Patton, J W; Choquette, P W; Guennel, G K; Kaltenback, A J; Moore, Andrew (1984): (Table 1) Petrographic descriptions grouped by age and lithostratigraphic unit at DSDP Leg 77 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809290, In supplement to: Patton, JW et al. (1984): Organic geochemistry and sedimentology of lower to mid-Cretaceous Deep-Sea Carbonates, Sites 535 and 540, Leg 77. In: Buffler, RT; Schlager, W; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 77, 417-443, https://doi.org/10.2973/dsdp.proc.77.110.1984
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 23.795333 * Median Longitude: -84.684167 * South-bound Latitude: 23.708000 * West-bound Longitude: -85.165500 * North-bound Latitude: 23.849200 * East-bound Longitude: -84.370800
Date/Time Start: 1980-12-29T00:00:00 * Date/Time End: 1981-01-19T00:00:00
Minimum Elevation: -3450.0 m * Maximum Elevation: -2742.0 m
Event(s):
77-535 * Latitude: 23.708000 * Longitude: -84.516200 * Date/Time: 1980-12-29T00:00:00 * Elevation: -3450.0 m * Penetration: 714 m * Recovery: 504.6 m * Location: Gulf of Mexico/BASIN * Campaign: Leg77 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 78 cores; 704.5 m cored; 9.5 m drilled; 71.6 % recovery
77-538A * Latitude: 23.849200 * Longitude: -85.165500 * Date/Time: 1981-01-14T00:00:00 * Elevation: -2742.0 m * Penetration: 332.5 m * Recovery: 137.6 m * Location: Gulf of Mexico/KNOLL * Campaign: Leg77 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 36 cores; 332.5 m cored; 0 m drilled; 41.4 % recovery
77-540 * Latitude: 23.828800 * Longitude: -84.370800 * Date/Time: 1981-01-19T00:00:00 * Elevation: -2926.0 m * Penetration: 745.5 m * Recovery: 335.1 m * Location: Gulf of Mexico * Campaign: Leg77 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 79 cores; 745.5 m cored; 0 m drilled; 44.9 % 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 code/label | Sample label | Patton, J W | DSDP/ODP/IODP sample designation | ||
6 | Sample, optional label/labor no | Lab no | Patton, J W | |||
7 | Piece | Piece | Patton, J W | |||
8 | Epoch | Epoch | Patton, J W | |||
9 | Lithologic unit/sequence | Unit | Patton, J W | |||
10 | Description | Description | Patton, J W | The abbreviations MS, WS, and PS refer to the textural carbonate classification (mudstone, wackestone, and packstone) of Dunham (1962) | ||
11 | Description 2 (continued) | Description 2 | Patton, J W |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
229 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Lab no | 7 Piece | 8 Epoch | 9 Unit | 10 Description | 11 Description 2 |
---|---|---|---|---|---|---|---|---|---|---|
77-538A | 23.8492 | -85.1655 | -2742 | 77-538A-16-5,21-27 | 27 | late Eocene | II | Siliceous lime WS, poorly laminated, with abundant, slightly to completely dissolved radiolarians and diatoms; matrix strongly compacted but siliceous organisms uncrushed; no molds are silica filled. | ||
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-37-1,44-53 | 28 | early Cenomanian | Uppermost IV | Laminated lime MS, 5Y 7/1 (Sample 28) to 5Y 5/1-6/1 (Sample 29); abundant planktonic foraminifers and organic matter in Sample 29; chalcedonic-quartz-filled molds of radiolarians(?) | abundant in a few mm laminae interspersed with rather featureless lime mudstone (micrite); foraminifers empty or barely lined with calcite microspar, and unbroken despite severe compaction of surrounding micrite (especially in Sample 29). | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-37-2,46-55 | 29 | early Cenomanian | Uppermost IV | Laminated lime MS, 5Y 7/1 (Sample 28) to 5Y 5/1-6/1 (Sample 29); abundant planktonic foraminifers and organic matter in Sample 29; chalcedonic-quartz-filled molds of radiolarians(?) | abundant in a few mm laminae interspersed with rather featureless lime mudstone (micrite); foraminifers empty or barely lined with calcite microspar, and unbroken despite severe compaction of surrounding micrite (especially in Sample 29). | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-42-2,27-34 | 30 | latest Albian | Middle of IV | Laminated lime MS as above, but without radiolarians; planktonic foraminifers rare to very abundant (15-20%), empty or filled with dirty-appearing chalcedonic quartz; planktonic foraminifers uncrushed; | smearedout, highly elongate compacted micrite pellets, with length-to-width ratios up to 10:1. