A simple mixing explanation for late Pleistocene changes in the Pacific-South Atlantic benthic δ<sup>13</sup>C gradient
The fact that the deep-ocean benthic δ<sup>13</sup>C minimum shifted from the North Pacific to the South Atlantic during the Last Glacial Maximum is often interpretted as evidence of a change in deep water circulation, such as the development of deep water ventilation in the North Pacifi...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2010-05-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/6/305/2010/cp-6-305-2010.pdf |