(Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany
Our study focuses on European loess sequences, particularly the eolian intervals in between the observed pedogenic units. The classical concept of soil formation from parent material is reformulated to estimate of the duration and the associated sedimentation rate (SR) and mass accumulation rate (MA...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.931638 2024-09-09T19:43:31+00:00 (Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany Rousseau, Denis-Didier Antoine, Pierre Sun, Youbin LATITUDE: 49.316390 * LONGITUDE: 8.731670 * MINIMUM ELEVATION: 175.0 m * MAXIMUM ELEVATION: 175.0 m 2021 text/tab-separated-values, 206 data points https://doi.pangaea.de/10.1594/PANGAEA.931638 https://doi.org/10.1594/PANGAEA.931638 en eng PANGAEA https://doi.org/10.1594/PANGAEA.931658 Rousseau, Denis-Didier; Antoine, Pierre; Sun, Youbin (2021): How dusty was the last glacial maximum over Europe? Quaternary Science Reviews, 254, 106775, https://doi.org/10.1016/j.quascirev.2020.106775 https://doi.pangaea.de/10.1594/PANGAEA.931638 https://doi.org/10.1594/PANGAEA.931638 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Accumulation rate dust per year sediment mean per year Age maximum/old minimum/young Comment Core Duration Eurasia Germany Last Glacial Maximum Layer description Layer thickness Loess Mass accumulation rates Millennial scale variability Nussloch sedimentation rate Sedimentation rate per year TiPES Tipping Points in the Earth System dataset 2021 ftpangaea https://doi.org/10.1594/PANGAEA.93163810.1594/PANGAEA.931658 2024-07-24T02:31:42Z Our study focuses on European loess sequences, particularly the eolian intervals in between the observed pedogenic units. The classical concept of soil formation from parent material is reformulated to estimate of the duration and the associated sedimentation rate (SR) and mass accumulation rate (MAR) of these paleodust intervals. We show that the Greenland Stadial (GS) duration in European loess deposits includes the thickness of the overlying pedogenic unit, which in fact developed downward into the upper part of the eolian unit. The lower stratigraphical limit of the eolian unit overlying the pedogenic unit corresponds to the restart of the dust sedimentation of the younger GS. We illustrate this interpretation first by computing both SRs and MARs first for the Nussloch key sequence, the most complete European series. The correlation between Nussloch and other European loess sequences, located along a 1,800 km longitudinal transect, allows computation of SR and MAR for several identified GS events. Comparing GS from marine and ice core records, our study shows that the two last Bond cycles are preserved in every European eolian record. Bulk SR and MAR are estimated and compared for these two Bond cycles, showing the highest SRs and MARs in western Europe. These indices also indicate that the last stadials, embedding an Henrich event, were not the dustiest in every Bond cycle. Our estimated MAR also differ from previously published computations, which did not take into account the various pedogenic units present in the studied loess sequences. The bulk SR and MAR estimates computed for the two last Bond Cycles from Chinese sequences from the Loess Plateau indicate lower atmospheric dust than in Europe during the Last Glacial Maximum. SR and MAR estimates computed from the fine-grained material for European records fit with Earth System model reconstructions. Dataset Greenland ice core PANGAEA - Data Publisher for Earth & Environmental Science Greenland ENVELOPE(8.731670,8.731670,49.316390,49.316390) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Accumulation rate dust per year sediment mean per year Age maximum/old minimum/young Comment Core Duration Eurasia Germany Last Glacial Maximum Layer description Layer thickness Loess Mass accumulation rates Millennial scale variability Nussloch sedimentation rate Sedimentation rate per year TiPES Tipping Points in the Earth System |
spellingShingle |
Accumulation rate dust per year sediment mean per year Age maximum/old minimum/young Comment Core Duration Eurasia Germany Last Glacial Maximum Layer description Layer thickness Loess Mass accumulation rates Millennial scale variability Nussloch sedimentation rate Sedimentation rate per year TiPES Tipping Points in the Earth System Rousseau, Denis-Didier Antoine, Pierre Sun, Youbin (Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany |
topic_facet |
Accumulation rate dust per year sediment mean per year Age maximum/old minimum/young Comment Core Duration Eurasia Germany Last Glacial Maximum Layer description Layer thickness Loess Mass accumulation rates Millennial scale variability Nussloch sedimentation rate Sedimentation rate per year TiPES Tipping Points in the Earth System |
description |
Our study focuses on European loess sequences, particularly the eolian intervals in between the observed pedogenic units. The classical concept of soil formation from parent material is reformulated to estimate of the duration and the associated sedimentation rate (SR) and mass accumulation rate (MAR) of these paleodust intervals. We show that the Greenland Stadial (GS) duration in European loess deposits includes the thickness of the overlying pedogenic unit, which in fact developed downward into the upper part of the eolian unit. The lower stratigraphical limit of the eolian unit overlying the pedogenic unit corresponds to the restart of the dust sedimentation of the younger GS. We illustrate this interpretation first by computing both SRs and MARs first for the Nussloch key sequence, the most complete European series. The correlation between Nussloch and other European loess sequences, located along a 1,800 km longitudinal transect, allows computation of SR and MAR for several identified GS events. Comparing GS from marine and ice core records, our study shows that the two last Bond cycles are preserved in every European eolian record. Bulk SR and MAR are estimated and compared for these two Bond cycles, showing the highest SRs and MARs in western Europe. These indices also indicate that the last stadials, embedding an Henrich event, were not the dustiest in every Bond cycle. Our estimated MAR also differ from previously published computations, which did not take into account the various pedogenic units present in the studied loess sequences. The bulk SR and MAR estimates computed for the two last Bond Cycles from Chinese sequences from the Loess Plateau indicate lower atmospheric dust than in Europe during the Last Glacial Maximum. SR and MAR estimates computed from the fine-grained material for European records fit with Earth System model reconstructions. |
format |
Dataset |
author |
Rousseau, Denis-Didier Antoine, Pierre Sun, Youbin |
author_facet |
Rousseau, Denis-Didier Antoine, Pierre Sun, Youbin |
author_sort |
Rousseau, Denis-Didier |
title |
(Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany |
title_short |
(Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany |
title_full |
(Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany |
title_fullStr |
(Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany |
title_full_unstemmed |
(Table 1) Sedimentation rate and mean accumulation rate of sediment and dust at Nussloch, Germany |
title_sort |
(table 1) sedimentation rate and mean accumulation rate of sediment and dust at nussloch, germany |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.931638 https://doi.org/10.1594/PANGAEA.931638 |
op_coverage |
LATITUDE: 49.316390 * LONGITUDE: 8.731670 * MINIMUM ELEVATION: 175.0 m * MAXIMUM ELEVATION: 175.0 m |
long_lat |
ENVELOPE(8.731670,8.731670,49.316390,49.316390) |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland ice core |
genre_facet |
Greenland ice core |
op_relation |
https://doi.org/10.1594/PANGAEA.931658 Rousseau, Denis-Didier; Antoine, Pierre; Sun, Youbin (2021): How dusty was the last glacial maximum over Europe? Quaternary Science Reviews, 254, 106775, https://doi.org/10.1016/j.quascirev.2020.106775 https://doi.pangaea.de/10.1594/PANGAEA.931638 https://doi.org/10.1594/PANGAEA.931638 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.93163810.1594/PANGAEA.931658 |
_version_ |
1809913020525051904 |