Facies

, Volume 60, Issue 4, pp 941–962 | Cite as

Lithofacies and biostratigraphical correlation of marine Carboniferous rocks in the Tindouf Basin, NW Africa

  • P. Cózar
  • A. García-Frank
  • I. D. Somerville
  • D. Vachard
  • S. Rodríguez
  • P. Medina-Varea
  • I. Said
Original Article

Abstract

Spatial and temporal variations of Carboniferous sediment accumulation within the northwestern part of the northern flank of the Tindouf Syncline in Saharan Morocco allowed to distinguish 16 lithofacies types. The predominant sedimentation pattern is cyclic, with the overall succession recording a major regressive trend. Outer platform siliciclastics in the lower part (Tournaisian and Viséan) pass up to middle and inner platform mixed siliciclastic and carbonate sediments (late Viséan–Serpukhovian) and finally to continental sandstones in the Bashkirian capping the marine carbonate sedimentation. The lack of similarities in a correlation with southern outcrops in the Tindouf Syncline suggests tectonically controlled sedimentation. The upper Tournaisian to lower Bashkirian succession records the incipient uplift of the Anti-Atlas Mountains, changing the paleogeography and, therefore, affecting the paleoecologic conditions, as well as the sedimentary environments in the Tindouf Basin. It is suggested that from the Serpukhovian onwards, much of the Anti-Atlas was uplifted, leading to subaerial conditions, while during the late Viséan, only a few small inliers had emerged. Although the number of Proterozoic emergent inliers of the Anti-Atlas is unknown, during the late Viséan, the Anti-Atlas Mountain belt is regarded as an emerging structure, with a distinct influence on the paleobiogeography of the region.

Keywords

Carboniferous Morocco Microfacies Depositional environments Tectonics Biostratigraphic correlation 

