{"id":32215,"date":"2023-01-27T06:59:04","date_gmt":"2023-01-27T05:59:04","guid":{"rendered":"https:\/\/karmaka.de\/?p=32215"},"modified":"2023-01-27T06:59:04","modified_gmt":"2023-01-27T05:59:04","slug":"nucleosynthetic-isotope-anomalies-of-zinc-in-meteorites-constrain-the-origin-of-earths-volatiles","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=32215","title":{"rendered":"Nucleosynthetic isotope anomalies of zinc in meteorites constrain the origin of Earth\u2019s volatiles"},"content":{"rendered":"\n<p>Rayssa Martins, Sven Kuthning, Barry J. Coles, Katharina Kreissig, and Mark Rehk\u00e4mper<\/p>\n\n\n\n<p>Science<br>26 Jan 2023<br>Vol 379, Issue 6630<br>pp. 369-372<\/p>\n\n\n\n<p><a href=\"https:\/\/www.science.org\/doi\/10.1126\/science.abn1021\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>LINK<\/strong><\/a><\/p>\n\n\n\n<p class=\"justify-text\">&#8220;Material inherited from different nucleosynthesis sources imparts distinct isotopic signatures to meteorites and terrestrial planets. These nucleosynthetic isotope anomalies have been used to constrain the origins of material that formed Earth. However, anomalies have only been identified for elements with high condensation temperatures, leaving the origin of Earth\u2019s volatile elements unconstrained. We determined the isotope composition of the moderately volatile element zinc in 18 bulk meteorites and identified nucleosynthetic zinc isotope anomalies. Using a mass-balance model, we find that carbonaceous bodies, which likely formed beyond the orbit of Jupiter, delivered about half of Earth\u2019s zinc inventory. Combined with previous constraints obtained from studies of other elements, these results indicate that ~10% of Earth\u2019s mass was provided by carbonaceous material.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Rayssa Martins, Sven Kuthning, Barry J. Coles, Katharina Kreissig, and Mark Rehk\u00e4mper Science26 Jan 2023Vol 379, Issue 6630pp. 369-372 LINK &#8220;Material inherited from different nucleosynthesis sources imparts distinct isotopic signatures to meteorites and terrestrial planets&#8230;.<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[74,112,8],"tags":[80,2001,3152,3297,1572,369,1692],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/32215"}],"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=32215"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/32215\/revisions"}],"predecessor-version":[{"id":32216,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/32215\/revisions\/32216"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=32215"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=32215"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=32215"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}