Changes in Paratethyan Marine Molluscs at the Early/Middle Miocene Transition: Diversity, Palaeo- Geography and Palaeoclimate
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Kamena Jedra Mehkužcev Iz Miocenskih Plasti Pri Beli Cerkvi Na Dolenjskem
KAMENA JEDRA MEHKUŽCEV IZ MIOCENSKIH PLASTI PRI BELI CERKVI NA DOLENJSKEM MOLLUSC INTERNAL CASTS FROM THE MIOCENE BEDS NEAR BELA CERKEV, SLOVENIA Vasja MIKUŽ1 IZVLEČEK UDK 57.071.64:594(497.434Bela Cerkev)"628.42" ABSTRACT UDC 57.071.64:594(497.434Bela Cerkev)"628.42" Kamena jedra mehkužcev iz miocenskih plasti pri Beli Mollusc internal casts from the Miocene beds near Bela Cerkvi na Dolenjskem Cerkev, Slovenia Raziskovana in obravnavana so kamena jedra miocen- We present a study of Miocene mollusc internal casts skih mehkužcev, ki so najdena v preperini laporastih in ko- found in the weathered marls and corallinacean limestones ralinacejskih apnencev na njivi blizu zaselka Bela Cerkev na in a field near Bela Cerkev in Dolenjska. Among the internal Dolenjskem. Prevladujejo kamena jedra školjk, ki so običaj- casts, bivalves are most abundant, complete specimens are no ohranjena v celoti. Veliko manj in slabše ohranjenih je common. Gastropod internal casts are much less abundant polžjih kamenih jeder. Ugotovljene oblike školjk in polžev so and poorly preserved. The determined specimens are of Ba- badenijske starosti. denian age. Ključne besede: kamena jedra, mehkužci - polži, školjke, Key words: internal casts, Mollusc - Gastropods, Bival- srednji miocen, badenij, Centralna Paratetida, Bela Cerkev, ves, Middle Miocene, Badenian, Central Paratethys, Bela Slovenija Cerkev, Slovenia 1 Univerza v Ljubljani, Naravoslovnotehniška fakulteta, Oddelek za geologijo, Privoz 11, SI – 1000 Ljubljana, Slovenija; vasja. [email protected] FOLIA BIOLOGICA ET GEOLOGICA 54/1, 95–107, LJUBLJANA 2013 VASJA MIKUŽ: KAMENA JEDRA MEHKUŽCEV IZ MIOCENSKIH PLASTI PRI BELI CERKVI NA DOLENJSKEM UVOD V Sloveniji je veliko najdišč s kamenimi jedri različnih Kamena jedra so pri školjkah večinoma ohranjena fosilnih ostankov v zelo različno starih kamninah. -
Mammalia, Felidae, Canidae, and Mustelidae) from the Earliest Hemphillian Screw Bean Local Fauna, Big Bend National Park, Brewster County, Texas
Chapter 9 Carnivora (Mammalia, Felidae, Canidae, and Mustelidae) From the Earliest Hemphillian Screw Bean Local Fauna, Big Bend National Park, Brewster County, Texas MARGARET SKEELS STEVENS1 AND JAMES BOWIE STEVENS2 ABSTRACT The Screw Bean Local Fauna is the earliest Hemphillian fauna of the southwestern United States. The fossil remains occur in all parts of the informal Banta Shut-in formation, nowhere very fossiliferous. The formation is informally subdivided on the basis of stepwise ®ning and slowing deposition into Lower (least fossiliferous), Middle, and Red clay members, succeeded by the valley-®lling, Bench member (most fossiliferous). Identi®ed Carnivora include: cf. Pseudaelurus sp. and cf. Nimravides catocopis, medium and large extinct cats; Epicyon haydeni, large borophagine dog; Vulpes sp., small fox; cf. Eucyon sp., extinct primitive canine; Buisnictis chisoensis, n. sp., extinct skunk; and Martes sp., marten. B. chisoensis may be allied with Spilogale on the basis of mastoid specialization. Some of the Screw Bean taxa are late survivors of the Clarendonian Chronofauna, which extended through most or all of the early Hemphillian. The early early Hemphillian, late Miocene age attributed to the fauna is based on the Screw Bean assemblage postdating or- eodont and predating North American edentate occurrences, on lack of de®ning Hemphillian taxa, and on stage of evolution. INTRODUCTION southwestern North America, and ®ll a pa- leobiogeographic gap. In Trans-Pecos Texas NAMING AND IMPORTANCE OF THE SCREW and adjacent Chihuahua and Coahuila, Mex- BEAN LOCAL FAUNA: The name ``Screw Bean ico, they provide an age determination for Local Fauna,'' Banta Shut-in formation, postvolcanic (,18±20 Ma; Henry et al., Trans-Pecos Texas (®g. -
JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb
JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 149 Heft 1 S. 61–109 Wien, Juli 2009 A Revision of the Tonnoidea (Caenogastropoda, Gastropoda) from the Miocene Paratethys and their Palaeobiogeographic Implications BERNARD LANDAU*), MATHIAS HARZHAUSER**) & ALAN G. BEU***) 2 Text-Figures, 10 Plates Paratethys Miozän Gastropoda Caenogastropoda Tonnoidea Österreichische Karte 1 : 50.000 Biogeographie Blatt 96 Taxonomie Contents 1. Zusammenfassung . 161 1. Abstract . 162 1. Introduction . 162 2. Geography and Stratigraphy . 162 3. Material . 163 4. Systematics . 163 1. 4.1. Family Tonnidae SUTER, 1913 (1825) . 163 1. 4.2. Family Cassidae LATREILLE, 1825 . 164 1. 4.3. Family Ranellidae J.E. GRAY, 1854 . 170 1. 4.4. Family Bursidae THIELE, 1925 . 175 1. 4.5. Family Personidae J.E. GRAY, 1854 . 179 5. Distribution of Species in Paratethyan Localities . 180 1. 5.1. Diversity versus Stratigraphy . 180 1. 5.2. The North–South Gradient . 181 1. 5.3. Comparison with the Pliocene Tonnoidean Fauna . 181 6. Conclusions . 182 3. Acknowledgements . 182 3. Plates 1–10 . 184 3. References . 104 Revision der Tonnoidea (Caenogastropoda, Gastropoda) aus dem Miozän der Paratethys und paläobiogeographische Folgerungen Zusammenfassung Die im Miozän der Paratethys vertretenen Gastropoden der Überfamilie Tonnoidea werden beschrieben und diskutiert. Insgesamt können 24 Arten nachgewiesen werden. Tonnoidea weisen generell eine ungewöhnliche weite geographische und stratigraphische Verbreitung auf, wie sie bei anderen Gastropoden unbekannt ist. Dementsprechend sind die paratethyalen Arten meist auch in der mediterranen und der atlantischen Bioprovinz vertreten. Einige Arten treten zuerst im mittleren Miozän der Paratethys auf. Insgesamt dokumentiert die Verteilung der tonnoiden Gastropoden in der Parate- thys einen starken klimatischen Einfluss. -
The Lower Pliocene Gastropods of Le Pigeon Blanc (Loire- Atlantique, Northwest France). Part 5* – Neogastropoda (Conoidea) and Heterobranchia (Fine)
Cainozoic Research, 18(2), pp. 89-176, December 2018 89 The lower Pliocene gastropods of Le Pigeon Blanc (Loire- Atlantique, northwest France). Part 5* – Neogastropoda (Conoidea) and Heterobranchia (fine) 1 2 3,4 Luc Ceulemans , Frank Van Dingenen & Bernard M. Landau 1 Avenue Général Naessens de Loncin 1, B-1330 Rixensart, Belgium; email: [email protected] 2 Cambeenboslaan A 11, B-2960 Brecht, Belgium; email: [email protected] 3 Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, Netherlands; Instituto Dom Luiz da Universidade de Lisboa, Campo Grande, 1749-016 Lisboa, Portugal; and International Health Centres, Av. Infante de Henrique 7, Areias São João, P-8200 Albufeira, Portugal; email: [email protected] 4 Corresponding author Received 25 February 2017, revised version accepted 7 July 2018 In this final paper reviewing the Zanclean lower Pliocene assemblage of Le Pigeon Blanc, Loire-Atlantique department, France, which we consider the ‘type’ locality for Assemblage III of Van Dingenen et al. (2015), we cover the Conoidea and the Heterobranchia. Fifty-nine species are recorded, of which 14 are new: Asthenotoma lanceolata nov. sp., Aphanitoma marqueti nov. sp., Clathurella pierreaimei nov. sp., Clavatula helwerdae nov. sp., Haedropleura fratemcontii nov. sp., Bela falbalae nov. sp., Raphitoma georgesi nov. sp., Raphitoma landreauensis nov. sp., Raphitoma palumbina nov. sp., Raphitoma turtaudierei nov. sp., Raphitoma vercingetorixi nov. sp., Raphitoma pseudoconcinna nov. sp., Adelphotectonica bieleri nov. sp., and Ondina asterixi nov. sp. One new name is erected: Genota maximei nov. nom. is proposed for Pleurotoma insignis Millet, non Edwards, 1861. Actaeonidea achatina Sacco, 1896 is considered a junior subjective synonym of Rictaxis tornatus (Millet, 1854). -
