A glimpse into the future: How the timing of sea ice formation influences associated microalgal communities

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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Publication Details

Journal
iScience
Published
2025-04-15
DOI
https://doi.org/10.1016/j.isci.2025.112417
Citations
3
Primary Topic
Marine and coastal plant biology
Type
article
Field-Weighted Citation Impact
5.38

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article

A glimpse into the future: How the timing of sea ice formation influences associated microalgal communities

Natalie Robinson, John K. Pearman, Ken G. Ryan, Jacqui Stuart et al.
3 citations
iScience
Marine and coastal plant biology
5.38
article

A glimpse into the future: How the timing of sea ice formation influences associated microalgal communities

Natalie Robinson, John K. Pearman, Ken G. Ryan, Jacqui Stuart, Kirsty F. Smith, Svenja Halfter, Greg H. Leonard, Craig Stewart
article en
3 citations

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.

iScienceVol. 28(5)
Victoria University of Wellington (NZ), National Institute of Water and Atmospheric Research (NZ), Cawthron Institute (NZ), University of Otago (NZ)
National Institute of Water and Atmospheric Research, Ministry of Business, Innovation and Employment
Life below water
Openalex Percentile: Top 5%
Marine and coastal plant biology
5.38
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