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Miospores – based palynostratigraphy of the Hojedk Formation at the Eshkeli Section, north of Kerman

Authors:
  • Research Institute of Forests and Rangelands, Agricultural Research Education and Extension Organization (AREEO), Tehran, Iran

Abstract

Reasonably diverse and fairly preserved palynoflora dominated by land-derived palynomorphs (miospores) in association with minor marine entities, such as dinoflagellate cysts, foraminiferal test linings, and acritarchs occur in surface samples of the Hojedk Formation, at the Eshkeli stratigraphic section, north of Kerman. Spores with radiosymmetrical symmetry (trilete spores), bisaccate and monosaccate pollen, in descending order, are abundant in the assemblages; twenty-six species of spores (assigned to 18 genera) and eight species of pollen (distributed among 7 genera) are recovered. Klukisporites Zone and Klukisporites variegatus Subzone are identified based on the notable abundance of the ubiquitous index species in the assemblages and dated as as late Bajocian-early Bathonian. Co-occurrence of miospores with known vertical ranges, viz., Klukisporites variegatus, Osmundacidites senectus, Concavissimisporites verrucosus, Striatella spp. suggests a Middle Jurassic age (late Bajocian-early Bathonian) for the host strata thus corraborating with the available palnt megafossil data.
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
Sajjadi@khayam.ut.ac.ir

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

Klukisporites variegatus
Klukisporites ZoneKlukisporites variegatus
SubzoneConcavissimisporites
verrucosusKlukisporites variegatusKlukisporites scaberisOsmundacidites senectusStriatella spp.

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 

     
     
  
      
       
       
        
Wilmsen et al., 2009b
Seyed-Emami & Alavi-Naini 1990Fursich et al.,
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      
    Seyed-Emami et al., 2004
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
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Paleontology
Spring & Summer 2014, 2 (1): 111-127
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 






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Kimiyai, 1968
Arjang, 1975Vassiliev, 1984Poole & Mirzaie
Ataabadi, 2005Fursich et al., 2009b





., 2009bet alFürsich





Barnard1967



Vassiliev1984


Schweitzer & Kirchner1996, 1998

Poole & Mirzaie
Ataabadi2005 

Vaez-Javadi & Mirzaei-Ataabadi2006
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113 
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



Phipps & Playford1984


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
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


Immersion Oil













 






Klukisporites variegates

Klukisporites ZoneKlukisporites
variegatusArjang, 1975

Arjang1975




Alisporites simillis, Araucariacites australis,
Retitriletes austroclavatidites, Chasmatosporites
major, Cycadopites spp., Cyathidites australis,
Ischyosporites crateris, Deltoidospora hallii,
Concavissimisporites punctatus, Dictyophyllidites
harrisii, Dictyophyllidites mortonii, Riccisporites
tuberculatus, Todisporites minor, Osmundacidites
senectus, Gleicheiniidites senonicus, Converru-
cosisporites parvitumulus, Klukisporites scaberis,
Biretisporites sp., Osmundacidites injunensis,
Podocarpidites biformis, Striatella seebergensis,
Limbosporites lundbladii, Callialasporites
dampieri, Alisporites australis, Concavissimis-
porites
subgranulosus, Granulatisporites granu-
latus, Sellaspora passa, Todisporites major,
Concavissimisporites verrucosus, Classopollis
simplex,
Cyathidites concavus, Osmundacidites
wellmanii.







Kimyai1968, 1974




Cyathidites, Deltoidospora, Dictyophyllidites,
Klukisporites, Osmundacidites, Todisporites,
Alisporites, Inaperturopollenites (Araucariacites),
Gleicheiniidites, Classopollis, Monosulcites
(Cycadopites), Ischyosporites, Podocarpidites,
Tsugapollenites (Callialasporites).
Arjang1975


Concavisporites
(Dictyophyllidites) Zone
Klukisporites ZoneKlukisporites
variegatus Subzone


Cyathidites australis
Osmundacidites wellmaniiTodisporites minor
Concavisporites labrapunctatus (Dictyophyllidites
harrisii)Concavisporites persicus (Dictyophyllidites
mortonii)Deltoidospora halliiLimbosporites
lundbladiiPodocarpidites biformis


