Thiede, Jörn (1973): Planktic foraminifera of surface sediments off Portugal and Morocco (Table 4) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.510743, In supplement to: Thiede, J (1973): Sedimentation rates of planktonic and benthic foraminifera in sediments from the Atlantic continental margin of Portugal and Morocco. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C16, 1-18
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Coverage:
Median Latitude: 36.119009 * Median Longitude: -9.681283 * South-bound Latitude: 33.432800 * West-bound Longitude: -10.853333 * North-bound Latitude: 37.916667 * East-bound Longitude: -9.133000
Date/Time Start: 1967-01-17T14:00:00 * Date/Time End: 1967-07-19T13:30:00
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
M8_004-2 (M8004B) * Latitude: 37.916000 * Longitude: -10.853000 * Date/Time Start: 1967-01-17T14:00:00 * Date/Time End: 1967-01-18T02:06:00 * Elevation: -4979.0 m * Recovery: 1.41 m * Location: South Atlantic Ocean * Campaign: M8 (Atlantische Kuppenfahrten 1967/1-3) * Basis: Meteor (1964) * Method/Device: Kasten corer (KAL)
M8_006-2 (M8006B) * Latitude: 37.716000 * Longitude: -10.550000 * Date/Time Start: 1967-07-19T07:30:00 * Date/Time End: 1967-07-19T13:30:00 * Elevation: -3666.0 m * Recovery: 3.09 m * Location: South Atlantic Ocean * Campaign: M8 (Atlantische Kuppenfahrten 1967/1-3) * Basis: Meteor (1964) * Method/Device: Kasten corer (KAL)
M8_007-2 (M8007B) * Latitude: 37.700000 * Longitude: -9.766000 * Date/Time Start: 1967-01-19T16:24:00 * Date/Time End: 1967-01-19T23:00:00 * Elevation: -1899.0 m * Recovery: 4.49 m * Location: South Atlantic Ocean * Campaign: M8 (Atlantische Kuppenfahrten 1967/1-3) * Basis: Meteor (1964) * Method/Device: Kasten corer (KAL)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | LATITUDE | Latitude | Geocode | |||
| 3 | LONGITUDE | Longitude | Geocode | |||
| 4 | Elevation of event | Elevation | m | |||
| 5 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 6 | Sedimentation rate | SR | cm/ka | Thiede, Jörn | Calculated | |
| 7 | Solution | Solu | % | Thiede, Jörn | ||
| 8 | Solution | Solu | % | Thiede, Jörn | Globorotalia truncatulinoides | |
| 9 | Foraminifera, benthic | Foram benth | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 10 | Foraminifera, planktic | Foram plankt | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 11 | Orbulina universa | O. universa | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 12 | Globigerinoides ruber | G. ruber | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 13 | Globigerinoides sacculifer | G. sacculifer | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 14 | Globigerina bulloides | G. bulloides | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 15 | Globigerina pachyderma | G. pachyderma | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 16 | Globorotalia hirsuta | G. hirsuta | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 17 | Globorotalia inflata | G. inflata | #/g | Thiede, Jörn | Counting 200-630 µm fraction | |
