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The Response of Antarctic Sea Ice Algae to Changes in pH and CO2
by
Ryan, Ken G.
, McMinn, Andrew
, Müller, Marius N.
, Martin, Andrew
in
Acidification
/ Algae
/ Antarctic Regions
/ Antarctic sea ice
/ Bicarbonate
/ Bicarbonates
/ Biology
/ Brines
/ Carbon
/ Carbon dioxide
/ Carbon Dioxide - pharmacology
/ Carbon dioxide concentration
/ Carbonates
/ Carbonates - analysis
/ Chemistry
/ Chlorophyll - metabolism
/ Earth Sciences
/ Ecosystem assessment
/ Ecosystems
/ Environmental changes
/ Eukaryota - drug effects
/ Eukaryota - growth & development
/ Eukaryota - physiology
/ Growth rate
/ Hydrogen ions
/ Hydrogen-Ion Concentration - drug effects
/ Ice
/ Ice Cover
/ Ice formation
/ Krill
/ Microbial activity
/ Microorganisms
/ Ocean acidification
/ Oceans
/ Overwintering
/ pH effects
/ Photosynthesis
/ Physiology
/ Phytoplankton
/ Plankton
/ Polar environments
/ Primary production
/ Saline water
/ Salinity
/ Salt water
/ Sea ice
/ Sea ice formation
/ Seawater
/ Seeding
/ Studies
/ Surface water
/ Thalassiosira pseudonana
/ Trophic levels
/ Zooplankton
2014
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The Response of Antarctic Sea Ice Algae to Changes in pH and CO2
by
Ryan, Ken G.
, McMinn, Andrew
, Müller, Marius N.
, Martin, Andrew
in
Acidification
/ Algae
/ Antarctic Regions
/ Antarctic sea ice
/ Bicarbonate
/ Bicarbonates
/ Biology
/ Brines
/ Carbon
/ Carbon dioxide
/ Carbon Dioxide - pharmacology
/ Carbon dioxide concentration
/ Carbonates
/ Carbonates - analysis
/ Chemistry
/ Chlorophyll - metabolism
/ Earth Sciences
/ Ecosystem assessment
/ Ecosystems
/ Environmental changes
/ Eukaryota - drug effects
/ Eukaryota - growth & development
/ Eukaryota - physiology
/ Growth rate
/ Hydrogen ions
/ Hydrogen-Ion Concentration - drug effects
/ Ice
/ Ice Cover
/ Ice formation
/ Krill
/ Microbial activity
/ Microorganisms
/ Ocean acidification
/ Oceans
/ Overwintering
/ pH effects
/ Photosynthesis
/ Physiology
/ Phytoplankton
/ Plankton
/ Polar environments
/ Primary production
/ Saline water
/ Salinity
/ Salt water
/ Sea ice
/ Sea ice formation
/ Seawater
/ Seeding
/ Studies
/ Surface water
/ Thalassiosira pseudonana
/ Trophic levels
/ Zooplankton
2014
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Do you wish to request the book?
The Response of Antarctic Sea Ice Algae to Changes in pH and CO2
by
Ryan, Ken G.
, McMinn, Andrew
, Müller, Marius N.
, Martin, Andrew
in
Acidification
/ Algae
/ Antarctic Regions
/ Antarctic sea ice
/ Bicarbonate
/ Bicarbonates
/ Biology
/ Brines
/ Carbon
/ Carbon dioxide
/ Carbon Dioxide - pharmacology
/ Carbon dioxide concentration
/ Carbonates
/ Carbonates - analysis
/ Chemistry
/ Chlorophyll - metabolism
/ Earth Sciences
/ Ecosystem assessment
/ Ecosystems
/ Environmental changes
/ Eukaryota - drug effects
/ Eukaryota - growth & development
/ Eukaryota - physiology
/ Growth rate
/ Hydrogen ions
/ Hydrogen-Ion Concentration - drug effects
/ Ice
/ Ice Cover
/ Ice formation
/ Krill
/ Microbial activity
/ Microorganisms
/ Ocean acidification
/ Oceans
/ Overwintering
/ pH effects
/ Photosynthesis
/ Physiology
/ Phytoplankton
/ Plankton
/ Polar environments
/ Primary production
/ Saline water
/ Salinity
/ Salt water
/ Sea ice
/ Sea ice formation
/ Seawater
/ Seeding
/ Studies
/ Surface water
/ Thalassiosira pseudonana
/ Trophic levels
/ Zooplankton
2014
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The Response of Antarctic Sea Ice Algae to Changes in pH and CO2
Journal Article
The Response of Antarctic Sea Ice Algae to Changes in pH and CO2
2014
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Overview
Ocean acidification substantially alters ocean carbon chemistry and hence pH but the effects on sea ice formation and the CO2 concentration in the enclosed brine channels are unknown. Microbial communities inhabiting sea ice ecosystems currently contribute 10-50% of the annual primary production of polar seas, supporting overwintering zooplankton species, especially Antarctic krill, and seeding spring phytoplankton blooms. Ocean acidification is occurring in all surface waters but the strongest effects will be experienced in polar ecosystems with significant effects on all trophic levels. Brine algae collected from McMurdo Sound (Antarctica) sea ice was incubated in situ under various carbonate chemistry conditions. The carbon chemistry was manipulated with acid, bicarbonate and bases to produce a pCO2 and pH range from 238 to 6066 µatm and 7.19 to 8.66, respectively. Elevated pCO2 positively affected the growth rate of the brine algal community, dominated by the unique ice dinoflagellate, Polarella glacialis. Growth rates were significantly reduced when pH dropped below 7.6. However, when the pH was held constant and the pCO2 increased, growth rates of the brine algae increased by more than 20% and showed no decline at pCO2 values more than five times current ambient levels. We suggest that projected increases in seawater pCO2, associated with OA, will not adversely impact brine algal communities.
Publisher
Public Library of Science,Public Library of Science (PLoS)
Subject
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