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Since then, Heusser has analyzed pollen in marine cores from all over the world, including Southern California, Japan, New Zealand, and Chile, establishing the first direct correlations between terrestrial and marine records in those regions. Her work has helped to illuminate how the planet has responded to climate change since the Miocene, a period approximately 2.3 million to 5 million years ago. Her work has documented, for example, the collapse of the California current, which brings cold, nutrient-rich water along the West Coast, during glacial periods over the past 550,000 years.
Heusser worked in Lamont’s Core Lab alongside the CLIMAP team, which was studying cores from the oceans in order to understand the Earth as it was during the last glacial period. Heusser contributed through her work on pollen off the coast of California and Washington, and through her paper with Shackleton. “It was a very dynamic time, a very exciting time,” she says.
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Geological Society of America eBookspp.215-227, (2022)
Linda E. Heusser, Mónica Wingenroth
Quaternary of South America and Antarctic Peninsulapp.79-91, (2020)
AGU Fall Meeting Abstracts (2020)
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Matthew E. Kirby,Linda E. Heusser,C. Scholz,R. Ramezan, M. A. Anderson,B. Markle,Edward J. Rhodes,K. C. Glover, J. Fantozzi, C. Hiner,B. Price, H. Rangel
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