Skip to main content
Log in

Nodular features from Proterozoic Sonia Sandstone, Jodhpur Group, Rajasthan: A litho-biotectonic perspective

  • Published:
Journal of Earth System Science Aims and scope Submit manuscript

The Sonia Sandstone of Proterozoic Jodhpur Group, Marwar Supergroup, exposed around the Sursagar dam area of Jodhpur town, Rajasthan exposes two varieties of nodular features, often spectacular in shape and size. On the basis of mode of occurrence (intra- or interbed) and stratal involvement (single or multiple) the features are classified as Type I and II. From granulometric and microscopic (optical and scanning electron) studies carried out on sandstones from the nodules and their host sandstones, geochemical analysis (SEM-EDAX) of intragranular cement present within Type I nodules, and appreciation of control of associated fracture system within Type II nodules, it is proposed that the two types of nodules vary in their formative mechanism and stage of formation. While Type I nodules are identified as product of processes operative at the early diagenetic, pre-lithification stage, the Type II nodules are undoubtedly the result of post-lithification origin triggered by formation of fracture system. Here we propose generation of vapour pressure (not exceeding the overlying hydrostatic pressure) by decay of thin, laterally impersistent organic mat as the causal factor for intrabed nodule (Type I) formation, which forced rarefication of local grain packing vis-a-vis early diagenetic silica cementation. The study warrants necessity of more studies on nodules to understand possible roles of organic matter and bed-transgressive fracture systems in their formation, going beyond the generalised secondary mineralisation hypothesis.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Figure 1
Figure 2
Figure 3
Figure 4
Figure 5
Figure 6
Figure 7
Figure 8
Figure 9

Similar content being viewed by others

References

  • Banerjee S and Jeevankumar S 2005 Microbially originated wrinkle structures on sandstone and their stratigraphic context: Palaeoproterozoic Koldaha Shale, central India; Sedim. Geol. 176 211–224.

    Article  Google Scholar 

  • Banerjee S and Jeevankumar S 2007 Facies and depositional sequence of the Mesoproterozoic Rohtas Limestone, eastern Son valley, India; J. Asian Earth Sci. 30 82–92.

    Article  Google Scholar 

  • Banerjee S, Sarkar S and Bhattacharyya S K 2005 Facies, dissolution seams and stable isotope characteristics of the Rohtas Limestone (Vindhyan Supergroup) in the Son valley area, central India; J. Earth Syst. Sci. 114 87–96.

    Article  Google Scholar 

  • Banerjee S, Bhattacharya S K and Sarkar S 2006a Carbon and oxygen isotope compositions of the carbonate facies in the Vindhyan Supergroup, central India; J. Earth Syst. Sci. 115 113–134.

    Article  Google Scholar 

  • Banerjee S, Jeevankumar S, Sanyal P and Bhattacharyya S K 2006b Stable isotope ratios and nodular limestone of the Proterozoic Rohtas Limestone, Vindhyan basin, India; Carbonates and Evaporites 21 133–143.

    Article  Google Scholar 

  • Banerjee S, Sarkar S, Eriksson P and Samanta P 2010 Microbially related structures in siliciclastic sediment resembling Ediacaran fossils: Examples from India, ancient and modern; In: Microbial Mats: Modern and Ancient Microorganisms in Stratified Systems (eds) Seckbach J and Oren A (Berlin: Springer-Verlag) 14 111–129.

    Google Scholar 

  • Bose P K, Eriksson P G, Sarkar S, Wright D T, Samanta P, Mukhopadhyay S, Mandal S, Banerjee S and Altermann W 2012 Sedimentation patterns during the Precambrian: A unique record?; Marine Petrol. Geol. 33 34–68.

    Article  Google Scholar 

  • Chanda S K, Bhattacharya A and Sarkar S 1977 Early diagenetic chert nodules in Bhander Limestone, Satna district, Maihar, India; J. Geol. 84 213–224.

    Article  Google Scholar 

  • Chauhan D S 1999 Tectonic and sedimentary evolution of the Marwar basin: A Neoproterozoic–Early Cambrian intracratonic sag basin; In: Proceedings of the Seminar on Geology of Rajasthan – Status and Perspective (ed.) Kataria P (A.B. Roy Felicitation Volume) Geology Department, MLSU, Udaipur, pp. 111–125.

  • Das Gupta S K 1996 Marwar Supergroup evaporates, Rajasthan; In: Recent advances in Vindhyan Geology (ed.) Ajit Bhattacharyya; Geol. Soc. India Memoir 36 49–58.

  • Das Gupta S K and Bulgauda S S 1994 An overview of the geology and hydrocarbon occurrence in western part of Bikaner–Nagaur basin; Indian J. Petrol. Geol. 3(1) 1–17.