References

  1. Boote DRD, Clark-Lowes DD, Traut MW (1998) Palaeozoic petroleum systems of North Africa. In: Macgregor DS, Moody RTJ, Clark-Lowes DD (eds) Petroleum Geology of North Africa. Geological Society London Special Publications, vol 132, pp 7–68Google Scholar
  2. Bourque PA, Madi A, Mamet B (1995) Waulsortian-type bioherm development and response to sea-level fluctuations: upper Viséan of Béchar Basin, western Algeria. J Sediment Res B65:80–95Google Scholar
  3. Brady HB (1870) Notes on the foraminifera of mineral veins and the adjacent strata. In: Moore C (ed) Report on mineral veins in Carboniferous limestones and their organic contents. Reports of the British Association for the Advancement of Science. London, 39th meeting, Exeter 1869, London, pp 381–382Google Scholar
  4. Brazhnikova NE, Vakarchuk GI, Vdovenko MV, Vinnichenko LV, Karpova MA, Kolomiets YaI, Potievskaya PD, Rostovtseva LF, Shevchenko, GD (1967) Microfaunal marker-horizons from the Carboniferous and Permian deposits of the Dnieper-Donets Depression. Akad Nauk Ukr SSR, Inst Geol Nauk, Trudy, Izdat Naukova Dumka, Kiev, pp 1–224 (in Russian)Google Scholar
  5. Catuneanu O, Galloway WE, Kendall CGSC, Miall AD, Posamentier HW, Strasser A, Tucker ME (2011) Sequence stratigraphy: methodology and nomenclature. Newsl Stratigr 44:173–245CrossRefGoogle Scholar
  6. Cavaroc VV, Padgett G, Stephens DG, Kanes WH, Boudda A, Woollen ID (1976) Late Paleozoic of the Tindouf Basin—North Africa. J Sediment Petrol 46:77–88CrossRefGoogle Scholar
  7. Choubert G (1952) Histoire géologique du Domaine de l’Anti-Atlas. Notes Mém Serv Géol 100:77–194Google Scholar
  8. Conil R, Lys M (1964) Matériaux pour l´étude micropaléontologique du Dinantien de la Belgique et de la France (Avesnois). Partie 2, foraminifères. Mém Inst géol Univ Louvain 23:1–296Google Scholar
  9. Conil R, Longerstaey PJ, Ramsbottom WHC (1980) Matériaux pour l´étude micropaléontologique du Dinantien de Grande-Bretagne. Mém Inst géol Univ Louvain 30:1–187Google Scholar
  10. Conil R, Groessens E, Laloux M, Poty E, Tourneur F (1991) Carboniferous guide foraminifera, corals and conodonts in the Franco-Belgian and Campine basins. Their potential for widespread correlation. Cour Forschinst Senckenberg 130:15–30Google Scholar
  11. Conrad J (1972a) L’âge et les modalités de la régression carbonifère au bord nord du bassin de Tindouf (Sahara occidental). C R Acad Sci Paris 274:1780–1783Google Scholar
  12. Conrad J (1972b) La régression namurienne sur le Nord de la plate-forme africaine. C R Acad Sci Paris 274:2003–2006Google Scholar
  13. Conrad J (1985) Northwestern and central Saharan areas: Tindouf Basin, North Africa. In: Wagner RH, Winkler Prins CF, Granados LF (eds) The Carboniferous of the World II: Australia, Indian subcontinent, South Africa, South America and North Africa. IUGS Publication No. 20, Madrid, pp 325–327Google Scholar
  14. Conrad J, Legrand-Blain M (1971) Titanaria africana nov. sp. un nouveau Gigantoproductidé du Namurien saharien. Bull Soc Hist Nat Afr Nord 62:107–131Google Scholar
  15. Cózar P, Somerville ID (2004) New algal and foraminiferal assemblages and evidence for recognition of the Asbian-Brigantian boundary in northern England. Proc Yorks Geol Soc 55:43–65CrossRefGoogle Scholar
  16. Cózar P, Vachard D, Somerville ID, Berkhli M, Medina-Varea P, Rodríguez S, Said I (2008) Late Viséan-Serpukhovian foraminiferans and calcareous algae from the Adarouch region (central Morocco), North Africa. Geol J 43:463–485CrossRefGoogle Scholar
  17. Cózar P, Medina-Varea P, Somerville ID, Vachard D, Rodríguez S, Said I (2014a) Foraminifers and conodonts from the late Viséan to early Bashkirian succession in the Saharan Tindouf Basin (southern Morocco): biostratigraphic refinements and implications for correlations in the western Palaeotethys. Geol J 49:271–302CrossRefGoogle Scholar
  18. Cózar P, Vachard D, Somerville ID, Medina-Varea P, Rodríguez S, Said I (2014b) The Tindouf Basin, a marine refuge during the Serpukhovian (Carboniferous) mass extinction in the northwestern Gondwana platform. Palaeogeogr Palaeoclimatol Palaeoecol 394:12–28CrossRefGoogle Scholar
  19. Cummings RH (1955) New genera of foraminifera from the British Lower Carboniferous. J Wash Acad Sci 45:1–8Google Scholar
  20. Davydov VI, Crowley JL, Schmitz MD, Poletaev VI (2010) High-precision U-Pb zircon age calibration of the global Carboniferous time scale in Milankovitch band cyclicity in the Donets Basin, eastern Ukraine. Geochem Geophy Geosyst 11:1–22CrossRefGoogle Scholar
  21. Dunham RJ (1962) Classification of carbonate rocks according to depositional texture. In: Ham WE (ed) Classification of carbonate rocks. Mem Am Ass Petrol Geol, vol 1, pp 108–121Google Scholar
