Channell, James E T (2020): Age model of IODP Site 303-U1305 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.919737, In: Channell, JET (2020): Age model, RPI and VGP from IODP Sites 303-U1304, 303-U1305 and 303-U1306 at the Matuyama-Brunhes boundary [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.919883
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Channell, James E T (2017): Complexity in Matuyama–Brunhes polarity transitions from North Atlantic IODP/ODP deep-sea sites. Earth and Planetary Science Letters, 467, 43-56, https://doi.org/10.1016/j.epsl.2017.03.019
Further details:
Hillaire-Marcel, Claude; de Vernal, Anne; McKay, Jennifer L (2011): Foraminifer isotope study of the Pleistocene Labrador Sea, northwest North Atlantic (IODP Sites 1302/03 and 1305), with emphasis on paleoceanographical differences between its “inner” and “outer” basins. Marine Geology, 279(1-4, 188-198, https://doi.org/10.1016/j.margeo.2010.11.001
Project(s):
Coverage:
Latitude: 57.475150 * Longitude: -48.529710
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 170.80 m
Event(s):
303-U1305 * Latitude: 57.475150 * Longitude: -48.529710 * Elevation: -3460.0 m * Location: Northwest Atlantic * Campaign: Exp303 (North Atlantic Climate 1) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Channell, James E T | Geocode – mcd | |
| 2 | Age model | Age model | ka | Channell, James E T | Age model, composite | see Hillaire-Marcel et al. (2011) |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
32 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0 |
| 10.03 | 14 |
| 13.00 | 29 |
| 17.00 | 57 |
| 18.50 | 71 |
| 24.90 | 115 |
| 32.00 | 130 |
| 35.09 | 191 |
| 48.31 | 243 |
| 56.00 | 300 |
| 61.99 | 337 |
| 65.15 | 374 |
| 78.13 | 424 |
| 80.58 | 478 |
| 96.50 | 533 |
| 99.10 | 563 |
| 109.00 | 621 |
| 112.00 | 676 |
| 122.50 | 712 |
| 127.50 | 761 |
| 127.90 | 780 |
| 132.00 | 790 |
| 133.50 | 814 |
| 141.00 | 866 |
| 149.00 | 936 |
| 153.20 | 959 |
| 154.51 | 970 |
| 157.20 | 990 |
| 161.89 | 1031 |
| 165.91 | 1062 |
| 168.35 | 1070 |
| 170.80 | 1081 |