Chaisson, William P; Keigwin, Lloyd D; Rio, Domenico; Acton, Gary D; Shipboard Scientific Party (2005): Paleontological investigation on planktonic foraminifers of ODP Hole 172-1062A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.271005
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: 28.246360 * Longitude: -74.406970
Date/Time Start: 1997-03-14T10:45:00 * Date/Time End: 1997-03-15T23:45:00
Minimum DEPTH, sediment/rock: 2.05 m * Maximum DEPTH, sediment/rock: 180.64 m
Event(s):
172-1062A * Latitude: 28.246360 * Longitude: -74.406970 * Date/Time Start: 1997-03-14T10:45:00 * Date/Time End: 1997-03-15T23:45:00 * Elevation: -4763.3 m * Penetration: 180.7 m * Recovery: 181.24 m * Location: Blake-Bahama Outer Ridge, North Atlantic Ocean * Campaign: Leg172 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 180.7 m cored; 0 m drilled; 100.3 % 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:
408 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 |
---|---|---|---|---|---|---|---|---|---|
2.05 | 2.05 | 172-1062A-1H-CC,8 | Pleistocene | N22 | C | M | |||
11.64 | 14.04 | 172-1062A-2H-CC,13 | Pleistocene | N22 | F | P | |||
15.40 | 18.32 | 172-1062A-3H-3,70 | Pleistocene | N22 | R | P | |||
16.90 | 19.82 | 172-1062A-3H-4,70 | Pleistocene | N22 | R | P | |||
18.40 | 21.32 | 172-1062A-3H-5,70 | Pleistocene | N22 | F | M | LO flexuosa | ||
21.38 | 24.30 | 172-1062A-3H-CC,0 | Pleistocene | N22 | C | G | dextral truncat>sinistral | ||
30.85 | 35.29 | 172-1062A-4H-CC,0 | Pleistocene | N22 | F | M | |||
40.52 | 45.32 | 172-1062A-5H-CC,19 | Pleistocene | N22 | F | M | sponge spicules | ||
49.98 | 57.00 | 172-1062A-6H-CC,17 | Pleistocene | N22 | F | M | pyritized burrows | ||
56.38 | 64.42 | 172-1062A-7H-5,68 | Pleistocene | N22 | F | M | |||
57.88 | 65.92 | 172-1062A-7H-6,68 | Pleistocene | N22 | R | P | many large fragments no flexuosa | ||
59.20 | 67.24 | 172-1062A-7H-7,50 | Pleistocene | N22 | F | M | glauconite | ||
59.69 | 67.73 | 172-1062A-7H-CC,34 | Pleistocene | N22 | C | G | |||
64.40 | 72.06 | 172-1062A-8H-4,70 | Pleistocene | N22 | T | P | |||
68.65 | 76.31 | 172-1062A-8H-CC,25 | Pleistocene | N22 | C | G | |||
78.34 | 85.34 | 172-1062A-9H-CC,40 | Pleistocene | N22 | F | M | |||
88.07 | 94.93 | 172-1062A-10H-CC,57 | Pleistocene | N22 | C | G | |||
94.39 | 101.83 | 172-1062A-11H-5,69 | Pleistocene | N22 | B | P | no forams - sample completly dissolved | ||
95.89 | 103.33 | 172-1062A-11H-6,69 | Pleistocene | N22 | T | P | no forams except 1 hirsuta | ||
97.56 | 105.00 | 172-1062A-11H-CC,28 | Pleistocene | N22 | A | G | |||
97.90 | 105.80 | 172-1062A-12H-1,70 | Pleistocene | N22 | R | P | |||
99.40 | 107.30 | 172-1062A-12H-2,70 | Pleistocene | N22 | B | P | sample completly dissolved | ||
100.90 | 108.80 | 172-1062A-12H-3,70 | Pleistocene | N22 | A | G | Ostra | ||
102.40 | 110.30 | 172-1062A-12H-4,70 | Pleistocene | N22 | T | P | dissolved sample | ||
106.64 | 114.54 | 172-1062A-12H-CC,17 | Pleistocene | N22 | R | P | sample dissolved mica 1 ostracode | ||
115.66 | 123.42 | 172-1062A-13H-CC,0 | Pleistocene | N22 | A | G | Ostra not hessi | ||
