Nouvelles Données Sur L'évolution Et La Classification
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Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
The Hauterivian-Barremian Stage Boundary in Svinita Area (Banat, Sw Romania)
Rom. J. Stratigraphy, 77, 4, p. 37-46, Bucure§ti, 1998 THE HAUTERIVIAN-BARREMIAN STAGE BOUNDARY IN SVINITA AREA (BANAT, SW ROMANIA) Emil AVRAM, Mihaela MELINTE Institutul Geologic al Romaniei, str. Caransebe§, nr. 1, R0-79678 Bucure§ti 32 Key words: Lower Cretaceous. Hauterivian-Barremian boundary. Inte grate paleontology. Ammonites. Dinoflagellatecys ts. N annofossils. Svini1a T region. South Carpathians. Romania. UN��,� Abstract: The genus Pseudothurmannia offers the best marker at the Hauterivian-Barremian stages boundary. Its range interval seems to be hetter defined as index species by Pseudothurmannia picteti than by P. IGCP-362 angulicostata. The same interval is also characterised by the first record of Tethyan and Boreal Pulchelliids ( Psilotissotia spp.) and is a little preceded by the first Che Cretaceous loniceratinae ( Paraspiticeras) and by a very significantevol utionary step in dinoflagellate assemblages (from the biozone with Oligosphaeridium com plex and Druggidium deflandre.i, to the biozone with Dingodinium albertii and Meiourogoniaulax stoveri, fide Antonescu, Avram, 1980). On the other hand, the firstmarkers of the Lower Barremian asaccepted by Hoedemaeker et al. (1993) pertain to the family Holcodiscidae, a group fully developed in Hauterivian. All these facts lead us to consider the Pseudothurmannia beds ( = P. angulicostata zone in litt.) as the base of the Barremian stage. 3. in the outer structural units of the Car 1. Introduction pathians ( or "the Moldavides", ibidem), in the Audia N appe; The Upper Hauterivian-Lower Barremian 4. in the southernmost foreland unit of the fossiliferous rock-sequences were recognised in Carpathians, i. e. the Moesian Platform (for Romania in several regions, namely: details, see Avram, 1988). -
Calcareous Nannofossils, Ammonites
De Kaenel et al. Swiss J Palaeontol (2020) 139:6 https://doi.org/10.1186/s13358-020-00209-5 Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access New biostratigraphical data (calcareous nannofossils, ammonites) and Early to Late Barremian transition in the Urgonien Jaune facies and Marnes de la Russille complex of the Swiss Jura Mountains Eric De Kaenel1*, Pierre‑Olivier Mojon2 and Antoine Pictet3 Abstract In the central Jura Mountains (Western Switzerland), the Urgonien Jaune (UJ) facies with the Marnes de la Russille beds (MRu) have provided very rich nannoforas associated with very rare Tethyan ammonites. A late Early Barremian nannofora of the Mid‑Barremian Event (MBE, following a regional tectonic event of an earliest Barremian synsedimentary tectonic crisis) was found in MRu of the lower UJ and includes 42 genera with 90 species. Among them, Biscutum jurensis De Kaenel, n. sp., Flabellites eclepensensis De Kaenel, n. sp., Palaeopontosphaera giraudii De Kaenel, n. sp., Rhagodiscus buisensis De Kaenel, n. sp., and Vagalapilla rutledgei De Kaenel, n. sp., are recognized as fve new species. This nannofora is a mixture of Boreal and Tethyan taxa with 20 nannofossil markers (Assipetra terebrodentarius, Broinsonia galloisii, Calcicalathina oblongata, Cyclagelosphaera rotaclypeata, Diloma placinum, Ethmorhabdus hauterivianus, Flabellites eclepensensis, Gorkaea pseudoanthophorus, Nannoconus abundans, Nannoconus pseudoseptentrionalis, Palaeopontosphaera giraudii, Palaeopontosphaera pinnata, Placozygus howei, Placozygus reticulatus, Reinhardtites scutula, Rhagodiscus buisensis, Rhagodiscus eboracensis, Tegulalithus septentrionalis, Tubodiscus jurapelagicus, Zeugrhabdotus moulladei) indicating very precisely the nannofossil Zones LK19 (Boreal)–NC5D (Tethyan) as well as the Elegans (Boreal) and Moutonianum (Tethyan) ammonite Zones of the latest Early Barremian. The ammonites in the basal UJ facies of Early Barremian age are reworked Lyticoceras claveli (Nodosoplicatum Zone, Early Hauterivian) and reworked Cruasiceras cf. -
Early Cretaceous (Albian) Ammonites from the Chitina Valley and Talkeetna Mountains, Alaska
