Calcification response of planktic foraminifera to environmental change in the western Mediterranean Sea during the industrial era

• Published in: Biogeosciences
• Main Authors: Béjard, Thibauld M., Rigual-Hernández, Andrés S., Flores, José A., Tarruella, Javier P., Durrieu de Madron, Xavier, Cacho, Isabel, Haghipour, Neghar, Hunter, Aidan, Sierro, Francisco J.
• Format: Text
• Language: English
• Published: 2023
• Subjects: Planktonic foraminifera
• Online Access: https://doi.org/10.5194/bg-20-1505-2023; https://bg.copernicus.org/articles/20/1505/2023/

The Mediterranean Sea sustains a rich and fragile ecosystem currently threatened by multiple anthropogenic impacts that include, among others, warming, pollution, and changes in seawater carbonate speciation associated to increasing uptake of atmospheric CO 2 . This environmental change represents a major risk for marine calcifiers such as planktonic foraminifera, key components of pelagic Mediterranean ecosystems and major exporters of calcium carbonate to the sea floor, thereby playing a major role in the marine carbon cycle. In this study, we investigate the response of planktic foraminifera calcification in the northwestern Mediterranean Sea on different timescales across the industrial era. This study is based on data from a 12-year-long sediment trap record retrieved in the in the Gulf of Lions and seabed sediment samples from the Gulf of Lions and the promontory of Menorca. Three different planktic foraminifera species were selected based on their different ecology and abundance: Globigerina bulloides , Neogloboquadrina incompta , and Globorotalia truncatulinoides . A total of 273 samples were weighted in both sediment trap and seabed samples. The results of our study suggest substantial different seasonal calcification patterns across species: G. bulloides shows a slight calcification increase during the high productivity period, while both N. incompta and G. truncatulinoides display a higher calcification during the low productivity period. The comparison of these patterns with environmental parameters indicate that controls on seasonal calcification are species-specific. Interannual analysis suggests that both G. bulloides and N. incompta did not significantly reduce their calcification between 1994 and 2005, while G. truncatulinoides exhibited a constant and pronounced increase in its calcification that translated in an increase of 20 % of its shell weight. The comparison of these patterns with environmental data reveals that optimum growth conditions affect positively and negatively G. bulloides and ...