Seawater carbonate chemistry and phytoplankton growth and mortality
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2021
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| _version_ | 1867170112065241088 |
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| author | Domingues, Rita B Barreto, Marcelle Brotas, Vanda Galvão, Helena M Barbosa, Ana B |
| author_facet | Domingues, Rita B Barreto, Marcelle Brotas, Vanda Galvão, Helena M Barbosa, Ana B |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Changes in temperature and CO2 are typically associated with climate change, but they also act on shorter time scales, leading to alterations in phytoplankton physiology and community structure. Interactions among stressors may cause synergistic or antagonistic effects on phytoplankton dynamics. Therefore, the main goal of this work is to understand the short-term isolated and interactive effects of warming and high CO2 on phytoplankton nutrient consumption, growth, production, and community structure in the Ria Formosa coastal lagoon (southern Portugal). We performed microcosm experiments with temperature and CO2 manipulation, and dilution experiments under temperature increase, using winter phytoplankton assemblages. Phytoplankton responses were evaluated using inverted and epifluorescence microscopy. Overall, phytoplankton growth and microzooplankton grazing on phytoplankton decreased with warming. Negative antagonist interactions with CO2 alleviated the negative effect of temperature on phytoplankton and cryptophytes. In contrast, higher temperature benefited smaller-sized phytoplankton, namely cyanobacteria and eukaryotic picophytoplankton. Diatom growth was not affected by temperature, probably due to nutrient limitation, but high CO2 had a positive effect on diatoms, alleviating the effect of nutrient limitation. Results suggest that this winter phytoplankton assemblage is well acclimated to ambient conditions, and short-term increases in temperature are detrimental, but can be alleviated by high CO2. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_939902 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Seawater carbonate chemistry and phytoplankton growth and mortality Domingues, Rita B Barreto, Marcelle Brotas, Vanda Galvão, Helena M Barbosa, Ana B Alkalinity, total; Ammonium consumption rate; Ammonium consumption rate, standard error; Aragonite saturation state; Bicarbonate ion; Bottles or small containers/Aquaria (<20 L); Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Community composition and diversity; Entire community; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard error; Irradiance; Laboratory experiment; Light saturation point; Light saturation point, standard error; Mediterranean Sea; Nitrate consumption rate; Nitrate consumption rate, standard error; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Other metabolic rates; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH, total scale; Phosphate consumption rate; Phosphate consumption rate, standard error; Photosynthetic efficiency, carbon production; Photosynthetic efficiency, standard error; Primary production/Photosynthesis; Production rate, maximal, light saturated, as carbon normalized to chlorophyll a, standard error; Production rate, maximal, light saturated, as carbon per chlorophyll a; Salinity; Silicate consumption rate; Silicate consumption rate, standard error; Specific primary production of carbon per Chlorophyll a; Temperate; Temperature; Temperature, water; Treatment; Type Changes in temperature and CO2 are typically associated with climate change, but they also act on shorter time scales, leading to alterations in phytoplankton physiology and community structure. Interactions among stressors may cause synergistic or antagonistic effects on phytoplankton dynamics. Therefore, the main goal of this work is to understand the short-term isolated and interactive effects of warming and high CO2 on phytoplankton nutrient consumption, growth, production, and community structure in the Ria Formosa coastal lagoon (southern Portugal). We performed microcosm experiments with temperature and CO2 manipulation, and dilution experiments under temperature increase, using winter phytoplankton assemblages. Phytoplankton responses were evaluated using inverted and epifluorescence microscopy. Overall, phytoplankton growth and microzooplankton grazing on phytoplankton decreased with warming. Negative antagonist interactions with CO2 alleviated the negative effect of temperature on phytoplankton and cryptophytes. In contrast, higher temperature benefited smaller-sized phytoplankton, namely cyanobacteria and eukaryotic picophytoplankton. Diatom growth was not affected by temperature, probably due to nutrient limitation, but high CO2 had a positive effect on diatoms, alleviating the effect of nutrient limitation. Results suggest that this winter phytoplankton assemblage is well acclimated to ambient conditions, and short-term increases in temperature are detrimental, but can be alleviated by high CO2. |
| title | Seawater carbonate chemistry and phytoplankton growth and mortality |
| topic | Alkalinity, total; Ammonium consumption rate; Ammonium consumption rate, standard error; Aragonite saturation state; Bicarbonate ion; Bottles or small containers/Aquaria (<20 L); Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Community composition and diversity; Entire community; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard error; Irradiance; Laboratory experiment; Light saturation point; Light saturation point, standard error; Mediterranean Sea; Nitrate consumption rate; Nitrate consumption rate, standard error; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Other metabolic rates; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH, total scale; Phosphate consumption rate; Phosphate consumption rate, standard error; Photosynthetic efficiency, carbon production; Photosynthetic efficiency, standard error; Primary production/Photosynthesis; Production rate, maximal, light saturated, as carbon normalized to chlorophyll a, standard error; Production rate, maximal, light saturated, as carbon per chlorophyll a; Salinity; Silicate consumption rate; Silicate consumption rate, standard error; Specific primary production of carbon per Chlorophyll a; Temperate; Temperature; Temperature, water; Treatment; Type |
| url | https://doi.org/10.1594/PANGAEA.939902 |