Mao, Shaozhi; Wise, Sherwood W (1994): (Table 8) Distribution of calcareous nannofossils in ODP Hole 139-857C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.820675, In supplement to: Mao, S; Wise, SW (1994): Late Quaternary Calcareous Nannofossils from the Sedimented Middle Valley of the Juan de Fuca Ridge, Leg 139. In: Mottl, MJ; Davis, EE; Fisher, AT; Slack, JF (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 139, 59-76, https://doi.org/10.2973/odp.proc.sr.139.208.1994
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 48.441400 * Longitude: -128.711000
Date/Time Start: 1991-08-08T13:30:00 * Date/Time End: 1991-08-09T08:00:00
Minimum DEPTH, sediment/rock: 2.75 m * Maximum DEPTH, sediment/rock: 392.23 m
Event(s):
139-857C * Latitude: 48.441400 * Longitude: -128.711000 * Date/Time Start: 1991-08-08T13:30:00 * Date/Time End: 1991-08-09T08:00:00 * Elevation: -2433.0 m * Penetration: 567.7 m * Recovery: 169.04 m * Location: North Pacific Ocean * Campaign: Leg139 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 68 cores; 514.7 m cored; 0 m drilled; 32.8 % recovery
Comment:
Species abundance: A = (abundant >10-100 specimens/field of view), C = common (1-10 specimens/field), F = few (1 specimen/2-10 fields), R = rare (1 specimen/11-100 fields).
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 | Mao, Shaozhi | DSDP/ODP/IODP sample designation | ||
3 | Nannofossil abundance | Nannos abund | Mao, Shaozhi | Smear slide analysis | A = abundanv, C = common, F = few, R = rare, B = barren | |
4 | Nannofossils preservation | Nannos preserv | Mao, Shaozhi | Smear slide analysis | G = good, M = moderate, P = poor, VP = very poor | |
5 | Braarudosphaera bigelowii | B. bigelowii | Mao, Shaozhi | Smear slide analysis | ||
6 | Calcidiscus leptoporus | C. leptoporus | Mao, Shaozhi | Smear slide analysis | ||
7 | Coccolithus crassipons | C. crassipons | Mao, Shaozhi | Smear slide analysis | ||
8 | Coccolithus pelagicus | C. pelagicus | Mao, Shaozhi | Smear slide analysis | ||
9 | Emiliania huxleyi | E. huxleyi | Mao, Shaozhi | Smear slide analysis | ||
10 | Gephyrocapsa spp. | Gephyrocapsa spp. | Mao, Shaozhi | Smear slide analysis | group 1 | |
11 | Gephyrocapsa spp. | Gephyrocapsa spp. | Mao, Shaozhi | Smear slide analysis | group 2 | |
12 | Gephyrocapsa spp. | Gephyrocapsa spp. | Mao, Shaozhi | Smear slide analysis | group 3 | |
13 | Gephyrocapsa spp. | Gephyrocapsa spp. | Mao, Shaozhi | Smear slide analysis | group 4 | |
14 | Pontosphaera sp. | Pontosphaera sp. | Mao, Shaozhi | Smear slide analysis | ||
15 | Reticulofenestra sp. | Reticulofenestra sp. | Mao, Shaozhi | Smear slide analysis | ||
16 | Nannofossil zone | Nannos zone | Mao, Shaozhi | Nannofossil Zone; Martini, 1971 | ||
17 | Epoch | Epoch | Mao, Shaozhi |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
816 data points
Data
1 Depth sed [m] | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Nannos abund (A = abundanv, C = common, F =...) | 4 Nannos preserv (G = good, M = moderate, P = p...) | 5 B. bigelowii (Smear slide analysis) | 6 C. leptoporus (Smear slide analysis) | 7 C. crassipons (Smear slide analysis) | 8 C. pelagicus (Smear slide analysis) | 9 E. huxleyi (Smear slide analysis) | 10 Gephyrocapsa spp. (group 1, Smear slide analysis) | 11 Gephyrocapsa spp. (group 2, Smear slide analysis) | 12 Gephyrocapsa spp. (group 3, Smear slide analysis) | 13 Gephyrocapsa spp. (group 4, Smear slide analysis) | 14 Pontosphaera sp. (Smear slide analysis) | 15 Reticulofenestra sp. (Smear slide analysis) | 16 Nannos zone (Nannofossil Zone; Martini, 1971) | 17 Epoch |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2.75 | 139-857C-1R-2,125-129 | C | P | - | - | - | F | F | C | F | - | R | - | - | NN21 | Holocene |
56.56 | 139-857C-2R-1,6-11 | C | P | R | - | R | C | R | C | F | - | R | - | - | NN21 | late Pleistocene |
58.50 | 139-857C-2R-2,50-53 | C | M | R | - | - | F | F | C | - | - | - | - | - | NN21 | late Pleistocene |
67.48 | 139-857C-3R-1,98100 | C | P | - | - | R | F | R | C | F | - | - | - | - | NN21 | late Pleistocene |
68.93 | 139-857C-3R-2,93-95 | C | M | - | - | - | R | F | C | R | - | - | - | - | NN21 | late Pleistocene |
