Potential for carbon sequestration in severely degraded temperate climate sites: Acrisol and Andosol gullies in Mexico

  • Michelle Carrillo-Castañeda Facultad de Ciencias, Universidad Nacional Autónoma de México, (UNAM), Ciudad Universitaria, Alcaldía Coyoacán, Ciudad de México, 04510 Mexico https://orcid.org/0009-0004-4146-8256
  • Aislinn A. Jiménez-Belmán Facultad de Biología, Universidad Michoacana de San Nicolás de Hidalgo (UMSNH), Morelia, Michoacán, 58030 Mexico https://orcid.org/0000-0002-8677-6533
  • Mariela Gómez-Romero Facultad de Biología, Universidad Michoacana de San Nicolás de Hidalgo (UMSNH), Morelia, Michoacán, 58030 Mexico / Cátedra, Consejo Nacional de Ciencia y Tecnología (CONACyT), Ciudad de México, 03940 Mexico https://orcid.org/0000-0003-4511-3001
  • Felipe García-Oliva Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México (UNAM), Morelia, Michoacán, 58190 Mexico https://orcid.org/0000-0003-4138-1850
  • Roberto Lindig-Cisneros Instituto de Investigaciones en Ecosistemas y Sustentabilidad, Universidad Nacional Autónoma de México (UNAM), Morelia, Michoacán, 58190 Mexico https://orcid.org/0000-0003-2542-7038
Keywords: ecological restoration, climate change, conifer, mitigation

Abstract

Aim of study: We assessed potential carbon (C) sequestration in gullies formed in Acrisols and Andosols, on the basis of long-term field restoration trials and GIS analysis.

Area of study: Two field trials in Michocán, Mexico, restored with Pinus pseudostrobus, Pinus greggii and Pinus devoniana in 2005 and 2009.

Material and methods: Soil C content was analyzed from field samples, and C content of aerial tree biomass of the three Pinus species was estimated by means of allometric equations. The potential restoration area was calculated with a GIS using available layers from the INEGI (Mexican National Institute for Geography and Statistics).

Main results: The spatial analysis showed that 1.83% of the Mexican territory are Acrisols and 1.18% are Andosols. From which, 40.87% of Acrisols and 42% of Andosols are eroded. The area with gullies was 2810 km² for both groups of soils within the elevational range of conifer forests in Mexico. C content at the two restored sites was on average of 1.27 t/ha. Soil C content in a 30-cm depth profile was 4.25 t/ha. The potential C sequestration for an average period of 13 years for an area of 2810 km² was 3.947 megatons of C (MtC). A total of four states ‒ Michoacán, Chiapas, Oaxaca, and Puebla ‒ concentrate 89% of the possible capture.

Research highlights: Severely degraded sites where gullying is dominant have a high potential for C sequestration once erosion has been controlled and plant cover has been restored.

Downloads

Download data is not yet available.

References

Bravo-Espinosa M, Mendoza ME, Medina-Orozco L, Sáenz-Reyes T, 2010. Características y control de cárcavas. Terra Latinoamericana 28: 281-285.

Duvert C, Gratiot N, Evrard O, Navratil O, Némery J, Prat C, et al., 2010. Drivers of erosion and suspended sediment transport in three headwater catchments of the Mexican Central Highlands. Geomorphology 123: 243-256. https://doi.org/10.1016/j.geomorph.2010.07.016

Farjon A, Pérez de la Rosa JA, Styles BT, 1997. Guía de campo de los pinos de México y América Central. Royal Botanical Gardens, Kew, UK.

Galicia L, Gamboa Cáceres AM, Cram S, Chávez Vergara B, Peña Ramírez V, Saynes V, et al., 2016. Almacén y dinámica del carbono orgánico del suelo en bosques templados de México. Terra Latinoamericana 34: 1-29.

Gómez-Pineda E, Sáenz-Romero C, Ortega-Rodríguez JM, Blanco-García A, Madrigal-Sánchez X, Lindig-Cisneros R, et al., 2020. Suitable climatic habitat changes for Mexican conifers along altitudinal gradients under climatic change scenarios. Ecol Appl 30(2): e02041. https://doi.org/10.1002/eap.2041

Gómez-Pineda E, Blanco-García A, Lindig-Cisneros R, O'Neill GA, Lopez-Toledo L, Sáenz-Romero C, 2021. Pinus pseudostrobus assisted migration trial with rain exclusion: maintaining Monarch Butterly Biosphere Reserve forest cover in an environment affected by climate change. New Forests 52: 995-1010. https://doi.org/10.1007/s11056-021-09838-1

Gómez-Romero M, Soto-Correa JC, Blanco-García JA, Sáenz-Romero C, Villegas J, Lindig-Cisneros R, 2012. Testing of pine species for restoration of degraded sites. Agrociencia 46: 795-807.

