Climatic responses of Pinus pseudostrobus and Abies religiosa in the Monarch Butterfly Biosphere Reserve,Central Mexico |
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Affiliation: | 1. Centro de Investigaciones en Geografía Ambiental, Universidad Nacional Autónoma de México, Morelia, Michoacán, México;2. Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México, Morelia, Michoacán, México;3. Instituto Nacional de Investigación Forestal y Agropecuaria, Centro Nacional de Investigación Disciplinaria Relación Agua-Suelo Planta-Atmósfera, Laboratorio de Dendrocronología, Gómez-Palacio, Durango, Mexico;4. Laboratorio de Dendrocronología y Cambio Global, Instituto de Conservación, Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia, Chile;5. Center for Climate and Resilience Research (CR)2, Chile;1. Soil Science Department, “Luiz de Queiroz” College of Agriculture, University of São Paulo (USP/ESALQ), Piracicaba, São Paulo, Brazil;2. Laboratory of Ecology and Forest Restoration, “Luiz de Queiroz” College of Agriculture, University of São Paulo (USP/ESALQ), Piracicaba, São Paulo, Brazil;1. Faculty of Earth Sciences, University of Silesia, Sosnowiec, Poland;2. Institute of Botany and Landscape Ecology, University Greifswald, Greifswald, Germany;3. Department of Geography, University of Cambridge, Cambridge, UK;4. Swiss Federal Research Institute WSL, Birmensdorf, Switzerland;5. Czech Globe and Masaryk University, Brno, Czech Republic;1. Montana State University, Bozeman, MT, United States;2. U. S. Forest Service, Rocky Mountain Research Station, Missoula, MT, United States;3. U.S. Geological Survey, Northern Rocky Mountain Science Center, Bozeman, MT, United States;4. Salish Kootenai College, Pablo, MT, United States;5. Montana State University, Bozeman, MT, United States;1. Council for Agricultural Research and Economics, Research Centre for Agriculture and Environment (CREA-AA), Rome, Italy;2. Council for Agricultural Research and Economics, Research Centre for Forestry and Wood (CREA-FL), Arezzo, Italy;3. Council for Agricultural Research and Economics, Research Centre for Engineering and Agro-Food Processing (CREA-IT), Monterotondo, Italy;4. Department of Environmental Biology, University of Rome “La Sapienza”, Rome, Italy |
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Abstract: | Understanding the effects of climate on the growth of trees is important to project the response of forests to climate change. Dendrochronological analysis offers a “proxy” source for the effects of climatic variation on tree growth at different spatial and temporal scales. To examine influences of temperature and precipitation on radial growth of Pinus pseudostrobus and Abies religiosa, this study combines measurements of radial growth patterns of forest trees in the Monarch Butterfly Biosphere Reserve (MBBR) in central Mexico with temperature and precipitation variables from instrumental records. Dendrochronological samples were collected as cross sections and increment cores by using a chainsaw and increment borers, respectively. Total ring-width chronologies were developed for each site. Principal component analyses (PCA) were used to identify common temperature, precipitation and tree growth variation patterns. Correlation and response function analyses between chronologies and records of temperature and precipitation were used to evaluate the relation of climate variables on tree growth. The months during which tree growth was most strongly affected by precipitation were January, February and October from the previous year; only the temperature of September from the previous year affected the tree growth. In some chronologies, May’s average monthly maximum temperature was negatively correlated with tree growth. PCA and a comparison of PCA factor scores of climatic variables and chronologies showed no significant differences between northern, central or southern portions of the MBBR. Apparently, tree growth in the MBBR is reduced in years of low January–May precipitation combined with high summer (September of the previous year) temperatures, a scenario which is likely to occur as a consequence of global climate change. |
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Keywords: | Dendrochronology Climatic variability Mexico Radial growth Precipitation Temperature Tree-ring growth |
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