Long-chain alkenones, long-chain diols and GDGTs over the last 90 Myrs for sediment core Bass River Site

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Autores principales: de Bar, Marijke W, Rampen, Sebastiaan W, Hopmans, Ellen C, Sinninghe Damsté, Jaap S, Schouten, Stefan
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2019
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author de Bar, Marijke W
Rampen, Sebastiaan W
Hopmans, Ellen C
Sinninghe Damsté, Jaap S
Schouten, Stefan
author_facet de Bar, Marijke W
Rampen, Sebastiaan W
Hopmans, Ellen C
Sinninghe Damsté, Jaap S
Schouten, Stefan
collection Datos científicos de ciencias marinas y ambientales
contents We evaluated changes in the distributions of long-chain alkenones, long-chain diols and GDGTs, lipids commonly used for paleothermometry, over the last 90 Myrs for sediments deposited on the New Jersey shelf (the Bass River site) and assessed potential effects of different ancestral producers and diagenesis on their distributions and their impact on the associated temperature proxies. As reported before, the Paleogene distributions of alkenones are generally similar to those in haptophytes, but unusual alkenone distributions, characterized by a dominant di-unsaturated C40 alkenone, are observed for Late Cretaceous sediments, suggesting different ancestral source organisms for alkenones in this interval. The isoprenoid GDGT distributions remained comparable to modern-day distributions, suggesting that the TEX86 can be applied up to ca. 90 Ma. The Miocene long-chain diol distributions are similar to modern-day distributions, but the older sediments reveal unusual distributions, dominated by the C28 1,12- and C26 1,13-diols, suggesting different source organisms before ~30 Ma. Accordingly, the LDI does not match other paleotemperature proxies, suggesting its applicability might be compromised for sediments older than the Miocene. Our results indicate that of the three proxies, the TEX86 seems to be the most applicable for deep time temperature reconstructions.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_897908
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Long-chain alkenones, long-chain diols and GDGTs over the last 90 Myrs for sediment core Bass River Site
de Bar, Marijke W
Rampen, Sebastiaan W
Hopmans, Ellen C
Sinninghe Damsté, Jaap S
Schouten, Stefan
Bass_River_Site; BR; DRILL; Drilling/drill rig; Leg174AX; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; North American East Coast; Ocean Drilling Program; ODP
We evaluated changes in the distributions of long-chain alkenones, long-chain diols and GDGTs, lipids commonly used for paleothermometry, over the last 90 Myrs for sediments deposited on the New Jersey shelf (the Bass River site) and assessed potential effects of different ancestral producers and diagenesis on their distributions and their impact on the associated temperature proxies. As reported before, the Paleogene distributions of alkenones are generally similar to those in haptophytes, but unusual alkenone distributions, characterized by a dominant di-unsaturated C40 alkenone, are observed for Late Cretaceous sediments, suggesting different ancestral source organisms for alkenones in this interval. The isoprenoid GDGT distributions remained comparable to modern-day distributions, suggesting that the TEX86 can be applied up to ca. 90 Ma. The Miocene long-chain diol distributions are similar to modern-day distributions, but the older sediments reveal unusual distributions, dominated by the C28 1,12- and C26 1,13-diols, suggesting different source organisms before ~30 Ma. Accordingly, the LDI does not match other paleotemperature proxies, suggesting its applicability might be compromised for sediments older than the Miocene. Our results indicate that of the three proxies, the TEX86 seems to be the most applicable for deep time temperature reconstructions.
title Long-chain alkenones, long-chain diols and GDGTs over the last 90 Myrs for sediment core Bass River Site
topic Bass_River_Site; BR; DRILL; Drilling/drill rig; Leg174AX; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; North American East Coast; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.897908