Holbourn, Ann E; Kuhnt, Wolfgang; Lyle, Mitchell W; Schneider, Leah; Romero, Oscar E; Andersen, Nils (2014): Geochemistry of IODP Site 321-U1338 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.820094, In supplement to: Holbourn, AE et al. (2014): Middle Miocene climate cooling linked to intensification of eastern equatorial Pacific upwelling. Geology, 42(1), 19-22, https://doi.org/10.1130/G34890.1
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Project(s):
Coverage:
Latitude: 2.507800 * Longitude: -117.969910
Minimum DEPTH, sediment/rock: 307.65 m * Maximum DEPTH, sediment/rock: 395.44 m
Event(s):
321-U1338 * Latitude: 2.507800 * Longitude: -117.969910 * Elevation: -4210.8 m * Campaign: Exp321 (Pacific Equatorial Age Transect II / Juan de Fuca) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Comment:
DEPTH, sediment/rock [m] gives the DEPTH (CSF-A) [m].
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Holbourn, Ann E | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Depth, composite | Depth comp | mcd | Holbourn, Ann E | Intercore correlation | CCSF-A |
| 4 | AGE | Age | ka BP | Geocode | ||
| 5 | Silicon (peak area) | Si peak area | Holbourn, Ann E | X-ray fluorescence (XRF) | ||
| 6 | log-Silicon/Titanium ratio | log(Si/Ti) | Holbourn, Ann E | X-ray fluorescence (XRF) | ||
| 7 | Calcium (peak area) | Ca peak area | Holbourn, Ann E | X-ray fluorescence (XRF) | ||
| 8 | Calcium carbonate | CaCO3 | % | Holbourn, Ann E | Estimated | |
| 9 | Titanium (peak area) | Ti peak area | Holbourn, Ann E | X-ray fluorescence (XRF) | ||
| 10 | - | - | Holbourn, Ann E | Calculated | Ti area + 4000 | |
| 11 | log-Titanium/Calcium ratio | log(Ti/Ca) | Holbourn, Ann E | X-ray fluorescence (XRF) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
32193 data points
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