Species-specific consequences of ocean acidification for the calcareous tropical green algae Halimeda
By N. Price, S. Hamilton, Jesse S. Tootell, J. Smith. 2011
110 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/a447ccf39b461ee1753b4d949a7a840286eab2ec
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In Ecology
- Peter J. Edmunds
- P. Mcelhany
- D. Shallin Busch
- R. Carpenter
- S. Comeau
- N. B. Spindel
- L. Hofmann
- K. Bischof
In Oceanography
- Peter J. Edmunds
- P. Mcelhany
- D. Shallin Busch
- L. Hofmann
- R. Carpenter
- K. Bischof
- S. Comeau
- N. B. Spindel
Citations in the corpus
- Appropriate pCO2 treatments in ocean acidification experiments (2013, background): “Due to practical limitations, all of the OA exposure experiments published in 2011 were conducted with constant pCO2 conditions, though several noted the need for dynamic manipulations (e.g., Price et al. 2011; Yu et al. 2011).”
- Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, background): “01) and growth of calcified segments (Price et al., 2011).”
- Ocean acidification effects on calcifying macroalgae (2014, background): “Furthermore, Price et al. (2011) found no pCO2 effect on the amount of CaCO3 in H. opuntia skeletons.”
- EFFECTS OF CLIMATE CHANGE ON GLOBAL SEAWEED COMMUNITIES (2012, background): “As these abiotic trends are thoroughly reviewed elsewhere (e.g., Feely et al. 2004, IPCC 2007, Rabalais et al. 2009, Wang et al. 2010, Zacharioudaki et al. 2011), we pause here only to highlight two salient features of this suite of anthropogenically forced environmental change.”
- Ocean acidification and marine microorganisms : responses and consequences (2015, background): “These variations in response of marine photosynthetic microbial community towards elevated pCO2 confirm that response towards OA is species specific (Price et al., 2011).”
- High-Frequency Dynamics of Ocean pH: A Multi-Ecosystem Comparison (2011, background): “Along with the calcification biology of the dominant scleractinian corals and coralline algae, the biodiversity on coral reefs includes many other calcifying species that will likely be affected [74–77].”
- The responses of eight coral reef calcifiers to increasing partial pressure of CO2 do not exhibit a tipping point (2013, background): “2011), or species-specific responses (Price et al. 2011).”