(Table 1) Age determination of sediment core PS51/092-12 ...

Diatom assemblages were employed to study temporal changes of Siberian river runoff on the Laptev Sea shelf. Using a correlation between freshwater diatoms (%) in core-top sediments and summer surface water salinities from the inner Kara Sea, salinity conditions were reconstructed for a site northea...

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Bibliographic Details
Main Authors: Bauch, Henning A, Polyakova, Ye I
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.841800
https://doi.pangaea.de/10.1594/PANGAEA.841800
id ftdatacite:10.1594/pangaea.841800
record_format openpolar
spelling ftdatacite:10.1594/pangaea.841800 2024-09-15T18:16:11+00:00 (Table 1) Age determination of sediment core PS51/092-12 ... Bauch, Henning A Polyakova, Ye I 2003 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.841800 https://doi.pangaea.de/10.1594/PANGAEA.841800 en eng PANGAEA https://dx.doi.org/10.1029/2002pa000847 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Laboratory code/label Age, dated material DEPTH, sediment/rock Age, dated Age, dated standard deviation Calendar age Kasten corer Age, 14C AMS Age, 14C calibrated, CALIB 4.3 Stuiver et al., 1998 ARK-XIV/1b Polarstern dataset Supplementary Dataset Dataset 2003 ftdatacite https://doi.org/10.1594/pangaea.84180010.1029/2002pa000847 2024-08-01T08:58:27Z Diatom assemblages were employed to study temporal changes of Siberian river runoff on the Laptev Sea shelf. Using a correlation between freshwater diatoms (%) in core-top sediments and summer surface water salinities from the inner Kara Sea, salinity conditions were reconstructed for a site northeast of the Lena River Delta (present water depth 32 m) since 9 calendar years (cal) ka. The reconstruction indicate a strong, near-coastal, and river-influenced environment at the site until about 8.6 cal ka. Corroborated by comparison with other proxy records from further to the east, surface salinities increased from 9 to 14 until about 7.4 cal ka, owing to ongoing global sea level rise and synchronous southward shift of the coastline. Although riverine water became less influential at the site since then, salinities still varied between 12.5 and 15, particularly during the last 3.5 kyr. These more recent salinity fluctuations agree well with reconstructions from just north of the Lena Delta, emphasizing the ... : Supplement to: Bauch, Henning A; Polyakova, Ye I (2003): Diatom-inferred salinity records from the Arctic Siberian Margin: Implications for fluvial runoff patterns during the Holocene. Paleoceanography, 18(2), 1027 ... Dataset Kara Sea laptev Laptev Sea lena delta lena river DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Laboratory code/label
Age, dated material
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Calendar age
Kasten corer
Age, 14C AMS
Age, 14C calibrated, CALIB 4.3 Stuiver et al., 1998
ARK-XIV/1b
Polarstern
spellingShingle Laboratory code/label
Age, dated material
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Calendar age
Kasten corer
Age, 14C AMS
Age, 14C calibrated, CALIB 4.3 Stuiver et al., 1998
ARK-XIV/1b
Polarstern
Bauch, Henning A
Polyakova, Ye I
(Table 1) Age determination of sediment core PS51/092-12 ...
topic_facet Laboratory code/label
Age, dated material
DEPTH, sediment/rock
Age, dated
Age, dated standard deviation
Calendar age
Kasten corer
Age, 14C AMS
Age, 14C calibrated, CALIB 4.3 Stuiver et al., 1998
ARK-XIV/1b
Polarstern
description Diatom assemblages were employed to study temporal changes of Siberian river runoff on the Laptev Sea shelf. Using a correlation between freshwater diatoms (%) in core-top sediments and summer surface water salinities from the inner Kara Sea, salinity conditions were reconstructed for a site northeast of the Lena River Delta (present water depth 32 m) since 9 calendar years (cal) ka. The reconstruction indicate a strong, near-coastal, and river-influenced environment at the site until about 8.6 cal ka. Corroborated by comparison with other proxy records from further to the east, surface salinities increased from 9 to 14 until about 7.4 cal ka, owing to ongoing global sea level rise and synchronous southward shift of the coastline. Although riverine water became less influential at the site since then, salinities still varied between 12.5 and 15, particularly during the last 3.5 kyr. These more recent salinity fluctuations agree well with reconstructions from just north of the Lena Delta, emphasizing the ... : Supplement to: Bauch, Henning A; Polyakova, Ye I (2003): Diatom-inferred salinity records from the Arctic Siberian Margin: Implications for fluvial runoff patterns during the Holocene. Paleoceanography, 18(2), 1027 ...
format Dataset
author Bauch, Henning A
Polyakova, Ye I
author_facet Bauch, Henning A
Polyakova, Ye I
author_sort Bauch, Henning A
title (Table 1) Age determination of sediment core PS51/092-12 ...
title_short (Table 1) Age determination of sediment core PS51/092-12 ...
title_full (Table 1) Age determination of sediment core PS51/092-12 ...
title_fullStr (Table 1) Age determination of sediment core PS51/092-12 ...
title_full_unstemmed (Table 1) Age determination of sediment core PS51/092-12 ...
title_sort (table 1) age determination of sediment core ps51/092-12 ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.841800
https://doi.pangaea.de/10.1594/PANGAEA.841800
genre Kara Sea
laptev
Laptev Sea
lena delta
lena river
genre_facet Kara Sea
laptev
Laptev Sea
lena delta
lena river
op_relation https://dx.doi.org/10.1029/2002pa000847
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.84180010.1029/2002pa000847
_version_ 1810454199865966592