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Temporal changes in soil bacterial diversity and humic substances degradation in subarctic tundra soil

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Cited 17 time in scopus
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Temporal changes in soil bacterial diversity and humic substances degradation in subarctic tundra soil
Park, Ha Ju
Chae, Namyi
Sul, Woo Jun
Lee, Bang Yong
Lee, Yoo Kyung
Kim, Dockyu
Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology
Degradation; Humic substances; Low temperature; Microbial community; Temperature rise; Tundra soil
Issue Date
Park, Ha Ju, et al. 2015. "Temporal changes in soil bacterial diversity and humic substances degradation in subarctic tundra soil". Microbial Ecology,, 69(3): 668-675.
Humic substances (HS), primarily humic acids (HA) and fulvic acids (FA), are the largest constituent of soil organic matter. In microcosm systems with subarctic HS-rich tundra soil (site AK 1-75; approximately 5.6 °C during the thawing period) from Council, Alaska, the HA content significantly decreased to 48 % after a 99-day incubation at 5 °C as part of a biologically mediated process. Accordingly, levels of FA, a putative byproduct of HA degradation, consistently increased to 172 % during an identical incubation process. Culture-independent microbial community analysis showed that during the microcosm experiments, the relative abundance of phyla Proteobacteria (bacteria) and Euryarchaeota (archaea) largely increased, indicating their involvement in HS degradation. When the indigenous bacteria in AK 1-75 were enriched in an artificial mineral medium spiked with HA, the changes in relative abundance were most conspicuous in Proteobacteria (from 60.2 to 79.0 %), specifically Betaproteobacteria-related bacteria. One hundred twentytwo HA-degrading bacterial strains, primarily from the genera Paenibacillus (phylum Firmicutes) and Pseudomonas (class Gammaproteobacteria), were cultivated from AK 1-75 and nearby sites. Through culture-dependent analysis with these bacterial isolates, we observed increasing HS-degradation rates in parallel with rising temperatures in a range of 0 °C to 20 °C, with the most notable increase occurring at 8 °C compared to 6 °C. Our results indicate that, although microbial-mediated HS degradation occurs at temperature as low as 5 °C in tundra ecosystems, increasing soil temperature caused by global climate change could enhance HS degradation rates. Extending the thawing period could also increase degradation activity, thereby directly affecting nearby microbial communities and rhizosphere environments.
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