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): Ca/Ti residual in sediment composite sediment core MD01-2444/2443 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.831756, 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
Always quote citation above when using data! You can download the citation in several formats below.
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
Coverage:
Latitude: 37.723000 * Longitude: -10.155000
Minimum Elevation: -2790.0 m * Maximum Elevation: -2790.0 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.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | AGE | Age | ka BP | Geocode | ||
2 | - | - | Hodell, David A | Ca/Ti residual derived by substracting the long-term trends using a weighted Least Squares error (Lowess) method (red). |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4202 data points
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