Carbon and microbes in a degrading palsa mire are distinct from a peatland and a wider connected sub-Arctic fluvial system
Nea Tuomela, Samu Elovaara, Jenni Hultman, Hermanni Kaartokallio, David N Thomas

TL;DR
This study compares carbon and microbial differences in a degrading palsa mire, a peatland, and a sub-Arctic river system, finding distinct characteristics in the palsa mire's ponds.
Contribution
The study reveals unique DOM and microbial patterns in thawing palsa mire ponds compared to peatlands and connected river systems.
Findings
Palsa ponds had higher DOM concentration and more aromatic DOM than peatland ponds.
Microbial communities in palsa ponds were distinct from those in peatland and other catchment areas.
Ultra-small Patescibacteria were abundant and dominated microbial communities across all sampled waters.
Abstract
Climate change is altering the biogeochemical cycling of carbon and nutrients in the northern peatland and permafrost regions, which provide two of the largest terrestrial carbon storages. Lateral transfer of carbon needs to be more widely studied, especially in smaller streams and catchments, as they receive high loading of organic matter and are hotspots of carbon degradation. In this study, we combined measurements of dissolved organic matter (DOM) quality and quantity with microbial community data from a small sub-Arctic catchment. Our aim was to understand how the catchment is affected by two subcatchments: Degrading palsa permafrost mire and peatland thawing in spring. The small thaw ponds in the palsa mire were clearly distinct from the rest of the catchment and ponds in the peatland: Palsa ponds had higher DOM concentration, more aromatic DOM, and distinctive microbial…
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Taxonomy
TopicsClimate change and permafrost · Peatlands and Wetlands Ecology · Polar Research and Ecology
