Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ...
In this paper, we summarize data on terrigenous sediment supply in the Kara Sea and its accumulation and spatial and temporal variability during Holocene times. Sedimentological, organic-geochemical, and micropaleontological proxies determined in surface sediments allow to characterize the modern (r...
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ftdatacite:10.1594/pangaea.119754 2024-09-15T18:16:08+00:00 Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... Stein, Ruediger Dittmers, Klaus Hauke Fahl, Kirsten Kraus, Matthias Matthiessen, Jens Niessen, Frank Pirrung, Michael Polyakova, Ye I Schoster, Frank Steinke, Tatjana Fütterer, Dieter K 2004 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.119754 https://doi.pangaea.de/10.1594/PANGAEA.119754 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2003.12.004 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label LATITUDE LONGITUDE Elevation of event DEPTH, sediment/rock Sand Silt Size fraction < 0.002 mm, clay Smectite Illite Chlorite Kaolinite MultiCorer Giant box corer Okean Grab Gravity corer Grain size, sieving Grain size, sieving/settling tube X-ray diffraction TEXTUR, clay fraction BP00 BP01 BP99 Akademik Boris Petrov Quaternary Environment of the Eurasian North QUEEN Siberian River Run-Off SIRRO dataset Supplementary Dataset Dataset 2004 ftdatacite https://doi.org/10.1594/pangaea.11975410.1016/j.quascirev.2003.12.004 2024-08-01T11:02:13Z In this paper, we summarize data on terrigenous sediment supply in the Kara Sea and its accumulation and spatial and temporal variability during Holocene times. Sedimentological, organic-geochemical, and micropaleontological proxies determined in surface sediments allow to characterize the modern (riverine) terrigenous sediment input. AMS-14C dated sediment cores from the Ob and Yenisei estuaries and the adjacent inner Kara Sea were investigated to determine the terrigenous sediment fluxes and their relationship to paleoenvironmental changes. The variability of sediment fluxes during Holocene times is related to the post-glacial sea-level rise and changes in river discharge and coastal erosion input. Whereas during the late/middle Holocene most of the terrigenous sediments were deposited in the estuaries and the areas directly off the estuaries, huge amounts of sediments accumulated on the Kara Sea shelf farther north during the early Holocene before about 9 cal kyr BP. The maximum accumulation at that time ... : Supplement to: Stein, Ruediger; Dittmers, Klaus Hauke; Fahl, Kirsten; Kraus, Matthias; Matthiessen, Jens; Niessen, Frank; Pirrung, Michael; Polyakova, Ye I; Schoster, Frank; Steinke, Tatjana; Fütterer, Dieter K (2004): Arctic (palaeo) river discharge and environmental change: evidence from the Holocene Kara Sea sedimentary record. Quaternary Science Reviews, 23(11-13), 1485-1511 ... Dataset Kara Sea DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label LATITUDE LONGITUDE Elevation of event DEPTH, sediment/rock Sand Silt Size fraction < 0.002 mm, clay Smectite Illite Chlorite Kaolinite MultiCorer Giant box corer Okean Grab Gravity corer Grain size, sieving Grain size, sieving/settling tube X-ray diffraction TEXTUR, clay fraction BP00 BP01 BP99 Akademik Boris Petrov Quaternary Environment of the Eurasian North QUEEN Siberian River Run-Off SIRRO |
spellingShingle |
Event label LATITUDE LONGITUDE Elevation of event DEPTH, sediment/rock Sand Silt Size fraction < 0.002 mm, clay Smectite Illite Chlorite Kaolinite MultiCorer Giant box corer Okean Grab Gravity corer Grain size, sieving Grain size, sieving/settling tube X-ray diffraction TEXTUR, clay fraction BP00 BP01 BP99 Akademik Boris Petrov Quaternary Environment of the Eurasian North QUEEN Siberian River Run-Off SIRRO Stein, Ruediger Dittmers, Klaus Hauke Fahl, Kirsten Kraus, Matthias Matthiessen, Jens Niessen, Frank Pirrung, Michael Polyakova, Ye I Schoster, Frank Steinke, Tatjana Fütterer, Dieter K Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... |
topic_facet |
Event label LATITUDE LONGITUDE Elevation of event DEPTH, sediment/rock Sand Silt Size fraction < 0.002 mm, clay Smectite Illite Chlorite Kaolinite MultiCorer Giant box corer Okean Grab Gravity corer Grain size, sieving Grain size, sieving/settling tube X-ray diffraction TEXTUR, clay fraction BP00 BP01 BP99 Akademik Boris Petrov Quaternary Environment of the Eurasian North QUEEN Siberian River Run-Off SIRRO |
description |
In this paper, we summarize data on terrigenous sediment supply in the Kara Sea and its accumulation and spatial and temporal variability during Holocene times. Sedimentological, organic-geochemical, and micropaleontological proxies determined in surface sediments allow to characterize the modern (riverine) terrigenous sediment input. AMS-14C dated sediment cores from the Ob and Yenisei estuaries and the adjacent inner Kara Sea were investigated to determine the terrigenous sediment fluxes and their relationship to paleoenvironmental changes. The variability of sediment fluxes during Holocene times is related to the post-glacial sea-level rise and changes in river discharge and coastal erosion input. Whereas during the late/middle Holocene most of the terrigenous sediments were deposited in the estuaries and the areas directly off the estuaries, huge amounts of sediments accumulated on the Kara Sea shelf farther north during the early Holocene before about 9 cal kyr BP. The maximum accumulation at that time ... : Supplement to: Stein, Ruediger; Dittmers, Klaus Hauke; Fahl, Kirsten; Kraus, Matthias; Matthiessen, Jens; Niessen, Frank; Pirrung, Michael; Polyakova, Ye I; Schoster, Frank; Steinke, Tatjana; Fütterer, Dieter K (2004): Arctic (palaeo) river discharge and environmental change: evidence from the Holocene Kara Sea sedimentary record. Quaternary Science Reviews, 23(11-13), 1485-1511 ... |
format |
Dataset |
author |
Stein, Ruediger Dittmers, Klaus Hauke Fahl, Kirsten Kraus, Matthias Matthiessen, Jens Niessen, Frank Pirrung, Michael Polyakova, Ye I Schoster, Frank Steinke, Tatjana Fütterer, Dieter K |
author_facet |
Stein, Ruediger Dittmers, Klaus Hauke Fahl, Kirsten Kraus, Matthias Matthiessen, Jens Niessen, Frank Pirrung, Michael Polyakova, Ye I Schoster, Frank Steinke, Tatjana Fütterer, Dieter K |
author_sort |
Stein, Ruediger |
title |
Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... |
title_short |
Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... |
title_full |
Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... |
title_fullStr |
Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... |
title_full_unstemmed |
Distribution of grain size and clay minerals in surface sediments of the Kara Sea (Fig 4, 5) ... |
title_sort |
distribution of grain size and clay minerals in surface sediments of the kara sea (fig 4, 5) ... |
publisher |
PANGAEA |
publishDate |
2004 |
url |
https://dx.doi.org/10.1594/pangaea.119754 https://doi.pangaea.de/10.1594/PANGAEA.119754 |
genre |
Kara Sea |
genre_facet |
Kara Sea |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2003.12.004 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.11975410.1016/j.quascirev.2003.12.004 |
_version_ |
1810454107613298688 |