Last glacial period lake sediment data from Lake Sihailongwan, N.E. China

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Main Authors: Mingram, Jens, Stebich, Martina, Schettler, Georg, Hu, Yaqin, Dulski, Peter, Nowaczyk, Norbert R, Liu, Qiang, Liu, Jiaqi, You, Haitao, Opitz, Stephan, Rioual, Patrick
Format: Dataset Open Access
Language:en
Published: PANGAEA 2018
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author Mingram, Jens
Stebich, Martina
Schettler, Georg
Hu, Yaqin
Dulski, Peter
Nowaczyk, Norbert R
Liu, Qiang
Liu, Jiaqi
You, Haitao
Opitz, Stephan
Rioual, Patrick
author_facet Mingram, Jens
Stebich, Martina
Schettler, Georg
Hu, Yaqin
Dulski, Peter
Nowaczyk, Norbert R
Liu, Qiang
Liu, Jiaqi
You, Haitao
Opitz, Stephan
Rioual, Patrick
collection Datos científicos de ciencias marinas y ambientales
contents Lake Sihailongwan in Jilin province, NE China, provides the first continuous and almost entirely seasonally laminated sediment record on the East Asian mainland comprising the complete Holocene, the Late-glacial period, and large parts of the Last Glacial. Sediment and palynological proxy data provide a finely resolved regional environmental history of the East Asian monsoon. A varve-based chronology (shl-vc2) has been established for the last 65,000 years and allows a detailed comparison with other long regional and global palaeoclimate records. Vegetation density of the study area depends, on the long run, on precessionally forced insolation changes, with superimposed millennial-scale variability during the Last Glacial. Periodic increase of organic carbon content and thermophilous tree species like Ulmus and Fraxinus and contemporary decrease of shrub Alnus precisely mirror millennial-scale climatic variations primarily known from Greenland ice-cores as Dansgaard-Oeschger cycles, as well as Late-glacial period climate changes. Percentages of trees & shrubs pollen and in particular lake productivity-related data reveal substantial differences between interstadial intensities, with those between 50 – 60 ka BP being more pronounced than the following ones.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_885907
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Last glacial period lake sediment data from Lake Sihailongwan, N.E. China
Mingram, Jens
Stebich, Martina
Schettler, Georg
Hu, Yaqin
Dulski, Peter
Nowaczyk, Norbert R
Liu, Qiang
Liu, Jiaqi
You, Haitao
Opitz, Stephan
Rioual, Patrick
Changbai Mountains region, Jilin Province, NE China; COMPCORE; Composite Core; GeoForschungszentrum Potsdam; GFZ; SHL; Sihailongwan Maar Lake
Lake Sihailongwan in Jilin province, NE China, provides the first continuous and almost entirely seasonally laminated sediment record on the East Asian mainland comprising the complete Holocene, the Late-glacial period, and large parts of the Last Glacial. Sediment and palynological proxy data provide a finely resolved regional environmental history of the East Asian monsoon. A varve-based chronology (shl-vc2) has been established for the last 65,000 years and allows a detailed comparison with other long regional and global palaeoclimate records. Vegetation density of the study area depends, on the long run, on precessionally forced insolation changes, with superimposed millennial-scale variability during the Last Glacial. Periodic increase of organic carbon content and thermophilous tree species like Ulmus and Fraxinus and contemporary decrease of shrub Alnus precisely mirror millennial-scale climatic variations primarily known from Greenland ice-cores as Dansgaard-Oeschger cycles, as well as Late-glacial period climate changes. Percentages of trees & shrubs pollen and in particular lake productivity-related data reveal substantial differences between interstadial intensities, with those between 50 – 60 ka BP being more pronounced than the following ones.
title Last glacial period lake sediment data from Lake Sihailongwan, N.E. China
topic Changbai Mountains region, Jilin Province, NE China; COMPCORE; Composite Core; GeoForschungszentrum Potsdam; GFZ; SHL; Sihailongwan Maar Lake
url https://doi.org/10.1594/PANGAEA.885907