Sea-surface temperature reconstruction of the South China Sea

The tropical ocean plays a major role in global climate. It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during past abrupt climate events in order to gain insight into the mechanisms of global climate change. Here we present alkenone sea...

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Bibliographic Details
Main Authors: Kienast, Markus, Steinke, Stephan, Stattegger, Karl, Calvert, Stephen E
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
GIK18252-3
GIK18287-3
Gravity corer (Kiel type)
SL
SO115
SO115_05
SO115_40
Sonne
SUNDAFLUT
Sunda Shelf
Vietnam shelf
Greenland
Sunda
Greenland Ice Sheet Project
ice core
Ice Sheet
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738464
https://doi.org/10.1594/PANGAEA.738464
Description
Summary:The tropical ocean plays a major role in global climate. It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during past abrupt climate events in order to gain insight into the mechanisms of global climate change. Here we present alkenone sea surface temperature (SST) records from the tropical South China Sea that show an abrupt temperature increase of at least 1°C at the end of the last glacial period. Within the recognized dating uncertainties, this SST increase is synchronous with the Bølling warming observed at 14.6 thousand years ago in the Greenland Ice Sheet Project 2 ice core.

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