{"id":163685,"date":"2025-09-23T14:40:12","date_gmt":"2025-09-23T14:40:12","guid":{"rendered":"https:\/\/www.newsbeep.com\/au\/163685\/"},"modified":"2025-09-23T14:40:12","modified_gmt":"2025-09-23T14:40:12","slug":"first-natural-evidence-of-nickel-rich-alloys-found-deep-in-earths-mantle","status":"publish","type":"post","link":"https:\/\/www.newsbeep.com\/au\/163685\/","title":{"rendered":"First natural evidence of nickel-rich alloys found deep in Earth&#8217;s mantle"},"content":{"rendered":"<p>The chemical mood of Earth\u2019s mantle, its redox state, is shaped by how iron and carbon behave as they gain or lose electrons. This redox balance affects everything, from the <a href=\"https:\/\/www.techexplorist.com\/ancient-seafloor-vents-supplied-life-giving-minerals-earth-early-oceans\/80566\/\" rel=\"nofollow noopener\" target=\"_blank\">formation of minerals<\/a> to the movement of heat and materials deep underground.<\/p>\n<p>Studies of mantle rocks (xenoliths), laboratory experiments, and thermodynamic models indicate that oxygen levels decrease with depth, particularly down to approximately 250 km. Around 250\u2013300 km, scientists expect a nickel-rich metallic alloy to form, resulting in a further decrease in oxygen.<\/p>\n<p>But here\u2019s the twist: garnets found between 250 and 500 km tell a different story. They exhibit signs of more oxidized conditions, and no nickel-rich alloy has ever been seen in these depths to support the prediction.<\/p>\n<p><img fetchpriority=\"high\" decoding=\"async\" width=\"700\" height=\"525\" src=\"data:image\/svg+xml,%3Csvg%20xmlns=\" http:=\"\" alt=\"Slice of African diamond with a clear core and cloudy, inclusion-rich rim\" class=\"wp-image-101077\" data-lazy- data-lazy- data-lazy-src=\"https:\/\/www.newsbeep.com\/au\/wp-content\/uploads\/2025\/09\/Slice-of-African-diamond.webp.webp\"\/>A diamond slice of an African diamond showing a clear core surrounded by a cloudy, inclusion-rich rim.<\/p>\n<p>Credit<br \/>\nYaakov Weiss<\/p>\n<p>A groundbreaking study in Nature Geoscience, led by researchers at the Hebrew University of Jerusalem, has uncovered tiny metallic and carbonate inclusions inside diamonds from South Africa\u2019s Voorspoed mine, offering a rare peek into <a href=\"https:\/\/www.techexplorist.com\/model-reveals-surprising-behavior-minerals-deep-planet-interior\/56368\/\" rel=\"nofollow noopener\" target=\"_blank\">Earth\u2019s deep mantle<\/a> chemistry.<\/p>\n<p class=\"also\"><a href=\"https:\/\/www.techexplorist.com\/identifying-areas-earthquake-waves-behave-differently\/95487\/\" rel=\"nofollow noopener\" target=\"_blank\">Are there lost worlds in\u00a0Earth\u2019s\u00a0interior?<\/a><\/p>\n<p>Working with scientists from the University of Nevada, the University of Cambridge, and the Nanocenter at Hebrew University, the team found nickel\u2013iron nanoinclusions and nickel-rich carbonate microinclusions in <a href=\"https:\/\/www.techexplorist.com\/earth-recycles-ocean-floor-salty-diamonds\/23661\/\" rel=\"nofollow noopener\" target=\"_blank\">diamonds formed 280\u2013470 km beneath Earth\u2019s surface<\/a>. These microscopic features provide the first direct evidence of nickel-rich alloys at the depths where they were long predicted to exist.<\/p>\n<p>This discovery validates key mantle redox models and helps explain how <a href=\"https:\/\/www.techexplorist.com\/density-liquid-iron-under-conditions-similar-earth-outer-core\/33374\/\" rel=\"nofollow noopener\" target=\"_blank\">iron and nickel behave deep underground<\/a>, shedding light on the chemical forces that shape our planet from within.