Bogdanov, Yury A; Dmitrenko, Olga B; Pavlidis, Yury A; Turpaeva, Elena P (1996): (Table 2) Content of biogenic skeleton fragments in bottom sediments from the Campeche Bank [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.759404, In supplement to: Bogdanov, YA et al. (1996): Bottom sediments of the Campeche Bank (Gulf of Mexico) and paleoceanological reconstructions. Translated from Okeanologiya, 1996, 36(5), 774-786, Oceanology, 36(5), 731-743
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 20.643725 * Median Longitude: -92.020900 * South-bound Latitude: 20.591700 * West-bound Longitude: -92.049100 * North-bound Latitude: 20.757100 * East-bound Longitude: -91.966600
Minimum DEPTH, sediment/rock: 0.075 m * Maximum DEPTH, sediment/rock: 4.100 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
5 | Depth, top/min | Depth top | m | Bogdanov, Yury A | ||
6 | Depth, bottom/max | Depth bot | m | Bogdanov, Yury A | ||
7 | Horizon | Horizon | Bogdanov, Yury A | lithostratigraphic | ||
8 | Sample, dry mass | Samp dm | g | Bogdanov, Yury A | ||
9 | Sceleton fragments | Scel fragm | g | Bogdanov, Yury A | ||
10 | Major fragments | Major fragm | g | Bogdanov, Yury A | ||
11 | Sceleton fragments | Scel fragm | % | Bogdanov, Yury A | ||
12 | Major fragments | Major fragm | % | Bogdanov, Yury A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
188 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Depth sed [m] | 5 Depth top [m] | 6 Depth bot [m] | 7 Horizon | 8 Samp dm [g] | 9 Scel fragm [g] | 10 Major fragm [g] | 11 Scel fragm [%] | 12 Major fragm [%] |
---|---|---|---|---|---|---|---|---|---|---|---|
AMK30-2877 | 20.7571 | -92.0491 | 0.075 | 0.00 | 0.15 | I | 525 | 40 | 2.20 | 7.6 | 0.4 |
AMK30-2877 | 20.7571 | -92.0491 | 0.400 | 0.30 | 0.50 | I | 979 | 60 | 7.40 | 6.1 | 0.8 |
AMK30-2877 | 20.7571 | -92.0491 | 0.965 | 0.90 | 1.03 | I | 485 | 100 | 7.60 | 20.5 | 1.6 |
AMK30-2877 | 20.7571 | -92.0491 | 1.450 | 1.30 | 1.60 | II | 836 | 360 | 122.00 | 43.1 | 14.6 |
AMK30-2924 | 20.6266 | -92.0338 | 0.375 | 0.25 | 0.50 | I | 901 | 49 | 2.50 | 5.4 | 0.6 |
AMK30-2924 | 20.6266 | -92.0338 | 1.100 | 1.00 | 1.20 | I | 1046 | 70 | 6.7 | ||
AMK30-2924 | 20.6266 | -92.0338 | 1.650 | 1.55 | 1.75 | I | 1136 | 75 | 2.80 | 6.6 | 0.3 |
AMK30-2924 | 20.6266 | -92.0338 | 2.065 | 1.83 | 2.30 | II | 1154 | 390 | 81.50 | 25.1 | 5.2 |
AMK30-2924 | 20.6266 | -92.0338 | 3.600 | 3.50 | 3.70 | III | 1233 | 22 | 1.10 | 1.8 | 0.1 |
AMK30-2924 | 20.6266 | -92.0338 | 3.925 | 3.85 | 4.00 | III | 1030 | 55 | 1.50 | 4.9 | 0.1 |
AMK30-2911 | 20.5917 | -92.0341 | 0.250 | 0.10 | 0.40 | I | 773 | 30 | 3.9 | ||
AMK30-2911 | 20.5917 | -92.0341 | 0.900 | 0.80 | 1.00 | I | 816 | 85 | 2.30 | 10.4 | 0.3 |
AMK30-2911 | 20.5917 | -92.0341 | 1.300 | 1.20 | 1.40 | I | 1163 | 120 | 4.15 | 10.3 | 0.4 |
AMK30-2911 | 20.5917 | -92.0341 | 1.700 | 1.60 | 1.80 | I | 1238 | 210 | 20.05 | 17.0 | 1.6 |
AMK30-2911 | 20.5917 | -92.0341 | 1.900 | 1.80 | 2.00 | II | 830 | 240 | 76.05 | 28.9 | 9.2 |
AMK30-2911 | 20.5917 | -92.0341 | 2.200 | 2.10 | 2.30 | II | 1188 | 279 | 112.60 | 25.6 | 9.5 |
AMK30-2911 | 20.5917 | -92.0341 | 2.600 | 2.50 | 2.70 | III | 952 | 50 | 10.00 | 5.3 | 1.1 |
AMK30-2911 | 20.5917 | -92.0341 | 3.135 | 3.00 | 3.27 | III | 1308 | 80 | 13.20 | 61.0 | 1.0 |
AMK30-2927 | 20.5995 | -91.9666 | 0.200 | 0.10 | 0.30 | I | 763 | 45 | 5.9 | ||
AMK30-2927 | 20.5995 | -91.9666 | 0.900 | 0.80 | 1.00 | I | 994 | 60 | 6.30 | 6.0 | |
AMK30-2927 | 20.5995 | -91.9666 | 1.500 | 1.40 | 1.60 | II | 806 | 35 | 11.30 | 4.3 | |
AMK30-2927 | 20.5995 | -91.9666 | 1.900 | 1.80 | 2.00 | II | 1085 | 200 | 73.30 | 18.4 | |
AMK30-2927 | 20.5995 | -91.9666 | 2.700 | 2.60 | 2.80 | III | 763 | 45 | 5.50 | 5.9 | |
AMK30-2927 | 20.5995 | -91.9666 | 3.200 | 3.10 | 3.30 | III | 884 | 165 | 21.80 | 2.3 | |
AMK30-2927 | 20.5995 | -91.9666 | 4.100 | 4.00 | 4.20 | III | 890 | 30 | 9.40 | 1.1 |