Tiedemann, Ralf; Sarnthein, Michael; Shackleton, Nicholas J (1994): Dust content in sediments of ODP Hole 108-659A in the North Atlantic [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52518, In supplement to: Tiedemann, R et al. (1994): Astronomic timescale for the Pliocene Atlantic d18O and dust flux records of Ocean Drilling Program site 659. Paleoceanography, 9(4), 619-638, https://doi.org/10.1029/94PA00208
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 18.077200 * Longitude: -21.026200
Date/Time Start: 1986-03-09T09:30:00 * Date/Time End: 1986-03-11T05:30:00
Minimum DEPTH, sediment/rock: 0.11 m * Maximum DEPTH, sediment/rock: 149.59 m
Event(s):
108-659A * Latitude: 18.077200 * Longitude: -21.026200 * Date/Time Start: 1986-03-09T09:30:00 * Date/Time End: 1986-03-11T05:30:00 * Elevation: -3082.0 m * Penetration: 273.8 m * Recovery: 174.95 m * Location: North Atlantic Ocean * Campaign: Leg108 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 273.8 m cored; 0 m drilled; 63.9 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Dust, aeolian | Dust | % | Tiedemann, Ralf | see comment | Depth is a result from correlations between holes A, B and C (see Depth, composite). The noncarbonate fraction (100% minus %CaCO3) is considered to be purely eaolian, because the concentrations of biogenic opal (<2%), organic carbon (<0.5%), and volcanic glass are negligible and fluvial sediment supply and turbidites cannot reach this position (Tiedemann et al., 1989) |
| 3 | Density, dry bulk | DBD | g/cm3 | Tiedemann, Ralf | Depth is a result from correlations between holes A, B and C (see Depth, composite). | |
| 4 | Accumulation rate, dust | DMAR | g/cm2/ka | Tiedemann, Ralf | Calculated | Depth is a result from correlations between holes A, B and C (see Depth, composite). The noncarbonate fraction (100% minus %CaCO3) is considered to be purely eaolian, because the concentrations of biogenic opal (<2%), organic carbon (<0.5%), and volcanic glass are negligible and fluvial sediment supply and turbidites cannot reach this position (Tiedemann et al., 1989) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3720 data points
Download Data
View dataset as HTML (shows only first 2000 rows)