Palaeogeography of Atlantic Canada 13–0 kyr
We combine isobase maps with a digital terrain model of Atlantic Canada to map coastlines from 13 14Ckyr BP to the present. At 13 14C kyrBP there are ridges of high relative sea level (rsl) values over Newfoundland and the Maritime Provinces, and a re-entrant of low values in the Gulf of St. Lawrenc...
| Main Authors: | , , |
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| Other Authors: | |
| Format: | Text |
| Language: | English |
| Published: |
2001
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| Subjects: | |
| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.458.7566 http://www.science.ulster.ac.uk/cma/slan/shawetal2002.pdf |
| Summary: | We combine isobase maps with a digital terrain model of Atlantic Canada to map coastlines from 13 14Ckyr BP to the present. At 13 14C kyrBP there are ridges of high relative sea level (rsl) values over Newfoundland and the Maritime Provinces, and a re-entrant of low values in the Gulf of St. Lawrence. This pattern persists well into the Holocene, and reflects crustal response to the slow wasting of ice caps that persisted in Newfoundland and the Maritime Provinces for up to five millennia after the removal of ice from the Gulf of St. Lawrence by a migrating calving embayment. The palaeogeographic reconstructions reveal an archipelago on the outer shelf, from Grand Bank to the continent, that persisted from>13 14CkyrBP until ca. 8 14C kyr BP. Much of the Magdalen Shelf was exposed, but the Magdalen Islands were never connected to the mainland. Prince Edward Island was initially separated from the mainland, became connected after 11 14C kyr BP, and was separated again just before 6 14C kyr BP, when Northumberland Strait formed. The reconstructions are highly sensitive to relatively small changes in isobase values, especially on the shallow banks |
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