{"id":32712,"date":"2023-05-24T13:14:25","date_gmt":"2023-05-24T11:14:25","guid":{"rendered":"https:\/\/cab.inta-csic.es\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/"},"modified":"2023-05-25T11:08:06","modified_gmt":"2023-05-25T09:08:06","slug":"biosignatures-of-earths-oldest-fossils","status":"publish","type":"seminarios-mdm","link":"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/","title":{"rendered":"Biosignatures of Earth&#8217;s oldest fossils"},"content":{"rendered":"\n<p>The oldest putative fossils occur as hematite filaments and tubes in jasper-carbonate banded iron formations (BIF) from the 4280- to 3750-Ma Nuvvuagittuq Supracrustal Belt (NSB), Qu\u00e9bec. If biological in origin, these filaments might have affinities with modern descendants; however, if abiotic, they could indicate complex prebiotic forms on early Earth. In this presentation, I will describe various microfossils, dubiofossils and pseudofossils that occur in the NSB jasper BIF. This will include descriptions of associated observations from mineralogy, sedimentology, petrology, and geochemistry. The latter in particular will include new observations of the organic geochemistry and trace metal composition of selected microfossils. The microstructures share resemblance to younger microfossils, modern Fe-oxidising bacteria from hydrothermal environments, and the experimental products of heated Fe-oxidizing bacteria. Collectively, the observations suggest a diverse microbial ecosystem on the primordial Earth, traces of which may be common on other planetary bodies with hydrothermalism, including Mars.<\/p>\n\n\n\n<div style=\"height:49px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p><strong>CAB YouTube channel<\/strong>:\u00a0<a href=\"https:\/\/www.youtube.com\/c\/CentrodeAstrobiologia%22%20%5Ct%20%22_blank\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/www.youtube.com\/c\/CentrodeAstrobiologia<\/a><br>\u00a0<\/p>\n\n\n\n<div style=\"height:49px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p>We invite you\u00a0to watch this video as a preview of tomorrow&#8217;s seminar, recorded after the discovery was published.\u00a0  <\/p>\n\n\n\n<p>Short video (1:45min)\u00a0<a href=\"https:\/\/www.youtube.com\/watch?v=jeAXmTjcPhI\" target=\"_blank\" rel=\"noopener\">https:\/\/www.youtube.com\/watch?v=jeAXmTjcPhI<\/a>  <\/p>\n\n\n\n<p>Long video (4:10min)\u00a0<a href=\"https:\/\/www.youtube.com\/watch?v=rynHqD3Elow\" target=\"_blank\" rel=\"noopener\">https:\/\/www.youtube.com\/watch?v=rynHqD3Elow<\/a> <\/p>\n","protected":false},"featured_media":0,"parent":0,"template":"","acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v20.0 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Biosignatures of Earth&#039;s oldest fossils &ndash; CAB<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Biosignatures of Earth&#039;s oldest fossils &ndash; CAB\" \/>\n<meta property=\"og:description\" content=\"The oldest putative fossils occur as hematite filaments and tubes in jasper-carbonate banded iron formations (BIF) from the 4280- to 3750-Ma Nuvvuagittuq Supracrustal Belt (NSB), Qu\u00e9bec. If biological in origin, these filaments might have affinities with modern descendants; however, if abiotic, they could indicate complex prebiotic forms on early Earth. In this presentation, I will [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/\" \/>\n<meta property=\"og:site_name\" content=\"CAB\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/CentroAstrobiologia\/\" \/>\n<meta property=\"article:modified_time\" content=\"2023-05-25T09:08:06+00:00\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:site\" content=\"@c_astrobiologia\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/\",\"url\":\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/\",\"name\":\"Biosignatures of Earth's oldest fossils &ndash; CAB\",\"isPartOf\":{\"@id\":\"https:\/\/cab.inta-csic.es\/#website\"},\"datePublished\":\"2023-05-24T11:14:25+00:00\",\"dateModified\":\"2023-05-25T09:08:06+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/\"]}]},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Portada\",\"item\":\"https:\/\/cab.inta-csic.es\/en\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Seminarios\",\"item\":\"https:\/\/cab.inta-csic.es\/seminarios-mdm\/\"},{\"@type\":\"ListItem\",\"position\":3,\"name\":\"Biosignatures of Earth&#8217;s oldest fossils\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/cab.inta-csic.es\/#website\",\"url\":\"https:\/\/cab.inta-csic.es\/\",\"name\":\"CAB\",\"description\":\"Centro de Astrobiolog\u00eda (CAB, CSIC-INTA)\",\"publisher\":{\"@id\":\"https:\/\/cab.inta-csic.es\/#organization\"},\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/cab.inta-csic.es\/?s={search_term_string}\"},\"query-input\":\"required name=search_term_string\"}],\"inLanguage\":\"en-US\"},{\"@type\":\"Organization\",\"@id\":\"https:\/\/cab.inta-csic.es\/#organization\",\"name\":\"Centro de Astrobiolog\u00eda (CAB)\",\"url\":\"https:\/\/cab.inta-csic.es\/\",\"logo\":{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/cab.inta-csic.es\/#\/schema\/logo\/image\/\",\"url\":\"https:\/\/cab.inta-csic.es\/wp-content\/uploads\/2021\/03\/1.LOGO-CAB-Oficial-CSIC-INTA-NASA_para-firma-scaled.jpg\",\"contentUrl\":\"https:\/\/cab.inta-csic.es\/wp-content\/uploads\/2021\/03\/1.LOGO-CAB-Oficial-CSIC-INTA-NASA_para-firma-scaled.jpg\",\"width\":2560,\"height\":561,\"caption\":\"Centro de Astrobiolog\u00eda (CAB)\"},\"image\":{\"@id\":\"https:\/\/cab.inta-csic.es\/#\/schema\/logo\/image\/\"},\"sameAs\":[\"https:\/\/www.instagram.com\/centro_astrobiologia\/\",\"https:\/\/es.linkedin.com\/company\/centro-de-astrobiologia-csic-inta-\",\"https:\/\/www.youtube.com\/c\/CentrodeAstrobiologia\",\"https:\/\/es.wikipedia.org\/wiki\/Centro_de_Astrobiolog\u00eda\",\"https:\/\/www.facebook.com\/CentroAstrobiologia\/\",\"https:\/\/twitter.com\/c_astrobiologia\"]}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Biosignatures of Earth's oldest fossils &ndash; CAB","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/cab.inta-csic.es\/en\/seminarios-mdm\/biosignatures-of-earths-oldest-fossils\/","og_locale":"en_US","og_type":"article","og_title":"Biosignatures of Earth's oldest fossils &ndash; CAB","og_description":"The oldest putative fossils occur as hematite filaments and tubes in jasper-carbonate banded iron formations (BIF) from the 4280- to 3750-Ma Nuvvuagittuq Supracrustal Belt (NSB), Qu\u00e9bec. 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