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
Main Authors: Gärtner, Andreas, Youbi, Nasrrddine, Villeneuve, Michel, Sagawe, Anja, Hofmann, Mandy, Mahmoudi, Abdelkader, Boumehdi, Moulay Ahmed, Linnemann, Ulf
Format: Journal Article
Language:English
Published: Berlin/Heidelberg Springer Berlin Heidelberg 01-11-2017
Springer Nature B.V
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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.
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
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  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
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  givenname: Michel
  surname: Villeneuve
  fullname: Villeneuve, Michel
  organization: CEREGE, Centre Saint-Charles, Aix-Marseille Université
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  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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Issue 8
Keywords West African Craton
U–Th–Pb geochronology
Palaeozoic sediment transport
Zircon morphology
Zircon from limestone
Language English
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Springer Verlag
Publisher_xml – name: Springer Berlin Heidelberg
– name: Springer Nature B.V
– name: Springer Verlag
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SSID ssj0014371
Score 2.4186418
Snippet Detrital zircon provenance studies are an established tool to develop palaeogeographic models, mostly based on zircon of siliciclastic rocks and isotope data....
SourceID hal
proquest
crossref
springer
SourceType Open Access Repository
Aggregation Database
Publisher
StartPage 2747
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
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Original Paper
Palaeozoic
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Sciences of the Universe
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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)
URI https://link.springer.com/article/10.1007/s00531-017-1457-x
https://www.proquest.com/docview/1951216856
https://hal.science/hal-01765602
Volume 106
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