Kirillova, Valeriia; Osborne, Anne H; Störling, Tjördis; Frank, Martin (2019): (Table 2a) Neodymium isotopic results for ODP Site 166-1006A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.904245, In supplement to: Kirillova, V et al. (2019): Miocene restriction of the Pacific-North Atlantic throughflow strengthened Atlantic overturning circulation. Nature Communications, 10(1), https://doi.org/10.1038/s41467-019-12034-7
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Coverage:
Latitude: 24.399800 * Longitude: -79.459000
Date/Time Start: 1996-03-20T05:54:00 * Date/Time End: 1996-03-24T04:40:00
Minimum DEPTH, sediment/rock: 4.22 m * Maximum DEPTH, sediment/rock: 673.57 m
Event(s):
166-1006A * Latitude: 24.399800 * Longitude: -79.459000 * Date/Time Start: 1996-03-20T05:54:00 * Date/Time End: 1996-03-24T04:40:00 * Elevation: -657.9 m * Penetration: 717.3 m * Recovery: 646.93 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 77 cores; 717.3 m cored; 0 m drilled; 90.2 % recovery
Comment:
(a) age model Kroon D, Williams T, Pirmez C, Spezzaferri S, Sato T, Wright JD. Coupled Early Pliocene-Middle Miocene bio-cyclostratigrahy of Site 1006 reveals orbitally induced cyclicity patterns of Great Bahama Bank carbonate production. Proc ODP, Scientific Results 166, 155-166 (2000).
(b) corrected to Tanaka T, et al. Jndi-1: a neodymium isotopic reference in consistency with LaJolla neodymium. Chemical Geology 168, 279-281 (2000).
(c) corrected for ingrowth of 143Nd using Sm/Nd ratio of 0.139 for foraminiferal calcite Osborne AH, Hathorne EC, Schijf J, Plancherel Y, Boning P, Frank M. The potential of sedimentary foraminiferal rare earth element patterns to trace water masses in the past. Geochemistry Geophysics Geosystems 18, 1550-1568 (2017).
(d) corrected for ingrowth of 143Nd using Sm/Nd ratio of 0.109 for detrital material, based on the average upper crustal ratio Taylor SR, McLennan SM. The Continental Crust: Its Composition and Evolution. Blackwell Scientific Publications (1985).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample ID | Sample ID | Osborne, Anne H | |||
| 2 | DEPTH, sediment/rock | Depth sed | m | Osborne, Anne H | Geocode | |
| 3 | Age model | Age model | ka | Osborne, Anne H | (a) | |
| 4 | Neodymium-143/Neodymium-144 ratio | 143Nd/144Nd | Osborne, Anne H | (b); Uncleaned Planktonic Foraminifera | ||
| 5 | ε-Neodymium (0) | ε-Nd(0) | Osborne, Anne H | Uncleaned Planktonic Foraminifera | ||
| 6 | ε-Neodymium (T) | ε-Nd(T) | Osborne, Anne H | (c); Uncleaned Planktonic Foraminifera | ||
| 7 | Foraminifera, planktic ε-Neodymium, standard deviation | Foram plankt ε-Nd std dev | ± | Osborne, Anne H | 2σ; Uncleaned Planktonic Foraminifera | |
| 8 | Neodymium-143/Neodymium-144 ratio | 143Nd/144Nd | Osborne, Anne H | (b); Detrital material | ||
| 9 | ε-Neodymium (0) | ε-Nd(0) | Osborne, Anne H | Detrital material | ||
| 10 | ε-Neodymium (T) | ε-Nd(T) | Osborne, Anne H | (d); Detrital material | ||
| 11 | ε-Neodymium, standard deviation | ε-Nd std dev | ± | Osborne, Anne H | 2σ; Detrital material |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
292 data points
Data
| 1 Sample ID | 2 Depth sed [m] | 3 Age model [ka] ((a)) | 4 143Nd/144Nd ((b); Uncleaned Planktonic For...) | 5 ε-Nd(0) (Uncleaned Planktonic Foramini...) | 6 ε-Nd(T) ((c); Uncleaned Planktonic For...) | 7 Foram plankt ε-Nd std dev [±] (2σ; Uncleaned Planktonic Fora...) | 8 143Nd/144Nd ((b); Detrital material) | 9 ε-Nd(0) (Detrital material) | 10 ε-Nd(T) ((d); Detrital material) | 11 ε-Nd std dev [±] (2σ; Detrital material) |
