Review of the dinosaur record from Iran with the description of new material (original) (raw)
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Rewiew of the dinosaur record from Iran with the description of new material.
The dinosaur record from Iran includes footprints from the Liassic Shemshak Formation of Neizar Valley (Kerman Province, SE Iran), a single footprint from the Shemshak Formation near Zerab (Alborz Mounts, NE Iran), and skeletal remains from the Late Jurassic-earliest Cretaceous Bidou Formation of the Ab Bid Syncline (Kerman Province). Contrary to previous identifications, no footprints from the Neizar Valley belong to ornithopods; they can all be referred to theropod trackmakers. The Zerab footprint, on which the ichnospecies Iranosauripus zerabensis is based, is an undiagnostic theropod footprint and probably was lost. The skeletal remains are represented by bone fragments and a tooth of a mid-sized theropod, which represent the first dinosaur osteological record in this part of the Middle East. The Ab Bid Syncline has a high potential for further future discoveries.
Palaeobiodiversity and Palaeoenvironments, 2021
A late early Maastrichtian dinosaur trampling site is reported from the Farrokhi Formation of the Khur area, Central Iran. The largely indeterminate footprints, some of which may represent undertracks, can be classified as natural moulds (i.e. concave epireliefs) bordered by a raised rim of displaced sediment. They reach diameters of up to 0.5 m and were impressed under very shallow to subaerial conditions in an inter-to supratidal environment. Two generations of traces have been imprinted, initially into a soft, fine-grained carbonate sand and afterwards into a superficially hardened substrate that was still plastic underneath; the change in substrate consistency is supported by a conspicuous cracking pattern around the footprints. As a result, hardly any details of the foot morphology of the trackmakers are recorded. Nevertheless, the occurrence improves our knowledge about dinoturbation and its preservation in different kinds of substrates. Furthermore, it is the youngest record (ca. 70 Ma) of dinosaur locomotion traces from Iran and, in all probability, the entire Middle East.
First Upper Cretaceous dinosaur track assemblage from Jordan (Middle East) – preliminary results
Annales Societatis Geologorum Poloniae
Dinosaur tracks from Jordan (Middle East) have only been briefly reported in geological overview papers and books. We present here the first description and documentation of Jordanian dinosaur tracks based on a new tracksite from the south-central part of the country. The track-bearing strata belong to marginal marine (tidal flat) deposits of the Na'ur Formation (Upper Cretaceous, Cenomanian). This unit largely consists of well-bedded limestones, dolomites and marls that contain abundant marine invertebrate fossils such as bivalves, ammonites and foraminifers. The dinosaur ichnofauna occurs on four different levels and comprises abundant theropod tracks and trackways as well as isolated sauropod and ornithopod tracks. Theropod trackways consist of two different morphotypes. Morphotype 1 is tridactyl (26 cm pes length) and with a broad, but short metatarsal area and resembles the ichnogenus Picunichnus from the Lower Cretaceous (Albian) of Argentina. Morphotype 2 (36 cm pes length) has extensive and narrow metatarsal impressions continuously occurring along regularly-spaced trackways. This suggests either a plantigrade movement of the trackmaker or reflects preservational factors. By their overall-shape with thin digits, Morphotype 2 resembles described penetrative tracks suggesting a strong influence of the substrate. Sauropod tracks are relatively small (40 cm pes length) and show low heteropody with a kidney-shaped manus imprint, pointing to a Sauropodichnus-like form. The single ornithopod pes track (18 cm in length) is similar to material described as Ornithopodichnus from the Lower Cretaceous of Korea. Due to the incomplete material of sauropod and ornithopod prints, no concrete assignment is given to this material and further study is needed. The presence of dinosaur tracks proves a temporary subaerial exposure of the surface whereas the main part of the Na'ur Formation is dominated by subaqueous activity of marine faunas.
