{"id":101027,"date":"2026-04-22T16:36:24","date_gmt":"2026-04-22T20:36:24","guid":{"rendered":"https:\/\/carleton.ca\/news\/?post_type=cu_story&#038;p=101027"},"modified":"2026-04-22T16:36:25","modified_gmt":"2026-04-22T20:36:25","slug":"curiosity-rover-mars-life","status":"publish","type":"cu_story","link":"https:\/\/carleton.ca\/news\/story\/curiosity-rover-mars-life\/","title":{"rendered":"Did NASA&#8217;s Curiosity Rover Find Signs of Ancient Life on Mars? An Astrobiologist Explains How We Determine &#8216;Life&#8217;"},"content":{"rendered":"\n<section class=\"w-screen px-6 cu-section cu-section--white ml-offset-center md:px-8 lg:px-14\">\n    <div class=\"space-y-6 cu-max-w-child-max  md:space-y-10 cu-prose-first-last\">\n\n        \n                    \n                    \n            \n    <div class=\"cu-wideimage relative flex items-center justify-center mx-auto px-8 overflow-hidden md:px-16 rounded-xl not-prose  my-6 md:my-12 first:mt-0 bg-opacity-50 bg-cover bg-cu-black-50 pt-24 pb-32 md:pt-28 md:pb-44 lg:pt-36 lg:pb-60 xl:pt-48 xl:pb-72\" style=\"background-image: url(https:\/\/carleton.ca\/news\/wp-content\/uploads\/sites\/162\/2026\/04\/mars-rover-1920x1080-1-1024x576.jpg); background-position: 49% 42%;\">\n\n                    <div class=\"absolute top-0 w-full h-screen\" style=\"background-color:rgba(0,0,0,0.600);\"><\/div>\n        \n        <div class=\"relative z-[2] max-w-4xl w-full flex flex-col items-center gap-2 cu-wideimage-image cu-zero-first-last\">\n            <header class=\"mx-auto mb-6 text-center text-white cu-pageheader cu-component-updated cu-pageheader--center md:mb-12\">\n\n                                    <h1 class=\"cu-prose-first-last font-semibold mb-2 text-3xl md:text-4xl lg:text-5xl lg:leading-[3.5rem] cu-pageheader--center text-center mx-auto after:left-px\">\n                        Did NASA&#8217;s Curiosity Rover Find Signs of Ancient Life on Mars? An Astrobiologist Explains How We Determine &#8216;Life&#8217;\n                    <\/h1>\n                \n                            <\/header>\n        <\/div>\n\n                    <svg xmlns=\"http:\/\/www.w3.org\/2000\/svg\" class=\"absolute bottom-0 w-full z-[1]\" fill=\"none\" viewbox=\"0 0 1280 312\">\n                <path fill=\"#fff\" d=\"M26.412 315.608c-.602-.268-6.655-2.412-13.524-4.769a1943.84 1943.84 0 0 1-14.682-5.144l-2.276-.858v-5.358c0-4.876.086-5.358.773-5.09 1.674.643 21.38 5.84 34.646 9.109 14.682 3.59 28.935 6.858 45.936 10.449l9.874 2.089H57.322c-16.4 0-30.31-.16-30.91-.428ZM460.019 315.233c42.974-10.074 75.602-19.88 132.443-39.867 76.16-26.791 152.063-57.709 222.385-90.663 16.7-7.823 21.336-10.074 44.262-21.273 85.004-41.688 134.719-64.193 195.291-88.413 66.55-26.577 145.2-53.584 194.27-66.765C1258.5 5.626 1281.34 0 1282.24 0c.17 0 .34 27.596.34 61.3v61.299l-2.23.375c-84.7 13.718-165.93 35.955-310.736 84.931-46.494 15.753-65.427 22.076-96.166 32.15-9.102 3-24.814 8.198-34.989 11.574-107.543 35.954-153.008 50.422-196.626 62.639l-6.74 1.876-89.126-.054c-78.135-.054-88.782-.161-85.948-.857ZM729.628 312.875c33.229-10.985 69.248-23.523 127.506-44.207 118.705-42.223 164.596-57.709 217.446-73.302 2.62-.75 8.29-2.465 12.67-3.751 56.19-16.772 126.94-33.597 184.17-43.671 5.07-.91 9.66-1.768 10.22-1.875l.94-.161v170.236l-281.28-.054H719.968l9.66-3.215ZM246.864 313.411c-65.041-2.251-143.047-12.11-208.432-26.256-18.375-3.965-41.73-9.538-42.202-10.074-.171-.214-.257-21.38-.214-47.046l.129-46.618 6.654 3.697c57.313 32.043 118.491 56.531 197.699 79.143 