Highlights
- Ocean acidification causes gastropod shell dissolution and microstructural change.
- Shell growth is inhibited below pH 7.5, with dissolution pits in the inner surface.
- At pH 7.1, shell surface erosion intensifies, with extensive periostracum peeling.
- Shell dissolution negatively correlates with pH, offering a new bio-proxy.
- Shell structural changes can assess past ocean acidification events.
Abstract
Global seawater pH is projected to decrease by 0.3–0.5 units on average by the end of this century, which is considered detrimental to the shells of marine calcareous organisms. However, there is limited understanding of how ocean acidification affects the morphology and structure of these shells, as well as the underlying mechanisms. This study examines the shell growth, surface erosion, and microstructural changes of the marine gastropod Lunella coronata granulata after 85 days of exposure to varying pH (8.1–7.1). The results reveal that at pH ≤ 7.5, shell growth is notably inhibited, with pronounced dissolution hole formation on the inner surface. At pH 7.1, shell surface erosion becomes more pronounced, accompanied by extensive peeling of the shell periostracum. These changes—dissolution hole formation and periostracum peeling—are critical indicators of gastropod shell response to ocean acidification and can serve as biological indicators reflecting current and past ocean acidification. Additionally, our study shows a clear negative correlation between shell dissolution and pH, providing new bio-proxy for indicating the pH changes.
Li X., Song H., Tian L., Chen X., Sun X., Yan J., Jia E., Feng Y. & Chu D., 2025. The impact of ocean acidification on gastropod shell dissolution and microstructure. Anthropocene 50: 100470. doi: 10.1016/j.ancene.2025.100470. Article (subscription required).
