McCartney, Kevin (1990): (Table 6) Relative abundance of Miocene and Pliocene sponge spicules from ODP Site 113-696 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.753486, In supplement to: McCartney, K (1990): Siliceous sponge spicules from Ocean Drilling Program Leg 113. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 963-970, https://doi.org/10.2973/odp.proc.sr.113.144.1990
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -61.849000 * Median Longitude: -42.933200 * South-bound Latitude: -61.849000 * West-bound Longitude: -42.933300 * North-bound Latitude: -61.849000 * East-bound Longitude: -42.933100
Date/Time Start: 1987-02-23T10:00:00 * Date/Time End: 1987-03-02T04:15:00
Minimum Elevation: -661.0 m * Maximum Elevation: -661.0 m
Event(s):
113-696A * Latitude: -61.849000 * Longitude: -42.933100 * Date/Time Start: 1987-02-23T10:00:00 * Date/Time End: 1987-02-24T16:30:00 * Elevation: -661.0 m * Penetration: 103 m * Recovery: 58.3 m * Location: Weddell Sea * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 12 cores; 106 m cored; 0 m drilled; 55 % recovery
113-696B * Latitude: -61.849000 * Longitude: -42.933300 * Date/Time Start: 1987-02-24T16:30:00 * Date/Time End: 1987-03-02T04:15:00 * Elevation: -661.0 m * Penetration: 645.6 m * Recovery: 156.69 m * Location: Weddell Sea * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 59 cores; 569 m cored; 0 m drilled; 27.5 % recovery
Comment:
X = present, - = absent, the occurrence of "actino"- specimens are designated by "a".
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Epoch | Epoch | McCartney, Kevin | |||
| 3 | Sample code/label | Sample label | McCartney, Kevin | DSDP/ODP/IODP sample designation | ||
| 4 | Sponge spiculae | Sponge spic | McCartney, Kevin | A = abundant (100-1000 spicule specimens), C = common (10-100 specimens), U = uncommon (1-10 specimens), N = not found | ||
| 5 | Oxeas | Oxeas | McCartney, Kevin | |||
| 6 | Styles | Styles | McCartney, Kevin | |||
| 7 | Strongyles | Strongyles | McCartney, Kevin | |||
| 8 | Tylostyles | Tylostyles | McCartney, Kevin | |||
| 9 | Sigmas | Sigmas | McCartney, Kevin | |||
| 10 | Isochelas | Isochelas | McCartney, Kevin | |||
| 11 | Dichotriaenes | Dichotriaenes | McCartney, Kevin | |||
| 12 | Oxyasters | Oxyasters | McCartney, Kevin | |||
| 13 | Discorhabds | Discorhabds | McCartney, Kevin |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
300 data points
Data
| 1 Event | 2 Epoch | 3 Sample label | 4 Sponge spic | 5 Oxeas | 6 Styles | 7 Strongyles | 8 Tylostyles | 9 Sigmas | 10 Isochelas | 11 Dichotriaenes | 12 Oxyasters | 13 Discorhabds |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 113-696A | late Pliocene | 113-696A-1H-2,30-32 | C | Xa | X | - | Xa | - | X | - | - | - |
| 113-696A | late Pliocene | 113-696A-2H-2,30-32 | C | Xa | - | - | - | - | X | - | - | - |
| 113-696A | late Pliocene | 113-696A-3H-2,37-39 | C | X | X | - | - | - | X | - | - | - |
| 113-696A | late Pliocene | 113-696A-4H-2,90-92 | C | X | - | - | - | - | X | - | - | - |
| 113-696A | late Pliocene | 113-696A-5H-2,30-32 | C | X | - | - | - | X | - | - | - | - |
| 113-696A | late Pliocene | 113-696A-6H-2,30-32 | U | X | - | - | - | - | - | - | - | - |
| 113-696A | late Pliocene | 113-696A-7H-2,30-32 | U | X | - | - | - | X | - | - | - | - |
| 113-696A | late Pliocene | 113-696A-8H-2,30-32 | U | X | - | - | - | - | - | - | - | - |
| 113-696A | late Pliocene | 113-696A-9H-2,30-32 | A | X | Xa | X | X | X | X | - | - | - |
| 113-696B | late Pliocene | 113-696B-2R-1,74-76 | U | X | - | - | - | - | - | - | - | - |
| 113-696B | early Pliocene | 113-696B-3R-1,129-131 | C | X | Xa | - | - | X | X | - | - | - |
| 113-696B | early Pliocene | 113-696B-5R-2,30-32 | N | - | - | - | - | - | - | - | - | - |
| 113-696B | early Pliocene | 113-696B-6R-2,30-32 | C | X | - | - | - | - | - | - | X | - |
| 113-696B | early Pliocene | 113-696B-7R-2,34-36 | C | X | - | - | - | - | - | - | - | - |
| 113-696B | early Pliocene | 113-696B-10R-1,31-33 | C | - | - | - | - | X | - | - | - | - |
| 113-696B | early Pliocene | 113-696B-13R-1,42-44 | C | X | X | X | - | X | X | - | - | - |
| 113-696B | early Pliocene | 113-696B-17R-1,130-132 | C | X | - | - | - | - | - | - | - | - |
| 113-696B | early Pliocene | 113-696B-19R-1,16-18 | C | X | - | - | - | X | X | - | - | - |
| 113-696B | early Pliocene | 113-696B-20R-1,130-132 | C | X | - | - | - | - | X | X | - | - |
| 113-696B | late Miocene | 113-696B-24R-2,30-32 | C | X | - | - | X | - | - | X | - | - |
| 113-696B | late Miocene | 113-696B-26R-2,30-32 | C | X | - | - | - | - | X | X | - | - |
| 113-696B | late Miocene | 113-696B-27R-2,30-32 | C | X | X | - | - | X | - | X | - | - |
| 113-696B | late Miocene | 113-696B-28R-2,30-32 | C | X | - | - | - | X | - | X | - | - |
| 113-696B | late Miocene | 113-696B-32R-2,30-32 | C | X | - | X | X | - | - | X | - | - |
| 113-696B | late Miocene | 113-696B-34R-2,30-32 | C | X | X | - | Xa | - | - | - | - | X |