Early-Middle Miocene (17-14Ma) Antarctic Ice Dynamics Reconstructed from the Heavy Mineral Provenance in the AND-2A Drill Core, Ross Sea, Antarctica

• Published in: Global and Planetary Change
• Main Authors: Hauptvogel, Daniel W., Passchier, Sandra
• Format: Text
• Language: unknown
• Published: Montclair State University Digital Commons 2012
• Subjects: ANDRILL; Antarctica; Heavy mineral analysis; Ice-sheet; Miocene; SEM-EDS; Antarctic; Ross Sea; West Antarctic Ice Sheet; East Antarctic Ice Sheet; Transantarctic Mountains; Antarc*; Ice Sheet
• Online Access: https://digitalcommons.montclair.edu/earth-environ-studies-facpubs/254; https://doi.org/10.1016/j.gloplacha.2011.11.003

The Miocene Climatic Optimum (17-15. Ma) and the rapid cooling of the Middle Miocene Climate Transition (15-13. Ma) together signal a major change in Earth's climate system. Here we examine the sediment provenance in the AND-2A drill core, located 10. km from the East Antarctic coastline, to significantly increase our understanding of Antarctic ice development, glacial erosion, and transport in the Ross embayment during this time. Heavy minerals are very diagnostic of source rock types and assemblages can be used to track changes in the areas of maximum erosion under the margin of an ice sheet. We used a combination of optical mineralogy and SEM-EDS analysis to characterize the heavy mineral fractions of diamictites and sandstones in the upper 650. m of AND-2A, which includes an expanded section dated between ~. 17 and 14. Ma. We find four diagnostic heavy mineral assemblages distributed in intervals throughout the core: I. (650-552. mbsf) elevated orthopyroxene, titanaugite, and carbonate contents; II. (552-308. mbsf) abundant diopside, pigeonite, and orthopyroxene, with sillimanite and kyanite; III. (308-250. mbsf) increasing contents of garnet and green hornblende; and IV. (250-20. mbsf) abundant green hornblende, titanaugite, green augite, and carbonate. Based on the heavy mineral analysis we demonstrate that (1) the ice sheet was grounded on the shelf at ~. 17.7-17.1. Ma, and it was eroding Cenozoic volcanic rocks to the south of the drillsite; (2) during the early part of the Miocene Climatic Optimum (~. 17.1-15.5. Ma) the East Antarctic Ice Sheet retreated landward into upland regions of the Transantarctic Mountains, where it eroded dolerite sills and high-grade metamorphic rocks; (3) immediately prior to the Middle Miocene Climate Transition (15.5-14.3. Ma), the East Antarctic ice advanced and eroded granitic and low-medium grade metamorphic basement rocks in the coastal sections of the Transantarctic Mountains; and (4) following this initial phase of ice growth, the West Antarctic Ice Sheet and the East ...