{"id":{"repo_id":"milano","oai_identifier":"oai:air.unimi.it:2434/231576"},"canonical_url":"https://search.dev.ndltd.org/etd/milano/oai:air.unimi.it:2434/231576","repository":{"repo_id":"milano","name":"Università degli Studi di Milano","base_url":"https://air.unimi.it/oai/request"},"display":{"title":"NETWORK THEORY IN ICHNOLOGY: FROM BEHAVIOURAL TOPOLOGY TO THE DEPOSITIONAL ENVIRONMENT","abstract":"This study aims to (1) develop quantitative approaches for the study of ichnological systems; (2) model, for the first time, ichnosites as networks; (3) analyze the response of ichnological systems to global dynamics, with particular regard to Late Paleozoic fluvial-influenced settings. In this regard, the modern peritidal environments of the Grado lagoon (Italy, Adriatic Sea), the Nurra ichnosite (Permian-Triassic; Italy) and the Pramollo ichnolagerstätte (Carboniferous-Permian; Italy) have been selected for developing, applying and testing network analysis for the study of ichnological systems. Results show that network theory is able to depict the traces-environment relationships both for modern and fossil ichnological systems. It is therefore suggested that network theory may have great potential for understanding Phanerozoic bioturbation patterns.","abstract_html":"This study aims to (1) develop quantitative approaches for the study of ichnological systems; (2) model, for the first time, ichnosites as networks; (3) analyze the response of ichnological systems to global dynamics, with particular regard to Late Paleozoic fluvial-influenced settings. In this regard, the modern peritidal environments of the Grado lagoon (Italy, Adriatic Sea), the Nurra ichnosite (Permian-Triassic; Italy) and the Pramollo ichnolagerstätte (Carboniferous-Permian; Italy) have been selected for developing, applying and testing network analysis for the study of ichnological systems. Results show that network theory is able to depict the traces-environment relationships both for modern and fossil ichnological systems. It is therefore suggested that network theory may have great potential for understanding Phanerozoic bioturbation patterns.","abstract_has_math":false,"creators":["BAUCON, ANDREA"],"institution":"Università degli Studi di Milano","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":["tutor: F. Felletti ; co-tutor: G. Muttoni ; coordinatore: E. Erba","A. Baucon","FELLETTI, FABRIZIO","ERBA, ELISABETTA"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2014,"date_issued":"2014-02-12","date_published":"2014-02-12","updated_at":"2026-07-27T20:19:15Z","subjects":["Settore GEO/02 - Geologia Stratigrafica e Sedimentologica","Settore GEO/01 - Paleontologia e Paleoecologia"],"languages":["eng"],"rights":["info:eu-repo/semantics/openAccess"],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.13130/baucon-andrea_phd2014-02-12"],"render_values":[{"text":"10.13130/baucon-andrea_phd2014-02-12","href":"https://doi.org/10.13130/baucon-andrea_phd2014-02-12","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/2434/231576","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["tutor: F. Felletti ; co-tutor: G. Muttoni ; coordinatore: E. Erba","A. Baucon","FELLETTI, FABRIZIO","ERBA, ELISABETTA"]},{"key":"dc:creator","label":"Author","values":["BAUCON, ANDREA"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["2014-02-12"]},{"key":"dc:publisher","label":"Institution","values":["Università degli Studi di Milano"]},{"key":"dc:type","label":"Dc Type","values":["info:eu-repo/semantics/doctoralThesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Settore GEO/02 - Geologia Stratigrafica e Sedimentologica","Settore GEO/01 - Paleontologia e Paleoecologia"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["eng"]},{"key":"dc:rights","label":"Dc Rights","values":["info:eu-repo/semantics/openAccess"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["http://hdl.handle.net/2434/231576","10.13130/baucon-andrea_phd2014-02-12"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["This study aims to (1) develop quantitative approaches for the study of ichnological systems; (2) model, for the first time, ichnosites as networks; (3) analyze the response of ichnological systems to global dynamics, with particular regard to Late Paleozoic fluvial-influenced settings. In this regard, the modern peritidal environments of the Grado lagoon (Italy, Adriatic Sea), the Nurra ichnosite (Permian-Triassic; Italy) and the Pramollo ichnolagerstätte (Carboniferous-Permian; Italy) have been selected for developing, applying and testing network analysis for the study of ichnological systems. Results show that network theory is able to depict the traces-environment relationships both for modern and fossil ichnological systems. It is therefore suggested that network theory may have great potential for understanding Phanerozoic bioturbation patterns."]},{"key":"dc:title","label":"Title","values":["NETWORK THEORY IN ICHNOLOGY: FROM BEHAVIOURAL TOPOLOGY TO THE DEPOSITIONAL ENVIRONMENT"]}]}],"canonical_facts":{"dc:contributor":["tutor: F. Felletti ; co-tutor: G. Muttoni ; coordinatore: E. Erba","A. Baucon","FELLETTI, FABRIZIO","ERBA, ELISABETTA"],"dc:creator":["BAUCON, ANDREA"],"dc:date":["2014-02-12"],"dc:description":["This study aims to (1) develop quantitative approaches for the study of ichnological systems; (2) model, for the first time, ichnosites as networks; (3) analyze the response of ichnological systems to global dynamics, with particular regard to Late Paleozoic fluvial-influenced settings. In this regard, the modern peritidal environments of the Grado lagoon (Italy, Adriatic Sea), the Nurra ichnosite (Permian-Triassic; Italy) and the Pramollo ichnolagerstätte (Carboniferous-Permian; Italy) have been selected for developing, applying and testing network analysis for the study of ichnological systems. Results show that network theory is able to depict the traces-environment relationships both for modern and fossil ichnological systems. It is therefore suggested that network theory may have great potential for understanding Phanerozoic bioturbation patterns."],"dc:identifier":["http://hdl.handle.net/2434/231576","10.13130/baucon-andrea_phd2014-02-12"],"dc:language":["eng"],"dc:publisher":["Università degli Studi di Milano"],"dc:rights":["info:eu-repo/semantics/openAccess"],"dc:subject":["Settore GEO/02 - Geologia Stratigrafica e Sedimentologica","Settore GEO/01 - Paleontologia e Paleoecologia"],"dc:title":["NETWORK THEORY IN ICHNOLOGY: FROM BEHAVIOURAL TOPOLOGY TO THE DEPOSITIONAL ENVIRONMENT"],"dc:type":["info:eu-repo/semantics/doctoralThesis"]},"updated_at":"2026-07-27T20:19:15Z"}