[meteorite-list] Curiosity Rover Findings Point to a More Earth-like Martian Past

From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Tue, 28 Jun 2016 12:03:58 -0700 (PDT)
Message-ID: <201606281903.u5SJ3wKF015948_at_zagami.jpl.nasa.gov>

http://www.jpl.nasa.gov/news/news.php?feature=6544

NASA Rover Findings Point to a More Earth-like Martian Past
Jet Propulsion Laboratory
June 27, 2016

Chemicals found in Martian rocks by NASA's Curiosity Mars rover suggest
the Red Planet once had more oxygen in its atmosphere than it does now.

Researchers found high levels of manganese oxides by using a laser-firing
instrument on the rover. This hint of more oxygen in Mars' early atmosphere
adds to other Curiosity findings -- such as evidence about ancient lakes
-- revealing how Earth-like our neighboring planet once was.

This research also adds important context to other clues about atmospheric
oxygen in Mars' past. The manganese oxides were found in mineral veins
within a geological setting the Curiosity mission has placed in a timeline
of ancient environmental conditions. From that context, the higher oxygen
level can be linked to a time when groundwater was present in the rover's
Gale Crater study area.

"The only ways on Earth that we know how to make these manganese materials
involve atmospheric oxygen or microbes," said Nina Lanza, a planetary
scientist at Los Alamos National Laboratory in New Mexico. "Now we're
seeing manganese oxides on Mars, and we're wondering how the heck these
could have formed?"

Microbes seem far-fetched at this point, but the other alternative --
that the Martian atmosphere contained more oxygen in the past than it
does now -- seems possible, Lanza said. "These high manganese materials
can't form without lots of liquid water and strongly oxidizing conditions.
Here on Earth, we had lots of water but no widespread deposits of manganese
oxides until after the oxygen levels in our atmosphere rose."

Lanza is the lead author of a new report about the Martian manganese oxides
in the American Geophysical Union's Geophysical Research Letters. She
uses Curiosity's Chemistry and Camera (ChemCam) instrument, which fires
laser pulses from atop the rover's mast and observes the spectrum of resulting
flashes of plasma to assess targets' chemical makeup.

In Earth's geological record, the appearance of high concentrations of
manganese oxide minerals is an important marker of a major shift in our
atmosphere's composition, from relatively low oxygen abundances to the
oxygen-rich atmosphere we see today. The presence of the same types of
materials on Mars suggests that oxygen levels rose there, too, before
declining to their present values. If that's the case, how was that oxygen-rich
environment formed?

"One potential way that oxygen could have gotten into the Martian atmosphere
is from the breakdown of water when Mars was losing its magnetic field,"
said Lanza. "It's thought that at this time in Mars' history, water was
much more abundant." Yet without a protective magnetic field to shield
the surface, ionizing radiation started splitting water molecules into
hydrogen and oxygen. Because of Mars' relatively low gravity, the planet
wasn't able to hold onto the very light hydrogen atoms, but the heavier
oxygen atoms remained behind. Much of this oxygen went into rocks, leading
to the rusty red dust that covers the surface today. While Mars' famous
red iron oxides require only a mildly oxidizing environment to form, manganese
oxides require a strongly oxidizing environment, more so than previously
known for Mars.

Lanza added, "It's hard to confirm whether this scenario for Martian atmospheric
oxygen actually occurred. But it's important to note that this idea represents
a departure in our understanding for how planetary atmospheres might become
oxygenated." Abundant atmospheric oxygen has been treated as a so-called
biosignature, or a sign of extant life, but this process does not require
life.

Curiosity has been investigating sites in Gale Crater since 2012. The
high-manganese materials it found are in mineral-filled cracks in sandstones
in the "Kimberley" region of the crater. But that's not the only place
on Mars where high manganese abundances have been found. NASA's Opportunity
rover, exploring Mars since 2004, also recently discovered high manganese
deposits thousands of miles from Curiosity. This supports the idea that
the conditions needed to form these materials were present well beyond
Gale Crater.

Los Alamos National Laboratory leads the U.S. and French team that jointly
developed and operates ChemCam. NASA's Jet Propulsion Laboratory, a division
of Caltech in Pasadena, California, built the rover and manages the Curiosity
mission for NASA's Science Mission Directorate, Washington.


News Media Contact

Guy Webster
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-6278
guy.webster at jpl.nasa.gov

Laura Mullane
Los Alamos National Laboratory, Los Alamos, N.M.
505-667-6012
mullane at lanl.gov

2016-161
Received on Tue 28 Jun 2016 03:03:58 PM PDT