and the present author. Pygidium (holotype NHMM 198243). rected nearly straight transversely, The main differences between these Lateral view (fig. 2b, 4b): Rhachis showing only very slight backward two taxa seem to be in the even much relatively low (ratio height of rhachis: curvature against the dorsal furrows; more spinous sculpture of the pygi- height of pleural field = 1:3), curving dorsal furrows rather distinct; pleural dium (both on the rhachis and the pleu- gently down backward to the last ring, fields with 11 ribs, no place for more ral fields) in the Belgian taxon, which 53 Natuurhistorisch Maandblad 71 (3).1982 reminds that of the fruit of the Erica- cean Arbutus and is comparable with the sculpture of the Japanese Carboni- ferous griffithidinid trilobite Parvidu- mus densigranulatus Kobayashi & Hamada 1980. At present, without ha- ving examined the Belgian specimens in detail, the preservation does not al- low an exact comparison, because the pygidium from Maastricht is exfoliated, while the Belgian ones are not. The differences in the sculpture could have been caused either by the different preservation or - perhaps more likely - by the more advanced development of Figure 5.
Load more

Recommended publications
  • University of Nevada Reno Correlation of the Fauna V from The
    University of Nevada Reno Correlation of the Fauna v from the Middle Permian Section at Black Rock Northwestern, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology Mines Library University of Nevada Reno, Nevada 89507 by Daniel Marshall Howe \\\ August 1975 ! K ilfE S EJBMRY T 2 o The thesis of Daniel Marshall Howe is approved: Dean; Graduate School University of Nevada Reno August, 1975 ACKNOWLEDGMENTS I would like to thank Dr. Joseph Lintz, Jr. for supervising and supporting the Masters problem. David Koliha and Larry Noble assisted in the field work. David was a constant source of enthusiasm and Larry's technical field knowledge and expertise were all invaluable to me. Diane Cornwall as curator of the University of Nevada museum helped with numerous tasks, and with Fred Gustafson they recommended numerous concepts and possible approaches I thank Mike Fiannaca. for his help in cutting the thin sections, and Wayne Kemp in helping to interpret them. I thank Dr. E.R. Larson in his availability and wisdom in keeping the original collections which he cheerfully made available to me when I enquired about the Black Rock. I thank Dr. Peter Comanor for joining my committee and spending time in the field with me. ABSTRACT Black Rock is located at the southwestern tip of the Black Rock Range in Humboldt County, northwestern Nevada. The Black Rock section consists of approxiamate- ly 2,500 feet of Middle Permian andesitic flows, lithic volcanic wackes, and limestone. Two of the limestone horizons have yielded faunules.
    [Show full text]
  • Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction by MACKENZIE GORDON, JR
    Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction By MACKENZIE GORDON, JR. Corals By WILLIAM J. SANDO Pelecypods By JOHN POJETA, JR. Gastropods By ELLIS L. YOCHELSON Trilobites By MACKENZIE GORDON, JR. Ostracodes By I. G. SOHN GEOLOGICAL SURVEY PROFESSIONAL PAPER 606-A, B, C, D, E, F Papers illustrating and describing certain of G. H. Girty' s invertebrate fossils from the Fayetteville Shale UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-650224 For sale by the Superintendent of Documents, U.S. Government Printing Office Washing.ton, D.C. 20402 CONTENTS [The letters in parentheses preceding the titles are those used to designate the chapters] Page (A) Introduction, by Mackenzie Gordon, Jr _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 1 (B) Corals, by William J. Sando__________________________________________________________________________________ 9 (C) Pelecypods, by John Pojeta, Jr _____ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 15 (D) Gastropods, by Ellis L.
