FOSSILS: RECORD OF LIFE IN THE PLANET EARTH

Through the study of fossils, it's possible to know the history of life in the geological past of planet Earth. The knowledge of the fossils has derived lines of investigation that help to understand the geological history of the planet. Thus, it is known that the geological time is divided bas...

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Prif Awduron:	Cuen Romero, Francisco Javier, Chacón-Baca, Elizabeth, Moreno-Bedmar, Josep, Velasco-de León, María Patricia
Fformat:	Online
Iaith:	spa
Cyhoeddwyd:	Universida de Sonora 2021
Mynediad Ar-lein:	https://epistemus.unison.mx/index.php/epistemus/article/view/124
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spelling	oai:http:--epistemus.unison.mx:article-1242021-08-12T17:47:08Z FOSSILS: RECORD OF LIFE IN THE PLANET EARTH FÓSILES: HISTORIA DE LA VIDA EN LA TIERRA Cuen Romero, Francisco Javier Chacón-Baca, Elizabeth Moreno-Bedmar, Josep Velasco-de León, María Patricia fósiles tiempo geología México Por medio de los fósiles es posible conocer la historia de la vida en el pasado geológico del planeta Tierra. fossils time geology Mexico Through the study of fossils, it is possible to know the history of life in the geological past of planet Earth. Through the study of fossils, it's possible to know the history of life in the geological past of planet Earth. The knowledge of the fossils has derived lines of investigation that help to understand the geological history of the planet. Thus, it is known that the geological time is divided based on the forms of life that inhabited the planet. Life likely originated in the early Precambrian, more than 3800 million years ago, however, the oldest fossil remains of lithified bacterial communities, known as stromatolites, date to approximately 3550 million years ago. During the Paleozoic, most of the groups of plants, invertebrates and vertebrates that are known today appeared. Among all the organisms that appear at that time, brachiopods, trilobites, and graptolites are the dominant forms. In the Mesozoic, large reptiles, such as the dinosaurs, dominated, however, the most notable index invertebrates of this time correspond to ammonites and belemnites. Por medio de los fósiles es posible conocer la historia de la vida en el pasado geológico del planeta Tierra.  Es probable que la vida se originó a inicios del Precámbrico, hace más de 3800 millones de años, sin embargo, los restos fósiles más antiguos de comunidades bacterianas litificadas, conocidos como estromatolitos, datan de hace aproximadamente 3550 millones de años. Durante el Paleozoico, aparecieron la mayoría de los grupos de plantas, invertebrados y vertebrados que se conocen actualmente. Entre todos los organismos que aparecen en este tiempo, los braquiópodos, trilobites y graptolites son las formas dominantes. En el Mesozoico dominaron los grandes reptiles, como son los dinosaurios, para México los fósiles índice notables de este tiempo corresponden a invertebrados como los ammonites y los belemnites. En el Cenozoico dominan los mamíferos, los cuales presentan una distribución mundial, entre estos los humanos. Universida de Sonora 2021-05-25 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Academy Academia application/pdf application/pdf https://epistemus.unison.mx/index.php/epistemus/article/view/124 10.36790/epistemus.v14i28.124 EPISTEMUS; Vol. 14 No. 28 (2020): Engineering, Administration, Philosophy and Social Responsibility; 51-62 EPISTEMUS; Vol. 14 Núm. 28 (2020): Ingeniería, Administración, Filosofía y Responsabilidad Social; 51-62 2007-8196 2007-4530 spa https://epistemus.unison.mx/index.php/epistemus/article/view/124/95 https://epistemus.unison.mx/index.php/epistemus/article/view/124/104 2020-2022 2020-2022 Derechos de autor 2021 EPISTEMUS https://creativecommons.org/licenses/by-nc-nd/4.0
institution	Epistemus
collection	OJS
language	spa
format	Online
author	Cuen Romero, Francisco Javier Chacón-Baca, Elizabeth Moreno-Bedmar, Josep Velasco-de León, María Patricia
spellingShingle	Cuen Romero, Francisco Javier Chacón-Baca, Elizabeth Moreno-Bedmar, Josep Velasco-de León, María Patricia FOSSILS: RECORD OF LIFE IN THE PLANET EARTH
author_facet	Cuen Romero, Francisco Javier Chacón-Baca, Elizabeth Moreno-Bedmar, Josep Velasco-de León, María Patricia
author_sort	Cuen Romero, Francisco Javier
title	FOSSILS: RECORD OF LIFE IN THE PLANET EARTH
title_short	FOSSILS: RECORD OF LIFE IN THE PLANET EARTH
title_full	FOSSILS: RECORD OF LIFE IN THE PLANET EARTH
title_fullStr	FOSSILS: RECORD OF LIFE IN THE PLANET EARTH
title_full_unstemmed	FOSSILS: RECORD OF LIFE IN THE PLANET EARTH
title_sort	fossils: record of life in the planet earth
description	Through the study of fossils, it's possible to know the history of life in the geological past of planet Earth. The knowledge of the fossils has derived lines of investigation that help to understand the geological history of the planet. Thus, it is known that the geological time is divided based on the forms of life that inhabited the planet. Life likely originated in the early Precambrian, more than 3800 million years ago, however, the oldest fossil remains of lithified bacterial communities, known as stromatolites, date to approximately 3550 million years ago. During the Paleozoic, most of the groups of plants, invertebrates and vertebrates that are known today appeared. Among all the organisms that appear at that time, brachiopods, trilobites, and graptolites are the dominant forms. In the Mesozoic, large reptiles, such as the dinosaurs, dominated, however, the most notable index invertebrates of this time correspond to ammonites and belemnites.
publisher	Universida de Sonora
publishDate	2021
url	https://epistemus.unison.mx/index.php/epistemus/article/view/124
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FOSSILS: RECORD OF LIFE IN THE PLANET EARTH

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