Chaisson, William P; Keigwin, Lloyd D; Rio, Domenico; Acton, Gary D; Shipboard Scientific Party (2005): Paleontological investigation on planktonic foraminifers of ODP Hole 172-1061A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.271004
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Keigwin, Lloyd D; Rio, Domenico; Acton, Gary D; et al. (1998): Proceedings of the Ocean Drilling Program 172 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 172, online, https://doi.org/10.2973/odp.proc.ir.172.1998
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: 29.974940 * Longitude: -73.599860
Date/Time Start: 1997-03-08T13:25:00 * Date/Time End: 1997-11-03T13:25:00
Minimum DEPTH, sediment/rock: 9.67 m * Maximum DEPTH, sediment/rock: 346.34 m
Event(s):
172-1061A * Latitude: 29.974940 * Longitude: -73.599860 * Date/Time Start: 1997-03-08T13:25:00 * Date/Time End: 1997-11-03T13:25:00 * Elevation: -4046.6 m * Penetration: 350.3 m * Recovery: 298.2 m * Location: Blake-Bahama Outer Ridge, North Atlantic Ocean * Campaign: Leg172 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 37 cores; 350.3 m cored; 0 m drilled; 85.1 % 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 | Chaisson, William P | ||
| 3 | Sample code/label | Sample label | Chaisson, William P | DSDP/ODP/IODP sample designation | ||
| 4 | Age, maximum/old | Age old | Chaisson, William P | |||
| 5 | Age, minimum/young | Age young | Chaisson, William P | |||
| 6 | Zone from (bottom) | Zone bot | Chaisson, William P | |||
| 7 | Zone to (top) | Zone top | Chaisson, William P | |||
| 8 | Abundance | Abund | Chaisson, William P | Planktonic foraminifers | ||
| 9 | Preservation | Preserv | Chaisson, William P | |||
| 10 | Comment | Comment | Chaisson, William P |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
476 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Age old | 5 Age young | 6 Zone bot | 7 Zone top | 8 Abund | 9 Preserv | 10 Comment |
|---|---|---|---|---|---|---|---|---|---|
| 9.67 | 21.07 | 172-1061A-1H-CC,24 | Pleistocene | N22 | C | M | pyrite | ||
| 17.70 | 30.79 | 172-1061A-2H-6,70 | Pleistocene | N22 | T | P | very bad preservation | ||
| 19.34 | 32.43 | 172-1061A-2H-CC,17 | Pleistocene | N22 | C | M | rads | ||
| 19.67 | 35.50 | 172-1061A-3H-1,67 | Pleistocene | N22 | C | M | Uvigerina present | ||
| 21.20 | 37.03 | 172-1061A-3H-2,70 | Pleistocene | N22 | T | P | too much dissolution | ||
| 22.70 | 38.53 | 172-1061A-3H-3,70 | Pleistocene | N22 | A | VG | |||
| 29.00 | 44.83 | 172-1061A-3H-CC,22 | Pleistocene | N22 | F | M | mica; pyrite burrows; rads | ||
| 38.12 | 54.57 | 172-1061A-4H-CC,0 | Pleistocene | N22 | F | M | mica; rads; black crud (iron-rich clay) | ||
| 48.02 | 67.03 | 172-1061A-5H-CC,20 | Pleistocene | N22 | C | G | Uvigerina present | ||
