Why only a small number of planets are suitable for life
Peer-Reviewed Publication
Updates every hour. Last Updated: 17-Apr-2026 02:15 ET (17-Apr-2026 06:15 GMT/UTC)
The right amount of oxygen being present when the Earth’s core was formed meant that there were sufficient phosphorus and nitrogen available in the mantle and crust. This means the Earth was the beneficiary of a stroke of chemical good fortune in the universe. It is located in a zone with optimal chemical conditions for the development of life. When searching for life elsewhere in the universe, scientists should therefore look for solar systems that resemble our own. Focusing on water is not sufficient.
New research from the University of East Anglia (UEA) finds that 'energy efficiency' appears to influence how mountain birds adapt to changes in climate. Researchers looked at seasonal changes in the elevational distributions of birds - how high in the mountain birds go at different times of year - for nearly 11,000 avian populations across 34 mountain regions worldwide, including in Asia, Europe and the Americas, as well as Southern African and Australia.
A University of Utah geoscientist, teamed with paleomagnetists from Japan and France, extracted sediment cores off Newfoundland that revealed a geomagnetic pole reversal that dragged on for 70,000 years—far longer than previously known.
An MIT study suggests some early life forms may have evolved the ability to use oxygen hundreds of millions of years before the Great Oxidation Event, when oxygen became a permanent fixture in the atmosphere. The findings may represent some of the earliest evidence of aerobic respiration on Earth.
Antigorite is the dominant serpentine mineral in serpentinite, a key target mineral for investigating the physical properties of tectonic plate boundaries in subduction zone regions. Now, researchers have found that antigorite deforms by a mechanism known as grain boundary sliding. Their study captures the characteristics of localized deformation occurring in earthquake source regions by examining microscopic deformation structures in natural rocks, thereby providing insights into “silent slip” processes progressing at depth.
A UT San Antonio-led international research team has identified chitin, the primary organic component of modern crab shells and insect exoskeletons, in trilobite fossils more than 500 million years old, marking the first confirmed detection of the molecule in this extinct group. The findings, led by Elizabeth Bailey, assistant professor of earth and planetary sciences at UT San Antonio, offer new insight into fossil preservation and Earth’s long-term carbon cycle.