Robinson, Rebecca S. and Meyers, Philip A. (2002): Biogeochemical changes within the Benguela Current upwelling system during the Matuyama diatom maximum; nitrogen isotope evidence from Ocean Drilling Program sites 1082 and 1084

Leg/Site/Hole:
ODP 175
ODP 175 1082
ODP 175 1084
Identifier:
2003-069537
georefid

10.1029/2001PA000659
doi

Creator:
Robinson, Rebecca S.
University of Michigan, Department of Geological Sciences, Ann Arbor, MI, United States
author

Meyers, Philip A.
author

Identification:
Biogeochemical changes within the Benguela Current upwelling system during the Matuyama diatom maximum; nitrogen isotope evidence from Ocean Drilling Program sites 1082 and 1084
2002
Paleoceanography
American Geophysical Union, Washington, DC, United States
17
4
The Matuyama Diatom Maximum (MDM) is a time of peak opal accumulation from 2.6 to 2.0 Ma within the Benguela Current upwelling system that was initiated by increased influence of Southern Ocean water on the eastern South Atlantic. This study measured opal, total organic carbon (TOC), and CaCO (sub 3) fluxes and C and N stable isotopes in sediments deposited from 2.4 to 1.95 Ma at Sites 1082 and 1084 to explore the biogeochemical dynamics within the Benguela region. The infusion of Southern Ocean water delivered dissolved nutrients and Southern Ocean flora and fauna. The bulk sediment (super 15) N records are taken to reflect changes in the (super 15) N of nitrate in the incoming water, where lower values at 2.4 Ma reflect less nitrate utilization in the Antarctic. (modified journ. abst.)
English
Coverage:Geographic coordinates:
North:75.0000
West:-180.0000East: 180.0000
South:-90.0000

Stratigraphy; Isotope geochemistry; algae; Atlantic Ocean; Benguela Current; biogenic processes; Cenozoic; diatoms; framework silicates; geochemistry; hydrochemistry; isotope ratios; isotopes; Leg 175; Matuyama Chron; microfossils; N-15/N-14; Neogene; nitrogen; Ocean Drilling Program; ODP Site 1082; ODP Site 1084; opal; organic compounds; paleo-oceanography; paleocirculation; paleocurrents; Plantae; Pliocene; sea water; silica minerals; silicates; South Atlantic; Southern Ocean; stable isotopes; Tertiary; total organic carbon; upper Cenozoic;

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