Antarctic Drilling Program

 

Title

Late Miocene submarine volcanism in ANDRILL AND-1B drill core, Ross Embayment, Antarctica

Date of this Version

10-2010

Comments

Published in Geosphere 6:5 (October 2010) pp. 524–536; doi: 10.1130/GES00537.1

Copyright © 2010 Geological Society of America.

The GSA does not permit archiving in this repository; the link at right (or below) goes to this article on their site. Payment or subscription may be required for full-text access. http://geosphere.geoscienceworld.org/cgi/content/abstract/6/5/524

Abstract

The ANDRILL McMurdo Ice Shelf initiative recovered a 1285-m-long core (AND-1B) composed of cyclic glacimarine sediments with interbedded volcanic deposits. The thickest continuous volcanic sequence by far is ~175 m long and is found at mid-core depths from 584.19 to 759.32 m below seafl oor. The sequence was logged, and initial interpretations of lithostratigraphic subdivisions were made on ice during drilling in late 2006. Subsequent observations, based on image, petrographic, and scanning electron microscopy–energy dispersive spectroscopy analyses, provide a more detailed, revised interpretation of a thick submarine to emergent volcanic succession.

The sequence is subdivided into two main subsequences on the basis of sediment composition, texture, and alteration style. The ~70-m-thick lower subsequence consists mostly of monothematic stacked volcanicrich mudstone and sandstone deposits, which are attributed to epiclastic gravity fl ow turbidite processes. This subsequence is consistent with abundant active volcanism that occurred at a distal site with respect to the drill site. The ~105-m-thick upper subsequence consists mainly of interbedded tuff, lapilli tuff, and volcanic diamictite. A Late Miocene (6.48 Ma) 2.81-m-thick subaqueously emplaced lava fl ow occurs within the second subsequence. This second subsequence is attributed to recurring cycles of submarine to emergent volcanic activity that occurred proximal to the drill site. This new data set provides (1) the fi rst rock evidence of signifi cant Late Miocene submarine volcanic activity in the Ross Embayment during a period of no to limited glaciation, and (2) a rich stratigraphic record that elucidates submarine volcano-sedimentary processes in an offshore setting.