Early Cretaceous (Albian) Ammonites From the Chitina Valley and Talkeetna Mountains, Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 354-D Early Cretaceous (Albian) Ammonites From the Chitina Valley and Talkeetna Mountains, Alaska By RALPH W. IMLAY SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 354-D The Early Cretaceous (Albian) ammonites in southern Alaska have strong affinities with those in California and Oregon but are in part of Boreal and Eurasian origin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. - Price SO cents (paper cover) CONTENTS Ammonite faunules and correlations Continued Abstract..________________________________________ 87 Bretrericeras breweri and B. cf. B. hulenense faunule__ 91 Introduction _______________________________________ 87 Frebnhliceros singulare faunule____________________ 92 Biologic analysis____________________________________ 87 Other Albian faunules.__________________________ 93 Stratigraphic summary ______________________________ 88 Comparisons with other faunas_______________________ 93 Talkeetna Mountains ___________________________ 88 Geographic distribution._____________________________ 93 Chitina Valley__________________________________ 88 Summary of results _________________________________ 93 Ammonite faunules and correlations.__________________ -
Evolution, Distribution, and Phylogenetic Clumping of a Repeated Gastropod Innovation
Zoological Journal of the Linnean Society, 2017, 180, 732–754. With 5 figures. The varix: evolution, distribution, and phylogenetic clumping of a repeated gastropod innovation NICOLE B. WEBSTER1* and GEERAT J. VERMEIJ2 1Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada T6G 2E9 2Department of Earth and Planetary Sciences, University of California, Davis, CA 95616, USA Received 27 June 2016; revised 4 October 2016; accepted for publication 25 October 2016 A recurrent theme in evolution is the repeated, independent origin of broadly adaptive, architecturally and function- ally similar traits and structures. One such is the varix, a shell-sculpture innovation in gastropods. This periodic shell thickening functions mainly to defend the animal against shell crushing and peeling predators. Varices can be highly elaborate, forming broad wings or spines, and are often aligned in synchronous patterns. Here we define the different types of varices, explore their function and morphological variation, document the recent and fossil distri- bution of varicate taxa, and discuss emergent patterns of evolution. We conservatively found 41 separate origins of varices, which were concentrated in the more derived gastropod clades and generally arose since the mid-Mesozoic. Varices are more prevalent among marine, warm, and shallow waters, where predation is intense, on high-spired shells and in clades with collabral ribs. Diversification rates were correlated in a few cases with the presence of varices, especially in the Muricidae and Tonnoidea, but more than half of the origins are represented by three or fewer genera. Varices arose many times in many forms, but generally in a phylogenetically clumped manner (more frequently in particular higher taxa), a pattern common to many adaptations. -
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. -
Berriasian Ammonites of Supposed Tethyan Origin from the Type ‘Ryazanian’, Russia: a Systematic Re-Interpretation Camille Frau, William A.P
Berriasian ammonites of supposed Tethyan origin from the type ‘Ryazanian’, Russia: a systematic re-interpretation Camille Frau, William A.P. Wimbledon, Christina Ifrim, Luc Bulot, Alexandre Pohl To cite this version: Camille Frau, William A.P. Wimbledon, Christina Ifrim, Luc Bulot, Alexandre Pohl. Berriasian am- monites of supposed Tethyan origin from the type ‘Ryazanian’, Russia: a systematic re-interpretation. Palaeoworld, 2020, 10.1016/j.palwor.2020.07.004. hal-03016238 HAL Id: hal-03016238 https://hal.archives-ouvertes.fr/hal-03016238 Submitted on 20 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Journal Pre-proof Berriasian ammonites of supposed Tethyan origin from the type ‘Ryazanian’, Russia: a systematic re-interpretation Camille Frau , William A.P. Wimbledon , Christina Ifrim , Luc G. Bulot , Alexandre Pohl PII: S1871-174X(20)30058-5 DOI: https://doi.org/10.1016/j.palwor.2020.07.004 Reference: PALWOR 586 To appear in: Palaeoworld Received date: 4 November 2019 Revised date: 15 June 2020 Accepted date: 15 July 2020 Please cite this article as: Camille Frau , William A.P. Wimbledon , Christina Ifrim , Luc G. Bulot , Alexandre Pohl , Berriasian ammonites of supposed Tethyan origin from the type ‘Ryazanian’, Russia: a systematic re-interpretation, Palaeoworld (2020), doi: https://doi.org/10.1016/j.palwor.2020.07.004 This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. -
Abbreviation Kiel S. 2005, New and Little Known Gastropods from the Albian of the Mahajanga Basin, Northwestern Madagaskar
