Ocean acidification in the Mediterranean is already affecting the calcification of marine plankton

The acidification of the oceans caused by human activity is already altering the production of marine plankton shells in the Mediterranean Sea. This is the worrying conclusion of a study led by the Institute of Environmental Science and Technology of the Universitat Autònoma de Barcelona (ICTA-UAB), which alerts of the impact the decrease in pH of the surface ocean has on the production of calcium carbonate by marine plankton, with negative consequences for marine ecosystems.

Credit: Photo: ICTA-UAB

The acidification of the oceans caused by human activity is already altering the production of marine plankton shells in the Mediterranean Sea. This is the worrying conclusion of a study led by the Institute of Environmental Science and Technology of the Universitat Autònoma de Barcelona (ICTA-UAB), which alerts of the impact the decrease in pH of the surface ocean has on the production of calcium carbonate by marine plankton, with negative consequences for marine ecosystems.

Anthropogenic carbon dioxide (CO2) emissions have increased alarmingly in recent decades. Since the Industrial Revolution, about 25% of anthropogenic CO2 has entered the ocean, changing water chemistry and lowering pH, a phenomenon known as ocean acidification.

The study, carried out in collaboration with researchers from the University of St Andrews (UK), the Max Planck Institute of Chemistry (MPIC) in Mainz (Germany) and the Spanish Council for Scientific Research (CSIC) in Barcelona (Spain) and published in the Nature Portfolio journal Communications Earth & Environment, assessed the impact of CO2 -induced changes in the Mediterranean Sea on foraminifera, a particular group of calcifying planktonic organisms.

To do this, they studied records from different Mediterranean sites: the Alboran Sea, off the coast of Barcelona, and the Strait of Sicily, spanning the past two thousand years. The researchers chose to study the western Mediterranean Sea because it is a region particularly affected by anthropogenic pressures and climate change. Due to the high alkalinity and the fast circulation of water masses in the basin, Mediterranean waters are susceptible to the uptake of anthropogenic carbon, which has led to a pH drop of 0.08 units since the Industrial Revolution, affecting the biogenic calcification of marine plankton.

The researchers found that ocean acidification caused by anthropogenic emissions is the main driver of the decline in foraminiferal calcite mass, while ocean warming may be mitigating this effect.

By reconstructing the records, the researchers were able to assess the impact of acidification on the calcification of planktonic foraminifera. The results can also be applied to other calcifying planktic organisms living in Mediterranean surface waters, such as coccolithophores or pteropods, which play an important role in the modulations of atmospheric CO2.

The results indicate that anthropogenic ocean acidification at the Mediterranean Sea surface has affected foraminiferal calcification during the 20th century. As calcifying plankton are an important component of both the marine food web architecture and biogeochemical cycles, continued ocean acidification would have a negative impact on marine ecosystem services, including climate regulation, ocean’s ecosystem functioning and food security, reiterating the importance of mitigating climate change by drastically reducing CO2 emissions.

Bioengineer, 12 November 2023. Press release.


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