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Foraminiferal dissolution at shallow depths of the Walvis Ridge and Rio Grande rise during the latest Cretaceous: Inferences for deep-water circulation in the South Atlantic
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
1997 (English)In: PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, ISSN 0031-0182, Vol. 129, no 3-4, 195-212 p.Article in journal (Refereed) Published
Abstract [en]

A high-resolution (10-20 kyr) record of variations in CaCO3 content and dissolution was established for latest Cretaceous (last 0.7 Myr) deep-sea sediments from the South Atlantic Ocean(DSDP Site 516 from the Rio Grande Rise, and sites 525 and 527 from th

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1997. Vol. 129, no 3-4, 195-212 p.
Keyword [en]
South Atlantic; Cretaceous; calcite; solution; foraminifera; upwelling; SEA DRILLING PROJECT; CARBONATE DISSOLUTION; TERTIARY BOUNDARY; PLANKTONIC-FORAMINIFERA; INDIAN-OCEAN; SEDIMENTS; LYSOCLINE; SITE-516; PATTERNS; LEG-72
Identifiers
URN: urn:nbn:se:uu:diva-27876OAI: oai:DiVA.org:uu-27876DiVA: diva2:55772
Note
Addresses: Kucera M, GOTHENBURG UNIV, CTR EARTH SCI, DEPT MARINE GEOL, S-41381 GOTHENBURG, SWEDEN. UNIV UPPSALA, INST EARTH SCI, DEPT HIST GEOL & PALAEONTOL, S-75236 UPPSALA, SWEDEN.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-15

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