Dating the change from endorheic to exorheic conditions in the drainage system of the Granada Basin (southern Spain)
The drainage system of the Granada Basin in southern Spain has evolved from endorheic to exorheic since the basin emerged and became continental in the latest Tortonian (late Miocene). The age of implementation for the recent exorheic, east-west drainage can now be identified by small mammal dating....
Gespeichert in:
| Veröffentlicht in: | Palaios 2009-08, Vol.24 (8), p.544-549 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 549 |
|---|---|
| container_issue | 8 |
| container_start_page | 544 |
| container_title | Palaios |
| container_volume | 24 |
| creator | García-alix, Antonio Minwer-Barakat, Raef Martín, José M Suárez, Elvira Martín Freudenthal, Matthijs |
| description | The drainage system of the Granada Basin in southern Spain has evolved from endorheic to exorheic since the basin emerged and became continental in the latest Tortonian (late Miocene). The age of implementation for the recent exorheic, east-west drainage can now be identified by small mammal dating. This drainage configuration began in the latest Pliocene–earliest Pleistocene due to the capture of the Genil River by a Cacín River tributary. It represented an important change in the behavior of the basin and therefore in the geomorphology, as depositional forms and processes were replaced by erosive ones. While the basin was endorheic, sedimentation was active throughout the basin. Afterward the change to exorheic and up to the present, erosion dominates and sedimentation occurs only in some small, fault-controlled depositional depocenters. |
| doi_str_mv | 10.2110/palo.2009.p09-015r |
| format | Article |
| fullrecord | <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_21071428</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>40606444</jstor_id><sourcerecordid>40606444</sourcerecordid><originalsourceid>FETCH-LOGICAL-a400t-cbc8b1ce2999c28fcb57b52d647739a87bf5e6a62b17aef2d8dd00d4b1df6b6a3</originalsourceid><addsrcrecordid>eNqNkE1rGzEQhkVpoW7aP1AI6BQawroj7Zf2mKRNWgj0kPYs9DFry6yljSTT5N9Hzoaee5ph5nkH6SHkM4M1Zwy-zmoKaw4wrGcYKmBtfENWbKhF1da8fktWIERdsbpl78mHlHZQEGj5iuRvKju_oXmL1GyV3yAdY9hT9DbELTpDc6D4-Nqb4K3LLvhEnX_J2KicVyWVnlLGPQ3jy_g2Kq-solcqFfBLCocyjZ7ezwU__0jejWpK-Om1npA_N99_X_-o7n7d_ry-vKtUA5Aro43QzCAfhsFwMRrd9rrltmv6vh6U6PXYYqc6rlmvcORWWAtgG83s2OlO1SfkbLk7x_BwwJTl3iWD06Q8hkOSnEHPGi4KyBfQxJBSxFHO0e1VfJIM5FGwPAqWR8GyCJZHwSV0uoR2KYf4L9FAB13TNGV_sew3GJJx6A3-DXGychcO0Zd_L_dAdH3LCg0LrV0IHv_nAc-NwJpa</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>21071428</pqid></control><display><type>article</type><title>Dating the change from endorheic to exorheic conditions in the drainage system of the Granada Basin (southern Spain)</title><source>BioOne Complete</source><source>JSTOR Archive Collection A-Z Listing</source><creator>García-alix, Antonio ; Minwer-Barakat, Raef ; Martín, José M ; Suárez, Elvira Martín ; Freudenthal, Matthijs</creator><creatorcontrib>García-alix, Antonio ; Minwer-Barakat, Raef ; Martín, José M ; Suárez, Elvira Martín ; Freudenthal, Matthijs</creatorcontrib><description>The drainage system of the Granada Basin in southern Spain has evolved from endorheic to exorheic since the basin emerged and became continental in the latest Tortonian (late Miocene). The age of implementation for the recent exorheic, east-west drainage can now be identified by small mammal dating. This drainage configuration began in the latest Pliocene–earliest Pleistocene due to the capture of the Genil River by a Cacín River tributary. It represented an important change in the behavior of the basin and therefore in the geomorphology, as depositional forms and processes were replaced by erosive ones. While the basin was endorheic, sedimentation was active throughout the basin. Afterward the change to exorheic and up to the present, erosion dominates and sedimentation occurs only in some small, fault-controlled depositional depocenters.</description><identifier>ISSN: 0883-1351</identifier><identifier>EISSN: 1938-5323</identifier><identifier>DOI: 10.2110/palo.2009.p09-015r</identifier><language>eng</language><publisher>Society for Sedimentary Geology</publisher><subject>Agricultural drainage systems ; Andalusia Spain ; assemblages ; Betic Cordillera ; biostratigraphy ; Cacin River ; Cacín River ; Cenozoic ; Chordata ; drainage ; Drainage basins ; Europe ; Fluvial erosion ; Genil River ; Geology ; Granada Depression ; Granada Spain ; Iberian Peninsula ; Lakes ; lithostratigraphy ; lower Pleistocene ; Mammalia ; Mammals ; Neogene ; paleogeography ; paleohydrology ; Pleistocene ; Pliocene ; Quaternary ; RESEARCH NOTE ; River basins ; Rodents ; Sediments ; small mammal ; Southern Europe ; Spain ; Stratigraphy ; Tertiary ; Tetrapoda ; Tributaries ; upper Pliocene ; Vertebrata</subject><ispartof>Palaios, 2009-08, Vol.24 (8), p.544-549</ispartof><rights>Society for Sedimentary Geology</rights><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from GeoScienceWorld @Alexandria, VA @USA @United States. Reference includes data supplied by SEPM (Society for Sedimentary Geology) @Tulsa, OK @USA @United States</rights><rights>2009 SEPM (Society for Sedimentary Geology)</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a400t-cbc8b1ce2999c28fcb57b52d647739a87bf5e6a62b17aef2d8dd00d4b1df6b6a3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://bioone.org/doi/pdf/10.2110/palo.2009.p09-015r$$EPDF$$P50$$Gbioone$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/40606444$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,26978,27924,27925,52363,58017,58250</link.rule.ids></links><search><creatorcontrib>García-alix, Antonio</creatorcontrib><creatorcontrib>Minwer-Barakat, Raef</creatorcontrib><creatorcontrib>Martín, José M</creatorcontrib><creatorcontrib>Suárez, Elvira Martín</creatorcontrib><creatorcontrib>Freudenthal, Matthijs</creatorcontrib><title>Dating the change from endorheic to exorheic conditions in the drainage system of the Granada Basin (southern Spain)</title><title>Palaios</title><description>The drainage system of the Granada Basin in southern Spain has evolved from endorheic to exorheic since the basin emerged and became continental in the latest Tortonian (late Miocene). The age of implementation for the recent exorheic, east-west drainage can now be identified by small mammal dating. This drainage configuration began in the latest Pliocene–earliest Pleistocene due to the capture of the Genil River by a Cacín River tributary. It represented an important change in the behavior of the basin and therefore in the geomorphology, as depositional forms and processes were replaced by erosive ones. While the basin was endorheic, sedimentation was active throughout the basin. Afterward the change to exorheic and up to the present, erosion dominates and sedimentation occurs only in some small, fault-controlled depositional depocenters.</description><subject>Agricultural drainage systems</subject><subject>Andalusia Spain</subject><subject>assemblages</subject><subject>Betic Cordillera</subject><subject>biostratigraphy</subject><subject>Cacin River</subject><subject>Cacín River</subject><subject>Cenozoic</subject><subject>Chordata</subject><subject>drainage</subject><subject>Drainage basins</subject><subject>Europe</subject><subject>Fluvial erosion</subject><subject>Genil River</subject><subject>Geology</subject><subject>Granada Depression</subject><subject>Granada Spain</subject><subject>Iberian Peninsula</subject><subject>Lakes</subject><subject>lithostratigraphy</subject><subject>lower Pleistocene</subject><subject>Mammalia</subject><subject>Mammals</subject><subject>Neogene</subject><subject>paleogeography</subject><subject>paleohydrology</subject><subject>Pleistocene</subject><subject>Pliocene</subject><subject>Quaternary</subject><subject>RESEARCH NOTE</subject><subject>River basins</subject><subject>Rodents</subject><subject>Sediments</subject><subject>small mammal</subject><subject>Southern Europe</subject><subject>Spain</subject><subject>Stratigraphy</subject><subject>Tertiary</subject><subject>Tetrapoda</subject><subject>Tributaries</subject><subject>upper Pliocene</subject><subject>Vertebrata</subject><issn>0883-1351</issn><issn>1938-5323</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><recordid>eNqNkE1rGzEQhkVpoW7aP1AI6BQawroj7Zf2mKRNWgj0kPYs9DFry6yljSTT5N9Hzoaee5ph5nkH6SHkM4M1Zwy-zmoKaw4wrGcYKmBtfENWbKhF1da8fktWIERdsbpl78mHlHZQEGj5iuRvKju_oXmL1GyV3yAdY9hT9DbELTpDc6D4-Nqb4K3LLvhEnX_J2KicVyWVnlLGPQ3jy_g2Kq-solcqFfBLCocyjZ7ezwU__0jejWpK-Om1npA_N99_X_-o7n7d_ry-vKtUA5Aro43QzCAfhsFwMRrd9rrltmv6vh6U6PXYYqc6rlmvcORWWAtgG83s2OlO1SfkbLk7x_BwwJTl3iWD06Q8hkOSnEHPGi4KyBfQxJBSxFHO0e1VfJIM5FGwPAqWR8GyCJZHwSV0uoR2KYf4L9FAB13TNGV_sew3GJJx6A3-DXGychcO0Zd_L_dAdH3LCg0LrV0IHv_nAc-NwJpa</recordid><startdate>200908</startdate><enddate>200908</enddate><creator>García-alix, Antonio</creator><creator>Minwer-Barakat, Raef</creator><creator>Martín, José M</creator><creator>Suárez, Elvira Martín</creator><creator>Freudenthal, Matthijs</creator><general>Society for Sedimentary Geology</general><general>SEPM (Society for Sedimentary Geology)</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>200908</creationdate><title>Dating the change from endorheic to exorheic conditions in the drainage system of the Granada Basin (southern Spain)</title><author>García-alix, Antonio ; Minwer-Barakat, Raef ; Martín, José M ; Suárez, Elvira Martín ; Freudenthal, Matthijs</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a400t-cbc8b1ce2999c28fcb57b52d647739a87bf5e6a62b17aef2d8dd00d4b1df6b6a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Agricultural drainage systems</topic><topic>Andalusia Spain</topic><topic>assemblages</topic><topic>Betic Cordillera</topic><topic>biostratigraphy</topic><topic>Cacin River</topic><topic>Cacín River</topic><topic>Cenozoic</topic><topic>Chordata</topic><topic>drainage</topic><topic>Drainage basins</topic><topic>Europe</topic><topic>Fluvial erosion</topic><topic>Genil River</topic><topic>Geology</topic><topic>Granada Depression</topic><topic>Granada Spain</topic><topic>Iberian Peninsula</topic><topic>Lakes</topic><topic>lithostratigraphy</topic><topic>lower Pleistocene</topic><topic>Mammalia</topic><topic>Mammals</topic><topic>Neogene</topic><topic>paleogeography</topic><topic>paleohydrology</topic><topic>Pleistocene</topic><topic>Pliocene</topic><topic>Quaternary</topic><topic>RESEARCH NOTE</topic><topic>River basins</topic><topic>Rodents</topic><topic>Sediments</topic><topic>small mammal</topic><topic>Southern Europe</topic><topic>Spain</topic><topic>Stratigraphy</topic><topic>Tertiary</topic><topic>Tetrapoda</topic><topic>Tributaries</topic><topic>upper Pliocene</topic><topic>Vertebrata</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>García-alix, Antonio</creatorcontrib><creatorcontrib>Minwer-Barakat, Raef</creatorcontrib><creatorcontrib>Martín, José M</creatorcontrib><creatorcontrib>Suárez, Elvira Martín</creatorcontrib><creatorcontrib>Freudenthal, Matthijs</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Palaios</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>García-alix, Antonio</au><au>Minwer-Barakat, Raef</au><au>Martín, José M</au><au>Suárez, Elvira Martín</au><au>Freudenthal, Matthijs</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dating the change from endorheic to exorheic conditions in the drainage system of the Granada Basin (southern Spain)</atitle><jtitle>Palaios</jtitle><date>2009-08</date><risdate>2009</risdate><volume>24</volume><issue>8</issue><spage>544</spage><epage>549</epage><pages>544-549</pages><issn>0883-1351</issn><eissn>1938-5323</eissn><abstract>The drainage system of the Granada Basin in southern Spain has evolved from endorheic to exorheic since the basin emerged and became continental in the latest Tortonian (late Miocene). The age of implementation for the recent exorheic, east-west drainage can now be identified by small mammal dating. This drainage configuration began in the latest Pliocene–earliest Pleistocene due to the capture of the Genil River by a Cacín River tributary. It represented an important change in the behavior of the basin and therefore in the geomorphology, as depositional forms and processes were replaced by erosive ones. While the basin was endorheic, sedimentation was active throughout the basin. Afterward the change to exorheic and up to the present, erosion dominates and sedimentation occurs only in some small, fault-controlled depositional depocenters.</abstract><pub>Society for Sedimentary Geology</pub><doi>10.2110/palo.2009.p09-015r</doi><tpages>6</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0883-1351 |
| ispartof | Palaios, 2009-08, Vol.24 (8), p.544-549 |
| issn | 0883-1351 1938-5323 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_21071428 |
| source | BioOne Complete; JSTOR Archive Collection A-Z Listing |
| subjects | Agricultural drainage systems Andalusia Spain assemblages Betic Cordillera biostratigraphy Cacin River Cacín River Cenozoic Chordata drainage Drainage basins Europe Fluvial erosion Genil River Geology Granada Depression Granada Spain Iberian Peninsula Lakes lithostratigraphy lower Pleistocene Mammalia Mammals Neogene paleogeography paleohydrology Pleistocene Pliocene Quaternary RESEARCH NOTE River basins Rodents Sediments small mammal Southern Europe Spain Stratigraphy Tertiary Tetrapoda Tributaries upper Pliocene Vertebrata |
| title | Dating the change from endorheic to exorheic conditions in the drainage system of the Granada Basin (southern Spain) |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-29T15%3A29%3A47IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Dating%20the%20change%20from%20endorheic%20to%20exorheic%20conditions%20in%20the%20drainage%20system%20of%20the%20Granada%20Basin%20(southern%20Spain)&rft.jtitle=Palaios&rft.au=Garc%C3%ADa-alix,%20Antonio&rft.date=2009-08&rft.volume=24&rft.issue=8&rft.spage=544&rft.epage=549&rft.pages=544-549&rft.issn=0883-1351&rft.eissn=1938-5323&rft_id=info:doi/10.2110/palo.2009.p09-015r&rft_dat=%3Cjstor_proqu%3E40606444%3C/jstor_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=21071428&rft_id=info:pmid/&rft_jstor_id=40606444&rfr_iscdi=true |