{"id":640,"date":"2015-05-10T10:24:13","date_gmt":"2015-05-10T08:24:13","guid":{"rendered":"http:\/\/www.paleurafrica.be\/?page_id=640"},"modified":"2016-10-15T16:42:01","modified_gmt":"2016-10-15T14:42:01","slug":"labo-mrac","status":"publish","type":"page","link":"https:\/\/www.paleurafrica.be\/?page_id=640","title":{"rendered":"<span data-icon=\"\ue0a5\"><\/span> Labo RMCA"},"content":{"rendered":"<p><span style=\"color: #000000;\"><div class=\"su-column su-column-size-2-5\"><div class=\"su-column-inner su-u-clearfix su-u-trim\"><\/span><\/p>\n<h5 style=\"text-align: justify;\"><span style=\"color: #000000;\"><strong>Sedimentological analysis of fossil-bearing strata, and valorisation of historical collections at the Royal Museum for Central Africa<br \/>\n<\/strong><\/span><\/h5>\n<p style=\"text-align: justify;\"><span style=\"color: #000000;\">The sediments and fossils studied for the project belong to the Paleogene, a poorly-documented period in the geological history of Central Africa. At that time, the Congo Basin experienced a starvation period, with limited contemporaneous deposition both in the continental part of the basin and in the offshore sediment fan. The Landana section provides a 35m-thick sediment record of a Lower Paleocene to Neogene interval. The section is composed of Paleogene shallow-marine foraminiferal limestone (~25m thickness), followed by Neogene terrigenous clastics. The RMCA team focuses on the sedimentary analysis of the section, including recognition of sedimentation gaps, paleosurface levels and mineral diagenesis. With age information derived from new biostratigraphical data provided by other project partners, events recorded by the Landana section will provide valuable information on Congo Basin dynamics during the Cenozoic. As part of the project, the collection of fossil specimens from Landana and other localities in western Central Africa, housed at the RMCA since the beginning of the 20<sup>th<\/sup> century, is being inventoried and reorganized. This has increased the accessibility of the collection, allowing its valorisation through revision of several taxa by project partners.<\/span><\/p>\n<p>&nbsp;<\/p>\n<p><span style=\"color: #000000;\"><\/div><\/div><div class=\"su-column su-column-size-1-2\"><div class=\"su-column-inner su-u-clearfix su-u-trim\"><div id=\"su_slider_69f2c1340b6a8\" class=\"su-slider su-slider-pages-yes su-slider-responsive-yes\" style=\"width:100%\" data-autoplay=\"5000\" data-speed=\"600\" data-mousewheel=\"true\"><div class=\"su-slider-slides\"><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-01.jpg\"  target=\"_blank\" title=\"01 Working session at RMCA (Tervuren) around rock sample collections collected by E. Dartevelle; from left to right: Johan Yans (UNamur), Thierry De Putter &#038; Florias Mees (RMCA), Gregg Gunnell (Duke Univ.) and Louis Taverne (RBINS)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-01-800x600.jpg\" alt=\"01 Working session at RMCA (Tervuren) around rock sample collections collected by E. Dartevelle; from left to right: Johan Yans (UNamur), Thierry De Putter &#038; Florias Mees (RMCA), Gregg Gunnell (Duke Univ.) and Louis Taverne (RBINS)\" \/><span class=\"su-slider-slide-title\">01 Working session at RMCA (Tervuren) around rock sample collections collected by E. Dartevelle; from left to right: Johan Yans (UNamur), Thierry De Putter &#038; Florias Mees (RMCA), Gregg Gunnell (Duke Univ.) and Louis Taverne (RBINS)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-02.jpg\"  target=\"_blank\" title=\"02 Specimens of the Paleocene crocodilian Congosaurus from Landana (Bequaert field campain, RMCA collections)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-02-800x600.jpg\" alt=\"02 Specimens of the Paleocene crocodilian Congosaurus from Landana (Bequaert field campain, RMCA collections)\" \/><span class=\"su-slider-slide-title\">02 Specimens of the Paleocene crocodilian Congosaurus from Landana (Bequaert field campain, RMCA collections)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-03.jpg\"  target=\"_blank\" title=\"03 Specimens of the Paleocene crocodilian Congosaurus from Landana (Dartevelle field campain, RMCA collections)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-03-800x600.jpg\" alt=\"03 Specimens of the Paleocene crocodilian Congosaurus from Landana (Dartevelle field campain, RMCA collections)\" \/><span class=\"su-slider-slide-title\">03 Specimens of the Paleocene crocodilian Congosaurus from Landana (Dartevelle field campain, RMCA collections)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-04.jpg\"  target=\"_blank\" title=\"04 Rock samples from the Landana section allowing the reconstruction of the Paleogene series in this area of central Africa (RMCA