Ryan, William B F; Hsü, Kenneth J (2005): Smear slide analysis of Hole 13-125. PANGAEA, https://doi.org/10.1594/PANGAEA.230352
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
Kaneps, Ansis G; Wezel, Forese C; Stradner, Herbert; Pautot, Guy; Nesteroff, Wladimir D; Maync, Wolf; Llort, Jennifer; Dumitrica, Paulian; Cita, Maria Bianca; Ryan, William B F; Hsü, Kenneth J (1973): Initial Reports of the Deep Sea Drilling Project 13. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XIII, 514 pp, https://doi.org/10.2973/dsdp.proc.13.1973
Further details:
Project(s):
Funding:
Sixth Framework Programme (FP6), grant/award no. 36949: Southern European Seas: Assessing and Modelling Ecosystem Changes
Coverage:
Latitude: 34.624800 * Longitude: 20.429300
Date/Time Start: 1970-09-01T00:00:00 * Date/Time End: 1970-09-01T00:00:00
Minimum DEPTH, sediment/rock: 1.27 m * Maximum DEPTH, sediment/rock: 89.60 m
Event(s):
13-125 * Latitude: 34.624800 * Longitude: 20.429300 * Date/Time: 1970-09-01T00:00:00 * Elevation: -2782.0 m * Penetration: 97 m * Recovery: 45.7 m * Location: Mediterranean Sea/RIDGE * Campaign: Leg13 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 71 m cored; 25.9 m drilled; 64.3 % 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 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Diatoms | Diatoms | % | Smear slide analysis | ||
14 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Anhydrite | Anh | % | Smear slide analysis | ||
16 | Gypsum | Gp | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Mica | Mica | % | Smear slide analysis | ||
19 | Glauconite | Glt | % | Smear slide analysis | ||
20 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
21 | Iron | Fe | % | Smear slide analysis | ||
22 | Limonite | Lm | % | Smear slide analysis | ||
23 | Spinel | Spl | % | Smear slide analysis | ||
24 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1421 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 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Diatoms [%] | 14 Spiculae [%] | 15 Anh [%] | 16 Gp [%] | 17 Qz [%] | 18 Mica [%] | 19 Glt [%] | 20 Py [%] | 21 Fe [%] | 22 Lm [%] | 23 Spl [%] | 24 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.27 | 13-125-1-11,127 | 3 | 17 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 80 | 5 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 2 | 0 | 0 | 0 | 0 |
1.30 | 13-125-1-11,130 | 2 | 8 | 90 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 1 | 80 | 3 | 0 | 0 | 0 | 0 | 1 | 15 | 0 | 0 | 0 | 0 | 0 | 0 |
1.99 | 13-125-1-2,49 | 0 | 5 | 95 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
2.40 | 13-125-1-2,90 | 0 | 10 | 90 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 87 | 8 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
2.60 | 13-125-1-21,110 | 2 | 13 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 85 | 2 | 0 | 0 | 0 | 0 | 2 | 12 | 0 | 1 | 0 | 0 | 0 | 0 |
3.05 | 13-125-1-3,5 | 10 | 10 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 82 | 8 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
3.72 | 13-125-1-3,72 | 5 | 25 | 70 | Pleistocene | SAPROPEL | Dominat lithology; relative abundance | 0 | 2 | 50 | 15 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 2 |
4.00 | 13-125-1-31,100 | 5 | 10 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 85 | 2 | 0 | 0 | 0 | 0 | 3 | 7 | 0 | 3 | 1 | 0 | 0 | 0 |
5.34 | 13-125-1-4,84 | 70 | 20 | 10 | Pleistocene | TEPHRA | Dominat lithology; relative abundance | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 3 | 1 | 0 | 0 | 82 |
5.67 | 13-125-1-41,117 | 15 | 35 | 50 | Pleistocene | SAPROPEL | Dominat lithology; numerical abundance | 0 | 2 | 33 | 15 | 0 | 0 | 0 | 0 | 5 | 15 | 0 | 0 | 0 | 0 | 5 | 0 |
5.73 | 13-125-1-41,123 | 5 | 30 | 65 | Pleistocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 0 | 68 | 5 | 0 | 0 | 0 | 0 | 7 | 10 | 0 | 10 | 0 | 0 | 0 | 0 |
7.60 | 13-125-1-CC,0 | 5 | 15 | 85 | Pleistocene | TERRIGENOUS FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 10 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