|---|---|---|---|---|---|---|---|---|---|---|
| 1006A-1H-3 122-122 | 4.22 | 250 | 0.512137 | -9.78 | -9.78 | 0.98 | 0.512122 | -10.10 | -10.06 | 0.40 |
| 1006A-5H-3 93-95 | 39.53 | 850 | 0.512131 | -9.89 | -9.88 | 0.98 | 0.512088 | -10.70 | -10.72 | 0.40 |
| 1006A-10H-6 118-120 | 91.78 | 1720 | 0.512190 | -8.73 | -8.72 | 0.98 | ||||
| 1006A-15H-750-52 | 140.00 | 2630 | 0.512233 | -7.91 | -7.89 | 0.98 | 0.512177 | -9.00 | -8.96 | 0.40 |
| 1006A-17H-4 90-92 | 155.00 | 2990 | 0.512266 | -7.27 | -7.24 | 0.98 | 0.512197 | -8.60 | -8.57 | 0.40 |
| 1006A-18H-5 40-42 | 165.50 | 3390 | 0.512242 | -7.73 | -7.71 | 0.98 | 0.512155 | -9.40 | -9.38 | 0.40 |
| 1006A-21H-2 90-92 | 190.00 | 3790 | 0.512207 | -8.40 | -8.37 | 0.98 | ||||
| 1006A-24H-4 40-42 | 221.00 | 4030 | 0.512319 | -6.22 | -6.19 | 0.98 | 0.512286 | -6.90 | -6.82 | 0.40 |
| 1006A-27H-4 90-92 | 250.00 | 4210 | 0.512279 | -7.00 | -6.96 | 0.40 | ||||
| 1006A-38X-4 85-87 | 345.15 | 4780 | 0.512267 | -7.24 | -7.20 | 0.98 | 0.512274 | -7.10 | -7.05 | 0.40 |
| 1006A-41X-4 35-37 | 372.15 | 5330 | 0.512207 | -8.40 | -8.36 | 0.98 | 0.512205 | -8.40 | -8.39 | 0.40 |
| 1006A-43X-145-47 | 385.55 | 5600 | 0.512294 | -6.71 | -6.67 | 0.98 | ||||
| 1006A-46X-6 46-48 | 421.36 | 6060 | 0.512332 | -5.97 | -5.92 | 0.98 | 0.512323 | -6.10 | -6.08 | 0.40 |
| 1006A-50X-6 85-87 | 458.45 | 6400 | 0.512291 | -6.77 | -6.72 | 0.98 | 0.512213 | -8.30 | -8.22 | 0.40 |
| 1006A-51X-1 20-22 | 459.50 | 6840 | 0.512183 | -8.89 | -8.84 | 0.98 | 0.512234 | -7.90 | -7.80 | 0.40 |
| 1006A-52X-4 85-87 | 474.55 | 7520 | 0.512201 | -8.52 | -8.46 | 0.98 | 0.512091 | -10.70 | -10.59 | 0.40 |
| 1006A-54X-6 85-87 | 495.55 | 8100 | 0.512278 | -7.02 | -6.96 | 0.98 | 0.512265 | -7.30 | -7.19 | 0.40 |
| 1006A-60X-3 85-87 | 547.75 | 8500 | 0.512263 | -7.31 | -7.25 | 0.98 | 0.512256 | -7.40 | -7.36 | 0.40 |
| 1006A-60X-5 50-52 | 550.40 | 8700 | 0.512260 | -7.38 | -7.32 | 0.66 | 0.512278 | -7.02 | -6.93 | 0.21 |
| 1006A-61X-2 50-52 | 555.50 | 9080 | 0.512294 | -6.72 | -6.65 | 0.66 | 0.512246 | -7.65 | -7.54 | 0.21 |
| 1006A-61X-5 85-87 | 560.35 | 9450 | 0.512284 | -6.90 | -6.83 | 0.98 | ||||
| 1006A-62X-2 50-52 | 565.20 | 9810 | 0.512252 | -7.53 | -7.45 | 0.33 | 0.512241 | -7.74 | -7.63 | 0.21 |
| 1006A-62X-5 50-52 | 569.70 | 10150 | 0.512227 | -8.01 | -7.94 | 0.41 | 0.512269 | -7.20 | -7.08 | 0.39 |
| 1006A-63X-1 85-87 | 573.65 | 10450 | 0.512270 | -7.20 | -7.06 | 0.40 | ||||
| 1006A-63X-4 50-52 | 577.80 | 10760 | 0.512217 | -8.21 | -8.13 | 0.33 | 0.512204 | -8.46 | -8.34 | 0.21 |
| 1006A-64X1 50-52 | 582.90 | 11150 | 0.512262 | -7.33 | -7.25 | 0.66 | ||||
| 1006A-65X-3 50-52 | 595.60 | 11510 | 0.512258 | -7.41 | -7.32 | 0.33 | 0.512220 | -8.15 | -8.02 | 0.21 |
| 1006A-67X-3 50-52 | 614.90 | 11720 | 0.512372 | -5.18 | -5.10 | 0.33 | ||||
| 1006A-68X-1 85-87 | 621.85 | 11800 | 0.512324 | -6.12 | -6.04 | 0.98 | 0.512245 | -7.70 | -7.53 | 0.40 |
| 1006A-69X-1 50-52 | 631.10 | 11870 | 0.512346 | -5.70 | -5.56 | 0.21 | ||||
| 1006A-70X-CC 30-32 | 640.50 | 11940 | 0.512327 | -6.06 | -5.97 | 0.41 | ||||
| 1006A-72X-1 50-52 | 660.00 | 12090 | 0.512301 | -6.57 | -6.48 | 0.33 | 0.512195 | -8.65 | -8.51 | 0.21 |
| 1006A-72X-2 70-72 | 661.70 | 12100 | 0.512396 | -4.72 | -4.63 | 0.98 | ||||
| 1006A-73X-3 137-139 | 673.57 | 12500 | 0.512197 | -8.60 | -8.46 | 0.40 |