The last deglaciation and its climatic events, such as the Bølling–Allerød (BA) and the
Younger–Dryas (YD), have been clearly recorded in the δ13C profiles of three stalagmites …

What role did the closing of the Central American Seaway play in enabling continental ice
sheets to wax and wane over North America and Fennoscandia? A summary of relevant …

Reconstructing sea-level changes during the last deglaciation provides a way of
understanding the ice dynamics that can perturb large continental ice sheets. The resolution …

Linked, abrupt changes of North Atlantic deep water formation, North Atlantic sea ice extent,
and widespread climate occurred repeatedly during the last ice age cycle and beyond in …

Abrupt changes in Western Mediterranean climate during the last deglaciation (20 to 6 cal
ka BP) are detected in marine core MD95-2043 (Alboran Sea) through the investigation of …

Oxygen-isotope variations were analyzed on bulk samples of shallow-water lake marl from
Gerzensee, Switzerland, in order to evaluate major and minor climatic oscillations during the …

The mummichog, Fundulus heteroclitus, exhibits extensive latitudinal clinal variation in a
number of physiological and biochemical traits, coupled with phylogeographical patterns at …

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 …

Shortly after 14,500 ybp during the deglaciation of the Laurentide Ice Sheet in eastern North
America, the 80 km wide Seneca-Cayuga paleo ice stream occupied the overdeepened …

In the context of the atmospheric CO 2 14 C/C (Δ C atm 14) changes since the last ice age,
two episodes of sharp Δ C atm 14 decline have been related to either the venting of deeply …