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Fire regime on a cultural landscape: Navajo Nation

Fire has played an important role in the evolutionary environment of global ecosystems, and Indigenous peoples have long managed natural resources in these fire‐prone environments. We worked with the Navajo Nation Forestry Department to evaluate the historical role of fire on a 50 km(2) landscape bi...

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Autores principales: Whitehair, Lionel, Fulé, Peter Z., Meador, Andrew Sánchez, Azpeleta Tarancón, Alicia, Kim, Yeon‐Su
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6202706/
https://www.ncbi.nlm.nih.gov/pubmed/30386580
http://dx.doi.org/10.1002/ece3.4470
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author Whitehair, Lionel
Fulé, Peter Z.
Meador, Andrew Sánchez
Azpeleta Tarancón, Alicia
Kim, Yeon‐Su
author_facet Whitehair, Lionel
Fulé, Peter Z.
Meador, Andrew Sánchez
Azpeleta Tarancón, Alicia
Kim, Yeon‐Su
author_sort Whitehair, Lionel
collection PubMed
description Fire has played an important role in the evolutionary environment of global ecosystems, and Indigenous peoples have long managed natural resources in these fire‐prone environments. We worked with the Navajo Nation Forestry Department to evaluate the historical role of fire on a 50 km(2) landscape bisected by a natural mountain pass. We used fifty 5‐ha circular plots to collect proxy fire history data on fire‐scarred trees, stumps, logs, and snags in a coniferous forest centered on a key mountain pass. The fire history data were categorized into three groups: All (all 50 plots), Corridor (25 plots closest to Buffalo Pass drainage), and Outer (remaining 25 plots, farther from pass). We assessed spatial and temporal patterns of fire recurrence and fire‐climate relationships. The landscape experienced frequent fires from 1644, the earliest fire date with sufficient sample depth, to 1920, after which fire occurrence was interrupted. The mean fire interval (MFI) for fire dates scarring 10% or more of the samples was 6.25 years; there were 13 large‐scale fires identified with the 25% filter with an MFI of 22.6 years. Fire regimes varied over the landscape, with an early reduction in fire occurrence after 1829, likely associated with pastoralism, in the outer uplands away from the pass. In contrast, the pass corridor had continuing fire occurrence until the early 20th century.Synthesis. Fires were synchronized with large‐scale top‐down climatic oscillations (drought and La Niña), but the spatially explicit landscape sampling design allowed us to detect bottom‐up factors of topography, livestock grazing, and human movement patterns that interacted in complex ways to influence the fire regime at fine scales. Since the early 20th century, however, fires have been completely excluded. Fuel accumulation in the absence of fire and warming climate present challenges for future management.
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spelling pubmed-62027062018-11-01 Fire regime on a cultural landscape: Navajo Nation Whitehair, Lionel Fulé, Peter Z. Meador, Andrew Sánchez Azpeleta Tarancón, Alicia Kim, Yeon‐Su Ecol Evol Original Research Fire has played an important role in the evolutionary environment of global ecosystems, and Indigenous peoples have long managed natural resources in these fire‐prone environments. We worked with the Navajo Nation Forestry Department to evaluate the historical role of fire on a 50 km(2) landscape bisected by a natural mountain pass. We used fifty 5‐ha circular plots to collect proxy fire history data on fire‐scarred trees, stumps, logs, and snags in a coniferous forest centered on a key mountain pass. The fire history data were categorized into three groups: All (all 50 plots), Corridor (25 plots closest to Buffalo Pass drainage), and Outer (remaining 25 plots, farther from pass). We assessed spatial and temporal patterns of fire recurrence and fire‐climate relationships. The landscape experienced frequent fires from 1644, the earliest fire date with sufficient sample depth, to 1920, after which fire occurrence was interrupted. The mean fire interval (MFI) for fire dates scarring 10% or more of the samples was 6.25 years; there were 13 large‐scale fires identified with the 25% filter with an MFI of 22.6 years. Fire regimes varied over the landscape, with an early reduction in fire occurrence after 1829, likely associated with pastoralism, in the outer uplands away from the pass. In contrast, the pass corridor had continuing fire occurrence until the early 20th century.Synthesis. Fires were synchronized with large‐scale top‐down climatic oscillations (drought and La Niña), but the spatially explicit landscape sampling design allowed us to detect bottom‐up factors of topography, livestock grazing, and human movement patterns that interacted in complex ways to influence the fire regime at fine scales. Since the early 20th century, however, fires have been completely excluded. Fuel accumulation in the absence of fire and warming climate present challenges for future management. John Wiley and Sons Inc. 2018-09-12 /pmc/articles/PMC6202706/ /pubmed/30386580 http://dx.doi.org/10.1002/ece3.4470 Text en © 2018 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd. This is an open access article under the terms of the http://creativecommons.org/licenses/by/4.0/ License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
spellingShingle Original Research
Whitehair, Lionel
Fulé, Peter Z.
Meador, Andrew Sánchez
Azpeleta Tarancón, Alicia
Kim, Yeon‐Su
Fire regime on a cultural landscape: Navajo Nation
title Fire regime on a cultural landscape: Navajo Nation
title_full Fire regime on a cultural landscape: Navajo Nation
title_fullStr Fire regime on a cultural landscape: Navajo Nation
title_full_unstemmed Fire regime on a cultural landscape: Navajo Nation
title_short Fire regime on a cultural landscape: Navajo Nation
title_sort fire regime on a cultural landscape: navajo nation
topic Original Research
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6202706/
https://www.ncbi.nlm.nih.gov/pubmed/30386580
http://dx.doi.org/10.1002/ece3.4470
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