ArticlePDF Available

Middle Jurassic palynology of the southwest Tabas Block, Central-East Iran

Authors:
  • University of Tehran, Tehran, I.S. Iran

Abstract

Diverse and moderately to poorly preserved palynofloras occur in the lower Middle Jurassic sediment of the Hojedk Formation in the Chahrekhneh, southwestern of Tabas, east central Iran. The palynofloras comprise fifty-six species including spores (fifteen species allocated to seven genera), various types of pollen (thirty species designated to sixteen genera), dinoflagellate cysts (ten species belonged to three genera), and one acritarch species. Vertical distribution of miospores allows erection within the Hojedk Formation of one biozone–Klukisporites variegatus- Callialasporites trilobatus Assemblage zone– based on the first observed occurrence (FOO) and the last observed occurrence (LOO) of selected taxa. Moreover, vertical distribution of dinoflagellate cysts allows erection within this formation of one biozone- Nannoceratopsis sp. cf. N. gracilis Interval zone. These biozones are compared with palynozones from ± coeval strata in Iran and elsewhere. Abundance of ferns and cycadophytes in parent floras implies that the host strata accumulated under a moist warm climate during the early Middle Jurassic in this locality. Based on various data of ecogroups in Chahrekhneh, it should be considered that there were several environments of upland, warmer lowland, wetter lowland, rivers and delta. Furthermore, based on the occurrence of dinoflagellate cysts it can conclude that Chahrekhneh located at the south coastal boundary of the Iran Plate, along the Tethys Ocean.
Journal Palynology
Submit an article Journal homepage/ New content alerts RSS/ Subscribe/ Citation search
Current issue /Browse list of issues
Articles
Middle Jurassic palynology of the
southwest Tabas Block, Central-East Iran
Fatemeh Vaez Javadi
Accepted author version posted online: 03 Jul 2019
Download citation
https://doi.org/10.1080/01916122.2019.1637954
Abstract
Diverse and moderately to poorly preserved palynofloras occur in the lower Middle Jurassic
sediment of the Hojedk Formation in the Chahrekhneh, southwestern of Tabas, east central
Iran. The palynofloras comprise fifty-six species including spores (fifteen species allocated to
seven genera), various types of pollen (thirty species designated to sixteen genera),
dinoflagellate cysts (ten species belonged to three genera), and one acritarch species. Vertical
distribution of miospores allows erection within the Hojedk Formation of one biozone
Klukisporites variegatus- Callialasporites trilobatus Assemblage zone based on the first
observed occurrence (FOO) and the last observed occurrence (LOO) of selected taxa.
Moreover, vertical distribution of dinoflagellate cysts allows erection within this formation of
one biozone- Nannoceratopsis sp. cf. N. gracilis Interval zone. These biozones are compared
with palynozones from ± coeval strata in Iran and elsewhere. Abundance of ferns and
cycadophytes in parent floras implies that the host strata accumulated under a moist warm
climate during the early Middle Jurassic in this locality. Based on various data of ecogroups
in Chahrekhneh, it should be considered that there were several environments of upland,
warmer lowland, wetter lowland, rivers and delta. Furthermore, based on the occurrence of
dinoflagellate cysts it can conclude that Chahrekhneh located at the south coastal boundary of
the Iran Plate, along the Tethys Ocean.
KEYWORDS: - Middle Jurassic, Palynostratigraphy, Palaeoclimate, Tabas Block, Iran
... Vaez-Javadi & Mirzaei-Ataabadi (2006) conducted a study on Jurassic plant macrofossils from the Hojedk Formation in east-central Iran, which suggested that the formation was of Bajocian-Bathonian age. Those researchers also found evidence of a uniform palaeoclimate and environment in Iran during this time, which is consistent with the findings of Vaez-Javadi's later studies on Middle Jurassic flora and palynology in Iran (Vaez-Javadi, 2018, 2019. In her 2018 study, Vaez-Javadi focused on the Hojedk Formation in south Kouchekali, the south-western area of Tabas City, and found that the relative abundance of certain plant groups suggested a humid subtropical climate for that locality. ...
