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Building blocks of life formed on Mars

A Carnegie Institution-led team finds organic compounds containing carbon and hydrogen in Martian meteorite Allan Hills 84001, suggesting that building blocks of life formed on Mars early in its history. The discovery was made by analyzing the rock's association with iron oxide mineral magnetite.

SourceCarnegie Institution for Science·JournalMeteoritics and Planetary Science·DateDec 11, 2007

Mars' molten past

Researchers found that Mars' surface remained molten for 100 million years, implying a thick atmosphere to insulate the planet and slow cooling. This persistence is surprisingly long, with implications for the planet's early history.

Mars with ice, shaken, not stirred

Recent high-resolution images from NASA's Mars orbiters show extensive evidence of ice-made features on the planet's surface, including glacial debris and valley deposits. The findings suggest a dynamic history of Martian climate change, with water ice playing a key role in shaping the planet's geology.

New evidence points to oceans on Mars

Researchers found changes in Mars' topography that could be explained by surface deformation from 'true polar wander', a phenomenon where a planet's spin axis shifts. The study suggests large oceans on Mars existed in the past, with evidence pointing to the presence of vast oceans and massive deformations along ancient shorelines.

Mars -- Red Planet once blue planet

A team of Canadian and U.S. researchers have found evidence that ragged features on Mars' surface were once shorelines of massive ancient oceans. The study suggests that a shift in Mars' spin axis within the past 2-3 billion years deformed these shorelines.

SourceUniversity of Toronto·JournalNature·DateJun 13, 2007

Dig deeper to find Martian life

Current drills may find essential signs of life on Mars but can't reach the living cells that could survive in ice at Elysium or recent craters due to radiation levels, scientists say. The team found that drilling depth required for finding living cells is much deeper than current probes can reach.

SourceUniversity College London·JournalGeophysical Research Letters·DateJan 30, 2007

Geologists finding a different Mars underneath

Researchers have found evidence of ancient impact basins and topographic depressions in the Martian lowlands using MARSIS instrument, confirming the subsurface's complexity. The discovery sheds light on the geologic evolution of Mars, revealing a dichotomy between the northern and southern hemispheres.

SourceSmithsonian·JournalNature·DateDec 13, 2006

Mineral discovery explains Mars' landscape

A Queen's University researcher has discovered a mineral that could explain the mountainous landscape of Mars, suggesting the planet was likely wetter in the past. The study reveals layering in rocks indicative of sediment manipulated by water, which would require significant water on the planet at some point.

SourceQueen's University·JournalGeology·DateOct 23, 2006

Decoding Mars's cryptic region

Mars Express's OMEGA instrument reveals a thick slab of dry ice in the cryptic region, but dust contamination is caused by geysers triggered by sunlight heating the soil beneath. The geysers create spots and fans, which suggest a process that could significantly contribute to the dust contamination observed.

SourceEuropean Space Agency·JournalNature·DateOct 19, 2006

AGU journal highlights - 31 May 2006

Research papers in Geophysical Research Letters highlight climate change impacts on Mars, with data from orbiting spacecraft and rovers revealing a hemispheric dichotomy. In the Arctic, sea ice reduction is linked to inflows from the Pacific Ocean, while the Indian Ocean experiences decadal variability in its circulation. Scientists st...

SourceAmerican Geophysical Union·JournalGeophysical Research Letters·DateMay 31, 2006

AGU journal highlights - 16 March 2006

Scientists studied magma chamber pressure changes following a massive lava-dome collapse on Montserrat, finding an unprecedented increase in pressure. Another study revealed a simplified model of rock fracture dissolution, which predicts a power-law distribution of channel lengths. Additionally, researchers explored aerosol transport a...

SourceAmerican Geophysical Union·JournalGeophysical Research Letters·DateMar 16, 2006

Buried craters and underground ice

The MARSIS radar has provided direct information about Mars' deep subsurface, revealing buried impact craters and hints of underground water-ice. The radar's measurements have changed our perception of the Red Planet, adding a new dimension to its knowledge.

SourceEuropean Space Agency·JournalNature·DateNov 30, 2005