| Literature DB >> 30971829 |
Oleg Korablev1, Ann Carine Vandaele2, Franck Montmessin3, Anna A Fedorova4, Alexander Trokhimovskiy4, François Forget5, Franck Lefèvre3, Frank Daerden2, Ian R Thomas2, Loïc Trompet2, Justin T Erwin2, Shohei Aoki2, Séverine Robert2, Lori Neary2, Sébastien Viscardy2, Alexey V Grigoriev4, Nikolay I Ignatiev4, Alexey Shakun4, Andrey Patrakeev4, Denis A Belyaev4, Jean-Loup Bertaux4,3, Kevin S Olsen3, Lucio Baggio3, Juan Alday6, Yuriy S Ivanov7, Bojan Ristic2, Jon Mason8, Yannick Willame2, Cédric Depiesse2, Laszlo Hetey2, Sophie Berkenbosch2, Roland Clairquin2, Claudio Queirolo2, Bram Beeckman2, Eddy Neefs2, Manish R Patel8, Giancarlo Bellucci9, Jose-Juan López-Moreno10, Colin F Wilson6, Giuseppe Etiope9,11,12, Lev Zelenyi4, Håkan Svedhem13, Jorge L Vago13.
Abstract
The detection of methane on Mars has been interpreted as indicating that geochemical or biotic activities could persist on Mars today1. A number of different measurements of methane show evidence of transient, locally elevated methane concentrations and seasonal variations in background methane concentrations2-5. These measurements, however, are difficult to reconcile with our current understanding of the chemistry and physics of the Martian atmosphere6,7, which-given methane's lifetime of several centuries-predicts an even, well mixed distribution of methane1,6,8. Here we report highly sensitive measurements of the atmosphere of Mars in an attempt to detect methane, using the ACS and NOMAD instruments onboard the ESA-Roscosmos ExoMars Trace Gas Orbiter from April to August 2018. We did not detect any methane over a range of latitudes in both hemispheres, obtaining an upper limit for methane of about 0.05 parts per billion by volume, which is 10 to 100 times lower than previously reported positive detections2,4. We suggest that reconciliation between the present findings and the background methane concentrations found in the Gale crater4 would require an unknown process that can rapidly remove or sequester methane from the lower atmosphere before it spreads globally.Entities:
Year: 2019 PMID: 30971829 DOI: 10.1038/s41586-019-1096-4
Source DB: PubMed Journal: Nature ISSN: 0028-0836 Impact factor: 49.962