Abstract
Undisturbed marine sediment cores raised from the oceans hold continuous records of sedimentation and palaeoenvironmental changes, hence it is suitable material for reconstructing past climate fluctuations. In the present study a marine sediment core about 124 cm raised from a depth of 250 m, near the Landfall Island, North Andaman, Bay of Bengal (BOB) was used to reconstruct the south west monsoonal shifts over the Indian sub-continent and BOB during the mid to late Holocene by using various proxies such as clay mineralogy, oxygen (δ18O) and carbon (δ13C) stable isotopes, and nanoplankton. Five organic carbon sediment samples were radiocarbon dated. The calibrated radiocarbon date ranges in age from (6078 to 1658 years BP) that is from the mid to late Holocene period. The texture analysis indicates that the sediments are predominantly clayey silt in nature. Smectite, illite, kaolinite and chlorite were the clay minerals present in the sediment core in which smectite and illite are dominant. The high smectite content reflects the weathering product of mafic rock contributed from the nearby island whereas illite is predominantly coming from the rivers such as Irrawaddy, Salween and Sittang rivers from Myanmar. Occurrence of nanoplankton such as Gephyrocapsa oceanica, Emiliania huxleyi, and Ascidian spicules in the calcareous nanoplankton assemblage suggest a mixed source also from the sedimentary rocks of the Mio-Pliocene age. The sediment core reveals layers of coarser sand flux since ~6500–6000 years BP and ~3300 years BP that reflects a strengthened South West Monsoon (SWM) in an overall weakening of the SWM from the middle Holocene (6000 yrs BP) to the late Holocene period (2000 years BP). This is also inferred from the high smectite, high C/I ratio and low K/C ratio. Within this period, an intense weakening of the SWM is noticed at ~4400–4200 years BP (Sub—Boreal Optimum), which is also supported by the δ18O data of G. ruber becoming more positive from −3.39 to −2.33‰. A major wet phase was found reaching its maximum around 3400–3200 years BP and amelioration in climate ~2000 years BP with a warm dry phase ~2200–1800 years BP (Roman Warm Period) followed by the Medieval Warm Period (1000–800 years BP).
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Achyuthan H, Farooqui A, Gopal VEE, Phartiyal B, Lone AM (2017) Late Quaternary to Holocene southwest monsoon reconstruction: a review based on lake and wetland systems (studies carried out during 2011–2016). Proc Indian Nat Sci Acad 82(3):847–868
Ahmad T, Dragusanu V, Tanaka T (2008) Provenance of Proterozoic Basal Aravalli mafic volcanic rocks from Rajasthan, Northwestern India: Nd isotopes evidence for enriched mantle reservoirs. Precamb Resour 162:150–159
Ahmad SM, Zheng H, Raza W, Zhou B, Lone MA, Raza T, Suseela G (2012) Glacial to Holocene changes in the surface and deep waters of the northeast Indian Ocean. Mar Geol 329(331):16–23
Bar-Matthews M, Ayalon A, Kaufman A, Wasserburg GJ (1999) The eastern Mediterranean palaeoclimate as a reflection of regional events: Soreq Cave, Israel. Earth Planet Sci Lett 166:85–95
Bhushan R, Singh SK, Burr GS, Jull AJT (2007) Palaeoclimatic studies from sediments in the Bay of Bengal. In: Proceedings 12th ISMAS symposium cum workshop on mass spectrometry, IRP-3
Bianchi GG, McCave IN (1999) Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature 397(6719):515–517
