Sea-ice distribution and ocean temperature variation in the Powell Basin and Scotia Sea, inferred from marine sediment cores PS118_63-1 and PS67/219-1

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Hauptverfasser: Khoo, Wee Wei, Esper, Oliver, Xiao, Wenshen, Hefter, Jens, Müller, Juliane
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2025
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author Khoo, Wee Wei
Esper, Oliver
Xiao, Wenshen
Hefter, Jens
Müller, Juliane
author_facet Khoo, Wee Wei
Esper, Oliver
Xiao, Wenshen
Hefter, Jens
Müller, Juliane
collection Datos científicos de ciencias marinas y ambientales
contents Presently, there is a scarcity of coastal (paleo) sea-ice reconstructions for periods prior to the Last Glacial Maximum. In this study, we investigated sea ice and ocean temperature proxies from marine sediment core PS118_63-1 from the Powell Basin, NW Weddell Sea. Past sea-ice characteristics inferred from the sea-ice biomarker IPSO25, alongside phytoplankton biomarkers, TOC, biogenic opal estimates and diatom assemblages provide a continuous record of past sea-ice conditions and ocean temperature variability, back to the Penultimate Glacial (ca. 145 ka BP). Our results reveal a highly dynamic sea-ice environment, characterized by significant shifts from perennial (sea) ice cover to more seasonal sea-ice cover to open ocean conditions, with no significant glacial-interglacial ocean temperature variability in the Powell Basin. Furthermore, latitudinal tracking of sea-ice distribution and sea surface temperature differences is enabled when comparing diatom-inferred data from the marine sediment core PS67/219-1.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_965042
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Sea-ice distribution and ocean temperature variation in the Powell Basin and Scotia Sea, inferred from marine sediment cores PS118_63-1 and PS67/219-1
Khoo, Wee Wei
Esper, Oliver
Xiao, Wenshen
Hefter, Jens
Müller, Juliane
AWI_Paleo; Biomarkers; Last Interglacial; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Powell basin; Sea ice; Weddell Sea
Presently, there is a scarcity of coastal (paleo) sea-ice reconstructions for periods prior to the Last Glacial Maximum. In this study, we investigated sea ice and ocean temperature proxies from marine sediment core PS118_63-1 from the Powell Basin, NW Weddell Sea. Past sea-ice characteristics inferred from the sea-ice biomarker IPSO25, alongside phytoplankton biomarkers, TOC, biogenic opal estimates and diatom assemblages provide a continuous record of past sea-ice conditions and ocean temperature variability, back to the Penultimate Glacial (ca. 145 ka BP). Our results reveal a highly dynamic sea-ice environment, characterized by significant shifts from perennial (sea) ice cover to more seasonal sea-ice cover to open ocean conditions, with no significant glacial-interglacial ocean temperature variability in the Powell Basin. Furthermore, latitudinal tracking of sea-ice distribution and sea surface temperature differences is enabled when comparing diatom-inferred data from the marine sediment core PS67/219-1.
title Sea-ice distribution and ocean temperature variation in the Powell Basin and Scotia Sea, inferred from marine sediment cores PS118_63-1 and PS67/219-1
topic AWI_Paleo; Biomarkers; Last Interglacial; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Powell basin; Sea ice; Weddell Sea
url https://doi.org/10.1594/PANGAEA.965042