69.97 | 139-857C-3R-3,47-49 | C | M | - | - | - | R | R | C | R | - | - | - | - | NN21 | late Pleistocene |
82.41 | 139-857C-5R-1,31-35 | R | VP | - | - | - | - | - | R | - | - | - | - | - | NN21 | late Pleistocene |
82.66 | 139-857C-5R-4,6-9 | R | VP | - | - | - | R | - | - | - | - | - | - | - | NN21 | late Pleistocene |
85.46 | 139-857C-5R-5,36-38 | R | VP | - | - | - | R | - | - | - | - | - | - | - | NN21 | late Pleistocene |
87.39 | 139-857C-6R-1,119-121 | F | P | - | - | - | R | - | F | F | R | - | - | - | NN21 | late Pleistocene |
88.64 | 139-857C-6R-2,94-69 | F | P | - | - | - | F | - | R | - | - | - | - | - | NN21 | late Pleistocene |
115.50 | 139-857C-9R-1,100-102 | R | P | - | - | - | R | - | R | - | - | - | - | - | NN21 | late Pleistocene |
124.13 | 139-857C-10R-1,3-5 | R | M | - | - | - | R | - | - | - | - | - | - | - | NN21 | late Pleistocene |
133.92 | 139-857C-11R-1,12-14 | F | M | - | - | - | R | F | F | F | R | - | - | R | NN21 | late Pleistocene |
134.66 | 139-857C-11R-1,86-88 | F | P | - | - | - | R | R | R | F | - | - | - | R | NN21 | late Pleistocene |
144.50 | 139-857C-12R-1,100-103 | F | P | - | - | - | R | - | R | - | - | R | - | - | NN21 | late Pleistocene |
145.63 | 139-857C-12R-2,63-66 | R | P | - | - | - | - | R | R | R | R | - | - | - | NN21 | late Pleistocene |
153.86 | 139-857C-13R-1,76-80 | R | M | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
155.15 | 139-857C-13R-2,55-57 | R | P | - | - | - | R | - | - | - | - | - | R | - | ? | ? |
156.46 | 139-857C-13R-3,36-38 | R | P | - | R | - | R | - | - | - | R | - | - | - | ? | ? |
163.04 | 139-857C-14R-1,24-28 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
172.77 | 139-857C-15R-1,27-29 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
174.29 | 139-857C-15R-2,29-31 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
175.90 | 139-857C-15R-3,40-42 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
202.52 | 139-857C-18R-1,92-96 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
232.97 | 139-857C-21R-1,88-89 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
275.10 | 139-857C-26R-1,60-62 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
294.92 | 139-857C-28R-1,112-114 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
295.46 | 139-857C-28R-2,16-18 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
296.99 | 139-857C-28R-3,19-22 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
303.85 | 139-857C-29R-1,45-49 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
316.17 | 139-857C-30R-3,7-9 | F | VP | - | - | - | F | - | R | - | - | - | - | - | ? | ? |
316.70 | 139-857C-30R-3,60-63 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
329.83 | 139-857C-33R-2,63-65 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
337.21 | 139-857C-34R-1,71-74 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
351.29 | 139-857C-37R-1,49-53 | F | P | - | - | - | F | - | - | - | - | - | - | - | ? | ? |
354.05 | 139-857C-37R-3,25-29 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
356.91 | 139-857C-38R-1,111-115 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
360.58 | 139-857C-39R-1,18-20 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
362.36 | 139-857C-39R-2,46-48 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
364.20 | 139-857C-39R-3,80-82 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
365.61 | 139-857C-40R-1,21-24 | F | P | - | - | - | F | - | - | - | - | - | - | - | ? | ? |
365.76 | 139-857C-40R-1,36-39 | F | P | - | - | - | F | - | - | - | - | - | - | - | ? | ? |
367.58 | 139-857C-40R-2,68-72 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
375.52 | 139-857C-41R-1,62-66 | F | P | - | - | - | F | - | - | - | - | - | - | - | ? | ? |
377.43 | 139-857C-41R-2,103-106 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
378.47 | 139-857C-41R-3,57-60 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
380.06 | 139-857C-42R-1,36-40 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
381.54 | 139-857C-42R-2,34-37 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
386.43 | 139-857C-43R-2,23-26 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |
392.23 | 139-857C-44R-2,105-109 | R | P | - | - | - | R | - | - | - | - | - | - | - | ? | ? |