    [Show full text]
  • Paleozoic Seas 290809New
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Berichte des Institutes für Geologie und Paläontologie der Karl- Franzens-Universität Graz Jahr/Year: 2009 Band/Volume: 14 Autor(en)/Author(s): Anonym Artikel/Article: Distribution of Paleozoic sedimentary units of Austria. 86-87 ©Institut f. Erdwissensch., Geol. u. Paläont., Karl-Franzens-Universität Graz; download www.biologiezentrum.at Ber. Inst. Erdwiss. K.-F.-Univ. Graz ISSN 1608-8166 Band 14 Graz 2009 Paleozoic Seas Symposium Graz, 14-18th September 2009 Distribution of Paleozoic sedimentary units of Austria During the meeting we are going to see some localities of the Graz Paleozoic and the Carnic Alps. On the map the distribution of major Paleozoic sedimentary units of Austria is indicated. Graz Paleozoic (D) The sequence includes Silurian to Carboniferous strata, of which the Devonian neritic units around Graz are very well developed. We are going to visit Emsian to Givetian sections such as the road-cut at St. Pankrazen or Forstweg Attems where coral frame- and rudstones are outcropping. Additionally to a very well known algal flora and coral fauna, some of these localities yield a diverse microfauna including scolecodonts, conodonts and other vertebrate remains like shark teeth or placoderm plates. Carnic Alps (G) The sequence includes Ordovician to Permian units, of which we are going to visit the Carboniferous of Nötsch and the Nassfeld area. At the first mentioned locality brachiopods like Gigantoproductus, trilobites (Proetidae, Phillipsiidae), gastropods, crinoids and ostracods occur. At the second locality, Mount Auernig, we are going to visit the Upper Carboniferous sequence yielding calcareous algae and silicified foraminifers (Fusulinoidea), bryozoans and ostracods.
    [Show full text]
  • ペ ル ム 紀）の Phillipsiidae新属三葉虫
    The AssooiationAssociation for the GeologioalGeological Collaboration in Japan (AGCJ)（AGCJ ｝ 地 球科学 26 巻 1 号 〔1972年 1 丿目） 阿 武 隈 山地 ・高 倉 山 層 群 （ペ ル ム 紀 ） の Phillipsiidae新属 三 葉虫 小 泉 斉 ＊ 学教室 の 浜 田 隆 士 博± に は ，終始御懇切 な 御指導 や原 稿 1 は じ め に 一 の 御校 閲な ど 煩 わ し た ．磐城高校 の 柳沢 郎博士 ，四 倉 の の の 南部 阿武隈山地 の 福島県 い わ き市四倉町玉 山砿泉 北 史学館 小桧山 元氏 ， 気仙沼 図 書館 荒木英夫氏 に は い 一 ペ ル ム が つ 電な が ら 方 な らぬ お 世話を い た だ い た ． を 西 に 位置す る 高倉山 （293m ）を 中心 に ， 紀 層 ， 標本 提 ・ …・ メ ソ バ ー て 供 して 下 さ っ た 鈴木 千里 高泉 弘 の 君 や ・ よ く 発達す る こ と は ， 平地学 同好会 の に ょ っ 幸 両 橋本 雄 一・ 大 内 ・鈴 ・ 正 の の に と こ ユ950年10月 に 確 認 され た ，こ の 高倉 山層群 は ， す で に ， 男 木直 大内 博 諸君 御協力 負 う ・ ろ も か っ た こ れ の 々 に し て 心 柳沢 根本 （1961）， 柳 沢 （1967） らに よ っ て 地 質学的 多 ， ら 方 対 衷 よ り感 謝を申 古生物学的研究 が お こ な わ れ て い る ．そ の ほ か に 早 坂 し上 げ ま す． の （1957， 1965＞ は 頭 足 類 ，中沢 と NEWELL （1968＞ 斧 ’ ll I aladin yanagisawai の 再 検討 か ら ・ の 三 の よ 足類 （二 枚 則 ， 遠 藤 松 本 （1962） 葉 虫 類 な ど 新 属 EndcPS の 記 載 て い が の うに それぞ れ 専問 的 な 研究 が な さ れ る ， そ 豊寓 に て （］rifiSthides cf ， brez，ieaudata な生 物群 は 充分に 研 究がすす ん で い な い ． 柳 沢 （1958） よ っ に さ れ た お よ び い つ か の か と こ ろ で ，高 倉山層群 に 三 葉 虫 が 産 轟す る こ と は 小 桧 i房定 標本 ， く 頭 部，少な ら ぬ Phillipsia？ sP ． の 尾 部 に よ っ て 記 載 さ れ た PaJadin yan −lgisawai lt 山 （1956）に よ っ て 尾部を と し て 報 告 数 ） − さ れ た ．更 に 小桧山 （1957） は 完 全体 を 発見 し て 1 fiiJ い くつ か の 点に お い て 不 備 な 記載 で あ っ た ． tiPsia sp ．110V ， KOBIY・zzEA と し て 記載 を し た が ，変形 ア メ リ カ の Lower Pennsyivanianか ら 知 ら れ た ’ Grifithides moptrotvensz ：s 1 CrxrHE ；Z を と し て 1936 が著 し く充 分な鑑定 に た え られ な か っ た ．と こ ろ が 1956 模式種 ’ て に WELLER に よ っ て 立 され た f aladin は 上 年 9 月 に 磐 誠高生 に よ っ て 発見 され た
