{"id":6439,"date":"2024-01-31T11:27:06","date_gmt":"2024-01-31T10:27:06","guid":{"rendered":"https:\/\/muzeumewolucji.pl\/?p=6439"},"modified":"2024-01-31T11:28:06","modified_gmt":"2024-01-31T10:28:06","slug":"bioerosion-traces-in-pliocene-solitary-corals","status":"publish","type":"post","link":"https:\/\/muzeumewolucji.pl\/?p=6439&lang=en","title":{"rendered":"Bioerosion traces in Pliocene solitary corals"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-post\" data-elementor-id=\"6439\" class=\"elementor elementor-6439\">\n\t\t\t\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-6d615e15 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"6d615e15\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-11e6e7a\" data-id=\"11e6e7a\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t\t<div class=\"elementor-element elementor-element-6f9c1462 elementor-widget elementor-widget-heading\" data-id=\"6f9c1462\" data-element_type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">Bioerosion traces in Pliocene solitary corals<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-a7f5452 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"a7f5452\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4e1eb91\" data-id=\"4e1eb91\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t\t<div class=\"elementor-element elementor-element-4e5ddb7 elementor-widget elementor-widget-text-editor\" data-id=\"4e5ddb7\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p><img fetchpriority=\"high\" decoding=\"async\" data-recalc-dims=\"1\" class=\" wp-image-6433 alignright\" src=\"https:\/\/i0.wp.com\/muzeumewolucji.pl\/wp-content\/uploads\/2024\/01\/Ceratotrochus-POP_JS.jpg?resize=567%2C293&#038;ssl=1\" alt=\"\" width=\"567\" height=\"293\" \/>One of the basic <a href=\"https:\/\/en.wikipedia.org\/wiki\/Taphonomy\" target=\"_blank\" rel=\"noopener\">taphonomic<\/a> questions is whether the borings in skeletal structures were produced <i>in vivo<\/i> or <i>post mortem<\/i>. Borings influencing the growth of the skeleton were produced during the life of the animal; the same for borings that are distributed very close to the surface of the skeletal structure and are elsewhere known from deep penetration into the substrate. Conversely, borings that penetrate deeply into the skeletal structure and those that are always close to the surface, irrespective of the substrate, can be regarded as produced <i>post mortem<\/i>. These criteria are used to distinguish the two categories of <a href=\"https:\/\/en.wikipedia.org\/wiki\/Polychaete\" target=\"_blank\" rel=\"noopener\">polychaete<\/a>, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Bryozoa\" target=\"_blank\" rel=\"noopener\">bryozoan<\/a>, and <a href=\"https:\/\/en.wikipedia.org\/wiki\/Phoronid\" target=\"_blank\" rel=\"noopener\">phoronid<\/a> borings made in coralla of fossil (<a href=\"https:\/\/en.wikipedia.org\/wiki\/Pliocene\" target=\"_blank\" rel=\"noopener\">Pliocene<\/a> of Tunisia) solitary <a href=\"https:\/\/en.wikipedia.org\/wiki\/Scleractinia\" target=\"_blank\" rel=\"noopener\">scleractinian<\/a> coral <i>Ceratotrochus<\/i>.<\/p><p>Figure: Corallum of solitary <i>Ceratotrochus (Edwardsotrochus) duodecimcostatus<\/i> from the upper Pliocene of Tunisia (distal and lateral views); longitudinal thin-section and virtual (mCT) longitudinal section of the coral skeleton with probably in-vivo polycha ete borings (ichnogenus <i>Maeandropolydora<\/i>).<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-010c73a elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"010c73a\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-aa4400e\" data-id=\"aa4400e\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t\t\t<div class=\"elementor-element elementor-element-6259b6f elementor-widget elementor-widget-text-editor\" data-id=\"6259b6f\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<p><b>PUBLICATION:<\/b> Gaaloul, N., Uchman, A., Riahi, S., <a href=\"http:\/\/biominerals.paleo.pan.pl\/pl\/pracownicy\/janiszewska\/katarzyna_janiszewska.html\" target=\"_blank\" rel=\"noopener\">Janiszewska, K.<\/a>, <a href=\"http:\/\/biominerals.paleo.pan.pl\/pl\/pracownicy\/stolarski\/jaroslaw_stolarski.html\" target=\"_blank\" rel=\"noopener\">Stolarski, J.<\/a>, Ko\u0142odziej, B., Ben Ali, S. 2023. In vivo and post-mortem bioerosion traces in solitary corals from the Pliocene of Tunisia. <a href=\"https:\/\/www.app.pan.pl\/archive\/published\/app68\/app010952023.pdf\" target=\"_blank\" rel=\"noopener\"><i>Acta Palaeontologica Polonica<\/i> 68:659-681<\/a>, doi: 10.4202\/app.01095.2023.<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>One of the basic taphonomic questions is whether the borings in skeletal structures were produced in vivo or post mortem.<\/p>\n","protected":false},"author":3,"featured_media":6433,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[93],"tags":[],"class_list":["post-6439","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sc_news"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v26.8 - 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