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Sr and Nd Isotopes as Tracers of Chemical and Physical Erosion

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Handbook of Environmental Isotope Geochemistry

Part of the book series: Advances in Isotope Geochemistry ((ADISOTOPE))

Abstract

The applications of radiogenic isotopes to investigate chemical and physical erosion processes, particularly in river basins of the Himalaya, have led to interesting inferences on the relationship between tectonics, weathering and climate. The chemical weathering studies rely more on Sr isotopes because of their widely different ratios in various end members, their uniform distribution in the oceans and the availability of continuous and robust record of marine 87Sr/86Sr through much of the geological past. The record for the Cenozoic shows steady increase in 87Sr/86Sr; one of the hypotheses suggested to explain this is enhanced continental silicate weathering due to the uplift of the Himalaya. This hypothesis linking tectonics-weathering-climate, based on 87Sr/86Sr as an index of silicate weathering, however, is being challenged by the recent observations that there are a variety of carbonates in the river basins of the Himalaya with 87Sr/86Sr similar to that of silicates which have the potential to contribute significantly to the high 87Sr/86Sr of rivers such as the Ganga-Brahmaputra. Further, the non-stochiometric release of Sr isotopes during chemical weathering of minerals and rocks, the imbalance of Sr isotope budget in the oceans and temporal variations in riverine fluxes due to impact of glaciations all have compounded the problem.

Studies on the provenance of sediments and physical erosion pattern employ both Sr and Nd isotopes under the assumption that their source signatures are preserved in sediments. Though there are concerns on how well this assumption is satisfied especially by the Sr isotope system, both Sr and Nd systems are being used to learn about physical erosion in the Himalaya, its variability and causative factors. The results show that at present the major source of sediments to the Ganga plain and the Bay of Bengal is the Higher Himalayan Crystallines and that physical erosion among the various sub-basins is very heterogeneous with maximum rates in regions of intense precipitation and high relief. There are three such “hot-spots”, one each in the basins of the Ganga, Brahmaputra and the Indus, which unload huge amount of sediments promoting rapid uplift of regions surrounding them and enhance chemical weathering by exposing fresh rock surfaces. The pattern of physical erosion and its temporal variations shows that it is influenced by climate change both on ky and My time scales though during the latter periods the erosion regime has been by and large stable. This article reviews investigations on the present and past chemical and physical erosion in river basins of the Himalaya using Sr and Nd isotope systematics in water and sediments.

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References

  • Ahmad S, Babu G, Padmakumari V et al (2005) Sr, Nd isotopic evidence of terrigenous flux variations in the Bay of Bengal: implications of monsoons during the last 34,000 years. Geophys Res Lett 32:1–4

    Google Scholar 

  • Ahmad S, Padmakumari V, Babu G (2009) Strontium and neodymium isotopic compositions in sediments from Godavari, Krishna and Pennar rivers. Curr Sci 97:1766–1769

    Google Scholar 

  • Allegre C, Dupre B, Negrel P et al (1996) Sr–Nd–Pb isotope systematics in Amazon and Congo River systems: constraints about erosion processes. Chem Geol 131:93–112

    Google Scholar 

  • Allegre C, Louvat P, Gaillardet J et al (2010) The fundamental role of island arc weathering in the oceanic Sr isotope budget. Earth Planet Sci Lett 292:51–56

    Google Scholar 

  • Amelin Y, Rotenberg E (2004) Sm-Nd systematics of chrondrites. Earth Planet Sci Lett 223:267–282

    Google Scholar 

  • Amiotte Suchet P, Probst J, Ludwig W (2003) Worldwide distribution of continental rock lithology: implications for the atmospheric/soil CO2 uptake by continental weathering and alkalinity river transport to the oceans. Glob Biogeochem Cycles 17:1038. doi:10.1029/2002GB001891

    Article  Google Scholar 

  • Anderasen R, Sharma M (2006) Solar Nebula heterogenity in p-process Samarium and Neodymium isotopes. Science 314:806–809

    Google Scholar 

  • Andersson P, Dahlqvist R, Ingri J et al (2001) The isotopic composition of Nd in a boreal river: a reflection of selective weathering and colloidal transport. Geochim Cosmochim Acta 65:521–527

    Google Scholar 

  • Armstrong RL (1971) Glacial erosion and the variable isotopic composition of strontium in seawater. Nature 230:132–134

    Google Scholar 

  • Asahara Y, Tanaka T, Kamioka H et al (1999) Provenance of the north Pacific sediments and process of source material transport as derived from Rb–Sr isotopic systematics. Chem Geol 158:271–291

    Google Scholar 

  • Aubert D, Stille P, Probst A (2001) REE fractionation during granite weathering and removal by waters and suspended loads: Sr and Nd isotopic evidence. Geochim Cosmochim Acta 65:387–406

