Soil fungal community development in a high Arctic glacier foreland follows a directional replacement model, with a mid-successional diversity maximum.

Six OTUs had an abundance of more than 2% of the total sequences, and four of these (OTU00026, OTU00034, OTU00037, and OTU00046, all classified as Ascomycota) showed a significant or marginally significant difference between the Early Stage and the Late Stage (p ≤ 0.05).

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Four of the six most abundant OTUs in the whole dataset were classified as Ascomycota and each showed a decreasing trend with deglaciated age.

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