The rise of harmful cyanobacteria blooms: The potential roles of eutrophication and climate change

Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal blooms in freshwater, estuarine, and marine ecosystems. Recent research suggests that eutrophication and climate change are two processes that may promote the proliferation and expansion of cyanobacterial harmful a...

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Published in	Harmful algae Vol. 14; pp. 313 - 334
Main Authors	O’Neil, J.M., Davis, T.W., Burford, M.A., Gobler, C.J.
Format	Journal Article
Language	English
Published	Elsevier B.V 01.02.2012
Subjects	algal blooms Anabaena Aphanizomenon carbon dioxide Climate change Cyanobacteria CyanoHABs Cylindrospermopsis ecosystems Eutrophication freshwater Harmful algae blooms Lyngbya Microcystis nitrogen Nodularia phytoplankton Synechococcus temperature Toxins Trichodesmium CyanoHABs Climate change Toxins Harmful algae blooms Cyanobacteria Eutrophication
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Abstract	Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal blooms in freshwater, estuarine, and marine ecosystems. Recent research suggests that eutrophication and climate change are two processes that may promote the proliferation and expansion of cyanobacterial harmful algal blooms. In this review, we specifically examine the relationships between eutrophication, climate change and representative cyanobacterial genera from freshwater ( Microcystis, Anabaena, Cylindrospermopsis), estuarine ( Nodularia, Aphanizomenon), and marine ecosystems ( Lyngbya, Synechococcus, Trichodesmium). Commonalities among cyanobacterial genera include being highly competitive for low concentrations of inorganic P (DIP) and the ability to acquire organic P compounds. Both diazotrophic (= nitrogen (N 2) fixers) and non-diazotrophic cyanobacteria display great flexibility in the N sources they exploit to form blooms. Hence, while some cyanobacterial blooms are associated with eutrophication, several form blooms when concentrations of inorganic N and P are low. Cyanobacteria dominate phytoplankton assemblages under higher temperatures due to both physiological (e.g. more rapid growth) and physical factors (e.g. enhanced stratification), with individual species showing different temperature optima. Significantly less is known regarding how increasing carbon dioxide (CO 2) concentrations will affect cyanobacteria, although some evidence suggests several genera of cyanobacteria are well-suited to bloom under low concentrations of CO 2. While the interactive effects of future eutrophication and climate change on harmful cyanobacterial blooms are complex, much of the current knowledge suggests these processes are likely to enhance the magnitude and frequency of these events.
AbstractList	Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal blooms in freshwater, estuarine, and marine ecosystems. Recent research suggests that eutrophication and climate change are two processes that may promote the proliferation and expansion of cyanobacterial harmful algal blooms. In this review, we specifically examine the relationships between eutrophication, climate change and representative cyanobacterial genera from freshwater ( Microcystis, Anabaena, Cylindrospermopsis), estuarine ( Nodularia, Aphanizomenon), and marine ecosystems ( Lyngbya, Synechococcus, Trichodesmium). Commonalities among cyanobacterial genera include being highly competitive for low concentrations of inorganic P (DIP) and the ability to acquire organic P compounds. Both diazotrophic (= nitrogen (N 2) fixers) and non-diazotrophic cyanobacteria display great flexibility in the N sources they exploit to form blooms. Hence, while some cyanobacterial blooms are associated with eutrophication, several form blooms when concentrations of inorganic N and P are low. Cyanobacteria dominate phytoplankton assemblages under higher temperatures due to both physiological (e.g. more rapid growth) and physical factors (e.g. enhanced stratification), with individual species showing different temperature optima. Significantly less is known regarding how increasing carbon dioxide (CO 2) concentrations will affect cyanobacteria, although some evidence suggests several genera of cyanobacteria are well-suited to bloom under low concentrations of CO 2. While the interactive effects of future eutrophication and climate change on harmful cyanobacterial blooms are complex, much of the current knowledge suggests these processes are likely to enhance the magnitude and frequency of these events. Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal blooms in freshwater, estuarine, and marine ecosystems. Recent research suggests that eutrophication and climate change are two processes that may promote the proliferation and expansion of cyanobacterial harmful algal blooms. In this review, we specifically examine the relationships between eutrophication, climate change and representative cyanobacterial genera from freshwater (Microcystis, Anabaena, Cylindrospermopsis), estuarine (Nodularia, Aphanizomenon), and marine ecosystems (Lyngbya, Synechococcus, Trichodesmium). Commonalities among cyanobacterial genera include being highly competitive for low concentrations of inorganic P (DIP) and the ability to acquire organic P compounds. Both diazotrophic (= nitrogen (N2) fixers) and non-diazotrophic cyanobacteria display great flexibility in the N sources they exploit to form blooms. Hence, while some cyanobacterial blooms are associated with eutrophication, several form blooms when concentrations of inorganic N and P are low. Cyanobacteria dominate phytoplankton assemblages under higher temperatures due to both physiological (e.g. more rapid growth) and physical factors (e.g. enhanced stratification), with individual species showing different temperature optima. Significantly less is known regarding how increasing carbon dioxide (CO2) concentrations will affect cyanobacteria, although some evidence suggests several genera of cyanobacteria are well-suited to bloom under low concentrations of CO2. While the interactive effects of future eutrophication and climate change on harmful cyanobacterial blooms are complex, much of the current knowledge suggests these processes are likely to enhance the magnitude and frequency of these events. Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal blooms in freshwater, estuarine, and marine ecosystems. Recent research suggests that eutrophication and climate change are two processes that may promote the proliferation and expansion of cyanobacterial harmful algal blooms. In this review, we specifically examine the relationships between eutrophication, climate change and representative cyanobacterial genera from freshwater (Microcystis, Anabaena, Cylindrospermopsis), estuarine (Nodularia, Aphanizomenon), and marine ecosystems (Lyngbya, Synechococcus, Trichodesmium). Commonalities among cyanobacterial genera include being highly competitive for low concentrations of inorganic P (DIP) and the ability to acquire organic P compounds. Both diazotrophic (= nitrogen (N₂) fixers) and non-diazotrophic cyanobacteria display great flexibility in the N sources they exploit to form blooms. Hence, while some cyanobacterial blooms are associated with eutrophication, several form blooms when concentrations of inorganic N and P are low. Cyanobacteria dominate phytoplankton assemblages under higher temperatures due to both physiological (e.g. more rapid growth) and physical factors (e.g. enhanced stratification), with individual species showing different temperature optima. Significantly less is known regarding how increasing carbon dioxide (CO₂) concentrations will affect cyanobacteria, although some evidence suggests several genera of cyanobacteria are well-suited to bloom under low concentrations of CO₂. While the interactive effects of future eutrophication and climate change on harmful cyanobacterial blooms are complex, much of the current knowledge suggests these processes are likely to enhance the magnitude and frequency of these events.
Author	O’Neil, J.M. Burford, M.A. Gobler, C.J. Davis, T.W.
Author_xml	– sequence: 1 givenname: J.M. surname: O’Neil fullname: O’Neil, J.M. email: joneil@hpl.umces.edu organization: University of Maryland, Center for Environmental Science, Horn Point Laboratory, Cambridge, MD 21613, USA – sequence: 2 givenname: T.W. surname: Davis fullname: Davis, T.W. organization: Griffith University, Australian Rivers Institute, Nathan, QLD 4111, Australia – sequence: 3 givenname: M.A. surname: Burford fullname: Burford, M.A. organization: Griffith University, Australian Rivers Institute, Nathan, QLD 4111, Australia – sequence: 4 givenname: C.J. surname: Gobler fullname: Gobler, C.J. organization: Stony Brook University, School of Marine and Atmospheric Science, Stony Brook, NY, USA
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Keywords	CyanoHABs Climate change Toxins Harmful algae blooms Cyanobacteria Eutrophication
Language	English
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PublicationDate	2012-02-01
PublicationDateYYYYMMDD	2012-02-01
PublicationDate_xml	– month: 02 year: 2012 text: 2012-02-01 day: 01
PublicationDecade	2010
PublicationTitle	Harmful algae
PublicationYear	2012
Publisher	Elsevier B.V
Publisher_xml	– name: Elsevier B.V
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Snippet	Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal blooms in freshwater, estuarine, and marine ecosystems. Recent research...
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SubjectTerms	algal blooms Anabaena Aphanizomenon carbon dioxide Climate change Cyanobacteria CyanoHABs Cylindrospermopsis ecosystems Eutrophication freshwater Harmful algae blooms Lyngbya Microcystis nitrogen Nodularia phytoplankton Synechococcus temperature Toxins Trichodesmium
Title	The rise of harmful cyanobacteria blooms: The potential roles of eutrophication and climate change
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