Project background
The skeletons of marine calcifiers are composed of aragonite and/or calcite, the primary minerals of calcium carbonate. Aragonite is typically more soluble than calcite, making the mineral composition of organisms’ skeletal structures a key factor in their response to ocean acidification. One of the main determinants of the mineral form of calcium carbonate is the Mg/Ca ratio in the surrounding solution during formation. Magnesium ions (Mg²⁺) act as a growth inhibitor for calcite, replacing calcium ions (Ca²⁺) within its crystal structure, a substitution that does not occur in aragonite. This incorporation of magnesium reduces the stability of calcite crystals, and the process is temperature-dependent, which is why the magnesium content in calcite can be used as a paleothermometer. Both Mg²⁺ and Ca²⁺ are among the most abundant cations in seawater, and their concentrations are influenced by slow geological processes, such as mid-ocean ridge activity and continental weathering (via river runoff). While the concentrations of Mg²⁺ and Ca²⁺ in global seawater change gradually over geological time scales, their fluctuations over millions of years are linked to shifts in the skeletal mineralogy of marine calcifiers.
In contrast to open ocean seawater, which has an average Mg/Ca ratio of 5.2, the Mg/Ca ratio in coastal waters can vary significantly, especially near rivers, where it is typically much lower. Preliminary data from Plymouth Sound indicate that the Mg/Ca ratio fluctuates between 5.5 and 4 over just a few days—equivalent to more than 10 million years of change in bulk ocean water. Plymouth Sound therefore serves as an excellent natural laboratory to explore the impact of seawater Mg/Ca variation on the mineral composition of calcifiers and the incorporation of magnesium into calcite.
In this project, you will collect seawater and intertidal calcifying organisms from shoreline locations along a transect extending farther from the influence of the Tamar River. Seawater samples will be analysed for major cations, while invertebrate calcite will be examined for magnesium content and the proportion of aragonite to calcite in the shells (for taxa that secrete both minerals). The results will shed light on how natural variation in seawater composition affects the skeletal structure of calcifiers, with potential implications for their vulnerability to ocean acidification. Additionally, understanding the variability of magnesium content in biomineralized calcite from coastal ecosystems will enhance the reliability of Mg-based thermometry for coastal species.
