2020
DOI: 10.1093/icesjms/fsaa195
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Physiological responses to temperature and ocean acidification in tropical fleshy macroalgae with varying affinities for inorganic carbon

Abstract: Marine macroalgae have variable carbon-uptake strategies that complicate predicting responses to environmental changes. In seawater, dissolved inorganic carbon availability can affect the underlying physiological mechanisms influencing carbon uptake. We tested the interactive effects of ocean acidification (OA) and warming on two HCO3−-users (Lobophora sp. and Amansia rhodantha), a predominately CO2-user (Avrainvillea nigricans), and a sole CO2-user (Plocamium hamatum) in the Great Barrier Reef, Australia. We … Show more

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Cited by 14 publications
(13 citation statements)
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“…A more prominent heat stress effects on growth rates than on photosynthesis was also reported in other tropical species (Sinutok et al, 2012;Terada et al, 2016), including P. acuta, and T. hemprichii (George et al, 2018;Poquita-Du et al, 2020;Ho et al, 2021). This implies that the general notion that photosynthesis is one of the most sensitive physiological processes (Bhagooli et al, 2021) and that its response may precede the response at growth level may not entirely hold true for heat stress or could not be supported by the chlorophyll fluorescence parameters measured in the present study.…”
Section: Effects Of Warming On Overall Performance Of Shallow-water Marine Organismscontrasting
confidence: 59%
“…A more prominent heat stress effects on growth rates than on photosynthesis was also reported in other tropical species (Sinutok et al, 2012;Terada et al, 2016), including P. acuta, and T. hemprichii (George et al, 2018;Poquita-Du et al, 2020;Ho et al, 2021). This implies that the general notion that photosynthesis is one of the most sensitive physiological processes (Bhagooli et al, 2021) and that its response may precede the response at growth level may not entirely hold true for heat stress or could not be supported by the chlorophyll fluorescence parameters measured in the present study.…”
Section: Effects Of Warming On Overall Performance Of Shallow-water Marine Organismscontrasting
confidence: 59%
“…Climate change threats to coral reef ecosystems include warming and ocean acidification, both of which are predicted to significantly degrade coral reefs around the globe in the coming decades (IPCC, 2022). Field and labbased studies have focused on the response of individual noncoral sessile groups to changes in temperature and pH, including sponges (Bell et al, 2018), ascidians (Peck et al, 2015), crustose coralline algae (CCA) (Kroeker et al, 2013;Cornwall et al, 2020), bryozoans (Pecquet et al, 2017), soft corals (Lopes et al, 2018), and fleshy encrusting macroalgae (Diaz-Pulido and Barroń, 2020;Ho et al, 2021). With newly developed methods furthering our ability to record in situ biogeochemical fluxes across benthic reef communities (Roth et al, 2019), studies are now needed to determine how cryptobenthic communities as a whole respond to combined stressors.…”
Section: Introductionmentioning
confidence: 99%
“…While the lack of macroalgae in the model may still be representative of reefs where herbivores are abundant, the outcome of competition under OA may be different on reefs that lack adequate herbivory. Indeed, some macroalgae can benefit from increases in CO 2 and/or HCO -3 under OA (Koch et al, 2013;Diaz-Pulido & Barrón, 2020;Ho et al, 2021), enhancing the competitive ability of macroalgae versus corals, and possibly increasing macroalgal dominance on reefs under OA (Anthony et al, 2011;Diaz-Pulido et al, 2011;Johnson et al, 2012). As such, it is important for future studies to build on the present approach with more sophisticated models (i.e., that may include macroalgal dynamics where applicable) that can be developed as suitable empirical data become available.…”
Section: Discussionmentioning
confidence: 99%