{"id":2150,"date":"2025-01-16T22:28:36","date_gmt":"2025-01-16T22:28:36","guid":{"rendered":"https:\/\/confer.co.nz\/isc2026\/?page_id=2150"},"modified":"2025-05-12T00:45:27","modified_gmt":"2025-05-12T00:45:27","slug":"sediments-plants-and-animals-fossils-trace-fossils-paleoecology-and-evolution","status":"publish","type":"page","link":"https:\/\/confer.co.nz\/isc2026\/sediments-plants-and-animals-fossils-trace-fossils-paleoecology-and-evolution\/","title":{"rendered":"Sediments, plants, and animals: fossils, trace fossils, paleoecology, and evolution"},"content":{"rendered":"\n\n\t<h1>Sediments, plants, and animals: fossils, trace fossils, paleoecology, and evolution<\/h1>\n<h2>\n\t\tDeep time biogeomorphology: life-sediment interactions in ancient clastic settings\n\t<\/h2>\n\t<p><strong>Professor Neil Davies<sup>1<\/sup>, Dr William McMahon<sup>1<\/sup>, Dr Anthony Shillito<sup>2<\/sup><\/strong><\/p>\n<p><em><sup>1<\/sup>University of Cambridge, Cambridge, United Kingdom, <sup>2<\/sup>University of Saskatchewan, Saskatoon, Canada<\/em><\/p>\n<p>In modern environments, biogeomorphology describes the two-way interaction between biotic and dynamic abiotic landscape elements and has risen to prominence in recent decades by recognizing the contribution of living organisms to landscape stability, dynamics and roughness.\u00a0 While there has been a lag in applying this knowledge to the ancient record, it is increasingly apparent that the frontier between palaeontology and sedimentary geology can be a blurred and complicated boundary. Ancient animals and plants were not always mere fossils in museum drawers, and sedimentary facies were not purely physical phenomena that provided a passive back-drop in the theatre of evolution. Elucidating the interactions between ancient life and environments can involve a variety of disciplines, ranging from ichnology, sedimentary architectural and facies analysis, modelling, and petrography. New insights from these fields are demonstrating that clastic strata &#8211; often seen as the &#8216;abiotic&#8217; sister to biogenic carbonates &#8211; can be rich records of biogeomorphology and geo-evolutionary feedback on scales from individual organisms and bedforms to the evolutionary history of entire groups of organisms and global stratigraphic facies shifts.<\/p>\n<p>This session aims to bring together novel research from several subdisciplines of sedimentology to ascertain the ancient record of life-sediment interactions on the full variety of spatio-temporal scales. It will, through the presentation of case studies within this theme, unravel the deep time landscape memory of evolution that underlies many sedimentary and geomorphic phenomena in modern siliciclastic sedimentary environments.<\/p>\n\t<h3>Ichnology and sedimentary basin research: assessing environmental conditions<\/h3>\n\t<p><strong>Dr Javier Dorador<sup>1<\/sup>, Dr Olmo Miguez-Salas<sup>2<\/sup>, Professor Francisco J. Rodr\u00edguez-Tovar<sup>1<\/sup><\/strong><\/p>\n<p><em><sup>1<\/sup>Universidad de Granada, Granada, Spain, <sup>2<\/sup>Universidad de Barcelona, Barcelona, Spain<\/em><\/p>\n<p>Trace makers community is highly sensitive to depositional and ecological parameters such as hydrodynamic energy, sedimentation rate, oxygenation, salinity or nutrients availability among others. Consequently, the ichnological record has been proved as a key tool for interpreting environmental conditions revealing important information on depositional environments, processes and final products. In recent years, numerous case studies from both marine and continental settings have been published. Of special interest is the integration of ichnology into multidisciplinary studies involving sedimentologists, oceanographers, climatologists or geochemists through the application of novel techniques and methodologies. This session aims to bring together a wide range of ichnological studies focused on sedimentary basin research, including outcrops and cores analysis, modern and ancient record, digital modelling and experimental approaches, from marine and continental environments.<\/p>\n\n","protected":false},"excerpt":{"rendered":"<p>Sediments, plants, and animals: fossils, trace fossils, paleoecology, and evolution Deep time biogeomorphology: life-sediment interactions in ancient clastic settings Professor Neil Davies1, Dr William McMahon1, Dr Anthony Shillito2 1University of Cambridge, Cambridge, United Kingdom, 2University of Saskatchewan, Saskatoon, Canada In modern environments, biogeomorphology describes the two-way interaction between biotic and dynamic abiotic landscape elements and&hellip;<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-2150","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.0 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Sediments, plants, and animals: fossils, trace fossils, paleoecology, and evolution - ISC2026<\/title>\n<meta name=\"description\" content=\"The ISC2026 conference theme is &#039;Sedimentation on active plate margins through time and space&#039;. Zealandia is a 4.9 Mkm2 region of continental crust in the South Pacific that was once part of Gondwana. Learn more.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/confer.co.nz\/isc2026\/sediments-plants-and-animals-fossils-trace-fossils-paleoecology-and-evolution\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Sediments, plants, and animals: fossils, trace fossils, paleoecology, and evolution - ISC2026\" \/>\n<meta property=\"og:description\" content=\"The ISC2026 conference theme is &#039;Sedimentation on active plate margins through time and space&#039;. Zealandia is a 4.9 Mkm2 region of continental crust in the South Pacific that was once part of Gondwana. 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