Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Reusch, Douglas N (2002): Mineralogy, geochemistry, isotopic ratios and foraminifer occurrence in ODP Hole 183-1139A. PANGAEA, https://doi.org/10.1594/PANGAEA.785307, Supplement to: Reusch, DN (2002): Oligocene-Miocene terrigenous and pelagic sediments, Skiff Bank, Kerguelen Plateau (ODP Leg 183, Site 1139). In: Frey, FA; Coffin, MF; Wallace, PJ; Quilty, PG (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 183, 1-31, https://doi.org/10.2973/odp.proc.sr.183.010.2002

Always quote above citation when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Mixed terrigenous-pelagic sediments from the Oligocene-lower Miocene interval of Hole 1139A accumulated on the flank of an eroded alkalic volcano, Skiff Bank. In this study, I explore relationships among sediment fluxes, especially of organic carbon and the clay mineral by-products of silicate weathering, and lithologic, tectonic, climatic, and biologic forcing factors. Benthic foraminifers indicate that Skiff Bank had subsided to lower bathyal depths (1000-2000 m) by the Oligocene. Two prominent maxima in noncarbonate concentration at 28 and 22 Ma correspond to peaks in the terrigenous flux; also, high noncarbonate concentrations are associated with larger grain sizes (silt) and higher opal concentrations. These and higher-frequency variations of noncarbonate concentration were probably controlled by glacioeustatic/climatic changes, with higher noncarbonate concentrations caused by increased erosion during glacial lowstands. Around 27 Ma, benthic foraminiferal d18O values decreased 0.7 per mil as the noncarbonate concentration decreased after the 28-Ma maximum. A paucity of clay-sized sediment and clay minerals suggests that physical erosion, by waves and/or ice, predominated under weathering-limited conditions. Low organic carbon concentrations (~0.13 wt%) also suggest a harsh environment and/or poor preservation in coarse (>2 µm) sediments that were extensively bioturbated below the oxygen minimum zone.
Project(s):
Coverage:
Latitude: -50.185050 * Longitude: 63.936530
Date/Time Start: 1999-01-15T10:23:00 * Date/Time End: 1999-01-21T16:30:00
Event(s):
183-1139A * Latitude: -50.185050 * Longitude: 63.936530 * Date/Time Start: 1999-01-15T10:23:00 * Date/Time End: 1999-01-21T16:30:00 * Elevation: -1415.3 m * Penetration: 694.2 m * Recovery: 356.88 m * Location: Indian Ocean * Campaign: Leg183 * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 73 cores; 694.2 m cored; 0 m drilled; 51.4 % recovery
Size:
7 datasets

Download Data

Download ZIP file containing all datasets as tab-delimited text (use the following character encoding: )