Date: 12 Feb 2013
Paleoenvironmental significance of clay mineral assemblages in the southeastern Arabian Sea during last 30 kyr
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A gravity core SK-221 recovered from the southeastern Arabian Sea near Laccadive–Chagos Ridge was examined to identify the sources of detrital clay minerals and to decipher paleoenvironmental changes for the last 30 kyr. The clay mineral assemblages predominantly consist of illite, kaolinite and chlorite with small amounts of smectite. Quartz, feldspar and occasionally gibbsite are the clay-sized non-clay minerals present in the examined section. The detrital clay minerals primarily originated from the hinterland and were supplied to the present site by the numerous small rivers draining western India during preglacial and Holocene periods, and partly by the strong reworking of Indian continental shelf during glacial period. The low values of humidity proxies (kaolinite content, kaolinite to illite and smectite to illite ratios) and better illite crystallinity indicate relatively weak summer monsoon condition that resulted in reduced chemical weathering during glacial period, which was interrupted by a discrete event of winter monsoon intensification at ~20–17 ka. The increased kaolinite content, higher values of humidity indices and poorer illite crystallinity reflect high humidity that resulted in strong hydrolysis activity during the preglacial and Holocene periods. The increased CaCO3 during above periods also indicates less terrigenous dilution and intensified southwest monsoon-led upwelling which result in higher surface biogenic productivity. The characteristic clay mineral associations broadly suggest dry to semi-drier conditions during Heinrich Events H1, H2, and H3 and also during Younger Dryas. The low values of biogenic carbonate and organic carbon also indicate low productivity associated with weak summer monsoons during Heinrich Events. Abrupt increased humidity was recorded at 15–12.7 ka (Bølling/Allerød Event) sandwiched between two lows of Heinrich Events. Cycles of millennial timescale variations 2300, 1800, 1300 and 1000 yr have been observed from the clay mineralogical data. All the cycles observed in the monsoonal climate appear to be part of global oscillations.
Adatte T, Keller G and Stinnesbeck W 2002 Late Cretaceous to early Paleocene climate and sea-level fluctuations: The Tunisian record; Palaeogeogr. Palaeoclimatol. Palaeoecol. 178 165–196.CrossRef
Alley R B, Mayewski P A, Sowers T, Stuiver M, Taylor K C and Clark P U 1997 Holocene climatic instability: A prominent, widespread event 8200 years ago; Geology 25 483–486.CrossRef
Banakar V K, Oba T, Chodankar A R, Kuramoto T, Yamamoto M and Minagawa M 2005 Monsoon related changes in sea surface productivity and water column denitrification in the eastern Arabian Sea during the last glacial cycle; Mar. Geol. 219 99–108.CrossRef
Birkeland P W 1984 Soils and geomorphology (New York: Oxford University Press), 372p.
Biscaye P E 1965 Mineralogy and sedimentation of deep sea clay in the Atlantic Ocean and adjacent sea and oceans; Bull. Geol. Soc. Am. 76 803–832.CrossRef
Cayre O and Bard E 1999 Planktonic foraminiferal and alkenone records of the Last Deglaciation from the Eastern Arabian Sea; Quat. Res. 52 337–342.CrossRef
Chamley H 1989 Clay sedimentology (Berlin: Springer-Verlag), 623p.
Chamley H 1997 Clay mineral sedimentation in the ocean; In: Soils and sediments, mineralogy and geochemistry (eds) Paquet H and Clauer N (Berlin, New York: Springer), pp. 269–302.CrossRef
Chauhan O S 1994 Influence of macrotidal environment on shelf sedimentation, Gulf of Kachchh, India; Cont. Shelf Res. 14 1477–1493.CrossRef
Chauhan O S and Gujar A R 1996 Surficial clay mineral distribution on the southwestern continental margin of India: Evidence of input from the Bay of Bengal; Cont. Shelf Res. 16 321–333.CrossRef
Cullen J L and Prell W L 1984 Planktonic foraminifera of the Northern Indian Ocean: Distribution and preservation in surface sediments; Mar. Micropaleontol. 9 1–52.CrossRef
Das S S, Maurya A S, Pandey A C, Uday Bhan and Rai A K 2008 Influence of sediment source and monsoonal variations on the late Quaternary clay mineral assemblages at ODP site 728A, northwestern Arabian Sea; Curr. Sci. 95 1320–1326.
