{"id":1606,"date":"2024-09-02T10:40:14","date_gmt":"2024-09-02T08:40:14","guid":{"rendered":"https:\/\/clientes.munecarusa.com\/mp\/?page_id=1606"},"modified":"2025-08-15T13:02:16","modified_gmt":"2025-08-15T11:02:16","slug":"era-paleozoica","status":"publish","type":"page","link":"https:\/\/clientes.munecarusa.com\/mp\/era-paleozoica\/","title":{"rendered":"Era Paleozoica"},"content":{"rendered":"<p>[et_pb_section fb_built=\u00bb1&#8243; custom_padding_last_edited=\u00bboff|phone\u00bb disabled_on=\u00bboff|off|off\u00bb admin_label=\u00bbFondo Men\u00fa\u00bb _builder_version=\u00bb4.27.0&#8243; background_color=\u00bb#006633&#8243; custom_margin=\u00bb0px||20px||false|false\u00bb custom_padding=\u00bb0px||0px||true|false\u00bb collapsed=\u00bbon\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_section][et_pb_section fb_built=\u00bb1&#8243; custom_padding_last_edited=\u00bbon|phone\u00bb disabled_on=\u00bboff|off|off\u00bb admin_label=\u00bbIntroducci\u00f3n\u00bb _builder_version=\u00bb4.27.0&#8243; background_enable_color=\u00bboff\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||0px||false|false\u00bb custom_padding_tablet=\u00bb10px||0px||false|false\u00bb custom_padding_phone=\u00bb20px||||false|false\u00bb global_colors_info=\u00bb{}\u00bb collapsed=\u00bbon\u00bb][et_pb_row make_equal=\u00bbon\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_post_title meta=\u00bboff\u00bb featured_image=\u00bboff\u00bb _builder_version=\u00bb4.27.0&#8243; _module_preset=\u00bbdefault\u00bb title_font=\u00bb|600||on|||||\u00bb title_text_align=\u00bbcenter\u00bb title_text_color=\u00bb#000000&#8243; title_font_size=\u00bb70px\u00bb title_letter_spacing=\u00bb1px\u00bb custom_margin=\u00bb||10px||false|false\u00bb animation_style=\u00bbslide\u00bb animation_direction=\u00bbbottom\u00bb title_font_size_tablet=\u00bb50px\u00bb title_font_size_phone=\u00bb30px\u00bb title_font_size_last_edited=\u00bbon|phone\u00bb title_text_shadow_style=\u00bbpreset1&#8243; global_colors_info=\u00bb{}\u00bb][\/et_pb_post_title][et_pb_text content_tablet=\u00bb<\/p>\n<h4>C\u00c1MBRICO &#8211; ORDOV\u00cdCICO &#8211; SIL\u00daRICO<br \/>\nDEV\u00d3NICO &#8211; CARBON\u00cdFERO &#8211; P\u00c9RMICO<\/h4>\n<p>\u00bb content_phone=\u00bb<\/p>\n<h4>C\u00c1MBRICO &#8211; ORDOV\u00cdCICO &#8211; SIL\u00daRICO<br \/>\nDEV\u00d3NICO &#8211; CARBON\u00cdFERO &#8211; P\u00c9RMICO<\/h4>\n<p>\u00bb content_last_edited=\u00bbon|desktop\u00bb _builder_version=\u00bb4.27.0&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb|700||on|||||\u00bb header_4_text_align=\u00bbcenter\u00bb header_4_text_color=\u00bb#006633&#8243; header_4_font_size=\u00bb30px\u00bb header_4_line_height=\u00bb1.4em\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb animation_style=\u00bbzoom\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_tablet=\u00bb22px\u00bb header_4_font_size_phone=\u00bb11px\u00bb header_4_font_size_last_edited=\u00bbon|phone\u00bb header_4_text_shadow_style=\u00bbpreset1&#8243; global_colors_info=\u00bb{}\u00bb header_4_text_color__hover_enabled=\u00bboff|hover\u00bb]<\/p>\n<h4>C\u00c1MBRICO &#8211; ORDOV\u00cdCICO &#8211; SIL\u00daRICO &#8211; DEV\u00d3NICO &#8211; CARBON\u00cdFERO &#8211; P\u00c9RMICO<\/h4>\n<p>[\/et_pb_text][et_pb_divider color=\u00bb#999999&#8243; admin_label=\u00bbSeparador\u00bb _builder_version=\u00bb4.27.0&#8243; _module_preset=\u00bbdefault\u00bb custom_margin=\u00bb-20px||0px||false|false\u00bb custom_padding=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_divider][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.4&#8243; text_text_color=\u00bb#444444&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb animation_style=\u00bbzoom\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb global_colors_info=\u00bb{}\u00bb]<\/p>\n<h2 style=\"text-align: justify;\"><img