North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ...
Heinrich events are well documented for the last glaciation, but little is known about their occurrence in older glacial periods of the Pleistocene. Here we report scanning XRF and bulk carbonate d18O results from Integrated Ocean Drilling Program Site U1308 (reoccupation of Deep Sea Drilling Projec...
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Online Access: | https://dx.doi.org/10.1594/pangaea.831743 https://doi.pangaea.de/10.1594/PANGAEA.831743 |
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ftdatacite:10.1594/pangaea.831743 2024-09-15T18:11:06+00:00 North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... Hodell, David A Channell, James E T Curtis, Jason H Romero, Oscar E Röhl, Ursula 2008 application/zip https://dx.doi.org/10.1594/pangaea.831743 https://doi.pangaea.de/10.1594/PANGAEA.831743 en eng PANGAEA https://dx.doi.org/10.1029/2008pa001591 https://dx.doi.org/10.25921/3jth-d104 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Exp303 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Collection Supplementary Publication Series of Datasets article 2008 ftdatacite https://doi.org/10.1594/pangaea.83174310.1029/2008pa00159110.25921/3jth-d104 2024-09-02T08:39:34Z Heinrich events are well documented for the last glaciation, but little is known about their occurrence in older glacial periods of the Pleistocene. Here we report scanning XRF and bulk carbonate d18O results from Integrated Ocean Drilling Program Site U1308 (reoccupation of Deep Sea Drilling Project Site 609) that are used to develop proxy records of ice-rafted detritus (IRD) for the last ~1.4 Ma. Ca/Sr is used as an indicator of IRD layers that are rich in detrital carbonate (i.e., Heinrich layers), whereas Si/Sr reflects layers that are poor in biogenic carbonate and relatively rich in detrital silicate minerals. A pronounced change occurred in the composition and frequency of IRD at ~640 ka during marine isotope stage (MIS) 16, coinciding with the end of the middle Pleistocene transition. At this time, "Hudson Strait" Heinrich layers suddenly appeared in the sedimentary record of Site U1308, and the dominant period of the Si/Sr proxy shifted from 41 ka prior to 640 ka to 100 ka afterward. The onset of ... : Supplement to: Hodell, David A; Channell, James E T; Curtis, Jason H; Romero, Oscar E; Röhl, Ursula (2008): Onset of 'Hudson Strait' Heinrich Events in the eastern North Atlantic at the end of the middle Pleistocene transition (~640 ka)? Paleoceanography, 23(4), PA4218 ... Article in Journal/Newspaper Hudson Strait North Atlantic DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Composite Core Exp303 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
spellingShingle |
Composite Core Exp303 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP Hodell, David A Channell, James E T Curtis, Jason H Romero, Oscar E Röhl, Ursula North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... |
topic_facet |
Composite Core Exp303 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP |
description |
Heinrich events are well documented for the last glaciation, but little is known about their occurrence in older glacial periods of the Pleistocene. Here we report scanning XRF and bulk carbonate d18O results from Integrated Ocean Drilling Program Site U1308 (reoccupation of Deep Sea Drilling Project Site 609) that are used to develop proxy records of ice-rafted detritus (IRD) for the last ~1.4 Ma. Ca/Sr is used as an indicator of IRD layers that are rich in detrital carbonate (i.e., Heinrich layers), whereas Si/Sr reflects layers that are poor in biogenic carbonate and relatively rich in detrital silicate minerals. A pronounced change occurred in the composition and frequency of IRD at ~640 ka during marine isotope stage (MIS) 16, coinciding with the end of the middle Pleistocene transition. At this time, "Hudson Strait" Heinrich layers suddenly appeared in the sedimentary record of Site U1308, and the dominant period of the Si/Sr proxy shifted from 41 ka prior to 640 ka to 100 ka afterward. The onset of ... : Supplement to: Hodell, David A; Channell, James E T; Curtis, Jason H; Romero, Oscar E; Röhl, Ursula (2008): Onset of 'Hudson Strait' Heinrich Events in the eastern North Atlantic at the end of the middle Pleistocene transition (~640 ka)? Paleoceanography, 23(4), PA4218 ... |
format |
Article in Journal/Newspaper |
author |
Hodell, David A Channell, James E T Curtis, Jason H Romero, Oscar E Röhl, Ursula |
author_facet |
Hodell, David A Channell, James E T Curtis, Jason H Romero, Oscar E Röhl, Ursula |
author_sort |
Hodell, David A |
title |
North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... |
title_short |
North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... |
title_full |
North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... |
title_fullStr |
North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... |
title_full_unstemmed |
North Atlantic IODP Site 303-U1308 Middle Pleistocene Heinrich Events record ... |
title_sort |
north atlantic iodp site 303-u1308 middle pleistocene heinrich events record ... |
publisher |
PANGAEA |
publishDate |
2008 |
url |
https://dx.doi.org/10.1594/pangaea.831743 https://doi.pangaea.de/10.1594/PANGAEA.831743 |
genre |
Hudson Strait North Atlantic |
genre_facet |
Hudson Strait North Atlantic |
op_relation |
https://dx.doi.org/10.1029/2008pa001591 https://dx.doi.org/10.25921/3jth-d104 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.83174310.1029/2008pa00159110.25921/3jth-d104 |
_version_ |
1810448702954799104 |