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"700\" height=\"525\" src=\"data:image\/svg+xml,%3Csvg%20xmlns=\" http:=\"\" alt=\"Diamond from South Africa with inclusion-rich zones and a clearer central region\" class=\"wp-image-101076\" data-lazy- data-lazy- data-lazy-src=\"https:\/\/www.newsbeep.com\/au\/wp-content\/uploads\/2025\/09\/clearer-central-region.webp.webp\"\/>For geochemists, the most scientifically valuable diamonds are those containing chemical impurities, which are the least prized in jewelry. This diamond from South Africa contains several inclusion-rich zones, and a middle part that is clearer. <\/p>\n<p>Credit<br \/>\nYaakov Weiss<\/p>\n<p>The diamonds from South Africa\u2019s Voorspoed mine carry more than sparkle; they hold clues to <a href=\"https:\/\/www.techexplorist.com\/new-research-unveiled-structures-deep-earth\/33007\/\" rel=\"nofollow noopener\" target=\"_blank\">Earth\u2019s deep interior<\/a>. Their mineral cargo includes coesite, potassium-rich aluminous phases, and solid nitrogen, all of which act as pressure markers that pinpoint their origin to the deep upper mantle and the shallow transition zone.<\/p>\n<p>But the real breakthrough goes beyond confirming theory. The presence of both nickel\u2013iron alloy and nickel-rich carbonate inside the diamonds suggests a dramatic underground event: a metasomatic redox-freezing reaction. In this process, an oxidized, carbon-rich melt infiltrates reduced, metal-bearing peridotite, triggering the formation of diamonds. This supports earlier findings from shallower depths, reinforcing the idea that such <a href=\"https:\/\/www.techexplorist.com\/heat-earths-crust-become-ultimate-energy-source\/24944\/\" rel=\"nofollow noopener\" target=\"_blank\">redox reactions<\/a> are a key pathway for the creation of natural diamonds.<\/p>\n<p class=\"also\"><a href=\"https:\/\/www.techexplorist.com\/potential-diamond-factory-existed-core-mantle-boundary-billions-years\/54039\/\" rel=\"nofollow noopener\" target=\"_blank\">Potential \u2018diamond factory\u2019 may have existed at the core-mantle boundary for billions of years<\/a><\/p>\n<p>In this deep mantle setting, iron oxidized more readily than nickel, leaving behind a nickel-rich metallic alloy. Meanwhile, nickel-rich carbonates and diamonds began to crystallize from the surrounding melt. The diamonds, in essence, captured a brief but <a href=\"https:\/\/www.techexplorist.com\/3-8-billion-year-old-crystal-point-earliest-geochemical-evidence-plate-tectonics\/46643\/\" rel=\"nofollow noopener\" target=\"_blank\">powerful geochemical transformation<\/a>, where reduced mantle rock was turned into a more oxidized, volatile-rich zone, and carbonates were reduced to form diamonds.<\/p>\n<p>\u201cThis is a rare snapshot of mantle chemistry in action,\u201d says Weiss. \u201cThe diamonds act as tiny time capsules, preserving a reaction that would otherwise vanish as minerals re-equilibrate with their surroundings.\u201d<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"700\" height=\"525\" src=\"data:image\/svg+xml,%3Csvg%20xmlns=\" http:=\"\" alt=\"\u2018Cloudy\u2019 South African diamond with microinclusion-rich interior and clear octahedral outer zone\" class=\"wp-image-101075\" data-lazy- data-lazy- data-lazy-src=\"https:\/\/www.newsbeep.com\/au\/wp-content\/uploads\/2025\/09\/Cloudy-South-African-diamond.webp.webp\"\/>\u2018Cloudy\u2019 diamond from South Africa, with an internal zone full of microinclusions, overgrown by a clear octahedral outer zone.<\/p>\n<p>Credit<br \/>\nYaakov Weiss<\/p>\n<p>Their microscopic inclusions suggest that localized redox reactions in the mantle can oxidize small pockets of rock. This may explain why some superdeep diamonds show unexpectedly high oxidation levels.