Multiproxy sedimentation patterns of sediment cores from the continental margin off northeast Brazil

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Main Authors: Jennerjahn, Tim C, Ittekkot, Venugopalan, Arz, Helge Wolfgang, Behling, Hermann, Pätzold, Jürgen, Wefer, Gerold
Format: Dataset Open Access
Language:en
Published: PANGAEA 2004
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author Jennerjahn, Tim C
Ittekkot, Venugopalan
Arz, Helge Wolfgang
Behling, Hermann
Pätzold, Jürgen
Wefer, Gerold
author_facet Jennerjahn, Tim C
Ittekkot, Venugopalan
Arz, Helge Wolfgang
Behling, Hermann
Pätzold, Jürgen
Wefer, Gerold
collection Datos científicos de ciencias marinas y ambientales
contents Tropical regions have been reported to play a key role in climate dynamics. To date, however, there are uncertainties in the timing and the amplitude of the response of tropical ecosystems to millennial-scale climate change. We present evidence of an asynchrony between terrestrial and marine signals of climate change during Heinrich events preserved in marine sediment cores from the Brazilian continental margin. The inferred time lag of about 1000 to 2000 years is much larger than the ecological response to recent climate change and appears to be related to the nature of hydrological changes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_779792
institution PANGAEA
language en
publishDate 2004
publisher PANGAEA
record_format pangaea
spellingShingle Multiproxy sedimentation patterns of sediment cores from the continental margin off northeast Brazil
Jennerjahn, Tim C
Ittekkot, Venugopalan
Arz, Helge Wolfgang
Behling, Hermann
Pätzold, Jürgen
Wefer, Gerold
Center for Marine Environmental Sciences; GeoB; GeoB3104-1; GeoB3911-3; GeoB3912-1; Geosciences, University of Bremen; Gravity corer (Kiel type); JOPSII-6; M34/4; MARUM; Meteor (1986); NE-Brazilian continental margin; Northeast Brasilian Margin; SL; Victor Hensen
Tropical regions have been reported to play a key role in climate dynamics. To date, however, there are uncertainties in the timing and the amplitude of the response of tropical ecosystems to millennial-scale climate change. We present evidence of an asynchrony between terrestrial and marine signals of climate change during Heinrich events preserved in marine sediment cores from the Brazilian continental margin. The inferred time lag of about 1000 to 2000 years is much larger than the ecological response to recent climate change and appears to be related to the nature of hydrological changes.
title Multiproxy sedimentation patterns of sediment cores from the continental margin off northeast Brazil
topic Center for Marine Environmental Sciences; GeoB; GeoB3104-1; GeoB3911-3; GeoB3912-1; Geosciences, University of Bremen; Gravity corer (Kiel type); JOPSII-6; M34/4; MARUM; Meteor (1986); NE-Brazilian continental margin; Northeast Brasilian Margin; SL; Victor Hensen
url https://doi.org/10.1594/PANGAEA.779792