Late Quaternary investigation of sediments from Vankervelsvlei

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Hauptverfasser: Strobel, Paul, Bliedtner, Marcel, Carr, Andrew S, Struck, Julian, Du Plessis, Nadia, Glaser, Bruno, Meadows, Michael E, Quick, Lynne J, Zech, Michael, Zech, Roland, Haberzettl, Torsten
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2022
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author Strobel, Paul
Bliedtner, Marcel
Carr, Andrew S
Struck, Julian
Du Plessis, Nadia
Glaser, Bruno
Meadows, Michael E
Quick, Lynne J
Zech, Michael
Zech, Roland
Haberzettl, Torsten
author_facet Strobel, Paul
Bliedtner, Marcel
Carr, Andrew S
Struck, Julian
Du Plessis, Nadia
Glaser, Bruno
Meadows, Michael E
Quick, Lynne J
Zech, Michael
Zech, Roland
Haberzettl, Torsten
collection Datos científicos de ciencias marinas y ambientales
contents This study investigates Late Quaternary sediments from Vankervelsvlei, a peatland located at 152 m above present sea level at the southern Cape coast of South Africa. A 15 m long sediment record was recovered from the site in 2016 and analysed using a multi-proxy approach. This includes analyses of water content, loss on ignition, grain size, organic (C, N and their isotopic composition) and inorganic (Al, Fe, Sr, Ti) elemental composition as well as compound-specific stable hydrogen and carbon isotopes from leaf wax-derived n-alkanes and compound-specific stable oxygen isotopes from hemicellulose-derived sugars. Stable hydrogen and oxygen isotopes are additionally coupled in a δ2Hn-alkane–δ18Osugar paleohygrometer. Parts of the data derive from a pioneer study by Strobel et al (2019) and have subsequently been extended by Strobel et al (submitted). Distinct environmental changes occurred at Vankervelsvlei during the Late Quaternary and the applied multi-proxy approach enables to reconstruct past variations in the atmospheric source of precipitation and local moisture availability at the site, which is coherent with other records located along the southern Cape coast of South Africa.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_940148
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Late Quaternary investigation of sediments from Vankervelsvlei
Strobel, Paul
Bliedtner, Marcel
Carr, Andrew S
Struck, Julian
Du Plessis, Nadia
Glaser, Bruno
Meadows, Michael E
Quick, Lynne J
Zech, Michael
Zech, Roland
Haberzettl, Torsten
African Summer Monsoon; Compound-specific carbon isotopes; Compound-specific hydrogen isotopes; Compound-specific oxygen isotopes; coupled δ2Hn-alkane–δ18Osugar paleohygrometer; elemental geochemistry; Grain Size; hydrology; leaf-wax n-alkane; Paleoclimate; peat geochemistry; precipitation reconstruction; relative humidity; South Africa; sugars; Westerlies
This study investigates Late Quaternary sediments from Vankervelsvlei, a peatland located at 152 m above present sea level at the southern Cape coast of South Africa. A 15 m long sediment record was recovered from the site in 2016 and analysed using a multi-proxy approach. This includes analyses of water content, loss on ignition, grain size, organic (C, N and their isotopic composition) and inorganic (Al, Fe, Sr, Ti) elemental composition as well as compound-specific stable hydrogen and carbon isotopes from leaf wax-derived n-alkanes and compound-specific stable oxygen isotopes from hemicellulose-derived sugars. Stable hydrogen and oxygen isotopes are additionally coupled in a δ2Hn-alkane–δ18Osugar paleohygrometer. Parts of the data derive from a pioneer study by Strobel et al (2019) and have subsequently been extended by Strobel et al (submitted). Distinct environmental changes occurred at Vankervelsvlei during the Late Quaternary and the applied multi-proxy approach enables to reconstruct past variations in the atmospheric source of precipitation and local moisture availability at the site, which is coherent with other records located along the southern Cape coast of South Africa.
title Late Quaternary investigation of sediments from Vankervelsvlei
topic African Summer Monsoon; Compound-specific carbon isotopes; Compound-specific hydrogen isotopes; Compound-specific oxygen isotopes; coupled δ2Hn-alkane–δ18Osugar paleohygrometer; elemental geochemistry; Grain Size; hydrology; leaf-wax n-alkane; Paleoclimate; peat geochemistry; precipitation reconstruction; relative humidity; South Africa; sugars; Westerlies
url https://doi.org/10.1594/PANGAEA.940148