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    早三叠世海洋异常的碳-氮-硫同位素记录

    宋虎跃 童金南 杜勇 宋海军 田力 楚道亮

    宋虎跃, 童金南, 杜勇, 宋海军, 田力, 楚道亮, 2018. 早三叠世海洋异常的碳-氮-硫同位素记录. 地球科学, 43(11): 3922-3931. doi: 10.3799/dqkx.2018.334
    引用本文: 宋虎跃, 童金南, 杜勇, 宋海军, 田力, 楚道亮, 2018. 早三叠世海洋异常的碳-氮-硫同位素记录. 地球科学, 43(11): 3922-3931. doi: 10.3799/dqkx.2018.334
    Song Huyue, Tong Jinnan, Du Yong, Song Haijun, Tian Li, Chu Daoliang, 2018. Large Perturbed Marine Carbon-Nitrogen-Sulfur Isotopes during Early Triassic. Earth Science, 43(11): 3922-3931. doi: 10.3799/dqkx.2018.334
    Citation: Song Huyue, Tong Jinnan, Du Yong, Song Haijun, Tian Li, Chu Daoliang, 2018. Large Perturbed Marine Carbon-Nitrogen-Sulfur Isotopes during Early Triassic. Earth Science, 43(11): 3922-3931. doi: 10.3799/dqkx.2018.334

    早三叠世海洋异常的碳-氮-硫同位素记录

    doi: 10.3799/dqkx.2018.334
    基金项目: 

    国家自然科学基金项目 41872033

    安徽省国土资源科技项目 2016-K-5

    湖北省自然科学基金项目 2017CFB610

    国家自然科学基金项目 41402302

    国家自然科学基金项目 41661134047

    详细信息
      作者简介:

      宋虎跃(1986-), 男, 副教授, 主要从事古-中生代之交古海洋环境演变研究

    • 中图分类号: P539.7

    Large Perturbed Marine Carbon-Nitrogen-Sulfur Isotopes during Early Triassic

    • 摘要: 早三叠世作为显生宙最大生物灭绝之后的一段特殊地质历史时期,不仅见证了海洋生物的迟缓复苏,而且记录了极其动荡的海洋环境变化,该时期异常的生物环境事件及其机制已经成为当前国际地质学者关注的重大科学问题之一.近些年来,研究学者在早三叠世的碳-氮-硫异常循环研究中取得了许多重要的进展,这对深入理解该时期的环境演变及其对生物复苏的影响十分重要.重点回顾近年来关于早三叠世古海洋碳-氮-硫循环方面的研究进展,对当前存在的科学问题及发展趋势进行分析和总结.

       

    • 图  1  早三叠世碳同位素组成全球对比

      δ13Ccarb结果均相对于VPDB;碳同位素分别引自:华南,Payne et al.(2004);意大利,Horacek et al.(2007a);伊朗,Horacek et al.(2007b);N代表碳同位素负偏事件,P代表碳同位素正漂事件

      Fig.  1.  Global correlation of the Early Triassic carbon isotope changes

      图  2  珠穆朗玛峰地区早三叠世全岩有机碳-氮同位素初步结果

      未发表数据;δ13Corg结果均相对于VPDB;δ15NTN结果均相对于空气中氮气;TN代表全岩总有机氮

      Fig.  2.  Early Triassic organic carbon-nitrogen isotope curves in the Everest area

      图  3  打讲、上关刀、下关刀剖面早三叠世δ34SCAS, δ13Ccarb曲线

      Song et al.(2014)δ13Ccarb结果均相对于VPDB;δ34SCAS结果均相对于VCDT.C.=Clarkina; H.=Hindeodus parvus; I.s.=Isarcicella staeschi; I.i.=Isarcicella isarcica; Ns.=Neospathodus; Nv.= Novispathodus; T.=Triassospathodus; Cs.=Chiosella; Ni.=Nicoraella; Pg.=Paragondolella; Bv.=Budurovignathus

      Fig.  3.  Early Triassic δ34SCAS, δ13Ccarb curves from Dajiang, Lower and Upper Guandao sections

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    • 收稿日期:  2017-12-20
    • 刊出日期:  2018-11-15

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