Eocene cooling linked to early flow across the Tasmanian Gateway

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

Volumn 110, Issue 24, 2013, Pages 9645-9650

  Bijl, Peter K ^a   Bendle, James A P ^b,m   Bohaty, Steven M ^c   Pross, Jörg ^d,e   Schouten, Stefan ^f   Tauxe, Lisa ^g   Stickley, Catherine E ^h   McKay, Robert M ⁱ   Roḧl, Ursula ^j   Olney, Matthew ^k   Sluijs, Appy ^a   Escutia, Carlota ^l   Brinkhuis, Henk ^a,f  

^a UTRECHT UNIVERSITY   (Netherlands)

^b UNIVERSITY OF GLASGOW   (United Kingdom)

^c UNIVERSITY OF SOUTHAMPTON   (United Kingdom)

^d GOETHE UNIVERSITY   (Germany)

^e BIODIVERSITY AND CLIMATE RESEARCH CENTRE BIK F   (Germany)

^f ROYAL NETHERLANDS INSTITUTE FOR SEA RESEARCH   (Netherlands)

^g UNIVERSITY OF CALIFORNIA   (United States)

^h UNIVERSITY OF TROMSØ   (Norway)

ⁱ VICTORIA UNIVERSITY OF WELLINGTON   (New Zealand)

^j UNIVERSITY OF BREMEN   (Germany)

^k UNIVERSITY OF SOUTH FLORIDA   (United States)

^l CSIC   (Spain)

^m UNIVERSITY OF BIRMINGHAM   (United Kingdom)

more..

Author keywords

Climate cooling; Dinoflagellate cysts; Organic palaeothermometry; Paleoceanography

Indexed keywords

SURFACE WATER;

ANTARCTICA; ARTICLE; CLIMATE; COOLING; ENVIRONMENTAL TEMPERATURE; EOCENE; PRIORITY JOURNAL; WATER FLOW; WATER TEMPERATURE;

DINOPHYCEAE;

EID: 84878972142     PISSN: 00278424     EISSN: 10916490     Source Type: Journal    
DOI: 10.1073/pnas.1220872110     Document Type: Article

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