Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...

Loess sequences are a particular record of paleoenvironments and paleoclimates and show regional peculiarities. Among those, European loess sequences show the occurrence of paleosols and other pedogenic units that have been demonstrated to correspond to the Greenland Interstadials (GIS) or Dansgaard...

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Main Authors: Rousseau, Denis-Didier, Antoine, Pierre, Sun, Youbin
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2021
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.931658
https://doi.pangaea.de/10.1594/PANGAEA.931658
id ftdatacite:10.1594/pangaea.931658
record_format openpolar
spelling ftdatacite:10.1594/pangaea.931658 2024-09-15T18:03:29+00:00 Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ... Rousseau, Denis-Didier Antoine, Pierre Sun, Youbin 2021 application/zip https://dx.doi.org/10.1594/pangaea.931658 https://doi.pangaea.de/10.1594/PANGAEA.931658 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2020.106775 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Eurasia Last Glacial Maximum Loess Mass accumulation rates Millennial scale variability sedimentation rate Core Tipping Points in the Earth System TiPES article Collection Bundled Publication of Datasets 2021 ftdatacite https://doi.org/10.1594/pangaea.93165810.1016/j.quascirev.2020.106775 2024-08-01T10:54:44Z Loess sequences are a particular record of paleoenvironments and paleoclimates and show regional peculiarities. Among those, European loess sequences show the occurrence of paleosols and other pedogenic units that have been demonstrated to correspond to the Greenland Interstadials (GIS) or Dansgaard-Oeschger events (DO), for the last climate cycle (Moine et al. 2017), of GIS-like for the penultimate climate cycle (Rousseau et al. 2020).During the last climate cycle, these paleosols developed synchronously over Europe along a wide longitude transect eastward in Ukraine (Rousseau et al., 2017). More interesting the development of these paleosols or pedogenic units, occurred during a stop of the dust deposition from the top of the most recently deposited eolian unit. Taking into consideration this point in our manuscript, we revisited the stratigraphy of the European loess sequences by considering the paleodust units, equivalent to Greenland Stadials (GS), as associating the lower loess unit and the overlying ... Article in Journal/Newspaper Dansgaard-Oeschger events Greenland DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Eurasia
Last Glacial Maximum
Loess
Mass accumulation rates
Millennial scale variability
sedimentation rate
Core
Tipping Points in the Earth System TiPES
spellingShingle Eurasia
Last Glacial Maximum
Loess
Mass accumulation rates
Millennial scale variability
sedimentation rate
Core
Tipping Points in the Earth System TiPES
Rousseau, Denis-Didier
Antoine, Pierre
Sun, Youbin
Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...
topic_facet Eurasia
Last Glacial Maximum
Loess
Mass accumulation rates
Millennial scale variability
sedimentation rate
Core
Tipping Points in the Earth System TiPES
description Loess sequences are a particular record of paleoenvironments and paleoclimates and show regional peculiarities. Among those, European loess sequences show the occurrence of paleosols and other pedogenic units that have been demonstrated to correspond to the Greenland Interstadials (GIS) or Dansgaard-Oeschger events (DO), for the last climate cycle (Moine et al. 2017), of GIS-like for the penultimate climate cycle (Rousseau et al. 2020).During the last climate cycle, these paleosols developed synchronously over Europe along a wide longitude transect eastward in Ukraine (Rousseau et al., 2017). More interesting the development of these paleosols or pedogenic units, occurred during a stop of the dust deposition from the top of the most recently deposited eolian unit. Taking into consideration this point in our manuscript, we revisited the stratigraphy of the European loess sequences by considering the paleodust units, equivalent to Greenland Stadials (GS), as associating the lower loess unit and the overlying ...
format Article in Journal/Newspaper
author Rousseau, Denis-Didier
Antoine, Pierre
Sun, Youbin
author_facet Rousseau, Denis-Didier
Antoine, Pierre
Sun, Youbin
author_sort Rousseau, Denis-Didier
title Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...
title_short Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...
title_full Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...
title_fullStr Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...
title_full_unstemmed Sedimentation rates and mass accumulation rates of sediment and dust in Europe and China ...
title_sort sedimentation rates and mass accumulation rates of sediment and dust in europe and china ...
publisher PANGAEA
publishDate 2021
url https://dx.doi.org/10.1594/pangaea.931658
https://doi.pangaea.de/10.1594/PANGAEA.931658
genre Dansgaard-Oeschger events
Greenland
genre_facet Dansgaard-Oeschger events
Greenland
op_relation https://dx.doi.org/10.1016/j.quascirev.2020.106775
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.93165810.1016/j.quascirev.2020.106775
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