Vanden Berg, Michael D; Jarrard, Richard D (2006): (Table T1) Mineralogy of ODP Leg 199 and DSDP Hole 16-162 sediments - comparison of methods [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.776949, Supplement to: Vanden Berg, MD; Jarrard, RD (2006): Data report: High-resolution mineralogy for Leg 199 based on reflectance spectroscopy and physical properties. In: Wilson, PA; Lyle, M; Firth, JV (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 199, 1-23, https://doi.org/10.2973/odp.proc.sr.199.203.2006
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Abstract:
During Ocean Drilling Program Leg 199 in the equatorial Pacific, visible and near-infrared spectroscopy (VNIS) was used to measure the reflectance spectra (350-2500 nm) of 1343 sediment samples. Reflectance spectra were also measured for a suite of 60 samples of known mineralogy, thereby providing a local ground-truth calibration of spectral features to percentages of calcite, opal, smectite, and illite. The associated algorithm was used to calculate mineral percentages from the 1343 spectra. Using multiple regression and VNIS mineralogy, multisensor track physical properties and light spectroscopy data were then converted into continuous high-resolution mineralogy logs.
Related to:
Lyle, Mitchell W; Wilson, Paul A; Janecek, Thomas R; et al. (2002): Proceedings of the Ocean Drilling Program, 199 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 199, online, https://doi.org/10.2973/odp.proc.ir.199.2002
Olivarez Lyle, Annette; Lyle, Mitchell W (2002): Determination of biogenic opal in pelagic marine sediments: A simple method revisited. In: Lyle, M; Wilson, PA; Janecek, TR; et al., Proceedings of the Ocean Drilling Program, Initial Reports. College Station, TX (Ocean Drilling Program), 199, 1-21, https://doi.org/10.2973/odp.proc.ir.199.106.2002
Project(s):
Deep Sea Drilling Project (DSDP)
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 14.798620 * Median Longitude: -140.844874 * South-bound Latitude: 5.000000 * West-bound Longitude: -147.933180 * North-bound Latitude: 26.029550 * East-bound Longitude: -135.366660
Date/Time Start: 1971-03-15T00:00:00 * Date/Time End: 2001-11-23T00:00:00
Minimum Elevation: -5395.6 m * Maximum Elevation: -999.0 m
Event(s):
16-162 * Latitude: 14.869800 * Longitude: -140.043500 * Date/Time: 1971-03-15T00:00:00 * Elevation: -4854.0 m * Penetration: 153 m * Recovery: 130.8 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 17 cores; 153 m cored; 0 m drilled; 85.5 % recovery
199-1215A * Latitude: 26.029550 * Longitude: -147.933180 * Date/Time: 2001-10-30T00:00:00 * Elevation: -5395.6 m * Penetration: 75.4 m * Recovery: 68.27 m * Location: North Pacific Ocean * Campaign: Leg199 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 75.4 m cored; 0 m drilled; 90.5 % recovery
199-1218A * Latitude: 8.889450 * Longitude: -135.366660 * Date/Time: 2001-11-14T00:00:00 * Elevation: -4826.3 m * Penetration: 276.8 m * Recovery: 266.42 m * Location: North Pacific Ocean * Campaign: Leg199 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 30 cores; 276.8 m cored; 0 m drilled; 96.3 % recovery
Comment:
Ground-truth data for calcite percentages for ODP Sites 199-1215, 1218, and 1219 are from Lyle, Wilson, Janecek, et al. (2002). Ground-truth data from site survey cores and Leg 162 are from Olivarez-Lyle and Lyle (2002). Clay was found by subtracting percent calcite from 100%. Opal was assumed to be negligible. The dominant clay mineral (smectite or illite) was identified from VNIS spectra.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Vanden Berg, Michael D | |||
