Ice volume and paleoclimate history of the Late Paleozoic Ice Age from conodont apatite oxygen isotopes from Naqing (Guizhou, China)
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- 作者：Bo Chena ; chenbo@nigpas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Michael M. Joachimskib ; Xiang-dong Wangc ; Shu-zhong Shena ; Yu-ping Qic ; Wen-kun Qiec
- 关键词：Oxygen isotopes ; Conodont apatite ; Late Palaeozoic Ice Age ; Bashkirian ; Maximum glaciation ; Naqing section
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：15 April 2016
- 年：2016
- 卷：448
- 期：Complete
- 页码：151-161
- 全文大小：4354 K
文摘
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High-resolution and continuous conodont oxygen isotope record spanning the LPIA is reported.
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The highest values of the presented δ18O record are observed in the Bashkirian.
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Bashkirian δ18O maximum coincides with the a major eustatic sea level fall.
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High δ18O values in Bashkirian are interpreted as representing the glacial maximum of the LPIA.