Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation

Proceedings of the National Academy of Sciences of the United States of America

Volumn 113, Issue 13, 2016, Pages 3465-3470

  Bauska, Thomas K ^a,b   Baggenstos, Daniel ^c   Brook, Edward J ^a   Mix, Alan C ^a   Marcott, Shaun A ^d   Petrenko, Vasilii V ^e   Schaefer, Hinrich ^f   Severinghaus, Jeffrey P ^c   Lee, James E ^a   Thiemens, Mark H ^g  

^a OREGON STATE UNIVERSITY   (United States)

^b UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^c UNIVERSITY OF CALIFORNIA   (United States)

^d UNIVERSITY OF WISCONSIN MADISON   (United States)

^e UNIVERSITY OF ROCHESTER   (United States)

^f NATIONAL INSTITUTE OF WATER AND ATMOSPHERIC RESEARCH   (New Zealand)

^g UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Atmospheric CO2; Carbon cycle; Ice cores; Last deglaciation; Paleoclimate

Indexed keywords

CARBON; CARBON DIOXIDE; ICE;

AIR; ANTARCTICA; ARTICLE; ATMOSPHERE; DEGLACIATION; GAS EXCHANGE; HOLOCENE; NORTHERN HEMISPHERE; OXIDATION; PRIORITY JOURNAL; SEA; TEMPERATURE; TREND STUDY;

EID: 84962074334     PISSN: 00278424     EISSN: 10916490     Source Type: Journal    
DOI: 10.1073/pnas.1513868113     Document Type: Article

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