loading=\"lazy\" decoding=\"async\" class=\" wp-image-4309 alignleft\" src=\"https:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/margen-huella.png\" alt=\"Era Paleozoica\" width=\"30\" height=\"50\" \/><\/h2>\n<p>El Paleozoico o era paleozoica es una divisi\u00f3n de la escala temporal geol\u00f3gica que pertenece al e\u00f3n Fanerozoico, con la categor\u00eda de era (como tiempo) y eratema (como conjunto de rocas). El Paleozoico sucede al supere\u00f3n Prec\u00e1mbrico y precede al Mesozoico. De m\u00e1s de 290 millones de a\u00f1os (M.a.) de duraci\u00f3n, se inici\u00f3 hace 541 millones de a\u00f1os y acab\u00f3 hace unos 252 millones de a\u00f1os.\u200b Su nombre procede del griego \u00abpalaio\/\u03c0\u03b1\u03bb\u03b1\u03b9\u03bf\u00bb (\u2018viejo\u2019) y \u00abzoe\/\u03b6\u03c9\u03b7\u00bb (\u2018vida\u2019), que significa \u2018vida antigua\u2019. Anteriormente era conocido por los t\u00e9rminos, hoy obsoletos, de Primario o era primaria.<\/p>\n<p>Geol\u00f3gicamente, la era paleozoica se inicia poco despu\u00e9s de la desintegraci\u00f3n del supercontinente Pannotia y acaba con la formaci\u00f3n del supercontinente Pangea. Durante la mayor parte de la era, la superficie de la Tierra se divide en un n\u00famero relativamente peque\u00f1o de continentes.<\/p>\n<p>El Paleozoico abarca desde la proliferaci\u00f3n de animales con concha y exoesqueleto hasta que el mundo empez\u00f3 a ser dominado por los grandes reptiles y por plantas relativamente modernas, como las con\u00edferas. [\/et_pb_text][et_pb_divider color=\u00bb#999999&#8243; admin_label=\u00bbSeparador\u00bb _builder_version=\u00bb4.27.0&#8243; _module_preset=\u00bbdefault\u00bb custom_margin=\u00bb||||false|false\u00bb custom_padding=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_divider][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=\u00bb1&#8243; custom_padding_last_edited=\u00bboff|phone\u00bb disabled_on=\u00bboff|off|off\u00bb admin_label=\u00bbContenido\u00bb _builder_version=\u00bb4.27.0&#8243; background_enable_color=\u00bboff\u00bb custom_margin=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb0px||0px||true|false\u00bb global_colors_info=\u00bb{}\u00bb collapsed=\u00bbon\u00bb][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb admin_label=\u00bbTect\u00f3nica\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||0px||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb disabled_on=\u00bboff|off|off\u00bb _builder_version=\u00bb4.27.0&#8243; header_4_font=\u00bb|700||on|||||\u00bb header_4_text_align=\u00bbleft\u00bb header_4_text_color=\u00bb#444444&#8243; header_4_font_size=\u00bb30px\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb animation_style=\u00bbzoom\u00bb text_font_size_last_edited=\u00bboff|phone\u00bb text_line_height_last_edited=\u00bboff|phone\u00bb header_4_font_size_tablet=\u00bb25px\u00bb header_4_font_size_phone=\u00bb20px\u00bb header_4_font_size_last_edited=\u00bbon|phone\u00bb global_colors_info=\u00bb{}\u00bb text_line_height__hover_enabled=\u00bboff|hover\u00bb]<\/p>\n<h4>TECT\u00d3NICA<\/h4>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00bb1_2,1_2&#8243; make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb0px||||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb0px||||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.2&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]Durante el per\u00edodo entre finales del Prec\u00e1mbrico y el Paleozoico, la mayor parte de la evidencia de la historia temprana de la Tierra fue destruida por la erosi\u00f3n. Desde el inicio de la era paleozoica, los mares poco profundos invadieron los continentes. La configuraci\u00f3n de los continentes era muy diferente de la actual. En primer lugar, en esta era se dan al menos dos orogenias, la Caledoniana (durante el Sil\u00farico superior) y la Herciniana (en el Permocarbon\u00edfero), que afectaron a toda la superficie terrestre, generando cadenas monta\u00f1osas como, por ejemplo, el macizo Hesp\u00e9rico en el hemisferio norte; aunque como se ha dicho, sus huellas se detectan por todo el globo.