Yu Z, Eicher U
Z. C. Yu, Department of Botany, University of Toronto, Toronto, Ontario M5S 3B2, Canada, and Centre for Biodiversity and Conservation Biology; Royal Ontario Museum, Toronto, Ontario M5S 2C6, Canada. U. Eicher, Climate and Environmental.
Science. 1998 Dec 18;282(5397):2235-8. doi: 10.1126/science.282.5397.2235.
Evidence from stable isotopes and a variety of proxies from two Ontario lakes demonstrate that many of the late glacial-to-early Holocene events that are well known from the North Atlantic seaboard, such as the Gerzensee-Killarney Oscillation (also known as the Intra-Allerod Cold Period), Younger Dryas, and Preboreal Oscillation, also occurred in central North America. These results thus imply that climatic forcing acted in the same manner in both regions and that atmospheric circulation played an important role in the propagation of these events.
来自安大略省两个湖泊的稳定同位素和各种代理指标的证据表明，许多在北大西洋沿岸广为人知的晚冰期到全新世早期事件，如格泽湖-基拉尼振荡（也称为阿勒罗德期内冷期）、新仙女木事件和前北方振荡，也发生在北美中部。因此，这些结果意味着气候强迫在这两个地区以相同的方式起作用，并且大气环流在这些事件的传播中发挥了重要作用。