Arjang1975
Ischyosporites (Klukisporites)
variegatusConcavisporites (Dictyophyllidites)

Achiilles et al.
1984



Duplexisporites
115 






Plate 1
Figs. 1-2. Dictyophyllidites mortonii (de Jersey) Playford & Dettmann, 1965; proximal foci. Fig. 3. Gleicheniidites senonicus Ross
emend. Skarby, 1964; proximal focus. Figs. 4-5. Ischyosporites crateris Balme, 1957; 4, 5a proximal foci. 5b distal focus. Figs. 6-
8. Klukisporites variegates Couper, 1958. median foci. Fig. 9. Striatella seebergensis Mädler, 1964. median focus. Fig. 10.
Limbosporites lundbladii Nilsson, 1958. median focus. Fig. 11. Sellaspora passa McKellar, 1998. median focus. Fig. 12.
Chasmatosporites major Nilsson, 1958. median focus. Fig. 13. Alisporites grandis (Cookson) Dettmann, 1963, median focus. Fig.
14. Concavissimisporites punctatus (Delcourt & Sprumont) Brenner, 1963. Proximal focus. Fig. 15 Cribroperidinium crispum
(Wetzel) Fenton, 1981.
 




117 






problematicus (Striatella seebergensis)
Ischyosporites (Klukisporites) variegates
Leptolepidites argenteaeformis Zone

Leptolepidites argenteaeformis


Dictyophyllidites mortonii

Limbosporites
lundbladii
Cyathidites australis

Achiilles et al.1984 Arjang1975
Ashraf1977
Ischyosporites (Klukisporites) variegatus
Concavisporites (Dictyophyllidites)




Bharadwaj & Kumar1986
A-C
Dictyophyllidites
Cyathidites

Klukisporites
Arjang1975
Klukisporites variegatus
                                   

B


Araucariacites, Cyathidites, Cycadopites,
Dictyophyllidites, Gleicheniidites, Retitriletes.




 






Alisporites similis, Araucariacites australis,
Biretisporites sp., Concavissimisporites punctatus,
Concavissimisporites subgranulosus,
Concavissimisporites verrucosus, Cyathidites
australis, Cyathidites minor, Dictyo-phyllidites
harrisii, Dictyophyllidites mortonii, Klukisporites
variegatus, Osmundacidites senectus, Todisporites
major, Todisporites minor.

 

Striatella seebergensis

Contignisporites burgeri



Alisporites australis, Alisporites simillis,
Araucariacites australis, Callialasporites
dampieri, Concavissimisporites verrucosus,
Cyathidites australis, Deltoidospora hallii,
Dictyophyllidites harrisii, Dictyophyllidites
mortonii, Gleicheiniidites senonicus, Limbosporites
lundbladii, Osmundacidites senectus, Retitriletes
austroclavatidites, Striatella seebergensis,
Todisporites minor.
Sajjadi et al., 2007
A-C



Alisporites similis, Araucariacites australis,
Callialasporites dampieri, Concavissimisporites
punctatus, Concavissimisporites verrucosus,
Cyathidites australis, Cyathidites minor,
Deltoidospora sp., Dictyophyllidites harrisii,
Dictyophyllidites mortonii, Gleicheniidites senonicus,
Klukisporites variegatus, Klukisporites variegatus,
Osmundacidites senectus, Osmundacidites wellmanii,
Sellaspora asperata, Todisporites minor.


Klukisporites variegatus
Klukisporites variegates Aboundance
Zone






Klukisporites ZoneKlukisporites
variegatus Subzone
Klukisporites variegatus

Callialasporites dampieri
Callialasporites dampieri

Dictyotosporites complex Oppel zone
Klukisporites variegatus Subzone







Alisporites australis, Alisporites simillis,
Araucariacites australis, Biretisporites sp.,
Callialasporites dampieri, Chasmatosporites
major, Classopollis simplex, Concavissimisporites
punctatus, Concavissimisporites verrucosus,
Converrucosisporites parvitumulus, Cyathidites
australis, Cyathidites
concavus, Cycadopites spp.,
Deltoidospora hallii, Dictyophyllidites harrisii,
Dictyophyllidites mortonii, Gleicheiniidites
119 






senonicus, Ischyosporites crateris, Limbosporites
lundbladii, Osmundacidites wellmanii, Retitriletes
austroclavatidites, Riccisporites tuberculatus,
Sellaspora passa, Striatella seebergensis,
Todisporites major, Todisporites minor.











