Geological formation in Morocco
Agoudim Formation Agoudim village
Type Geological Formation Underlies
Overlies
Thickness 2,000 m (6,600 ft) (up to 5,000 m (16,000 ft) reported) Primary Marl , Marly Limestone , Bioclastic limestoneLocation Er-Rich Coordinates 32°15′N 4°30′W / 32.25°N 4.50°W / 32.25; -4.50 Approximate paleocoordinates 27°00′N 3°00′W / 27.0°N 3.0°W / 27.0; -3.0 Region High Atlas and Middle Atlas Country Morocco Named for Agoudim Named by M. Studer Year defined 1980 Region Er-Rich, Midelt Province Thickness at type section ~4,500–5,000 m (14,800–16,400 ft) Agoudim Formation (Morocco)
The Agoudim Formation (also known as the "Marnes et Marno-Calcaires d'Agoudim") is a geological formation of late Toarcian to Bajocian (Lower –Middle Jurassic [ 1] ) age in the central High Atlas and Middle Atlas (particularly around Rich and extending to areas like Midelt , Boulemane , and Beni Mellal ) of Morocco .[ 2] [ 3] The formation is also known as the "Formation Marneuse d’Amane-Ilila ", "Marnes de Boulemane ", "Marnes de Taffert " and "Calcaires à Cancellophycus ".[ 2] [ 4]
Location of the High Atlas basin and Geological overview of the main sectors
The Agoudim Formation is a substantial geological unit primarily composed of marls and marly limestones, representing a continuation from the underlying Tagoudite or Jbel Ouchbis formations and marking a significant shift toward more clay-rich (argillaceous) sedimentation.[ 2] [ 5] This shift is periodically interrupted by layers of bioclastic material (deposits rich in shell fragments and other organic debris) that increase in both frequency and thickness moving upward through the formation. It is stratigraphically divided into two main members: a lower marly member dominated by gray-blue marls with occasional nodular bioclastic limestone beds, and an upper member characterized by more calcareous and bioclastic rocks with greater lithological variability.[ 6] The boundary between these members is often marked by a distinctive layer of organogenic turbidites, notably the "Calcaires à Cancellophycus", which forms a prominent brown cuesta and serves as an important marker horizon for geological mapping.[ 5] [ 7]
The lower member consists of monotonous, micritic marls that reflect relatively quiet hemipelagic depositional conditions, where fine clay and carbonate mud settled along with benthic material.[ 2] This distal sedimentation was influenced by intermittent turbiditic currents transporting detrital quartz and glauconite, indicating periodic sediment input from nearby land areas and submarine slopes. In contrast, the upper member shows increasingly energetic conditions with cycles of sedimentation starting with lumachellic limestones (shell-rich limestones with oblique lamination) and ending in thick bioclastic marls.[ 5] [ 6] This member records frequent synsedimentary slumps and spectacular deformation structures like ball-and-pillow folds (phacoids), which are indicative of tectonic instability and sediment loading on unstable slopes. The evolution upward culminates with a thick limestone cap dominated by oolitic limestones and bioherms (reef-like carbonate buildups that further highlight the transition to shallower marine conditions).[ 6] [ 7]
The Agoudim Formation records multiple Paleoenvironments in a Shallowing basin, from Cold Seep deposits to shallower Reefs