    [Show full text]
  • Sepkoski, J.J. 1992. Compendium of Fossil Marine Animal Families
    MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. Department of the Geophysical Sciences University of Chicago Chicago, Illinois 60637 Milwaukee Public Museum Contributions in Biology and Geology Rodney Watkins, Editor (Reviewer for this paper was P.M. Sheehan) This publication is priced at $25.00 and may be obtained by writing to the Museum Gift Shop, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Orders must also include $3.00 for shipping and handling ($4.00 for foreign destinations) and must be accompanied by money order or check drawn on U.S. bank. Money orders or checks should be made payable to the Milwaukee Public Museum. Wisconsin residents please add 5% sales tax. In addition, a diskette in ASCII format (DOS) containing the data in this publication is priced at $25.00. Diskettes should be ordered from the Geology Section, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Specify 3Y. inch or 5Y. inch diskette size when ordering. Checks or money orders for diskettes should be made payable to "GeologySection, Milwaukee Public Museum," and fees for shipping and handling included as stated above. Profits support the research effort of the GeologySection. ISBN 0-89326-168-8 ©1992Milwaukee Public Museum Sponsored by Milwaukee County Contents Abstract ....... 1 Introduction.. ... 2 Stratigraphic codes. 8 The Compendium 14 Actinopoda.
    [Show full text]
  • Jahresberichte Des Naturwissenschaftlichen Vereins in Wuppertal 41
    Jahresberichte des Naturwissenschaftlichen Vereins in Wuppertal 41. Heft Herausgegeben von Wolfgang Kolbe Wuppertal 10. Oktober 1988 Naturwissenschaftlicher Verein Wuppertal und FUHLROTT-Museum Wuppertal Redaktions-Komitee: C. BRAUCKMANN, M. LÜCKE Geologie, Paläontologie und Mineralogie H. KNÜBEL Geographie H. SUNDERMANN, W. STIEGLITZ Botanik unter Ausschluß der Mykologie H. WOLLWEBER Mykologie R. SKlBA Ornithologie W. KOLBE Zoologie unter Ausschluß der Ornithologie Schriitentausch und -vertrieb: FUHLROTT-Museum Auer Schulstraße 20 D-5600 Wuppertal 1 Inhaltsverzeichnis Seite Faunistik, Ökologie: SKIBA, R.: Die Fledermäusedes Bergischen Landes ............................. MEINIG, H.: Die Kleinsäugerfaunadesoberen Gelpetales(Insectivora, Rodentia) ... WENZEL, E.: Die Käferfaunades oberbergischen Ülfetals, Teil I ................... Floristik: WEBER, G.: Die Makrophyten der Wupper, Teil I: Diesubmersvegetation .... Ökotoxikologie: KOLBE, W.: Die Staphyliniden (Coleoptera) der Waldböden und ihre Beeinflussung durch Na-PCP ......................................................... DORN, K.: Dipterenemergenzen in PCP-belasteten Waldböden des Staatswaldes Burgholz-die Nematoceren im Buchen- und Fichtenforst, Teil II ........... NIPPEL, F.: Großschmetterlinge aus dem Burgholz-Projekt, die mit Hilfe von Bo- den-Photoeklektoren erfaßt wurden ..................................... PLATEN, R.: Der Einfluß von Na-Pentachlorphenol auf die Spinnen- (Araneida) und Weberknechtfauna (Opilionida) zweier unterschiedlicher Bestände des Staatswaldes Burgholz,
    [Show full text]