11.90 | 13-125-2-3,90 | 5 | 15 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 72 | 10 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 3 | 0 | 0 | 0 |
12.98 | 13-125-2-4,48 | 2 | 18 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 1 | 82 | 0 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
15.35 | 13-125-2-51,135 | 0 | 0 | 0 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 2 | 85 | 3 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 5 | 1 | 0 | 0 | 0 |
15.60 | 13-125-2-CC,0 | 3 | 12 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 5 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
18.30 | 13-125-3-11,130 | 2 | 13 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 1 | 85 | 5 | 0 | 0 | 0 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 |
18.34 | 13-125-3-11,134 | 30 | 10 | 60 | Pleistocene | PYRITIC SANDY OOZE | Dominat lithology; relative abundance | 0 | 1 | 10 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 83 | 0 | 0 | 0 | 2 |
18.42 | 13-125-3-11,142 | 5 | 20 | 75 | Pleistocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 5 | 65 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 15 | 5 | 0 | 0 | 0 |
18.49 | 13-125-3-11,149 | 5 | 10 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 3 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 2 | 0 | 0 | 0 | 0 |
18.88 | 13-125-3-2,38 | 5 | 15 | 80 | Pleistocene | PYRITIC NANNO OOZE | Minor lithology; numerical abundance | 0 | 1 | 81 | 10 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 5 | 0 | 0 | 0 | 0 |
19.70 | 13-125-3-21,120 | 3 | 17 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 2 | 72 | 5 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 3 | 3 | 0 | 0 | 0 |
20.30 | 13-125-3-3,30 | 1 | 10 | 89 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 85 | 5 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 3 | 1 | 0 | 0 | 1 |
21.84 | 13-125-3-4,34 | 5 | 20 | 75 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 80 | 5 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
21.87 | 13-125-3-4,37 | 10 | 30 | 60 | Pleistocene | PYRITIC MARL OOZE | Minor lithology; relative abundance | 0 | 2 | 55 | 1 | 0 | 0 | 0 | 0 | 2 | 12 | 0 | 30 | 0 | 0 | 0 | 2 |
22.17 | 13-125-3-4,67 | 5 | 10 | 85 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 3 | 70 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 7 |
22.60 | 13-125-3-41,110 | 10 | 15 | 75 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 5 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 5 | 0 | 0 | 0 | 2 |
23.30 | 13-125-3-5,30 | 0 | 10 | 90 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 80 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 5 | 0 | 0 | 0 |
25.20 | 13-125-3-6,70 | 0 | 10 | 90 | Pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 83 | 7 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
26.10 | 13-125-3-CC,0 | 0 | 30 | 10 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 10 | 1 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
26.10 | 13-125-3-CC,0 | 60 | 5 | 95 | Lower pleistocene | SAPROPEL AND FORAM SAND | Dominat lithology; numerical abundance | 0 | 0 | 89 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
26.65 | 13-125-4-1,50 | 15 | 20 | 65 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 75 | 10 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 0 | 3 | 0 | 0 | 0 |
26.65 | 13-125-4-1,50 | 15 | 20 | 65 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 85 | 10 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
28.48 | 13-125-4-2,83 | 5 | 20 | 75 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 5 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 5 | 0 | 0 | 0 |
28.75 | 13-125-4-21,110 | 20 | 10 | 70 | Lower pleistocene | numerical abundance | 0 | 0 | 69 | 20 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | |
29.49 | 13-125-4-3,34 | 1 | 9 | 90 | Lower pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 91 | 1 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 2 | 1 | 0 | 0 | 0 |
29.85 | 13-125-4-3,70 | 20 | 15 | 65 | Lower pleistocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 7 | 66 | 7 | 0 | 0 | 0 | 0 | 10 | 2 | 1 | 2 | 5 | 0 | 0 | 0 |
