Cronan, David S; van Andel, Tjeerd H; Heath, G Ross; Dinkelman, Menno G; Bennett, Richard H; Bukry, David; Kaneps, Ansis G; Rodolfo, Kelvin S; Yeats, Robert S (1972): (Table 1) Composition of basal sediments collected during DSDP Leg 16 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.772167, Supplement to: Cronan, DS et al. (1972): Iron-rich basal sediments from the eastern Equatorial Pacific: Leg 16, Deep Sea Drilling Project. Science, 175(4017), 61-63, https://doi.org/10.1126/science.175.4017.61
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Abstract:
Iron-rich sediments chemically similar to those forming at present on the crest of the East Pacific Rise have been found just above basement at widely separated drill sites in the eastern equatorial Pacific, including three sites of Leg 16 of the Deep Sea Drilling Project. These sediments were probably formed when the basement was at the crest of this rise and have moved to their present location as a result of sea-floor spreading.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 12.394375 * Median Longitude: -133.291500 * South-bound Latitude: 10.671200 * West-bound Longitude: -140.043500 * North-bound Latitude: 14.869800 * East-bound Longitude: -122.287800
Date/Time Start: 1971-03-01T00:00:00 * Date/Time End: 1971-03-15T00:00:00
Minimum DEPTH, sediment/rock: 9 m * Maximum DEPTH, sediment/rock: 238 m
Event(s):
16-159 * Latitude: 12.332000 * Longitude: -122.287800 * Date/Time: 1971-03-01T00:00:00 * Elevation: -4484.0 m * Penetration: 245.1 m * Recovery: 90.8 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 99.1 m cored; 10 m drilled; 91.6 % recovery
16-160 * Latitude: 11.704500 * Longitude: -130.880200 * Date/Time: 1971-03-05T00:00:00 * Elevation: -4940.0 m * Penetration: 114 m * Recovery: 94.9 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 114 m cored; 0 m drilled; 83.2 % recovery
16-161A * Latitude: 10.671200 * Longitude: -139.954500 * Date/Time: 1971-03-09T00:00:00 * Elevation: -4939.0 m * Penetration: 245.1 m * Recovery: 87.5 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 126.1 m cored; 0 m drilled; 69.4 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Cronan, David S | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 4 | Height | Height | m | Cronan, David S | above basalt | |
| 5 | Iron | Fe | % | Cronan, David S | ||
| 6 | Manganese | Mn | % | Cronan, David S | ||
| 7 | Nickel | Ni | mg/kg | Cronan, David S | ||
| 8 | Cobalt | Co | mg/kg | Cronan, David S | ||
| 9 | Copper | Cu | mg/kg | Cronan, David S | ||
| 10 | Lead | Pb | mg/kg | Cronan, David S | ||
| 11 | Zinc | Zn | mg/kg | Cronan, David S | ||
| 12 | Epoch | Epoch | Cronan, David S | |||
| 13 | Lithology/composition/facies | Lithology | Cronan, David S |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
220 data points
Data
| 1 Event | 2 Sample label | 3 Depth sed [m] | 4 Height [m] | 5 Fe [%] | 6 Mn [%] | 7 Ni [mg/kg] | 8 Co [mg/kg] | 9 Cu [mg/kg] | 10 Pb [mg/kg] | 11 Zn [mg/kg] | 12 Epoch | 13 Lithology |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 16-159 | 16-159-2-1,38-43 | 9 | 99 | 4.74 | 0.72 | 336 | 183 | 816 | 40 | 219 | Late Miocene | Radiolarian clay |
| 16-159 | 16-159-10-6,90-95 | 89 | 19 | 18.27 | 4.60 | 438 | 78 | 1044 | 130 | 443 | Early Miocene | Nannofossil marl |
| 16-159 | 16-159-12-1,25-30 | 99 | 9 | 16.77 | 4.48 | 472 | 76 | 762 | 122 | 427 | Early Miocene | Nannofossil marl |
| 16-159 | 16-159-12-6,103-108 | 107 | 1 | 19.10 | 5.15 | 496 | 95 | 840 | 152 | 458 | Early Miocene | Nannofossil marl |
| 16-159 | 16-159-13-2,95-100 | 107 | 1 | 15.96 | 3.56 | 385 | 79 | 611 | 106 | 518 | Early Miocene | Nannofossil marl |
| 16-159 | 16-159-13-4,133-137 | 108 | 0 | 15.96 | 3.16 | 345 | 79 | 744 | 106 | 438 | Early Miocene | Nannofossil marl |
| 16-160 | 16-160-3-4,78-83 | 23 | 86 | 6.42 | 1.10 | 187 | 64 | 749 | 42 | 230 | Early Miocene | Zeolitic clay |
| 16-160 | 16-160-10-6,125-130 | 90 | 19 | 2.06 | 0.36 | 243 | 121 | 364 | 304 | 206 | Early Oligocene | Nannofossil chalk ooze |
| 16-160 | 16-160-11-6,135-140 | 99 | 10 | 2.29 | 0.36 | 241 | 120 | 362 | 302 | 205 | Early Oligocene | Nannofossil chalk ooze |
| 16-160 | 16-160-12-5,135-140 | 106 | 3 | 3.09 | 0.35 | 158 | 71 | 431 | 179 | 179 | Early Oligocene | Nannofossil chalk ooze |
| 16-160 | 16-160-13-1,99-103 | 109 | 0 | 8.52 | 1.86 | 994 | 56 | 994 | 56 | 262 | Early Oligocene | Nannofossil marl |
| 16-161A | 16-161A-12-1,59-64 | 218 | 26 | 5.94 | 1.04 | 113 | 27 | 475 | 34 | 183 | Late Eocene | Radiolarian ooze |
| 16-161A | 16-161A-12-1,139-144 | 219 | 25 | 6.48 | 1.09 | 108 | 27 | 536 | 37 | 189 | Late Eocene | Radiolarian ooze |
| 16-161A | 16-161A-13-1,136-141 | 227 | 17 | 3.91 | 0.84 | 61 | 20 | 350 | 29 | 95 | Late Eocene | Radiolarian ooze |
| 16-161A | 16-161A-14-1,148-150 | 236 | 8 | 4.74 | 1.10 | 169 | 33 | 508 | 58 | 183 | Middle Eocene | Radiolarian ooze |
| 16-161A | 16-161A-14-2,149-151 | 238 | 6 | 4.48 | 0.92 | 105 | 17 | 402 | 34 | 149 | Middle Eocene | Radiolarian ooze |
| 16-162 | 16-162-12-2,104-109 | 102 | 51 | 6.04 | 0.63 | 56 | 12 | 226 | 31 | 126 | Middle Eocene | Clayey marl ooze |
| 16-162 | 16-162-16-3,76-81 | 138 | 25 | 3.87 | 1.03 | 86 | 15 | 244 | 28 | 91 | Middle Eocene | Clayey radiolarian ooze |
| 16-162 | 16-162-17-1,62-67 | 145 | 8 | 19.42 | 7.10 | 488 | 99 | 1498 | 149 | 33 | Middle Eocene | Ferruginous clay |
| 16-162 | 16-162-17-4,101-106 | 150 | 3 | 30.56 | 9.55 | 1680 | 171 | 1814 | 229 | 515 | Middle Eocene | Clayey marl |