dor_id: 19281

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Investigaciones Geográficas", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Sistema Regional de Información en Línea para Revistas Científicas de América Latina, el Caribe, España y Portugal (Latindex); Scientific Electronic Library Online (SciELO); SCOPUS, Scimago Journal Rank (SJR); Bibliografía Latinoamericana en revistas de Investigación Científica y social (BIBLAT); Science Direct (Elsevier); Directory of Open Access Journals (DOAJ); Geographical Abstracts, Current, Geographical Publications, GeoDados

561.#.#.u: https://www.geografia.unam.mx/

650.#.4.x: Ciencias Sociales y Económicas

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://www.investigacionesgeograficas.unam.mx/index.php/rig/index

351.#.#.b: Investigaciones Geográficas

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

590.#.#.b: Concentrador

883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://www.investigacionesgeograficas.unam.mx/index.php/rig/article/view/43338/43783

100.1.#.a: Marlès Magre, Jaume; Valor Ivars, Teresa; Claramunt López, Bernat; Maneja Zaragoza, Roser; Pérez Salicrup, Diego R.; Sánchez Mateo, Sònia; Boada Juncà, Martí

524.#.#.a: Marlès Magre, Jaume, et al. (2015). Dendroclimatic analysis of Pinus pseudostrobus and Pinus devoniana in the municipalities of Áporo and Zitácuaro (Michoacán), Monarch Butterfly Biosphere Reserve. Investigaciones Geográficas; Núm. 88. Recuperado de https://repositorio.unam.mx/contenidos/19281

245.1.0.a: Dendroclimatic analysis of Pinus pseudostrobus and Pinus devoniana in the municipalities of Áporo and Zitácuaro (Michoacán), Monarch Butterfly Biosphere Reserve

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geografía, UNAM

264.#.0.c: 2015

264.#.1.c: 2015-12-01

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC 4.0 Internacional, https://creativecommons.org/licenses/by-nc/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico dianachg@igg.unam.mx

884.#.#.k: http://www.investigacionesgeograficas.unam.mx/index.php/rig/article/view/43338

001.#.#.#: 073.oai:ojs.pkp.sfu.ca:article/43338

041.#.7.h: spa

520.3.#.a: This article presents the first study on dendroclimatology of Pinus pseudostrobus and Pinus devoniana in the state of Michoacán (Mexico), specifically in the municipalities of Áporo and Zitácuaro, both municipalities within the Monarch Butterfly Biosphere Reserve (MBBR). The sampling in Áporo, northwest of the MBBR, was held in Los Ejidos del Rincón del Soto and Arroyo Seco, in Sierra Chincúa (May 2011). In Zitácuaro, southwest of the reserve, a sampling was performed in the Ejido de San Juan de Zitácuaro, in the area of Ocotal and Palma, and Meso Sedano (June 2011). There were a total of 38 Pinus pseudostrobus and 12 Pinus devoniana sampled in both areas of the study and distributed in 28 trees in the municipality of Áporo and 22 in Zitácuaro. Two samples per tree were taken at 1.3 m height, resulting in a total of 100 tree cores. The dendrochronological series in Áporo for the species Pinus pseudostrobus were extended to 62 years (1949-2010) and for Pinus devoniana 86 years (1925-2010); and the series in Zitácuaro for Pinus pseudostrobus and Pinus devoniana were extended to 47 years (1964-2010) and 44 years (1967-2010), respectively. The ring chronologies were validated using the program COFECHA, which calculates the cross correlations between individual series of the tree-growth, five series were eliminated due to very low or negative correlations. The climate data from Zitácuaro were obtained from two weather stations located in the same municipality. And, in the case of Áporo, the data was obtained from stations located in Senguio. The growth rates related to the climate were obtained by removing the growth trend of each tree due to the age, size and other factors such as the competition, using the program ARSTAN. The following statistics were used to evaluate the quality of the residual chronologies and to determine the potential dendrochronology of species for the different populations: the average correlation between series (Rbar), the signal expressed by the population (EPS), medium sensitivity (MS), and the auto-correlation of first order (AC). To analyze the correlation and the function of response between the radial growth and climate variables, the waste medium chronologies of the growth rates for both species, and the records of temperature and precipitation, were evaluated through the Dendroclim2002, which determines the period of the year that most influences the radial growth of Pinus in relation to monthly climate data. In order to establish the climatic parameters that control the radial growth of the studied species, the Pinus pseudostrobus was found to be the potential series to perform the dendrochronological study in Zitácuaro. The value of the series of Pinus devoniana is slightly lower (0.81) than the acceptance value (0.85). The series of radial growth were compared with the climate records of monthly precipitation, average monthly temperature, and average maximum and minimum monthly temperatures. Correlation functions indicate that the width of the rings of both species is regulated significantly by rainfall and the average maximum temperature in Zitácuaro. Both species react similarly to the climate, but with some differences. There is a positive relationship between radial growth of Pinus pseudostrobus and the increasing rainfall in April of the current year; and there is a negative relationship between radial growth and the increasing average maximum temperature in August the previous year. For Pinus devoniana there is a negative relationship between radial growth and the increasing rainfall in November of the previous year, and a positive relationship in February of the current year; and there is a negative relationship between radial growth and the increasing average of maximum temperature in July and August last year.

