Stable carbon isotope ratios of alkane of IODP Hole 302-M0004A ...

The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming approx ~55 million years ago, superimposed on an already warm world (Zachos et al., 2003, doi:10.1126/science.1090110; Bowen et al., 2004, doi:10.1038/nature03115; Thomas et al., 2002, doi:10.1130/0091-7613(20...

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Bibliographic Details
Main Authors: Pagani, Mark, Pedentchouk, Nikolai, Huber, Matthew, Sluijs, Appy, Schouten, Stefan, Brinkhuis, Henk, Sinninghe Damsté, Jaap S, Dickens, Gerald Roy, Expedition 302 Scientists
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
DEPTH, sediment/rock
Sample code/label
n-Alkane C17, δ13C
n-Alkane C17, δ13C, standard deviation
n-Alkane C27, δ13C
n-Alkane C27, δ13C, standard deviation
n-Alkane C29, δ13C
n-Alkane C29, δ13C, standard deviation
n-Alkane C17, δD
n-Alkane C17, δD, standard deviation
n-Alkane C27, δD
n-Alkane C27, δD, standard deviation
n-Alkane C29, δD
n-Alkane C29, δD, standard deviation
Mass spectrometer, Finnigan, MAT 253
Exp302
CCGS Captain Molly Kool Vidar Viking
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Arctic Ocean
Global warming
Online Access:https://dx.doi.org/10.1594/pangaea.733130
https://doi.pangaea.de/10.1594/PANGAEA.733130
Description
Summary:The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme global warming approx ~55 million years ago, superimposed on an already warm world (Zachos et al., 2003, doi:10.1126/science.1090110; Bowen et al., 2004, doi:10.1038/nature03115; Thomas et al., 2002, doi:10.1130/0091-7613(2002)030<1067:WTFFTF>2.0.CO;2). This warming is associated with a severe shoaling of the ocean calcite compensation depth **4 and a >2.5 per mil negative carbon isotope excursion in marine and soil carbonates (Zachos et al., 2003, doi:10.1126/science.1090110; Bowen et al., 2004, doi:10.1038/nature03115; Thomas et al., 2002, doi:10.1130/0091-7613(2002)030<1067:WTFFTF>2.0.CO;2; Zachos et al., doi:10.1126/science.1109004). Together these observations indicate a massive release of 13C-depleted carbon (Zachos et al., doi:10.1126/science.1109004) and greenhouse-gas-induced warming. Recently, sediments were recovered from the central Arctic Ocean (Backman et al., 2006, doi:10.2204/iodp.proc.302.2006), ... : Depth, sediment=Depth (mcd) ...

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