Rapid oceanic and atmospheric changes during the Younger Dryas cold period

2009 ◽  
Vol 2 (3) ◽  
pp. 202-205 ◽  
Author(s):  
Jostein Bakke ◽  
Øyvind Lie ◽  
Einar Heegaard ◽  
Trond Dokken ◽  
Gerald H. Haug ◽  
...  
Keyword(s):  
Younger Dryas ◽  
Cold Period ◽  
Atmospheric Changes

scholarly journals A modeling study of oceanic nitrous oxide during the Younger Dryas cold period

2003 ◽  
Vol 30 (2) ◽  
Author(s):  
Beat Goldstein ◽  
Fortunat Joos ◽  
Thomas F. Stocker
Keyword(s):  
Nitrous Oxide ◽  
Younger Dryas ◽  
Cold Period ◽  
Modeling Study

Opening of glacial Lake Agassiz’s eastern outlets by the start of the Younger Dryas cold period

Geology ◽  
2018 ◽  
Vol 46 (2) ◽  
pp. 155-158 ◽  
Author(s):  
David J. Leydet ◽  
Anders E. Carlson ◽  
James T. Teller ◽  
Andrew Breckenridge ◽  
Aaron M. Barth ◽  
...  
Keyword(s):  
Younger Dryas ◽  
Cold Period ◽  
Glacial Lake

An abrupt wind shift in western Europe at the onset of the Younger Dryas cold period

2008 ◽  
Vol 1 (8) ◽  
pp. 520-523 ◽  
Author(s):  
Achim Brauer ◽  
Gerald H. Haug ◽  
Peter Dulski ◽  
Daniel M. Sigman ◽  
Jörg F. W. Negendank
Keyword(s):  
Western Europe ◽  
Younger Dryas ◽  
Cold Period

Radiocarbon dates, Mya arenaria phase of the Champlain Sea

1969 ◽  
Vol 6 (3) ◽  
pp. 367-372 ◽  
Author(s):  
John A. Elson
Keyword(s):  
Younger Dryas ◽  
Mya Arenaria ◽  
Cold Period ◽  
Water Phase ◽  
Radiocarbon Dates ◽  
History Of

The history of the Champlain Sea is divided into an early cold period of subarctic water termed the Hiatella phase that lasted from its inception, about 11 800 years ago (Two Creeks time), until a low water phase about 10 800 years ago (Younger Dryas or Valders time). This was followed by an interval of warmer boreal water, here called the Mya arenaria phase, that lasted from about 10 800 years ago until 10 200 years ago or the end of the Champlain Sea.General descriptions, previously unpublished, of Groningen dates GrN 2031 (10 870 ± 100 B.P.), GrN 2032(10 450 ± 80 B.P.), GrN 2034 (10 590 ± 100 B.P.), and GrN 2035 (10 330 ± 100 B.P.) are presented. These dates record the Mya arenaria phase of the Champlain Sea, which may have had an initial rising (transgressive) phase, though the stratigraphic evidence, supported by three sets of radiocarbon dates, is not wholly conclusive.

scholarly journals Multiple causes of the Younger Dryas cold period

2015 ◽  
Vol 8 (12) ◽  
pp. 946-949 ◽  
Author(s):  
Hans Renssen ◽  
Aurélien Mairesse ◽  
Hugues Goosse ◽  
Pierre Mathiot ◽  
Oliver Heiri ◽  
...  
Keyword(s):  
Younger Dryas ◽  
Cold Period ◽  
Multiple Causes
Sign in / Sign up

Export Citation Format

Share Document