Kirby, Nicola; Bailey, Ian; Lang, David C; Brombacher, Anieke; Chalk, Thomas B; Parker, Rebecca L; Crocker, Anya J; Taylor, Victoria E; Milton, J Andy; Foster, Gavin L; Raymo, Maureen E; Kroon, Dick; Bell, David B; Wilson, Paul A (2020): Neodymium isotopes of fish debris from IODP Site 306-U1313 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.925558, In: Kirby, N et al. (2020): Neodymium isotopes, B/Ca and δ¹³C, and fresh sand volcanic glass count data from ODP Site 208-1267 and IODP Site 306-U1313 for MIS M2, MIS 100 and the Last Glacial-Holocene [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.925562
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Abstract:
Fish debris Nd isotope data from IODP Site U1313 for Marine Isotope Stage (MIS) M2 and MIS 100.
Related to:
Kirby, Nicola; Bailey, Ian; Lang, David C; Brombacher, Anieke; Chalk, Thomas B; Parker, Rebecca L; Crocker, Anya J; Taylor, Victoria E; Milton, J Andy; Foster, Gavin L; Raymo, Maureen E; Kroon, Dick; Bell, David B; Wilson, Paul A (2020): On climate and abyssal circulation in the Atlantic Ocean during late Pliocene marine isotope stage M2, ∼3.3 million years ago. Quaternary Science Reviews, 250, 106644, https://doi.org/10.1016/j.quascirev.2020.106644
Lang, David C; Bailey, Ian; Wilson, Paul A; Chalk, Thomas B; Foster, Gavin L; Gutjahr, Marcus (2016): Incursions of southern-sourced water into the deep North Atlantic during late Pliocene glacial intensification. Nature Geoscience, 9(5), 375-379, https://doi.org/10.1038/ngeo2688
Coverage:
Median Latitude: 41.000021 * Median Longitude: -32.957207 * South-bound Latitude: 41.000019 * West-bound Longitude: -32.957310 * North-bound Latitude: 41.000023 * East-bound Longitude: -32.957010
Minimum Elevation: -3413.5 m * Maximum Elevation: -3412.3 m
Event(s):
306-U1313A * Latitude: 41.000019 * Longitude: -32.957310 * Elevation: -3412.3 m * Recovery: 319.64 m * Campaign: Exp306 (North Atlantic Climate 2) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 33 cores; 308.6 m cored; 103.6 % recovered; 0 m drilled; 308.6 m penetrated
306-U1313B * Latitude: 41.000023 * Longitude: -32.957300 * Elevation: -3413.5 m * Recovery: 306.54 m * Campaign: Exp306 (North Atlantic Climate 2) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 32 cores; 300.4 m cored; 102 % recovered; 2 m drilled; 302.4 m penetrated
306-U1313C * Latitude: 41.000022 * Longitude: -32.957010 * Elevation: -3412.7 m * Recovery: 305.79 m * Campaign: Exp306 (North Atlantic Climate 2) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 32 cores; 293.4 m cored; 104.2 % recovered; 0 m drilled; 293.4 m penetrated
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Kirby, Nicola | |||
2 | Marine isotope stage | MIS | Kirby, Nicola | |||
3 | Sample code/label | Sample label | Kirby, Nicola | DSDP/ODP/IODP sample designation | ||
4 | Depth, composite | Depth comp | mcd | Kirby, Nicola | secondary splice | |
5 | AGE | Age | ka BP | Kirby, Nicola | Geocode | |
6 | ε-Neodymium | ε-Nd | Kirby, Nicola | Samarium corrected | ||
7 | ε-Neodymium, error | ε-Nd e | ± | Kirby, Nicola | ||
8 | Reference/source | Reference | Kirby, Nicola |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
504 data points
Data
1 Event | 2 MIS | 3 Sample label | 4 Depth comp [mcd] | 5 Age [ka BP] | 6 ε-Nd | 7 ε-Nd e [±] | 8 Reference |
---|---|---|---|---|---|---|---|
306-U1313A | 100 | 306-U1313A-12H-4,120 | 118.74 | 2498.9 | -13.03 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-4,125 | 118.79 | 2500.0 | -12.85 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-4,130 | 118.84 | 2501.2 | -12.45 | 0.21 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-4,135 | 118.89 | 2502.3 | -12.31 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-4,140 | 118.94 | 2503.5 | -11.82 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,0 | 119.04 | 2505.8 | -11.31 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-5,5 | 119.09 | 2507.0 | -11.08 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,11 | 119.15 | 2508.3 | -11.00 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,15 | 119.19 | 2509.3 | -11.06 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,20 | 119.24 | 2510.4 | -10.52 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,25 | 119.29 | 2511.6 | -10.36 | 0.20 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,30 | 119.34 | 2512.7 | -9.54 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,35 | 119.39 | 2513.9 | -9.98 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-5,40 | 119.44 | 2515.0 | -9.81 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,45 | 119.49 | 2516.0 | -9.93 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,50 | 119.54 | 2517.0 | -10.01 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,55 | 119.59 | 2518.0 | -10.28 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,60 | 119.64 | 2519.0 | -9.56 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-5,65 | 119.69 | 2520.0 | -10.20 | 0.27 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,70 | 119.74 | 2521.0 | -10.46 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,75 | 119.79 | 2522.0 | -10.67 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,80 | 119.84 | 2523.0 | -10.69 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,88 | 119.92 | 2524.6 | -11.12 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-5,95 | 119.99 | 2526.0 | -10.46 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,100 | 120.04 | 2526.9 | -10.77 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,105 | 120.09 | 2527.9 | -10.65 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,110 | 120.14 | 2528.9 | -11.00 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,115 | 120.19 | 2529.9 | -10.98 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,120 | 120.24 | 2530.9 | -10.91 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-5,125 | 120.29 | 2531.9 | -9.87 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,130 | 120.34 | 2532.9 | -11.04 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,135 | 120.39 | 2533.9 | -10.93 | 0.20 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,140 | 120.44 | 2534.9 | -11.12 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-5,145 | 120.49 | 2535.9 | -11.49 | 0.21 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,0 | 120.54 | 2536.9 | -11.84 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-6,5 | 120.59 | 2537.9 | -11.96 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,10 | 120.64 | 2538.8 | -12.25 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,15 | 120.69 | 2539.8 | -12.25 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,20 | 120.74 | 2540.7 | -12.37 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,25 | 120.79 | 2541.4 | -12.52 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,30 | 120.84 | 2542.2 | -12.46 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-6,35 | 120.89 | 2542.9 | -12.60 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,40 | 120.94 | 2543.7 | -12.43 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,45 | 120.99 | 2544.4 | -12.29 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,50 | 121.04 | 2545.2 | -12.25 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,55 | 121.09 | 2545.9 | -12.34 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-6,60 | 121.14 | 2546.7 | -12.41 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,65 | 121.19 | 2547.4 | -12.35 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,70 | 121.24 | 2548.2 | -12.76 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,75 | 121.29 | 2548.9 | -13.07 | 0.13 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,85 | 121.39 | 2550.4 | -13.27 | 0.26 | Kirby et al. |
306-U1313A | 100 | 306-U1313A-12H-6,90 | 121.44 | 2551.2 | -12.63 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-6,115 | 121.69 | 2554.9 | -11.87 | 0.13 | Lang et al. (2016) |
306-U1313A | 100 | 306-U1313A-12H-7,15 | 122.19 | 2562.4 | -11.48 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-5,20 | 150.48 | 3224.5 | -11.58 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-5,70 | 150.98 | 3237.0 | -11.55 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-5,90 | 151.18 | 3242.0 | -12.24 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-5,126.5 | 151.56 | 3251.5 | -12.24 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-5,140 | 151.68 | 3254.5 | -12.05 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-6,30 | 152.08 | 3264.4 | -12.39 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-6,60 | 152.38 | 3271.9 | -11.97 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-6,70 | 152.48 | 3274.4 | -11.51 | 0.13 | Kirby et al. |
306-U1313B | M2 | 306-U1313B-15H-6,80 | 152.58 | 3276.9 | -11.29 | 0.32 | Kirby et al. |
306-U1313B | M2 | 306-U1313B-15H-6,90 | 152.68 | 3279.4 | -11.22 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-6,100 | 152.78 | 3281.9 | -10.69 | 0.13 | Kirby et al. |
306-U1313B | M2 | 306-U1313B-15H-6,110 | 152.88 | 3284.4 | -10.42 | 0.13 | Kirby et al. |
306-U1313B | M2 | 306-U1313B-15H-6,120 | 152.98 | 3286.9 | -10.29 | 0.13 | Lang et al. (2016) |
306-U1313B | M2 | 306-U1313B-15H-6,130 | 153.08 | 3288.8 | -10.94 | 0.13 | Kirby et al. |
306-U1313B | M2 | 306-U1313B-15H-6,140 | 153.18 | 3290.6 | -11.07 | 0.13 | Lang et al. (2016) |
306-U1313C | M2 | 306-U1313C-16H-2,80 | 153.28 | 3292.4 | -11.56 | 0.19 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-2,90 | 153.38 | 3294.2 | -10.71 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-2,100 | 153.48 | 3296.0 | -11.15 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-2,107 | 153.56 | 3297.5 | -11.73 | 0.13 | Lang et al. (2016) |
306-U1313C | M2 | 306-U1313C-16H-2,120 | 153.68 | 3299.6 | -11.94 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-2,130 | 153.78 | 3301.5 | -11.57 | 0.13 | Lang et al. (2016) |
306-U1313C | M2 | 306-U1313C-16H-2,140 | 153.88 | 3303.3 | -10.29 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-3,0 | 153.98 | 3305.1 | -9.75 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-3,10 | 154.08 | 3306.9 | -11.43 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-3,20 | 154.18 | 3308.7 | -11.99 | 0.13 | Lang et al. (2016) |
306-U1313C | M2 | 306-U1313C-16H-3,30 | 154.28 | 3310.5 | -12.70 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-3,40 | 154.38 | 3312.3 | -12.84 | 0.13 | Kirby et al. |
306-U1313C | M2 | 306-U1313C-16H-3,61.5 | 154.60 | 3316.3 | -11.36 | 0.13 | Lang et al. (2016) |
306-U1313C | M2 | 306-U1313C-16H-3,90 | 154.88 | 3321.3 | -12.01 | 0.13 | Lang et al. (2016) |
306-U1313C | M2 | 306-U1313C-16H-3,120 | 155.18 | 3326.8 | -11.45 | 0.13 | Lang et al. (2016) |