Talexirhynchia, a new rhynchonellid genus from the Jurassic Ethiopian Province of Jordan

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• 作者：Howard R. Feldman (1)
  Mena Schemm-Gregory (2) (3)
  Mark A. Wilson (4)
  Fayez Ahmad (5)
  
  1. Division of Paleontology (Invertebrates) ; American Museum of Natural History ; New York ; NY ; 10024 ; USA
  2. Centro de Geoci锚ncias e Departamento de Ci锚ncias da Terra ; Universidade de Coimbra ; Largo Marqu锚s de Pombal ; 3000-272 ; Coimbra ; Portugal
  3. Museu Geol贸gico ; Laborat贸rio Nacional de Energia e Geologia (LNEG) ; Rua Academia das Ci锚ncias ; 19 ; 1200-003 ; Lisbon ; Portugal
  4. Department of Geology ; The College of Wooster ; 944 College Mall ; Wooster ; OH ; 44691 ; USA
  5. Department of Earth and Environmental Sciences ; Faculty of Natural Resources and Environment ; The Hashemite University ; P.O. Box 150459 ; 13115 ; Zarqa ; Jordan
  
• 关键词：Talexirhynchia ; Rhynchonellida ; Brachiopoda ; Middle Jurassic ; Ethiopian Province ; Jordan ; Talexirhynchia ; Rhynchonellida ; Brachiopoda ; Mittel ; Jura ; 脛thiopische Provinz ; Jordanian
• 刊名：Pal?ontologische Zeitschrift
• 出版年：2015
• 出版时间：March 2015
• 年：2015
• 卷：89
• 期：1
• 页码：25-35
• 全文大小：1,780 KB
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• 刊物类别：Earth and Environmental Science
• 刊物主题：Paleontology
  Geology
  
• 出版者：Springer Berlin Heidelberg
• ISSN：1867-6812

文摘

A new genus and species of a rhynchonellide brachiopod from the Jurassic of Jordan, Talexirhynchia kadishi gen. et sp. nov., is described. The specimens were collected from the Mughanniyya Formation (Callovian) of Wadi Zarqa from alternating claystones, siltstones, and marly limestones with minor dolomite, dolomitic limestone, and coquinas that represent the upper part of the Jurassic sequence in Jordan. The environment of deposition was neritic; food supply and light were unlikely to have been limiting factors. The specimens are related to Ethiopian-Somali taxa and are consistent with the endemism that characterizes the rhynchonellide brachiopod faunas of the Jurassic Ethiopian Province. Specimens of Talexirhynchia lived with the umbo in an upright position directed toward the seafloor or with the dorsal valve slightly above the ventral valve. Juveniles were attached to the seafloor by the pedicle; carbonate shell material as well as other debris scattered on a limy substrate, such as shells and rocks, could have served as an attachment site for juveniles. With increasing growth, the loss of the pedicle and a semi-infaunal position resulted in an increasingly incurved ventral umbo that concealed the foramen.