Biscaye PE (1965) Mineralogy and sedimentation of recent deep-sea clays in the Atlantic Ocean and adjacent seas and oceans. Bull Geol Soc Am 76:803–832
Breitenbach SFM, Adkins JF, Meyer H, Marwan N, Kumar KK, Haug GH (2010) Strong influence of water vapor source dynamics on stable isotopes in precipitation observed in Southern Meghalaya, NE India. Earth Planet Sci Lett 292:212–220
Bukry D (1971) Calcareouss nanofossils’ Coccolith Stratigraphy leg 13, Deep sea drilling project, initial report. U. S. Geol Surv, La Jolla, California, pp 817–822
Carver RE (1971) Procedures in sediment petrol. Wiley and Sons. Inc., New York, p 653
Chauhan OS (2003) Past 20,000 years history of Himalayan aridity: evidence from the oxygen isotope record of Bay of Bengal. Curr Sci 84:90–93
Chauhan OS, Suneethi J (2001) 18 ka BP records of climatic changes, Bay of Bengal: isotopic and sedimentological evidences. Curr Sci 81:1231–1234
Chauhan OS, Vogelsang E (2006) Climate induced changes in the circulation and dispersal patterns of the fluvial sources during late quaternary in the middle Bengal Fan. J Earth Syst Sci 115(3):379–386
Chauhan OS, Borole DV, Gujar AR, Antonio M, Mislanker PG, Rao ChM (1993) Evidences of climatic variations during Late Pleistocene-Holocene in the eastern Bay of Bengal. Curr Sci 65(7):558–562
Chauhan OS, Jayakumar S, Menezes AAS, Rajawat AS, Nayak, SR (2006) Anomalous inland influx of the River Indus, Gulf of Kachchh, India. Mar Geol 229:91–100. https://doi.org/10.1016/j.margeo.2005.12.003
Chauhan OS, Patil SK, Suneethi J (2004) Fluvial influx and weathering history of the Himalayas since Last Glacial Maxima; isotopic, sedimentological and magnetic records from the Bay of Bengal. Curr Sci 87(4):509–515
Chauhan OS, Sukhija BS, Gujar AR, Nagabhushanam N, Paropkari AL (2000) Late quaternary variations in clay mineral along the SW continental margin of India: evidence of climatic variations. Geo Mar Lett 20:118–122. https://doi.org/10.1007/s003670000043
Colin C, Turpin L, Bertauz J, Despraries A, Kissel C (1999) Erosional history of the Himalayas and Burman ranges during the last two glacial-interglacial cycles. Earth Planet Sci Lett 171:647–660
Colin C, Turpin L, Blamart D, Frank N, Kissel C, Duchamp S (2006) Evolution of weathering patterns in the Indo-Burman ranges over the last 280 kyr: effects of sediment provenance on 87Sr/86Sr ratios tracer. Geochem Geophys Geosys 7(3):Q03007. https://doi.org/10.1029/2005GC000962
Contreras-Rosales A, Jennerjahn T, Tharammal T, Lückge A, Paul A, Schefuß E (2014) Evolution of the Indian Summer Monsoon and terrestrial vegetation in the Bengal region during the past 18 ka. Quat Sci Rev 102:133–148
Dash SK, Kumar JR, Shekhar MS (2004) On the decreasing frequency of monsoon depressions over the Indian region. Curr Sci 86:1404–1411
Desprat S, Sánchez-Goñi MF, Loutre MF (2003) Revealing climatic variability of the last three millennia in northwestern Iberia using pollen influx data. Earth and Planet Sci Lett 213:63–78
Ding YH (1994) Monsoons over China. Kluwer Academic Publishers, pp 432
Duplessy JG (1982) Glacial to interglacial contrast in the northern Indian Ocean. Nature 295:494–498
Eksambekar SP (2002) Contribution of the study of phytoliths to Bioarchaeology. Unpublished Ph.D. thesis, Deccan College PGRI (Deemed University), Pune, India
