Response of vegetation and carbon fluxes to brown lemming herbivory in Northern Alaska

• Main Authors: Plein, Jessica, Clark, Rulon W., Arndt, Kyle A., Oechel, Walter C., Stow, Douglas, Zona, Donatella
• Format: Text
• Language: English
• Published: 2021
• Subjects: Arctic; Lemmus trimucronatus; Tundra; Alaska
• Online Access: https://doi.org/10.5194/bg-2021-286; https://bg.copernicus.org/preprints/bg-2021-286/

The Arctic is warming at double the average global rate, affecting the carbon cycle of tundra ecosystems. Most research on carbon fluxes from Arctic tundra ecosystems has focused on abiotic environmental controls (e.g. temperature, rainfall, or radiation). However, Arctic tundra vegetation, and therefore the carbon balance of these ecosystems, can be substantially impacted by herbivory. In this study we tested how vegetation consumption by brown lemmings ( Lemmus trimucronatus ) can impact carbon exchange of a wet-sedge tundra ecosystem near Utqiaġvik, Alaska during the summer, and the recovery of vegetation during a following summer. We placed brown lemmings in individual enclosure plots and tested the impact of lemmings’ herbivory on carbon dioxide (CO 2 ) and methane (CH 4 ) fluxes and the normalized difference vegetation index (NDVI) immediately after lemming removal and during the following growing season. During the first summer of the experiment, lemmings’ herbivory reduced plant biomass (as shown by the decrease in the NDVI) and decreased CO 2 uptake, while not significantly impacting CH 4 emissions. Methane emissions were likely not significantly affected due to CH 4 being produced deeper in the soil and escaping from the stem bases of the vascular plants. The summer following the lemming treatments, NDVI and CO 2 fluxes returned to magnitudes similar to those observed before the start of the experiment, suggesting recovery of the vegetation, and a transitory nature of the impact of lemming herbivory. Overall, lemming herbivory has short-term but substantial effects on carbon sequestration by vegetation and might contribute to the considerable interannual variability in CO 2 fluxes from tundra ecosystems.