Bader, Richard G; Gerard, Robert D (2005): Smear slide analysis of Hole 4-29 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230689
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
Sayles, Frederick L; Riedel, William R; Ruef, Michael H; Rothwell, W Thomas; Hay, William W; Bolli, Hans M; Benson, William E; Gerard, Robert D; Bader, Richard G (1970): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, IV, 751 pp, https://doi.org/10.2973/dsdp.proc.4.1970
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 14.785200 * Longitude: -69.322700
Date/Time Start: 1969-03-08T00:00:00 * Date/Time End: 1969-03-08T00:00:00
Minimum DEPTH, sediment/rock: 0.30 m * Maximum DEPTH, sediment/rock: 223.80 m
Event(s):
4-29 * Latitude: 14.785200 * Longitude: -69.322700 * Date/Time: 1969-03-08T00:00:00 * Elevation: -4247.0 m * Penetration: 229.5 m * Recovery: 84.1 m * Location: Caribbean Sea/BASIN * Campaign: Leg4 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 152.5 m cored; 3 m drilled; 55.1 % 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 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Lamellibranchiata | Lamellibranchiata | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Clay minerals | Clay min | % | Smear slide analysis | ||
17 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
18 | Fecal pellets | Fecal pel | % | Smear slide analysis | ||
19 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1350 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Nannos [%] | 11 Foram [%] | 12 Lamellibranchiata [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Clay min [%] | 17 Volc glass [%] | 18 Fecal pel [%] | 19 Minerals [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.30 | 4-29-1-1,30 | 20 | 20 | 60 | Pleistocene | FORAM NANNOS CLAY OOZE | Dominat lithology; numerical abundance | 0 | 30 | 20 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 |
1.16 | 4-29-1-11,116 | 20 | 30 | 50 | Pleistocene | FORAM NANNOS CLAY OOZE | Dominat lithology; relative abundance | 0 | 30 | 30 | 0 | 2 | 0 | 0 | 40 | 0 | 0 | 0 |
1.86 | 4-29-1-2,36 | 5 | 25 | 70 | Pleistocene | FORAM NANNOS CLAY OOZE | Dominat lithology; relative abundance | 0 | 30 | 5 | 0 | 2 | 0 | 0 | 65 | 0 | 0 | 0 |
2.92 | 4-29-1-21,142 | 1 | 40 | 60 | Pleistocene | NANNOS AND CLAY OOZE | Dominat lithology; relative abundance | 0 | 34 | 2 | 0 | 2 | 0 | 0 | 70 | 0 | 0 | 0 |
3.50 | 4-29-1-3,50 | 20 | 30 | 50 | Pleistocene | FORAM NANNOS CLAY | Dominat lithology; numerical abundance | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 |
4.16 | 4-29-1-31,116 | 1 | 50 | 50 | Pleistocene | BLACK BLOB | Minor lithology; relative abundance | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 45 |
4.34 | 4-29-1-31,134 | 5 | 45 | 50 | Pleistocene | NANNOS AND CLAY OOZE | Dominat lithology; relative abundance | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 |
4.60 | 4-29-1-CC,0 | 60 | 15 | 25 | Pleistocene | PLANKTONIC FORAM OOZE | Dominat lithology; relative abundance | 5 | 0 | 70 | 0 | 0 | 2 | 0 | 25 | 0 | 0 | 0 |
9.45 | 4-29-2-1,45 | 1 | 40 | 60 | Pleistocene | NANNOS FORAM OOZE | Dominat lithology; numerical abundance | 0 | 10 | 10 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 |
10.10 | 4-29-2-11,110 | 1 | 40 | 60 | Pleistocene | NANNOS FORAM OOZE | Dominat lithology; numerical abundance | 0 | 25 | 5 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 |
10.90 | 4-29-2-2,40 | 5 | 45 | 50 | Pleistocene | NANNOS FORAM OOZE | Dominat lithology; numerical abundance | 0 | 30 | 5 | 0 | 0 | 0 | 0 | 65 | 0 | 0 | 0 |
11.70 | 4-29-2-21,120 | 1 | 30 | 70 | Pleistocene | NANNOS FORAM OOZE | Dominat lithology; relative abundance | 0 | 20 | 2 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 |
12.40 | 4-29-2-3,40 | 5 | 30 | 65 | Upper pliocene | FORAM NANNOS OOZE | Dominat lithology; numerical abundance | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 |