1 Reference (Explanations see mollusca-database.eu) Abbreviation Kiel S. 2005, New and little known gastropods from the Albian of the Mahajanga Basin, Northwestern Madagaskar. AF01 http://www.geowiss.uni-hamburg.de/i-geolo/Palaeontologie/ForschungImadagaskar.htm (11.03.2007, abstract) Bandel K. 2003, Cretaceous volutid Neogastropoda from the Western Desert of Egypt and their place within the noegastropoda AF02 (Mollusca). Mitt. Geol.-Paläont. Inst. Univ. Hamburg, Heft 87, p 73-98, 49 figs., Hamburg (abstract). www.geowiss.uni-hamburg.de/i-geolo/Palaeontologie/Forschung/publications.htm (29.10.2007) Kiel S. & Bandel K. 2003, New taxonomic data for the gastropod fauna of the Uzamba Formation (Santonian-Campanian, South AF03 Africa) based on newly collected material. Cretaceous research 24, p. 449-475, 10 figs., Elsevier (abstract). www.geowiss.uni-hamburg.de/i-geolo/Palaeontologie/Forschung/publications.htm (29.10.2007) Emberton K.C. 2002, Owengriffithsius , a new genus of cyclophorid land snails endemic to northern Madagascar. The Veliger 45 (3) : AF04 203-217. http://www.theveliger.org/index.html Emberton K.C. 2002, Ankoravaratra , a new genus of landsnails endemic to northern Madagascar (Cyclophoroidea: Maizaniidae?). AF05 The Veliger 45 (4) : 278-289. http://www.theveliger.org/volume45(4).html Blaison & Bourquin 1966, Révision des "Collotia sensu lato": un nouveau sous-genre "Tintanticeras". Ann. sci. univ. Besancon, 3ème AF06 série, geologie. fasc.2 :69-77 (Abstract). www.fossile.org/pages-web/bibliographie_consacree_au_ammon.htp (20.7.2005) Bensalah M., Adaci M., Mahboubi M. & Kazi-Tani O., 2005, Les sediments continentaux d'age tertiaire dans les Hautes Plaines AF07 Oranaises et le Tell Tlemcenien (Algerie occidentale). -
Western Cuba)
ACTA PALAEONTOLOGICA POLONICA Vol. 22 1 8 7 7 No. 2 RYSZARD MYCZYNSKI LOWER CRETACEOUS AMMONITES FROM SIERRA DEL ROSARIO (WESTERN CUBA) Abstract. - Lower Cretaceous ammonites from the Artemisa, Poller and Lucas For mations of the Pinar del Rio province, are described. The assemblage comprises 47 species, including four new: KaTsteniceTas polieTi, CrioceTas pinaTensis, ACTioceras (PaTaspinoceTas) TosaTiensis and ?PleuTohoplites machini. Some of them are common for Cuba, Mexico and south Andes. Typical west - Tethyan ammonites form a noti ceable part of the Cuban assemblage. INTRODUCTION Lower Cretaceous ammonites from Cuba were not hitherto paleonto logically studied. The paper presents paleontological descriptions of Lower Cretaceous ammonites from Sierra del Rosario, western Cuba. They were found in the course of field works connected with preparation of the Geological Map of Pinar del Rio province, scale 1:250000, carried out by the team of the Polish Academy of Sciences and Cuban Academy of Sciences. Tintinids (de la Torre 1972-1975, MS) and the ammonites collected made possible to establish the stratigraphy of Lower Cretaceous strata of that region and to correlate lithostratigraphic units distinguished here. Ammonites occurring in the Lower Cretaceous strata of ,Sierra del Rosario are very rare and poorly preserved, usually as moulds. Never theless, all these finds are of a remarkable importance for the strati graphy of the Lower Cretaceous of that region as well as of the whole western Cuba. All specimens here described are housed in the Paleontological Mu seum of the Institute of Geology and Paleontology, Havana, Cuba. Acknowledgements. - Warm thanks are due to the Director of the Institute of Geology and Paleontology of the Cuban Academy of Sciences for the loan of the ammonite material from Sierra del Rosario fot detailed studies. -
Ecological Disparity Is More Susceptible to Environmental
Swiss J Palaeontol (2018) 137:49–64 https://doi.org/10.1007/s13358-017-0140-y REGULAR RESEARCH ARTICLE Ecological disparity is more susceptible to environmental changes than familial taxonomic richness during the Cretaceous in the Alpstein region (northeastern Switzerland) 1 2 1 Amane Tajika • Peter Ku¨rsteiner • Christian Klug Received: 12 June 2017 / Accepted: 26 September 2017 / Published online: 12 October 2017 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2017 Abstract Studies of global palaeoecology through time disparity are decoupled and that the ecological disparity is usually ignore regional details. Such regional studies on more highly variable in response to environmental changes palaeoecology are required to better understand both than familial taxonomic richness. regional- and global-scale palaeoecolgical changes. We analyzed the palaeoecolgy of a Cretaceous sedimentary Keywords Palaeoecology Á Diversity Á Ecological sequence in the Alpstein (cantons of Appenzell Ausser- disparity Á Cretaceous Á Switzerland rhoden, Appenzell Innerrhoden and St. Gallen, northeast- ern Switzerland), which covers from the Barremian to Cenomanian stage. Two diversity indices of familial tax- Introduction onomic richness and ecological disparity (ecospace occu- pation) with the trophic nucleus concept were employed in The ‘Big Five’ mass extinctions (End-Ordovician, Late order to document changes in palaeocommunities through Devonian, End-Permian, End-Triassic and End-Cretaceous) time. Our results illustrate that taxonomic richness did not are known to have severely affected the earth’s ecosystems change dramatically, while distinct changes occurred in and ecology (e.g., Murphy et al. 2000; Sheehan 2001;Hes- ecospace occupation through time. The changes in eco- selbo et al. 2007; Knoll et al. -
