Coral resilience to ocean acidification and global warming through pH up-regulation

By M. McCulloch, J. Falter, J. Trotter, P. Montagna. 2012

577 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/1aad633a5127539eb99061a35087df31c9ab82f8

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Citations in the corpus

Impacts of ocean acidification on marine organisms: quantifying sensitivities and interaction with warming (2013, background): “…0.4 0.5 0.6 1 0 -1 -2 Reduction in pH from control Reduction in pH from control E! ec t s iz e (L nR R) B) CALCIFYING ALGAE PHOTOSYNTHESIS E) SEAGRASS PHOTOSYNTHESIS E! ec t s iz e (L nR R) D) COCCOLITHOPHORE PHOTOSYNTHESISA) OVERALL PHOTOSYNTHESIS E! ec t s iz e (L nR R) C) CORAL PHOTOSYNTHESIS”
The Omega Myth: What Really Drives Lower Calcification Rates in an Acidifying Ocean (2016, background): “Recent work has demonstrated that corals can actively control carbonate chemistry at the site of calcification (Venn et al., 2011; McCulloch et al., 2012), which brings into question the mechanistic understanding of how external seawater V could influence organismal calcification rates.”
Fast coral reef calcifiers are more sensitive to ocean acidification in short‐term laboratory incubations (2014, background): “15), two conditions that favor the precipitation of calcium carbonate (McCulloch et al. 2012).”
Conserving potential coral reef refuges at high latitudes (2014, background): “…evidence suggests that internal pHvalues in both invertebrate and calcifying algae bodies exceed those predicted as future ambient pH-values (Hurd et al., 2011; McCulloch et al., 2012) and that pH-value has little effect on the larval development of some invertebrates (Byrne et al., 2009).”
Ocean acidification effects on calcifying macroalgae (2014, result): “…et al. 2000, 2003, Leclercq et al. 2000, Guinotte et al. 2003, Jokiel et al. 2008, Andersson et al. 2009, Albright et al. 2010, Albright 2011) while others have shown mixed responses (Andersson et al. 2009, Ries 2009, Fabricius et al. 2011, Rodolofo-Metalpa et al. 2011, McCulloch et al. 2012).”
Adaptation and the physiology of ocean acidification (2013, unknown): “Recent work also shows that corals exert substantial control over pH at the site of calcification, with internal pH falling at only half the rate of external seawater under acidified conditions (McCulloch et al. 2012).”
MiFish metabarcoding: a high-throughput approach for simultaneous detection of multiple fish species from environmental DNA and other samples (2020, background): “Well-known examples include global warming and ocean acidification (Hoegh-Guldberg et al. 2007; Pandolfi et al. 2011; McCulloch et al. 2012; Six et al. 2013), both of which are causing ecosystem changes (Pörtner 2008; Robison 2009) and, in turn, have a serious impact on human life including fisherie”
Integrating climate-related stressor effects on marine organisms: unifying principles linking molecule to ecosystem-level changes (2012, background): “As an example, this principle mediates the correlation between calcification rates and calcium carbonate saturation levels in the water, the pattern of correlation being influenced by pH compensation capacity (e.g. McCulloch et al. 2012).”
Ocean acidification and marine microorganisms : responses and consequences (2015, background): “As a result, calcifiers which produce aragonite are more susceptible to OA or calcium carbonate saturation (McCulloch et al., 2012; Yool et al., 2013).”
Biological mechanisms supporting adaptation to ocean acidification in coastal ecosystems (2015, unknown): “This behaviour is simply attributable to Ωcf >> Ωsw with the extent of enrichment being attributable to mainly increased pHcf through up-regulation, and for zooxanthellate corals, combined with an approximately twofold enrichment in DIC (McCulloch et al., 2012a).”
Overview of the conservation status of Mediterranean anthozoa (2017, background): “Mediterranean deep water corals grow slowly and calcification in aragonite-limited waters could make them especially vulnerable to ocean acidification (McCulloch et al. 2012; Movilla et al. 2014b).”
The responses of eight coral reef calcifiers to increasing partial pressure of CO2 do not exhibit a tipping point (2013, background): “Such resistance to decreasing pH potentially may be due to the capacity to up-regulate pH at the site of calcification (McCulloch et al. 2012), which might be a critical factor in determining the dominant species in the high-CO2 oceans of the future.”
Thermal and pCO2 Stress Elicit Divergent Transcriptomic Responses in a Resilient Coral (2016, background): “…has previously been proposed as a mechanism for coral calcification (Cohen and McConnaughey, 2003), with microelectrode (Ries, 2011), boron isotope (McCulloch et al., 2012), antibody immunolabeling (Barott et al., 2015), and pHsensitive dye studies (Venn et al., 2013) demonstrating that corals are…”
Mangrove and Seagrass Beds Provide Different Biogeochemical Services for Corals Threatened by Climate Change (2016, background): “556 Collectively however our results suggest that photosynthesis and calcification were most likely 557 impaired by the metabolic costs of maintaining cellular homeostasis within a low pH 558 environment (Anthony et al., 2008; McCulloch et al., 2012).”