773.1.#.t: Investigaciones Geográficas; Núm. 88

773.1.#.o: http://www.investigacionesgeograficas.unam.mx/index.php/rig/index

022.#.#.a: ISSN electrónico: 2448-7279; ISSN impreso: 0188-4611

310.#.#.a: Cuatrimestral

264.#.1.b: Instituto de Geografía, UNAM

doi: https://doi.org/10.14350/rig.43338

handle: 00a979fa04ea93d6

harvesting_date: 2023-08-23 17:00:00.0

856.#.0.q: application/pdf

245.1.0.b: Análisis dendroclimático de Pinus pseudostrobus y Pinus devoniana en los municipios de Áporo y Zitácuaro (Michoacán), Reserva de la Biósfera de la Mariposa Monarca

last_modified: 2023-08-23 17:00:00

license_url: https://creativecommons.org/licenses/by-nc/4.0/legalcode.es

license_type: by-nc

_deleted_conflicts: 2-ab52a8a0d5ca209afe2ba94d640ba76a

No entro en nada

No entro en nada 2

Artículo

Dendroclimatic analysis of Pinus pseudostrobus and Pinus devoniana in the municipalities of Áporo and Zitácuaro (Michoacán), Monarch Butterfly Biosphere Reserve

Marlès Magre, Jaume; Valor Ivars, Teresa; Claramunt López, Bernat; Maneja Zaragoza, Roser; Pérez Salicrup, Diego R.; Sánchez Mateo, Sònia; Boada Juncà, Martí

Instituto de Geografía, UNAM, publicado en Investigaciones Geográficas, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geografía, UNAM
Revista
Investigaciones Geográficas
Repositorio
Revistas UNAM
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Marlès Magre, Jaume, et al. (2015). Dendroclimatic analysis of Pinus pseudostrobus and Pinus devoniana in the municipalities of Áporo and Zitácuaro (Michoacán), Monarch Butterfly Biosphere Reserve. Investigaciones Geográficas; Núm. 88. Recuperado de https://repositorio.unam.mx/contenidos/19281

Descripción del recurso

Autor(es)
Marlès Magre, Jaume; Valor Ivars, Teresa; Claramunt López, Bernat; Maneja Zaragoza, Roser; Pérez Salicrup, Diego R.; Sánchez Mateo, Sònia; Boada Juncà, Martí
Tipo
Artículo de Investigación
Área del conocimiento
Ciencias Sociales y Económicas
Título
Dendroclimatic analysis of Pinus pseudostrobus and Pinus devoniana in the municipalities of Áporo and Zitácuaro (Michoacán), Monarch Butterfly Biosphere Reserve
Fecha
2015-12-01
Resumen
This article presents the first study on dendroclimatology of Pinus pseudostrobus and Pinus devoniana in the state of Michoacán (Mexico), specifically in the municipalities of Áporo and Zitácuaro, both municipalities within the Monarch Butterfly Biosphere Reserve (MBBR). The sampling in Áporo, northwest of the MBBR, was held in Los Ejidos del Rincón del Soto and Arroyo Seco, in Sierra Chincúa (May 2011). In Zitácuaro, southwest of the reserve, a sampling was performed in the Ejido de San Juan de Zitácuaro, in the area of Ocotal and Palma, and Meso Sedano (June 2011). There were a total of 38 Pinus pseudostrobus and 12 Pinus devoniana sampled in both areas of the study and distributed in 28 trees in the municipality of Áporo and 22 in Zitácuaro. Two samples per tree were taken at 1.3 m height, resulting in a total of 100 tree cores. The dendrochronological series in Áporo for the species Pinus pseudostrobus were extended to 62 years (1949-2010) and for Pinus devoniana 86 years (1925-2010); and the series in Zitácuaro for Pinus pseudostrobus and Pinus devoniana were extended to 47 years (1964-2010) and 44 years (1967-2010), respectively. The ring chronologies were validated using the program COFECHA, which calculates the cross correlations between individual series of the tree-growth, five series were eliminated due to very low or negative correlations. The climate data from Zitácuaro were obtained from two weather stations located in the same municipality. And, in the case of Áporo, the data was obtained from stations located in Senguio. The growth rates related to the climate were obtained by removing the growth trend of each tree due to the age, size and other factors such as the competition, using the program ARSTAN. The following statistics were used to evaluate the quality of the residual chronologies and to determine the potential dendrochronology of species for the different populations: the average correlation between series (Rbar), the signal expressed by the population (EPS), medium sensitivity (MS), and the auto-correlation of first order (AC). To analyze the correlation and the function of response between the radial growth and climate variables, the waste medium chronologies of the growth rates for both species, and the records of temperature and precipitation, were evaluated through the Dendroclim2002, which determines the period of the year that most influences the radial growth of Pinus in relation to monthly climate data. In order to establish the climatic parameters that control the radial growth of the studied species, the Pinus pseudostrobus was found to be the potential series to perform the dendrochronological study in Zitácuaro. The value of the series of Pinus devoniana is slightly lower (0.81) than the acceptance value (0.85). The series of radial growth were compared with the climate records of monthly precipitation, average monthly temperature, and average maximum and minimum monthly temperatures. Correlation functions indicate that the width of the rings of both species is regulated significantly by rainfall and the average maximum temperature in Zitácuaro. Both species react similarly to the climate, but with some differences. There is a positive relationship between radial growth of Pinus pseudostrobus and the increasing rainfall in April of the current year; and there is a negative relationship between radial growth and the increasing average maximum temperature in August the previous year. For Pinus devoniana there is a negative relationship between radial growth and the increasing rainfall in November of the previous year, and a positive relationship in February of the current year; and there is a negative relationship between radial growth and the increasing average of maximum temperature in July and August last year.
Idioma
spa
ISSN
ISSN electrónico: 2448-7279; ISSN impreso: 0188-4611

Enlaces