  • ' ~§~IF~C-~D~ 6Tj~R~!Tu~£\~> ~
    ,- -, " ,~ .. ...:.,-..- I." " "-".-:-;- '~'- .~'. - - "'7 ~-_.- '-:...... ~~~'~'--~'-' .. .;'-:-- ''''~ ~:~=., ,,~: - ,t-" .::.;. '- .c ~I·:.-':'-~":'~ ~- .o.r ._ -.~-~~;.__ ......,~_. ;:._~~- ~ _r ~ ?:f;~~.-~:;..-~.-; ~ , :'~::':.' C •• ,··'· .• >.,' _'. ,', .• '" ", ' ..C . _ '. (.,~~ ._ -~-_-.,.: _.~~~.t-~~ ._ ~ ... ;.-~~~~;~~< '::-'~':·~-~·:~--:Z-~:~:_~~ _,;'-~·~~-~·~t~:·;-,~·~,,~:~~:~ .,:~ - ._. '; '. ~ . ~"'- J-1:0"'--~'-~ ", . '- ·:~tc;·PERMIAN~:~TRILOBITESOF>J.APAN~ ',' '" ." ' .. - - ',. ~ ~;,~-~-~ .. ;:~.~-~.' . ~ - - -::-....... -~ -~ ~ ~ . -'. -. ~ -.' --''- - ~ ',. '--:-" ..~~~:;·~·IN· COMPARISQN·:wtrH-~AsIA~,,= --~ ,~: .-~-~,-!- -' .. ' ~§~IF~C-~D~ 6Tj~R~!tU~£\~>_~ ..- r,-."- e ,;.... :.-. ~ By' - ~:~.~.- '.- ".' -- si-;~~~~~'~· -~-. .~~-:----- '.. \~. - --'~- , ~Tetichi· KOBAYASHI:Jnd-Tak~s41'HAMiJ)A. ' -'!II • -.~:~~: - ~.•.• ~.,.~~,< .", . -. .. -~f::=:- ~". - . ::,",-- :.--.., "-,-- "'.~---.- '- -'." - .. ~=,.;--. - .-:.:. '~-,--.."":"'.::.....:: -.. '~ -~~: . -' -. .', --,: .' ~.~. ""1-_:-' : .... '"=:.,-:" . .-- .. -.:.:---"-"';- ,~\.- .:._-: j : ~:~7 ~~. :.:;"),~. .- -:s:.....:. -- -.- . '" . ",.~-'. ,<~~.'- ---~-t:., -',;;:,~._ ._'--- .. .;. "~" .. ~...... --: - --- . - ' .... f .. " 4-.' ~ '_, - :-: :-. - :"J:- .- :~ .' - ... ,.- - '"-:-.' . ;'-:--=::\~.':~~--t>~·.~ .. ~,< . '~--'~-'~;....:-.~--. --~. .':"";' .'; -~-P<' ~'.,;!... - ~'"":~~';-?';'~h.:.:~-?-~-:" '~:-'.-' '"-..; . <>" _~ '-. ~ )r>< _ -- . ,~_:-:_. ----,;:;..;.~~~.,'.' ~,_. "'~ ".:'! . 'C:~'1" _,_~' ~... ,~ .,: ~ ._, ,"j., , /~ ·.S~:iaLj,:~~~:~,p;laeo~to19ii2aVSQci~t;~~fj~pah
    [Show full text]
  • Full Text -.: Palaeontologia Polonica
    ACADEMIE POLONAISE DES SCIENCES INSTITUT DE PALEOZOOLOGIE P ALAEONTOLOGIA POLONICA-No.Z3,1970 REVISION OF NON-CYRTOSYMBOLINID TRILOBITES FROM THE TOURNAISIAN­ NAMURIAN OF EURASIA (REWIZJA TRYLOBIT6w, PR6cz CYRTOSYMBOLINAE, Z TURNEJU­ NAMURU EURAZJI) BY HALSZKA OSM6LSKA (WITH 9 TEXT-FIGURES, 2 TABLES AND 22 PLATES) WAR S Z A W A 1970 PANSTWOWE WYDAWN ICTWO NA UKOWE REDAKTOR - ReDACTEUR RO MAN KOZLOWSKI Czlonek rzecz ywisty Polskiej Akademit Nauk Membre de I'Acadernie Polonaise des Sciences ZA STJ;PCA REDAKTORA - ReDACTEUR SU PPLeANT ZOFIA KIELAN-JAWOROWSKA Czlonek kore spondenl Po1sk iej Ak ademii Nauk Membre correspo ndant de I'Ac ad emie Polonaise des Sciences Redakto r techniczn y - Redacteur technique M. Tom aszewska-Kukulska Adres Redakcji - Adr esse de la Red action In st itut de Pa leozo ologie de I'Academ ic Polonaise des Sciences Wars zawa 22, AI. Zwirki i Wigury 93 Co pyright by Pan stwowe Wydawnictwo Na ukowe 1970 Printed in Poland Pan stw owe Wydawnictwo N aukowc -: Warszawa Nakl ad 650 + 90 egz, Ark. wyd.22.25. Ar ku szy druk. 10' /.+22 wkladki. Papier rotogr , sal . kl, III 61 x 86 125 g. Od dan o do skladania 30. IX . 1969 r, Podp isano do druku 18.VIII. 1970 r. Druk uk onczono w pazd ziern iku 1970 r, Drukarnia Uniwersytetu Jag iellonskiego w Krakowie Zarn, 824 /69 CONTENTS Page Introduction .. 7 Ac knowledgements 8 GENERAL PART Systematics of the Carboniferous proetids . .. ... 11 Diagnostic importan ce of some tr ilobite characters ... .. 14 Stratigraphic and geog raphic range of the Carboniferous proetid subfamilies 16 Carboniferous trilobites in Eurasia .
