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Dr. Evan J. Gowan
evangowan.bsky.social
did:plc:rx6oszpl5ictnnwupkxaxyq5
There aren't very many proxies of past sea level during the Last Glacial Maximum (27,000-19,000 ybp). Jones et al present a sediment core from Beringia that transitioned from being a lake to being submerged by the ocean during the early parts of the deglaciation. https://www.tandfonline.com/doi/abs/10.1080/15230430.2025.2557062%4010.1080/tfocoll.2024.0.issue-beringian-environments
2025-10-13T05:32:21.683Z