(Table 1) Age determination of North Atlantic sediment cores

High-resolution sediment cores from the Vøring Plateau, the North Iceland shelf, and the East Greenland shelf have been studied to investigate the stability of major surface currents in the Nordic Seas during the Holocene. Results from diatom assemblages and reconstructed sea-surface temperatures (S...

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Bibliographic Details
Main Authors: Andersen, Catherine, Koç, Nalân, Jennings, Anne E, Andrews, John T
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
Age
BC
GC
GKG
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.839405
https://doi.org/10.1594/PANGAEA.839405
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.839405
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.839405 2023-05-15T16:03:37+02:00 (Table 1) Age determination of North Atlantic sediment cores Andersen, Catherine Koç, Nalân Jennings, Anne E Andrews, John T MEDIAN LATITUDE: 66.961305 * MEDIAN LONGITUDE: -13.457761 * SOUTH-BOUND LATITUDE: 66.641333 * WEST-BOUND LONGITUDE: -30.904300 * NORTH-BOUND LATITUDE: 67.125700 * EAST-BOUND LONGITUDE: 7.639330 * DATE/TIME START: 1995-06-08T00:00:00 * DATE/TIME END: 1999-08-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.0025 m * MAXIMUM DEPTH, sediment/rock: 25.3200 m 2004-11-24 text/tab-separated-values, 192 data points https://doi.pangaea.de/10.1594/PANGAEA.839405 https://doi.org/10.1594/PANGAEA.839405 en eng PANGAEA Groenvold, K; Oskarsson, N; Johnsen, Sigfús Jóhann; Clausen, Henrik Brink; Hammer, C U; Bond, Gerard C; Bard, Edouard (1995): Ash layers from Iceland in the Greenland GRIP ice core correlated with oceanic and land sediments. Earth and Planetary Science Letters, 135(1-4), 149-155, https://doi.org/10.1016/0012-821X(95)00145-3 https://doi.pangaea.de/10.1594/PANGAEA.839405 https://doi.org/10.1594/PANGAEA.839405 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Andersen, Catherine; Koç, Nalân; Jennings, Anne E; Andrews, John T (2004): Nonuniform response of the major surface currents in the Nordic Seas to insolation forcing: Implications for the Holocene climate variability. Paleoceanography, 19(2), PA2003, https://doi.org/10.1029/2002PA000873 79US/Fr Age 14C AMS 14C calibrated comment dated dated material dated standard deviation BC Box corer BS88/6_5 Calendar age CALYPSO Calypso Corer DEPTH sediment/rock Elevation of event Event label GC Giant box corer GKG Gravity corer HU93030-019 HUD93/30 Hudson IMAGES I IMAGES V JM97-948/2A Laboratory code/label Latitude of event Longitude of event Marion Dufresne (1995) MD101 MD114 MD952011 MD95-2011 MD99-2269 N.Iceland shelf Reykjafjardarall Voring Plateau Dataset 2004 ftpangaea https://doi.org/10.1594/PANGAEA.839405 https://doi.org/10.1029/2002PA000873 https://doi.org/10.1016/0012-821X(95)00145-3 2023-01-20T09:04:44Z High-resolution sediment cores from the Vøring Plateau, the North Iceland shelf, and the East Greenland shelf have been studied to investigate the stability of major surface currents in the Nordic Seas during the Holocene. Results from diatom assemblages and reconstructed sea-surface temperatures (SSTs) indicate a division of the Holocene into three periods: the Holocene Climate Optimum (9500-6500 calendar (cal) years BP), the Holocene Transition Period (6500-3000 cal years BP) and the Cool Late Holocene Period (3000-0 cal years BP). The overall climate development is in step with the decreasing insolation on the Northern Hemisphere, but regional differences occur regarding both timing and magnitude of SST changes. Sites under the direct influence of the Norwegian Atlantic Current and the Irminger Current indicate SST cooling of 4-5°C from early Holocene to present, compared to 2°C recorded under the East Greenland Current. Superimposed on the general Holocene cooling trend, there is a high-frequency SST variability, which is in the order of 1-1.5°C for the Vøring Plateau and the East Greenland shelf and 2.5-3°C on the North Iceland shelf. Dataset East Greenland east greenland current Greenland Iceland Nordic Seas North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science Greenland Hudson Vøring Plateau ENVELOPE(4.000,4.000,67.000,67.000) ENVELOPE(-30.904300,7.639330,67.125700,66.641333)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 79US/Fr
Age
14C AMS
14C calibrated
comment
dated
dated material
dated standard deviation
BC
Box corer
BS88/6_5
Calendar age
CALYPSO
Calypso Corer
DEPTH
sediment/rock
Elevation of event
Event label
GC
Giant box corer
GKG
Gravity corer
HU93030-019
HUD93/30
Hudson
IMAGES I
IMAGES V
JM97-948/2A
Laboratory code/label
Latitude of event
Longitude of event
Marion Dufresne (1995)
MD101
MD114
MD952011
MD95-2011