40.313 11.521 83.459 18.058 138.669 21.059 15.584.857 65.685.857 81.14 0 33.744-1.876 61.306-4.93 88.396-9.806 6.396-1.126 11.634-1.983 11.722-1.929.255.375-20.48 7.769-30.999 11.038-28.592 8.948-59.288 15.646-91.873 20.147-26.36 3.59-50.015 5.627-78.35 6.698-15.584.59-55.209.59-72.339-.053Z\"><\/path>\n                <path fill=\"#fff\" d=\"M-3.066 295.067 32.06 304.1v9.033H-3.066v-18.066Z\"><\/path>\n            <\/svg>\n            <\/div>\n\n    \n\n    <\/div>\n<\/section>\n\n\n\n<p>NASA&#8217;s <a href=\"https:\/\/www.nasa.gov\/missions\/mars-science-laboratory\/curiosity-rover\/nasas-curiosity-finds-organic-molecules-never-seen-before-on-mars\/\" target=\"_blank\" rel=\"noreferrer noopener\">Curiosity rover has identified seven new organic compounds on the planet Mars<\/a>, according to new research published in <em>Nature Communications<\/em>.<\/p>\n\n\n\n<p>The researchers believe this <a href=\"https:\/\/doi.org\/10.1038\/s41467-026-70656-0\" target=\"_blank\" rel=\"noreferrer noopener\">organic matter may have been preserved on Mars for more than 3.4 billion years<\/a>. But is it evidence of life?<\/p>\n\n\n\n<p>It&#8217;s not yet possible to determine whether it was delivered by a meteor (or comet or interplanetary dust particles), was formed through geological processes or <a href=\"https:\/\/www.cbc.ca\/news\/science\/nasa-mars-curiosity-rover-life-organic-compounds-9.7172210\" target=\"_blank\" rel=\"noreferrer noopener\">may be linked to potential ancient life on Mars<\/a>.<\/p>\n\n\n\n<p>This begs a few questions: What exactly is life? How do we know what to look for? Why is it so hard to determine if an organic compound came from life or not?<\/p>\n\n\n\n<p>As an astrobiologist, <a href=\"https:\/\/carleton.ca\/biology\/people\/allyson-brady\/\" target=\"_blank\" rel=\"noreferrer noopener\">my job is to study life in the universe<\/a>. I have participated in several NASA and Canadian Space Agency (CSA) projects focused on learning how to detect signs of life, as well as <a href=\"https:\/\/www.cbc.ca\/news\/science\/astronauts-explore-space-science-in-b-c-lake-1.968849\" target=\"_blank\" rel=\"noreferrer noopener\">training astronauts to be field scientists<\/a>.<\/p>\n\n\n\n<p>This has taken me to field sites in the <a href=\"https:\/\/doi.org\/10.1007\/s10533-023-01053-8\" target=\"_blank\" rel=\"noreferrer noopener\">Antarctic<\/a>, <a href=\"https:\/\/doi.org\/10.1038\/ismej.2013.237\" target=\"_blank\" rel=\"noreferrer noopener\">hot springs in Western Canada<\/a>, <a href=\"https:\/\/doi.org\/10.1089\/ast.2018.1850\" target=\"_blank\" rel=\"noreferrer noopener\">volcanoes in Hawaii<\/a> and <a href=\"https:\/\/youtu.be\/qMo17RzYdig\" target=\"_blank\" rel=\"noreferrer noopener\">underwater in British Columbia<\/a>.<\/p>\n\n\n\n<p>The study of extreme environments on Earth, along with <a href=\"https:\/\/www.nasa.gov\/humans-in-space\/artemis-ii-science\/\" target=\"_blank\" rel=\"noreferrer noopener\">exploration of the lifeless surface of the moon<\/a>, can help us understand what life can look like. It can also help us understand the other potential non-biological processes that can form organic compounds like ones that have been found on Mars.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter\"><a href=\"https:\/\/images.theconversation.com\/files\/731749\/original\/file-20260422-57-nmgh29.jpg?ixlib=rb-4.1.0&amp;q=45&amp;auto=format&amp;w=1000&amp;fit=clip\" target=\"_blank\" rel=\"noreferrer noopener\"><img decoding=\"async\" src=\"https:\/\/images.theconversation.com\/files\/731749\/original\/file-20260422-57-nmgh29.jpg?ixlib=rb-4.1.0&amp;q=45&amp;auto=format&amp;w=754&amp;fit=clip\" alt=\"Astronaut diving in Pavilion Lake to study microbialites, supporting Curiosity rover Mars life research.