Oceanic nutrient cycles are coupled, yet carbon-nitrogen-phosphorus (C: N: P) stoichiometry
in marine ecosystems is variable through space and time, with no clear consensus on the …

Phytoplankton elemental composition regulates the efficiency of energy and material
transfer in the interface between phytoplankton and their consumers. The ratio of particulate …

Concentrations and elemental stoichiometry of suspended particulate organic carbon,
nitrogen, phosphorus, and oxygen demand for respiration (C: N: P:− O2) play a vital role in …

Phytoplankton stoichiometry modulates the interaction between carbon, nitrogen and
phosphorus cycles. Environmentally driven variations in phytoplankton C: N: P can alter …

Climate warming likely drives ocean deoxygenation, but models still cannot fully explain
observed declines in oxygen. One unconstrained parameter is the oxygen demand per …

Introduction Accurate models of lake primary production are crucial for understanding
ecosystem function and predicting ecosystem responses to global change. However, current …

Recent studies have demonstrated regional differences in marine ecosystem C: N: P with
implications for carbon and nutrient cycles. Due to strong co-variance, temperature and …

Phytoplankton are globally responsible for~ 50% of the global oxygen production via
primary production, fuelling food webs, and can alter biogeochemical cycles. Grazing forms …