Novak, Joseph B; Caballero-Gill, Rocio P; Rose, Rebecca; Herbert, Timothy D; Dowsett, Harry J (2024): Calcium carbonate weight percent and mass accumulation rates of ODP Site 145-883 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.967372, In: Novak, JB et al. (2024): Multiproxy paleoceanographic dataset from ODP sites 883 and 887 and compiled mid Piacenzian benthic foraminiferal stable carbon isotope data from 23 IODP/ODP/DSDP sites [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.967342
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Abstract:
Here we present new and shipboard calcium carbonate weight percent and mass accumulation rates in discrete samples from ODP 883B. 71 accelerated solvent extractor sample residues were analyzed for calcium carbonate to supplement the 23 measurements in our study interval made by the shipboard scientific party (total N = 94). Approximately 30–60 mg of freeze-dried sediment was weighed prior to analysis in a UIC Coulometrics CO2 Coulometer in the Marine Analytical Lab at the University of California, Santa Cruz. Samples were acidified with 2 M HS and heated to 60°C. Measured C was converted to CaCO3 by a conversion factor of 8.33, determined by dividing the molecular weight of CaCO3 by that of C. Measurement error was ±1.85%, determined by repeated analysis of a homogenized laboratory standard calcium carbonate. Calcium carbonate mass accumulation rates were calculated as the product of weight percent CaCO3, dry bulk density, and sedimentation rate. Sedimentation rates were derived from the ODP 883 orbitally tuned age model presented in this study. Dry bulk density was estimated using the relationship between GRAPE WBD and measured dry bulk density in cores 9H–19H from hole 883C . CaCO3 weight percent was correlated to GRAPE WBD from hole 883B by resampling GRAPE WBD to the CaCO3 data using the "approx" function in .R.
Keyword(s):
Related to:
Sager, William W; Winterer, Edward L; Firth, John V; et al. (1993): Proceedings of the Ocean Drilling Program, 143 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 143, 996 pp, https://doi.org/10.2973/odp.proc.ir.143.1993
Project(s):
Ocean Drilling Program (ODP)
Funding:
National Science Foundation (NSF), grant/award no. 1545859: PIRE: DUST stimulated drawn-down of atmospheric CO2 as a trigger for Northern Hemisphere Glaciation
National Science Foundation (NSF), grant/award no. 1602331: Collaborative Research: Did the SE Pacific Gyre become a Hot Spot for N2 Fixation during Dusty Glacial Conditions?
Coverage:
Latitude: 51.198500 * Longitude: 167.768800
Date/Time Start: 1992-08-09T09:40:00 * Date/Time End: 1992-08-12T09:00:00
Minimum DEPTH, sediment/rock: 85.02 m * Maximum DEPTH, sediment/rock: 166.82 m
Event(s):