    Google Scholar 

  • Banner J (2004) Radiogenic isotopes: systematics and applications to earth surface processes and chemical startigraphy. Earth Sci Rev 65:141–194

    Google Scholar 

  • Barroux G, Sonke J, Boaventura G et al (2006) Seasonal dissolved rare earth element dynamics of the Amazon River main stem, its tributaries, and the Curuaí floodplain. Geochem Geophys Geosyst 7:Q12005. doi:10.1029/2006GC001244

    Article  Google Scholar 

  • Barun JJ, Pagel M, Herbillon A et al (1993) Mobilization and redistribution of REEs and thorium in a syenitic lateritic profile: a mass balance study. Geochim Cosmochim Acta 57:4419–4434

    Google Scholar 

  • Basu A, Jacobsen S, Poreda R et al (2001) Large groundwater strontium flux to the oceans from the Bengal basin and the marine strontium isotope record. Science 293:1470–1473

    Google Scholar 

  • Berner R, Lasaga A, Garrels R (1983) The carbonate–silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years. Am J Sci 283:641–683

    Google Scholar 

  • Bickle M, Harris N, Bunbury J et al (2001) Controls on the 87Sr/86Sr ratio of carbonates in the Garhwal Himalaya, Headwaters of the Ganges. J Geol 109:737–753

    Google Scholar 

  • Bickle M, Bunbury J, Chapman H et al (2003) Fluxes of Sr into the headwaters of the Ganges. Geochim Cosmochim Acta 67:2567–2584

    Google Scholar 

  • Bickle M, Chapman H, Bunbury J et al (2005) Relative contributions of silicate and carbonate rocks to riverine Sr fluxes in the headwaters of the Ganges. Geochim Cosmochim Acta 69:2221–2240

    Google Scholar 

  • Blum JD, Erel Y (1995) A silicate weathering mechanism linking increases in marine Sr-87/Sr-86 with global glaciation. Nature 373:415–418

    Google Scholar 

  • Blum JD, Erel Y (1997) Rb-Sr isotope systematics of a granitic soil chronosequence: the importance of biotite weathering. Geochim Cosmochim Acta 61:3193–3204

    Google Scholar 

  • Blum JD, Erel Y (2003) Radiogenic isotopes in weathering and hydrology. In: Holland HD, Turekian KK (eds) Surface and ground water, weathering and soils, vol. 5, Treatise on geochemistry. Elsevier-Pergamon, Oxford, pp 365–392

    Google Scholar 

  • Blum JD, Gazis CA, Jacobson A et al (1998) Carbonate versus silicate weathering rates in the Raikot watershed within the High Himalayan crystalline series. Geology 26:411–414

    Google Scholar 

  • Bluth G, Kump L (1994) Lithologic and climatologic controls of river chemistry. Geochim Cosmochim Acta 58:2341–2359

    Google Scholar 

  • Brantley S, Chesley J, Stillings L (1998) Isotopic ratios and release rates of strontium measured from weathering feldspars. Geochim Cosmochim Acta 62:1493–1500

    Google Scholar 

  • Brass GW (1976) The variation of the marine 87Sr/86Sr ratio during Phanerozoic time; interpretation using a flux model. Geochim Cosmochim Acta 40:721–730

    Google Scholar 

  • Bullen T, White A, Blum A et al (1997) Chemical weathering of a soil chronosequence on granitoid alluvium: II mineralogic and isotopic constraints on the behavior of strontium. Geochim Cosmochim Acta 61:291–306

    Google Scholar 

  • Burbank D, Blythe A, Putkonen J et al (2003) Decoupling of erosion and precipitation in the Himalayas. Nature 426:652–655

    Google Scholar 

  • Burke W, Denison R, Hetherington E et al (1982) Variation of seawater 87Sr/86Sr throughout Phanerozoic time. Geology 10:516–519

    Google Scholar 

  • Chabaux F, Riotte J, Clauer N et al (2001) Isotopic tracing of the dissolved U fluxes of Himalayan rivers: implications for present and past U budgets of the Ganges-Brahmaputra system. Geochim Cosmochim Acta 65:3201–3217

    Google Scholar 

  • Chabaux F, Bourdon B, Riotte J (2008) U-series geochemistry in weathering profiles, river waters and lakes. In: Krishnaswami S, Cochran JK (eds) U/Th series radionuclides in aquatic systems, vol 13, Radioactivity in the environment. Elsevier, New York, NY, pp 49–104

    Google Scholar 

  • Clift P (2006) Controls on the erosion of Cenozoic Asia and the flux of clastic sediment to the ocean. Earth Planet Sci Lett 241:571–590

    Google Scholar 

  • Clift P, Blusztajn J (2005) Reorganization of the western Himalayan river system after five million years ago. Nature 438:1001–1003