| 57.12 | 76.47 | 172-1061A-6H-CC,10 | Pleistocene | N22 | F | M | Uvigerina present; rads present, but fewer than in previous cc´s of this hole | ||
| 67.05 | 89.10 | 172-1061A-7H-CC,23 | Pleistocene | N22 | F | M | -huge numbers of diatoms; some rads -examined the >250 micron fraction to r... | ||
| 76.28 | 99.33 | 172-1061A-8H-CC,18 | Pleistocene | N22 | F | P | Uvigerina present dissolution has removed susceptible spp. | ||
| 86.12 | 111.17 | 172-1061A-9H-CC,22 | Pleistocene | N22 | F | P | mica, diatoms, rads, sponge spicules | ||
| 89.20 | 114.45 | 172-1061A-10H-3,70 | Pleistocene | N22 | C | G | |||
| 90.70 | 115.95 | 172-1061A-10H-4,70 | Pleistocene | N22 | F | P | no flexuosa | ||
| 92.20 | 117.45 | 172-1061A-10H-5,70 | Pleistocene | N22 | T | P | almost no forams pk | ||
| 93.70 | 118.95 | 172-1061A-10H-6,70 | Pleistocene | N22 | R | P | no flexuosa | ||
| 95.47 | 120.72 | 172-1061A-10H-CC,20 | Pleistocene | N22 | F | M | |||
| 98.70 | 124.99 | 172-1061A-11H-3,70 | |||||||
| 105.04 | 131.33 | 172-1061A-11H-CC,14 | Pleistocene | N22 | F | P | clay, mica, rads and no inflata | ||
| 114.39 | 142.19 | 172-1061A-12H-CC,9 | Pleistocene | N22 | F | P | mica | ||
| 124.23 | 153.57 | 172-1061A-13H-CC,27 | Pleistocene | N22 | C | G | pyrite | ||
| 132.95 | 164.81 | 172-1061A-14H-CC,21 | Pleistocene | N22 | R | P | pyrite Uvigerina abundant | ||
| 143.07 | 175.79 | 172-1061A-15H-CC,19 | Pleistocene | N22 | C | G | |||
| 147.16 | 182.28 | 172-1061A-16H-5,68 | Pleistocene | N22 | T | P | basically just inflata remains | ||
| 148.66 | 183.78 | 172-1061A-16H-6,68 | Pleistocene | N22 | C | G | hessi present | ||
| 150.18 | 185.30 | 172-1061A-16H-7,70 | Pleistocene | N22 | R | P | no crassaformis | ||
| 151.62 | 186.74 | 172-1061A-16H-CC,64 | Pleistocene | N22 | R | M | pyrite, mica, quartz or feldspath Uvigerina present | ||
| 152.68 | 188.79 | 172-1061A-17X-1,68 | Pleistocene | N22 | T | P | |||
| 154.18 | 190.29 | 172-1061A-17X-2,68 | Pleistocene | N22 | T | M | |||
| 155.68 | 191.79 | 172-1061A-17X-3,68 | Pleistocene | N22 | T | P | |||
| 157.09 | 193.20 | 172-1061A-17X-CC,0 | Pleistocene | N22 | R | P | pyrite very abundant all forams are rare | ||
| 164.90 | 202.42 | 172-1061A-18X-CC,16 | Pleistocene | N22 | T | P | clays pyrite | ||
| 175.43 | 214.70 | 172-1061A-19X-CC,27 | Pleistocene | N22 | R | P | almost no forams | ||
| 183.79 | 223.06 | 172-1061A-20X-CC,33 | Pleistocene | N22 | R | P | hematite? very few forams... | ||
| 194.21 | 233.48 | 172-1061A-21X-CC,19 | Pleistocene | N22 | R | P | pyrite | ||
| 203.44 | 242.71 | 172-1061A-22X-CC,34 | Pleistocene | N22 | C | G | Uvigerina present | ||
| 212.01 | 251.28 | 172-1061A-23X-CC,23 | Pleistocene | N22 | R | P | mostly pyrite and mica | ||
| 222.42 | 261.69 | 172-1061A-24X-CC,13 | Pleistocene | N22 | R | P | |||