145-883B * Latitude: 51.198500 * Longitude: 167.768800 * Date/Time Start: 1992-08-09T09:40:00 * Date/Time End: 1992-08-12T09:00:00 * Elevation: -2395.0 m * Penetration: 840.7 m * Recovery: 695.41 m * Location: North Pacific Ocean * Campaign: Leg145 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 88 cores; 840.7 m cored; 0 m drilled; 82.7 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Novak, Joseph B | |||
2 | Sample code/label | Sample label | Novak, Joseph B | DSDP/ODP/IODP sample designation | ||
3 | DEPTH, sediment/rock | Depth sed | m | Novak, Joseph B | Geocode – mbsf | |
4 | Depth, composite | Depth comp | mcd | Novak, Joseph B | ||
5 | AGE | Age | ka BP | Novak, Joseph B | Geocode | |
6 | Calcium carbonate | CaCO3 | % | Novak, Joseph B | wt. % | |
7 | Carbon, organic, total | TOC | % | Novak, Joseph B | wt. % | |
8 | Sedimentation rate | SR | cm/ka | Novak, Joseph B | ||
9 | Accumulation rate, calcium carbonate | Acc rate CaCO3 | g/cm2/ka | Novak, Joseph B | Calculated | |
10 | Reference/source | Reference | Novak, Joseph B |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
583 data points
Data
1 Event | 2 Sample label | 3 Depth sed [m] | 4 Depth comp [mcd] | 5 Age [ka BP] | 6 CaCO3 [%] | 7 TOC [%] | 8 SR [cm/ka] | 9 Acc rate CaCO3 [g/cm2/ka] | 10 Reference |
---|---|---|---|---|---|---|---|---|---|
145-883B | 145-883B-10H-1,112-113 | 85.02 | 85.13 | 2686.45 | 0.0 | 0.12 | 2.900 | 0.000 | Sager et al. (1993) |
145-883B | 145-883B-10H-3,112-113 | 88.02 | 87.20 | 2727.34 | 0.0 | 0.13 | 10.023 | 0.000 | Sager et al. (1993) |
145-883B | 145-883B-11H-1,112-113 | 94.52 | 94.29 | 2798.13 | 2.3 | 10.023 | 0.088 | Sager et al. (1993) | |
145-883B | 145-883B-11H-3,112-113 | 97.52 | 96.84 | 2823.55 | 3.1 | 0.12 | 10.023 | 0.120 | Sager et al. (1993) |
145-883B | 145-883B-11H-5,112-113 | 100.52 | 99.35 | 2850.05 | 1.2 | 0.00 | 10.020 | 0.049 | Sager et al. (1993) |
145-883B | 145-883B-12H-1,11-13 | 103.01 | 102.99 | 2890.80 | 2.2 | 9.620 | 0.138 | this study | |
145-883B | 145-883B-12H-1,20-22 | 103.10 | 103.07 | 2891.50 | 0.0 | 10.430 | 0.000 | this study | |
145-883B | 145-883B-12H-1,47-49 | 103.37 | 103.29 | 2893.70 | 0.0 | 10.430 | 0.000 | this study | |
145-883B | 145-883B-12H-1,79-81 | 103.69 | 103.56 | 2896.30 | 0.0 | 10.430 | 0.000 | this study | |
145-883B | 145-883B-12H-1,111-113 | 104.01 | 103.83 | 2898.80 | 1.0 | 10.430 | 0.053 | this study | |
145-883B | 145-883B-12H-1,143-145 | 104.33 | 104.09 | 2901.40 | 5.1 | 10.430 | 0.264 | this study | |
145-883B | 145-883B-12H-2,1-3 | 104.41 | 104.16 | 2902.00 | 4.2 | 10.430 | 0.188 | this study | |
145-883B | 145-883B-12H-2,33-35 | 104.73 | 104.43 | 2904.60 | 9.0 | 10.430 | 0.432 | this study | |
145-883B | 145-883B-12H-2,65-67 | 105.05 | 104.70 | 2906.80 | 14.6 | 12.290 | 0.914 | this study | |
