High‐amplitude variations in North Atlantic sea surface temperature during the early Pliocene warm period

Paleoceanography - Tập 24 Số 2 - 2009
K. T. Lawrence1, Timothy D. Herbert2, Catherine Brown2, Maureen E. Raymo3, Alan M. Haywood4
1Department of Geology and Environmental Geosciences Lafayette College Easton Pennsylvania USA
2Department of Geological Sciences, Brown University, Providence, Rhode Island, USA
3Department of Earth Sciences Boston University Boston Massachusetts USA
4School of Earth and Environment, University of Leeds, Leeds, UK

Tóm tắt

We provide the first continuous, orbital‐resolution sea surface temperature (SST) record from the high‐latitude North Atlantic, a region critical to understanding the origin of the Plio‐Pleistocene ice ages and proximal to regions that became frequently glaciated after ∼2.7 Ma. We analyzed sediments from Ocean Drilling Program Site 982 over the last 4 Ma for their alkenone unsaturation index and compared this surface water signal to a benthic δ18O record obtained from the same section. We find that while ocean surface temperatures were significantly warmer (∼6°C) than modern temperatures during the early Pliocene, they were also as variable as those during the late Pleistocene, a surprising result in light of the subdued variance of oxygen isotopic time series during the interval of 3–5 Ma. We propose two possible explanations for the high orbital‐scale SST variability observed: either that a strong, high‐latitude feedback mechanism not involving large continental ice sheets alternately cooled and warmed a broad region of the northern high latitudes or that by virtue of its location near the northern margin of the North Atlantic Drift, the site was unusually sensitive to obliquity‐driven climate shifts. On supraorbital time scales, a strong, sustained cooling of North Atlantic SSTs (∼4.5°C) occurred from 3.5 to 2.5 Ma and was followed by an interval of more modest cooling (an additional 1.5°C) from 2.5 Ma to the present. Evolutionary orbital‐scale phase relationships between North Atlantic SST and benthic δ18O show that SST began to lead δ18O significantly coincident with the onset of strong cooling at Site 982 (∼3.5 Ma). We speculate that these changes were related to the growth and subsequent persistence of a Greenland ice sheet of approximately modern size through interglacial states.

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Paleoceanography

Tập 24 Số 2

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