115 Matching Annotations
- May 2021
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salinity
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estuaries
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www-jstor-org.dlsu.idm.oclc.org www-jstor-org.dlsu.idm.oclc.org
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ocean acidifica-tion
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decreasing seawater pH
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ocean acidification
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temperature increases
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ocean acidification
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ocean acidification
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ocean acidification
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owered pH levels
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pH changes
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ocean acidification
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ocean acidification
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Elevated CO2
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elevated-CO2
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ocean acidification
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ocean acidification
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elevated-CO2
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ocean acidification
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ocean acidification
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Ocean acidification
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hypoxia
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elevated tempera-tures
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ocean acidification
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ocean acidification
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ocean acidification
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ocean acidification
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ocean acidification
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ocean acidification
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high-CO2 conditions
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temperature
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increasing CO2
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Ocean acidification
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elevated-CO2conditions
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ocean acidification
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ocean acidification
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ocean acidification
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temperature increases,
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temperature
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ocean acidification
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temperature increase
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ocean acidification
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increases in temperature
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Temperature
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ocean acidifica-tion
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acidification
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ocean acidification
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low pH
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changes in the CO2
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ocean acidification
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concentrations of CO2, CO32–, and HCO3–.
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Ca2+ concentration
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Ocean acidification
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calcium ion concentration
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carbonate ion concentration
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ocean acidification
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ocean acidification
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elevated-CO2 conditions
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ocean acidifi-cation
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Ocean acidification
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increased carbon dioxide
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ocean acidification
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www.researchgate.net www.researchgate.net
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sat-uration state
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temperature
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temperatures
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aragonite saturation states
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temperatures
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lowering of saturation state
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Increasing temperature
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Saturation state reduction
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global warming
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Temperatures
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temperature
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ragonite saturation state
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ow temperature
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temperatures
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temperatures
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temperatures
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High temper-ature
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climate change
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temperature
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saturation state
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high temperature
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temperature
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temperature
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temperature
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Elevation of temperature
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high temperature
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low saturation state
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low temperature
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low saturation state
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highsaturation state
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aragonite saturation state
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Temperaturehas
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sea surface temperature
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aragonite saturation state
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temperature
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saturation state
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temperature
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CO2concentratio
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aragonite satura-tion state
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temperature
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light
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ow temperatures
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ow temperatures
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temperature
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decreasing aragonite satura-tion state]
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ncreasing seasurface temperatures
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light
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salinity
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temperature
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low aragonite saturation state
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low ligh
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low salinity
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low temperature
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