The Agoudim Formation records a progressive transition from deep to shallow marine settings under the influence of rifting , subsidence, and environmental perturbations.[ 8] The lower marly members were deposited in hemipelagic conditions below storm wave base, with pelagic sedimentation, fine siliciclastic influx from nearby uplifts, and reworked carbonate from Liassic platforms.[ 9] [ 10] Fossils such as ammonites, radiolarians , foraminifera , small bivalves, and echinoderm debris confirm a low-energy offshore environment. Rapid subsidence and sea-level rise during the Early Bajocian led to a drowning phase of the neritic carbonate factory, favoring marl sedimentation locally enriched in organic matter.[ 11] Within these successions, several intervals of authigenic carbonates developed, notably yellow micritic nodules, tubular and chimney-like concretions, and conical chemoherms, interpreted as the record of hydrocarbon Cold seep . Petrographic, isotopic, and sedimentological evidence indicates that the second and third authigenic horizons formed at active seep sites, with feeder-pipes, carbonate crusts, microbialites, and bioclast-rich infills, while the yellow nodules of the lower interval likely reflect organic matter remineralization without direct seepage.[ 12] Strongly depleted Δ13C values (down to −19‰) point to fluids rich in dissolved inorganic carbon generated by organic matter degradation, likely through bacterial sulfate reduction and anaerobic oxidation of hydrocarbons, rather than pure methane seepage. These processes created localized hardgrounds, serpulidae and oyster colonization, and chemoherm buildups on the seafloor.[ 12] [ 13] As sedimentation continued, carbonate production recovered, and three reefal complexes developed, ranging from microbial-coral patch reefs to larger coral–sponge–algal bioherms, accompanied by ooid–peloid shoals and brachiopod-rich limestones.[ 14] [ 15] [ 16] These buildups evolved from small mounds to coalescing reefs, shaped by constructive growth, storm reworking, bioerosion, and micritization.[ 14] [ 15] [ 16] The upper part of the formation is dominated by shallow platform deposits with abundant brachiopods, gastropods, corals, and reefal frameworks.[ 14] [ 16] [ 17] [ 18] Some areas, like the Agoudim valley record excepcionally preserved platform sections, showing it´s inner ramp had high-energy ooid–peloid shoals, microbial mounds, and small patch reefs and a proximal middle ramp with mixed coral–sponge–bryozoan–brachiopod assemblages in lower energy waters.[ 19] The distal ramp consisted of marl–limestone alternations with storm beds and oyster–coral–sponge buildups. Local syndepositional highs and terrigenous input created semi-restricted zones with fluctuating oxygenation and nutrients.[ 19]
Taxa
Species
Locality
Member
Material
Notes
Images
Actinostreon [ 12] [ 15]
sp.
Assameur n’Ait Fergane, Boukendil
IV
Shells
Gryphaeidae
Alocolytoceras [ 1]
ophioneum
Gheris Valley
I
Shells
Lytoceratidae
Ambersites [ 1]
sp.
Rich region
II–III
Shells
Hammatoceratidae
Ancolioceras [ 27]
opalinoides
n’Zala (Jbel Aouja)
I–II
Shells
Graphoceratidae
Asthenoceras [ 1]
sp.
Rich (Concavum–Discites zones)
II–III
Shells
Sonniniidae
Belemnopsis [ 28]
baculiformis
Iwansitn
III
Rostra
Belemnopseidae
pougatchevskae
Iwansitn
III
Rostra
Belemnopseidae
Bositra [ 1]
buchi
Amellago; Rich
I–III
Shells
Posidoniidae
Botula [ 15]
sp.
Boukendil area
IV
Shells, borings
Mytilidae
Bradfordia [ 1]
costata
Rich region
III
Shells
Oppeliidae
sp.
Rich region
III
Shells
Oppeliidae
Calabribelus [ 28]
combemoreli
Rich (Jbel Bou Kandil), Iwansitn (Middle Atlas)
II–III
Rostra
Holcobelidae
tetramerus
Rich, Iwansitn
II–III
Rostra
Holcobelidae
Calliphylloceras [ 29]
C. nilssoni
Amellago
I
Shells
Phylloceratidae
Catulloceras [ 1]
sp.
n’Zala (Jbel Aouja)
I
Shells
Graphoceratidae
Chlamys [ 1]
sp.
Rich, Amellago
II–III
Shells
Pectinidae
Conobelemnopsis [ 28]
sp. A
Rich, Iwansitn
III
Rostra
Belemnopseidae
Cotteswoldia [ 27]
sp.
n’Zala (Jbel Aouja)
I
Shells
Graphoceratidae
Ctenostreon [ 1]
sp.
