Skip to main content

Glacial Sediments of Schirmacher Oasis, East Antarctica and their Characteristics

  • Chapter
  • First Online:
Climate Change and the White World

Abstract

Schirmacher Oasis in Central Dronning Maud Land of East Antarctica represents a polar and periglacial environment that exhibits large accumulation of unconsolidated sediments as moraines and debris dropped by retreating ice sheet and admixture of sand-silt-clay deposited by the melt water channels. Study involved collection of sediments from various depositional environments for analyses. The sand-silt-clay ratios determined from these samples show that the sand percentage is varying between 71% and 95.22%, silt percentage varies between 3.06% and 15.54% and the clay percentage falls within 1.72–13.46% range indicating that the sand constitutes major part of the soil while clay fraction is generally negligible to minimum. It is in the vertical sections of some lake margins that fine lamiae of clay are seen. The organic carbon content and the inorganic carbon, as also the variation in the CaCO3 in the samples is very low. The sediments indicate a quartzose provenance and abundance of heavy minerals. Glacial till around Maitri were mapped on 1:1000 scale to understand the depositional history of sediments. The samples collected from each level were analysed for Accelerated Mass Spectrometer (AMS) dating. The results indicate four distinct surfaces of these deposits between the Priyadarshini Lake (towards north) and the area in the immediate vicinity of Maitri Station deposited between the span of 4702 and 8942 years BP. The surface textures and the morphological features on the quartz grains further indicate differential transportation, essentially by the glacial agency as the angularities of the edges are still preserved and the sub-rounding to rounding of the grains, typical of the fluvial action, is present only in case of channel deposits. Periods of residency of the grains for long span of time is shown by the engraved features on the surfaces of the quartz grains.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 79.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 99.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 129.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

  • Achyuthan H, Asthana R, Ravindra R, Eastoe C (2008) Radiocarbon dates and sedimentation within the Schirmacher Oasis, East Antarctica. Abstract SCAR’s Open Science Congress, St. Petersburg

    Google Scholar 

  • Asthana R, Chaturvedi A (1998) The grain size behaviour and morphoscopy of supraglacial sediments south of Schirmacher Oasis East Antarctica. J Geol Soc India 52:557–568

    CAS  Google Scholar 

  • Asthana R, shrivastava PK, Beg MJ, Shome S, Kachroo K (2009) Surface microtextures of quartz grains from glaciolacustrine sediment core from Priyadarshini Lake, Schirmacher Oasis, East Antarctica as revealed under scanning electron microscope. Indian J Geosci 63(2):205–214

    CAS  Google Scholar 

  • Asthana R, Beg MJ, Swain AK, Dharwadkar A, Roy SK, Srivastava HB (2013) Sedimentary processes in two different polar periglacial environments: examples from Schirmacher Oasis and Larsemann Hills, East Antarctica. Geol Soc Lond Spec Publ 381:411–427

    Article  Google Scholar 

  • Baba S, Owada M, Grew ES, Shirajshi K (2006) Granulite from Schirmacher Hills, central Dronning Land. In: Fütterer DK, Damaske D, Kleinschmidt G, Miller H, Tessensohn F (eds) Antarctic contributions to global Earth science. Springer, Berlin

    Google Scholar 

  • Bardin VJ (1971) Moraines of Antarctica. In: Adie RJ (ed) Antarctic geology and geophysics. Universitetes for laget, Oslo, pp 663–667

    Google Scholar 

  • Bera SK (2004) Late Holocene palaeo-winds and climatic changes in Eastern Antarctica as indicated by long distance transported pollen-spores and local microbiota in polar lake core sediments. Curr Sci 86(11):1485–1488

    Google Scholar 

  • Buckley DE, Cranston RE (1991) The use of grain size information in marine geochemistry. In: Syvitski JPM (ed) Principles, methods, and application of particle size analysis. Cambridge University Press, New York, pp 311–331

    Chapter  Google Scholar 

  • Calvert SE, Pedersen TF (1993) Geochemistry of recent toxic and anoxic marine sediments: implications for the geological record. Mar Geol 113:67–88

    Article  CAS  Google Scholar 

  • Geological Survey of India (2006) Gemorphological Map of Schirmacher Oasis, East Antarctica on 1:25,000 scale

    Google Scholar 

  • Hiller A, Wand U, Kampf H, Stackebrandt W (1988) Occupation of the Antarctic continent by petrels during the past 35 000 years: inferences from a 14C study of stomach oil deposits. Polar Biol 9:69–77

    Article  Google Scholar 

  • Jacobs J, Thomas RJ (2002) The Mozambique Belt from an East Antarctic perspective. IN Antarctica at the close of a Millennium. R Soc N Z Bull 35:3–18

