Martian slope streaks as plausible indicators of transient water activity

Abstract Slope streaks have been frequently observed in the equatorial, low thermal inertia and dusty regions of Mars. The reason behind their formation remains unclear with proposed hypotheses for both dry and wet mechanisms. Here, we report an up-to-date distribution and morphometric investigation...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Anshuman Bhardwaj, Lydia Sam, F. Javier Martín-Torres, María-Paz Zorzano, Ricardo M. Fonseca
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
Materias:
R
Q
Acceso en línea:https://doaj.org/article/dbda4fb90d61409fb6241c67da00c0a1
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:dbda4fb90d61409fb6241c67da00c0a1
record_format dspace
spelling oai:doaj.org-article:dbda4fb90d61409fb6241c67da00c0a12021-12-02T15:06:18ZMartian slope streaks as plausible indicators of transient water activity10.1038/s41598-017-07453-92045-2322https://doaj.org/article/dbda4fb90d61409fb6241c67da00c0a12017-08-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-07453-9https://doaj.org/toc/2045-2322Abstract Slope streaks have been frequently observed in the equatorial, low thermal inertia and dusty regions of Mars. The reason behind their formation remains unclear with proposed hypotheses for both dry and wet mechanisms. Here, we report an up-to-date distribution and morphometric investigation of Martian slope streaks. We find: (i) a remarkable coexistence of the slope streak distribution with the regions on Mars with high abundances of water-equivalent hydrogen, chlorine, and iron; (ii) favourable thermodynamic conditions for transient deliquescence and brine development in the slope streak regions; (iii) a significant concurrence of slope streak distribution with the regions of enhanced atmospheric water vapour concentration, thus suggestive of a present-day regolith-atmosphere water cycle; and (iv) terrain preferences and flow patterns supporting a wet mechanism for slope streaks. These results suggest a strong local regolith-atmosphere water coupling in the slope streak regions that leads to the formation of these fluidised features. Our conclusions can have profound astrobiological, habitability, environmental, and planetary protection implications.Anshuman BhardwajLydia SamF. Javier Martín-TorresMaría-Paz ZorzanoRicardo M. FonsecaNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-14 (2017)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Anshuman Bhardwaj
Lydia Sam
F. Javier Martín-Torres
María-Paz Zorzano
Ricardo M. Fonseca
Martian slope streaks as plausible indicators of transient water activity
description Abstract Slope streaks have been frequently observed in the equatorial, low thermal inertia and dusty regions of Mars. The reason behind their formation remains unclear with proposed hypotheses for both dry and wet mechanisms. Here, we report an up-to-date distribution and morphometric investigation of Martian slope streaks. We find: (i) a remarkable coexistence of the slope streak distribution with the regions on Mars with high abundances of water-equivalent hydrogen, chlorine, and iron; (ii) favourable thermodynamic conditions for transient deliquescence and brine development in the slope streak regions; (iii) a significant concurrence of slope streak distribution with the regions of enhanced atmospheric water vapour concentration, thus suggestive of a present-day regolith-atmosphere water cycle; and (iv) terrain preferences and flow patterns supporting a wet mechanism for slope streaks. These results suggest a strong local regolith-atmosphere water coupling in the slope streak regions that leads to the formation of these fluidised features. Our conclusions can have profound astrobiological, habitability, environmental, and planetary protection implications.
format article
author Anshuman Bhardwaj
Lydia Sam
F. Javier Martín-Torres
María-Paz Zorzano
Ricardo M. Fonseca
author_facet Anshuman Bhardwaj
Lydia Sam
F. Javier Martín-Torres
María-Paz Zorzano
Ricardo M. Fonseca
author_sort Anshuman Bhardwaj
title Martian slope streaks as plausible indicators of transient water activity
title_short Martian slope streaks as plausible indicators of transient water activity
title_full Martian slope streaks as plausible indicators of transient water activity
title_fullStr Martian slope streaks as plausible indicators of transient water activity
title_full_unstemmed Martian slope streaks as plausible indicators of transient water activity
title_sort martian slope streaks as plausible indicators of transient water activity
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/dbda4fb90d61409fb6241c67da00c0a1
work_keys_str_mv AT anshumanbhardwaj martianslopestreaksasplausibleindicatorsoftransientwateractivity
AT lydiasam martianslopestreaksasplausibleindicatorsoftransientwateractivity
AT fjaviermartintorres martianslopestreaksasplausibleindicatorsoftransientwateractivity
AT mariapazzorzano martianslopestreaksasplausibleindicatorsoftransientwateractivity
AT ricardomfonseca martianslopestreaksasplausibleindicatorsoftransientwateractivity
_version_ 1718388546804383744