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首页> 外文期刊>Micropaleontology >Paleoecology and taxonomy of Early Miocene Ostracoda and paleoenvironments of the eastern Setouchi Province, central Japan
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Paleoecology and taxonomy of Early Miocene Ostracoda and paleoenvironments of the eastern Setouchi Province, central Japan

机译:日本中部濑户内省东部早期中新世龙骨纲和古环境的古生态学和分类学

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Seventy-nine fossil ostracode species were identified in 40 of 80 samples from 15 sites of the Lower Miocene Mizunami and Iwamura Groups (ca. 18 Ma), eastern Setouchi Province, central Japan. Six ostracode associations and seven biofacies were discriminated, mainly on the basis of R-mode and Q-mode cluster analyses, respectively. Species that lived in the innermost part of enclosed brackish bay habitats became extinct and their Recent related species are absent. Most Miocene species of the genera Schizocythere, Cornucoquimba and Loxoconcha inhabited similar environments to related living species. They lived in nearshore sand and silty sand bottoms with Zostera beds under the influence of subtropical-water currents as inferred from fossil molluscan assemblages. Pseudoaurila species, which are extinct, are estimated to have been dominant on seagrass or algae during the late Early to early Middle Miocene, but after that, they were replaced by diverse Aurila and Loxoconcha species. Species of the genera Palmenella, Kotoracythere, Acanthocythereis, Robertsonites, Celtia, Elofsonella and Laperousecythere are nearly identical morphologically to cryophilic or cir-cumpolar species living in cold water masses of northern high-latitude seas or lower sublittoral to bathyal zones in the Sea of Japan. They occur in Miocene sediments, however, in association with subtropical to mild-temperate, upper to middle sublittoral molluscan species. Ancestors of Recent cold-water species have thus inhabited Japan since at least the Early Miocene. They expanded their habitats southward according with global cooling in chron C5Dr interval (late Early Miocene) correlated with the the oxygen isotope maximum period (the base of the Zone Mi 1 b; ca. 18 Ma). Eleven new species are described. This study presents the earliest Miocene record of ostracodes in and around Japan and contributes to inferences on the origin, phylogeny and speciation of Recent ostracodes living in high-latitude seas in the Northern Hemisphere.
机译:在日本中部濑户内省东部的下中新世水浪组和岩村组(约18 Ma)的15个地点的80个样品中,有40个被鉴定出79种ostracode物种。分别基于R模式和Q模式聚类分析,区分了六个ostracode关联和七个生物相。生活在封闭的半咸水海湾栖息地最内层的物种已灭绝,而它们最近的相关物种却不存在。 Schizocythere,Cornucoquimba和Loxoconcha属的大多数中新世物种居住在与相关生物物种相似的环境中。根据化石软体动物组合推断,他们生活在亚热带水流的影响下,在带Zostera床的近岸砂和粉质砂底部。在中新世中期早期至早期,已灭绝的假金龟属物种在海草或藻类中占主导地位,但此后,它们被不同的金刚鹦鹉属和Loxoconcha物种所取代。 Palmenella,Kotoracythere,Acanthocythereis,Robertsonites,Celtia,Elofsonella和Laperousecythere的种类在形态上几乎与生活在日本北海高纬度海或下沿海至深水区的冷水或嗜冷极性物种相同。 。它们发生在中新世沉积物中,但与亚热带至温带,中上沿海的软体动物种类有关。至少从中新世早期以来,日本才有近来冷水物种的祖先居住。他们根据时间C5Dr间隔(中新世晚期)的全球冷却,向南扩展了栖息地,这与氧同位素的最大时期(Mi 1b区的底部;约18 Ma)有关。描述了11个新物种。这项研究提供了日本及其周围地区中新世最早的中新世记录,并有助于推断出生活在北半球高纬度海域的新近新中新雌成虫的起源,系统发育和物种形成。

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