Abstract

Coralline algae are globally distributed benthic primary producers that secrete calcium carbonate skeletons. In the context of ocean acidification, they have received much recent attention due to the potential vulnerability of their high‐Mg calcite skeletons and their many important ecological roles. Herein, we summarize what is known about coralline algal ecology and physiology, providing context to understand their responses to global climate change. We review the impacts of these changes, including ocean acidification, rising temperatures, and pollution, on coralline algal growth and calcification. We also assess the ongoing use of coralline algae as marine climate proxies via calibration of skeletal morphology and geochemistry to environmental conditions. Finally, we indicate critical gaps in our understanding of coralline algal calcification and physiology and highlight key areas for future research. These include analytical areas that recently have become more accessible, such as resolving phylogenetic relationships at all taxonomic ranks, elucidating the genes regulating algal photosynthesis and calcification, and calibrating skeletal geochemical metrics, as well as research directions that are broadly applicable to global change ecology, such as the importance of community‐scale and long‐term experiments in stress response.

Highlights

  • We summarize what is known about coralline algal ecology and physiology, providing context to understand their responses to global climate change

  • We review the impacts of these changes, including ocean acidification, rising temperatures, and pollution, on coralline algal growth and calcification

  • We indicate critical gaps in our understanding of coralline algal calcification and physiology and highlight key areas for future research. These include analytical areas that recently have become more accessible, such as resolving phylogenetic relationships at all taxonomic ranks, elucidating the genes regulating algal photosynthesis and calcification, and calibrating skeletal geochemical metrics, as well as research directions that are broadly applicable to global change ecology, such as the importance of community-scale and long-term experiments in stress response

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Summary

CORALLINE ALGAL ECOLOGY

Nongeniculate coralline algae, or coralline algae lacking noncalcified articulations (genicula) between calcified segments (Fig. 1, A and B), are some of the most abundant organisms throughout the hard-bottom marine photic zone (Adey and Macintyre 1973, Steneck 1986) This group includes crustose and rhodolith (or maerl) morphologies (Foster 2001). Crustose forms often cover a high proportion of primary space despite a relatively flat morphology that makes them easy to overgrow (Dethier and Steneck 2001) Such areas are referred to as crustose coralline carpets (Paine 1984). Rhodolith beds form in the absence of intense water movement, which could scatter or bury slow-growing rhodoliths

Articulated Geniculate growth form
ECOSYSTEM SERVICES
PHOTOSYNTHESIS AND CALCIFICATION
GLOBAL CHANGE IMPACTS ON PHYSIOLOGY
Findings
PALEOENVIRONMENTAL RECORDERS
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