Perspective on the response of marine calcifiers to global warming and ocean acidification—Behavior of corals and foraminifera in a high CO2 world “hot house”

• Published in: Progress in earth and planetary science Vol. 6; no. 1; pp. 1 - 37
• Main Authors: Kawahata, Hodaka, Fujita, Kazuhiko, Iguchi, Akira, Inoue, Mayuri, Iwasaki, Shinya, Kuroyanagi, Azumi, Maeda, Ayumi, Manaka, Takuya, Moriya, Kazuyoshi, Takagi, Haruka, Toyofuku, Takashi, Yoshimura, Toshihiro, Suzuki, Atsushi
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 17.01.2019; Springer Nature B.V; SpringerOpen
• Subjects: 5. Biogeosciences; Acidification; Acidity; Alkalinity; Anthropogenic factors; Atmospheric Sciences; Biogeosciences; Bleaching; Calcification; Carbon cycle; Carbon cycle models; Carbon dioxide; Carbon dioxide concentration; Climate change; Coral; Deep water; Dissolved inorganic carbon; Earth and Environmental Science; Earth Sciences; Earth surface; Ecology; Environmental changes; Eocene; Foraminifera; Geophysics/Geodesy; Global temperatures; Global warming; Heat stress; High pressure; High temperature; Hydrogeology; Light intensity; Low temperature; Mean temperatures; Minerals; Ocean acidification; Ocean warming; Oceans; Organic matter; Paleocene; Partial pressure of CO2; Planetology; Precipitation rate; Review; Seawater; Seawater pH; Synergistic effect; Carbon cycle; Partial pressure of CO; Aragonite; Saturation state; Organic matter; Coral; Bleaching; Foraminifera; Global warming; Alkalinity; Ocean acidification; Calcite
• ISSN: 2197-4284; 2197-4284
• DOI: 10.1186/s40645-018-0239-9

The CO 2 concentration of air has increased over the last two centuries and recently surpassed 400 ppm. Carbon cycle models project CO 2 concentrations of 720 to 1000 ppm for the IPCC intermediate scenario (RCP 6.0), resulting in an increase in global mean temperature of ~ 2.6 °C and a decrease in seawater pH of ~ 0.3. Together, global warming and ocean acidification are often referred to as the “evil twins” of climate change, potentially inducing severe threats in the near future. In this paper, our discussion is focused on the response of two major calcifiers, foraminifera and corals, which contribute much to the global carbonate burial rate. Photosymbiosis is regarded as an adaptive ecology for living in warm and oligotrophic oceans, especially for reef-building corals and larger reef-dwelling benthic foraminifera. As a consequence of global warming, bleaching may be a global threat to algal symbiont-bearing marine calcifying organisms under conditions of high temperature and light intensity. If CO 2 is dissolved in seawater, the partial pressure of CO 2 in seawater ( p CO 2 ) and dissolved inorganic carbon (DIC) increases while pH and the saturation state of carbonate minerals decreases without any change in total alkalinity. Generally, marine calcifying organisms show decreases in calcification rates in response to acidified seawater. However, the response often differs depending on situations, species, and life-cycle stage. Some benthic foraminifera showed a positive response to low pH conditions. The Acropora digitifera coral calcification of adult branches was not reduced markedly at higher p CO 2 conditions, although calcification tended to decrease versus p CO 2 in both aposymbiotic and symbiotic polyps. New analytical technologies help identify important constraints on calcification processes. Based upon Ca isotopes, the transport path of Ca 2+ and the degree of its activity would predominantly control the carbonate precipitation rate. Visualization of the extracellular pH distribution shows that proton pumping produces the high internal pH and large internal–external pH gap in association with foraminiferal calcification. From the perspective of a long-term change in the Earth’s surface environment, foraminifera seem to be more adaptive and robust than corals in coping with ocean warming and acidification but it is necessary to further understand the mechanisms underlying variations in sensitivity to heat stress and acidified seawater for future prediction. Since CO 2 is more soluble in lower temperature seawater, ocean acidification is more critical in the polar and high-latitude regions. Additionally, older deep-water has enhanced acidity owing to the addition of CO 2 from the degradation of organic matter via a synergistic effect with high pressure. With current ocean acidification, pH and the saturation state of carbonate minerals are decreasing without any change in total alkalinity. However, in the Earth’s history, it is well known that alkalinity has fluctuated significantly. Therefore, it is necessary to quantitatively reconstruct alkalinity, which is another key factor determining the saturation state of carbonate minerals. The rapid release of anthropogenic CO 2 (in the present day and at the Paleocene/Eocene boundary) induces severe ocean acidification, whereas in the Cretaceous, slow environmental change, even at high levels of p CO 2 , could raise alkalinity, thereby neutralizing ocean acidification.