Carbonate precipitation in oceans is essential for the carbonate-silicate cycle (inorganic carbon cycle) to maintain temperate climates.
Biogeochemical Cycles & Geobiology
Enabling Ice Core Science On Mars And Ocean Worlds
Ice deposits on Earth provide an extended record of volcanism, planetary climate, and life.
Mars Curiosity Rover Discovers Water-rich Fracture Halo’s in Gale Crater
A research team using new methods to analyze data from NASA’s Curiosity rover and its neutron spectrometer Dynamic Albedo of Neutrons, or DAN, on Mars was able to independently verify […]
A 3-Dimension Model of Volcanism Volatiles Contribution on Atmospheric Chemical Abundance of Habitable Planets
The volcanism plays an important part in mass exchange circle to bring matter from core of planet to atmosphere.
Perseverance Rover Starts To Collect Regolith Samples
NASA’s Perseverance rover snagged two new samples from the Martian surface on Dec. 2 and 6. But unlike the 15 rock cores collected to date, these newest samples came from […]
Early Earth Forests Did Not Significantly Change Atmospheric CO2
Scientists have discovered that the atmosphere contained far less CO2 than previously thought when forests emerged on our planet, the new study has important implications for understanding how land plants […]
Sedimentary Rock Chert Records Cooling Of Earth Over Billions Of Years
Several billion years ago, the oceans were probably not as hot as often assumed, but were instead at much more moderate temperatures.
Earth Can Regulate Its Own Temperature Over Millennia
The Earth’s climate has undergone some big changes, from global volcanism to planet-cooling ice ages and dramatic shifts in solar radiation. And yet life, for the last 3.7 billion years, […]
Two Exoplanets May Be Mostly Water, NASA’s Hubble and Spitzer Find
A team led by of researchers at the University of Montreal has found evidence that two exoplanets orbiting a red dwarf star are “water worlds,” where water makes up a […]
We Drink Good 4.5-Billion-Year-Old Water On Earth
Water is crucial for the emergence and evolution of life on Earth.
