Schmitz, Birger (1987): (Table 1) Distribution of TiO2 in DSDP Leg 22 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.761014, Supplement to: Schmitz, B (1987): The TiO2/Al2O3 ratio in the Cenozoic Bengal Abyssal Fan sediments and its use as a paleostream energy indicator. Marine Geology, 76, 195-206, https://doi.org/10.1016/0025-3227(87)90029-6
Always quote citation above when using data! You can download the citation in several formats below.
Published: 1987 (exact date unknown) • DOI registered: 2011-06-23
Abstract:
The TiO2/Al2O3 ratio in the Cenozoic Bengal Abyssal Fan sediments displays decisive potential as a paleostream velocity indicator. The reason for this is that, even in the finest fan suspendates, hydrodynamic sorting determines the amounts of heavy TiO2-rich minerals relative to lighter Al2O3-rich clay minerals.
In five Deep Sea Drilling Project cores (213 - 217), which have been recovered in, and south of, the Bay of Bengal, TiO2/Al2O3 ratios increase linearly with time from the Late Miocene to Recent. The increase reflects fan progradation and intensified bottom current activity on the southern Bengal Fan. These processes are related to the Himalayan elevation by factors such as the maturation of northern India river systems, evolution of orographic monsoon rains and elevation-attributed increases in denudation rates.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: -1.725950 * Median Longitude: 90.115250 * South-bound Latitude: -11.336800 * West-bound Longitude: 86.791700 * North-bound Latitude: 8.926200 * East-bound Longitude: 93.896200
Date/Time Start: 1972-02-04T00:00:00 * Date/Time End: 1972-02-24T00:00:00
Minimum DEPTH, sediment/rock: 0.30 m * Maximum DEPTH, sediment/rock: 404.66 m
Event(s):
22-213 * Latitude: -10.211800 * Longitude: 93.896200 * Date/Time: 1972-02-04T00:00:00 * Elevation: -5601.0 m * Penetration: 163 m * Recovery: 143.6 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 163 m cored; 0 m drilled; 88.1 % recovery
22-214 * Latitude: -11.336800 * Longitude: 88.718000 * Date/Time: 1972-02-08T00:00:00 * Elevation: -1655.0 m * Penetration: 500 m * Recovery: 340.9 m * Location: Indian Ocean//RIDGE * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 53 cores; 492.5 m cored; 2.5 m drilled; 69.2 % recovery
22-215 * Latitude: -8.121700 * Longitude: 86.791700 * Date/Time: 1972-02-13T00:00:00 * Elevation: -5309.0 m * Penetration: 175 m * Recovery: 116 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 175 m cored; 0 m drilled; 66.3 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Epoch | Epoch | Schmitz, Birger | |||
| 4 | Titanium dioxide, normalized | TiO2* | Schmitz, Birger | Calculated | TiO2* = TiO2/Al2O3*15 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
468 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Epoch | 4 TiO2* |
|---|---|---|---|
| 22-213 | 0.30 | Quaternary | 0.608 |
| 22-213 | 0.81 | Quaternary | 0.617 |
| 22-213 | 2.00 | Quaternary | 0.595 |
| 22-213 | 2.40 | Quaternary | 0.604 |
| 22-213 | 3.25 | Quaternary | 0.610 |
| 22-213 | 3.72 | Quaternary | 0.655 |
| 22-213 | 5.22 | Quaternary | 0.616 |
| 22-213 | 9.72 | Quaternary | 0.561 |
