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New Fossil Record of Two Warm-water Bivalves from the Pleistocene Itaya Formation, Toyama Prefecture, Central Japan

机译:日本中部富山县更新世板谷板谷组两个温水双壳类的新化石记录

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摘要

Two warm-water species, Pecten (Pecten) byoritsuensis Nomura, 1933 and Oxyperas (Oxyperas) bernardi (Pilsbry, 1904) have been obtained from the Lower Pleistocene Itaya Formation in Toyama Prefecture. Based on the fossil occurrences recorded by previous studies as well as this study, these species are rare and first appeared in the Early Pleistocene in the Japan Sea borderland. P. (P.) byoritsuensis became extinct at the end of the Early Pleistocene as a result of deteriorating environments associatedwith glacial periods in the Japan Sea. O. (O.) bernardi survived these conditions because of its wide distribution, as with Pecten (Notovola) naganumanus Yokoyama, 1920 and P. (N.) albicans (Schroter, 1802). Detailed examination of molluscan fossils from the Itaya Formation and their ages indicates that the Tagawa assemblage from the Lower Pleistocene Omma Formation in Oyabe City can be correlated with the Itaya assemblage, not with the Zukawa.
机译:从富山县下更新世板谷组获得了两种暖水物种,即1933年野村的Pecten(Pecten)和1904年的Pysbry的Oxyperas(Oxyperas)bernardi。根据以前的研究和本次研究记录的化石发生,这些物种是罕见的,并且首先出现在日本海边界地区的早更新世。由于日本海冰川期相关环境的恶化,byoritsuensis的P.(P.)byoritsuensis在早更新世末期灭绝。 O.(O.)bernardi因其分布广泛而幸免于这些条件,例如Pecten(Notovola)naganumanus Yokoyama,1920年和P.(N.)albicans(Schroter,1802年)。从板岩组的软体动物化石及其年龄进行的详细检查表明,大部部市下更新世Omma组的田川组合可能与板岩组合有关,与Zukawa组合无关。

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