van Andel, Tjeerd H; Heath, G Ross (2005): Smear slide analysis of Hole 16-161A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230402
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Yeats, Robert S; Rodolfo, Kelvin S; Kaneps, Ansis G; Dinkelman, Menno G; Cronan, David S; Charleston, Santiago; Bukry, David; Bennett, Richard H; van Andel, Tjeerd H; Heath, G Ross (1973): Initial Reports of the Deep Sea Drilling Project 16. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVI, 949 pp, https://doi.org/10.2973/dsdp.proc.16.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 10.671200 * Longitude: -139.954500
Date/Time Start: 1971-03-09T00:00:00 * Date/Time End: 1971-03-09T00:00:00
Minimum DEPTH, sediment/rock: 64.90 m * Maximum DEPTH, sediment/rock: 237.88 m
Event(s):
16-161A * Latitude: 10.671200 * Longitude: -139.954500 * Date/Time: 1971-03-09T00:00:00 * Elevation: -4939.0 m * Penetration: 245.1 m * Recovery: 87.5 m * Location: North Pacific/CONT RISE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 126.1 m cored; 0 m drilled; 69.4 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Nannofossils | Nannos | % | Smear slide analysis | ||
10 | Foraminifera | Foram | % | Smear slide analysis | ||
11 | Radiolarians | Rad | % | Smear slide analysis | ||
12 | Diatoms | Diatoms | % | Smear slide analysis | ||
13 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
14 | Iron | Fe | % | Smear slide analysis | ||
15 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
16 | Fecal pellets | Fecal pel | % | Smear slide analysis | ||
17 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
960 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Nannos [%] | 10 Foram [%] | 11 Rad [%] | 12 Diatoms [%] | 13 Silicoflag [%] | 14 Fe [%] | 15 Volc glass [%] | 16 Fecal pel [%] | 17 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
64.90 | 16-161A-1-2,40 | 0 | 0 | 0 | Upper oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 1 |
65.30 | 16-161A-1-2,80 | 0 | 0 | 0 | Upper oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 1 | 0 | 1 | 1 | 0 | 0 |
66.20 | 16-161A-1-3,20 | 0 | 0 | 1 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 57 | 1 | 23 | 1 | 0 | 1 | 0 | 0 | 0 |
67.80 | 16-161A-1-4,30 | 0 | 0 | 1 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 57 | 1 | 23 | 1 | 0 | 1 | 0 | 0 | 0 |
68.46 | 16-161A-1-4,96 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 57 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 |
70.32 | 16-161A-1-51,132 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 |
70.45 | 16-161A-1-51,145 | 0 | 0 | 1 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 82 | 1 | 14 | 1 | 0 | 1 | 0 | 0 | 1 |
70.75 | 16-161A-1-6,25 | 0 | 0 | 0 | Upper oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 |
71.12 | 16-161A-1-6,62 | 0 | 0 | 0 | Upper oligocene | NANNOC HALK | Dominat lithology; relative abundance | 57 | 1 | 23 | 23 | 0 | 1 | 0 | 0 | 1 |
128.60 | 16-161A-2-1,60 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 1 | 23 | 0 | 0 | 0 | 0 | 0 |
133.50 | 16-161A-2-41,100 | 0 | 0 | 0 | Lower oligocene | COCCOLITH OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
136.90 | 16-161A-2-61,140 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 2 | 1 | 23 | 23 | 1 | 1 | 0 | 0 | 0 |
139.73 | 16-161A-3-21,123 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 78 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 |
142.40 | 16-161A-3-4,90 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 23 | 0 | 0 | 0 | 0 | 0 |
