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N and P constrain C in ecosystems under climate change: Role of nutrient redistribution, accumulation, and stoichiometry.


ABSTRACT: We use the Multiple Element Limitation (MEL) model to examine responses of 12 ecosystems to elevated carbon dioxide (CO2 ), warming, and 20% decreases or increases in precipitation. Ecosystems respond synergistically to elevated CO2 , warming, and decreased precipitation combined because higher water-use efficiency with elevated CO2 and higher fertility with warming compensate for responses to drought. Response to elevated CO2 , warming, and increased precipitation combined is additive. We analyze changes in ecosystem carbon (C) based on four nitrogen (N) and four phosphorus (P) attribution factors: (1) changes in total ecosystem N and P, (2) changes in N and P distribution between vegetation and soil, (3) changes in vegetation C:N and C:P ratios, and (4) changes in soil C:N and C:P ratios. In the combined CO2 and climate change simulations, all ecosystems gain C. The contributions of these four attribution factors to changes in ecosystem C storage varies among ecosystems because of differences in the initial distributions of N and P between vegetation and soil and the openness of the ecosystem N and P cycles. The net transfer of N and P from soil to vegetation dominates the C response of forests. For tundra and grasslands, the C gain is also associated with increased soil C:N and C:P. In ecosystems with symbiotic N fixation, C gains resulted from N accumulation. Because of differences in N versus P cycle openness and the distribution of organic matter between vegetation and soil, changes in the N and P attribution factors do not always parallel one another. Differences among ecosystems in C-nutrient interactions and the amount of woody biomass interact to shape ecosystem C sequestration under simulated global change. We suggest that future studies quantify the openness of the N and P cycles and changes in the distribution of C, N, and P among ecosystem components, which currently limit understanding of nutrient effects on C sequestration and responses to elevated CO2 and climate change.

SUBMITTER: Rastetter EB 

PROVIDER: S-EPMC10078338 | biostudies-literature | 2022 Dec

REPOSITORIES: biostudies-literature

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N and P constrain C in ecosystems under climate change: Role of nutrient redistribution, accumulation, and stoichiometry.

Rastetter Edward B EB   Kwiatkowski Bonnie L BL   Kicklighter David W DW   Barker Plotkin Audrey A   Genet Helene H   Nippert Jesse B JB   O'Keefe Kimberly K   Perakis Steven S SS   Porder Stephen S   Roley Sarah S SS   Ruess Roger W RW   Thompson Jonathan R JR   Wieder William R WR   Wilcox Kevin K   Yanai Ruth D RD  

Ecological applications : a publication of the Ecological Society of America 20220725 8


We use the Multiple Element Limitation (MEL) model to examine responses of 12 ecosystems to elevated carbon dioxide (CO<sub>2</sub> ), warming, and 20% decreases or increases in precipitation. Ecosystems respond synergistically to elevated CO<sub>2</sub> , warming, and decreased precipitation combined because higher water-use efficiency with elevated CO<sub>2</sub> and higher fertility with warming compensate for responses to drought. Response to elevated CO<sub>2</sub> , warming, and increased  ...[more]

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