{"id":735,"date":"2021-01-05T16:03:59","date_gmt":"2021-01-05T19:03:59","guid":{"rendered":"https:\/\/www.ufrgs.br\/museupaleonto\/?page_id=735"},"modified":"2021-06-10T14:52:30","modified_gmt":"2021-06-10T17:52:30","slug":"fosseis","status":"publish","type":"page","link":"https:\/\/www.ufrgs.br\/museupaleonto\/?page_id=735","title":{"rendered":"F\u00f3sseis"},"content":{"rendered":"\n<div class=\"wp-block-cover alignfull has-background-dim-20 has-background-dim has-parallax is-style-default\" style=\"background-image:url(https:\/\/macrocollum.files.wordpress.com\/2020\/06\/img_5807.jpg)\"><div class=\"wp-block-cover__inner-container\">\n<p class=\"has-text-align-center has-large-font-size\"><\/p>\n<\/div><\/div>\n\n\n\n<div class=\"is-layout-flow wp-block-group alignfull has-background\" style=\"background-color:#ffffff\"><div class=\"wp-block-group__inner-container\">\n<div class=\"wp-block-jetpack-layout-grid alignfull column1-desktop-grid__span-9 column1-desktop-grid__row-1 column2-desktop-grid__span-3 column2-desktop-grid__start-10 column2-desktop-grid__row-1 column1-tablet-grid__span-6 column1-tablet-grid__row-1 column2-tablet-grid__span-2 column2-tablet-grid__start-7 column2-tablet-grid__row-1 column1-mobile-grid__span-4 column1-mobile-grid__row-1 column2-mobile-grid__span-4 column2-mobile-grid__row-2\">\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\">\n<p class=\"has-drop-cap has-text-align-justify\">O termo <strong>f\u00f3ssil<\/strong> \u00e9 proveniente do latim <em>fossilis<\/em>, que significa \u201ctirado da terra\u201d. F\u00f3sseis podem ser definidos como restos ou vest\u00edgios de seres vivos que habitaram o planeta Terra no passado e s\u00e3o o objeto de estudo da <strong>Paleontologia<\/strong>. \u00c9 atrav\u00e9s deles que torna-se poss\u00edvel obter informa\u00e7\u00f5es a respeito dos seres que viveram em um per\u00edodo de tempo geol\u00f3gico anterior ao atual, sendo importantes para o entendimento da evolu\u00e7\u00e3o da vida atrav\u00e9s do tempo.<\/p>\n\n\n\n<p class=\"has-text-align-justify\">Os f\u00f3sseis s\u00e3o encontrados nas <strong>rochas sedimentares<\/strong>, rochas formadas a partir de sedimentos (fragmentos de outras rochas) que s\u00e3o transportados atrav\u00e9s de agentes como vento e rios e se depositam em um determinado local. Portanto, a g\u00eanese de um f\u00f3ssil est\u00e1, muitas vezes, diretamente relacionada \u00e0 g\u00eanese da rocha sedimentar a qual est\u00e1 incorporado. \u00c9 na rocha que est\u00e3o as informa\u00e7\u00f5es sobre o ambiente habitado pelo ser vivo ou, no caso de ter havido transporte do material biol\u00f3gico, o ambiente em que foi soterrado.<\/p>\n\n\n\n<p class=\"has-text-align-justify\">Diversos grupos de seres vivos est\u00e3o representados no <strong>registro fossil\u00edfero<\/strong>, de modo que a variedade dos materiais encontrados \u00e9 muito grande, existindo desde grandes mam\u00edferos e gigantescos dinossauros, at\u00e9 polens e esporos de plantas que s\u00f3 conseguimos observar atrav\u00e9s de microsc\u00f3pios. Comumente associamos os f\u00f3sseis a imagens de grandes ossadas de dinossauros, mas esta \u00e9 somente uma fra\u00e7\u00e3o do registro dos seres do passado. \u00c9 poss\u00edvel acharmos f\u00f3sseis de ossos, troncos, folhas, carapa\u00e7as, conchas, pegadas, tocas, ovos, fezes, impress\u00f5es de pele, etc.