El Mers Group
{{Short description|Geological group in the Middle Atlas of Morocco}}
{{Infobox rockunit
| name = El Mers Group
| period = Bathonian
| age = Bajocian-Callovian
~{{fossil range|168|161}}
| image = {{Multiple image
| perrow = 2/2/2
| width = 135
| caption_align = center
| image1 = El Mers I Formation Thaghzout river canyon.jpg
| caption1 = El Mers I Formation at Thaghzout river canyon
| image2 = El Mers II Formation El Mers river bed 1.jpg
| caption2 = El Mers II along the El Mers river
| image3 = El Mers II Formation El Mers river bed 2.jpg
| caption3 = El Mers II along the El Mers river
| image4 = Thyreosaurus excavation site.jpg
| caption4 = El Mers III Dinosaur Bearing beds
| border = infobox
}}
| imagesize =
| caption =
| type = Group
| prilithology = Marl, gypsum (only in unit 3)
| otherlithology = Sandstone, limestone
| unitof =
| subunits = El Mers Formations 1–3
| underlies = Unconformity with Barremian or Plio-Pleistocene sediments
| overlies = Ich Timellaline–Bou Akrabene Formation
| thickness = Over {{convert|500|m|ft|abbr=on}}
| area =
| map = {{Location map+ | Morocco
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | Morocco
| lat_deg = 33.5
| lon_deg = -4.3
| mark = Blue pog.svg
| marksize = 12
}}
}}
| map_caption =
| location =
| coordinates = {{coord|33.5|N|4.3|W|display=inline,title}}
| paleocoordinates = {{coord|28.3|N|2.0|W|display=inline}}
| region = Boulemane and Azilal Provinces
| country = Morocco
| extent = Middle Atlas
| namedfor =
| namedby =
| year_ts =
| location_ts =
| coordinates_ts =
| paleocoordinates_ts =
| region_ts =
| country_ts =
| thickness_ts =
}}
The El Mers Group is a geological group in the Middle Atlas of Morocco. It is subdivided into three formations named the El Mers I, II, and III Formations, respectively. It is a marine deposit primarily consisting of marl, with gypsum present in the upper part of unit 3. It is the lateral equivalent of the terrestrial Guettioua Sandstone. Dinosaur remains are among the fossils that have been recovered from the group, most notably those of sauropods and the unusual thyreophorans Adratiklit, Thyreosaurus, and Spicomellus. This formation records a series of coastal to shallow marine settings of Middle Jurassic (with an age of Bajocian-Bathonian for El Mers 1 and a Bathonian-Callovian? for El Mers II-III), based on detailed stratigraphical biomarkers such as ammonites or Foranimifera.{{Cite journal |last=Khaffou |first=Hanane |last2=Hssaida |first2=Touria |last3=Oukassou |first3=Mostafa |last4=Maatouf |first4=Wafaa |last5=Afenzar |first5=Abdelkrim |last6=Zafaty |first6=Omar |last7=Chakir |first7=Sara |last8=Jaydawi |first8=Soukaina |last9=Chafai |first9=Khaoula |last10=Charrière |first10=André |date=2023 |title=Bajocian–Bathonian dinoflagellate cyst assemblages from the Middle Atlas, Morocco: Palynostratigraphic and paleoenvironmental implications |url=https://doi.org/10.1016/j.revpalbo.2023.104862 |journal=Review of Palaeobotany and Palynology |volume=312 |pages=104862 |doi=10.1016/j.revpalbo.2023.104862 |issn=0034-6667}}
Paleoenvironment
File:Staying Still 110 - Coorong.jpg.]]
