Frenz, Michael; Henrich, Rüdiger (2003): Carbonate silt grain-size distribution of sediment core GeoB1101-5, representing the LGM [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.95245
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Frenz, Michael (2003): Grain-size composition of Quaternary South Atlantic sediments and its paleoceanographic significance. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 213, 123 pp, urn:nbn:de:gbv:46-ep000103333
Frenz, Michael; Henrich, Rüdiger (2007): Carbonate dissolution revealed by silt grain-size distribution: comparison of Holocene and Last Glacial Maximum sediments from the pelagic South Atlantic. Sedimentology, 54(2), 391-404, https://doi.org/10.1111/j.1365-3091.2006.00841.x
Project(s):
Coverage:
Latitude: 1.658330 * Longitude: -10.980000
Date/Time Start: 1989-02-22T00:00:00 * Date/Time End: 1989-02-22T00:00:00
Minimum DEPTH, sediment/rock: 0.31 m * Maximum DEPTH, sediment/rock: 0.46 m
Event(s):
GeoB1101-5 * Latitude: 1.658330 * Longitude: -10.980000 * Date/Time: 1989-02-22T00:00:00 * Elevation: -4588.0 m * Penetration: 16 m * Recovery: 13.61 m * Location: Guinea Basin * Campaign: M9/4 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: cc: Ton, Foram., sandig
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
156 data points
Data
| 1 Depth sed [m] | 2 3.9-4.0 phi [%] | 3 4.0-4.1 phi [%] | 4 4.1-4.2 phi [%] | 5 4.2-4.3 phi [%] | 6 4.3-4.4 phi [%] | 7 4.4-4.5 phi [%] | 8 4.5-4.6 phi [%] | 9 4.6-4.7 phi [%] | 10 4.7-4.8 phi [%] | 11 4.8-4.9 phi [%] | 12 4.9-5.0 phi [%] | 13 5.0-5.1 phi [%] | 14 5.1-5.2 phi [%] | 15 5.2-5.3 phi [%] | 16 5.3-5.4 phi [%] | 17 5.4-5.5 phi [%] | 18 5.5-5.6 phi [%] | 19 5.6-5.7 phi [%] | 20 5.7-5.8 phi [%] | 21 5.8-5.9 phi [%] | 22 5.9-6.0 phi [%] | 23 6.0-6.1 phi [%] | 24 6.1-6.2 phi [%] | 25 6.2-6.3 phi [%] | 26 6.3-6.4 phi [%] | 27 6.4-6.5 phi [%] | 28 6.5-6.6 phi [%] | 29 6.6-6.7 phi [%] | 30 6.7-6.8 phi [%] | 31 6.8-6.9 phi [%] | 32 6.9-7.0 phi [%] | 33 7.0-7.1 phi [%] | 34 7.1-7.2 phi [%] | 35 7.2-7.3 phi [%] | 36 7.3-7.4 phi [%] | 37 7.4-7.5 phi [%] | 38 7.5-7.6 phi [%] | 39 7.6-7.7 phi [%] | 40 7.7-7.8 phi [%] | 41 7.8-7.9 phi [%] | 42 7.9-8.0 phi [%] | 43 8.0-8.1 phi [%] | 44 8.1-8.2 phi [%] | 45 8.2-8.3 phi [%] | 46 8.3-8.4 phi [%] | 47 8.4-8.5 phi [%] | 48 8.5-8.6 phi [%] | 49 8.6-8.7 phi [%] | 50 8.7-8.8 phi [%] | 51 8.8-8.9 phi [%] | 52 8.9-9.0 phi [%] | 53 9.0-9.1 phi [%] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.31 | 0.00 | 0.68 | 1.01 | 1.40 | 1.86 | 2.31 | 2.71 | 2.95 | 3.09 | 3.13 | 3.17 | 3.29 | 3.52 | 3.85 | 4.14 | 4.33 | 4.32 | 4.14 | 3.87 | 3.67 | 3.55 | 3.55 | 3.60 | 3.61 | 3.45 | 3.17 | 2.81 | 2.43 | 2.08 | 1.80 | 1.59 | 1.43 | 1.30 | 1.17 | 1.05 | 0.95 | 0.84 | 0.78 | 0.73 | 0.68 | 0.57 | 0.41 | 0.22 | 0.09 | 0.01 | 0.07 | 0.14 | 0.18 | 0.16 | 0.11 | 0.05 | 0.00 |
| 0.37 | 0.00 | 0.33 | 0.47 | 0.62 | 0.86 | 1.09 | 1.37 | 1.74 | 2.01 | 2.30 | 2.50 | 2.75 | 2.94 | 3.09 | 3.25 | 3.36 | 3.43 | 3.44 | 3.45 | 3.44 | 3.41 | 3.36 | 3.30 | 3.16 | 3.00 | 2.86 | 2.71 | 2.62 | 2.48 | 2.35 | 2.18 | 1.98 | 1.80 | 1.66 | 1.61 | 1.60 | 1.66 | 1.70 | 1.70 | 1.64 | 1.56 | 1.43 | 1.32 | 1.23 | 1.17 | 1.07 | 0.96 | 0.78 | 0.59 | 0.41 | 0.29 | 0.00 |
| 0.46 | 0.00 | 0.38 | 0.46 | 0.58 | 0.78 | 1.07 | 1.42 | 1.88 | 2.33 | 2.81 | 3.22 | 3.58 | 3.84 | 4.02 | 4.13 | 4.22 | 4.26 | 4.26 | 4.23 | 4.10 | 3.91 | 3.67 | 3.40 | 3.09 | 2.82 | 2.53 | 2.32 | 2.12 | 2.01 | 1.87 | 1.76 | 1.61 | 1.45 | 1.34 | 1.24 | 1.19 | 1.18 | 1.13 | 1.06 | 0.97 | 0.90 | 0.84 | 0.82 | 0.82 | 0.83 | 0.81 | 0.73 | 0.65 | 0.53 | 0.45 | 0.38 | 0.00 |