<\/p>\n\n\n\n<div class=\"is-layout-flow wp-block-group alignfull has-background-background-color has-background\"><div class=\"wp-block-group__inner-container\">\n<div class=\"wp-block-jetpack-layout-grid alignfull column1-desktop-grid__span-4 column1-desktop-grid__row-1 column2-desktop-grid__span-4 column2-desktop-grid__start-5 column2-desktop-grid__row-1 column3-desktop-grid__span-4 column3-desktop-grid__start-9 column3-desktop-grid__row-1 column1-tablet-grid__span-4 column1-tablet-grid__row-1 column2-tablet-grid__span-4 column2-tablet-grid__start-5 column2-tablet-grid__row-1 column3-tablet-grid__span-8 column3-tablet-grid__row-2 column1-mobile-grid__span-4 column1-mobile-grid__row-1 column2-mobile-grid__span-4 column2-mobile-grid__row-2 column3-mobile-grid__span-4 column3-mobile-grid__row-3\">\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\">\n<div class=\"wp-block-image is-style-rounded\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/fc3b3ssil-pegada.jpg?w=1024\" alt=\"\" class=\"wp-image-578\" width=\"256\" height=\"256\"\/><figcaption>F\u00f3ssil de pegada de dinossauro ter\u00f3pode do Jur\u00e1ssico do Rio Grande do Sul. Foto por Arielle Both Gazzana, 2019.<\/figcaption><\/figure><\/div>\n\n\n\n<p><\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\">\n<div class=\"wp-block-image is-style-rounded\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/img_5745.jpg?w=580\" alt=\"\" class=\"wp-image-307\" width=\"290\" height=\"218\" srcset=\"https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5745.jpg 1984w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5745-300x225.jpg 300w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5745-768x576.jpg 768w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5745-1024x768.jpg 1024w\" sizes=\"(max-width: 290px) 100vw, 290px\" \/><figcaption>F\u00f3ssil do peixe <em>Dastilbe<\/em>, proveniente do Cret\u00e1ceo do Cear\u00e1. Foto por Arielle Both Gazzana, 2019.<\/figcaption><\/figure><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\">\n<div class=\"wp-block-image is-style-rounded\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/dente-mamute.jpg?w=1024\" alt=\"\" class=\"wp-image-579\" width=\"256\" height=\"256\"\/><figcaption>F\u00f3ssil de dente do mamute <em>Elephas primigenius<\/em>, do Pleistoceno da Inglaterra. Foto por Arielle Both Gazzana, 2019.<\/figcaption><\/figure><\/div>\n<\/div>\n<\/div>\n<\/div><\/div>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p class=\"has-text-align-justify\">F\u00f3sseis de ossos, troncos e folhas s\u00e3o classificados como <strong>restos (ou somatof\u00f3sseis)<\/strong>, visto que representam a preserva\u00e7\u00e3o de partes do corpo do pr\u00f3prio organismo. J\u00e1 pegadas, fezes, tocas e trilhas s\u00e3o classificados como <strong>vest\u00edgios<\/strong> <strong>(ou icnof\u00f3sseis)<\/strong>, estruturas resultantes da atividade em vida de um organismo que modifica o substrato e \u00e9 preservada no registro fossil\u00edfero.