Balme1957
IIIaIIb
 
I
Corollina (Classopollis)Exesipollenites
Exesipollenites Assemblage
IIa
Callialsporites dampieri
Podosporites
Microcachryidites
Dampieri Assemblage
IIb
Microcachryidites Assemblage 
(Balme, 1964)
Balme1964Dampieri
Assemblage






Araucariacites australis, Gleicheniidites,
Corollina (Classopollis), Lycopodiumsporites
(Retitriletes), Cyathidites, bisaccate pollen.
Reiser & Williams1969(Surat)
Tsugapollenites
(Callialasporites) segmentatus - Tsugapollenites
dampieri Assemblage zone





Callialasporites dampieriCyathidites
spp.Dictyophyllidites mortoni
Filatoff1975
Exesipolleinites tumulus Assemblage zone
Callialasporites dampieri
Assemblage zone
(Pert)



Dictyotosporites complex Oppel zone



Converrucosisporites variverrucatus (verrucosus),
Duplexisporites (Striatella) problematicus
(seebergensis), Gleicheniidites senonicus,
Klukisporites neovariegatus (variegatus),
Lycopodiumsporites (Retitriletes) austroclavatidites,
Callialasporites dampieri.
Ashraf1977
 
Ischyosporites (Klukisporites)
 



Concavisporites (Dictyophyllidites)
Ischyosporites (Klukisporites) variegatus-
Duplexisporites (Striatella) problematicus
(seebergensis)

BiretisporitesCycadopites
Gleicheiniidites
KlukisporitesPodocarpidites
Todisporites

Helby et al.
1987
Callialasporites dampieri Superzone
Microcachryidites Superzone




Dictyotosporites complex
Oppel Zone (Filatoff, 1975 - modified)


Retitriletes
circolumenusContignisporites cooksoniae



Duplexisporites (Striatella) problematicus
(seebergensis), Gleicheniidites senonicus,
Callialasporites dampieri, Corollina (Classopollis)
simplex.
Filatoff & Price1988
Contignisporites
Striatella


Striatella seebergensis


.
McKellar1998


Retitriletes circolumenus Association Zone


Aequitriradites norrisii

 Corollina (Classopollis) spp., Callialasporites
spp., Klukisporites scaberis, Klukisporites
variegates.
Mantle & Riding2012



Alisporites, Araucariacites, Classopollis,
Concavissimisporites, Cyathidites, Dictyophyllidites,
Gleicheniidites, Klukisporites, Osmundacidites,
Striatella.
Tripathi2001
(Rajmahal)

Assemblage 5
                                                  

Alisporites, Araucariacites, Callialasporites,
Cyathidites, Podocarpidites.
Ibrahim et al.2001
Zone II: Converrucosisporites spp.,
Verrucosisporites spp., Trilobosporites spp.
assemblage zone

Classopollis (Corollina) torosa

Concavissimisporites variverrucatus (verrucosus)
Camarozonosporites sp. (ramosus)Dictyophyllidites
harrisii

Klukisporites variegatus
Verrucosisporites
varians
Cicatricosisporites spp.

121 







ConcavissimisporitesConverrucosisporites
KlukisporitesTrilobosporitesVerrucosisporites
Verrucosisporites
Trilobosporites


Yin & Zhang2002
Cyathidites-Psophophaera-Cycadopites

Cyathidites-Quadraeculina-
ClassopollisCyathidites-
Callialasporites-Classopollis


Neoraistrickia gristhorpensis (truncata)
Cyathidites
Deltoidospora
Neoraistrickia gristhorpensis
(truncata)






Araucariacites australis, Callialasporites
dampieri, Cyathidites australis, Cyathidites minor,
Dictyophyllidites mortoni, Osmundacidites
wellmanii.



