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Lake and Marine Paleoseismology - Paleoecology - Multivariate Statistics - Geochronology

I use a wide variety of analytical and statistical methods to disentangle complex sedimentary records to differentiate between influences - such as earthquakes and climate - on lake and marine sediments. To do this, I use high-resolution, non-destructive methods such as micro-Xray fluorescence, computed tomography (CT density), along with petrophysical property data (magnetic susceptibility and gamma ray density), laser diffraction particle size, X-ray diffraction, and microscopic smear slide composition to characterize sediment. I have experience modeling radiocarbon and other age data, and have used multivariate statistics and ecological transfer functions to infer past environments from microfossil assemblages preserved in the sedimentary record.

NEW! Video Clip by J. Anderson, Terramar Productions: