HR: 0800h
AN: OS11A-0196    [Abstracts]
TI: Strontium Isotope Dating of Metalliferous Sediment in the SW Pacific Basin
AU: * Stancin, A M
EM: astancin@umich.edu
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AU: Gleason, J D
EM: jdgleaso@umich.edu
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AU: Owen, B M
EM: rowen@umich.edu
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AU: Rea, D K
EM: davidrea@umich.edu
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AU: Moore, T C
EM: tedmoore@umich.edu
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AU: Hendy, I L
EM: ihendy@umich.edu
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AU: Lyle, M W
EM: mlyle@ocean.tamu.edu
AF: Texas A & M University, Department of Oceanography, College Station, TX 77843, United States
AU: Blum, J D
AF: University of Michigan, Department of Geological Sciences 1100 N. University, Ann Arbor, MI 48109, United States
AB: A 2 million km2 region virtually devoid of sediment was identified in the remote SW Pacific Basin during the TUIM- 3 2005 drill site survey cruise. This region, termed the "South Pacific Bare Zone", comprises ocean floor dating back to the Late Cretaceous. Within the Bare Zone, a small (1km2) abyssal valley containing sediment to a depth of 24 m was sampled using a large diameter piston core (MV0502-15JC, 31 ° 42.194'S, 143 ° 30.331'W), leading to recovery of 8.35 m of metalliferous sediment at 5082 m water depth. Fish-teeth Sr-isotope stratigraphy reveals a continuous record of sedimentation from 31 Ma to present at this site. The fish teeth age-depth profile and INAA geochemistry reveal an exponentially decreasing hydrothermal flux, with sedimentation rates approaching 0.05 mm/kyr after 20 Ma. The source of hydrothermal activity at this site was likely the Pacific- Farallon Ridge, which went extinct at 20 Ma. A second piston core (MV0502-16JC; 28 ° 05.151'S, 140 ° 14.140'W) was collected near MacDonald Seamounts located on the southeastern end of the Cook-Austral island chain outside the Bare Zone and recovered 10.5 m of hydrothermal sediment and biogenic ooze. The lower 65 cm of the core consists of a coccolith ooze. From 10 mbsf depth to 1.5 mbsf depth, the core contians reddish black zeolitic clay, while the upper 1.5 mbsf contains biogenic ooze associated with abundant Late Pleistocene foraminifera remains. Concordant nannofossil and fish teeth ages at the base of the core (27-28 Ma), and Pleistocene ages near the top of the core reinforce the validity of the Sr fish teeth method for dating hydrothermal cores. These independent records suggest that regional hydrothermal activity during the Oligocene may have been related to a series of late Eocene/early Oligocene ridge jumps, propagating rifts and seafloor spreading centers that accompanied large-scale plate tectonic reorganization of South Pacific seafloor.
DE: 1040 Radiogenic isotope geochemistry
DE: 3017 Hydrothermal systems (0450, 1034, 3616, 4832, 8135, 8424)
DE: 3022 Marine sediments: processes and transport
DE: 4835 Marine inorganic chemistry (1050)
SC: Ocean Sciences [OS]
MN: 2007 Fall Meeting