Enzel Y, Ely LL, Mishra S, Ramesh R, Amit R, Lazar B, Rajaguru SN, Baker VR, Sandler A (1999) High-resolution Holocene environmental changes in the Thar Desert. Northwestern India. Science 284(5411):125–128
Fleitmann D (2007) Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen (Socotra). Quat Sci Rev 26:170–188
Fleitmann D, Matter A (2009) The Speleothem record of climate variability in Southern Arabia. Comptes Rendus Geosci 341:633–642
Fleitmann D, Burns SJ, Mudelsee M, Neff N, Kramers J, Mangini A, Matter A (2003) Holocene forcing of the Indian monsoon recorded in a stalagmite from Southern Oman. Science 300:1737–1739
Fleitmann D, Burns SJ, Neff U, Mudelsee M, Mangini A, Matter A (2004) Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually laminated speleothems from Southern Oman. Quat Sci Rev 23:935–945
Giosan L, Orsi W, Collen MJL, Wuchter C, Dunlea AG, Thirumalai K, Munoz SE, Clift P, Fuller DQ (2018) Neoglacial climate Anomalies and the Harappan Metamorphosis. Climate Past, Under Rev. https://doi.org/10.5194/cp-2018-37
Gorsky G, Chertiennot-Dinet MJ, Blanchot J, Palazzoli I (1999) Picoplankton and nanoplankton aggregate on by appendicularian fecal pellet contents of Megalocercus huxleyi in the equatorial Pacific. J Geophys Oceans 104:3381–3390
Griffin RE (1968) Clay mineralogy. McGraw Hill, New York, p 565
Griffin WL, Zhang AD, O’Reilly SY, Ryan CG (1998) Phanerozoic evolution of the lithosphere beneath the Sino-Korean Craton. Mantle Dyn Plate Interact East Asia 27:107–126. In: Flower MFJ, Chung SL, Lo CH, Lee TY (eds) Amer Geophys Union, Geodynam Ser
Gupta AK, Thamban M (2008) Holocene Indian monsoon variability. Glimpses Geosci Res India, pp 28–31
Gupta AK, Anderson DM, Overpeck JT (2003) Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature 421:354–357
Hughes MK, Diaz HF (1994) Was there a ‘Medieval Warm Period. and if so, where and when. Clim Change 26:109–142
Jochem F (1989) Distribution and importance of autotrophic ultra-plankton in a boreal inshore area (Kiel Bight, Western Baltic). Marine Ecol Progr Ser 53:153–169
Kessarkar PM, Rao VP, Ahmad SM, Patil SK, Anil Kumar A, Anil Babu G, Chakraborty S, Soundar Rajan R (2005) Changing sedimentary environment during the Late Quaternary: sedimentological and isotopic evidence from the distal Bengal Fan. Deep Sea Res Part I 52:1591–1615
Kotlia BS, Ahmed SM, Zhao J, Raza W, Collerson KD, Joshi LM, Sanwal J (2012) Climatic fluctuations during the LIA and post-LIA in the Kumaun Lesser Himalaya, India: evidence from a 400 y old stalagmite record. Quat Intl 263:129–138
Krumbein WC, Pettijohn FJ (1938) Manual of sedimentary petrography. Appleton-Century-Crofts, Inc, New York
Kudrass HR, Hofman A, Doose H, Emeis K, Erlenkeuser H (2001) Modulation and amplification of climatic changes in the Northern Hemisphere by the Indian summer monsoon during the past 80 ky. Geology 29:63–66
Kuppusamy M, Ghosh P (2012) Cenozoic climatic record for monsoonal rainfall over the Indian region. Mod Climat. In: Wang SY (ed). In Tech. ISBN 978-953-51-0095-9. https://doi.org/10.5772/36206
Kurian S, Nath BN, Ramaswamy V, Naman D, Rao TG, Kamesh Raju KA, Selvaraj K, Chen CTA (2008) Possible detrital, diagenetic and hydrothermal sources for Holocene sediments of the Andaman backarc basin. Mar Geol 247:178–193
Laskar AH, Raghav S, Yadava MG, Jani RA, Narayana AC, Ramesh R (2011) Potential of stable carbon and oxygen isotope variations of speleothems from Andaman Islands, India, for paleomonsoon reconstruction. J Geolog Res 2011. https://doi.org/10.1155/2011/272971
