Cook, Alan C; Karner, Garry D (2002): (Table T3) Vitrinite reflection of samples obtained from ODP Leg 180 sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.787012, Supplement to: Cook, AC; Karner, GD (2002): Data report: Organic petrology of Leg 180 samples, western Woodlark Basin, Papua New Guinea. In: Huchon, P; Taylor, B; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 180, 1-35, https://doi.org/10.2973/odp.proc.sr.180.157.2002
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Abstract:
Seventy-one samples from Ocean Drilling Program Leg 180 sites were analyzed for vitrinite reflectance and organic type. The objective was to define maximum paleotemperatures across the western Woodlark Basin as a function of depth. The organic matter is of early Pliocene to Holocene age and was recovered from drilled depths of 4.5 to 851.3 meters below seafloor. Organic matter is generally restricted to woody fragments within the sediment, although in a number of fine-grained samples, organic matter is dispersed throughout the sample. Virtually all samples contain vitrinite, part of which may be derived from drifted logs. One sample was found to be barren of organic matter, and two contain only fusinite and semifusinite.
Variation of vitrinite reflectance is not systematic with either depth or location, and it appears that formation temperatures have been insufficient to cause an increase in vitrinite reflectance levels. Textural variations within the vitrinite show better correlation with depth. Samples of hypautochthonous peats represent either a terrestrial phase of sedimentation or large peat intraclasts within the section, possibly produced by forest fires in the source areas of the organic matter. The vitrinite and peat-derived samples appear to come from eucalyptus forest settings away from the coastline. Liptinite is not abundant in most of the samples (excluding suberinite associated with woody tissues). Marine liptinite is rare to absent, although many of the samples contain abundant foraminiferal tests. Pyrite is abundant in many of the wood fragments, and some pyritization of woody tissues has taken place.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -9.507969 * Median Longitude: 151.579686 * South-bound Latitude: -9.865560 * West-bound Longitude: 151.572580 * North-bound Latitude: -9.189700 * East-bound Longitude: 151.625710
Date/Time Start: 1998-06-17T15:30:00 * Date/Time End: 1998-08-05T04:30:00
Minimum DEPTH, sediment/rock: 3.72 m * Maximum DEPTH, sediment/rock: 851.30 m
Event(s):
180-1108B * Latitude: -9.745400 * Longitude: 151.625710 * Date/Time Start: 1998-06-17T15:30:00 * Date/Time End: 1998-06-24T09:00:00 * Elevation: -3177.2 m * Penetration: 485.2 m * Recovery: 148.58 m * Location: Solomon Sea * Campaign: Leg180 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 51 core; 485.2 m cored; 0 m drilled; 30.6 % recovery
180-1109C * Latitude: -9.506500 * Longitude: 151.573200 * Date/Time Start: 1998-06-24T18:30:00 * Date/Time End: 1998-06-27T08:00:00 * Elevation: -2211.0 m * Penetration: 375.7 m * Recovery: 323.11 m * Location: Solomon Sea * Campaign: Leg180 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 41 core; 375.7 m cored; 0 m drilled; 86 % recovery
180-1109D * Latitude: -9.506330 * Longitude: 151.572580 * Date/Time Start: 1998-06-27T08:00:00 * Date/Time End: 1998-07-04T00:15:00 * Elevation: -2211.0 m * Penetration: 802 m * Recovery: 299.87 m * Location: Solomon Sea * Campaign: Leg180 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 51 core; 449.2 m cored; 352.8 m drilled; 66.8 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Sample ID | Sample ID | Cook, Alan C | |||
| 6 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 7 | Vitrinite reflection | Vitr refl | % | Cook, Alan C | Microphotometer LEITZ MPV 1.1 | max |
| 8 | Vitrinite reflection | Vitr refl | % | Cook, Alan C | Microphotometer LEITZ MPV 1.1 | range low |
| 9 | Vitrinite reflection | Vitr refl | % | Cook, Alan C | Microphotometer LEITZ MPV 1.1 | range high |
| 10 | Sample amount | N | # | Cook, Alan C | no. of analysis | |
| 11 | Sample comment | Sample comment | Cook, Alan C | DOM = dispersed organic matter, TV = telovitrinite, DV = detrovitrinite |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
