Gespeichert in:
Bibliographische Detailangaben
1. Verfasser: Dearing Crampton-Flood, Emily
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2026
Schlagworte:
Online-Zugang:https://doi.org/10.1594/PANGAEA.912082
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
_version_ 1867171374155431936
author Dearing Crampton-Flood, Emily
author_facet Dearing Crampton-Flood, Emily
collection Datos científicos de ciencias marinas y ambientales
contents The mid-Piacenzian Warm Period (mPWP, 3264-3025 ka) represents the most recent interval in Earth's history where atmospheric CO2 levels were similar to today. Here, we present a multi-proxy record of Pliocene climate change in the coastal Southern North Sea Basin (SNSB) based on the sedimentary record from borehole Hank, the Netherlands (drilled by TNO, Dutch Geological Survey). We present the stable oxygen and carbon isotope (δ18O and δ13C) measurements of the endobenthic foraminifera species Cassidulina laevigata, and present a new age model for the late Pliocene of the Southern North Sea. This results in a tuned age framework for the SNSB for the Late Pliocene (~3190-2770 ka). Our multi-proxy climate reconstruction for this interval includes biomarker-based SST reconstructions (TEX86, UK37, LDI).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_912082
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Climate proxies recorded in sediments from borehole Hank, Netherlands, for the Pliocene of the North Sea
Dearing Crampton-Flood, Emily
Age model; Biomarkers; North Sea; Pliocene climate; temperature reconstruction
The mid-Piacenzian Warm Period (mPWP, 3264-3025 ka) represents the most recent interval in Earth's history where atmospheric CO2 levels were similar to today. Here, we present a multi-proxy record of Pliocene climate change in the coastal Southern North Sea Basin (SNSB) based on the sedimentary record from borehole Hank, the Netherlands (drilled by TNO, Dutch Geological Survey). We present the stable oxygen and carbon isotope (δ18O and δ13C) measurements of the endobenthic foraminifera species Cassidulina laevigata, and present a new age model for the late Pliocene of the Southern North Sea. This results in a tuned age framework for the SNSB for the Late Pliocene (~3190-2770 ka). Our multi-proxy climate reconstruction for this interval includes biomarker-based SST reconstructions (TEX86, UK37, LDI).
title Climate proxies recorded in sediments from borehole Hank, Netherlands, for the Pliocene of the North Sea
topic Age model; Biomarkers; North Sea; Pliocene climate; temperature reconstruction
url https://doi.org/10.1594/PANGAEA.912082