Influence of soil properties on woody vegetation structure, diversity and seasonality in Neotropical savannas

• Published in: Austral ecology Vol. 49; no. 3
• Main Authors: Veríssimo, Arthur Aires, Silvério, Divino Vicente, Abadia, Ana Clara, Carrijo, Daielle, da Silveira‐Filho, Ricardo Rodrigues, Santos‐Silva, Domingos Lucas, Vergara Fagundes, Marina, Martins, Jhany, Gonçalves, Lorrayne Aparecida, Lenza, Eddie
• Format: Journal Article
• Language: English
• Published: Richmond Blackwell Publishing Ltd 01.03.2024
• Subjects: Alluvial deposits; Composition; Ecological effects; Ecological studies; Grasslands; Iron; Manganese; Normalized difference vegetative index; Planting density; Population density; Savannahs; Seasonal variations; Silt; Soil fertility; Soil properties; Soils; Species composition; Species richness; Vegetation; Woody plants; Cerrado Biome
• ISSN: 1442-9985; 1442-9993
• DOI: 10.1111/aec.13501

Abstract Understanding how savanna soil properties influence vegetation diversity and function is a major challenge in ecological studies. We investigated the effects of soil properties on woody species density, richness, composition, and vegetative phenology (inferred by the Normalized Difference Vegetation Index (NDVI)) in two alluvial and two interfluvial savanna sites (1 block of 10 plots of 20 × 50 m in each site), in the Brazilian Cerrado. We showed that plots in alluvial savannas present less fertile soils and have lower plant densities and species richness and higher seasonality of NDVI than plots in the interfluvial savannas. The species composition of the sites was associated with the P, Fe, K, and Mn content of the soil. Soil K, Fe, and Ca contents were the main variables associated with plant density in a linear mixed model (LMM) that explained 79% of data variability (r 2 c = 0.79%), and K, Fe, and Al were the main predictors to explain species richness (r 2 c = 0.81%). Soil K, pH, and Silt were the best predictors of the seasonality in NDVI (r 2 c = 0.14%). We highlight the all‐encompassing effect of K soil content on species density, richness, composition, and NDVI and argue that this macronutrient and a few other soil properties (e.g., P, Fe, Al, and Silt) are the main factors mediating plant responses to water and nutrient stress in woody savanna communities occurring in the Cerrado–Amazônia transition.