<\/p>\n\n\n\n<p class=\"has-text-align-justify\">O processo pelo qual os restos e vest\u00edgios dos organismos s\u00e3o preservados nas rochas \u00e9 chamado de <strong>fossiliza\u00e7\u00e3o<\/strong>, um evento extremamente raro, visto que a maior parte dos seres vivos acaba sendo decomposta ap\u00f3s sua morte, impossibilitando a preserva\u00e7\u00e3o de seus restos. Muitos dos vest\u00edgios deixados por estes organismos s\u00e3o destru\u00eddos pelo intemperismo, pela eros\u00e3o ou pela a\u00e7\u00e3o biol\u00f3gica de outros organismos. Ainda, mesmo que um organismo seja fossilizado, durante o curso de milh\u00f5es de anos \u00e9 poss\u00edvel que este seja exposto e erodido antes que seja encontrado, isto \u00e9, destru\u00eddo antes mesmo de tomarmos ci\u00eancia de sua exist\u00eancia. Portanto, os f\u00f3sseis s\u00e3o materiais raros que representam uma por\u00e7\u00e3o limitada do que foi a realidade da biodiversidade no passado geol\u00f3gico.<\/p>\n\n\n\n<p class=\"has-text-align-justify\">A fossiliza\u00e7\u00e3o \u00e9 um processo que varia de acordo com o tipo de material fossilizado, as caracter\u00edsticas do sedimento ao qual \u00e9 incorporado e ao tipo de ambiente em que ocorre. Alguns dos tipos de fossiliza\u00e7\u00e3o existentes s\u00e3o:<\/p>\n\n\n\n<ul><li><strong>Permineraliza\u00e7\u00e3o:<\/strong> ocorre quando partes duras de um organismo, como troncos de \u00e1rvores e esqueletos \u00f3sseos, t\u00eam seus poros e cavidades preenchidos por sedimento e subst\u00e2ncias minerais como s\u00edlica e carbonato de c\u00e1lcio, transportados pela \u00e1gua.<\/li><\/ul>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/img_5828.jpg?w=580\" alt=\"\" class=\"wp-image-391\" width=\"290\" height=\"218\" srcset=\"https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5828.jpg 1984w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5828-300x225.jpg 300w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5828-768x576.jpg 768w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5828-1024x768.jpg 1024w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5828-1200x900.jpg 1200w, https:\/\/www.ufrgs.br\/museupaleonto\/wp-content\/uploads\/2020\/06\/img_5828-1980x1485.jpg 1980w\" sizes=\"(max-width: 290px) 100vw, 290px\" \/><figcaption>Cr\u00e2nio de <em>Jachaleria candelariensis<\/em> que apresenta permineraliza\u00e7\u00e3o. Uma das consequ\u00eancias deste processo \u00e9 o aumento no volume do material. Foto por Arielle Both Gazzana, 2019.<\/figcaption><\/figure><\/div>\n\n\n\n<ul><li><strong>Substitui\u00e7\u00e3o: <\/strong>processo em que a constitui\u00e7\u00e3o mineral\u00f3gica de estruturas como conchas, ossos e dentes modifica-se atrav\u00e9s da dissolu\u00e7\u00e3o do mineral original e a substitui\u00e7\u00e3o concomitante por outro abundante no meio. O mineral original pode ser substitu\u00eddo por minerais como s\u00edlica, pirita, carbonatos e limonita.<\/li><\/ul>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img decoding=\"async\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/07\/whatsapp-image-2020-06-24-at-15.10.21.jpeg?w=374\" alt=\"\" class=\"wp-image-719\"\/><figcaption>F\u00f3ssil de concha de <em>Australospirifer<\/em>, braqui\u00f3pode do Devoniano de Ponta Grossa, Paran\u00e1. Foto por Cristina Silveira Vega.<\/figcaption><\/figure><\/div>\n\n\n\n<p><\/p>\n\n\n\n<ul><li> <strong>Recristaliza\u00e7\u00e3o: <\/strong>\u00e9 quando ocorre o rearranjo da estrutura cristalina de minerais inst\u00e1veis de partes duras de um organismo, que se modificam para formas mais est\u00e1veis, dando origem a outros minerais, mantendo a mesma composi\u00e7\u00e3o qu\u00edmica. Como exemplo, temos a convers\u00e3o da aragonita das conchas de moluscos para calcita. Na recristaliza\u00e7\u00e3o as estruturas mais finas da morfologia dos restos \u00e9 perdida.