@article{Bond17021995,
author = {Bond, Gerard C. and Lotti, Rusty}, 
title = {Iceberg Discharges into the North Atlantic on Millennial Time Scales During the Last Glaciation}, 
volume = {267}, 
number = {5200}, 
pages = {1005-1010}, 
year = {1995}, 
doi = {10.1126/science.267.5200.1005}, 
abstract ={High-resolution studies of North Atlantic deep sea cores demonstrate that prominent increases in iceberg calving recurred at intervals of 2000 to 3000 years, much more frequently than the 7000-to 10,000-year pacing of massive ice discharges associated with Heinrich events. The calving cycles correlate with warm-cold oscillations, called Dansgaard-Oeschger events, in Greenland ice cores. Each cycle records synchronous discharges of ice from different sources, and the cycles are decoupled from sea-surface temperatures. These findings point to a mechanism operating within the atmosphere that caused rapid oscillations in air temperatures above Greenland and in calving from more than one ice sheet.}, 
URL = {http://www.sciencemag.org/content/267/5200/1005.abstract}, 
eprint = {http://www.sciencemag.org/content/267/5200/1005.full.pdf}, 
journal = {Science} 
}