Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms

By J. Orr, V. Fabry, O. Aumont, L. Bopp, S. Doney, R. Feely, A. Gnanadesikan, N. Gruber, A. Ishida, F. Joos and 17 more. Nature, 2005

4,765 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/37126de1bbf70ba0349d8b72af8bb9357c3b12cf

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

In Global and Planetary Change

In Oceanography

Citations in the corpus

Calcifying coral abundance near low-pH springs: implications for future ocean acidification (2012, background): “Atmospheric CO2 is currently on the rise, and its equilibration with surface seawater is expected to reduce the pH of the surface oceans by approximately 0.4 pH units by year 2100 (Caldeira and Wickett 2005; Orr et al. 2005; Doney et al. 2009).”
Potential impacts of future ocean acidification on marine ecosystems and fisheries: current knowledge and recommendations for future research (2011, background): “by the end of this century, depending on the selected CO2 emission scenario (Orr et al., 2005; Meehl et al., 2007).”
Effects of ocean acidification on hatch size and larval growth of walleye pollock (Theragra chalcogramma) (2013, background): “due to the release of terrestrially sequestered CO2 into the atmosphere and the subsequent diffusion of approximately one-third of that anthropogenically released CO2 into the ocean (Feely et al., 2004; Sabine et al., 2004; Orr et al., 2005).”
Multi-model ensemble projections of climate change effects on global marine biodiversity (2015, background): “…environment (Portner, 2001), there is increasing concern for species’ ability to survive long-term changes in the mean climatic conditions, as well as increased climatic variability, acidification, and expansion of oxygen minimum zones (Orr et al., 2005; Fabry et al., 2008; Cheung et al., 2011).”
Resolving the effect of climate change on fish populations (2009, background): “Several authors have stated that marine fish are likely to be less affected by an increase in oceanic CO2 and a corresponding decrease in pH compared with invertebrate groups, such as molluscs and corals (Feely et al., 2004; Orr et al., 2005; Fabry et al., 2008).”
The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals (2011, background): “Rising concentrations of atmospheric carbon dioxide (CO2) are lowering the carbonate concentration ([CO3 2-]), pH, and aragonite saturation state (Xar) of the surface ocean (Orr et al. 2005; Bates 2007).”
Interannual variability in Antarctic krill (Euphausia superba) density at South Georgia, Southern Ocean: 1997–2013 (2014, background): “This habitat is undergoing rapid environmental change such as loss of sea ice (Stammerjohn et al., 2008), increasing sea temperatures (Turner et al., 2005; Whitehouse et al., 2008) and ocean acidification (Orr et al., 2005); with recent changes and impacts summarized by Flores et al. (2012).”
Comparing the effect of elevated pCO2 and temperature on the fertilization and early development of two species of oysters (2010, background): “For a description of seawater chemistry, refer to Feely et al. (2004) and Orr et al. (2005).”
Long-term climate-associated dynamics of a tropical seagrass meadow: implications for the future (2011, background): “…resulting in habitat degradation, species loss and range changes caused by increases in temperature (McCarty 2001, Poloczanska et al. 2007), storm frequency and intensity (Harley et al. 2006, Crabbe et al. 2008) and acidification of aquatic environments (Kleypas et al. 1999, Orr et al. 2005).”
Regulation of atmospheric CO2 by deep‐sea sediments in an Earth system model (2007, background): “…the continued dissolution of fossil fuel CO2 in the surface waters of the ocean and associated decrease in ambient carbonate ion concentration [Orr et al., 2005] and pH (termed ocean ‘‘acidification’’ [Caldeira andWickett, 2003]) may adversely affect the ability of calcifying plankton such as…”