Late Pleistocene and Holocene hydroclimate change in the Southeastern United States: Sedimentary, pedogenic, and stable carbon isotope evidence in Tennessee River floodplain paleosols

• Main Author: Kocis, James Joseph
• Format: Text
• Language: unknown
• Published: TRACE: Tennessee Research and Creative Exchange 2011
• Subjects: Late Quaternary paleohydroclimates; floodplain geochronology; alluvial paleosols; sedimentology; stable carbon isotopes; Southeastern North America; Earth Sciences; Geochemistry; Geology; Stratigraphy; Nash; North Atlantic
• Online Access: https://trace.tennessee.edu/utk_gradthes/1077; https://trace.tennessee.edu/context/utk_gradthes/article/2231/viewcontent/KocisJamesDecember2011.pdf

In order to understand hydroclimate variability of future climate change, it is important to know the timing and range of natural climate change in the past. The Southeastern United States (SE) is situated along the poleward extent of projected subtropical drying, where the expression of past hydrol...