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DePaolo, Donald J (1986): (Table 1) Strontium content and isotope ratio of pore waters from DSDP Hole 590B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711799, In: DePaolo, DJ (2009): Strontium isotopic data for calcareous ooze, chalk, and pore waters from DSDP Hole 590B [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.711800

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Related to:
DePaolo, Donald J (1986): Detailed record of the Neogene Sr isotopic evolution of seawater from DSDP Site 590B. Geology, 14(2), 103-106, https://doi.org/10.1130/0091-7613(1986)14%3C103:DROTNS%3E2.0.CO;2
Project(s):
Coverage:
Latitude: -31.167000 * Longitude: 163.358500
Date/Time Start: 1982-12-15T00:00:00 * Date/Time End: 1982-12-15T00:00:00
Minimum DEPTH, sediment/rock: 134 m * Maximum DEPTH, sediment/rock: 487 m
Event(s):
90-590B * Latitude: -31.167000 * Longitude: 163.358500 * Date/Time: 1982-12-15T00:00:00 * Elevation: -1299.0 m * Penetration: 499.1 m * Recovery: 464.6 m * Location: South Pacific/Tasman Sea/CONT RISE * Campaign: Leg90 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 53 cores; 499.1 m cored; 0 m drilled; 93.1 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Sample code/labelSample labelDePaolo, Donald JDSDP/ODP/IODP sample designation
StrontiumSr%DePaolo, Donald JIsotope ratio mass spectrometrySr content of distilled water rinse of wet sediment as a fraction of the Sr contained in the solid fraction
Strontium-87/Strontium-86 ratio87Sr/86SrDePaolo, Donald JIsotope ratio mass spectrometry
Strontium-87/Strontium-86 ratio, error87Sr/86Sr e±DePaolo, Donald JCalculated
Sample commentSample commentDePaolo, Donald J
Size:
26 data points

Data

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


Depth sed [m]

Sample label

Sr [%]

87Sr/86Sr

87Sr/86Sr e [±]

Sample comment
13490-590B-15-58.10.7090650.000028some fine-grained solids were probably present
16690-590B-19-117.60.7090630.000028some fine-grained solids were probably present
27290-590B-30-34.20.7089740.000029
39990-590B-43-43.00.7087700.000027
46390-590B-50-22.30.7086160.000026
48790-590B-52-52.40.7085060.000014