Journal article
Punctuated shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1
- Abstract:
-
The Greenland Stadial 1 (GS-1; ~12.9 to 11.65 kyr cal BP) was a period of North Atlantic cooling, thought to have been initiated by North America fresh water runoff that caused a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphase temperature response between the hemispheres (the ‘bipolar seesaw’). Here we exploit sub-fossil New Zealand kauri trees to report the first securely dated, decadally-resolved atmospheric radiocarbon (14C) record...
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- Publication status:
- Published
- Peer review status:
- Peer reviewed
Actions
Authors
Funding
+ Natural Environment Research Council
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Grant:
NE/H009922/1
NER/A/S/2001/01037
NE/I007660/1
NE/H007865/1
+ Ministry for Business, Innovation and Employment
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Grant:
MBIE)-PROP-20224-SFK-UOA
Royal Society of New Zealand
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Bibliographic Details
- Publisher:
- Nature Publishing Group: Open Access Journals - Option C Publisher's website
- Journal:
- Scientific Reports Journal website
- Publication date:
- 2016-05-19
- Acceptance date:
- 2016-04-21
- DOI:
- ISSN:
-
2045-2322
Item Description
- Keywords:
- Pubs id:
-
pubs:623024
- UUID:
-
uuid:0cc17cee-3dfc-458d-8769-8db5d720f4cb
- Local pid:
- pubs:623024
- Source identifiers:
-
623024
- Deposit date:
- 2016-05-19
Terms of use
- Copyright holder:
- Hogg et al
- Copyright date:
- 2016
- Notes:
- Author(s) retain copyright; published by Nature Publishing Group under license. This work is licensed under a Creative Commons Attribution 4.0 International License.
- Licence:
- CC Attribution (CC BY)
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