Debrabant P, Krissek L, Bouquillon A and Chamley H 1991 Clay mineralogy of Neogene sediments of the western Arabian Sea: Mineral abundances and palaeoenvironmental implications; In: Proceedings ODP, Scientific Results, Leg#117 (eds) Prell W L et al., College Station, TX, pp. 183–196.
Deepthy R and Balakrishnan S 2005 Climatic control on clay mineral formation: Evidence from weathering profiles developed on either side of the Western Ghats; J. Earth Syst. Sci. 114 545–556.CrossRef
Dou Y, Yang S, Liu Z, Clift P D, Yu H, Berne S and Shi X 2010 Clay mineral evolution in the central Okinawa Trough since 28 ka: Implications for sediment provenance and paleoenvironmental change; Palaeogeogr. Palaeoclimatol. Palaeoecol. 288 108–117.CrossRef
Duplessy J C 1982 Glacial to interglacial contrast in the northern Indian Ocean; Nature 295 494–498.CrossRef
Dutta K, Bhushan R and Somayajulu B L K 2001 Δ-R correction values in the Northern Indian Ocean; Radiocarbon 43(2a) 483–488.
Eglinton G, Bradshaw S, Resell A, Sarnthein M, Pflaumann U and Tiedemann R 1992 Molecular record of secular sea surface temperature changes on 100-year timescales for glacial terminations I, II and IV; Nature 356 423–426.CrossRef
Ehrmann W, Schmiedl G, Hamann Y, Kuhnt T, Hembleben C and Siebel W 2007 Clay minerals in late glacial and Holocene sediments of the northern and southern Aegean Sea; Palaeogeogr. Palaeoclimatol. Palaeoecol. 249 36–57.CrossRef
Emeis K C, Anderson D M, Doose H, Kroon D and Schultz-Bull D 1995 Sea-surface temperature and history of monsoon upwelling in the northwest Arabian Sea during the last 500,000 years; Quat. Res. 43 355–361.CrossRef
Esquevin J 1969 Influence de la composition chimique des illites sur le cristllinite; Bull. Centre Rechcherche Pau – SNPA 3 147–154.
Fairbanks R G 1992 Barbados sea level and Th/U 14C calibration; IGBP PAGES/World Data Center-A for Paleoclimatology Data Contribution Series 92-020. NOAA/NGDC Paleoclimatology Program, Boulder, CO.
Gaudette H E, Flight W R, Toner L and Folger D W 1974 An inexpensive titration method for the determination of organic carbon in recent sediments; J. Sedim. Petrol. 44 249–253.
Gingele F X 1996 Holocene climatic optimum in southwest Africa – Evidence from the marine clay mineral record; Palaeogeogr. Palaeoclimatol. Palaeoecol. 122 77–87.CrossRef
Griffin J, Windom H and Goldberg E D 1968 The distribution of clay minerals in the word ocean; Deep-Sea Res. 15 433–459.
Grim R E 1968 Clay mineralogy (New York: McGraw Hill), 596p.
Gunnel Y 2001a Dynamics and kinematics of rifting and uplift at the western continental margin of India: Insights from geophysical and numerical models; In: Sahyadri: The great escarpment of the Indian subcontinent (eds) Gunnell Y and Radhakrishna B P, Geol. Soc. India Memoir 47 475–496.
Gunnel Y 2001b Environmental changes in the Western Ghats during the Quaternary; In: Sahyadri: The great escarpment of the Indian subcontinent (eds) Gunnell Y and Radhakrishna B P, Geol. Soc. India Memoir 47 817–832.
