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Irino, Tomohisa; Pedersen, Thomas F (2000): (Table 1) Minor and trace element composition of ODP Hole 167-1017E sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.796246, Supplement to: Irino, T; Pedersen, TF (2000): Geochemical character of glacial to interglacial sediments at Site 1017, southern California margin: minor and trace elements. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC Jr (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 1-9, https://doi.org/10.2973/odp.proc.sr.167.209.2000

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Published: 2000 (exact date unknown)DOI registered: 2012-12-03

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Abstract:
We analyzed selected minor and trace element contents to examine the sources and transport paths of sediments deposited at Ocean Drilling Program Site 1017 during the last 25 k.y. Elements are subsequently classified as being of diagenetic, biogenic, and/or terrigenous origins. Re, U, Mo, and As are diagenetically enriched within sediments, reflecting millennial-scale variability in bottom-water oxygenation and/or the sedimentary redox boundary depth. Sr variation is largely controlled by the input of biogenic carbonate. Using Q-mode factor analysis, variations in the 12 elements of detrital origin that remain can be explained by three factors (end-members) attributable to sand- and silt-sized detritus (Factor 2), and fine fractions with mafic (Factor 3) and felsic (Factor 1) characteristics. Elimination of the influence of grain size, temporal variations in the relative contribution from mafic materials shows that more detritus from the mafic Franciscan Complex was transported to the site during marine isotope Stage 2 than during the Holocene. This was probably due to enhanced southward littoral transport of detritus along the California margin during the latest Pleistocene.
Project(s):
Coverage:
Latitude: 34.535000 * Longitude: -121.107000
Date/Time Start: 1996-05-28T02:00:00 * Date/Time End: 1996-05-28T06:30:00
Minimum DEPTH, sediment/rock: 0.015 m * Maximum DEPTH, sediment/rock: 5.885 m
Event(s):
167-1017E * Latitude: 34.535000 * Longitude: -121.107000 * Date/Time Start: 1996-05-28T02:00:00 * Date/Time End: 1996-05-28T06:30:00 * Elevation: -955.5 m * Penetration: 24.9 m * Recovery: 25.71 m * Location: North Pacific Ocean * Campaign: Leg167 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 3 cores; 24.9 m cored; 0 m drilled; 103.3 % recovery
Comment:
All minor and trace element concentration data have been corrected for dilution by salt. The sample depths (in mbsf) have not been corrected for core expansion.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelIrino, TomohisaDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode
3ChlorineCl%Irino, TomohisaTitration, Mohr-Knudsen
4VanadiumVmg/kgIrino, TomohisaX-ray spectrometry
5ChromiumCrmg/kgIrino, TomohisaX-ray spectrometry
6ManganeseMnmg/kgIrino, TomohisaX-ray spectrometry
7CobaltComg/kgIrino, TomohisaX-ray spectrometry
8NickelNimg/kgIrino, TomohisaX-ray spectrometry
9CopperCumg/kgIrino, TomohisaX-ray spectrometry
10ZincZnmg/kgIrino, TomohisaX-ray spectrometry
11ArsenicAsmg/kgIrino, TomohisaX-ray spectrometry
12RubidiumRbmg/kgIrino, TomohisaX-ray spectrometry
13StrontiumSrmg/kgIrino, TomohisaX-ray spectrometry
14YttriumYmg/kgIrino, TomohisaX-ray spectrometry
15ZirconiumZrmg/kgIrino, TomohisaX-ray spectrometry
16NiobiumNbmg/kgIrino, TomohisaX-ray spectrometry
17BariumBamg/kgIrino, TomohisaX-ray spectrometry
18LeadPbmg/kgIrino, TomohisaX-ray spectrometry
19TitaniumTimg/kgIrino, TomohisaX-ray spectrometry
20RheniumReµg/kgIrino, TomohisaIsotope dilution inductively coupled plasma mass spectrometry
21MolybdenumMomg/kgIrino, TomohisaIsotope dilution inductively coupled plasma mass spectrometry
22UraniumUmg/kgIrino, TomohisaIsotope dilution inductively coupled plasma mass spectrometry
Size:
4080 data points

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