The Mount Feather Diamicton of the Sirius Group: an accumulation of indicators of Neogene Antarctic glacial and climatic history

• Main Authors: Wilson, G. A., Barron, J. A., Ashworth, A. C., Askin, R. A., Carter, J. A., Curren, M. G., Dalhuisen, D. H., Friedmann, E. I., Fyodorov-Davidov, D. G., Gilichinsky, D. A., Harper, M. A., Harwood, David M., Hiemstra, J. F., Janecek, T. R., Licht, K. J., Ostroumov, V. E., Powell, R. D., Rivkina, E. M., Rose, S. A., Stroeven, A. P., Stroeven, P., van der Meer, J. J. M., Wizevich, M. C.
• Format: Text
• Language: unknown
• Published: DigitalCommons@University of Nebraska - Lincoln 2002
• Subjects: Antarctica; ice sheet; Sirius Group; climate; coring; microfossils; Earth Sciences; Antarctic; The Antarctic; East Antarctic Ice Sheet; Transantarctic Mountains; Sirius; Mount Feather; Antarc*; Ice; Ice Sheet; permafrost
• Online Access: https://digitalcommons.unl.edu/geosciencefacpub/48; https://digitalcommons.unl.edu/context/geosciencefacpub/article/1047/viewcontent/Harwood_PALAEO_2002_Mt_Feather__USGS.pdf

A paucity of data from the Antarctic continent has resulted in conflicting interpretations of Neogene Antarctic glacial history. Much of the debate centres on interpretations of the glacigene Sirius Group strata that crop out as discrete deposits along the length of the Transantarctic Mountains and in particular on its age and the origin of the siliceous microfossils it encloses. Pliocene marine diatoms enclosed within Sirius Group strata are inferred to indicate a dynamic East Antarctic ice sheet that was much reduced, compared with today, in the early-middle Pliocene and then expanded again in the late Pliocene. However, the geomorphology of the Dry Valleys region is interpreted to represent a relatively long-lived (middle Miocene-recent) and stable polar climatic regime similar to that of today. The Mount Feather Diamicton infills a palaeovalley at ca. 2500 m on the NE flank of Mount Feather in the Dry Valleys region and has been included within the Sirius Group. We obtained four shallow cores (COMRAC 8, 9, 10 and 11) from beneath the permafrost boundary in the Mount Feather Diamicton in order to understand its origin and relationship with the surrounding landscape. Detailed studies of these cores (stratigraphy, sedimentology, palaeontology, micromorphology, petrography and fabric) have yielded new data that demonstrate a much more complex climatic and glacial history for the Mount Feather Diamicton than in previous interpretations. The data indicate that the Mount Feather Diamicton was deposited beneath a wet based glacier fed from a larger ice sheet behind the Transantarctic Mountains. It is, however, unlikely that this ice sheet overtopped Mount Feather (2985 m). A near-in situ non-marine diatom assemblage was recovered from 90 cm depth in COMRAC 10 and indicates a maximum depositional age of Late Miocene for the Mount Feather Diamicton. A subsequent glacial episode has distributed a boulder blanket across the surface of the diamicton. Other post-depositional processes include drying, infilling of surface ...