Hsü, Kenneth J; Montadert, Lucien; Ross, David A (2005): Smear slide analysis of Hole 42-378 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230712
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
Worstell, Paula J; Mélières, Frédéric; Bernoulli, Daniel; Erickson, A J; Wright, Ramil; Bizon, G; Cita, Maria Bianca; Müller, Carla; Kidd, Robert B; Fabricius, F H; Garrison, Robert E; Hsü, Kenneth J; Montadert, Lucien (1978): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XLII Pt. 1, 1249 pp + 1244 pp, https://doi.org/10.2973/dsdp.proc.42-1.1978
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Funding:
Sixth Framework Programme (FP6), grant/award no. 36949: Southern European Seas: Assessing and Modelling Ecosystem Changes
Coverage:
Latitude: 35.927800 * Longitude: 25.116200
Date/Time Start: 1975-05-17T00:00:00 * Date/Time End: 1975-05-17T00:00:00
Minimum DEPTH, sediment/rock: 85.10 m * Maximum DEPTH, sediment/rock: 308.60 m
Event(s):
42-378 * Latitude: 35.927800 * Longitude: 25.116200 * Date/Time: 1975-05-17T00:00:00 * Elevation: -1835.0 m * Penetration: 312 m * Recovery: 34.3 m * Location: Aegean Sea/BASIN * Campaign: Leg42 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 103.5 m cored; 0 m drilled; 33.2 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Mica | Mica | % | Smear slide analysis | ||
20 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Glauconite | Glt | % | Smear slide analysis | ||
22 | Opaque minerals | Opaque | % | Smear slide analysis | ||
23 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
24 | Iron | Fe | % | Smear slide analysis | ||
25 | Heavy minerals | HM | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Organic matter | OM | % | Smear slide analysis | organic debris |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1482 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 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Mica [%] | 20 Clay min [%] | 21 Glt [%] | 22 Opaque [%] | 23 Py [%] | 24 Fe [%] | 25 HM [%] | 26 Volc glass [%] | 27 OM [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
85.10 | 42-378-1-11,110 | 0 | 10 | 90 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
85.70 | 42-378-1-2,20 | 10 | 20 | 80 | Pleistocene | NANNO MARL (SAPROPELIC) | Minor lithology; relative abundance | 10 | 0 | 30 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 0 | 0 | 20 |
86.18 | 42-378-1-2,68 | 0 | 20 | 0 | Pleistocene | NANNO SAPROPEL MARL | Dominat lithology; relative abundance | 10 | 0 | 40 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 8 | 0 | 0 | 0 | 40 |
86.57 | 42-378-1-21,107 | 10 | 20 | 80 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 5 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
87.10 | 42-378-1-CC,0 | 5 | 30 | 65 | Pleistocene | NANNO MARL | Dominat lithology; numerical abundance | 10 | 0 | 40 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
94.86 | 42-378-2-11,136 | 10 | 10 | 90 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 45 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 45 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
95.75 | 42-378-2-2,75 | 10 | 10 | 90 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
98.75 | 42-378-2-4,75 | 5 | 10 | 85 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 45 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
100.24 | 42-378-2-5,74 | 10 | 10 | 90 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
100.75 | 42-378-2-51,125 | 5 | 15 | 80 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 20 | 0 | 50 | 6 | 2 | 0 | 0 | 0 | 6 | 0 | 0 | 20 | 0 | 0 | 6 | 0 | 0 | 0 | 10 |
101.10 | 42-378-2-CC,0 | 10 | 15 | 80 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
103.87 | 42-378-3-1,87 | 5 | 20 | 75 | Pleistocene | NANNO SAPROPELIC MARL | Minor lithology; relative abundance | 15 | 0 | 25 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 5 | 0 | 0 | 0 | 30 |
104.20 | 42-378-3-11,120 | 5 | 10 | 85 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 0 | 0 | 50 | 5 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
