Sea surface temperature record of ODP Site 202-1233

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Autores principales: Kaiser, Jérôme, Lamy, Frank, Hebbeln, Dierk
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2005
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author Kaiser, Jérôme
Lamy, Frank
Hebbeln, Dierk
author_facet Kaiser, Jérôme
Lamy, Frank
Hebbeln, Dierk
collection Datos científicos de ciencias marinas y ambientales
contents We present the first high-resolution alkenone-derived sea surface temperature (SST) reconstruction in the southeast Pacific (Ocean Drilling Program Site 1233) covering the major part of the last glacial period and the Holocene. The record shows a clear millennial-scale pattern that is very similar to climate fluctuations observed in Antarctic ice cores, suggesting that the Southern Hemisphere high-latitude climate changes extended into the midlatitudes, involving simultaneous changes in air temperatures over Antarctica, sea ice extent, extension of the Antarctic Circumpolar Current, and westerly atmospheric circulation. A comparison to other midlatitude surface ocean records suggests that this "Antarctic" millennial-scale pattern was probably a hemisphere-wide phenomenon. In addition, we performed SST gradient reconstructions over the complete latitudinal range of the Pacific Eastern Boundary Current System for different time intervals during the last 70 kyr. The main results suggest an equatorward displaced subtropical gyre circulation during marine isotope stages 2 and 4.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_737972
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle Sea surface temperature record of ODP Site 202-1233
Kaiser, Jérôme
Lamy, Frank
Hebbeln, Dierk
202-1233; Center for Marine Environmental Sciences; COMPCORE; Composite Core; Joides Resolution; Leg202; MARUM; Ocean Drilling Program; ODP; South-East Pacific
We present the first high-resolution alkenone-derived sea surface temperature (SST) reconstruction in the southeast Pacific (Ocean Drilling Program Site 1233) covering the major part of the last glacial period and the Holocene. The record shows a clear millennial-scale pattern that is very similar to climate fluctuations observed in Antarctic ice cores, suggesting that the Southern Hemisphere high-latitude climate changes extended into the midlatitudes, involving simultaneous changes in air temperatures over Antarctica, sea ice extent, extension of the Antarctic Circumpolar Current, and westerly atmospheric circulation. A comparison to other midlatitude surface ocean records suggests that this "Antarctic" millennial-scale pattern was probably a hemisphere-wide phenomenon. In addition, we performed SST gradient reconstructions over the complete latitudinal range of the Pacific Eastern Boundary Current System for different time intervals during the last 70 kyr. The main results suggest an equatorward displaced subtropical gyre circulation during marine isotope stages 2 and 4.
title Sea surface temperature record of ODP Site 202-1233
topic 202-1233; Center for Marine Environmental Sciences; COMPCORE; Composite Core; Joides Resolution; Leg202; MARUM; Ocean Drilling Program; ODP; South-East Pacific
url https://doi.org/10.1594/PANGAEA.737972