Radiocarbon age differences between coexisting foraminiferal species

Paleoceanography

Volumn 14, Issue 4, 1999, Pages 431-436

  Broecker, Wallace ^a   Matsumoto, Katsumi ^a   Clark, Elizabeth ^a   Hajdas, Irka ^b   Bonani, Georges ^b  

^a Department of Earth and Environmental Sciences   (United States)

^b ETH ZURICH   (Switzerland)

Author keywords

[No Author keywords available]

Indexed keywords

DEEP-SEA SEDIMENT; FORAMINIFERA; QUATERNARY; RADIOCARBON DATING;

ATLANTIC OCEAN; CEARA RISE;

GLOBOROTALIA MENARDII; PULLENIATINA OBLIQUILOCULATA;

EID: 0033394423     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999PA900019     Document Type: Article

References (5)

1. 14C ages measured in planktonic foraminifera: Paleoceanographic implications, Paleoceanography, 3, 635-645, 1988.
2. Broecker, W. S., T.-H. Peng, S. Trumbore, G. Bonani, and W. Wolfli, The distribution of radiocarbon in the glacial ocean, Global Biogeochem. Cycles, 4, 103-117, 1990.
3. 3 preservation event, Paleoceanography, 8, 333-339, 1993.
4. Peng, T.-H., and W. S. Broecker, The impacts of bioturbation on the age difference between benthic and planktonic foraminifera in deep sea sediments, Nucl, Instrum. Methods Phys. Res., B5, 346-352, 1984.
5. Richardson, D. S., The origin of iron-rich layers in sediments of the western equatorial Atlantic Ocean, Ph.D. thesis, Fac. of Pure Sci., Columbia Univ., New York, 1974.