119.90 | 128.26 | 172-1062A-14H-3,70 | Pleistocene | N22 | R | P | no obliquus | ||
121.40 | 129.76 | 172-1062A-14H-4,70 | Pleistocene | N22 | T | P | sample almost completly dissolved only inflata left | ||
122.90 | 131.26 | 172-1062A-14H-5,70 | Pleistocene | N22 | A | G | |||
124.16 | 132.52 | 172-1062A-14H-CC,14 | Pleistocene | N22 | A | G | Ostra | ||
126.40 | 134.86 | 172-1062A-15H-1,70 | Pleistocene | N22 | A | G | small forams | ||
133.90 | 142.36 | 172-1062A-15H-6,70 | Pleistocene | N22 | A | VG | |||
134.76 | 143.22 | 172-1062A-15H-7,6 | Late Pliocene | N21 | C | G | |||
135.17 | 143.63 | 172-1062A-15H-CC,0 | Pleistocene | N22 | A | G | Ostra pyrite | ||
144.55 | 153.57 | 172-1062A-16H-CC,35 | Late Pliocene | N21 | C | G | |||
145.40 | 155.34 | 172-1062A-17H-1,70 | Pleistocene | N22 | F | M | |||
146.90 | 156.84 | 172-1062A-17H-2,70 | Late Pliocene | N21 | F | G | no trunc. | ||
148.42 | 158.36 | 172-1062A-17H-3,72 | Late Pliocene | N21 | T | P | inflata is nearly the only thing left | ||
149.90 | 159.84 | 172-1062A-17H-4,70 | Late Pliocene | N21 | R | P | glauconite no inflata | ||
151.40 | 161.34 | 172-1062A-17H-5,70 | Late Pliocene | N21 | C | G | small five chamb. neogloboquadrinids | ||
152.90 | 162.84 | 172-1062A-17H-6,70 | Late Pliocene | N21 | C | M | no inflata | ||
153.91 | 163.85 | 172-1062A-17H-CC,0 | Late Pliocene | N21 | C | G | Ostra no truncat. inflata rare | ||
154.90 | 166.84 | 172-1062A-18H-1,70 | Late Pliocene | N21 | R | P | pyrite around 10 forams no inflata | ||
156.40 | 168.34 | 172-1062A-18H-2,70 | R | P | |||||
157.90 | 169.84 | 172-1062A-18H-3,70 | F | M | no Pulleniatina and no miocenica | ||||
159.37 | 171.31 | 172-1062A-18H-4,67 | Late Pliocene | N21 | T | P | |||
160.90 | 172.84 | 172-1062A-18H-5,70 | Late Pliocene | N21 | T | P | dissolved pyrite 1 ostracode | ||
162.31 | 174.25 | 172-1062A-18H-6,61 | Late Pliocene | N21 | R | P | dissolved | ||
163.40 | 175.34 | 172-1062A-18H-CC,0 | Late Pliocene | N21 | R | M | mica | ||
164.40 | 176.34 | 172-1062A-19H-1,70 | Late Pliocene | Late Pliocene | N20 | N21 | F | G | |
165.90 | 177.84 | 172-1062A-19H-2,70 | Middle Pliocene | Late Pliocene | N20 | N21 | R | P | |
167.40 | 179.34 | 172-1062A-19H-3,70 | Middle Pliocene | Late Pliocene | N20 | N21 | R | P | |
168.90 | 180.84 | 172-1062A-19H-4,70 | R | P | no marker spp | ||||
170.40 | 182.34 | 172-1062A-19H-5,70 | R | P | low inflata | ||||
171.97 | 183.91 | 172-1062A-19H-6,77 | B | P | |||||
172.66 | 184.60 | 172-1062A-19H-CC,0 | Middle Pliocene | Late Pliocene | N20 | N21 | C | G | pyrite filled burrows |
173.90 | 185.84 | 172-1062A-20H-1,70 | Middle Pliocene | Late Pliocene | N20 | N21 | R | P | |
175.40 | 187.34 | 172-1062A-20H-2,70 | Middle Pliocene | Late Pliocene | N20 | N21 | R | P | |
176.90 | 188.84 | 172-1062A-20H-3,70 | Middle Pliocene | Late Pliocene | N20 | N21 | no altispira | ||
178.40 | 190.34 | 172-1062A-20H-4,70 | R | P | pyrite dissolved | ||||
179.90 | 191.84 | 172-1062A-20H-5,70 | R | P | dissolved | ||||
180.64 | 192.58 | 172-1062A-20H-CC,33 | Middle Pliocene | Late Pliocene | N20 | N21 | F | M | mica and pyrite burrows |