Schulz, Hartmut (1995): Planktic foraminifera assemblage in sediment core 108-659A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.134090, In supplement to: Schulz, H (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums = Sea-surface temperatures 10,000 years B.P. - consequences of the early Holocene insolation maximum. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp, https://doi.org/10.2312/reports-gpi.1995.73
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Project(s):
Coverage:
Latitude: 18.077200 * Longitude: -21.026200
Date/Time Start: 1986-03-09T09:30:00 * Date/Time End: 1986-03-11T05:30:00
Minimum DEPTH, sediment/rock: 0.550 m * Maximum DEPTH, sediment/rock: 0.550 m
Event(s):
108-659A * Latitude: 18.077200 * Longitude: -21.026200 * Date/Time Start: 1986-03-09T09:30:00 * Date/Time End: 1986-03-11T05:30:00 * Elevation: -3082.0 m * Penetration: 273.8 m * Recovery: 174.95 m * Location: North Atlantic Ocean * Campaign: Leg108 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 273.8 m cored; 0 m drilled; 63.9 % recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
35 data points
Data
1 Depth sed [m] | 2 G. aequilateralis [%] | 3 G. bulloides [%] | 4 G. calida [%] | 5 G. conglomerata [%] | 6 G. conglobatus [%] | 7 G. crassaformis [%] | 8 S. dehiscens [%] | 9 G. digitata [%] | 10 N. dutertrei [%] | 11 G. falconensis [%] | 12 G. glutinata [%] | 13 G. hirsuta [%] | 14 G. humilis [%] | 15 G. inflata [%] | 16 G. menardii [%] | 17 C. nitida [%] | 18 P. obliquiloculata [%] | 19 N. pachyderma s [%] | 20 P/D int [%] | 21 H. pelagica [%] | 22 G. quinqueloba [%] | 23 G. ruber p [%] | 24 G. ruber w [%] | 25 G. rubescens [%] | 26 G. trilobus sac [%] | 27 G. sacculifer sac [%] | 28 G. scitula [%] | 29 G. tenellus [%] | 30 G. truncatulinoides s [%] | 31 G. truncatulinoides d [%] | 32 G. truncatulinoides [%] | 33 G. tumida [%] | 34 O. universa [%] | 35 G. uvula [%] | 36 N. pachyderma d [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.550 | 1.3 | 22.3 | 0.5 | 0.0 | 0.0 | 0.2 | 0.0 | 1.1 | 5.3 | 0.0 | 10.6 | 0.0 | 0.0 | 25.4 | 0.3 | 0.0 | 0.4 | 0.0 | 10.1 | 0.0 | 0.5 | 6.9 | 9.3 | 1.1 | 1.1 | 0.3 | 0.0 | 1.1 | 1.3 | 0.0 | 1.3 | 0.1 | 0.9 | 0.0 | 10.1 |