Concavissimisporites variverrucatus (verrucosus),
Duplexisporites (Striatella) problematicus
(seebergensis), Klukisporites variegatus.
Tripathi2004(Rajmahal)


Callialasporites


                                        

Assemblage 1

CallialasporitesConcavissimisporitesKlukisporites
Contignisporites
Contignisporites


Vijaya & Sen2005Contignisporites
cooksoniae Assemblage

Callialasporites
Callialasporites dampieriCallialasporites
turbatus
Callialasporites trilobatus
Callialasporites
segmentatus



Araucariacites australis, Classopollis simplex,
Dictyophyllidites harisii, Duplexisporites
(Striatella) problematicus (seebergensis),
Gleicheniidites senonicus, Lycopodiacidites
(Sellaspora) asperatus (asperata), Osmundacidites
wellmanii, Podocarpidites spp.
Jiang et al.
2008
Tarim


Alisporites lowoodensis, Callialasporites dampieri,
Chasmatosporites major, Cyathidites australis,
Cyathidites minor, Dictyophyllidites harrisii,
Klukisporites variegatus, Osmundacidites
wellmanii, Todisporites minor
Stefanowicz2008
(A-E)
D
 





Ischyosporites (Klukisporites)Araucariacites
ClassopollisRetitriletesCallialasporites
Volkheimer et al.2008



Alisporites, Araucariacites, Callialasporites,
Classopollis, Dictyophyllidites, Podocarpidites.
Ainsword & Riley2010

Converrucosisporites
Deltoidospora

Callialasporites
Gleicheniidites


Rostortseva2011
Palynocomplex I
Palynocomplex II


Alisporites, Classopollis, Cyathidites australis,
Cyathidites minor, Duplexisporites (Striatella),
Gleicheniidites senonicus, Klukisporites
variegatus, Lycopodiumsporites (Retitriletes),
Osmundacidites, Podocarpidites.
Zobaa et al.
2013




Araucariacites australis, Classopollis spp.,
Deltoidospora hallii, Dictyophyllidites harrisii,
Gleicheniidites senonicus, Osmundacidites
wellmanii,


Klukisporites variegatus
Klukisporites
ZoneKlukisporites variegatus Subzone
Arjang1975
Arjang1975


Klukia exilis (Philips) Raciborski, 1890

Klukisporites variegatus

Klukisporites
variegatus




Arjang1975Achilles et al.1984
Baharadwaj & Kumar1986Kimyai1975,
1977



Filatoff, 1975Backhouse, 1988
McKellar, 1998Sajjadi & Playford, 2002a
(Koppelhus & Dam, 2003)

Osmundacidites senectus
Balme, 1963
Playford & Dettmann, 1965Burger, 1996
Concavissimisporites verrucosus

Filatoff, 1975Burger, 1976,
1996Helby et al., 1987Backhouse, 1988


123 






Plate 2
Fig. 1. Elatides thomasii Hasris, 1979; Fig. 2. Klukia exilis
(Philips) Raciborski emend. Harris, 1961; Fig. 3. Klukia westi
Jacob & Shukia, 1955.
Klukisporites scaberis
McKellar, 1998


Filatoff & Price1988

StriatellaContignisporites
burgeri
Striatella


Contignisporites burgeri


Cribroperidinium crispum
Woollam & Riding,
1983







Cribroperidinium crispum
Total Range Biozone
Acanthaulax crispa
(Cribroperidinium crispum)

Cribroperidinium crispum


Cribroperidinium sp.Pareodinia sp.


Beania cf. mamayiCladophlebis
aktashensisConiopteris hymenophylloidesEquisetites
columnarisFerizianopteris undulateNilssonia
bozorgaNilssonia feriziensisNilssonia ingens
Nilssonia macrophyllaNilssonia sarakhs
Otozamites cf. graphicusTodites princeps

Vaez-Javadi & Mirzaei-Ataabadi,
2006Klukia exilis (Philips) Raciborski
emend. Harris, 1961

Fakhr, 1977
Vaez - Javadi & Mirzaei - Ataabadi, 2006
Vaez-Javadi & Abbasi, 2012
Klukia exilis



 




 





Klukisporites variegatus

Klukisporites ZoneKlukisporites
variegatus Subzone

Klukisporites variegatusKlukisporites scaberis
Concavissimisporites verrucosusOsmundacidites
senectusStriatella spp.






