Wara, M. W. et al. (2003): Possible roles of pH, temperature, and partial dissolution in determining boron concentration and isotopic composition in planktonic foraminifera
Leg/Site/Hole:
Related Expeditions:
ODP 130
Identifier:
ID:
2007-019633
Type:
georefid
ID:
10.1029/2002PA000797
Type:
doi
Creator:
Name:
Wara, M. W.
Affiliation:
University of California at Santa Cruz, Department of Ocean Sciences, Santa Cruz, CA, United States
Role:
author
Name:
Delaney, M. L.
Affiliation:
U. S. Geological Survey, United States
Role:
author
Name:
Bullen, T. D.
Affiliation:
Role:
author
Name:
Ravelo, A. C.
Affiliation:
Role:
author
Identification:
Title:
Possible roles of pH, temperature, and partial dissolution in determining boron concentration and isotopic composition in planktonic foraminifera
Year:
2003
Source:
Paleoceanography
Publisher:
American Geophysical Union, Washington, DC, United States
Volume:
18
Issue:
4
Pages:
Abstract:
Language:
English
Genre:
Serial
Rights:
URL:
Coverage: Geographic coordinates: North:0.1907 West:159.2140 East:
159.2142 South:0.1906
Keywords: Stratigraphy; alkaline earth metals; alkalinity; B-11/B-10; boron; calcification; calcite; calcium; carbon dioxide; carbonates; Cenozoic; concentration; cores; dissolved materials; Equatorial Pacific; Foraminifera; geochemistry; Globogerinoides sacculifer; Invertebrata; isotope ratios; isotopes; Leg 130; magnesium; metals; microfossils; Neogene; O-18/O-16; Ocean Drilling Program; ODP Site 806; oxygen; Pacific Ocean; paleo-oceanography; paleoatmosphere; paleotemperature; pH; planktonic taxa; Pliocene; Protista; Quaternary; sea water; solubility; stable isotopes; temperature; Tertiary; trace elements;
.