| 18 | Globorotalia truncatulinoides | G. truncatulinoides | #/g | Thiede, Jörn | Counting 200-630 µm fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
200 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 SR [cm/ka] (Calculated) | 7 Solu [%] | 8 Solu [%] (Globorotalia truncatulinoides) | 9 Foram benth [#/g] (Counting 200-630 µm fraction) | 10 Foram plankt [#/g] (Counting 200-630 µm fraction) | 11 O. universa [#/g] (Counting 200-630 µm fraction) | 12 G. ruber [#/g] (Counting 200-630 µm fraction) | 13 G. sacculifer [#/g] (Counting 200-630 µm fraction) | 14 G. bulloides [#/g] (Counting 200-630 µm fraction) | 15 G. pachyderma [#/g] (Counting 200-630 µm fraction) | 16 G. hirsuta [#/g] (Counting 200-630 µm fraction) | 17 G. inflata [#/g] (Counting 200-630 µm fraction) | 18 G. truncatulinoides [#/g] (Counting 200-630 µm fraction) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| M10773-2 | 37.7033 | -9.4733 | -1071.0 | 0 | 123 | 1802 | 42 | 163 | 76 | 732 | 233 | 32 | 261 | 107 | |||
| M10774-1 | 37.6117 | -9.2833 | -600.0 | 0 | 436 | 1951 | 56 | 50 | 44 | 789 | 330 | 35 | 265 | 147 | |||
| M8_004-2 | 37.9167 | -10.8533 | -4979.0 | 0 | 9 | 165 | 5 | 9 | 6 | 11 | 20 | 8 | 85 | 8 | |||
| M8_006-2 | 37.7167 | -10.5500 | -3666.0 | 0 | 19 | 576 | 17 | 53 | 54 | 88 | 82 | 21 | 187 | 27 | |||
| M8_007-2 | 37.7000 | -9.7667 | -1899.0 | 0 | 26 | 345 | 11 | 35 | 33 | 103 | 45 | 10 | 51 | 21 | |||
| M8_008-3 | 37.6500 | -9.5333 | -1148.0 | 0 | 46 | 715 | 13 | 55 | 40 | 284 | 80 | 14 | 98 | 51 | |||
| M8_016-2 | 33.8498 | -9.7170 | -4354.0 | 0 | 7.1 | 5 | 10 | 25 | 1797 | 34 | 377 | 315 | 402 | 46 | 56 | 184 | 164 |
| M8_017-2 | 33.6200 | -9.4083 | -3016.0 | 0 | 5.7 | 0 | 10 | 14 | 2352 | 47 | 501 | 289 | 495 | 85 | 59 | 278 | 249 |
| M8_018-4 | 33.5998 | -9.3998 | -1754.0 | 0 | 2.9 | 10 | 12 | 52 | 2745 | 83 | 566 | 330 | 636 | 73 | 90 | 351 | 320 |
| M8_019-2 | 33.5533 | -9.3383 | -1311.0 | 0 | 5.7 | 20 | 13 | 238 | 4954 | 143 | 956 | 469 | 885 | 291 | 226 | 909 | 624 |
| M8_020-2 | 33.4500 | -9.3167 | -823.0 | 0 | 14.3 | 10 | 20 | 377 | 4045 | 81 | 637 | 383 | 962 | 284 | 145 | 701 | 533 |
| M8_021-3 | 33.4328 | -9.1330 | -510.0 | 0 | 30 | 28 | 1109 | 3866 | 15 | 121 | 749 | 1200 | 327 | 137 | 547 | 410 | |
| M8_031-2 | 34.7998 | -10.2500 | -4144.0 | 0 | 2.9 | 10 | 11 | 28 | 3563 | 67 | 790 | 595 | 666 | 96 | 103 | 471 | 383 |
| M8_057-2 | 37.6833 | -10.0833 | -2811.0 | 0 | 5 | 379 | 5 | 45 | 23 | 80 | 62 | 19 | 107 | 17 | |||
| M8_058-2 | 37.7500 | -9.7333 | -1819.0 | 0 | 23 | 357 | 9 | 32 | 23 | 128 | 33 | 13 | 78 | 12 | |||
| M8_061-1 | 37.7083 | -9.2267 | -498.0 | 0 | 449 | 977 | 18 | 65 | 16 | 437 | 130 | 34 | 163 | 65 | |||
| M8_066-2 | 37.0000 | -9.8000 | -2710.0 | 0 | 5 | 213 | 7 | 37 | 16 | 31 | 24 | 8 | 53 | 7 | |||
| M8_074-2 | 37.3967 | -9.3967 | -1088.0 | 0 | 30 | 224 | 6 | 14 | 16 | 102 | 14 | 6 | 40 | 6 |