388 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample ID | 6 Depth sed [m] (mbsf) | 7 Vitr refl [%] (max) | 8 Vitr refl [%] (range low) | 9 Vitr refl [%] (range high) | 10 N [#] (no. of analysis) | 11 Sample comment (DOM = dispersed organic matte...) |
|---|---|---|---|---|---|---|---|---|---|---|
| 180-1108B | -9.7454 | 151.6257 | -3177 | T5799 | 216.82 | 0.38 | 0.27 | 0.49 | 27 | TV probably large piece of wood, suberinite present |
| 180-1108B | -9.7454 | 151.6257 | -3177 | T5800 | 235.77 | Barren | ||||
| 180-1108B | -9.7454 | 151.6257 | -3177 | T5801 | 306.35 | 0.34 | 0.25 | 0.46 | 26 | Coalified wood, massive |
| 180-1108B | -9.7454 | 151.6257 | -3177 | T5802 | 315.79 | 0.37 | 0.27 | 0.50 | 27 | Large pieces of coalified wood |
| 180-1108B | -9.7454 | 151.6257 | -3177 | T5803 | 324.40 | 0.39 | 0.31 | 0.50 | 29 | Coalified wood fragments |
| 180-1108B | -9.7454 | 151.6257 | -3177 | T5804 | 333.28 | 0.41 | 0.30 | 0.53 | 26 | Coalified wood fragments |
| 180-1109C | -9.5065 | 151.5732 | -2211 | T5805 | 180.23 | 0.36 | 0.24 | 0.58 | 9 | Bryozoan fragments, DOM rare |
| 180-1109C | -9.5065 | 151.5732 | -2211 | T5806 | 217.32 | 0.35 | 0.24 | 0.45 | 28 | Abundant coal, probably drifted logs |
| 180-1109C | -9.5065 | 151.5732 | -2211 | T5807 | 296.96 | 0.36 | 0.28 | 0.46 | 11 | Bryozoan fragments, DOM rare |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5808 | 379.99 | 0.23 | 0.20 | 0.25 | 15 | Abundant coal, probably drifted wood |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5809 | 387.86 | 0.36 | 0.28 | 0.40 | 28 | Coalified drifted wood |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5810 | 427.06 | 0.28 | 0.20 | 0.50 | 12 | Coalified drifted wood |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5811 | 447.72 | 0.34 | 0.24 | 0.46 | 6 | Coalified drifted wood |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5812 | 533.81 | 0.35 | 0.16 | 0.53 | 20 | Large coalified wood fragments |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5813 | 543.38 | 0.36 | 0.24 | 0.46 | 26 | DOM sparse |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5814 | 551.24 | 0.31 | 0.21 | 0.48 | 26 | DOM sparse |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5815 | 591.05 | 0.24 | 0.20 | 0.33 | 25 | Strong fluorescence from coalified wood |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5816 | 672.57 | 0.29 | 0.22 | 0.41 | 27 | DOM sparse |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5817 | 688.21 | 0.40 | 0.24 | 0.54 | 25 | Suberinite present in drifted wood |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5818 | 696.89 | 0.28 | 0.22 | 0.35 | 29 | Coal representing a peat bed |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5819 | 703.23 | 0.39 | 0.28 | 0.49 | 25 | Coal representing a peat bed |
| 180-1109D | -9.5063 | 151.5726 | -2211 | T5820 | 706.56 | 0.30 | 0.22 | 0.40 | 25 | Probably drifted wood but similar to coals |
| 180-1114A | -9.7935 | 151.5751 | -406 | T5821 | 55.42 | 0.31 | 0.21 | 0.42 | 29 | Drifted wood, coalified |
| 180-1114A | -9.7935 | 151.5751 | -406 | T5822 | 64.72 | 0.32 | 0.24 | 0.44 | 27 | Coalified drifted wood |
| 180-1114A | -9.7935 | 151.5751 | -406 | T5823 | 76.20 | 0.32 | 0.21 | 0.42 | 27 | Rare glauconite |
| 180-1114A | -9.7935 | 151.5751 | -406 | T5824 | 85.05 | 0.33 | 0.22 | 0.43 | 27 | DOM abundant, rare drifted wood |
| 180-1114A | -9.7935 | 151.5751 | -406 | T5825 | 123.29 | Barren, carbonate cement | ||||
| 180-1114A | -9.7935 | 151.5751 | -406 | T5826 | 133.23 | 0.30 | 0.24 | 0.36 | 26 | Drifted wood with some bark |
| 180-1115A | -9.1898 | 151.5742 | -1150 | T5827 | 3.72 | 0.17 | 0.10 | 0.27 | 25 | Wood but fluorescence similar to suberinite |
| 180-1115B | -9.1897 | 151.5740 | -1149 | T5828 | 241.48 | 0.22 | 0.12 | 0.53 | 21 | Bark and wood tissues |
| 180-1115B | -9.1897 | 151.5740 | -1149 | T5829 | 272.84 | -3.44 | Fusinite and semifusinite representing charred wood | |||
| 180-1115B | -9.1897 | 151.5740 | -1149 | T5830 | 291.07 | 0.25 | 0.17 | 0.40 | 26 | Wood structures well preserved |