    

















           .(


























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
Miospores based Palynostratigraphy of the Hojedk Formation,
Eshkeli, north of Kerman
Hashemi-Yazdi, F.1*, Sajjadi, F.2, Hashemi, H.3
1- Ph.D. Student in Stratigraphy & Paleontology, School of Geology, College of Sciences, University of Tehran, Tehran, Iran
2- Associate Professor, School of Geology, College of Sciences, University of Tehran, Tehran, Iran
3- Associate Professor, Department of Geology, Faculty of Earth Sciences, Kharazmi University, Tehran, Iran
*E-mail: Sajjadi@khayam.ut.ac.ir
Abstract
Reasonably diverse and fairly preserved palynoflora, dominated by land-derived palynomorphs
(miospores) in association with minor marine entities, such as dinoflagellate cysts, foraminiferal test
linings, and acritarchs, occur in surface samples of the Hojedk Formation, at the Eshkeli
stratigraphic section, north of Kerman. Spores with radiosymmetrical symmetry (trilete spores),
bisaccate and monosaccate pollen, in descending order, are abundant in the assemblages; twenty-six
species of spores (assigned to 18 genera) and eight species of pollen (distributed among 7 genera)
are recovered. Klukisporites Zone and Klukisporites variegatus Subzone are identified based on the
notable abundance of the ubiquitous index species in the assemblages and dated as Late Bajocian-
Early Bathonian. Co-occurrence of miospores with known vertical ranges, viz., Klukisporites
variegatus, Osmundacidites senectus, Concavissimisporites verrucosus, Striatella spp. suggests a
Middle Jurassic age (Late Bajocian-Early Bathonian) for the host strata thus corroborating with the
available plant megafossil data.
Keywords: Palynostratigraphy; Middle Jurassic; Hojedk Formation; central Iran; Kerman.
... This early work was continued by a series of contributions by Vassiliev (1984), Kirchner (1996, 1998), Poole and Mirzaie Ataabadi (2005) and Vaez-Javadi and Mirzaei-Ataabadi (2006) which contributed to the knowledge of the Middle Jurassic flora of this formation. In addition, the palynoflora from the Middle Jurassic of the Hojedk Formation has so far only been studied in the Kerman Block (Kimyai 1968;Arjang 1975;Bhardwaj and Kumar 1986;Hashemi-Yazdi et al. 2014;Hashemi-Yazdi 2015). Kimyai (1968) reported a palynoflora from the upper-Middle Jurassic in the northwest of the Kerman area, and reported the following genera, which were also found in this study: Araucariacites, Cyathidites, Deltoidospora, Dictyophyllidites, Klukisporites and Osmundacidites. ...
... Araucariacites australis, Callialasporites dampieri, and Cycadopites spp. Hashemi-Yazdi et al. (2014) and Hashemi-Yazdi (2015) studied the Hojedk Formation in the Eshkeli section in the Kerman Block and found the Klukisporites Zone and the K. variegatus Subzone of Arjang (1975), which are indicative of late Bajocian-Bathonian. They reported some miospores among which the following are in common with the current study: Cyathidites australis, Concavissimisporites punctatus, Dictyophyllidites harrisii, Klukisporites scaberis, Limbosporites lundbladii, Osmundacidites wellmanii and Callialasporites dampieri. ...
... Since the late 1950s, many studies were conducted on Jurassic sediments and a number of palynozones have been introduced for this period (cf. Hashemi-Yazdi et al. 2014). In this section, we compare our results with those of previous studies on Jurassic successions in other regions of the world. ...
