川东北上思剖面瓜达鲁阶(中二叠世)牙形刺动物群

Sun Yadong , Lai Xulong , Jiang Haishui , Luo Genming , Sun Si , Yan Chunbo , Paul B Wignall
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引用次数: 28

摘要

本研究在川东北上思剖面上发现了瓜达鲁阶牙形刺动物群。鉴定出4属9种,识别并建立了3个牙形刺带;它们包括金诺贡多莱拉带、阿塞拉塔带和后塞拉塔带。Roadian和Wordian边界位于距86层顶部5m的间隔内,由牙形石J.aserrata首次出现。Wordian和Capitanian的边界是由J.postserrata首次出现时在距离95号床顶部2.3米的间隔内确定的。大多数样品的颜色蚀变指数(CAI)较低,为1.5–3,表明茅口组大部分地区可能具有形成油源岩的合适热条件。
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Guadalupian (Middle Permian) Conodont Faunas at Shangsi Section, Northeast Sichuan Province

This study recovered the Guadalupian conodont faunas from Shangsi Section in Northeast Sichuan. Four genera and nine species were identified, and three conodont zones were recognized and established; they include Jinogondolella nankingensis Zone, J. aserrata Zone, and J. postserrata Zone. The Roadian and Wordian boundary is set in the interval 5 m from the top of Bed 86 by the first appearance of the conodont J. aserrata. The Wordian and Capitanian boundary is set in the interval 2.3 m from the top of the Bed 95 by the first appearance of J. postserrata. Most of the specimens demonstrated low color alteration index (CAI) as 1.5–3, indicating that most part of the Maokou Formation may have the suitable thermal conditions for the formation of oil source rocks.

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