Long-term effects of nutrient and CO2 enrichment on the temperate coral Astrangia poculata (Ellis and Solander, 1786)

By M. Holcomb, D. McCorkle, A. Cohen. 2010

168 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/e450de8d5147023d09ca4e0ee5b1f3cc3a84ce61

How researchers see this paper

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

In Ecology

1. J. Ries
2. Peter J. Edmunds
3. A. Cohen
4. D. McCorkle
5. R. Thresher
6. B. Tilbrook
7. J. Adkins
8. N. Wilson

In Oceanography

1. J. Ries
2. Peter J. Edmunds
3. A. Cohen
4. D. McCorkle
5. B. Tilbrook
6. R. Thresher
7. N. Wilson
8. J. Adkins

Citations in the corpus

• The influence of food supply on the response of Olympia oyster larvae to ocean acidification (2013, background): “However, few tests have been performed to determine whether improved 5 or impaired nutrition can ameliorate or exacerbate the negative effects of ocean acidification (but see Holcomb et al., 2010, 2012; Melzner et al., 2011; Thomsen et al., 2013; Comeau et al., 2013).”
• Is the response of coral calcification to seawater acidification related to nutrient loading? (2011, background): “Some of them suggest that nutrient-enriched corals may be less sensitive to acidification (Atkinson et al. 1995; Langdon and Atkinson 2005; Holcomb et al. 2010) or vice versa that dissolved inorganic carbon (DIC) addition to seawater could mitigate the detrimental effect of nutrient enrichment (Maru”
• Effects of chronic low carbonate saturation levels on the distribution, growth and skeletal chemistry of deep-sea corals and other seamount megabenthos (2011, result): “These data suggest a threshold carbonate level below which the isidids could no longer sustain ‘normal’ skeletal structure, composition and growth rate, which is consistent with laboratory evidence of a non-linear response by corals to ocean acidification (Holcomb et al. 2010, Ries et al. 2010).”
• Zooplanktivory ameliorates the effects of ocean acidification on the reef coral Porites spp (2011, background): “This concentration was not intended to be ecologically relevant (Jacobson and Edmunds 2010); rather, it was designed to provide ad libitum access to zooplankton in order to explore the potential of food to affect the response to OA.”
• A physicochemical framework for interpreting the biological calcification response to CO 2 -induced ocean acidification (2011, background): “Yet Holcomb et al. (2010) also showed that calcification rates of A. poculata are unimpaired by this increase in atmospheric pCO2 when reared under nutrientenriched conditions.”
• A nonlinear calcification response to CO2-induced ocean acidification by the coral Oculina arbuscula (2010, background): “…have shown that some tropical (Reynaud et al. 2003; Cohen et al. 2009; Jury et al. 2009) as well as temperate species (RodolfoMetalpa et al. 2010; Holcomb et al. 2010) of scleractinian corals exhibit either no response and/or a nonlinear response to CO2-induced reductions in seawater [CO3 2-].”
• Biological mechanisms supporting adaptation to ocean acidification in coastal ecosystems (2015, unknown): “trations are elevated (Atkinson et al., 1995; Holcomb et al., 2010), and nutrient addition can reduce the effect of declining aragonite”
• The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals (2011, background): “…under nutrient-replete conditions were significantly less sensitive to decreased Xar than corals reared under ambient nutrient conditions, and Holcomb et al. (2010) found that calcification by nutrient-replete corals reared under 780 ppm CO2 was not statistically different from calcification…”