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We performed a palynological study on Jurassic successions of the Hojedk Formation, Central Iran. The sampled material was recovered from well no. 233, South Kuchak-Ali area belonging to the Tabas Block. The lithology comprises 475.80m of green-grey shales and sandstones. Palynological assemblages were recovered including spores, pollen grains, dinoflagellate cysts, woody debris and amorphous organic matter (AOM). Furthermore, 22 taxa of plant macrofossils were identified. We analyzed 48 samples which resulted in identification of 13 spore species (belonging to 11 genera) and three pollen species (from three genera) with fair preservation quality. Trilete spores dominate while pollen grains only represent 11.5% of the total particulate organic matter. Representatives of the fern spores Klukisporites are particularly abundant and the K. variegatus acme zone, which is of biostratigraphical importance, is identified in the host strata. The abundance of K. variegatus and K. scaberis suggests a Middle Jurassic (Bajocian-Bathonian?) age for the host strata. This age designation corroborates previous stratigraphic interpretations, mainly based on plant macrofossils for this formation. The palynomorphs indicate deposition in an oxygenated environment close to the shoreline in a deltaic system. The presence of subordinate marine palynomorphs (proximate dinoflagellate cysts) is indicative of intermittent sea level transgression. The affinity of the palynological assemblages from the Hojedk Formation indicate diverse parental flora of, in descending quantitative order, ferns, bryophytes and gymnosperms, the latter mainly represented by conifers and ginkgophytes. Comparisons with modern plant ecology indicates accumulation of palynomorphs under a moist warm climate during the Middle Jurassic (Bajocian-Bathonian?) time. The comparison of parental plants with previous paleofloristic studies indicates that the Tabas Block was located in the Mid-Asian part of the Indo-European floristic province of the Northern Hemisphere.
... Spores The Namin biozonation scheme is compared ( Figure 3) with ±coeval palynozones introduced from Gondwana (e.g., Balme, 1957Balme, , 1964Filatoff, 1975;McKellar, 1998;Mantle and Riding, 2012;Ibrahim et al., 2001;Tripathi, 2004;Quattrocchio et al., 2001;Stukins et al., 2013) and Eurasia (e.g., Stefanowicz, 2008;Rostovtseva, 2011;Ashraf, 1977;Ashraf et al., 1999Ashraf et al., , 2010Arjang, 1975;Achilles et al., 1984;Bharadwaj and Kumar, 1986;Sajjadi et al., 2007;Dehbozorgi, 2014;Hashemi Yazdi et al., 2014;Sajjadi and Dermanaki Farahani, 2017;Hashemi Yazdi et al. 2018;Badihagh et al., 2019). ...
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Palynomorphs are used for palynostratigraphy, and to derive paleoecological and paleobiogeographical inferences from the Middle Jurassic Shemshak Formation, Alborz Ranges, northwestern Iran. The rock unit contains diverse, reasonably preserved palynofloras dominated by miospores and dinoflagellate cysts. Vertical distribution of miospores allows for the introduction of Klukisporites variegatus -Striatella spp.- Contignisporites burgeri assemblage zone in the host strata. The presence of such key miospore species as Striatella jurassica, S. patenii, S. seebergensis, and Contignisporites burgeri indicates a Middle Jurassic (late Bajocian–Bathonian) age. Based on the stratigraphic distribution of dinoflagellate cysts, encountered Cribroperidinium crispum Total Range Biozone (late Bajocian); Dichadogonyaulax sellwoodii Interval Biozone (Bathonian–early Callovian), and Subzone “a” of the D. sellwoodii Zone (early–middle Bathonian) are identified. Miospores dominating the examined assemblages are assigned, in ascending order of abundance, to Pterophyta, Coniferophyta, Pteridospermophyta, Lycophyta, Ginkgophyta, Cycadophyta, and Sphenophyta. Such parental vegetation apparently flourished under a wet, warm-to-warm-temperate climate. The co-occurrence of such index warm-moderate water dinoflagellate cysts as Pareodinia halosa, Ctenidodinium continuum, and Pareodinia ceratophora supports this overview. The assemblages though contain both Eurasian and Gondwanan elements but bear closer similarity to those from the former, thus suggesting paleoproximity to the northeastern margin of the Neotethys Ocean during the Middle Jurassic.