<\/p>\n<p>These reactions also help us understand how volatile-rich magmas form. When mantle peridotite is enriched with carbonate, potassium, and other elements during redox events, it sets the stage for explosive magmas like kimberlites and lamprophyres, and even some <a href=\"https:\/\/www.techexplorist.com\/unveiling-earth-past-2-5-billion-year-old-pacific-rock-samples\/82801\/\" rel=\"nofollow noopener\" target=\"_blank\">ocean island basalts<\/a>. In short, these tiny mineral traces reveal sweeping connections between subduction, mantle chemistry, and the fiery <a href=\"https:\/\/www.techexplorist.com\/unexpected-distortion-worlds-largest-continental-rift\/62123\/\" rel=\"nofollow noopener\" target=\"_blank\">forces that shape continents<\/a> and deliver diamonds to the surface.<\/p>\n<p class=\"also\"><a href=\"https:\/\/www.techexplorist.com\/unraveling-secrets-diamond-formation\/21114\/\" rel=\"nofollow noopener\" target=\"_blank\">Unraveling secrets of\u00a0diamond\u00a0formation<\/a><\/p>\n<p>The study underscores the scientific value of diamonds as more than just gemstones. Their inclusions, whether nanometer-scale alloys or high-pressure minerals, offer one of the only natural records of conditions hundreds of kilometers beneath our feet.<\/p>\n<p>Kempe and Weiss\u2019s research marks a breakthrough, the first natural evidence of nickel-rich alloys at the depths long predicted by mantle models. These tiny inclusions within diamonds provide a vivid snapshot of how Earth\u2019s deep redox landscape evolves through melt-rock interactions.<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" width=\"700\" height=\"561\" src=\"data:image\/svg+xml,%3Csvg%20xmlns=\" http:=\"\" alt=\"Coated Diamond with Microinclusion-Rich Rim\" class=\"wp-image-101074\" data-lazy- data-lazy- data-lazy-src=\"https:\/\/www.newsbeep.com\/au\/wp-content\/uploads\/2025\/09\/Coated-Diamond.webp.webp\"\/>\u2018Coated\u2019 diamond from Africa, consists of an octahedral non-fibrous monocrystalline core (not seen in the picture) and a concentric coat containing microinclusions.<\/p>\n<p>Credit<br \/>\nYaakov Weiss<\/p>\n<p>Far from being static symbols of permanence, diamonds are emerging as storytellers of transformation. Locked within their crystal structure are clues to the mantle\u2019s hidden chemistry, records of oxidation, volatile enrichment, and dynamic processes that continue to shape our planet from within. As scientists delve deeper into these mineral time capsules, they\u2019re uncovering a rich narrative of Earth\u2019s evolving interior.<\/p>\n<p class=\"reference\">Journal Reference:<\/p>\n<p>Kempe, Y., Remennik, S., Tschauner, O. et al. Redox state of the deep upper mantle recorded by nickel-rich diamond inclusions. Nat. Geosci. (2025). DOI: <a href=\"https:\/\/doi.org\/10.1038\/s41561-025-01791-4\" rel=\"nofollow noopener\" target=\"_blank\">10.1038\/s41561-025-01791-4<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"The chemical mood of Earth\u2019s mantle, its redox state, is shaped by how iron and carbon behave as&hellip;\n","protected":false},"author":2,"featured_media":163686,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[64,63,129,107952,128],"class_list":["post-163685","post","type-post","status-publish","format-standard","has-post-thumbnail","category-science","tag-au","tag-australia","tag-earth","tag-earths-mantle","tag-science"],"_links":{"self":[{"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/posts\/163685","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/comments?post=163685"}],"version-history":[{"count":0,"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/posts\/163685\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/media\/163686"}],"wp:attachment":[{"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/media?parent=163685"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/categories?post=163685"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.newsbeep.com\/au\/wp-json\/wp\/v2\/tags?post=163685"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}