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Els rius - (B) i (C) - que anteriorment drenaven la Mediterr\u00e0nia, van escavar en els marges continentals profunds congostos erosius; (D) l'evaporaci\u00f3 de la Mediterr\u00e0nia va dur a la saturaci\u00f3 de la sal en les seves aig\u00fces i a la precipitaci\u00f3 de capes de sal de m\u00e9s d'un kil\u00f2metre de gruix; (E) a les parts m\u00e9s profundes del mar hi van quedar llacs on s'evaporava l'aigua recollida de la conca mediterr\u00e0nia. La vinyeta recrea el tr\u00e0nsit de mam\u00edfers, com els cam\u00e8lids i els jerbus petits, a trav\u00e9s de l'estret de Gibraltar.Interpretaci\u00f3 art\u00edstica realitzada per Pau Bah\u00ed amb la supervisi\u00f3 cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsic de l'Institut de Ci\u00e8ncies de la Terra Jaume Almera (CSIC)","language":"ca"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"aa8a6e8a1d0f9352fecdb579e54e9e7762d95700","datavalue":{"value":{"text":"Cierre del \u00faltimo canal de conexi\u00f3n entre el Mediterr\u00e1neo y el Atl\u00e1ntico, conduciendo a la desecaci\u00f3n completa del primero durante la Crisis Salina Mesiniense hace 5,96 millones de a\u00f1os. Los r\u00edos - (B) y (C) - que anteriormente drenaban al Mediterr\u00e1neo excavaron en los m\u00e1rgenes continentales profundas gargantas erosivas; (D) la evaporaci\u00f3n del Mediterr\u00e1neo condujo a la saturaci\u00f3n de la sal en sus aguas y a la precipitaci\u00f3n de capas de sal de m\u00e1s de un kil\u00f3metro de espesor; (E) en las partes m\u00e1s profundas del mar quedaron lagos donde se evaporaba el agua recogida de la cuenca mediterr\u00e1nea. La vi\u00f1eta recrea el tr\u00e1nsito de mam\u00edferos, como cam\u00e9lidos y gerbillos, a trav\u00e9s del estrecho de Gibraltar.Interpretaci\u00f3n art\u00edstica realizada por Pau Bah\u00ed bajo la supervisi\u00f3n cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsico del Instituto de Ciencias de la Tierra Jaume Almera (CSIC)","language":"es"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"5916c7fb39f77315e232c5178e47c7fc605e31be","datavalue":{"value":{"text":"Closing the last channel connecting the Mediterranean and the Atlantic, leading to the first drying during the Messinian salinity crisis 5.96 million years ago. Rivers - (B) and (C) - which previoust drained to the Mediterranean excavated erosion gorges in the continental margins; (D) evaporation of the Mediterranean led to saturation of the salt in its waters and precipitation of salt layers over a kilometer thick; (E) in the deeper parts of the sea were lakes where water collected from the Mediterranean basin evaporated. The inset box recreates the mammalian, like cam\u00e9lidos and gerbils, transit across the Strait.Artistic interpretation by Pau Bah\u00ed under the scientific supervision of Daniel Garcia Castellanos, geophysicist at the Institute of Earth Sciences Jaume Almera (CSIC)","language":"en"},"type":"monolingualtext"},"datatype":"monolingualtext"}]},"qualifiers-order":["P2096"],"id":"Q605948$1c21083a-487c-ab91-4bca-9e1d8eb60fa5","rank":"normal"},{"mainsnak":{"snaktype":"value","property":"P18","hash":"2966c9e63b3179f120af4edacf66cf73690d14db","datavalue":{"value":"Messinian salinity crisis 5.3 mya stage - flooding.jpg","type":"string"},"datatype":"commonsMedia"},"type":"statement","qualifiers":{"P2096":[{"snaktype":"value","property":"P2096","hash":"9b94d45f26bb240ee8b3c5c231a25c2f18556452","datavalue":{"value":{"text":"Reinundaci\u00f3 de la Mediterr\u00e0nia per aig\u00fces atl\u00e0ntiques que pos\u00e0 fi a la Crisi Salina del Messini\u00e0 fa 5,3 milions d'anys. L'entrada d'aigua es va produir a trav\u00e9s de l'estret de Gibraltar (A) i al omplir la conca mediterr\u00e0nia occidental pass\u00e0 a inundar la oriental, probablement a trav\u00e9s de l'actual estret de Sicilia (F)Interpretaci\u00f3 art\u00edstica realitzada per Pau Bah\u00ed amb la supervisi\u00f3 cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsic de