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Westerhold, Thomas; Bickert, Torsten; Röhl, Ursula (2005): (Appendix A7) Stable isotope data of ODP Hole175-1085A-42X to -63X (382.40-594.12 mbsf). PANGAEA, https://doi.org/10.1594/PANGAEA.230283, In supplement to: Westerhold, T et al. (2005): Middle to late Miocene oxygen isotope stratigraphy of ODP site 1085 (SE Atlantic): new constrains on Miocene climate variability and sea-level fluctuations. Palaeogeography, Palaeoclimatology, Palaeoecology, 217(3-4), 205-222, https://doi.org/10.1016/j.palaeo.2004.12.001

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Related to:
Westerhold, Thomas (2003): The Middle Miocene Carbonate Crash: Relationship to Neogene Changes inOcean Circulation and Global Climate. PhD Thesis, Elektronische Dissertationen an der Staats- und Universitätsbibliothek Bremen, Germany, urn:nbn:de:gbv:46-diss000007286
Coverage:
Latitude: -29.374410 * Longitude: 13.990110
Date/Time Start: 1997-09-26T00:15:00 * Date/Time End: 1997-09-29T18:15:00
Minimum DEPTH, sediment/rock: 382.42 m * Maximum DEPTH, sediment/rock: 594.12 m
Event(s):
175-1085A * Latitude: -29.374410 * Longitude: 13.990110 * Date/Time Start: 1997-09-26T00:15:00 * Date/Time End: 1997-09-29T18:15:00 * Elevation: -1713.2 m * Penetration: 604 m * Recovery: 594.39 m * Location: Benguela Current, South Atlantic Ocean * Campaign: Leg175 * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 64 cores; 604 m cored; 0 m drilled; 98.4 % recovery
Comment:
Reference depth=logging depth (mbsf) / The Hole was logged with a downhole logging tool string which included the NGT (Natural Gamma Tool) sondes.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1AGEAgeka BPGeocode
2DEPTH, sediment/rockDepthmGeocode
3Depth, referenceDepth refmWesterhold, Thomas
4Sample code/labelSample labelWesterhold, ThomasODP sample designation
5Cibicidoides wuellerstorfi, δ18OC. wuellerstorfi δ18O‰ PDBWesterhold, ThomasMass spectrometer Finnigan MAT 252
6Cibicidoides kullenbergi, δ18OC. kullenbergi δ18O‰ PDBWesterhold, ThomasMass spectrometer Finnigan MAT 252
Size:
7641 data points

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