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2016JG003439
2016JG003439
http://dx.doi.org/10.1002/2016JG003439
Oxalate formation under the hyperarid conditions of the Atacama desert as a mineral marker to provide clues to the source of organic carbon on Mars
P356
Q57859123-48F02B3E-65C7-46EE-9F11-4E04BA847E5B
P356
2016JG003439
http://dx.doi.org/10.1002/2016JG003439