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Perspectivas atuais sobre tecidos moles não mineralizados em fósseis de dinossauros não avianos
Entrada monumental da Gruta do Lago Azul, ricamente ornamentada por estalactites e estalagmites, situada no município de Bonito, a E da Serra da Bodoquena e a sudoeste do município de Miranda. A região serrana foi edificada em unidades carbonáticas dos grupos Cuiabá e Corumbá, de idade Neoproterozoica. Fotografia: Adriano Gambarini.
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Palavras-chave

Paleontologia molecular
Preservação excepcional
Moléculas orgânicas
Mesozoico

Como Citar

ALVES, Everton Fernando; MACHADO, Marcio Fraiberg. Perspectivas atuais sobre tecidos moles não mineralizados em fósseis de dinossauros não avianos. Terrae Didatica, Campinas, SP, v. 16, p. e020028, 2020. DOI: 10.20396/td.v16i0.8659539. Disponível em: https://periodicos.sbu.unicamp.br/ojs/index.php/td/article/view/8659539. Acesso em: 26 abr. 2024.

Resumo

Dados a respeito da frequência de achados de tecidos moles não mineralizados ainda são escassos e os que já foram sistematizados estão dispersos na literatura, associando a ideia das descobertas a fenômenos isolados. Este artigo apresenta uma revisão da literatura, publicada nos últimos 50 anos, com o objetivo de compreender a frequência de tecidos moles não mineralizados em fósseis de dinossauros não avianos e os atuais limites temporais de sobrevivência esperada dessas biomoléculas. Os resultados identificaram 52 artigos que descrevem material orgânico preservado em fósseis de dinossauros não avianos, considerados geológica, geográfica e taxonomicamente abrangentes nas rochas mesozoicas. Ainda assim, acredita-se que a frequência é subnotificada devido à atual resistência em aceitar as descobertas como sendo de remanescentes orgânicos e à falta de recursos para esse tipo de detecção. A partir do desenvolvimento de novas tecnologias, pode-se prever que tais achados provavelmente serão a norma e não a exceção.

https://doi.org/10.20396/td.v16i0.8659539
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