Drury, Anna Joy; John, Cédric M (2016): (Supplementary Table 2) Overview of clumped isotope derived temperatures and comparable Uk37 data [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.865018, In supplement to: Drury, AJ; John, CM (2016): Exploring the potential of clumped isotope thermometry on coccolith-rich sediments as a sea surface temperature proxy. Geochemistry, Geophysics, Geosystems, 17(10), 4092-4104, https://doi.org/10.1002/2016GC006459
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Project(s):
Coverage:
Latitude: 2.507820 * Longitude: -117.969560
Minimum DEPTH, sediment/rock: 76.18 m * Maximum DEPTH, sediment/rock: 105.32 m
Event(s):
321-U1338B * Latitude: 2.507820 * Longitude: -117.969560 * Elevation: -4209.9 m * Recovery: 417.18 m * Campaign: Exp321 (Pacific Equatorial Age Transect II / Juan de Fuca) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 45 cores; 413.6 m cored; 100.87 % recovered; 2.5 m drilled; 416.1 m penetrated
Comment:
Depth is m CCSF-A (core composite depth below sea floor) from Wilkens et al., 2013.
Age from Drury et al., 2016.
Sample ID and depth information as reported by Rousselle et al., 2013. The depth reported in brackets is the CCSF-B depth on the shipboard splice (Expedition 320/321 Scientists, 2010).
Uk'37 temperatures from Rousselle et al., 2013 using the Conte et al., 2006 calibration.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
104 data points