Information for possible research collaboratorsBruce Railsback, Department of Geology, University of Georgia
In research projects using stalagmites as records of paleoclimate, my unique contribution is using the petrography of stalagmites to constrain and enrich interpretations of paleoclimate. Specifically, I look at variation in spelean minerals, detrital non-carbonate materials, crystal forms and fabrics, and layer relationships as evidence regarding environmental change. I further hopefully contribute by integrating those observations with isotopic and growth-rate data. Railsback, L. Bruce, Brook, George A., Chen, Jian, Kalin, Robert, and Fleisher, Christopher J., 1994, Environmental controls on the petrology of a Late Holocene speleothem from Botswana with annual layers of aragonite and calcite: Journal of Sedimentary Research, v. A64, p. 147-155. James W. Webster, George A. Brook, L. Bruce Railsback, Hai Cheng, R. Lawrence Edwards, Clark Alexander, and Philip P. Reeder, 2007, Stalagmite evidence from Belize indicating significant droughts at the time of Preclassic Abandonment, the Maya Hiatus, and the Classic Maya Collapse: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 250, p. 1-17. Railsback, L. Bruce, Fuyuan Liang, Juan Ramón Vidal Romaní, Aurora Grandal d'Anglade, Marcos Vaqueiro Rodríguez, Luisa Santos Fidalgo, Daniel Fernández Mosquera, Hai Cheng, and R. Lawrence Edwards, A stalagmite record of Holocene long-term climate change and shorter-term environmental shifts from the Serra do Courel of northwestern Spain: in revision for Palaeogeography, Palaeoclimatology, Palaeoecology. Last updated 15 February 2011.
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