Comment on “Coccolith Sr/Ca records of productivity during the Paleocene‐Eocene thermal maximum from the Weddell Sea” by Heather M. Stoll and Santo Bains

Comment on “Coccolith Sr/Ca records of productivity during the Paleocene‐Eocene thermal maximum from the Weddell Sea” by Heather M. Stoll and Santo Bains
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对希瑟·M·斯托尔 (Heather M. Stoll) 和桑托·贝恩斯 (Santo Bains) 撰写的“威德尔海古新世-始新世热最大值期间的石珊瑚 Sr/Ca 生产力记录”的评论

DOI：
10.1029/2003pa000953
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发表时间：
2004
期刊：
影响因子：
--
通讯作者：
D. J. Thomas
D. J. Thomas
中科院分区：
--
文献类型：
--
作者：
T. Bralower;D. Kelly;D. J. Thomas

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[01] The introduction of massive amounts of carbon to the atmosphere-ocean system during the Paleocene-Eocene thermal maximum (PETM) at 55 Ma is associated with transient ($120–200 kyr duration) global warming and a host of other environmental changes. Recent investigations have focused on the response of the surface ocean and its role in the removal of excess carbon [Bains et al., 2000;