105.25 | 42-378-3-2,75 | 10 | 20 | 80 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 40 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
106.75 | 42-378-3-3,75 | 0 | 10 | 90 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 40 | 6 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 35 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
107.17 | 42-378-3-31,117 | 5 | 30 | 65 | Pleistocene | SILTY SAPROPEL MARL | Dominat lithology; relative abundance | 10 | 0 | 10 | 6 | 2 | 0 | 0 | 6 | 5 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 40 |
107.41 | 42-378-3-31,140.5 | 10 | 20 | 80 | Pleistocene | NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 40 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 2 | 0 |
112.60 | 42-378-4-CC,0 | 0 | 0 | 0 | Pleistocene | INSOLUBLE RESIDUE | Dominat lithology; relative abundance | 10 | 0 | 50 | 3 | 0 | 0 | 2 | 5 | 2 | 0 | 6 | 40 | 2 | 0 | 5 | 0 | 6 | 5 | 0 |
112.60 | 42-378-4-CC,0 | 10 | 10 | 90 | Pleistocene | NANNO MARL | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
122.83 | 42-378-5-1,83 | 10 | 40 | 60 | Upper pliocene | DIAT NANNO MARL (SLIGHTLY SAPROPELIC) | Minor lithology; relative abundance | 0 | 0 | 40 | 0 | 6 | 20 | 6 | 6 | 5 | 0 | 0 | 35 | 0 | 0 | 6 | 0 | 0 | 0 | 10 |
123.00 | 42-378-5-11,100 | 1 | 5 | 95 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 5 | 0 | 50 | 6 | 0 | 2 | 0 | 2 | 6 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
142.34 | 42-378-6-11,134 | 10 | 30 | 70 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 50 | 5 | 0 | 0 | 0 | 0 | 6 | 0 | 2 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
142.46 | 42-378-6-11,146 | 10 | 15 | 85 | Upper pliocene | SAPROPEL | Minor lithology; relative abundance | 10 | 0 | 35 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 20 | 0 | 0 | 5 | 0 | 0 | 2 | 25 |
143.25 | 42-378-6-2,75 | 10 | 20 | 80 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 6 | 0 | 2 | 40 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
144.60 | 42-378-6-3,60 | 10 | 10 | 90 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
144.84 | 42-378-6-3,84 | 10 | 10 | 90 | Upper pliocene | SAPROPEL | Minor lithology; relative abundance | 10 | 0 | 40 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 0 | 20 |
170.14 | 42-378-7-1,64 | 10 | 15 | 85 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 15 | 0 | 40 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
171.05 | 42-378-7-2,5 | 15 | 55 | 30 | Upper pliocene | SANDY MUD | Minor lithology; relative abundance | 15 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 50 | 5 | 0 | 15 | 0 | 5 | 5 | 0 | 0 | 6 | 0 |
171.73 | 42-378-7-2,73 | 10 | 10 | 90 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 15 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
172.56 | 42-378-7-3,6 | 10 | 10 | 90 | Upper pliocene | NANNO MARL | Minor lithology; numerical abundance | 20 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
173.25 | 42-378-7-3,75 | 0 | 10 | 90 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 40 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
173.76 | 42-378-7-31,126.5 | 5 | 10 | 0 | Upper pliocene | NANNO MARL | Minor lithology; relative abundance | 20 | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 6 | 15 | 0 |
174.40 | 42-378-7-4,40 | 10 | 20 | 80 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 30 | 5 | 0 | 0 | 0 | 0 | 5 | 0 | 6 | 40 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
174.46 | 42-378-7-4,46 | 5 | 20 | 75 | Upper pliocene | SILTY NANNO MARL (SAPROPEL) | Dominat lithology; relative abundance | 10 | 0 | 30 | 5 | 0 | 0 | 0 | 6 | 6 | 0 | 2 | 30 | 0 | 0 | 5 | 0 | 0 | 0 | 20 |
174.71 | 42-378-7-4,71 | 5 | 0 | 0 | Upper pliocene | NANNO BEARING MARL (SAPROPEL) | Minor lithology; relative abundance | 0 | 0 | 30 | 5 | 2 | 0 | 0 | 6 | 5 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 30 |
174.90 | 42-378-7-4,90 | 5 | 30 | 65 | Upper pliocene | SANDY NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 30 | 5 | 0 | 0 | 0 | 6 | 5 | 0 | 0 | 35 | 0 | 0 | 6 | 0 | 6 | 0 | 10 |
