Rosemarie Came
Research Interests
My primary area of research is paleoclimatology, with a specific interest in the forcings that initiate climate changes, and the mechanisms by which climatic signals propagate globally. To this end, I have investigated abrupt climate events of the recent geologic past (i.e., since the last glacial period), as well as the evolution of the Earth's climate over the last 600 million years.
My laboratory methods include foraminiferal trace and minor element geochemistry, and carbonate clumped isotope geochemistry. I am especially interested in the integration of paleoclimate data and model simulations, which is achieved through collaborations with climate modelers and dynamicists.
I am happy to speak with motivated prospective graduate students.
Courses Taught
- ESCI 409: Geology and the Environment
- ESCI 444: Honors/Phil of Earth Science
- ESCI 501: Introduction to Oceanography
- ESCI 514: Introduction to Climate
- ESCI 760: Paleoceanography
- ESCI 997: Seminar in Earth Sciences
Selected Publications
Came, R. E., Azmy, K., Tripati, A., & Olanipekun, B. -J. (2017). Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73–176 °C. Geochimica et Cosmochimica Acta, 199, 31-47. doi:10.1016/j.gca.2016.10.028
Brand, U., Blamey, N., Garbelli, C., Griesshaber, E., Posenato, R., Angiolini, L., . . . Came, R. (2016). Methane Hydrate: Killer cause of Earth's greatest mass extinction. Palaeoworld, 25(4), 496-507. doi:10.1016/j.palwor.2016.06.002
Brand, U., Came, R. E., Affek, H., Azmy, K., Mooi, R., & Layton, K. (2014). Climate-forced change in Hudson Bay seawater composition and temperature, Arctic Canada. Chemical Geology, 388, 78-86. doi:10.1016/j.chemgeo.2014.08.028
Came, R. E., Brand, U., & Affek, H. P. (2014). Clumped isotope signatures in modern brachiopod carbonate. Chemical Geology, 377, 20-30. doi:10.1016/j.chemgeo.2014.04.004
Brand, U., Azmy, K., Bitner, M. A., Logan, A., Zuschin, M., Came, R., & Ruggiero, E. (2013). Oxygen isotopes and MgCO3 in brachiopod calcite and a new paleotemperature equation. Chemical Geology, 359, 23-31. doi:10.1016/j.chemgeo.2013.09.014
Brand, U., Posenato, R., Came, R., Affek, H., Angiolini, L., Azmy, K., & Farabegoli, E. (2012). The end‐Permian mass extinction: A rapid volcanic CO2 and CH4‐climatic catastrophe. Chemical Geology, 322-323, 121-144. doi:10.1016/j.chemgeo.2012.06.015
Huntington, K. W., Eiler, J. M., Affek, H. P., Guo, W., Bonifacie, M., Yeung, L. Y., . . . Came, R. (2009). Methods and limitations of ‘clumped’ CO2isotope (Δ47) analysis by gas-source isotope ratio mass spectrometry. Journal of Mass Spectrometry, 44(9), 1318-1329. doi:10.1002/jms.1614
Carlson, A. E., Legrande, A. N., Oppo, D. W., Came, R. E., Schmidt, G. A., Anslow, F. S., . . . Obbink, E. A. (2008). Rapid early Holocene deglaciation of the Laurentide ice sheet. NATURE GEOSCIENCE, 1(9), 620-624. doi:10.1038/ngeo285
Came, R. E., Eiler, J. M., Veizer, J., Azmy, K., Brand, U., & Weidman, C. R. (2007). Coupling of surface temperatures and atmospheric CO2 concentrations during the Palaeozoic era. Nature, 449(7159), 198-201. doi:10.1038/nature06085
Came, R. E., Oppo, D. W., & McManus, J. F. (2007). Amplitude and timing of temperature and salinity variability in the subpolar North Atlantic over the past 10 k.y.. Geology, 35(4), 315. doi:10.1130/g23455a.1
Most Cited Publications