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Gillis, Kathryn M; Coogan, Laurence A (2011): (Table A2) Geochemistry and calculated temperatures for carbonates of ocean crust [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.786467, In supplement to: Gillis, KM; Coogan, LA (2011): Secular variation in carbon uptake into the ocean crust. Earth and Planetary Science Letters, 302(3-4), 385-392, https://doi.org/10.1016/j.epsl.2010.12.030

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Project(s):
Coverage:
Median Latitude: 11.358278 * Median Longitude: -78.971733 * South-bound Latitude: -23.822300 * West-bound Longitude: -165.526800 * North-bound Latitude: 38.939700 * East-bound Longitude: -34.685300
Date/Time Start: 1976-02-06T00:00:00 * Date/Time End: 1983-03-02T00:00:00
Minimum DEPTH, sediment/rock: 58.3 m * Maximum DEPTH, sediment/rock: 621.4 m
Event(s):
46-396B * Latitude: 22.985667 * Longitude: -43.515000 * Date/Time: 1976-02-06T00:00:00 * Elevation: -4459.0 m * Penetration: 405.5 m * Recovery: 63.56 m * Campaign: Leg46 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL)
78-543A * Latitude: 15.712300 * Longitude: -58.653700 * Date/Time: 1981-02-28T00:00:00 * Elevation: -5633.0 m * Penetration: 455 m * Recovery: 64.2 m * Location: North Atlantic/CONT RISE * Campaign: Leg78 (Leg78AB) * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 132.5 m cored; 0 m drilled; 48.5 % recovery
82-556 * Latitude: 38.939700 * Longitude: -34.685300 * Date/Time: 1981-09-22T00:00:00 * Elevation: -3672.0 m * Penetration: 639 m * Recovery: 80.9 m * Location: North Atlantic/RIDGE * Campaign: Leg82 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 166 m cored; 0 m drilled; 48.7 % recovery
Comment:
Sediment depth is given in mbsf. Age represents the crustal age. Carbonate powders were analysed for C and O isotopes in a Finnigan Delta XL Plus mass spectrometer, using a gas bench with A200s autosampler at the Pacific Centre for Isotopic and Geochemical Research, University of British Columbia. Helium was used to displace air in the headspace and CO2 gas was liberated using 100% phosphoric acid. The results are reported using the d notation measured in per mil relative to the VSMOW standard. After correction for fractionation, repeated analyses of NBS 18 gave an average d13C value of -5.01 ± 0.07? and d18O value of 7.23 ± 0.08 per mil, NBS 19 gave an average d13C value of 1.93 ± 0.08 per mil and d18O value of 28.74 ± 0.18 per mil. Precision was ± 0.1 per mil on 13C and ± 0.2 per mil on 18O. Strontium isotopes were measured Strontium was separated by standard cation exchange techniques (Weis et al., 2006) and measured using a Triton thermal ionization mass spectrometry at the Pacific Centre for Isotopic and Geochemical Research, University of British Columbia. The NBS 987 standard gave 87Sr/86Sr = 0.710241 ± 0.000025 (2 s.d., n= 12); the average reproducibility was ± 0.000012 (n=3).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Latitude of eventLatitude
3Longitude of eventLongitude
4Elevation of eventElevationm
5AGEAgeka BPGeocode
6Layer thicknessThicknessmGillis, Kathryn Msediment
7Sample code/labelSample labelGillis, Kathryn MDSDP/ODP/IODP sample designationD = duplicate
8DEPTH, sediment/rockDepth sedmGeocode
9Depth, relativeDepth relmGillis, Kathryn Mbelow sediment
10TypeTypeGillis, Kathryn Mcarbonate
11δ13Cδ13C‰ PDBGillis, Kathryn MMass spectrometer Finnigan Delta Plus XL
12δ18Oδ18OGillis, Kathryn MMass spectrometer Finnigan Delta Plus XLwith respect to SMOW
13Temperature, calculatedT cal°CGillis, Kathryn M
14Strontium-87/Strontium-86 ratio87Sr/86SrGillis, Kathryn MFinnigan TRITON thermal ionization mass spectrometer (TIMS)
15Strontium-87/Strontium-86 ratio, error87Sr/86Sr e±Gillis, Kathryn MFinnigan TRITON thermal ionization mass spectrometer (TIMS)2 sigma
Size:
571 data points

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