Tiki Fm
Type Locality and Naming
South Rewa Basin: Many workers had lumped Pali and Tiki formations together. According to Hughes (1881) and Aggarwal et al. (1993) they are two distinct lithological units. Fox (1931) named the sedimentary beds occurring in low-lying tracts between Somarkoini and Tiki as “Tiki Beds”. Tiki and Pali beds were placed together in Pali Formation (Sastry et al., 1977). Kundu et al. (1993) held the opinion that these two lithounits should be separated from each other because of their lithological and faunal distinctiveness. Johilla river section between Beohari hills (near Tiki) to Neosi is designated as the type section. [Original Publications: Hughes, T.W.H., 1881. Notes on the South Rewa Gondwana Basin. Records of Geological Survey of lndia 14, 126 -138; Fox, C.S. 1931. Gondwana System and related formations. Memoirs of Geological Survey of India 8, 1-241; Sastry, M.V.A., Acharyya, S.K., Shah, S.C., Satsangi, P.P., Ghosh, S.C., Raha, P.K., Singh, G., Ghosh, R.N. 1977. Stratigraphic lexicon of Gondwana formations of India. Geol. Surv. India, Misc. Publ. 36: 1-170; Agarwal, R.P., Dotiwala, S.F., Bhoj, R., 1993. Structural framework of Son-Mahanadi Gondwana basin based on the study of remote sensing data: Gondwana Geol. Magazine, Spec. Vol. Birbal Sahni Centre, National Symposium Gondwana, India, 207– 217; Kundu, A., Pillai, A., Thanavelu, C. 1993. Elucidation of the stratigraphic interrelationship of Pali, Tiki and Parsora formations of South Rewa Basin. Gondwana Geological Magazine Special Publication, Birbal Sahni Centenary National Symposium on Gondwana of India, Nagpur, 49-55.]
[Figure 1: A) Map major Gondwana basins of the peninsular India; B) Locatioon of Tiki within the Rewa basin (after Mukherjee et al., 2012); (C) Geological Map of the study area, Tiki area in parts of Shahdol district of Madhya Pradesh, India (after Datta and Das, 2001; Datta et al., 2004; Mukherjee, et al., 2012); D). Composite litholog of Tiki area, south Rewa Gondwana basin, Sahdol, M.P. India, (after Datta and Das, 2001; Datta et al., 2004; Kumar & Sharma, 2019)]
Lithology and Thickness
Claystone. The Tiki Formation is primarily a mud-dominated unit with subordinate amount of coarse to fine-grained quartz-feldspathic sandstone units. Mudstone units vary in color from dark reddish-brown to moderate red to very dark red (field photograph A). The Tiki mudstones show well-developed paleosol horizons and pedogenic features (Mukherjee et al., 2012). Besides mudstones, carbonate grainstone conglomerates in the form of caliche-derived calcirudite/calcarenite units is the second constituent of the Tiki Formation. Most of these multistoried units with large trough-cross-bedding occur within the red mudstone beds. The sandstones of the Tiki Formation are coarse grained, pinkish-gray to pale orange in color and at places pebbly or medium grained and grade into mudstone units at the top (field photographs B and C). The thickness of the formation is about 400 m (Mukherjee et al., 2012).
[Figure 2 A,B,C: Field photographs of red mudstones (A), multistoried channel sandstone (B), and thick sandstone unit overlying red mudstones (C) of the Tiki Formation near Tiki village (after Mukherrjee et al., 2012)]
Relationships and Distribution
Lower contact
Mukherjee et al. (2012) opined that the Tiki Formation has a sharp contact with the underlying Karki Fm.
Upper contact
The Tiki Formation has an unconformble contact with the overlying Parsora Fm.
Regional extent
South Rewa Basin: Johilla river between Beohari Hills, Neosi, Hartala Hills, Janar river, Harai, Son river sections, Giar, Tharipathar.
GeoJSON
Fossils
Vertebrate taxa recovered from the Tiki Formation comprises Fish: Ptychoceratodus (Ceratodus) sp. (Sastry et al., 1977; Martin, 1982), Ptychoceratodus oldhami, Gnathorhiza sp., (Bhat and Ray, 2018), Lonchidion estesi, Lonchidion incumbens (Prasad et al., 2008), Parvodus (Pristrisodus) tikiensis, Lissodus (Pristrisodus) duffini (Prasad et al., 2008; Bhat et al., 2018a), Mooreodontus (Xenacanthus) indicus (Jain, 1980; Hampe and Schneider, 2010; Bhat et al., 2018b), Mooreodontus jaini, Tikiodontus asymmetricus, Elasmobranchii incertae sedis (Bhat et al., 2018b); Amphibian: Panthasaurus (Metoposaurus) maleriensis (Sengupta, 1992, 2002; Hunt, 1993; Chakravorti and Sengupta, 2018); Reptiles: Hyperodapedon tikiensis (Mukherjee and Ray, 2014), Parasuchus hislopi (Chatterjee, 1978), Tikisuchus romeri (Chaterjee and Majumdar, 1987), Tikiguania estesi (Datta and Ray, 2006), Rewaconodon tikiensis (Datta et al., 2004), Ruberodon roychowdhurii (Ray, 2015), Theropoda indet., Dinosauria indet. (Rakshit et al., 2018); Mammals: Gondwanadon tapani (Datta and Das, 1996), Tikitherium copei (Datta, 2005). Megaflora: Lepidopteris madagascarensis, L. stormbergensis, Dicroidium hughesii, D. zuberi, D. giarensis, D. coriaceum, Elatocladus denticulatus, E. raoi, Sphenobaiera janarensis, Pagiophyllum bosei, Yabiella indica, Desmiophyllum singhii, Xylopteris sp. Baiera sp. (Pal, 1984); Podocarpoxylon tikiense (Awatar and Rajanikanth, 2007). Plant assemblage comprises microspores: Staurosaccites. Samaropollenites, Aulisporites. Todisporites, Carnisporites, Rimaesporites, Falcisporites, Dictyophyllidites, Infernopollenites, Tikisporites, Camaerozonosporites, Brachysaccus and Chordasporites (Maheshwari and Kumaran, 1979; Kumaran and Maheshwari, 1980); megaspores: Bokarosporites, Banksisporites, Biharisporite, Verrutriletes, Bacutriletes, Horstisporites, Erlansonisporites, Hughesisporites, Nathorstisporites, Minerisporites and Aneuletes (Banerji et al., 1978; Pal, 1991, 1996)
Age
Depositional setting
The Tiki Formation was deposited in a fluvial regime. Laterally connected channel-fill sand bodies and presence of thick mudstone units suggest channel and overbank facies where the river channel was confined within the extensive floodplain deposits of the Tiki Formation (Mukherjee et al., 2012). The exposed areas of the Tiki floodplain were subjected to soil forming processes resulting in the formation of caliche profiles (Mukherjee et al., 2012). The red coloration of the floodplain fines and the calcareous paleosol profiles indicate a semi-arid climate with seasonal rainfall during the deposition of Tiki sediments (Retallack et al., 1996).
Additional Information
References
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