Laskar AH, Yadava MG, Sharma N, Ramesh R (2013a) Late Holocene climate in the Lower Narmada valley, Gujarat, Western India, inferred using sedimentary carbon and oxygen isotope ratios. Holocene 23(8):1115–1122
Laskar AH, Yadava MG, Ramesh R, Polyak VJ, Asmerom Y (2013b) A 4 kyr stalagmite oxygen isotopic record of the past Indian Summer Monsoon in the Andaman Islands. Geochem Geophys Geosys 14(9):3555–3566
Liu ZT, Colin C, Trentesaux A, Blamart D, Bassinot F, Siani G, Sicre MA (2004) Erosional history of the eastern Tibetan Plateau over the past 190 kyr: clay mineralogical and geochemical investigations from the southwestern South China Sea. Mar Geol 209:1–18
Liu ZT, Colin C, Trentesaux A, Siani G, Frank N, Blamart D, Farid S (2005) Late quaternary climatic control on erosion and weathering in the eastern Tibetan Plateau and the Mekong Basin. Quat Resou 63(3):316–328
Loring DH, Rantala RTT (1992) Manual for the geochemical analyses of marine sediments and suspended particulate matter. Regional seas, reference methods for marine pollution studies, United Nations Environment Programme. Earth-Sci Rev 32(63):235–283
Lückge A, Doose‐Rolinski H, Khan AA, Schulz H, von Rad U (2001) Monsoonal variability in the northeastern Arabian Sea during the past 5000 years: geochemical evidence from laminated sediments. Palaeogeogr Palaeoclimatol Palaeoecol 167:273–286
Mann ME (2002a) Medieval climatic optimum, in Encyclopedia of global environmental change. In: MacCracken MC, Perry JS (eds) Wiley, Chichester, U.K, pp 514–516
Mann ME (2002b) Little ice age. In: MacCracken MC, Perry JS (eds) Wiley, Chichester, U.K, pp 504–509
Martinez-Cortizas A, Pontedevedra-Pombal X, Garcia-Rodeja E, Novoa-Munoz JC, Shotyk W (1999) Mercury in a Spanish peat bog archive of climate change and atmospheric metal deposition. Science 284:939–942
Masud Alam AKM, Xie S, Wallis LA (2009) Reconstructing late Holocene palaeoenvironments in Bangladesh: phytolith analysis of archaeological soils from Somapura Mahavihara site in the Paharpur area, Badalgacchi Upazila, Naogaon District, Bangladesh. J Archaeol Sci 36:504–512
Mathien E, Bassinot F (2008) Abrupt hydrographic changes in the Bay of Bengal during the Holocene. Geophys Res Abst, EGU2008-A-09423
Milliman JD, Meade RH (1983) World-wide delivery of river sediment to the oceans. J Geol 9:1–19
Moore GF, Curray JR, Emmel FJ (1982) Sedimentation in the Sunda trench and forearc region. Geol Soc London, Spl Publ 10:245–258. In: Legget JK (ed) Trench-forearc geology: sedimentation and tectonics on modern and ancient active plate margins
Morrill C, Overpeck JT, Cole JE (2003) A synthesis of abrupt changes in the Asian summer monsoon since the last deglaciation. Holocene 13:465–476
Naidu PD, Patil JS, Narale DD, Anil AC (2012) A first look at the dinoflagellate cysts abundance in the Bay of Bengal: implications on Late Quaternary productivity and climate change. Curr Sci 102(3):495–499
Nath BN, Gupta SM, Mislankar P.G, Rao BR, Parthiban G, Roelands I, Patil SK (2005) Evidence of Himalayan erosional event at approx. 0.5 Ma from a sediment core from the equatorial Indian ocean in the vicinity of ODP Leg 116 sites. Deep Sea Res 52(2):2061–2077
Nigam R, Hashimi NH (1995) Marine sediments and palaeoclimatic variations since the Late Pleistocene: an overview of Arabian sea. Mem Geol Soc India 32:380–390