<\/li><\/ul>\n\n\n\n<ul><li><strong>Carbonifica\u00e7\u00e3o ou Incarboniza\u00e7\u00e3o: <\/strong>\u00e9 quando h\u00e1 a elimina\u00e7\u00e3o de elementos vol\u00e1teis da mat\u00e9ria org\u00e2nica, como hidrog\u00eanio, oxig\u00eanio e nitrog\u00eanio, preservando o carbono original. Ocorre em restos que n\u00e3o foram totalmente decompostos quando soterrados e \u00e9 comum em f\u00f3sseis de vegetais.<\/li><\/ul>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/planta-carbonizada.jpg?w=960\" alt=\"\" class=\"wp-image-568\" width=\"240\" height=\"240\"\/><figcaption>F\u00f3sseis de folhas de <em>Glossopteris<\/em> preservadas por carbonifica\u00e7\u00e3o. Neste processo o material apresenta uma colora\u00e7\u00e3o escura devido a uma fina pel\u00edcula carbonosa. Foto por Arielle Both Gazzana, 2019.<\/figcaption><\/figure><\/div>\n\n\n\n<ul><li><strong>Incrusta\u00e7\u00e3o: <\/strong>\u00e9 quando minerais carregados pela \u00e1gua precipitam-se sobre os restos org\u00e2nicos formando uma cobertura mineral que favorece sua preserva\u00e7\u00e3o durante a fossiliza\u00e7\u00e3o. \u00c9 comum em ossos e conchas de ambientes de caverna, onde a \u00e1gua \u00e9 rica em minerais como o carbonato de c\u00e1lcio.<\/li><\/ul>\n\n\n\n<ul><li><strong>Concre\u00e7\u00e3o: <\/strong>\u00e9 quando durante o processo de decomposi\u00e7\u00e3o dos organismos, s\u00e3o liberados compostos que desencadeiam rea\u00e7\u00f5es qu\u00edmicas que ocasionam a precipita\u00e7\u00e3o de subst\u00e2ncias que envolvem os restos org\u00e2nicos em n\u00f3dulos. Os f\u00f3sseis da Bacia do Araripe s\u00e3o um exemplo de concre\u00e7\u00e3o; os peixes ao serem decompostos nos fundos de lagos liberavam am\u00f4nia que facilitava a forma\u00e7\u00e3o de carbonato de c\u00e1lcio ao redor de seus restos, preservando sua forma dentro de n\u00f3dulos que hoje s\u00e3o encontrados e coletados.&nbsp;&nbsp;<\/li><\/ul>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/07\/araripe-3-e1593744839279.jpg\" alt=\"\" class=\"wp-image-716\" width=\"480\" height=\"360\"\/><figcaption>Concre\u00e7\u00e3o carbon\u00e1tica com peixe da Bacia do Araripe, do Cret\u00e1ceo do Nordeste. A preserva\u00e7\u00e3o excepcional permite a observa\u00e7\u00e3o de detalhes do animal. Foto por Heitor Francischini, 2020<\/figcaption><\/figure><\/div>\n\n\n\n<p class=\"has-text-align-justify\">\u00c9 poss\u00edvel tamb\u00e9m que, durante a litifica\u00e7\u00e3o, o sedimento que envolve o material biog\u00eanico preserve a forma do resto mesmo que este seja totalmente destru\u00eddo. O tipo de f\u00f3ssil resultante desse processo \u00e9 chamado de <strong>molde<\/strong>. Vale a pena mencionar que, apesar de tamb\u00e9m serem vest\u00edgios de um organismo, os moldes n\u00e3o podem ser classificados como icnof\u00f3sseis, j\u00e1 que n\u00e3o foram produzidos por um organismo em vida. Os principais tipos de moldes s\u00e3o:<\/p>\n\n\n\n<ul><li><strong>Molde Interno:<\/strong> ocorre quando o espa\u00e7o interno do f\u00f3ssil \u00e9 preenchido por sedimento, preservando suas fei\u00e7\u00f5es. Moldes de conchas e carapa\u00e7as de invertebrados s\u00e3o os exemplos mais comuns, mas este tipo de preserva\u00e7\u00e3o tamb\u00e9m pode ocorrer com cavidades cranianas de vertebrados, por exemplo.