Tiedemann, Ralf; Sarnthein, Michael; Stein, Ruediger (1989): (Appendix D) Physical properties, grain size, and bulk mineralogy of ODP Site 108-661 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.746248, In supplement to: Tiedemann, R et al. (1989): Climatic changes in the western Sahara: aeolo-marine sediment record of the last 8 million years (Sites 657-661). In: Ruddiman, W; Sarnthein, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 108, 241-277, https://doi.org/10.2973/odp.proc.sr.108.169.1989
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 9.446800 * Longitude: -19.386100
Date/Time Start: 1986-03-17T00:00:00 * Date/Time End: 1986-03-21T00:00:00
Minimum DEPTH, sediment/rock: 1.05 m * Maximum DEPTH, sediment/rock: 84.65 m
Event(s):
108-661 * Latitude: 9.446800 * Longitude: -19.386100 * Date/Time Start: 1986-03-17T00:00:00 * Date/Time End: 1986-03-21T00:00:00 * Elevation: -4023.5 m * Penetration: 377.8 m * Recovery: 316.4 m * Location: South Atlantic Ocean * Campaign: Leg108 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 41 cores; 377.8 m cored; 0 m drilled; 83.7% recovery
Comment:
Depth, sediment is composite depth (mcd)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | AGE | Age | ka BP | Geocode | ||
| 3 | Density, dry bulk | DBD | g/cm3 | Tiedemann, Ralf | Weighted | |
| 4 | Calcium carbonate | CaCO3 | % | Tiedemann, Ralf | ||
| 5 | Siliciclastics | Siliciclast | % | Tiedemann, Ralf | X-ray diffraction (XRD) | |
| 6 | Quartz | Qz | % | Tiedemann, Ralf | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
199 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 DBD [g/cm3] | 4 CaCO3 [%] | 5 Siliciclast [%] | 6 Qz [%] |
|---|---|---|---|---|---|
| 1.05 | 64 | 0.52 | 11.6 | 88.4 | 39 |
| 2.65 | 162 | 0.52 | 11.0 | 89.0 | 43 |
| 5.65 | 346 | 0.54 | 21.4 | 78.6 | 35 |
| 7.15 | 438 | 0.63 | 42.8 | 57.2 | 23 |
| 8.65 | 530 | 0.62 | 51.2 | 48.8 | 11 |
| 10.15 | 622 | 0.52 | 24.9 | 75.1 | 36 |
| 12.15 | 745 | 0.39 | 5.7 | 94.3 | 23 |
| 15.15 | 929 | 0.58 | 51.2 | 48.8 | 10 |
| 16.65 | 1020 | 0.69 | 38.3 | 61.7 | 18 |
| 18.15 | 1112 | 0.56 | 56.7 | 43.3 | 12 |
| 19.61 | 1202 | 0.69 | 43.9 | 56.1 | 15 |
| 21.63 | 1326 | 0.68 | 65.1 | 34.9 | 11 |
| 23.10 | 1416 | 0.69 | 37.1 | 62.9 | 17 |
| 24.57 | 1506 | 0.59 | 70.0 | 30.0 | 5 |
| 26.04 | 1596 | 0.66 | 64.6 | 35.4 | 9 |
| 27.51 | 1686 | 0.72 | 48.6 | 51.4 | 14 |
| 28.98 | 1776 | 0.73 | 29.3 | 70.7 | 20 |
| 31.16 | 1915 | 0.74 | 51.7 | 48.3 | 5 |
| 32.66 | 2052 | 0.76 | 55.5 | 44.5 | 9 |
| 34.16 | 2190 | 0.76 | 57.1 | 42.9 | 9 |
| 35.66 | 2327 | 0.70 | 48.7 | 51.3 | 10 |
| 37.16 | 2460 | 0.73 | 71.5 | 28.5 | 6 |
| 38.66 | 2551 | 0.79 | 44.4 | 55.6 | 13 |
| 40.65 | 2672 | 0.74 | 76.0 | 24.0 | 4 |
| 42.12 | 2761 | 0.81 | 61.7 | 38.3 | 8 |
| 43.64 | 2854 | 0.86 | 65.1 | 34.9 | 10 |
| 45.14 | 2945 | 0.80 | 68.3 | 31.7 | 5 |
| 46.64 | 3036 | 0.80 | 79.0 | 21.0 | 3 |
| 48.14 | 3127 | 0.79 | 52.1 | 47.9 | 9 |
| 50.15 | 3249 | 0.77 | 72.1 | 27.9 | 5 |
| 51.65 | 3340 | 0.90 | 65.4 | 34.6 | 9 |
| 53.15 | 3432 | 0.97 | 59.7 | 40.3 | 5 |
| 54.65 | 3523 | 0.97 | 53.7 | 46.3 | 10 |
| 56.15 | 3614 | 0.90 | 68.9 | 31.1 | 10 |
| 57.65 | 3705 | 0.89 | 71.6 | 28.4 | 4 |
| 59.65 | 3827 | 0.99 | 44.5 | 55.5 | 11 |
| 61.15 | 3918 | 0.79 | 52.7 | 47.3 | 9 |
| 62.65 | 4009 | 0.96 | 63.0 | 37.0 | 8 |
| 64.15 | 4418 | 0.99 | 35.0 | 65.0 | 13 |
| 65.65 | 4798 | 0.98 | 45.3 | 54.7 | 8 |
| 67.15 | 5178 | 0.95 | 69.7 | 30.3 | 5 |
| 69.15 | 5685 | 1.01 | 50.5 | 49.5 | 8 |
| 72.15 | 6445 | 1.07 | 26.3 | 73.7 | 13 |
| 73.65 | 6825 | 0.97 | 0.3 | 99.7 | |
| 75.15 | 7205 | 0.98 | 0.3 | 99.7 | |
| 76.65 | 7585 | 0.95 | 0.0 | 100.0 | |
| 78.65 | 8091 | 1.09 | 40.8 | 59.2 | 12 |
| 80.15 | 8471 | 1.01 | 50.2 | 49.8 | 8 |
| 81.65 | 8851 | 1.04 | 33.9 | 66.1 | 9 |
| 83.15 | 9231 | 0.98 | 0.3 | 99.7 | |
| 84.65 | 9611 | 1.09 | 0.0 | 100.0 |