Frenz, Michael; Henrich, Rüdiger (2003): Carbonate silt grain-size distribution of sediment core GeoB1503-1, representing the LGM [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.95255
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: 2.311667 * Longitude: -30.646667
Date/Time Start: 1991-05-02T00:00:00 * Date/Time End: 1991-05-02T00:00:00
Minimum DEPTH, sediment/rock: 0.25 m * Maximum DEPTH, sediment/rock: 0.43 m
Event(s):
GeoB1503-1 * Latitude: 2.311667 * Longitude: -30.646667 * Date/Time: 1991-05-02T00:00:00 * Elevation: -2306.0 m * Recovery: 5.2 m * Location: Brazil Basin * Campaign: M16/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
208 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 [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.25 | 0.00 | 1.12 | 1.66 | 2.21 | 2.86 | 3.39 | 3.94 | 4.28 | 4.50 | 4.57 | 4.50 | 4.35 | 4.16 | 3.92 | 3.63 | 3.30 | 2.97 | 2.63 | 2.33 | 2.08 | 1.89 | 1.76 | 1.67 | 1.59 | 1.53 | 1.46 | 1.36 | 1.27 | 1.16 | 1.07 | 0.99 | 0.95 | 0.91 | 0.90 | 0.90 | 0.92 | 0.96 | 0.98 | 1.01 | 1.02 | 1.01 | 1.04 | 1.09 | 1.18 | 1.30 | 1.40 | 1.45 | 1.41 | 1.30 | 1.14 | 0.97 | 0.00 |
0.29 | 0.00 | 1.04 | 1.57 | 2.06 | 2.74 | 3.37 | 3.99 | 4.51 | 4.82 | 4.94 | 4.88 | 4.65 | 4.33 | 3.94 | 3.55 | 3.15 | 2.79 | 2.47 | 2.20 | 1.97 | 1.79 | 1.63 | 1.50 | 1.38 | 1.30 | 1.23 | 1.16 | 1.09 | 1.01 | 0.94 | 0.87 | 0.82 | 0.80 | 0.80 | 0.80 | 0.81 | 0.84 | 0.87 | 0.94 | 1.02 | 1.10 | 1.21 | 1.34 | 1.47 | 1.60 | 1.70 | 1.71 | 1.63 | 1.45 | 1.23 | 0.98 | 0.00 |
0.34 | 0.00 | 0.56 | 0.89 | 1.30 | 1.70 | 2.17 | 2.57 | 2.96 | 3.26 | 3.43 | 3.50 | 3.47 | 3.38 | 3.23 | 3.04 | 2.85 | 2.65 | 2.47 | 2.31 | 2.16 | 2.02 | 1.91 | 1.78 | 1.68 | 1.57 | 1.52 | 1.45 | 1.41 | 1.37 | 1.32 | 1.29 | 1.28 | 1.28 | 1.30 | 1.34 | 1.38 | 1.44 | 1.52 | 1.60 | 1.69 | 1.78 | 1.86 | 1.95 | 2.06 | 2.18 | 2.27 | 2.32 | 2.25 | 2.07 | 1.80 | 1.44 | 0.00 |
0.43 | 0.00 | 1.00 | 1.41 | 1.81 | 2.26 | 2.70 | 3.08 | 3.40 | 3.61 | 3.69 | 3.69 | 3.57 | 3.37 | 3.10 | 2.80 | 2.52 | 2.26 | 2.07 | 1.94 | 1.85 | 1.79 | 1.73 | 1.65 | 1.56 | 1.46 | 1.37 | 1.28 | 1.22 | 1.20 | 1.18 | 1.16 | 1.17 | 1.17 | 1.21 | 1.27 | 1.37 | 1.49 | 1.62 | 1.73 | 1.82 | 1.90 | 1.96 | 2.01 | 2.08 | 2.13 | 2.17 | 2.17 | 2.07 | 1.90 | 1.67 | 1.37 | 0.00 |