Pal T, Chakraborty PP, Duttagupta T, Singh DC (2003) Geodynamic evolution of the outer-arc-forearc belt in the Andaman Islands, the central part of the Burma-Java subduction complex. Geol Mag 140(3):289–307
Pandey DN, Gupta AK, Anderson DM (2003) Rainwater harvesting as an adaptation to climate change. Curr Sci 85:46–59
Patnaik R, Gupta AK, Naidu PD, Yadav RR, Bhattacharyya A, Kumar M (2012) Indian Monsoon variability at different time scales: marine and terrestrial proxy records. Procs Indian Nat Sci Acad 78(3):535–547
Patterson WP, Dietrich KA, Holmden C, Andrews JT (2010) Two millennia of North Atlantic seasonality and implications for Norse colonies. Procs Nat Acad Sci USA 107(12):5306–5310
Phadtare NR (2000) Sharp decrease in summer monsoon strength 4000-3500 cal yr BP in the central Higher Himalaya of India based on pollen evidence from alpine peat. Quat Res 53:122–129
Piperno DR (1988) Phytolith analysis: an archaeological and geological perspective. Academic Press, New York, p 280
Ponton C, Giosan L, Eglinton TI, Fuller DQ, Johnson JE, Kumar P, Collett TS (2012) Holocene aridification of India. Geophys Res Lett 39:L03704. https://doi.org/10.1029/2011GL050722
Ramesh S, Ramasamy S (1997) Rare earth element geochemistry of a sediment core from lower Bengal Fan. J Geol Soc India 50:339–406
Rao VP (1983) Clay minerals in the sediments around the Andaman Islands. Indian J Mar Sci 12:17–20
Rao VP, Rao BR (1995) Provenance and distribution of clay minerals in the continental shelf and slope sediments of the west coast of India. Continental Shelf Res 15:1757–1771
Rashid H, England E, Thompson L, Polyak L (2011) Late Glacial to Holocene Indian Summer Monsoon variability based upon sediment records taken from the Bay of Bengal. Terrestrial Atmospheric Ocean Sci 22(2):215–228
Rashid H, Flower BP, Poore RZ, Quinn TM (2007) A ∼25 ka Indian Ocean monsoon variability record from the Andaman Sea. Quat Sci Rev 26:2586–2597
Ray D, Rajan S, Ravindra R, Jana A (2011) Microtextural and mineral chemical analyses of andesite-dacite from Barren and Narcondam islands: evidences for magma mixing and petrological implications. J Earth Syst Sci 120(1):145–155
Sarin MM, Borole DV, Krishnaswami S (1979) Geochemistry and geochronology of sediments from the Bay of Bengal and the equatorial Indian Ocean. Procs Indian Acad Sci 88:131–154
Sarkar S, Prasad S, Wilkes H, Niedel R, Stibich M, Basavaiah N, Sachse D (2015) Monsoon source shifts during the drying mid-Holocene: Biomarker isotope based evidence from the core ‘monsoon zone’ (CMZ) of India. Quaternary Sci Rev 123:144–157
Sarkar A, Ramesh R, Bhattacharya SK, Rajagopalan G (1990) Oxygen isotope evidence for a stronger winter monsoon current during the last glaciations. Nature 343:549–551
Sarkar A, Ramesh R, Somayajulu BLK, Agnihotri R, Jull AJT, Burr GS (2000) High resolution Holocene palaeomonsoon record from Eastern Arabian Sea. Earth Plan Sci Lett 177:209–218
Saxena A, Prasad V, Singh IB (2013) Holocene palaeoclimate reconstruction from the phytoliths of the lake-fill sequence of Ganga Plain. Curr Sci 104(8):1054–1062
Severdrup HU, Johnson MW, Fleming RH (1942) The oceans their physics, chemistry and general biology. Prentice Hall, New York, p 1087
Sharma S, Joachimski MM, Tobschall HJ, Singh IB, Sharma C, Chauhan MS (2006) Correlative evidence of monsoon variability, vegetation change and human habitation in Senai lake deposit, Ganga plain. Curr Sci 90:973–978