MD99-2269
N.Iceland shelf
Reykjafjardarall
Voring Plateau
spellingShingle 79US/Fr
Age
14C AMS
14C calibrated
comment
dated
dated material
dated standard deviation
BC
Box corer
BS88/6_5
Calendar age
CALYPSO
Calypso Corer
DEPTH
sediment/rock
Elevation of event
Event label
GC
Giant box corer
GKG
Gravity corer
HU93030-019
HUD93/30
Hudson
IMAGES I
IMAGES V
JM97-948/2A
Laboratory code/label
Latitude of event
Longitude of event
Marion Dufresne (1995)
MD101
MD114
MD952011
MD95-2011
MD99-2269
N.Iceland shelf
Reykjafjardarall
Voring Plateau
Andersen, Catherine
Koç, Nalân
Jennings, Anne E
Andrews, John T
(Table 1) Age determination of North Atlantic sediment cores
topic_facet 79US/Fr
Age
14C AMS
14C calibrated
comment
dated
dated material
dated standard deviation
BC
Box corer
BS88/6_5
Calendar age
CALYPSO
Calypso Corer
DEPTH
sediment/rock
Elevation of event
Event label
GC
Giant box corer
GKG
Gravity corer
HU93030-019
HUD93/30
Hudson
IMAGES I
IMAGES V
JM97-948/2A
Laboratory code/label
Latitude of event
Longitude of event
Marion Dufresne (1995)
MD101
MD114
MD952011
MD95-2011
MD99-2269
N.Iceland shelf
Reykjafjardarall
Voring Plateau
description High-resolution sediment cores from the Vøring Plateau, the North Iceland shelf, and the East Greenland shelf have been studied to investigate the stability of major surface currents in the Nordic Seas during the Holocene. Results from diatom assemblages and reconstructed sea-surface temperatures (SSTs) indicate a division of the Holocene into three periods: the Holocene Climate Optimum (9500-6500 calendar (cal) years BP), the Holocene Transition Period (6500-3000 cal years BP) and the Cool Late Holocene Period (3000-0 cal years BP). The overall climate development is in step with the decreasing insolation on the Northern Hemisphere, but regional differences occur regarding both timing and magnitude of SST changes. Sites under the direct influence of the Norwegian Atlantic Current and the Irminger Current indicate SST cooling of 4-5°C from early Holocene to present, compared to 2°C recorded under the East Greenland Current. Superimposed on the general Holocene cooling trend, there is a high-frequency SST variability, which is in the order of 1-1.5°C for the Vøring Plateau and the East Greenland shelf and 2.5-3°C on the North Iceland shelf.
format Dataset
author Andersen, Catherine
Koç, Nalân
Jennings, Anne E
Andrews, John T
author_facet Andersen, Catherine
Koç, Nalân
Jennings, Anne E
Andrews, John T
author_sort Andersen, Catherine
title (Table 1) Age determination of North Atlantic sediment cores
title_short (Table 1) Age determination of North Atlantic sediment cores
title_full (Table 1) Age determination of North Atlantic sediment cores
title_fullStr (Table 1) Age determination of North Atlantic sediment cores
title_full_unstemmed (Table 1) Age determination of North Atlantic sediment cores
title_sort (table 1) age determination of north atlantic sediment cores
publisher PANGAEA
publishDate 2004
url https://doi.pangaea.de/10.1594/PANGAEA.839405
https://doi.org/10.1594/PANGAEA.839405
op_coverage MEDIAN LATITUDE: 66.961305 * MEDIAN LONGITUDE: -13.457761 * SOUTH-BOUND LATITUDE: 66.641333 * WEST-BOUND LONGITUDE: -30.904300 * NORTH-BOUND LATITUDE: 67.125700 * EAST-BOUND LONGITUDE: 7.639330 * DATE/TIME START: 1995-06-08T00:00:00 * DATE/TIME END: 1999-08-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.0025 m * MAXIMUM DEPTH, sediment/rock: 25.3200 m
long_lat ENVELOPE(4.000,4.000,67.000,67.000)
ENVELOPE(-30.904300,7.639330,67.125700,66.641333)
geographic Greenland
Hudson
Vøring Plateau
geographic_facet Greenland
Hudson
Vøring Plateau
genre East Greenland
east greenland current
Greenland
Iceland
Nordic Seas
North Atlantic
genre_facet East Greenland
east greenland current
Greenland
Iceland
Nordic Seas
North Atlantic
op_source Supplement to: Andersen, Catherine; Koç, Nalân; Jennings, Anne E; Andrews, John T (2004): Nonuniform response of the major surface currents in the Nordic Seas to insolation forcing: Implications for the Holocene climate variability. Paleoceanography, 19(2), PA2003, https://doi.org/10.1029/2002PA000873
op_relation Groenvold, K; Oskarsson, N; Johnsen, Sigfús Jóhann; Clausen, Henrik Brink; Hammer, C U; Bond, Gerard C; Bard, Edouard (1995): Ash layers from Iceland in the Greenland GRIP ice core correlated with oceanic and land sediments. Earth and Planetary Science Letters, 135(1-4), 149-155, https://doi.org/10.1016/0012-821X(95)00145-3
https://doi.pangaea.de/10.1594/PANGAEA.839405
https://doi.org/10.1594/PANGAEA.839405
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.839405
https://doi.org/10.1029/2002PA000873
https://doi.org/10.1016/0012-821X(95)00145-3
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