The Tagoudite Formation (also known as the "Upper Tamadout Formation") is a geological formation of Toarcian (Lower Jurassic ) age in the Béni-Mellal , Imilchil , Tinerhir , Tinejdad and Errachidia areas of the High Atlas (reaching areas near Rich in the Middle Atlas[ 1] ) of Morocco .[ 2] [ 3]
Description
Profile at Ouguerd Zegzaoune with the Tagoudite and Tafraout Fms
The Tagoudite Formation marks a major shift in Liassic sedimentation, replacing the carbonate turbidites of the Ouchbis Formation with mostly siliciclastic layers. These layers alternate between gray and green sandstone, sandy marls, and siltstones, forming sequences up to 20 meters thick.[ 4] They show a decrease in grain size and an increase in marl content from bottom to top, with features like ripple marks and laminations. Microscopically, the turbidites are mainly fine silt, with varying amounts of quartz, feldspar, and carbonate detritus, and occasional pyrite. This formation suggests an open marine environment with sediment interruptions and materials coming from distant areas. It is widespread in the Central High Atlas, with thicknesses reaching up to 320 meters, and varies across different regions like Tounfite and Beni Mellal. In the Central Middle Atlas, sedimentation was interrupted by emersion before the formation's deposition.[ 4] The deposits of the Tagoudite Formation are mostly restricted to the central High Atlas, with a thickness of approx. 200 m in the northwest vs at 30–70 m in the southeast, but retaining around 200 m at center areas like Foum Tillicht.[ 5] More at the E it starts to disappear like at the Cirque de Jaafar , SW of Midelt or more at the E at Bou Redine Gorges, were the Agoudim 1 Formation directly overlies the Pliensbachian.[ 6]
Biota
Phytoplankton marks oscillations of negative carbon isotope excursions at T-OAE and Pliensbachian-Toarcian (Pl-To) transition, dominated by open marine haptophytan or incertade sedis coccoliths like Biscutum, Carinolithus (including the index C. superbus , marker of the Polymorphum biozone), Calcivascularis , Calyculus, Lotharingius, Mitrolithus, Parhabdolithus or Schizosphaerella, measured in the Tagoudite Fm in areas like Amellago or Talghemt.[ 7] [ 8] [ 9] Dinoflagellates are rare and limited to taxa such as Luehndea, Mancodinium and Mendicodinium.[ 10]
Color key
Notes Uncertain or tentative taxa are in small text ; crossed out taxa are discredited.
Foraminifera
Genus
Species
Location
Material
Notes
Images
Dentalina [ 11]
Tests/shells
A foraminifer of the family Nodosariinae.
Citharina [ 12]
Tests/shells
A foraminifer of the family Vaginulininae.
Everticyclammina [ 11] [ 13]
Aguerd N´Igli
Aguerd N´Wahmane
Col de Ghnim
Ouguerd Zegzaoune
Tizi n-M´Barek
Tests/shells
A foraminifer of the Everticyclamminidae family.
Ichtyolaria [ 11] [ 14]
Tests/shells
A foraminifer of the family Ichthyolariinae.
Lenticulina [ 15] [ 14] [ 16]
L. matutina
L. gottingensis
L. acutiangulata
L. münsteri
L. toarcense
L. chichery
L. sp.
Anergui
Bou-Oumardoul
Taquat N'Agrd
Talghemt
Tests/shells
A foraminifer of the family Lenticulininae.
Lingulina [ 15]
L. brizaeformis
L. pupa
L. dentaliformis
L. tenera
Bou-Oumardoul
Taquat N'Agrd
Tests/shells
A foraminifer of the family Lenticulininae.
Marginulina [ 15]
Tests/shells
A foraminifer of the family Marginulininae.
Ophtalmidium[ 13] [ 15] [ 17] [ 16]
Aguerd N´Igli
Anergui
Bou-Oumardoul
Ilourhmane
Jebel Toksine
Ouguerd Zegzaoune
Taquat N'Agrd
Timghissine
Tests/shells
A foraminifer of the family Ophthalmidiidae.
Orbitopsella [ 18]
Tests/shells
A foraminifer of the family Orbitopsellinae.
Pseudocyclammina [ 11] [ 13]
Aguerd N´Igli
Bou-Oumardoul
Tests/shells
A foraminifer of the family Hauraniidae.
