Late glacial and deglacial age model and biomarker analyses of sediment core MSM05/5_712-2 from the western continental slope of Svalbard

The transition from last glacial to deglacial and subsequently to modern interglacial climate conditions was accompanied by abrupt shifts in the palaeoceanographic setting in the subpolar North Atlantic. Knowledge about the role that sea ice coverage played during these rapid climate reversals is li...

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Bibliographic Details
Main Authors: Müller, Juliane, Stein, Ruediger
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
2,10,14-Trimethyl-6-enyl-7-(3-methylpent-1-enyl)pentadecene
per unit mass total organic carbon
2,10,14-Trimethyl-6-enyl-7-(3-methylpent-1-enyl)pentadecene/2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane ratio
2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane
24-Methylcholesta-5,22E-dien-3beta-ol
4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol
AGE
AWI_Paleo
Calculated
Carbon
organic
total
DEPTH
sediment/rock
Element analyser CHN
LECO
Fram Strait
Gas chromatography - Mass spectrometry (GC-MS)
KAL
Kasten corer
Maria S. Merian
MSM05/5
MSM05/5_712-2
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Phytoplankton biomarker Brassicasterol IP25 index
Phytoplankton biomarker Dinosterol IP25 index
Sedimentation rate
Arctic Ocean
North Atlantic
Phytoplankton
Sea ice
Svalbard
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.833668
https://doi.org/10.1594/PANGAEA.833668

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