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MagnetoSusceptibility Event and Cyclostratigraphy (MSEC) of the Eifelian- Givetian GSSP and associated boundary sequences in north Africa and Europe

机译:北非和欧洲的伊非利亚-吉维安GSSP的磁化率事件和旋回地层学(MSEC)及其相关的边界层序

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摘要

Magnetosusceptibility event and cyclostratigraphy (MSEC) is used to define magnetic susceptibility (MS) signatures for the Eifelian-Givetian GSSP in southern Morocco and four other Eifelian-Givetian boundary sequences in Morocco, southern France, and the Czech Republic. MSEC data from the GSSP are used to identify nine first-order isochronous MSEC events for chronocorrelation. MSEC data clearly define a new abiotic Late Eifelian MSEC Event that immediately precedes the Eifelian-Givetian boundary and encompasses the biotic Kacdk and otomari Events. The MSEC event begins in the upper Tortodus kockelianus kockelianus Zone and ends in the upper Polygnathus ensensis Zone. This Event occurs in the same stratigraphic position in the boundary sequences studied. The characteristics of the Late Eifelian MSEC Event are those of a prolonged high stand in global sea level.
机译:磁化率事件和旋回地层学(MSEC)用于定义摩洛哥南部的Eifelian-Givetian GSSP以及摩洛哥,法国南部和捷克共和国的其他四个Eifelian-Givetian边界序列的磁化率(MS)签名。来自GSSP的MSEC数据用于识别9个一阶等时MSEC事件以进行时间相关。 MSEC数据清楚地定义了一个新的非生物非伊比利亚晚期MSEC事件,该事件紧接在Eifelian-Givetian边界之前,涵盖了生物性Kacdk和otomari事件。 MSEC事件始于Tortodus kockelianus kockelianus上部地区,结束于Polygnathus ensensis上部地区。该事件在所研究的边界层序中处于相同的地层位置。 Eifelian MSEC事件晚期的特征是全球海平面长期处于高位。

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