The Cambrian Explosion in which life on Earth underwent massive diversification was likely triggered by eccentricities in Earth’s orbit around our Sun. Or so say the authors of a new paper just ...
"Inorganic Evolution Theory" is a serialized project from the Beyondge Future Research Institute, published chapter by ...
Our Earth is around 4.5 billion years old. Way back in its earliest years, vast oceans dominated. There were frequent volcanic eruptions and, because there was no free oxygen in the atmosphere, there ...
We have only one example of biology forming in the universe – life on Earth. But what if life can form in other ways? How do you look for alien life when you don’t know what alien life might look like ...
Watch the Earth's tectonic plates grow, shrink, and jostle for position in this new model of the last billion years on the ...
An interdisciplinary international research team has recently discovered that a massive anomaly deep within the Earth’s interior may be a remnant of the collision about 4.5 billion years ago that ...
Forbes contributors publish independent expert analyses and insights. David Bressan is a geologist who covers curiosities about Earth. The chemistry of crystals in some of Earth’s oldest rocks may ...
Stars that pass by our solar system have altered the long-term orbital evolution of planets, including Earth, and, by extension, modified our climate. "Perturbations—a minor deviation in the course of ...
A new simulation model shows Earth's evolution over the past 100 million years in a very detailed manner. The sun sets behind artist Luke Jerram's 'Floating Earth' at Pennington Flash on November 22, ...
Top panel shows reconstructed sediment fluxes to the oceans vs diversity of marine animals. Bottom panel shows sediment cover in continental regions vs the long-term trend in land-plant diversity.
It’s been a while since I’ve reviewed a book by publisher What on Earth, and some time since I reviewed a book about evolution. It’s a happy alignment then that my next book is for both: Evolution by ...