Projection of future biosphere-climate feedbacks heavily relies on robust simulations of land surface carbon dynamics. Furthermore, soil Nitrogen (N) and Phosphorus (P) availability strongly modulate the terrestrial ecosystem carbon cycle, including how plants respond to the elevated atmospheric CO2 concentration. The success of plant growth and ecosystem carbon accumulation depends on plant strategies of nutrient uptake and how nutrients are used to support biomass accumulation under the uneven stress of N versus P availability. Acknowledging the importance of N/P limitations, two fundamental laws have been widely supported in the literature: Liebig’s Law of the Minimum (LLM) and the Multiple Limitation Hypothesis (MLH). For example, applying LLM, a more limited supply of ecosystem P in the future compared with N will dramatically dampen the rate of ecosystem carbon accumulation. Conversely, based on MLH, terrestrial plants possess multiple pathways to overcome the uneven N/P co-limitation and achieve reasonably high growth, through adjusting photosynthesis rates based on leaf N/P concentrations, investing resources to enhance phosphatese or nirogenase activity, and so on.
Results/Conclusions
We implemented these two contrasting co-limitation laws to the Energy Exascale Earth System Model (E3SM) land model (ELM) and find that MLH better captures observed plant responses to different nutrient perturbations (n = 98), while LLM fails to capture how nitrogen and phosphorus limited systems respond to phosphorus and nitrogen fertilization, respectively. More importantly, LLM and MLH diverge dramatically in simulating the future responses of plant growth and ecosystem carbon accumulation to elevated CO2 in the future and lead to large ecosystem carbon differences. This analysis provides quantitative evidence on how co-limitation laws could affect understanding and prediction of the future carbon cycle.