Ostracoda in five sediment cores from the Laptev and Kara seas ...

Fossil ostracods were investigated in five AMS14C-dated cores from different parts of the Laptev and Kara seas. Three cores from the Laptev Sea shelf are located in river paleovalleys, and one core originates from the western continental slope. The core from the Kara Sea was obtained in the eastern...

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Main Author: Stepanova, Anna Yu
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735539
https://doi.pangaea.de/10.1594/PANGAEA.735539
id ftdatacite:10.1594/pangaea.735539
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735539 2024-09-15T18:16:10+00:00 Ostracoda in five sediment cores from the Laptev and Kara seas ... Stepanova, Anna Yu 2010 application/zip https://dx.doi.org/10.1594/pangaea.735539 https://doi.pangaea.de/10.1594/PANGAEA.735539 en eng PANGAEA https://dx.doi.org/10.1111/j.1502-3885.2012.00254.x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kasten corer Gravity corer Kiel type BP00 ARK-XIV/1b Akademik Boris Petrov Polarstern article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.73553910.1111/j.1502-3885.2012.00254.x 2024-08-01T08:58:27Z Fossil ostracods were investigated in five AMS14C-dated cores from different parts of the Laptev and Kara seas. Three cores from the Laptev Sea shelf are located in river paleovalleys, and one core originates from the western continental slope. The core from the Kara Sea was obtained in the eastern shelf region. Six fossil assemblages were distinguished: estuarine (1), inner-shelf (2), middle-shelf (3), outer-shelf (4), Pre-Holocene upper continental slope (5), and Holocene upper continental slope (6). They show that during the Postglacial sea-level rise there was a transition from estuarine brackish-water environment to modern marine conditions. Assemblages 1-3 are present in the eastern Laptev Sea with the oldest ostracod-bearing samples aging back to 11.4-11.3 cal.ka. Cores from the western Laptev Sea (12.3 cal.ka, assemblages 1-4) and the Kara Sea (8.1 cal.ka, assemblages 2-4) demonstrate similar pattern in assemblage replacement, but contain a number of relatively deep-water species reflecting stronger ... : Supplement to: Stepanova, Anna Yu; Taldenkova, Ekaterina; Bauch, Henning A (2012): Ostracod palaeoecology and environmental change in the Laptev and Kara seas (Siberian Arctic) during the last 18 000 years. Boreas, 41(4), 557-577 ... Article in Journal/Newspaper Kara Sea laptev Laptev Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer
Kasten corer
Gravity corer Kiel type
BP00
ARK-XIV/1b
Akademik Boris Petrov
Polarstern
spellingShingle Gravity corer
Kasten corer
Gravity corer Kiel type
BP00
ARK-XIV/1b
Akademik Boris Petrov
Polarstern
Stepanova, Anna Yu
Ostracoda in five sediment cores from the Laptev and Kara seas ...
topic_facet Gravity corer
Kasten corer
Gravity corer Kiel type
BP00
ARK-XIV/1b
Akademik Boris Petrov
Polarstern
description Fossil ostracods were investigated in five AMS14C-dated cores from different parts of the Laptev and Kara seas. Three cores from the Laptev Sea shelf are located in river paleovalleys, and one core originates from the western continental slope. The core from the Kara Sea was obtained in the eastern shelf region. Six fossil assemblages were distinguished: estuarine (1), inner-shelf (2), middle-shelf (3), outer-shelf (4), Pre-Holocene upper continental slope (5), and Holocene upper continental slope (6). They show that during the Postglacial sea-level rise there was a transition from estuarine brackish-water environment to modern marine conditions. Assemblages 1-3 are present in the eastern Laptev Sea with the oldest ostracod-bearing samples aging back to 11.4-11.3 cal.ka. Cores from the western Laptev Sea (12.3 cal.ka, assemblages 1-4) and the Kara Sea (8.1 cal.ka, assemblages 2-4) demonstrate similar pattern in assemblage replacement, but contain a number of relatively deep-water species reflecting stronger ... : Supplement to: Stepanova, Anna Yu; Taldenkova, Ekaterina; Bauch, Henning A (2012): Ostracod palaeoecology and environmental change in the Laptev and Kara seas (Siberian Arctic) during the last 18 000 years. Boreas, 41(4), 557-577 ...
format Article in Journal/Newspaper
author Stepanova, Anna Yu
author_facet Stepanova, Anna Yu
author_sort Stepanova, Anna Yu
title Ostracoda in five sediment cores from the Laptev and Kara seas ...
title_short Ostracoda in five sediment cores from the Laptev and Kara seas ...
title_full Ostracoda in five sediment cores from the Laptev and Kara seas ...
title_fullStr Ostracoda in five sediment cores from the Laptev and Kara seas ...
title_full_unstemmed Ostracoda in five sediment cores from the Laptev and Kara seas ...
title_sort ostracoda in five sediment cores from the laptev and kara seas ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.735539
https://doi.pangaea.de/10.1594/PANGAEA.735539
genre Kara Sea
laptev
Laptev Sea
genre_facet Kara Sea
laptev
Laptev Sea
op_relation https://dx.doi.org/10.1111/j.1502-3885.2012.00254.x
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.73553910.1111/j.1502-3885.2012.00254.x
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