... 2, 3). 164 Fakhr (1977) Chen et al., 2001;Sun et al., 2007;Ding et al., 2010;Wu 296 et al., 2016;Sun et al., 2018) for the Middle Jurassic period 297 and are listed on Table 2 and Fig. 4 (Vassiliev 306 1984;Schweitzer and Kirchner, 1995, 1998, 2003307 Schweitzer et al., 1997307 Schweitzer et al., , 2000307 Schweitzer et al., , 2009 and palynological 308 (Sajjadi et al., 2007;Ghasemi-Nejad et al., 2012;309 Dehbozorgi et al., 2013;Hashemi Yazdi et al., 2014, 310 2018Sajjadi et al., in preparation) The NLEs method has been widely applied to recon- cies. These authors concluded that the results of the SR Table 2 Paleo-CO 2 values estimated from plant stomatal parameters of the Middle Jurassic in Iran and previously published results from other regions worldwide. ...
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... On the other hand, there are numerous studies on the macrofloras and palynology of the Hojedk Formation from several locations on the Tabas Block (e.g. Hashemi-Yazdi et al. 2014;Vaez-Javadi, 2016;Khalilizadeh et al. 2019Khalilizadeh et al. , 2022, providing important climatic and palaeoenvironmental information. The Middle Jurassic Hojedk Formation is of major importance for understanding the regional geodynamic and palaeoclimatic evolution of the Cimmerian terranes in east-central Iran that represent a crucial part of a larger superimposed orogenic belt that extended from the Iran Plate to southeast Asia (e.g. ...
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... Spores The Namin biozonation scheme is compared ( Figure 3) with ±coeval palynozones introduced from Gondwana (e.g., Balme, 1957Balme, , 1964Filatoff, 1975;McKellar, 1998;Mantle and Riding, 2012;Ibrahim et al., 2001;Tripathi, 2004;Quattrocchio et al., 2001;Stukins et al., 2013) and Eurasia (e.g., Stefanowicz, 2008;Rostovtseva, 2011;Ashraf, 1977;Ashraf et al., 1999Ashraf et al., , 2010Arjang, 1975;Achilles et al., 1984;Bharadwaj and Kumar, 1986;Sajjadi et al., 2007;Dehbozorgi, 2014;Hashemi Yazdi et al., 2014;Sajjadi and Dermanaki Farahani, 2017;Hashemi Yazdi et al. 2018;Badihagh et al., 2019). ...
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In this work, we present a global distribution and diversification of Elatocladus morphogenus was investigated during the Mesozoic. In addition, the first occurrence of Elatocladus laxus from the Middle Jurassic of Tabas Block, Central Iran.
... I RANIAN Jurassic palynological assemblages have been investigated by Arjang (1975), Kimyai (1968Kimyai ( , 1974Kimyai ( , 1977, Achilles et al. (1984), Bharadwaj and Kumar (1986), Wheeler and Sarjeant (1990), Vaez-Javadi and Ghavidel-Syooki (2005), Sajjadi et al. (2010), Dehbozorgi et al. (2013), Navidi-Izad et al. (2015) and Hashemi-Yazdi et al. (2014). Despite these studies, palynological contents of the Jurassic deposits, however, remain unexplored, especially in east-central of Iran. ...
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Diverse and moderately preserved palynofloras occur in the Middle Jurassic sediments of the Hojedk Formation in the South Kouchekali, southwestern of Tabas, east central Iran. The palynofloras comprise thirty–nine species including spores (fourteen species allocated to nine genera) and various types of pollen (twenty–five species designated to thirteen genera). Vertical distribution of miospores allows erection within the Hojedk Formation of one biozone–Klukisporites variegatus Assemblage zone–and two distinctive stratigraphically successive biozones, viz. Callialasporites trilobatus–Parcisporites cacheutensis Assemblage zone, and Contignisporites problematicus Taxon range zone based on the first observed occurrence (FOO) and the last observed occurrence (LOO) of selected taxa. These biozones are compared with palynozones from ±coeval strata in Iran and elsewhere. Based on the association of key miospore species such as Klukisporites variegatus, and Callialasporites dampieri within the Hojedk palynofloras, the host strata are assigned to the Middle Jurassic. Abundance of ferns and cycadophytes in parent floras implies that the host strata accumulated under a moist warm climate during the Middle Jurassic in this locality.
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