\"\/><\/a><figcaption class=\"wp-element-caption\">Astronaut Chris Hadfield dives into Pavilion Lake, B.C., as part of an international, multidisciplinary project to explore the origin of rare freshwater carbonate rock formations (microbialites). Similar processes possibly occurred on other planets. (CSA\/Donnie Reid)<\/figcaption><\/figure>\n\n\n\n<h2 id=\"life-in-extreme-environments-on-earth\" class=\"wp-block-heading has-text-align-center\">Life in extreme environments on Earth<\/h2>\n\n\n\n<p>On Earth, scientists study life in extreme environments that we might also expect to find on early Earth or other planets such as Mars. We call these \u201canalogue\u201d environments.<\/p>\n\n\n\n<p>For example, micro-organisms can thrive in <a href=\"https:\/\/doi.org\/10.1038\/s41598-022-22047-w\" target=\"_blank\" rel=\"noreferrer noopener\">the hot springs<\/a> of Yellowstone National Park, <a href=\"https:\/\/doi.org\/10.1111\/1751-7915.70286\" target=\"_blank\" rel=\"noreferrer noopener\">deep underground<\/a> or in <a href=\"https:\/\/doi.org\/10.1007\/s10533-023-01053-8\" target=\"_blank\" rel=\"noreferrer noopener\">cold icy places like Antarctica<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter\"><img decoding=\"async\" src=\"https:\/\/images.theconversation.com\/files\/731514\/original\/file-20260421-71-gtoro2.jpg?ixlib=rb-4.1.0&amp;q=45&amp;auto=format&amp;w=754&amp;fit=clip\" alt=\"Two people in red snow coats on a frozen lake with deep blue sky in the background.\"\/><figcaption class=\"wp-element-caption\">The author (left) collects water samples from Lake Untersee for a biosignature study. This is one of Antarctica&#8217;s largest and deepest surface lakes, known for its distinctive water chemistry. (Klemens Weisleitner)<\/figcaption><\/figure>\n\n\n\n<p>As astrobiologists, we can use these analogue environments to <a href=\"https:\/\/www.nasa.gov\/analog-missions\/\" target=\"_blank\" rel=\"noreferrer noopener\">test equipment and concepts of operation<\/a> that may be used to plan life-detection missions on other planets. They also help us better understand how life can survive in extreme environments.<\/p>\n\n\n\n<p>Importantly, these environments help us recognize what kinds of evidence life can leave behind. Identifying biosignatures, or unambiguous signs of life, that can be targeted when looking for life elsewhere is critically important.<\/p>\n\n\n\n<p>On Earth, it&#8217;s not hard to find evidence of life. Simply look around you. We are also constantly discovering the existence of life in places where it may have once seemed impossible, such as these microbes buried deep in ocean mud.<\/p>\n\n\n\n<p>In fact, finding locations where there is no life is often more challenging.<\/p>\n\n\n\n<figure class=\"wp-block-embed is-type-video is-provider-youtube wp-block-embed-youtube wp-embed-aspect-16-9 wp-has-aspect-ratio\"><div class=\"wp-block-embed__wrapper\">\n<iframe loading=\"lazy\" title=\"This deep-sea mystery is changing our understanding of life | Karen Lloyd\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/PbgB2TaYhio?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe>\n<\/div><\/figure>\n\n\n\n<h2 id=\"what-is-not-a-sign-of-life\" class=\"wp-block-heading has-text-align-center\">What is <em>not<\/em> a sign of life?