TEXL86-based oceanic temperatures in sediment core MD03-2601

We reconstructed subsurface (~45-200 m water depth) temperature variability in the eastern Antarctic continental margin during the late Holocene, using an archaeal lipid-based temperature proxy (TEX86L). Our results reveal that subsurface temperature changes were probably positively coupled to the v...

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Bibliographic Details
Main Authors: Kim, Jung-Hyun, Crosta, Xavier, Willmott, Verónica, Renssen, Hans, Bonnin, Jerome, Helmke, Peer, Schouten, Stefan, Sinninghe Damsté, Jaap S
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
AGE
Calculated from TEX86 (Kim et al.
2010)
CALYPSO
Calypso Corer
DEPTH
sediment/rock
IMAGES X - CADO
Marion Dufresne (1995)
MD032601
MD03-2601
MD130
Southern Ocean
Subsurface temperature
Antarctic
The Antarctic
Antarc*
Ice Sheet
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.788511
https://doi.org/10.1594/PANGAEA.788511
Description
Summary:We reconstructed subsurface (~45-200 m water depth) temperature variability in the eastern Antarctic continental margin during the late Holocene, using an archaeal lipid-based temperature proxy (TEX86L). Our results reveal that subsurface temperature changes were probably positively coupled to the variability of warmer, nutrient-rich Modified Circumpolar Deep Water (MCDW, deep water of the Antarctic circumpolar current) intrusion onto the continental shelf. The TEX86L record, in combination with previously published climatic records, indicates that this coupling was probably related to the thermohaline circulation, seasonal variability in sea ice extent, sea temperature, and wind associated with high frequency climate dynamics at low-latitudes such as internal El Niño Southern Oscillation (ENSO). This in turn suggests a linkage between centennial ENSO-like variability at low-latitudes and intrusion variability of MCDW into the eastern Antarctic continental shelf, which might have further impact on ice sheet evolution.

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