Quaternary Science Revi r D

• Other Authors: The Pennsylvania State University CiteSeerX Archives
• Format: Text
• Language: English
• Subjects: Lawrence River; North Atlantic
• Online Access: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.552.259; http://www.geology.wisc.edu/~davem/abstracts/08-4.pdf

con rm of ng acia or al o during T-I AMOC increased relatively early. During T-I, the eastward routing of freshwater that caused the Younger Dryas happened North Atlantic region (Clark et al., 2002), in subtropical records influenced by monsoon intensity (Yuan et al., 2004; Lawrence River 12.9 kyr BP (Johnson and McClure, 1976; Rooth, 1982; Broecker et al., 1989). This increased freshwater discharge freshened the northern North Atlan-which in part led modeling studies to suggest alternative freshwater sources as the cause of this event (Tarasov and routing hypothesis as the cause of the Younger Dryas (Carlson et al., 2007). However, evidence for a Younger Dryas-like event is equivocal during earlier deglaciations