卵微化石科(古生代钙质微化石)的新发现及地层分布

Axel Munnecke , Thomas Servais , Daniel Vachard
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引用次数: 8

摘要

利用扫描电子显微镜对古生代石灰石的抛光、刻蚀切片进行观察,发现了钙质微化石和纳米化石,这些化石可归因于Incertae Sedis科Ovummuridae Munnecke, Servais和Vachard, 2000。这些微化石仅保存于Konservat-Lagerstätten,无晚成岩叠印。在捷克巴兰地地区的上志留纪、乌克兰顿涅茨盆地的上石炭世、俄罗斯乌拉尔山脉的下二叠纪和阿富汗兴都库什山脉的上二叠纪都有新的发现。迄今为止完全不为人所知的卵虫科可能在所有古生代,至少从志留纪开始的碳酸盐岩台地中都非常丰富。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New findings and stratigraphical distribution of the Ovummuridae (Palaeozoic calcareous microfossils)

The observation with the scanning electron microscope of polished, etched sections of Palaeozoic limestones enables the discovery of calcareous micro- and nannofossils, which can be attributed to the Incertae Sedis family Ovummuridae Munnecke, Servais and Vachard, 2000. These microfossils are only preserved in Konservat-Lagerstätten without late diagenetic overprint. New findings are made in sections of the Upper Silurian of the Barrandian area, Czech Republic, the Upper Carboniferous of the Donetz basin, Ukraine, the Lower Permian of the Ural mountains, Russia, and the Upper Permian of the Hindu Kush, Afghanistan. The Ovummuridae, which were totally unknown up to now, were possibly very abundant in carbonate platforms of all Palaeozoic periods, at least from the Silurian onward.

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