  22. Embry AF, Klovan JE (1971) A Late Devonian reef tract on northeastern Banks Island, Northwest Territories. Bull Can Petrol Geol 19:730–781Google Scholar
  23. Fabre J (2005) Géologie du Sahara occidental et central. Tervuren Afr Geosci Coll 108:1–572Google Scholar
  24. Grozdilova LP, Lebedeva NS (1954) Foraminifers of the Lower Carboniferous and Bashkirian Stage of the Middle Carboniferous of the Kolva-Vishera area. Trudy Vses Neft Nauch-Issle Geol-razved Inst (VNIGRI), Mikrofauna SSSR Sb 7, nov ser 81:4–235 (in Russian)Google Scholar
  25. Guiraud R, Bosworth W, Thierry J, Delplanque A (2005) Phanerozoic geological evolution of Northern and Central Africa: an overview. J Afr Earth Sci 43:83–143CrossRefGoogle Scholar
  26. Hoepffner Ch, Soulaimani A, Piqué A (2005) The Moroccan Hercynides. J Afr Earth Sci 43:144–165CrossRefGoogle Scholar
  27. Hollard H (1970) Sur la transgression dinantienne du Maroc présaharien. In: International Carboniferous Congress, Sheffield (1967), Rpt., vol 3, pp 923–936Google Scholar
  28. Hollard H, Jacquemont P (1956) Note sur l’âge de la série de la Betaïna (vallée du Dra, Sud-Marocain). C R Acad Sci Paris 1956:2651–2654Google Scholar
  29. Klug C, Döring S, Korn D, Ebbinghausen V (2006) The Viséan sedimentary succession at the Gara el Itima (Anti-Atlas, Morocco) and its ammonoid faunas. Foss Rec 9:3–60CrossRefGoogle Scholar
  30. Legrand-Blain M (1973) Les Gigantoproductidés (brachiopodes) du Sahara algérien. I. Gigantoproductides viséens. Bull Soc Hist Nat Afr Nord 64:79–157Google Scholar
  31. Legrand-Blain M (1987) Les Gigantoproductidae (brachiopodes) namuriens du Sahara algérien. Bull Soc Belge Géol Paléont Hydrol 96:159–194Google Scholar
  32. Legrand-Blain M, Aretz M, Atif KFT (2010) Discussion of “Carboniferous stratigraphy and depositional environments in the Ahnet Mouydir area (Algerian Sahara)”. By Wendt et al. (Facies 55(3): 443–472. doi:10.1007/s10347-008-176y). Facies 56:471–476
  33. Lys M (1979) Micropaléontologie (Foraminifères) des formations marines du Carbonifère saharien In: 8ème Congrès International du Stratigraphie du Carbonifère, Moscow, 1975, vol. 2, pp 37–47Google Scholar
  34. Lys M (1985) North Africa—Foraminifera. In: Wagner RH, Winkler-Prins CF, Granados LF (eds) The Carboniferous of the World II: Australia, Indian subcontinent, South Africa and North Africa. IUGS publication No. 20 Madrid, pp 354–364Google Scholar
  35. Malti FZ, Benhamou M, Mekahli L, Benyoucef M (2008) The development of the Carboniferous Ben-Zireg-Zousfana Trough in the northern part of the Béchar Basin, Western Algeria: implications for its structural evolution, sequence stratigraphy and palaeogeography. Geol J 43:337–360CrossRefGoogle Scholar
  36. Mamet BL, Choubert G, Hottinger G (1966) Notes sur le Carbonifère du Jebel Ouarkziz. Étude du passage du Viséen au Namurien d´après les foraminifères. Notes serv géol Maroc 27(198):7–21Google Scholar
  37. Massa D (1985) North Africa—Libya. In: Wagner RH, Winkler Prins CF, Granados LF (eds) The Carboniferous of the World II: Australia, Indian subcontinent, South Africa, South America and North Africa. IUGS Publication No. 20, Madrid, pp 344–347Google Scholar
  38. Michard A, Yazidi A, Benziane F, Hollard H, Willefert S (1982) Foreland thrusts and olistostromes on the pre-Sahara margin of the Variscan orogen, Morocco. Geology 10:253–256CrossRefGoogle Scholar
  39. Michard A, Hoepffner C, Soulaimani A, Baidder L (2008) The Variscan Belt. In: Michard A, Saddiqi O, Chalouan A, Frizon de Lamotte D (eds) Continental evolution. The geology of Morocco. Lecture Notes in Earth Science, vol 116, pp 65–132Google Scholar
  40. Murphy JB, Nance RD, Cawood PA (2010) Contrasting modes of supercontinent formation and the conundrum of Pangea. Gondwana Res 15:408–420CrossRefGoogle Scholar
  41. Nance RD, Gutiérrez-Alonso G, Duncan-Keppie J, Linnemann U, Murphy JB, Quesada C, Strachan RA, Woodcock NH (2010) Evolution of the Rheic Ocean. Gondwana Res 17:194–222CrossRefGoogle Scholar
  42. Pareyn C (1961) Les massifs carbonifères du Sahara sud-oranais. I: Stratigraphie et tectonique. II: paléontologie stratigraphique. Publ Centre Rech Sahar Géol 1, I: 1–326, II: 1–224Google Scholar
  43. Pelipenko Y (1990) Homogénéisation de la stratigraphie des séries paléozoïques sahariennes. 1ère partie: le Carbonifère. Rapport Sonatrach, pp 1–21 (internal report)Google Scholar
  44. Peterson JA (1985) Geology and petroleum resource or North-Central and Northeastern Africa. US Geol Surv Open-File Rep 85-709, pp 1–54 Google Scholar
  45. Peterson JA (1986) Geology and petroleum resource assessment of onshore northwestern Africa. US Geol Surv Open-File Rep 86-183, pp 1–25Google Scholar
  46. Piqué A (2001) Geology of Northwest Africa. Borntraeger, BerlinGoogle Scholar