<\/p>\n<p>La era paleozoica se inicia poco despu\u00e9s de la desintegraci\u00f3n del supercontinente Pannotia y el final de una era glacial. Durante el Paleozoico inferior, la superficie de la Tierra se divide en un n\u00famero relativamente peque\u00f1o de continentes. Hacia el final de la era, los continentes se reunieron en el supercontinente Pangea, que inclu\u00eda la mayor parte de la superficie terrestre del planeta. [\/et_pb_text][\/et_pb_column][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_image src=\u00bbhttps:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/Mapa-Era-Paleozoica.webp\u00bb alt=\u00bbEra Paleozoica\u00bb show_in_lightbox=\u00bbon\u00bb use_overlay=\u00bbon\u00bb overlay_icon_color=\u00bb#660000&#8243; hover_overlay_color=\u00bbrgba(0,0,0,0.5)\u00bb force_fullwidth=\u00bbon\u00bb overlay_icon_color_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb admin_label=\u00bbSubdivisiones\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||0px||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb disabled_on=\u00bboff|off|off\u00bb _builder_version=\u00bb4.27.0&#8243; header_4_font=\u00bb|700||on|||||\u00bb header_4_text_align=\u00bbleft\u00bb header_4_text_color=\u00bb#444444&#8243; header_4_font_size=\u00bb30px\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb animation_style=\u00bbzoom\u00bb text_font_size_last_edited=\u00bboff|phone\u00bb text_line_height_last_edited=\u00bboff|phone\u00bb header_4_font_size_tablet=\u00bb25px\u00bb header_4_font_size_phone=\u00bb20px\u00bb header_4_font_size_last_edited=\u00bbon|phone\u00bb global_colors_info=\u00bb{}\u00bb text_line_height__hover_enabled=\u00bboff|hover\u00bb]<\/p>\n<h4>SUBDIVISIONES<\/h4>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00bb1_2,1_2&#8243; make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb0px||||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb0px||||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.2&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]La era paleozoica, al igual que las dem\u00e1s, se divide en per\u00edodos. Este sistema geol\u00f3gico de divisi\u00f3n por per\u00edodos nos permite conocer a profundidad qu\u00e9 sucedi\u00f3 en cada etapa y observar de una manera m\u00e1s espec\u00edfica los procesos que marcaron la historia. Vamos a conocer los per\u00edodos en los que se subdivide el paleozoico.<\/p>\n<p>La era paleozoica se divide en seis per\u00edodos: C\u00e1mbrico (la vida animal florece en los mares), Ordov\u00edcico (dominan los invertebrados), Sil\u00farico (primer animal de respiraci\u00f3n a\u00e9rea), Dev\u00f3nico (aparecen peces con escamas duras y los anfibios), Carbon\u00edfero (aparecen grandes bosques de helechos, primeros reptiles y los primeros insectos voladores), y P\u00e9rmico (al final del P\u00e9rmico ocurre la mayor extinci\u00f3n, la extinci\u00f3n masiva del P\u00e9rmico-Tri\u00e1sico).[\/et_pb_text][\/et_pb_column][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_image src=\u00bbhttps:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/Subdivisiones-Era-Paleozoica.webp\u00bb alt=\u00bbEra Paleozoica\u00bb show_in_lightbox=\u00bbon\u00bb use_overlay=\u00bbon\u00bb overlay_icon_color=\u00bb#660000&#8243; hover_overlay_color=\u00bbrgba(0,0,0,0.5)\u00bb force_fullwidth=\u00bbon\u00bb overlay_icon_color_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb admin_label=\u00bbClima\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||0px||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb disabled_on=\u00bboff|off|off\u00bb _builder_version=\u00bb4.27.0&#8243; header_4_font=\u00bb|700||on|||||\u00bb