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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):
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):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Latitude of eventLatitude
Longitude of eventLongitude
Elevation of eventElevationm
Sample code/labelSample labelPatton, J WDSDP/ODP/IODP sample designation
Sample, optional label/labor noLab noPatton, J W
PiecePiecePatton, J W
EpochEpochPatton, J W
Lithologic unit/sequenceUnitPatton, J W
10 DescriptionDescriptionPatton, J WThe abbreviations MS, WS, and PS refer to the textural carbonate classification (mudstone, wackestone, and packstone) of Dunham (1962)
11 Description 2 (continued)Description 2Patton, J W
Size:
229 data points

Data

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Event

Latitude

Longitude

Elevation [m]

Sample label

Lab no

Piece

Epoch

Unit
10 
Description
11 
Description 2
77-538A 23.8492-85.1655-274277-538A-16-5,21-2727late EoceneIISiliceous 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 23.8288-84.3708-292677-540-37-1,44-5328early CenomanianUppermost IVLaminated 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).
77-54023.8288-84.3708-292677-540-37-2,46-5529early CenomanianUppermost IVLaminated 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).
77-54023.8288-84.3708-292677-540-42-2,27-3430latest AlbianMiddle of IVLaminated 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.
77-54023.8288-84.3708-292677-540-43-2,60-6031latest AlbianMiddle of IVLaminated 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.
77-54023.8288-84.3708-292677-540-44-2,74-7732latest AlbianMiddle of IVLaminated 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.
77-54023.8288-84.3708-292677-540-45-1,50-5833latest AlbianMiddle of IVLaminated 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.
77-54023.8288-84.3708-292677-540-45-2,93-10034latest AlbianMiddle of IVLaminated 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.
77-54023.8288-84.3708-292677-540-46-1,74-8035late AlbianMiddle and lower parts of IVLaminated 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.
77-54023.8288-84.3708-292677-540-47-1,78-8436late AlbianMiddle and lower parts of IVLaminated 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.
77-54023.8288-84.3708-292677-540-48-1,138-14237late AlbianMiddle and lower parts of IVLaminated 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.
77-54023.8288-84.3708-292677-540-50-2,38-5238late AlbianMiddle and lower parts of IVLaminated 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.
77-54023.8288-84.3708-292677-540-63-1,80-8639late AlbianSubunit VaLaminated 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 23.7080-84.5162-345077-535-31-7,0-141Cenomanian(?)Upper part of IILime 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.
77-53523.7080-84.5162-345077-535-35-5,6-202Cenomanian(?)Upper part of IILime 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.
77-53523.7080-84.5162-345077-535-42-5,120-1303Cenomanian(?)Near base of IILime 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.
77-53523.7080-84.5162-345077-535-42-5,23-324Cenomanian(?)Near base of IILime 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.
77-53523.7080-84.5162-345077-535-44-1,80-1285AptianUpper part of IIILime MS-WS, like Sample 4 but with abundant compacted pellets; no planktonic foraminifers, traces of silt-sized phosphate grains.
77-53523.7080-84.5162-345077-535-50-2,77-966late HauterivianBottom of IIILime 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(?).
77-53523.7080-84.5162-345077-535-50-3,27-347alate HauterivianBottom of IIILime 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(?).
77-53523.7080-84.5162-345077-535-50-3,27-348blate HauterivianBottom of IIILime 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(?).
77-53523.7080-84.5162-345077-535-50-3,27-349clate HauterivianBottom of IIILime 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(?).
77-53523.7080-84.5162-345077-535-52-1,69-8510early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-53-3,0-3211early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-43-6,53-7212early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-55-4,51-7213early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-56-7,73-8714early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-58-2,103-10815early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-58-4,3-4616early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-58-4,19-2040early HauterivianUpper half of IVLime 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.
77-53523.7080-84.5162-345077-535-61-1,29-4217late ValanginianBottom half of IVLime 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.
77-53523.7080-84.5162-345077-535-63-4,97-11518late ValanginianBottom half of IVLime 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.
77-53523.7080-84.5162-345077-535-64-4,60-8619late ValanginianBottom half of IVLime 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.
77-53523.7080-84.5162-345077-535-66-2,20-3920late ValanginianBase of IVLime 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.
77-53523.7080-84.5162-345077-535-67-2,126-13421late ValanginianBase of IVLime 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.
77-53523.7080-84.5162-345077-535-68-5,109-12522late ValanginianUpper part of VLime 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).
77-53523.7080-84.5162-345077-535-69-5,60-6823late ValanginianUpper part of VLime 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).
77-53523.7080-84.5162-345077-535-70-3,133-14824late ValanginianUpper part of VLime 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).
77-53523.7080-84.5162-345077-535-71-3,97-12325late ValanginianUpper part of VLime 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).
77-53523.7080-84.5162-345077-535-78-1,89-9726late BerriasianVLime MS similar to Sample 25; 10-15% dolomite; strongly compacted fabric with rare flattened pellets.