(Table 1) Age determination of sediment core MD97-2141 ...
The primary productivity dynamics of the last 200,000 years in the Sulu Sea was reconstructed using the abundance of the coccolithophore Florisphaera profunda in the IMAGES MD97-2141 core. We find that primary productivity was enhanced during glacial periods, which we suggest is due to a stronger Ea...
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ftdatacite:10.1594/pangaea.846603 2024-10-13T14:07:47+00:00 (Table 1) Age determination of sediment core MD97-2141 ... de Garidel-Thoron, Thibault Beaufort, Luc Linsley, Braddock K Dannenmann, Stefanie 2001 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.846603 https://doi.pangaea.de/10.1594/PANGAEA.846603 en eng PANGAEA https://dx.doi.org/10.1029/2000pa000557 https://dx.doi.org/10.1017/s0033822200013886 https://dx.doi.org/10.1017/s0033822200013874 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Age, dated Age, dated standard deviation Calendar age Age, dated material Laboratory code/label Age, comment Calypso Corer Age, 14C AMS Age, 14C calibrated MD106 Marion Dufresne 1995 Dataset dataset Supplementary Dataset 2001 ftdatacite https://doi.org/10.1594/pangaea.84660310.1029/2000pa00055710.1017/s003382220001388610.1017/s0033822200013874 2024-10-01T11:05:53Z The primary productivity dynamics of the last 200,000 years in the Sulu Sea was reconstructed using the abundance of the coccolithophore Florisphaera profunda in the IMAGES MD97-2141 core. We find that primary productivity was enhanced during glacial periods, which we suggest is due to a stronger East Asian winter monsoon. During the last 80 kyr, eight significant increases in primary productivity (PP) in the Sulu Sea are similar to East Asian winter monsoon changes recorded in Chinese loess. The PP maxima are not linked with Heinrich events (HE) in the North Atlantic, although four PP peaks are synchronous with HE. The PP oscillations have frequencies near those of the Dansgaard-Oeschger cycles in Northern Hemisphere ice records and indicate a teleconnection of the East Asian winter monsoon with Greenland climate. In this Sulu Sea record the East Asian winter monsoon oscillates with periodicities of ~6, 4.2-3.4, 2.3, and 1.5 kyr. In particular, the 1.5 kyr cycle exhibits a strong and pervasive signal from ... : Calendar ages have been calculated using a 400 year reservoir correction and applying the Stuiver and Braziunas (1993) calibration curve for samples younger than 20,000 calendar years in age and a U/Th calibration curve for the samples older than 20,000 calendar years (Bard et al., 2993). ... Dataset Greenland North Atlantic DataCite Greenland |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock Age, dated Age, dated standard deviation Calendar age Age, dated material Laboratory code/label Age, comment Calypso Corer Age, 14C AMS Age, 14C calibrated MD106 Marion Dufresne 1995 |
spellingShingle |
DEPTH, sediment/rock Age, dated Age, dated standard deviation Calendar age Age, dated material Laboratory code/label Age, comment Calypso Corer Age, 14C AMS Age, 14C calibrated MD106 Marion Dufresne 1995 de Garidel-Thoron, Thibault Beaufort, Luc Linsley, Braddock K Dannenmann, Stefanie (Table 1) Age determination of sediment core MD97-2141 ... |
topic_facet |
DEPTH, sediment/rock Age, dated Age, dated standard deviation Calendar age Age, dated material Laboratory code/label Age, comment Calypso Corer Age, 14C AMS Age, 14C calibrated MD106 Marion Dufresne 1995 |
description |
The primary productivity dynamics of the last 200,000 years in the Sulu Sea was reconstructed using the abundance of the coccolithophore Florisphaera profunda in the IMAGES MD97-2141 core. We find that primary productivity was enhanced during glacial periods, which we suggest is due to a stronger East Asian winter monsoon. During the last 80 kyr, eight significant increases in primary productivity (PP) in the Sulu Sea are similar to East Asian winter monsoon changes recorded in Chinese loess. The PP maxima are not linked with Heinrich events (HE) in the North Atlantic, although four PP peaks are synchronous with HE. The PP oscillations have frequencies near those of the Dansgaard-Oeschger cycles in Northern Hemisphere ice records and indicate a teleconnection of the East Asian winter monsoon with Greenland climate. In this Sulu Sea record the East Asian winter monsoon oscillates with periodicities of ~6, 4.2-3.4, 2.3, and 1.5 kyr. In particular, the 1.5 kyr cycle exhibits a strong and pervasive signal from ... : Calendar ages have been calculated using a 400 year reservoir correction and applying the Stuiver and Braziunas (1993) calibration curve for samples younger than 20,000 calendar years in age and a U/Th calibration curve for the samples older than 20,000 calendar years (Bard et al., 2993). ... |
format |
Dataset |
author |
de Garidel-Thoron, Thibault Beaufort, Luc Linsley, Braddock K Dannenmann, Stefanie |
author_facet |
de Garidel-Thoron, Thibault Beaufort, Luc Linsley, Braddock K Dannenmann, Stefanie |
author_sort |
de Garidel-Thoron, Thibault |
title |
(Table 1) Age determination of sediment core MD97-2141 ... |
title_short |
(Table 1) Age determination of sediment core MD97-2141 ... |
title_full |
(Table 1) Age determination of sediment core MD97-2141 ... |
title_fullStr |
(Table 1) Age determination of sediment core MD97-2141 ... |
title_full_unstemmed |
(Table 1) Age determination of sediment core MD97-2141 ... |
title_sort |
(table 1) age determination of sediment core md97-2141 ... |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://dx.doi.org/10.1594/pangaea.846603 https://doi.pangaea.de/10.1594/PANGAEA.846603 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland North Atlantic |
genre_facet |
Greenland North Atlantic |
op_relation |
https://dx.doi.org/10.1029/2000pa000557 https://dx.doi.org/10.1017/s0033822200013886 https://dx.doi.org/10.1017/s0033822200013874 |
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.84660310.1029/2000pa00055710.1017/s003382220001388610.1017/s0033822200013874 |
_version_ |
1812814307906289664 |