The diversity and abundance of chytrids on the Greenland Ice Sheet

格陵兰冰盖上壶菌的多样性和丰度

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Abstract

Zoosporic fungi of the Chytridiomycota phylum are lethal parasites of algae in Arctic freshwater and marine environments. The presence of members of the Chytridiomycota phylum has also been confirmed by amplicon sequencing and microscopy in various habitats on the Greenland Ice Sheet. Glacier ice algae of the genus Ancylonema (Zygnematophyceae, Streptophyta) dominate microbial communities on the margins of the Greenland Ice Sheet and play key roles in darkening and melting of surface ice. Recent studies and in-situ observations have identified undescribed chytrids infecting Ancylonema spp. blooms on the Greenland Ice Sheet. In this study, the diversity and abundance of Chytridiomycota fungi were assessed by collection of ice surface and cryoconite holes samples from several locations on the ice sheet. We provide the first quantitative assessment, using qPCR, to reveal that uncultured chytridiomycetous fungi on dark ice were one order of magnitude higher than in cryoconites throughout the 2022 melt season on the Central-West margin of the Greenland Ice Sheet. Phylogenetic trees, based on the assembled environmental 18S rRNA genes, highlight that surface ice habitats dominated by glacier ice algae or snow algae harbor a great diversity of fungi belonging to the Blastocladiomycota, Monoblepharidomycota and Chytridiomycota phyla. They appear to be potential novel taxa, based on small subunit (18S) rRNA gene sequence similarity analysis, increasing our knowledge of chytrids diversity in Arctic environments. The number of novel lineages distinguished from described taxa varied from 63 to 81, based on two sequence identity thresholds (> 97% and > 98%), respectively. Overall, this study addresses the lack of quantitative and phylogenetically resolved information on chytrids in supraglacial environments by providing the first assessment of their abundance and diversity across the Greenland Ice Sheet. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1038/s41598-026-41468-5.

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