Climate change: a catalyst for global expansion of harmful cyanobacterial blooms.

By Hans W. Paerl, J. Huisman. Environmental Microbiology Reports, 2009

1,558 citations recorded by the source corpus.

Subfields: Ecology, Environmental Chemistry, Oceanography

View Paper: https://www.semanticscholar.org/paper/2cb99453396e685c7d1a2a2305838266a74f1bd9

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Citations in the corpus

Understanding cyanobacteria‐zooplankton interactions in a more eutrophic world (2014, background): “Few doubt that global changes will lead to intensified cyanobacterial dominance of aquatic systems (Paerl & Huisman, 2009).”
Deciphering the effects of nitrogen, phosphorus, and temperature on cyanobacterial bloom intensification, diversity, and toxicity in western Lake Erie (2019, background): “Given that temperatures are expected to rise through this century regardless of global carbon measures (Edenhofer et al. 2014), restrictions to nutrient loads will be needed to mitigate cyanobacteria proliferation (Conley et al. 2009; Paerl and Huisman 2009; Michalak et al. 2013).”
Estimating the abundance of toxic Microcystis in the San Francisco Estuary using quantitative real-time PCR (2010, background): “Furthermore, the role of climate change has been suggested as a potent catalyst for the further expansion of cyanobacterial blooms in eutrophic waters on a global scale (Paerl and Huisman, 2009).”
Sustainability and cyanobacteria (blue-green algae): facts and challenges (2011, background): “In the last 20 years, excessive nutrient inputs from agricultural fertiliser run off, and/or domestic and industrial effluents, as well as climatic change have greatly enhanced the incidence of cyanobacterial blooms globally (Paerl and Huisman 2009).”
Invited Review - Fight on Plankton! or, Phytoplankton Shape and Size as Adaptive Tools to Get Ahead in the Struggle for Life (2011, background): “Although a few data are still available, some evidences exist that climate change can promote pseudo-eutrophication events (see Paerl & Huisman, 2009; Nõges et al., 2010) and, by altering the hydraulic balance in shallow lakes, cause a shift between a clear macrophyte-dominated state and a turbid…”
The effects of changing climate on microzooplankton grazing and community structure: drivers, predictions and knowledge gaps (2013, background): “…temperatures have been strongly implicated in the increased frequency of the dominance of cyanobacterial species in freshwater (Paerl and Huisman, 2008; Paerl and Huisman, 2009; Paerl and Paul, 2011), but stimulation of certain marine cyanobacterial taxa has also been reported (Fu et al., 2007).”
Effects of rising CO₂ on the harmful cyanobacterium Microcystis (2016, background): “…freshwater cyanobacteria like Microcystis will benefit from elevated CO 2 concentrations and rising temperatures, and also from increasing N and P loads associated with climate change (Davis et al. , 2009; Paerl and Huisman, 2009; O’Neil et al. , 2012; Verspagen et al. , 2014b; Chapter 7 ).”
Climate change: links to global expansion of harmful cyanobacteria. (2012, background): “Figure adapted from (west Asia), Patos Lagoon Estuary (Brazil), the Oued Mellah reservoir (Morocco), the Swan River Estuary (Australia), San Francisco Bay (California, USA), Lake Ponchartrain (Louisiana, USA), and the Kucukcekmece Lagoon (Turkey) (Paerl and Huisman, 2009; Akcaalan et al., 2009).”
Comparison of cyanobacterial and green algal growth rates at different temperatures (2013, background): “E-mail: miquel.lurling@wur.nl Freshwater Biology (2013) 58, 552–559 doi:10.1111/j.1365-2427.2012.02866.x 552 2012 Blackwell Publishing Ltd 2006; Paerl, 2008; Paerl & Huisman, 2008, 2009).”
Use of flow management to mitigate cyanobacterial blooms in the Lower Darling River, Australia (2011, background): “Global climate change is expected to increase the incidence of blooms worldwide (Viney et al., 2007; Paerl and Huisman, 2009) and water availability for environmental management purposes is likely to become scarcer.”
Linking traits to species diversity and community structure in phytoplankton (2010, background): “Marine HAB species were selected from Sunda et al. (2006), and freshwater HAB species from Paerl & Huisman (2009) from the size of the phytoplankton species.”
Phytoplankton community composition can be predicted best in terms of morphological groups (2011, background): “The best explained groups corresponded to Cyanobacteria and included: filamentous non–N-fixing groups (S1: R2 5 0.47, p , 0.001, df 5 71; and S2: R2 5 0.53, p , 0.001, df 5 71), filamentous N-fixing groups (H1: R2 5 0.67, p , 0.001, df 5 71), colonial large-celled groups (M: R2 5 0.41, p , 0.01, df ”
Phytoplankton blooms in estuarine and coastal waters: Seasonal patterns and key species (2015, background): “, 2011) when dissolved inorganic nitrogen is depleted from the surface layer and temperatures are high (Paerl and Huisman, 2009).”