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Mg-Ca, B-Ca and U-Ca in shells of benthic foraminifers

tracers of temperature and seawater carbonate chemistry

Raitzsch, Markus
2008
Univ. Bremen
Monography
Verlagsversion
Englisch
DOI: https://doi.org/10.23689/fidgeo-183
Raitzsch, Markus, 2008: Mg-Ca, B-Ca and U-Ca in shells of benthic foraminifers - tracers of temperature and seawater carbonate chemistry. Univ. Bremen, 88 S., DOI: 10.23689/fidgeo-183.
 
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  • Abstract
Mg/Ca ratios in benthic foraminiferal shells are frequently used in paleoceanographic studies to estimate past bottom water temperatures. Apart from temperature, other factors may exert additional influences on foraminiferal Mg/Ca. These include the Mg/Ca ratio of seawater, partial dissolution of shell calcite, salinity, physiological effects, and, probably of capital importance, the carbonate chemistry of seawater. In this context, the seperate effects of temperature and seawater carbonate chemistry on the magnesium incorporation into benthic foraminideral calcite are unraveled and quantified in this thesis...
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  • Paläontologie, Geobiologie [311]
Subjects:
Protozoa {Paläozoologie}
Geochemie der Fauna
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