Bijl, Peter K; Schouten, Stefan; Sluijs, Appy; Reichart, Gert-Jan; Zachos, James C; Brinkhuis, Henk (2009): (Table S1) Age model of ODP Site 189-1172 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.769677, In supplement to: Bijl, PK et al. (2009): Early Palaeogene temperature evolution of the southwest Pacific Ocean. Nature, 461, 776-779, https://doi.org/10.1038/nature08399
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -43.959517 * Longitude: 149.928433
Date/Time Start: 2000-04-22T00:00:00 * Date/Time End: 2000-04-22T00:00:00
Minimum DEPTH, sediment/rock: 357.300 m * Maximum DEPTH, sediment/rock: 736.600 m
Event(s):
189-1172 * Latitude: -43.959517 * Longitude: 149.928433 * Date/Time: 2000-04-22T00:00:00 * Elevation: -2621.9 m * Penetration: 1662.5 m * Recovery: 1100.2 m * Location: Tasman Sea * Campaign: Leg189 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 127 cores; 1193.9 m cored; 468.6 m drilled; 92.1% recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Age, comment | Comm | Bijl, Peter K | |||
| 2 | Ageprofile Datum Description | Ageprof dat des | Bijl, Peter K | O = onset, T = termination | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 4 | Age model | Age model | ka | Bijl, Peter K |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
120 data points
Data
| 1 Comm | 2 Ageprof dat des | 3 Depth sed [m] | 4 Age model [ka] |
|---|---|---|---|
| magnetic recersal | T C11n.2n | 357.300 | 29853 |
| magnetic recersal | O C11n.2n | 358.600 | 30217 |
| magnetic recersal | T C13n | 358.800 | 33270 |
| magnetic recersal | O C13n | 358.900 | 33740 |
| magnetic recersal | T C15n | 359.700 | 34780 |
| magnetic recersal | O C15n | 359.900 | 35040 |
| magnetic recersal | T C16n.1n | 360.100 | 35400 |
| magnetic recersal | O C16n.1n | 361.300 | 35570 |
| magnetic recersal | T C16n.2n | 361.500 | 35710 |
| magnetic recersal | O C16n.2n | 365.000 | 36280 |
| magnetic recersal | T C17n | 367.100 | 36510 |
| magnetic recersal | O C17n | 373.900 | 37550 |
| magnetic recersal | T C18n.1n | 382.100 | 38032 |
| magnetic recersal | O C18n.2n | 432.000 | 39460 |
| magnetic recersal | T C19n | 444.000 | 40440 |
| magnetic recersal | O C19n | 456.000 | 40670 |
| magnetic recersal | T C20n | 500.000 | 41590 |
| magnetic recersal | O C20n | 519.000 | 42770 |
| magnetic recersal | T C21n | 526.400 | 45350 |
| magnetic recersal | O C21n | 540.000 | 47240 |
| magnetic recersal | T C22n | 555.900 | 48600 |
| magnetic recersal | O C22n | 570.000 | 49430 |
| magnetic recersal | T C23n | 581.000 | 50730 |
| magnetic recersal | O C23n | 585.000 | 51900 |
| magnetic recersal | T C24n | 585.010 | 52730 |
| magnetic recersal | O C24n | 594.200 | 53530 |
| isotope event | T PETM | 610.800 | 54850 |
| isotope event | O PETM | 611.800 | 55000 |
| magnetic recersal | T C25n | 618.000 | 56650 |
| magnetic recersal | O C26n | 634.800 | 58700 |
| magnetic recersal | T C27n | 670.000 | 61650 |
| magnetic recersal | O C27n | 670.750 | 61983 |
| magnetic recersal | T C28n | 685.000 | 63104 |
| magnetic recersal | O C28n | 685.010 | 64128 |
| magnetic recersal | T C29n | 692.600 | 64432 |
| magnetic recersal | O C29n | 695.990 | 65118 |
| magnetic recersal | T C30n | 695.991 | 65861 |
| magnetic recersal | O C30n | 709.100 | 67696 |
| magnetic recersal | T C31n | 713.300 | 67809 |
| magnetic recersal | O C31n | 736.600 | 68732 |