Gunnell Y and Radhakrishna B P (eds) 2001 Sahyadri: The great escarpment of the Indian subcontinent, Geol. Soc. India Memoir 47 1054p.
Gupta A K 2010 Evolution of the Indian monsoon since late Miocene intensification – marine and land proxy records; J. Paleontol. Soc. India 55 1–9.
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.CrossRef
Gupta M V S, Naidu P D, Haake B G and Schiebel R 2005 Carbonate and carbon fluctuations in the eastern Arabian Sea over 140 ka: Implications on productivity changes; Deep-Sea Res. II 52 1981–1993.CrossRef
Hagelberg T K, Bond G and deMenocal P 1994 Milankovitch band forcing of sub-Milankovitch climate variability during the Pleistocene; Paleoceanography 9 545–558.CrossRef
Honjo S, Dymond D, Prell W L and Ittekkot V 1999 Monsoon controlled export fluxes to the interior of the Arabian Sea; U.S. JGOFS 1994–95 Experiment; Deep-Sea Res. II 46 1859–1902.CrossRef
Hughen K A, Baillie M G L and Bard E 2004 Marine radiocarbon age calibration, 0–26 cal kyr BP; Radiocarbon 46 1059–1086.
Ivanova E, Schiebel R, Singh A D, Schmied G, Niebler H S and Hemleben Ch 2003 Primary production in the Arabian Sea during the last 135,000 years; Palaeogeogr. Palaeoclimatol. Palaeoecol. 197 61–82.CrossRef
Kale V S and Shejwalkar N 2007 Western Ghat escarpment evolution in the Deccan Basalt Province: Geomorphic observations based on DEM analysis; J. Geol. Soc. India 70 459–473.
Kale V S and Shejwalkar N 2008 Uplift along the western margin of the Deccan Basalt Province: Is there any geomorphometric evidence?; J. Earth Syst. Sci. 117 959–971.CrossRef
Kessarkar P M, Rao V P, Ahmad S M and Anil Babu G 2003 Clay minerals and Sr–Nd isotopes of the sediments along the western margin of India and their implication for sediment provenance; Mar. Geol. 202 55–69.CrossRef
Kolla V, Henderson L and Biscaye P E 1976 Clay mineralogy and sedimentation in the western Indian Ocean; Deep-Sea Res. Oceanogr. Abstr. 23/10 949–961.CrossRef
Kolla V, Kostecki J A, Robinson F, Biscaye P and Ray P K 1981 Distribution and origin of clay minerals and quartz in surface sediments of the Arabian Sea; J. Sedim. Petrol. 51 563–569.
Mallison D J, Flower B, Hine A, Brooks G and Garza R M 2003 Paleoclimatic implications of high latitude precession scale mineralogic fluctuations during early Oligocene Antarctic glaciation: The Great Australian Bight record; Global Planet. Change 39 257–269.CrossRef
Mommersteeg H J P M, Loutre M F, Baert E and Berger A 1998 Orbital forcing and cyclic abrupt climatic change during the last 170,000 years. Evidence from high resolution palynological records of the Colombian eastern Cordillera, In: Vegetation development and cyclic and abrupt climatic change during Late Quaternary (ed.) Mommersteeg H J P M, Unpublished Ph.D. thesis, University of Amsterdam.
Moore D M and Reynolds R C Jr 1997 X-ray diffraction and the identification and analysis of clay minerals, 2nd edn (Oxford: Oxford University Press), 378p.
Naidu P D 1991 Glacial to interglacial contrasts in the calcium carbonate content and influence of Indus discharge in two eastern Arabian Sea cores; Palaeogeogr. Palaeoclimatol. Palaeoecol. 86 255–263.CrossRef
Naidu P D and Malmgren B A 1995 A 2200 years periodicity in the Asian Monsoon System; Geophys. Res. Lett. 22 2361–2364.CrossRef
Naidu P D and Malmgren B A 1996 A high-resolution record of late Quaternary upwelling along the Oman margin, Arabian Sea, based on planktic foraminifera; Paleoceanography 11 129–140.CrossRef
Naidu P D and Malmgren B A 1999 Quaternary carbonate record from the equatorial Indian Ocean and its relationship with productivity changes. Mar. Geol. 161 49–62.CrossRef
Naidu A S and Shankar R 1999 Palaeomonsoon history during Late Quaternary: Results of a pilot study on sediments from the Laccadive trough southeastern Arabian Sea; J. Geol. Soc. India 53 401–406.
