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A Cordylodus fauna from the SW Gulf of Bothnia, Sweden

机译:来自瑞典博特尼亚海湾的线虫类动物

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摘要

A conodont fauna including several species of Cordylodus was retrieved from two glacial siltstone boulders found on the shore of Lilltuppen, a small island immediately off the Swedish coast in the Gulf of Bothnia at c. 61 degrees N, 17 degrees E. The erratics are remnants of a poorly known level in the Swedish stratigraphic succession. They probably derive from a nearby point on the floor of the Baltic Sea and constitute an example of an "eastern facies", reminiscent of part of the Kallavere Formation in northern Estonia. The conodont fauna closely resembles that of the Maardu Member of the Kallavere Formation, and indicates a position in the Corcylodus lindstromi conodont zone just at the Cambrian-Ordovician boundary.
机译:从Lilltuppen岸上发现的两个冰川粉砂岩巨石中检索到了包括几种虫科的牙形动物区系,Lilltuppen是一个位于瑞典沿海地区的小岛,位于博特尼亚湾,大约在c。北纬61度,东经17度。不稳定因素是瑞典地层演替中未知水平的残余物。它们可能来自波罗的海海底附近的一个点,构成了“东部相”的一个例子,让人联想到爱沙尼亚北部的卡拉维雷组。该牙形动物区系与Kallavere组的Maardu成员非常相似,并指示在寒武纪-奥陶纪边界的Corcylodus lindstromi牙形石区域中的位置。

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