Combined ages of excess 210Pb and 137Cs of sediment core JPS-1 from Lake Jingpo, northeast China

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1. Verfasser: Katsuta, Nagayoshi
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Sprache:en
Veröffentlicht: PANGAEA 2026
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author Katsuta, Nagayoshi
author_facet Katsuta, Nagayoshi
collection Datos científicos de ciencias marinas y ambientales
contents Due to changing East Asian summer monsoon (EASM) and East Asian winter monsoon (EAWM) during Holocene, the sediment cores were collected in Lake Jingpo in northeast China and were investigated to understand the variability of EASM precipitation and its possible mechanism. Sediment cores JB-A (9.76 m) and JPS-1 (0.32 m) were collected in August 2012 using the piston corer and gravity core sampler, respectively. The ages of JB-A and JPS-1 cores are 6092 years and 100 years based on the14C dates and the combined ages of excess 210Pb and 137Cs. Geochemical proxies of EASM precipitation were reconstructed by elemental compositions such as SiO2, TiO2, Al2O3, Fe2O3, MnO, CaO, Na2O, K2O, P2O5, CIA, and LOI, analyzed with the glass-bead XRF quantitative method. Multi-proxies of EAWM wind strength were reconstructed from the Mn/Fe ratio, grain-sizes, and biogenic silica, analyzed with the glass-bead XRF quantitative method, the laser diffraction, and the ICP-AES, respectively.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_974365
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Combined ages of excess 210Pb and 137Cs of sediment core JPS-1 from Lake Jingpo, northeast China
Katsuta, Nagayoshi
14C dating; Caesium-137; Caesium-137, standard deviation; CIA; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; JPS-1; Lake Jingpo; Lake Jinpo; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Lead-214; Lead-214, standard deviation; Northeast China; Potassium-40; Potassium-40, standard deviation; Sample code/label; Sedimentary geochemistry
Due to changing East Asian summer monsoon (EASM) and East Asian winter monsoon (EAWM) during Holocene, the sediment cores were collected in Lake Jingpo in northeast China and were investigated to understand the variability of EASM precipitation and its possible mechanism. Sediment cores JB-A (9.76 m) and JPS-1 (0.32 m) were collected in August 2012 using the piston corer and gravity core sampler, respectively. The ages of JB-A and JPS-1 cores are 6092 years and 100 years based on the14C dates and the combined ages of excess 210Pb and 137Cs. Geochemical proxies of EASM precipitation were reconstructed by elemental compositions such as SiO2, TiO2, Al2O3, Fe2O3, MnO, CaO, Na2O, K2O, P2O5, CIA, and LOI, analyzed with the glass-bead XRF quantitative method. Multi-proxies of EAWM wind strength were reconstructed from the Mn/Fe ratio, grain-sizes, and biogenic silica, analyzed with the glass-bead XRF quantitative method, the laser diffraction, and the ICP-AES, respectively.
title Combined ages of excess 210Pb and 137Cs of sediment core JPS-1 from Lake Jingpo, northeast China
topic 14C dating; Caesium-137; Caesium-137, standard deviation; CIA; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; JPS-1; Lake Jingpo; Lake Jinpo; Lead-210; Lead-210, standard deviation; Lead-210 excess; Lead-210 excess, standard deviation; Lead-214; Lead-214, standard deviation; Northeast China; Potassium-40; Potassium-40, standard deviation; Sample code/label; Sedimentary geochemistry
url https://doi.org/10.1594/PANGAEA.974365