Howe, Jacob N W; Piotrowski, Alexander M; Hu, Rong; Bory, Aloys J-M (2017): (Table A6) Uncleaned planktic foraminiferal and detrital epsilon-Nd from sediment core BOFS30/3K [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.874892, In supplement to: Howe, JNW et al. (2017): Reconstruction of east–west deep water exchange in the low latitude Atlantic Ocean over the past 25,000 years. Earth and Planetary Science Letters, 458, 327-336, https://doi.org/10.1016/j.epsl.2016.10.048
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Project(s):
Coverage:
Latitude: 22.545600 * Longitude: -21.999700
Date/Time Start: 1990-10-21T00:00:00 * Date/Time End: 1990-10-21T00:00:00
Event(s):
BOFS32/4K (BOFS32#4) * Latitude: 22.545600 * Longitude: -21.999700 * Date/Time: 1990-10-21T00:00:00 * Location: Northeast Atlantic * Campaign: CD53 * Basis: Charles Darwin * Method/Device: Kasten corer (KAL) * Comment: BOFS-ID 18726
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Depth, composite | Depth comp | mcd | Howe, Jacob N W | ||
| 2 | AGE | Age | ka BP | Howe, Jacob N W | Geocode | |
| 3 | ε-Neodymium | ε-Nd | Howe, Jacob N W | |||
| 4 | ε-Neodymium, standard deviation | ε-Nd std dev | ± | Howe, Jacob N W | 2 sigma, external | |
| 5 | ε-Neodymium, standard deviation | ε-Nd std dev | ± | Howe, Jacob N W | 2 sigma, internal | |
| 6 | ε-Neodymium, standard deviation | ε-Nd std dev | ± | Howe, Jacob N W |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
45 data points
Data
| 1 Depth comp [mcd] | 2 Age [ka BP] | 3 ε-Nd | 4 ε-Nd std dev [±] (2 sigma, external) | 5 ε-Nd std dev [±] (2 sigma, internal) | 6 ε-Nd std dev [±] |
|---|---|---|---|---|---|
| 0.00 | 3.60 | -11.9 | 0.210 | 0.100 | 0.21 |
| 0.13 | 7.40 | -12.0 | 0.210 | 0.100 | 0.21 |
| 0.17 | 9.60 | -11.8 | 0.140 | 0.070 | 0.14 |
| 0.21 | 11.40 | -11.5 | 0.140 | 0.090 | 0.14 |
| 0.26 | 13.60 | -11.2 | 0.210 | 0.100 | 0.21 |
| 0.31 | 15.90 | -10.7 | 0.140 | 0.090 | 0.14 |
| 0.36 | 18.30 | -10.4 | 0.140 | 0.110 | 0.14 |
| 0.47 | 23.30 | -10.2 | 0.140 | 0.100 | 0.14 |
| 0.55 | 27.00 | -10.7 | 0.210 | 0.100 | 0.21 |