{"title":"Carbon storage in mountain cloud forest communities, Jalpan de Serra, Querétaro, México","authors":"Fuentes-Romero Elizabeth, García Calderón Norma Eugenia, Sedov Sergey, López-Binnqüist Citlalli, Noé Velázquez-Rosas","doi":"10.1186/s13021-025-00324-1","DOIUrl":null,"url":null,"abstract":"<div><h3>Background</h3><p>Mountain cloud forests (MCF) are vulnerable ecosystems that harbor considerable biodiversity and are essential carbon regulators. However, information is scarce on the carbon storage potential and its patterns of variability across the conservation gradient in these forests. This study determined the carbon storage potential, the contribution of different pools, and their relationship with the degree of forest and soil conservation.</p><h3>Results</h3><p>The organic carbon storage of the communities ranged from 145.9 to 279 Mg C ha<sup>−1</sup>. Soil was the primary pool (68.08–198.1 Mg C ha<sup>−1</sup>), followed by above-ground biomass (42.87 – 116.74 Mg C ha<sup>−1</sup>), while the contribution of litter and roots was less. The contribution of above-ground biomass to the carbon stock was low due to the level of timber and fuelwood extraction present in these communities. The high carbon storage potential of the soil pool is determined by the presence of the O horizon, with a thickness of 8–10 cm, forming mull-type humus and a deep organo-mineral surface horizon with a high carbon content > 10 g kg<sup>−1</sup>, and with varying degrees of humification. The formation of clay-humus complexes maintains carbon stabilization and the formation of deep surface horizons (between 20 and 38 cm deep).</p><h3>Conclusion</h3><p>The results show that the carbon sequestration potential of the MCF is found in the soil associated with the organic horizons that develop at the surface and the presence of deep A horizons with high carbon content. The conservation of these layers, despite forest management, reflected in the aerial biomass, demonstrates the resilience of the soil due to carbon stabilization, attributed to the composition of resistant organic compounds and the formation of clay-humus complexes, which reduce the impact of degradation from erosion. This indicates that the conditions of the MCF still sustain the ecological and biogeochemical processes that support carbon sequestration and are regulated by the conservation policies of the Sierra Gorda Biosphere Reserve, Querétaro, Mexico.</p></div>","PeriodicalId":505,"journal":{"name":"Carbon Balance and Management","volume":"20 1","pages":""},"PeriodicalIF":5.8000,"publicationDate":"2025-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://cbmjournal.biomedcentral.com/counter/pdf/10.1186/s13021-025-00324-1","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Carbon Balance and Management","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1186/s13021-025-00324-1","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Background
Mountain cloud forests (MCF) are vulnerable ecosystems that harbor considerable biodiversity and are essential carbon regulators. However, information is scarce on the carbon storage potential and its patterns of variability across the conservation gradient in these forests. This study determined the carbon storage potential, the contribution of different pools, and their relationship with the degree of forest and soil conservation.
Results
The organic carbon storage of the communities ranged from 145.9 to 279 Mg C ha−1. Soil was the primary pool (68.08–198.1 Mg C ha−1), followed by above-ground biomass (42.87 – 116.74 Mg C ha−1), while the contribution of litter and roots was less. The contribution of above-ground biomass to the carbon stock was low due to the level of timber and fuelwood extraction present in these communities. The high carbon storage potential of the soil pool is determined by the presence of the O horizon, with a thickness of 8–10 cm, forming mull-type humus and a deep organo-mineral surface horizon with a high carbon content > 10 g kg−1, and with varying degrees of humification. The formation of clay-humus complexes maintains carbon stabilization and the formation of deep surface horizons (between 20 and 38 cm deep).
Conclusion
The results show that the carbon sequestration potential of the MCF is found in the soil associated with the organic horizons that develop at the surface and the presence of deep A horizons with high carbon content. The conservation of these layers, despite forest management, reflected in the aerial biomass, demonstrates the resilience of the soil due to carbon stabilization, attributed to the composition of resistant organic compounds and the formation of clay-humus complexes, which reduce the impact of degradation from erosion. This indicates that the conditions of the MCF still sustain the ecological and biogeochemical processes that support carbon sequestration and are regulated by the conservation policies of the Sierra Gorda Biosphere Reserve, Querétaro, Mexico.
期刊介绍:
Carbon Balance and Management is an open access, peer-reviewed online journal that encompasses all aspects of research aimed at developing a comprehensive policy relevant to the understanding of the global carbon cycle.
The global carbon cycle involves important couplings between climate, atmospheric CO2 and the terrestrial and oceanic biospheres. The current transformation of the carbon cycle due to changes in climate and atmospheric composition is widely recognized as potentially dangerous for the biosphere and for the well-being of humankind, and therefore monitoring, understanding and predicting the evolution of the carbon cycle in the context of the whole biosphere (both terrestrial and marine) is a challenge to the scientific community.
This demands interdisciplinary research and new approaches for studying geographical and temporal distributions of carbon pools and fluxes, control and feedback mechanisms of the carbon-climate system, points of intervention and windows of opportunity for managing the carbon-climate-human system.
Carbon Balance and Management is a medium for researchers in the field to convey the results of their research across disciplinary boundaries. Through this dissemination of research, the journal aims to support the work of the Intergovernmental Panel for Climate Change (IPCC) and to provide governmental and non-governmental organizations with instantaneous access to continually emerging knowledge, including paradigm shifts and consensual views.