Rich, Amellago
II–III
Shells
Limidae
Cypholioceras [ 27]
sp.
n’Zala (Jbel Aouja)
II
Shells
Graphoceratidae
Dactylioceras [ 20] [ 29]
(Eodactylites) mirabile
Amellago
I
Shells
Dactylioceratidae
Dactylioceras reconstruction
(Eodactylites) pseudocommune
Amellago
I
Shells
Dactylioceratidae
(Eodactylites) simplex
Talghemt Ridge
I
Shells
Dactylioceratidae
(Orthodactylites) aff. crosbeyi
Amellago
I
Shells
Dactylioceratidae
(Orthodactylites) cf. semiannulatum
Amellago
I
Shells
Dactylioceratidae
?Dicoelites [ 28]
sp. A
Iwansitn
III
Rostra
Dicoelitidae
Docidoceras [ 1]
wysogorskii
Rich
III
Shells
Otoitidae
Eleganticeras [ 29]
exaratum
Amellago
I
Shells
Dactylioceratidae
sp.
Amellago
I
Shells
Dactylioceratidae
Emileia [ 30]
(Emileia ) polymera
Boukendil, Assameur
IV
Shells
Otoitidae
Eudmetoceras [ 1]
flexuosum
Rich
II–III
Shells
Hammatoceratidae
masticonense
Rich
III
Shells
Hammatoceratidae
eudmetum
Rich
III
Shells
Hammatoceratidae
sp.
Rich
II–III
Shells
Hammatoceratidae
Euaptetoceras [ 1]
amaltheiforme
Rich
III
Shells
Hammatoceratidae
amplectens
Rich
III
Shells
Hammatoceratidae
sp.
Rich
II–III
Shells
Hammatoceratidae
Fontannesia [ 1]
aurita
Rich
II
Shells
Sonniniidae
montillanensis
Rich
II
Shells
Sonniniidae
sp.
Rich
II–III
Shells
Sonniniidae
Grammatodon [ 1]
sp.
Rich
II–III
Shells
Parallelodontidae
Hammatoceras [ 29]
H. aff. insigne
n’Zala (Jbel Aouja)
I
Shells
Hammatoceratidae
Harpoceras [ 29]
falciferum
Amellago
I
Shells
Hildoceratidae
Harpoceras reconstruction
pseudoserpentinum
Amellago
I
Shells
Hildoceratidae
serpentinum
Amellago
I
Shells
Hildoceratidae
subplanatum
Amellago
I
Shells
Hildoceratidae
Hildaites [ 29]
forte
Amellago
I
Shells
Hildoceratidae
levisoni
Amellago
I
Shells
Hildoceratidae
cf. serpentiniformis
Amellago
I
Shells
Hildoceratidae
cf. subserpentinus
Amellago
I
Shells
Hildoceratidae
striatus
Amellago
I
Shells
Hildoceratidae
wrighti
Amellago
I
Shells
Hildoceratidae
Hildoceras [ 20] [ 29]
bifrons
Amellago; Talghemt Ridge
I
Shells
Hildoceratidae
Hildoceras sublevisoni
lusitanicum
Amellago; Talghemt Ridge
I
Shells
Hildoceratidae
semipolitum
Amellago; Talghemt Ridge
I
Shells
Hildoceratidae
sublevisoni
Amellago; Talghemt Ridge
I
Shells
Hildoceratidae
bonarellii
Talghemt Ridge
I–II
Shells
Hildoceratidae
sp.
Amellago
I
Shells
Hildoceratidae
Hyperlioceras [ 1]
walkeri
Rich
III
Shells
Graphoceratidae
incisum
Rich
III
Shells
Graphoceratidae
inclusum
Rich
III
Shells
Graphoceratidae
mundum
Rich
III
Shells
Graphoceratidae
sp.
Rich
III
Shells
Graphoceratidae
Leioceras [ 27]
cf. comptum
n’Zala (Jbel Aouja)
II
Shells
Graphoceratidae
costusum
n’Zala (Jbel Aouja)
II
Shells
Graphoceratidae
Lithophaga [ 16]
sp.
Boukendil area
IV
Shells, borings
Mytilidae
Lithophaga specimen
Ludwigia [ 27]
aff. haugi
n’Zala (Jbel Aouja)
II
Shells
Graphoceratidae
Lytoceras [ 29] [ 31]
siemensi
Amellago; n’Zala
I
Shells
Lytoceratidae
Lytoceras fimbriatum
subfimbriatum
n’Zala
II
Shells
Lytoceratidae
sp.
