{"id":5483,"date":"2022-02-02T12:58:53","date_gmt":"2022-02-02T11:58:53","guid":{"rendered":"https:\/\/lyon-geologie.univ-lyon1.fr\/?page_id=5483"},"modified":"2023-01-27T10:04:32","modified_gmt":"2023-01-27T09:04:32","slug":"m2_paleobio","status":"publish","type":"page","link":"https:\/\/lyongeologie.fr\/en\/m2-geosciences\/m2_paleobio\/","title":{"rendered":"M2 Pal\u00e9o-biog\u00e9ographie et Macro\u00e9cologie"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"5483\" class=\"elementor elementor-5483\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-3be7e560 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"3be7e560\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-d73f33e\" data-id=\"d73f33e\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-9f89f6a elementor-widget elementor-widget-text-editor\" data-id=\"9f89f6a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<h2><strong>Paleo-biogeography and Macroecology<br \/><\/strong><\/h2>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-de8a187 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"de8a187\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-33 elementor-top-column elementor-element elementor-element-2a140e0d\" data-id=\"2a140e0d\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-42087840 elementor-widget elementor-widget-text-editor\" data-id=\"42087840\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><em>3 Credits<\/em><\/p><p><em>Contact: <a href=\"mailto:bertrand.lefebvre@univ-lyon1.fr\">Bertrand LEFEBVRE<\/a><br \/><\/em><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-08aced3 elementor-widget elementor-widget-image\" data-id=\"08aced3\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"150\" height=\"150\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/Bertrand_Lefebvre.png\" class=\"attachment-large size-large wp-image-8871\" alt=\"\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-2030ad91 elementor-align-center elementor-widget elementor-widget-button\" data-id=\"2030ad91\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"button.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div class=\"elementor-button-wrapper\">\n\t\t\t\t\t<a class=\"elementor-button elementor-button-link elementor-size-sm\" href=\"https:\/\/lyon-geologie.univ-lyon1.fr\/en\/m2-geosciences\/#m2_opt\">\n\t\t\t\t\t\t<span class=\"elementor-button-content-wrapper\">\n\t\t\t\t\t\t\t\t\t<span class=\"elementor-button-text\">Back to the previous page<\/span>\n\t\t\t\t\t<\/span>\n\t\t\t\t\t<\/a>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-66 elementor-top-column elementor-element elementor-element-a034379\" data-id=\"a034379\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-2b2df09b elementor-widget elementor-widget-text-editor\" data-id=\"2b2df09b\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>For more than two centuries, the geography of the living world has been questioned: evolutionary history, geographical and climatic constraints and ecosystem functioning appear to be the main biotic and abiotic drivers of spatio-temporal variations in species distribution (biogeography) and, more broadly, of biodiversity (macroecology). In the fossil record as well as in present-day nature, numerous examples illustrate the modalities of action of these drivers as well as their consequences, outlining different universal 'rules' and patterns that this course proposes to explore (e.g., diversity gradients, eco-geographic 'laws', species-area relationships, insularity syndromes). Prior to the critical analysis of these 'rules' and patterns, particular attention will be paid to the methodologies underlying the development of chrono- and geo-referenced databases.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-732e1039 elementor-widget elementor-widget-image\" data-id=\"732e1039\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"768\" height=\"545\" src=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/M2_paleobio.png\" class=\"attachment-large size-large wp-image-5495\" alt=\"\" srcset=\"https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/M2_paleobio.png 768w, https:\/\/lyongeologie.fr\/wp-content\/uploads\/2022\/02\/M2_paleobio-300x213.png 300w\" sizes=\"(max-width: 768px) 100vw, 768px\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\"><i><small>A pteraspidomorph (Sacabambaspis) swims in the Ordovician Ocean under the anachronistic gaze of two Quaternary island species: the giant non-flying galliform from New Caledonia Sylviornis neocaledoniae (right) and the dwarf hominin from Flores Homo floresiensis (left, compared to its ancestor H. erectus). Species appearing, evolving, migrating and finally becoming extinct on a planet in permanent change, notably geographical and climatic: life is not, and has never been, a bed of roses!<\/small><\/i><\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-1b8bae03 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"1b8bae03\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-281b1215\" data-id=\"281b1215\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Pal\u00e9o-biog\u00e9ographie et Macro\u00e9cologie Cr\u00e9dits : 3 ECTS Responsable : Bertrand LEFEBVRE Retour \u00e0 la liste des UEs Depuis plus de deux si\u00e8cles, la g\u00e9ographie du monde vivant interroge : histoire \u00e9volutive, contraintes g\u00e9ographiques et climatiques et fonctionnement des \u00e9cosyst\u00e8mes apparaissent comme les principaux d\u00e9terminants biotiques et abiotiques des variations spatio-temporelles de la distribution des esp\u00e8ces [&hellip;]<\/p>\n","protected":false},"author":5,"featured_media":0,"parent":521,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"site-sidebar-layout":"no-sidebar","site-content-layout":"page-builder","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"disabled","ast-breadcrumbs-content":"","ast-featured-img":"disabled","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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