Botanica Marina· 2026Q2· Review
Pathways to calcification in coccolithophores
- 1citations
- Q2SCImago
- 2026year
Short summary
Coccolithophores form calcite plates (coccoliths) within a Golgi-derived compartment and secrete them to form a protective outer shell (coccosphere).
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Key points
- Coccolithophores produce calcite coccoliths internally within a Golgi-derived compartment.
- Coccoliths are secreted to the cell surface, forming the coccosphere.
- Calcification requires membrane transport of inorganic carbon and calcium into the cell.
- Proton removal is a critical byproduct of the calcification reaction.
AI-generated from the title and abstract; the full text is not read.
Abstract
Abstract Calcification by coccolithophores represents a major biogeochemical process in the oceans. Calcification involves the formation of calcite coccoliths within a Golgi-derived compartment inside the cell. These are secreted to the cell surface where they form the coccosphere. Coccolithophore calcification is underpinned by membrane transport processes that deliver the inorganic carbon and calcium substrates from the external seawater to the site of calcification and by the removal of products, namely protons produced in the calcification reactions. Understanding these critical aspects of calcification will provide clearer insights into the responses of coccolithophores to chemical and physical conditions, both in terms of short-term acclimation and long-term adaptation to a changing ocean. In this review we consider these processes, their localization and the specific transporters likely to be involved. We also consider how transport processes are linked to structural aspects of the cell, providing specialized pathways for the substantial ion fluxes involved.
The authors' abstract, as published at the source. Botanica Marina, 2026 · DOI ↗
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Field: Biomaterials
BiomaterialsMaterials Science