Bond events are North Atlanticice rafting events that are tentatively linked to climate fluctuations in the Holocene. Eight such events have been identified. Bond events were previously believed to exhibit a roughly c. 1,500-year cycle, but the primary period of variability is now put at c. 1,000 years.[1][2]
Gerard C. Bond of the Lamont–Doherty Earth Observatory at Columbia University was the lead author of the 1997 paper that postulated the theory of 1470-year climate cycles in the Late Pleistocene and Holocene, mainly based on petrologic tracers of drift ice in the North Atlantic.[1][3] However, more recent work at a single site suggested that these tracers did not provide sufficient support for 1,500-year intervals of climate change, and suggested that the reported c. 1,500 ± 500-year period was a statistical artifact.[2]
Furthermore, following publication of the Greenland Ice Core Chronology 2005 (GICC05)[4] for the North GRIPice core, it became clear that Dansgaard–Oeschger events also show no such pattern.[2][5][6] The North Atlantic ice-rafting events happen to correlate with episodes of lowered lake levels in the Mid-Atlantic region of the United States,[7] the weakest[clarification needed] events of the Asianmonsoon for at least the past 9,000 years,[8][9] and also correlate with most aridification events in the Middle East for the past 55,000 years (both Heinrich and Bond events).[10][11]
^Obrochta, Stephen P.; Yokoyama, Yusuke; Morén, Jan; Crowley, Thomas J. (2014-04-01). "Conversion of GISP2-based sediment core age models to the GICC05 extended chronology". Quaternary Geochronology. 20: 1–7. Bibcode:2014QuGeo..20....1O. doi:10.1016/j.quageo.2013.09.001.
^Li, Yong-Xiang; Yu, Zicheng; Kodama, Kenneth P. (2007). "Sensitive moisture response to Holocene millennial-scale climate variations in the Mid-Atlantic region, USA". The Holocene. 17 (1): 3–8. Bibcode:2007Holoc..17....3L. doi:10.1177/0959683606069386. S2CID2206358.