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Richter, Frank M; DePaolo, Donald J (1988): (Table 3) Depth, age, insoluble residue fraction and Sr isotopic data for sediments from DSDP Hole 90-590B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.700901, In supplement to: Richter, FM; DePaolo, DJ (1988): Diagenesis and Sr isotopic evolution of seawater using data from DSDP 590B and 575. Earth and Planetary Science Letters, 90(4), 382-394, https://doi.org/10.1016/0012-821X(88)90137-9

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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: m * Maximum DEPTH, sediment/rock: 498 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
Comment:
Age data are based on calcareous nannofossil biostratigraphy and time scales of Berggren et al. (1985, doi:10.1130/0016-7606(1985)96<1407:CG>2.0.CO;2) and Barron et al. (1985)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
Sample code/labelSample labelRichter, Frank MDSDP/ODP/IODP sample designation
Insoluble residueInsol res%Richter, Frank M% of weight of sample insoluble in 5 molal (mol/kg) acetic acid
Strontium-87/Strontium-86 ratio87Sr/86SrRichter, Frank Mnormalized to 84Sr/88Sr = 0.1194 with +/- 2 sigma. NBS 987 is measured as 0.710330 +/- 0.000005
Strontium-87/Strontium-86 ratio, error87Sr/86Sr e±Richter, Frank M2 sigma
Size:
127 data points

Data

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Depth sed [m]

Age [ka BP]

Sample label

Insol res [%]

87Sr/86Sr

87Sr/86Sr e [±]
110090-590B-1-15.30.7092560.000011
30180090-590B-4-65.60.7091610.000007
39210090-590B-5-67.10.7091490.000013
44230090-590B-6-32.70.7091220.000006
68310090-590B-8-64.30.7091260.000005
107360090-590B-12-61.90.7091210.000016
134380090-590B-15-518.90.7091020.000030
153430090-590B-17-52.40.7091160.000010
166460090-590B-19-12.40.7090960.000005
185560090-590B-21-11.70.7090800.000005
224600090-590B-25-13.10.7090310.000005
272640090-590B-30-32.30.7090240.000005
300690090-590B-33-20.7090160.000005
323740090-590B-35-53.40.7089920.000005
332790090-590B-36-45.80.7089780.000014
341840090-590B-37-44.60.7089750.000005
354890090-590B-38-64.90.7089800.000017
373990090-590B-40-62.60.7089580.000005
3831070090-590B-41-64.60.7089600.000011
3931120090-590B-42-65.60.7089260.000015
3991140090-590B-43-43.00.7088950.000022
4101180090-590B-44-56.00.7088920.000009
4211250090-590B-45-55.30.7088890.000016
4301330090-590B-46-65.60.7088890.000014
4361390090-590B-47-46.10.7088700.000005
4481500090-590B-48-57.30.7088580.000009
4591560090-590B-49-45.70.7088480.000008
4631600090-590B-50-24.00.7087920.000019
4771880090-590B-51-54.50.7086060.000005
4872000090-590B-52-56.10.7085580.000011
4912080090-590B-53-16.10.7085440.000005
4982220090-590B-53-76.40.7085220.000013