Pseudonodosaria [ 15] [ 14]
P. tennis
P. multicostata
P. gr.pygmea
P. sp.
Bou-Oumardoul
Ilourhmane
Ouguerd Zegzaoune
Talghemt
Taquat N'Agrd
Tests/shells
A foraminifer of the family Nodosariinae.
Reinholdella [ 11] [ 13] [ 16]
Tests/shells
A foraminifer of the family Ceratobuliminidae.
Verneuilinoides [ 14]
Tests/shells
A foraminifer of the family Verneuilinoidinae
Ichnofossils
Brachiopoda
Genus
Species
Location
Material
Notes
Images
Quadratirhynchia [ 22]
Akka n’Igoulzane
Jebel Bou Ifliyou
Jebel Ich Taskouine
Shells
A brachiopod of the family Tetrarhynchiidae
Homoeorhynchia [ 23] [ 22]
H. meridionalis
H. batalleri
Akka n’Igoulzane
Jebel Bou Ifliyou
Jebel Ich Taskouine
Oued Mijdider
Shells
A brachiopod of the family Rhynchonellinae.
Pseudogibbirhynchia [ 22]
Shells
A brachiopod of the family Pamirorhynchiinae
Soaresirhynchia [ 22]
S. tamazirta
S. bouchardi
Shells
A brachiopod of the family Basiliolinae
Telothyris [ 23] [ 22]
Akka n’Igoulzane
Jebel Bou Ifliyou
Jebel Ich Taskouine
Shells
A brachiopod of the family Lobothyrididae.
Mollusks
Arthropoda
Genus
Species
Location
Material
Notes
Images
Bairdia [ 36]
Shells
A marine ostracod of the family Bairdiinae.
Bairdiacypris [ 36]
Shells
A marine ostracod of the family Bairdiinae.
Kinkelinella [ 36]
Shells
A marine ostracod of the family Protocytheridae . Local dominant Lower Toarcian taxon
Ogmoconcha [ 36]
Shells
A marine ostracod of the family Healdiidae.
Polycope [ 37]
Shells
A marine ostracod of the family Polycopidae .
Echinodermata
Rare Ophiuroid impressions can be observed.[ 38]
Genus
Species
Location
Material
Notes
Images
Apiocrinites [ 39]
Columnar ossicles
A crinoid of the family Apiocrinitidae
Cotylederma[ 39]
Columnar ossicles
A crinoid of the family Cotyledermatidae
Diplechinus[ 39]
Ambulacrum, spines
An echinoid of the family Stomechinidae
Diplocidaris [ 39]
Ambulacrum, spines
An echinoid of the family Diplocidaridae
Dubarechinus[ 39]
Ambulacrum, spines
An echinoid of the family Orthopsidae
Firmacidaris[ 39]
Ambulacrum, spines
An echinoid of the family Cidaridae
Hemicidaris [ 39]
H. (Dorycidaris) termieri
Ambulacrum, spines
An echinoid of the family Hemicidaridae
Pentacrinites [ 39]
Columnar ossicles
A crinoid of the family Pentacrinitidae
Reconstruction of a few specimens
Polypedina[ 39]
Ambulacrum, spines
An echinoid of the family Pedinidae
Actinopteri
Several scales and teeth of fishes are know from several locations, coming from freshwater/lagoonal layers.[ 40]
Genus
Species
Location
Material
Notes
Images
Leptolepis [ 41] [ 42]
Semiarticulated specimens
Marine bony fish of the family Leptolepidae .
L. coryphaenoides specime
Viridiplantae
Phytoclasts , spores, pollen and Tasmanites & Botryococcus algae indicate that the palaeoenvironment of the lower Toarcian Amellago area was likely proximal continental shelf with a high terrestrial input, and notorious influence of brackish water in the depositional environment.[ 43] This interval is numerically dominated by Classopollis , which usually accounts for more than 60.95% of the palynomorphs present.[ 43]
See also
Toarcian turnover
Toarcian formations
Tafraout Formation , SISTER UNIT, Morocco
Azilal Formation , SISTER UNIT, Morocco
Aganane Formation , Morocco
Calcaires du Bou Dahar , Morocco
Marne di Monte Serrone , Italy
Podpeč Limestone , Slovenia
El Pedregal Formation , Spain
Mizur Formation , North Caucasus
Sachrang Formation , Austria
Posidonia Shale , Lagerstätte in Germany
Irlbach Sandstone , Germany
Ciechocinek Formation , Germany and Poland
Krempachy Marl Formation , Poland and Slovakia
Djupadal Formation , Central Skane
Lava Formation , Lithuania
Whitby Mudstone , England
Fernie Formation , Alberta and British Columbia
Whiteaves Formation , British Columbia
Navajo Sandstone , Utah
Los Molles Formation , Argentina
Mawson Formation , Antarctica
Kandreho Formation , Madagascar
Kota Formation , India
Cattamarra Coal Measures , Australia
References
^ Hauptmann, Manfred (1990). "Untersuchungen zur Mikrofazies, Stratigraphie und Paläogeographie jurassischer Karbonat-Gesteine im Atlas-System Zentral-Marokkos" . Selbstverlag Fachbereich Geowissenschaften, FU Berlin . doi :10.23689/fidgeo-6546 .
