{"id":293,"date":"2010-06-28T10:48:09","date_gmt":"2010-06-28T08:48:09","guid":{"rendered":"http:\/\/wp.unil.ch\/sciencesaucarre\/?p=293"},"modified":"2010-11-16T14:21:51","modified_gmt":"2010-11-16T13:21:51","slug":"follmi-karl","status":"publish","type":"post","link":"https:\/\/wp.unil.ch\/sciencesaucarre\/follmi-karl\/","title":{"rendered":"F\u00f6llmi Karl"},"content":{"rendered":"

Professeur<\/strong><\/p>\n

Facult\u00e9 des g\u00e9osciences et de l’environnement – UNIL<\/em><\/p>\n

Institut de g\u00e9ologie et pal\u00e9ontologie [site web<\/a>]\n karl.foellmi@unil.ch<\/a>
\nT\u00e9l. +41 21 692 43 63
\n<\/em><\/p>\n

Langues d’enseignement<\/h4>\n

Fran\u00e7ais, anglais<\/p>\n

Th\u00e8mes de pr\u00e9dilection<\/h4>\n

Earth history
\nPaleoenvironmental change
\nClimate change during Earth history
\nCarbon and Phosphorus cycles during the past<\/p>\n

Comp\u00e9tences \u00e9largies<\/h4>\n

The interests of our research group are centered on large-scale processes during Earth’s history, which have relevance to present-day environmental change. They include research on paleo-environmental change in carbonate platforms (present-day analogue: coral reefs), phosphorite deposits (carrying the essential nutrient phosphate), organic-carbon-rich deposits (sinks for atmospheric CO2), weathering processes on the continent (as a source for essential biophile elements), major extinction events, trace-metal contaminations, and paleoclimatic reconstructions.<\/p>\n

Th\u00e8mes de recherche sp\u00e9cifique<\/h4>\n

Major extinction events during the Late Devonian, at the Cretaceous-Tertiary boundary and at the Paleocene-Eocene boundary
\nDiagenesis of complex multiphase drowning surfaces preserved in sediments of the Lower Cretaceous carbonate platform in the northern Tethyan realm
\nGenesis of the Rhaetian phosphatic bonebed in central and northwestern Europe
\nAnomalous cadmium enrichments in Jurassic carbonates
\nThe early Valanginian and the Barremian-Aptian boundary time intervals: Episodes of important change in the evolution of the early Cretaceous northern Tethyan carbonate platform
\nGenesis of the Rhaetian phosphatic bonebed in central and northwestern Europe
\nPhosphorus and carbon burial during Late Cretaceous oceanic anoxic events, links with climate changes
\nSedimentology and geochemistry of the Early Aptian Gr\u00fcnten Member (Helvetic Nappes, northern Tethyan Margin)
\nSedimentology, geochemistry and mineralogy of the Paleogene sediments from Egypt<\/p>\n","protected":false},"excerpt":{"rendered":"

Professeur Facult\u00e9 des g\u00e9osciences et de l’environnement – UNIL<\/p>\n","protected":false},"author":236,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_seopress_titles_title":"","_seopress_titles_desc":"","_seopress_robots_index":"","_seopress_robots_follow":"","_seopress_robots_imageindex":"","_seopress_robots_snippet":"","_seopress_robots_primary_cat":"","_seopress_robots_breadcrumbs":"","_seopress_robots_freeze_modified_date":"","_seopress_robots_custom_modified_date":"","_seopress_robots_canonical":"","_seopress_social_fb_title":"","_seopress_social_fb_desc":"","_seopress_social_fb_img":"","_seopress_social_fb_img_attachment_id":0,"_seopress_social_fb_img_width":0,"_seopress_social_fb_img_height":0,"_seopress_social_twitter_title":"","_seopress_social_twitter_desc":"","_seopress_social_twitter_img":"","_seopress_social_twitter_img_attachment_id":0,"_seopress_social_twitter_img_width":0,"_seopress_social_twitter_img_height":0,"_seopress_redirections_value":"","_seopress_redirections_enabled":"","_seopress_redirections_enabled_regex":"","_seopress_redirections_logged_status":"","_seopress_redirections_param":"","_seopress_redirections_type":0,"_seopress_analysis_target_kw":"","_seopress_news_disabled":"","_seopress_video_disabled":"","_seopress_video":[],"_seopress_pro_schemas_manual":[],"_seopress_pro_rich_snippets_disable_all":"","_seopress_pro_rich_snippets_disable":[],"_seopress_pro_schemas":[],"footnotes":""},"categories":[39],"tags":[640,638,639,641],"class_list":["post-293","post","type-post","status-publish","format-standard","category-geosciences","tag-carbon-cycle","tag-earth-history","tag-paleoenvironmental-change","tag-phosphorus-cycle"],"_links":{"self":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/posts\/293","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/users\/236"}],"replies":[{"embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/comments?post=293"}],"version-history":[{"count":0,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/posts\/293\/revisions"}],"wp:attachment":[{"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/media?parent=293"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/categories?post=293"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/wp.unil.ch\/sciencesaucarre\/wp-json\/wp\/v2\/tags?post=293"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}