13.04 | 4-29-2-31,104 | 10 | 10 | 80 | Upper pliocene | FORAM NANNOS OOZE | Dominat lithology; numerical abundance | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 |
13.41 | 4-29-2-31,141 | 5 | 20 | 75 | Upper pliocene | FORAM NANNOS OOZE | Dominat lithology; numerical abundance | 0 | 20 | 10 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 |
13.60 | 4-29-2-CC,0 | 30 | 55 | 15 | Upper pliocene | PLANKTONIC FORAM CHALK OOZE | Dominat lithology; numerical abundance | 25 | 0 | 70 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
19.60 | 4-29-3-CC,0 | 25 | 35 | 40 | Upper pliocene | FORAMS NANNOS CHALK OOZE | Dominat lithology; numerical abundance | 20 | 20 | 50 | 0 | 0 | 5 | 0 | 5 | 0 | 0 | 0 |
28.63 | 4-29-4-2,13 | 5 | 45 | 50 | Lower pliocene | FORAM NANNOS OOZE | Dominat lithology; numerical abundance | 0 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 |
28.74 | 4-29-4-2,24 | 1 | 20 | 80 | Lower pliocene | FORAM NANNOS OOZE | Dominat lithology; numerical abundance | 0 | 20 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 75 |
31.02 | 4-29-4-31,102 | 1 | 40 | 60 | Lower pliocene | NANNOS OOZE | Dominat lithology; relative abundance | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 |
31.16 | 4-29-4-31,116 | 1 | 20 | 80 | Lower pliocene | NANNOS OOZE | Dominat lithology; relative abundance | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 |
32.00 | 4-29-4-4,50 | 1 | 40 | 60 | Lower pliocene | NANNOS OOZE | Dominat lithology; relative abundance | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 |
32.62 | 4-29-4-41,112 | 10 | 50 | 40 | Upper miocene | NANNOS FORAM OOZE | Dominat lithology; numerical abundance | 0 | 30 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 |
33.10 | 4-29-4-CC,0 | 1 | 30 | 70 | Upper miocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 |
38.08 | 4-29-5-11,108 | 1 | 50 | 50 | Upper miocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 |
46.91 | 4-29-6-1,91 | 1 | 40 | 60 | Upper miocene | CLAY | Dominat lithology; relative abundance | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 |
47.27 | 4-29-6-11,127 | 1 | 40 | 60 | Upper miocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 |
136.65 | 4-29-9-2,15 | 40 | 50 | 10 | Middle eocene | RADS NANNOS OOZE | Dominat lithology; relative abundance | 5 | 5 | 0 | 0 | 50 | 2 | 10 | 0 | 0 | 10 | 0 |
137.30 | 4-29-9-2,80 | 45 | 55 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 65 | 0 | 10 | 0 | 0 | 0 | 0 |
138.15 | 4-29-9-3,15 | 55 | 40 | 5 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 75 | 0 | 15 | 0 | 0 | 0 | 0 |
139.10 | 4-29-9-31,110 | 55 | 35 | 10 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 70 | 0 | 20 | 0 | 0 | 0 | 0 |
140.25 | 4-29-9-4,75 | 40 | 60 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 60 | 0 | 10 | 0 | 0 | 0 | 0 |
144.55 | 4-29-10-1,55 | 75 | 25 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 5 |
145.10 | 4-29-10-11,110 | 45 | 55 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 5 | 0 | 0 | 0 | 5 |
146.00 | 4-29-10-2,50 | 35 | 60 | 5 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 5 | 0 | 0 | 0 |
147.70 | 4-29-10-3,70 | 40 | 60 | 1 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 2 | 0 | 0 | 0 |
149.20 | 4-29-10-4,70 | 30 | 60 | 10 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 10 | 0 | 0 | 0 |
150.40 | 4-29-10-5,40 | 45 | 45 | 10 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 10 | 0 | 0 | 0 |
150.90 | 4-29-10-5,90 | 30 | 50 | 20 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 20 | 0 | 0 | 0 |
157.90 | 4-29-11-1,90 | 50 | 50 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 |
162.70 | 4-29-12-1,70 | 25 | 60 | 15 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 85 | 0 | 0 | 15 | 0 | 0 | 0 |
164.30 | 4-29-12-2,80 | 35 | 60 | 5 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 5 | 5 | 0 | 0 | 0 |
165.75 | 4-29-12-3,75 | 55 | 40 | 5 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 50 | 0 | 15 | 5 | 0 | 0 | 0 |