header_4_text_align=\u00bbleft\u00bb header_4_text_color=\u00bb#444444&#8243; header_4_font_size=\u00bb30px\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb animation_style=\u00bbzoom\u00bb text_font_size_last_edited=\u00bboff|phone\u00bb text_line_height_last_edited=\u00bboff|phone\u00bb header_4_font_size_tablet=\u00bb25px\u00bb header_4_font_size_phone=\u00bb20px\u00bb header_4_font_size_last_edited=\u00bbon|tablet\u00bb global_colors_info=\u00bb{}\u00bb text_line_height__hover_enabled=\u00bboff|hover\u00bb]<\/p>\n<h4>CLIMA<\/h4>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00bb1_2,1_2&#8243; make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb0px||0px||true|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb0px||0px||true|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.0&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]El Paleozoico inferior probablemente ten\u00eda un clima moderado al inicio, pero se torn\u00f3 cada vez m\u00e1s c\u00e1lido en el transcurso del C\u00e1mbrico. Tambi\u00e9n se produjo el segundo incremento sostenido del nivel del mar m\u00e1s grande del Fanerozoico. Sin embargo, esta tendencia se vio contrarrestada por el desplazamiento de Gondwana hacia el sur con velocidad considerable, por lo que, en tiempos de Ordov\u00edcico, la mayor\u00eda de Gondwana occidental (\u00c1frica y Am\u00e9rica del Sur) se asent\u00f3 directamente sobre el Polo Sur.<\/p>\n<p>En esta \u00e9poca el clima est\u00e1 tambi\u00e9n fuertemente influenciado por la zona, con el resultado de que el \u00abclima\u00bb, en un sentido global, se convirti\u00f3 en c\u00e1lido. Sin embargo, el medio ambiente de la mayor\u00eda de los organismos de la \u00e9poca, la plataforma marina continental, se fue enfriando paulatinamente. Por otro lado, B\u00e1ltica (Europa del Norte y Rusia) y Laurentia (este de Am\u00e9rica del Norte y Groenlandia) se mantuvo en la zona tropical, mientras que China y Australia se situaban en aguas m\u00e1s templadas.[\/et_pb_text][\/et_pb_column][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_image src=\u00bbhttps:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/Clima-Era-Paleozoica.webp\u00bb alt=\u00bbEra Paleozoica\u00bb show_in_lightbox=\u00bbon\u00bb use_overlay=\u00bbon\u00bb overlay_icon_color=\u00bb#660000&#8243; hover_overlay_color=\u00bbrgba(0,0,0,0.5)\u00bb force_fullwidth=\u00bbon\u00bb overlay_icon_color_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.2&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]El Paleozoico inferior termin\u00f3, bastante abruptamente, con la corta, pero al parecer intensa, glaciaci\u00f3n del Ordov\u00edcico superior. Esta ola de fr\u00edo caus\u00f3 la segunda mayor extinci\u00f3n masiva del E\u00f3n Fanerozoico. Con el tiempo, el clima se fue haciendo m\u00e1s c\u00e1lido.<\/p>\n<p>El Paleozoico medio fue una \u00e9poca de gran estabilidad. El nivel del mar hab\u00eda descendido coincidiendo con la glaciaci\u00f3n, pero se recuper\u00f3 lentamente durante el transcurso del Sil\u00farico y Dev\u00f3nico. La lenta fusi\u00f3n de Laurentia y B\u00e1ltica, y el lento movimiento hacia el norte de los fragmentos de Gondwana crearon numerosas nuevas regiones de aguas relativamente c\u00e1lidas. Como las plantas colonizaron los m\u00e1rgenes continentales, el nivel de ox\u00edgeno se increment\u00f3 y el di\u00f3xido de carbono disminuy\u00f3, aunque mucho menos dram\u00e1ticamente.<\/p>\n<p>El gradiente de temperaturas norte-sur tambi\u00e9n parece haber sido moderado, o simplemente los organismos metazoarios se hicieron m\u00e1s resistentes, o ambas cosas. En cualquier caso, el extremo sur de los m\u00e1rgenes continentales de la Ant\u00e1rtida y el Oeste de Gondwana cada vez se hicieron menos est\u00e9riles.