The Bemaraha Formation is a
Middle Jurassic
The Middle Jurassic is the second epoch of the Jurassic Period. It lasted from about 174.1 to 163.5 million years ago. Fossils of land-dwelling animals, such as dinosaurs, from the Middle Jurassic are relatively rare, but geological formations co ...
(early
Bajocian to early
Bathonian)
geological formation of the
Morondava Basin of
Madagascar. The
lime mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...
s,
grainstones and
limestones of the formation were deposited in
lagoonal and
reefal
environments
Environment most often refers to:
__NOTOC__
* Natural environment, all living and non-living things occurring naturally
* Biophysical environment, the physical and biological factors along with their chemical interactions that affect an organism or ...
. Fossils of groups of invertebrates and
theropod and
sauropod
Sauropoda (), whose members are known as sauropods (; from '' sauro-'' + '' -pod'', 'lizard-footed'), is a clade of saurischian ('lizard-hipped') dinosaurs. Sauropods had very long necks, long tails, small heads (relative to the rest of their bo ...
tracks have been found in the formation.
Tsiandro tracksite
at Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database
The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals ...
.org The Sahalaly River tracksite yielded a single trackway belonging to a quadrupedal dinosaur, possibly a sauropod.[Wagensommer et al., 2010, p.127] Sauropod tracks are rare, making up as little as 1 percent of the present sample. The best-preserved tracks are assigned to the ichnogenus '' Kayentapus''.[Wagensommer et al., 2012, p.124]
Description
The limestones of the Bemaraha Formation have been interpreted as a coastal barrier/lagoon complex of Middle Jurassic age (Bajocian, about 170 Ma). At that time, Madagascar had already separated from Africa, but was still attached to India and Antarctica. Since Antarctica was connected to southern Africa, a land bridge really existed between Madagascar and all major southern hemisphere landmasses. Faunal exchanges were possible and endemism was probably very low. Madagascar was to become an island only some 80-90 million years later, during the Late Cretaceous. During Bajocian times, a narrow seaway stretched between eastern Africa and western Madagascar, much in the same position as today's Mozambique Channel. Along the shores of western Madagascar, coral reefs separated wide lagoons from the open sea. The remnants of this reef/lagoon complex is what today, after the coastline shifted several tens of kilometers westward, is seen in the limestones of the Bemaraha Formation.[
The Bemaraha limestones stretches over an area of roughly ,][Wagensommer et al., 2012, p.111] and are best exposed in the area between the towns of Bekopaka and Antsalova, in the northern half of the Morondava Basin. The outcropping limestones can roughly be divided into a western and an eastern belt with different facies
In geology, a facies ( , ; same pronunciation and spelling in the plural) is a body of rock with specified characteristics, which can be any observable attribute of rocks (such as their overall appearance, composition, or condition of formatio ...
.[
In the western belt, the formation mainly consists of massive limestones with metre-scale bedding or no recognizable bedding at all. ]Oolite
Oolite or oölite (''egg stone'') is a sedimentary rock formed from ooids, spherical grains composed of concentric layers. The name derives from the Ancient Greek word for egg (ᾠόν). Strictly, oolites consist of ooids of diameter 0.25–2 ...
s and fossils of reefal organisms (mainly corals) are common in places. This region is affected by the spectacular karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant ro ...
features known as " tsingy" and for this reason most of the area is part of the Tsingy de Bemaraha National Park, included in the UNESCO World Heritage Sites list. The facies in the eastern belt is made up mainly of fine-grained and well-bedded limestones with the average thickness of the individual beds being a few tens of centimeters. Beds are often laminated and invertebrate fossils (gastropod
The gastropods (), commonly known as snails and slugs, belong to a large taxonomic class of invertebrates within the phylum Mollusca called Gastropoda ().
This class comprises snails and slugs from saltwater, from freshwater, and from land. T ...
s, bivalve
Bivalvia (), in previous centuries referred to as the Lamellibranchiata and Pelecypoda, is a class of marine and freshwater molluscs that have laterally compressed bodies enclosed by a shell consisting of two hinged parts. As a group, bival ...
s, brachiopods, echinoids and isolated coral fragments) are common in some beds, while others are devoid of fossils.[D'Orazi Porchetti et al., 2010, p.8]
In the south-western Majunga Basin, interbedded limestones and mudstones (shales and marls) above the Aalenian Sandstone were attributed to a Bajocian carbonate platform formed by the Bemaraha Formation. The carbonate platform at the Manambolo ''For the river with the same name, see Manambolo (disambiguation)''
Manambolo is a town and commune ( mg, kaominina) in Madagascar. It belongs to the district of Maroantsetra, which is a part of Analanjirofo Region. The population of the commune ...
and Tsiribihina River gorges, which cut through the Bemaraha plateau, are likewise assigned to the Early Bajocian. At the eastern margin of the Bemaraha Plateau, the carbonate succession directly rests on Isalo sandstones. Farther south at Besabora (along National Road RN35), limestones with the foraminifera '' Mesoendothyra croatica'' and '' Protopeneroplis striata'' support a Middle Jurassic (Bajocian to Early Bathonian) age.[Geiger & Schweigert, 2005, p.5]
See also
* List of stratigraphic units with dinosaur tracks
** List of stratigraphic units with theropod tracks
** List of stratigraphic units with sauropodomorph tracks
* List of fossiliferous stratigraphic units in Madagascar
Several fossiliferous stratigraphic units in Madagascar have provided fossils, most notably the Maastrichtian Maevarano Formation and the Jurassic Isalo III Formation. The oldest fossil-bearing formations date to ages before the break-up o ...
* Geology of Madagascar
* Isalo III Formation
* Kandreho Formation
* Etjo Sandstone
References
Bibliography
*
*
*
*
* {{cite LSA , last=Wagensommer , first=A. , last2=Latiano , first2=M. , last3=Nicosia , first3=U. , year=2010 , title=First report of dinosaur footprints from Madagascar: two tracksites from the Middle Jurassic Bemaraha Formation , url=https://www.researchgate.net/publication/233239183_First_Report_of_Dinosaur_Footprints_from_Madagascar_Two_Tracksites_from_the_Middle_Jurassic_Bemaraha_Formation , journal=Ichnos Trace fossils are classified in various ways for different purposes. Traces can be classified taxonomically (by morphology), ethologically (by behavior), and toponomically, that is, according to their relationship to the surrounding sedimentary l ...
, volume=17 , pages=127–136 , accessdate=2018-08-30
Geologic formations of Madagascar
Jurassic System of Africa
Middle Jurassic Africa
Jurassic Madagascar
Bajocian Stage
Bathonian Stage
Mudstone formations
Limestone formations
Lagoonal deposits
Reef deposits
Ichnofossiliferous formations
Paleontology in Madagascar
Formations