Get access

Soil carbon storage under simulated climate change is mediated by plant functional type

Authors


Elise Pendall, tel. +1 307 766 6293, e-mail: pendall@uwyo.edu

Abstract

The stability of soil organic matter (SOM) pools exposed to elevated CO2 and warming has not been evaluated adequately in long-term experiments and represents a substantial source of uncertainty in predicting ecosystem feedbacks to climate change. We conducted a 6-year experiment combining free-air CO2 enrichment (FACE, 550 ppm) and warming (+2 °C) to evaluate changes in SOM accumulation in native Australian grassland. In this system, competitive interactions appear to favor C4 over C3 species under FACE and warming. We therefore investigated the role of plant functional type (FT) on biomass and SOM responses to the long-term treatments by carefully sampling soil under patches of C3- and C4-dominated vegetation. We used physical fractionation to quantify particulate organic matter (POM) and long-term incubation to assess potential decomposition rates. Aboveground production of C4 grasses increased in response to FACE, but total root biomass declined. Across treatments, C : N ratios were higher in leaves, roots and POM of C4 vegetation. CO2 and temperature treatments interacted with FT to influence SOM, and especially POM, such that soil carbon was increased by warming under C4 vegetation, but not in combination with elevated CO2. Potential decomposition rates increased in response to FACE and decreased with warming, possibly owing to treatment effects on soil moisture and microbial community composition. Decomposition was also inversely correlated with root N concentration, suggesting increased microbial demand for older, N-rich SOM in treatments with low root N inputs. This research suggests that C3–C4 vegetation responses to future climate conditions will strongly influence SOM storage in temperate grasslands.

Get access to the full text of this article

Ancillary