{"@context":"https://schema.org","@type":"ScholarlyArticle","headline":"Martian dunes indicative of wind regime shift in line with end of ice age.","author":[{"@type":"Person","name":"Jianjun Liu"},{"@type":"Person","name":"Xiaoguang Qin"},{"@type":"Person","name":"Xin Ren"},{"@type":"Person","name":"Xu Wang"},{"@type":"Person","name":"Yong Sun"},{"@type":"Person","name":"Xingguo Zeng"},{"@type":"Person","name":"Haibin Wu"},{"@type":"Person","name":"Zhaopeng Chen"},{"@type":"Person","name":"Wangli Chen"},{"@type":"Person","name":"Yuan Chen"},{"@type":"Person","name":"Cheng Wang"},{"@type":"Person","name":"Zezhou Sun"},{"@type":"Person","name":"Rongqiao Zhang"},{"@type":"Person","name":"Ziyuan Ouyang"},{"@type":"Person","name":"Zhengtang Guo"},{"@type":"Person","name":"James W Head"},{"@type":"Person","name":"Chunlai Li"}],"datePublished":"2023","isPartOf":{"@type":"Periodical","name":"Nature"},"identifier":"https://doi.org/10.1038/s41586-023-06206-1","description":"AbstractOrbital observations suggest that Mars underwent a recent ‘ice age’ (roughly 0.4–2.1 million years ago), during which a latitude-dependent ice-dust mantle (LDM)1,2was emplaced. A subsequent decrease in obliquity amplitude resulted in the emergence of an ‘interglacial period’1,3during which the lowermost latitude LDM ice4–6was etched and removed, returning it to the polar cap. These observations are consistent with polar cap stratigraphy1,7, but lower- to mid-latitude in situ surface observations in support of a glacial–interglacial transition that can be reconciled with mesoscale and global atmospheric circulation models8is lacking. Here we present a suite of measurements obtained by the Zhurong rover during its traverse across the southern LDM region in Utopia Planitia, Mars. We find evidence for a stratigraphic sequence involving initial barchan dune formation, indicative of north-easterly winds, cementation of dune sediments, followed by their erosion by north-westerly winds, eroding the barchan dunes and producing distinctive longitudinal dunes, with the transition in wind regime consistent with the end of the ice age. The results are compatible with the Martian polar stratigraphic record and will help improve our understanding of the ancient climate history of Mars9.","url":"https://innscience.ca/en/community/literature/f4275b84-d5f3-4111-8310-45a172367f2d"}