Vertebrate Footprints from the Miocene Upper Red Formation, Shokorchi Area, Zanjan Province, NW Iran
Ichnos-an International Journal for Plant and Animal Traces, 2010
Bird, carnivore, and artiodactyl mammal footprints were found in the Miocene Upper Red Formation in the Shokorchi area, west Zanjan, NW Iran. The Upper Red Formation section (about 50 m thick) to the east of Shokorchi village is mainly composed of marls and hard, thin- to thick-bedded sandstone layers. Sinuous ripple marks, mud cracks, and raindrop prints are common on the bedding planes, and flute casts and ripple marks show north-northwest to south-southeast paleocurrent directions. The bird tracks include digitigrade tridactyl footprints without hallux or metatarsus imprints and are assigned to Iranipeda, Antarctichnus and Avipeda isp. These bird tracks were made mainly by charadriiform birds such as sandpipers or snipes and large birds such as cranes. Mammal tracks include carnivore footprints with manus and pes imprints. The manus imprints are better preserved than the pes imprints and are semiplantigrade with five short digits. Digit V is clearly distinct from digits I-IV. The tips of manus digit traces are rounded without claw marks. The pes imprints are poorly preserved as a rounded or oval shape with no digit imprints and only one or two depressions in the mid to front parts of pes imprints. It seems that these footprints belonged to a carnivore in which the forefeet supported most of the animal's weight. These imprints determined as Platykopus ilycalcator and were made by large ursid. Artiodactyl footprints vary from wedge to rounded rectangular or heart shaped. Digits III and IV imprints are distinct with interungual ridges in the median or posterior region. The artiodactyl footprints are Pecoripeda (Gazellipeda) gazella, and because of the high density of tracks, distinguishing pes and manus imprints are impossible. These may have been made by a herd of artiodactyls that traversed a broad area.
Geosciences
Calcareous nannofossils are used here for the first time in order to establish a precise biostratigraphic framework for the Kermanshah Radiolarite Formation, an outcropping in Western Iran. The new data presented here challenge the previous tentative age interpretations (Pliensbachian to early Toarcian) based upon radiolarians. Calcareous nannofossil assemblages and events unequivocally indicated that the pelagic limestones and marls are late Sinemurian in age (NJT 3b nannofossil subzone), and that these are thrusted over shales and cherts dated as uppermost Sinemurian (NJT 3b-c nannofossil subzone) and lowermost Pliensbachian (NJT 4 nannofossil zone). This result leads not only to reconsideration of the age of the radiolarite formations, which are widespread in the Zagros orogenic system, but also a better understanding of the stratigraphic relationships between the various lithological units known in the area. Besides these new stratigraphic inferences, the calcareous nannofossil ...
Continental Trace Fossils in the Semnan Area (Northern Iran)
Open Journal of Geology, 2013
Continental ichnology has been taking an ever increasing importance in stratigraphy. In this paper, Continental Trace Fossils in Semnan area have been studied. Semnan Province is one of the 31 provinces which is located in the north of Iran. In the East of Semnan City, Quaternary deposits occupy about 93% of the surface area, of which the Alluvial represents one of the most important geomorphological features in the area. Nevertheless, the outspread ichnological studies in Semnan City have received lesser attention in Continental Trace Fossils. Based on the systematic ichnology, 6 trace fossils are distinguished, namely Celliforma isp, Coprinisphaera isp, Palaeophycus tubularis, planolithes isp, Tombownichnus plenus, and Skolithos isp. The existence of Rhizoliths along with the tetrapod footprints and the survey of lithofacies all indicate that the trace fossils are related to Coprinisphaera ichnofacies. Based on ichnological and sedimentary facies analysis, the Continental Trace Fossils, in the study area, are located in the flood plain, point bar, and playa environment.
A summary of the Jurassic System in North and East-Central Iran
Zitteliana, 2021
Jurassic rocks show a wide distribution in North and Central Iran, attain great thicknesses and are commonly superbly exposed. The present paper is a short synopsis of the extensive investigations of the sedimentary strata of the Jurassic System in North and East-Central Iran, carried out over the last 20 years by teams from Iran
Popov, L.E., Hairapetian, V., Evans, D.H., Ghobadi Pour, M., Holmer, L.E. and Baars, C. 2015. Review of the Ordovician stratigraphy and fauna of the Anarak Region in Central Iran. Acta Geologica Polonica, 65 (4), 403-435. Warszawa.