UC Davis UC Davis Previously Published Works
UC Davis UC Davis Previously Published Works Title Molluscan marginalia: Serration at the lip edge in gastropods Permalink https://escholarship.org/uc/item/2mx5c6w9 Journal Journal of Molluscan Studies, 80(3) ISSN 0260-1230 Author Vermeij, GJ Publication Date 2014 DOI 10.1093/mollus/eyu020 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Journal of The Malacological Society of London Molluscan Studies Journal of Molluscan Studies (2014) 80: 326–336. doi:10.1093/mollus/eyu020 Advance Access publication date: 16 April 2014 Molluscan marginalia: serration at the lip edge in gastropods Geerat J. Vermeij Geology Department, University of California, One Shields Avenue, Davis, CA 95616, USA Correspondence: G.J. Vermeij; e-mail: [email protected] Downloaded from (Received 5 September 2013; accepted 10 February 2014) ABSTRACT The shells of many marine gastropods have ventrally directed serrations (serial projections) at the edge http://mollus.oxfordjournals.org/ of the adult outer lip. These poorly studied projections arise as extensions either of external spiral cords or of interspaces between cords. This paper describes taxonomic, phylogenetic, architectural and func- tional aspects of serrations. Cord-associated serrations occur in cerithiids, strombids, the personid Distorsio anus, ocenebrine muricids and some cancellariids. Interspace-associated serrations are phylo- genetically much more widespread, and occur in at least 16 family-level groups. The nature of serration may be taxonomically informative in some fissurellids, littorinids, strombids and costellariids, among other groups. Serrated outer lips occur only in gastropods in which the apex points more backward than upward, but the presence of serrations is not a necessary byproduct of the formation of spiral sculp- tural elements. -
Gradual Miocene to Pleistocene Uplift of the Central American Isthmus: Evidence from Tropical American Tonnoidean Gastropods Alan G
J. Paleont., 75(3), 2001, pp. 706±720 Copyright q 2001, The Paleontological Society 0022-3360/01/0075-706$03.00 GRADUAL MIOCENE TO PLEISTOCENE UPLIFT OF THE CENTRAL AMERICAN ISTHMUS: EVIDENCE FROM TROPICAL AMERICAN TONNOIDEAN GASTROPODS ALAN G. BEU Institute of Geological and Nuclear Sciences, P O Box 30368, Lower Hutt, New Zealand, ,[email protected]. ABSTRACTÐTonnoidean gastropods have planktotrophic larval lives of up to a year and are widely dispersed in ocean currents; the larvae maintain genetic exchange between adult populations. They therefore are expected to respond rapidly to new geographic barriers by either extinction or speciation. Fossil tonnoideans on the opposite coast of the Americas from their present-day range demonstrate that larval transport still was possible through Central America at the time of deposition of the fossils. Early Miocene occurrences of Cypraecassis tenuis (now eastern Paci®c) in the Caribbean probably indicate that constriction of the Central American seaway had commenced by Middle Miocene time. Pliocene larval transport through the seaway is demonstrated by Bursa rugosa (now eastern Paci®c) in Caribbean Miocene-latest Pliocene/Early Pleistocene rocks; Crossata ventricosa (eastern Paci®c) in late Pliocene rocks of Atlantic Panama; Distorsio clathrata (western Atlantic) in middle Pliocene rocks of Ecuador; Cymatium wiegmanni (eastern Paci®c) in middle Pliocene rocks of Atlantic Costa Rica; Sconsia sublaevigata (western Atlantic) in Pliocene rocks of Darien, Paci®c Panama; and Distorsio constricta (eastern Paci®c) in latest Pliocene-Early Pleistocene rocks of Atlantic Costa Rica. Continued Early or middle Pleistocene connections are demonstrated by Cymatium cingulatum (now Atlantic) in the Armuelles Formation of Paci®c Panama. -
