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Hodell, David A; Crowhurst, Simon J; Skinner, Luke C; Tzedakis, Polychronis C; Margari, Vasiliki; Channell, James E T; Kamenov, George D; Maclachlan, Suzanne; Rothwell, Robin Guy (2013): Age model of composite sediment core MD01-2444/2443 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.831753, In supplement to: Hodell, DA et al. (2013): Response of Iberian Margin sediments to orbital and suborbital forcing over the past 420 ka. Paleoceanography, 28(1), 185-199, https://doi.org/10.1002/palo.20017

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Other version:
Hodell, David A; Crowhurst, Simon J; Skinner, Luke C; Tzedakis, Polychronis C; Margari, Vasiliki; Channell, James E T; Kamenov, George D; Maclachlan, Suzanne; Rothwell, Robin Guy (2013): NOAA/WDS Paleoclimatology - Iberian Margin 420KYr Geochemical and Color Variations Data. NOAA National Centers for Environmental Information, https://doi.org/10.25921/8KZ8-V888
Further details:
Coverage:
Latitude: 37.723000 * Longitude: -10.155000
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 37.99 m
Event(s):
MD01-2444/2443 * Latitude: 37.723000 * Longitude: -10.155000 * Elevation: -2790.0 m * Campaign: MD123 (GEOSCIENCES, MARMARCORE) * Basis: Marion Dufresne (1995) * Method/Device: Composite Core (COMPCORE)
Comment:
A composite section was created by splicing Cores MD01-2444 and MD01-2443 together at ~194 ka. The splice tie point corresponds to a depth of 27.42 mbsf in MD01-2444 and 16.74 mbsf in Core MD01-2443. The age model is a modified version of the one derived by Barker et al. (2011) based on correlation of millennial variability in MD01-2444 and MD01-2443 records to a synthetic Greenland temperature record produced using the EPICA Dome C (EDC) ice core and placed on the absolute speleothem timescale (GLt_syn age).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Age modelAge modelkaHodell, David A
Size:
66 data points

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