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Stratigraphical and Palynological Appraisal of the Late Quaternary Mangrove Deposits of the West Coast of India

Published online by Cambridge University Press:  20 January 2017

K.P.N. Kumaran ,
K.M. Nair ,
Mahesh Shindikar ,
Ruta B. Limaye  and
D. Padmalal
K.P.N. Kumaran
Affiliation:
Palynology and Palaeoclimate Laboratory, Geology and Palaeontology Group, Agharkar Research Institute, Pune 411 004, India
K.M. Nair
Affiliation:
Vakkom Maulvi Foundation Trust, Thekkummodu Jn., Trivandrum, Kerala 695 037, India
Mahesh Shindikar
Affiliation:
Palynology and Palaeoclimate Laboratory, Geology and Palaeontology Group, Agharkar Research Institute, Pune 411 004, India
Ruta B. Limaye
Affiliation:
Palynology and Palaeoclimate Laboratory, Geology and Palaeontology Group, Agharkar Research Institute, Pune 411 004, India
D. Padmalal
Affiliation:
Centre for Earth Science Studies, Akkulam, Trivandrum, Kerala 695 031, India
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Abstract

The organic deposits derived from the mangrove swamps form reliable stratigraphic markers within the Late Quaternary sequence of Kerala–Konkan Basin. Three generations of such deposits have been identified. The older one is dated to around 43,000–40,000 14C yr B.P., with a few dates beyond the range of radiocarbon. The younger ones date from the Middle Holocene to latest Pleistocene (10,760–4540 14C yr B.P.) and the Late Holocene (<4000 14C yr B.P.). Pollen analyses confirm that the deposits are mostly derived from the mangrove vegetation. Peat accumulation during the period 40,000–28,000 14C yr B.P. can be correlated with the excess rainfall, 40–100% greater than modern values, of the Asian summer monsoon. The low occurrence of mangrove between 22,000 and 18,000 14C yr B.P. can be attributed to the prevailing aridity and/or reduced precipitation associated worldwide with Last Glacial Maximum, because exposure surfaces and ferruginous layers are commonly found in intervals representing this period. The high rainfall of 11,000–4000 14C yr B.P. is found to be the most significant as the mangrove reached an optimum growth around 11,000 14C yr B.P. but with periods of punctuated weaker monsoons. From the present and previous studies, it has been observed that after about 5000 or 4000 14C yr B.P., the monsoons became gradually reduced leading to drying up of many of the marginal marine mangrove ecosystems. A case study of Hadi profile provided an insight to the relevance of magnetic susceptibility (χ) to record the ecological shift in Late Holocene.

Keywords

Mangrove depositsStratigraphyPalynologyPalaeomonsoonPalaeoclimateEnvironmental magnetismWest Coast India
Type
Special issue articles
Information
Quaternary Research , Volume 64 , Issue 3 , November 2005 , pp. 418 - 431
Copyright
University of Washington