| 180-1116A | -9.8656 | 151.5751 | -1851 | T5852 | 24.68 | 0.30 | 0.18 | 0.40 | 15 | Large wood fragments, DOM common |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5831 | 303.88 | 0.32 | 0.18 | 0.47 | 20 | Air-fall tuffs, DOM rare |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5832 | 304.21 | 0.33 | 0.23 | 0.43 | 26 | Air-fall tuffs, DOM rare |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5833 | 323.12 | 0.32 | 0.23 | 0.40 | 26 | Coalified wood, DOM rare |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5834 | 325.62 | 0.27 | 0.19 | 0.44 | 26 | Large coalified wood fragments, air-fall tuffs |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5835 | 392.67 | 0.30 | 0.22 | 0.41 | 26 | Large coalified wood fragments, DOM rare |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5836 | 401.04 | 0.34 | 0.23 | 0.45 | 27 | Some wood, variable coalification |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5837 | 411.60 | 0.33 | 0.22 | 0.41 | 27 | Some wood, variable coalification |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5938 | 422.84 | 0.33 | 0.27 | 0.41 | 14 | Large drifted coalified wood fragments |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5839 | 448.10 | 0.35 | 0.22 | 0.45 | 16 | Fungal sclerotia present, tuffaceous |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5840 | 489.50 | 0.29 | 0.16 | 0.49 | 25 | Pyritized wood |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5841 | 505.71 | 0.24 | 0.12 | 0.42 | 26 | Low reflecting wood tissue dominant |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5842 | 514.24 | 0.29 | 0.20 | 0.39 | 27 | Leaf tissues present |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5843 | 562.86 | 0.29 | 0.20 | 0.38 | 28 | Large drifted coalified wood fragments |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5844 | 563.60 | 0.29 | 0.22 | 0.40 | 27 | Drifted coalified logs within sediment |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5845 | 690.30 | 0.31 | 0.23 | 0.43 | 25 | Oil drops present, DOM common |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5846 | 708.03 | 0.31 | 0.23 | 0.39 | 28 | DOM abundant. TV less common |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5847 | 722.26 | 0.33 | 0.26 | 0.43 | 30 | Some more highly reflecting TV |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5848 | 737.63 | 0.34 | 0.23 | 0.44 | 29 | Some resinous woods |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5849 | 746.03 | 0.33 | 0.28 | 0.48 | 28 | DOM abundant, air-fall tuffs |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5850 | 757.19 | 0.33 | 0.23 | 0.43 | 27 | DOM common, DV>TV |
| 180-1115C | -9.1897 | 151.5737 | -1149 | T5851 | 776.48 | 0.35 | 0.24 | 0.46 | 27 | DOM abundant, air-fall tuff present |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5857 | 286.47 | 0.26 | 0.16 | 0.35 | 25 | Immature textinite |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5858 | 485.79 | 0.27 | 0.17 | 0.43 | 17 | DOM rare, air-fall tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5859 | 580.69 | 0.27 | 0.21 | 0.34 | 19 | DOM abundant, DV dominantly ?bark derived, fresh crystal tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5860 | 624.68 | 0.33 | 0.20 | 0.44 | 26 | Xylem-derived TV, air-fall tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5861 | 725.88 | -1.00 | Fusinite and semifusinite from charred wood fragments | |||
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5862 | 735.65 | 0.28 | 0.20 | 0.35 | 25 | Some bark tissue; pyritized foraminifers, tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5863 | 744.23 | 0.36 | 0.24 | 0.54 | 26 | Ulminite, some with higher reflectance tissues |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5864 | 763.26 | 0.25 | 0.15 | 0.46 | 20 | Coalified wood, some low reflecting TV but with telocollinite texture |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5865 | 765.56 | 0.28 | 0.17 | 0.46 | 28 | DOM abundant, bark tissues dominant, crystal tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5866 | 774.45 | 0.32 | 0.22 | 0.50 | 27 | DOM abundant, some texto-ulminite, air-fall tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5867 | 811.15 | 0.19 | 0.14 | 0.37 | 14 | Small part hand-picked sample, vitrinite porous, possible cellulose present |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5868 | 827.36 | 0.26 | 0.20 | 0.34 | 28 | DOM major, eu-ulminite dominant, air-fall tuffs |
| 180-1118A | -9.5852 | 151.5737 | -2304 | T5869 | 851.30 | 0.21 | 0.19 | 0.23 | 3 | DOM rare, air-fall tuffs |