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Abstract: Isotopic and mineralogical fingerprinting of late Pleistocene iron oxide “Rattle Stones” in southern New England and implications for a potential Last Glacial Maximum sea-level highstand (AGU25)

Isotopic and mineralogical fingerprinting of late Pleistocene iron oxide “Rattle Stones” in southern New England and implications for a potential Last Glacial Maximum sea-level highstand

Noah Johnson1, Isaiah Olds-Campanile1, Eben Blake Hodgin2, Daniel Enrique Ibarra3, Kevin Robertson4, Jamie Pahigian4 and Jiquan Chen5, (1)Brown University, Providence, United States, (2)Harvard University, Cambridge, United States, (3)Brown University, Department of Earth, Environmental and Planetary Sciences, Providence, United States, (4)Brown University, Department of Earth, Environmental, and Planetary Sciences, Providence, United States, (5)China University of Geosciences, Beijing, China
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