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Soil CO2 exchange controlled by the interaction of biocrust successional stage and environmental variables in two semiarid ecosystems
- Miralles, I., Ladrón de Guevara, M., Chamizo, S., Rodríguez-Caballero, E., Ortega, R., van Wesemael, B., Cantón, Y.
- Soil biology & biochemistry 2018 v.124 pp. 11-23
- Cyanobacteria, air temperature, annuals, arid lands, balance studies, biomass, carbon, carbon dioxide, carbon dioxide fixation, drought, ecosystems, environmental factors, growth and development, humidity, lichens, microbial communities, mosses and liverworts, photosynthesis, photosynthetically active radiation, rain, semiarid zones, soil profiles, soil water, temporal variation
- Biocrusts are a critical biological community that represents one of the most important photosynthetic biomass pools in dryland regions. Thus, they play an important role in CO₂ fluxes in these regions, where water availability limits vascular plant growth and development. The effect of biocrusts on CO₂ fluxes was expected to be controlled by the interplay of several environmental factors, as well as biocrust developmental stage and coverage. To test this hypothesis, we performed an in situ study during which we measured net CO₂ fluxes and dark respiration over biocrusted soils at different successional stages in two semiarid ecosystems, where biocrusts are one of the main surface components. In addition, CO₂ flux was measured in annual plants, which were an abundant interplant cover in one of the study sites during the measurement period. Field campaigns were conducted from early morning to dusk on selected days with different environmental conditions over the year. Gross photosynthesis was calculated from net CO₂ flux and dark respiration.Biocrusts showed contrasting responses in CO₂ exchange depending on environmental conditions during the day and the year and depending on biocrust developmental stage. CO₂ flux in biocrusts was highly correlated with soil moisture, but also with photosynthetically active radiation and temperature. During dry soil periods, soils colonized by biocrusts had net CO₂ fluxes close to zero, but after precipitation events (light or heavy) all the biocrust types began to photosynthesize. When the rainfall was right after an extended drought, the respiration by biocrusts themselves and underlying soil exceeded the biocrust gross photosynthesis, and consequently soils colonized by biocrusts behaved as CO₂ sources. On the contrary, consecutive precipitation events and mild temperatures caused soil colonization by biocrusts to behave as CO₂ sinks. Annual plants were measured during their senescence and acted as CO₂ sources during all measurement campaigns. The time of day when the biocrusts showed net CO₂ fixation depended on the interplay of humidity just above them, air temperature and photosynthetically active radiation. The biocrust type also significantly influenced CO₂ fluxes in both semiarid ecosystems. In general, during wet periods, late successional biocrusts (i.e. lichens and mosses) had higher gross photosynthesis than early successional biocrusts (developed and incipient cyanobacteria crusts). Nevertheless, dark respiration from late successional biocrusts and underlying soils was also higher than from early successional biocrusts, so both biocrust types had similar net CO₂ fluxes. These results highlight the importance of considering the whole soil profile under biocrusts with their associated microbial communities as well as the temporal variability of CO₂ fluxes in soils covered by biocrusts in carbon balance studies in semiarid regions.