Sharma C, Chauhan MS, Gupta A, Rajagopalan G (1995) In: Symposium volume, “recent advances in geological studies of Northwest Himalaya and Foredeep”. Geological Survey of India, Lucknow, pp 90
Sharma MC, Owen LA (1996) Quaternary glacial history of the NW Garhwal, central Himalayas, India. Quat Sci Rev 15:335–365
Shepard F (1954) Nomenclature based on sand-silt-clay ratios. J Sed Petrol 24:151–158
Shetye SR, Shenoi SSC, Gouveia AD, Michael GS, Sundar D, Nampoothri G (1991) Wind driven coastal upwelling along the western boundary of the Bay of Bengal during southwest monsoon. Continental Shelf Res 11:1397–1408
Shetye SR, Gouveia A, Shenoi SSC, Sundar D, Michael GS, Nampoothri G (1993) The western boundary current in the seasonal subtropical gyre in the Bay of Bengal. J Geophys Res 98:945–954
Siby K, Nath BN, Ramaswamy V, Naman D, Gnaneshwar Rao T, Kamesh Raju KA, Selvaraj K, Chen CTA (2008) Possible detrital, diagenetic and hydrothermal sources for Holocene sediments of the Andaman backarc basin. Mar Geol 247(3–4):178–193
Singh G, Wasson RJ, Agrawal DP (1990) Vegetational and seasonal climate changes since last full glacial in the Thar Desert. Rev Palaeobot Palynol 64:351–358
Sinha A, Cannariato KG, Stott LD, Cheng H, Edwards RL, Yadava MG, Ramesh R, Singh IB (2007) A 900-year (600 to 1500 AD) record of the Indian summer monsoon precipitation from the core monsoon zone of India. Geophys Res Lett 34:L16707. https://doi.org/10.1029/2007GL030431
Sirocko F, Sarnthein M, Erlenkeuser H, Lange H, Arnold M, Duplessy JC (1993) Century scale events in monsoon climate over the past 24,000 years. Nature 364:322–324
Staubwasser M, Weiss H (2006) Holocene climate and cultural evolution in late prehistoric-early historic West Asia. Quat Res. https://doi.org/10.1016/j.yqres.2006.09.001
Stewart RA, Pilkey OH, Nelson BW (1965) Sediments of the Northern Arabian Sea. Mar Geol 3:411–427
Stuiver M, Reimer PJ (1993) Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35:215–230
Stuiver M, Reimer PJ, Reimer RW (2010) CALIB 6.0. Available online from http://calib.qub.ac.uk/calib
Subramanian V (1985) Geochemistry of river basins in the Indian Subcontinent, part I: water chemistry, chemical erosion and water-mineral equilibria. Transp Carbon Min Major World Rivers, Part 3 58: 495–512. In: Degens ET, Kempe S (eds) Mittilungen aus dem Geologisch-Palaeontologischen, Institut der Universitat Hamburg
Subramanian V (1993) Sediment load of Indian rivers. Curr Sci 64:928–930
Thamban M, Kawahata H, Rao VP (2007) Indian summer monsoon variability during the Holocene as recorded in sediments of the Arabian Sea: timing and implications. J Oceanogr 63:1009–1020
Thamban M, Rao VP, Schneider RR (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
Tiwari MR, Ramesh MG, Yadava BLK, Somayajulu AJ, Jull T, Burr S (2006) Is there a persistent control of monsoon winds by precipitation during the late Holocene. Geochem Geophys Geosys 7:Q03001. https://doi.org/10.1029/2005GC001095
Triantaphyllou MV, Antonarakou A, Dimiza M, Anagnostou C (2009) Calcareous nannofossil and planktonic foraminiferal distributional patterns during deposition of Sapropels S6, S5 and S1 in the Libyan Sea (Eastern Mediterranean). Geo-Mar Lett 30(1):1–13
