Emmanuel, Laurent et al. (2004): Trace element geochemistry of Cenozoic cool-water carbonates, Sites 1126-1132, Great Australian Bight

Leg/Site/Hole:
ODP 182
Identifier:
2005-041676
georefid
10.2973/odp.proc.sr.182.008.2002
doi
Creator:
Emmanuel, Laurent
Universite de Bourgogne, Centre des Sciences de la Terre, Dijon, France
author
Robin, Cecile
Australian Geological Survey Organisation, Australia
author
Renard, Maurice
Texas A&M University, United States
author
Identification:
Trace element geochemistry of Cenozoic cool-water carbonates, Sites 1126-1132, Great Australian Bight
2004
In: Hine, Albert C., Feary, David A., Malone, Mitchell J., Andres, Miriam, Betzler, Christian, Brooks, Gregg R., Brunner, Charlotte A., Fuller, Michael, Molina Garza, Roberto S., Holbourn, Ann E., Huuse, Mads, Isern, Alexandra R., James, Noel P., Ladner, Bryan C., Li, Qianyu, Machiyama, Hideaki, Mallinson, David J., Matsuda, Hiroki, Mitterer, Richard M., Robin, Cecile, Russell, Joellen L., Shafik, Samir, Simo, J. A., Smart, Peter L., Spence, Guy H., Surlyk, Finn C., Swart, Peter K., Wortmann, Ulrich G., Proceedings of the Ocean Drilling Program; scientific results; Great Australian Bight; Cenozoic cool-water carbonates; covering Leg 182 of the cruises of the drilling vessel JOIDES Resolution; Wellington, New Zealand, to Fremantle, Australia; Sites 1126-1134, 8 October-7 December 1998
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
182
An intensive geochemical investigation was conducted on carbonate sediments recovered during Ocean Drilling Program Leg 182. Four trace elements in 635 sediment samples from Sites 1126-1132 on the Great Australian Bight were examined by atomic absorption spectrometry on the acid-soluble fraction. Downhole profiles of these elements exhibit complicated fluctuations throughout the late Eocene to Pleistocene, principally because of the variations in the acid-soluble fraction. The purpose of this study is to present initial results on the geochemical composition of Cenozoic cool-water carbonates as a basis for a future detailed investigation to determine the paleoenvironment of a carbonate-dominated continental margin during the evolution of the Southern Ocean.
English
Serial
Coverage:Geographic coordinates:
North:-33.1720
West:127.1500East: 128.5500
South:-34.2330
Geochemistry of rocks, soils, and sediments; Oceanography; algae; atomic absorption spectra; Australasia; Australia; biostratigraphy; biozones; carbonate sediments; carbonates; Cenozoic; cores; Foraminifera; geochemistry; Great Australian Bight; Indian Ocean; Invertebrata; Leg 182; lithostratigraphy; marine sediments; microfossils; nannofossils; Ocean Drilling Program; ocean floors; paleoenvironment; Plantae; Protista; sediments; spectra; trace elements;
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