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.
• More diversity observed in March-ice condition EMCs.
• No biomass difference between conditions, but SIPL had more than fast ice.
• EMC composition differs in March-ice and both September ice conditions.
• Microalgal indicator species found in each ice condition.