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Ford, Heather L; Ravelo, Ana Christina; Hovan, Steven A (2012): Stable isotopes and Mg/Ca ratios of Globorotalia tumida of ODP Site 138-849 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.834322, In supplement to: Ford, HL et al. (2012): A deep Eastern Equatorial Pacific thermocline during the early Pliocene warm period. Earth and Planetary Science Letters, 355-356, 152-161, https://doi.org/10.1016/j.epsl.2012.08.027

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Project(s):
Coverage:
Latitude: 0.183330 * Longitude: -110.518330
Date/Time Start: 1991-06-12T00:00:00 * Date/Time End: 1991-09-07T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 156.79 m
Event(s):
138-849 * Latitude: 0.183330 * Longitude: -110.518330 * Date/Time Start: 1991-09-07T00:00:00 * Date/Time End: 1991-06-12T00:00:00 * Elevation: -3839.0 m * Penetration: 791.4 m * Recovery: 777.62 m * Location: North Pacific Ocean * Campaign: Leg138 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 83 cores; 786.4 m cored; 0 m drilled; 98.9 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2AGEAgeka BPGeocode
3Globorotalia tumida, δ13CG. tumida δ13C‰ PDBFord, Heather LIsotope ratio mass spectrometrywith respect to VPDB, size fraction 355-425 µm
4Globorotalia tumida, δ18OG. tumida δ18O‰ PDBFord, Heather LIsotope ratio mass spectrometrywith respect to VPDB, size fraction 355-425 µm
5Globorotalia tumida, Magnesium/Calcium ratioG. tumida Mg/Cammol/molFord, Heather LICP-OES, Inductively coupled plasma - optical emission spectrometry
6Sub-surface temperatureSubT°CFord, Heather LCalculated from Mg/Ca ratios (Anand et al., 2003)and depth correction factor G. sacculifer from Dekens et al. (2002) for the Pacific: Mg/Ca = 0.38exp0.09[T-0.36(core depth in km)-2.0C]
7Sample code/labelSample labelFord, Heather LDSDP/ODP/IODP sample designation
Size:
1075 data points

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