    Google Scholar 

  • Clift P, Lee J, Hildebrand P et al (2002) Nd and Pb isotope variability in the Indus river system: implications for crustal heterogeneity in the western Himalya. Earth Planet Sci Lett 200:91–106

    Google Scholar 

  • Clift P, Giosan L, Blusztajn J et al (2008) Holocene erosion of the Lesser Himalaya triggered by intensified summer monsoon. Geology 36:79–82

    Google Scholar 

  • Colin C, Turpin L, Bertaux J et al (1999) Erosional history of the Himalayan and Burman ranges during the last two glacial-interglacial cycles. Earth Planet Sci Lett 171:647–660

    Google Scholar 

  • Colin C, Turpin L, Blamart D et al (2006) Evolution of weathering patterns in the Indo-Burman ranges over 280 kyr: effects of sediment provenance on 87Sr/86Sr ratios tracer. Geochem Geophys Geosyst 7:Q03007. doi:10.1029/2005GC000962

    Article  Google Scholar 

  • Dalai T, Krishnaswami S, Kumar A (2003) Sr and 87Sr/86Sr in the Yamuna River System in the Himalaya: sources, fluxes, and controls on Sr isotope composition. Geochim Cosmochim Acta 67:2931–2948

    Google Scholar 

  • Das A, Krishnaswami S, Sarin M et al (2005) Chemical weathering in the Krishna Basin and Western Ghats of the Deccan Traps, India: rates of basalt weathering and their controls. Geochim Cosmochim Acta 69:2067–2084

    Google Scholar 

  • Das A, Krishnaswami S, Kumar A (2006) Sr and 87Sr/86Sr in rivers draining the Deccan Traps (India): implications to weathering, Sr fluxes and marine 87Sr/86Sr record around K/T. Geochem Geophys Geosyst 7:Q06014. doi:10.1029/2005GC001081

    Article  Google Scholar 

  • Dasch E (1969) Strontium isotopes in weathering profiles, deep-sea sediments, and sedimentary rocks. Geochim Cosmochim Acta 33:1521–1552

    Google Scholar 

  • Davis A, Bickle M, Teagle D (2003) Imbalance in the oceanic strontium budget. Earth Planet Sci Lett 211:173–187

    Google Scholar 

  • DePaolo D, Wasserburg G (1976) Nd isotopic variations and petrogenetic models. Geophys Res Lett 3:249–252

    Google Scholar 

  • Derry L, France-Lanord C (1996) Neogene Himalayan weathering history and river 87Sr/86Sr: impact on the marine Sr record. Earth Planet Sci Lett 142:59–74

    Google Scholar 

  • Derry L, France-Lanord C (1997) Himalayan weathering and erosion fluxes: climate and tectonic controls. In: Ruddiman WF (ed) Tectonic uplift and climate change. Plenum, New York, pp 290–312

    Google Scholar 

  • Dessert C, Dupre B, Francois L et al (2001) Erosion of Deccan Traps determined by river geochemistry: impact on the global climate and the 87Sr/86Sr ratio of sea water. Earth Planet Sci Lett 188:459–474

    Google Scholar 

  • Dessert C, Dupre B, Gaillardet J et al (2003) Basalt weathering laws and the impact of basalt weathering on the global carbon cycle. Chem Geol 20:1–17

    Google Scholar 

  • Dia A, Dupré B, Allègre C (1992) Nd isotopes in Indian Ocean sediments used as a tracer of supply to the ocean and circulation paths. Mar Geol 103:349–359

    Google Scholar 

  • Drever J (1997) The geochemistry of natural waters, 3rd edn. Prentice Hall, NJ, p 436

    Google Scholar 

  • Edmond JM (1992) Himalayan tectonics, weathering processes, and the strontium isotope record in marine limestone. Science 258:1594–1597

    Google Scholar 

  • Edmond J, Huh Y (1997) Chemical weathering yields from basement and orogenic terrains in hot and cold climates. In: Ruddiman WF (ed) Tectonic Uplift and Climate Change. Plenum Press, New York, pp 330–351

    Google Scholar 

  • Erel Y, Blum JD, Roueff E et al (2004) Lead and strontium isotopes as monitors of experimental granitoid mineral dissolution. Geochim Cosmochim Acta 68:4649–4663

    Google Scholar 

  • Evans M, Derry L, Anderson S et al (2001) Hydrothermal source of radiogenic Sr to Himalayan rivers. Geology 29:803–806

    Google Scholar 

  • Evans M, Derry L, France-Lanord C (2004) Geothermal fluxes of alkalinity in the Narayani river system of central Nepal. Geochem Geophys Geosyst 5:Q08011. doi:10.1029/2004GC000719

    Article  Google Scholar 

  • Faure G (1986) Principles of Isotope Geology, 2nd edn. Wiley, Hoboken, N.J

    Google Scholar 

  • France-Lanord C, Derry L (1997) Organic carbon burial forcing of the carbon cycle from Himalayan erosion. Nature 390:65–67