Early Pliocene Molluscs from the Easternmost Mediterranean Region (SE Turkey): Biostratigraphic, Ecostratigraphic, and Palaeobiogeographic Implications
Turkish Journal of Earth Sciences Turkish J Earth Sci (2017) 26: http://journals.tubitak.gov.tr/earth/ © TÜBİTAK Research Article doi:10.3906/yer-1705-2 Early Pliocene molluscs from the easternmost Mediterranean region (SE Turkey): biostratigraphic, ecostratigraphic, and palaeobiogeographic implications 1, 2 3 4 5 2 Yeşim BÜYÜKMERİÇ *, Erdoğan TEKİN , Erdal HERECE , Koray SÖZERİ , Nihal AKÇA , Baki VAROL 1 Department of Geological Engineering, Faculty of Engineering, Bülent Ecevit University, İncivez, Zonguldak, Turkey 2 Department of Geological Engineering, Faculty of Engineering, Ankara University, Gölbaşı Campus, Gölbaşı, Ankara, Turkey 3 Department of Geological Research, General Directorate of Mineral Research and Exploration (MTA), Balgat, Ankara, Turkey 4 Natural History Museum, General Directorate of Mineral Research and Exploration (MTA), Balgat, Ankara, Turkey 5 Research Centre, Turkish Petroleum Corporation (TPAO), Esentepe, Ankara, Turkey Received: 04.05.2017 Accepted/Published Online: 05.12.2017 Final Version: 00.00.2016 Abstract: The mollusc faunas from Pliocene deposits of the Hatay-İskenderun region were investigated at nine localities and complemented with three localities from earlier studies. The Pliocene units were deposited in three adjacent subbasins, Hatay-Samandağ (HS), Altınözü-Babatorun (AB), and İskenderun-Arsuz (İA); the first two are also known as the Hatay Graben. Basin configurations and shape, environmental evolution, and faunal compositions were affected by differential tectonic histories since the Late Miocene. In total 162 species (94 gastropod, 61 bivalve, and 7 scaphopod) are recorded, 80 of which are recorded for the first time from the region. The occurrence of tropical stenohaline benthic taxa (such as Persististrombus coronatus and some conid gastropod species) and a number of chronostratigraphically well-constrained mollusc species shows a Zanclean age. -
A Review of Fossil Bursidae and Their Use for Phylogeny Calibration
geodiversitas 2019 ● 41 ● 5 DIRECTEUR DE LA PUBLICATION : Bruno David, Président du Muséum national d’Histoire naturelle RÉDACTEUR EN CHEF / EDITOR-IN-CHIEF : Didier Merle ASSISTANTS DE RÉDACTION / ASSISTANT EDITORS : Emmanuel Côtez ([email protected]) ; Anne Mabille MISE EN PAGE / PAGE LAYOUT : Emmanuel Côtez COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD : Christine Argot (MNHN, Paris) Beatrix Azanza (Museo Nacional de Ciencias Naturales, Madrid) Raymond L. Bernor (Howard University, Washington DC) Alain Blieck (chercheur CNRS retraité, Haubourdin) Henning Blom (Uppsala University) Jean Broutin (UPMC, Paris) Gaël Clément (MNHN, Paris) Ted Daeschler (Academy of Natural Sciences, Philadelphie) Bruno David (MNHN, Paris) Gregory D. Edgecombe (The Natural History Museum, Londres) Ursula Göhlich (Natural History Museum Vienna) Jin Meng (American Museum of Natural History, New York) Brigitte Meyer-Berthaud (CIRAD, Montpellier) Zhu Min (Chinese Academy of Sciences, Pékin) Isabelle Rouget (UPMC, Paris) Sevket Sen (MNHN, Paris) Stanislav Štamberg (Museum of Eastern Bohemia, Hradec Králové) Paul Taylor (The Natural History Museum, Londres) COUVERTURE / COVER : Aquitanobursa tuberosa (Grateloup, 1833) n. comb., MNHN.F.A70285, Burdigalian of le Peloua, Staadt coll. Geodiversitas est indexé dans / Geodiversitas is indexed in: – Science Citation Index Expanded (SciSearch®) – ISI Alerting Services® – Current Contents® / Physical, Chemical, and Earth Sciences® – Scopus® Geodiversitas est distribué en version électronique par / Geodiversitas is distributed electronically -
