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Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene

H.J. Dowsett·T. M. Cronin·R.Z. Poore·R.S. Thompson·R.C. Whatley·A.M. Wood
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Abstract

The Middle Pliocene (∼3 million years ago) has been identified as the last time the Earth was significantly warmer than it was during the Last Interglacial and Holocene. A quantitative micropaleontological paleotemperature transect from equator to high latitudes in the North Atlantic indicates that Middle Pliocene warmth involved increased meridional oceanic heat transport.

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H.J. Dowsett, T. M. Cronin, R.Z. Poore, R.S. Thompson, R.C. Whatley, A.M. Wood. 1992. Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene. https://doi.org/10.1126/science.258.5085.1133

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