Evidence for Upwelling of Corrosive "Acidified" Water onto the Continental Shelf

By R. Feely, C. Sabine, J. M. Hernández-Ayón, D. Ianson, B. Hales. Science, 2008

1,525 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/8ccd59fb833343008a966ae061872687c2ca1bd5

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Citations in the corpus

Larvae of the pteropod Cavolinia inflexa exposed to aragonite undersaturation are viable but shell-less (2010, background): “However, Cavolinia sp. can already face seasonal undersaturation with respect to aragonite in some temperate areas, such as the California upwelling zone, and such corrosive areas are extending as a result of ocean acidiWcation (Feely et al. 2008).”
Local adaptation in marine invertebrates. (2011, background): “…from population I. Note that the persistence of each population depends not just on the range of tolerance phenotypes in the species as a whole but also on the distribution of those phenotypes among and within populations. associated with centers of upwelling (Feely et al. 2008, Hauri et al. 2009).”
Chemical and biological impacts of ocean acidification along the west coast of North America (2015, methodology): “The uptake of Canth has caused the aragonite saturation horizon to shoal by approximately 30e50 m since the preindustrial period so that undersaturated waters are well within the regions of the continental shelf that affect the shell dissolution of living pteropods (Feely et al., 2008).”
Nutrition and income from molluscs today imply vulnerability to ocean acidification tomorrow (2012, background): “…Pacific oysters (Crassostrea gigas, Ostreidae) in coastal seawater have experienced mass larval mortality 2011 Blackwell Publishing Ltd, F I S H and F I S H E R I E S , 13, 182–215 199 during periodic upwelling events that accelerate ocean acidification’s effects (Feely et al. 2008).”
High-Frequency Dynamics of Ocean pH: A Multi-Ecosystem Comparison (2011, background): “Organisms living in upwelling regions may be acclimatized and adapted to extremes in seawater chemistry; here, deep CO2enriched waters reach the surface and may shoal onto the benthos on the continental shelf [31,32].”
Linking the biological impacts of ocean acidification on oysters to changes in ecosystem services: A review (2017, background): “…million, 701 but since 2007, several oyster hatcheries have suffered from mass mortalities of 702 oyster larvae of up to 70-80% due to the upwelling of waters that were acidified, 703 highly saline and rich in V. tubiashii (Barton et al., 2015; Elston et al., 2008; 704 Feely et al., 2008).”
Effects of ocean acidification and high temperatures on the bryozoan Myriapora truncata at natural CO2 vents (2010, background): “Shells can dissolve when exposed to seawater with low carbonate saturation states such as in estuaries (Marshall et al. 2008), in upwelling areas (Feely et al. 2008) and around volcanic CO2 vents (Hall-Spencer et al. 2008).”
Potential impacts of future ocean acidification on marine ecosystems and fisheries: current knowledge and recommendations for future research (2011, positive): “, 2005) or even 850 matm (Feely et al., 2008).”
Reduced pH sea water disrupts chemo-responsive behaviour in an intertidal crustacean (2012, background): “Extreme and localised high-CO2/low pH events could also occur due to leaks from CO2 geological storage sites, proposed as a mitigating strategy for CO2 emissions (Hawkins, 2004; Seibel and Walsh, 2001); and from the periodic upwelling of CO2-enriched sea water in some coastal regions (Feely et al., ”
A laboratory‐based, experimental system for the study of ocean acidification effects on marine invertebrate larvae (2010, methodology): “Our CO2 mixing system delivered gas with a CO2 content ranging from 355-1101 ppm CO2, and has been used to reach higher levels of 1600 ppm CO2, which are consistent with pCO2’s found in upwelled water (Feely et al. 2008).”
Moderate seawater acidification does not elicit long-term metabolic depression in the blue mussel Mytilus edulis (2010, background): “Long-term acclimation of Mytilus edulis from the Western Baltic Sea to elevated seawater pCO2 resulted in an increase in aerobic metabolic rates during moderate hypercapnia, rather than metabolic depression.”
Adaptation and the physiology of ocean acidification (2013, positive): “Low-pH ‘hot spots’ can be caused by upwelling of deeper acidified water onto continental shelves (Feely et al. 2008) and on smaller scales by high levels of localized recurring heterotrophic respiration (Marshall et al. 2008; Wootton, Pfister & Forester 2008).”
Effect of ocean acidification on the early life stages of the blue mussel Mytilus edulis (2010, background): “, 2008), from upwellings (Feely et al., 2008) and due to intense rates of organic matter degradation and/or nitrification (Hof mann et al.”
Impacts of ocean acidification on marine shelled molluscs (2013, background): “Furthermore, in some coastal areas, the episodic or permanent input of low pH water from rivers (Salisbury et al. 2008) and from the upwelling of CO 2 rich waters (Feely et al. 2008; Thomsen et al. 2010) can generate high surface p CO 2 levels.”