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Tiedemann, Ralf; Sturm, Arne; Steph, Silke; Lund, Steven P; Stoner, Joseph S (2007): (Table T4) Ages of the magnetic reversals for ODP Site 202-1237. PANGAEA, https://doi.org/10.1594/PANGAEA.773998, In supplement to: Tiedemann, R et al. (2007): Astronomically calibrated timescales from 6 to 2.5 Ma and benthic isotope stratigraphies, Sites 1236, 1237, 1239, and 1241. In: Tiedemann, R; Mix, AC; Richter, C; Ruddiman, WF (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 202, 1-69, https://doi.org/10.2973/odp.proc.sr.202.210.2007

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Related to:
Lourens, Lucas Joost; Hilgen, Frederik J; Laskar, Jacques; Shackleton, Nicholas J; Wilson, D (2004): The Neogene period. In: Gradstein, FM; Ogg, J; Smith, AG (eds.) A Geologic Time Scale 2004. Cambridge (Cambridge University Press), 409-440
Mix, Alan C; Tiedemann, Ralf; Blum, Peter; et al. (2003): Proceedings of the Ocean Drilling Program, 202 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 202, online, https://doi.org/10.2973/odp.proc.ir.202.2003
Shackleton, Nicholas J; Hagelberg, Teresa King; Crowhurst, Simon J (1995): Evaluating the success of astronomical tuning: Pitfalls of using coherence as a criterion for assessing pre-Pleistocene timescales. Paleoceanography, 10(4), 693-697, https://doi.org/10.1029/95PA01454
Project(s):
Coverage:
Latitude: -16.007017 * Longitude: -76.378083
Date/Time Start: 2002-04-26T00:00:00 * Date/Time End: 2002-04-26T00:00:00
Minimum DEPTH, sediment/rock: 41.35 m * Maximum DEPTH, sediment/rock: 98.00 m
Event(s):
202-1237 * Latitude: -16.007017 * Longitude: -76.378083 * Date/Time: 2002-04-26T00:00:00 * Elevation: -3212.3 m * Penetration: 896.2 m * Recovery: 771 m * Location: South Pacific Ocean * Campaign: Leg202 * Basis: Joides Resolution * Device: Composite Core (COMPCORE) * Comment: 79 cores; 744.7 m cored; 151.5 m drilled; 103.5 % recovery
Comment:
Note that the age models according to Lourens et al. (2004), Shackleton et al. (1995) and Cande and Kent (1995) do not differentiate between top, mean and base of reversal boundary. Sediment depth in mcd. The reversals were determined at sections that did not belong to the mcd splice. Using core logging data, these sections were more precisely matched to the mcd splice.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2Datum levelDLTiedemann, Ralf* = depth ranges of reversals are different to those published in Mix et al. (2003)
3Age modelAge modelkaTiedemann, Ralf
4Age model, optionalAge model optkaTiedemann, RalfAge model, ATNTS2004, Lourens et al., 2004Ages according to Lourens et al. (2004)
5Age model, optionalAge model optkaTiedemann, RalfAges according to Shackleton et al. (1995)
6Age model, optionalAge model optkaTiedemann, RalfAge model, GPTS (geomagnetic polarity timescale), Cande and Kent (1995)Ages according to Cande and Kent (1995)
Size:
222 data points

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