<\/p>\n<p>El Dev\u00f3nico termin\u00f3 con una serie de pulsos que acabaron con gran parte de los vertebrados del Paleozoico Medio, sin reducir notablemente la diversidad de especies en general.<\/p>\n<p>El Paleozoico superior fue una \u00e9poca que nos ha dejado un gran n\u00famero de preguntas sin respuesta. El Misis\u00edpico comenz\u00f3 con un repunte en el ox\u00edgeno atmosf\u00e9rico, mientras que el di\u00f3xido de carbono cay\u00f3 a m\u00ednimos. Esto desestabiliz\u00f3 el clima y llev\u00f3 a una, tal vez dos, glaciaciones durante el Carbon\u00edfero. Estas son mucho m\u00e1s severas que la breve glaciaci\u00f3n del Ordov\u00edcico superior, pero esta vez los efectos sobre la biota fueron intrascendentes.<\/p>\n<p>Para comienzo del P\u00e9rmico, tanto el ox\u00edgeno como el di\u00f3xido de carbono se hab\u00eda recuperado a niveles m\u00e1s normales. Por otro lado, la formaci\u00f3n de Pangea cre\u00f3 extensas regiones interiores \u00e1ridas sujetas a temperaturas extremas. El P\u00e9rmico superior se asocia con la ca\u00edda del nivel del mar, el aumento del di\u00f3xido de carbono y un deterioro clim\u00e1tico general, que culmin\u00f3 con la devastaci\u00f3n de la extinci\u00f3n masiva del P\u00e9rmico-Tri\u00e1sico.[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb admin_label=\u00bbFlora\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||0px||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb disabled_on=\u00bboff|off|off\u00bb _builder_version=\u00bb4.27.0&#8243; header_4_font=\u00bb|700||on|||||\u00bb header_4_text_align=\u00bbleft\u00bb header_4_text_color=\u00bb#444444&#8243; header_4_font_size=\u00bb30px\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb animation_style=\u00bbzoom\u00bb text_font_size_last_edited=\u00bboff|phone\u00bb text_line_height_last_edited=\u00bboff|phone\u00bb header_4_font_size_tablet=\u00bb25px\u00bb header_4_font_size_phone=\u00bb20px\u00bb header_4_font_size_last_edited=\u00bbon|tablet\u00bb global_colors_info=\u00bb{}\u00bb text_line_height__hover_enabled=\u00bboff|hover\u00bb]<\/p>\n<h4>FLORA<\/h4>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00bb1_2,1_2&#8243; make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb0px||0px||true|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb0px||0px||true|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.0&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]En la era paleozoica la vida estaba confinada casi exclusivamente a los oc\u00e9anos. En este entorno marino, las formas de vida predominantes inclu\u00edan el fitoplancton, las algas, esponjas y bacterias fotosint\u00e9ticas, que formaban la base de las cadenas alimenticias. Los organismos unicelulares y multicelulares simples prosperaban en los mares, ya que la vida terrestre todav\u00eda no hab\u00eda comenzado a desarrollarse. Durante este tiempo, la fotos\u00edntesis ya jugaba un papel crucial en la producci\u00f3n de ox\u00edgeno y en el equilibrio ecol\u00f3gico de los oc\u00e9anos.<\/p>\n<p>A medida que avanzaba la era Paleozoica, la vida experiment\u00f3 una diversificaci\u00f3n sin precedentes. En el per\u00edodo Sil\u00farico, aproximadamente hace 443 millones de a\u00f1os, aparecieron las primeras plantas terrestres. Estas primitivas formas de vida vegetal, aunque fundamentales para la colonizaci\u00f3n de la tierra firme, carec\u00edan de tejidos vasculares, lo que les limitaba su capacidad para absorber agua y nutrientes del suelo de manera eficiente. Por ello, se cree que estas plantas eran de tama\u00f1o peque\u00f1o y estaban limitadas a h\u00e1bitats h\u00famedos, donde el agua era m\u00e1s accesible.<\/p>\n<p>El cambio m\u00e1s significativo en la flora ocurri\u00f3 durante el Dev\u00f3nico, hace unos 419 millones de a\u00f1os, cuando las plantas comenzaron a evolucionar para adaptarse mejor al entorno terrestre. Aqu\u00ed es donde surgieron los primeros helechos, as\u00ed como plantas m\u00e1s complejas que presentaban estructuras vasculares. Esta innovaci\u00f3n permiti\u00f3 que las plantas pudieran crecer en tama\u00f1o, llegando a formar los primeros \u00e1rboles y arbustos, lo que marc\u00f3 el inicio de los primeros ecosistemas boscosos en la Tierra.