Swart, Peter K; Isern, Alexandra R; Elderfield, Henry; McKenzie, Judith A (1993): (Table 1) Stable carbon and oxygen isotope ratios of interstitial-water samples of ODP Leg 133 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.786893, Supplement to: Swart, PK et al. (1993): A summary of interstitial-water geochemistry of Leg 133. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 705-721, https://doi.org/10.2973/odp.proc.sr.133.258.1993
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Published: 1993 (exact date unknown) • DOI registered: 2012-08-30
Abstract:
The chemical compositions of the interstitial pore-water samples measured on board the JOIDES Resolution are compared with shore-based analyses of the samplesÆ strontium, oxygen, and carbon isotopic compositions. These analyses support conclusions of large-scale water movement through the sediment overlying the Queensland Plateau at Sites 811, 812, 813, and 814, possibly leading to massive platform dolomitization.
At the Queensland continental margin sites, complete sulfate reduction and abundant methanogenesis occurs, yet little evidence of these processes is seen in the d13C of the pore waters. The failure to observe these signatures is a consequence of large-scale recrystallization of carbonate sediments masking the isotopic signatures of these processes. Although abundant igneous material is present at these sites, we do not think that significant alteration of these minerals is taking place in situ. Decreases in the Mg2+ and Ca2+ concentration result from the formation of dolomite and calcite; decreases in K+ are a consequence of absorption onto clays; and decreases in the d18O are caused by carbonate recrystallization, with perhaps some minor influence from the alteration of volcanic glass.
At several sites there is evidence of diffusion of saline fluids from an underlying source, presumably evaporitic in nature, but this cannot be confirmed using either Sr or O isotopic data.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -17.225000 * Median Longitude: 148.173049 * South-bound Latitude: -19.199000 * West-bound Longitude: 146.215000 * North-bound Latitude: -16.423000 * East-bound Longitude: 150.042200
Date/Time Start: 1990-08-17T01:00:00 * Date/Time End: 1990-10-07T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 990.50 m
Event(s):
133-811A * Latitude: -16.515000 * Longitude: 148.158000 * Date/Time Start: 1990-08-17T01:00:00 * Date/Time End: 1990-08-17T22:04:00 * Elevation: -948.0 m * Penetration: 214.5 m * Recovery: 213.4 m * Location: Coral Sea * Campaign: Leg133 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 214.5 m cored; 0 m drilled; 99.5 % recovery
133-811B * Latitude: -16.515000 * Longitude: 148.158000 * Date/Time Start: 1990-08-17T22:04:00 * Date/Time End: 1990-08-19T22:15:00 * Elevation: -948.0 m * Penetration: 392.5 m * Recovery: 15.55 m * Location: Coral Sea * Campaign: Leg133 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 199.3 m cored; 0 m drilled; 7.8 % recovery
133-812 * Latitude: -17.814000 * Longitude: 149.605000 * Date/Time Start: 1990-08-20T00:00:00 * Date/Time End: 1990-08-27T00:00:00 * Elevation: -473.0 m * Penetration: 627.7 m * Recovery: 163.4 m * Location: Coral Sea * Campaign: Leg133 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 54 cores; 476.9 m cored; 0 m drilled; 34.3% recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Swart, Peter K | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 4 | δ13C, dissolved inorganic carbon | δ13C DIC | ‰ PDB | Swart, Peter K | Mass spectrometer Finnigan MAT 251 | |
| 5 | δ18O, water | δ18O H2O | ‰ SMOW | Swart, Peter K | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
617 data points
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Datasets with similar metadata
- Swart, PK (1993): (Table 1) Pore-water chemistry, mineralogy and stable isotope ratios for ODP Leg 133 holes. https://doi.org/10.1594/PANGAEA.786577
- McKenzie, JA; Isern, AR; Elderfield, H et al. (1993): (Table 1) Stontium isotope ratios for ODP Leg 133 sediments. https://doi.org/10.1594/PANGAEA.786573
- McKenzie, JA; Isern, AR; Elderfield, H et al. (1993): (Table 2) Stable isotope ratios for ODP Leg 133 sediments. https://doi.org/10.1594/PANGAEA.786574