Diversity of carbon use strategies in a kelp forest community: implications for a high CO2 ocean

By C. Hepburn, D. Pritchard, C. Cornwall, R. McLeod, John Beardall, John A Raven, C. Hurd. 2011

305 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/6e18056cf3cd2b25b9235d488fb86cfa65693359

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. M. Roleda
2. L. Hofmann
3. K. Bischof
4. F. Fernandes
5. J. Hall‐Spencer
6. E. Serrão
7. F. Arenas
8. J. Assis

In Oceanography

1. K. Bischof
2. M. Roleda
3. L. Hofmann
4. J. Hall‐Spencer
5. E. Serrão
6. F. Arenas
7. C. Ross
8. Andrew J. Davies

Citations in the corpus

• Responses of marine benthic microalgae to elevated CO2 (2011, unknown): “2011; Hepburn et al. 2011).”
• European seaweeds under pressure: Consequences for communities and ecosystem functioning (2015, background): “For example, responses of macroalgae to elevated CO2 seem to be highlymodified by light intensity (Gao et al., 2012b; Hepburn et al., 2011).”
• Competition between calcifying and noncalcifying temperate marine macroalgae under elevated CO2 levels (2012, background): “…communities outside of the Mediterranean, de spite the fact that both crustose and articulated coralline algae co-exist with noncalcifying species in diverse macroalgal communities (Hall-Spencer et al. 2008, Martin et al. 2008, Hepburn et al. 2011, Porzio et al. 2011, Russell et al. 2011).”
• Macroalgal responses to ocean acidification depend on nutrient and light levels (2015, background): “As some primary producers are better able to capitalize on increasing carbon availability than others, this is expected to alter marine communities (Hepburn et al., 2011; Connell et al., 2013; Koch et al., 2013; Gaylord et al., 2015).”
• Seaweed nutrient physiology: application of concepts to aquaculture and bioremediation (2019, background): “Similarly, diffusive uptake of CO2 by seaweeds increases relative to active uptake of HCO3 − in low-light environments, and this, too, is considered a mechanism for reducing energetic costs when light is a limiting factor (Cornwall et al. 2015; Hepburn et al. 2011).”
• 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 (Beardall”
• Climate change and ocean acidification effects on seagrasses and marine macroalgae (2013, methodology): “Hepburn et al. (2011) used d13C values below 30& to indicate HCO3 use in temperate brown macroalgae, and suggested the possible operation of a HCO3 -based CCM.”