THOMAS F. ANDERSON

Professor
Ph.D., Columbia University, 1967
Low-Temperature Geochemistry, Stable Isotope Geochemistry


The focus of Dr. Anderson's research is geochemical processes in sediment-water systems and the application of stable isotope variations to investigating those processes and systems. He is particularly interested in (1) the biogeochemical cycle of sulfur, (2) paleo-climatic and paleo-oceanographic reconstructions, (3) diagenetic reactions in carbonate rocks and sediments, and (4) the geochemistry of groundwaters. He and his students collaborate with researchers at several institutions in the United States and Great Britain.

More Research


Selected Recent Publications

Hudson, J. D., and T. F. Anderson. 1989. Ocean temperatures and isotopic compositions through time. Transactions of the Royal Society of Edinburgh 80: 183-192.

Woo, K. S., T. F. Anderson, L. B. Railsback, and P. A. Sandberg. 1993. Oxygen isotopic evidence for high-salinity surface seawater in the Mid-Cretaceous Gulf of Mexico: Implications for warm, saline deepwater formation. Paleoceanography 7: 673-685.

Anderson, T. F., B. N. Popp, A. C. Williams, L. Z. Ho, and J. D. Hudson. 1994. The stable isotopic records of fossils from the Peterborough Member, Oxford Clay Formation (Middle Jurassic): Palaeoenvironmental implications. Journal of the Geological Society 151: 125-138.

Anderson, T. F. and L. M. Pratt. 1995. Isotopic evidence for the origin of organic sulfur and elemental sulfur in marine sediments. In: Geochemical Transformations of Sedimentary Sulfur (M. A. Vairavamurthy and M. A. A. Schoonen, eds.), American Chemical Society Symposium (in press).

Bruchert, V., L. M. Pratt, T. F. Anderson, and S. R. Hoffmann. 1995. Abundance and isotopic composition of organic and inorganic sulfur species in laminated and bioturbated sediments at Hole 893A, Santa Barbara Basin. Proceedings of the Ocean Drilling Project, vol. 146 (in press).