    Google Scholar 

  • Folk R L and Lynch F L 1997 The possible role of nanobacterial (dwarf bacteria) in clay-mineral diagenesis and the importance of careful sample preparation in high-magnification SEM study; J. Sedim. Res. 67 583–589.

    Google Scholar 

  • Garlick W G 1988 Algal mats, load structures, and synsedimentary sulfides in Revett quartzites of Montana and Idaho; Econ. Geol. 83 1259–1278.

    Article  Google Scholar 

  • Gerdes G, Claes M, Dunajtschik-Piewak K, Riege H, Krumbein W E and Reineck H E 1993 Contribution of microbial mats to sedimentary surface structures; Facies 29 61–74.

    Article  Google Scholar 

  • James N P and Choquette P W 1983 Diagenesis 6. Limestones – The seafloor diagenetic environment; Geoscience Canada 10 162–179.

    Google Scholar 

  • Johnston D T, Wing B A, Farquhar J, Kaufman A J, Strauss H, Lyons T W, Kah L C and Canfield D E 2005 Active microbial sulfur disproportionation in the Mesoproterozoic; Science 310 1477–1479.

    Article  Google Scholar 

  • Knoll A H 1985 Exceptional preservation of photosynthetic organisms in silicified carbonates and silicified peats; Phil. Trans. Roy. Soc. London, Ser. B 311 111–122.

    Article  Google Scholar 

  • Kumar S, Pandey S K and Ahmad S 2011 Occurrence of giant nodules in the jodhpur sandstone, Sursagar area, Jodhpur, Rajasthan; Curr. Sci. 100(9) 1294–1296.

    Google Scholar 

  • Lan Z W and Chen Z Q 2012 Exceptionally preserved microbially induced sedimentary structures from the Ediacaran post-glacial successions in the Kimberley region, northwestern Australia; Precamb. Res. 200–203 1–25.

    Article  Google Scholar 

  • Logan B W, Hoffman P and Gebelein C D 1974 Algal mats, cryptalgal fabrics, and structures, Hamelin Pool, Western Australia; In: Evolution and Diagenesis of Quaternary Carbonate Sequence Shark Bay West Australia (eds) Logan B W, Hoffman P, Gebelein C D; AAPG Memoir 22 140–194.

  • Malone S J, Meert J G, Banerjee D M, Pandit M K, Tamrat E, Kamenov G D, Pradhan V R and Sohl L E 2008 Paleomagnetism and Detrital Zircon Geochronology of the Upper Vindhyan Sequence, Son Valley and Rajasthan, India: A ca. 1000 Ma age for the Purana Basins?; Precamb. Res. 164 137–159.

    Article  Google Scholar 

  • Mazumdar A and Bhattacharya S K 2004 Stable isotopic study from late Neoproterozoic–early Cambrian (?) sediments from Nagaur–Ganganagar Basin, western India: Possible signatures of global and regional C-isotopic events; Geochem. J. 38 163–175.

    Article  Google Scholar 

  • Mazzoli S and Carnemolla S 1993 Effects of the superposition of compaction and tectonic strain during folding of a multilayer sequence – model and observations; J. Struct. Geol. 15 277–291.

    Article  Google Scholar 

  • McBride E F, Picard M D and Folk R L 1994 Oriented concretions Ionian coast, Italy: Evidence of groundwater flow direction; J. Sedim. Res. A64 535–540.

    Google Scholar 

  • Molenaar N and Martinius A W 1990 Origin of nodules in mixed siliciclastic–carbonate sandstones, the Lower Eocene Roda Sandstone Member, southern Pyrenees, Spain; Sedim. Geol. 66 277–293.

    Article  Google Scholar 

  • Moller N K and Kvingan K 1988 The genesis of nodular limestones in the Ordovician and Silurian of the Oslo Region; Sedimentology 35 405–420.

    Article  Google Scholar 

  • Mozley P S and Davis J M 1996 Relationship between oriented calcite concretions and permeability correlation structure in an alluvial aquifer, Sierra Ladrones Formation, New Mexico; J. Sedim. Res 66 11–16.

    Google Scholar 

  • Pareek H S 1984 Pre-Quaternary geology and mineral resources of northwestern Rajasthan; Geol. Surv. India Memoir 115 1–95.

    Google Scholar 

  • Pettijohn F J 1984 Sedimentary rocks (3rd edn), Harper and Row Publ., 628p.

  • Pomar L, Westphal H and Obrador A 2004 Oriented calcite concretions in upper miocene carbonate rocks of menorca, Spain: Evidence for fluid flow through a heterogeneous porous system; Geologica Acta 2 271–284.

    Google Scholar 

  • Rahmani R A 1970 Carbonate concretions in the Upper Cretaceous Cedar District Formation, British Columbia; Bull. Can. Pet. Geol. 18 282–288.

