This paper reviews the phosphate phases in meteorites and those measured by landed spacecraft, what they reveal about past igneous and aqueous conditions on Mars, and important implications for potential […]
Gale Crater
New Insights Into How Mars Became Uninhabitable
NASA’s Curiosity rover, currently exploring Gale Crater on Mars, is providing new details about how the ancient Martian climate went from potentially suitable for life — with evidence for widespread […]
Rocks from Mars’ Jezero Crater, Which Likely Predate Life On Earth, Contain Signs Of Water
In a new study appearing today in the journal AGU Advances, scientists at MIT and NASA report that seven rock samples collected along the “fan front” of Mars’ Jezero Crater […]
Taphonomy Of Biosignatures In Carbonate Nodules From The Mars-analog Qaidam Basin
Early diagenetic nodules with low permeable and weather-resistant structures are considered to be favorable for biosignature preservation.
Mars Likely Had A Cold And Icy Past
The question of whether Mars ever supported life has captivated the imagination of scientists and the public for decades. Central to the discovery is gaining insight into the past climate […]
Tracing The Origins of Organic Matter in Martian Sediments
Although Mars presents a barren, dusty landscape with no signs of life so far, its geological features such as deltas, lakebeds, and river valleys strongly suggest a past where water […]
New Findings Point To An Earth-like Environment On Ancient Mars
A research team using the ChemCam instrument onboard NASA’s Curiosity rover discovered higher-than-usual amounts of manganese in lakebed rocks within Gale Crater on Mars, which indicates that the sediments were […]
Why Is Methane Seeping on Mars? NASA Scientists Have New Ideas
A recent paper may help explain why a portable chemistry lab on NASA’s Curiosity rover has continually sniffed out traces of the gas near the surface of Gale Crater.
Curiosity Rover Searches For New Clues About Mars’ Ancient Water
The rover has arrived at an area that may show evidence liquid water flowed on this part of Mars for much longer than previously thought.
Are Large Sulfur Isotope Variations Biosignatures in an Ancient, Impact-Induced Hydrothermal Mars Analog?
Discrepancies have emerged concerning the application of sulfur stable isotope ratios as a biosignature in impact crater paleolakes.