Gómez-Romero M, Villegas J, Sáenz-Romero C, Lindig-Cisneros R, 2013. Effect of mycorrhyzation in the establishment of Pinus pseudostrobus in gullies. Madera y Bosques 19(3): 51-63. https://doi.org/10.21829/myb.2013.193327

Huffman EN, 1997. Performance of a new automatic carbon dioxide coulometer. Microchem J 2: 567-573. https://doi.org/10.1016/0026-265X(77)90128-X

INEGI, 2001. Hipsometría de México. [.shp]. Escala 1:4000000. Instituto Nacional de Estadística y Geografía, México.

INEGI, 2005. Datos edafológicos de México. [.shp]. 1:1000000. Instituto Nacional de Estadística y Geografía, México.

INEGI, 2014. Datos erosión del suelo de México Serie l. [.shp]. 1:250000. Instituto Nacional de Estadística y Geografía, México.

IPCC, 2021. Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the 6th Assessment Report of the IPCC; Masson-Delmotte V et al. (eds.). Cambridge University Press.

Lal R, 2004. Soil carbon sequestration impacts on global climate change and food security. Science 304: 1623-1627. https://doi.org/10.1126/science.1097396

Lindig-Cisneros R, Villegas J, Báez-Pérez A, Gómez-Romero M, 2019. Biomass and iron accumulation in plants of Pinus pseudotrobus and Fraxinus uhdei in Acrisols from Western-Mexico with endo- and ectomycorrhiza. Catena 173: 410-413. https://doi.org/10.1016/j.catena.2018.10.033

Oliet J, Planelles R, Artero F, Jacobs D, 2005. Nursery fertilization and tree shelters affect long-term field response of Acacia salicina Lindl. planted in Mediterranean semiarid conditions. Forest Ecol Manage 215(1-3): 339-351. https://doi.org/10.1016/j.foreco.2005.05.024

Pérez-Nieto J, Valdés VE, Ordaz CVM, 2012. Cobertura vegetal y erosión del suelo en sistemas agroforestales de café bajo sombra. Terra Latinoamericana 30(3): 249-259.

QGIS, 2022. QGIS Geographic Information System. QGIS Association. http://www.qgis.org

Sáenz-Romero C, Rehfeldt GE, Crookston NL, Duval P, St-Amant R, Beaulieu J, et al., 2010. Spline models of contemporary, 2030, 2060 and 2090 climates for Mexico and their use in understanding climate-change impacts on the vegetation. Climatic Change 102(3-4): 595-623. https://doi.org/10.1007/s10584-009-9753-5

Sánchez Morales DV, 2008. Características hidrofísicas de andosles y acrisoles y su funcionamiento en dos cuencas del Estado de Michoacán. Tesis de Maestría, Universidad Nacional Autónoma de México, Ciudad de México, México. http://132.248.9.195/ptd2009/enero/0638756/0638756_A1.pdf.

Seneviratne SI, Zhang X, Adnan M, Badi W, Dereczynski C, Di Luca A, et al., 2021. Weather and climate extreme events in a changing climate. In: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the 6th Assessment Report of the IPCC; Masson-Delmotte V et al. (eds.). Cambridge University Press, pp. 1513-1766.

Solleiro-Rebolledo E, Rivera-Uria Y, Chávez-Vergara B, Díaz-Ortega J, Sedov S, Alcalá-Martínez JR, et al., 2019. Evolution of the landscape and pedodiversity on volcanic deposits in the south of the Basin of Mexico and its relationship with agricultural activities. Terra Latinoamericana 37: 501-518. https://doi.org/10.28940/terra.v37i4.565

Velasco BE, Romero SE, González HA, Moreno SF, Pérez MR, 2012. Funciones de biomasa y carbono aéreo aplicables a árboles de Pinus pseudostrobus Lindl. en México. Sociedad Española de Ciencias Forestales 34: 315-319.

Zhou Y, Zihang B, Qin W, Deng Q, Luo J, Liu H, et al., 2021. Primary environmental factor controlling gully distribution at the local and regional scale: An example from Northeastern China. Int Soil Water Conserv Res 9: 58-68. https://doi.org/10.1016/j.iswcr.2020.08.004

Published
2024-06-14
How to Cite
Carrillo-Castañeda, M., Jiménez-Belmán, A. A., Gómez-Romero, M., García-Oliva, F., & Lindig-Cisneros, R. (2024). Potential for carbon sequestration in severely degraded temperate climate sites: Acrisol and Andosol gullies in Mexico. Forest Systems, 33(2), eSC04. https://doi.org/10.5424/fs/2024332-20888
Section
Short communications