Coupled sedimentary and δ13C records of late Mississippian platform-to-slope successions from South China: Insight into δ13C chemostratigraphy
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- 作者：Jitao Chena ; b ; jtchen@nigpas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Isabel P. Montañ ; ezb ; ipmontanez@ucdavis.edu" class="auth_mail" title="E-mail the corresponding author ; Yuping Qia ; ypqi@nigpas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Xiangdong Wanga ; xdwang@nigpas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Qiulai Wanga ; qiulai.wang@yandex.com" class="auth_mail" title="E-mail the corresponding author ; Wei Lina ; wlin@nigpas.ac.cn" class="auth_mail" title="E-mail the corresponding author
- 关键词：Carbon isotopes of carbonates ; Sedimentary facies ; Stratigraphic correlation ; Visean ; Serpukhovian ; Late Paleozoic ice age ; Karstification
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：15 April 2016
- 年：2016
- 卷：448
- 期：Complete
- 页码：162-178
- 全文大小：7505 K
文摘
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Facies analysis indicates a significant sea-level fall at the V–S boundary interval.
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Well correlated δ13C negative excursions among slope sections are present in the Visean and right above V–S boundary.
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Negative δ13C trend in the Serpukhovian caused by local carbon cycling in a restricted platform
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Correlation between South China section and USA section by both depositional sequences and negative shifting in δ13C values