期刊
AQUATIC ECOSYSTEM HEALTH & MANAGEMENT
卷 11, 期 2, 页码 137-143出版社
TAYLOR & FRANCIS INC
DOI: 10.1080/14634980802097236
关键词
ostracodes; Goderich Basin; Manitoulin Basin; glacial meltwater
Meltwater events that affected Lake Huron during the last 12,000 years using the oxygen-isotope records provided by ostracodes have been identified. Three sediment cores were collected from Lake Huron; two from the Goderich Basin and one from the southern Manitoulin Basin. At certain times, these regions were isolated from each other and from other basins in the lake. The oxygen-isotope values obtained for the ostracodes indicate large variations in the composition of lake water, as has been reported elsewhere in Lake Huron. Lake Huron was inundated at least three times by water with very low delta O-18 values (similar to-20 versus similar to-7.5% for modern Lake Huron water). This low-O-18 water originated from the retreating Laurentide ice sheet. It was likely derived from proglacial Lake Agassiz, and may have been released during very short intervals of time. Other periods were characterized by lake water with much higher delta O-18 values, reaching a maximum of -6.1%. Overall, the oxygen-isotope compositions of early Lake Huron water and its precursors are characterized by extreme variations, which arose both from changing sources and regional climate change.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据