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-43-2,60-60 | 31 | latest Albian | Middle of IV | Laminated lime MS as above, but without radiolarians; planktonic foraminifers rare to very abundant (15-20%), empty or filled with dirty-appearing chalcedonic quartz; planktonic foraminifers uncrushed; | smearedout, highly elongate compacted micrite pellets, with length-to-width ratios up to 10:1. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-44-2,74-77 | 32 | latest Albian | Middle of IV | Laminated lime MS as above, but without radiolarians; planktonic foraminifers rare to very abundant (15-20%), empty or filled with dirty-appearing chalcedonic quartz; planktonic foraminifers uncrushed; | smearedout, highly elongate compacted micrite pellets, with length-to-width ratios up to 10:1. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-45-1,50-58 | 33 | latest Albian | Middle of IV | Laminated lime MS as above, but without radiolarians; planktonic foraminifers rare to very abundant (15-20%), empty or filled with dirty-appearing chalcedonic quartz; planktonic foraminifers uncrushed; | smearedout, highly elongate compacted micrite pellets, with length-to-width ratios up to 10:1. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-45-2,93-100 | 34 | latest Albian | Middle of IV | Laminated lime MS as above, but without radiolarians; planktonic foraminifers rare to very abundant (15-20%), empty or filled with dirty-appearing chalcedonic quartz; planktonic foraminifers uncrushed; | smearedout, highly elongate compacted micrite pellets, with length-to-width ratios up to 10:1. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-46-1,74-80 | 35 | late Albian | Middle and lower parts of IV | Laminated to streaky laminated WS/PS and (Sample 38) MS, 5Y 4/1 (moderately dark) to 5Y 6/1-7/1 (light), with sparser planktonic foraminifers than above (Samples 29- 34), but relatively abundant uncompacted pellets of micrite; | abundances of pellets correlate crudely with organic carbon contents, S1 and S2; moderately to strongly compacted. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-47-1,78-84 | 36 | late Albian | Middle and lower parts of IV | Laminated to streaky laminated WS/PS and (Sample 38) MS, 5Y 4/1 (moderately dark) to 5Y 6/1-7/1 (light), with sparser planktonic foraminifers than above (Samples 29- 34), but relatively abundant uncompacted pellets of micrite; | abundances of pellets correlate crudely with organic carbon contents, S1 and S2; moderately to strongly compacted. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-48-1,138-142 | 37 | late Albian | Middle and lower parts of IV | Laminated to streaky laminated WS/PS and (Sample 38) MS, 5Y 4/1 (moderately dark) to 5Y 6/1-7/1 (light), with sparser planktonic foraminifers than above (Samples 29- 34), but relatively abundant uncompacted pellets of micrite; | abundances of pellets correlate crudely with organic carbon contents, S1 and S2; moderately to strongly compacted. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-50-2,38-52 | 38 | late Albian | Middle and lower parts of IV | Laminated to streaky laminated WS/PS and (Sample 38) MS, 5Y 4/1 (moderately dark) to 5Y 6/1-7/1 (light), with sparser planktonic foraminifers than above (Samples 29- 34), but relatively abundant uncompacted pellets of micrite; | abundances of pellets correlate crudely with organic carbon contents, S1 and S2; moderately to strongly compacted. | |