| 3 | Calcite | Cal | % | Vanden Berg, Michael D | ground-truth data | |
| 4 | Calcite | Cal | % | Vanden Berg, Michael D | Visible and near-infrared spectroscopy (VNIS) | |
| 5 | Opal, biogenic silica | bSiO2 | % | Vanden Berg, Michael D | ground-truth data | |
| 6 | Opal, biogenic silica | bSiO2 | % | Vanden Berg, Michael D | Visible and near-infrared spectroscopy (VNIS) | |
| 7 | Smectite | Sme | % | Vanden Berg, Michael D | ground-truth data | |
| 8 | Smectite | Sme | % | Vanden Berg, Michael D | Visible and near-infrared spectroscopy (VNIS) | |
| 9 | Illite | Ill | % | Vanden Berg, Michael D | ground-truth data | |
| 10 | Illite | Ill | % | Vanden Berg, Michael D | Visible and near-infrared spectroscopy (VNIS) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
540 data points
Data
| 1 Event | 2 Sample label | 3 Cal [%] (ground-truth data) | 4 Cal [%] | 5 bSiO2 [%] (ground-truth data) | 6 bSiO2 [%] | 7 Sme [%] (ground-truth data) | 8 Sme [%] | 9 Ill [%] (ground-truth data) | 10 Ill [%] |
|---|---|---|---|---|---|---|---|---|---|
| 199-1215A | 199-1215A-1H-1,49-51 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 6.82 | 100.00 | 93.18 |
| 199-1215A | 199-1215A-2H-1,23-25 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 6.95 | 100.00 | 93.05 |
| 199-1215A | 199-1215A-2H-1,75-77 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 100.00 | 100.00 |
| 199-1215A | 199-1215A-4H-5,75-77 | 54.50 | 48.23 | 0.00 | 0.00 | 45.50 | 51.77 | 0.00 | 0.00 |
| 199-1215A | 199-1215A-5H-5,75-77 | 80.15 | 89.00 | 0.00 | 0.00 | 19.85 | 11.00 | 0.00 | 0.00 |
| 199-1215A | 199-1215A-9H-2,84-86 | 68.93 | 75.05 | 0.00 | 1.76 | 31.07 | 23.19 | 0.00 | 0.00 |
| 199-1218A | 199-1218A-16H-6,81-83 | 93.18 | 93.20 | 0.00 | 0.00 | 6.82 | 6.80 | 0.00 | 0.00 |
| 199-1218A | 199-1218A-17H-6,75-77 | 92.47 | 97.49 | 0.00 | 0.00 | 7.53 | 2.51 | 0.00 | 0.00 |
| 199-1218A | 199-1218A-19H-2,75-77 | 92.65 | 90.32 | 0.00 | 0.00 | 7.35 | 9.68 | 0.00 | 0.00 |
| 199-1219A | 199-1219A-12H-4,69-71 | 92.36 | 94.68 | 0.00 | 0.00 | 7.64 | 5.32 | 0.00 | 0.00 |
| 199-1219A | 199-1219A-13H-4,75-77 | 91.62 | 89.64 | 0.00 | 2.39 | 8.38 | 7.96 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),33-35 | 0.22 | 0.00 | 12.00 | 0.00 | 0.00 | 12.53 | 87.78 | 87.47 |
| EW9709-03PC | EW9709-3PC(PAT-13),314-316 | 0.04 | 7.74 | 15.50 | 23.73 | 84.46 | 68.53 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),433-435 | 0.14 | 2.33 | 20.70 | 27.56 | 79.16 | 70.11 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),773-775 | 0.12 | 0.00 | 52.60 | 53.44 | 47.28 | 46.56 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),830-832 | 0.33 | 0.00 | 60.90 | 59.04 | 38.77 | 40.96 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),933-935 | 0.09 | 0.00 | 57.90 | 56.54 | 42.01 | 43.46 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),1192-1194 | 0.09 | 0.00 | 55.90 | 55.67 | 44.01 | 44.33 | 0.00 | 0.00 |
| EW9709-03PC | EW9709-3PC(PAT-13),1337-1339 | 0.08 | 0.00 | 57.00 | 58.32 | 42.92 | 41.68 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),122-124 | 0.16 | 1.87 | 17.70 | 21.96 | 82.14 | 76.17 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),335-337 | 0.30 | 0.00 | 24.70 | 25.08 | 75.00 | 74.92 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),387-389 | 0.31 | 0.00 | 22.20 | 20.72 | 77.49 | 79.28 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),518-520 | 0.33 | 0.00 | 20.60 | 18.75 | 79.07 | 81.25 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),696-698 | 0.34 | 10.08 | 32.10 | 25.41 | 67.56 | 64.51 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),804-806 | 52.46 | 43.39 | 14.40 | 15.87 | 33.14 | 40.74 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),829-831 | 67.50 | 56.96 | 8.90 | 9.22 | 23.60 | 33.82 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),982-984 | 0.36 | 10.70 | 34.60 | 26.02 | 65.04 | 63.28 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1163-1165 | 0.31 | 9.86 | 31.90 | 33.15 | 67.79 | 56.99 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1252-1254 | 0.26 | 7.40 | 29.70 | 27.21 | 70.04 | 65.38 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1317-1319 | 16.45 | 19.09 | 24.90 | 23.27 | 58.65 | 57.64 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1367-1369 | 17.24 | 20.69 | 31.70 | 23.13 | 51.06 | 56.18 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1436-1438 | 30.35 | 26.90 | 24.00 | 23.35 | 45.65 | 49.75 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1466-1468 | 27.04 | 30.41 | 22.20 | 20.94 | 50.76 | 48.65 | 0.00 | 0.00 |
| EW9709-07PC | EW9709-7PC(PAT-8),1518-1520 | 78.91 | 74.85 | 7.00 | 3.11 | 14.09 | 22.04 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),258-260 | 0.18 | 6.76 | 36.30 | 31.97 | 63.52 | 61.27 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),473-475 | 43.67 | 32.94 | 22.90 | 30.05 | 33.43 | 37.01 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),593-595 | 36.53 | 41.68 | 26.10 | 23.89 | 37.37 | 34.43 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),740-742 | 0.29 | 7.36 | 42.50 | 41.32 | 57.21 | 51.32 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),833-835 | 0.22 | 7.44 | 50.80 | 45.38 | 48.98 | 47.18 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),979-981 | 0.14 | 6.83 | 37.30 | 39.75 | 62.56 | 53.42 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),1074-1076 | 0.03 | 6.75 | 45.80 | 43.89 | 54.17 | 49.36 | 0.00 | 0.00 |
| EW9709-12PC | EW9709-12PC(PAT-17),1261-1263 | 63.63 | 58.34 | 15.10 | 17.68 | 21.27 | 23.99 | 0.00 | 0.00 |
| EW9709-21GC | EW9709-21GC(PAT-15),20-22 | 0.37 | 0.00 | 10.60 | 0.00 | 0.00 | 0.00 | 89.03 | 100.00 |
| EW9709-21GC | EW9709-21GC(PAT-15),115-117 | 0.11 | 0.00 | 9.30 | 0.00 | 0.00 | 0.00 | 90.59 | 100.00 |
| EW9709-21GC | EW9709-21GC(PAT-15),175-177 | 0.07 | 0.00 | 10.60 | 0.00 | 0.00 | 0.10 | 89.33 | 99.90 |
| EW9709-21GC | EW9709-21GC(PAT-15),235-237 | 0.04 | 0.00 | 12.20 | 0.00 | 0.00 | 20.70 | 87.76 | 79.30 |
| 16-162 | 16-162-1R-1,91-92 | 51.68 | 34.88 | 15.08 | 24.03 | 33.24 | 41.09 | 0.00 | 0.00 |
| 16-162 | 16-162-1R-2,61-62 | 46.94 | 36.34 | 18.39 | 23.45 | 34.67 | 40.21 | 0.00 | 0.00 |
| 16-162 | 16-162-1R-3,80-81 | 60.02 | 33.92 | 7.79 | 21.75 | 32.19 | 44.32 | 0.00 | 0.00 |
| 16-162 | 16-162-3R-2,80-81 | 72.33 | 65.44 | 10.90 | 10.86 | 16.77 | 23.70 | 0.00 | 0.00 |
| 16-162 | 16-162-3R-3,80-81 | 67.64 | 58.35 | 10.32 | 14.67 | 22.04 | 26.97 | 0.00 | 0.00 |
| 16-162 | 16-162-3R-4,80-81 | 77.60 | 68.64 | 7.32 | 10.21 | 15.08 | 21.15 | 0.00 | 0.00 |
| 16-162 | 16-162-3R-5,70-71 | 57.34 | 79.72 | 6.50 | 5.39 | 36.16 | 14.88 | 0.00 | 0.00 |
| 16-162 | 16-162-4R-3,79-80 | 3.97 | 4.81 | 43.43 | 37.85 | 52.60 | 57.33 | 0.00 | 0.00 |
| 16-162 | 16-162-4R-4,80-81 | 3.56 | 13.91 | 45.26 | 38.51 | 51.18 | 47.57 | 0.00 | 0.00 |
| 16-162 | 16-162-4R-5,77-78 | 3.14 | 10.05 | 48.89 | 52.40 | 47.97 | 37.55 | 0.00 | 0.00 |
| 16-162 | 16-162-4R-6,60-61 | 5.96 | 8.46 | 54.27 | 52.15 | 39.77 | 39.39 | 0.00 | 0.00 |
| 16-162 | 16-162-14R-2,80-81 | 16.03 | 25.21 | 52.02 | 39.58 | 31.95 | 35.21 | 0.00 | 0.00 |
| 16-162 | 16-162-14R-3,81-82 | 28.66 | 17.89 | 42.15 | 41.67 | 29.19 | 40.43 | 0.00 | 0.00 |
| 16-162 | 16-162-14R-4,80-81 | 35.26 | 28.91 | 37.14 | 39.07 | 27.60 | 32.02 | 0.00 | 0.00 |