(Table 1) Age determination of sediment core RC11-83

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Hauptverfasser: Charles, Christopher D, Lynch-Stieglitz, Jean, Ninnemann, Ulysses S, Fairbanks, Richard G
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1996
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author Charles, Christopher D
Lynch-Stieglitz, Jean
Ninnemann, Ulysses S
Fairbanks, Richard G
author_facet Charles, Christopher D
Lynch-Stieglitz, Jean
Ninnemann, Ulysses S
Fairbanks, Richard G
collection Datos científicos de ciencias marinas y ambientales
contents Correlation of Southern Ocean deep sea sediment core records with ice core records of polar climate delineates with unprecedented detail the relationship between high latitude climate and the ocean's thermohaline circulation over the last 80,000 years. Our observations suggest that, while North Atlantic Deep Water variability manifests itself clearly in Southern Ocean nutrient proxy records over periods as short as 500 yr, this deep water variability did not promote a direct link between climate variability in the high latitudes of the two hemispheres on millennial timescales. In particular, the proxy records indicate that, on average, northern hemisphere climate fluctuations lagged those of the southern hemisphere by 1500 yr.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_837314
institution PANGAEA
language en
publishDate 1996
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Age determination of sediment core RC11-83
Charles, Christopher D
Lynch-Stieglitz, Jean
Ninnemann, Ulysses S
Fairbanks, Richard G
Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated material; Calendar age; DEPTH, sediment/rock; Laboratory code/label; PC; Piston corer; RC11; RC1112; RC11-83; Robert Conrad
Correlation of Southern Ocean deep sea sediment core records with ice core records of polar climate delineates with unprecedented detail the relationship between high latitude climate and the ocean's thermohaline circulation over the last 80,000 years. Our observations suggest that, while North Atlantic Deep Water variability manifests itself clearly in Southern Ocean nutrient proxy records over periods as short as 500 yr, this deep water variability did not promote a direct link between climate variability in the high latitudes of the two hemispheres on millennial timescales. In particular, the proxy records indicate that, on average, northern hemisphere climate fluctuations lagged those of the southern hemisphere by 1500 yr.
title (Table 1) Age determination of sediment core RC11-83
topic Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated material; Calendar age; DEPTH, sediment/rock; Laboratory code/label; PC; Piston corer; RC11; RC1112; RC11-83; Robert Conrad
url https://doi.org/10.1594/PANGAEA.837314