(Table 2) Age determination of sediment cores from the Portuguese Margin
We demonstrate that changes in the behavior of the Mediterranean Outflow Water (MOW) prior to and through the last deglaciation played an important role in promoting Meridional Overturning Circulation (MOC). Estimation of past MOW salt and heat fluxes indicates that they gradually increased through...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.833682 2023-05-15T17:28:44+02:00 (Table 2) Age determination of sediment cores from the Portuguese Margin Rogerson, Mike Rohling, Eelco J Weaver, Philip PE MEDIAN LATITUDE: 35.905557 * MEDIAN LONGITUDE: -7.333333 * SOUTH-BOUND LATITUDE: 35.816670 * WEST-BOUND LONGITUDE: -7.516670 * NORTH-BOUND LATITUDE: 36.050000 * EAST-BOUND LONGITUDE: -7.183330 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 4.02 m 2014-06-27 text/tab-separated-values, 32 data points https://doi.pangaea.de/10.1594/PANGAEA.833682 https://doi.org/10.1594/PANGAEA.833682 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.833682 https://doi.org/10.1594/PANGAEA.833682 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Rogerson, Mike; Rohling, Eelco J; Weaver, Philip PE (2006): Promotion of meridional overturning by Mediterranean-derived salt during the last deglaciation. Paleoceanography, 21(4), PA4101, https://doi.org/10.1029/2006PA001306 Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Calendar age D13686 D13896 D13900 D249 DEPTH sediment/rock Discovery (1962) Elevation of event Event label Laboratory code/label Latitude of event Longitude of event PC Piston corer Portuguese Margin Dataset 2014 ftpangaea https://doi.org/10.1594/PANGAEA.833682 https://doi.org/10.1029/2006PA001306 2023-01-20T09:03:26Z We demonstrate that changes in the behavior of the Mediterranean Outflow Water (MOW) prior to and through the last deglaciation played an important role in promoting Meridional Overturning Circulation (MOC). Estimation of past MOW salt and heat fluxes indicates that they gradually increased through the last deglaciation. Between 17.5 and 14.6 thousand years ago (ka B.P., where B.P. references year 1950), net evaporation from the Mediterranean exported sufficient fresh water from the North Atlantic catchment to cause an average salinity increase of 0.5 psu throughout the upper 2000 m of the entire North Atlantic to the north of 25°N. Combined with rapid intensification and shoaling of the MOW plume, which we identify around 15-14.5 ka B.P., this deglacial MOW-related salt accumulation preconditioned the North Atlantic for abrupt resumption of the MOC at 14.6 ka B.P. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-7.516670,-7.183330,36.050000,35.816670) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Calendar age D13686 D13896 D13900 D249 DEPTH sediment/rock Discovery (1962) Elevation of event Event label Laboratory code/label Latitude of event Longitude of event PC Piston corer Portuguese Margin |
spellingShingle |
Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Calendar age D13686 D13896 D13900 D249 DEPTH sediment/rock Discovery (1962) Elevation of event Event label Laboratory code/label Latitude of event Longitude of event PC Piston corer Portuguese Margin Rogerson, Mike Rohling, Eelco J Weaver, Philip PE (Table 2) Age determination of sediment cores from the Portuguese Margin |
topic_facet |
Age 14C AMS 14C milieu/reservoir corrected (-400 yr) dated dated standard deviation Calendar age D13686 D13896 D13900 D249 DEPTH sediment/rock Discovery (1962) Elevation of event Event label Laboratory code/label Latitude of event Longitude of event PC Piston corer Portuguese Margin |
description |
We demonstrate that changes in the behavior of the Mediterranean Outflow Water (MOW) prior to and through the last deglaciation played an important role in promoting Meridional Overturning Circulation (MOC). Estimation of past MOW salt and heat fluxes indicates that they gradually increased through the last deglaciation. Between 17.5 and 14.6 thousand years ago (ka B.P., where B.P. references year 1950), net evaporation from the Mediterranean exported sufficient fresh water from the North Atlantic catchment to cause an average salinity increase of 0.5 psu throughout the upper 2000 m of the entire North Atlantic to the north of 25°N. Combined with rapid intensification and shoaling of the MOW plume, which we identify around 15-14.5 ka B.P., this deglacial MOW-related salt accumulation preconditioned the North Atlantic for abrupt resumption of the MOC at 14.6 ka B.P. |
format |
Dataset |
author |
Rogerson, Mike Rohling, Eelco J Weaver, Philip PE |
author_facet |
Rogerson, Mike Rohling, Eelco J Weaver, Philip PE |
author_sort |
Rogerson, Mike |
title |
(Table 2) Age determination of sediment cores from the Portuguese Margin |
title_short |
(Table 2) Age determination of sediment cores from the Portuguese Margin |
title_full |
(Table 2) Age determination of sediment cores from the Portuguese Margin |
title_fullStr |
(Table 2) Age determination of sediment cores from the Portuguese Margin |
title_full_unstemmed |
(Table 2) Age determination of sediment cores from the Portuguese Margin |
title_sort |
(table 2) age determination of sediment cores from the portuguese margin |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.833682 https://doi.org/10.1594/PANGAEA.833682 |
op_coverage |
MEDIAN LATITUDE: 35.905557 * MEDIAN LONGITUDE: -7.333333 * SOUTH-BOUND LATITUDE: 35.816670 * WEST-BOUND LONGITUDE: -7.516670 * NORTH-BOUND LATITUDE: 36.050000 * EAST-BOUND LONGITUDE: -7.183330 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 4.02 m |
long_lat |
ENVELOPE(-7.516670,-7.183330,36.050000,35.816670) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Rogerson, Mike; Rohling, Eelco J; Weaver, Philip PE (2006): Promotion of meridional overturning by Mediterranean-derived salt during the last deglaciation. Paleoceanography, 21(4), PA4101, https://doi.org/10.1029/2006PA001306 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.833682 https://doi.org/10.1594/PANGAEA.833682 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.833682 https://doi.org/10.1029/2006PA001306 |
_version_ |
1766121593138839552 |