Management Plan for Antarctic Specially Protected Area No. 126 BYERS PENINSULA, LIVINGSTON ISLAND, SOUTH SHETLAND ISLANDS
Measure 4 (2016) Management Plan for Antarctic Specially Protected Area No. 126 BYERS PENINSULA, LIVINGSTON ISLAND, SOUTH SHETLAND ISLANDS Introduction The primary reason for the designation of Byers Peninsula (latitude 62°34'35" S, longitude 61°13'07" W), Livingston Island, South Shetland Islands, as an Antarctic Specially Protected Area (ASPA) is to protect the terrestrial and lacustrine habitats within the Area. Byers Peninsula was originally designated as Specially Protected Area (SPA) No. 10 through Recommendation IV-10 in 1966. This area included the ice-free ground west of the western margin of the permanent ice sheet on Livingston Island, below Rotch Dome, as well as Window Island about 500 m off the northwest coast and five small ice-free areas on the south coast immediately to the east of Byers Peninsula. Values protected under the original designation included the diversity of plant and animal life, many invertebrates, a substantial population of southern elephant seals (Mirounga leonina), small colonies of Antarctic fur seals (Arctocephalus gazella), and the outstanding scientific values associated with such a large variety of plants and animals within a relatively small area. Designation as an SPA was terminated through Recommendation VIII-2 and redesignation as a Site of Special Scientific Interest (SSSI) was made through Recommendation VIII-4 (1975, SSSI No. 6). The new designation as an SSSI more specifically sought to protect four smaller ice-free sites on the peninsula of Jurassic and Cretaceous sedimentary and fossiliferous strata, considered of outstanding scientific value for study of the former link between Antarctica and other southern continents. Following a proposal by Chile and the United Kingdom, the SSSI was subsequently extended through Recommendation XVI-5 (1991) to include boundaries similar to those of the original SPA: i.e. -
Conoidea (Neogastropoda) Assemblage from the Lower Badenian (Middle Miocene) Deposits of Letkés (Hungary), Part II. (Borsoniida
151/2, 137–158., Budapest, 2021 DOI: 10.23928/foldt.kozl.2021.151.2.137 Conoidea (Neogastropoda) assemblage from the Lower Badenian (Middle Miocene) deposits of Letkés (Hungary), Part II. (Borsoniidae, Cochlespiridae, Clavatulidae, Turridae, Fusiturridae) KOVÁCS, Zoltán1 & VICIÁN, Zoltán2 1H–1147 Budapest, Kerékgyártó utca 27/A, Hungary. E-mail: [email protected]; Orcid.org/0000-0001-7276-7321 2H–1158 Budapest, Neptun utca 86. 10/42, Hungary. E-mail: [email protected] Conoidea (Neogastropoda) fauna Letkés alsó badeni (középső miocén) üledékeiből, II. rész (Borsoniidae, Cochlespiridae, Clavatulidae, Turridae, Fusiturridae) Összefoglalás Tanulmányunk Letkés (Börzsöny hegység) középső miocén gastropoda-faunájának ismeretéhez járul hozzá öt Conoidea-család (Borsoniidae, Cochlespiridae, Clavatulidae, Turridae, Fusiturridae) 41 fajának leírásával és ábrázo - lásával. A közismert lelőhely agyagos, homokos üledékei a Lajtai Mészkő Formáció alsó badeni Pécsszabolcsi Tagozatát képviselik, és – ma már kijelenthető – Magyarország leggazdagabb badeni tengeri molluszkaanyagát tartalmazzák. A jelen tanulmányban vizsgált Conoidea-fauna néhány nagyon ritka faj [pl. Cochlespira serrata (BELLARDI), Clavatula sidoniae (HOERNES & AUINGER) stb.] újabb előfordulásának igazolása mellett a tudományra nézve öt új faj bevezetését is lehetővé tette: Clavatula hirmetzli n. sp., Clavatula santhai n. sp., Clavatula szekelyhidiae n. sp., Perrona harzhauseri n. sp., Perrona nemethi n. sp. A kutatás során a vonatkozó korábbi magyarországi szakirodalom revízióját -
