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Forest Ecosystems 2022, 9(1): 100007 https://doi.org/10.1016/j.fecs.2022.100007
Research Article | Open Access | Issue | Published: 25 February 2022

Conifer establishment after the eruption of the Paricutin volcano in central Mexico

Show Author's Information Jesús Eduardo Sáenz-Cejaa,  Blanca Lizeth Sáenz-Cejab,  J. Trinidad Sáenz-Reyesc,  Diego Rafael Pérez-Salicrupa( )
Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México, Antigua Carretera a Pátzcuaro 8701 Col. Ex hacienda San José de la Huerta, 58190, Morelia, Mexico
Escuela Nacional de Estudios Superiores Unidad Morelia, Universidad Nacional Autónoma de México, Antigua Carretera a Pátzcuaro 8701 Col. Ex hacienda San José de la Huerta, 58190, Morelia, Mexico
Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias, Campo Experimental Uruapan, Av. Latinoamericana 1101, Col. Revolución, 60500, Uruapan, Mexico
Keywords:
Age structure, Dendrochronology, Lava flow, Primary succession, Tropical montane forest
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Sáenz-Ceja JE, Sáenz-Ceja BL, Sáenz-Reyes JT, et al. Conifer establishment after the eruption of the Paricutin volcano in central Mexico. Forest Ecosystems, 2022, 9(1): 100007. https://doi.org/10.1016/j.fecs.2022.100007
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Abstract Full text About this article
Background

Volcanic eruptions have large effects on forest ecosystems and create new substrates, triggering primary succession processes. The Paricutín volcano, born in central-western Mexico, erupted between 1943 and 1952. After the cessation of the eruptive activity, plant colonization began on the lava flows and tephra deposits, including the conifer species that dominate the surrounding mature forests. This study aims to reconstruct the history of the establishment of conifer trees on the substrates created by the Paricutín eruption.

Methods

16 sampling plots were established along three transects with northern, southern, and south-western aspects, located every 250 ​m from the preserved forest to the volcanic cone. Increment cores from 400 conifer trees were extracted and their age was determined by cross-dating annual tree rings. The order of the species colonization and the tree establishment, abundance, and dominance patterns were characterized. Also, the influence of the distance from the mature forests and the inter-annual climatic conditions on the temporal tree establishment pattern was evaluated.

Results

Eight pine and one fir species have been established since 1970, only 18 years after the end of the eruptive period. However, tree establishment increased by 12.9% annually after 1995, with the youngest tree in our sample getting established in 2015. We did not find a well-defined temporal and spatial pattern of species arrival, which suggests that colonization occurred randomly, although the four pine species that were established early became the most abundant and dominant. Tree establishment was not influenced by the distance from the mature forest, and wet inter-annual conditions did not enhance pulses of tree recruitment, exhibiting a continuous tree establishment pattern.

Conclusions

Conifer species have shown a great capacity for colonizing volcanic substrates created by the Paricutín eruption, which suggests that tropical montane conifers can regenerate rapidly under high-magnitude disturbances. These findings support the use of these forest species for ecological restoration.


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Abstract
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About this article

Conifer establishment after the eruption of the Paricutin volcano in central Mexico

Show Author's information Jesús Eduardo Sáenz-Cejaa, Blanca Lizeth Sáenz-Cejab, J. Trinidad Sáenz-Reyesc, Diego Rafael Pérez-Salicrupa( )
Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México, Antigua Carretera a Pátzcuaro 8701 Col. Ex hacienda San José de la Huerta, 58190, Morelia, Mexico
Escuela Nacional de Estudios Superiores Unidad Morelia, Universidad Nacional Autónoma de México, Antigua Carretera a Pátzcuaro 8701 Col. Ex hacienda San José de la Huerta, 58190, Morelia, Mexico
Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias, Campo Experimental Uruapan, Av. Latinoamericana 1101, Col. Revolución, 60500, Uruapan, Mexico

Abstract

Background

Volcanic eruptions have large effects on forest ecosystems and create new substrates, triggering primary succession processes. The Paricutín volcano, born in central-western Mexico, erupted between 1943 and 1952. After the cessation of the eruptive activity, plant colonization began on the lava flows and tephra deposits, including the conifer species that dominate the surrounding mature forests. This study aims to reconstruct the history of the establishment of conifer trees on the substrates created by the Paricutín eruption.

Methods

16 sampling plots were established along three transects with northern, southern, and south-western aspects, located every 250 ​m from the preserved forest to the volcanic cone. Increment cores from 400 conifer trees were extracted and their age was determined by cross-dating annual tree rings. The order of the species colonization and the tree establishment, abundance, and dominance patterns were characterized. Also, the influence of the distance from the mature forests and the inter-annual climatic conditions on the temporal tree establishment pattern was evaluated.

Results

Eight pine and one fir species have been established since 1970, only 18 years after the end of the eruptive period. However, tree establishment increased by 12.9% annually after 1995, with the youngest tree in our sample getting established in 2015. We did not find a well-defined temporal and spatial pattern of species arrival, which suggests that colonization occurred randomly, although the four pine species that were established early became the most abundant and dominant. Tree establishment was not influenced by the distance from the mature forest, and wet inter-annual conditions did not enhance pulses of tree recruitment, exhibiting a continuous tree establishment pattern.

Conclusions

Conifer species have shown a great capacity for colonizing volcanic substrates created by the Paricutín eruption, which suggests that tropical montane conifers can regenerate rapidly under high-magnitude disturbances. These findings support the use of these forest species for ecological restoration.

Keywords: Age structure, Dendrochronology, Lava flow, Primary succession, Tropical montane forest

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Published: 25 February 2022
Issue date: February 2022

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© 2022 Beijing Forestry University. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd.

Acknowledgements

The first author is grateful for the support of the Graduate Program in Biological Sciences at the Universidad Nacional Autónoma de Mexico, and the Mexican Council of Science and Technology (Conacyt) for the scholarship received to carry out graduate studies. The second author thanks the Undergraduate Program in Geosciences at the Escuela Nacional de Estudios Superiores (ENES), UNAM Campus Morelia. All the authors thank the authorities of the Caltzontzin Indigenous Community for the facilities granted for performing this study, and especially Jerónimo Ángel, Ignacio Cabrera, Luis Lara, and Ramón Guerrero for their support during the field sampling, as well as the Ecojardín at the Instituto de Investigaciones en Ecosistemas y Sustentabilidad for the space provided for the processing of dendrochronological samples. Finally, we thank Mary-Ann Hall for the editorial revision of the manuscript.

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