Oxburgh, Rachel; Pierson-Wickmann, Anne-Catherine; Reisberg, Laurie; Hemming, Sidney R (2007): Osmium concentration and isotope composition of ODP Hole 165-1002C (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.725507, Supplement to: Oxburgh, R et al. (2007): Climate-correlated variations in seawater 187Os/188Os over the past 200,000 yr: Evidence from the Cariaco Basin, Venezuela. Earth and Planetary Science Letters, 263(3-4), 246-258, https://doi.org/10.1016/j.epsl.2007.08.033
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Abstract:
A high resolution record of seawater osmium isotopic composition (35 samples over the past 191,000 yr) has been obtained from sediments from Ocean Drilling Program (ODP) Leg 165 Site 1002 in the Cariaco Basin, Venezuela. Strong correlations are observed between 187Os/188Os and both the local and global oxygen isotopic records, with less radiogenic values observed during glacial intervals. In conjunction with previous analyses of sediments from the East Pacific Rise, the Santa Barbara Basin, and the Japan Sea, the data demonstrate conclusively that there have been ocean-wide changes in seawater 187Os/188Os over the Pleistocene. Global seawater excursions to relatively unradiogenic 187Os/188Os, indicating decreased continental inputs, occur during cold intervals, times of increased aridity and increased ice cover of old (radiogenic) continental masses. The data thus indicate a direct climatic control on chemical weathering rates and/or composition of weathering products on a glacial-interglacial timescale.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 10.706100 * Longitude: -65.169400
Date/Time Start: 1996-02-18T16:30:00 * Date/Time End: 1996-02-19T04:30:00
Minimum DEPTH, sediment/rock: 0.3 m * Maximum DEPTH, sediment/rock: 64.9 m
Event(s):
165-1002C * Latitude: 10.706100 * Longitude: -65.169400 * Date/Time Start: 1996-02-18T16:30:00 * Date/Time End: 1996-02-19T04:30:00 * Elevation: -892.6 m * Penetration: 170.1 m * Recovery: 186 m * Location: Cayman Rise, Caribbean Sea * Campaign: Leg165 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 19 cores; 170.1 m cored; 0 m drilled; 109.3 % recovery
Comment:
Ages before 65 ka based on correlation of G. ruber delta18O record with SPECMAP stack (Peterson et al., 2000 doi:10.2973/odp.proc.sr.165.017.2000), followed by age conversion to the Lisiecki and Raymo (2005 doi:10.1029/2004PA001071) age model. Ages after 65 ka based on linear regression of high resolution ODP Site 1002 14C age record calibrated to the GISP2 Greenland ice core ((Hughen et al., 2004a doi:10.1126/science.1092995) and (Hughen et al., 2004b doi:10.1126/science.1090300))
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Oxburgh, Rachel | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | AGE | Age | ka BP | Geocode | ||
| 4 | Osmium-187/Osmium-188 ratio | 187Os/188Os | Oxburgh, Rachel | Negative-thermal ionization mass spectrometry (N-TIMS) | in-run precision for all data is better than 4 per mil (external standard reproducibility) and often better than 2 per mil | |
| 5 | Osmium | Os | ng/kg | Oxburgh, Rachel | ||
