{"id":100218,"date":"2026-02-04T11:01:18","date_gmt":"2026-02-04T16:01:18","guid":{"rendered":"https:\/\/carleton.ca\/news\/?post_type=cu_story&#038;p=100218"},"modified":"2026-02-04T11:02:02","modified_gmt":"2026-02-04T16:02:02","slug":"arctic-rhino-fossil-nunavut","status":"publish","type":"cu_story","link":"https:\/\/carleton.ca\/news\/story\/arctic-rhino-fossil-nunavut\/","title":{"rendered":"Epiaceratherium Itjilik: The Rhino That Lived in the Arctic"},"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\/02\/baffin-island-nunavut-1920x1280-1-768x512.jpg); background-position: 50% 50%;\">\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                        Epiaceratherium Itjilik: The Rhino That Lived in the Arctic\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>Paleontologists at the Canadian Museum of Nature have recently been studying the skeletal remains of a rhinoceros. This might not sound remarkable at first, but what makes these remains fascinating is that they were found on Devon Island in the Canadian Arctic.<\/p>\n\n\n\n<p>Today, mammals inhabit nearly every corner of the Earth. In Asia, Europe and North America, mammals arrived via three routes, one over the Bering Strait and two over the North Atlantic.<\/p>\n\n\n\n<p>The Bering Land Bridge is the best known, having enabled the arrival of humans in North America approximately 20,000 years ago and shaped the population genetics of animals such as <a href=\"https:\/\/doi.org\/10.1111\/mec.16267\" target=\"_blank\" rel=\"noreferrer noopener\">bears, lions<\/a> and <a href=\"https:\/\/doi.org\/10.1126\/science.adr2355\" target=\"_blank\" rel=\"noreferrer noopener\">horses<\/a>.<\/p>\n\n\n\n<p>Less well known are the two routes that traversed the North Atlantic, one from the Scandinavian Peninsula over Svalbard and Greenland, and another from Scotland over Iceland to Greenland and the Canadian Arctic.<\/p>\n\n\n\n<p>However, it has typically <a href=\"https:\/\/doi.org\/10.1111\/jbi.12310\" target=\"_blank\" rel=\"noreferrer noopener\">been thought that land animals could not have crossed the North Atlantic<\/a> by the <a href=\"https:\/\/theconversation.com\/how-ancient-warm-periods-can-help-predict-future-climate-change-58036\" target=\"_blank\" rel=\"noreferrer noopener\">Early Eocene<\/a>, a period around 50 million years ago when the Earth&#8217;s climate was warmer.<\/p>\n\n\n\n<p>However, the Arctic rhino&#8217;s remains provide tantalizing evidence that land mammals were able to traverse the North Atlantic using frozen land bridges much more recently than the Early Eocene.<\/p>\n\n\n\n<h2 id=\"a-rhinoceros-in-the-arctic\" class=\"wp-block-heading has-text-align-center\">A rhinoceros in the Arctic<\/h2>\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=\"Discovery of an extinct rhino from Canada\u2019s High Arctic\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/pJZEEYaQRkc?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<p>The new species of rhinoceros was discovered from a nearly complete specimen collected from the <a href=\"https:\/\/www.planetary.org\/articles\/haughton_crater\" target=\"_blank\" rel=\"noreferrer noopener\">Haughton Formation of Devon Island in Nunavut<\/a> \u2014 lake sediments formed in an asteroid impact crater that likely date to the Early Miocene, around 23 million years ago.<\/p>\n\n\n\n<p>The sediments of the Haughton Formation preserve plants, mammals and birds, among others. The majority of the rhinoceros was collected in the 1980s by paleontologist Mary Dawson and her team, with additional collections by paleontologists Natalia Rybczynski, Marisa Gilbert and their team in the 2010s.<\/p>\n\n\n\n<p>The rhinoceros lacked a horn, which is common among extinct rhinos. It is remarkable, however, in possessing features of much more ancient forms, like teeth of forms many millions of years older. It also has a fifth toe on the forefoot, which is rare among rhinoceroses.<\/p>\n\n\n\n<p>Anatomical comparison and evolutionary analysis suggest the specimen belongs to an existing genus, <em>Epiaceratherium<\/em>, found only in Europe and western Asia. In naming the new species, the team consulted with <a href=\"https:\/\/nature.ca\/en\/about-the-museum\/media-centre\/a-rhino-from-the-arctic\/\" target=\"_blank\" rel=\"noreferrer noopener\">Jarloo Kiguktak<\/a>, an elder from the nearest Indigenous community to the Haughton Crater, Aujuittuq (Grise Fiord). Together, they named it <em>Epiaceratherium itjilik<\/em>. Itjilik is an Inuktitut word meaning frost or frosty, an homage to the Arctic setting where the specimen was found.<\/p>\n\n\n\n<p>Most surprisingly, the team&#8217;s evolutionary analysis placed <em>E. itjilik<\/em> closest to the European species of <em>Epiaceratherium<\/em>. This indicates that its ancestors likely crossed from Europe to North America via the North Atlantic at some point during the late Eocene period around 33-38 million years ago.<\/p>\n\n\n\n<p>Bio-geographic analyses further revealed a surprisingly high number of rhinoceros crossings over the North Atlantic directly between Europe and North America, some in the last 20 million years. While a finding of such a recent crossing via the North Atlantic has often been considered unlikely, emerging geological evidence tells a different story.<\/p>\n\n\n\n<h2 id=\"how-did-rhinos-get-to-the-arctic\" class=\"wp-block-heading has-text-align-center\">How did rhinos get to the Arctic?