Hodell, David A; Mueller, Paul A; McKenzie, Judith A; Mead, Gregory (1989): (Table 1) 87Sr/86Sr ratios of planktonic foraminifera from DSDP Hole 90-588 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.712322, In supplement to: Hodell, DA et al. (1989): Strontium isotope stratigraphy and geochemistry of the late Neogene ocean. Earth and Planetary Science Letters, 92(2), 165-178, https://doi.org/10.1016/0012-821X(89)90044-7
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -26.111700 * Longitude: 161.226700
Date/Time Start: 1982-12-06T00:00:00 * Date/Time End: 1982-12-06T00:00:00
Minimum DEPTH, sediment/rock: 22.30 m * Maximum DEPTH, sediment/rock: 217.15 m
Event(s):
90-588 * Latitude: -26.111700 * Longitude: 161.226700 * Date/Time: 1982-12-06T00:00:00 * Elevation: -1533.0 m * Penetration: 245.6 m * Recovery: 220.8 m * Location: South Pacific/Tasman Sea/CONT RISE * Campaign: Leg90 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 226.4 m cored; 19.2 m drilled; 97.5 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | AGE | Age | ka BP | Geocode | ||
| 3 | Sample code/label | Sample label | Hodell, David A | DSDP/ODP/IODP sample designation | ||
| 4 | Strontium-87/Strontium-86 ratio | 87Sr/86Sr | Hodell, David A | normalized to the SRM-987 standard = 0.710235 and to 86Sr/8sSr = 0.1194 | ||
| 5 | Strontium-87/Strontium-86 ratio, error | 87Sr/86Sr e | ± | Hodell, David A | 2 standard errors of the mean of 100-200 individual measurements | |
| 6 | δ87Sr | δ87Sr | Hodell, David A | d87Sr = [(87Sr/86Sr)sample/(87Sr/86Sr)seawater - 1] x 10**5 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
84 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 Sample label | 4 87Sr/86Sr | 5 87Sr/86Sr e [±] | 6 δ87Sr |
|---|---|---|---|---|---|
| 22.30 | 2000 | 90-588-3-5,110 | 0.709070 | 0.000006 | -14.8 |
| 23.05 | 2060 | 90-588-3-6,35 | 0.709046 | 0.000005 | -18.2 |
| 46.30 | 3400 | 90-588-6-2,80 | 0.709035 | 0.000005 | -19.7 |
| 50.35 | 3460 | 90-588-6-5,35 | 0.709046 | 0.000005 | -18.2 |
| 79.91 | 3880 | 90-588-9-5,110 | 0.709044 | 0.000005 | -18.5 |
| 86.50 | 4340 | 90-588-10-3,110 | 0.709031 | 0.000010 | -20.3 |
| 86.50 | 4340 | 90-588-10-3,110 | 0.709029 | 0.000011 | -20.6 |
| 90.25 | 4470 | 90-588-10-6,35 | 0.709021 | 0.000011 | -21.7 |
| 103.45 | 4920 | 90-588-12-2,35 | 0.709030 | 0.000007 | -20.5 |
| 107.20 | 5020 | 90-588-12-4,110 | 0.709004 | 0.000008 | -24.1 |
| 107.20 | 5020 | 90-588-12-4,110 | 0.708989 | 0.000008 | -26.2 |
| 114.55 | 5180 | 90-588-13-3,36 | 0.709039 | 0.000010 | -19.2 |
| 114.55 | 5180 | 90-588-13-3,36 | 0.708998 | 0.000009 | -25.0 |
| 124.15 | 5410 | 90-588-14-3,35 | 0.709006 | 0.000007 | -23.8 |
| 125.65 | 5450 | 90-588-14-4,35 | 0.708948 | 0.000009 | -32.0 |
| 125.65 | 5450 | 90-588-14-4,35 | 0.708931 | 0.000008 | -34.4 |
| 145.60 | 5990 | 90-588-16-4,111 | 0.708929 | 0.000009 | -34.7 |
| 145.60 | 5990 | 90-588-16-4,111 | 0.708901 | 0.000011 | -38.6 |
| 169.30 | 6630 | 90-588-19-1,50 | 0.708946 | 0.000009 | -32.3 |
| 205.45 | 8210 | 90-588-22-6,35 | 0.708923 | 0.000010 | -35.5 |
| 217.15 | 8800 | 90-588-24-1,35 | 0.708922 | 0.000008 | -35.7 |