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Abstract

Abstract

Each warm season, meltwater ponds form upon the debris-covered ice shelves located off the coast of Antarctica’s Bratina Island. The ponds, scattered irregularly across the landscape, constitute an ephemeral environment with rich microbial communities whose compositions are stable long-term ( ). Though the meltwater ponds form in close proximity, their physicochemical conditions can vastly differ, and, as a result, they each host distinct microbial assemblages ( ). Such environments may serve as analogs to ancient refugia during periods of Earth history characterized by planet-scale glaciations such as the Cryogenian ( ).

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/content/papers/10.3997/2214-4609.202333120
2023-09-10
2026-02-07
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References

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/content/papers/10.3997/2214-4609.202333120
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