    [Show full text]
  • Appendix 7.4: Functional Diversity of Marine Ecosystems After the Late Permian Mass Extinction Event
    University of Plymouth PEARL https://pearl.plymouth.ac.uk 04 University of Plymouth Research Theses 01 Research Theses Main Collection 2015 Palaeoecology of the late Permian mass extinction and subsequent recovery Foster, William J. http://hdl.handle.net/10026.1/5467 Plymouth University All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Appendix 7.4: Functional diversity of marine ecosystems after the Late Permian mass extinction event Mode of Life assignments Table S1: Mode of Life assignments. In the functional columns each number corresponds to the model in Bambach et al. (S1), where for Tiering: 2 = erect; 3 = surficial; 4 = semi-infaunal; 5 = shallow infaunal; 6 = deep infaunal; for Motility: 1 = fast motile; 2 = slow motile; 3 = facultatively motile, unattached; 4 = facultatively motile, attached; 5 = stationary, unattached; 6 = stationary, attached; and for Feeding: 1 = suspension feeder; 2 = deposit feeder; 3 = miner; 4 = grazer; 5 = predator; 6 = other (i.e. chemosymbiosis).
    [Show full text]
  • Preliminary Report on the New Findings of Mississippian Trilobites in the Březina Formation (Moravian Karst, Czech Republic)
    GEOL. VÝZK. MOR. SLEZ., BRNO 2012 PRELIMINARY REPORT ON THE NEW FINDINGS OF MISSISSIPPIAN TRILOBITES IN THE BŘEZINA FORMATION (MORAVIAN KARST, CZECH REPUBLIC) Tomáš Weiner1, Carsten Brauckmann2, Hedvika Poukarová1, Štěpán Rak3, Jiří Kalvoda1 1 Masaryk University, Department of Geological Sciences, Kotlářská 2, 611 37 Brno, Czech Republic; e-mail: [email protected] 2 Clausthal University of Technology, Geology and Palaeontology, Leibnizstrasse 10, D-38678 Clausthal-Zellerfeld, Germany 3 Charles University, Institute of Geology and Palaeontology, Albertov 6, 128 43 Praha 2, Czech Republic (24-41 Vyškov) Key words: Moravian Karst, Březina Formation, Mississippian, Viséan, trilobites Abstract New fossiliferous layers of the Březina Formation were discovered in the valley of the Říčka Brook SSW of the village of Ochoz u Brna in 2011. Four taxa of trilobites were preliminary determined: Archegonus (Phillibole) cf. polleni (Woodward, 1894), Archegonus (Phillibole) cf. cauliquercus Brauckmann 1981, Liobole (Liobole) glabra proxima Chlupáč, 1966 and ?Spinibole sp. Th e newly dis- covered fossiliferous beds belong to the Viséan (Lower to ?Upper Viséan, approximately cu IIγ–cu IIδ). Th e occurrence of limestone pebbles and limestone cobbles in aleuropelitic shales was also recorded. Th e Late Tournaisian foraminifer Darjella monilis Malak- hova, 1964 was discovered in a dark grey limestone cobble derived from the Hády-Říčka limestone sequence of the Líšeň Formation. Introduction New trilobite-bearing beds of the Březina Formation Trilobites from
    [Show full text]
  • Pennsylvanian Trilobites of Ohio
