Reconstruction of the Kuroshio Current Extension through the Pliocene to earliest Pleistocene

Friday, November 19, 2021 11:00to12:00
FDA 232 (Gill Room) and Zoom
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Dr. Adriane R. Lam 

Postdoctoral Fellow, Department of Geological Sciences and Environmental Studies, Binghamton University 

Hybrid Seminar: Friday, November 19, 2021 11:00 AM

           The Kuroshio Current Extension (KCE) is the major northwest Pacific Ocean western boundary current as part of the North Pacific Subtropical Gyre. This region is home to some of the highest biodiversity in our world ocean today. This high biodiversity sustains Japan’s fishing industry, and supplies food for millions of people around the world. In addition, the current plays a large role in dispersal dynamics of marine organisms, such as the Japanese eel, and may be an area that promotes speciation. Today, the KCE is warming and shifting northward under increasing atmospheric carbon dioxide levels. However, it is currently unknown to what extent the current can shift north, how warm it can become and the rate of warming, and how these factors will affect marine organisms living in the current. To begin answering these questions, this study reconstructs the behavior of the KCE during the Pliocene to earliest Pleistocene (5–2.5 Ma), a time of tectonic gateway closure and climate shifts, when atmospheric CO2 levels were similar to today. Using stable isotopic analyses from surface dwelling planktic foraminifera from three Ocean Drilling Program sites that lie across the modern-day position of the KCE, we find that the current was highly sensitive to major global warming and cooling events. We also identify several times at which the current may have experienced latitudinal shifts. These data, combined with additional datasets, indicate the KCE has the potential to greatly warm under increasing atmospheric carbon dioxide concentrations such as those projected for the future.


Meeting ID: 875 7599 6613            Passcode: 215159

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