Calcium Carbonate Biomineralisation: Insights from Trace Elements

The concentrations of trace elements in carbonate biominerals can provide critical proxy records of past chemical and physical environmental conditions. However, the concentrations of these elements within biominerals are influenced by the diverse biological processes that govern mineralisation. This allows us to use the trace element content of biominerals grown under known conditions to infer the biological, physical, and dynamical processes that are involved in biomineralisation mechanisms. Here we introduce how key biomineralisation mechanisms can influence trace element incorporation, and we offer a high-level overview of how trace elements are used to infer the relative importance of these mechanisms in major groups of marine calcifiers.

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December 2025 --The Variscan Orogeny in Europe – Understanding Supercontinent Formation

The Variscan orogen formed between 380 and 300 million years ago through several accretionary and collisional cycles, culminating with the construction of the Pangea supercontinent. This process occurred via sequential opening and closure of oceanic basins, synchronous detachment of Gondwana derived continental ribbons, and their outboard amalgamation onto the Laurussia margin. The Variscan orogen is rather unique compared with other orogenic belts on Earth: its overthickened and dominantly magmatic crust in the central belt, surprisingly minor mantle involvement in the magmatic and geodynamic processes, coherent and pulsed magmatism along the collision suture, and its complex accretionary history. Because its final product, Pangea, is the youngest and best-understood supercontinent on Earth, the Variscan orogeny offers clues for understanding the mechanisms of supercontinent formation.