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Age model for the period spanning 140-118 ka of ODP Site 177-1094
The age model for the period spanning 140-118 ka was derived by tuning the TEX86L temperature record from ODP1094 to the Antarctic ice core temperature record on the Antarctic... -
(Table 2) Tie points of DSDP Site 94-609 and Greenland ice cores
DEPTH, sediment/rock gives meters below seafloor [mbsf]. The tie points to GISP2 used to produce the age model for Site 609 are shown at left (Bond et al., 1999). These data are... -
Age control points of sediment core PS75/093-1
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Age control points of sediment core PS75/083-1
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Age control points of sediment core PS75/079-2
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Age control points of sediment core PS75/076-2
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Age control points of sediment core PS75/074-3
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Age control points of sediment core PS75/059-2
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Age control points of sediment core PS75/056-1
Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM. -
Pollen and age analysis of terrestrial plant wax from ODP Hole 175-1085A
The composite depth is after the logging depth of Westerhold et al. (2005; Palaeogeography, Palaeoclimatology, Palaeoecology 217: 205) and the revised composite depth of Vidal... -
Tiepoints for ODP Site 108-658
XRF match: matching XRF-derived Ca counts from 658A/B to %CaCO3 from radiocarbon-dated 658C (deMenocal et al. 2000; Quaternary Science Reviews; 658C age model as in Adkins et... -
230Th-normalized opal flux analyses of sediment core MD03-2705
The age model was derived using linear interpolation between radiocarbon dates reported by Jullien et al. (2007). -
ln(Si/Al) record from ODP Site 108-658, off Mauritania
Depth, sediment [m] = mbsf ODP (m)New composite depth was derived based on the XRF data obtained in this study; for intervals with overlapping data, only data from one hole were... -
(Table 13) Diatom biostratigraphy of ODP Site 167-1022 sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 12) Diatom biostratigraphy of ODP Hole 167-1021B sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 11) Diatom biostratigraphy of ODP Hole 167-1020C sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and - = not found. -
(Table 10) Diatom biostratigraphy of ODP Hole 167-1020B sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 9) Diatom biostratigraphy of ODP Hole 167-1019C sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 8) Diatom biostratigraphy of ODP Hole 167-1018A sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 7) Diatom biostratigraphy of ODP Hole 167-1016A sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found.
