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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Main Authors: 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
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.119754
https://doi.pangaea.de/10.1594/PANGAEA.119754
id ftdatacite:10.1594/pangaea.119754
record_format openpolar
spelling 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
institution 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