Early successional changes in biological soil crust community assembly and nutrient capture in mining impacted landscapes

• Main Authors: Cowden, Phaedra, Hanner, Robert, Kuzmina, Maria, Conway, Alix, Collis, Brianna, Ivanova, Natalia, Stewart, Katherine
• Format: Dataset
• Language: unknown
• Published: 2022
• Subjects: bryophytes; 16S; Earth and Environmental Sciences; community assembly; ITS2; Biological soil crust; Arctic; Canada
• Online Access: https://search.dataone.org/view/sha256:a308f05797915b0475fcacddbc2ee2e0082c713a678ed077908110f7844f3b9c

Biological soil crusts (BSCs) are communities of bryophytes, lichens, bacteria, and fungi and are the primary colonizing communities in early successional landscapes. Investigating the role of BSCs in early ecosystem development have demonstrated that they often improve the physical and chemical conditions while also promoting soil microbial communities in early developing ecosystems. Although BSCs are considered ecosystem engineers in many early successional environments, the links between BSC functional processes and their developmental stage are unclear, especially in landscapes recovering from anthropogenic disturbances. In this study we examined natural BSC development over a 30-year chronosequence on two mining impacted landscapes in both boreal and arctic regions of Canada. The macro (bryophyte and lichen) and micro (bacteria and fungi)-phyla communities were identified through a combination of Ion torrent (16S) and Illumina MiSeq (ITS2) sequencing. We found similar ubiquitous ruderal bryophytes and bacteria species common at both mine sites, but significant differences in lichen and fungal community structure between the two study locations. In addition, community assembly of BSC macro (bryophytes and lichens) and micro (bacteria and fungi)-phyla changed over the first 30 years of recovery at both mine sites, however, these changes were unique to each mine site. We observed nutrient accumulation in the crust layer but did not find clear trends in available nutrients or gas flux over time. Instead, changes in our functional measurements were associated with colonization by specific BSC species. Further, the bacterial community at both mines seemed to be responding to changes in the bryophyte communities as they developed over time. This suggests that the establishment of bryophyte communities in early succession may be driving micro-phyla BSC community composition. A holistic view of BSCs as they develop over time in relation to their functional abilities needs further investigation. This knowledge will improve both our understanding of early stage BSC development and our ability to develop restoration techniques to effectively restore landscapes disturbed by anthropogenic activities.