From Core to Crust: The Significance of Magma’s Oxidation in Earth’s Formation
How has the atmosphere and mantle oxidation state of the Earth changed? The connection between a planet’s interior and its surface plays a pivotal role…
How has the atmosphere and mantle oxidation state of the Earth changed? The connection between a planet’s interior and its surface plays a pivotal role…
Black holes with exceptionally large masses—over a million times the mass of the Sun, known as supermassive black holes (SMBHs)—are commonly found in the universe…
New research suggests early Earth had a highly oxidized magma ocean, leading to a CO2 and SO2-rich atmosphere. The subsequent accretion of reducing materials was…
New study sheds light on the composition of the Earth’s earliest atmosphere. Understanding the atmospheric and surface conditions of early Earth, especially before life originated,…
The beetles of the family Erotylidae (Coleoptera: Cucujoidea) are morphologically and biologically diversified into six subfamilies, 10 tribes, and over 3,500 species. The tribe Toramini…
Peculiar Bi provoked nanostructures in compound semiconductor nanowires controlled by atomically precise epitaxial crystal growth. Nanowire is a rod-structure with a diameter typically narrower than…
It is generally accepted that planetary surfaces were covered with molten silicate, a “magma ocean,” during the formation of terrestrial planets. In a deep magma…