The El Mers formations are composed primarily of marls with intermittent layers of limestone and sandstone, characterized by abundant organic matter and benthic fauna.{{Cite journal|last1=Oukassou|first1=M.|last2=Boumir|first2=Kh.|last3=Benshili|first3=Kh.|last4=Ouarhache|first4=D.|last5=Lagnaoui|first5=A.|last6=Charrière|first6=A.|date=June 2019|title=The Tichoukt Massif: a Geotouristic Play in the Folded Middle Atlas (Morocco)|journal=Geoheritage|volume=11|issue=2|pages=371–379|doi=10.1007/s12371-018-0287-y|bibcode=2019Geohe..11..371O |s2cid=134800520 |issn=1867-2477}} It is delineated into five distinct members, each exhibiting diverse lithological characteristics. The three members comprise a combination of layers of marls, sandstones, and limestones, marked by various unique fossils and organic materials. Sedimentary discontinuities reveal deltaic sequences that exhibit varying sedimentary structures and lithological compositions, reflecting dynamic depositional environments ranging from subtidal to continental. The facies associations within the El Mers Group are organized into elementary and mesosequences, delineating the transition from prodelta to deltaic plain environments. These sequences capture the evolution of tidal regimes and depositional dynamics.{{Cite journal |last1=Soufiani |first1=N. |last2=Fedan |first2=B. |date=2002 |title=Les dépôts bathoniens du synclinal d'El Mers (Moyen Atlas, Maroc): unités formationnelles, analyse et cadre géodynamique |url=http://www.israbat.ac.ma/wp-content/uploads/2015/03/01-%20Soufiani%20et%20al.%20(01-14).pdf |journal=Bulletin de l'Institut scientifique |volume=24 |issue=6 |pages=1–14}}{{Cite journal |last=Dresnay |first=Renaud du |date=1963-01-01 |title=Donnees stratigraphiques complementaires sur le Jurassique moyen des synclinaux d'El Mers et de Skoura (Moyen-Atlas, Maroc) |url=https://pubs.geoscienceworld.org/sgf/bsgf/article-abstract/S7-V/6/883/518424/Donnees-stratigraphiques-complementaires-sur-le |journal=Bulletin de la Société Géologique de France |volume=S7-V |issue=6 |pages=883–900 |doi=10.2113/gssgfbull.S7-V.6.883 |issn=0037-9409}}
During the Bajocian-Bathonian transition the local faices paint a picture of a dynamic paleoenvironment, where the interplay between land and sea was pronounced. This setting oscillated between a proximal continental shelf, marked by significant terrestrial input, and episodic marine incursions that suggest fluctuating sea levels. The lower parts of the section hint at shallow, sometimes oxygen-deprived, stagnant waters, much like modern lagoon or restricted bays where circulation is limited. Upwards there are signs of marine influence growing stronger, particularly at the base of "Interval C", where a notable sea-level rise seems to have occurred, akin to what we might see on today's outer continental shelves, like those in the North Sea, where marine life diversity peaks, specially Bivalves and Ammonites. However, this marine dominance is not consistent, reverting back to a more coastal, land-influenced environment towards the top, similar to modern deltaic regions where riverine and marine waters mix, such as the Louisiana coast or the Coorong National Park. The environment would have experienced variable salinity, much like estuaries where fresh and marine waters blend, affecting the types of biota that could thrive.
The shifts in facies and microfauna evolution in the area revelated intriguing patterns, from the establishment of initial supratidal environments characterized by charophytic marls and ostracod limestones followed by a resurgence of marine conditions, evident from the reappearance of coastal facies and the diversification of ostracod faunas, indicating a significant transgressive phase during the Upper Bathonian–Lower Callovian period. While in the Central High Atlas marine influences ceased by the Upper Bajocian–Lower Bathonian giving way to continental red layers, in the Middle Atlas marine influences persisted until the Upper Bathonian–Lower Callovian boundary, indicating a diachronic filling of the Atlas gulfs towards the Tethyan domain from west to east.{{Cite journal |last1=Charrière |first1=André |last2=Dépêche |first2=Françoise |last3=Feist |first3=Monique |last4=Grambast-Fessard |first4=Nicole |last5=Jaffrezo |first5=Michel |last6=Peybernès |first6=Bernard |last7=Ramalho |first7=Miguel |date=1994 |title=Microfaunes, microflores et paléoenvironnements successifs dans la formation d'El Mers (Bathonien-?Callovien) du synclinal de Skoura (Moyen-Atlas, Maroc) |url=http://dx.doi.org/10.1016/s0016-6995(94)80002-2 |journal=Geobios |volume=27 |issue=2 |pages=157–174 |doi=10.1016/s0016-6995(94)80002-2 |bibcode=1994Geobi..27..157C |issn=0016-6995}}
