{"id":656,"date":"2021-02-03T10:29:19","date_gmt":"2021-02-03T10:29:19","guid":{"rendered":"http:\/\/http:\/\/geomuseu.upc.edu\/\/?p=656"},"modified":"2021-07-15T08:48:37","modified_gmt":"2021-07-15T08:48:37","slug":"eocene-fossils-fossils-and-climate-change","status":"publish","type":"post","link":"https:\/\/geomuseu.upc.edu\/index.php\/en\/eocene-fossils-fossils-and-climate-change\/","title":{"rendered":"Eocene fossils: Fossils and climate change"},"content":{"rendered":"\n

 North sideboard (N): Current mangroves and fossil mangroves<\/strong><\/p>\n\n\n\n

\"\"<\/figure><\/div>\n\n\n\n

Comparison between biotic elements of current and fossil mangrove ecosystems. Arrangement composed of imported specimens of fauna and flora from the Indo-Pacific zone and fossils from the Eocene of Bages, extracted from the museum’s paleontological collection.<\/p>\n\n\n\n

South sideboard (S): Las Palmeras de Catalunya <\/strong>(photo 1)<\/em><\/p>\n\n\n\n

Compilation of citations from the fossil record of palm trees in Catalonia. Evidence of paleobiodiversity and the relationship of Paleobotany with mining areas and the exploitation of quarries in Catalonia.<\/p>\n\n\n\n

East sideboard (E): Las Palmeras and Climate Change<\/strong><\/p>\n\n\n\n

\"\"<\/figure><\/div>\n\n\n\n

Exhibition of the biogeographical changes carried out by palm tree communities, in the course of geological times and on a global scale. Explanatory panels showing evidence that palm trees are reliable indicators of climate change. Examples of comparative anatomy between fossil palm leaves and current palm leaves.<\/p>\n\n\n\n

West sideboard (W): Las Palmeras Nypa <\/strong>(photo 2)<\/em><\/p>\n\n\n\n

An exhibition of the abundant fossil record of this palm, also discovered in the eocenic lands of Central Catalonia. A comparison of current fructifications with the remains of fossil specimens from the Museum’s collections. Explanatory panels that show how a palm tree with the greatest worldwide geographic distribution in the Cenozoic era, is still confined to the mangroves of Southeast Asiana.<\/p>\n","protected":false},"excerpt":{"rendered":"

 North sideboard (N): Current mangroves and fossil mangroves Comparison between biotic elements of current and...<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[79],"tags":[],"class_list":["post-656","post","type-post","status-publish","format-standard","hentry","category-display-cases"],"_links":{"self":[{"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/posts\/656","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/comments?post=656"}],"version-history":[{"count":4,"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/posts\/656\/revisions"}],"predecessor-version":[{"id":1729,"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/posts\/656\/revisions\/1729"}],"wp:attachment":[{"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/media?parent=656"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/categories?post=656"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/geomuseu.upc.edu\/index.php\/wp-json\/wp\/v2\/tags?post=656"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}