Environmental Internship Program - 2023 Booklet
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Rebecca Cho ’26<br />
GEOSCIENCES<br />
OCEANS AND<br />
ATMOSPHERE<br />
PROJECT TITLE<br />
Reconstructing the Marine<br />
<strong>Environmental</strong> Changes<br />
Across the Cretaceous-<br />
Paleogene Mass<br />
Extinction With Nitrogen<br />
Isotopes in Planktonic<br />
Foraminifera<br />
ORGANIZATION(S)<br />
Sigman Research<br />
Laboratory, Department<br />
of Geosciences, Princeton<br />
University<br />
LOCATION(S)<br />
Princeton, New Jersey<br />
MENTOR(S)<br />
Daniel Sigman,<br />
Dusenbury Professor of<br />
Geological and<br />
Geophysical Sciences,<br />
Professor of Geosciences;<br />
Crystal Rao, Ph.D.<br />
candidate, Geosciences<br />
Reconstructions of how marine environments<br />
responded to past global disturbances can<br />
improve our understanding of the modern ocean.<br />
Foraminifera, marine microorganisms with<br />
calcium carbonate shells, preserve records of past<br />
ocean conditions in their shells. Approximately<br />
66 million years ago, the Cretaceous-Paleogene<br />
mass extinction event caused significant<br />
ecological turnover and impacted the ocean’s<br />
biogeochemical cycling. Analyzing the nitrogen<br />
isotopic signatures of organic matter bound in<br />
foraminiferal shells from this period allows us<br />
to infer how this event impacted the marine<br />
nitrogen cycle and oxygenation. I assisted in<br />
generating the nitrogen isotope records of fossil<br />
planktonic foraminifera shells preserved in deep<br />
ocean sediment from western North Atlantic<br />
Ocean Drilling <strong>Program</strong> sites by washing and<br />
sieving bulk sediment to collect foraminifera<br />
shells and assisted with chemical cleaning<br />
and subsequent isotope analysis. I developed<br />
skills for the preparation of geologic marine<br />
sediments, foundational laboratory procedures<br />
in geochemistry, and a novel method for nitrogen<br />
isotope analysis developed in the Sigman<br />
Laboratory and its application to marine nitrogen<br />
cycling dynamics. This experience solidified my<br />
interest in paleoceanography and geochemical<br />
reconstruction with biological proxies and I<br />
plan to pursue research of similar significance<br />
to ascertain historical associations between the<br />
ocean and environmental perturbations.<br />
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