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References

Agrawal, D.P., Gupta, S.K., and Kusumgar, S. (1970). Radiocarbon dates of Quaternary Samples. Current Science 30, 219–222.Google Scholar
Basavaiah, N., and Khadkikar, A.S. (2004). Environmental magnetism and its application towards paleomonsoon reconstruction. The Journal of the Indian Geophysical Union 8, 1–14.Google Scholar
Blasco, F. (1975). The mangroves of India, Travaux de la Section Scientifique et Technique. French Institute of Pondicherry 14, 1–125.Google Scholar
Blasco, F. (1984). In: Mangroves ecosystem research methods. p.18–35. (eds. S.C., Snedaker and J.G., Snedaker), UNESCO, Paris.,36–49.Google Scholar
Caratini, C., Delibrias, G., and Rajagopalan, G. (1990). Palaeomangroves of Kanra coast, Karnataka, India and their implications on Late Pleistocene sea-level changes. Palaeobotanist 38, 370–378.Google Scholar
Caratini, C., Bentaleb, L., Fontigue, M., Morzadee Kerfourn, M.T., Pascal, J.P., and Tissot, C. (1994). A less humid climate since 3500 yr BP, from marine cores off Karwar, Western India. Palaeogeography, Palaeoclimatology, Palaeoecology 109, 371–384.Google Scholar
Deshpande, G.G. (1998). Geology of Maharashtra. Geological Society of India, Bangalore.223 Google Scholar
Erdtman, G. (1966). Pollen morphology and plant taxonomy. Angiosperms Hafner Publishing Company, New York.Corrected reprintGoogle Scholar
Faegri, K., and Iversen, J. (1975). Text Book of Pollen Analysis. Munksgaard, Copenhagen, Denmark.Google Scholar
Furukawa, K., and Wolanski, E. (1996). Sedimentation in mangrove forests. Mangroves and Salt Marshes 1, 3–10.CrossRefGoogle Scholar
Geetha, R., Sukumar, R., Ramesh, R., Pant, R.K., and Rajgopalan, G. (1997). Late Quternary vegetal and climatic changes from tropical peats in southern India, an extended record up to 40,000 yr B.P.. Current Science 73, 60–63.Google Scholar
Guinet, Ph. (1962). Pollen d' Asie tropicale. Travaux de la Section Scientifique et Technique. Institut Francais de Pondichery 5, 1–8.(52 pl)Google Scholar
Gupta, A.K., Anderson, D.M., and Overpeck, J.T. (2003). Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature 421, 354–357.Google Scholar
Jayalakshmi, K., Nair, K.M., Kumai, H., and Santosh, M. (2004). Late Pleistocene–Holocene palaeoclimatic history of the southern Kerala Basin, Southwest India. Gondwana Research 7, 585–594.Google Scholar
Kale, V.S., and Rajaguru, S.N. (1983). Mid-Holocene fossil woods from Colva, Goa. Current Science 52, 778–779.Google Scholar
Kale, V.S., Gupta, A., and Singhvi, A.K. (2003). Late Pleistocene Holocene palaeohydrology and monsoon Asia.Gregory, K.J., Benito, G. Palaeohydrology: Understanding Global Change John Wiley and Sons, New York.213–232.Google Scholar
Krauss, K.W., Allen, J.A., and Cahoon, D.R. (2003). Differential rates of vertical accretion and elevation change among aerial root types in Micronesian mangrove fossils. Estuarine Coastal Shelf Science 56, 251–259.Google Scholar
K.P.N., Kumaran (2001). Quaternary sea level oscillations, geological and geomorphological evolution of south Kerala sedimentary basin.Report on the palynological analysis of subsurface samples.DST project interim report 1–22 p.Google Scholar
Kumaran, K.P.N., and Nair, K.M. (2005). Tracing Palaeoclimatic signatures in fossil woods and sub-fossil logs of Kerala, Southwestern India. Pages News 13, 15–17.Google Scholar
Kumaran, K.P.N., Limaye, R.B., Rajshekhar, C., and Rajgopalan, G. (2001). Palynoflora and radiocarbon dates of Holocene deposits of Dhamapur, Sindhudurg District, Maharashtra. Current Science 80, 1331–1336.Google Scholar
Kumaran, K.P.N., Shindikar, M.R., and Mudgal, T.R. (2004a). )Floristic composition, palynology and sedimentary facies of Hadi mangrove swamp (Maharashtra). Journal of Indian Geophysical Union 8, 55–63.Google Scholar