    P' STATE OF OHIO Richard F. Celeste, Governor DEPARTMENT OF NATURAL RESOURCES Joseph J. Sommer, Director DIVISION OF GEOLOGICAL SURVEY Thomas M . Berg, Chief Report of Investigations No. 142 PENNSYLVANIAN TRILOBITES OF OHIO by David K. Brezinski Myron T. Sturgeon and Richard D. Hoare Columbus 1989 DIVISION OF GEOLOGICAL SURVEY FOUNTAIN SQUARE, BUILDING B OD~ COLUMBUS, OHIO 43224 OHIO DEPARTMENT OF (614) 265-6605 (Voice) NATURAL RESOURCES (614) 265-6994 (TDD) SCIENTIFIC AND TECHNICAL STAFF OF THE DIVISION OF GEOLOGICAL SURVEY ADMINISTRATION Thomas M. Berg, MS, State Geologist and Division Chief Robert G. Van Horn, MS, Geologist and Assistant Chief Barbara J. Adams, Administrative Secretary Catherine C. Chaney, B. Mus. Ed., Administrative Secretary James M. Miller, BA, Fiscal Administrator REGIONAL GEOLOGY LAKE ERIE Dennis N. Hull, MS, Geologist and Section Head Jonathan A. Fuller, MS, Geologist Richard W. Carlton, PhD, Geologist Donald E. Guy, Jr., MS, Geologist Kim E. Daniels, BS, Geologist Dale L. Liebenthal, Research Vessel Operator Michael C. Hansen, PhD, Geologist Mary Lou McGurk, Typist Sherry W. Lopez, MS, Geologist Toni McCall, Word-Processing Specialist SUBSURFACE GEOLOGY L-Ower Pal£ozoic Geology David A. Stith, MS, Edward Mac Swinford, MS, Geologist and Coordinator Geologist and Acting Section Head Mark T. Baranoski, MS, Geologist Gregory A. Schumacher, MS, Geologist Ronald A. Riley, MS, Douglas L. Shrake, BS, Geologist Geologist Lawrence H. Wickstrom, MS, Geologist Upper Pai,eozoic Geology Angelena M. Bailey, Administrative Assistant Linda F. Dunbar, Ronald G. Rea, MS, Geologist and Coordinator Public Inquiries Assistant Patricia A. Nicklaus, Public Inquiries Assistant Michael R. Caudill, BS, Geologist Glenn E.
    [Show full text]
  • From the Permian Jamal Formation, Isfahan, Iran
    Journal of Sciences, Islamic Republic of Iran 28(4): 325 - 336 (2017) http://jsciences.ut.ac.ir University of Tehran, ISSN 1016-1104 Pseudophillipsia (Carniphillipsia) (Trilobite) from the Permian Jamal Formation, Isfahan, Iran H. Ameri*1, M. Yazdi2, and A. Bahrami2 1Department of Ecology, Institute of Science, High Technology and Environmental Science, Graduate University of Advanced Technology, Kerman, Islamic Republic of Iran 2Department of Geology, Faculty of Sciences, University of Isfahan, Isfahan, Islamic Republic of Iran Received: 24 July 2016 / Revised: 27 October 2016 / Accepted: 25 January 2017 Abstract The aim of this study is to bridge a gap in the existence of Trilobites in the marine Permian successions of Iran by exploring a stratigraphic section of the Permian in Jamal Formation (Dizlu section). Based on comprehensive field studies and laboratory investigations three Trilobite specimens were identified in the study area including Pseudophillipsia (Carniphillipsia) dizluensis sp. nov., Pseudophillipsia (Carniphillipsia) sagittalis and Pseudophillipsia (Carniphillipsia) sp.. A new occurrence of trilobites collected from the Permian (Wordian) Jamal Formation at a section at Dizlu, Isfahan Province, Iran, is documented. They belong to a new species of Pseudophillipsia (Carniphillipsia), which is described herein, and can be attributed to the a group of species centered on P.(C). paffenholzi (Weber). It is based on 30 specimens from a single horizon, most of which are enrolled. Co-occurrence of Pseudophillipsia (Carniphillipsia) sp. A. and stenohalin groups such as brachiopods, bryozoans, and crinoids are indicating that this species were preferred shallow and carbonate environments. This is the first time that the existences of these specimens are reported in Dizlu section.
    [Show full text]