144.20 | 16-161A-3-51,120 | 0 | 0 | 0 | Lower oligocene | COCCOLITH OOZE | Dominat lithology; relative abundance | 78 | 0 | 1 | 23 | 0 | 0 | 1 | 0 | 0 |
146.34 | 16-161A-4-1,10 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE WITH DISC | Dominat lithology; relative abundance | 55 | 0 | 1 | 23 | 0 | 0 | 0 | 0 | 0 |
149.44 | 16-161A-4-3,20 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 56 | 1 | 1 | 23 | 0 | 0 | 0 | 0 | 0 |
153.24 | 16-161A-4-51,100 | 0 | 0 | 1 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; relative abundance | 56 | 1 | 55 | 23 | 0 | 0 | 0 | 0 | 0 |
153.94 | 16-161A-4-6,20 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK OOZE | Dominat lithology; numerical abundance | 77 | 1 | 11 | 11 | 0 | 0 | 0 | 0 | 0 |
155.27 | 16-161A-5-1,27 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK | Dominat lithology; relative abundance | 78 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
158.90 | 16-161A-5-3,90 | 0 | 0 | 0 | Lower oligocene | COCCOLITH CHALK | Dominat lithology; relative abundance | 56 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
161.30 | 16-161A-5-5,30 | 0 | 0 | 0 | Lower oligocene | COCCOLITH OOZE | Dominat lithology; relative abundance | 78 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
166.31 | 16-161A-6-2,55 | 0 | 0 | 0 | Lower oligocene | RAD NANNO MARL | Minor lithology; relative abundance | 55 | 1 | 55 | 0 | 0 | 1 | 0 | 0 | 0 |
171.28 | 16-161A-6-51,102 | 0 | 0 | 1 | Lower oligocene | NANNO (COCCOLITH) CHALK | Dominat lithology; numerical abundance | 84 | 0 | 15 | 1 | 0 | 0 | 0 | 0 | 0 |
173.16 | 16-161A-6-61,140 | 0 | 0 | 0 | Lower oligocene | RAD NANNO CHALK | Dominat lithology; relative abundance | 55 | 1 | 23 | 1 | 0 | 1 | 0 | 0 | 1 |
173.62 | 16-161A-7-1,38 | 0 | 0 | 0 | Lower oligocene | NANNO COCCOLITH CHALK | Dominat lithology; relative abundance | 55 | 0 | 46 | 1 | 0 | 1 | 0 | 0 | 0 |
176.94 | 16-161A-7-3,70 | 0 | 0 | 1 | Lower oligocene | RAD NANNO CHALK | Dominat lithology; relative abundance | 55 | 1 | 55 | 1 | 0 | 1 | 0 | 0 | 0 |
179.54 | 16-161A-7-5,30 | 0 | 0 | 1 | Lower oligocene | DIATOMACEOUS RAD NANNO CHALK | Dominat lithology; relative abundance | 55 | 1 | 23 | 23 | 0 | 1 | 0 | 0 | 0 |
184.75 | 16-161A-8-21,125 | 0 | 0 | 0 | Lower oligocene | DIATOMACEOUS RAD CHALK | Dominat lithology; relative abundance | 55 | 1 | 23 | 23 | 0 | 0 | 0 | 0 | 0 |
185.90 | 16-161A-8-3,90 | 0 | 0 | 0 | Lower oligocene | DIATOMACEOUS RAD CHALK | Dominat lithology; relative abundance | 55 | 0 | 23 | 23 | 0 | 0 | 0 | 0 | 0 |
186.46 | 16-161A-8-31,145.5 | 0 | 0 | 0 | Lower oligocene | RAD CHALK | Minor lithology; relative abundance | 55 | 0 | 55 | 23 | 0 | 1 | 0 | 0 | 0 |
192.30 | 16-161A-9-11,130 | 0 | 0 | 1 | Lower oligocene | DIATOMACEOUS RAD NANNO CHALK | Minor lithology; relative abundance | 55 | 0 | 23 | 23 | 0 | 0 | 0 | 0 | 0 |
193.76 | 16-161A-9-21,126 | 0 | 0 | 0 | Lower oligocene | RAD DIATOMACEOUS MARL | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
194.80 | 16-161A-9-3,80 | 0 | 0 | 35 | Lower oligocene | COCCOLITH MARL | Dominat lithology; relative abundance | 1 | 55 | 1 | 1 | 0 | 0 | 0 | 0 | 0 |
200.27 | 16-161A-10-1,27 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS CLAYEY RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 55 | 0 | 0 | 23 |
202.32 | 16-161A-10-2,82 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS CLAYEY RADIOLARITE | Dominat lithology; numerical abundance | 15 | 0 | 35 | 1 | 0 | 35 | 0 | 0 | 15 |
