Sikora, Paul; Mahoney, John J; Fitton, J Godfrey; Wallace, Paul J; Shipboard Scientific Party (2005): Paleontological investigation on benthic foraminifers of ODP Hole 192-1185A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.270034
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Mahoney, John J; Fitton, J Godfrey; Wallace, Paul J; et al. (2001): Proceedings of the Ocean Drilling Program, 192 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 192, online, https://doi.org/10.2973/odp.proc.ir.192.2001
ODP/TAMU (2005): JANUS Database. Ocean Drilling Program, Texas A&M University, College Station TX 77845-9547, USA; (data copied from Janus 2005-02 to 2005-06), http://www-odp.tamu.edu/database/
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -0.357600 * Longitude: 161.667700
Date/Time Start: 2000-10-10T00:00:00 * Date/Time End: 2000-10-10T00:00:00
Minimum DEPTH, sediment/rock: 250.67 m * Maximum DEPTH, sediment/rock: 322.98 m
Event(s):
192-1185A * Latitude: -0.357600 * Longitude: 161.667700 * Date/Time: 2000-10-10T00:00:00 * Elevation: -3898.9 m * Penetration: 328.7 m * Recovery: 24.99 m * Location: South Pacific Ocean * Campaign: Leg192 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 78.1 m cored; 0 m drilled; 32 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, composite | Depth comp | mcd | Sikora, Paul | ||
3 | Sample code/label | Sample label | Sikora, Paul | DSDP/ODP/IODP sample designation | ||
4 | Abundance | Abund | Sikora, Paul | Benthic foraminifers | ||
5 | Preservation | Preserv | Sikora, Paul | |||
6 | Comment | Comment | Sikora, Paul |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
84 data points
Data
1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Abund | 5 Preserv | 6 Comment |
---|---|---|---|---|---|
250.67 | 250.67 | 192-1185A-2R-1,7 | |||
252.17 | 252.17 | 192-1185A-2R-2,7 | |||
252.72 | 252.72 | 192-1185A-2R-2,62 | R | M | latest Eocene - upper P16 to P17; thin section #107 |
253.22 | 253.22 | 192-1185A-2R-CC,18 | C | G | latest Eocene - upper P16 to P17 |
262.21 | 262.21 | 192-1185A-3R-CC,13 | C | G | latest Eocene - upper P16 to P17 |
270.02 | 270.02 | 192-1185A-4R-1,22 | R | G | thin section #108 |
271.61 | 271.61 | 192-1185A-4R-CC,17 | C | G | Below FG lysocline - grimsdalei declines, praemundulus, spissaformis and diss |
279.71 | 279.71 | 192-1185A-5R-1,21 | R | M | Near FG lysocline - planktics rare but not as rare as in core 4; thin secti... |
281.28 | 281.28 | 192-1185A-5R-CC,9 | C | G | latest Eocene - upper P16 to P17; dissonata now dominantes with truempyi 2n... |
289.15 | 289.15 | 192-1185A-6R-1,5 | T | M | |
289.61 | 289.61 | 192-1185A-6R-1,51 | C | G | truempyi now most common; no FG, but residue only 10cc |
290.16 | 290.16 | 192-1185A-6R-1,106 | C | M | truempyi dominant; praemundulus is absent and grimsdalei and dissonata cras... |
290.64 | 290.64 | 192-1185A-6R-2,4 | C | M | truempyi less dominant; dissonata moderate rise; no FG, but residue only 10cc |
291.27 | 291.27 | 192-1185A-6R-CC,21 | A | G | truempyi still most common species, but grimdalei increases sharply and speci |
299.69 | 299.69 | 192-1185A-7R-1,89 | F | M | thin section #111; probably comparable to washed residue assemblages, but s... |
301.82 | 301.82 | 192-1185A-7R-CC,48 | A | G | truempyi and grimsdalei no equal in abund;species diversiy remains high, bu... |
308.41 | 308.41 | 192-1185A-8R-1,1 | F | P | truempyi dominates rare assemblage from indurated limestone above basalt; p... |
308.43 | 308.43 | 192-1185A-8R-1,3 | F | P | |
322.98 | 322.98 | 192-1185A-10R-1,38 |