Last glacial maximum ecology and climate from terrestrial gastropod assemblages in Peoria loess, western Kentucky

• Published in: Journal of Quaternary Science
• Main Authors: Grimley, David A., Counts, Ronald C., Conroy, Jessica L., Wang, Hong, Dendy, Sarah N., Nield, Catherine B.
• Other Authors: Division of Earth Sciences
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2020
• Subjects: Peoria; Ice Sheet
• Online Access: http://dx.doi.org/10.1002/jqs.3206; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3206; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3206; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3206; https://onlinelibrary.wiley.com/doi/am-pdf/10.1002/jqs.3206

ABSTRACT The Rocks loess section, in unglaciated western Kentucky, provides a high‐resolution environmental record during the last glacial maximum onset. The Peoria Silt (9 m thick) contains 26 terrestrial gastropod species, with up to 15 species within a single 5 cm interval. Thirteen radiocarbon ages, using shells or charcoal, range between 30 and 24.5 cal ka; younger loess has been leached or eroded. Stratigraphic shifts in gastropod assemblages imply significant cooling, particularly ~27 cal ka, as solar insolation was decreasing and the southern Laurentide Ice Sheet rapidly advancing. Midwestern to southern species (e.g. Anguispira kochi , Gastrocopta pentodon , Hawaii miniscula , Helicodiscus parallelus , Vallonia perspectiva ) occur only in the lowermost Peoria Silt (~30–27 cal ka). In contrast, cold‐tolerant species ( Columella alticola , Vertigo modesta, Vallonia gracilicosta) occur only in full glacial Peoria Silt (27–24.5 cal ka). Inferred mean July temperatures, from mutual climatic range methods, range from ~23 °C at 30 cal ka, cooling to ~18 °C by 26 cal ka; about 3–8 °C cooler than today (~26 °C). Superimposed on this cooling trend are multi‐centennial variations in detrital carbonate, fossil shell concentrations, palaeotemperature estimates, and oxygen isotope values ( Vertigo , Discus, Helicodiscus ). The finer‐scale variations imply relatively synchronous fluctuations in glacial sediment supply, loess sedimentation, and climate.