Global Patterns and Controls of Nutrient Immobilization on Decomposing Cellulose in Riverine Ecosystems

dc.contributor.authorDavid M. Costello
dc.contributor.authorScott D. Tiegs
dc.contributor.authorLuz Boyero
dc.contributor.authorCristina Canhoto
dc.contributor.authorKrista A. Capps
dc.contributor.authorMichaël Danger
dc.contributor.authorPaul C. Frost
dc.contributor.authorMark O. Gessner
dc.contributor.authorNatalie A. Griffiths
dc.contributor.authorHalvor M. Halvorson
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T14:15:38Z
dc.date.available2026-03-22T14:15:38Z
dc.date.issued2022
dc.descriptionCitaciones: 22
dc.description.abstractAbstract Microbes play a critical role in plant litter decomposition and influence the fate of carbon in rivers and riparian zones. When decomposing low‐nutrient plant litter, microbes acquire nitrogen (N) and phosphorus (P) from the environment (i.e., nutrient immobilization), and this process is potentially sensitive to nutrient loading and changing climate. Nonetheless, environmental controls on immobilization are poorly understood because rates are also influenced by plant litter chemistry, which is coupled to the same environmental factors. Here we used a standardized, low‐nutrient organic matter substrate (cotton strips) to quantify nutrient immobilization at 100 paired stream and riparian sites representing 11 biomes worldwide. Immobilization rates varied by three orders of magnitude, were greater in rivers than riparian zones, and were strongly correlated to decomposition rates. In rivers, P immobilization rates were controlled by surface water phosphate concentrations, but N immobilization rates were not related to inorganic N. The N:P of immobilized nutrients was tightly constrained to a molar ratio of 10:1 despite wide variation in surface water N:P. Immobilization rates were temperature‐dependent in riparian zones but not related to temperature in rivers. However, in rivers nutrient supply ultimately controlled whether microbes could achieve the maximum expected decomposition rate at a given temperature. Collectively, we demonstrated that exogenous nutrient supply and immobilization are critical control points for decomposition of organic matter.
dc.identifier.doi10.1029/2021gb007163
dc.identifier.urihttps://doi.org/10.1029/2021gb007163
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/45472
dc.language.isoen
dc.publisherWiley
dc.relation.ispartofGlobal Biogeochemical Cycles
dc.sourceKent State University
dc.subjectNutrient
dc.subjectRiparian zone
dc.subjectPhosphorus
dc.subjectNutrient cycle
dc.subjectEnvironmental science
dc.subjectOrganic matter
dc.subjectEcosystem
dc.subjectLitter
dc.subjectEnvironmental chemistry
dc.subjectEutrophication
dc.titleGlobal Patterns and Controls of Nutrient Immobilization on Decomposing Cellulose in Riverine Ecosystems
dc.typearticle

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