Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone.
International audience The precise documentation of the natural variability of the THC during the interglacials in North Atlantic is of critical interest for the understanding of its future evolution under the effect of global warming. It is one of the goals of the AMOCINT project (06-EuroMARC-FP-00...
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ftccsdartic:oai:HAL:hal-04113724v1 2023-07-23T04:20:26+02:00 Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. Kissel, C. Turon, J. L. Cortijo, E. Laj, C. Laboratoire des Sciences du Climat et de l'Environnement (LSCE) Commissariat à l'énergie atomique et aux énergies alternatives (CEA) à renseigner, Unknown Region 2023-06-01 https://hal.science/hal-04113724 en eng HAL CCSD hal-04113724 https://hal.science/hal-04113724 BIBCODE: 2009EGUGA.11.3415K EGU General Assembly 2009 https://hal.science/hal-04113724 EGU General Assembly 2009, 0000, à renseigner, Unknown Region. pp.3415 [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/conferenceObject Conference papers 2023 ftccsdartic 2023-07-01T23:07:38Z International audience The precise documentation of the natural variability of the THC during the interglacials in North Atlantic is of critical interest for the understanding of its future evolution under the effect of global warming. It is one of the goals of the AMOCINT project (06-EuroMARC-FP-008). We report on detailed magnetic analyses of a Holocene marine sequence taken at the Charlie-Gibbs fracture zone (52°S), on the path of the contourite drift at the place where it turns around the Reykjanes ridge, from the Gardar drift northward. This location has been sampled twice. The first core (gravity) has been taken in 1977 with the R.V. J. Charcot from IFREMER. The second one (Casq core) has been taken during the IMAGES MD168-AMOCINT cruise on board the R. V. Marion Dufresne in 2008 (IPEV). In the first core, the apparent sedimentation rate varies between 50 and 79 cm/kyr and it obviously results from compaction as the second one known to be free of any distortion has sedimentation rates of the order of 50 to 140 cm/kyr between present and 10 kyr B.P. The two cores can be perfectly correlated using any physical property allowing to precisely transfer the 19 radiocarbon dates from the old series to the new one. Detailed magnetic analyses have been performed on both cores and will be compared. The magnetic fraction is uniformly composed during the Holocene period of magnetites with a grain size distribution in the pseudo-single domain range (a few micrometers). The magnetic concentration varies in time on both long and short terms. The long-term trends may be fitted by a 4th order polynomial with an increase of the bottom circulation strength in the mid-Holocene. We shall discuss these long term trends together with the short term features in terms of changes in the strength of the bottom current through Holocene and compare them to other proxies an other records also obtained from North Atlantic. Conference Object North Atlantic Deep Water North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Charcot ENVELOPE(139.017,139.017,-69.367,-69.367) Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU]Sciences of the Universe [physics] |
spellingShingle |
[SDU]Sciences of the Universe [physics] Kissel, C. Turon, J. L. Cortijo, E. Laj, C. Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. |
topic_facet |
[SDU]Sciences of the Universe [physics] |
description |
International audience The precise documentation of the natural variability of the THC during the interglacials in North Atlantic is of critical interest for the understanding of its future evolution under the effect of global warming. It is one of the goals of the AMOCINT project (06-EuroMARC-FP-008). We report on detailed magnetic analyses of a Holocene marine sequence taken at the Charlie-Gibbs fracture zone (52°S), on the path of the contourite drift at the place where it turns around the Reykjanes ridge, from the Gardar drift northward. This location has been sampled twice. The first core (gravity) has been taken in 1977 with the R.V. J. Charcot from IFREMER. The second one (Casq core) has been taken during the IMAGES MD168-AMOCINT cruise on board the R. V. Marion Dufresne in 2008 (IPEV). In the first core, the apparent sedimentation rate varies between 50 and 79 cm/kyr and it obviously results from compaction as the second one known to be free of any distortion has sedimentation rates of the order of 50 to 140 cm/kyr between present and 10 kyr B.P. The two cores can be perfectly correlated using any physical property allowing to precisely transfer the 19 radiocarbon dates from the old series to the new one. Detailed magnetic analyses have been performed on both cores and will be compared. The magnetic fraction is uniformly composed during the Holocene period of magnetites with a grain size distribution in the pseudo-single domain range (a few micrometers). The magnetic concentration varies in time on both long and short terms. The long-term trends may be fitted by a 4th order polynomial with an increase of the bottom circulation strength in the mid-Holocene. We shall discuss these long term trends together with the short term features in terms of changes in the strength of the bottom current through Holocene and compare them to other proxies an other records also obtained from North Atlantic. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement (LSCE) Commissariat à l'énergie atomique et aux énergies alternatives (CEA) |
format |
Conference Object |
author |
Kissel, C. Turon, J. L. Cortijo, E. Laj, C. |
author_facet |
Kissel, C. Turon, J. L. Cortijo, E. Laj, C. |
author_sort |
Kissel, C. |
title |
Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. |
title_short |
Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. |
title_full |
Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. |
title_fullStr |
Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. |
title_full_unstemmed |
Long- and Short Term Holocene Variations in the Strength of the North Atlantic Deep Water at the Charlie-Gibbs fracture zone. |
title_sort |
long- and short term holocene variations in the strength of the north atlantic deep water at the charlie-gibbs fracture zone. |
publisher |
HAL CCSD |
publishDate |
2023 |
url |
https://hal.science/hal-04113724 |
op_coverage |
à renseigner, Unknown Region |
long_lat |
ENVELOPE(139.017,139.017,-69.367,-69.367) ENVELOPE(-22.250,-22.250,65.467,65.467) |
geographic |
Charcot Reykjanes |
geographic_facet |
Charcot Reykjanes |
genre |
North Atlantic Deep Water North Atlantic |
genre_facet |
North Atlantic Deep Water North Atlantic |
op_source |
EGU General Assembly 2009 https://hal.science/hal-04113724 EGU General Assembly 2009, 0000, à renseigner, Unknown Region. pp.3415 |
op_relation |
hal-04113724 https://hal.science/hal-04113724 BIBCODE: 2009EGUGA.11.3415K |
_version_ |
1772184761834405888 |