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首页> 外文期刊>Estonian Journal of Earth Sciences >The early Katian (Late Ordovician) reefs near Saku, northern Estonia and the age of the Saku Member, Vasalemma Formation
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The early Katian (Late Ordovician) reefs near Saku, northern Estonia and the age of the Saku Member, Vasalemma Formation

机译:爱沙尼亚北部萨库附近的早期凯迪安(晚奥陶纪)珊瑚礁以及萨库成员瓦萨勒玛组的年龄

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>>Reefs developed simultaneously during the latest Sandbian/earliest Katian global Guttenberg Isotopic Carbon Excursion (GICE) in several places across Baltoscandia. Latest Sandbian/earliest Katian patch reefs are also described from the Vasalemma Formation of northern Estonia. The Saku Member of the Vasalemma Formation was previously considered as a proximal facies related to the reefs. However, the Saku Member clearly post-dates the GICE interval and ranges from the latest Keila to Rakvere in terms of regional stages. Some small reefs occur in direct proximity to the stratotype of the Saku Member. New ?′13C data from the stratotype section and the adjacent reefs indicate that these reefs developed before the deposition of the Saku Member during the GICE interval. The chemostratigraphic data support the hypothesis of a short-time Baltoscandian reef growth event that terminated during the GICE interval.
机译:> >在最新的桑第人/最古老的凯迪安全球古腾堡同位素碳游览(GICE)中,珊瑚礁同时在巴尔托斯坎迪亚的多个地方同时发展。从爱沙尼亚北部的瓦萨勒玛组也描述了最新的桑迪比亚/最早的凯迪安斑礁。 Vasalemma组的Saku成员以前被认为是与珊瑚礁相关的近海相。但是,佐久成员显然将GICE的时间间隔推迟了,从区域阶段来看,范围从最新的凯伊拉到拉克韦尔。一些小珊瑚礁直接出现在佐久成员的地层上。从平流层剖面和邻近的礁石获得的新的α' 13 C数据表明,这些礁石是在GICE间隔期间在Saku成员沉积之前发育的。化学地层学数据支持了在GICE间隔内终止的短期巴尔托斯卡尼礁生长事件的假说。

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