The potential effects of global climate change on microalgal photosynthesis, growth and ecology

By John Beardall, J. Raven. 2004

349 citations recorded by the source corpus.

Subfields: Oceanography, Renewable Energy, Sustainability and the Environment

View Paper: https://www.semanticscholar.org/paper/d3e29ae1b8c6e391178d2c11135d476690ae4eda

How researchers see this paper

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

In Oceanography

1. D. Hutchins
2. J. Raven
3. Raphael M. Kudela
4. Feixue Fu
5. W. Cochlan
6. Mark E. Warner
7. Z. Finkel
8. Yuanyuan Feng

In Renewable Energy, Sustainability and the Environment

1. J. Raven
2. Z. Finkel
3. D. Thornton
4. John Beardall
5. G. Hallegraeff
6. V. Fabry
7. J. Guinotte
8. M. Giordano

Citations in the corpus

• Effect of UV stress on the fatty acid and lipid class composition in two marine microalgae Pavlova lutheri (Pavlovophyceae) and Odontella aurita (Bacillariophyceae) (2010, background): “UVA-R (315–400 nm) and UVB-R (280–315 nm) induce genetically and physiologically deleterious effects on many life forms of terrestrial and aquatic ecosystems (Hessen et al. 1997; Beardall and Raven 2004; Holzinger and Lütz 2006).”
• Responses of marine benthic microalgae to elevated CO2 (2011, neutral): “…it is thought that rising CO 2 will benefit different species to varying degrees (Hein and Sand-Jensen 1997; Tortell et al. 2000; Rost et al. 2003; Beardall and Raven 2004; Riebesell 2004; Fu et al. 2008b) and may result in dramatic community shifts with profound consequences for marine…”
• Ocean Acidification and Its Potential Effects on Marine Ecosystems (2008, background): “…rates when grown under high pCO2 conditions equivalent to ca. 760 micro atmosphere (µatm) (Tortell et al. 1997; Hein & Sand-Jensen 1997; Burkhardt et al. 2001; Tortell and Morel 2002; Rost et al. 2003; Beardall & Raven 2004; Schippers et al. 2004; Giordano et al. 2005; Martin & Tortell 2006).”
• The C:N:P stoichiometry of organisms and ecosystems in a changing world: A review and perspectives (2012, background): “The environmental impact of elevated [CO2] levels can act in parallel to other factors that promote global change (e.g., warming, UV-B radiation, eutrophication), which can affect C and N cycling in ecosystems in several ways (Beardall and Raven, 2004; Kuijper et al., 2005).”
• The future of seaweed aquaculture in a rapidly changing world (2017, background): “The impacts of global change on microalgae have been dealt with extensively elsewhere (Beardall & Raven, 2004; Beardall et al., 2009, 2014; Gao et al., 2012; Johnson et al., 2013), so here we concentrate on the impacts on seaweeds, especially those of potential importance for the aquaculture…”
• Dissolved organic matter (DOM) release by phytoplankton in the contemporary and future ocean (2014, background): “Consequently, photosynthesis may not be significantly stimulated under ocean acidification conditions (Beardall & Raven, 2004; Royal Society, 2005) and there may be shifts in phytoplankton community structure as the ocean acidifies based on the competitive costs and benefits of different inorganic…”
• Reviews and syntheses: Calculating the global contribution of coralline algae to total carbon burial (2015, background): “Significantly, around 50 % of the global primary production (which uses pCO2) is by marine organisms (Beardall and Raven, 2004) with marine microalgae and bacteria being the dominant source of primary production and respiration (Duarte and Cebrian, 1996; del Giorgio and Duarte, 2002; Duarte et…”
• Effects of pre‐processing of Raman spectra on in vivo classification of nutrient status of microalgal cells (2006, background): “Microalgae are involved in 50% of planetary C fixation (65 billion tonnes year ), and are hence of major ecological importance [1].”
• CO2 concentrating mechanisms in algae: mechanisms, environmental modulation, and evolution. (2005, background): “CAM: crassulacean acid metabolism ating in what is essentially, in geological terms at least (20), a low-CO2 environment.”
• Biogenically driven organic contribution to marine aerosol (2004, background): “Given that the evolution of micro-algae is driven by environmental change, particularly increasing oceanic temperature”
• EFFECTS OF INCREASED TEMPERATURE AND CO2 ON PHOTOSYNTHESIS, GROWTH, AND ELEMENTAL RATIOS IN MARINE SYNECHOCOCCUS AND PROCHLOROCOCCUS (CYANOBACTERIA) 1 (2007, background): “Increasing temperature will increase the substratesaturated reaction rate of RUBISCO and thus the potential growth rates of phytoplankton, if growth is not limited by inorganic carbon or other factors (Beardall and Raven 2004).”
• The microbial aspect of climate change (2016, background): “complex interactions between climate change and other environmental factors (Beardall and Raven 2004).”
• OCEAN CLIMATE CHANGE, PHYTOPLANKTON COMMUNITY RESPONSES, AND HARMFUL ALGAL BLOOMS: A FORMIDABLE PREDICTIVE CHALLENGE 1 (2010, background): “However, photosynthetic performance in diatom species such as Skeletonema, for which photosynthesis is already CO2 saturated, will remain constant (Beardall and Raven 2004).”