Do beaver ponds increase methane emissions along Arctic tundra streams?

• Published in: Environmental research letters Vol. 18; no. 7; pp. 75004 - 75014
• Main Authors: Clark, Jason A, Tape, Ken D, Baskaran, Latha, Elder, Clayton, Miller, Charles, Miner, Kimberley, O’Donnell, Jonathan A, Jones, Benjamin M
• Format: Journal Article
• Language: English
• Published: Bristol IOP Publishing 01-07-2023
• Subjects: Anaerobic conditions; Arctic; AVIRIS; beavers; Carbon cycle; Climate change; Climate effects; Disturbance; Emission measurements; Emissions; Geomorphology; Hot spots; Hydrology; hyperspectral remote sensing; Lakes; Methane; Permafrost; Polar environments; Ponds; Remote sensing; Sediments; Spectroscopy; Streams; Thawing; Tundra; Water table; Arctic region
• ISSN: 1748-9326; 1748-9326
• DOI: 10.1088/1748-9326/acde8e

Beaver engineering in the Arctic tundra induces hydrologic and geomorphic changes that are favorable to methane (CH
4
) production. Beaver-mediated methane emissions are driven by inundation of existing vegetation, conversion from lotic to lentic systems, accumulation of organic rich sediments, elevated water tables, anaerobic conditions, and thawing permafrost. Ground-based measurements of CH
4
emissions from beaver ponds in permafrost landscapes are scarce, but hyperspectral remote sensing data (AVIRIS-NG) permit mapping of ‘hotspots’ thought to represent locations of high CH
4
emission. We surveyed a 429.5 km
2
area in Northwestern Alaska using hyperspectral airborne imaging spectroscopy at ∼5 m pixel resolution (14.7 million observations) to examine spatial relationships between CH
4
hotspots and 118 beaver ponds. AVIRIS-NG CH
4
hotspots covered 0.539% (2.3 km
2
) of the study area, and were concentrated within 30 m of waterbodies. Comparing beaver ponds to all non-beaver waterbodies (including waterbodies >450 m from beaver-affected water), we found significantly greater CH
4
hotspot occurrences around beaver ponds, extending to a distance of 60 m. We found a 51% greater CH
4
hotspot occurrence ratio around beaver ponds relative to nearby non-beaver waterbodies. Dammed lake outlets showed no significant differences in CH
4
hotspot ratios compared to non-beaver lakes, likely due to little change in inundation extent. The enhancement in AVIRIS-NG CH
4
hotspots adjacent to beaver ponds is an example of a new disturbance regime, wrought by an ecosystem engineer, accelerating the effects of climate change in the Arctic. As beavers continue to expand into the Arctic and reshape lowland ecosystems, we expect continued wetland creation, permafrost thaw and alteration of the Arctic carbon cycle, as well as myriad physical and biological changes.