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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

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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):
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):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
Sedimentation rateSRcm/kaMangelsdorf, Kai
Reference/sourceReferenceMangelsdorf, KaiAge model of
Size:
123 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Depth sed [m]

Age [ka BP]

SR [cm/ka]

Reference
167-1017B 2.0559.4121.67Kennett et al. 2000
167-1017B2.74512.1924.80Kennett et al. 2000
167-1017B2.88514.366.45Kennett et al. 2000
167-1017B3.37516.8719.55Kennett et al. 2000
167-1017B3.95518.9727.64Kennett et al. 2000
167-1017B4.69521.4330.03Kennett et al. 2000
167-1017B6.07528.5519.40Kennett et al. 2000
167-1017B7.44532.9631.04Kennett et al. 2000
167-1017B12.24558.9618.46Kennett et al. 2000
167-1017B13.54973.918.72Kennett et al. 2000
167-1017B14.76579.2522.77Kennett et al. 2000
167-1017B16.49590.9514.78Kennett et al. 2000
167-1017B20.775110.7921.57Kennett et al. 2000
167-1017B22.945123.8216.65Kennett et al. 2000
167-1017B24.115129.8419.43Kennett et al. 2000
167-1017B28.313160.0013.92SST comparison
167-1018A 0.0008.00Lyle et al., 2000
167-1018A1.61013.5928.80Lyle et al., 2000
167-1018A4.24020.1640.03Lyle et al., 2000
167-1018A6.09025.5334.45Lyle et al., 2000
167-1018A8.44032.9231.80Lyle et al., 2000
167-1018A9.44036.5727.39Lyle et al., 2000
167-1018A10.04039.1523.26Lyle et al., 2000
167-1018A11.33044.2125.49Lyle et al., 2000
167-1018A11.73045.9123.53Lyle et al., 2000
167-1018A13.13052.9719.83Lyle et al., 2000
167-1018A16.57067.2224.14Lyle et al., 2000
167-1018A19.00075.3629.85Lyle et al., 2000
167-1018A20.00079.5323.98Lyle et al., 2000
167-1018A20.29081.1817.58Lyle et al., 2000
167-1018A20.89085.9412.61Lyle et al., 2000
167-1018A21.89094.7211.39Lyle et al., 2000
167-1018A22.29097.8012.99Lyle et al., 2000
167-1018A22.890101.7715.11Lyle et al., 2000
167-1018A24.090108.6517.44Lyle et al., 2000
167-1018A24.490111.1815.81Lyle et al., 2000
167-1018A25.890121.7413.26Lyle et al., 2000
167-1018A28.180136.9715.04Lyle et al., 2000
167-1018A28.780140.3617.70Lyle et al., 2000
167-1018A29.410143.4520.39Lyle et al., 2000
167-1018A30.610148.4823.86Lyle et al., 2000
167-1018A31.770152.3929.67Lyle et al., 2000
167-1018A34.370160.1833.38Lyle et al., 2000
167-1019C 4.1809.8042.65Mix et al., 2000
167-1019C7.18014.7061.24Mix et al., 2000
167-1019C8.21017.0044.78Mix et al., 2000
167-1019C11.71022.6761.67Mix et al., 2000
167-1019C14.61030.0239.48Mix et al., 2000
167-1019C15.81034.5626.43Mix et al., 2000
167-1019C18.00047.7916.55Mix et al., 2000
167-1019C18.95055.5312.27Mix et al., 2000
167-1019C20.27062.3419.38Mix et al., 2000
167-1019C21.81071.2717.25Mix et al., 2000
167-1019C23.61077.7727.69Mix et al., 2000
167-1019C24.62083.0819.02Mix et al., 2000
167-1019C27.890107.2513.53Mix et al., 2000
167-1019C28.400109.8719.47Mix et al., 2000
167-1019C29.140112.8125.17Mix et al., 2000
167-1019C31.400119.8632.05Mix et al., 2000
167-1019C39.660139.6541.74Mix et al., 2000
167-1019C40.310143.0419.17Mix et al., 2000
167-1019C45.560160.0630.85Mix et al., 2000