(Q97323697)

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Warm upwelling regions in the Pliocene warm period

scientific article published on 10 August 2007

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Warm upwelling regions in the Pliocene warm period (English)

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Petra S. Dekens

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Ana Christina Ravelo

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Matthew D. McCarthy

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publication date

10 August 2007

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published in

Paleoceanography

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22

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3

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Global climate change and intensification of coastal ocean upwelling

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Closing of the Indonesian seaway as a precursor to east African aridification around 3–4 million years ago

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The Pliocene paradox (mechanisms for a permanent El Niño).

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Pliocene mixed-layer oceanography for Site 1241, using combined Mg/Ca and d18O analyses of Globigerinoides sacculifer

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How Can Tropical Pacific Ocean Heat Transport Vary?

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Evolution of the eastern tropical Pacific through Plio-Pleistocene glaciation

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Evidence for slow mixing across the pycnocline from an open-ocean tracer-release experiment

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The Pacific Decadal Oscillation

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Calibration of the alkenone paleotemperature index U37K′ based on core-tops from the eastern South Atlantic and the global ocean (60°N-60°S)

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Post-depositional stability of long-chain alkenones under contrasting redox conditions

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Regional climate shifts caused by gradual global cooling in the Pliocene epoch

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Climatic warming and the decline of zooplankton in the california current

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Air–Sea Interaction and the Seasonal Cycle of the Subtropical Anticyclones*

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An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677

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Future climate change and upwelling in the California Current

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Permanent El Niño-like conditions during the Pliocene warm period

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The Importance of Tropical Sea Surface Temperature Patterns in Simulations of Last Glacial Maximum Climate

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10.1029/2006PA001394

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(Q97323697)

Warm upwelling regions in the Pliocene warm period

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