| 226.92 | 266.19 | 172-1061A-25X-2,62 | Pleistocene | N22 | T | P | |||
| 228.39 | 267.66 | 172-1061A-25X-3,59 | Pleistocene | N22 | T | P | |||
| 229.96 | 269.23 | 172-1061A-25X-4,66 | Pleistocene | N22 | T | P | pyrite | ||
| 231.48 | 270.75 | 172-1061A-25X-CC,38 | Pleistocene | N22 | F | M | |||
| 235.20 | 274.47 | 172-1061A-26X-1,70 | Late Pliocene | Pleistocene | N22 | T | P | pyrite | |
| 241.34 | 280.61 | 172-1061A-26X-CC,28 | Late Pliocene | Pleistocene | N22 | R | P | ||
| 251.61 | 290.88 | 172-1061A-27X-CC,61 | Late Pliocene | Pleistocene | N22 | R | P | no truncat | |
| 261.00 | 300.27 | 172-1061A-28X-CC,77 | Late Pliocene | Pleistocene | N22 | F | M | Uvigerina; mica; pyritized burrows no obliquus found | |
| 271.50 | 310.77 | 172-1061A-29X-CC,24 | Late Pliocene | Pleistocene | N22 | F | M | slim tumida no truncat | |
| 281.66 | 320.93 | 172-1061A-30X-CC,39 | Late Pliocene | Pleistocene | N22 | F | M | mica | |
| 289.23 | 328.50 | 172-1061A-31X-CC,48 | Late Pliocene | Pleistocene | N22 | R | P | ||
| 292.53 | 331.80 | 172-1061A-32X-CC,13 | Late Pliocene | Pleistocene | N22 | R | P | mica | |
| 302.67 | 341.94 | 172-1061A-33X-1,67 | Late Pliocene | N22 | T | P | around 30 forams only | ||
| 304.30 | 343.57 | 172-1061A-33X-2,80 | Late Pliocene | N21 | A | G | no truncat. | ||
| 305.65 | 344.92 | 172-1061A-33X-3,65 | Late Pliocene | N21 | T | P | no truncat | ||
| 307.13 | 346.40 | 172-1061A-33X-4,63 | Late Pliocene | N21 | T | P | almost nothing | ||
| 308.28 | 347.55 | 172-1061A-33X-CC,28 | Late Pliocene | N21 | T | P | mica pyrite inflata present | ||
| 312.35 | 351.62 | 172-1061A-34X-1,65 | Late Pliocene | N21 | R | P | |||
| 313.85 | 353.12 | 172-1061A-34X-2,65 | Late Pliocene | N21 | C | M | pyrite (burrows) | ||
| 315.49 | 354.76 | 172-1061A-34X-CC,30 | Late Pliocene | N21 | R | M | mica pyrite no trunc. or inflata | ||
| 321.98 | 361.25 | 172-1061A-35X-1,68 | Late Pliocene | N21 | T | P | around 20 forams | ||
| 323.46 | 362.73 | 172-1061A-35X-2,66 | Late Pliocene | N21 | T | P | |||
| 324.93 | 364.20 | 172-1061A-35X-3,63 | Late Pliocene | N21 | T | P | 1 foram (ruber white) | ||
| 326.47 | 365.74 | 172-1061A-35X-CC,28 | Late Pliocene | N21 | A | VG | pyrite/ Ostra | ||
| 331.58 | 370.85 | 172-1061A-36X-1,68 | R | P | pyrite | ||||
| 333.01 | 372.28 | 172-1061A-36X-2,61 | Middle Pliocene | N20 | R | P | pyrite | ||
| 334.47 | 373.74 | 172-1061A-36X-3,62 | Middle Pliocene | N20 | R | P | pyrite | ||
| 335.61 | 374.88 | 172-1061A-36X-4,64 | Middle Pliocene | N20 | R | P | |||
| 337.13 | 376.40 | 172-1061A-36X-5,66 | Middle Pliocene | Late Pliocene | N20 | N21 | R | P | |
| 338.70 | 377.97 | 172-1061A-36X-CC,37 | Middle Pliocene | N20 | C | G | pyrite/ Ostra >3.1 Ma | ||
| 346.34 | 385.61 | 172-1061A-37X-CC,37 | Middle Pliocene | N20 | C | M | forams diluted by abundant pyrite |