Article
Full-text available
The present study discusses the outcome of palynlogical and palaeobotanocal investigations of Middle Jurassic strata of the Tabas Block. The most commonly identified spore type is a trilete spore, Klukisporites, which accounts for 30 per cent, and the genus Ischyosporites which makes up 12 per cent of the spore collection. Plant fossils recovered from the borehole studied are indicative of a varied assemblage, starting with a diverse range of ferns and followed by Cycadophytes, Ginkgophytes and Coniferophytes. The predominance of the Lowland group in the Tabas Block during the Bajocian–Bathonian, as indicated by the Sporomorph EcoGroup (SEG) and Plant EcoGroup (PEG) models, suggests that the strata studied were laid down mainly in a lowland environment. Dinoflagellate cysts were found in locations that correspond to river and coastal ecogroups, hinting at marine influence.
... A total of 302 core samples from different wells (locations shown in Then, they were washed into a neutral environment and centrifuged with heavy liquid to obtain organic residues. These organic residues were made into thin sections for observation and identification under the microscope, and the types, abundances and assemblages of spore-pollens were systematically determined by point counting (Javadi, 2020). ...
Article
Full-text available
The Early‐Middle Jurassic is one of the crucial coal‐forming geologic periods in the world and an important target for hydrocarbon exploration in the Turpan‐Hami Basin, China. The paleoenvironment and vegetation reconstruction of the Early‐Middle Jurassic have been investigated using elemental geochemistry and palynological analysis to reveal paleoclimate evolution. A total of 48 genera of pteridophyte spore and 35 genera of gymnosperm pollen were identified, and 5 palynological assemblages were longitudinally divided, which showed significant differences in geochemical behaviours. The paleoenvironment was a transition from suboxidation to anoxia and then to an oxidation environment under freshwater conditions. The paleowater in the northern Taibei Sag was deeper than that in the southern part during the Middle Jurassic, which coincided with the sedimentary background of the sublacustrine fan in the north and the shallow braided river delta in the south. The paleovegetation evolved from mixed lowland–upland forest in the Hettangian‐Toarcian, to lowland fern forest in the Aalenian‐Bajocian, to upland conifers forest in the early Bathonian, to upland Cheirolepidiaceae forest in the late Bathonian‐Callovian. The Toarcian and Bathonian‐Callovian arid climate and the Hettangian‐Pliensbachian and Aalenian‐Bajocian warm‐humid climate were responses to the continued global warming events and the intensification of the East Asian monsoon circulation, respectively. The influence of the Bathonian‐Callovian aridification event on the sedimentary response in the southern Taibei Sag will be delayed due to the gradual southward migration of the depositional centre.
Article
Since the publication of five literature compilations issued between 2012 and 2020, 63 further published contributions on Triassic, Jurassic and earliest Cretaceous (Berriasian) dinoflagellate cysts have been discovered, or were issued in the last 14 months (i.e. between February 2019 and March 2020). These studies are on North Africa, Southern Africa, East Arctic, West Arctic, east and west sub-Arctic Canada, China and Japan, East Europe, West Europe, the Middle East, and sub-Arctic Russia west of the Ural Mountains, plus multi-region studies and items with no geographical focus. The single-region studies are mostly focused on Africa, the Arctic, Europe and the Middle East. All the 63 publications are listed herein with doi numbers where applicable, and a description of each item as a string of keywords.
Article
Full-text available
During the Jurassic, Sardinia was close to continental Europe. Emerged lands started from a single island forming in time a progressively sinking archipelago. This complex palaeogeographic situation gave origin to a diverse landscape with a variety of habitats. Collection- and literature-based palaeobotanical, palynological and lithofacies studies were carried out on the Genna Selole Formation for palaeoenvironmental interpretations. They evidence a generally warm and humid climate, affected occasionally by drier periods. Several distinct ecosystems can be discerned in this climate, including alluvial fans with braided streams (Laconi-Gadoni lithofacies), paralic swamps and coasts (Nurri-Escalaplano lithofacies), and lagoons and shallow marine environments (Ussassai-Perdasdefogu lithofacies). The non-marine environments were covered by extensive lowland and a reduced coastal and tidally influenced environment. Both the river and the upland/hinterland environments are of limited impact for the reconstruction. The difference between the composition of the palynological and palaeobotanical associations evidence the discrepancies obtained using only one of those proxies. The macroremains reflect the local palaeoenvironments better, although subjected to a transport bias (e.g. missing upland elements and delicate organs), whereas the palynomorphs permit to reconstruct the regional palaeoclimate. Considering that the flora of Sardinia is the southernmost of all Middle Jurassic European floras, this multidisciplinary study increases our understanding of the terrestrial environments during that period of time.