| 22-213 | 14.20 | Late Pliocene | 0.610 |
| 22-213 | 19.22 | Late Pliocene | 0.615 |
| 22-213 | 20.62 | Late Pliocene | 0.599 |
| 22-213 | 20.72 | Late Pliocene | 0.605 |
| 22-213 | 20.81 | Late Pliocene | 0.614 |
| 22-213 | 24.95 | Late Pliocene | 0.633 |
| 22-213 | 30.22 | Late Pliocene | 0.605 |
| 22-213 | 31.72 | Late Pliocene | 0.591 |
| 22-213 | 36.20 | Late Pliocene | 0.605 |
| 22-213 | 41.17 | Early Pliocene | 0.615 |
| 22-213 | 42.72 | Early Pliocene | 0.572 |
| 22-213 | 45.72 | Early Pliocene | 0.552 |
| 22-213 | 50.75 | Early Pliocene | 0.566 |
| 22-213 | 52.22 | Early Pliocene | 0.589 |
| 22-213 | 55.00 | Early Pliocene | 0.527 |
| 22-213 | 58.72 | Late Miocene | 0.571 |
| 22-213 | 61.72 | Late Miocene | 0.574 |
| 22-213 | 68.18 | Late Miocene | 0.532 |
| 22-213 | 71.22 | Late Miocene | 0.545 |
| 22-213 | 74.22 | Late Miocene | 0.561 |
| 22-213 | 77.69 | Late Miocene | 0.535 |
| 22-213 | 80.68 | Late Miocene | 0.542 |
| 22-213 | 83.72 | Late Miocene | 0.518 |
| 22-213 | 87.22 | Middle Miocene | 0.517 |
| 22-213 | 90.18 | Middle Miocene | 0.471 |
| 22-213 | 93.17 | ? | 0.470 |
| 22-213 | 98.20 | ? | 0.575 |
| 22-213 | 99.78 | ? | 0.595 |
| 22-213 | 109.24 | ? | 0.655 |
| 22-213 | 112.20 | ? | 0.802 |
| 22-213 | 115.72 | ? | 0.931 |
| 22-213 | 118.73 | ? | 0.878 |
| 22-213 | 121.72 | ? | 0.753 |
| 22-213 | 125.22 | ? | 1.162 |
| 22-213 | 128.22 | ? | 0.809 |
| 22-213 | 129.71 | Early Eocene | 0.959 |
| 22-213 | 130.75 | Early Eocene | 0.828 |
| 22-213 | 131.45 | Early Eocene | 0.803 |
| 22-213 | 133.23 | Early Eocene | 0.738 |
| 22-213 | 136.19 | Early Eocene | 1.040 |
| 22-213 | 139.22 | Early Eocene | 0.974 |
| 22-213 | 140.72 | Early Eocene | 0.803 |
| 22-213 | 144.16 | Late Paleocene | 1.092 |
| 22-213 | 145.70 | Late Paleocene | 0.669 |
| 22-214 | 0.40 | Quaternary | 0.620 |
| 22-214 | 5.52 | Quaternary | 0.685 |
| 22-214 | 11.25 | Quaternary | 0.664 |
| 22-214 | 12.72 | Quaternary | 0.604 |
| 22-214 | 15.72 | Quaternary | 0.673 |
| 22-214 | 21.02 | Quaternary | 0.601 |
| 22-214 | 24.19 | Pliocene | 0.633 |
| 22-214 | 27.26 | Pliocene | 0.648 |
| 22-214 | 35.25 | Pliocene | 0.554 |
| 22-214 | 40.22 | Pliocene | 0.671 |
| 22-214 | 43.21 | Pliocene | 0.588 |
| 22-214 | 51.24 | Pliocene | 0.562 |
| 22-214 | 57.71 | Pliocene | 0.646 |
| 22-214 | 65.21 | Pliocene | 0.565 |
| 22-214 | 70.23 | Pliocene | 0.530 |
| 22-214 | 76.71 | Pliocene | 0.587 |
| 22-214 | 84.60 | Pliocene | 0.535 |
| 22-214 | 89.13 | Late Miocene | 0.563 |
| 22-214 | 97.26 | Late Miocene | 0.498 |
| 22-214 | 103.25 | Late Miocene | 0.506 |
| 22-214 | 108.23 | Late Miocene | 0.526 |
| 22-214 | 120.75 | Late Miocene | 0.504 |
| 22-214 | 127.35 | Late Miocene | 0.528 |
| 22-214 | 131.72 | Late Miocene | 0.529 |
| 22-214 | 136.68 | Late Miocene | 0.499 |
| 22-214 | 151.15 | Late Miocene | 0.543 |
| 22-214 | 156.22 | Middle Miocene | 0.575 |
| 22-214 | 164.22 | Middle Miocene | 0.643 |
| 22-214 | 168.68 | Middle Miocene | 0.570 |
| 22-214 | 175.22 | Middle Miocene | 0.473 |
| 22-214 | 181.22 | Middle Miocene | 0.452 |
| 22-214 | 184.66 | Middle Miocene | 0.461 |
| 22-214 | 192.68 | Middle Miocene | 0.591 |
