Chaisson, William P; Keigwin, Lloyd D; Rio, Domenico; Acton, Gary D; Shipboard Scientific Party (2005): Paleontological investigation on planktonic foraminifers of ODP Hole 172-1060A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.271003
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: 30.759940 * Longitude: -74.466500
Date/Time Start: 1997-03-05T23:00:00 * Date/Time End: 1997-03-06T22:00:00
Minimum DEPTH, sediment/rock: 9.03 m * Maximum DEPTH, sediment/rock: 170.11 m
Event(s):
172-1060A * Latitude: 30.759940 * Longitude: -74.466500 * Date/Time Start: 1997-03-05T23:00:00 * Date/Time End: 1997-03-06T22:00:00 * Elevation: -3481.2 m * Penetration: 170.1 m * Recovery: 177.74 m * Location: Blake-Bahama Outer Ridge, North Atlantic Ocean * Campaign: Leg172 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 170.1 m cored; 0 m drilled; 104.5 % 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, minimum/young | Age young | Chaisson, William P | |||
| 5 | Zone to (top) | Zone top | Chaisson, William P | |||
| 6 | Abundance | Abund | Chaisson, William P | Planktonic foraminifers | ||
| 7 | Preservation | Preserv | Chaisson, William P | |||
| 8 | Comment | Comment | Chaisson, William P |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
217 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Age young | 5 Zone top | 6 Abund | 7 Preserv | 8 Comment |
|---|---|---|---|---|---|---|---|
| 9.03 | 9.03 | 172-1060A-1H-CC,12 | Pleistocene | N22 | F | P | may be Holocene; 1 menardii found rads and organic muds present |
| 18.94 | 20.88 | 172-1060A-2H-CC,20 | Pleistocene | N22 | C | M | |
| 26.70 | 30.70 | 172-1060A-3H-6,70 | Pleistocene | N22 | F | P | pyrite, 13 Uvigerina |
| 28.32 | 32.32 | 172-1060A-3H-CC,23 | Pleistocene | N22 | F | P | many rads |
| 28.70 | 33.32 | 172-1060A-4H-1,70 | Pleistocene | N22 | C | G | no flexuosa |
| 30.20 | 34.82 | 172-1060A-4H-2,70 | Pleistocene | N22 | C | G | no flexuosa |
| 31.70 | 36.32 | 172-1060A-4H-3,70 | Pleistocene | N22 | R | P | no flexuosa |
| 34.70 | 39.32 | 172-1060A-4H-5,70 | Pleistocene | N22 | R | P | almost nothing >150 microns |
| 38.16 | 42.78 | 172-1060A-4H-CC,27 | Pleistocene | N22 | C | M | many rads and some ostracods |
| 47.57 | 53.44 | 172-1060A-5H-CC,26 | Pleistocene | N22 | F | P | much black clayey material |
| 57.12 | 66.61 | 172-1060A-6H-CC,24 | Pleistocene | N22 | C | M | some rads |
| 66.50 | 76.89 | 172-1060A-7H-CC,28 | Pleistocene | N22 | F | G | |
| 75.31 | 87.38 | 172-1060A-8H-CC,31 | Pleistocene | N22 | F | M | a lot of pyrite filled burrows |
| 85.66 | 97.82 | 172-1060A-9H-CC,29 | Pleistocene | N22 | F | M | very small forams pyrite |
| 95.15 | 108.33 | 172-1060A-10H-CC,29 | Pleistocene | N22 | C | G | |
| 104.63 | 119.82 | 172-1060A-11H-CC,21 | Pleistocene | N22 | A | VG | interglacial stage all species abundant |
| 104.70 | 121.03 | 172-1060A-12H-1,70 | Pleistocene | N22 | C | G | |
| 109.28 | 125.61 | 172-1060A-12H-4,78 | Pleistocene | N22 | R | M | very diluted by clay |
| 114.13 | 130.46 | 172-1060A-12H-CC,38 | Pleistocene | N22 | R | very few foram no species are abundant P. lacunosa was found in this cc | |
| 118.70 | 137.53 | 172-1060A-13H-4,70 | Pleistocene | N22 | F | P | |
| 123.25 | 142.08 | 172-1060A-13H-CC,0 | Pleistocene | N22 | A | G | interglacial stage? |
| 133.08 | 153.71 | 172-1060A-14H-CC,21 | Pleistocene | N22 | C | G | pyrite |
| 151.63 | 172.26 | 172-1060A-16H-CC,0 | Pleistocene | N22 | C | G | |
| 155.20 | 175.83 | 172-1060A-17H-3,70 | Pleistocene | N22 | F | G | |
| 156.70 | 177.33 | 172-1060A-17H-4,70 | Pleistocene | N22 | F | M | |
| 158.20 | 178.83 | 172-1060A-17H-5,70 | Pleistocene | N22 | R | P | |
| 159.70 | 180.33 | 172-1060A-17H-6,70 | Pleistocene | N22 | R | P | pyrite almost no forams |
| 160.54 | 181.17 | 172-1060A-17H-CC,20 | Pleistocene | N22 | F | G | almost only pyrite |
| 161.70 | 182.33 | 172-1060A-18H-1,70 | Pleistocene | N22 | A | M | |
| 163.20 | 183.83 | 172-1060A-18H-2,70 | Pleistocene | N22 | A | G | |
| 164.70 | 185.33 | 172-1060A-18H-3,70 | Pleistocene | N22 | C | G | |
| 165.90 | 186.53 | 172-1060A-18H-4,70 | Pleistocene | N22 | C | M | |
| 170.11 | 190.74 | 172-1060A-18H-CC,15 | Pleistocene | N22 | C | M | a lot of inflata = dissolution? |