Analytical results from sediment core MD03-2698

It is well established that orbital scale sea-level changes generated larger transport of sediments into the deep-sea during the last glacial maximum than the Holocene. However, the response of sedimentary processes to abrupt millennial-scale climate variability is rather unknown. Frequency of dista...

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Bibliographic Details
Main Authors: Lebreiro, Susana Martin, Voelker, Antje H L, Vizcaino, Alexis, Abrantes, Fatima F, Alt-Epping, Ulrich, Jung, S, Thouveny, Nicolas, Gràcia, Eulàlia
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
CALYPSO
Calypso Corer
IMAGES
International Marine Global Change Study
Marion Dufresne (1995)
MD03-2698
MD134
PICABIA
Tagus-Sado canyon system
Antarctic
Greenland
Antarc*
Antarctica
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.733461
https://doi.org/10.1594/PANGAEA.733461

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