Amellago; n’Zala
I–II
Shells
Lytoceratidae
Maconiceras [ 29]
soloniacense
Amellago
I
Shells
Hammatoceratidae
Malladaites [ 1]
pertinax
Rich
III
Shells
Hammatoceratidae
Nerinea [ 16]
sp.
Assameur n’Ait Fergane
IV
Shells
Nerineidae
Nicaniella [ 1]
sp.
Rich, Amellago
II–III
Shells
Astartidae
Palaeonucula [ 1]
hammeri
Rich, Amellago
II–III
Shells
Nuculidae
Palaeoneilo [ 1]
sp.
Rich
III
Shells
Malletiidae
Phylloceras [ 29]
sp.
Amellago; n’Zala
I–II
Shells
Phylloceratidae
Phylloceras reconstruction
Pholadomya [ 24]
(Bucardiomya) bucardium
Jebel Assameur; Boukendil; Rich-Gourrama area
IV
Shells
Pholadomyidae
Planammatoceras [ 27]
sp.
n’Zala (Jbel Aouja)
II
Shells
Hammatoceratidae
Pleydellia [ 27]
aalensis
n’Zala (Jbel Aouja)
II
Shells
Graphoceratidae
Polyplectus [ 29]
pluricostatum
Amellago
I
Shells
Hammatoceratidae
sp.
Amellago
I
Shells
Hammatoceratidae
Porpoceras [ 29]
gr. vortex-verticosum
Amellago; Talghemt Ridge
I
Shells
Dactylioceratidae
Praestrigites [ 1]
sp.
Rich
III
Shells
Strigoceratidae
Praeoppelia [ 1]
sp.
Rich
III
Shells
Oppeliidae
Protetragonites [ 31]
sp.
n’Zala
II
Shells
Lytoceratidae
Protoecotraustes [ 1]
sp.
Rich
III
Shells
Haploceratidae
Rastellum [ 16]
sp.
Assameur n’Ait Fergane, Boukendil
IV
Shells
Ostreidae
Rastellum fossil
Saxicava [ 16]
sp.
Boukendil area
IV
Shells, borings
Hiatellidae
Sonninia [ 1]
dominans
Rich
III
Shells
Sonniniidae
modestum
Rich
III
Shells
Sonniniidae
nannomorpha
Rich
III
Shells
Sonniniidae
Tmetoceras [ 27]
T. scissum
n’Zala (Jbel Aouja)
I–II
Shells
Hammatoceratidae
Toxamblyites [ 30]
densicostatus
Boukendil, Assameur
IV
Shells
Haploceratidae
Trigonia [ 1]
sp.
Rich
III
Shells
Trigoniidae
Trilobiticeras [ 1]
platygaster
Rich
III
Shells
Otoitidae
trilobitoides
Rich
III
Shells
Otoitidae
sp.
Rich
III
Shells
Otoitidae
Tylostoma [ 1]
globosum
Rich
III
Shells
Tylostomatidae
Vacekia [ 27]
sp.
n’Zala (Jbel Aouja)
I–II
Shells
Graphoceratidae
Zurcheria [ 1]
sp.
Rich
III
Shells
Hammatoceratidae
Genus
Species
Locality
Member
Material
Notes
Images
Nogrobs [ 30]
moroccensis
Boukendil, Assameur
IV
Quadrangular tubes
Serpulidae
Serpula [ 12] [ 16]
socialis
Assameur n’Ait Fergane, Boukendil; Jebel Bou Kendill (cap bed)
III–IV
Tubes / colonies
Serpulidae
Serpula vermicularis
sp.
Assameur n’Ait Fergane, Boukendil; Jebel Bou Kendill (cap bed)
III–IV
Tubes / colonies
Serpulidae
Terebella [ 16]
lapilloides
Assameur n’Ait Fergane, Boukendil; Jebel Bou Kendill (cap bed)
III–IV
Tubes / colonies
Terebellidae
Terebella
Taxa
Species
Locality
Member
Material
Notes
Images
Strophodus [ 32]
atlasensis
Talsint (eastern High Atlas)
III–IV
Articulated dentition (holotype PIMUZ A/I 5181)
Hybodontidae
Strophodus atlasensis
Toarcian turnover
Toarcian formations
Tafraout Formation , SISTER UNIT, Morocco
Tagoudite 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
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