Matsuda, Hiroki; Machiyama, Hideaki; James, Noel P (2002): (Table T1) Calcium carbonate mineralogy and stable isotopic composition of ODP Hole 182-1132C sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.785997, Supplement to: Matsuda, H et al. (2002): Data report: Petrography and stable isotope geochemistry of lower Oligocene to middle Miocene carbonates, Site 1132, Great Australian Bight. In: Hine, AC; Feary, DA; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 182, 1-11, https://doi.org/10.2973/odp.proc.sr.182.002.2002
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Abstract:
Petrographic observation and carbonate mineralogic and stable isotopic investigation were conducted on lower Oligocene to middle Miocene sediments recovered during Ocean Drilling Program Leg 182 from Site 1132, located at a water depth of 218.5 m immediately seaward of the shelf-slope break of the eastern Eyre Terrace in the western Great Australian Bight. The middle Miocene section consists of bioclastic packstone and grainstone with an interval of partially silicified nannofossil-foraminiferal chalk and is slightly to densely dolomitized. By contrast, the lower Oligocene to lower Miocene section is characterized by a predominance of planktonic and benthic foraminifers, high porosity, absence of chert, and weak dolomitization. The carbon and oxygen isotopic composition of calcites and dolomites between two sections, however, shows no significant difference.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -33.316030 * Longitude: 127.602060
Date/Time Start: 1998-11-22T04:25:00 * Date/Time End: 1998-11-24T18:15:00
Minimum DEPTH, sediment/rock: 255.80 m * Maximum DEPTH, sediment/rock: 517.40 m
Event(s):
182-1132C * Latitude: -33.316030 * Longitude: 127.602060 * Date/Time Start: 1998-11-22T04:25:00 * Date/Time End: 1998-11-24T18:15:00 * Elevation: -218.5 m * Penetration: 603.2 m * Recovery: 22.42 m * Location: Great Australian Bight * Campaign: Leg182 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 39 cores; 366.2 m cored; 237 m drilled; 6.1 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Matsuda, Hiroki | DSDP/ODP/IODP sample designation | ||
| 2 | Lithologic unit/sequence | Unit | Matsuda, Hiroki | |||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 4 | Calcium carbonate | CaCO3 | % | Matsuda, Hiroki | X-ray diffraction (XRD) | |
| 5 | Low magnesium calcite | LMC | % | Matsuda, Hiroki | X-ray diffraction (XRD) | |
| 6 | Dolomite | Dol | % | Matsuda, Hiroki | X-ray diffraction (XRD) | |
| 7 | δ13C, calcite | δ13C cal | ‰ PDB | Matsuda, Hiroki | Mass spectrometer Finnigan Delta Plus | low-magnesium calcite |
| 8 | δ18O, calcite | δ18O cal | ‰ PDB | Matsuda, Hiroki | Mass spectrometer Finnigan Delta Plus | low-magnesium calcite |
| 9 | δ13C, dolomite | δ13C dol | ‰ PDB | Matsuda, Hiroki | Mass spectrometer Finnigan Delta Plus | |
| 10 | δ18O, dolomite | δ18O dol | ‰ PDB | Matsuda, Hiroki | Mass spectrometer Finnigan Delta Plus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
254 data points
Data
