Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean
Mass accumulation rates (MAR) of different components of North Pacific deep-sea sediment provide detailed information about the timing of the onset of major Northern Hemisphere glaciation that occurred at 2.65 Ma. An increase in explosive volcanism in the Kamchatka-Kurile and Aleutian arcs occured a...
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2001
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.706310 2023-05-15T16:59:17+02:00 Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean Prueher, Libby M Rea, David K MEDIAN LATITUDE: 51.975767 * MEDIAN LONGITUDE: -177.692544 * SOUTH-BOUND LATITUDE: 50.363300 * WEST-BOUND LONGITUDE: 167.599800 * NORTH-BOUND LATITUDE: 54.365500 * EAST-BOUND LONGITUDE: -148.446000 * DATE/TIME START: 1992-08-05T00:00:00 * DATE/TIME END: 1992-09-16T00:00:00 2001-10-22 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.706310 https://doi.org/10.1594/PANGAEA.706310 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.706310 https://doi.org/10.1594/PANGAEA.706310 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Prueher, Libby M; Rea, David K (2001): Volcanic triggering of late Pliocene glaciation: evidence from the flux of volcanic glass and ice-rafted debris to the North Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 173(3-4), 215-230, https://doi.org/10.1016/S0031-0182(01)00323-6 145-882 145-883 145-887 COMPCORE Composite Core Joides Resolution Leg145 North Pacific Ocean Ocean Drilling Program ODP Dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.706310 https://doi.org/10.1016/S0031-0182(01)00323-6 2023-01-20T07:31:15Z Mass accumulation rates (MAR) of different components of North Pacific deep-sea sediment provide detailed information about the timing of the onset of major Northern Hemisphere glaciation that occurred at 2.65 Ma. An increase in explosive volcanism in the Kamchatka-Kurile and Aleutian arcs occured at this same time, suggesting a link between volcanism and glaciation. Sediments recovered by piston-coring techniques during ODP Leg 145 provide a unique opportunity to undertake a detailed test of this possibility. Here we use volcanic glass as a proxy for explosive volcanism and ice-rafted debris (IRD) as a proxy for glaciation. The MAR of both glass and IRD increase markedly at 2.65 Ma. Further, the flux of the volcanic glass increased just prior the flix of ice-radted material, suggesting that the cooling resulting from explosive volcanic eruptions may have been the ultimate trigger for the mid-Pliocene glacial intensification. Dataset Kamchatka PANGAEA - Data Publisher for Earth & Environmental Science Pacific ENVELOPE(167.599800,-148.446000,54.365500,50.363300) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
145-882 145-883 145-887 COMPCORE Composite Core Joides Resolution Leg145 North Pacific Ocean Ocean Drilling Program ODP |
spellingShingle |
145-882 145-883 145-887 COMPCORE Composite Core Joides Resolution Leg145 North Pacific Ocean Ocean Drilling Program ODP Prueher, Libby M Rea, David K Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean |
topic_facet |
145-882 145-883 145-887 COMPCORE Composite Core Joides Resolution Leg145 North Pacific Ocean Ocean Drilling Program ODP |
description |
Mass accumulation rates (MAR) of different components of North Pacific deep-sea sediment provide detailed information about the timing of the onset of major Northern Hemisphere glaciation that occurred at 2.65 Ma. An increase in explosive volcanism in the Kamchatka-Kurile and Aleutian arcs occured at this same time, suggesting a link between volcanism and glaciation. Sediments recovered by piston-coring techniques during ODP Leg 145 provide a unique opportunity to undertake a detailed test of this possibility. Here we use volcanic glass as a proxy for explosive volcanism and ice-rafted debris (IRD) as a proxy for glaciation. The MAR of both glass and IRD increase markedly at 2.65 Ma. Further, the flux of the volcanic glass increased just prior the flix of ice-radted material, suggesting that the cooling resulting from explosive volcanic eruptions may have been the ultimate trigger for the mid-Pliocene glacial intensification. |
format |
Dataset |
author |
Prueher, Libby M Rea, David K |
author_facet |
Prueher, Libby M Rea, David K |
author_sort |
Prueher, Libby M |
title |
Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean |
title_short |
Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean |
title_full |
Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean |
title_fullStr |
Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean |
title_full_unstemmed |
Accumulation rates of volcanic glass and ice-rafted debris in sediments of the North Pacific Ocean |
title_sort |
accumulation rates of volcanic glass and ice-rafted debris in sediments of the north pacific ocean |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.706310 https://doi.org/10.1594/PANGAEA.706310 |
op_coverage |
MEDIAN LATITUDE: 51.975767 * MEDIAN LONGITUDE: -177.692544 * SOUTH-BOUND LATITUDE: 50.363300 * WEST-BOUND LONGITUDE: 167.599800 * NORTH-BOUND LATITUDE: 54.365500 * EAST-BOUND LONGITUDE: -148.446000 * DATE/TIME START: 1992-08-05T00:00:00 * DATE/TIME END: 1992-09-16T00:00:00 |
long_lat |
ENVELOPE(167.599800,-148.446000,54.365500,50.363300) |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Supplement to: Prueher, Libby M; Rea, David K (2001): Volcanic triggering of late Pliocene glaciation: evidence from the flux of volcanic glass and ice-rafted debris to the North Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 173(3-4), 215-230, https://doi.org/10.1016/S0031-0182(01)00323-6 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.706310 https://doi.org/10.1594/PANGAEA.706310 |
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.706310 https://doi.org/10.1016/S0031-0182(01)00323-6 |
_version_ |
1766051513323487232 |