Last Glacial Maximum seawater temperature estimates based on planktonic foraminifera

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Bibliographic Details
Main Authors: Jonkers, Lukas, Laepple, Thomas, Rillo, Marina C, Shi, Xiaoxu, Dolman, Andrew M, Lohmann, Gerrit, Paul, André, Mix, Alan C, Kucera, Michal
Format: Dataset Open Access
Language:en
Published: PANGAEA 2023
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author Jonkers, Lukas
Laepple, Thomas
Rillo, Marina C
Shi, Xiaoxu
Dolman, Andrew M
Lohmann, Gerrit
Paul, André
Mix, Alan C
Kucera, Michal
author_facet Jonkers, Lukas
Laepple, Thomas
Rillo, Marina C
Shi, Xiaoxu
Dolman, Andrew M
Lohmann, Gerrit
Paul, André
Mix, Alan C
Kucera, Michal
collection Datos científicos de ciencias marinas y ambientales
contents Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS synthesis (https://doi.org/10.1594/PANGAEA.873570; https://doi.org/10.1038/sdata.2017.109) and World Ocean Atlas 1998 temperature (http://www.nodc.noaa.gov/oc5/woa98.html) for calibration. Dissimilarity to the core top data was calculated using the square-chord distance and the temperatures are the weighted averages of the 10 closest analogues. Estimates were averaged for sites where more than a single sample is available.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_962958
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Last Glacial Maximum seawater temperature estimates based on planktonic foraminifera
Jonkers, Lukas
Laepple, Thomas
Rillo, Marina C
Shi, Xiaoxu
Dolman, Andrew M
Lohmann, Gerrit
Paul, André
Mix, Alan C
Kucera, Michal
Center for Marine Environmental Sciences; LGM; MARUM; Planktonic foraminifera; Seawater temperature; transfer function
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS synthesis (https://doi.org/10.1594/PANGAEA.873570; https://doi.org/10.1038/sdata.2017.109) and World Ocean Atlas 1998 temperature (http://www.nodc.noaa.gov/oc5/woa98.html) for calibration. Dissimilarity to the core top data was calculated using the square-chord distance and the temperatures are the weighted averages of the 10 closest analogues. Estimates were averaged for sites where more than a single sample is available.
title Last Glacial Maximum seawater temperature estimates based on planktonic foraminifera
topic Center for Marine Environmental Sciences; LGM; MARUM; Planktonic foraminifera; Seawater temperature; transfer function
url https://doi.org/10.1594/PANGAEA.962958