l'Institut de Ci\u00e8ncies de la Terra Jaume Almera (CSIC)","language":"ca"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"9491814ae29f805aa9482c13729b630b016173aa","datavalue":{"value":{"text":"Reinundaci\u00f3n del Mediterr\u00e1neo por aguas atl\u00e1nticas que puso fin a la Crisis Salina Mesiniense hace 5,3 millones de a\u00f1os. La entrada de agua se produjo a trav\u00e9s del estrecho de Gibraltar (A) y al colmatar la cuenca mediterr\u00e1nea occidental pas\u00f3 a inundar la oriental, probablemente a trav\u00e9s del actual estrecho de Sicilia (F).Interpretaci\u00f3n art\u00edstica realizada por Pau Bah\u00ed bajo la supervisi\u00f3n cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsico del Instituto de Ciencias de la Tierra Jaume Almera (CSIC)","language":"es"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"4c5824328b638c1fa0571983af20fa04a9cd2f98","datavalue":{"value":{"text":"Re-flooding of the Mediterranean by Atlantic waters that ended the Messinian salinity crisis 5.3 million years ago (Zanclean flood). Water intrusion occurred across the Strait of Gibraltar (A) and clog the western Mediterranean basin flooded eastern, probably through the current Strait of Sicily (F).Artistic interpretation by Pau Bah\u00ed under the scientific supervision of Daniel Garcia Castellanos, geophysicist at the Institute of Earth Sciences Jaume Almera (CSIC)","language":"en"},"type":"monolingualtext"},"datatype":"monolingualtext"}]},"qualifiers-order":["P2096"],"id":"Q605948$743bc7be-4753-c8b4-53b6-a0ee266ffe71","rank":"normal"},{"mainsnak":{"snaktype":"value","property":"P18","hash":"523774caf4bdd9d38d047562e51902ccddcfba71","datavalue":{"value":"Messinian salinity crisis 6 mya stage - last canal.jpg","type":"string"},"datatype":"commonsMedia"},"type":"statement","qualifiers":{"P2096":[{"snaktype":"value","property":"P2096","hash":"92e6329bbce2b8597e9e73a5f94fd24b0e5d9348","datavalue":{"value":{"text":"Darrera connexi\u00f3 entre l'Atl\u00e0ntic i la Mediterr\u00e0nia que va sobreviure a l'aixecament de l'Arc de Gibraltar fa 6 milions d'anys. Aquest canal va permetre l'entrada d'aig\u00fces atl\u00e0ntiques que compensaven el d\u00e8ficit h\u00eddric de la Mediterr\u00e0nia que rep menys aigua dels rius de la que evapora la seva superf\u00edcie. Al mateix temps, aquest flux entrant d'aigua va produir prou erosi\u00f3 perqu\u00e8 el canal es mantingu\u00e9s malgrat el continuu aixecament de la serralada b\u00e8tica. El tancament de la resta de canals de connexi\u00f3 va causar la hipersalinitat de les aig\u00fces mediterr\u00e0nies i l'inici de la Crisi Salina del Messini\u00e0. La vinyeta mostra l'aixecament de l'Arc de Gibraltar entre la zona b\u00e8tica i la del Rif. Tamb\u00e9 mostra com una part de l'escor\u00e7a es subsumeix en el mantell mentre part del magma m\u00e9s fos puja per esquerdes en l'escor\u00e7a.Interpretaci\u00f3 art\u00edstica realitzada per Pau Bah\u00ed amb la supervisi\u00f3 cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsic de l'Institut de Ci\u00e8ncies de la Terra Jaume Almera (CSIC)","language":"ca"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"0a66bf1e777e93531c350c42d074656ba7a599de","datavalue":{"value":{"text":"\u00daltimo canal de conexi\u00f3n entre el Atl\u00e1ntico y Mediterr\u00e1neo que sobrevivi\u00f3 el levantamiento del Arco de Gibraltar hace 6 millones de a\u00f1os. Ese canal permiti\u00f3 la entrada de aguas atl\u00e1nticas que compensaran el d\u00e9ficit h\u00eddrico del Mediterr\u00e1neo, que recibe menos agua de los r\u00edos de la que evapora en su superficie. A la vez, ese flujo de agua entrante produjo suficiente erosi\u00f3n como para que el canal perviviera pese al continuo levantamiento de la cordillera b\u00e9tica. La clausura de los dem\u00e1s canales de conexi\u00f3n caus\u00f3 la hipersalinidad de las aguas mediterr\u00e1neas y el inicio de la Crisis Salina Mesiniense. La vi\u00f1eta muestra el alzamiento del Arco de Gibraltar entre la zona b\u00e9tica y el Rif. Tambi\u00e9n muestra