Bioremediation: Working with Bacteria

Soil bioremediation is a complex and costly process that aims to restore contaminated sites to environmentally sustainable conditions using microorganisms. The process relies upon the ability of microorganisms to degrade organic molecules, but it also depends on the microorganisms coming into contact with the contaminants, and the environment in the contaminated soil being conducive to the survival of the bacteria. A wide variety of techniques have been developed to ensure that these latter two constraints are overcome and to enhance contaminant biodegradation. Future developments in bioremediation are likely to lead to a reduction in both the energy used and the resulting pollutant and greenhouse gas emissions.

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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.