As a postdoctoral researcher, I have expanded my research direction to include questions at the intersection of climate and life. I am using triple oxygen isotopes and stable carbon isotopes of biominerals (specifically, tooth enamel carbonate and eggshell carbonate) to address these questions.
An important first step toward robust paleoclimate and paleoecological interpretation is developing robust analytical and sample preparation methodologies. In my first project at Yale, I tested the effects of chemical pretreatments on the triple oxygen isotope composition of modern and fossil biomineral samples (Katz et al., 2026). This work will serve as a guide to practitioners as they select sample pretreatment methodologies and set standards for reporting pretreatment methodologies in future studies.
My other postdoc projects are applied research addressing paleoclimate and paleoecology questions. I'm especially interested in how climate affects terrestrial environments (from a landscape, vegetation, and water perspective), and how animals adapt or go extinct as a result of these ecological pressures. These interconnections have guided the trajectory of my active postdoc research program, and I hope to continue exploring this theme in the future. Currently I am leading active projects in Texas during the Late Quaternary (Katz et al., in prep), Africa during the Holocene, and Florida from the Miocene to recent. Check back soon for additional updates!
Related publications:
Katz, S.A., Bertacchi, A., Yarian, D.A., Wostbrock, J.A.G., (2026) "Carbonate triple oxygen and carbon isotope effects of chemical pretreatments on tooth enamel and eggshell." Chemical Geology (10.1016/j.chemgeo.2026.123551).
Katz, S.A., Koch, P.L., Yarian, D.A., and Wostbrock, J.A.G. (in prep) “Diminished dietary and water use niche space of North American herbivores following the Late Quaternary megafauna extinctions.” Expected submission late summer 2026.
More detailed descriptions of these projects are included below.
In this exciting new work, we are employing triple oxygen isotopes of tooth enamel from fossil localities in northcentral Texas to test the hypothesis that decreasing access to surface water during the Last Glacial termination contributed to North America's megagfaunal extinctions.
We expect this manuscript to be submitted close to the end of summer 2026, so I hope to share more details about this project soon.
White tailed deer tooth from the Dallas, Texas region sampled at the SMU Shuler Museum of Paleontology.
TILDAS instrument used to make carbon and triple oxygen isotope measurements at the Yale DELTA Lab (Wostbrock Lab).
Triple oxygen isotope analysis of biominerals (e.g., tooth enamel, eggshell calcite) has rapidly expanded in the past decade. However, despite knowing that common chemical pretreatments can affect sample mineralogy, mineral structure, and carbon and oxygen isotope values, we lack information about the potential effect(s) of chemical pretreatments on biomineral triple oxygen isotope values. In this work, we applied common chemical pretreatments to a suite of modern and fossil biomineral samples to provide researchers within important and timely information about pretreatment effects on sample mineral structure and isotope values. This work is published in Chemical Geology (DOI: 10.1016/j.chemgeo.2026.123551)