Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change

Understanding feedbacks between terrestrial and atmospheric systems is vital for predicting the consequences of global change, particularly in the rapidly changing Arctic. Fire is a key process in this context, but the consequences of altered fire regimes in tundra ecosystems are rarely considered,...

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Published in:PLoS ONE
Main Authors: Higuera, Philip E., Brubaker, Linda B., Anderson, Patricia M., Brown, Thomas A., Kennedy, Alison T., Hu, Feng Sheng
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1627343
https://www.osti.gov/biblio/1627343
https://doi.org/10.1371/journal.pone.0001744
id ftosti:oai:osti.gov:1627343
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spelling ftosti:oai:osti.gov:1627343 2023-07-30T04:01:09+02:00 Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change Higuera, Philip E. Brubaker, Linda B. Anderson, Patricia M. Brown, Thomas A. Kennedy, Alison T. Hu, Feng Sheng 2023-07-03 application/pdf http://www.osti.gov/servlets/purl/1627343 https://www.osti.gov/biblio/1627343 https://doi.org/10.1371/journal.pone.0001744 unknown http://www.osti.gov/servlets/purl/1627343 https://www.osti.gov/biblio/1627343 https://doi.org/10.1371/journal.pone.0001744 doi:10.1371/journal.pone.0001744 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1371/journal.pone.0001744 2023-07-11T09:42:39Z Understanding feedbacks between terrestrial and atmospheric systems is vital for predicting the consequences of global change, particularly in the rapidly changing Arctic. Fire is a key process in this context, but the consequences of altered fire regimes in tundra ecosystems are rarely considered, largely because tundra fires occur infrequently on the modern landscape. We present paleoecological data that indicate frequent tundra fires in northcentral Alaska between 14,000 and 10,000 years ago. Charcoal and pollen from lake sediments reveal that ancient birch-dominated shrub tundra burned as often as modern boreal forests in the region, every 144 years on average (+/- 90 s.d.; n = 44). Although paleoclimate interpretations and data from modern tundra fires suggest that increased burning was aided by low effective moisture, vegetation cover clearly played a critical role in facilitating the paleofires by creating an abundance of fine fuels. These records suggest that greater fire activity will likely accompany temperature-related increases in shrub-dominated tundra predicted for the 21 st century and beyond. Increased tundra burning will have broad impacts on physical and biological systems as well as on land-atmosphere interactions in the Arctic, including the potential to release stored organic carbon to the atmosphere. Other/Unknown Material Arctic Tundra Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic PLoS ONE 3 3 e0001744
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Higuera, Philip E.
Brubaker, Linda B.
Anderson, Patricia M.
Brown, Thomas A.
Kennedy, Alison T.
Hu, Feng Sheng
Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change
topic_facet 54 ENVIRONMENTAL SCIENCES
description Understanding feedbacks between terrestrial and atmospheric systems is vital for predicting the consequences of global change, particularly in the rapidly changing Arctic. Fire is a key process in this context, but the consequences of altered fire regimes in tundra ecosystems are rarely considered, largely because tundra fires occur infrequently on the modern landscape. We present paleoecological data that indicate frequent tundra fires in northcentral Alaska between 14,000 and 10,000 years ago. Charcoal and pollen from lake sediments reveal that ancient birch-dominated shrub tundra burned as often as modern boreal forests in the region, every 144 years on average (+/- 90 s.d.; n = 44). Although paleoclimate interpretations and data from modern tundra fires suggest that increased burning was aided by low effective moisture, vegetation cover clearly played a critical role in facilitating the paleofires by creating an abundance of fine fuels. These records suggest that greater fire activity will likely accompany temperature-related increases in shrub-dominated tundra predicted for the 21 st century and beyond. Increased tundra burning will have broad impacts on physical and biological systems as well as on land-atmosphere interactions in the Arctic, including the potential to release stored organic carbon to the atmosphere.
author Higuera, Philip E.
Brubaker, Linda B.
Anderson, Patricia M.
Brown, Thomas A.
Kennedy, Alison T.
Hu, Feng Sheng
author_facet Higuera, Philip E.
Brubaker, Linda B.
Anderson, Patricia M.
Brown, Thomas A.
Kennedy, Alison T.
Hu, Feng Sheng
author_sort Higuera, Philip E.
title Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change
title_short Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change
title_full Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change
title_fullStr Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change
title_full_unstemmed Frequent Fires in Ancient Shrub Tundra: Implications of Paleorecords for Arctic Environmental Change
title_sort frequent fires in ancient shrub tundra: implications of paleorecords for arctic environmental change
publishDate 2023
url http://www.osti.gov/servlets/purl/1627343
https://www.osti.gov/biblio/1627343
https://doi.org/10.1371/journal.pone.0001744
geographic Arctic
geographic_facet Arctic
genre Arctic
Tundra
Alaska
genre_facet Arctic
Tundra
Alaska
op_relation http://www.osti.gov/servlets/purl/1627343
https://www.osti.gov/biblio/1627343
https://doi.org/10.1371/journal.pone.0001744
doi:10.1371/journal.pone.0001744
op_doi https://doi.org/10.1371/journal.pone.0001744
container_title PLoS ONE
container_volume 3
container_issue 3
container_start_page e0001744
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