Late Pliocene to late Pleistocene environments preserved at the Palisades Site, central Yukon River, Alaska

• Published in: Quaternary Research
• Main Authors: Matheus, Paul, Begét, James, Mason, Owen, Gelvin-Reymiller, Carol
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2003
• Subjects: Yukon; Palisades; The Palisades; Dawson; Ice; Old Crow; permafrost; taiga; wedge*; Yukon river; Alaska
• Online Access: http://dx.doi.org/10.1016/s0033-5894(03)00091-7; http://api.elsevier.com/content/article/PII:S0033589403000917?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:S0033589403000917?httpAccept=text/plain; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400012242

Abstract The Palisades Site is an extensive silt-loam bluff complex on the central Yukon River preserving a nearly continuous record of the last 2 myr. Volcanic ash deposits present include the Old Crow (OCt; 140,000 yr), Sheep Creek (SCt; 190,000 yr), PA (2.02 myr), EC (ca. 2 myr), and Mining Camp (ca. 2 myr) tephras. Two new tephras, PAL and PAU, are geochemically similar to the PA and EC tephras and appear to be comagmatic. The PA tephra occurs in ice-wedge casts and solifluction deposits, marking the oldest occurrence of permafrost in central Alaska. Three buried forest horizons are present in association with dated tephras. The uppermost forest bed occurs immediately above the OCt; the middle forest horizon occurs below the SCt. The lowest forest bed occurs between the EC and the PA tephras, and correlates with the Dawson Cut Forest Bed. Plant taxa in all three peats are common elements of moist taiga forest found in lowlands of central Alaska today. Large mammal fossils are all from common late Pleistocene taxa. Those recovered in situ came from a single horizon radiocarbon dated to ca. 27,000 14 C yr B.P. The incongruous small mammal assemblage in that horizon reflects a diverse landscape with both wet and mesic environments.