Volokhin, Yu G; Astakhov, Anatolii S; Vashchenkova, N G (2004): (Table 1) Sedimentation rates and accumulation rates of Upper Pleistocene and Holocene bottom sediments from the Sea of Okhotsk and silica accumulation rates in these sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.785139, In supplement to: Volokhin, YG et al. (2004): Holocene Siliceous Sediments in the Sea of Okhotsk. Lithology and Mineral Resources, 39(3), 259-280, https://doi.org/10.1023/B:LIMI.0000027612.41153.6c
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 52.630679 * Median Longitude: 148.771291 * South-bound Latitude: 46.973300 * West-bound Longitude: 144.731700 * North-bound Latitude: 58.583333 * East-bound Longitude: 153.623300
Date/Time Start: 1996-09-20T00:00:00 * Date/Time End: 1996-09-20T00:00:00
Minimum DEPTH, sediment/rock: 0.150 m * Maximum DEPTH, sediment/rock: 5.740 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
6 | Depth, top/min | Depth top | m | Volokhin, Yu G | ||
7 | Depth, bottom/max | Depth bot | m | Volokhin, Yu G | ||
8 | Stage | Stage | Volokhin, Yu G | oxygen isotope (OIS) | ||
9 | Epoch | Epoch | Volokhin, Yu G | |||
10 | Sedimentation rate | SR | cm/ka | Volokhin, Yu G | ||
11 | Accumulation rate, mass | MAR | g/cm2/ka | Volokhin, Yu G | ||
12 | Accumulation rate, opal | Acc rate opal | g/cm2/ka | Volokhin, Yu G | ||
13 | Accumulation rate, silica | Acc rate SiO2 | g/cm2/ka | Volokhin, Yu G | free |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
136 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Depth top [m] | 7 Depth bot [m] | 8 Stage | 9 Epoch | 10 SR [cm/ka] | 11 MAR [g/cm2/ka] | 12 Acc rate opal [g/cm2/ka] | 13 Acc rate SiO2 [g/cm2/ka] |
---|---|---|---|---|---|---|---|---|---|---|---|---|
MG34-89211 | 58.5833 | 145.4700 | -140 | 0.925 | 0.00 | 1.85 | I | Holocene | 17.5 | 12.3 | 1.61 | 4.89 |
MG34-89211 | 58.5833 | 145.4700 | -140 | 1.900 | 1.85 | 1.95 | II | Late Pleistocene | ||||
MG34-89224 | 57.1667 | 144.7317 | -235 | 0.200 | 0.00 | 0.40 | I | Holocene | 3.2 | 2.8 | 0.67 | 1.34 |
MG34-89224 | 57.1667 | 144.7317 | -235 | 0.435 | 0.40 | 0.47 | II | Late Pleistocene | ||||
LV27-2 | 54.5025 | 144.7523 | -1305 | 2.050 | 0.00 | 4.10 | I | Holocene | 32.8 | 12.5 | 3.84 | 6.82 |
LV27-2 | 54.5025 | 144.7523 | -1305 | 5.740 | 4.10 | 7.38 | II | Late Pleistocene | >28.5 | >18.5 | >1.42 | >4.83 |
LV27-5-3 | 54.7682 | 149.4985 | -482 | 0.275 | 0.00 | 0.55 | I | Holocene | 4.4 | 2.1 | 0.65 | 1.11 |
LV27-5-3 | 54.7682 | 149.4985 | -482 | 1.175 | 0.55 | 1.80 | II | Late Pleistocene | 10.9 | 11.1 | ||
AN25-936 | 51.0150 | 148.3133 | -1310 | 0.800 | 0.00 | 1.60 | I | Holocene | 12.8 | 4.2 | 1.56 | 2.44 |
AN25-936 | 51.0150 | 148.3133 | -1310 | 2.300 | 1.60 | 3.00 | II | Late Pleistocene | 12.2 | 4.6 | ||
AN25-935 | 49.2967 | 150.3217 | -1110 | 0.150 | 0.00 | 0.30 | I | Holocene | 2.4 | 1.8 | 0.05 | 0.53 |
AN25-935 | 49.2967 | 150.3217 | -1110 | 1.600 | 0.30 | 2.90 | II | Late Pleistocene | 22.6 | 15.1 | ||
AN25-934 | 48.5417 | 150.6817 | -2195 | 2.000 | 0.00 | 4.00 | I | Holocene | 32.0 | 11.2 | 4.61 | 6.47 |
AN25-934 | 48.5417 | 150.6817 | -2195 | 4.550 | 4.00 | 5.10 | II | Late Pleistocene | ||||
AN25-931 | 48.2517 | 150.4200 | -3255 | 2.650 | 0.00 | 5.30 | I | Holocene | 42.5 | 23.0 | 5.70 | 11.60 |
AN25-931 | 48.2517 | 150.4200 | -3255 | 5.500 | 5.30 | 5.70 | II | Late Pleistocene | ||||
HS-2 | 46.9733 | 150.9700 | -3300 | 0.300 | 0.00 | 0.60 | I | Holocene | >4.8 | >7.5 | >1.12 | >3.08 |
N7-974 | 55.5667 | 153.6233 | -710 | 1.500 | 0.00 | 3.00 | I | Holocene | >24.0 | >15.1 | >2.78 | >6.80 |
N7-986 | 54.2717 | 147.7017 | -950 | 0.350 | 0.00 | 0.70 | I | Holocene | 5.6 | 3.0 | 0.66 | 1.32 |
N7-986 | 54.2717 | 147.7017 | -950 | 0.950 | 0.70 | 1.20 | II | Late Pleistocene | 4.3 | 2.4 |