Late-glacial, fine-resolution pollen and sediment analyses of Little Dyke Lake sediments, Central Nova Scotia.
A detailed analyses of Little Dyke Lake basal sediments revealed two environmental disturbances occurred during the late-glacial. These disturbances were correlated to the previously reported Killarney and Younger Dryas climatic oscillations of the Maritimes. Organic accumulation commenced at about...
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Format: | Thesis |
Language: | unknown |
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University of Ottawa (Canada)
1996
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Online Access: | http://hdl.handle.net/10393/10247 https://doi.org/10.20381/ruor-8197 |