Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013
This NSF funded project was dedicated to testing the idea that the Younger Dryas cold epoch (~13,000 to ~12700 years Before Present) was caused by a massive flood of fresh water via Mackenzie River to the eastern Beaufort Sea. It was noted in a 1975 paper in Science by Kennett and Shackleton that th...
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ftdatacite:10.18739/a2qz22h33 2023-05-15T15:18:36+02:00 Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 Keigwin, Lloyd Driscoll, Neal 2018 text/xml https://dx.doi.org/10.18739/a2qz22h33 https://arcticdata.io/catalog/#view/doi:10.18739/A2QZ22H33 en eng Arctic Data Center piston core foraminifera oxygen isotopes deglaciation meltwater Mackenzie River Younger Dryas radiocarbon dataset Dataset 2018 ftdatacite https://doi.org/10.18739/a2qz22h33 2021-11-05T12:55:41Z This NSF funded project was dedicated to testing the idea that the Younger Dryas cold epoch (~13,000 to ~12700 years Before Present) was caused by a massive flood of fresh water via Mackenzie River to the eastern Beaufort Sea. It was noted in a 1975 paper in Science by Kennett and Shackleton that the flood of fresh water down Mississippi River was interrupted at about 13 kilo annums (ka), even though there was no reason to suspect a pause in glacial ice melt. The Kennett and Shackleton hypothesis led to the expectation that as glacial ice continued to melt and retreat northward, at some point eastern outlets for meltwater must have opened to the St. Lawrence system around the time the Mississippi flood ended. However, researchers looked for decades for the signal of low δ18O in planktonic foraminifera off eastern Canada, to no avail. The only other logical direction for meltwater would have been to the north through Mackenzie River. Two piston cores recovered during USCGC Healy Cruise 2013 near Mackenzie River have the low δ18O signal of the flood beginning at 12.9 ka according to radiocarbon dating. Those flood waters most likely reduced the surface ocean salinity in the Nordic Seas, reducing the production of deep water, and thereby reducing the northward the flux of warm salty waters that account for the temperate climate in northern Europe today. This flood was most likely the trigger for the younger Dryas cooling. Analytical data associated with this project, and especially those data published in Keigwin et al. (2018, "Deglacial floods in the Beaufort Sea preceded Younger Dryas cooling," Nature Geoscience, dos/10.1038/s41561-018-0169-6), can be found in the NOAA WDS paleoclimatology database (https://www.ncdc.noaa.gov/paleo/study/24790). Those data are mostly the metadata, the chronology, and the stable isotope results. The metadata are repeated here. Supplementary information to Keigwin et al. 2018 may be found at the Nature Geoscience url shown above. Underway geophysical data can be found here: doi.org/10.18739/A2FB4WK7X. Dataset Arctic Arctic Ocean Beaufort Sea Foraminifera* Mackenzie river Nordic Seas Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Canada Kennett ENVELOPE(-65.167,-65.167,-67.117,-67.117) Mackenzie River Shackleton |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
piston core foraminifera oxygen isotopes deglaciation meltwater Mackenzie River Younger Dryas radiocarbon |
spellingShingle |
piston core foraminifera oxygen isotopes deglaciation meltwater Mackenzie River Younger Dryas radiocarbon Keigwin, Lloyd Driscoll, Neal Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 |
topic_facet |
piston core foraminifera oxygen isotopes deglaciation meltwater Mackenzie River Younger Dryas radiocarbon |
description |
This NSF funded project was dedicated to testing the idea that the Younger Dryas cold epoch (~13,000 to ~12700 years Before Present) was caused by a massive flood of fresh water via Mackenzie River to the eastern Beaufort Sea. It was noted in a 1975 paper in Science by Kennett and Shackleton that the flood of fresh water down Mississippi River was interrupted at about 13 kilo annums (ka), even though there was no reason to suspect a pause in glacial ice melt. The Kennett and Shackleton hypothesis led to the expectation that as glacial ice continued to melt and retreat northward, at some point eastern outlets for meltwater must have opened to the St. Lawrence system around the time the Mississippi flood ended. However, researchers looked for decades for the signal of low δ18O in planktonic foraminifera off eastern Canada, to no avail. The only other logical direction for meltwater would have been to the north through Mackenzie River. Two piston cores recovered during USCGC Healy Cruise 2013 near Mackenzie River have the low δ18O signal of the flood beginning at 12.9 ka according to radiocarbon dating. Those flood waters most likely reduced the surface ocean salinity in the Nordic Seas, reducing the production of deep water, and thereby reducing the northward the flux of warm salty waters that account for the temperate climate in northern Europe today. This flood was most likely the trigger for the younger Dryas cooling. Analytical data associated with this project, and especially those data published in Keigwin et al. (2018, "Deglacial floods in the Beaufort Sea preceded Younger Dryas cooling," Nature Geoscience, dos/10.1038/s41561-018-0169-6), can be found in the NOAA WDS paleoclimatology database (https://www.ncdc.noaa.gov/paleo/study/24790). Those data are mostly the metadata, the chronology, and the stable isotope results. The metadata are repeated here. Supplementary information to Keigwin et al. 2018 may be found at the Nature Geoscience url shown above. Underway geophysical data can be found here: doi.org/10.18739/A2FB4WK7X. |
format |
Dataset |
author |
Keigwin, Lloyd Driscoll, Neal |
author_facet |
Keigwin, Lloyd Driscoll, Neal |
author_sort |
Keigwin, Lloyd |
title |
Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 |
title_short |
Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 |
title_full |
Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 |
title_fullStr |
Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 |
title_full_unstemmed |
Sediment cores from Younger Dryas cold epoch, United States Coast Guard Cutter (USCGC) Healy cruise, Eastern Beaufort Sea, Arctic Ocean, 2013 |
title_sort |
sediment cores from younger dryas cold epoch, united states coast guard cutter (uscgc) healy cruise, eastern beaufort sea, arctic ocean, 2013 |
publisher |
Arctic Data Center |
publishDate |
2018 |
url |
https://dx.doi.org/10.18739/a2qz22h33 https://arcticdata.io/catalog/#view/doi:10.18739/A2QZ22H33 |
long_lat |
ENVELOPE(-65.167,-65.167,-67.117,-67.117) |
geographic |
Arctic Arctic Ocean Canada Kennett Mackenzie River Shackleton |
geographic_facet |
Arctic Arctic Ocean Canada Kennett Mackenzie River Shackleton |
genre |
Arctic Arctic Ocean Beaufort Sea Foraminifera* Mackenzie river Nordic Seas Planktonic foraminifera |
genre_facet |
Arctic Arctic Ocean Beaufort Sea Foraminifera* Mackenzie river Nordic Seas Planktonic foraminifera |
op_doi |
https://doi.org/10.18739/a2qz22h33 |
_version_ |
1766348798954569728 |