77-540 | 23.8288 | -84.3708 | -2926 | 77-540-63-1,80-86 | 39 | late Albian | Subunit Va | Laminated to streaky laminated WS/PS and (Sample 38) MS, 5Y 4/1 (moderately dark) to 5Y 6/1-7/1 (light), with sparser planktonic foraminifers than above (Samples 29- 34), but relatively abundant uncompacted pellets of micrite; | abundances of pellets correlate crudely with organic carbon contents, S1 and S2; moderately to strongly compacted. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-31-7,0-14 | 1 | Cenomanian(?) | Upper part of II | Lime MS with sparce calcispheres (Sample 1) and laminated WS/PS with rare phosphate grains and abundant compacted pellets and organic matter (Sample 2); trains and isolated crystals of iron sulfides. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-35-5,6-20 | 2 | Cenomanian(?) | Upper part of II | Lime MS with sparce calcispheres (Sample 1) and laminated WS/PS with rare phosphate grains and abundant compacted pellets and organic matter (Sample 2); trains and isolated crystals of iron sulfides. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-42-5,120-130 | 3 | Cenomanian(?) | Near base of II | Lime MS, laminated, dark (5Y 4/1-5/1) with rare phosphate grains and unidentified silt-sized bioclastic debris, as well as common compacted pellets; trace-1% dolomite in 10- 15 µm rhombs. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-42-5,23-32 | 4 | Cenomanian(?) | Near base of II | Lime MS, laminated, dark (5Y 4/1-5/1) with rare phosphate grains and unidentified silt-sized bioclastic debris, as well as common compacted pellets; trace-1% dolomite in 10- 15 µm rhombs. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-44-1,80-128 | 5 | Aptian | Upper part of III | Lime MS-WS, like Sample 4 but with abundant compacted pellets; no planktonic foraminifers, traces of silt-sized phosphate grains. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-50-2,77-96 | 6 | late Hauterivian | Bottom of III | Lime MS-WS (Samples 6 and 7) as above. Sample 8 is lightcolored chert; silicified MS with rare silicified calcispheres and rather abundant grainy organic matter. Sample 9 is very dark (5Y 3/1), organic matter-rich, sulfide-rich MS/WS(?). | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-50-3,27-34 | 7 | a | late Hauterivian | Bottom of III | Lime MS-WS (Samples 6 and 7) as above. Sample 8 is lightcolored chert; silicified MS with rare silicified calcispheres and rather abundant grainy organic matter. Sample 9 is very dark (5Y 3/1), organic matter-rich, sulfide-rich MS/WS(?). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-50-3,27-34 | 8 | b | late Hauterivian | Bottom of III | Lime MS-WS (Samples 6 and 7) as above. Sample 8 is lightcolored chert; silicified MS with rare silicified calcispheres and rather abundant grainy organic matter. Sample 9 is very dark (5Y 3/1), organic matter-rich, sulfide-rich MS/WS(?). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-50-3,27-34 | 9 | c | late Hauterivian | Bottom of III | Lime MS-WS (Samples 6 and 7) as above. Sample 8 is lightcolored chert; silicified MS with rare silicified calcispheres and rather abundant grainy organic matter. Sample 9 is very dark (5Y 3/1), organic matter-rich, sulfide-rich MS/WS(?). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-52-1,69-85 | 10 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-53-3,0-32 | 11 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-43-6,53-72 | 12 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-55-4,51-72 | 13 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-56-7,73-87 | 14 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-58-2,103-108 | 15 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-58-4,3-46 | 16 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-58-4,19-20 | 40 | early Hauterivian | Upper half of IV | Lime MS-WS for the most part, very evenly laminated, dark to moderately light (5Y 2/1-5Y 6/1), with common to abundant flattened pellets and rare to common (trace- 15%) dolomite in the form of dolomitized burrow(?) fillings and scattered rhombs; | dolomite is microcrystalline to finely crystalline. Sample 16 is calcisphere MS-WS in which calcite spar fills the calcispheres and only slight compaction is apparent; strongly flattened pellets are abundant in the rest; Sample 40 is tar/asphalt. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-61-1,29-42 | 17 | late Valanginian | Bottom half of IV | Lime MS as above, with common-to-abundant flattened burrows or flattened soft pellets; Sample 21 is like Samples 17-19, and Sample 20 has several percent flattened clay-quartz pellets(?), calcispheres, and unidentified bioclastic grains. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-63-4,97-115 | 18 | late Valanginian | Bottom half of IV | Lime MS as above, with common-to-abundant flattened burrows or flattened soft pellets; Sample 21 is like Samples 17-19, and Sample 20 has several percent flattened clay-quartz pellets(?), calcispheres, and unidentified bioclastic grains. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-64-4,60-86 | 19 | late Valanginian | Bottom half of IV | Lime MS as above, with common-to-abundant flattened burrows or flattened soft pellets; Sample 21 is like Samples 17-19, and Sample 20 has several percent flattened clay-quartz pellets(?), calcispheres, and unidentified bioclastic grains. | ||
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-66-2,20-39 | 20 | late Valanginian | Base of IV | Lime MS-WS, well laminated; Sample 20 has abundant flattened burrows or pellets (in Sample 21 they are rare); | Sample 21 is like Samples 17-19, and Sample 20 has several percent flattened clay-quartz pellets(?), calcispheres, and unidentified bioclastic grains. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-67-2,126-134 | 21 | late Valanginian | Base of IV | Lime MS-WS, well laminated; Sample 20 has abundant flattened burrows or pellets (in Sample 21 they are rare); | Sample 21 is like Samples 17-19, and Sample 20 has several percent flattened clay-quartz pellets(?), calcispheres, and unidentified bioclastic grains. | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-68-5,109-125 | 22 | late Valanginian | Upper part of V | Lime MS, rather poorly laminated and in some centimeters burrowed beds; trace to 2-4% siliciclastic, silt-sized grains (quartz and a little clay) | pellets rare or absent, no planktonic foraminifers, and trace to 15-20% dolomite; dominantly light colored (5Y 7/1-6/1) with interlaminated dark MS (5Y 4/1-3/1). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-69-5,60-68 | 23 | late Valanginian | Upper part of V | Lime MS, rather poorly laminated and in some centimeters burrowed beds; trace to 2-4% siliciclastic, silt-sized grains (quartz and a little clay) | pellets rare or absent, no planktonic foraminifers, and trace to 15-20% dolomite; dominantly light colored (5Y 7/1-6/1) with interlaminated dark MS (5Y 4/1-3/1). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-70-3,133-148 | 24 | late Valanginian | Upper part of V | Lime MS, rather poorly laminated and in some centimeters burrowed beds; trace to 2-4% siliciclastic, silt-sized grains (quartz and a little clay) | pellets rare or absent, no planktonic foraminifers, and trace to 15-20% dolomite; dominantly light colored (5Y 7/1-6/1) with interlaminated dark MS (5Y 4/1-3/1). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-71-3,97-123 | 25 | late Valanginian | Upper part of V | Lime MS, rather poorly laminated and in some centimeters burrowed beds; trace to 2-4% siliciclastic, silt-sized grains (quartz and a little clay) | pellets rare or absent, no planktonic foraminifers, and trace to 15-20% dolomite; dominantly light colored (5Y 7/1-6/1) with interlaminated dark MS (5Y 4/1-3/1). | |
77-535 | 23.7080 | -84.5162 | -3450 | 77-535-78-1,89-97 | 26 | late Berriasian | V | Lime MS similar to Sample 25; 10-15% dolomite; strongly compacted fabric with rare flattened pellets. |