David W. P. Manning

Riverine Particulate Carbon, Nitrogen, and Phosphorus Are Decoupled From Land Cover at the Continental Scale

Resource quantity and quality co‐limit consumer production in forest streams

Experimental nutrient enrichment of forest streams reduces ecosystem nitrogen and phosphorus storage

Nitrogen and Phosphorus Uptake Stoichiometry Tracks Supply Ratio During 2-year Whole-Ecosystem Nutrient Additions

Transport of N and P in U.S. streams and rivers differs with land use and between dissolved and particulate forms

Plant phylogenetic history explains in‐stream decomposition at a global scale

Nutrients and temperature additively increase stream microbial respiration

Experimental nitrogen and phosphorus additions increase rates of stream ecosystem respiration and carbon loss

Global synthesis of the temperature sensitivity of leaf litter breakdown in streams and rivers

Convergence of detrital stoichiometry predicts thresholds of nutrient‐stimulated breakdown in streams

Experimental nutrient additions accelerate terrestrial carbon loss from stream ecosystems

Detrital stoichiometry as a critical nexus for the effects of streamwater nutrients on leaf litter breakdown rates

Low‐to‐moderate nitrogen and phosphorus concentrations accelerate microbially driven litter breakdown rates