    Google Scholar 

  • France-Lanord C, Derry L, Michard A (1993) Evolution of the Himalaya since Miocene time: isotopic and sedimentologic evidence from the Bengal Fan. In: Treloar PJ, Searle M (eds) Himalayan tectonics, vol 74, Geological Society of London Special Publication. Geological Society of London, London, pp 603–621

    Google Scholar 

  • Frank M (2002) Radiogenic isotopes: tracers of past ocean circulation and erosional input. Rev Geophys 40(1):1001. doi:10.1029/2000RG000094

    Article  Google Scholar 

  • Gaillardet J (2008) Isotope geochemistry as a tool for deciphering kinetics of water-rock interaction. In: Brantley S, Kubicki J, White A (eds) Kinetics of water-rock interaction, Chap. 12. Spinger, New York, pp 611–674

    Google Scholar 

  • Gaillardet J, Dupre B, Allegre C (1997) Chemical and physical denudation in the Amazon river basin. Chem Geol 142:141–173

    Google Scholar 

  • Gaillardet J, Dupre B, Louvat P et al (1999) Global silicate weathering and CO2 consumption rates deduced from the chemistry of large rivers. Chem Geol 159:3–30

    Google Scholar 

  • Galy A, France-Lanord C (1999) Weathering processes in the Ganges-Brahmaputra basin and the riverine alkalinity budget. Chem Geol 159:31–60

    Google Scholar 

  • Galy A, France-Lanord C, Derry L (1999) The strontium isotopic budget of Himalayan Rivers in Nepal and Bangladesh. Geochim Cosmochim Acta 63:1905–1925

    Google Scholar 

  • Galy V, France-Lanord C, Peucker-Ehrenbrink B et al (2010) Sr–Nd–Os evidence for a stable erosion regime in the Himalaya during the past 12 Myr. Earth Planet Sci Lett 290:474–480

    Google Scholar 

  • Goldstein SL, Jacobsen SB (1987) The Nd and Sr isotopic systematics of river-water dissolved material: implications for the sources of Nd and Sr in the seawater. Chem Geol 66:245–272

    Google Scholar 

  • Goldstein SL, O'Nions RK (1981) Nd and Sr isotopic relationships in pelagic clays and ferromanganese deposits. Nature 292:324–327

    Google Scholar 

  • Harlavan Y, Erel Y (2002) The release of Pb and REE from granitoids by the dissolution of accessory phases. Geochim Cosmochim Acta 66:837–848

    Google Scholar 

  • Harlavan Y, Erel Y, Blum JD (2009) The coupled release of REE and Pb to the soil labile pool with time by weathering of accessory phases, Wind River Mountains, WY. Geochim Cosmochim Acta 73:320–336

    Google Scholar 

  • Harris N, Bickle M, Chapman H et al (1998) The significance of Himalayan rivers for silicate weathering rates: evidence from the Bhote Kosi tributary. Chem Geol 144:205–220

    Google Scholar 

  • Hren M, Chamberlain C, Hilley G et al (2007) Major ion chemistry of the Yarlung Tsangpo-Brahmaputra river: chemical weathering, erosion, and CO2 consumption in the southern Tibetan Plateau and eastern syntaxis of the Himalaya. Geochim Cosmochim Acta 71:2907–2935

    Google Scholar 

  • Huh Y, Edmond J (1999) The fluvial geochemistry of the rivers of Eastern Siberia: III Tributaries of the Lena and Anbar draining the basement terrain of the Siberian Craton and the Trans-Baikal Highlands. Geochim Cosmochim Acta 63:967–987

    Google Scholar 

  • Ingri J, Widerlund A, Land M et al (2000) Temporal variations in the fractionation of the rare earth elements in a boreal river; the role of colloidal particles. Chem Geol 166:23–45

    Google Scholar 

  • Jacobsen S, Wasserburg G (1980) Sm-Nd isotopic evolution of chondrites. Earth Planet Sci Lett 50:139–155

    Google Scholar 

  • Jacobson AD, Blum JD (2000) The Ca/Sr and 87Sr/86Sr geochemistry of disseminated calcite in Himalayan silicate rocks from Nanga Parbat: influence on river water chemistry. Geology 28:463–466

    Google Scholar 

  • Jacobson AD, Blum JD, Chamberlain CP et al (2002) The Ca/Sr and Sr isotope systematics of a Himalayan glacial chronosequence: carbonate versus silicate weathering rates as a function of landscape surface age. Geochim Cosmochim Acta 66:13–27

    Google Scholar 

  • Jeandel C, Arsouze T, Lacan F et al (2007) Isotopic Nd compositions and concentrations of the lithogenic inputs into the ocean: a compilation, with an emphasis on the margins. Chem Geol 239:156–164

