{"id":9587,"date":"2025-04-18T14:59:04","date_gmt":"2025-04-18T18:59:04","guid":{"rendered":"https:\/\/spaceandplanetarynewswire.com\/?p=9587"},"modified":"2025-04-18T14:59:04","modified_gmt":"2025-04-18T18:59:04","slug":"new-study-unveils-volcanic-history-and-clues-to-ancient-life-on-mars","status":"publish","type":"post","link":"https:\/\/spaceandplanetarynewswire.com\/?p=9587","title":{"rendered":"New Study Unveils Volcanic History and Clues to Ancient Life on Mars"},"content":{"rendered":"<p><em><strong>The proof may be in the pudding, but according to a Texas A&amp;M University geologist, when it comes to ancient life on the Red Planet, the proof is in the rocks.<\/strong><\/em><\/p>\n<figure style=\"width: 700px\" class=\"wp-caption alignnone\"><img decoding=\"async\" class=\"size-medium\" src=\"https:\/\/mediasvc.eurekalert.org\/Api\/v1\/Multimedia\/7a886c5b-8fa4-4915-89cf-bd86540b2490\/Rendition\/low-res\/Content\/Public\" width=\"700\" height=\"459\"><figcaption class=\"wp-caption-text\">A mosaic of two pictures showing the rover arm after scanning and sampling one of the rocks discussed in the paper. The rock itself is in the lower right and clearly shows the hole where the sample was collected. The rock was given the informal name &#8220;Rochette&#8221; by the Perseverance science team.<\/figcaption><\/figure>\n<p>In a groundbreaking study co-authored by a Texas A&amp;M University scientist, researchers have revealed new insights into the geological history of Mars&#8217; Jezero Crater, the landing site of NASA\u2019s Perseverance rover. Their findings suggest that the crater&#8217;s floor is composed of a diverse array of iron-rich volcanic rocks, providing a window into the planet\u2019s distant past and the closest chance yet to uncover signs of ancient life.<\/p>\n<p>Research scientist&nbsp;<a href=\"https:\/\/artsci.tamu.edu\/geology-geophysics\/contact\/profiles\/michael-tice.html\">Dr. Michael Tice<\/a>, who studies geobiology and sedimentary geology in the Texas A&amp;M College of Arts and Sciences, is part of an international team exploring the surface of Mars. He and his co-authors published their findings in&nbsp;<a href=\"https:\/\/www.science.org\/doi\/full\/10.1126\/sciadv.adr2613?rfr_dat=cr_pub++0pubmed&amp;url_ver=Z39.88-2003&amp;rfr_id=ori%3Arid%3Acrossref.org\"><em>Science Advances<\/em><\/a><em>.<\/em><\/p>\n<p>\u201cBy analyzing these diverse volcanic rocks, we\u2019ve gained valuable insights into the processes that shaped this region of Mars,\u201d Tice said. \u201cThis enhances our understanding of the planet\u2019s geological history and its potential to have supported life.\u201d<\/p>\n<p><strong>Unlocking Mars\u2019 Secrets With Unrivaled Technology<\/strong><\/p>\n<p>Perseverance, NASA\u2019s most advanced robotic explorer, landed in the Jezero Crater on Feb. 18, 2021, as part of the&nbsp;<a href=\"https:\/\/science.nasa.gov\/mission\/mars-2020-perseverance\/\">Mars 2020 mission<\/a>\u2019s search for signs of ancient microbial life on the Red Planet. The rover is collecting core samples of Martian rock and regolith (broken rock and soil) for possible future analysis on Earth.<\/p>\n<p>Meanwhile, scientists like Tice are using the rover\u2019s high-tech tools to analyze Martian rocks to determine their chemical composition and detect compounds that could be signs of past life. The rover also has a high-resolution camera system that provides detailed images of rock texture and structures. But Tice said the technology is so advanced compared to that of past NASA rovers that they are gathering new information at unprecedented levels.<\/p>\n<p>&#8220;We\u2019re not just looking at pictures \u2014 we\u2019re getting detailed chemical data, mineral compositions and even microscopic textures,\u201d Tice said. \u201cIt\u2019s like having a mobile lab on another planet.&#8221;<\/p>\n<p>Tice and his co-authors analyzed the rock formations within the crater to better understand Mars&#8217; volcanic and hydrological history. The team used the Planetary Instrument for X-ray Lithochemistry (PIXL), an advanced spectrometer, to analyze the chemical composition and textures of rocks in the M\u00e1az formation, a key geological area within Jezero Crater. PIXL\u2019s high-resolution X-ray capabilities allow for unprecedented detail in studying the elements in the rocks.<\/p>\n<p>Tice noted the importance of the technology in revolutionizing Martian exploration. \u201cEvery rover that has ever gone to Mars has been a technological marvel, but this is the first time we\u2019ve been able to analyze rocks in such high resolution using X-ray fluorescence. It has completely changed the way we think about the history of rocks on Mars,\u201d he said.