Kumaran, K.P.N., Shindikar, M., and Limaye, R.B. (2004b). )Mangrove deposits as archives of palaeomonsoon records: the palynological assessment of the Late Quaternary deposits of West Coast of India. Polen 14, 246–247.Google Scholar
R.B., Limaye (2004). Contribution to Palaeopalynology and palaeoecology of the coastal deposits of Maharashtra, India.Ph.D. Dissertation,University of Pune, Pune.Google Scholar
Mascarenhas, A. (1997). Significance of peat on western continental shelf of India. Journal of Geological Society of India 49, 145–152.Google Scholar
Mascarenhas, A., Paropkari, A.L., Prakash Babu, (1993). On the possibility of allochthonons peat on the inner shelf off Karwar. Current Science 64, 684–687.Google Scholar
Moore, P.D., and Webb, J.A. (1978). An illustrated guide to Pollen analysis. Hodder and Stoughton, London.Google Scholar
Muller, J. (1981). Fossil pollen records of extant angiosperms. Botanical Review 47, 1–142.CrossRefGoogle Scholar
K.M., Nair, and Padmalal, D. (2003). Quaternary Sea level Oscillations, Geological and Geomorphological Evolution of South Kerala Sedimentary Basin.PCR ESS/23/VES/6/98; Report submitted to DST, GOI.,1–60. p.Google Scholar
K.M., Nair, Padmalal, D., K.P.N., Kumaran in press. Quaternary geology of south Kerala sedimentary basin–An outline.Journal of Geological Society of India.Google Scholar
Nayak, S., and Bahuguna, A. (2001). Application of remote sensing data to monitor mangroves and other coastal vegetation of India. Indian Journal of Marine Sciences 30, 195–213.Google Scholar
Nayar, T.S. (1990). Pollen flora of Maharashtra State, India. Today and Tomorrow's Printers and Publishers, New Delhi.15767 plGoogle Scholar
Nigam, R. (1993). Foraminifera and change pattern of monsoon rainfall. Current Science 64, 935–937.Google Scholar
Nigam, R., and Khare, N. (1999). Spatial and unequal distribution of foraminifers in sediments off the central west coast of India and use of their test morphologies for the reconstructions of palaeomonsoon precipitation. Micropalaeontology 45, 285–300.Google Scholar
Pandarinath, K., Shankar, R., and Yadava, M.G. (2001). Late Quaternary changes in sea level and sedimentation rate along the seacoast of India: evidence from radiocarbon dates. Current Science 81, 594–600.Google Scholar
S.D., Pawar, Venkatramana, B., Mathai, T., and Mallikarjuna, C. (1983). Systematic geological mapping around Chertallai–Vaikom–Aleppey–Kottayam and Panthalam in parts of Aleppey and Kottayam districts/Kerala state.Unpublished report,Geological Survey of India, .Google Scholar
Phadtare, N.R. (2000). Sharp decrease in summer monsoon strength 4000–3500 cal yr B.P. in the central Himalaya of India based on pollen evidences from offshore peat. Quaternary Research 53, 122–129.CrossRefGoogle Scholar
Quadros, G., and Athalye, R.P. (2002). Intertidal macrobenthos from Ulhas river estuary and Thane creek. Proceedings National Seminar on Creeks, Estuaries and Mangroves–Pollution and Conservation 216–222.Google Scholar
Rajendran, C.P., and Rajagopalan, G. (1989). Quaternary Geology of India : evidence from radiocarbon dates. Journal of Geological Society of India 33, 218–222.Google Scholar
Rajshekhar, C., and Kumaran, K.P.N. (1998). Micropalaeontological evidence for tectonic uplift of near-shore deposits around Bankot-Velas, Ratnagiri district, Maharashtra. Current Science 74, 705–708.Google Scholar
K.K., Ramchandran, Balsubramanian, G., Kurian, J., and Thomas, J. (1985). The mangrove ecosystem of Kerala, its mapping, inventory and some environmental aspects.Interim report–Centre for Earth Science studies,Trivandrum., pp. 1–52.Google Scholar
Sarkar, A., Ramesh, R., Somayajulu, B.G.K., Agnihotri, R., Jull, A.J.T., and Burr, G.S. (2000). High resolution Holocene monsoon record from the eastern Arabian Sea. Earth Planet Science Letters 177, 209–218.CrossRefGoogle Scholar
Selvam, V. (2003). Environmental classification of mangrove wetlands of India. Current Science 84, 757–765.Google Scholar