145-883B | 145-883B-12H-2,97-99 | 105.37 | 104.96 | 2908.70 | 12.8 | 14.190 | 0.917 | this study | |
145-883B | 145-883B-12H-2,129-131 | 105.69 | 105.23 | 2910.50 | 8.9 | 14.190 | 0.597 | this study | |
145-883B | 145-883B-12H-2,147-149 | 105.87 | 105.38 | 2911.60 | 4.3 | 14.190 | 0.271 | this study | |
145-883B | 145-883B-12H-3,1-3 | 105.91 | 105.41 | 2911.80 | 7.2 | 14.190 | 0.464 | this study | |
145-883B | 145-883B-12H-3,33-35 | 106.23 | 105.68 | 2913.70 | 1.8 | 14.190 | 0.119 | this study | |
145-883B | 145-883B-12H-3,65-67 | 106.55 | 105.95 | 2915.60 | 1.0 | 14.190 | 0.060 | this study | |
145-883B | 145-883B-12H-3,97-99 | 106.87 | 106.22 | 2917.49 | 1.0 | 14.190 | 0.062 | this study | |
145-883B | 145-883B-12H-3,129-131 | 107.19 | 106.48 | 2919.40 | 1.5 | 14.190 | 0.106 | this study | |
145-883B | 145-883B-12H-4,1-3 | 107.41 | 106.66 | 2920.60 | 0.0 | 14.190 | 0.000 | this study | |
145-883B | 145-883B-12H-6,147-148 | 111.87 | 110.39 | 2944.10 | 0.0 | 17.000 | 0.000 | this study | |
145-883B | 145-883B-12H-7,30-31 | 112.20 | 110.67 | 2945.70 | 0.0 | 17.000 | 0.001 | this study | |
145-883B | 145-883B-13H-1,30-31 | 112.70 | 112.64 | 2957.29 | 0.4 | 17.000 | 0.028 | this study | |
145-883B | 145-883B-13H-1,112-113 | 113.52 | 113.29 | 2961.14 | 1.1 | 0.01 | 17.000 | 0.085 | Sager et al. (1993) |
145-883B | 145-883B-13H-1,147-149 | 113.88 | 113.58 | 2962.82 | 23.5 | 17.000 | 2.102 | this study | |
145-883B | 145-883B-13H-2,1-3 | 113.91 | 113.60 | 2962.96 | 23.3 | 17.000 | 2.058 | this study | |
145-883B | 145-883B-13H-2,33-35 | 114.23 | 113.86 | 2964.46 | 26.7 | 17.000 | 2.590 | this study | |
145-883B | 145-883B-13H-2,65-67 | 114.90 | 114.14 | 2966.10 | 29.9 | 17.000 | 2.815 | this study | |
145-883B | 145-883B-13H-2,147-149 | 115.22 | 114.39 | 2968.20 | 27.1 | 10.170 | 1.501 | this study | |
145-883B | 145-883B-13H-3,1-3 | 115.35 | 114.49 | 2969.22 | 25.3 | 10.170 | 1.582 | this study | |
145-883B | 145-883B-13H-2,97-99 | 115.41 | 114.68 | 2971.02 | 35.0 | 10.170 | 1.728 | this study | |
145-883B | 145-883B-13H-3,33-35 | 115.73 | 114.93 | 2973.52 | 26.7 | 10.170 | 1.584 | this study | |
145-883B | 145-883B-13H-3,65-67 | 116.05 | 115.56 | 2977.20 | 26.1 | 10.170 | 1.404 | this study | |
145-883B | 145-883B-13H-3,97-99 | 116.37 | 115.68 | 2979.71 | 23.0 | 10.170 | 1.137 | this study | |
145-883B | 145-883B-13H-3,112-113 | 116.52 | 115.82 | 2980.88 | 25.2 | 0.18 | 10.170 | 1.210 | Sager et al. (1993) |
145-883B | 145-883B-13H-3,129-131 | 116.69 | 115.82 | 2982.21 | 18.5 | 10.170 | 0.910 | this study | |
145-883B | 145-883B-13H-2,129-131 | 118.04 | 115.31 | 2982.29 | 36.3 | 10.170 | 2.038 | this study | |
145-883B | 145-883B-13H-3,147-149 | 117.04 | 115.96 | 2983.62 | 7.2 | 10.170 | 0.345 | this study | |
