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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 [dataset]. 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):
Ocean Drilling Program (ODP)
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 * Method/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 InvestigatorMethod/DeviceComment
1 DEPTH, sediment/rockDepth sedmGeocode
2 Datum levelDLTiedemann, Ralf* = depth ranges of reversals are different to those published in Mix et al. (2003)
3 Age modelAge modelkaTiedemann, Ralf
4 Age model, optionalAge model optkaTiedemann, RalfAge model, ATNTS2004, Lourens et al., 2004Ages according to Lourens et al. (2004)
5 Age model, optionalAge model optkaTiedemann, RalfAges according to Shackleton et al. (1995)
6 Age model, optionalAge model optkaTiedemann, RalfAge model, GPTS (geomagnetic polarity timescale), Cande and Kent (1995)Ages according to Cande and Kent (1995)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
222 data points

Data

Download dataset as tab-delimited text — use the following character encoding:

1 
Depth sed [m]		2 
DL
(* = depth ranges of reversals...)		3 
Age model [ka]		4 
Age model opt [ka]
(Ages according to Lourens et ...)		5 
Age model opt [ka]
(Ages according to Shackleton ...)		6 
Age model opt [ka]
(Ages according to Cande and K...)
41.35Reunion (Base) - Top214221482150
41.81Reunion (Base) - Mean216621482150
42.36Reunion (Base) - Base219821482150
47.82Gauss/Matuyama - Top2583258126002600
47.93Gauss/Matuyama - Mean2591258126002600
48.04Gauss/Matuyama - Base2600258126002600
56.61Kaena (Top) - Top*3061303230463040
56.70Kaena (Top) - Mean*3065303230463040
56.80Kaena (Top) - Base*3070303230463040
57.60Kaena (Base) - Top*3111311631313110
57.73Kaena (Base) - Mean*3119311631313110
57.86Kaena (Base) - Base*3126311631313110
58.80Mammoth (Top) - Top*3197320732333220
58.85Mammoth (Top) - Mean*3201320732333220
58.99Mammoth (Top) - Base*3211320732333220
60.60Mammoth (Base) - Top3310333033313330
60.94Mammoth (Base) - Mean3331333033313330
61.28Mammoth (Base) - Base3351333033313330
65.53Gilbert/Gauss - Top3582359635943580
65.92Gilbert/Gauss - Mean3611359635943580
66.31Gilbert/Gauss - Base3627359635943580
75.13Cochiti (Top) - Top4162418741994180
75.48Cochiti (Top) - Mean4184418741994180
75.83Cochiti (Top) - Base4201418741994180
77.37Cochiti (Base) - Top4302430043164290
77.57Cochiti (Base) - Mean4314430043164290
77.76Cochiti (Base) - Base4325430043164290
81.00Nunivak (Top) - Top4487449344794480
81.17Nunivak (Top) - Mean4495449344794480
81.34Nunivak (Top) - Base4503449344794480
83.68Nunivak (Base) - Top4616463146234620
83.86Nunivak (Base) - Mean4624463146234620
84.04Nunivak (Base) - Base4633463146234620
87.37Sidufjall (Top) - Top4787479947814800
87.65Sidufjall (Top) - Mean4802479947814800
87.93Sidufjall (Top) - Base4817479947814800
88.77Sidufjall (Base) - Top*4860489648784890
89.07Sidufjall (Base) - Mean*4876489648784890
89.27Sidufjall (Base) - Base4888489648784890
90.83Thvera (Top) - Top4956499749774980
91.50Thvera (Top) - Mean4983499749774980
92.17Thvera (Top) - Base5008499749774980
96.64Thvera (Base) - Top5211523552325230
97.32Thvera (Base) - Mean5242523552325230
98.00Thvera (Base) - Base5272523552325230