Cara Thompson

Kah, L.C., Thompson, C.K., Henderson, M.A., Zhan, R., in press. Behavior of Marine Sulfur in the Ordovician. Palaeogeography, Palaeoclimatology, Palaeoecology.

Thompson, C.K., Kah, L.C., 2012. Sulfur isotope evidence for widespread euxinia and fluctuating oxycline in the Early to Middle Ordovician greenhouse ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 313-314, 189-214.

Thompson, C.K., Kah, L.C., Astini, R., Bowring, S.A., Buchwaldt, R., 2012. Bentonite geochronology, marine geochemistry, and the Great Ordovician Biodiversification Event (GOBE). Palaeogeography, Palaeoclimatology, Palaeoecology 321-322, 88-101.

Thompson, C.K., Kah, L.C., Kaufman, A.J., in preparation. Sulphur isotopes mark end of Ordovician greenhouse climate in Darriwilian. Nature Geoscience.

Thompson, C.K., 2011. Carbon and sulfur cycling in early Paleozoic oceans. University of Tennessee, Ph.D. Dissertation.

Thompson, C.K., 2005. High-temperature, high-pressure HDAC study of the Mg-carbonate mineral, nesquehonite: University of Tennessee, M.S. Thesis.