Minerals as Substrates for Life: The Prokaryotic View

Conceptually, minerals represent challenging “substrates” (sources of nutrients and/or energy) for prokaryotes because they can transfer only soluble compounds into or out of their cells. Yet, prokaryotes are able to use a wide array of minerals as sources of energy, trace nutrients, electron acceptors and, remarkably, for positioning themselves using the Earth’s magnetic field. Mineral dissolution exposes microorganisms to a wide range of soluble and potentially toxic metals. Conversely, microbial mineralformation processes can entrap cells, producing microfossils. Intuitively, mineral dissolution and mineral precipitation must provide a benefit for the organism, that is, they must supply the cell with the energy and materials needed to maintain cell structure and function.

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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.