Breathing more deeply: Deep ocean carbon storage during the mid Pleistocene Transition
The ~100 k.y. cyclicity of the late Pleistocene ice ages started during the mid-Pleistocene transition (MPT), as ice sheets became larger and persisted for longer. The climate system feedbacks responsible for introducing this nonlinear ice sheet response to orbital variations in insolation remain un...
| Main Authors: | , , , , , |
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| Format: | Journal article |
| Published: |
Geological Society of America
2016
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