Pleistocene horse remains from NW Banks Island, Canadian Arctic Archipelago: implications for long-term landscape evolution
| dc.contributor.author | Furze, Mark F.A. | |
| dc.date.accessioned | 2022-05-27T01:13:52Z | |
| dc.date.available | 2022-05-27T01:13:52Z | |
| dc.date.issued | 2012 | |
| dc.description.abstract | Recent work on NW Banks Island in the western Canadian Arctic Archipelago (CAA) has overturned the long-held paradigm that the area was never glaciated. However, occurrence of rare remains of mammoth from Banks and Melville islands (25.9-24.6 cal ka BP) suggests herb-rich tundra persisted for much of the Wisconsinan, and constrains the timing of glaciation. | |
| dc.description.uri | http://library.macewan.ca/cgi-bin/SFX/url.pl/7NF | |
| dc.identifier.uri | https://hdl.handle.net/20.500.14078/294 | |
| dc.language | English | |
| dc.language.iso | en | |
| dc.rights | All Rights Reserved | |
| dc.title | Pleistocene horse remains from NW Banks Island, Canadian Arctic Archipelago: implications for long-term landscape evolution | en |
| dc.type | Article | |
| dspace.entity.type |