Stratigraphic tie points of sediment core PS69/899-2

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Main Authors: Fripiat, François, Sigman, Daniel M, Ai, Xuyuan E, Dumoulin, Cédric, Moretti, Simone, Studer, Anja S, Diekmann, Bernhard, Esper, Oliver, Frederichs, Thomas, Lamy, Frank, Liu, Ling, Pattyn, Frank, Schmitt, Mareike, Tiedemann, Ralf, Haug, Gerald H, Martínez-García, Alfredo
Format: Dataset Open Access
Language:en
Published: PANGAEA 2026
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author Fripiat, François
Sigman, Daniel M
Ai, Xuyuan E
Dumoulin, Cédric
Moretti, Simone
Studer, Anja S
Diekmann, Bernhard
Esper, Oliver
Frederichs, Thomas
Lamy, Frank
Liu, Ling
Pattyn, Frank
Schmitt, Mareike
Tiedemann, Ralf
Haug, Gerald H
Martínez-García, Alfredo
author_facet Fripiat, François
Sigman, Daniel M
Ai, Xuyuan E
Dumoulin, Cédric
Moretti, Simone
Studer, Anja S
Diekmann, Bernhard
Esper, Oliver
Frederichs, Thomas
Lamy, Frank
Liu, Ling
Pattyn, Frank
Schmitt, Mareike
Tiedemann, Ralf
Haug, Gerald H
Martínez-García, Alfredo
collection Datos científicos de ciencias marinas y ambientales
contents The age model for PS69/899-2 (doi:10.1594/PANGAEA.983936) was developed using a combination of stratigraphic markers and Undatable age-depth modeling routine (Lougheed and Obrochta, 2019). Stratigraphic markers employed include TEX86-based SST, RPI, radiocarbon ages on total sedimentary organic matter, and the last occurence datum of the diatom Rouxia leventerae (Zielinski et al., 2002). The TEX86-based SST record from core PS69/899-2 was aligned with the Antarctic temperature stack compiled from ice core data (Parrenin et al., 2013), while the RPI record was aligned with the PISO-1500 paleointensity stack (Channell et al., 2009). Radiocarbon ages were calibrated using the Marine 20 calibration data (Heaton et al., 2023), assuming a marine reservoir age of 1200 years for the Holocene and of 2200 years for glacial periods (Rafter et al., 2022).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_983940
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Stratigraphic tie points of sediment core PS69/899-2
Fripiat, François
Sigman, Daniel M
Ai, Xuyuan E
Dumoulin, Cédric
Moretti, Simone
Studer, Anja S
Diekmann, Bernhard
Esper, Oliver
Frederichs, Thomas
Lamy, Frank
Liu, Ling
Pattyn, Frank
Schmitt, Mareike
Tiedemann, Ralf
Haug, Gerald H
Martínez-García, Alfredo
Age, dated; Age, dated, standard deviation; Age, dating method; ANT-XXIII/9; DEPTH, sediment/rock; Diatom; Indian Ocean; IRD; KL; nitrogen isotope; Piston corer (BGR type); Polarstern; PS69; PS69/899-2; RPI; Southern Ocean; TEX86
The age model for PS69/899-2 (doi:10.1594/PANGAEA.983936) was developed using a combination of stratigraphic markers and Undatable age-depth modeling routine (Lougheed and Obrochta, 2019). Stratigraphic markers employed include TEX86-based SST, RPI, radiocarbon ages on total sedimentary organic matter, and the last occurence datum of the diatom Rouxia leventerae (Zielinski et al., 2002). The TEX86-based SST record from core PS69/899-2 was aligned with the Antarctic temperature stack compiled from ice core data (Parrenin et al., 2013), while the RPI record was aligned with the PISO-1500 paleointensity stack (Channell et al., 2009). Radiocarbon ages were calibrated using the Marine 20 calibration data (Heaton et al., 2023), assuming a marine reservoir age of 1200 years for the Holocene and of 2200 years for glacial periods (Rafter et al., 2022).
title Stratigraphic tie points of sediment core PS69/899-2
topic Age, dated; Age, dated, standard deviation; Age, dating method; ANT-XXIII/9; DEPTH, sediment/rock; Diatom; Indian Ocean; IRD; KL; nitrogen isotope; Piston corer (BGR type); Polarstern; PS69; PS69/899-2; RPI; Southern Ocean; TEX86
url https://doi.org/10.1594/PANGAEA.983940