Fossils
{{paleobiota-key-compact}}
= Foraminifera =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
style="background:#D1FFCF;" |Bullopora
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Tests/Shells | style="background:#D1FFCF;" |A benthic foraminiferan of the family Polymorphinidae | style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Pfenderella
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Tests/Shells | style="background:#D1FFCF;" |A benthic foraminiferan of the family Pfenderininae | style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Praekurnubia
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Tests/Shells | style="background:#D1FFCF;" |A benthic foraminiferan of the family Pfenderinidae; a genus found in the Tethys between Bajocian and Oxfordian-aged layers | style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Pseudocyclammina
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Tests/Shells | style="background:#D1FFCF;" |A benthic foraminiferan of the family Hauraniidae | style="background:#D1FFCF;" | |
= Dinoflajellates =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
style="background:#D1FFCF;" |Aldorfia
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Cysts | style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae | style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Cribroperidinium
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Ctenidodinium
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate, incertae sedis |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Dichadogonyaulax
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate, incertae sedis |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Korystocysta
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Meiourogonyaulax
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Nannoceratopsis
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Nannoceratopsiaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Pareodinia
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Pareodiniaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Rhynchodiniopsis
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Trichodinium
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Tubotuberella
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Wanaea
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate of the family Gonyaulacaceae |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Willeidinum
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Cysts |style="background:#D1FFCF;" |A Dinoflajellate, incertae sedis |style="background:#D1FFCF;" | |
= Brachiopoda =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
Formosarhynchia
|
|
|Isolated shells |A branchipod of the family Rhynchonellidae |
= Ostracoda =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
Cytherella
|
|
|Valves |A freshwater/brackish ostracod of the family Cytherellidae | |
Fastigatocythere
|
|
|Valves |A freshwater/brackish ostracod of the family Progonocytheridae | |
Kinkelinella
|
|
|Valves |A freshwater ostracod of the family Progonocytheridae | |
Metacypris
|
|
|Valves |A freshwater ostracod of the family Limnocytheridae. Local members of the genus genus would not be confined to limnic environments, but would be euryhaline or brackish, since they disappear when faunal diversity is at its maximum. | |
Procytheridea
|
|
|Valves |A freshwater ostracod of the family Schulerideidae | |
= Xiphosura =
= Mollusca =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
Cadomites
|
|
|Isolated shells |An ammonite of the family Stephanoceratidae and indicator of the Bathonian age |File:31 - Muséum de Toulouse - Cadomites deslongchampsii - Bayeux Calvados France.jpg |
Cercomya
|
|
|Isolated shells |A marine clam of the family Laternulidae | |
Choffatia
|
|
|Isolated shells |An ammonite of the family Perisphinctidae and indicator of the Callovian age | |
Corbula
|
|
|Isolated shells |A marine clam of the family Corbulidae | |
Clydoniceras
|
|
|Isolated shells |An ammonite of the family Clydoniceratidae | |
Eomiodon
|
|
|Isolated Shells |A marine clam of the family Neomiodontidae | |
Isognomon
|
|
