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首页> 外文期刊>Hydrobiologia >The eveolutionary history of Late Permian Darwinulocopina Sohn, 1988 (Ostracoda) from the Russian Plate
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The eveolutionary history of Late Permian Darwinulocopina Sohn, 1988 (Ostracoda) from the Russian Plate

机译:俄国板块晚期二叠纪达尔文·洛科皮纳·索恩(Ostracoda),1988年的进化史

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Evolutionary trends in Late Permian Darwinulocopina are summarised with reference to extensive collections from eastern European Russia, from the White Sea in the North to the Cis-Caspian in the South. They inhabited large, shallow lakes in which the variety of habitats was favourable for high ostracod diversity. Theree superfamilies are represented:the Darwinuloidea preferred lakes with terrigenous sedimentation and insignificant bicarbonate, the Suchonelloidea inhabited lakes with increased bicarbonate and could also live in low-sulphate waters, and the Darwinuloidoidea inhabited high-bicarbonate water bodies and could also survive in low-magnesium waters. Different evolutionary trends account for the different ages of the crucial stages of development of each super family:the beginning of themid-Taarian for the Darwinuloidea, the late Tatarian for the Suchonelloidea and Darwinuloidoidea.
机译:总结了晚二叠纪达尔文鲁科皮纳河的演变趋势,并参考了东欧俄罗斯的大量藏品,从北部的白海到南部的Cis-里海。他们居住在大而浅的湖泊中,其中多种多样的生境有利于虾类的大量繁殖。其中有超家族:Darwinuloidea喜欢有陆源性沉积和不重要的碳酸氢盐的湖泊,Suchonelloidea栖息于碳酸氢盐增加的湖泊中,也可以生活在低硫酸盐的水域中,而Darwinuloidoidea居住在高碳酸氢盐的水体中,也可以在低镁水中生存水域。不同的进化趋势解释了每个超家族发展关键阶段的不同年龄:达尔文河纲的中泰安时期的开始,苏孔氏纲和达尔文纲的晚期塔塔里时期的开始。

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