K.P., Shajan (1998). Studies on the Late Quaternary sediments and sea level changes of central Kerala coast, India.PhD thesis,Cochin University of Science and Technology, Kochi.Google Scholar
Shi, Y., Yu, G., Liu, X., Li, B., and Yao, T. (2001). Reconstruction of 30–40 Ka BP enhanced Indian climate based on geological records from the Tibet plateau. Plaeoclimatology, Palaeogeography, Palaeoecology 169, 69–83.Google Scholar
Shindikar, M., Limaye, R.B., Kumaran, K.P.N., and Gunale, V.R. (2004). Past and present mangrove flora along Konkan, West Coast, India. National seminar on ‘New Frontiers in Plant Taxonomy and Biodiversity Conservation’ Thiruvanathpuram, India 46AbstractGoogle Scholar
Sirocko, F., Sarnthein, M., Erienkeuser, H., Arnold, M., and Duplessy, J.C. (1993). Century-scale events in monsoonal climate over the past 24,000 years. Nature 364, 322–324.Google Scholar
Soman, K. (2002). Geology of Kerala. Geological Society of India, Bangalore.375 Google Scholar
Stuiver, M., and Pearson, G.W. (1993). High precision bidecadal calibration of the radiocarbon time scale, AD 1950–500 BC and 2500–6000 BC.Stuiver, M., Long, A., Kra, R.S. Calibration 1993 Radiocarbon vol. 35, 1–23.Google Scholar
Thanikaimoni, G. (1987). Mangrove Palynology. Travaux de la Section Scientifique et Technique. French Institute of Pondicherry 24, (100 pp.)Google Scholar
Thanikaimoni, G., Caratini, C., Venkatachala, B.S., Ramanujam, C.G.K., and Kar, R.K. (1984). Selected Tertiary angiosperm pollens from India and their relationship with African Tertiary pollen, Travaux de la Section Scientifique et Technique. French Institute of Pondicherry 19, (93 pp., 72. pl)Google Scholar
Thom, B.G. (1984). Coastal landforms and geomorphic processes.Snedaker, S.C., Snedaker, J.G. The Mangrove Ecosystem: Research Methods Unesco, 3–17.Google Scholar
Thompson, R., and Oldfield, F. (1986). Environmental Magnetism. Allen and Unwin, London.227 pp.Google Scholar
Tissot, C. (1990). Late Holocene environment in Coondapur area, Karnataka, Preliminary palynological results.Jain, K.P., Tiwari, R.S. Proceedings of Symposium Vistas in Indian Palaeobotany Palaeobotanist vol. 38, 348–358.Google Scholar
Tissot, C., Chikhi, H., and Nayar, T.S. (1994). Pollen of wet evergreen forests of the Western Ghats, India. Instuitut Francais de Pondichery 35, 133 pp.Google Scholar
Tomlinson, P.B. (1986). The Botany of Mangroves. Cambridge Univ. Press, U.K..Google Scholar
Traverse, A. (1988). Palaeo-Palynology. Unwin Hyman Publishers, London.Google Scholar
Untawale, A.G. (1987). Country Report–India.Umali, R.M. Mangrove Ecosystem of Asia and The Pacific: Status and Management UNESCO regional office, New Delhi 51–87.Google Scholar
E., Van Campo (1983). Palaeoclimatologie des bordures de la mer d' Arabie depuis 150,000 ana.Analysepollinique et stratigraphie isotopique. Thesis,Monpellier.Google Scholar
Van Campo, E. (1986). Monsoon fluctuations in two 20,000 yr B.P. Oxygen-isotope/pollen records off southwest India. Quaternary Research 26, 376–388.Google Scholar
Verosub, K.L., and Roberts, A.P. (1995). Environmental magnetism: past, present and future. Journal of Geophysical Research 100, 2175–2192.CrossRefGoogle Scholar
Vishnu-Mitre, , and Guzder, S.J. (1975). Stratigraphy and Palynology of the mangrove swamps of Bombay. Palaeobotanist 22, 111–117.Google Scholar
Williamson, D., Jelinowska, A., Kissel, C., Tucholka, P., Gilbert, E., Gasse, F., Massault, M., Taieb, M., Van Campo, E., and Wieckowski, K. (1998). Mineral magnetic proxies of erosion/oxidation cycles in tropical marr-like sediments (Lake Tritrivakely, Madagascar): palaeoenvironmental implications. Earth and Planetary Science Letters 155, 205–219.Google Scholar
Wolanski, E. (1995). Transport of sediment in mangrove swamps. Hydrobiologia 295, 31–42.Google Scholar
Yadava, M.G., and Ramesh, R. (1999). Palaeomonsoon record of the last 3400 years from speleothems of tropical India. Gondwana Geological Magazine 4, 141–156.Google Scholar