<\/h2>\n\n\n\n<p>The moon does not contain life. Unlike Mars, <a href=\"https:\/\/www.seti.org\/news\/new-discoveries-on-mars-and-habitability\/\" target=\"_blank\" rel=\"noreferrer noopener\">where there&#8217;s mounting evidence of a warmer watery past<\/a>, as far as we know there&#8217;s little evidence to suggest the moon ever had the right conditions to support life.<\/p>\n\n\n\n<p>The moon is a valuable study site for astrobiology because it offers clues about what is <em>not<\/em> a sign of life. The moon is constantly being hit by objects such as meteorites and asteroids, objects that would have also hit early Earth and Mars, leaving visible craters on the surface.<\/p>\n\n\n\n<p><a href=\"https:\/\/doi.org\/10.1038\/s41598-023-33595-0\" target=\"_blank\" rel=\"noreferrer noopener\">Meteorites can contain organic molecules<\/a> such as amino acids and hydrocarbons that look very much like ones we would expect to be left behind by living organisms.<\/p>\n\n\n\n<p>Micro-organisms, just like your own cells, contain lipids, proteins and nucleic acids. When they die, their organic molecules can become trapped in material such as <a href=\"https:\/\/doi.org\/10.1177\/15311074251366268\" target=\"_blank\" rel=\"noreferrer noopener\">sediments<\/a> or <a href=\"https:\/\/doi.org\/10.1089\/ast.2024.0020\" target=\"_blank\" rel=\"noreferrer noopener\">minerals<\/a>, and in some cases, preserved over long periods of time. Even if somewhat degraded, they might survive over millions or even billions of years in a recognizable form even if life itself is no longer present.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter\"><img decoding=\"async\" src=\"https:\/\/images.theconversation.com\/files\/731516\/original\/file-20260421-85-wspcb1.jpg?ixlib=rb-4.1.0&amp;q=45&amp;auto=format&amp;w=754&amp;fit=clip\" alt=\"A closeup view of the moon's cratered surface, grey in colour.\"\/><figcaption class=\"wp-element-caption\">A closeup view taken by the Artemis II crew of Vavilov Crater, on the rim of the older and larger Hertzsprung basin, on the surface of the moon. (NASA)<\/figcaption><\/figure>\n\n\n\n<p>But life is not the only way organic molecules can form. Some <a href=\"https:\/\/doi.org\/10.1029\/98JE02142\" target=\"_blank\" rel=\"noreferrer noopener\">abiotic chemical reactions can produce organic molecules<\/a> with no life required. These abiotic processes can lead to the formation of simple organic molecules, <a href=\"https:\/\/doi.org\/10.1038\/s41467-020-20038-x\" target=\"_blank\" rel=\"noreferrer noopener\">life&#8217;s building blocks<\/a>, that form the basis of more complex components.<\/p>\n\n\n\n<p>Reports of <a href=\"https:\/\/doi.org\/10.1089\/ast.2018.1917\" target=\"_blank\" rel=\"noreferrer noopener\">gases such as methane<\/a> or the <a href=\"https:\/\/doi.org\/10.1177\/15311074261417879\" target=\"_blank\" rel=\"noreferrer noopener\">detection of hydrocarbons<\/a> on Mars could be related to life. However, scientists know that there are other ways these could have formed. As with the <a href=\"https:\/\/www.theguardian.com\/science\/2026\/apr\/21\/nasa-curiosity-rover-finds-organic-molecules-mars\" target=\"_blank\" rel=\"noreferrer noopener\">compounds discovered by NASA&#8217;s Curiosity rover<\/a>, they may not readily meet the biosignature criteria of being unambiguously biological.