^ Krencker, F.-N.; Fantasia, A.; El Ouali, M.; Kabiri, L.; Bodin, S. (2022). "The effects of strong sediment-supply variability on the sequence stratigraphic architecture: Insights from early Toarcian carbonate factory collapses" . Marine and Petroleum Geology . 136 105469. Bibcode :2022MarPG.13605469K . doi :10.1016/j.marpetgeo.2021.105469 . ISSN 0264-8172 .
^ Milhi, Abdellah; Ettaki, Mohammed; Chellaï, El Hassane; Hadri, Majid (2002). "Les formations lithostratigraphiques jurassiques du Haut Atlas central (Maroc) : corrélations et reconstitutions paléogéographiques" . Documents des laboratoires de géologie Lyon . 156 (1): 163. Retrieved 25 January 2022 .
^ a b Milhi, Abdellah (1992). Stratigraphie, Fazies und Paläogeographie des Jura am Südrand des zentralen Hohen Atlas (Marokko) . Selbstverlag Fachbereich Geowissenschaften, FU Berlin. OCLC 763029903 .
^ Martinez, Mathieu; Krencker, François-Nicolas; Mattioli, Emanuela; Bodin, Stéphane (2017-01-01). "Orbital chronology of the Pliensbachian – Toarcian transition from the Central High Atlas Basin (Morocco)" . Newsletters on Stratigraphy . 50 (1): 47– 69. doi :10.1127/nos/2016/0311 . ISSN 0078-0421 .
^ Hauptmann, Manfred (1990). "Untersuchungen zur Mikrofazies, Stratigraphie und Paläogeographie jurassischer Karbonat-Gesteine im Atlas-System Zentral-Marokkos" . Selbstverlag Fachbereich Geowissenschaften, FU Berlin . doi :10.23689/fidgeo-6546 .
^ Martinez, Mathieu; Krencker, François-Nicolas; Mattioli, Emanuela; Bodin, Stéphane (2017-01-01). "Orbital chronology of the Pliensbachian – Toarcian transition from the Central High Atlas Basin (Morocco)" . Newsletters on Stratigraphy . 50 (1): 47– 69. doi :10.1127/nos/2016/0311 . ISSN 0078-0421 .
^ Bodin, S.; Mattioli, E.; Frohlich, S.; Marshall, J.D.; Boutib, L.; Lahsini, S.; Redfern, J. (2010). "Toarcian carbon isotope shifts and nutrient changes from the Northern margin of Gondwana (High Atlas, Morocco, Jurassic): palaeoenvironmental implications" (PDF) . Palaeogeogr. Palaeoclimatol. Palaeoecol . 297 (1): 377– 390. Bibcode :2010PPP...297..377B . doi :10.1016/j.palaeo.2010.08.018 . S2CID 128495419 .
^ Boulila, Slah; Galbrun, Bruno; Sadki, Driss; Gardin, Silvia; Bartolini, Annachiara (2019). "Constraints on the duration of the early Toarcian T-OAE and evidence for carbon-reservoir change from the High Atlas (Morocco)" . Global and Planetary Change . 175 : 113– 128. doi :10.1016/j.gloplacha.2019.02.005 . ISSN 0921-8181 .
^ Khaffou, H.; Hssaida, T.; Maatouf, W.; Essafraoui, B.; El Ouali, M.; Essamoud, R.; Louaya, A.; Rachid, J.; Chakir, S.; Jaydawi, S.; Chafai, K. (2023). "Le Toarcien (sommet de la Zone à Polymorphum–Zone à Bonarelli) d'Amellagou (Haut Atlas Central, Maroc) : Palynostratigraphie et Paléoenvironnement" (PDF) . Bulletin de l'Institut Scientifique, Rabat, Section Sciences de la Terre . 45 (6): 111– 130.