Chapter
Full-text available
Range tops of 41 dinoflagellate cyst taxa occur within the Upper Triassic to Lower Cretaceous of northwest Europe. These range tops form the basis of a proposed biostratigraphy of the Upper Triassic, Jurassic and Lower Cretaceous strata of the region, the subdivision of which is of value to industrial palynologists who work mainly with drill cuttings from oil and gas exploration boreholes.
Article
Full-text available
The Jurassic dinoflagellate cyst zonation for the British-Danish area is revised and discussed in relation to palaeoenvironmental factors, in particular, eustatic changes and fluctuations in palaeotemperature. The stepwise evolution of dinoflagellate cyst assemblages as defined by inceptions and apparent extinctions was largely controlled by sea-level change, particularly during intervals with significant short-term eustatic fluctuations. During times characterised by less pronounced, or longer term, sea-level change, fluctuations in oceanic palaeotemperatures appear to have influenced dinoflagellate evolution. Differences in the ranges of certain taxa between Denmark and the United Kingdom may be partly related to differences in palaeotemperature.
Article
Full-text available
Palynological data are used to draw paleoecological inferences for the Dalichai Formation, northeast of Semnan, northeastern Iran. All samples examined yield well-preserved, diverse palynofloras consisting predominantly of miospores; dinoflagellate cysts, foraminiferal test linings, and fungal spores occur as minor constituents. Fifty-four species of spores (37 genera), 18 species of pollen (9 genera), and 16 species of dinoflagellate cysts (13 genera) are recognized. Co-occurrence of such miospore species with known vertical ranges as Klukisporites variegatus, Sellaspora asperata, Murospora florida, and Concavissimisporites verrucosus suggests a Middle Jurassic (Bajocian-Callovian) age for the host strata, thus corroborating the available paleozoological evidence. Such spore species as Klukisporites, Cyathidites, and Dictyophyllidites known to have been produced by Pterophyta dominate the palynofloras. Thus the contemporaneous coastal vegetation was characterized by predominance of Pterophyta whereas representatives of Ginkgophyta, Pteridospermophyta, Lycophyta, Coniferophyta, and Bryophyta were rarely represented. This reconstruction implies that a moist, warm climate prevailed in northeastern Iran during the Middle Jurassic (Bajocian-Callovian). This is confirmed by occurrence of fungal spores accompanied by such warm water dinoflagellate cysts as Mendicodinium groenlandicum, Pareodinia ceratophora, and Gonyaulacysta jurassica. Abundance of Amorphous Organic Matter (AOM) signifies a shallow, low-energy, dysoxic-anoxic depositional site for the host strata. Furthermore, the ratio of AOM to marine palynomorphs as well as abundance of blade-shaped to eqiudimensional opaque palynomacerals could indicate low sedimentation rate in a shallow, low-oxygenated marine environment. Additionally, occurrence of chorate dinoflagellate cysts (e.g., Adnatosphaeridium caulleryi) and acritarchs bearing relatively long processes (e.g., Micrhystridium) possibly suggests deepening upward in the study section.
Article
Full-text available
The Binalud Mountains of NE Iran represent the easternmost extension of the Alborz Range. After the Mid-Cimmerian orogenic event and rapid subsidence, the deep marine sediments of the Dalichai Formation were deposited. A well-preserved section of the formation was sampled for palynological purposes. The study revealed diverse and nearly well-preserved dinoflagellate cyst assemblages. Thirty-six dinoflagellate cyst species identified lead to identification of four biozones: Cribroperidinium crispum (Late Bajocian), Dichadogonyaulax sellwoodii (Bathonian to Early Callovian), Ctenidodinium continuum (Early to Late Callovian), and Ctenidodinium tenellum (Early Oxfordian) biozones. The close similarities of dinoflagellate cyst assemblages between Binalud Mountains, NE Iran, with those of Alborz Mountains (Northern Iran) during Middle Jurassic confirm the connection between two sedimentary basins during this time in Iran. Meanwhile, this biozonation corresponds largely to that established in Northwest Europe and reveals the marine connection between NE and North of Iran with Northwest Europe and the Northwestern Tethys during the Late Bajocian to Early Oxfordian.