como una parte de la corteza es subsumida en el manto terrestre y una parte del magma fundido sube por las grietas de la corteza.Interpretaci\u00f3n art\u00edstica realizada por Pau Bah\u00ed bajo la supervisi\u00f3n cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsico del Instituto de Ciencias de la Tierra Jaume Almera (CSIC)","language":"es"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"6341dca67a036e33bfbb6981284f4687c5ab55f5","datavalue":{"value":{"text":"Last canal connecting the Atlantic and Mediterranean which survived the uprising of the Gibraltar Arc 6 million years ago. The canal enabled the entry of Atlantic waters to offset the Mediterranean water deficit, which receives less river water that evaporates from its surface. At the same time, the flow of incoming water erosion produced enough to keep the channel despite the continued rise of the Betic Cordillera. The closure of the other connecting channels caused hypersaline Mediterranean water and the beginning of the Messinian salinity crisis. The inset box shows the rise of the Gibraltar Arc area between the Betic and Rif. Also shown as a part of the crust is subsumed in the Earth's mantle and a portion of molten magma rises through cracks in the crust.Artistic interpretation by Pau Bah\u00ed under the scientific supervision of Daniel Garcia Castellanos, geophysicist at the Institute of Earth Sciences Jaume Almera (CSIC)","language":"en"},"type":"monolingualtext"},"datatype":"monolingualtext"}]},"qualifiers-order":["P2096"],"id":"Q605948$d8ce8fcc-47ee-727c-b2a2-fcaa98393563","rank":"normal"},{"mainsnak":{"snaktype":"value","property":"P18","hash":"205078ddaf78e16b8c49cb23b6e5c198bab79c39","datavalue":{"value":"Messinian salinity crisis 6.5 mya stage.jpg","type":"string"},"datatype":"commonsMedia"},"type":"statement","qualifiers":{"P2096":[{"snaktype":"value","property":"P2096","hash":"a63ec6ae64b48c34cd0d905e1f6ed04235afa63f","datavalue":{"value":{"text":"Restricci\u00f3 dels canals d'intercanvi d'aigua marina entre l'Atl\u00e0ntic i la Mediterr\u00e0nia fa uns 6,5 milions d'anys, abans de la Crisi Salina del Messini\u00e0. La pres\u00e8ncia de diversos canals i la seva profunditat permetia mantenir la salinitat de la Mediterr\u00e0nia a nivells normals, com passa avui en dia gr\u00e0cies als corrents de l'Estret de Gibraltar.Interpretaci\u00f3 art\u00edstica realitzada per Pau Bah\u00ed amb la supervisi\u00f3 cient\u00edfica de Daniel Garc\u00eda Castellanos, geof\u00edsic de l'Institut de Ci\u00e8ncies de la Terra Jaume Almera (CSIC)","language":"ca"},"type":"monolingualtext"},"datatype":"monolingualtext"},{"snaktype":"value","property":"P2096","hash":"4bbd5decc8145faf3750a70ce3bd6b6dc0d10856","datavalue":{"value":{"text":"Restricci\u00f3n de los canales de intercambio de agua marina entre el Atl\u00e1ntico y el Mediterr\u00e1neo hace unos 6.5 millones de a\u00f1os, antes de la Crisis Salina Mesiniense. 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The presence of several corridors and its depth allowed to maintain salinity of the Mediterranean to normal levels as happens today due to the Strait of Gibraltar flows.Artistic interpretation by Pau Bah\u00ed under the scientific supervision of Daniel Garcia Castellanos, geophysicist at the Institute of Earth Sciences Jaume Almera (CSIC)","language":"en"},"type":"monolingualtext"},"datatype":"monolingualtext"}]},"qualifiers-order":["P2096"],"id":"Q605948$13b24cd8-447c-5ea9-d4d9-e9bf2a903c8e","rank":"normal"}],"P276":[{"mainsnak":{"snaktype":"value","property":"P276","hash":"e6c6fbe5c6a4f816df49b8c9be836a2ffcbf7579","datavalue":{"value":{"entity-type":"item","numeric-id":4918,"id":"Q4918"},"type":"wikibase-entityid"},"datatype":"wikibase-item"},"type":"statement","id":"Q605948$58ed3771-4024-c2e4-20bf-ad07380e277e","rank":"normal"}],"P10":[{"mainsnak":{"snaktype":"value","property":"P10","hash":"042b21e4daad264d0d3fbb99eef0f6a3217f4963","datavalue":{"value":"Crisis salina del 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