|Isolated shells |A marine oyster of the family Malleidae |
Lima
|
|
|Isolated shells |A marine file clam of the family Limidae |
Lopha
|
|
|Isolated shells |A marine oyster of the family Ostreidae |
Modiolus
|
|
|Isolated shells |A marine mussel of the family Mytilidae |
Morphoceras
|
|
|Isolated shells |An ammonite of the family Morphoceratidae and indicator of the Bathonian age | |
Mytilus
|
|
|Isolated shells |A marine mussel of the family Mytilidae |
Nucula
|
|
|Isolated shells |A marine nut clam of the family Nuculanidae |
Oraniceras
|
|
|Isolated shells |An ammonite of the family Parkinsoniidae and indicator of the Bathonian age | |
Orionoides
|
|
|Isolated shells |An ammonite of the family Perisphinctidae | |
Ostrea
|
|
|Isolated shells |A marine oyster of the family Ostreidae |
Paracenoceras
|
|
|Isolated shells |A Nautilidan of the family Paracenoceratidae |
Parkinsonia
|
|
|Isolated shells |An ammonite of the family Parkinsoniidae and indicator of the Bajocian age for the lower portions of the Group |
Protocardia
|
|
|Isolated shells |A marine cockle of the family Cardiidae | |
= Echinoderms =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
Acrosalenia
|
|
|Isolated Individuals |An Echinoidean of the family Acrosaleniidae | |
Hemicidaris
|
|
|Isolated Individuals |An Echinoidean of the family Hemicidaridae |
= Fishes =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
Lepidotes{{Cite journal |last=Beltan |first=Laurence |date=1957-01-01 |title=Etude d'un neurocrane de Lepidotes du Bathonien du Maroc |url=http://dx.doi.org/10.2113/gssgfbull.s6-vii.8-9.1091 |journal=Bulletin de la Société Géologique de France |volume=S6-VII |issue=8–9 |pages=1091–1106 |doi=10.2113/gssgfbull.s6-vii.8-9.1091 |issn=1777-5817}}
|
|
|Cranial material, isolated teeth and scales |A marine/brackish bony fish of the family Lepidotidae |File:Lepidotes sp. - Naturhistorisches Museum, Braunschweig, Germany - DSC05183.JPG |
Scheenstia
|
|
|Partial specimen wirth cranial material |A marine/brackish bony fish of the family Lepidotidae |
= Testudinata =
= Crocodylomorpha =
=Dinosauria=
== Theropoda ==
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
style="background:#FEF6E4;" |Carmelopodus
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |Footprints | style="background:#FEF6E4;" |Theropod tracks of uncertain affinity, suggested to come from Ceratosauria members | style="background:#FEF6E4;" | |
style="background:#FEF6E4;" |Grallator?
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |Footprints | style="background:#FEF6E4;" |Theropod Tracks, referred usually to small-medium sized Genera | style="background:#FEF6E4;" | |
style="background:#FEF6E4;" |Hispanosauropus?
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |Footprints | style="background:#FEF6E4;" |Theropod tracks of uncertain affinity, different from Megalosauripus in the larger metatarsophalangeal region | style="background:#FEF6E4;" | |
style="background:#FEF6E4;" |Megalosauripus{{Cite journal |last1=Hadri |first1=M. |last2=Lorente |first2=F. P. |date=2012 |title=Historia de yacimientos con huellas de dinosaurio, desde su descubrimiento hasta su primer estudio: alrededores de El Mers (Marruecos) |url=https://dialnet.unirioja.es/descarga/articulo/4118092.pdf |journal=Zubia |volume=30 |issue=6 |pages=93–147}}
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |Footprints | style="background:#FEF6E4;" |Traces of theropods; members of the ichnofiber family Eubrontidae, incertae sedis within Theropoda | style="background:#FEF6E4;" | |
Averostra
|
|
|Isolated Teeth |Isolated teeth of unidentified or undescribed/studied theropods. Teeth associated with the Teleosaur "Megalosaurus" mersensis have recently been suggesting to come from indeterminate Averostrans. Other remains need revision.{{Cite web |title=Non-theropods |url=https://theropoddatabase.github.io/Non-theropods.htm#Megalosaurusmersensis |access-date=2024-10-05 |website=theropoddatabase.github.io}}{{Cite web |title=Neotheropoda |url=https://theropoddatabase.github.io/Neotheropoda.htm#Averostra |access-date=2024-11-01 |website=theropoddatabase.github.io}} | |
style="background:#FEF6E4;" |Theropodipedia{{Cite journal |last1=Jenny |first1=Jacques |last2=Le Marrec |first2=Alain |last3=Monbaron |first3=Michel |date=1981 |title=Les empreintes de pas de Dinosauriens dans le Jurassique moyen du Haut Atlas central (Maroc): Nouveaux gisements et precisions stratigraphiques |url=http://dx.doi.org/10.1016/s0016-6995(81)80186-6 |journal=Geobios |volume=14 |issue=3 |pages=427–431 |doi=10.1016/s0016-6995(81)80186-6 |bibcode=1981Geobi..14..427J |issn=0016-6995}}
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |
| style="background:#FEF6E4;" |Footprints | style="background:#FEF6E4;" |Theropod tracks of uncertain affinity, suggested to come from "allosaurs or megalosaurs" | style="background:#FEF6E4;" | |
== Sauropoda ==
== Ornithischia ==
= Dasycladales =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
style="background:#D1FFCF;" |Heteroporella
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Calcareous imprints | style="background:#D1FFCF;" |A dasycladacean algae of the family Dasycladaceae | style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Sarfiatella
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Calcareous imprints | style="background:#D1FFCF;" |A dasycladacean algae, associated in adjacent regions with Aalenian–Bajocian faunas | style="background:#D1FFCF;" | |
= Charophyta =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
style="background:#D1FFCF;" |Porochara
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Oogonia | style="background:#D1FFCF;" |A characean algae of the family Porocharaceae; charophytes are abundant in lower levels, associated with freshwater ostracods | style="background:#D1FFCF;" |File:CharaFragilis.jpg |
= Plantae =
class="wikitable"
!Genus !Species !Stratigraphic position !Material !Notes !Images |
style="background:#D1FFCF;" |Araucariacites
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Pollen |style="background:#D1FFCF;" |Affinities with Araucariaceae inside Coniferae. | rowspan="2" style="background:#D1FFCF;" |File:Araucaria cunninghamii cones.jpg cones]] |
style="background:#D1FFCF;" |Callialasporites
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Pollen |style="background:#D1FFCF;" |Affinities with Araucariaceae inside Coniferae. |
style="background:#D1FFCF;" |Classopollis
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Pollen |style="background:#D1FFCF;" |Affinities with Cheirolepidiaceae inside Coniferae. |style="background:#D1FFCF;" | |
style="background:#D1FFCF;" |Cyathidites
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Spores |style="background:#D1FFCF;" |Affinities with the family Cyatheaceae inside Cyatheales. Arboreal Fern Spores |style="background:#D1FFCF;" |File:Cyathea arborea.JPG, Cyathidites come probably from similar genera]] |
style="background:#D1FFCF;" |Densoisporites
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Spores |style="background:#D1FFCF;" |Affinities with the Selaginellaceae in the Lycopsida. |style="background:#D1FFCF;" |File:Selaginella_erythropus_kz02.jpg. Densoisporites probably come from a similar Plant]] |
style="background:#D1FFCF;" |Lycopodiumsporites
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |Spores |style="background:#D1FFCF;" |Affinities with the family Lycopodiaceae in the Lycopodiopsida. Lycopod spores, related to herbaceous flora common in humid environments. |style="background:#D1FFCF;" |File:Lycopodium_annotinum_161102.jpg. Lycopodiumsporites probably come from a similar plant]] |
style="background:#D1FFCF;" |Protocupressinoxylon{{Cite journal |last1=Philippe |first1=M. |last2=Bamford |first2=M. |last3=McLoughlin |first3=S. |last4=Alves |first4=L.S.R. |last5=Falcon-Lang |first5=H.J. |last6=Gnaedinger |first6=S. |last7=Ottone |first7=E.G. |last8=Pole |first8=M. |last9=Rajanikanth |first9=A. |last10=Shoemaker |first10=R.E. |last11=Torres |first11=T. |last12=Zamuner |first12=A. |date=2004 |title=Biogeographic analysis of Jurassic–Early Cretaceous wood assemblages from Gondwana |url=http://dx.doi.org/10.1016/j.revpalbo.2004.01.005 |journal=Review of Palaeobotany and Palynology |volume=129 |issue=3 |pages=141–173 |doi=10.1016/j.revpalbo.2004.01.005 |bibcode=2004RPaPa.129..141P |issn=0034-6667}}
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |Fossil wood | style="background:#D1FFCF;" |Conifer wood of the family Hirmeriellaceae, considered to be a potential synonym of the genus Brachyoxylon | style="background:#D1FFCF;" |File:Protocupressinoxylon.JPG trunk of the same genus (from an unknown location)]] |
See also
- Tafraout Group (Toarcian–Aalenian)
- Azilal Formation (Toarcian-Aalenian)
- Guettioua Formation (Bathonian–?Callovian)
- Anoual Formation (Bathonian)
- Ksar Metlili Formation (Tithonian–?Berrasian)