Soil carbon stocks in temperate grasslands differ strongly across sites but are insensitive to decade‐long fertilization

• Published in: Global change biology Vol. 28; no. 4; pp. 1659 - 1677
• Main Authors: Keller, Adrienne B., Borer, Elizabeth T., Collins, Scott L., DeLancey, Lang C., Fay, Philip A., Hofmockel, Kirsten S., Leakey, Andrew D.B., Mayes, Melanie A., Seabloom, Eric W., Walter, Christopher A., Wang, Yong, Zhao, Qian, Hobbie, Sarah E.
• Format: Journal Article
• Language: English
• Published: England Blackwell Publishing Ltd 01.02.2022
• Subjects: Agricultural land; Biological fertilization; Biomass; Carbon; carbon cycling; Carbon dioxide; carbon sequestration; Ecosystem; Fertilization; Fractions; Grassland; Grasslands; Greenhouse effect; Greenhouse gases; Humans; Land use; Limiting factors; Limiting nutrients; Mineralogy; Moisture index; Nitrogen; Nitrogen - analysis; nutrient network; Nutrients; Organic matter; Particulate organic matter; Phosphorus; piecewise structural equation model; Plant biomass; Soil; soil carbon fractions; Soil fertility; Soil mineralogy; Soil moisture; Soil properties; Soil texture; Soils; Stocks; Storage; Structural equation modeling; Texture; carbon cycling; soil carbon fractions; nutrient network; fertilization; piecewise structural equation model; carbon sequestration
• ISSN: 1354-1013; 1365-2486
• DOI: 10.1111/gcb.15988

Enhancing soil carbon (C) storage has the potential to offset human‐caused increases in atmospheric CO2. Rising CO2 has occurred concurrently with increasing supply rates of biologically limiting nutrients such as nitrogen (N) and phosphorus (P). However, it is unclear how increased supplies of N and P will alter soil C sequestration, particularly in grasslands, which make up nearly a third of non‐agricultural land worldwide. Here, we leverage a globally distributed nutrient addition experiment (the Nutrient Network) to examine how a decade of N and P fertilization (alone and in combination) influenced soil C and N stocks at nine grassland sites spanning the continental United States. We measured changes in bulk soil C and N stocks and in three soil C fractions (light and heavy particulate organic matter, and mineral‐associated organic matter fractions). Nutrient amendment had variable effects on soil C and N pools that ranged from strongly positive to strongly negative, while soil C and N pool sizes varied by more than an order of magnitude across sites. Piecewise SEM clarified that small increases in plant C inputs with fertilization did not translate to greater soil C storage. Nevertheless, peak season aboveground plant biomass (but not root biomass or production) was strongly positively related to soil C storage at seven of the nine sites, and across all nine sites, soil C covaried with moisture index and soil mineralogy, regardless of fertilization. Overall, we show that site factors such as moisture index, plant productivity, soil texture, and mineralogy were key predictors of cross‐site soil C, while nutrient amendment had weaker and site‐specific effects on C sequestration. This suggests that prioritizing the protection of highly productive temperate grasslands is critical for reducing future greenhouse gas losses arising from land use change. We examined how soil carbon pools across nine United States grasslands respond to elevated nitrogen and phosphorus supply. We found that nutrient amendment had variable effects on soil C and N pools ranging from strongly positive to strongly negative, while soil C and N pool sizes varied by more than an order of magnitude across sites.