Brunner, Charlotte A; Bornhold, Brian D; Firth, John V; Shipboard Scientific Party (2005): Range table from planktonic foraminifers in ODP Hole 169-1035D [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.315466
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Related to:
Fouquet, Yves; Zierenberg, Robert A; Miller, David J; et al. (1998): Proceedings of the Ocean Drilling Program, 169 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 169, online, https://doi.org/10.2973/odp.proc.ir.169.1998
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: 48.433660 * Longitude: -128.679970
Date/Time Start: 1996-09-13T00:00:00 * Date/Time End: 1996-09-15T01:45:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 24.43 m
Event(s):
169-1035D * Latitude: 48.433660 * Longitude: -128.679970 * Date/Time Start: 1996-09-13T00:00:00 * Date/Time End: 1996-09-15T01:45:00 * Elevation: -2448.3 m * Penetration: 178.5 m * Recovery: 51.37 m * Location: Dead Dog vent field, North Pacific Ocean * Campaign: Leg169 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 176.9 m cored; 0 m drilled; 29 % 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 | Brunner, Charlotte A | ||
| 3 | Sample code/label | Sample label | Brunner, Charlotte A | DSDP/ODP/IODP sample designation | ||
| 4 | Foraminifera, planktic abundance | Foram plankt | Brunner, Charlotte A | Abundance estimate | ||
| 5 | Foraminifera, planktic preservation | Foram plankt preserv | Brunner, Charlotte A | Abundance estimate | ||
| 6 | Neogloboquadrina pachyderma sinistral | N. pachyderma s | Brunner, Charlotte A | Abundance estimate | ||
| 7 | Turborotalita quinqueloba | T. quinqueloba | Brunner, Charlotte A | Abundance estimate | ||
| 8 | Neogloboquadrina pachyderma dextral | N. pachyderma d | Brunner, Charlotte A | Abundance estimate | ||
| 9 | Globigerinita glutinata | G. glutinata | Brunner, Charlotte A | Abundance estimate | ||
| 10 | Globigerina bulloides | G. bulloides | Brunner, Charlotte A | Abundance estimate | ||
| 11 | Globorotalia scitula | G. scitula | Brunner, Charlotte A | Abundance estimate | ||
| 12 | Globigerinita uvula uvula | G. uvula uvula | Brunner, Charlotte A | Abundance estimate | ||
| 13 | Globigerinita uvula minuta | G. uvula minuta | Brunner, Charlotte A | Abundance estimate | ||
| 14 | Globigerina bulloides umbilicata | G. bulloides umbilicata | Brunner, Charlotte A | Abundance estimate | ||
| 15 | Orbulina universa | O. universa | Brunner, Charlotte A | Abundance estimate | ||
| 16 | Comment | Comment | Brunner, Charlotte A | Abundance estimate |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
197 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Foram plankt | 5 Foram plankt preserv | 6 N. pachyderma s | 7 T. quinqueloba | 8 N. pachyderma d | 9 G. glutinata | 10 G. bulloides | 11 G. scitula | 12 G. uvula uvula | 13 G. uvula minuta | 14 G. bulloides umbilicata | 15 O. universa | 16 Comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.00 | 0.00 | 169-1035D-1H-1,0 | A | M | C | C | R | F | C | R | F | R | Planktonic foraminifers dominate with agglutinated benthonic foraminifers, radiolarians, diatoms, iron staining. Is this really Holocene? | ||
| 0.50 | 0.50 | 169-1035D-1H-1,50 | A | G | C | F | F | C | F | C | Planktonic foraminifers dominate the sand. Common radiolarians. | ||||
| 0.76 | 0.76 | 169-1035D-1H-1,76 | A | G | C | F | F | C | F | C | F | Planktonic foraminifers dominate the sand with few benthonic foraminifers, mineral grains like mica, quartz, etc., a trace of ostracodes, urchin spines | |||
| 1.09 | 1.09 | 169-1035D-1H-1,109 | A | M | C | F | R | C | R | F | C | R | Planktonic foraminifers dominate with benthonic foraminifers rare, no mineral grains in the sand! | ||
| 1.50 | 1.50 | 169-1035D-1H-2,0 | A | M | C | R | R | C | R | R | C | R | Planktonic foraminifers dominate with rare benthonic foraminifers, mineral grains, a trace of radiolarians, pyrite (framboidal) | ||
| 1.96 | 1.96 | 169-1035D-1H-2,46 | A | M | C | R | R | C | F | C | Planktonic foraminifers dominate with rare benthonic foraminifers, a trace of mineral grains, pyrite, and radiolarians. Some of the pyrite is framboidal. | ||||
| 2.88 | 2.88 | 169-1035D-1H-2,138 | A | M | C | F | R | C | R | F | C | F | Half planktonic foraminifers and half sulfides. Rare benthonic foraminifers, mineral grains, a trace of radiolarians | ||
| 3.00 | 3.00 | 169-1035D-1H-3,0 | C | P | C | R | R | C | R | R | Dominated by sulfides with rare planktonic foraminifers, a trace of benthonic foraminifers | ||||
| 4.50 | 4.50 | 169-1035D-1H-4,0 | F | P | C | F | C | R | Dominated by sulfides (pyrrhotite) with rare planktonic foraminifers, a trace of benthonic foraminifers. Anhydrite. | ||||||
| 4.86 | 4.86 | 169-1035D-1H-CC,0 | C | P | C | F | R | C | R | F | Dominated by sulfides (pyrrhotite) and green clay (chlorite?) with few planktonic foraminifers and rare green tubes of benthonic agglutinated foraminifers slumped in with the high temperature sulfides | ||||
| 5.01 | 5.01 | 169-1035D-1H-CC,15 | A | P | C | F | F | C | R | F | C | F | Half and half planktonic foraminifers and sulfides (pyrrhotite) with rare benthonic foraminifers and a trace of siliceous urchin spines, radiolarians, and anhydrite. | ||
| 9.98 | 9.98 | 169-1035D-2H-4,38 | R | P | R | R | Dominated by mineral grains although the total sand fraction is very small. Minor siliceous urchin spines and sponge? spicules, minor framboidal pyrite, 2 planktonic foraminifers. | ||||||||
| 12.31 | 12.31 | 169-1035D-2H-5,121 | F | P | F | R | R | F | Mineral grains dominate, with minor planktonic foraminifers and a few benthonic foraminifers. A few siliceous urchin spines | ||||||
| 12.80 | 12.80 | 169-1035D-2H-6,20 | C | P | C | F | R | C | R | R | R | Planktonic foraminifers dominate with common benthonic foraminifers which are mostly lower bathyal types. | |||
| 13.88 | 13.88 | 169-1035D-2H-6,128 | R | P | R | R | Dominated by mineral grains with pyrrhotite and rare planktonic foraminifers and pyrrhotite. | ||||||||
| 14.40 | 14.40 | 169-1035D-2H-7,30 | R | P | R | Barite roses?, zeolites?, mineral grains, pyrite crystals | |||||||||
| 15.15 | 15.15 | 169-1035D-3H-1,55 | A | P | A | F | C | R | Planktonic foraminifers dominate, rare pyrite | ||||||
| 16.46 | 16.46 | 169-1035D-3H-2,36 | C | P | C | C | C | R | Poured into 3H-1 by mistake. | ||||||
| 24.43 | 24.43 | 169-1035D-3H-CC,9 | R | P | R | R | R | Pyrite, anhydrite, mineral grains and very rare planktonic foraminifers. |