MUDROCK GEOCHEMISTRY AS INDICATORS OF SEDIMENT PROVENANCE AND CENOZOIC PALEOCLIMATES, CAPE ROBERTS PROJECT DRILLCORES, MCMURDO SOUND, ANTARCTICA
Maximum Al/Ti ratios and minimum Sr contents in the basal ~500 m indicate limited input from the Ferrar Dolerite (FD) relative to input from the Beacon Supergroup (BSG) and local basement (BSM) during the early Oligocene/?late Eocene?. Higher Al/Ti ratios and intermediate Sr contents indicate a mixed input of FD, BSG, and BSM detritus from the early Oligocene to the late(?) Oligocene. High Nb contents and low Al/Ti ratios record significant addition of McMurdo Volcanic Group (MVG) detritus since the late(?) Oligocene.
These provenance changes dominate the mudrock CIA record, so interpretations of the CRP paleoclimatic record remain preliminary until the source area contributions can be quantified and a "provenance-normalized" CIA record can be calculated. However, a preliminary qualitative analysis suggests that chemical weathering intensity increased briefly during the early Oligocene, interpreted as a climatic moderation that ended at approximately the time when significant glacial influence began to be recorded in these sediments.