Recent warming and glacier retreat in the Svalbard Archipelago, part of the Arctic cryosphere, have become increasingly evident. The present study investigated the foreland of Austre Brøggerbreen near Ny-Ålesund to clarify how soil nitrification responds to changing conditions. Two sites, exposed for different periods following glacier retreat, were compared. A manipulation experiment using open-top chambers (OTCs) and homogenized initial soil conditions was conducted to assess the effects of site differences, the OTC treatment, soil depth, and interannual variations on soil and nitrification properties. Although the OTC treatment slightly increased soil temperature and moisture, its overall effect on soil properties, ammonia oxidation potential (AOP), and microbial properties was negligible. In contrast, homogenization markedly increased total nitrogen at both sites and temporarily boosted AOPs for two years before levels returned to baseline. Site 2, exposed for longer, contained more soil nitrogen and showed higher AOP than Site 1. For example, in 2015, AOPs at 10°C were 3.5 and 2.4 ng N g–1 dry soil h–1 at Sites 2 and 1, respectively. Ammonia-oxidizing bacteria (AOB) and archaea (AOA) were both more abundant at Site 2, although AOB clearly dominated at both sites. While AOB-amoA operational taxonomic units (OTUs) were mostly shared between sites, community compositions differed: OTU2 was prevalent at Site 1, but minor at Site 2. OTU2 may act as a pioneer taxon that declines in later stages, or its pattern may reflect site-specific soil conditions. A phylogenetic analysis showed that OTU2 and OTU3 belonged to Cluster ME found near Mount Everest.
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