Living in the now: physiological mechanisms to tolerate a rapidly changing environment.

By Gretchen E. Hofmann, A. Todgham. Annual Review of Physiology, 2010

628 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/79774287783faf49d63b434022eecb15bea1926a

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Citations in the corpus

The physiological and molecular responses of larvae from the reef-building coral Pocillopora damicornis exposed to near-future increases in temperature and pCO2 (2012, background): “Increased temperature has well-documented negative impacts on organismal physiology, specifically above organisms’ thermal optima (Hofmann and Todgham 2010).”
High-Frequency Dynamics of Ocean pH: A Multi-Ecosystem Comparison (2011, background): “Instead, such a range of variation may mean that the organisms resident in tidal, estuarine, and upwelling regions are already operating at the limits of their physiological tolerances (a la the classic tolerance windows of Fox – see [68]).”
Vulnerability to climate warming and acclimation capacity of tropical and temperate coastal organisms (2016, background): “…(Angilletta, 2009) and accordingly can: (a) disperse to more hospitable habitats, (b) tolerate the new conditions through phenotypic and physiological plasticity, or (c) adapt to the new environment through genetic change via the process of evolution (see review by Hoffmann and Todgham, 2010).”
Differential plasticity of metabolic rate phenotypes in a tropical fish facing environmental change (2016, background): “…environ- mental change; Price, Qvarnstr€om & Irwin 2003; Proulx & Phillips 2005) among members of the population (Brad- shaw & Holzapfel 2006; Visser 2008; Hofmann & Todg- ham 2010), research on interindividual variation provides a valuable yet under-exploited avenue for investigating potential…”
Ocean acidification does not affect the early life history development of a tropical marine fish. (2011, background): “Determining which marine species are sensitive to elevated CO2 and reduced pH, and which species can tolerate these changes, is critical for assessing the impacts of ocean acidification on marine biodiversity and ecosystem function (Fabry et al. 2008, Melzner et al. 2009, Hofman & Todgham 2010).”
Interactive effects of ocean acidification and temperature on two scleractinian corals from Moorea, French Polynesia (2012, background): “…relationship with pH (Hoegh-Guldberg et al., 2007; Erez et al., 2011), it can also function as an important biological property (sensu Pistevos et al., 2011) of use in furthering the objective of elucidating the genetic basis of organism vulnerability to climate change (Hofmann & Todgham, 2010).”
Offspring sensitivity to ocean acidification changes seasonally in a coastal marine fish (2014, background): “One such factor is the spatio temporal CO2 and pH variability in marine habitats (Hendriks et al. 2010, Hofmann & Todgham 2010, Hofmann et al. 2011, McElhany & Busch 2012) that appears critical for 2 reasons.”
Interactions between climate and habitat loss effects on biodiversity: a systematic review and meta‐analysis (2012, background): “For example, it has been well documented that species can change physiologically and morphologically to adapt to their environment (e.g. Davis & Shaw, 2001; Losos & Ricklefs, 2009; Berg et al., 2010; Hofmann & Todgham, 2010; Hill et al., 2011).”
A laboratory‐based, experimental system for the study of ocean acidification effects on marine invertebrate larvae (2010, background): “…these manipulative experiments is clear: they begin to reveal the current physiological plasticity possessed by marine organisms, which may allow them to tolerate and/or compensate for the altered seawater chemistry (e.g., Fabry et al. 2008; Widdicombe and Spicer 2008; Hofmann and Todgham 2010).”
Chemical and biological impacts of ocean acidification along the west coast of North America (2015, background): “Organisms that produce calcium carbonate (CaCO3) shells or skeletons made of aragonite or calcite are expected to encounter increasing physiological challenges as the saturation state of aragonite and calcite decreases due to OA (Fabry et al., 2008; Guinotte and Fabry, 2008; Hofmann and Todgham, 201”