30.61 | 13-125-4-31,146 | 40 | 10 | 50 | Lower pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 55 | 30 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.85 | 13-125-4-4,20 | 10 | 30 | 60 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 3 | 72 | 7 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 3 | 3 | 0 | 0 | 0 |
31.22 | 13-125-4-4,57 | 10 | 20 | 70 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 3 | 76 | 10 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
32.77 | 13-125-4-5,62 | 0 | 0 | 0 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 10 | 78 | 5 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
33.22 | 13-125-4-51,107 | 10 | 20 | 70 | Upper pliocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 5 | 75 | 5 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
33.80 | 13-125-4-6,15 | 0 | 35 | 65 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 4 | 71 | 7 | 0 | 0 | 0 | 0 | 3 | 10 | 0 | 0 | 2 | 0 | 0 | 0 |
34.18 | 13-125-4-6,53 | 15 | 10 | 75 | Upper pliocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 2 | 51 | 15 | 0 | 0 | 0 | 0 | 3 | 12 | 0 | 0 | 0 | 0 | 0 | 0 |
34.65 | 13-125-4-61,100 | 10 | 20 | 70 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 2 | 73 | 5 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 5 | 0 | 0 | 0 |
35.20 | 13-125-5-1,20 | 0 | 40 | 60 | Upper pliocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 10 | 73 | 2 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 3 | 0 | 0 | 0 |
35.60 | 13-125-5-1,60 | 0 | 15 | 85 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 2 | 81 | 5 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 2 | 0 | 0 | 0 | 0 |
36.28 | 13-125-5-11,128 | 0 | 10 | 90 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 80 | 0 | 0 | 0 | 0 | 0 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
36.31 | 13-125-5-11,131 | 30 | 40 | 30 | Upper pliocene | SAPROPELIC SILT | Dominat lithology; numerical abundance | 20 | 10 | 25 | 0 | 0 | 0 | 0 | 10 | 20 | 0 | 0 | 10 | 5 | 0 | 0 | 0 |
38.10 | 13-125-5-CC,0 | 20 | 10 | 50 | Upper pliocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 1 | 50 | 10 | 2 | 4 | 0 | 0 | 5 | 15 | 0 | 7 | 2 | 5 | 0 | 0 |
38.10 | 13-125-5-CC,0 | 5 | 30 | 85 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 7 | 0 | 0 | 0 | 0 | 7 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
45.00 | 13-125-6-11,100 | 1 | 9 | 90 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 3 | 85 | 0 | 0 | 0 | 0 | 0 | 4 | 5 | 0 | 3 | 1 | 0 | 0 | 0 |
46.58 | 13-125-6-21,108 | 2 | 18 | 80 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 3 | 80 | 3 | 0 | 0 | 0 | 0 | 4 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
47.82 | 13-125-6-3,82 | 15 | 20 | 65 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 3 | 85 | 5 | 0 | 0 | 2 | 0 | 3 | 1 | 0 | 3 | 0 | 0 | 0 | 0 |
55.15 | 13-125-7-2,65 | 5 | 20 | 75 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 5 | 82 | 7 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
58.00 | 13-125-7-4,50 | 10 | 15 | 75 | Upper pliocene | MARL OOZE | Dominat lithology; numerical abundance | 0 | 5 | 52 | 20 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 3 | 7 | 0 | 3 |
59.40 | 13-125-7-5,40 | 0 | 10 | 90 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 3 | 77 | 10 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 0 | 0 | 0 | 0 | 0 |
62.45 | 13-125-8-CC,45 | 2 | 13 | 85 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 82 | 0 | 0 | 0 | 0 | 0 | 5 | 12 | 0 | 3 | 0 | 0 | 0 | 2 |
71.10 | 13-125-9-CC,0 | 0 | 0 | 0 | DOLOMITE, ANHYDRITE | Dominat lithology; numerical abundance | 15 | 30 | 0 | 30 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | |
80.40 | 13-125-10-CC,0 | 0 | 0 | 0 | ANHYDRITE OOZE | Dominat lithology; numerical abundance | 0 | 0 | 50 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | |
89.60 | 13-125-11-CC,0 | 0 | 0 | 0 | MARL | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
89.60 | 13-125-11-CC,0 | 0 | 0 | 0 | OOLITIC TYPE ANHYDRITE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |