The DOI matches its Crossref record; 118 of the 118 references it cites were found in a registry or an index.
The Source of Ions for Biomineralization in Foraminifera and Their Implications for Paleoceanographic Proxies
Abstract
The global carbon cycle is strongly perturbed by fossil fuel burning leading to atmospheric CO2 increase. Climatic warming followed by polar ice melting and global sea level rise are predicted due to the greenhouse effect of increasing CO2 in the atmosphere (Houghton et al. 1995). The ocean plays a major role in neutralizing the excess CO2 because the amount of inorganic carbon available for exchange with the atmosphere in the ocean is approximately 50–60 times larger than in the atmosphere (e.g., Siegenthaler and Sarmiento 1993). The bulk of the atmospheric CO2 excess will eventually be neutralized by CaCO3 dissolution in the deep marine environment. This is, however, is a relatively slow process that operates on the time scale of ocean circulation (1000 yrs) and is therefore causing an accumulation of CO2 in the atmosphere. This phenomenon will result in potentially severe consequences to the well being of global ecological systems. Obviously the scientific attention of many biogeochemists is focused on processes controlling the response of the marine system to changes in atmospheric CO2 concentrations (e.g., Archer and Maier-Reimer 1994; Broecker 1997; Sigman and Boyle 2000; Berger 2002).
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Cites
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Cited by
An Overview of Biomineralization Processes and the Problem of the Vital Effect
Weiner, S. (2003) · Reviews in Mineralogy and Geochemistry · doi:10.2113/0540001 · Cited by 1,022
Obst, M., Dynes, J. J., Lawrence, J. R., Swerhone, G. D. W., Benzerara, K., Karunakaran, C., Kaznatcheev, K., Tyliszczak, T., & Hitchcock, A. P. (2009) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2009.04.013 · Cited by 304
Sr2+/Ca2+ and 44Ca/40Ca fractionation during inorganic calcite formation: II. Ca isotopes
Tang, J., Dietzel, M., Böhm, F., Köhler, S. J., & Eisenhauer, A. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2008.05.033 · Cited by 301
Chapter Six Planktonic Foraminifera as Tracers of Past Oceanic Environments
Kucera, M. (2007) · Developments in Marine Geology · doi:10.1016/s1572-5480(07)01011-1 · Cited by 277
Carbonate clumped isotope compositions of modern marine mollusk and brachiopod shells
Henkes, G. A., Passey, B. H., Wanamaker, A. D., Grossman, E. L., Ambrose, W. G., & Carroll, M. L. (2013) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.12.020 · Cited by 264
Metadata
- Authors
- Erez, J.
- Venue
- Reviews in Mineralogy and Geochemistry
- Publisher
- Mineralogical Society of America
- Published
- 2003-01-01
- Volume
- 54
- Issue
- 1
- Pages
- 115-149
- ISSN
- 1529-6466 (ISSN-L)
- OpenAlex
- W2086782132
- Cited by
- 555
- References
- 118
- FWCI
- 7.51
- Type
- journal article
- Language
- en
- Open access
- closed
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- Erez, J. (2003). The Source of Ions for Biomineralization in Foraminifera and Their Implications for Paleoceanographic Proxies. Reviews in Mineralogy and Geochemistry. https://doi.org/10.2113/0540115
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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