Palaeobiogeography, palaeoecology and evolution of Lower Ordovician conulariids and Sphenothallus (Medusozoa, Cnidaria), with emphasis on the Fezouata Shale of southeastern Morocco
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- 作者：Heyo Van Itena ; b ; vaniten@hanover.edu" class="auth_mail" title="E-mail the corresponding author ; Lucy Muirc ; lucy@asoldasthehills.org" class="auth_mail" title="E-mail the corresponding author ; Marcello G. Simõ ; esd ; profmgsimoes@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Juliana M. Lemee ; leme@usp.br" class="auth_mail" title="E-mail the corresponding author ; Antonio C. Marquesf ; g ; marques@ib.usp.br" class="auth_mail" title="E-mail the corresponding author ; Naomi Yoderh ; naomi.yoder@eagles.usm.edu" class="auth_mail" title="E-mail the corresponding author
- 关键词：Conulariids ; Sphenothallus ; Medusozoa ; Lower Ordovician ; Gondwana ; Fezouata
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：15 October 2016
- 年：2016
- 卷：460
- 期：Complete
- 页码：170-178
- 全文大小：2446 K
文摘
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The Fezouata Shale contains Archaeoconularia, Eoconularia and Sphenothallus.
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Eoconularia sp. attached at their apex to shells of phosphatic brachiopods.
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Archaeoconularia and Eoconularia are also present in coeval strata of Wales.