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Alcalá-Herrera, Javier A; Grossman, Ethan L; Gartner, Stefan (1992): (Appendix) Stable carbon and oxygen isotope ratios of fine-fraction sediments across the Cretaceous/Tertiary boundary of DSDP Hole 74-528 from Walvis Ridge, South Atlantic [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.683529, In supplement to: Alcalá-Herrera, JA et al. (1992): Nannofossil diversity and equitability and fine-fraction d13C across the Cretaceous/Tertiary boundary at Walvis Ridge Leg 74, South Atlantic. Marine Micropaleontology, 20(1), 77-88, https://doi.org/10.1016/0377-8398(92)90010-H

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Project(s):
Coverage:
Latitude: -28.524800 * Longitude: 2.324000
Date/Time Start: 1980-07-04T00:00:00 * Date/Time End: 1980-07-04T00:00:00
Minimum DEPTH, sediment/rock: 363.44 m * Maximum DEPTH, sediment/rock: 466.10 m
Event(s):
74-528 * Latitude: -28.524800 * Longitude: 2.324000 * Date/Time: 1980-07-04T00:00:00 * Elevation: -3800.0 m * Penetration: 555 m * Recovery: 271.9 m * Location: South Atlantic/RIDGE * Campaign: Leg74 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 47 cores; 441 m cored; 0 m drilled; 61.7 % recovery
Comment:
Ages were obtained using the magnetostratigraphy data reported by Chave (1984) and age interpretation made by Shackleton and Hall (1984). The K/T boundary is assumed to have an absolute age of 64.5 Ma. based on recent precise determinations of the age of the K/T boundary (Izett et al., 1991).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
δ13C, carbonateδ13C carb‰ PDBAlcalá-Herrera, Javier A2-63 µm size fraction, mainly formed by calcareous nannoplankton
δ18O, carbonateδ18O carb‰ PDBAlcalá-Herrera, Javier A2-63 µm size fraction, mainly formed by calcareous nannoplankton
Size:
68 data points

Data

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


Depth sed [m]

Age [ka BP]

δ13C carb [‰ PDB]

δ18O carb [‰ PDB]
363.4459547.02.93-1.20
370.6959767.03.27-1.01
381.7060213.02.59-0.92
391.0861027.01.95-0.35
398.6663353.81.70-0.89
399.0063432.02.030.10
399.7863572.01.93-0.11
400.2863623.50.96-0.89
400.5063646.01.570.07
401.7063769.91.971.12
402.4863850.31.74-1.22
402.5363855.42.23-0.63
403.2063924.51.68-1.05
403.7663982.01.71-0.08
404.0064006.91.64-0.15
404.5464062.61.24-0.88
404.7864087.30.88-3.04
405.8264165.01.290.13
406.5064359.01.44-0.35
406.6664404.01.59-0.70
406.8664461.01.63-0.12
407.0064500.02.030.10
407.2064508.82.940.02
407.9764543.02.89-0.44
408.9464586.02.30-0.16
411.9364717.72.78-0.65
417.5164996.62.79-1.02
418.5865052.22.74-1.15
423.1565289.03.010.52
428.3365558.03.30-0.44
436.0065237.03.30-0.13
446.3566494.02.58-0.91
451.7866776.02.73-0.36
466.1067519.02.57-0.37