Abstract

Ocean acidification has been broadly recognised to have effects on the structure and functioning of marine benthic communities. The selection of tolerant or vulnerable species can also occur during settlement phases, especially for calcifying organisms which are more vulnerable to low pH–high pCO2 conditions. Here, we use three natural CO2 vents (Castello Aragonese north and south sides, and Vullatura, Ischia, Italy) to assess the effect of a decrease of seawater pH on the settlement of Mollusca in Posidonia oceanica meadows, and to test the possible buffering effect provided by the seagrass. Artificial collectors were installed and collected after 33 days, during April–May 2019, in three different microhabitats within the meadow (canopy, bottom/rhizome level, and dead matte without plant cover), following a pH decreasing gradient from an extremely low pH zone (pH < 7.4), to ambient pH conditions (pH = 8.10). A total of 4659 specimens of Mollusca, belonging to 57 different taxa, were collected. The number of taxa was lower in low and extremely low pH conditions. Reduced mollusc assemblages were reported at the acidified stations, where few taxa accounted for a high number of individuals. Multivariate analyses revealed significant differences in mollusc assemblages among pH conditions, microhabitat, and the interaction of these two factors. Acanthocardia echinata, Alvania lineata, Alvania sp. juv, Eatonina fulgida, Hiatella arctica, Mytilys galloprovincialis, Musculus subpictus, Phorcus sp. juv, and Rissoa variabilis were the species mostly found in low and extremely low pH stations, and were all relatively robust to acidified conditions. Samples placed on the dead matte under acidified conditions at the Vullatura vent showed lower diversity and abundances if compared to canopy and bottom/rhizome samples, suggesting a possible buffering role of the Posidonia on mollusc settlement. Our study provides new evidence of shifts in marine benthic communities due to ocean acidification and evidence of how P. oceanica meadows could mitigate its effects on associated biota in light of future climate change.

Highlights

  • In the last two centuries, the atmospheric CO2 concentration levels have steadily increased due to anthropic activities, rising from 280 ppm during the Industrial Revolution to 411.5 ppm today [1]

  • Oceans act as an essential carbon sink, absorbing part of anthropogenic CO2 emissions; this is causing a rise in pCO2 concentrations at the sea surface, leading to a decrease in the ocean pH level and change in carbonate chemistry, a process broadly known as “ocean acidification” (OA) [2]

  • This study aims to assess the effect of the pH variation, along a natural gradient of OA in three CO2 vent’s systems, on the settlement of invertebrate fauna associated with

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Summary

Introduction

In the last two centuries, the atmospheric CO2 concentration levels have steadily increased due to anthropic activities, rising from 280 ppm during the Industrial Revolution to 411.5 ppm today [1]. Oceans act as an essential carbon sink, absorbing part of anthropogenic CO2 emissions; this is causing a rise in pCO2 concentrations at the sea surface, leading to a decrease in the ocean pH level and change in carbonate chemistry, a process broadly known as “ocean acidification” (OA) [2]. The Intergovernmental Panel on Climate Change models [3] predict that the pH of surface seawater will drop by 0.4 units by the year 2100, increasing the acidity levels by 170% compared to the pre-industrial ones. OA is an ongoing process expected to intensify in the future, which, together with the other aspects of Global Climate Change, drastically threatens the structure and functioning of marine ecosystems, especially in a semi-closed basin such as the Mediterranean Sea [4]. The rise of CO2 in ocean waters leads, to more corrosive conditions, as well as a depletion of calcium carbonate, that affect calcifying organisms hindering them from building and maintain their carbonate shells and skeletons [7,8]

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