^ a b c d e Ettaki, Mohammed; Chellaï, El Hassane (2005-07-01). "Le Toarcien inférieur du Haut Atlas de Todrha–Dadès (Maroc) : sédimentologie et lithostratigraphie" . Comptes Rendus Geoscience . 337 (9): 814– 823. Bibcode :2005CRGeo.337..814E . doi :10.1016/j.crte.2005.04.007 . ISSN 1631-0713 .
^ Souhel, A. (1996). "Le Mésozoïque dans Haut Atlas de Beni-Mellal (Maroc). Stratigraphie, sédimentologie et évolution géodynamique" (PDF) . Strata: Série 2, Mémoires . 27 (6): 1– 227. Retrieved 12 May 2022 .
^ a b c d Bouchouata, Abdelaziz (1994-01-01). La ride de Talmest-Tazoult (haut Atlas central, Maroc) : Lithostratigraphie, biostratigraphie et relations tectonique-sédimentation au cours du Jurassique (These de doctorat thesis). Toulouse 3.
^ a b c d El Kamar, A.; Boutakiout, M.; Elmi, S.; Sadki, D.; Ruget, C. (1998). "Foraminifères et ostracodes du Lias supérieur et du Bajocien de la Ride de Talghemt (Haut-Atlas central, Maroc)" (PDF) . Bulletin de l'Institut Scientifique . 21 (1): 31– 41.
^ a b c d e Souhel, A. (1996). "Le Mésozoïque dans Haut Atlas de Beni-Mellal (Maroc). Stratigraphie, sédimentologie et évolution géodynamique" (PDF) . Strata: Série 2, Mémoires . 27 (6): 1– 227. Retrieved 12 May 2022 .
^ a b c Fadile, A. (2003). "Carte géologique du Maroc au 1/100 000, feuille d'Imilchil" . Notes et Mémoires du Service géologique du Maroc . 397 .
^ Fonville, Tanner; Martindale, Rowan C.; N. Stone, Travis; Septfontaine, Michel; Bodin, Stéphane; Krencker, François-Nicolas; Kabiri, Lahcen (2024). "Early Jurassic Benthic Foraminiferal Ecology From The Central High Atlas Mountains, Morocco" . PALAIOS . 39 (8): 277– 299. Bibcode :2024Palai..39..277F . doi :10.2110/palo.2023.026 .
^ Löwner, Ralf (2009). "Recherches sedimentologiques et structurales à l'articulation entre Haut et Moyen Atlas et la Haute Moulouya, Maroc". Publications of the Universität Berlin . 356 (2): 2– 212. doi :10.14279/DEPOSITONCE-2264 . S2CID 132486463 .
^ a b c d Krencker, F. N.; Fantasia, A.; Danisch, J.; Martindale, R.; Kabiri, L.; El Ouali, M.; Bodin, S. (2020). "Two-phased Collapse of the Shallow-water Carbonate Factory during the Late Pliensbachian–Toarcian Driven by Changing Climate and Enhanced Continental Weathering in the Northwestern Gondwana Margin". Earth-Science Reviews . 208 (1): 103– 254. Bibcode :2020ESRv..20803254K . doi :10.1016/j.earscirev.2020.103254 . S2CID 225669068 .
^ a b c d e f Rodríguez-Tovar, F. J. (2021). "Ichnology of the Toarcian Oceanic Anoxic Event: An understimated tool to assess palaeoenvironmental interpretations". Earth-Science Reviews . 216 (1) 103579: 103– 119. Bibcode :2021ESRv..21603579R . doi :10.1016/j.earscirev.2021.103579 . S2CID 233849558 .
^ Krencker, F. N.; Bodin, S.; Hoffmann, R.; Suan, G.; Mattioli, E.; Kabiri, L.; Immenhauser, A. (2014). "The middle Toarcian cold snap: trigger of mass extinction and carbonate factory demise" . Global and Planetary Change . 117 (1): 64– 78. Bibcode :2014GPC...117...64K . doi :10.1016/j.gloplacha.2014.03.008 . Retrieved 25 January 2022 .
^ a b c d e Alméras, Y.; Fauré, P.; Cougnon, M. (2017). "Brachiopodes toarciens du Haut-Atlas central (Maroc). Implications biostratigraphiques et paléobiogéographiques" . Bulletin de la Société d'histoire naturelle de Toulouse . 153 (5): 47– 66.