Gastropodes Du Miocene Moyen
GASTROPODES DU MIOCENE MOYEN DU BASSIN DE LA LOIRE INTRODUCTION Les saules calcareux coquilliers ou « Faluns » du Bassin de la Loire on L, depuis longtemps, attire !'attention des paleontologistes, par l'abondance, la varietc et le bon etal de conservation des coquilles fossiles qu'ils renferment. Ces << Faluns de la Touraine », qui constituent le Miocene moyen typique duns l'Ouest d.e la Fra11ce, ne sont plus representes aujourd'hui que par des lambeaux de peu d'etendue, mais la repartition g-eographique de ces derniers revele que ces sediments se sont deposes, a l'origine, dans un vaste bras de mer, allonge et digite, s'etendant depuis les cOtes du Nord de la Bretagne jusqu'aux environs de Blois, et clont Rennes et Angers divisent la ligne mediane longitu- dinale en trois parties a peu pres egales C). Ces Faluns ont ete observes et ·etudies tout d'abord sur la rive gauche de la Loire, au Sud de Tours, ou ils ont le plus de puissance et o\.1 se situent plusieurs des gites fo ssiliferes les plus riches, notamment Louans, Le Louroux, Sainte Catherine de Fierbois, Manthelan, Bossee, Sainte-Maure, La Chapelle-Blanche, Sepmes, Ferriere-Larc;on, Paul my. Un autre ilot, bien connu des chercheurs, comprend, plus a l'Est, au Sud de Blois, les gites celebres de Pontlevoy et de Thenay. Enfin, sur la rive droite, cette fois, en Maine-et-Loire, se situent les gites classique de Genneteil et de Sceaux. J e rappellerai ici les eta pes principales du progres de nos connaissance con cernant Ia faune malacologique fossile des Faluns vincloboniens de la Touraine. -
Current Status of Philippine Mollusk Museum Collections and Research, and Their Implications on Biodiversity Science and Conservation
Philippine Journal of Science 147 (1): 123-163, March 2018 ISSN 0031 - 7683 Date Received: 28 Feb 2017 Current Status of Philippine Mollusk Museum Collections and Research, and their Implications on Biodiversity Science and Conservation Dino Angelo E. Ramos2*, Gizelle A. Batomalaque1,3, and Jonathan A. Anticamara1,2 1Ecology and Taxonomy Academic Group (ETAG), Institute of Biology, University of the Philippines, Diliman, Quezon City 1101 Philippines 2UP Biology Invertebrate Museum, Institute of Biology, University of the Philippines, Diliman, Quezon City 1101 Philippines 3Department of Biodiversity, Earth, and Environmental Science, Drexel University, Philadelphia, Pennsylvania 19104 USA Mollusks are an invaluable resource in the Philippines, but recent reviews on the status of museum collections of mollusks or research trends in the country are lacking. Such assessments can contribute to a more comprehensive evaluation of natural history museums in the Philippines, as well as biodiversity management. This review showed that local museums in the Philippines have much to improve in terms of their accessibility and geographic coverage in order to effectively cater to research and conservation needs of the country. Online access to databases was lacking for local museums, making it cumbersome to retrieve collection information. The UST museum held the most species and subspecies across all museums (4899), comparable to the national museums of countries such as the USA and France. In terms of size, there were larger Philippine mollusk collections in museums abroad. Majority of mollusk specimens come from Regions 4 and 7, while the CAR and Region 12 were least sampled. Publications on Philippine mollusks are dominated by taxonomic and biodiversity research.