Eutrophic soils and weathering levels influence the distribution of seasonally dry forests in Brazil

IF 3.1 2区 农林科学 Q2 SOIL SCIENCE
Sara Ramos dos Santos , Carolina Malala Martins Souza , David Lukas de Arruda , Danilo de Lima Camêlo , Jairo Tronto , Greice Leal Pereira , Danilo Cesar de Mello , Wilson Tadeu Lopes da Silva , Liovando Marciano da Costa , Carlos Ernesto Gonçalves Reynaud Schaefer
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引用次数: 0

Abstract

Seasonally Dry Forests, or ‘Dry Forests,’ are characterized by deciduous vegetation that sheds leaf during the dry season due to strong soil moisture stress. Despite their ecological significance, as part of the Atlantic Forest realm, research on the diversity, genesis, and soil-vegetation interactions in these ecosystems remains limited. This study investigated the soil attributes of Dry Forests of an ecotonal zone, comparing with the neighboring biomes, the Caatinga (Steppe Savanna) and Cerrado (Brazilian Savanna). We analyzed 16 soil profiles, evaluating their physical, chemical, and mineralogical properties using Principal Component Analysis (PCA). Dry Forest soils (DFS) showed higher amounts of exchangeable cations such as Ca2+, Mg2+, and K+ (Sum of Bases: 2.84–14.79 cmolc dm−3 in the surface horizons) and no detectable Al3+. The clay fraction of DFS is mainly illite and kaolinite. The PCA results (PC1: 29.4 %) revealed that Dry Forest soils, particularly on limestone, are more fertile than adjacent Caatinga and Cerrado soils. In contrast, according to the interpretation of PC2 (19.5 %) Cerrado soils are much more weathered and nutrient-depleted (Sum of Bases: 0.37–1.29 cmolc dm−3 in the surface horizons), while Caatinga soils exhibit an intermediate fertility (Sum of Bases: 1.48–21.81 cmolc dm−3 in the surface horizons), and less weathered. The lithologies under DFS at northern Minas Gerais are limestones of the Bambuí Group, resistant sedimentary rocks of the Macaúbas Group, and Granite/gneisses of the Crystalline Basement, which strongly influence soil fertility, mineralogy, and weathering degree. The higher nutrient levels and organic matter contents (2.05–12.03 % in the surface horizons) in DFS support greater productivity and biomass accumulation. These findings highlight the ecological significance of DFS on diverse geological substrates, offering insights for conservation, sustainable management, and ecological restoration in the face of increasing deforestation and land degradation threats.
富营养化土壤和风化程度影响巴西季节性干旱森林的分布
季节性干林或“干林”的特点是,由于强烈的土壤水分压力,落叶植被在干旱季节脱落叶子。尽管它们具有重要的生态意义,但作为大西洋森林领域的一部分,对这些生态系统的多样性、成因和土壤-植被相互作用的研究仍然有限。本文通过与邻近的Caatinga(草原稀树草原)和Cerrado(巴西稀树草原)生物群落的比较,研究了干旱林的土壤属性。我们分析了16个土壤剖面,利用主成分分析(PCA)评价了它们的物理、化学和矿物学性质。干燥森林土壤中Ca2+、Mg2+、K+等交换性阳离子含量较高(表层碱基总和为2.84 ~ 14.79 cmolc dm−3),Al3+未检测到。DFS的粘土组分主要为伊利石和高岭石。主成分分析结果(PC1: 29.4%)表明,干燥森林土壤,特别是石灰岩土壤,比邻近的Caatinga和Cerrado土壤更肥沃。相比之下,根据PC2(19.5%)的解释,Cerrado土壤的风化程度和养分消耗程度要高得多(表层层的碱基总和为0.37 ~ 1.29 cmolc dm−3),而Caatinga土壤则表现出中等的肥力(表层层的碱基总和为1.48 ~ 21.81 cmolc dm−3),而且风化程度较低。在米纳斯吉拉斯北部,DFS下的岩性为Bambuí组灰岩、Macaúbas组耐蚀沉积岩和结晶基底花岗岩/片麻质,它们强烈影响土壤肥力、矿物学和风化程度。高营养水平和有机质含量(表层2.05 ~ 12.03%)支持较高的生产力和生物量积累。这些发现突出了DFS在不同地质基质上的生态意义,为面对日益严重的森林砍伐和土地退化威胁的保护、可持续管理和生态恢复提供了见解。
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来源期刊
Geoderma Regional
Geoderma Regional Agricultural and Biological Sciences-Soil Science
CiteScore
6.10
自引率
7.30%
发文量
122
审稿时长
76 days
期刊介绍: Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.
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