^ a b Ettaki, M.; Ibouh, H.; Chellaï, E. H. (2007). "Événements tectono-sédimentaires au Lias-Dogger de la frange méridionale du Haut-Atlas central, Maroc" . Estudios Geológicos . 63 (2): 103– 125. Retrieved 2 February 2022 .
^ a b c d e f g h Dubar, G.; Mouterde, R. (1978). "Les formations à ammonites du Lias Moyen dans Ie Haut Atlas du Midelt et du Tadla" (PDF) . Notes & M. Servo Geo/. Maroc . 274 (4): 77.
^ a b c d e f g h i j Benzaggagh, Mohamed; Khaffou, Hanane; Salamon, Mariusz A.; Hssaida, Touria; Ouali, Mohamed El; Essafraoui, Badre (2022). "ammonites du Toarcien du Haut Atlas central (Maroc)" . Annales de Paléontologie . 108 (2): 102540. Bibcode :2022AnPal.10802540B . doi :10.1016/j.annpal.2022.102540 . ISSN 0753-3969 .
^ a b Dubar, G. (1948). "Etudes paléontologiques sur le lias du Maroc: La faune domérienne du Jebel Bou-Dahar, près de Béni-Tajjite: Bivalvia" (PDF) . Notes et mémoires du Service géologique du Maroc . 68 (2): 147– 2011.
^ a b Milhi, Abdellah (1992). Stratigraphie, Fazies und Paläogeographie des Jura am Südrand des zentralen Hohen Atlas (Marokko) . Selbstverlag Fachbereich Geowissenschaften, FU Berlin. OCLC 763029903 .
^ a b Souhel, A. (1996). "Le Mésozoïque dans Haut Atlas de Beni-Mellal (Maroc). Stratigraphie, sédimentologie et évolution géodynamique" (PDF) . Strata: Série 2, Mémoires . 27 (6): 1– 227. Retrieved 12 May 2022 .
^ a b Bodin, S.; Krencker, F. N.; Kothe, T.; Hoffmann, R.; Mattioli, E.; Heimhofer, U.; Kabiri, L. (2016). "Perturbation of the carbon cycle during the late Pliensbachian–early Toarcian: New insight from high-resolution carbon isotope records in Morocco". Journal of African Earth Sciences . 116 (2): 89– 104. Bibcode :2016JAfES.116...89B . doi :10.1016/j.jafrearsci.2015.12.018 .
^ Wilmsen, M.; F., Neuweiler (2008). "Biosedimentology of the Early Jurassic post-extinction carbonate depositional system, central High Atlas rift basin, Morocco" . Sedimentology . 54 (4): 773– 807. Bibcode :2008Sedim..55..773W . doi :10.1111/j.1365-3091.2007.00921.x . S2CID 128536733 . Retrieved 3 January 2022 .
^ Martinez, Mathieu; Krencker, François-Nicolas; Mattioli, Emanuela; Bodin, Stéphane (2017-01-01). "Orbital chronology of the Pliensbachian – Toarcian transition from the Central High Atlas Basin (Morocco)" . Newsletters on Stratigraphy . 50 (1): 47– 69. doi :10.1127/nos/2016/0311 . ISSN 0078-0421 .
^ a b c Boulila, Slah; Galbrun, Bruno; Sadki, Driss; Gardin, Silvia; Bartolini, Annachiara (2019). "Constraints on the duration of the early Toarcian T-OAE and evidence for carbon-reservoir change from the High Atlas (Morocco)" . Global and Planetary Change . 175 : 113– 128. doi :10.1016/j.gloplacha.2019.02.005 . ISSN 0921-8181 .
^ Brame, H. M. R.; Martindale, R. C.; Ettinger, N. P.; Debeljak, I.; Vasseur, R.; Lathuilière, B.; Bodin, S. (2019). "Stratigraphic distribution and paleoecological significance of Early Jurassic (Pliensbachian-Toarcian) lithiotid-coral reefal deposits from the Central High Atlas of Morocco" . Palaeogeography, Palaeoclimatology, Palaeoecology . 514 (2): 813– 837. Bibcode :2019PPP...514..813B . doi :10.1016/j.palaeo.2018.09.001 .
