8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland

The best-known climate change in the middle part of the Holocene is an abrupt cooling around 8200 cal. yrs BP (e.g. O’Brien et al., 1995; Bond et al., 1997). This oscillation, known as the 8.2 ka event, was recognised in all most important past climate records, i.e. in the Greenland ice cores (GRIP...

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Main Author: Magdalena FIŁOC
Format: Article in Journal/Newspaper
Language:English
Published: „Ștefan cel Mare” University Press 2016
Subjects:
Q
Online Access:https://doaj.org/article/4db87c37d1314411b9379c3c97ac89a5
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spelling ftdoajarticles:oai:doaj.org/article:4db87c37d1314411b9379c3c97ac89a5 2023-05-15T16:28:09+02:00 8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland Magdalena FIŁOC 2016-06-01T00:00:00Z https://doaj.org/article/4db87c37d1314411b9379c3c97ac89a5 EN eng „Ștefan cel Mare” University Press http://georeview.ro/ojs/index.php/revista/article/view/301 https://doaj.org/toc/1583-1469 1583-1469 https://doaj.org/article/4db87c37d1314411b9379c3c97ac89a5 GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series, Vol 26, Iss 2, Pp 16-18 (2016) Science Q Science (General) Q1-390 article 2016 ftdoajarticles 2022-12-31T06:42:37Z The best-known climate change in the middle part of the Holocene is an abrupt cooling around 8200 cal. yrs BP (e.g. O’Brien et al., 1995; Bond et al., 1997). This oscillation, known as the 8.2 ka event, was recognised in all most important past climate records, i.e. in the Greenland ice cores (GRIP and GRIP2) and in North Atlantic deep sea cores (O’Brien et al., 1995; Bond et al., 1997), and then it was demonstrated in many records in the world Article in Journal/Newspaper Greenland Greenland ice cores GRIP North Atlantic Directory of Open Access Journals: DOAJ Articles Greenland
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Science (General)
Q1-390
spellingShingle Science
Q
Science (General)
Q1-390
Magdalena FIŁOC
8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
topic_facet Science
Q
Science (General)
Q1-390
description The best-known climate change in the middle part of the Holocene is an abrupt cooling around 8200 cal. yrs BP (e.g. O’Brien et al., 1995; Bond et al., 1997). This oscillation, known as the 8.2 ka event, was recognised in all most important past climate records, i.e. in the Greenland ice cores (GRIP and GRIP2) and in North Atlantic deep sea cores (O’Brien et al., 1995; Bond et al., 1997), and then it was demonstrated in many records in the world
format Article in Journal/Newspaper
author Magdalena FIŁOC
author_facet Magdalena FIŁOC
author_sort Magdalena FIŁOC
title 8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
title_short 8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
title_full 8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
title_fullStr 8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
title_full_unstemmed 8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
title_sort 8.2 ka event and others cold climate oscillations in middle holocene – evidence from suchar wielki lake, ne poland
publisher „Ștefan cel Mare” University Press
publishDate 2016
url https://doaj.org/article/4db87c37d1314411b9379c3c97ac89a5
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland ice cores
GRIP
North Atlantic
genre_facet Greenland
Greenland ice cores
GRIP
North Atlantic
op_source GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series, Vol 26, Iss 2, Pp 16-18 (2016)
op_relation http://georeview.ro/ojs/index.php/revista/article/view/301
https://doaj.org/toc/1583-1469
1583-1469
https://doaj.org/article/4db87c37d1314411b9379c3c97ac89a5
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