Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages
Clay mineralogy and grain-size properties from two well-dated, high resolution sediment cores recovered from the western Alaskan continental are used to decipher millennial-scale changes in sediment provenance and sedimentary transport during the last 32 kyrs. During the last glacial maximum, the de...
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ftawi:oai:epic.awi.de:44780 2023-05-15T15:43:28+02:00 Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages Wang, R. Kühn, H. Gersonde, R. Biskaborn, Boris K. Kuhn, Gerhard Diekmann, Bernhard 2017 https://epic.awi.de/id/eprint/44780/ https://hdl.handle.net/10013/epic.51009 unknown Wang, R. , Kühn, H. , Gersonde, R. , Biskaborn, B. K. orcid:0000-0003-2378-0348 , Kuhn, G. orcid:0000-0001-6069-7485 and Diekmann, B. orcid:0000-0001-5129-3649 (2017) Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages , PAGES 5th Open Scientific Meeting, Zaragoza, Spain, 9 May 2017 - 13 May 2017 . hdl:10013/epic.51009 EPIC3PAGES 5th Open Scientific Meeting, Zaragoza, Spain, 2017-05-09-2017-05-13 Conference notRev 2017 ftawi 2022-10-02T23:12:36Z Clay mineralogy and grain-size properties from two well-dated, high resolution sediment cores recovered from the western Alaskan continental are used to decipher millennial-scale changes in sediment provenance and sedimentary transport during the last 32 kyrs. During the last glacial maximum, the depositional environment was characterized by hemipelagic background sedimentation with overregional sediment sources. Maximum values of fluvial suspensions and kaolinite concentration occur during the late Heinrich event 1 (H1), which point to the sudden influx of clay-laden meltwaters from Northern Alaska. For the subsequent deglacial Bølling-Allerød (BA) interval, meltwater supply changed from glacial-fluvial to more fluvial, caused by warming that probably led to increased snow melt and permafrost thaw. The fresh-water lid might have eased local overturning ventilation in the Bering Sea water that promoted the deposition of laminated sediments. During Holocene sea-level rise the shore line moved far away from the site and reduced terrigenous sediment influx. Strong contour currents possibly led to the winnowing of sediments and caused residual sand enrichment. Conference Object Bering Sea permafrost Alaska Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Bering Sea |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
Clay mineralogy and grain-size properties from two well-dated, high resolution sediment cores recovered from the western Alaskan continental are used to decipher millennial-scale changes in sediment provenance and sedimentary transport during the last 32 kyrs. During the last glacial maximum, the depositional environment was characterized by hemipelagic background sedimentation with overregional sediment sources. Maximum values of fluvial suspensions and kaolinite concentration occur during the late Heinrich event 1 (H1), which point to the sudden influx of clay-laden meltwaters from Northern Alaska. For the subsequent deglacial Bølling-Allerød (BA) interval, meltwater supply changed from glacial-fluvial to more fluvial, caused by warming that probably led to increased snow melt and permafrost thaw. The fresh-water lid might have eased local overturning ventilation in the Bering Sea water that promoted the deposition of laminated sediments. During Holocene sea-level rise the shore line moved far away from the site and reduced terrigenous sediment influx. Strong contour currents possibly led to the winnowing of sediments and caused residual sand enrichment. |
format |
Conference Object |
author |
Wang, R. Kühn, H. Gersonde, R. Biskaborn, Boris K. Kuhn, Gerhard Diekmann, Bernhard |
spellingShingle |
Wang, R. Kühn, H. Gersonde, R. Biskaborn, Boris K. Kuhn, Gerhard Diekmann, Bernhard Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages |
author_facet |
Wang, R. Kühn, H. Gersonde, R. Biskaborn, Boris K. Kuhn, Gerhard Diekmann, Bernhard |
author_sort |
Wang, R. |
title |
Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages |
title_short |
Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages |
title_full |
Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages |
title_fullStr |
Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages |
title_full_unstemmed |
Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages |
title_sort |
provenance and dispersal of terrigenous sediments in the bering sea slope: implications for late glacial land-ocean linkages |
publishDate |
2017 |
url |
https://epic.awi.de/id/eprint/44780/ https://hdl.handle.net/10013/epic.51009 |
geographic |
Bering Sea |
geographic_facet |
Bering Sea |
genre |
Bering Sea permafrost Alaska |
genre_facet |
Bering Sea permafrost Alaska |
op_source |
EPIC3PAGES 5th Open Scientific Meeting, Zaragoza, Spain, 2017-05-09-2017-05-13 |
op_relation |
Wang, R. , Kühn, H. , Gersonde, R. , Biskaborn, B. K. orcid:0000-0003-2378-0348 , Kuhn, G. orcid:0000-0001-6069-7485 and Diekmann, B. orcid:0000-0001-5129-3649 (2017) Provenance and dispersal of terrigenous sediments in the Bering Sea slope: Implications for late glacial land-ocean linkages , PAGES 5th Open Scientific Meeting, Zaragoza, Spain, 9 May 2017 - 13 May 2017 . hdl:10013/epic.51009 |
_version_ |
1766377627496480768 |