Effects of pH on coastal marine phytoplankton

By K. Hinga. 2002

329 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/5a03dce9f82c73ac09f1dba222b888c5add0d415

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Citations in the corpus

The biological pump in a high CO 2 world (2012, background): “Inorganic carbon speciation and availability Culture experiments have revealed that many phytoplankton species grow well over a large range of pH (Hinga 2002, Berge et al. 2010, Liu et al. 2010, Joint et al. 2011) especially when the pH change was caused by TA perturbations.”
On the presence of Pseudo-nitzschia calliantha Lundholm, Moestrup et Hasle and Pseudo-nitzschia delicatissima (Cleve) Heiden in the Southern Adriatic Sea (Mediterranean Sea, Italy) (2005, background): “It must be acknowledged that irradiance (Fehling et al., 2005) and pH (Hinga, 2002; Lundholm et al., 2004) could significantly affect the population dynamics, but these data were not taken.”
Future high CO2 in the intertidal may compromise adult barnacle Semibalanus balanoides survival and embryonic development rate. (2009, background): “Coastal shelf seas experience a greater range of pH than open oceans due to terrestrial influences such as river run-off and nutrient enrichment as well as large temperature and salinity fluctuations (Hinga 2002, Blackford & Gilbert 2007).”
Ocean Acidification and Its Potential Effects on Marine Ecosystems (2008, background): “In a review of coastal marine phytoplankton, Hinga (2002) found that while some species grow well at a wide range of pH, others have growth rates that vary greatly over a 0.5 to 1.0 pH unit change.”
Responses of marine benthic microalgae to elevated CO2 (2011, unknown): “Several diatom species are relatively insensitive to changes in pH (Hinga 2002), and some oceanic diatoms show little response over a large CO 2 range (Tortell et al. 1997; Burkhardt et al. 2001), although other experiments haveshownpositiveresponsesofdiatoms toCO 2 enrichment (Riebesell et al.…”
Ocean acidification and seaweed reproduction: increased CO2 ameliorates the negative effect of lowered pH on meiospore germination in the giant kelp Macrocystis pyrifera (Laminariales, Phaeophyceae) (2012, background): “Furthermore, OA can potentially affect all marine primary producers (phytoplankton and seaweeds, e.g., Hinga, 2002; Hurd et al., 2009, 2011; Cornwall et al., 2011; Hepburn et al., 2011) because their growth and productivity are dependent on the supply of inorganic carbon for photosynthesis…”
The effect of pCO2 on carbon acquisition and intracellular assimilation in four marine diatoms (2009, background): “occurrence in coastal areas that display regular and large changes in CO2 levels (Hansen, 2002; Hinga, 2002) as well as highly variable light conditions (MacIntyre et al.”
A developmental and energetic basis linking larval oyster shell formation to acidification sensitivity (2013, background): “In coastal environments, carbonate chemistry may vary widely both spatially and temporally [Hinga, 2002; Hofmann et al., 2011; Waldbusser et al., 2011] and can result in transient conditions (in excess of global averages) that are unfavorable for sensitive species [Gruber et al., 2012; Hauri et…”
Death by dissolution: Sediment saturation state as a mortality factor for juvenile bivalves (2009, background): “These coastal habitats and their calcifying organisms are already subject to highly variable pH (Hinga 1992, 2002; Blackford and Gilbert 2007), and additional lowering of pH may result in substantial ecological and economic effects.”
Effect of pH on growth and domoic acid production by potentially toxic diatoms of the genera Pseudo-nitzschia and Nitzschia (2004, background): “These results support previous findings of pH as a limiting factor for growth of other microalgae grown in 7 Mar Ecol Prog Ser 273: 1–15, 2004 nutrient-rich media such as f/2 growth medium (e.g. Schmidt & Hansen 2001, Hansen 2002, Hinga 2002).”
CO2-induced seawater acidification affects physiological performance of the marine diatom Phaeodactylum tricornutum (2010, background): “Responses of phytoplankton to reduced pH in a high CO2 ocean are likely to be speciesspecific, with potential ‘winners’ and “losers” (Hinga, 2002).”
Size-dependent pH effect on calcification in post-larval hard clam Mercenaria spp. (2010, background): “…processes that induce pH variability in coastal ecosystems (Soetaert et al. 2007) including daily production– respiration and seasonal bloom cycles (Hinga 2002, Wootton et al. 2008), hydrology and coastal upwelling (Feely et al. 2008, Salisbury et al. 2008, 2009), changes in other atmospheric…”
Harmful algal blooms and climate change: Learning from the past and present to forecast the future (2015, background): “…organisms (e.g., Bednarsek et al., 2014; Orr et al., 2005), the pH dependent changes in the marine carbonate system also have broad implications for carbon acquisition for both marine phytoplankton (e.g., Beardall et al., 2009; Hansen, 2002; Hinga, 2002) and microbes (e.g., Hutchins et al., 2009).”