Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Late Holocene Storm Records from Lower Reaches of Narmada Valley, Western India


Affiliations
1 Institute of Seismological Research, Gandhinagar - 382 009, India
2 Department of Geology, Wadia college, Pune - 411 001, India
3 Department of Geology, India
4 Department of Archaeology and Ancient History, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, India
     

   Subscribe/Renew Journal


Storms from the Arabian Sea are the most significant meteorological feature in western India that brings extreme rainy days together with catastrophic flooding. The present study reports two such palaeo-storm horizons at 1.16 m and 3.2 m above the present day water level in the Narmada channel, 56 km inland based on sedimentology and foraminiferal records. Both the horizons show similar sediment facies and foraminiferal assemblage. The present findings instigate to look for such new sites and build palaeo-storm records for western India.

Keywords

Palaeo-Storm, Late Holocene, Foraminifera, Flood Plain, Narmada Valley, Western India.
Subscription Login to verify subscription
User
Notifications
Font Size

  • CULVER, S. (1988) New foraminiferal depth zonation of the northwestern Gulf of Mexico. Palaios, v.3, pp.69-85.

  • EDWARDS, R. and HORTON, B. (2000) Reconstructing relative sea-level change using UK salt-marsh foraminifera. Marine Geol., v.169, pp.41-56.

  • FOLK, R.L. and WARD, W.C. (1957) Brazos River bar: a study in the significance of grain size parameters. Jour. Sediment. Petrol., v.27, pp.3-26.

  • FRIEDMAN, G.M. and SANDERS, J. 1978. Principles of Sedimentology, New York, Wiley.

  • FRONTALINI, F. and COCCIONI, R. (2008) Benthic foraminifera for heavy metal pollution monitoring: A case study from the central Adriatic Sea coast of Italy. Estuarine, Coastal and Shelf Science, v. 76, pp. 404-417.

  • GEBHARDT, H., KUHNT, W. and HOLBOURN, A. (2004) Foraminiferal response to sea level change, organic flux and oxygen deficiency in the Cenomanian of the Tarfaya Basin, southern Morocco. Marine Micropaleontology, v.53, pp.133-157.

  • GEHRELS, W. (1999) Middle and late Holocene sea-level changes in eastern Maine reconstructed from foraminiferal saltmarsh stratigraphy and AMS 14C dates on basal peat. Quaternary Res., v. 52, pp. 350-359.

  • GHOSH, A., SAHA, S., SARASWATI, P., BANERJEE, S. and BURLEY, S. (2009) Intertidal foraminifera in the macro-tidal estuaries of the Gulf of Cambay: Implications for interpreting sea-level change in palaeo-estuaries. Marine and Petroleum Geology, v.26, pp.1592-1599.

  • GHOSH, A., SAHA, S., SARASWATI, P. K., BANERJEE, S., BURLEY, S. and RAO, G. (2008) Gallitellia–a proxy for palaeo-monsoonal upwelling on the western coast of India? Curr. Sci., v.95, pp.1608-1611.

  • HALLOCK, P., LIDZ, B., COCKEY-BURKHARD, E. and DONNELLY, K. (2003) Foraminifera as bioindicators in coral reef assessment and monitoring: The FORAM Index. Environmental Monitoring and Assessment, v.81, pp.221-238.

  • HAYWARD, B.W., GRENFELL, H.R., SABAA, A.T. and KAY, J. (2010) Using foraminiferal faunas as proxies for low tide level in the estimation of Holocene tectonic subsidence, New Zealand. Marine Micropaleontology, v.76, pp.23-36.

  • HORTON, B.P., EDWARDS, R.J. and LLOYD, J.M. (1999) UK intertidal foraminiferal distributions: implications for sea-level studies. Marine Micropaleontology, v.36, pp.205-223.

  • MASSEY, A., GEHRELS, W., CHARMAN, D. and WHITE, S. (2006) An intertidal foraminifera-based transfer function for reconstructing Holocene sea-level change in southwest England. Jour. Foraminiferal Res, v.36, pp.215.

  • RAJ, R. and YADAVA, M. G. (2009) Late Holocene uplift in the lower Narmada basin, western India. Curr. Sci., v.96, pp.985-988.

  • SCHAFER, C. (2000) Monitoring nearshore marine environments using benthic foraminifera: some protocols and pitfalls. Micropaleontology, v.46, pp.161-169.

  • SUKUMARAN, P., SANT, D. A., KRISHNAN, K. and RANGARAJAN, G. (2012) High Resolution Facies record on Late Holocene Flood Plain Sediments from Lower reaches of Narmada Valley, Western India. Jour. Geol. Soc. India, v.79, pp.41-52.

  • WOODROFFE, S. (2009) Recognising subtidal foraminiferal assemblages: implications for quantitative sea-level reconstructions using a foraminifera-based transfer function. Jour. Quaternary Sci., v. 24, pp. 215-223.

  • ZERVAS, D., NICHOLS, G. J., HALL, R., SMYTH, H. R., LNTHJE, C. and MURTAGH, F. (2009) SedLog: A shareware program for drawing graphic logs and log data manipulation. Computers and Geosciences, v. 35, pp. 2151-2159.


Abstract Views: 724

PDF Views: 0




  • Late Holocene Storm Records from Lower Reaches of Narmada Valley, Western India

Abstract Views: 724  |  PDF Views: 0

Authors

Prabhin Sukumaran
Institute of Seismological Research, Gandhinagar - 382 009, India
C. Rajshekhar
Department of Geology, Wadia college, Pune - 411 001, India
Dhananjay A. Sant
Department of Geology, India
K. Krishnan
Department of Archaeology and Ancient History, The Maharaja Sayajirao University of Baroda, Vadodara - 390 002, India

Abstract


Storms from the Arabian Sea are the most significant meteorological feature in western India that brings extreme rainy days together with catastrophic flooding. The present study reports two such palaeo-storm horizons at 1.16 m and 3.2 m above the present day water level in the Narmada channel, 56 km inland based on sedimentology and foraminiferal records. Both the horizons show similar sediment facies and foraminiferal assemblage. The present findings instigate to look for such new sites and build palaeo-storm records for western India.

Keywords


Palaeo-Storm, Late Holocene, Foraminifera, Flood Plain, Narmada Valley, Western India.

References