| 22-214 | 194.18 | Middle Miocene | 0.583 |
| 22-214 | 200.90 | Early Miocene | 0.602 |
| 22-214 | 208.70 | Early Miocene | 0.803 |
| 22-214 | 216.17 | Early Miocene | 0.722 |
| 22-214 | 221.18 | Late Oligocene | 0.779 |
| 22-214 | 227.19 | Late Oligocene | 0.653 |
| 22-214 | 236.72 | Late Oligocene | 0.742 |
| 22-214 | 241.70 | Middle Oligocene | 0.907 |
| 22-214 | 246.21 | Middle Oligocene | 1.029 |
| 22-214 | 252.70 | Early Oligocene | 0.988 |
| 22-214 | 260.48 | Late Eocene | 1.077 |
| 22-214 | 282.22 | Late Eocene | 0.942 |
| 22-214 | 265.75 | Late Eocene | 0.852 |
| 22-214 | 270.22 | Middle Eocene | 1.095 |
| 22-214 | 274.22 | Middle Eocene | 0.903 |
| 22-214 | 281.22 | Middle Eocene | 0.956 |
| 22-214 | 288.60 | Middle Eocene | 1.018 |
| 22-214 | 290.72 | Middle Eocene | 1.014 |
| 22-214 | 297.35 | Middle Eocene | 1.045 |
| 22-214 | 303.22 | Middle Eocene | 1.067 |
| 22-214 | 309.74 | Early Eocene | 1.075 |
| 22-214 | 316.22 | Early Eocene | 1.113 |
| 22-214 | 322.22 | Early Eocene | 1.120 |
| 22-214 | 327.13 | Early Eocene | 2.732 |
| 22-214 | 335.23 | Late Paleocene | 3.652 |
| 22-214 | 343.19 | Paleocene | 1.984 |
| 22-214 | 365.32 | Paleocene | 2.140 |
| 22-215 | 0.72 | Quaternary | 0.588 |
| 22-215 | 2.18 | Quaternary | 0.618 |
| 22-215 | 3.74 | Quaternary | 0.591 |
| 22-215 | 5.20 | Quaternary | 0.601 |
| 22-215 | 6.72 | Late Pliocene | 0.563 |
| 22-215 | 8.03 | Late Pliocene | 0.575 |
| 22-215 | 10.22 | Late Pliocene | 0.554 |
| 22-215 | 19.23 | Early Pliocene | 0.529 |
| 22-215 | 22.22 | Early Pliocene | 0.544 |
| 22-215 | 25.19 | Early Pliocene | 0.547 |
| 22-215 | 27.22 | Early Pliocene | 0.473 |
| 22-215 | 30.23 | Early Pliocene | 0.521 |
| 22-215 | 33.23 | Early Pliocene | 0.496 |
| 22-215 | 34.73 | Early Pliocene | 0.468 |
| 22-215 | 36.72 | Late Miocene | 0.514 |
| 22-215 | 38.21 | Late Miocene | 0.450 |
| 22-215 | 39.75 | Late Miocene | 0.505 |
| 22-215 | 41.56 | Late Miocene | 0.485 |
| 22-215 | 46.70 | Late Miocene | 0.532 |
| 22-215 | 47.96 | Late Miocene | 0.675 |
| 22-215 | 49.22 | Late Miocene | 0.585 |
| 22-215 | 57.19 | Late Miocene | 0.508 |
| 22-215 | 65.54 | Late Miocene | 0.505 |
| 22-215 | 66.64 | Late Miocene | 0.499 |
| 22-215 | 68.00 | Late Miocene | 0.503 |
| 22-215 | 76.18 | Early Eocene | 0.874 |
| 22-215 | 77.17 | Early Eocene | 0.908 |
| 22-215 | 77.98 | Early Eocene | 0.905 |
| 22-215 | 85.72 | Early Eocene | 0.879 |
| 22-215 | 93.68 | Early Eocene | 0.687 |
| 22-215 | 98.18 | ? | 0.652 |
| 22-215 | 104.69 | Paleocene | 0.742 |
| 22-215 | 110.67 | Paleocene | 0.678 |
| 22-215 | 115.68 | Paleocene | 0.802 |
| 22-215 | 123.73 | Paleocene | 1.029 |
| 22-215 | 129.72 | Paleocene | 0.884 |
| 22-215 | 137.71 | Paleocene | 1.243 |
| 22-215 | 146.04 | Paleocene | 0.945 |
| 22-216 | 3.42 | Quaternary | 0.750 |
| 22-216 | 3.82 | Quaternary | 0.706 |
| 22-216 | 4.22 | Quaternary | 0.749 |
| 22-216 | 5.22 | Quaternary | 0.659 |
| 22-216 | 8.23 | Quaternary | 0.734 |
| 22-216 | 45.20 | Pliocene | 0.621 |
| 22-216 | 48.24 | Pliocene | 0.468 |
| 22-216 | 51.22 | Pliocene | 0.657 |
| 22-216 | 52.66 | Pliocene | 0.598 |
| 22-216 | 84.74 | Late Miocene | 0.568 |
| 22-216 | 122.72 | Middle Miocene | 0.598 |