<\/h2>\n\n\n\n<p>Today, land animals are impeded from crossing between Europe and North America by several deep, wide waterways. The Faroe Islands, Iceland and Greenland are separated by the Faroe-Bank Channel, Faroe Shetland Channel and the Denmark Strait. Between the Scandinavian Peninsula, Svalbard and Greenland are the Barents Sea and Fram Strait. It is believed that land animals could traverse at least one of these areas only up until the Early Eocene about 50 million years ago.<\/p>\n\n\n\n<p><a href=\"https:\/\/doi.org\/10.1016\/j.gr.2020.05.011\" target=\"_blank\" rel=\"noreferrer noopener\">Recent studies<\/a>, however, are starting to paint a more complex picture of North Atlantic geological change. Estimates for the timing of formation of the various channels that now break up North Atlantic land masses are highly variable.<\/p>\n\n\n\n<p><a href=\"https:\/\/doi.org\/10.1038\/s43247-023-00899-y\" target=\"_blank\" rel=\"noreferrer noopener\">Mathematical modelling<\/a> suggests a highland connected Svalbard to northern Europe as recently as the 2.7 million years ago. <a href=\"https:\/\/doi.org\/10.1016\/j.gr.2020.05.011\" target=\"_blank\" rel=\"noreferrer noopener\">An array of new data<\/a> also suggest the Fram Strait was shallow and narrow until the Early Miocene, around 23 million years ago. The Faroe-Shetland channel may have opened between 50 and 34 million years ago, while the Iceland-Faroe Channel and Denmark Strait were submerged later, 34 to 10 million years ago.<\/p>\n\n\n\n<p>This suggests that rhinoceroses could have walked on land for at least part of their journey across the North Atlantic. They could possibly have swum the relatively short distances between land masses but the team hypothesized that seasonal sea ice may also have facilitated their movement.<\/p>\n\n\n\n<h2 id=\"seasonal-ice\" class=\"wp-block-heading has-text-align-center\">Seasonal ice<\/h2>\n\n\n\n<p><a href=\"https:\/\/doi.org\/10.1016\/j.quascirev.2010.02.010\" target=\"_blank\" rel=\"noreferrer noopener\">More than 47 million years ago<\/a>, the Arctic Ocean and surrounding regions were ice-free all year. <a href=\"https:\/\/doi.org\/10.1038\/ngeo2068\" target=\"_blank\" rel=\"noreferrer noopener\">Ocean cores<\/a> collected from the Arctic Ocean \u2014 samples of mud, sand and organic material drilled from the seafloor \u2014 contain evidence of ice-rafted debris during the Middle Eocene, approximately 47 to 38 million years ago. This indicates the presence of seasonal ice.<\/p>\n\n\n\n<p><a href=\"https:\/\/doi.org\/10.1038\/s41467-018-03180-5\" target=\"_blank\" rel=\"noreferrer noopener\">Another ocean core<\/a> collected between Greenland and Svalbard also contains ice-rafted debris originating from across the Arctic dating from between 48 to 26 million years ago. What is emerging, therefore, is the possibility that land animals crossed the North Atlantic by a combination of routes formed over land and seasonal ice.<\/p>\n\n\n\n<p>Vertebrate fossils from the islands that once comprised the North Atlantic land bridges are extremely rare. Given that much of the land bridges are now submerged, direct evidence for how animals spread across the North Atlantic may be lost.<\/p>\n\n\n\n<p>Bio-geographic studies like the one conducted by the team at the Canadian Museum of Nature highlight how discoveries in the Arctic are reshaping what we know about mammal evolution. These insights further our understanding of how animals moved across our planet.<\/p>\n\n\n\n<p>\u2013<br><em class=\"myprefix-text-italic\"><a href=\"https:\/\/carleton.ca\/biology\/people\/danielle-fraser\/\" target=\"_blank\" rel=\"noreferrer noopener\">Danielle Fraser<\/a> is an adjunct research professor of 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\/epiaceratherium-itjilik-the-rhino-that-lived-in-the-arctic-269484\" 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>Paleontologists at the Canadian Museum of Nature have recently been studying the skeletal remains of a rhinoceros. This might not sound remarkable at first, but what makes these remains fascinating is that they were found on Devon Island in the Canadian Arctic. Today, mammals inhabit nearly every corner of the Earth. In Asia, Europe and [&hellip;]<\/p>\n","protected":false},"author":52,"featured_media":100221,"template":"","meta":{"_acf_changed":false,"footnotes":"","_links_to":"","_links_to_target":""},"cu_story_type":[1623],"cu_story_tag":[1919,1925],"class_list":["post-100218","cu_story","type-cu_story","status-publish","has-post-thumbnail","hentry","cu_story_type-expert-perspectives","cu_story_tag-faculty-of-science","cu_story_tag-research"],"acf":{"cu_post_thumbnail":""},"_links":{"self":[{"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story\/100218","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":2,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story\/100218\/revisions"}],"predecessor-version":[{"id":100222,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story\/100218\/revisions\/100222"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/media\/100221"}],"wp:attachment":[{"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/media?parent=100218"}],"wp:term":[{"taxonomy":"cu_story_type","embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story_type?post=100218"},{"taxonomy":"cu_story_tag","embeddable":true,"href":"https:\/\/carleton.ca\/news\/wp-json\/wp\/v2\/cu_story_tag?post=100218"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}