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    <gco:CharacterString>STUDY NOTES: Data collected by David J.R. Thornalley (Univ. of Cambridge); Principal Investigator: I. Nick McCave (Univ. of Cambridge); cruise CD-159, funded by UK RAPID program. Stable isotope values relative to VPDB standard, run in Godwin Laboratory, Univ. of Cambridge. Temperature calculated using Mg/Ca = B exp (0.1 × T). B = 0.794, 0.76 and 0.52 for G. bulloides, G. inflata and N. pachy. (s) respectively. RAPiD-10-1P: N. pachy. (s) and Cib. spp. isotope data originally presented in Thornalley, Elderfield &amp; McCave, 2010, DOI:10.1029/2009PA001833. RAPiD-12-1K: Please cite Thornalley, Elderfield &amp; McCave, Nature, 2009. For % sand and G. inflata d13C data, please cite Thornalley, Elderfield &amp; McCave, 2010, Paleoceanography, DOI:10.1029/2009PA001833. Vital effect of -0.24 applied to Melonis d18O data. Salinity calculated using Kim and O&apos;Neil (1997) to obtain d18Osw, including a 0.6‰ offset for G. bulloides, and VPDB to SMOW conversion of 0.27‰; Converted to salinity using Schmidt and Legrande (2006) N. Atlantic d18Osw-S relationship; Also corrected for whole ocean d18O and salinity changes (1 per mil glacial-interglacial) scaled to Fairbanks (1989) sea-level curve. Core-top age assignment: The core-top was not lost; assume 0cm=2004AD, but account for top 2 cm well mixed by bioturbation. RAPiD-15-4P: All data except N. pachy.(s) originally presented in Thornalley, McCave &amp; Elderfield, 2010, Paleoceanography, DOI:10.1029/2009PA001772. N. pachy. (s) isotope data originally presented in Thornalley, Elderfield &amp; McCave, 2010, Paleoceanography, DOI:10.1029/2009PA001833. d18Osw calculated using Kim and O&apos;Neil (1997), including a -0.6‰ offset for G. bulloides. Note - no offset used for N. pachy.(s) contrary to manuscript, and VPDB to SMOW conversion of 0.27‰ &quot;Ice-volume corrected&quot; for whole ocean changes using Fairbanks (1989) sea-level curve, assuming a LGM to late Holocene shift of 1‰. Salinity calculated based on North Atlantic relation of LeGrande and Schmidt (2006) and also for N. pachyderma for mixing with a freshwater endmember RAPiD-17-5P: C. wuell. And IRD data originally presented in Thornalley, Elderfield &amp; McCave, 2010, Paleoceanography, DOI:10.1029/2009PA001833. d18Osw calculated using Kim and O&apos;Neil (1997), including a 0.6‰ offset for G. bulloides, and VPDB to SMOW conversion of 0.27‰ &quot;Ice-volume corrected&quot; for whole ocean changes using Fairbanks (1989) sea-level curve, assuming a LGM to late Holocene shift of 1‰. 
ABSTRACT SUPPLIED BY ORIGINATOR: Greenland ice core records indicate that the last deglaciation (~7-21 ka) was punctuated by numerous abrupt climate reversals involving temperature changes of up to 5°C-10°C within decades. However, the cause behind many of these events is uncertain. A likely candidate may have been the input of deglacial meltwater, from the Laurentide ice sheet (LIS), to the high-latitude North Atlantic, which disrupted ocean circulation and triggered cooling. Yet the direct evidence of meltwater input for many of these events has so far remained undetected. In this study, we use the geochemistry (paired Mg/Ca-d18O) of planktonic foraminifera from a sediment core south of Iceland to reconstruct the input of freshwater to the northern North Atlantic during abrupt deglacial climate change. Our record can be placed on the same timescale as ice cores and therefore provides a direct comparison between the timing of freshwater input and climate variability. Meltwater events coincide with the onset of numerous cold intervals, including the Older Dryas (14.0 ka), two events during the Allerød (at ~13.1 and 13.6 ka), the Younger Dryas (12.9 ka), and the 8.2 ka event, supporting a causal link between these abrupt climate changes and meltwater input. During the Bølling-Allerød warm interval, we find that periods of warming are associated with an increased meltwater flux to the northern North Atlantic, which in turn induces abrupt cooling, a cessation in meltwater input, and eventual climate recovery. This implies that feedback between climate and meltwater input produced a highly variable climate. A comparison to published data sets suggests that this feedback likely included fluctuations in the southern margin of the LIS causing rerouting of LIS meltwater between southern and eastern drainage outlets, as proposed by Clark et al. (2001).</gco:CharacterString>
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