2022
DOI: 10.1007/s42729-022-00890-0
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Does Structural Equation Modeling Provide a Holistic View of Phosphorus Acquisition Strategies in Soils of Amazon Forest?

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Cited by 5 publications
(2 citation statements)
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“…On the other hand, older and weathered soils are characterized by the continuous loss of N and P and the accumulation of P as occluded forms (Crews et al, 1995), with the organic forms of both elements exerting a strong control on the nutrient availability to plants (da Silva et al, 2022). The predominant low nutritional status of the soils in the fitting dataset and the positive relation between total N and total P indicates that in the very old and weathered soils of the pan-Amazon region, the low availability of P may be a limiting factor for biological N fixation (Liese et al, 2017;Van Langenhove et al, 2021;Zhang et al, 2022).…”
Section: Important Variables and Partial Dependencementioning
confidence: 99%
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“…On the other hand, older and weathered soils are characterized by the continuous loss of N and P and the accumulation of P as occluded forms (Crews et al, 1995), with the organic forms of both elements exerting a strong control on the nutrient availability to plants (da Silva et al, 2022). The predominant low nutritional status of the soils in the fitting dataset and the positive relation between total N and total P indicates that in the very old and weathered soils of the pan-Amazon region, the low availability of P may be a limiting factor for biological N fixation (Liese et al, 2017;Van Langenhove et al, 2021;Zhang et al, 2022).…”
Section: Important Variables and Partial Dependencementioning
confidence: 99%
“…Phosphorus (P) is one of the main plant macronutrients and it is known to pose major limitations on the terrestrial primary productivity in the tropics (Wollast et al, 1993, Du et al, 2020Cunha et al, 2022). In ecosystems with highly weathered soils, as in the pan-Amazon region (RAISG, 2022), the processes that govern the local readily available P (orthophosphates, i.e., salts and esters of the orthophosphoric acid) in soils are largely related to the mineralization of organic matter mediated by decomposers (da Silva et al, 2022). In such weathered soils, the readily available P for living organisms, including plants, is only a small fraction of the total P (Quesada et al, 2010;Vitousek et al, 2010;Walker and Syers, 1976), whereas most of the P is chemically bound or adsorbed to other molecules, forming stable organic and inorganic compounds (Buendia et al, 2014;Smeck, 1985).…”
Section: Introductionmentioning
confidence: 99%