日本西南黑川地区志留纪放射虫的U/Pb SHRIMP年龄

Jonathan C. Aitchison , Shigeki Hada , Trevor Ireland , Shin-ichi Yoshikura
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引用次数: 41

摘要

放射虫在日本西南部黑川地体中古生代凝灰岩中有丰富的分布。本文描述了从几个地方恢复的保存完好的志留纪放射虫动物群,包括四个新种:Ceratoikiscum kurosegum n. sp., Fusalfanus?Futobari的kononomoriensis n.sp ?京加莫里氏菌(jingamoriensis n.sp)和Futobari?在同一地层中,缺少属于其他分类群的化石,这给确定黑川放射虫动物群的精确年龄带来了困难。序列内凝灰岩单元火山碎屑锆石U/Pb SHRIMP年龄反映了温洛克期[427.2±7.6]和普里多期[408.9±7.6]年龄,消除了对黑泽川层序凝灰岩志留纪年龄的模糊性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ages of Silurian radiolarians from the Kurosegawa terrane, southwest Japan constrained by U/Pb SHRIMP data

Radiolarians are abundant in mid-Paleozoic tuffs of the Kurosegawa terrane of southwest Japan. Well preserved Silurian radiolarian faunas recovered from several localities are described herein and include four new species: Ceratoikiscum kurosegum n. sp., Fusalfanus? konomoriensis n. sp., Futobari? jingamoriensis n. sp., and Futobari? tosaensis n. sp. The absence, within the same strata, of fossils belonging to other taxonomic groups has presented difficulties in determining the precise ages of the Kurosegawa radiolarian faunas. U/Pb SHRIMP ages of pyroclastic zircons from tuff units within the succession indicate Wenlockian [427.2 ± 7.6] and Pridolian [408.9 ± 7.6] ages and remove ambiguity regarding the Silurian age of tuffaceous rocks in the Kurosegawa sequence.

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