<\/p>\n\n\n\n<p>It&#8217;s not easy to decide <a href=\"https:\/\/doi.org\/10.1093\/pnasnexus\/pgaf334\" target=\"_blank\" rel=\"noreferrer noopener\">what is a biosignature and what might have an alternative explanation<\/a>. Studying other locations or materials without life can help.<\/p>\n\n\n\n<p>Analysis of samples brought back to Earth from the <a href=\"https:\/\/www.nasa.gov\/missions\/osiris-rex\/sugars-gum-stardust-found-in-nasas-asteroid-bennu-samples\/\" target=\"_blank\" rel=\"noreferrer noopener\">asteroid Bennu in 2023 found organics such as sugars, including ribose<\/a>, for example. Ribose is a component of RNA. This does not mean that there is life on Bennu, instead it shows that these biologically important molecules may be widely distributed in the solar system.<\/p>\n\n\n\n<p>These kinds of investigations tell us that there are some organics that may not make good biosignatures because there is an alternative non-biological explanation.<\/p>\n\n\n\n<h2 id=\"from-the-moon-to-mars\" class=\"wp-block-heading has-text-align-center\">From the moon to Mars<\/h2>\n\n\n\n<p>Exploration of the moon helps create an inventory of organic molecules that, while often associated with life, also have another explanation. They may have been delivered by a meteorite and been preserved all this time.<\/p>\n\n\n\n<p>For example, studies of lunar regolith \u2014 the dusty moon version of soil \u2014 brought back from the <a href=\"https:\/\/doi.org\/10.1029\/2023JE008133\" target=\"_blank\" rel=\"noreferrer noopener\">Apollo missions<\/a> and from <a href=\"https:\/\/doi.org\/10.1126\/sciadv.aed4951\" target=\"_blank\" rel=\"noreferrer noopener\">recent Chinese-led missions<\/a> have identified organic molecules such as amino acids, ketones and amines. If these same organics are found on other planets, it means that they are not necessarily signs of life. At least, not on their own.<\/p>\n\n\n\n<p>Prior to NASA&#8217;s recent Artemis II mission, astronauts, including Canadian Jeremy Hansen, underwent <a href=\"https:\/\/www.asc-csa.gc.ca\/eng\/astronauts\/about-the-job\/space-mission-simulations\/training-in-geology.asp\" target=\"_blank\" rel=\"noreferrer noopener\">geology training at sites like the Kamestastin Lake impact structure in Labrador<\/a>. This training prepared them to make detailed <a href=\"https:\/\/theconversation.com\/how-the-artemis-ii-crew-trained-to-observe-and-photograph-the-moon-a-nasa-science-team-geologist-explains-279829\" target=\"_blank\" rel=\"noreferrer noopener\">geological observations of the moon<\/a>.<\/p>\n\n\n\n<figure class=\"wp-block-image aligncenter\"><a href=\"https:\/\/images.theconversation.com\/files\/731524\/original\/file-20260422-57-nsi3b1.jpg?ixlib=rb-4.1.0&amp;q=45&amp;auto=format&amp;w=1000&amp;fit=clip\" target=\"_blank\" rel=\"noreferrer noopener\"><img decoding=\"async\" src=\"https:\/\/images.theconversation.com\/files\/731524\/original\/file-20260422-57-nsi3b1.jpg?ixlib=rb-4.1.0&amp;q=45&amp;auto=format&amp;w=754&amp;fit=clip\" alt=\"Artemis II crew Victor Glover, Reid Wiseman and Jeremy Hansen huddle around a camera in the Orion spacecraft.\"\/><\/a><figcaption class=\"wp-element-caption\">Artemis II crew Victor Glover, Reid Wiseman and Jeremy Hansen configure their camera equipment shortly before beginning their lunar flyby observations, April 2026. (NASA)<\/figcaption><\/figure>\n\n\n\n<p>These geological features might play a role in the preservation of organics, possibly shielding them from high temperatures and destructive radiation, sort of like a fridge. Similar features on Mars may then be good targets for astrobiology investigations.