Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale

Gale Crater on Mars has been demonstrated to have once hosted water, but its chemistry is still under debate. Here the authors use mineralogical rock compositions and show the once saline character of Gale Crater—a result of warmer climate periods during the Hesperian period.

Guardado en:

Detalles Bibliográficos
Autores principales:	Keisuke Fukushi, Yasuhito Sekine, Hiroshi Sakuma, Koki Morida, Robin Wordsworth
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/366a18d70a044a16aea4f6cd62882998
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:366a18d70a044a16aea4f6cd62882998
record_format	dspace
spelling	oai:doaj.org-article:366a18d70a044a16aea4f6cd628829982021-12-02T16:57:09ZSemiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale10.1038/s41467-019-12871-62041-1723https://doaj.org/article/366a18d70a044a16aea4f6cd628829982019-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-12871-6https://doaj.org/toc/2041-1723Gale Crater on Mars has been demonstrated to have once hosted water, but its chemistry is still under debate. Here the authors use mineralogical rock compositions and show the once saline character of Gale Crater—a result of warmer climate periods during the Hesperian period.Keisuke FukushiYasuhito SekineHiroshi SakumaKoki MoridaRobin WordsworthNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-11 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Keisuke Fukushi Yasuhito Sekine Hiroshi Sakuma Koki Morida Robin Wordsworth Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale
description	Gale Crater on Mars has been demonstrated to have once hosted water, but its chemistry is still under debate. Here the authors use mineralogical rock compositions and show the once saline character of Gale Crater—a result of warmer climate periods during the Hesperian period.
format	article
author	Keisuke Fukushi Yasuhito Sekine Hiroshi Sakuma Koki Morida Robin Wordsworth
author_facet	Keisuke Fukushi Yasuhito Sekine Hiroshi Sakuma Koki Morida Robin Wordsworth
author_sort	Keisuke Fukushi
title	Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale
title_short	Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale
title_full	Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale
title_fullStr	Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale
title_full_unstemmed	Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale
title_sort	semiarid climate and hyposaline lake on early mars inferred from reconstructed water chemistry at gale
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/366a18d70a044a16aea4f6cd62882998
work_keys_str_mv	AT keisukefukushi semiaridclimateandhyposalinelakeonearlymarsinferredfromreconstructedwaterchemistryatgale AT yasuhitosekine semiaridclimateandhyposalinelakeonearlymarsinferredfromreconstructedwaterchemistryatgale AT hiroshisakuma semiaridclimateandhyposalinelakeonearlymarsinferredfromreconstructedwaterchemistryatgale AT kokimorida semiaridclimateandhyposalinelakeonearlymarsinferredfromreconstructedwaterchemistryatgale AT robinwordsworth semiaridclimateandhyposalinelakeonearlymarsinferredfromreconstructedwaterchemistryatgale
_version_	1718382617317867520

Semiarid climate and hyposaline lake on early Mars inferred from reconstructed water chemistry at Gale

Ejemplares similares