(Table 1) Age determination of sediment profile JM96-1225 ...
The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and ice rafted debris (IRD). The stratigraphy spans 57 to 6 calibrated (cal) ka years and reveals sea surface temperatures that...
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ftdatacite:10.1594/pangaea.842445 2024-09-15T18:03:36+00:00 (Table 1) Age determination of sediment profile JM96-1225 ... Hagen, Sveinung Hald, Morten 2002 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.842445 https://doi.pangaea.de/10.1594/PANGAEA.842445 en eng PANGAEA https://dx.doi.org/10.1029/2001pa000632 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Laboratory code/label Core DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated material Age, dated Age, dated standard error Calendar age Gravity corer Age, 14C AMS Age, 14C milieu/reservoir corrected -400 yr Age, 14C calibrated JM96 Jan Mayen dataset Supplementary Dataset Dataset 2002 ftdatacite https://doi.org/10.1594/pangaea.84244510.1029/2001pa000632 2024-08-01T10:56:44Z The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and ice rafted debris (IRD). The stratigraphy spans 57 to 6 calibrated (cal) ka years and reveals sea surface temperatures that covary with Greenland ice core temperatures throughout marine isotope stages (MIS) 3 and 2. Planktonic d18O minima, interpreted as meltwater events, follow sea surface warming. IRD from both the Greenland and Iceland Ice Sheets was delayed by ~2 ka relative to the North Atlantic Heinrich events. Ventilation of bottom water was mostly sustained through open ocean convection associated with North Atlantic Deep Water production or by convection of glacial North Atlantic Intermediate Water, except for two episodes at ~54 cal ka (MIS 3.31) and 18–15 cal ka (termination I). During these two periods we suggest that deep water ventilation was accomplished mainly by brine formation. ... : Supplement to: Hagen, Sveinung; Hald, Morten (2002): Variation in surface and deep water circulation in the Denmark Strait, North Atlantic, during marine isotope stages 3 and 2. Paleoceanography, 17(4), 13-1-13-16 ... Dataset Denmark Strait Greenland Greenland ice core ice core Iceland Jan Mayen North Atlantic Deep Water North Atlantic Planktonic foraminifera DataCite |
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ftdatacite |
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English |
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Laboratory code/label Core DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated material Age, dated Age, dated standard error Calendar age Gravity corer Age, 14C AMS Age, 14C milieu/reservoir corrected -400 yr Age, 14C calibrated JM96 Jan Mayen |
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Laboratory code/label Core DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated material Age, dated Age, dated standard error Calendar age Gravity corer Age, 14C AMS Age, 14C milieu/reservoir corrected -400 yr Age, 14C calibrated JM96 Jan Mayen Hagen, Sveinung Hald, Morten (Table 1) Age determination of sediment profile JM96-1225 ... |
topic_facet |
Laboratory code/label Core DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated material Age, dated Age, dated standard error Calendar age Gravity corer Age, 14C AMS Age, 14C milieu/reservoir corrected -400 yr Age, 14C calibrated JM96 Jan Mayen |
description |
The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and ice rafted debris (IRD). The stratigraphy spans 57 to 6 calibrated (cal) ka years and reveals sea surface temperatures that covary with Greenland ice core temperatures throughout marine isotope stages (MIS) 3 and 2. Planktonic d18O minima, interpreted as meltwater events, follow sea surface warming. IRD from both the Greenland and Iceland Ice Sheets was delayed by ~2 ka relative to the North Atlantic Heinrich events. Ventilation of bottom water was mostly sustained through open ocean convection associated with North Atlantic Deep Water production or by convection of glacial North Atlantic Intermediate Water, except for two episodes at ~54 cal ka (MIS 3.31) and 18–15 cal ka (termination I). During these two periods we suggest that deep water ventilation was accomplished mainly by brine formation. ... : Supplement to: Hagen, Sveinung; Hald, Morten (2002): Variation in surface and deep water circulation in the Denmark Strait, North Atlantic, during marine isotope stages 3 and 2. Paleoceanography, 17(4), 13-1-13-16 ... |
format |
Dataset |
author |
Hagen, Sveinung Hald, Morten |
author_facet |
Hagen, Sveinung Hald, Morten |
author_sort |
Hagen, Sveinung |
title |
(Table 1) Age determination of sediment profile JM96-1225 ... |
title_short |
(Table 1) Age determination of sediment profile JM96-1225 ... |
title_full |
(Table 1) Age determination of sediment profile JM96-1225 ... |
title_fullStr |
(Table 1) Age determination of sediment profile JM96-1225 ... |
title_full_unstemmed |
(Table 1) Age determination of sediment profile JM96-1225 ... |
title_sort |
(table 1) age determination of sediment profile jm96-1225 ... |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://dx.doi.org/10.1594/pangaea.842445 https://doi.pangaea.de/10.1594/PANGAEA.842445 |
genre |
Denmark Strait Greenland Greenland ice core ice core Iceland Jan Mayen North Atlantic Deep Water North Atlantic Planktonic foraminifera |
genre_facet |
Denmark Strait Greenland Greenland ice core ice core Iceland Jan Mayen North Atlantic Deep Water North Atlantic Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.1029/2001pa000632 |
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.84244510.1029/2001pa000632 |
_version_ |
1810441088315424768 |