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Progress in Earth and Planetary Science
Fig. 15 | Progress in Earth and Planetary Science

Fig. 15

From: 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”

Fig. 15

Gametogenesis rates (left) and days to gametogenesis (right) in Orbulina universa (solid red line) and Globigerina bulloides (broken blue line) at different dissolved oxygen (DO) saturation levels (figure modified from Kuroyanagi et al. 2013). Although DO environments are classified differently in different studies (e.g., Jorissen et al. 2007), a DO of 10% (~ 0.7 mg O2 L−1 or ~ 22 mmol O2 m−3) was generally classified as “dysoxic”

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