{"id":10246,"date":"2021-11-23T08:47:00","date_gmt":"2021-11-23T13:47:00","guid":{"rendered":"http:\/\/all-geo.org\/highlyallochthonous\/?p=10246"},"modified":"2022-10-31T21:11:14","modified_gmt":"2022-11-01T02:11:14","slug":"weird-rocky-exoplanets","status":"publish","type":"post","link":"https:\/\/all-geo.org\/highlyallochthonous\/2021\/11\/weird-rocky-exoplanets\/","title":{"rendered":"Weird rocky exoplanets"},"content":{"rendered":"\n<p><a href=\"https:\/\/www.sciencenews.org\/article\/rocky-planets-exotic-chemical-elements-mantle-white-dwarf-stars\">Obtaining the composition of rocky exoplanets from the spectral signature produced when their dying parent star eats them<\/a>&nbsp;is already pretty mind-blowing. But the results &#8211; which suggest that on some of these worlds, quartz is substituted for olivine in their mantles? That\u2019s a mind-supernova.<\/p>\n\n\n\n<p>I\u2019m not even sure how you could get such a composition &#8211; coalescing from a particularly iron poor planetary nebula, perhaps? But given how Earth\u2019s mantle is dominated by olivine and its pressure-induced phase changes, there could be profound differences in how an olivine-free mantle convects and loses heat.<\/p>\n\n\n\n<p><a href=\"https:\/\/www.nature.com\/articles\/s41467-021-26403-8#Fig3\">As this figure from the paper shows<\/a>, the data also point to another kind of rocky exoplanet rich in periclase (MgO) rather than orthopyroxene. In other words, a significant non-silicate phase!<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"511\" src=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2022\/10\/41467_2021_26403_Fig3_HTML-600x511.png\" alt=\"\" class=\"wp-image-10247\" srcset=\"https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2022\/10\/41467_2021_26403_Fig3_HTML-600x511.png 600w, https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2022\/10\/41467_2021_26403_Fig3_HTML-300x255.png 300w, https:\/\/all-geo.org\/highlyallochthonous\/wp-content\/uploads\/2022\/10\/41467_2021_26403_Fig3_HTML.png 685w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption>Figure 3 of Putirka &amp; Xu (2021) plotting estimated compositions of exoplanetary mantles (large diamonds) on one of 3 ternary diagrams. Top left: components are Olivine, Orthopyroxene (Opx) and Clinopyroxene (Cpx), like the Earth&#8217;s mantle. Note how the light grey and dark grey diamonds plot way outside the ternary diagram, indicating at least one of the three components is not present. Centre: components are Quartz (replacing Olivine as in Earth&#8217;s continental crust), Opx, and Cpx. Bottom right: olivine, Cpx and periclase (MgO) replacing Opx.<\/figcaption><\/figure>\n\n\n\n<p>So what does this mean? The authors suggest that \u201cquartz-rich mantles might create thicker crusts, while the periclase-saturated mantles could plausibly yield, on a wet planet like Earth, crusts made of serpentinite.\u201d<\/p>\n\n\n\n<p>Of course, there are some sizeable (acknowledged) caveats, given the rather extreme detection method. We\u2019ll have to see whether these inferences stand up to scrutiny. But it&#8217;s yet more evidence that beyond our solar system, many surprises about the way planets work await.<\/p>\n\n\n\n<p>[This post was collated from <a href=\"https:\/\/twitter.com\/Allochthonous\/status\/1463244675926667269\">this Twitter thread<\/a>]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Obtaining the composition of rocky exoplanets from the spectral signature produced when their dying parent star eats them&nbsp;is already pretty mind-blowing. But the results &#8211; which suggest that on some of these worlds, quartz is substituted for olivine in their &hellip; <a href=\"https:\/\/all-geo.org\/highlyallochthonous\/2021\/11\/weird-rocky-exoplanets\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[4,15,18],"tags":[308,427],"class_list":["post-10246","post","type-post","status-publish","format-standard","hentry","category-geology","category-planets","category-rocks-minerals","tag-exoplanets","tag-weird-geology"],"_links":{"self":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/10246","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/comments?post=10246"}],"version-history":[{"count":3,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/10246\/revisions"}],"predecessor-version":[{"id":10263,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/posts\/10246\/revisions\/10263"}],"wp:attachment":[{"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/media?parent=10246"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/categories?post=10246"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/all-geo.org\/highlyallochthonous\/wp-json\/wp\/v2\/tags?post=10246"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}