{"id":918,"date":"2015-12-18T09:27:14","date_gmt":"2015-12-18T08:27:14","guid":{"rendered":"http:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15.jpg"},"modified":"2015-12-18T09:27:26","modified_gmt":"2015-12-18T08:27:26","slug":"integrated-bio-chemostratigraphical-correlations-and-climatic-ev","status":"inherit","type":"attachment","link":"https:\/\/www.paleurafrica.be\/?attachment_id=918","title":{"rendered":"High-resolution geochemistry, carbon isotope, oxygen isotope, \u039413C and biostratigraphy across the Danian\u2013Selandian boundary in the Loubieng section"},"author":1,"comment_status":"open","ping_status":"open","template":"","meta":[],"description":{"rendered":"<p class=\"attachment\"><a href='https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15.jpg'><img width=\"300\" height=\"191\" src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15-300x191.jpg\" class=\"attachment-medium size-medium\" alt=\"\" loading=\"lazy\" srcset=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15-300x191.jpg 300w, https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15-80x50.jpg 80w, https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15.jpg 1000w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n<p>Palaeogeography, Palaeoclimatology, Palaeoecology, Corrected proof. doi:10.1016\/j.palaeo.2014.09.002<\/p>\n"},"caption":{"rendered":"<p>Palaeogeography, Palaeoclimatology, Palaeoecology, Corrected proof. doi:10.1016\/j.palaeo.2014.09.002<\/p>\n"},"alt_text":"","media_type":"image","mime_type":"image\/jpeg","media_details":{"width":1000,"height":637,"file":"2015\/12\/Figure-15.jpg","sizes":{"thumbnail":{"file":"Figure-15-150x150.jpg","width":150,"height":150,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15-150x150.jpg"},"medium":{"file":"Figure-15-300x191.jpg","width":300,"height":191,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15-300x191.jpg"},"widget-thumb":{"file":"Figure-15-80x50.jpg","width":80,"height":50,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15-80x50.jpg"},"full":{"file":"Figure-15.jpg","width":1000,"height":637,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15.jpg"}},"image_meta":{"aperture":0,"credit":"Jean-Yves Storme","camera":"","caption":"Palaeogeography, Palaeoclimatology, Palaeoecology, Corrected proof. doi:10.1016\/j.palaeo.2014.09.002","created_timestamp":0,"copyright":"","focal_length":0,"iso":0,"shutter_speed":0,"title":"Integrated bio-chemostratigraphical correlations and climatic ev","orientation":1,"resized_images":["1000x637","700x446","656x418"]}},"post":null,"source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/Figure-15.jpg","_links":{"self":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/media\/918"}],"collection":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/media"}],"about":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/types\/attachment"}],"author":[{"embeddable":true,"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=918"}]}}