Frontiers in Ecology and Evolution (Jan 2023)

Biological responses to change in Antarctic sea ice habitats

  • Kerrie M. Swadling,
  • Kerrie M. Swadling,
  • Andrew J. Constable,
  • Alexander D. Fraser,
  • Robert A. Massom,
  • Robert A. Massom,
  • Robert A. Massom,
  • Melanie D. Borup,
  • Laura Ghigliotti,
  • Antonia Granata,
  • Letterio Guglielmo,
  • Nadine M. Johnston,
  • So Kawaguchi,
  • So Kawaguchi,
  • Fraser Kennedy,
  • Rainer Kiko,
  • Philippe Koubbi,
  • Philippe Koubbi,
  • Ryosuke Makabe,
  • Ryosuke Makabe,
  • Ryosuke Makabe,
  • Andrew Martin,
  • Andrew McMinn,
  • Andrew McMinn,
  • Masato Moteki,
  • Masato Moteki,
  • Evgeny A. Pakhomov,
  • Ilka Peeken,
  • Jody Reimer,
  • Jody Reimer,
  • Phillip Reid,
  • Phillip Reid,
  • Ken G. Ryan,
  • Marino Vacchi,
  • Patti Virtue,
  • Patti Virtue,
  • Patti Virtue,
  • Patti Virtue,
  • Christine K. Weldrick,
  • Pat Wongpan,
  • Simon J. Wotherspoon

DOI
https://doi.org/10.3389/fevo.2022.1073823
Journal volume & issue
Vol. 10

Abstract

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Sea ice is a key habitat in the high latitude Southern Ocean and is predicted to change in its extent, thickness and duration in coming decades. The sea-ice cover is instrumental in mediating ocean–atmosphere exchanges and provides an important substrate for organisms from microbes and algae to predators. Antarctic krill, Euphausia superba, is reliant on sea ice during key phases of its life cycle, particularly during the larval stages, for food and refuge from their predators, while other small grazers, including copepods and amphipods, either live in the brine channel system or find food and shelter at the ice-water interface and in gaps between rafted ice blocks. Fish, such as the Antarctic silverfish Pleuragramma antarcticum, use platelet ice (loosely-formed frazil crystals) as an essential hatching and nursery ground. In this paper, we apply the framework of the Marine Ecosystem Assessment for the Southern Ocean (MEASO) to review current knowledge about relationships between sea ice and associated primary production and secondary consumers, their status and the drivers of sea-ice change in this ocean. We then use qualitative network modelling to explore possible responses of lower trophic level sea-ice biota to different perturbations, including warming air and ocean temperatures, increased storminess and reduced annual sea-ice duration. This modelling shows that pelagic algae, copepods, krill and fish are likely to decrease in response to warming temperatures and reduced sea-ice duration, while salp populations will likely increase under conditions of reduced sea-ice duration and increased number of days of >0°C. Differences in responses to these pressures between the five MEASO sectors were also explored. Greater impacts of environmental pressures on ice-related biota occurring presently were found for the West and East Pacific sectors (notably the Ross Sea and western Antarctic Peninsula), with likely flow-on effects to the wider ecosystem. All sectors are expected to be impacted over coming decades. Finally, we highlight priorities for future sea ice biological research to address knowledge gaps in this field.

Keywords