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Article Abstract

This study investigates the impact of unseasonable storm events in McMurdo Sound, Antarctica, in 2022 on eukaryotic microalgal communities (EMCs). We assessed EMCs from the fast-ice and sub-ice platelet layer (SIPL) associated with fast-ice formed during March (historical timing) and September (five months later). We compared three ice conditions: March-ice (fast ice with SIPL, frozen in March), September-ice (fast ice with SIPL, frozen in September), and September-no-SIPL (fast-ice without SIPL, frozen in September). Using metabarcoding and light microscopy, results showed higher diversity in March-ice EMCs compared to September-no-SIPL. Community structure was significantly influenced by ice condition and ice type. March-ice had the most unique ASVs, of all ice conditions. Biomass peaked in March-ice SIPLs at 25-50 cm, while September-ice SIPLs peaked at 0-25 cm. These findings demonstrate delayed ice formation alters EMC structure, diversity, and biomass, potentially impacting primary productivity, nutrient cycling, and Antarctic sea ice ecosystems.

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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC12063147PMC
http://dx.doi.org/10.1016/j.isci.2025.112417DOI Listing

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This study investigates the impact of unseasonable storm events in McMurdo Sound, Antarctica, in 2022 on eukaryotic microalgal communities (EMCs). We assessed EMCs from the fast-ice and sub-ice platelet layer (SIPL) associated with fast-ice formed during March (historical timing) and September (five months later). We compared three ice conditions: March-ice (fast ice with SIPL, frozen in March), September-ice (fast ice with SIPL, frozen in September), and September-no-SIPL (fast-ice without SIPL, frozen in September).

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