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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Université d'Ottawa / University of Ottawa
1996
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| Online Access: | https://dx.doi.org/10.20381/ruor-8197 http://www.ruor.uottawa.ca/handle/10393/10247 |