^ a b Dubar, G. (1948). "Etudes paléontologiques sur le lias du Maroc: La faune domérienne du Jebel Bou-Dahar, près de Béni-Tajjite: Gastropoda" (PDF) . Notes et mémoires du Service géologique du Maroc . 68 (2): 40– 144.
^ a b Pierre, A.; Durlet, C.; Razin, P.; Chellai, E. H. (2010). "Spatial and temporal distribution of ooids along a Jurassic carbonate ramp: Amellago outcrop transect, High-Atlas, Morocco" . Geological Society, London, Special Publications . 329 (1): 65– 88. Bibcode :2010GSLSP.329...65P . doi :10.1144/sp329.4 . ISSN 0305-8719 .
^ a b c d El Kamar, A.; Boutakiout, M.; Elmi, S.; Sadki, D.; Ruget, C. (1998). "Foraminifères et ostracodes du Lias supérieur et du Bajocien de la Ride de Talghemt (Haut-Atlas central, Maroc)" (PDF) . Bulletin de l'Institut Scientifique . 21 (1): 31– 41.
^ Ettaki, Mohammed; Chellaï, El Hassane (2005-07-01). "Le Toarcien inférieur du Haut Atlas de Todrha–Dadès (Maroc) : sédimentologie et lithostratigraphie" . Comptes Rendus Geoscience . 337 (9): 814– 823. Bibcode :2005CRGeo.337..814E . doi :10.1016/j.crte.2005.04.007 . ISSN 1631-0713 .
^ Krencker, F. N.; Fantasia, A.; Danisch, J.; Martindale, R.; Kabiri, L.; El Ouali, M.; Bodin, S. (2020). "Two-phased Collapse of the Shallow-water Carbonate Factory during the Late Pliensbachian–Toarcian Driven by Changing Climate and Enhanced Continental Weathering in the Northwestern Gondwana Margin". Earth-Science Reviews . 208 (1): 103– 254. Bibcode :2020ESRv..20803254K . doi :10.1016/j.earscirev.2020.103254 . S2CID 225669068 .
^ a b c d e f g h i Dubar, G.; Mouterde, R. (1978). "Les formations à ammonites du Lias Moyen dans Ie Haut Atlas du Midelt et du Tadla" (PDF) . Notes & M. Servo Geo/. Maroc . 274 (4): 77.
^ Jenny, J. (1988). "Carte géologique du Maroc au 1/100 000: feuille Azilal (Haut Atlas central). Mémoire explicatif" . Notes et Mémoires du Service géologique . 378 (1): 1– 122. Retrieved 25 January 2022 .
^ Milhi, Abdellah (1992). Stratigraphie, Fazies und Paläogeographie des Jura am Südrand des zentralen Hohen Atlas (Marokko) . Selbstverlag Fachbereich Geowissenschaften, FU Berlin. OCLC 763029903 .
^ Ettaki, Mohammed; Chellaï, El Hassane (2005-07-01). "Le Toarcien inférieur du Haut Atlas de Todrha–Dadès (Maroc) : sédimentologie et lithostratigraphie" . Comptes Rendus Geoscience . 337 (9): 814– 823. Bibcode :2005CRGeo.337..814E . doi :10.1016/j.crte.2005.04.007 . ISSN 1631-0713 .
^ a b Khaffou, H.; Hssaida, T.; Maatouf, W.; Essafraoui, B.; El Ouali, M.; Essamoud, R.; Louaya, A.; Rachid, J.; Chakir, S.; Jaydawi, S.; Chafai, K. (2023). "Le Toarcien (sommet de la Zone à Polymorphum–Zone à Bonarelli) d'Amellagou (Haut Atlas Central, Maroc) : Palynostratigraphie et Paléoenvironnement" (PDF) . Bulletin de l'Institut Scientifique, Rabat, Section Sciences de la Terre . 45 (6): 111– 130.
^ a b c d e f g Khaffou, H.; Hssaida, T.; Maatouf, W.; Essafraoui, B.; El Ouali, M.; Essamoud, R.; Louaya, A.; Rachid, J.; Chakir, S.; Jaydawi, S.; Chafai, K. (2023). "Le Toarcien (sommet de la Zone à Polymorphum–Zone à Bonarelli) d'Amellagou (Haut Atlas Central, Maroc) : Palynostratigraphie et Paléoenvironnement" (PDF) . Bulletin de l'Institut Scientifique, Rabat, Section Sciences de la Terre . 45 (6): 111– 130.