Biogeochemistry sulfur

Biogeochemistry- Study of microbially mediated chemical transformations of geochemical interest, such as nitrogen or sulfur cycling. 

Bruchert V, Knoblauch C, Jorgensen BB (2001) Controls on stable sulfur isotope fractionation during bacterial sulfate reduction in Arctic sediments. Geochim Cosmochim Acta 65 763-776 Bryan BA, Shearer G, Skeeters JL, Kohl DH (1983) Variable expression of the nitrogen isotope effect associated with denitrification of nitrate. J Biol Chem 258 8613-8617 Canfield DE (2001) Biogeochemistry of sulfur isotopes. Rev Mineral Geochem 43 607-636 Chau YK, Riley JP (1965) The determination of selenium in sea water, silicates, and marine organisms. Anal Chim Acta 33 36-49... 

Jensen ML, Nakai N (1962) Sulfur isotope meteorite standards, results and recommendations. In Jensen ML (ed) Biogeochemistry of sulfur isotopes, NSE Symp Vol, p 31 Jia Y (2006) Nitrogen isotope fractionations during progressive metamorphism a case study from the Paleozoic Cooma metasedimentary complex, southeastern Australia, Geochim Cosmochim Acta 70 5201-5214... 

Schindler, J.E., D.J. Williams, and A.P. Zimmerman. 1976. Investigation of extracellular electron transport by humic acids. In J.O. Nriagu, ed., Environmental Biogeochemistry, Vol. 1. Carbon, Nitrogen, Phosphorus, Sulfur, and Selenium Cycles, pp. 109-115, Ann Arbor Science Ann Arbor. 

Mopper, K., and D. J. Kieber. 2002. Impact of DOM photochemistry on the biogeochemical cycling of carbon, nitrogen, sulfur and phosphorus in the sea. In Biogeochemistry of Marine Dissolved Organic Matter (D. Hansell and C. A. Carlson, Eds.), pp. 455-489 Academic Press, New York. 

It is also possible that bacterial decomposition of sulfur containing organic compounds may account for some DMS in natural waters (31-36). Conversely, bacteria may also utilize DMS and therefore act as a sink (37-39). The contribution of bacterial processes to the DMS/DMSP cycle in open ocean environments has not been addressed and is as yet not understood. However, studies to better understand the biogeochemistry of DMS can not exclude bacterial processes (e.g. 4041). 

Rafter, T. A. In Biogeochemistry of Sulfur Isotopes Jensen, M. L., Ed. Proc. National Science Foundation Symposium, Yale University, New Haven 1962 pp 42-60. 

Bottcher, M.E., and Lepland, A. (2000) Biogeochemistry of sulfur in a sediment core from the west-central Baltic Sea evidence from stable isotopes and pyrite textures. J. Mar. Syst. 25, 299-312. 

Howarth, R.W. (1984) The ecological significance of sulfur in the energy dynamics of salt marsh and coastal sediments. Biogeochemistry 1, 5-27. 

Roden, E.E., and Tuttle, J.H. (1993b) Inorganic sulfur turnover in oligohaline estuarine sediments. Biogeochemistry 22, 81-105. 

Sciare, J., Mihalopoulos, N., and Nguyen, B.C. (2002) Spatial and temporal variability of dissolved sulfur compounds in European estuaries. Biogeochemistry 59, 121-141. 

Zopfi J, Ferdelman TG, Fossing H (2004) Distribution and fate of sulfur intermediates - sulfite, tetrathionate, thiosulfate, and elemental sulfur - in marine sediments. In Amend JP, Edwards KJ, Lyons TW (eds) Sulfur biogeochemistry - past and present. Geological Society of America special paper 379, p 97... 

Jensen, M. L. Biogeochemistry of sulfur isotopes, 193 pp. Proc. of a Nat. Science Found. Symp. New Haven, Conn. Yale Univ. 1962. 

Turner, S. M., Harvey, M. J., Law, C. S., Nightingale, P. D. Liss, P. S. (2004). Iron-induced changes in oceanic sulfur biogeochemistry. Geophysical Research Letters, 31,... 

Mopper, K., and Kieber, D. J. (2002). Photochemistry and the cycling of carbon, sulfur, nitrogen and phosphorus. Biogeochemistry of marine dissolved organic matter (HanseU, Carlson, eds.). Academic Press, Amsterdam. 

Holmer, M., Duarte, C. M., and Marba, N. (2003). Sulfur cycling and seagrass Posidonia oceanica) status in carbonate sediments. Biogeochemistry 66, 223—239. 

Solute isotope biogeochemistry focuses on isotopes of constituents that are dissolved in the water or are carried in the gas phase. The most commonly studied solute isotopes are the isotopes of carbon, nitrogen, and sulfur. Less commonly investigated stable, nonradiogenic isotopes include lithium, chloride, boron, and iron. 

Mitchell M. J., Krouse H. R., Mayer B., Stam A. C., and Zhang Y. (1998) Use of stable isotopes in evaluating sulfur biogeochemistry of forest ecosystems. In Isotope Tracers in Catchment Hydrology (eds. C. Kendall and J. J. McDonnell). Elsevier, Amsterdam, pp. 489—518. 

Berner R. A. (1962) Experimental smdies of the formation of sedimentary iron sulfides. In Biogeochemistry of Sulfur Isotopes Symposium (ed. M. LeRoy), Yale University, New Haven. 

Nissenbaum A. and Kaplan I. R. (1976) Sulfur and carbon isotopic evidence for biogeochemical processes in the Dead Sea ecosystem. In Environmental Biogeochemistry Carbon, Nitrogen, Phosphorus, Sulfur and Selenium Cycles (ed. J. O. Nriagu). Ann Arbor Sci. Publ, Ann Arbor, vol. 1, pp. 309-325. 

Ohmoto H. (1992) Biogeochemistry of sulfur and the mechanisms of sulfide-sulfate minerahzation in Archean oceans. In Early Organic Evolution Implications for Mineral and Energy Resources (eds. M. Schidlowdd, S. Golubic, M. M. Kimberly, and P. A. Trudinger). Springer, Berlin. 

Schouten S., De Loureiro M. R. B., Sinninghe Damste J. S., and de Leeuw J. W. (2001a) Molecular biogeochemistry of Monterey sediments, Naples Beach, California I. Distributions of hydrocarbons and organic sulfur compounds. In The Monterey Formation from Rocks to Molecules (eds. C. M. Isaacs and J. Rullkotter). Columbia University Press, New York, pp. 150-174. 

Dornblaser M., Giblin A. E., Fry B., and Peterson B. J. (1994) Effects of sulfate concentration in the overlying water on sulfate reduction and sulfur storage in lake sediments. Biogeochemistry 2A, 129-144. 

Kelly D. P. and Smith N. A. (1990) Organic sulfur compounds in the environment biogeochemistry, microbiology, and ecological aspects. Adv. Microb. Ecol. 11, 345-385. 

Visscher P. T. and Van Gemerden H. (1993) Sulfur cycling in laminated marine ecosystems. In Biogeochemistry of Global Change Radiatively Active Trace Gases (ed. R. S. Oremland). Chapman and Hall, New York, pp. 672-693. 

Wieder R. K. and Lang G. E. (1988) Cycling of inorganic and organic sulfur in peat from Big Run Bog, West Virginia. Biogeochemistry 5, 221-242. 

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