Abstract
A sediment gravity core recovered from the North-Eastern Arabian Sea was investigated for sediment grain size, total organic carbon (TOC) and selected trace metals to understand the changes in the depositional environment over time. The core exhibited three distinct zones of sediment, the lower zone I, middle zone II and upper zone III, representing the varying conditions of sediment deposition. The lower zone is dominated by the silt-sized fraction with low organic carbon that revealed a shallow depositional environment and led to oxidation of organic matter, while the low metal concentration in this zone was either due to the low intensity of monsoon or the dilution by biogenic components and aeolian sediment influx. On other hand, the middle zone represented a transition phase where metal along with clay and organic carbon concentration started increasing due to strengthening monsoon intensity. Further, the upper zone that represented the Holocene sediments pointed to the increase in concentration of metals Al, Fe, Co and Cu that indicated an increase in the intensity of the South-West Monsoon and led to large fluvial inputs. TOC also increased towards the surface, indicating an increase in productivity that was controlled by South-West Monsoon.
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Agnihotri R, Sarin MM, Somayajulu BLK, Jull AT, Burr GS (2003) Late Quaternary biogenic productivity and organic carbon deposition in the eastern Arabian Sea. Palaeogeogr Palaeoclimatol Palaeoecol 197(1):43–60
Alagarsamy R, Zhang J (2005) Comparative studies on trace metal geochemistry in Indian and Chinese rivers. Curr Sci 89:299–309
Avinash K, Manjunath BR, Kurian PJ (2015) Glacial–interglacial productivity contrasts along the eastern Arabian Sea: dominance of convective mixing over upwelling. Geosci Front 6(6):913–925
Avinash K, Kurian PJ, Warrier AK, Shankar R, Vineesh TC, Ravindra R (2016) Sedimentary sources and processes in the eastern Arabian Sea: insights from environmental magnetism, geochemistry and clay mineralogy. Geosci Front 7(2):253–264
Azharuddin S, Govil P, Singh AD, Mishra R, Agrawal S, Tiwari AK, Kumar K (2017) Monsoon-influenced variations in productivity and lithogenic flux along offshore Saurashtra, NE Arabian Sea during the Holocene and Younger Dryas: a multi-proxy approach. Palaeogeogr Palaeoclimatol Palaeoecol 483:136–146
Banakar VK, Oba T, Chodankar AR, Kuramoto T, Yamamoto M, 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(2):99–108
Banakar VK, Mahesh BS, Burr G, Chodankar AR (2010) Climatology of the Eastern Arabian Sea during the last glacial cycle reconstructed from paired measurement of foraminiferal δ18O and Mg/Ca. Quat Res 73(3):535–540
Boothman WS (1988) Characterization of trace metal associations with polluted marine sediments by selective extractions. In: Lichtenberg J, Winter J, Weber C, Frandkin L (eds) Chemical and biological characterization of municipal sludges, sediments, dredge spoils and drilling muds. ASTM International, West Conshohocken, pp 81–92
Borole DV, Sarin MM, Somayajulu BLK (1982) Composition of Narbada and Tapti estuarine particles and adjacent Arabian Sea sediments. Indian J Mar Sci 11:51–62
Calvert SE, Pedersen TF (1993) Geochemistry of recent oxic and anoxic marine sediments: implications for the geological record. Mar Geol 113(1–2):67–88
Calvert SE, Pedersen TF, Naidu PD, Von Stackelberg U (1995) On the organic carbon maximum on the continental slope of the eastern Arabian Sea. J Mar Res 53(2):269–296
Chandana KR, Banerji US, Bhushan R (2018) Review on Indian summer monsoon (ISM) reconstruction since LGM from Northern Indian Ocean. Earth Sci India 11:71–84
Clemens S, Prell W (1991) Forcing mechanisms of the Indian Ocean monsoon. Nature 353(6346):720–725
Folk RL (1968) Petrology of sedimentary rocks. Hemphillis, Austin, p 177
Forstner U, Wittmann GTM (1983) Metal pollution in the aquatic environment, 2nd edn. Springer, Berlin, p 486