<\/p>\n<p>Hacia el final del Paleozoico, especialmente durante el Carbon\u00edfero, hace aproximadamente 359 millones de a\u00f1os, vastas extensiones de bosques ya cubr\u00edan los continentes. Estos bosques consist\u00edan en helechos gigantes, equisetos y otras plantas que dominaron la superficie terrestre.<\/p>\n<p>Adem\u00e1s, la alta concentraci\u00f3n de ox\u00edgeno en la atm\u00f3sfera contribuy\u00f3 al desarrollo de una flora exuberante.[\/et_pb_text][\/et_pb_column][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_image src=\u00bbhttps:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/Flora-Era-Paleozoica.webp\u00bb alt=\u00bbEra Paleozoica\u00bb show_in_lightbox=\u00bbon\u00bb use_overlay=\u00bbon\u00bb overlay_icon_color=\u00bb#660000&#8243; hover_overlay_color=\u00bbrgba(0,0,0,0.5)\u00bb force_fullwidth=\u00bbon\u00bb overlay_icon_color_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_padding=\u00bb||0px||false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.0&#8243; text_text_color=\u00bb#FFFFFF\u00bb header_4_font=\u00bb||||||||\u00bb background_color=\u00bb#660000&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbcenter\u00bb custom_padding=\u00bb20px|30px|20px|30px|true|true\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]Neuropteris del carbon\u00edfero superior.[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.2&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]Durante el P\u00e9rmico, hacia el final del Paleozoico, las primeras con\u00edferas hicieron su aparici\u00f3n, marcando el surgimiento de plantas m\u00e1s modernas y resistentes, que lograr\u00edan perdurar y evolucionar en las eras siguientes.<\/p>\n<p>El Dev\u00f3nico termin\u00f3 con una serie de pulsos que acabaron con gran parte de los vertebrados del Paleozoico Medio, sin reducir notablemente la diversidad de especies en general.<\/p>\n<p>El Paleozoico superior fue una \u00e9poca que nos ha dejado un gran n\u00famero de preguntas sin respuesta. El Misis\u00edpico comenz\u00f3 con un repunte en el ox\u00edgeno atmosf\u00e9rico, mientras que el di\u00f3xido de carbono cay\u00f3 a m\u00ednimos. Esto desestabiliz\u00f3 el clima y llev\u00f3 a una, tal vez dos, glaciaciones durante el Carbon\u00edfero. Estas son mucho m\u00e1s severas que la breve glaciaci\u00f3n del Ordov\u00edcico superior, pero esta vez los efectos sobre la biota fueron intrascendentes.<\/p>\n<p>Para comienzo del P\u00e9rmico, tanto el ox\u00edgeno como el di\u00f3xido de carbono se hab\u00eda recuperado a niveles m\u00e1s normales. Por otro lado, la formaci\u00f3n de Pangea cre\u00f3 extensas regiones interiores \u00e1ridas sujetas a temperaturas extremas. El P\u00e9rmico superior se asocia con la ca\u00edda del nivel del mar, el aumento del di\u00f3xido de carbono y un deterioro clim\u00e1tico general, que culmin\u00f3 con la devastaci\u00f3n de la extinci\u00f3n masiva del P\u00e9rmico-Tri\u00e1sico.[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb admin_label=\u00bbFauna\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb||0px||false|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb disabled_on=\u00bboff|off|off\u00bb _builder_version=\u00bb4.27.0&#8243; header_4_font=\u00bb|700||on|||||\u00bb header_4_text_align=\u00bbleft\u00bb header_4_text_color=\u00bb#444444&#8243; header_4_font_size=\u00bb30px\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb animation_style=\u00bbzoom\u00bb text_font_size_last_edited=\u00bboff|phone\u00bb text_line_height_last_edited=\u00bboff|phone\u00bb header_4_font_size_tablet=\u00bb25px\u00bb