<\/li><\/ul>\n\n\n\n<ul><li><strong>Molde Externo:<\/strong> ocorre quando a parte externa do organismo \u00e9 coberto por sedimento que preserva suas fei\u00e7\u00f5es externas. Novamente, os exemplos mais comuns incluem os invertebrados e plantas.<\/li><\/ul>\n\n\n\n<ul><li><strong>Contramolde: <\/strong>ocorre quando a cavidade m\u00f3ldica (espa\u00e7o vazio no sedimento, que era ocupado pelo resto do organismo antes de sua dissolu\u00e7\u00e3o) \u00e9 preenchida, preservando tanto as fei\u00e7\u00f5es externas quanto internas do organismo. Desta forma, uma \u201cr\u00e9plica\u201d do organismo \u00e9 produzida.<\/li><\/ul>\n\n\n\n<p class=\"has-text-align-justify\">F\u00f3sseis s\u00e3o encontrados em todos os lugares do planeta, desde os \u00e1ridos desertos da Mong\u00f3lia at\u00e9 as geladas terras da Ant\u00e1rtica. Em conjunto, s\u00e3o capazes de reconstituir os cen\u00e1rios da biodiversidade existente em cada per\u00edodo geol\u00f3gico e demonstrar sua modifica\u00e7\u00e3o ao longo do tempo. Microf\u00f3sseis como conodontes, ostracodes e foramin\u00edferos s\u00e3o utilizados na ind\u00fastria petrol\u00edfera, possuindo al\u00e9m de seu valor cient\u00edfico um valor econ\u00f4mico expressivo. \u00c9 atrav\u00e9s dos f\u00f3sseis que podemos reconstruir seres que tanto nos encantam, como dinossauros, pterossauros, mamutes e tigres dente-de-sabre. S\u00e3o, portanto, o objeto de fasc\u00ednio que faz da Paleontologia uma ci\u00eancia t\u00e3o cativante.<\/p>\n\n\n\n<h4>Materiais de Refer\u00eancia<\/h4>\n\n\n\n<p>BENTON, Michael J.; HARPER, David. A. T. <strong>Introduction to Paleobiology and the Fossil Record. <\/strong>1.ed. Nova Jersey: Wiley-Blackwell, 2013. 608 p.<\/p>\n\n\n\n<p>CASSAB, Rita de Cassia Tardin. Objetivos e Princ\u00edpios <em>In:<\/em> CARVALHO, Ismar de Souza (Org.). <strong>Paleontologia &#8211; Volume 1: <\/strong>Conceitos e M\u00e9todos. 3.ed. Rio de Janeiro: Editora Interci\u00eancia, 2010. 756 p.<\/p>\n\n\n\n<p>VEGA, C. S.; DIAS, E. V.; RODRIGUES, S. C. F\u00f3sseis e Processos de Fossiliza\u00e7\u00e3o. <em>In: <\/em>SOARES, M.B.(Org.). <strong>A paleontologia na sala de aula. <\/strong>Ribeir\u00e3o Preto: Sociedade Brasileira de Paleontologia, 2015. p. 90-102.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\"><\/div>\n<\/div>\n\n\n\n<p><\/p>\n<\/div><\/div>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"is-layout-flow wp-block-group alignfull has-background\" style=\"background-color:#ffffff\"><div class=\"wp-block-group__inner-container\">\n<div class=\"wp-block-jetpack-layout-grid alignfull column1-desktop-grid__span-5 column1-desktop-grid__row-1 column2-desktop-grid__span-5 column2-desktop-grid__start-8 column2-desktop-grid__row-1 column1-tablet-grid__span-4 column1-tablet-grid__row-1 column2-tablet-grid__span-4 column2-tablet-grid__start-5 column2-tablet-grid__row-1 column1-mobile-grid__span-4 column1-mobile-grid__row-1 column2-mobile-grid__span-4 column2-mobile-grid__row-2\">\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\">\n<figure class=\"wp-block-image size-large is-resized is-style-rounded\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/whatsapp-image-2020-06-16-at-00.48.52.jpeg?w=580\" alt=\"\" class=\"wp-image-489\" width=\"290\" height=\"290\"\/><\/figure>\n\n\n\n<h4>Sobre o autor<\/h4>\n\n\n\n<p class=\"has-text-align-justify has-small-font-size\">Lucca Cunha \u00e9 licenciando em Geografia na UFRGS e atua como bolsista de inicia\u00e7\u00e3o \u00e0 populariza\u00e7\u00e3o da ci\u00eancia no programa <em>Ci\u00eancia na Sociedade, Ci\u00eancia na Escola<\/em> da Propesq. Tamb\u00e9m atua como volunt\u00e1rio no Laborat\u00f3rio de Paleovertebrados do Departamento de Paleontologia e Estratigrafia do Instituto de Geoci\u00eancias da UFRGS.