Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain
The Late Permian (Wuchiapingian) Alcotas Formation in the SE Iberian Ranges consists of one red alluvial succession where abundant soil profiles developed. Detailed petrographical and sedimentological studies in seven sections of the Alcotas Formation allow six different types of palaeosols, with di...
| Autores: | ; ; ; ; ; |
|---|---|
| Tipo de documento: | Artículo |
| Fecha de publicación: | 2008 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Lenguaje: | Inglés |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/50321 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/50321 |
| Nivel de acceso: | Acceso abierto |
| Palabra clave: | 551.736(234.1) Biotic crisis Iberian Ranges Late Permian Palaeosols Permian- Triassic boundary Geología estratigráfica 2506.19 Estratigrafía |
| _version_ | 1878737128425259008 |
|---|---|
| author | Horra Del Barco, Raúl De La |
| author2 | Benito Moreno, María Isabel López Gómez, José Arche, Alfredo Fernández Barrenechea, José María Luque Del Villar, Francisco Javier |
| author2_role | author author author author author |
| author_browse | Arche, Alfredo Benito Moreno, María Isabel Fernández Barrenechea, José María Horra Del Barco, Raúl De La Luque Del Villar, Francisco Javier López Gómez, José |
| author_facet | Horra Del Barco, Raúl De La Benito Moreno, María Isabel López Gómez, José Arche, Alfredo Fernández Barrenechea, José María Luque Del Villar, Francisco Javier |
| author_role | author |
| collection | Docta Complutense |
| description | The Late Permian (Wuchiapingian) Alcotas Formation in the SE Iberian Ranges consists of one red alluvial succession where abundant soil profiles developed. Detailed petrographical and sedimentological studies in seven sections of the Alcotas Formation allow six different types of palaeosols, with distinctive characteristics and different palaeogeographical distribution, to be distinguished throughout the South-eastern Iberian Basin. These characteristics are, in turn, related to topographic, climatic and tectonic controls. The vertical distribution of the palaeosols is used to differentiate the formation in three parts from bottom to top showing both drastic and gradual vertical upwards palaeoenvironmental changes in the sections. Reconstruction of palaeoenvironmental conditions based on palaeosols provides evidence for understanding the events that occurred during the Late Permian, some few millions of years before the well-known Permian-Triassic global crisis. |
| eu_rights_str_mv | openAccess |
| format | article |
| id | ES_9b1ac46d09cd0d8adb81508f2ed547f6 |
| institution | Universidad Complutense de Madrid (UCM) |
| instname_str | Universidad Complutense de Madrid (UCM) |
| language | eng |
| network_acronym_str | ES |
| network_name_str | España |
| oai_identifier_str | oai:docta.ucm.es:20.500.14352/50321 |
| publishDate | 2008 |
| publishDateSort | 2008 |
| publisher | Blackwell Publishing Ltd |
| publisherStr | Blackwell Publishing Ltd |
| reponame_str | Docta Complutense |
| spelling | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain Horra Del Barco, Raúl De La Benito Moreno, María Isabel López Gómez, José Arche, Alfredo Fernández Barrenechea, José María Luque Del Villar, Francisco Javier 551.736(234.1) Biotic crisis Iberian Ranges Late Permian Palaeosols Permian- Triassic boundary Geología estratigráfica 2506.19 Estratigrafía The Late Permian (Wuchiapingian) Alcotas Formation in the SE Iberian Ranges consists of one red alluvial succession where abundant soil profiles developed. Detailed petrographical and sedimentological studies in seven sections of the Alcotas Formation allow six different types of palaeosols, with distinctive characteristics and different palaeogeographical distribution, to be distinguished throughout the South-eastern Iberian Basin. These characteristics are, in turn, related to topographic, climatic and tectonic controls. The vertical distribution of the palaeosols is used to differentiate the formation in three parts from bottom to top showing both drastic and gradual vertical upwards palaeoenvironmental changes in the sections. Reconstruction of palaeoenvironmental conditions based on palaeosols provides evidence for understanding the events that occurred during the Late Permian, some few millions of years before the well-known Permian-Triassic global crisis. Blackwell Publishing Ltd https://hdl.handle.net/20.500.14352/50321 |
| spellingShingle | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain Horra Del Barco, Raúl De La 551.736(234.1) Biotic crisis Iberian Ranges Late Permian Palaeosols Permian- Triassic boundary Geología estratigráfica 2506.19 Estratigrafía |
| title | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain |
| title_full | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain |
| title_fullStr | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain |
| title_full_unstemmed | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain |
| title_short | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain |
| title_sort | Palaeoenvironmental significance of Late Permian palaeosols in the South-Eastern Iberian Ranges, Spain |
| topic | 551.736(234.1) Biotic crisis Iberian Ranges Late Permian Palaeosols Permian- Triassic boundary Geología estratigráfica 2506.19 Estratigrafía |
| topic_facet | 551.736(234.1) Biotic crisis Iberian Ranges Late Permian Palaeosols Permian- Triassic boundary Geología estratigráfica 2506.19 Estratigrafía |
| url | https://hdl.handle.net/20.500.14352/50321 |