    Google Scholar 

  • Johannesson K, Tang J, Daniels J et al (2004) Rare earth element concentrations and speciation in organic-rich blackwaters of the Great Dismal Swamp, Virginia. USA Chem Geol 209:271–294

    Google Scholar 

  • Krishnaswami S, Singh SK (2005) Chemical weathering in the river basins of the Himalaya. India Curr Sci 89:841–849

    Google Scholar 

  • Krishnaswami S, Trivedi JR, Sarin MM et al (1992) Strontium isotopes and rubidium in the Ganga-Brahmaputra river system: weathering in the Himalaya, fluxes to the Bay of Bengal and contributions to the evolution of oceanic 87Sr/86Sr. Earth Planet Sci Lett 109:243–253

    Google Scholar 

  • Krishnaswami S, Singh SK, Dalai TK (1999) Silicate weathering in the Himalaya: role in contributing to major ions and radiogenic Sr to the Bay of Bengal. In: Somayajulu BLK (ed) Ocean science, trends and future directions. Indian National Science Academy and Akademia International, New Delhi, pp 23–51

    Google Scholar 

  • Kump LR, Brantley SL, Arthur MA (2000) Chemical weathering, atmospheric CO2 and climate. Annu Rev Earth Planet Sci 28:611–667

    Google Scholar 

  • Leland J, Reid MR, Burbank DW et al (1998) Incision and differential bedrock uplift along the Indus River near Nanga Parbat, Pakistan Himalaya, from 10Be and 26Al exposure age dating of bedrock straths. Earth Planet Sci Lett 154:93–107

    Google Scholar 

  • Li XH, Wei GJ, Shao L et al (2003) Geochemical and Nd isotopic variations in sediments of the South China Sea: a response to Cenozoic tectonism in SE Asia. Earth Planet Sci Lett 211:207–220

    Google Scholar 

  • Ma J, Wei G, Xu Y et al (2007) Mobilization and re-distribution of major and trace elements during extreme weathering of basalt in Hainan Island, South China. Geochim Cosmochim Acta 71:3223–3237

    Google Scholar 

  • Ma J, Wei G, Xu Y et al (2010) Variations of Sr–Nd–Hf isotopic systematics in basalt during intensive weathering. Chem Geol 269:376–385

    Google Scholar 

  • MacFarlane A, Danielson A, Holland H et al (1994) REE chemistry and Sm-Nd systematics of late Archean weathering profiles in the Fortescue Group, Western Australia. Geochim Cosmochim Acta 58:1777–1794

    Google Scholar 

  • McCauley S, DePaolo D (1997) The marine 87Sr/86Sr and δ18O records, Himalayan alkalinity fluxes and Cenozoic climate records. In: Ruddiman W (ed) Tectonics uplift and climate change. Plenum, New York, pp 428–467

    Google Scholar 

  • Milliman J, Meade R (1983) World-wide delivery of river sediment to the oceans. J Geol 91:1–21

    Google Scholar 

  • Milliman JD, Syvitski PM (1992) Geomorphic/Tectonic control of sediment discharge to the ocean: the importance of small mountainous rivers. J Geol 100:525–544

    Google Scholar 

  • Millot R, Gaillardet J, Dupre B et al (2002) The global control of silicate weathering rates and the coupling with physical erosion: new insights from rivers of the Canadian Shield. Earth Planet Sci Lett 196:83–98

    Google Scholar 

  • Millot R, Gaillardet J, Dupre B et al (2003) Northern latitude chemical weathering rates: clues from the Mackenzie River basin, Canada. Geochim Cosmochim Acta 67:1305–1329

    Google Scholar 

  • Molnar P, England P (1990) Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? Nature 346:29–34

    Google Scholar 

  • Montgomery DR (1994) Valley incision and the uplift of mountain peaks. J Geophys Res 99:913–921

    Google Scholar 

  • Moon S, Huh Y, Qin J et al (2007) Chemical weathering in the Hong (Red) River basin: rates of silicate weathering and their controlling factors. Geochim Cosmochim Acta 71:1411–1430

    Google Scholar 

  • Moon S, Huh Y, Zitsev A (2009) Hydrochemistry of the Amur River: weathering in a northern temperate basin. Aquat Geochem 15:497–527

    Google Scholar 

  • Negrel P, Allegre CJ, Dupre B et al (1993) Erosion sources determined by inversion of major and trace element ratios and strontium isotopic ratios in river water: the Congo Basin case. Earth Planet Sci Lett 120:59–76

    Google Scholar 

  • Nesbitt H (1979) Mobility and fractionation of rare earth elements during weathering of a granodiorite. Nature 279:206–210

