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Colin Lee Tucker

Publications and source records attributed to Colin Lee Tucker.

2 recordsLinked to original sources

Biocrust restoration in novel climates: Assisted migration, habitat amelioration, and varied community composition as climate-smart techniques

Introduction Successful restoration of terrestrial drylands depends on stable, fertile soils that retain water. These functions are provided by biological soil crusts (biocrust), suggesting their reestablishment is a critical step in dryland restoration. Restoration may be hindered by the increasingly documented negative effects of climate change, while new climate-smart biocrust restoration methods may improve short- and long-term restoration outcomes. Objectives In this study, we evaluated three approaches to climate-smart biocrust restoration: assisted migration, habitat amelioration via shading, and varied community composition. Methods We collected biocrusts from across wide geographic gradients spanning multiple climate regimes, including wide ranges of mean annual temperature, mean annual precipitation, and precipitation seasonality. We used biocrust from these different environments as inoculum in two common garden restoration trials, in a research greenhouse testing shading and drying, and at a rangeland field site evaluating shading and warming. Results Community composition was related to climate across the natal (inoculum source) sites, and differences in the initial proportion of moss, lichen, and cyanobacteria resulted in different responses to experimental restoration treatments. We found mixed support for the efficacy of assisted migration and likely not enough success to outweigh the potential risks at present. Shading facilitated moss establishment even under warmer and drier conditions but inhibited lichen establishment and had little effect on cyanobacteria, which colonized quickly between mosses and lichens. Conclusion Overall, our results suggest several potential paths forward for biocrust restoration in warming drylands.

western United States↗

Warming induces unexpectedly high soil respiration in a wet tropical forest

Tropical forests are a dominant regulator of the global carbon cycle, exchanging more carbon dioxide with the atmosphere than any other terrestrial biome. Climate models predict unprecedented climatic warming in tropical regions in the coming decades; however, in situ field warming studies are severely lacking in tropical forests. Here we present results from an in situ warming experiment in Puerto Rico, where soil respiration responses to + 4 o C warming were assessed half-hourly for a year. Soil respiration rates were 42-204% higher in warmed relative to ambient plots, representing some of the highest soil respiration rates reported for any terrestrial ecosystem. While respiration rates were significantly higher in the warmed plots, the temperature sensitivity (Q 10 ) was 71.7% lower, pointing to a mechanistic shift. Even with reduced Q 10 , if observed soil respiration rates persist in a warmer world, the feedback to future climate could be considerably greater than previously predicted or observed.

Puerto Rico↗