  47. Rauser-Chernousova DM, Belyaev G, Reitlinger EA (1936) Upper Paleozoic foraminifers of the Pechora region. Akad nauk SSSR, Trudy Poly Kom 28:159–232 (in Russian)Google Scholar
  48. Reitlinger EA (1949) Smaller foraminifers in the lower part of the Middle Carboniferous of the Middle Urals and Kama River area. Izv Akad Nauk SSSR Ser Geol 6:149–164 (in Russian)Google Scholar
  49. Reitlinger EA (1961) Stratigraphy of Middle Carboniferous deposits of the Sky. No. 1 section, Red Glades of the middle Volga. Akad nauk SSSR, Geol Inst Nauk, Min Neft Prom SSSR, Trudy, 380 p (in Russian)Google Scholar
  50. Rodríguez S, Somerville ID, Said I, Cózar P (2013a) An upper Viséan (Asbian-Brigantian) and Serpukhovian coral succession at Djebel Ouarkziz (northern Tindouf Basin, southern Morocco). Riv Ital Paleont Stratigr 119:3–18Google Scholar
  51. Rodríguez S, Somerville ID, Said I, Cózar P (2013b) Mississippian-like rugose corals from a Bashkirian biostrome in the Tindouf basin, S. Morocco. Span J Palaeont 28:253–282 Google Scholar
  52. Sebbar A (1998) Foraminifères et Algues calcaires du Carbonifère, bassin de Reggane, Sahara central, Algérie. Bull Serv Géol Algér 9:123–147Google Scholar
  53. Sebbar A (2000) Dynamique des microfossiles (foraminifères benthiques et algues calcaires) en relation avec leurs microfaciès carbonifères dans le Sahara nord-ouest algérien (bassins de Béchar, Reganne et Tindouf). Unpubl PhD Thesis Algiers, 01/2000, 370 pGoogle Scholar
  54. Sebbar A, Préat A, Mamet BL (2000) Microfaciès et biozonation de la rampe mixte carbonifère du bassin de Tindouf, Algérie. Bull Centr Rech Explor Prod Elf-Aquitaine 22:203–239Google Scholar
  55. Sebti S, Saddiqi O, El Haïmer FZ, Baidder L, Michard A, Ruiz GMH, Bousquet R, Frizon de Lamotte D (2009) Vertical movements at the fringe of the West African Craton: first zircon fission track datings from the Anti-Atlas Precambrian basement, Morocco. CR Geosci 341:71–77CrossRefGoogle Scholar
  56. Somerville ID (2008) Biostratigraphic zonation and correlation of Mississippian rocks in Western Europe: some case studies in the late Viséan/Serpukhovian. Geol J 43:209–240CrossRefGoogle Scholar
  57. Somerville ID, Cózar P (2005) Late Asbian to Brigantian (Mississippian) foraminifera from south-east Ireland: comparison with Northern England assemblages. J Micropalaeont 24:131–142CrossRefGoogle Scholar
  58. Somerville ID, Cózar P, Said I, Vachard D, Medina-Varea P, Rodríguez S (2013) Palaeobiogeographic constraints on the distribution of foraminifers and rugose corals in the Carboniferous Tindouf Basin, S. Morocco. J Palaeogeogr 2:1–18Google Scholar
  59. Stache G (1883) Fragmente einer afrikanischen Kohlenkalkfauna aus dem Gebiete der West-Sahara. Bericht über die Untersuchung der von Dr. Oskar Lenz auf der Reise von Marokko nach Timbuktu gesammelten paläozoischen Gesteine und Fossilreste. Sitzber Kais Akad Wiss Math-nat wiss Cl46:369–418Google Scholar
  60. Tucker ME (2003) Mixed clastic-carbonate cycles and sequences: quaternary of Egypt and carboniferous of England. Geol Croat 56:19–37Google Scholar
  61. Tucker ME, Gallagher J, Leng MJ (2009) Are beds in shelf carbonate millennial-scale cycles? An example from the mid-carboniferous of northern England. Sediment geol 214:19–34Google Scholar
  62. Villeneuve M (2005) Paleozoic basins in West Africa and the Mauritanide thrust belt. J Afr Earth Sci 43:166–195CrossRefGoogle Scholar
  63. Wendt J (1985) Disintegration of the continental margin of northwestern Gondwana: Late Devonian of the eastern Anti-Atlas (Morocco). Geology 13:815–818CrossRefGoogle Scholar
  64. Wendt J, Kaufmann B, Belka Z, Korn D (2009) Carboniferous stratigraphy and depositional environments in the Ahnet Mouydir area (Algerian Sahara). Facies 55:269–299CrossRefGoogle Scholar
  65. Wendt J, Kaufmann B, Belka Z, Korn D (2010) Carboniferous stratigraphy and depositional environments in the Ahnet Mouydir area (Algerian Sahara): reply to the discussion by Legrand-Blain et al. (doi:10.1007/s10347-010-0214-4). Facies 56:477–481

Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  • P. Cózar
    • 1
  • A. García-Frank
    • 2
  • I. D. Somerville
    • 3
  • D. Vachard
    • 4
  • S. Rodríguez
    • 2
  • P. Medina-Varea
    • 2
  • I. Said
    • 5
  1. 1.Instituto de Geociencias (CSIC, UCM)MadridSpain
  2. 2.Departamento de PaleontologíaUniversidad Complutense de MadridMadridSpain
  3. 3.UCD School of Geological SciencesUniversity College DublinDublin 4Ireland
  4. 4.Université de Lille 1, UMR 8217 du CNRS: GéosystèmesVilleneuve d’AscqFrance
  5. 5.Division du Patrimoine Géologique (DPG), Direction du Développement Minier (DDM)Ministère de l’Énergie, des Mines, de l’Eau et de l’EnvironnementRabatMorocco

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