    Google Scholar 

  • Nesbitt HW, Markovics G (1997) Weathering of granodioritic crust, long-term storage of elements in weathering profiles, and petrogenesis of silicate minerals. Geochim Cosmochim Acta 61:1653–1670

    Google Scholar 

  • Noh H, Huh Y, Qin J et al (2009) Chemical weathering in the three rivers region of Eastern Tibet. Geochim Cosmochim Acta 73:1857–1877

    Google Scholar 

  • Ohlander B, Ingri J, Land M et al (2000) Change of Sm-Nd isotope composition during weathering of till. Geochim Cosmochim Acta 64:813–820

    Google Scholar 

  • Oliva P, Dupre B, Martin F et al (2004) The role of trace minerals in chemical weathering in a high-elevation granitic watershed (Estibere, France): chemical and mineralogical evidence. Geochim Cosmochim Acta 68:2223–2243

    Google Scholar 

  • Oliver L, Harris N, Bickle M et al (2003) Silicate weathering rates decoupled from the 87Sr/86Sr ratio of the dissolved load during Himalayan erosion. Chem Geol 201:119–139

    Google Scholar 

  • Palmer M, Edmond J (1989) The strontium isotope budget of the modern ocean. Earth Planet Sci Lett 92:11–26

    Google Scholar 

  • Palmer MR, Edmond JM (1992) Controls over the strontium isotope composition of river water. Geochim Cosmochim Acta 56:2099–2111

    Google Scholar 

  • Pande K, Sarin MM, Trivedi JR et al (1994) The Indus river system (India-Pakistan): major-ion chemistry, uranium and strontium isotopes. Chem Geol 116:245–259

    Google Scholar 

  • Pattanaik J, Balakrishnan S, Bhutani R et al (2007) Chemical and strontium isotopic composition of Kaveri, Palar and Ponnaiyar rivers: significance to weathering of granulites and granitic gneisses of southern Peninsular India. Curr Sci 93:523–531

    Google Scholar 

  • Peucker-Ehrenbrink B (2009) Land2Sea database of river drainage basin sizes, annual water discharges, and suspended sediment fluxes. Geochem Geophys Geosyst 10:Q06014. doi:10.1029/2008GC002356

    Article  Google Scholar 

  • Peucker-Ehrenbrink B, Miller MW, Arsouze T et al (2010) Continental bedrock and riverine fluxes of strontium and neodymium isotopes to the oceans. Geochem Geophys Geosyst 11:Q03016. doi:10.1029/2009GC002869

    Article  Google Scholar 

  • Pierson-Wickmann AC, Reisberg L, France-Lanord C et al (2001) Os-Sr-Nd results from sediments in the Bay of Bengal: implications for sediment transport and the marine Os record. Paleoceanography 16:435–444

    Google Scholar 

  • Porcelli D, Anderson P, Baskaran M et al (2009) The distribution of neodymium isotopes in Arctic Ocean basins. Geochim Cosmochim Acta 73:2645–2659

    Google Scholar 

  • Quade J, Roe L, DeCelles P et al (1997) The late neogene 87Sr/86Sr record of lowland Himalayan rivers. Science 276:1828–1831

    Google Scholar 

  • Rad S, Allegre C, Lovat P (2007) Hidden erosion on volcanic islands. Earth Planet Sci Lett 262:109–124

    Google Scholar 

  • Rahaman W, Singh SK, Sinha R et al (2009) Climate control on erosion distribution over the Himalaya during the past 100 ka. Geology 37:559–562

    Google Scholar 

  • Rai SK, Singh SK (2007) Temporal variation in Sr and 87Sr/86Sr of the Brahmaputra: implications for annual fluxes and tracking flash floods through chemical and isotope composition. Geochem Geophys Geosyst 8:Q08008

    Google Scholar 

  • Rai SK, Singh SK, Krishnaswami S (2010) Chemical weathering in the plain and peninsular sub-basins of the Ganga: impact on major ion chemistry and elemental fluxes. Geochim Cosmochim Acta 74:2340–2355

    Google Scholar 

  • Ravizza G, Zachos J (2003) Records of Cenozoic chemistry. In: Holland HD, Turekian KK (eds) The oceans and marine chemistry, vol. 6, Treatise on geochemistry. Elsevier-Pergamon, Oxford, pp 551–582

    Google Scholar 

  • Raymo ME, Ruddiman WF (1992) Tectonic forcing of late Cenozoic climate. Nature 359:117–122

    Google Scholar 

  • Raymo ME, Ruddiman WF, Froelich PN (1988) Influence of late Cenozoic mountain building on ocean geochemical cycles. Geology 16:649–653

    Google Scholar 

  • Reynolds B (2011) Silicon isotopes as tracers of terrestrial processes. In: Baskaran M (ed) Handbook of environmental isotope geochemistry. Chapter 6. Springer, Heidelberg