García CL, Lucchi RG, Orellana JG, Artigas MC, Masqué P, Mas CP, Lavoie C (2010) Modern sedimentation patterns and human impacts on the Barcelona continental shelf (NE Spain). Geol Acta 8(2):169–187
Hanson PJ, Evans DW, Colby DR, Zdanowicz VS (1993) Assessment of elemental contamination in estuarine and coastal environments based on geochemical and statistical modeling of sediments. Mar Environ Res 36(4):237–266
Higginson MJ, Altabet MA, Wincze L, Herbert TD, Murray DW (2004) A solar (irradiance) trigger for millennial-scale abrupt changes in the southwest monsoon? Paleoceanography 19(3):33
Kessarkar PM, Rao PV (2007) Organic carbon in sediments of the southwestern margin of India: influence of productivity and monsoon variability during the Late Quaternary. Geol Soc India 69:42–52
Kolla V, Kostecki JA, Robinson F, Biscaye PE, Ray PK (1981) Distribution and origin of clay minerals and quartz in the surface sediments of the Arabian Sea. J Sediment Petrol 51:563–569
Kumar AA, Rao VP, Patil SK, Kessarkar PM, Thamban M (2005) Rock magnetic records of the sediments of the eastern Arabian Sea: evidence for late Quaternary climatic change. Mar Geol 220:59–82
Laluraj CM, Nair SM (2006) Geochemical index of trace metals in the surficial sediments from the western continental shelf of India, Arabian Sea. Environ Geochem Health 28(6):509–518
Loring DH, Rantala RTT (1992) Manual for the geochemical analyses of marine sediments and suspended particulate matter. Earth Sci Rev 32(4):235–283
Meyers PA (1994) Preservation of elemental and isotopic source identification of sedimentary organic matter. Chem Geol 114(3–4):289–302
Milliman JD, Quraishee GS, Beg MAA (1984) Sediment discharge from the Indus river to the ocean: past, present and future. In: Haq BU, Milliman JD (eds) Marine geology and oceanography of Arabian Sea and coastal Pakistan. Van Nostrand and Reinhold, New York, pp 65–70
Müller PJ, Suess E (1979) Productivity, sedimentation rate, and sedimentary organic matter in the oceans—I. Organic carbon preservation. Deep Sea Res Part A Oceanogr Res Pap 26(12):1347–1362
Naidu PD, Kumar R, M.R., and Ramesh Babu V (1999) Time and space variations of monsoonal upwelling along the west and east coasts of India. Cont Shelf Res 19:559–572
Naik DK, Saraswat R, Lea DW, Kurtarkar SR, Mackensen A (2017) Last glacial–interglacial productivity and associated changes in the eastern Arabian Sea. Palaeogeogr Palaeoclimatol Palaeoecol 483:147–156
Nair RR, Ittekkot V, Manganini SJ, Ramaswamy V, Haake B, Degens ET, Desai BN, Honjo S (1989) Increased particle flux to the deep ocean related to monsoon. Nature 338:749–751
Naqvi SWA, Noronha RJ, Somasundar K, Sen Gupta R (1990) Seasonal changes in the denitrification regime of the Arabian Sea. Deep Sea Res 37:593–611
Overpeck J, Anderson D, Trumbore S, Prell W (1996) The southwest Indian Monsoon over the last 18 000 years. Clim Dyn 12(3):213–225
Paropkari AL, Babu CP, Mascarenhas A (1992) A critical evaluation of depositional parameters controlling the variability of organic carbon in Arabian Sea sediments. Mar Geol 107(3):213–226
PrakashBabu C, Pattan JN, Dutta K, Basavaiah N (2010) Shift in detrital sedimentation in the eastern Bay of Bengal during the late Quaternary. J Earth Syst Sci 119(3):285–295
Prell WL, Kutzbach JE (1987) Monsoon variability over the past 150,000 years. J Geophys Res Atmos 92(D7):8411–8425
Prins MA, Postma G, Weltje GJ (2000) Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Makran continental slope. Mar Geol 169(3):351–371
Ramaswamy V, Nair RR, Manganini S, Haake B, Ittekkot V (1991) Lithogenic fluxes to the deep Arabian Sea measured by sediment traps. Deep Sea Res Part A Oceanogr Res Pap 38(2):169–184
Rao VP, Rao BR (1995) Provenance and distribution of clay minerals in the sediments of the western continental shelf and slope of India. Cont Shelf Res 15(14):1757–1771
Rao VP, Kumar AA, Naqvi SWA, Chivas AR, Sekar B, Kessarkar PM (2012) Lime muds and their genesis off-Northwestern India during the late Quaternary. J Earth Syst Sci 121(3):769–779