<\/p>\n\n\n\n<ul class=\"is-layout-flex wp-block-social-links aligncenter\"><li class=\"wp-social-link wp-social-link-facebook wp-block-social-link\"><a href=\"https:\/\/facebook.com\/lucca.cunha.3\"  class=\"wp-block-social-link-anchor\"><svg width=\"24\" height=\"24\" viewBox=\"0 0 24 24\" version=\"1.1\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" aria-hidden=\"true\" focusable=\"false\"><path d=\"M12 2C6.5 2 2 6.5 2 12c0 5 3.7 9.1 8.4 9.9v-7H7.9V12h2.5V9.8c0-2.5 1.5-3.9 3.8-3.9 1.1 0 2.2.2 2.2.2v2.5h-1.3c-1.2 0-1.6.8-1.6 1.6V12h2.8l-.4 2.9h-2.3v7C18.3 21.1 22 17 22 12c0-5.5-4.5-10-10-10z\"><\/path><\/svg><span class=\"wp-block-social-link-label screen-reader-text\">Facebook<\/span><\/a><\/li>\n\n\n\n<li class=\"wp-social-link wp-social-link-instagram wp-block-social-link\"><a href=\"https:\/\/instagram.com\/luccasantoscunha\"  class=\"wp-block-social-link-anchor\"><svg width=\"24\" height=\"24\" viewBox=\"0 0 24 24\" version=\"1.1\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" aria-hidden=\"true\" focusable=\"false\"><path d=\"M12,4.622c2.403,0,2.688,0.009,3.637,0.052c0.877,0.04,1.354,0.187,1.671,0.31c0.42,0.163,0.72,0.358,1.035,0.673 c0.315,0.315,0.51,0.615,0.673,1.035c0.123,0.317,0.27,0.794,0.31,1.671c0.043,0.949,0.052,1.234,0.052,3.637 s-0.009,2.688-0.052,3.637c-0.04,0.877-0.187,1.354-0.31,1.671c-0.163,0.42-0.358,0.72-0.673,1.035 c-0.315,0.315-0.615,0.51-1.035,0.673c-0.317,0.123-0.794,0.27-1.671,0.31c-0.949,0.043-1.233,0.052-3.637,0.052 s-2.688-0.009-3.637-0.052c-0.877-0.04-1.354-0.187-1.671-0.31c-0.42-0.163-0.72-0.358-1.035-0.673 c-0.315-0.315-0.51-0.615-0.673-1.035c-0.123-0.317-0.27-0.794-0.31-1.671C4.631,14.688,4.622,14.403,4.622,12 s0.009-2.688,0.052-3.637c0.04-0.877,0.187-1.354,0.31-1.671c0.163-0.42,0.358-0.72,0.673-1.035 c0.315-0.315,0.615-0.51,1.035-0.673c0.317-0.123,0.794-0.27,1.671-0.31C9.312,4.631,9.597,4.622,12,4.622 M12,3 C9.556,3,9.249,3.01,8.289,3.054C7.331,3.098,6.677,3.25,6.105,3.472C5.513,3.702,5.011,4.01,4.511,4.511 c-0.5,0.5-0.808,1.002-1.038,1.594C3.25,6.677,3.098,7.331,3.054,8.289C3.01,9.249,3,9.556,3,12c0,2.444,0.01,2.751,0.054,3.711 c0.044,0.958,0.196,1.612,0.418,2.185c0.23,0.592,0.538,1.094,1.038,1.594c0.5,0.5,1.002,0.808,1.594,1.038 c0.572,0.222,1.227,0.375,2.185,0.418C9.249,20.99,9.556,21,12,21s2.751-0.01,3.711-0.054c0.958-0.044,1.612-0.196,2.185-0.418 c0.592-0.23,1.094-0.538,1.594-1.038c0.5-0.5,0.808-1.002,1.038-1.594c0.222-0.572,0.375-1.227,0.418-2.185 C20.99,14.751,21,14.444,21,12s-0.01-2.751-0.054-3.711c-0.044-0.958-0.196-1.612-0.418-2.185c-0.23-0.592-0.538-1.094-1.038-1.594 c-0.5-0.5-1.002-0.808-1.594-1.038c-0.572-0.222-1.227-0.375-2.185-0.418C14.751,3.01,14.444,3,12,3L12,3z M12,7.378 c-2.552,0-4.622,2.069-4.622,4.622S9.448,16.622,12,16.622s4.622-2.069,4.622-4.622S14.552,7.378,12,7.378z M12,15 c-1.657,0-3-1.343-3-3s1.343-3,3-3s3,1.343,3,3S13.657,15,12,15z M16.804,6.116c-0.596,0-1.08,0.484-1.08,1.08 s0.484,1.08,1.08,1.08c0.596,0,1.08-0.484,1.08-1.08S17.401,6.116,16.804,6.116z\"><\/path><\/svg><span