header_4_font_size_phone=\u00bb20px\u00bb header_4_font_size_last_edited=\u00bbon|phone\u00bb global_colors_info=\u00bb{}\u00bb text_line_height__hover_enabled=\u00bboff|hover\u00bb]<\/p>\n<h4>FAUNA<\/h4>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=\u00bb1_2,1_2&#8243; make_equal=\u00bbon\u00bb custom_padding_last_edited=\u00bboff|phone\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb0px||0px||true|false\u00bb custom_margin_phone=\u00bb||||false|false\u00bb custom_margin_last_edited=\u00bboff|phone\u00bb custom_padding=\u00bb0px||0px||true|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.0&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]El contenido biol\u00f3gico de la era paleozoica es bastante rico; comprende numerosas formas de vida acu\u00e1tica: algas, esponjas, corales, braqui\u00f3podos, moluscos bivalvos, gaster\u00f3podos y cefal\u00f3podos; entre los artr\u00f3podos destacan los trilobites y los primeros insectos; aparte, tambi\u00e9n los primeros ar\u00e1cnidos (que son los primeros animales terrestres) y los equinodermos. Se desarrollan las plantas vasculares y pteridofitas (o helechos), especialmente abundantes durante el Carbon\u00edfero. Tambi\u00e9n en esta era aparecen los primeros vertebrados, peces cartilaginosos, anfibios e, incluso, los primeros reptiles.<\/p>\n<p>El l\u00edmite inferior (m\u00e1s antiguo) de esta era, cl\u00e1sicamente la marcaba la primera aparici\u00f3n de criaturas tales como trilobites y arqueociatos. La pr\u00e1ctica moderna establece este l\u00edmite como la primera aparici\u00f3n del distintivo icnof\u00f3sil Trichophycus pedum.<\/p>\n<p>El l\u00edmite superior (m\u00e1s joven) se ha fijado en el gran evento de extinci\u00f3n masiva ocurrido 300 millones de a\u00f1os m\u00e1s tarde, la extinci\u00f3n masiva del P\u00e9rmico-Tri\u00e1sico.[\/et_pb_text][\/et_pb_column][et_pb_column type=\u00bb1_2&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_image src=\u00bbhttps:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/Fauna-Era-Paleozoica.webp\u00bb alt=\u00bbEra Paleozoica\u00bb show_in_lightbox=\u00bbon\u00bb use_overlay=\u00bbon\u00bb overlay_icon_color=\u00bb#660000&#8243; hover_overlay_color=\u00bbrgba(0,0,0,0.5)\u00bb force_fullwidth=\u00bbon\u00bb overlay_icon_color_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb custom_margin=\u00bb||0px||false|false\u00bb custom_padding=\u00bb||0px||false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_image][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.0&#8243; text_text_color=\u00bb#FFFFFF\u00bb header_4_font=\u00bb||||||||\u00bb background_color=\u00bb#660000&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbcenter\u00bb custom_padding=\u00bb20px|30px|20px|30px|true|true\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]Nueva especie de Trilobites (Chelediscus Garzoni).[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row make_equal=\u00bbon\u00bb _builder_version=\u00bb4.27.0&#8243; background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb custom_margin=\u00bb||||false|false\u00bb custom_padding=\u00bb||||false|false\u00bb animation_style=\u00bbslide\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb4_4&#8243; _builder_version=\u00bb4.16&#8243; custom_padding=\u00bb|||\u00bb global_colors_info=\u00bb{}\u00bb custom_padding__hover=\u00bb|||\u00bb][et_pb_text content_last_edited=\u00bboff|desktop\u00bb _builder_version=\u00bb4.27.2&#8243; text_text_color=\u00bb#444444&#8243; header_4_font=\u00bb||||||||\u00bb background_size=\u00bbinitial\u00bb background_position=\u00bbtop_left\u00bb background_repeat=\u00bbrepeat\u00bb text_orientation=\u00bbjustified\u00bb text_font_size_tablet=\u00bb16px\u00bb text_font_size_phone=\u00bb14px\u00bb text_font_size_last_edited=\u00bbon|phone\u00bb text_line_height_tablet=\u00bb1.7em\u00bb text_line_height_phone=\u00bb1.6em\u00bb text_line_height_last_edited=\u00bbon|phone\u00bb header_4_font_size_last_edited=\u00bboff|phone\u00bb global_colors_info=\u00bb{}\u00bb]Al comienzo de la \u00e9poca, las formas de vida se limitan a bacterias, algas, esponjas y una gran variedad de formas pluricelulares enigm\u00e1ticas conocidas colectivamente como fauna de Ediacara. Un gran n\u00famero de planes corporales aparecieron casi simult\u00e1neamente al comienzo de la era, un fen\u00f3meno conocido como explosi\u00f3n c\u00e1mbrica.