{"id":4036,"date":"2026-07-30T22:12:00","date_gmt":"2026-07-30T20:12:00","guid":{"rendered":"https:\/\/www.palaeonavix.org\/portfolio\/carboniferous-driftwood-shark\/"},"modified":"2026-08-01T00:54:13","modified_gmt":"2026-07-31T22:54:13","slug":"carboniferous-driftwood-shark","status":"publish","type":"avada_portfolio","link":"https:\/\/www.palaeonavix.org\/en\/portfolio\/carboniferous-driftwood-shark\/","title":{"rendered":"Carboniferous driftwood"},"content":{"rendered":"<p>In this case, the xenacanthid shark is not much more but a time marker, indicating a late Palaeozoic age of the scene, if you are familiar for ancient fishes and faunas. A characteristic double-tipped tooth was indeed found in the redbeds of the Kyffh\u00e4user mountains in Germany. But the story is about latest Carboniferous wood and its mineralisation. Not only are petrified trunks a great archive for environments, as well as their taphonomy preserves the sedimentary bedding conditions around. The very minerals that copied the original plant in sub-cell details helped scientists to reconstruct tectonic events throughout their silent history as a fossil \u2013 which is more than 300 million years!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Digital painting of a Late Palaeozoic river landscape \u2014 petrified wood as an archive of tectonic history.<\/p>\n","protected":false},"author":1,"featured_media":4034,"menu_order":0,"comment_status":"open","ping_status":"closed","template":"","format":"standard","meta":{"_acf_changed":false,"pn_jahr":"2020","pn_taxon":"Xenacanthiformes","pn_auftraggeber":"","pn_ausstellung":"","pn_masse":"","pn_quelle_url":"https:\/\/doi.org\/10.1038\/s41598-026-60054-3; https:\/\/doi.org\/10.1111\/sed.12692","pn_lizenz":"\u00a9 Palaeonavix","pn_alt_url":"https:\/\/www.palaeonavix.org\/index.php\/palaeo-illustration\/carboniferous-driftwood-shark","pn_mitwirkende":"","footnotes":""},"portfolio_category":[158],"portfolio_skills":[],"portfolio_tags":[],"class_list":["post-4036","avada_portfolio","type-avada_portfolio","status-publish","format-standard","has-post-thumbnail","hentry","portfolio_category-palaeo-illustration"],"acf":{"pn_jahr":"2020","pn_taxon":"Xenacanthiformes","pn_auftraggeber":"","pn_ausstellung":"","pn_masse":"","pn_quelle_url":"https:\/\/doi.org\/10.1038\/s41598-026-60054-3; https:\/\/doi.org\/10.1111\/sed.12692","pn_lizenz":"\u00a9 Palaeonavix","pn_mitwirkende":"","pn_verwandte":[3777],"pn_links":null,"pn_publikationen":[{"zitat":"Tr\u00fcmper, S., Franz, M., Sosa, G., van den Kerkhof, A., Zeh, A., Tatzel, M., Kronz, A., Techmer, K., Di Rocco, T., Pack, A., & R\u00f6\u00dfler, R. (2016): Fossil wood cells recorded 300 million years of Europe\u2019s tectonic history. Nature Scientific Reports, 16: 22068.","url":"https:\/\/doi.org\/10.1038\/s41598-026-60054-3"},{"zitat":"Tr\u00fcmper, S., Gaitzsch, B., Schneider, J.W., Ehling, B.C., Kleeberg, R., & R\u00f6\u00dfler, R. (2020): Late Palaeozoic red beds elucidate fluvial architectures preserving large woody debris in the seasonal tropics of central Pangaea. Sedimentology, 67(4): 1973-2012.","url":"https:\/\/doi.org\/10.1111\/sed.12692"}],"pn_alt_url":"https:\/\/www.palaeonavix.org\/index.php\/palaeo-illustration\/carboniferous-driftwood-shark"},"_links":{"self":[{"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/avada_portfolio\/4036","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/avada_portfolio"}],"about":[{"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/types\/avada_portfolio"}],"author":[{"embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/comments?post=4036"}],"version-history":[{"count":1,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/avada_portfolio\/4036\/revisions"}],"predecessor-version":[{"id":4055,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/avada_portfolio\/4036\/revisions\/4055"}],"acf:post":[{"embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/avada_portfolio\/3777"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/media\/4034"}],"wp:attachment":[{"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/media?parent=4036"}],"wp:term":[{"taxonomy":"portfolio_category","embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/portfolio_category?post=4036"},{"taxonomy":"portfolio_skills","embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/portfolio_skills?post=4036"},{"taxonomy":"portfolio_tags","embeddable":true,"href":"https:\/\/www.palaeonavix.org\/en\/wp-json\/wp\/v2\/portfolio_tags?post=4036"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}