class=\"wp-block-social-link-label screen-reader-text\">Instagram<\/span><\/a><\/li>\n\n\n\n<li class=\"wp-social-link wp-social-link-youtube wp-block-social-link\"><a href=\"https:\/\/www.youtube.com\/channel\/UCMBbYAIZ9ysPvmzw02nLg4A\"  class=\"wp-block-social-link-anchor\"><svg width=\"24\" height=\"24\" viewBox=\"0 0 24 24\" version=\"1.1\" xmlns=\"http:\/\/www.w3.org\/2000\/svg\" aria-hidden=\"true\" focusable=\"false\"><path d=\"M21.8,8.001c0,0-0.195-1.378-0.795-1.985c-0.76-0.797-1.613-0.801-2.004-0.847c-2.799-0.202-6.997-0.202-6.997-0.202 h-0.009c0,0-4.198,0-6.997,0.202C4.608,5.216,3.756,5.22,2.995,6.016C2.395,6.623,2.2,8.001,2.2,8.001S2,9.62,2,11.238v1.517 c0,1.618,0.2,3.237,0.2,3.237s0.195,1.378,0.795,1.985c0.761,0.797,1.76,0.771,2.205,0.855c1.6,0.153,6.8,0.201,6.8,0.201 s4.203-0.006,7.001-0.209c0.391-0.047,1.243-0.051,2.004-0.847c0.6-0.607,0.795-1.985,0.795-1.985s0.2-1.618,0.2-3.237v-1.517 C22,9.62,21.8,8.001,21.8,8.001z M9.935,14.594l-0.001-5.62l5.404,2.82L9.935,14.594z\"><\/path><\/svg><span class=\"wp-block-social-link-label screen-reader-text\">YouTube<\/span><\/a><\/li><\/ul>\n<\/div>\n\n\n\n<div class=\"wp-block-jetpack-layout-grid-column wp-block-jetpack-layout-grid__padding-none\">\n<figure class=\"wp-block-image size-large is-resized is-style-rounded\"><img decoding=\"async\" loading=\"lazy\" src=\"https:\/\/macrocollum.files.wordpress.com\/2020\/06\/heitor-lattes.jpg?w=779\" alt=\"\" class=\"wp-image-557\" width=\"290\" height=\"290\"\/><\/figure>\n\n\n\n<h4>Sobre o autor<\/h4>\n\n\n\n<p class=\"has-text-align-justify has-small-font-size\">Heitor Francischini \u00e9 licenciado em Ci\u00eancias Biol\u00f3gicas pela Universidade Federal de S\u00e3o Carlos. Mestre em Geoci\u00eancias (\u00c1rea de Concentra\u00e7\u00e3o: Paleontologia; 2014) e Doutor em Ci\u00eancias (\u00c1rea de Concentra\u00e7\u00e3o: Paleontologia; 2018) pelo PPGGeo-UFRGS. Durante o doutorado realizou per\u00edodo sandu\u00edche no New Mexico Museum of Natural History and Science (em Albuquerque, EUA) e, durante a gradua\u00e7\u00e3o, realizou interc\u00e2mbio na Universidad de la Republica (em Montevid\u00e9u, Uruguai). Atualmente \u00e9 Professor Adjunto A da Universidade Federal do Rio Grande do Sul, ministrando as disciplinas Paleontologia Aplicada \u00e0 Biologia, Paleontologia II e Paleontologia de Vertebrados para os cursos de Ci\u00eancias Biol\u00f3gicas (Licenciatura e Bacharelado) e Geologia. Possui experi\u00eancia com os seguintes temas: Paleontologia, Paleobiologia e Paleoicnologia, com \u00eanfase no registro de vertebrados continentais do Paleozoico e Mesozoico, principais temas de sua pesquisa. \u00c9 membro da Sociedade Brasileira de Paleontologia<\/p>\n<\/div>\n<\/div>\n\n\n\n<p><\/p>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"spay_email":""},"_links":{"self":[{"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=\/wp\/v2\/pages\/735"}],"collection":[{"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=735"}],"version-history":[{"count":5,"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=\/wp\/v2\/pages\/735\/revisions"}],"predecessor-version":[{"id":1254,"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=\/wp\/v2\/pages\/735\/revisions\/1254"}],"wp:attachment":[{"href":"https:\/\/www.ufrgs.br\/museupaleonto\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=735"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}