collections)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-04-800x600.jpg\" alt=\"04 Rock samples from the Landana section allowing the reconstruction of the Paleogene series in this area of central Africa (RMCA collections)\" \/><span class=\"su-slider-slide-title\">04 Rock samples from the Landana section allowing the reconstruction of the Paleogene series in this area of central Africa (RMCA collections)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-05.jpg\"  target=\"_blank\" title=\"05 Conglomerate with siltite matrix including numerous coprolites and fossil remains (e.g. ray teeth, bottom of the picture); Landana section, layer 12 (RMCA collections)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-05-800x600.jpg\" alt=\"05 Conglomerate with siltite matrix including numerous coprolites and fossil remains (e.g. ray teeth, bottom of the picture); Landana section, layer 12 (RMCA collections)\" \/><span class=\"su-slider-slide-title\">05 Conglomerate with siltite matrix including numerous coprolites and fossil remains (e.g. ray teeth, bottom of the picture); Landana section, layer 12 (RMCA collections)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-06.jpg\"  target=\"_blank\" title=\"06 Nautilid Cimonia landanensis (paratype) collected by Didderich in Landana (RMCA collections)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-06-800x600.jpg\" alt=\"06 Nautilid Cimonia landanensis (paratype) collected by Didderich in Landana (RMCA collections)\" \/><span class=\"su-slider-slide-title\">06 Nautilid Cimonia landanensis (paratype) collected by Didderich in Landana (RMCA collections)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-07.jpg\"  target=\"_blank\" title=\"07 Phosphatized biogenic fragment (fish ?) in a thin recrystallized and dolomitised carbonated sediment (Landana section, layer 31)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-07-800x600.jpg\" alt=\"07 Phosphatized biogenic fragment (fish ?) in a thin recrystallized and dolomitised carbonated sediment (Landana section, layer 31)\" \/><span class=\"su-slider-slide-title\">07 Phosphatized biogenic fragment (fish ?) in a thin recrystallized and dolomitised carbonated sediment (Landana section, layer 31)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-08.jpg\"  target=\"_blank\" title=\"08 Carbonated sediment made by accumulation of foraminifera tests and a few other fossils (foraminifera packstone\/grainstone); typical facies of the lower part (Paleocene) of the Landana section (layer 8)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-08-800x600.jpg\" alt=\"08 Carbonated sediment made by accumulation of foraminifera tests and a few other fossils (foraminifera packstone\/grainstone); typical facies of the lower part (Paleocene) of the Landana section (layer 8)\" \/><span class=\"su-slider-slide-title\">08 Carbonated sediment made by accumulation of foraminifera tests and a few other fossils (foraminifera packstone\/grainstone); typical facies of the lower part (Paleocene) of the Landana section (layer 8)<\/span><\/a><\/div><div class=\"su-slider-slide\"><a href=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-09.jpg\"  target=\"_blank\" title=\"09 Sandstone with dolomitic cement, typical of the upper part (Neogene) of the Landana section (layer 35)\"><img src=\"https:\/\/www.paleurafrica.be\/wp-content\/uploads\/2015\/12\/MRAC-09-800x600.jpg\" alt=\"09 Sandstone with dolomitic cement, typical of the upper part (Neogene) of the Landana section (layer 35)\" \/><span class=\"su-slider-slide-title\">09 Sandstone with dolomitic cement, typical of the upper part (Neogene) of the Landana section (layer 35)<\/span><\/a><\/div><\/div><div class=\"su-slider-nav\"><div class=\"su-slider-direction\"><span class=\"su-slider-prev\"><\/span><span class=\"su-slider-next\"><\/span><\/div><div class=\"su-slider-pagination\"><\/div><\/div><\/div><\/div><\/div><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":603,"menu_order":0,"comment_status":"open","ping_status":"open","template":"page-templates\/contact.php","meta":[],"_links":{"self":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/pages\/640"}],"collection":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/types\/page"}],"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=640"}],"version-history":[{"count":21,"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/pages\/640\/revisions"}],"predecessor-version":[{"id":1296,"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/pages\/640\/revisions\/1296"}],"up":[{"embeddable":true,"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=\/wp\/v2\/pages\/603"}],"wp:attachment":[{"href":"https:\/\/www.paleurafrica.be\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=640"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}