203.92 | 16-161A-10-3,92 | 0 | 0 | 1 | Upper eocene | FERRUGINOUS RADIOLARITE | Minor lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 24 | 0 | 0 | 23 |
204.01 | 16-161A-10-31,101 | 0 | 0 | 35 | Upper eocene | RADIOLARIAN OOZE | Dominat lithology; relative abundance | 1 | 0 | 55 | 23 | 0 | 1 | 0 | 0 | 1 |
204.19 | 16-161A-10-31,119 | 0 | 0 | 35 | Upper eocene | RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 1 | 0 | 0 | 1 |
204.78 | 16-161A-10-4,28 | 0 | 0 | 0 | Upper eocene | FERRUGINOUS RAD OOZE | Minor lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 23 | 0 | 0 | 23 |
204.80 | 16-161A-10-4,30 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Minor lithology; relative abundance | 0 | 0 | 55 | 1 | 0 | 24 | 0 | 0 | 23 |
205.55 | 16-161A-10-41,105 | 0 | 0 | 35 | Upper eocene | RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 0 | 0 | 0 | 0 |
208.71 | 16-161A-10-61,121 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 1 | 0 | 0 | 1 |
208.77 | 16-161A-10-61,127 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; relative abundance | 23 | 0 | 23 | 23 | 0 | 55 | 0 | 0 | 0 |
208.79 | 16-161A-10-61,129 | 0 | 0 | 0 | Upper eocene | DIATOMACEOUS RADIOLARITE | Minor lithology; relative abundance | 1 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 |
208.81 | 16-161A-10-61,131 | 0 | 0 | 35 | Upper eocene | RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 23 | 0 | 2 | 0 | 0 | 0 |
208.85 | 16-161A-10-61,135 | 0 | 0 | 0 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 0 | 1 | 0 | 23 | 0 | 0 | 1 |
213.10 | 16-161A-11-31,110 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE/CALCAREOUS | Dominat lithology; relative abundance | 23 | 0 | 55 | 1 | 0 | 23 | 0 | 0 | 23 |
213.78 | 16-161A-11-4,28 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 23 | 0 | 0 | 23 |
216.10 | 16-161A-11-51,110 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Minor lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 24 | 0 | 0 | 23 |
216.16 | 16-161A-11-51,116 | 0 | 0 | 35 | Upper eocene | RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 1 | 0 | 1 | 0 | 0 | 1 |
218.19 | 16-161A-12-1,19 | 0 | 0 | 35 | Upper eocene | RADIOLARITE | Minor lithology; relative abundance | 6 | 0 | 55 | 1 | 0 | 2 | 0 | 1 | 1 |
218.68 | 16-161A-12-1,68 | 0 | 0 | 0 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; numerical abundance | 1 | 0 | 32 | 1 | 0 | 33 | 0 | 1 | 32 |
218.78 | 16-161A-12-1,78 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; relative abundance | 1 | 0 | 55 | 0 | 0 | 24 | 0 | 0 | 23 |
227.35 | 16-161A-13-1,35 | 0 | 0 | 35 | Upper eocene | FERRUGINOUS RADIOLARITE | Dominat lithology; relative abundance | 0 | 0 | 55 | 1 | 0 | 24 | 1 | 0 | 23 |
227.61 | 16-161A-13-1,61 | 0 | 0 | 60 | Upper eocene | FERRUGINOUS RADIOLARIAN BROWN CLAY/CALCAREOUS | Minor lithology; relative abundance | 1 | 0 | 55 | 0 | 0 | 24 | 0 | 0 | 23 |
235.56 | 16-161A-14-1,56 | 0 | 0 | 60 | Middle eocene | RADIOLARIAN BROWN MARL | Minor lithology; relative abundance | 55 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 |
237.18 | 16-161A-14-2,68 | 0 | 0 | 60 | Middle eocene | NANNO RAD CHALK | Minor lithology; relative abundance | 55 | 0 | 23 | 0 | 0 | 23 | 0 | 0 | 23 |
237.40 | 16-161A-14-2,90 | 0 | 0 | 60 | Middle eocene | RAD NANNO CHALK TO MARL | Minor lithology; relative abundance | 1 | 0 | 55 | 0 | 0 | 23 | 0 | 0 | 23 |
237.88 | 16-161A-14-21,138 | 0 | 0 | 60 | Middle eocene | RADIOLARITE | Dominat lithology; relative abundance | 0 | 0 | 55 | 0 | 0 | 56 | 0 | 0 | 1 |