Twiss PCA (2001) Curmudgeons view of Grass Phytolithology. Phytoliths: Appl Earth Sci Human History. In: Meunier JD, Colin F (eds) A. A. Balkema Publishers, Lisse, pp 7–25
Varkey MJ, Murty VSN, Suryanarayana A (1996) Physical oceanography of the Bay of Bengal and Andaman sea. Oceanogr Mar Biol 34:1–70
Vollweiler N, Scholz D, Muhlinghaus C, Mangini A, Spotl C (2006) A precisely dated climate record for the last 9 kyr from three high alpine stalagmites, Spannagel Cave, Austria. Geophys Res Lett 33:L20703. https://doi.org/10.1029/2006GL027662
Von Rad U, Schaaf M, Michels KH, Schulz HW, Berger H, Sirocko F (1999) A 5000-yr record of climate change in varved sediments from the oxygen minimum zone off Pakistan, Northeastern Arabian Sea. Quat Res 51:39–53
Wang PX (1999) Response of western Pacific marginal seas to glacial cycles: palaeoceanographic and sedimentological features. Mar Geol 16:5–39
Wang T, Surge D, Walker K Jo (2013) Seasonal climate change across the Roman Warm Period/Vandal Minimum transition using isotope sclerochronology in archaeological shells and otoliths, southwest Florida, USA. Quat Int 308–309:230–241. https://doi.org/10.1016/j.quaint.2012.11.013
Wang B, Wu R, Li T (2003) Atmosphere–warm ocean interaction and its impact on Asian-Australian monsoon variation. J Clim 16:1195–1211
Weaver CE (1989) Clays, muds and shales, vol 44. Developments in: Sedimentology. Elsevier, Amsterdam, p 819
Wei GJ, Liu Y, Li XH, Shao L, Liang X (2003) Climatic impact on Al, K, Sc and Ti in marine sediments: evidence from ODP site 1144, South China Sea. Geochem J 37:593–602
Werner JP, Wang J, Gómez-Navarro JJ, Steiger N, Neukom R (2019) No evidence for globally coherent warm and cold periods over the preindustrial Common Era. Nature 571:550–554. https://doi.org/10.1038/s41586-019-1401-2
Xiao JL, Wu JT, Si B, Liang WD, Nakamura T, Liu BL, Inouchi Y (2006) Holocene climate changes in the monsoon/arid transition reflected by carbon concentration in Daihai Lake of Inner Mongolia. Holocene 16:551–560
Xu H, Hong Y, Lin Q, Hong B, Jiang H, Zhu Y (2002) Temperature variations in the past 6000 years inferred from 618O of peat cellulose from Hongyuan, China. Chinese Sci Bull 7:1578–1584
Yadava MG, Ramesh R (2005) Monsoon reconstruction from radiocarbon dated tropical Indian Speleothem. Holocene 15:48–59
Yadava MG, Ramesh R, Pandarinath K (2007) A positive ‘amount effect’ in the Sahayadri (Western Ghats) rainfall. Curr Sci 93:560–564
Yang B, Braeuning A, Johnson KR, Yafeng S (2002) General characteristics of temperature variation in China during the last two millennia. Geophys Res Lett, vol 29. https://doi.org/10.1029/2001gl014485
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We thank Dr. Jyotiranjan Ray, PRL Ahmedabad for giving us an opportunity to submit this manuscript and the two anonymous reviewers who painstakingly read through our work and suggested constructive comments that helped in the presentation of our work.
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Nagasundaram, M., Achyuthan, H., Rai, J. (2020). Mid to Late Holocene Reconstruction of the Southwest Monsoonal Shifts Based on a Marine Sediment Core, off the Landfall Island, Bay of Bengal. In: Ray, J., Radhakrishna, M. (eds) The Andaman Islands and Adjoining Offshore: Geology, Tectonics and Palaeoclimate. Society of Earth Scientists Series. Springer, Cham. https://doi.org/10.1007/978-3-030-39843-9_15
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