I research the influence of external climate drivers and boundary conditions on regional ecosystems and hydroclimate. I am interested in how human responses to temporal and spatial environmental variations in the past can inform our understanding of the sensitivity of vulnerable regions to modern global warming. My work has focused primarily on Africa, where many regions are highly water- and resource-stressed according to the IPCC, yet the continent is historically under-studied and we lack full understanding of environmental sensitivity to natural and human-induced climate changes. Understanding past climate change and natural oscillations will provide further characterization of vulnerability to a changing world. Additionally, increasingly more hominin fossil and archaeological finds constrain the history of our human ancestors, but comparisons of evolutionary change with the human environment remains poorly understood due to the lack of high-resolution, geochemical climate and vegetation records.
I utilize the novel geochemical proxies of leaf wax biomarker hydrogen and carbon isotopes to quantitatively reproduce past hydroclimate and vegetation. Plants produce waxes to prevent evaporation from and physical damage to their leaves. Leaf waxes are hydrocarbon chains that incorporate a hydrogen isotopic signature from the water they use to photosynthesize, and thus reflect rainfall amount in the tropics. Carbon isotope signatures from the same leaf wax compounds are determined by the plant type, i.e. trees vs. grasses. These geochemical signals of climate are obtained by extracting the leaf waxes from sediment, performing liquid chromatography separations, and running isolated compounds on an isotope ratio mass spectrometer (IRMS) coupled to a gas chromatograph (GC) to measure the hydrogen and carbon isotope ratios. With these paleoclimate records of rainfall and environment, I perform time series and statistical analyses to understand how environments changed and what drove climate through the Oligocene, Miocene, Pliocene, and Pleistocene.
Hominin Sites and Paleolakes Drilling Project
My dissertation work was part of HSPDP, an international effort to use lacustrine deep drill cores to reconstruct Plio-Pleistocene climate and answer pressing questions on the role of environmental change in driving human evolution. Lead by both paleoclimatologists and paleoanthropologists, the project successfully obtained six cores from East African basins famous for hominin fossils and archaeological artifacts.
As a member of the organic geochemistry team in HSPDP, I worked to produce leaf wax biomarker hydrogen and carbon isotope records from many of these lake cores. I have studied everything from long term million-year climate trends, to millennial-scale hydroclimate fluctuation. I implemented time series analysis tools to pick up statistically significant changes in environmental variability, periodicity, and trend, linking East African climate to global-scale climate transitions. I currently have one paper published, two in review, and two in preparation that have come out of my dissertation work. Please view my CV or contact me with any questions or to request the PDF.
In addition to the biomarker isotope work as part of HSPDP, I have aided in the production of age models, time series analyses of grain size and other lithological indicators, and GDGT work.
North African Climate from ODP 966/967 Sapropels
Sapropels are dark, organic-rich layers in sediment that form in the Mediterranean Sea when intense North African rainfall flows from the Nile River basin and provides a freshwater cap to limit oxygenation of the deep sea. These layers have been used in astrochronological reconstructions to demonstrate their faithful response to precession and eccentricity cycles. Dr. Cassy Rose demonstrated that measuring leaf wax isotopes preserved in the ODP 966 and 967 cores from the Eastern Mediterranean Sea was a wonderful technique to quantify past climate to understand the strength of precession minima and maxima.
For my postdoc in the same laboratory, I will be measuring the hydrogen and carbon isotopic makeup of leaf waxes from each of the sapropel layers over the past ~4.5 million years. This, along with a precise astronomically-tuned age model, will allow us to better understand long term climate change, as well as eccentricity’s role in amplifying precession-driven monsoon systems.