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首页> 外文期刊>Acta Palaeontologica Polonica >Worldwide distribution of the modiomorphid bivalve genus caspiconcha in late mesozoic hydrocarbon seeps
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Worldwide distribution of the modiomorphid bivalve genus caspiconcha in late mesozoic hydrocarbon seeps

机译:晚期中生代烃渗流中模态双壳类双孢霉属的全球分布

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Exceptionally well preserved specimens of the bivalve mollusc Modiola major were collected from a Lower Cretaceous (Barremian) hydrocarbon seep deposit in northern California. This material, together with the type series of M. major, and various other specimens from Upper Jurassic to Lower Cretaceous seep localities in California, is redescribed and referred to the hydrocarbon seep-restricted modiomorphid genus Caspiconcha. We include also a description of Myoconcha americana because some previous reports have incorrectly synonymized Myoconcha americana with Caspiconcha major. In addition, we report Caspiconcha sp. from a Lower Cretaceous (Albian) hydrocarbon seep from Hokkaido, Japan, and we review all currently described species of Caspiconcha, and other species that probably belong to this genus. We demonstrate that Caspiconcha had a widespread distribution in Late Jurassic to Early Cretaceous hydrocarbon seeps, but became rare thereafter, with the last representative occurring in Upper Cretaceous strata of Japan. This macroevolutionary pattern is similar to that observed in the seep-restricted brachiopods. After the decline of Caspiconcha at the end of the Early Cretaceous and its last occurrence in the Campanian, the ecological niche of epifaunal to semi-infaunal seep endemic bivalves was largely vacant and not reoccupied until the Eocene with the appearance of the vesicomyid and bathymodiolin bivalves. The formal placement of M. major into the genus Caspiconcha restricts the fossil record of mytilids at seeps to post-Mesozoic times, and thus there is less discrepancy between the fossil record of chemosynthetic mytilids and their divergence age estimates from molecular data.
机译:从加利福尼亚北部的一个下白垩统(巴雷米亚)的烃类渗流矿床中收集了保存完好的双壳软体动物Modiola major的标本。重新描述了这种材料,以及M. major的类型系列以及加利福尼亚上侏罗纪至下白垩统渗漏部位的各种其他标本,并将其称为烃渗漏限制型单孢子虫属Caspiconcha。我们还包括对美洲Myoconcha的描述,因为以前的一些报道错误地将美洲Myoconcha与Caspiconcha major同义词。另外,我们报告Caspiconcha sp。来自日本北海道的下白垩统(阿拉伯)碳氢化合物的渗漏,我们审查了目前描述的所有隐孢子虫属物种,以及其他可能属于该属的物种。我们证明,Caspiconcha在侏罗纪晚期至白垩纪早期的烃类渗流中分布广泛,但此后变得稀少,最后一个代表发生在日本的上白垩统地层。这种宏观进化的模式类似于在渗透受限的腕足类动物中观察到的模式。在早白垩世末期Caspiconcha下降及其在Campanian的最后一次出现之后,表生真菌到表生真菌的生态位大部分处于空缺状态,直到始新世才出现,并出现了囊藻和双桥odi藻类双壳虫。 。正式将M.major放到Caspiconcha属中,将在渗水处的Mytilids化石记录限制在中生代以后,因此化学合成Mytilids的化石记录与其根据分子数据得出的发散年龄估计之间的差异较小。

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