Naidu P D, Malmgren B A and Bornmalm L 1993 Quaternary history of calcium carbonate fluctuations in the western equatorial Indian Ocean (Somali Basin); Paleogeogr. Paleoclimatol. Paleoecol. 103 21–30.CrossRef
Nair A M and Mathai T 1981 Geochemical trends in some laterite profiles of north Kerala; In: Proc. Intr. Sem. Lateritisation processes (Trivandrum-1979) (New Delhi: Oxford and IBH Publishing Co.), pp. 114–119.
Nair R R, Hashimi N H and Rao V P 1982a On the possibility of high velocity tidal streams as dynamic barriers to longshore sediment transport: Evidence from the continental shelf of the Gulf of Kutch, India; Mar. Geol. 47 77–86.CrossRef
Nair R R, Hashimi N H and Rao V P 1982b Distribution and dispersal of clay minerals on the western continental shelf of India; Mar. Geol. 50 Ml–M9.CrossRef
Nair R R, Ittekot V, Manganini S J, Ramswamy V, Haake B, Degens E T, Desai B N and Honjo S 1989 Increased particle fluxes to the oceans related to the monsoons; Nature 338 749–751.CrossRef
Narayana A C, Naidu P D, Shinu N, Nagabhushanam P and Sukhija B S 2009 Carbonate and organic carbon content changes over last 20 ka in the southeastern Arabian Sea: Paleoceanographic implications; Quat. Int. 206 72–77.CrossRef
Oba T 1969 Science Report, 2nd Series (Geology) (2) Biostratigraphy and isotopic paleotemperature of some deep-sea cores from the Indian Ocean; Tohoka University, 41 129–195.
Pattan J N, Masuzawa T, Naidu P D, Parthiban G and Yamamoto M 2003 Productivity fluctuations in the southeastern Arabian Sea during the last 140 ka; Paleogeogr. Paleoclimatol. Paleoecol. 193 575–590.CrossRef
Pattan J N, Masuzawa T and Yamamoto M 2005 Variations in terrigenous sediment discharge in a sediment core from southeastern Arabian Sea during the last 140 ka; Curr. Sci. 89 1421–1425.
Pederson T, Shimmield G B and Price N B 1992 Lack of enhanced preservation of organic matter in sediments under the oxygen minimum on the Oman Margin; Geochim. Cosmochim. Acta 56 545–551.CrossRef
Pestiaux P, van der Mersch I, Berger A and Duplessy J C 1988 Paleoclimate variability at frequencies ranging from 1 cycle per 10,000 years to 1 cycle per 1000 years: Evidence for nonlinear behaviour of the climate system; Climatic Change 12 9–37.CrossRef
Peterson L C and Prell W L 1985 Carbonate preservation and rates of climatic change: An 800 ka record from the Indian Ocean. In: The carbon cycle and atmospheric CO 2 : Natural variations Archean to present (eds) Sundquist E and Broecker W S, Geophysical Monograph Series. American Geophysical Union, Washington D.C., 32 251–270.CrossRef
Prabhu C N and Shankar R 2005 Palaeoproductivity of the eastern Arabian Sea during the past 200 ka: A multi-proxy investigation; Deep-Sea Res. II 52 1994–2002.CrossRef
Prell W L 1984 Variation of monsoonal upwelling: A response to changing solar radiation; In: Climate processes and climate sensitivity (eds) Hansen J E and Takahashi T, Geophysical Monograph, American Geophysical Union, Washington, D.C., pp. 48–57.CrossRef
Prell W L, Hutson W H, Williams D F, Allan W H, Geitzenauer B K and Molfino B 1980 Surface circulation of the Indian Ocean during the last glacial maximum, approximately 18,000 yr B.P., Quat. Res. 14 309–336.CrossRef
Rai A K and Das S S 2011 Late Quaternary changes in surface productivity and oxygen minimum zone (OMZ) in the northwestern Arabian Sea: Micropaleontologic and sedimentary record at ODP site 728A; J. Earth Syst. Sci. 120 113–121.CrossRef
Rajamani V, Tripathi J K and Malviya V 2009 Weathering of lower crustal rocks in the Kaveri river catchment, southern India: Implication to sediment geochemistry; Chem. Geol. 265 410–419.CrossRef
Rao V P and Rao B R 1995 Provenance and distribtuion of clay minerals in the sediments of the western continental shelf and slope of India; Cont. Shelf Res. 15 1757–1771.CrossRef
Rao V P and Wagle B G 1997 Geomorphology and surficial geology of the western continental shelf and slope of India: A review; Curr. Sci. 73 330–350.
