Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada
A pollen record from a lake sediment core from southeastern Prince of Wales Island, Nunavut, Canada (SW08; 72.3177, −97.2678, 104 m a.s.l) provides the first high-resolution July temperature reconstruction for the last 1,000 years for the central Canadian Arctic Archipelago. The vegetation underwent...
Published in: | Arctic, Antarctic, and Alpine Research |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Taylor & Francis Group
2019
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Online Access: | https://doi.org/10.1080/15230430.2019.1640527 https://doaj.org/article/3c6e1847f01d4a7da301d831bd66aff8 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:3c6e1847f01d4a7da301d831bd66aff8 2023-05-15T14:14:23+02:00 Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada Camille Tamo K. Gajewski 2019-01-01 https://doi.org/10.1080/15230430.2019.1640527 https://doaj.org/article/3c6e1847f01d4a7da301d831bd66aff8 en eng Taylor & Francis Group 1523-0430 1938-4246 doi:10.1080/15230430.2019.1640527 https://doaj.org/article/3c6e1847f01d4a7da301d831bd66aff8 undefined Arctic, Antarctic, and Alpine Research, Vol 51, Iss 1, Pp 348-365 (2019) quantitative paleoclimate reconstruction pollen medieval climate anomaly little ice age common era arctic anthro-bio geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.1080/15230430.2019.1640527 2023-01-22T19:16:45Z A pollen record from a lake sediment core from southeastern Prince of Wales Island, Nunavut, Canada (SW08; 72.3177, −97.2678, 104 m a.s.l) provides the first high-resolution July temperature reconstruction for the last 1,000 years for the central Canadian Arctic Archipelago. The vegetation underwent marked transitions during the Little Ice Age (LIA; 1500–1800 CE) and Medieval Climate Anomaly (MCA; 1090–1250 CE), which was primarily observed in the proportion of Cyperaceae, Poaceae, and Salix pollen. Cyperaceae pollen was highest in the samples corresponding to the MCA, whereas Poaceae increased during the LIA. In the last 30 years, Salix and Betula pollen increased. The mean July temperature reconstruction showed a long-term cooling from 1080–1915 CE with a sustained cold period from 1800–1915 CE prior to twentieth-century warming. A synthesis of paleoclimate records from across the Arctic demonstrates that pollen-based reconstructions record both high and low frequency climate variability, when sampling resolution is sufficient, and can improve regional climate reconstructions. Article in Journal/Newspaper Antarctic and Alpine Research Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Nunavut Prince of Wales Island Unknown Arctic Canada Canadian Arctic Archipelago Nunavut Prince of Wales Island ENVELOPE(-99.001,-99.001,72.668,72.668) Arctic, Antarctic, and Alpine Research 51 1 348 365 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
quantitative paleoclimate reconstruction pollen medieval climate anomaly little ice age common era arctic anthro-bio geo |
spellingShingle |
quantitative paleoclimate reconstruction pollen medieval climate anomaly little ice age common era arctic anthro-bio geo Camille Tamo K. Gajewski Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada |
topic_facet |
quantitative paleoclimate reconstruction pollen medieval climate anomaly little ice age common era arctic anthro-bio geo |
description |
A pollen record from a lake sediment core from southeastern Prince of Wales Island, Nunavut, Canada (SW08; 72.3177, −97.2678, 104 m a.s.l) provides the first high-resolution July temperature reconstruction for the last 1,000 years for the central Canadian Arctic Archipelago. The vegetation underwent marked transitions during the Little Ice Age (LIA; 1500–1800 CE) and Medieval Climate Anomaly (MCA; 1090–1250 CE), which was primarily observed in the proportion of Cyperaceae, Poaceae, and Salix pollen. Cyperaceae pollen was highest in the samples corresponding to the MCA, whereas Poaceae increased during the LIA. In the last 30 years, Salix and Betula pollen increased. The mean July temperature reconstruction showed a long-term cooling from 1080–1915 CE with a sustained cold period from 1800–1915 CE prior to twentieth-century warming. A synthesis of paleoclimate records from across the Arctic demonstrates that pollen-based reconstructions record both high and low frequency climate variability, when sampling resolution is sufficient, and can improve regional climate reconstructions. |
format |
Article in Journal/Newspaper |
author |
Camille Tamo K. Gajewski |
author_facet |
Camille Tamo K. Gajewski |
author_sort |
Camille Tamo |
title |
Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada |
title_short |
Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada |
title_full |
Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada |
title_fullStr |
Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada |
title_full_unstemmed |
Environmental changes of the last 1000 years on Prince of Wales Island, Nunavut, Canada |
title_sort |
environmental changes of the last 1000 years on prince of wales island, nunavut, canada |
publisher |
Taylor & Francis Group |
publishDate |
2019 |
url |
https://doi.org/10.1080/15230430.2019.1640527 https://doaj.org/article/3c6e1847f01d4a7da301d831bd66aff8 |
long_lat |
ENVELOPE(-99.001,-99.001,72.668,72.668) |
geographic |
Arctic Canada Canadian Arctic Archipelago Nunavut Prince of Wales Island |
geographic_facet |
Arctic Canada Canadian Arctic Archipelago Nunavut Prince of Wales Island |
genre |
Antarctic and Alpine Research Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Nunavut Prince of Wales Island |
genre_facet |
Antarctic and Alpine Research Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Nunavut Prince of Wales Island |
op_source |
Arctic, Antarctic, and Alpine Research, Vol 51, Iss 1, Pp 348-365 (2019) |
op_relation |
1523-0430 1938-4246 doi:10.1080/15230430.2019.1640527 https://doaj.org/article/3c6e1847f01d4a7da301d831bd66aff8 |
op_rights |
undefined |
op_doi |
https://doi.org/10.1080/15230430.2019.1640527 |
container_title |
Arctic, Antarctic, and Alpine Research |
container_volume |
51 |
container_issue |
1 |
container_start_page |
348 |
op_container_end_page |
365 |
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1766286877343612928 |