Deep sea corals off Brazil verify a poorly ventilated Southern Pacific Ocean during H2, H1 and the Younger Dryas

Earth and Planetary Science Letters

Volumn 293, Issue 3-4, 2010, Pages 269-276

  Mangini, A ^a   Godoy, J M ^b   Godoy, M L ^b   Kowsmann, R ^c   Santos, G M ^d   Ruckelshausen, M ^a   Schroeder Ritzrau, A ^a   Wacker, L ^e  

^a HEIDELBERG ACADEMY OF SCIENCES AND HUMANITIES   (Germany)

^b INSTITUTO DE RADIOPROTEÇÃO E DOSIMETRIA   (Brazil)

^c PETROBRAS   (Brazil)

^d UNIVERSITY OF CALIFORNIA   (United States)

^e ETH ZURICH   (Switzerland)

Author keywords

14C; Deep sea corals; Heinrich events; Mystery Interval; Ocean circulation; Ocean ventilation

Indexed keywords

ACTIVITY RATIOS; ANTARCTIC INTERMEDIATE WATERS; ATLANTIC OCEAN; CALIFORNIA; DEEP SEA; DEEP-OCEAN CIRCULATION; EASTERN PACIFIC; GAS EXCHANGE; HEINRICH EVENTS; NORTH ATLANTIC DEEP WATER FORMATIONS; OCEAN CIRCULATION; PACIFIC OCEAN; SEDIMENT CORE; YOUNGER DRYAS;

SEDIMENTOLOGY; VENTILATION;

OCEANOGRAPHY;

CORAL; DEEP WATER VENTILATION; GAS EXCHANGE; HEINRICH EVENT; MARINE SEDIMENT; OCEANIC CIRCULATION; PALEOCEANOGRAPHY; RADIOCARBON DATING; SEDIMENT CORE; URANIUM SERIES DATING; YOUNGER DRYAS;

BRAZIL; PACIFIC OCEAN; PACIFIC OCEAN (SOUTH);

ANTHOZOA; CITRUS MAXIMA;

EID: 77951621885     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2010.02.041     Document Type: Article

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