Recently in the Geobiology Category

Hold on to your hats, because scientists have found more evidence that Earth tips over from time to time.

Massive steam and CO2 atmospheres have been proposed for magma ocean outgassing of Earth and terrestrial planets.

Photosynthesis, the process by which plants and other organisms convert sunlight into chemical energy, has been a major player during the evolution of life and our planet's atmosphere.

A new study led by a University of Alberta PhD student--and published in Nature--is examining the Earth's carbon cycle in new depth, using diamonds as breadcrumbs of insight into some of Earth's deepest geologic mechanisms.

Dust plays a crucial role in the life and health of our planet. In our modern world, dust-borne nutrients traveling in great dust storms from the Saharan Desert fertilize the soil in the Amazon Rainforest and feed photosynthetic organisms like algae in the Atlantic Ocean. In turn, it is those organisms that breathe in carbon dioxide and expel oxygen.

Researchers supported in part by the Exobiology Program have provided new information about the oxygenation history of the Earth's oceans during the mid-Proterozoic using uranium (U) isotope data.

The remains of a microscopic drop of ancient seawater has assisted in rewriting the history of Earth's evolution when it was used to re-establish the time that plate tectonics started on the planet.

The longevity of Earth's continents in the face of destructive tectonic activity is an essential geologic backdrop for the emergence of life on our planet.

By acting as gatekeepers, microbes can affect geological processes that move carbon from the earth's surface into its deep interior, according to a study published in Nature and coauthored by microbiologists at the University of Tennessee, Knoxville.

Microscopic plant-like organisms called phytoplankton are known to support the diversity of life in the ocean.