环北极地区的泥盆纪更新世事件

J. Marshall, Gunn Mangerud, M. Bringué, J. Bujak
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引用次数: 1

摘要

现今北极的泥盆纪地层包含丰富多样的陆生地貌组合,特别是中、上泥盆纪剖面;下泥盆统和志留纪地层的孢粉学研究表明,该区孢粉花具有很强的相似性。基于已发表的记录,我们提出了6个末次事件(LOs), 44个首次事件(FOs)和一个顶点事件的汇编,这些事件已被证明在当今北极具有相关性。虽然它们的年代地层分辨率相对较低,而且缺乏独立的年龄控制妨碍了精确的年龄分配,但孢粉学是唯一可以对大多数北极泥盆纪地层进行可靠的年代地层对比的生物地层学学科。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Devonian palynoevents in the circum-Arctic region
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial palynomorphs, particularly from Middle and Upper Devonian sections; few intervals of Lower Devonian and Silurian strata have been palynologically studied, and these demonstrate strong palynofloral similarities across the region. Based on published records, we present a compilation of six last occurrence events (LOs), 44 first occurrence events (FOs) and one acme event that have proven of value in correlation in the present-day Arctic. Although their chronostratigraphic resolution is relatively low, and a scarcity of independent age control hampers precise age assignments, palynology is the only biostratigraphic discipline available for confident chronostratigraphic correlation of most Arctic Devonian strata.
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