145-883B | 145-883B-13H-4,1-3 | 116.91 | 115.99 | 2983.94 | 7.4 | 10.170 | 0.357 | this study | |
145-883B | 145-883B-13H-4,33-35 | 117.23 | 116.25 | 2985.97 | 9.0 | 12.520 | 0.493 | this study | |
145-883B | 145-883B-13H-4,65-67 | 117.55 | 116.50 | 2987.53 | 19.2 | 16.380 | 1.450 | this study | |
145-883B | 145-883B-13H-4,97-99 | 117.87 | 116.76 | 2989.08 | 24.9 | 16.380 | 1.973 | this study | |
145-883B | 145-883B-13H-4,120-121 | 118.10 | 116.94 | 2990.20 | 29.3 | 16.380 | 2.718 | this study | |
145-883B | 145-883B-13H-4,129-131 | 118.20 | 117.02 | 2990.69 | 27.0 | 16.380 | 2.379 | this study | |
145-883B | 145-883B-13H-4,147-149 | 118.37 | 117.16 | 2991.57 | 21.5 | 15.730 | 1.783 | this study | |
145-883B | 145-883B-13H-5,1-3 | 118.41 | 117.19 | 2991.78 | 26.7 | 15.060 | 2.159 | this study | |
145-883B | 145-883B-13H-5,33-35 | 118.73 | 117.44 | 2993.47 | 23.4 | 15.060 | 1.832 | this study | |
145-883B | 145-883B-13H-5,65-67 | 119.05 | 117.69 | 2995.15 | 19.3 | 15.060 | 1.514 | this study | |
145-883B | 145-883B-13H-5,97-99 | 119.37 | 117.95 | 2996.84 | 16.0 | 15.060 | 1.201 | this study | |
145-883B | 145-883B-13H-5,112-113 | 119.52 | 118.07 | 2997.63 | 12.2 | 0.09 | 15.060 | 0.888 | Sager et al. (1993) |
145-883B | 145-883B-13H-5,129-131 | 119.69 | 118.20 | 2998.54 | 12.1 | 15.060 | 0.781 | this study | |
145-883B | 145-883B-14H-1,35-36 | 121.73 | 121.26 | 3018.82 | 4.0 | 15.060 | 0.178 | this study | |
145-883B | 145-883B-14H-1,60-61 | 122.50 | 121.82 | 3022.57 | 1.2 | 15.060 | 0.087 | this study | |
145-883B | 145-883B-14H-1,112-113 | 123.02 | 122.20 | 3025.10 | 3.0 | 0.03 | 15.060 | 0.220 | Sager et al. (1993) |
145-883B | 145-883B-14H-2,20-22 | 123.60 | 122.63 | 3027.93 | 1.2 | 15.060 | 0.078 | this study | |
145-883B | 145-883B-14H-2,115-117 | 125.13 | 124.06 | 3038.81 | 6.2 | 15.060 | 0.427 | this study | |
145-883B | 145-883B-14H-3,112-113 | 126.02 | 124.65 | 3045.03 | 8.0 | 0.10 | 9.550 | 0.272 | Sager et al. (1993) |
145-883B | 145-883B-14H-3,128-129 | 126.18 | 124.76 | 3046.15 | 2.4 | 9.550 | 0.098 | this study | |
145-883B | 145-883B-14H-4,1-3 | 126.41 | 124.91 | 3047.76 | 5.6 | 9.550 | 0.243 | this study | |
145-883B | 145-883B-14H-4,33-35 | 126.73 | 125.13 | 3050.00 | 1.6 | 9.550 | 0.064 | this study | |
145-883B | 145-883B-14H-4,65-67 | 127.05 | 125.34 | 3052.64 | 0.5 | 8.100 | 0.015 | this study | |
145-883B | 145-883B-14H-5,60-61 | 128.33 | 126.19 | 3063.19 | 3.4 | 8.100 | 0.134 | this study | |
145-883B | 145-883B-14H-4,142-143 | 128.85 | 126.54 | 3067.47 | 0.9 | 8.100 | 0.036 | this study | |
145-883B | 145-883B-14H-5,112-113 | 129.02 | 126.66 | 3068.87 | 7.5 | 0.08 | 8.100 | 0.322 | Sager et al. (1993) |
145-883B | 145-883B-15H-1,112-113 | 132.52 | 129.78 | 3101.32 | 22.4 | 0.01 | 10.420 | 1.156 | Sager et al. (1993) |
