Assoc. Prof. Dr. David Andrew Fike
Earth
Washington University in St. Louis, USA
May 2012
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Aug 2012
Fellow
Feb 2011
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Aug 2011
Fellow

Projects & Publications
Scale-Depending Coupling of Microbial-Geochemical Sulfur Cycling
| Feb 2011
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Aug 2012
Cooperation partner
Prof. Dr. Wolfgang Bach, Universität Bremen
Dr. Timothy Ferdelman, Max-Planck-Institut für Marine Mikrobiologie, Bremen
Publications
Finnegan S., Fike D. A., Jones D., and Fischer W. W. (2012). A Temperature-Dependent Positive Feedback on the Magnitude of Carbon Isotope Excursions. Geoscience Canada, 139, 122-131. https://www.erudit.org/en/journals/geocan/2012-v39-n3-geocan39_3/geocan39_3pfh01/
Paul Gorjan, Kunio Kaiho, David A. Fike, Chen Xu (2012). Carbon- and sulfur-isotope geochemistry of the Hirnantian (Late Ordovician) Wangjiawan (Riverside) section, South China: Global correlation and environmental event interpretation. Palaeogeography, Palaeoclimatology, Palaeoecology, 337–338, 14-22. https://doi.org/10.1016/j.palaeo.2012.03.021
Jones, D. S. and Fike, D. A. (2013). Dynamic sulfur and carbon cycling through the end-Ordovician extinction revealed by paired sulfate–pyrite δ34S. Earth and Planetary Science Letters, 363, 144-155. https://doi.org/10.1016/j.epsl.2012.12.015
Grotzinger, J., Fike, D. & Fischer, W. (2011). Enigmatic origin of the largest-known carbon isotope excursion in Earth's history. Nature Geoscience, 4, 285–292. https://doi.org/10.1038/ngeo1138
Megan Rohrssen, Gordon D. Love, Woodward Fischer, Seth Finnegan, David A. Fike (2013). Lipid biomarkers record fundamental changes in the microbial community structure of tropical seas during the Late Ordovician Hirnantian glaciation. Geology, 41 (2), 127–130. https://doi.org/10.1130/G33671.1
Metzger J. G. and Fike D. A. (2013). Techniques for assessing spatial heterogeneity of carbonate d13C values: Implications for craton-wide isotope gradients. Sedimentology, 60 (6), 1405-1431. https://doi.org/10.1111/sed.12033