{"id":1142,"date":"2016-09-21T10:40:49","date_gmt":"2016-09-21T08:40:49","guid":{"rendered":"http:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5.jpg"},"modified":"2016-09-21T11:23:01","modified_gmt":"2016-09-21T09:23:01","slug":"new-bio-chemostratigraphic-dating-of-a-unique-early-eocene-seque","status":"inherit","type":"attachment","link":"https:\/\/www.paleurafrica.be\/?attachment_id=1142","title":{"rendered":"Correlation of the organic carbon (\u03b413Corg) isotope curve of the Minervois  with the standard marine composite bulk carbonate (\u03b413Ccarb) isotope curve of the Ypresian and with the calcareous nannofossil and larger benthic foraminiferal zones. Black bone indicates mammalian localities; Nannofossils: biostratigraphic control (calcareous nannofossil dating); Pal. = Paleocene; p. = pars."},"author":1,"comment_status":"open","ping_status":"open","template":"","meta":[],"description":{"rendered":"<p class=\"attachment\"><a href='https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5.jpg'><img width=\"300\" height=\"152\" src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-300x152.jpg\" class=\"attachment-medium size-medium\" alt=\"\" loading=\"lazy\" srcset=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-300x152.jpg 300w, https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-1024x521.jpg 1024w, https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5.jpg 1181w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n"},"caption":{"rendered":""},"alt_text":"","media_type":"image","mime_type":"image\/jpeg","media_details":{"width":1181,"height":601,"file":"2016\/09\/Figure-5.jpg","sizes":{"thumbnail":{"file":"Figure-5-150x150.jpg","width":150,"height":150,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-150x150.jpg"},"medium":{"file":"Figure-5-300x152.jpg","width":300,"height":152,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-300x152.jpg"},"large":{"file":"Figure-5-1024x521.jpg","width":1024,"height":521,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-1024x521.jpg"},"widget-thumb":{"file":"Figure-5-80x50.jpg","width":80,"height":50,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5-80x50.jpg"},"full":{"file":"Figure-5.jpg","width":1181,"height":601,"mime_type":"image\/jpeg","source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5.jpg"}},"image_meta":{"aperture":0,"credit":"Corentin Noiret ; Etienne Steurb","camera":"","caption":"","created_timestamp":0,"copyright":"","focal_length":0,"iso":0,"shutter_speed":0,"title":"New bio-chemostratigraphic dating of a unique early Eocene seque","orientation":1,"resized_images":["656x334"]}},"post":null,"source_url":"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2016\/09\/Figure-5.jpg","_links":{"self":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/media\/1142"}],"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=1142"}]}}