145-883B | 145-883B-15H-3,60-61 | 135.00 | 132.26 | 3125.12 | 11.2 | 10.420 | 0.598 | this study | |
145-883B | 145-883B-15H-3,112-113 | 135.52 | 132.78 | 3130.12 | 12.2 | 0.02 | 10.420 | 0.598 | Sager et al. (1993) |
145-883B | 145-883B-15H-5,112-113 | 138.52 | 135.78 | 3153.81 | 22.5 | 0.19 | 14.270 | 1.979 | Sager et al. (1993) |
145-883B | 145-883B-15H-6,61-62 | 139.51 | 136.70 | 3164.27 | 20.1 | 8.110 | 0.677 | this study | |
145-883B | 145-883B-16H-1,30-32 | 141.21 | 141.12 | 3218.81 | 20.4 | 8.110 | 0.927 | this study | |
145-883B | 145-883B-16H-1,91-93 | 141.82 | 141.56 | 3224.18 | 15.8 | 8.110 | 0.612 | this study | |
145-883B | 145-883B-16H-1,112-113 | 142.03 | 141.71 | 3226.03 | 14.6 | 0.15 | 8.110 | 0.591 | Sager et al. (1993) |
145-883B | 145-883B-16H-3,20-21 | 143.88 | 143.19 | 3242.47 | 14.8 | 10.130 | 0.701 | this study | |
145-883B | 145-883B-16H-3,40-41 | 144.08 | 143.33 | 3243.87 | 17.1 | 10.130 | 0.906 | this study | |
145-883B | 145-883B-16H-3,90-91 | 144.80 | 143.68 | 3247.32 | 8.1 | 10.130 | 0.458 | this study | |
145-883B | 145-883B-16H-3,112-113 | 145.03 | 143.85 | 3248.94 | 21.7 | 0.16 | 10.127 | 1.130 | Sager et al. (1993) |
145-883B | 145-883B-16H-3,145-146 | 145.35 | 144.07 | 3251.20 | 26.5 | 10.130 | 1.495 | this study | |
145-883B | 145-883B-16H-4,3-4 | 145.43 | 144.13 | 3251.76 | 27.1 | 10.130 | 1.128 | this study | |
145-883B | 145-883B-16H-5,112-113 | 148.03 | 145.98 | 3270.07 | 13.3 | 0.18 | 10.130 | 0.777 | Sager et al. (1993) |
145-883B | 145-883B-16H-6,147-148 | 149.88 | 147.28 | 3280.97 | 7.4 | 13.420 | 0.390 | this study | |
145-883B | 145-883B-16H-7,3-5 | 149.93 | 147.32 | 3281.22 | 4.5 | 13.420 | 0.246 | this study | |
145-883B | 145-883B-16H-7,30-32 | 150.20 | 147.50 | 3282.58 | 3.5 | 13.420 | 0.220 | this study | |
145-883B | 145-883B-16H-7,60-61 | 150.50 | 147.70 | 3284.10 | 3.5 | 13.420 | 0.202 | this study | |
145-883B | 145-883B-16H-7,83-85 | 150.73 | 147.86 | 3285.26 | 2.1 | 13.418 | 0.133 | this study | |
145-883B | 145-883B-17H-1,112-113 | 151.52 | 150.96 | 3304.69 | 2.7 | 0.15 | 23.880 | 0.288 | Sager et al. (1993) |
145-883B | 145-883B-17H-2,130-131 | 153.20 | 152.65 | 3311.79 | 2.7 | 23.880 | 0.259 | this study | |
145-883B | 145-883B-17H-3,112-113 | 154.52 | 153.81 | 3318.68 | 16.2 | 0.00 | 10.840 | 0.794 | Sager et al. (1993) |
145-883B | 145-883B-17H-5,112-113 | 157.52 | 156.30 | 3367.02 | 17.5 | 0.19 | 9.180 | 0.809 | Sager et al. (1993) |
145-883B | 145-883B-18H-1,112-113 | 161.02 | 160.83 | 3397.33 | 25.2 | 12.585 | 1.557 | Sager et al. (1993) | |
145-883B | 145-883B-18H-3,112-113 | 163.82 | 163.17 | 3418.46 | 36.3 | 12.100 | 2.522 | Sager et al. (1993) | |
145-883B | 145-883B-18H-5,112-113 | 166.82 | 165.67 | 3447.40 | 15.3 | 9.190 | 0.851 | Sager et al. (1993) |