“…Five of these samples were recovered from three detrital carbonate-rich layers, respectively: the so-called detrital carbonate (DC) 1 related to HE 1, DC 0 related to HE 0 during the YD cold event, and a light detrital carbonate layer (see Stoner et al, 1996). (modified from McCartney, 1992;Schmitz and McCartney, 1993;Dickson and Brown, 1994;Lucotte and Hillaire-Marcel, 1994), and structural terranes outcropping in the nearby continents (after Bridgewater et al, 1991;Kalsbeek et al, 1993;Campbell et al, 1996) Nd isotopic data have been reported in Fagel et al (1999). Ages reported for each sample depth were estimated by direct linear interpolation of available AMS 14 C ages (italics), assuming a constant sedimentation rate, since they are relatively constant over short time intervals (Hillaire-Marcel et al, 1994b).…”