<\/p>\n<p><strong>What The Rocks Reveal<\/strong><\/p>\n<p>The team\u2019s analysis revealed two distinct types of volcanic rocks. The first type, dark-toned and rich in iron and magnesium, contains intergrown minerals such as pyroxene and plagioclase feldspar, with evidence of altered olivine. The second type, a lighter-toned rock classified as trachy-andesite, includes plagioclase crystals within a potassium-rich groundmass. These findings indicate a complex volcanic history involving multiple lava flows with varying compositions.<\/p>\n<p>To determine how these rocks formed, researchers conducted thermodynamic modeling \u2014 a method that simulates the conditions under which the minerals solidified. Their results suggest that the unique compositions resulted from high-degree fractional crystallization, a process where different minerals separate from molten rock as it cools. They also found signs that the lava may have mixed with iron-rich material from Mars&#8217; crust, changing the rocks&#8217; composition even more.<\/p>\n<p>\u201cThe processes we see here \u2014 fractional crystallization and crustal assimilation \u2014 happen in active volcanic systems on Earth,\u201d said Tice. \u201cIt suggests that this part of Mars may have had prolonged volcanic activity, which in turn could have provided a sustained source for different compounds used by life.\u201d<\/p>\n<p>This discovery is crucial for understanding Mars&#8217; potential habitability. If Mars had an active volcanic system for an extended period, it might have also maintained conditions suitable for life for long portions of Mars\u2019 early history.<\/p>\n<p>\u201cWe\u2019ve carefully selected these rocks because they contain clues to Mars\u2019 past environments,\u201d Tice said. \u201cWhen we get them back to Earth and can analyze them with laboratory instruments, we\u2019ll be able to ask much more detailed questions about their history and potential biological signatures.\u201d<\/p>\n<p>The&nbsp;<a href=\"https:\/\/science.nasa.gov\/mission\/mars-sample-return\/\">Mars Sample Return mission<\/a>, a collaborative effort between NASA and the European Space Agency, aims to bring the samples back within the next decade. Once on Earth, scientists will have access to more advanced laboratory techniques to analyze them in greater detail.<\/p>\n<p>Tice said that given the astounding level of technology on Perseverance, more discoveries are ahead. \u201cSome of the most exciting work is still ahead of us. This study is just the beginning. We&#8217;re seeing things that we never expected, and I think in the next few years, we\u2019ll be able to refine our understanding of Mars\u2019 geological history in ways we never imagined.\u201d<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The proof may be in the pudding, but according to a Texas A&amp;M University geologist, when it comes to ancient life on the Red Planet, the proof is in the rocks. In a groundbreaking study co-authored by a Texas A&amp;M University scientist, researchers have revealed new insights into the geological history of Mars&#8217; Jezero Crater,&hellip;<\/p>\n","protected":false},"author":71,"featured_media":9588,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"ngg_post_thumbnail":0,"fifu_image_url":"https:\/\/mediasvc.eurekalert.org\/Api\/v1\/Multimedia\/7a886c5b-8fa4-4915-89cf-bd86540b2490\/Rendition\/low-res\/Content\/Public","fifu_image_alt":"","footnotes":""},"categories":[216],"tags":[],"class_list":["post-9587","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-discovery"],"_links":{"self":[{"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/posts\/9587","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/users\/71"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=9587"}],"version-history":[{"count":1,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/posts\/9587\/revisions"}],"predecessor-version":[{"id":9589,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/posts\/9587\/revisions\/9589"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=\/wp\/v2\/media\/9588"}],"wp:attachment":[{"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=9587"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=9587"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceandplanetarynewswire.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=9587"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}