| 22-216 | 124.22 | Middle Miocene | 0.616 |
| 22-216 | 128.72 | Middle Miocene | 0.598 |
| 22-216 | 162.20 | Eary Miocene | 0.480 |
| 22-216 | 165.20 | Eary Miocene | 0.471 |
| 22-216 | 166.77 | Eary Miocene | 0.475 |
| 22-216 | 170.20 | Eary Miocene | 0.493 |
| 22-216 | 176.28 | Eary Miocene | 0.456 |
| 22-216 | 178.18 | Late Oligocene | 0.481 |
| 22-216 | 189.17 | Late Oligocene | 0.476 |
| 22-216 | 189.72 | Late Oligocene | 0.475 |
| 22-216 | 197.06 | Late Oligocene | 0.512 |
| 22-216 | 198.78 | Late Oligocene | 0.520 |
| 22-216 | 206.93 | Late Oligocene | 0.477 |
| 22-216 | 226.17 | Late Oligocene | 0.482 |
| 22-216 | 247.23 | Oligocene | 0.524 |
| 22-216 | 247.68 | Oligocene | 0.540 |
| 22-216 | 254.34 | Oligocene | 0.457 |
| 22-216 | 255.73 | Oligocene | 0.375 |
| 22-216 | 264.22 | Middle Eocene | 0.556 |
| 22-216 | 285.34 | Middle Eocene | 0.436 |
| 22-216 | 273.26 | Middle Eocene | 0.450 |
| 22-216 | 274.84 | Middle Eocene | 0.494 |
| 22-216 | 303.22 | Paleocene | 1.097 |
| 22-216 | 304.72 | Paleocene | 1.111 |
| 22-216 | 311.60 | Paleocene | 0.985 |
| 22-216 | 312.66 | Paleocene | 0.964 |
| 22-216 | 321.05 | Middle Paleocene | 0.969 |
| 22-216 | 322.18 | Middle Paleocene | 0.952 |
| 22-217 | 0.34 | Quaternary | 0.746 |
| 22-217 | 2.24 | Quaternary | 0.749 |
| 22-217 | 3.44 | Quaternary | 0.719 |
| 22-217 | 5.22 | Quaternary | 0.713 |
| 22-217 | 8.02 | Quaternary | 0.737 |
| 22-217 | 42.56 | Early Pliocene | 0.613 |
| 22-217 | 43.63 | Early Pliocene | 0.605 |
| 22-217 | 45.22 | Early Pliocene | 0.624 |
| 22-217 | 70.75 | Late Miocene | 0.569 |
| 22-217 | 72.22 | Late Miocene | 0.597 |
| 22-217 | 119.73 | Late Miocene | 0.626 |
| 22-217 | 122.72 | Late Miocene | 0.649 |
| 22-217 | 124.23 | Late Miocene | 0.621 |
| 22-217 | 183.40 | Middle Miocene | 0.656 |
| 22-217 | 184.90 | Middle Miocene | 0.649 |
| 22-217 | 186.60 | Middle Miocene | 0.621 |
| 22-217 | 187.90 | Middle Miocene | 0.624 |
| 22-217 | 190.90 | Early Miocene | 0.611 |
| 22-217 | 232.47 | Oligocene | 0.625 |
| 22-217 | 233.73 | Oligocene | 0.570 |
| 22-217 | 236.73 | Oligocene | 0.592 |
| 22-217 | 237.74 | Oligocene | 0.589 |
| 22-217 | 238.38 | Oligocene | 0.634 |
| 22-217 | 268.81 | Late Oligocene | 0.595 |
| 22-217 | 271.68 | Late Oligocene | 0.616 |
| 22-217 | 276.18 | Late Oligocene | 0.575 |
| 22-217 | 306.70 | Middle Oligocene | 0.553 |
| 22-217 | 309.68 | Middle Oligocene | 0.491 |
| 22-217 | 311.16 | Middle Oligocene | 0.503 |
| 22-217 | 314.22 | Late Eocene | 0.539 |
| 22-217 | 346.34 | Middle Eocene | 0.596 |
| 22-217 | 347.74 | Middle Eocene | 0.594 |
| 22-217 | 350.78 | Middle Eocene | 0.585 |
| 22-217 | 394.63 | Middle Paleocene | 0.846 |
| 22-217 | 396.18 | Middle Paleocene | 0.959 |
| 22-217 | 397.67 | Middle Paleocene | 0.909 |
| 22-217 | 399.24 | Middle Paleocene | 0.941 |
| 22-217 | 403.83 | Paleocene | 0.898 |
| 22-217 | 404.66 | Paleocene | 1.383 |
| 22-217A | 2.22 | Quaternary | 0.743 |
| 22-217A | 5.28 | Quaternary | 0.710 |
| 22-217A | 11.91 | Quaternary | 0.702 |
| 22-217A | 24.15 | Late Pliocene | 0.715 |
| 22-217A | 31.22 | Late Pliocene | 0.635 |
| 22-217A | 32.72 | Late Pliocene | 0.563 |
