Kuhnt, Wolfgang (1992): (Table 1) Diversity of agglutinated foraminifera from Cenomanian to Santonian sediments of ODP Hole 103-641A in the eastern North Atlantic [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.690405, In supplement to: Kuhnt, W (1992): Abyssal recolonization by benthic foraminifera after the Cenomanian/Turonian boundary anoxic event in the North Atlantic. Marine Micropaleontology, 19(3), 257-274, https://doi.org/10.1016/0377-8398(92)90032-F
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 42.155000 * Longitude: -12.181700
Date/Time Start: 1985-06-08T03:30:00 * Date/Time End: 1985-06-10T14:30:00
Minimum Elevation: -4646.0 m * Maximum Elevation: -4646.0 m
Event(s):
103-641A * Latitude: 42.155000 * Longitude: -12.181700 * Date/Time Start: 1985-06-08T03:30:00 * Date/Time End: 1985-06-10T14:30:00 * Elevation: -4646.0 m * Penetration: 63.6 m * Recovery: 40.37 m * Location: South Atlantic Ocean * Campaign: Leg103 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 7 cores; 63.6 m cored; 0 m drilled; 63.5 % recovery
Comment:
20 to 30 cm**3 sample size, completely disaggregated in a calgon-water solution
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Kuhnt, Wolfgang | DSDP/ODP/IODP sample designation | ||
| 2 | Number of species | Spec No | # | Kuhnt, Wolfgang | Counting >63 µm fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
| 1 Sample label | 2 Spec No [#] |
|---|---|
| 103-641A-4-1,20 | 14 |
| 103-641A-4-1,48 | 19 |
| 103-641A-4-1,65 | 9 |
| 103-641A-4-CC | 17 |
| 103-641A-5-1,40 | 9 |
| 103-641A-5-1,71 | 11 |
| 103-641A-5-2,50 | 8 |
| 103-641A-5-2,96 | 10 |
| 103-641A-5-3,40 | 9 |
| 103-641A-5-3,55 | 9 |
| 103-641A-5-CC | 18 |
| 103-641A-6-1,95 | 3 |
| 103-641A-6-2,30 | 9 |
| 103-641A-6-2,56 | 7 |
| 103-641A-6-2,95 | 6 |
| 103-641A-6-3,30 | 6 |
| 103-641A-6-3,94 | 4 |
| 103-641A-6-4,30 | 5 |
| 103-641A-6-4,76 | 4 |
| 103-641A-6-6,33 | 10 |
| 103-641A-6-7,15 | 10 |
| 103-641A-6-7,24 | 4 |
| 103-641A-6-7,26 | 7 |
| 103-641A-6-7,31 | 2 |
| 103-641A-6-7,35 | 0 |