Article
The Upper Palaeozoic Godar-e-Siah Complex of Jandaq, Central Iran, comprises three isolated, fault-bounded outcrops exposing Palaeozoic fossiliferous carbonates, volcanics and siliciclastics, which are markedly distinct from the surrounding sedimentary successions. The three outcrops, that emerge below Cretaceous and younger sediments, are the Chah Rizab outcrop, the Godar-e-Siah northern outcrop, and the Godar-e-Siah central outcrop. Their sedimentary successions strongly differ from the typical passive margin successions of Gondwanan affinity that characterize the Yazd, Lut and Tabas blocks of Central Iran and the Alborz in North Iran. To understand the origin of these profound differences, we first calibrated the age of the Jandaq successions: U-Pb radiometric zircons ages, obtained from granitoid boulders in the conglomerates at Chah Rizab and in the Godar-e-Siah northern outcrop, gave a Late Devonian to Mississippian age. Biostratigraphic data from brachiopods and fusulinids from the Godar-e-Siah northern and central outcrops indicate a Pennsylvanian age. The age of the successions is thus post-Visean to Pennsylvanian. The petrographic composition of the siliciclastic deposits indicates the erosion of a magmatic arc. To understand where the Jandaq complex could have been located at that time, we have assessed the palaeobiogeographic affinity of the faunas. The collected brachiopods and fusulinids assemblages are mostly similar to coeval faunas from Spain, Donbass, Urals, and Yukon Territory (Canada) and have a North-Palaeotethyan affinity. The Godar-e-Siah Complex of Jandaq likely represents part of the southern active margin of Eurasia (northern margin of the Palaeotethys), in contrast to the surrounding Central and North Iran blocks, which were at that time located along the southern margin of the Neotethys. Our investigations confirm a complex palaeogeographic evolution for the studied outcrops, suggesting that they represent fragments of the southern Eurasian active margin - today preserved in NE Iran - displaced by crustal-scale wrench motions related to the opening and closure of the Sabzear Ocean and to the Cenozoic activity of the Great Kavir-Doruneh Fault and its possible precursors.
Article
Among all Mesozoic plant groups in the Middle Orient the bennettitaleans are the richest in species. In the present monography 57 species are treated, among them 42 leaves, 2 perianth scales, 8 female and 3 male flowers as well as 2 axes. Remains of other species exist. However, they are too poorly or incompletely preserved for publishing. Within the leaf-genera species may occur where the leaves are nearly indistinguishable in their morphology, although they show distinct differences in the cuticular structure. Therefore, it is not always possible to match leaf-impressions with species which are established from fossils with preserved cuticles. In such cases we have added a cf. to our determination. Morphological convergences are not only restricted to the bennettitalean leaves themselves but also occur between these and the Cycadales and Nilssoniales. Generally, a bermettitalean leaf is characterized by dichotomising veins and transversal wrinkles on the rachids. However, there are also species with undivided veins. Moreover, the transversal wrinkles depend on the mode of preservation. They reflect internal structures (presumably bands of sclerenchymatic cells) and may be, therefore, invisible on the surface of intact rachids. Therefore, their occurrence, or absence, is not necessarily a specific feature.
Article
The occurrence in Iran of several ophiolite belts dating between Late Palaeozoic to Triassic poses several questions on the possible existence of various sutures marking the closure of the Palaeotethys ocean between Eurasia and this Gondwana-derived microplate. In this scenario, the Anarak region in Central Iran still represents a conundrum. Contrasting geochronological, paleontological, paleomagnetic data and reported field evidence suggest different origins for the Anarak Metamorphic Complex (AMC). The AMC is either interpreted, as: (1) relict of an accretionary wedge developed at the Eurasia margin during the Palaeotethys subduction as part of the Cimmerian suture zone of NE Iran, displaced to Central Iran by a large counter-clockwise rotation of the central Iranian blocks; (2) autochthonous unit forming a secondary branch of the main suture zone.