Mangelsdorf, Kai; Günter, Ute; Rullkötter, Jürgen (2000): (Table 1) Sedimentation rates of ODP Leg 167 holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.757217, In supplement to: Mangelsdorf, K et al. (2000): Climatic and oceanographic variations on the California continental margin during the last 160 kyr. Organic Geochemistry, 31(9), 829-846, https://doi.org/10.1016/S0146-6380(00)00066-8
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Kennett, James P; Roark, E Brendan; Cannariato, Kevin G; Ingram, B Lynn; Tada, Ryuji (2000): Latest Quaternary paleoclimatic and radiocarbon chronology, Hole 1017E, southern California Margin. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 249-254, https://doi.org/10.2973/odp.proc.sr.167.242.2000
Lyle, Mitchell W; Mix, Alan C; Ravelo, Ana Christina; Andreasen, Dyke; Heusser, Linda E; Olivarez, Annette (2000): Millennial-scale CaCO3 and Corg events along the northern and central California margins: stratigraphy and origins. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC Jr (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 1-20, https://doi.org/10.2973/odp.proc.sr.167.214.2000
Mix, Alan C; Lund, David C; Pisias, Nicklas G; Bodén, Per; Bornmalm, Lennart; Pike, Jennifer (1999): Rapid climate oscillations in the northeast Pacific during the last glaciation reflect northern and southern hemispheric sources. In: Clark, Peter U; Webb, Robert S; Keigwin, Lloyd D (eds.), Mechanisms of Millennial-scale Global Climate Change, American Geophysical Union Monography, 112, 127-148, https://doi.org/10.1029/GM112p0127
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 37.735367 * Median Longitude: -123.105000 * South-bound Latitude: 34.534900 * West-bound Longitude: -124.932000 * North-bound Latitude: 41.682900 * East-bound Longitude: -121.106000
Date/Time Start: 1996-05-26T09:30:00 * Date/Time End: 1996-06-06T18:45:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 45.560 m
Event(s):
167-1017B * Latitude: 34.534900 * Longitude: -121.106000 * Date/Time Start: 1996-05-26T09:30:00 * Date/Time End: 1996-05-27T00:00:00 * Elevation: -955.1 m * Penetration: 204.2 m * Recovery: 188.74 m * Location: North Pacific Ocean * Campaign: Leg167 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 204.2 m cored; 0 m drilled; 92.4 % recovery
167-1018A * Latitude: 36.988300 * Longitude: -123.277000 * Date/Time Start: 1996-05-29T01:15:00 * Date/Time End: 1996-06-01T07:30:00 * Elevation: -2477.0 m * Penetration: 426.2 m * Recovery: 426.85 m * Location: North Pacific Ocean * Campaign: Leg167 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 45 cores; 426.2 m cored; 0 m drilled; 100.2 % recovery
167-1019C * Latitude: 41.682900 * Longitude: -124.932000 * Date/Time Start: 1996-06-05T05:00:00 * Date/Time End: 1996-06-06T18:45:00 * Elevation: -946.9 m * Penetration: 247.8 m * Recovery: 213.97 m * Location: North Pacific Ocean * Campaign: Leg167 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 247.8 m cored; 0 m drilled; 86.3 % recovery
Comment:
Sediment depth is composite depth (mcd)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | AGE | Age | ka BP | Geocode | ||
4 | Sedimentation rate | SR | cm/ka | Mangelsdorf, Kai | ||
5 | Reference/source | Reference | Mangelsdorf, Kai | Age model of |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
123 data points
Data
1 Event | 2 Depth sed [m] | 3 Age [ka BP] | 4 SR [cm/ka] | 5 Reference |
---|---|---|---|---|
167-1017B | 2.055 | 9.41 | 21.67 | Kennett et al. 2000 |