    Google Scholar 

  • Raiswell R 1971 The growth of Cambrian and Liassic concretions; Sedimentology 17 147–171.

    Article  Google Scholar 

  • Rathore S S, Venkatesan T R and Srivastava R K 1996 Rb–Sr and Ar–Ar systematics of Malani volcanic rocks of southwest Rajasthan: Evidence for a younger post- crystallization thermal event; Proc. Indian Acad. Sci. (Earth Planet. Sci.) 105 131–141.

    Google Scholar 

  • Rathore S S, Venkatesan T R and Srivastava R K 1998 Rb–Sr isotope dating of Neoproterozoic (Malani Group) magmatism from southwest Rajasthan, India: Evidence of younger Pan-African thermal event by 40Ar–39Ar-studies; Gondwana Res. 2(2) 271–281.

    Article  Google Scholar 

  • Samanta P, Mukhopadhyay S, Mondal A and Sarkar S 2011 Microbial mat structures in profile: The Neoproterozoic Sonia sandstone, Rajasthan, India; J. Asian Earth Sci. 40 542–549.

    Article  Google Scholar 

  • Sarkar S, Banerjee S and Eriksson P G 2004 Microbial mat features in sandstones illustrated; In: The Precambrian Earth: Tempos and Events (eds) Eriksson P G, Altermann W, Nelson D R, Mueller W U and Catuneanu O, Dev. Precamb. Geol. (Elsevier: Amsterdam) 12 673–675.

  • Sarkar S, Banerjee S, Eriksson P G and Catuneanu O 2005 Microbial mat control on siliciclastic Precambrian sequence stratigraphic architecture: Examples from India; Sedim. Geol. 176 195–209.

    Article  Google Scholar 

  • Sarkar S, Banerjee S, Samanta P and Jeevankumar S 2006 Microbial mat induced sedimentary structures in siliciclastic sediments: Examples from the 1.6 Ga Churhat Sandstone, Vindhyan Supergroup, M.P., India; J. Earth Syst. Sci. 115(1) 49–60.

    Article  Google Scholar 

  • Sarkar S, Bose P K, Samanta P, Sengupta P and Eriksson G 2008 Microbial mat mediated structures in the Ediacaran Sonia Sandstone, Rajasthan, India, and their implications for Proterozoic sedimentation; Precamb. Res. 162 248–263.

    Article  Google Scholar 

  • Sarkar S, Samanta P, Mukhopadhyay S and Bose P K 2012 Stratigraphic architecture of the Sonia Fluvial interval, India in its Precambrian context; Precamb. Res. 214–215 210–226.

    Article  Google Scholar 

  • Schieber J 1999 Microbial mats in terrigenous clastics: The challenge of identification in the rock record; Palaios 14 3–12.

    Article  Google Scholar 

  • Schieber J, Bose P K, Eriksson P G, Banerjee S, Sarkar S, Altermann W and Catuneau O 2007 Atlas of microbial mat features preserved within the siliciclastic rock record; Atlases in Geosciences, Elsevier, 311p.

  • Siever R 1962 Silica solubility, 0°C–200°C, and the diagenesis of siliceous sediments; J. Geol. 70(2) 127–150.

    Article  Google Scholar 

  • Simonson B M 1987 Early silica cementation and subsequent diagenesis in arenites from four early Proterozoic iron formations of North America; J. Sedim. Petrol. 57 494–511.

    Google Scholar 

  • Skyring G W, Lynch R M and Smith G D 1989 Quantitative relationships between carbon, hydrogen and sulphur metabolism in cyanobacterial mats; In: Physiological Ecology of Benthic Microbial Communities (eds) Cohen C and Rosenberg E, Microbial Mats, American Society of Microbiology, pp. 170–179.

  • Theakstone W H 1981 Concretions in glacial sediments at seglvetnet, Norway; J. Sedim. Petrol. 51 191–196.

    Google Scholar 

  • Tucker M E and Wright V P 1990 Carbonate sedimentology; Blackwell Science, 422p.

  • Valdiya K S 1999 Marwar’s connection with the Himalayas; In: Geological Evolution of Northwestern India (ed.) Paliwal B S, Scientific Publishers India, pp. 1–18.

Download references

Acknowledgements

The authors thankfully acknowledge research funding from University of Delhi. Department of Geology, University of Delhi provided necessary infrastructure and instrumental facilities.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to PARTHA PRATIM CHAKRABORTY.

Rights and permissions

Reprints and permissions

About this article

Cite this article

SINGH, A., ANAND, V., PANDEY, P. et al. Nodular features from Proterozoic Sonia Sandstone, Jodhpur Group, Rajasthan: A litho-biotectonic perspective. J Earth Syst Sci 122, 309–320 (2013). https://doi.org/10.1007/s12040-013-0274-2

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12040-013-0274-2

Keywords

Navigation