167.00 | 4-29-12-4,50 | 45 | 55 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 65 | 0 | 5 | 0 | 0 | 0 | 0 |
168.40 | 4-29-12-5,40 | 45 | 55 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 60 | 0 | 15 | 0 | 0 | 0 | 0 |
170.45 | 4-29-12-6,95 | 45 | 50 | 5 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 40 | 0 | 15 | 0 | 0 | 0 | 0 |
171.10 | 4-29-12-CC,0 | 60 | 40 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 0 | 0 |
172.00 | 4-29-13-1,0 | 30 | 70 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 |
184.00 | 4-29-14-1,0 | 80 | 20 | 1 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 5 | 0 | 0 | 0 |
186.22 | 4-29-14-2,44 | 25 | 60 | 15 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 2 | 0 | 0 | 0 |
187.60 | 4-29-14-3,60 | 10 | 70 | 20 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 1 | 0 | 0 | 0 | 96 | 0 | 0 | 3 | 0 | 0 | 0 |
188.50 | 4-29-14-4,0 | 60 | 40 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 |
190.55 | 4-29-14-5,55 | 90 | 10 | 0 | Middle eocene | GRAY MATERIAL | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 100 | 0 | 0 |
191.00 | 4-29-14-51,100 | 70 | 20 | 10 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 90 | 2 | 0 | 10 | 0 | 0 | 0 |
192.27 | 4-29-14-6,77 | 80 | 10 | 10 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 90 | 2 | 0 | 10 | 0 | 0 | 0 |
193.10 | 4-29-14-CC,0 | 30 | 70 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 |
193.79 | 4-29-15-1,79 | 70 | 20 | 10 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 80 | 10 | 0 | 10 | 0 | 0 | 0 |
195.15 | 4-29-15-2,65 | 70 | 25 | 5 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 95 | 2 | 0 | 5 | 0 | 0 | 0 |
196.00 | 4-29-15-3,0 | 20 | 45 | 25 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 |
198.10 | 4-29-15-4,60 | 30 | 70 | 0 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 |
200.50 | 4-29-15-6,0 | 40 | 60 | 0 | Middle eocene | CALCEROUS RAD OOZE | Dominat lithology; numerical abundance | 10 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 0 |
203.00 | 4-29-16-11,100 | 70 | 20 | 10 | Middle eocene | RAD DIATOM OOZE | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 75 | 10 | 0 | 10 | 0 | 0 | 0 |
204.20 | 4-29-16-2,70 | 70 | 20 | 10 | Middle eocene | RADS OOZE | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 85 | 5 | 0 | 10 | 0 | 0 | 0 |
205.70 | 4-29-16-3,70 | 55 | 35 | 10 | Middle eocene | RADS DIATOM OOZE | Dominat lithology; relative abundance | 0 | 5 | 2 | 0 | 65 | 20 | 0 | 10 | 0 | 0 | 0 |
207.20 | 4-29-16-4,70 | 60 | 30 | 10 | Middle eocene | RADS DIATOM OOZE | Dominat lithology; relative abundance | 0 | 10 | 2 | 0 | 70 | 10 | 0 | 10 | 0 | 0 | 0 |
208.70 | 4-29-16-5,70 | 75 | 15 | 10 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 5 | 0 | 0 | 80 | 5 | 0 | 10 | 0 | 0 | 0 |
210.20 | 4-29-16-6,70 | 60 | 30 | 10 | Middle eocene | RADS DIATOM OOZE | Dominat lithology; relative abundance | 0 | 10 | 2 | 0 | 60 | 20 | 0 | 10 | 0 | 0 | 0 |
211.70 | 4-29-17-1,70 | 80 | 10 | 10 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 85 | 10 | 0 | 10 | 0 | 0 | 0 |
213.10 | 4-29-17-2,60 | 80 | 10 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 85 | 0 | 15 | 0 | 0 | 0 | 0 |
214.60 | 4-29-17-3,60 | 50 | 50 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 85 | 0 | 15 | 0 | 0 | 0 | 0 |
216.25 | 4-29-17-4,75 | 75 | 25 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 80 | 0 | 20 | 0 | 0 | 0 | 0 |
217.70 | 4-29-17-5,70 | 50 | 50 | 0 | Middle eocene | SP.SPIC RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 80 | 0 | 20 | 0 | 0 | 0 | 0 |
219.50 | 4-29-17-61,100 | 40 | 60 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 10 | 0 | 0 | 0 | 0 |
222.30 | 4-29-18-2,80 | 40 | 60 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 90 | 0 | 10 | 0 | 0 | 0 | 0 |
223.80 | 4-29-18-3,80 | 50 | 50 | 0 | Middle eocene | RADS OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 80 | 0 | 20 | 0 | 0 | 0 | 0 |