Rea D K and Leinen M 1988 Asian aridity and the zonal westerlies: Late Pleistocene and Holocene record of eolian deposition in the Northwest Pacific Ocean; Palaeogeogr. Palaeoclimatol. Palaeoecol. 66 1–8.CrossRef
Robert C and Kennett J P 1997 Antarctic continental weathering changes during Eocene–Oligocene cryosphere expansion: Clay mineral and oxygen isotope evidence; Geology 25 587–590.CrossRef
Rostek F, Bard E, Beafort L, Sonzogni C and Ganssen G 1997 Sea surface temperature and productivity record for the past 240 ka in the Arabian Sea; Deep-Sea Res. II 44 1461–1480.CrossRef
Schulte S, Rostek F, Bard E, Rullkotter J and Marchal O 1999 Variation of oxygen minimum and primary productivity recorded in sediments of the Arabian Sea; Earth Planet. Sci. Lett. 177 209–218.
Schulz M and Stattegger K 1997 Spectrum: Spectral analysis of unevenly spaced paleoclimatic time series; Comput. Geosci. 23(9) 929–945.CrossRef
Shetye S R, Gouveia A D, Shenoi S S C, Sunder D, Michael G S, Almeida A M and Santanam K 1990 Hydrography and circulation of the west coast of India during the southwest monsoon 1987; J. Mar. Res. 48 359–378.CrossRef
Shimmield G B, Mowbray S R and Weedon G P 1990 A 350 ka history of the Indian southwest monsoon: Evidence from deep sea cores, northwest Arabian Sea; Transactions of the Royal Society of Edinburgh; Earth Sci. 81 289–299.
Singer A 1984 The palaeoclimatic interpretation of clay minerals in sediments – a review; Earth Sci. Rev. 21 251–293.CrossRef
Singh A D, Kroon D and Ganeshram R S 2006 Millennial scale variations in productivity and OMZ intensity in the eastern Arabian Sea; J. Geol. Soc. India 68 369–377.
Singh A D, Jung S J A, Darling K, Geneshram R S, Ivanochko T and Kroon D 2011 Productivity collapses in the Arabian Sea during glacial cold phases; Paleoceanography; doi: 10.1029/2009PA001923.
Sirocko F and Lange H 1991 Clay accumulation rates in the Arabian Sea during the late Quaternary; Mar. Geol. 97 105–119.CrossRef
Sirocko F, Garbe-Schonberg D, McIntyre A and Molfino B 1996 Teleconnections between the subtropical monsoons and high-latitude climates during the last deglaciation; Science 272 526–529.CrossRef
Sirocko F, Garbe-Schönberg D and Devey C 2000 Processes controlling trace element geochemistry of Arabian Sea sediments during the last 25,000 years; Global Planet. Change 26 217–303.CrossRef
Southon J, Kashgarian M, Fontugne M, Metivier B and Yim W W S 2002 Marine reservoir corrections for the Indian Ocean and Southeast Asia; Radiocarbon 44 167–180.