| 6 | Accumulation rate, Osmium | Acc rate Os | pg/cm2/ka | Oxburgh, Rachel | Calculated | multiplying the linear sedimentation rate (obtained from the ages and depths of the overlying and underlying samples) by the Os concentration and by a dry bulk density of 0.85 g/ccm (representative value suggested by Yarcinik et al., 2000, doi:10.1029/1999PA900048) |
| 7 | Comment | Comment | Oxburgh, Rachel |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
162 data points
Data
| 1 Sample label | 2 Depth sed [m] | 3 Age [ka BP] | 4 187Os/188Os | 5 Os [ng/kg] | 6 Acc rate Os [pg/cm2/ka] | 7 Comment |
|---|---|---|---|---|---|---|
| 165-1002C-1H-1,32-34 | 0.3 | 0.7 | 1.0458 | 252 | ||
| 165-1002C-1H-2,82-84 | 2.3 | 5.0 | 1.0453 | 254 | 9900 | |
| 165-1002C-1H-3,132-134 | 4.3 | 9.3 | 1.0448 | 165 | 6500 | |
| 165-1002C-1H-5,32-34 | 6.3 | 13.7 | 1.0200 | 247 | 9700 | |
| 165-1002C-1H-6,61-63 | 8.1 | 17.6 | 0.9773 | 139 | 5400 | |
| 165-1002C-2H-2,42-44 | 10.3 | 22.4 | 0.9823 | 126 | 4900 | |
| 165-1002C-2H-3,93-95 | 12.3 | 26.7 | 0.9806 | 133 | 5200 | |
| 165-1002C-2H-4,142-144 | 14.3 | 31.1 | 0.9881 | 124 | 4900 | |
| 165-1002C-2H-6,42-44 | 16.3 | 35.4 | 0.9906 | 127 | 5000 | |
| 165-1002C-3H-1,42-44 | 18.3 | 39.7 | 1.0127 | 149 | 5800 | |
| 165-1002C-3H-2,92-94 | 20.3 | 44.1 | 0.9832 | 108 | 4200 | |
| 165-1002C-3H-2,92-94 | 20.3 | 44.1 | 0.9772 | 111 | duplicate | |
| 165-1002C-3H-3,142-144 | 22.3 | 48.4 | 0.9425 | 99 | 3900 | |
| 165-1002C-3H-5,42-44 | 24.3 | 52.8 | 0.9546 | 119 | 4700 | |
| 165-1002C-3H-5,42-44 | 24.3 | 52.8 | 0.9448 | 114 | duplicate | |
| 165-1002C-3H-5,42-44 | 24.3 | 52.8 | 0.9487 | Leachate L1 solution: 0.2 N HNO3 and 5% H2O2 for 15 min | ||
| 165-1002C-3H-6,91-93 | 26.3 | 57.1 | 0.9519 | 117 | 4600 | |
| 165-1002C-4H-1,92-94 | 28.3 | 61.5 | 0.9147 | 93 | 3600 | |
| 165-1002C-4H-1,92-94 | 28.3 | 61.5 | 0.9052 | 106 | duplicate | |
| 165-1002C-4H-1,92-94 | 28.3 | 61.5 | 0.9062 | solution: 0.5N HNO3 and 5% H2O2 for 15 min | ||
| 165-1002C-4H-1,92-94 | 28.3 | 61.5 | 0.9181 | Leachate L3 solution: 1.2N H2SO4 and 5% H2O2 for 24 h | ||
| 165-1002C-4H-2,141-143 | 30.3 | 65.8 | 0.9689 | 141 | 5500 | |
| 165-1002C-4H-2,141-143 | 30.3 | 65.8 | 0.9861 | 144 | duplicate | |
| 165-1002C-4H-4,41-43 | 32.4 | 70.3 | 1.0326 | 103 | 2700 | |
| 165-1002C-4H-6,140-142 | 36.5 | 86.2 | 1.0326 | 90 | 1800 | |
| 165-1002C-5H-1,140-142 | 38.3 | 96.4 | 1.0457 | 141 | 2500 | |
| 165-1002C-5H-3,41-43 | 40.3 | 105.5 | 1.0472 | 142 | 2800 | |
| 165-1002C-5H-4,91-93 | 42.3 | 114.6 | 1.0546 | 178 | 3500 | |
| 165-1002C-5H-5,140-142 | 44.3 | 123.6 | 1.0608 | 190 | 3800 | |
| 165-1002C-5H-7,41-43 | 46.3 | 132.8 | 1.0471 | 94 | 1500 | |
| 165-1002C-6H-2,41-43 | 47.1 | 136.2 | 0.9654 | 139 | 2200 | |
| 165-1002C-6H-3,92-94 | 50.3 | 151.4 | 0.9842 | 165 | 3300 | |
| 165-1002C-6H-4,140-142 | 51.1 | 153.0 | 0.9823 | 106 | 3000 | |
| 165-1002C-6H-6,40-42 | 53.1 | 159.9 | 0.9891 | 167 | 3800 | |
| 165-1002C-7H-1,42-44 | 56.3 | 172.6 | 1.0045 | 95 | 2300 | |
| 165-1002C-7H-2,82-84 | 57.6 | 175.9 | 1.0472 | 90 | 2900 | |
| 165-1002C-7H-3,142-144 | 59.7 | 181.5 | 1.0184 | 122 | 4100 | |
| 165-1002C-7H-4,92-94 | 60.7 | 183.7 | 0.9650 | 118 | 4500 | |
| 165-1002C-7H-5,42-44 | 61.8 | 186.1 | 0.9688 | 89 | 4300 | |
| 165-1002C-7H-5,142-144 | 62.8 | 187.4 | 1.0186 | 120 | 9200 | |
| 165-1002C-7H-6,91-93 | 63.8 | 188.3 | 1.0208 | 142 | 7100 | |
| 165-1002C-7H-7,42-44 | 64.9 | 191.0 | 1.0313 |