Diferencia entre revisiones de «Ciclos climáticos de 1500 años»

* ≈9,400 BP (Bond event 6) &mdash; coincidente con el [[evento Erdalen]] de la actividad glaciar en Noruega,<ref>{{ cite journal | last = Dahl | first = Svein Olaf | authorlink = | coauthors = ''et al.'' | year = 2002 | month = | title = Timing, equilibrium-line altitudes and climatic implications of two early-Holocene glacier readvances during the Erdalen Event at Jostedalsbreen, western Norway | journal = The Holocene | volume = 12 | issue = 1 | pages = 17&ndash;25 | doi = 10.1191/0959683602hl516rp | url = | accessdate = | quote = }}</ref> así como con un período frío en China.<ref name="Zhou2007">{{ cite journal | author = Zhou Jing | authorlink = | coauthors = Wang Sumin; Yang Guishan; Xiao Haifeng | year = 2007 | month = | title = Younger Dryas Event and Cold Events in Early-Mid Holocene: Record from the sediment of Erhai Lake | journal = Advances in Climate Change Research | volume = 3 | issue = Suppl. | pages = 1673&ndash;1719 | id = | url = http://www.climatechange.cn/qikan/manage/wenzhang/08.pdf | accessdate = | quote = }}</ref>

* ≈10,300 BP (Bond event 7) &mdash;

 

==Referencias==