167-1017B | 2.745 | 12.19 | 24.80 | Kennett et al. 2000 |
167-1017B | 2.885 | 14.36 | 6.45 | Kennett et al. 2000 |
167-1017B | 3.375 | 16.87 | 19.55 | Kennett et al. 2000 |
167-1017B | 3.955 | 18.97 | 27.64 | Kennett et al. 2000 |
167-1017B | 4.695 | 21.43 | 30.03 | Kennett et al. 2000 |
167-1017B | 6.075 | 28.55 | 19.40 | Kennett et al. 2000 |
167-1017B | 7.445 | 32.96 | 31.04 | Kennett et al. 2000 |
167-1017B | 12.245 | 58.96 | 18.46 | Kennett et al. 2000 |
167-1017B | 13.549 | 73.91 | 8.72 | Kennett et al. 2000 |
167-1017B | 14.765 | 79.25 | 22.77 | Kennett et al. 2000 |
167-1017B | 16.495 | 90.95 | 14.78 | Kennett et al. 2000 |
167-1017B | 20.775 | 110.79 | 21.57 | Kennett et al. 2000 |
167-1017B | 22.945 | 123.82 | 16.65 | Kennett et al. 2000 |
167-1017B | 24.115 | 129.84 | 19.43 | Kennett et al. 2000 |
167-1017B | 28.313 | 160.00 | 13.92 | SST comparison |
167-1018A | 0.000 | 8.00 | Lyle et al., 2000 | |
167-1018A | 1.610 | 13.59 | 28.80 | Lyle et al., 2000 |
167-1018A | 4.240 | 20.16 | 40.03 | Lyle et al., 2000 |
167-1018A | 6.090 | 25.53 | 34.45 | Lyle et al., 2000 |
167-1018A | 8.440 | 32.92 | 31.80 | Lyle et al., 2000 |
167-1018A | 9.440 | 36.57 | 27.39 | Lyle et al., 2000 |
167-1018A | 10.040 | 39.15 | 23.26 | Lyle et al., 2000 |
167-1018A | 11.330 | 44.21 | 25.49 | Lyle et al., 2000 |
167-1018A | 11.730 | 45.91 | 23.53 | Lyle et al., 2000 |
167-1018A | 13.130 | 52.97 | 19.83 | Lyle et al., 2000 |
167-1018A | 16.570 | 67.22 | 24.14 | Lyle et al., 2000 |
167-1018A | 19.000 | 75.36 | 29.85 | Lyle et al., 2000 |
167-1018A | 20.000 | 79.53 | 23.98 | Lyle et al., 2000 |
167-1018A | 20.290 | 81.18 | 17.58 | Lyle et al., 2000 |
167-1018A | 20.890 | 85.94 | 12.61 | Lyle et al., 2000 |
167-1018A | 21.890 | 94.72 | 11.39 | Lyle et al., 2000 |
167-1018A | 22.290 | 97.80 | 12.99 | Lyle et al., 2000 |
167-1018A | 22.890 | 101.77 | 15.11 | Lyle et al., 2000 |
167-1018A | 24.090 | 108.65 | 17.44 | Lyle et al., 2000 |
167-1018A | 24.490 | 111.18 | 15.81 | Lyle et al., 2000 |
167-1018A | 25.890 | 121.74 | 13.26 | Lyle et al., 2000 |
167-1018A | 28.180 | 136.97 | 15.04 | Lyle et al., 2000 |
167-1018A | 28.780 | 140.36 | 17.70 | Lyle et al., 2000 |
167-1018A | 29.410 | 143.45 | 20.39 | Lyle et al., 2000 |
167-1018A | 30.610 | 148.48 | 23.86 | Lyle et al., 2000 |
167-1018A | 31.770 | 152.39 | 29.67 | Lyle et al., 2000 |
167-1018A | 34.370 | 160.18 | 33.38 | Lyle et al., 2000 |
167-1019C | 4.180 | 9.80 | 42.65 | Mix et al., 2000 |
167-1019C | 7.180 | 14.70 | 61.24 | Mix et al., 2000 |
167-1019C | 8.210 | 17.00 | 44.78 | Mix et al., 2000 |
167-1019C | 11.710 | 22.67 | 61.67 | Mix et al., 2000 |
167-1019C | 14.610 | 30.02 | 39.48 | Mix et al., 2000 |
167-1019C | 15.810 | 34.56 | 26.43 | Mix et al., 2000 |
167-1019C | 18.000 | 47.79 | 16.55 | Mix et al., 2000 |
167-1019C | 18.950 | 55.53 | 12.27 | Mix et al., 2000 |
167-1019C | 20.270 | 62.34 | 19.38 | Mix et al., 2000 |
167-1019C | 21.810 | 71.27 | 17.25 | Mix et al., 2000 |
167-1019C | 23.610 | 77.77 | 27.69 | Mix et al., 2000 |
167-1019C | 24.620 | 83.08 | 19.02 | Mix et al., 2000 |
167-1019C | 27.890 | 107.25 | 13.53 | Mix et al., 2000 |
167-1019C | 28.400 | 109.87 | 19.47 | Mix et al., 2000 |
167-1019C | 29.140 | 112.81 | 25.17 | Mix et al., 2000 |
167-1019C | 31.400 | 119.86 | 32.05 | Mix et al., 2000 |
167-1019C | 39.660 | 139.65 | 41.74 | Mix et al., 2000 |
167-1019C | 40.310 | 143.04 | 19.17 | Mix et al., 2000 |
167-1019C | 45.560 | 160.06 | 30.85 | Mix et al., 2000 |