<\/p>\n<p>Hay algunas pruebas de que formas simples de vida hab\u00edan invadido la tierra al inicio dela era paleozoica, pero la mayor parte de las plantas y animales no colonizaron la tierra hasta el Sil\u00farico y no prosperaron hasta el Dev\u00f3nico. Aunque se conocen vertebrados primitivos al principio del Paleozoico, la fauna est\u00e1 dominada por los invertebrados hasta mediados del Paleozoico. Los peces se diversifican en el Dev\u00f3nico.<\/p>\n<p>Durante el Paleozoico tard\u00edo, grandes bosques de plantas primitivas prosperaron en tierra, formando los grandes yacimientos de carb\u00f3n de Europa y del Este de Norteam\u00e9rica. A finales de la era se desarrollaron los primeros grandes reptiles y las primeras plantas modernas (con\u00edferas).[\/et_pb_text][et_pb_divider color=\u00bb#999999&#8243; admin_label=\u00bbSeparador\u00bb _builder_version=\u00bb4.27.0&#8243; _module_preset=\u00bbdefault\u00bb custom_margin=\u00bb||||false|false\u00bb custom_padding=\u00bb||||false|false\u00bb global_colors_info=\u00bb{}\u00bb][\/et_pb_divider][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=\u00bb1&#8243; custom_padding_last_edited=\u00bboff|desktop\u00bb admin_label=\u00bbApartados\u00bb _builder_version=\u00bb4.27.0&#8243; custom_margin=\u00bb||||false|false\u00bb custom_padding=\u00bb0px||0px||true|false\u00bb custom_padding_tablet=\u00bb||||false|false\u00bb custom_padding_phone=\u00bb||||false|false\u00bb collapsed=\u00bbon\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_row column_structure=\u00bb1_3,1_3,1_3&#8243; _builder_version=\u00bb4.27.0&#8243; _module_preset=\u00bbdefault\u00bb animation_style=\u00bbslide\u00bb animation_direction=\u00bbbottom\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_column type=\u00bb1_3&#8243; _builder_version=\u00bb4.27.0&#8243; _module_preset=\u00bbdefault\u00bb global_colors_info=\u00bb{}\u00bb][et_pb_blurb title=\u00bbPER\u00cdODO C\u00c1MBRICO\u00bb image=\u00bbhttps:\/\/clientes.munecarusa.com\/mp\/wp-content\/uploads\/2025\/01\/icono-0006633.png\u00bb alt=\u00bbPer\u00edodo C\u00e1mbrico\u00bb icon_placement=\u00bbleft\u00bb image_icon_width=\u00bb200%\u00bb content_max_width=\u00bb100%\u00bb _builder_version=\u00bb4.27.4&#8243; _module_preset=\u00bbdefault\u00bb header_level=\u00bbh3&#8243; header_font=\u00bb|700|||||||\u00bb header_text_color=\u00bb#000000&#8243; header_font_size=\u00bb28px\u00bb body_text_align=\u00bbjustify\u00bb body_text_color=\u00bb#444444&#8243; custom_margin=\u00bb||10px||false|false\u00bb header_font_size_tablet=\u00bb22px\u00bb header_font_size_phone=\u00bb15px\u00bb header_font_size_last_edited=\u00bbon|desktop\u00bb header_line_height_tablet=\u00bb\u00bb header_line_height_phone=\u00bb1.2em\u00bb header_line_height_last_edited=\u00bbon|phone\u00bb body_font_size_tablet=\u00bb16px\u00bb body_font_size_phone=\u00bb14px\u00bb body_font_size_last_edited=\u00bbon|phone\u00bb body_line_height_tablet=\u00bb1.7em\u00bb body_line_height_phone=\u00bb1.6em\u00bb body_line_height_last_edited=\u00bbon|phone\u00bb header_text_shadow_style=\u00bbpreset1&#8243; global_colors_info=\u00bb{}\u00bb]Un gran s\u00faper continente Gondwana, se localiza al sur del planeta con tres \u00fanicos continentes, Siberia, B\u00e1ltica y Laurentia, se desplazan hacia el norte. 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