Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum
The assemblages of marine sediments on the SW Iberian shelf have been controlled by contributions from distinct sources, which have varied in response to environmental changes since the Last Glacial Maximum (LGM). The rapid, decadal scale Mediterranean overturning circulation permits mixing of suspe...
Published in: | Earth and Planetary Science Letters |
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Online Access: | https://oceanrep.geomar.de/id/eprint/12574/ https://oceanrep.geomar.de/id/eprint/12574/1/Stumpf.pdf https://doi.org/10.1016/j.epsl.2011.10.002 |
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ftoceanrep:oai:oceanrep.geomar.de:12574 2023-05-15T17:36:08+02:00 Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum Stumpf, Roland Frank, Martin Schönfeld, Joachim Haley, Brian A. 2011 text https://oceanrep.geomar.de/id/eprint/12574/ https://oceanrep.geomar.de/id/eprint/12574/1/Stumpf.pdf https://doi.org/10.1016/j.epsl.2011.10.002 en eng Elsevier https://oceanrep.geomar.de/id/eprint/12574/1/Stumpf.pdf Stumpf, R., Frank, M. , Schönfeld, J. and Haley, B. A. (2011) Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum. Earth and Planetary Science Letters, 312 (1-2). pp. 80-90. DOI 10.1016/j.epsl.2011.10.002 <https://doi.org/10.1016/j.epsl.2011.10.002>. doi:10.1016/j.epsl.2011.10.002 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2011 ftoceanrep https://doi.org/10.1016/j.epsl.2011.10.002 2023-04-07T15:01:05Z The assemblages of marine sediments on the SW Iberian shelf have been controlled by contributions from distinct sources, which have varied in response to environmental changes since the Last Glacial Maximum (LGM). The rapid, decadal scale Mediterranean overturning circulation permits mixing of suspended particles from the entire Mediterranean Sea. They are entrained into the suspended particulate matter (SPM) carried by Mediterranean Outflow Water (MOW), which enters the eastern North Atlantic through the Strait of Gibraltar and spreads at intermediate depths in the Gulf of Cadiz and along the Portuguese continental margin. Other major sediment sources that have contributed to the characteristics and budget of SPM along the flow path of MOW on the SW Iberian shelf are North African dust and river-transported particles from the Iberian Peninsula. To reconstruct climate- and circulation-driven changes in the supply of sediments over the past ~ 23 000 cal yr B.P., radiogenic Nd, Sr and Pb isotope records of the clay-size sediment fraction were obtained from one gravity core in the Gulf of Cadiz (577 m water depth) and from two gravity cores on the Portuguese shelf (1745 m, 1974 m water depth). These records are supplemented by time series analyses of clay mineral abundances from the same set of samples. Contrary to expectations, the transition from the LGM to the Holocene was not accompanied by strong changes in sediment provenance or transport, whereas Heinrich Event 1 (H1) and the African Humid Period (AHP) were marked by significantly different isotopic signatures reflecting changes in source contributions caused by supply of ice rafted material originating from the North American craton during H1 and diminished supply of Saharan dust during the AHP. The data also reveal that the timing of variations in the clay mineral abundances was decoupled from that of the radiogenic isotope signatures. Article in Journal/Newspaper North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Earth and Planetary Science Letters 312 1-2 80 90 |
institution |
Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
The assemblages of marine sediments on the SW Iberian shelf have been controlled by contributions from distinct sources, which have varied in response to environmental changes since the Last Glacial Maximum (LGM). The rapid, decadal scale Mediterranean overturning circulation permits mixing of suspended particles from the entire Mediterranean Sea. They are entrained into the suspended particulate matter (SPM) carried by Mediterranean Outflow Water (MOW), which enters the eastern North Atlantic through the Strait of Gibraltar and spreads at intermediate depths in the Gulf of Cadiz and along the Portuguese continental margin. Other major sediment sources that have contributed to the characteristics and budget of SPM along the flow path of MOW on the SW Iberian shelf are North African dust and river-transported particles from the Iberian Peninsula. To reconstruct climate- and circulation-driven changes in the supply of sediments over the past ~ 23 000 cal yr B.P., radiogenic Nd, Sr and Pb isotope records of the clay-size sediment fraction were obtained from one gravity core in the Gulf of Cadiz (577 m water depth) and from two gravity cores on the Portuguese shelf (1745 m, 1974 m water depth). These records are supplemented by time series analyses of clay mineral abundances from the same set of samples. Contrary to expectations, the transition from the LGM to the Holocene was not accompanied by strong changes in sediment provenance or transport, whereas Heinrich Event 1 (H1) and the African Humid Period (AHP) were marked by significantly different isotopic signatures reflecting changes in source contributions caused by supply of ice rafted material originating from the North American craton during H1 and diminished supply of Saharan dust during the AHP. The data also reveal that the timing of variations in the clay mineral abundances was decoupled from that of the radiogenic isotope signatures. |
format |
Article in Journal/Newspaper |
author |
Stumpf, Roland Frank, Martin Schönfeld, Joachim Haley, Brian A. |
spellingShingle |
Stumpf, Roland Frank, Martin Schönfeld, Joachim Haley, Brian A. Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum |
author_facet |
Stumpf, Roland Frank, Martin Schönfeld, Joachim Haley, Brian A. |
author_sort |
Stumpf, Roland |
title |
Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum |
title_short |
Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum |
title_full |
Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum |
title_fullStr |
Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum |
title_full_unstemmed |
Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum |
title_sort |
climatically driven changes in sediment supply on the sw iberian shelf since the last glacial maximum |
publisher |
Elsevier |
publishDate |
2011 |
url |
https://oceanrep.geomar.de/id/eprint/12574/ https://oceanrep.geomar.de/id/eprint/12574/1/Stumpf.pdf https://doi.org/10.1016/j.epsl.2011.10.002 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/12574/1/Stumpf.pdf Stumpf, R., Frank, M. , Schönfeld, J. and Haley, B. A. (2011) Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum. Earth and Planetary Science Letters, 312 (1-2). pp. 80-90. DOI 10.1016/j.epsl.2011.10.002 <https://doi.org/10.1016/j.epsl.2011.10.002>. doi:10.1016/j.epsl.2011.10.002 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.epsl.2011.10.002 |
container_title |
Earth and Planetary Science Letters |
container_volume |
312 |
container_issue |
1-2 |
container_start_page |
80 |
op_container_end_page |
90 |
_version_ |
1766135535911305216 |