Nannoconid Assemblages in Upper Hauterivian-Lower Aptian Limestones of Cuba: Their Correlation with Ammonites and Some Planktonic Foraminifers2
STUDIA GEOLOGI CA POLONICA Vol. 114, Krak6w 1999, pp. 35-75. Mesozoic stratigraphy of Cuba Edited by A. Pszczolkowski Andrzej PSZCZOL• KOWSKI 1 & Ryszard MYCZYNSKI' I Nannoconid assemblages in Upper Hauterivian-Lower Aptian limestones of Cuba: their correlation with ammonites and some planktonic foraminifers2 (Figs 1- 13, Tabs 1- 3) Abstract. The nannoconids are abundant in the Lower Cretaceous pelagic limestones in western and central Cuba. In some lin1estone beds, these nannofossils occur together with ammonites or planktonic foraminifers. Our samples were collected from the Polier, Veloz and Paraiso formations. The Late Hauterivian to Early Aptian age of the studied samples is based mainly on ammonites. The nannoconids identified in these samples are grouped in 4 assemblages: Late Hauterivian, Early Barremian, Late Barremian and late Early Aptian. In the Early Barremian assemblage, the narrow canal nannoconids are by far more frequent than the wide-canal ones. Small specimens, classified herein provisionally as N truittii truittii, occur also in this assemblage. On the other hand, the representatives of the Nannoconus steinmannii group are absent in the late Early Aptian assemblage, which includes the wide canal forms only. Nannoconids found in one sample may represent an assemblage of the earliest Aptian age. Key words: Nannoconid assemblages, ammonites, planktonic foraminifers, Lower Cretaceous, western and central Cuba. INTRODUCTION Pelagic limestones are the most important lithologic components of the Creta ceous passive continental margin and basinal successions in Cuba. These fine grained limestones often lack identifiable macrofauna, while stratigraphically use ful microfossils are scarce or absent, especially in the Hauterivian to Aptian carbon ate rocks. -
New Biostratigraphic Data on an Upper Hauterivianeupper Barremian Ammonite Assemblage from the Dolomites (Southern Alps, Italy)
Cretaceous Research 35 (2012) 1e21 Contents lists available at SciVerse ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes New biostratigraphic data on an Upper HauterivianeUpper Barremian ammonite assemblage from the Dolomites (Southern Alps, Italy) Alexander Lukeneder Natural History Museum, Geological-Paleontological Department, Burgring 7, 1010 Wien, Austria article info abstract Article history: A biostratigraphic subdivision, based on ammonites, is proposed for the Lower Cretaceous pelagic to Received 13 April 2011 hemipelagic succession of the Puez area (Southern Alps, Italy). Abundant ammonites enable recognition Accepted in revised form 6 November 2011 of recently established Mediterranean ammonite zones from the upper Hauterivian Balearites balearis Available online 15 November 2011 Zone (Crioceratites krenkeli Subzone) to the upper Barremian Gerhardtia sartousiana Zone (Gerhardtia sartousiana Subzone). Ammonites are restricted to the lowermost part of the Puez Formation, the Puez Keywords: Limestone Member (ca. 50 m; marly limestones; HauterivianeBarremian). Numerous ammonite speci- Hauterivian mens are documented for the first time from the Southern Alps (e.g., Dolomites). Ammonite abundances Barremian Lower Cretaceous are clearly linked to sea-level changes from Late Hauterivian to mid Late Barremian times. Abundance Ammonites and diversity peaks occur during phases of high sea-level pulses and the corresponding maximum Biostratigraphy flooding surfaces (P. mortilleti/P. picteti and G. sartousiana zones). The ammonite composition of the Puez Dolomites Formation sheds light on the Early Cretaceous palaeobiogeography of the Dolomites. It also highlights the Italy palaeoenvironmental evolution of basins and plateaus and provides insights into the faunal composition and distribution within the investigated interval. The intermittent palaeogeographic situation of the Puez locality during the Early Cretaceous serves as a key for understanding Mediterranean ammonite distribution.