The Dawn of Humanity: What Can Paleoanthropologists and Geoscientists Learn from One Another?

Establishing a scientific narrative of human origins requires a better understanding of the geological processes that facilitated the fossil- ization and recovery of hominins and associated fauna that inform us about our human ancestors’ past environments. Paleoanthropologists rely on geologists, particularly volcanologists, geochemists, sedimentologists, and geochronologists, to help them tease out the depositional and preservation history of fossils. Here, we provide an overview of how geology has contributed to major paleoanthropological discoveries from select Plio–Pleistocene locali- ties in eastern Africa, Tanzania (Oldupai* (Olduvai) Gorge and Laetoli), Kenya (Allia Bay, Kanapoi, and Koobi Fora), and Ethiopia (Hadar, Woranso-Mille, and Dikika) over the past 75 years of research.

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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.