    Google Scholar 

  • Richter FM, Rowley DB, DePaolo DJ (1992) Sr isotope evolution of seawater: the role of tectonics. Earth Planet Sci Lett 109:11–23

    Google Scholar 

  • Ruddiman W (1997) Tectonic Uplift and Climate Change. Plenum, New York, p 535

    Google Scholar 

  • Shiller A (2010) Dissolved rare earth elements in a seasonally snow-covered, alpine/subalpine watershed, Loch Vale, Colorado. Geochim Cosmochim Acta 74:2040–2052

    Google Scholar 

  • Sholkovitz E (1995) The aquatic chemistry of rare earth elements in rivers and estuaries. Aquat Geochem 1:1–34

    Google Scholar 

  • Sholkovitz E, Szymczak R (2000) The estuarine chemistry of rare earth elements: comparison of the Amazon, Fly, Sepik and the Gulf of Papua systems. Earth Planet Sci Lett 179:299–309

    Google Scholar 

  • Singh SK (2006) Spatial variability in erosion in the Brahmaputra basin: causes and impacts. Curr Sci 90:1271–1276

    Google Scholar 

  • Singh SK (2007) Erosion and weathering in the Brahmaputra river system. In: Gupta A (ed) Large rivers. Wiley, Chichester, pp 373–393

    Google Scholar 

  • Singh SK, France-Lanord C (2002) Tracing the distribution of erosion in the Brahmaputra watershed from isotopic compositions of stream sediments. Earth Planet Sci Lett 202:645–662

    Google Scholar 

  • Singh SK, Trivedi JR, Pande K et al (1998) Chemical and strontium, oxygen, and carbon isotopic compositions of carbonates from the Lesser Himalaya: implications to the strontium isotope composition of the source waters of the Ganga, Ghaghara, and the Indus Rivers. Geochim Cosmochim Acta 62:743–755

    Google Scholar 

  • Singh SK, Sarin MM, France-Lanord C (2005) Chemical erosion in the eastern Himalaya: major ion composition of the Brahmaputra and δ13C of dissolved inorganic carbon. Geochim Cosmochim Acta 69:3573–3588

    Google Scholar 

  • Singh SK, Rai SK, Krishnaswami S (2008) Sr and Nd isotopes in river sediments from the Ganga basin: sediment provenance and spatial variability in physical erosion. J Geophys Res 113:F03006. doi:10.1029/2007JF000909

    Article  Google Scholar 

  • Stallard RF, Edmond JM (1983) Geochemistry of the Amazon 2. J Geophys Res 88:9671–9688

    Google Scholar 

  • Steinmann M, Stille P (2008) Controls on transport and fractionation of the rare earth elements in stream water of a mixed basaltic-granitic catchment basin (Massif Central, France). Chem Geol 254:1–18

    Google Scholar 

  • Tachikawa K, Athias V, Jeandel C (2003) Neodymium budget in the modern ocean and paleo-oceanographic implications. J Geophys Res 108:3254. doi:10.1029/1999JC000285

    Article  Google Scholar 

  • Taylor AS, Lasaga AC (1999) The role of basalt weathering in the Sr isotope budget of the oceans. Chem Geol 161:199–214

    Google Scholar 

  • Taylor AS, Blum JD, Lasaga AC et al (2000) Kinetics of dissolution and Sr release during biotite and phlogopite weathering. Geochim Cosmochim Acta 64:1191–1208

    Google Scholar 

  • Tipper E, Bickle M, Galy A et al (2006a) The short term climatic sensitivity of carbonate and silicate weathering fluxes: insight from seasonal variations in river chemistry. Geochim Cosmochim Acta 70:2737–2754

    Google Scholar 

  • Tipper E, Galy A, Gaillardet J et al (2006b) The magnesium isotope budget of the modern ocean: constraints from riverine magnesium isotope ratios. Earth Planet Sci Lett 250:241–253

    Google Scholar 

  • Tipper E, Galy A, Bickle M (2008) Calcium and magnesium isotope systematics in rivers draining the Himalaya-Tibetan-Plateau region: lithological or fractionation control? Geochim Cosmochim Acta 72:1057–1075

    Google Scholar 

  • Tricca A, Stille P, Steinmann M et al (1999) Rare earth elements and Sr and Nd isotopic compositions of dissolved and suspended loads from small river systems in the Vosges mountains (France), the river Rhine and groundwater. Chem Geol 160:139–158

    Google Scholar 

  • Tripathy GR, Singh SK (2010) Chemical erosion rates of river basins of the Ganga system in the Himalaya: reanalysis based on inversion of dissolved major ions, Sr, and 87Sr/86Sr. Geochem Geophys Geosyst 11:Q03013. doi:10.1029/2009GC002862