<\/p>\n\n\n\n<p>With a <a href=\"https:\/\/www.nasa.gov\/mission\/artemis-iv\/\" target=\"_blank\" rel=\"noreferrer noopener\">2028 moon landing planned for NASA&#8217;s Artemis IV mission<\/a>, we will soon have even more lunar material to study. These missions are critical for helping astrobiologists fine-tune those unambiguous signs of life that we can then search for when we get to Mars.<\/p>\n\n\n\n<p>As NASA&#8217;s <a href=\"https:\/\/science.nasa.gov\/mission\/msl-curiosity\/science\/\" target=\"_blank\" rel=\"noreferrer noopener\">Curiosity<\/a> and <a href=\"https:\/\/science.nasa.gov\/mission\/mars-2020-perseverance\/\" target=\"_blank\" rel=\"noreferrer noopener\">Perseverance<\/a> rovers continue exploring Mars, and new missions are planned, in the future we may be able to more confidently answer the question of <em>is it life?<\/em><\/p>\n\n\n\n<p>\u2013<br><em class=\"myprefix-text-italic\"><a href=\"https:\/\/carleton.ca\/biology\/people\/allyson-brady\/\" target=\"_blank\" rel=\"noreferrer noopener\">Allyson Brady<\/a>\u00a0is an assistant professor in biology at Carleton University.<\/em><\/p>\n\n\n\n<p><em class=\"myprefix-text-italic\">This article is\u00a0<a href=\"https:\/\/theconversation.com\/did-nasas-curiosity-rover-find-signs-of-ancient-life-on-mars-an-astrobiologist-explains-how-we-determine-life-280658\" target=\"_blank\" rel=\"noreferrer noopener\">republished<\/a>\u00a0from The Conversation under a Creative Commons licence. All photos provided by\u00a0<a href=\"https:\/\/theconversation.com\/\" target=\"_blank\" rel=\"noreferrer noopener\">The Conversation<\/a>\u00a0from various from various sources.<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p>NASA&#8217;s Curiosity rover has identified seven new organic compounds on the planet Mars, according to new research published in Nature Communications. The researchers believe this organic matter may have been preserved on Mars for more than 3.4 billion years. But is it evidence of life? It&#8217;s not yet possible to determine whether it was delivered [&hellip;]<\/p>\n","protected":false},"author":52,"featured_media":101031,"template":"","meta":{"_acf_changed":false,"footnotes":"","_links_to":"","_links_to_target":""},"cu_story_type":[1623],"cu_story_tag":[1919],"class_list":["post-101027","cu_story","type-cu_story","status-publish","has-post-thumbnail","hentry","cu_story_type-expert-perspectives","cu_story_tag-faculty-of-science"],"acf":{"cu_post_thumbnail":""},"_links":{"self":[{"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story\/101027","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story"}],"about":[{"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/types\/cu_story"}],"author":[{"embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/users\/52"}],"version-history":[{"count":5,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story\/101027\/revisions"}],"predecessor-version":[{"id":101036,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story\/101027\/revisions\/101036"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/media\/101031"}],"wp:attachment":[{"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/media?parent=101027"}],"wp:term":[{"taxonomy":"cu_story_type","embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story_type?post=101027"},{"taxonomy":"cu_story_tag","embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story_tag?post=101027"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}