The zircon evidence of temporally changing sediment transport—the NW Gondwana margin during Cambrian to Devonian time (Aoucert and Smara areas, Moroccan Sahara)
Detrital zircon provenance studies are an established tool to develop palaeogeographic models, mostly based on zircon of siliciclastic rocks and isotope data. But zircon is more than just istopes and features well definable morphological characteristics. The latter may indicate single grain transpor...
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Published in: | International journal of earth sciences : Geologische Rundschau Vol. 106; no. 8; pp. 2747 - 2769 |
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Abstract | Detrital zircon provenance studies are an established tool to develop palaeogeographic models, mostly based on zircon of siliciclastic rocks and isotope data. But zircon is more than just istopes and features well definable morphological characteristics. The latter may indicate single grain transport histories independent of the individual grade of concordance. This additional tool for palaeogeoraphic reconstructions was tested on zircon from siliciclastic and carbonate sedimentary rocks of Palaeozoic age from the Aoucert and Smara areas of the Souttoufides, while findings of zircon in limestone generally open new archives for sedimentary provenance analysis. The morphologies—length, width, roundness, grain surfaces—of 834 detrital zircons from sediments of allochthonous Cambrian, and (par-)autochthonous Ordovician, and Devonian units were studied, while 772 of them were analysed for their U–Th–Pb isotopes by LA-ICP-MS. Mesoproterozoic zircon contents of more than 10% in the Cambrian sediments exclude the West African Craton (WAC) as exclusive source area. Thus, at least one additional external source is suggested. This is likely the western Adrar Souttouf Massif with its significant Mesoproterozoic zircon inheritance, or comparable, yet unknown sources. Decreasing Mesoproterozoic zircon age populations in Ordovician sediments are thought to be linked to the rifting of the terranes in the course of the Rheic Ocean opening and a predominant supply of WAC detritus. The Devonian sediments likely contain reworked material from the Cambrian siliciclastics, which is shown by the zircon age distribution pattern and the zircon morphologies. Therefore, multiple shifts in the direction of sedimentary transport are indicated. |
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AbstractList | Detrital zircon provenance studies are an established tool to develop palaeogeographic models, mostly based on zircon of siliciclastic rocks and isotope data. But zircon is more than just istopes and features well definable morphological characteristics. The latter may indicate single grain transport histories independent of the individual grade of concordance. This additional tool for palaeogeoraphic reconstructions was tested on zircon from siliciclastic and carbonate sedimentary rocks of Palaeozoic age from the Aoucert and Smara areas of the Souttoufides, while findings of zircon in limestone generally open new archives for sedimentary provenance analysis. The morphologies-length, width, roundness, grain surfaces-of 834 detrital zircons from sediments of allochthonous Cambrian, and (par-)autochthonous Ordovician, and Devonian units were studied, while 772 of them were analysed for their U-Th-Pb isotopes by LA-ICP-MS. Mesoproterozoic zircon contents of more than 10% in the Cambrian sediments exclude the West African Craton (WAC) as exclusive source area. Thus, at least one additional external source is suggested. This is likely the western Adrar Souttouf Massif with its significant Mesoproterozoic zircon inheritance, or comparable, yet unknown sources. Decreasing Mesoproterozoic zircon age populations in Ordovician sediments are thought to be linked to the rifting of the terranes in the course of the Rheic Ocean opening and a predominant supply of WAC detritus. The Devonian sediments likely contain reworked material from the Cambrian siliciclastics, which is shown by the zircon age distribution pattern and the zircon morphologies. Therefore, multiple shifts in the direction of sedimentary transport are indicated. |
Author | Mahmoudi, Abdelkader Gärtner, Andreas Boumehdi, Moulay Ahmed Linnemann, Ulf Villeneuve, Michel Hofmann, Mandy Youbi, Nasrrddine Sagawe, Anja |
Author_xml | – sequence: 1 givenname: Andreas orcidid: 0000-0002-1670-7305 surname: Gärtner fullname: Gärtner, Andreas email: andreas.gaertner@senckenberg.de organization: Museum für Mineralogie und Geologie, Sektion Geochronologie, GeoPlasma Lab, Senckenberg Naturhistorische Sammlungen Dresden – sequence: 2 givenname: Nasrrddine surname: Youbi fullname: Youbi, Nasrrddine organization: Department of Geology, Faculty of Sciences-Semlalia, Cadi Ayyad University, Instituto Dom Luiz, Faculdade de Ciências, Universidade de Lisboa – sequence: 3 givenname: Michel surname: Villeneuve fullname: Villeneuve, Michel organization: CEREGE, Centre Saint-Charles, Aix-Marseille Université – sequence: 4 givenname: Anja surname: Sagawe fullname: Sagawe, Anja organization: Museum für Mineralogie und Geologie, Sektion Geochronologie, GeoPlasma Lab, Senckenberg Naturhistorische Sammlungen Dresden – sequence: 5 givenname: Mandy surname: Hofmann fullname: Hofmann, Mandy organization: Museum für Mineralogie und Geologie, Sektion Geochronologie, GeoPlasma Lab, Senckenberg Naturhistorische Sammlungen Dresden – sequence: 6 givenname: Abdelkader surname: Mahmoudi fullname: Mahmoudi, Abdelkader organization: Department of Geology, Faculty of Sciences, Moulay Ismail University – sequence: 7 givenname: Moulay Ahmed surname: Boumehdi fullname: Boumehdi, Moulay Ahmed organization: Department of Geology, Faculty of Sciences-Semlalia, Cadi Ayyad University – sequence: 8 givenname: Ulf surname: Linnemann fullname: Linnemann, Ulf organization: Museum für Mineralogie und Geologie, Sektion Geochronologie, GeoPlasma Lab, Senckenberg Naturhistorische Sammlungen Dresden |
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Keywords | West African Craton U–Th–Pb geochronology Palaeozoic sediment transport Zircon morphology Zircon from limestone |
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Snippet | Detrital zircon provenance studies are an established tool to develop palaeogeographic models, mostly based on zircon of siliciclastic rocks and isotope data.... |
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SubjectTerms | Age Age composition Allochthonous deposits Archives & records Cambrian Carbonates Cratons Detritus Devonian Earth and Environmental Science Earth Sciences Geochemistry Geological time Geology Geophysics/Geodesy Grain Heredity Isotopes Limestone Mineral Resources Ordovician Original Paper Palaeozoic Paleozoic Provenance Rifting Rock Roundness Sciences of the Universe Sediment Sediment transport Sedimentary rocks Sedimentology Sediments Structural Geology Transport Zircon Zirconium |
Title | The zircon evidence of temporally changing sediment transport—the NW Gondwana margin during Cambrian to Devonian time (Aoucert and Smara areas, Moroccan Sahara) |
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