Reichart GJ, den Dulk M, Visser HJ, van der Weijden CH, Zachariasse WJ (1997) A 225 kyr record of dust supply, paleoproductivity and the oxygen minimum zone from the Murray Ridge (northern Arabian Sea). Palaeogeogr Palaeoclimatol Palaeoecol 134(1–4):149–169
Sardessai S (1994) Organic-carbon and humic-acids in sediments of the Arabian Sea and factors governing their distribution. Oceanol Acta 17(3):263–270
Sarkar A, Ramesh R, Somayajulu BLK, Agnihotri R, Jull AJT, Burr GS (2000) High resolution Holocene monsoon record from the eastern Arabian Sea. Earth Planet Sci Lett 177(3):209–218
Sarupriya JS, Bhargava RMS (1993) Seasonal primary production in different sectors of the EEZ of India. Mahasagar 26:139–137
Schnetger B, Brumsack HJ, Schale H, Hinrichs J, Dittert L (2000) Geochemical characteristics of deep-sea sediments from the Arabian Sea: a high-resolution study. Deep Sea Res Part II 47(14):2735–2768
Shetye SS, Sudhakar M, Mohan R, Tyagi A (2009) Implication of organic carbon, trace elemental and CaCO3 variations in a sediment core from Arabian Sea. Indian J Mar Sci 38(4):432–438
Shetye SS, Sudhakar M, Mohan R, Jena B (2014) Contrasting productivity and redox potential in Arabian Sea and Bay of Bengal. J Earth Sci 25(2):366–370
Shimmield GB, Mowbray SR, Weedon GP (1990) A 350 ka history of the Indian Southwest Monsoon—evidence from deep-sea cores, northwest Arabian Sea. Trans R Soc Edinb Earth Sci 81(04):289–299
Sirocko F, Lange H (1991) Clay-mineral accumulation rates in the Arabian Sea during the late Quaternary. Mar Geol 97(1–2):105–119
Sirocko F, Garbe-Schönberg D, Devey C (2000) Processes controlling trace element geochemistry of Arabian Sea sediments during the last 25,000 years. Glob Planet Change 26(1):217–303
Somayajulu BLK, Bhushan R, Narvekar PV (1999) AMC, ZCOZ and salinity of the Western Indian Ocean deep waters: spatial and temporal variations. Geophys Res Lett 26(18):2869–2872
Sruthi KV, Kurian PJ, Rajani PR (2014) Distribution of major and trace elements of a sediment core from the eastern Arabian Sea and its environmental significance. Curr Sci 107(7):1161–1167 (00113891)
Thamban M, Rao VP, Schneider RR, Grootes PM (2001) Glacial to Holocene fluctuations in hydrography and productivity along the southwestern continental margin of India. Palaeogeogr Palaeoclimatol Palaeoecol 165(1):113–127
Thuy HTT, Tobschall HJ, An PV (2000) Trace element distributions in aquatic sediments of Danang–Hoian area, Vietnam. Environ Geol 39(7):733–740
Turekian KK, Wedepohl KH (1961) Distribution of the elements in some major units of the earth’s crust. Geol Soc Am Bull 72(2):175–192
Van Campo E (1986) Monsoon fluctuations in two 20,000-yr BP oxygen-isotope/pollen records off southwest India. Quat Res 26(3):376–388
van der Weijden CH, Reichart GJ, van Os BJ (2006) Sedimentary trace element records over the last 200 kyr from within and below the northern Arabian Sea oxygen minimum zone. Mar Geol 231(1):69–88
von Rad U, Schulz H, Riech V, den Dulk M, Berner U, 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(1):129–161
Walkey A, Black JA (1934) The determination of organic carbon by rapid titration method. Soil Sci 37:29–38
Wyrtki K (1971) Oceanographic atlas of international Indian Ocean expedition. National Science Foundation, Washington, DC, p 531
Zhao D, Wan S, Toucanne S, Clift PD, Tada R, Révillon S, Kubota Y, Zheng X, Yu Z, Huang J, Jiang H (2017) Distinct control mechanism of fine-grained sediments from Yellow River and Kyushu supply in the northern Okinawa Trough since the last glacial. Geochem Geophys Geosyst 18(8):2949–2969
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Diniz, J.E., Nayak, G.N., Noronha-D’Mello, C.A. et al. Reconstruction of palaeo-depositional environment in North-Eastern Arabian Sea. Environ Earth Sci 77, 665 (2018). https://doi.org/10.1007/s12665-018-7838-z
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DOI: https://doi.org/10.1007/s12665-018-7838-z