Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400
Archaeological and paleoecological investigations were undertaken at Uivak Point (HjCl-09 located in Okak Bay, Labrador), a site that consists of a winter village comprising the ruins of nine sod houses and a number of tent ring, cache, and other structures. The site was occupied during the late 18t...
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crsagepubl:10.1177/0959683615591350 2024-06-23T07:54:12+00:00 Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 Roy, Natasha Woollett, James Bhiry, Najat 2015 http://dx.doi.org/10.1177/0959683615591350 http://journals.sagepub.com/doi/pdf/10.1177/0959683615591350 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615591350 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 25, issue 11, page 1742-1755 ISSN 0959-6836 1477-0911 journal-article 2015 crsagepubl https://doi.org/10.1177/0959683615591350 2024-06-11T04:32:15Z Archaeological and paleoecological investigations were undertaken at Uivak Point (HjCl-09 located in Okak Bay, Labrador), a site that consists of a winter village comprising the ruins of nine sod houses and a number of tent ring, cache, and other structures. The site was occupied during the late 18th to early 19th centuries, although the immediate area has been used by many cultural groups spanning from Labrador’s early prehistory into the 20th century. Between ca. 3030 and ca. 710 cal. yr BP, cold and dry climate conditions corresponding to the late Neoglacial period generated the abundance of shrub tundra. From ca. 710 to ca. 550 cal. yr BP, conditions became warmer and wetter, triggering the expansion of trees. Since ca. 550 cal. yr BP, there has been an abundance of dry taxa which may reflect the colder conditions of the ‘Little Ice Age’. Subsequent climate warming has allowed the re-expansion of trees and shrubs over the last 200 years. Moreover, our results indicate that the Thule/Inuit harvested many plant species that grew in the vicinity of Uivak Point for food, raw material, and fuel. For example, many anthropogenic remains (burnt fat, burnt moss leaves, and charcoal) were incorporated into the soil. These activities also triggered the establishment of some weeds and apophytes ( Montia Fontana and Silene). Furthermore, our chronostratigraphical and paleoecological data suggest that the site was occupied on an irregular basis since approximately AD 1400. Article in Journal/Newspaper inuit Tundra SAGE Publications Fontana ENVELOPE(-60.586,-60.586,-62.996,-62.996) Okak ENVELOPE(-61.965,-61.965,57.550,57.550) Okak Bay ENVELOPE(-62.331,-62.331,57.467,57.467) The Holocene 25 11 1742 1755 |
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Open Polar |
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SAGE Publications |
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English |
description |
Archaeological and paleoecological investigations were undertaken at Uivak Point (HjCl-09 located in Okak Bay, Labrador), a site that consists of a winter village comprising the ruins of nine sod houses and a number of tent ring, cache, and other structures. The site was occupied during the late 18th to early 19th centuries, although the immediate area has been used by many cultural groups spanning from Labrador’s early prehistory into the 20th century. Between ca. 3030 and ca. 710 cal. yr BP, cold and dry climate conditions corresponding to the late Neoglacial period generated the abundance of shrub tundra. From ca. 710 to ca. 550 cal. yr BP, conditions became warmer and wetter, triggering the expansion of trees. Since ca. 550 cal. yr BP, there has been an abundance of dry taxa which may reflect the colder conditions of the ‘Little Ice Age’. Subsequent climate warming has allowed the re-expansion of trees and shrubs over the last 200 years. Moreover, our results indicate that the Thule/Inuit harvested many plant species that grew in the vicinity of Uivak Point for food, raw material, and fuel. For example, many anthropogenic remains (burnt fat, burnt moss leaves, and charcoal) were incorporated into the soil. These activities also triggered the establishment of some weeds and apophytes ( Montia Fontana and Silene). Furthermore, our chronostratigraphical and paleoecological data suggest that the site was occupied on an irregular basis since approximately AD 1400. |
format |
Article in Journal/Newspaper |
author |
Roy, Natasha Woollett, James Bhiry, Najat |
spellingShingle |
Roy, Natasha Woollett, James Bhiry, Najat Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 |
author_facet |
Roy, Natasha Woollett, James Bhiry, Najat |
author_sort |
Roy, Natasha |
title |
Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 |
title_short |
Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 |
title_full |
Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 |
title_fullStr |
Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 |
title_full_unstemmed |
Paleoecological perspectives on landscape history and anthropogenic impacts at Uivak Point, Labrador, since AD 1400 |
title_sort |
paleoecological perspectives on landscape history and anthropogenic impacts at uivak point, labrador, since ad 1400 |
publisher |
SAGE Publications |
publishDate |
2015 |
url |
http://dx.doi.org/10.1177/0959683615591350 http://journals.sagepub.com/doi/pdf/10.1177/0959683615591350 http://journals.sagepub.com/doi/full-xml/10.1177/0959683615591350 |
long_lat |
ENVELOPE(-60.586,-60.586,-62.996,-62.996) ENVELOPE(-61.965,-61.965,57.550,57.550) ENVELOPE(-62.331,-62.331,57.467,57.467) |
geographic |
Fontana Okak Okak Bay |
geographic_facet |
Fontana Okak Okak Bay |
genre |
inuit Tundra |
genre_facet |
inuit Tundra |
op_source |
The Holocene volume 25, issue 11, page 1742-1755 ISSN 0959-6836 1477-0911 |
op_rights |
http://journals.sagepub.com/page/policies/text-and-data-mining-license |
op_doi |
https://doi.org/10.1177/0959683615591350 |
container_title |
The Holocene |
container_volume |
25 |
container_issue |
11 |
container_start_page |
1742 |
op_container_end_page |
1755 |
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1802646251825528832 |