176.35 | 42-378-7-5,85 | 10 | 20 | 80 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 5 | 0 | 2 | 0 | 0 |
217.60 | 42-378-8-1,60 | 10 | 15 | 85 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 15 | 0 | 40 | 6 | 0 | 6 | 6 | 6 | 6 | 0 | 0 | 45 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
218.25 | 42-378-8-11,125 | 10 | 30 | 60 | Upper pliocene | DIAT NANNO MUD | Minor lithology; relative abundance | 10 | 0 | 25 | 5 | 0 | 2 | 6 | 5 | 5 | 0 | 0 | 10 | 0 | 0 | 6 | 0 | 0 | 0 | 20 |
218.50 | 42-378-8-2,0 | 0 | 30 | 70 | Upper pliocene | NANNO DIAT MUD | Minor lithology; relative abundance | 10 | 0 | 30 | 6 | 0 | 40 | 6 | 2 | 5 | 0 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
218.98 | 42-378-8-2,48 | 60 | 30 | 10 | Upper pliocene | TEPHRA SAND | Minor lithology; relative abundance | 5 | 0 | 30 | 6 | 0 | 6 | 0 | 0 | 6 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 50 | 0 |
219.07 | 42-378-8-2,57 | 10 | 10 | 90 | Upper pliocene | NANNO MARL | Minor lithology; relative abundance | 10 | 0 | 40 | 5 | 0 | 6 | 0 | 2 | 6 | 0 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 5 |
219.60 | 42-378-8-21,110 | 0 | 10 | 90 | Upper pliocene | NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 40 | 6 | 0 | 6 | 2 | 2 | 0 | 0 | 0 | 40 | 2 | 0 | 0 | 0 | 0 | 2 | 0 |
220.10 | 42-378-8-CC,0 | 5 | 30 | 65 | Upper pliocene | DIAT BEARING NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 30 | 0 | 0 | 20 | 2 | 5 | 6 | 0 | 0 | 35 | 0 | 0 | 0 | 0 | 0 | 2 | 6 |
283.60 | 42-378-10-CC,0 | 0 | 20 | 80 | Lower pliocene | SILTY NANNO MARL | Dominat lithology; relative abundance | 10 | 0 | 50 | 6 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 35 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
303.96 | 42-378-11-11,146 | 10 | 20 | 80 | Lower pliocene | NANNO MARL (SAPROPELIC) | Minor lithology; relative abundance | 20 | 0 | 35 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 6 | 6 | 0 | 0 | 20 |
304.02 | 42-378-11-2,2 | 0 | 10 | 90 | Lower pliocene | NANNO SAPROPEL (MARLY) | Minor lithology; relative abundance | 15 | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 0 | 20 |
304.03 | 42-378-11-2,2 | 10 | 20 | 80 | Lower pliocene | SAPROPELIC MUD | Minor lithology; relative abundance | 10 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 6 | 40 | 0 | 0 | 6 | 0 | 0 | 6 | 15 |
304.25 | 42-378-11-2,25 | 0 | 20 | 80 | Lower pliocene | SAPROPELIC NANNO MARL | Minor lithology; relative abundance | 15 | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 30 | 0 | 0 | 3 | 0 | 0 | 0 | 15 |
304.76 | 42-378-11-2,76 | 5 | 15 | 80 | Lower pliocene | NANNO MARL | Dominat lithology; relative abundance | 30 | 0 | 30 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
305.32 | 42-378-11-21,132 | 0 | 10 | 90 | Lower pliocene | SAPROPELIC NANNO MARL | Minor lithology; relative abundance | 10 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 30 | 0 | 0 | 3 | 0 | 0 | 0 | 20 |
307.65 | 42-378-11-4,65 | 10 | 15 | 85 | Lower pliocene | (SILTY) SAPROPELIC NANNO MARL | Minor lithology; relative abundance | 10 | 0 | 30 | 6 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 35 | 0 | 0 | 3 | 0 | 0 | 2 | 20 |
307.90 | 42-378-11-4,90 | 0 | 10 | 90 | Lower pliocene | NANNO MARL | Dominat lithology; relative abundance | 20 | 0 | 45 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 30 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
308.28 | 42-378-11-41,128 | 10 | 30 | 60 | Lower pliocene | SAPROPELIC MARL | Minor lithology; relative abundance | 20 | 0 | 10 | 6 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 40 | 0 | 0 | 6 | 0 | 2 | 0 | 20 |
308.60 | 42-378-11-CC,0 | 0 | 0 | 0 | Lower pliocene | CALC MARL | Dominat lithology; relative abundance | 40 | 1 | 20 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
308.60 | 42-378-11-CC,0 | 0 | 10 | 80 | Lower pliocene | DOLOMITE | Dominat lithology; relative abundance | 5 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
308.60 | 42-378-11-CC,0 | 0 | 20 | 90 | Lower pliocene | NANNO MARL | Minor lithology; relative abundance | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |