Sediment depth is given in mcd. Additional comments: Between 1R-2,47 and 1R-3,48: Possible gap of P15 foram zone (uppermost middle Eocene; lower upper Eocene); between 3R-4,36 and 4R-1,67: GAP of 10 meters = C19n/C19r??; 8R-4,84: Was run as 84.042 (label on minicore), but actually should be 84.084 (actual location in Bremen core!); 8-R-3,2: Was run as 83.117 (label on vial), but actually should be 83.002 (actual location in Bremen core!); between 6R-1,118 and 7R-1,14: Gap...
Depth, sediment is given in mbsf.
All d15N expressed relative to atmospheric N2. Total organic carbon (TOC) and total nitrogen (TN) concentrations are given on a whole-sediment basis.
(Fig. 5.2) Profile of Lead/Calcium ratios of an Arctica islandica shell collected off the coast of Northeast IcelandJacqueline Krause-Nehring, Thomas Brey & Simon R Thorrold
Shell increments were used to assign calendar years to all Pb/Ca values.
(Appendix A) Radiolarian abundance in ODP Hole 202-1241A, supplement to: Kamikuri, Shin-Ichi; Motoyama, Isao; Nishi, Hiroshi; Iwai, Masao (2009): Evolution of Eastern Pacific Warm Pool and upwelling processes since the middle Miocene based on analysis of radiolarian assemblages: Response to Indonesian and Central American Seaways. Palaeogeography, Palaeoclimatology, Palaeoecology, 280(3-4), 469-479Shin-Ichi Kamikuri, Isao Motoyama, Hiroshi Nishi & Masao Iwai
A quantitative radiolarian study at Ocean Drilling Program Site 1241 in the eastern tropical Pacific enables us to reconstruct paleoceanographic changes that occurred since the latest middle Miocene. Today, this site is located just under the Eastern Pacific Warm Pool (EPWP). Based on the abundance variations of radiolarian characteristic species which are indicators of upwelling and thermocline changes, it is suggested that three notable changes occurred at 10.6, 9.8, and 4.2 Ma in the region....
Project: Convective and Orographically-induced Precipitation Study - Weather forecast models have not been successful in improving the Quantitative Precipitation Forecast during the last 16 years. One reason for this stagnation is the lack of comprehensive, high-quality data sets usable for model validation as well as for data assimilation, thus leading to improved initial fields in numerical models. Theoretical analyses have identified the requirements measured data have to meet in order to close the gaps in...
The file "EDC_DustFlux_25yr.dat" contains the 25-year constant time-step averages of the high-resolution 1cm data, averages being made of many data-points at the top, but only one or two at the bottom of the core. Please read the methods section of the paper before you do any variability analysis.
File format description see: Data Acquisition of ATLAS PARASTORE, Atlas Hydrographic (2007), Operator Manual ATLAS PARASTORE, Doc. Id.: ED 6006 G 212:/Version: 4.0/Edition: 05/2007, hdl:10013/epic.35589.d001.
(Table T3) Velocity changes applied to ODP Sites 188-1166 and 119-742 impedance logs to match synthetic seismograms to seismic profilesDavid A Handwerger, Alan K Cooper, Philip E O'Brien, Trevor Williams, Samantha R Barr, Robert B Dunbar, Amy Leventer & Richard D Jarrard
Lower boundary sediment depth is given in mbsf. Note that for Site 188-1166, the changes are too large to be realistic.
(Table T17) Constant rate of strain consolidation test conditions and consolidation properties of ODP Site 204-1244 sedimentsBrian Tan, John T Germaine & Peter B Flemings
All stresses / pressures were originally measured in ksc (kgf/cm**2). The conversion of ksc to SI units is 1 ksc = 98.07 kPa. Test samples CRS499 and CRS577 were omitted because of lacking ODP sample labels.
Concentrations (mg/kg) of terrigenous elements (i.e., Al, Fe, K, Ti and Si) in the 18-63 µm-sub-fraction of 16 samples from Core GeoB9504-3 determined by XRF powder measurement and ICP-OESJean Nizou, Till J J Hanebuth & Christoph Vogt
Only the terrigenous fraction of the sediment was analyzed, i.e., organic matter, carbonate and biogenic opal were removed chemically before measurement. Precision on ICP-OES measurements is 2%. Samples smaller than 1 g could not be analyzed with the XRF powder measurement device.
French National Centre for Scientific Research36
University of British Columbia28
University of California, Davis22
University of Cambridge19
University of Lausanne19
University of Exeter19
University of California, Berkeley18
University of Edinburgh18