Greg Ludvigson, Kansas Geological Survey, Lawrence, Kansas
Q. What’s your research?
A. I work on the Mesozoic and Cenozoic terrestrial paleoclimatology of stacks of paleosols in the clastic deposits filling continental sedimentary basins. I do this using petrographic and stable isotope techniques to investigate the diagenesis and paleohydrology of terrestrial carbonates. A lot of effort in recent years has been devoted to improvements in chronostratigraphic resolution using carbon isotope chemostratigraphy and collaborative efforts with U-Pb geochronologists.
Q. Where is your favorite field area (and why?)?
A. I keep going back over and over again to the San Rafael desert in eastern Utah to investigate the paleopedology, paleoclimatology, and chronostratigraphy of the Early Cretaceous Cedar Mountain Formation. This work has been carried out in concert with a group of colleagues and students who are similarly drawn to this awesome landscape and set of allied scientific questions.
Q. What do you enjoy about serving as JSR AE?
A. Just from having been around long enough, I can quickly think of appropriate peer reviewers to tap in case the author’s suggested reviewers don’t work out. In those instances, that helps me accelerate the peer review process for the journal. My term has been long enough to get a good sense of the wide range in the quality of submitted manuscripts, and that has helped me to quicken the pace of making recommendations to the Editors. I have really enjoyed having the chance to monitor new developments in the field of sedimentary geology through AE service to JSR.
Q. What was your favorite JSR paper from “back in the day” (or a recent year)?
A. I think back to my early years as a Ph.D student, and the impact that Robert Berner’s 1981 paper “A New Geochemical Classification of Sedimentary Environments” (JSP, v. 51, no. 2, p. 359-365) had on me at the time. It was a simple, elegant paper that pulled together a framework on how to interpret the presence of redox-sensitive authigenic minerals, and what they indicated about depositional environments. I read that paper at just the right time to begin collating my own field experiences and develop a world view on how redox processes are encoded in the sedimentary rock record.
Q. What are your hobbies?
A. I plant trees. I live on a rural acreage with a lot of space, meaning that my long-standing impulse toward therapeutic silviculture is not very well constrained. I am tending to an embarrassingly large number of sapling trees, and I enjoy making daily to weekly visits to see how they are doing. They live in slow-motion time scales relative to our daily human experiences, but if you look closely, they offer lots of clues.
Q. What’s on your favorite Pandora station?
A. I let my involvement with Pandora lapse some time ago. I am drawn to American Roots and folk music, and my exposure to new material in this genre comes from listening to local NPR affiliates on FM radio. Pretty old school, I know.