Biocalcification crisis in the continental shelf under ocean acidification

• Published in: Geoscience Frontiers
• Main Authors: Shuaishuai Dong, Yanli Lei, Tiegang Li, Yifei Cao, Kuidong Xu
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2023
• Subjects: Benthic foraminifera; pCO2; Ocean acidification; Continental shelf; Calcium carbonate deposit; Yellow Sea; Geology; QE1-996.5; Pacific
• Online Access: https://doi.org/10.1016/j.gsf.2023.101622; https://doaj.org/article/24f60ddace3549e7a06c673d9c3efd01

Ocean acidification (OA) is a persistent challenge for humans and is predicted to have deleterious effects on marine organisms, especially marine calcifiers such as coral and foraminifera. Benthic foraminifera is an important component of sediment in the continental shelf, while little is known about the impact of ocean acidification on benthic foraminifera both at the community and individual level and associated calcium carbonate deposition. We conducted eight months continued culture experiment under the scenario of 400, 800, 1200 and 1600 ppm pCO2 gradients on living benthic foraminifera from four stations in the continental shelf of the West Pacific Ocean. Statistic results showed OA had a negative effect on the abundance of benthic foraminifera. In contrast, the diversity increased roughly under OA conditions implying OA might stimulate the emergence of rare species and promote community diversity to some extent. In addition, we confirmed that the offshore area wasn’t the refuge for benthic foraminifera while the nearshore one had more resistance to moderate acidification. Calcareous species Protelphidium tuberculatum was the dominant species occupying on average 75% in all treatments and its shell diameter, weight and thickness showed a decrease, indicating the decrease of calcification of benthic foraminifera. A relationship between the weight of P. tuberculatum and pCO2 (R2 = 0.96) was established. Based on the present work, calcareous benthic foraminifera deposited 8.57 × 104 t calcium carbonate per year and this might reduce by nearly half and 90% under 800 and 1200 ppm scenarios, which indicates a biocalcification crisis under ongoing OA. This work shows an analogy for palaeoceanic OA and also provides new insights into the sediment of calcium carbonate in the future.