Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years

A strong outflow event from Lake Agassiz at the end of the Bølling-Allerød plausibly caused the Younger Dryas cold period by an abrupt Arctic freshening, according to geochemical investigation of sediment cores from the Canadian Arctic.

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Finn Süfke, Marcus Gutjahr, Lloyd D. Keigwin, Brendan Reilly, Liviu Giosan, Jörg Lippold
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2022
Subjects:
geo
anthro-bio
Arctic
Ice Sheet
Online Access:https://doi.org/10.1038/s43247-022-00428-3
https://doaj.org/article/a0c8c68e612a4d3db33b73a07abca5cf
id fttriple:oai:gotriple.eu:oai:doaj.org/article:a0c8c68e612a4d3db33b73a07abca5cf
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:a0c8c68e612a4d3db33b73a07abca5cf 2023-05-15T14:32:54+02:00 Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years Finn Süfke Marcus Gutjahr Lloyd D. Keigwin Brendan Reilly Liviu Giosan Jörg Lippold 2022-04-01 https://doi.org/10.1038/s43247-022-00428-3 https://doaj.org/article/a0c8c68e612a4d3db33b73a07abca5cf en eng Nature Portfolio doi:10.1038/s43247-022-00428-3 2662-4435 https://doaj.org/article/a0c8c68e612a4d3db33b73a07abca5cf undefined Communications Earth & Environment, Vol 3, Iss 1, Pp 1-11 (2022) geo anthro-bio Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.1038/s43247-022-00428-3 2023-01-22T18:24:29Z A strong outflow event from Lake Agassiz at the end of the Bølling-Allerød plausibly caused the Younger Dryas cold period by an abrupt Arctic freshening, according to geochemical investigation of sediment cores from the Canadian Arctic. Article in Journal/Newspaper Arctic Ice Sheet Unknown Arctic Communications Earth & Environment 3 1
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
anthro-bio
spellingShingle geo
anthro-bio
Finn Süfke
Marcus Gutjahr
Lloyd D. Keigwin
Brendan Reilly
Liviu Giosan
Jörg Lippold
Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years
topic_facet geo
anthro-bio
description A strong outflow event from Lake Agassiz at the end of the Bølling-Allerød plausibly caused the Younger Dryas cold period by an abrupt Arctic freshening, according to geochemical investigation of sediment cores from the Canadian Arctic.
format Article in Journal/Newspaper
author Finn Süfke
Marcus Gutjahr
Lloyd D. Keigwin
Brendan Reilly
Liviu Giosan
Jörg Lippold
author_facet Finn Süfke
Marcus Gutjahr
Lloyd D. Keigwin
Brendan Reilly
Liviu Giosan
Jörg Lippold
author_sort Finn Süfke
title Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years
title_short Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years
title_full Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years
title_fullStr Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years
title_full_unstemmed Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years
title_sort arctic drainage of laurentide ice sheet meltwater throughout the past 14,700 years
publisher Nature Portfolio
publishDate 2022
url https://doi.org/10.1038/s43247-022-00428-3
https://doaj.org/article/a0c8c68e612a4d3db33b73a07abca5cf
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice Sheet
genre_facet Arctic
Ice Sheet
op_source Communications Earth & Environment, Vol 3, Iss 1, Pp 1-11 (2022)
op_relation doi:10.1038/s43247-022-00428-3
2662-4435
https://doaj.org/article/a0c8c68e612a4d3db33b73a07abca5cf
op_rights undefined
op_doi https://doi.org/10.1038/s43247-022-00428-3
container_title Communications Earth & Environment
container_volume 3
container_issue 1
_version_ 1766306230651846656

Similar Items