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Kozdon, Reinhard; Kelly, Daniel Clay; Kitajima, K; Strickland, A; Fournelle, John H; Valley, John W (2013): (Table S4) In situ Mg and Sr measurements in diagenetic cements and muricae of ODP Hole 143-865C, electron microprobe [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.821551, In supplement to: Kozdon, R et al. (2013): In situ d18O and Mg/Ca analyses of diagenetic and planktic foraminiferal calcite preserved in a deep-sea record of the Paleocene-Eocene thermal maximum|. Paleoceanography, 28(3), 517-528, https://doi.org/10.1002/palo.20048

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Further details:
Berggren, William A; Kent, Dennis V; Swisher, Carl C, III; Aubry, Marie-Pierre (1995): A revised Cenozoic geochronology and chronostratigraphy. In: Berggren, W.A., Kent, D.V., Aubry, M.-P., Hardenbol, J. (eds.), Geochronology, time scales and global stratigraphic correlation. Special Publication - SEPM (Society for Sedimentary Geology), 54, 129-212, https://doi.org/10.2110/pec.95.04.0129
Bralower, Timothy J; Mutterlose, Jörg (1995): Calcareous nannofossil biostratigraphy of Site 865, Allison Guyot, Central Pacific Ocean: A tropical Paleogene reference section. In: Winterer, EL; Sager, WW; Firth, JV; Sinton, JM (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 143, 31-74, https://doi.org/10.2973/odp.proc.sr.143.204.1995
Project(s):
Coverage:
Latitude: 18.440400 * Longitude: -179.555000
Date/Time Start: 1992-04-04T01:30:00 * Date/Time End: 1992-04-04T14:15:00
Minimum DEPTH, sediment/rock: 102.87 m * Maximum DEPTH, sediment/rock: 102.90 m
Event(s):
143-865C * Latitude: 18.440400 * Longitude: -179.555000 * Date/Time Start: 1992-04-04T01:30:00 * Date/Time End: 1992-04-04T14:15:00 * Elevation: -1528.0 m * Penetration: 136.3 m * Recovery: 114.11 m * Location: North Pacific Ocean * Campaign: Leg143 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 15 cores; 136.3 m cored; 0 m drilled; 83.7 % recovery
Comment:
Sediment depth is given in mbsf. The age model was constructed using the published nannofossil biostratigraphy (Bralower and Mutterlose, 1995) and the ages assigned to the datums upon which this biozonation is based (Berggren et al. 1995).
Size:
303 data points

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