    Article  Google Scholar 

  • Tripathy GR, Goswami V, Singh SK et al (2010) Temporal variations in Sr and 87Sr/86Sr of the Ganga headwaters: estimate of dissolved Sr flux to the mainstream. Hydrol Process 24:1159–1171. doi:10.1002/hyp. 7572

    Article  Google Scholar 

  • Trivedi J, Pande K, Krishnaswami S et al (1995) Sr isotopes in rivers of India and Pakistan: a reconnaissance study. Curr Sci 69:171–178

    Google Scholar 

  • Tutken T, Eisenhauer A, Wiegand B et al (2002) Glacial-interglacial cycles in Sr and Nd isotopic composition of Arctic marine sediments triggered by the Svalbard/Barents Sea ice sheet. Mar Geol 182:351–372

    Google Scholar 

  • Vance D, Teagle D, Foster G (2009) Variable Quaternary chemical weathering fluxes and imbalances in marine geochemical budgets. Nature 458:493–496

    Google Scholar 

  • Veizer J (1989) Strontium isotopes in sea water through time. Annu Rev Earth Planet Sci 17:141–168

    Google Scholar 

  • Viers J, Wasserburg GJ (2004) Behavior of Sm and Nd in a lateritic soil profile. Geochim Cosmochim Acta 68:2043–2054

    Google Scholar 

  • Viers J, Roddaz M, Filizola N et al (2008) Seasonal and provenance controls on Nd–Sr isotopic compositions of Amazon river suspended sediments and implications for Nd and Sr fluxes exported to the Atlantic Ocean. Earth Planet Sci Lett 274:511–523

    Google Scholar 

  • Vigier N, Bourdon B (2011) Constraining rates of chemical and physical erosion using U-series radionuclides. In: Baskaran M (ed) Handbook of environmental isotope geochemistry, Chapter 27. Springer, Heidelberg

    Google Scholar 

  • Walker J, Hays P, Kasting J (1981) A negative feedback mechanism for the long-term stabilization of Earth’s surface temperature. J Geophy Res 86:9776–9782

    Google Scholar 

  • Walter HJ, Hegner E, Diekmann B et al (2000) Provenance and transport of terrigenous sediment in the south Atlantic Ocean and their relations to glacial and interglacial cycles: Nd and Sr isotopic evidence. Geochim Cosmochim Acta 64:3813–3827

    Google Scholar 

  • West AJ, Galy A, Bickle M (2005) Tectonic and climatic controls on silicate weathering. Earth Planet Sci Lett 235:211–228

    Google Scholar 

  • Willenbring JK, Blanckenburg FV (2010) Long-term stability of global erosion rates and weathering during late-Cenozoic cooling. Nature 465:211–214

    Google Scholar 

  • Winter B, Johnson C, Clark D (1997) Strontium, neodymium and lead isotope variations of authigenic and silicate sediment components from the Late Cenozoic Arctic Ocean: implications for sediment provenance and source of trace metals in sea water. Geochim Cosmochim Acta 61:4181–4200

    Google Scholar 

  • Wu L, Huh Y, Qin J et al (2005) Chemical weathering in the Upper Huang He (Yellow River) draining the eastern Qinghai-Tibet Plateau. Geochim Cosmochim Acta 69:5279–5294

    Google Scholar 

  • Xu Y, Marcantonio F (2007) Strontium isotope variations in the lower Mississippi River and its estuarine mixing zone. Mar Chem 105:118–128

    Google Scholar 

  • Yang C, Telmer K, Veizer J (1996) Chemical dynamics of the “St. Lawrence” riverine system: δDH2O, δ18OH2O, δ13CDIC, δ34Ssulfate, and dissolved 87Sr/86Sr. Geochim Cosmochim Acta 60:851–866

    Google Scholar 

  • Yang S, Jiang S, Ling H et al (2007) Sr-Nd isotopic compositions of the Changjiang sediments: implications for tracing sediment sources. Sci China Ser D-Earth Sci 50:1556–1565

    Google Scholar 

  • Zachos J, Opdyke B, Quinn T et al (1999) Early Cenozoic glaciation, Antarctic weathering, and seawater 87Sr/86Sr: is there a link? Chem Geol 161:165–180

    Google Scholar 

  • Zeitler P, Koons P, Bishop M et al (2001) Erosion, Himalayan geodynamics, and the geomorphology of metamorphism. GSA Today 11:4–9

    Google Scholar 

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Acknowledgements

SK thanks the Indian National Science Academy, New Delhi for Senior Scientistship and the Director, PRL for logistical support. Reviews and comments from Prof. M. Baskaran and two anonymous reviewers have helped improve the article.

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Tripathy, G.R., Singh, S.K., Krishnaswami, S. (2012). Sr and Nd Isotopes as Tracers of Chemical and Physical Erosion. In: Baskaran, M. (eds) Handbook of Environmental Isotope Geochemistry. Advances in Isotope Geochemistry. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-10637-8_26

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