{"id":20272,"date":"2019-08-12T18:31:08","date_gmt":"2019-08-12T16:31:08","guid":{"rendered":"http:\/\/karmaka.de\/?p=20272"},"modified":"2019-08-12T22:08:08","modified_gmt":"2019-08-12T20:08:08","slug":"selenium-isotopes-as-tracers-of-a-late-volatile-contribution-to-earth-from-the-outer-solar-system","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=20272","title":{"rendered":"Selenium isotopes as tracers of a late volatile contribution to Earth from the outer Solar System"},"content":{"rendered":"\n<p>Mar\u00eda Isabel Varas-Reus, Stephan K\u00f6nig, Aierken Yierpan, Jean-Pierre Lorand &amp; Ronny Schoenberg<\/p>\n\n\n\n<p>Nature Geoscience, 1\u20134, Published: 12 August 2019<\/p>\n\n\n\n<p><a href=\"https:\/\/www.nature.com\/articles\/s41561-019-0414-7\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>LINK<\/strong><\/a><\/p>\n\n\n\n<p class=\"justify-text\">&#8220;The origin of Earth\u2019s volatiles has been attributed to a late addition of meteoritic material after core\u2013mantle differentiation. The nature and consequences of this \u2018late veneer\u2019 are debated, but may be traced by isotopes of the highly siderophile, or iron-loving, and volatile element selenium. Here we present high-precision selenium isotope data for mantle peridotites, from double spike and hydride-generation multicollector inductively coupled plasma mass spectrometry. These data indicate that the selenium isotopic composition of peridotites is unaffected by petrological processes, such as melt depletion and melt-rock reaction, and thus a narrow range is preserved that is representative of the silicate Earth. We show that selenium isotopes record a signature of late accretion after core formation and that this signature overlaps only with that of the CI-type carbonaceous chondrites. We conclude that these isotopic constraints indicate the late veneer originated from the outer Solar System and was of lower mass than previously estimated. Thus, we suggest a late and highly concentrated delivery of volatiles enabled Earth to become habitable.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Mar\u00eda Isabel Varas-Reus, Stephan K\u00f6nig, Aierken Yierpan, Jean-Pierre Lorand &amp; Ronny Schoenberg Nature Geoscience, 1\u20134, Published: 12 August 2019 LINK &#8220;The origin of Earth\u2019s volatiles has been attributed to a late addition of meteoritic material&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[9,10,72,112,71],"tags":[733,3273,1809,3152,642,2406,110,4269],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/20272"}],"collection":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=20272"}],"version-history":[{"count":2,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/20272\/revisions"}],"predecessor-version":[{"id":20274,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/20272\/revisions\/20274"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=20272"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=20272"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=20272"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}