Reactive Transport Modeling of Microbial Dynamics

Reactive transport modeling of microbially mediated processes has contributed significantly to an improved understanding of elemental cycling in Earth’s near-surface environments. We describe key characteristics of microbial reactive transport models, recent advances in modeling approaches, and the application of such models to terrestrial and marine environmental problems. We introduce relevant case studies and discuss ways to integrate omics data (e.g., genomics, proteomics, metabolomics) that can inform and validate microbial reactive transport models, thereby improving our ability to address some of the grand challenges in a changing world.

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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.