Spaulding S A and Oba T 1992 Association of late Pleistocene Calcareous Nannofossil Assemblages and 18O and 13C Isotopic Changes, ODP Leg 117, Oman Margin, Arabian Sea. Memoirs Science – Geology, University of Padova XLIII, pp. 389–407.
Steinke S, Hanebuth T J J, Vogt C and Stattegger K 2008 Sea level induced variations in clay mineral composition in the southwestern South China Sea over the past 17000 yr; Mar. Geol. 250 199–210.CrossRef
Stuiver M and Polach H A 1977 Discussion: Reporting of 14C data; Radiocarbon 19(3) 355–363.
Stuiver M and Reimer P J 1993 Extended 14C database and revised CALIB radiocarbon calibration program; Radiocarbon 35 215–230.
Stuiver M, Branziunas T F, Becker B and Kromer B 1991 Climatic, solar, oceanic, and geomagnetic influences on late-glacial and holocene atmospheric 14C12C change; Quat. Res. 35 1–24.CrossRef
Thamban M, Rao V P, Schneider R and Grootes P M 2001 Glacial to Holocene fluctuations in hydrography and productivity along the southwestern continental margin of India; Paleogeogr. Paleoclimatol. Paleoecol. 165 113–127.CrossRef
Thamban M, Rao V P and Schneider R R 2002 Reconstruction of late Quaternary monsoon oscillations based on clay mineral proxies using sediment cores from the western margin of India; Mar. Geol. 186 527–539.CrossRef
Thiry M 2000 Palaeoclimatic interpretation of clay minerals in marine deposits: An outlook from the continental origin; Earth Sci. Rev. 49 201–221.CrossRef
Tripathi J K and Rajamani V 2007 Geochemistry and origin of ferruginous nodules in weathered granodioritic gneisses, Mysore plateau, southern India; Geochim. Cosmochim. Acta 71 1674–1688.CrossRef
Valdiya K S 2001 Tectonic resurgence of the Mysore plateau and surrounding regions in cratonic southern India; Curr. Sci. 81 1068–1090.
Valdiya K S and Narayana A C 2007 River response to neotectonic activity: Example from Kerala, India; J. Geol. Soc. India 70 427–443.
Van Campo E 1986 Monsoon fluctuations in two 20 000 yr B.P. Oxygen-isotope/pollen records off southwest India; Quat. Res. 26 376–388.CrossRef
Van Campo E, Duplessy J C and Rossgnol-Strick M 1982 Climatic conditions deduced from a 150 ky. Oxygen isotope–pollen record from Arabian Sea; Nature 296 56–59.CrossRef
von Rad U, Schulz H, Riech V, den Dulk M, Berner U and Sirocko F 1999 Multiple monsoon-controlled breakdown of oxygen-minimum conditions during the past 30,000 years documented in laminated sediments off Pakistan; Palaeogeogr. Palaeoclimatol. Palaeoecol. 152 129–161.CrossRef
White A F and Blum A E 1995 Effects of climate on chemical weathering in watersheds; Geochim. Cosmochim. Acta 59 1729–1747.CrossRef
Zhifei L, Trentesaux A and Clemens S C 2003 Quaternary clay mineralogy in the northern South China Sea (ODP site 1146): Implications for oceanic current transport and east Asian monsoon evolution; Sci. China (series D) 46/12 1223–1235.
- Paleoenvironmental significance of clay mineral assemblages in the southeastern Arabian Sea during last 30 kyr
Journal of Earth System Science
Volume 122, Issue 1 , pp 173-185
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- Author Affiliations
- 1. Department of Earth & Planetary Sciences, University of Allahabad, Allahabad, 211 002, India
- 2. Department of Ocean & Atmospheric Studies, University of Allahabad, Allahabad, 211 002, India
- 3. Institute of Physics, Bhubaneswar, 751 005, India
- 4. University of Minnesota, Duluth, MN, 55812, USA
- 5. University of Georgia, Athens, GA, 30602, USA