| 1 Sample label | 2 Unit | 3 Depth sed [m] | 4 CaCO3 [%] | 5 LMC [%] | 6 Dol [%] | 7 δ13C cal [‰ PDB] | 8 δ18O cal [‰ PDB] | 9 δ13C dol [‰ PDB] | 10 δ18O dol [‰ PDB] |
|---|---|---|---|---|---|---|---|---|---|
| 182-1132C-3R-CC,0-1 | IV | 255.80 | 81 | 19 | 0.69 | 0.81 | 1.23 | 0.96 | |
| 182-1132C-7R-CC,0-1 | IV | 293.10 | 92 | 8 | |||||
| 182-1132C-7R-CC,1-2 | IV | 293.11 | 90 | 10 | |||||
| 182-1132C-7R-CC,6-9 | IV | 293.16 | 96.5 | 96 | 4 | 1.37 | 1.42 | 1.58 | 0.91 |
| 182-1132C-13R-CC,3-6 | IV | 348.13 | 75 | 25 | |||||
| 182-1132C-13R-CC,6-8 | IV | 348.16 | 83 | 17 | |||||
| 182-1132C-13R-CC,10-13 | IV | 348.20 | 79 | 21 | 0.87 | 0.05 | 1.31 | -0.40 | |
| 182-1132C-18R-CC,3-5 | IV | 394.73 | 94.3 | 89 | 11 | ||||
| 182-1132C-18R-CC,5-6 | IV | 394.75 | 86 | 14 | |||||
| 182-1132C-18R-CC,6-9 | IV | 394.76 | 85 | 15 | 1.15 | 1.01 | 1.36 | -1.05 | |
| 182-1132C-20R-CC,6-8 | IV | 413.66 | 51 | 49 | 1.74 | 1.06 | |||
| 182-1132C-20R-CC,12-14 | IV | 413.72 | 79 | 21 | |||||
| 182-1132C-20R-CC,17-20 | IV | 413.77 | 90.0 | 83 | 17 | 1.11 | 0.07 | ||
| 182-1132C-21R-CC,8-9 | IV | 422.98 | 8 | 92 | |||||
| 182-1132C-21R-CC,9-11 | IV | 422.99 | 8 | 92 | |||||
| 182-1132C-21R-CC,12-14 | IV | 423.02 | 9 | 91 | 1.42 | 0.26 | 1.99 | 2.40 | |
| 182-1132C-21R-CC,18-22 | IV | 423.08 | 26 | 74 | |||||
| 182-1132C-22R-CC,0-3 | IV | 432.20 | 41 | 59 | |||||
| 182-1132C-22R-CC,3-6 | IV | 432.23 | 49 | 51 | 1.44 | 1.21 | 1.92 | 1.74 | |
| 182-1132C-23R-CC,1-5 | V | 441.51 | 99 | 1 | 1.58 | 0.79 | |||
| 182-1132C-23R-CC,5-8 | V | 441.55 | 100 | 0 | |||||
| 182-1132C-23R-CC,10-13 | V | 441.60 | 98 | 2 | |||||
| 182-1132C-23R-CC,13-16 | V | 441.63 | 98 | 2 | |||||
| 182-1132C-24R-CC,0-4 | V | 450.80 | 97.0 | 99 | 1 | 1.33 | 0.30 | ||
| 182-1132C-24R-CC,4-8 | V | 450.84 | 99 | 1 | |||||
| 182-1132C-24R-CC,8-11 | V | 450.88 | 100 | 0 | |||||
| 182-1132C-25R-CC,0-3 | V | 459.70 | 99 | 1 | 1.23 | 0.71 | |||
| 182-1132C-25R-CC,4-7 | V | 459.74 | 100 | 0 | |||||
| 182-1132C-26R-CC,0-4 | V | 468.60 | 97.5 | 100 | 0 | 1.40 | 1.07 | ||
| 182-1132C-26R-CC,5-8 | V | 468.65 | 98 | 2 | |||||
| 182-1132C-26R-CC,11-14 | V | 468.71 | 100 | 0 | |||||
| 182-1132C-26R-CC,14-18 | V | 468.74 | 99 | 1 | |||||
| 182-1132C-27R-CC,5-8 | V | 478.05 | 99 | 1 | 0.71 | 0.95 | |||
| 182-1132C-27R-CC,9-12 | V | 478.09 | 100 | 0 | |||||
| 182-1132C-27R-CC,14-17 | V | 478.14 | 100 | 0 | |||||
| 182-1132C-28R-CC,0-3 | V | 487.70 | 97.1 | 99 | 1 | 0.88 | 0.74 | ||
| 182-1132C-28R-CC,3-5 | V | 487.73 | 100 | 0 | |||||
| 182-1132C-28R-CC,11-13 | V | 487.81 | 99 | 1 | |||||
| 182-1132C-28R-CC,14-16 | V | 487.84 | 100 | 0 | |||||
| 182-1132C-29R-CC,1-2 | V | 497.41 | 100 | 0 | |||||
| 182-1132C-29R-CC,4-7 | V | 497.44 | 100 | 0 | |||||
| 182-1132C-29R-CC,16-18 | V | 497.56 | 95.3 | 100 | 0 | 1.25 | 0.60 | ||
| 182-1132C-29R-CC,19-22 | V | 497.59 | 100 | 0 | |||||
| 182-1132C-30R-CC,0-3 | V | 507.10 | 94.0 | 92 | 8 | 1.06 | 0.92 | 1.42 | 0.86 |
| 182-1132C-30R-CC,4-7 | V | 507.14 | 99 | 1 | |||||
| 182-1132C-30R-CC,13-17 | V | 507.23 | 92 | 8 | |||||
| 182-1132C-31R-1,8-11 | V | 516.78 | 96.6 | 98 | 2 | 1.13 | 0.75 | ||
| 182-1132C-31R-1,70-74 | V | 517.40 | 89.2 | 93 | 7 | 1.28 | 1.15 | 1.40 | 0.89 |