    Google Scholar 

  • Kaul MK, Singh RK, Srivastava D, Jayaram S, Mukerji S (1991) Petrological and structural characteristics of a part of East Antarctic Craton, Queens Maud land, Antarctica. In: Thompson MRA, Crane JA, Thomson JW (eds) Geological evolution of Antarctica. Cambridge University Press, Cambridge, pp 89–94

    Google Scholar 

  • Krause WE, Krbetschek MR, Stolz W (1997) Dating of quaternary lake sediments from the Schirmacher Oasis (East Antarctica) by infra-red stimulated luminescence (IRSL) detected at the wavelength of 560 NM. Quat Sci Rev (Quat Geochronol) 16:387–392

    Article  Google Scholar 

  • Krinsley DH, Doornkamp JC (1973) Atlas of quartz sand surface textures. Cambridge University Press, Cambridge, pp 7–15

    Google Scholar 

  • Mahaney WC (1995) Glacial crushing, weathering and diagenetic histories of quartz grains inferred from scanning Electron Microscopy. In: Menzies J (ed) Modern glacial environment, processes, dynamics and sediments, vol 1. Batter worth Heinemann, Oxford, pp 487–506

    Google Scholar 

  • Mahesh BS, Warrier AK, Mohan R, Tiwari M, Anila B, Awasthi C, Astahna R, Ravindra R (2015) Response of long lake sediments to Antarctic climate: a perspective gained from sedimentary organic geochemistry and particle size analysis. Pol Sci 90:359–367

    Google Scholar 

  • Pant NC, Kundu A, D’Souza MJ, Saikia A (2013) Petrology of the Neoproterozoic granulites from Central Dronning Maud land, East Antarctica- implications for southward extension of East African Orogen (EAO). Precambrian Res 227:389–408

    Article  CAS  Google Scholar 

  • Phartiyal B (2014) Holocene paleoclimatic variation in the Schirmacher Oasis, East Antarctica: a mineral magnetic approach. Pol Sci 8(4):357–369

    Article  Google Scholar 

  • Phartiyal B, Sharma A, Bera SK (2011) Glacial lakes and geomorphological evolution of Schirmacher Oasis, East Antarctica, during late quaternary. Quat Int 235(1–2):128–136

    Article  Google Scholar 

  • Ravikant V, Laux JH, PIementel MM (2007) Sm-Nd and U-Pb isotopic constraints for crustal evolution during Late Neoproterozoic from rocks of the Schirmacher Oasis, East Antarctica: geodynamic development coeval with East African Orogeny. USGS and the National Academies. https://doi.org/10.3133/0f2007

  • Ravindra R (2001) Geomorphology of Schirmacher Oasis, East Antarctica. Proceeding symposium on snow, ice and glaciers. Geol Surv India 53:379–390

    Google Scholar 

  • Ravindra R (2013) Evolution of rocky oases in eastern Antarctica: studies by Indian scientists. In: Ramesh R, Sudhakar M, Chattopadhyay S (eds) Scientific and Geopolitical Interests in Arctic and Antarctic. In: Proceedings of international conference on science and geopolitics of Arctic and Antarctic, (SaGAA). LIGHTS, Research Foundation, New Delhi, p 296

    Google Scholar 

  • Ravindra R, Pandit MK (2000) Geochemistry and geochronology of A-type granite from northern Humboldt Mountain, East Antarctica: vestige of Pan-African event. J Geol Soc India 56:253–262

    CAS  Google Scholar 

  • Ravindra R, Pant NC, D’Souza MJ (1989) Geology of Central Queen Maud Land, East Antarctica. Geol Surv Ind Rec 122(2):197–199

    Google Scholar 

  • Ravindra R, Pant NC, D’Souza MJ (1991) Landscape Evalution of Humboldt and adjacent areas, Wohlthat Mountains, East Antarctica. J Geol Soc lndia 37(2):172–183

    Google Scholar 

  • Ravindra R, Dey A, Beg MJ, Kaul MK (1994) Observation on the snow accumulation/ablation over shelf and continental ice in parts of central dronning Maud Land, East Antarctica. Scientific report of ninth Indian expedition to Antarctica. DOD Tech Publ 6:227–238

    Google Scholar 

  • Ravindra R, Chaturvedi A, Beg MJ (2001) In: Sahoo DB, Pandey PC (eds) Melt-water Lakes of Schirmacher oasis-their genetic aspects and classification. Advances in Marine and Antarctic Sciences, New Delhi, pp 301–313

    Google Scholar 

  • Richter W, Bormann P (1993) In: Schirmacher (ed) Geomorphology. Schirmacher Oasis, Queen Maud Land, pp 171–206

    Google Scholar 

  • Richter W, Stranch G (1983) Deuterium and 1SO variation in lakes of the Schumacher oasis (East Antarctica). Isotopen Praxis 19(5):145–153

    CAS  Google Scholar 

  • Roy SK, Pant NC et al (2017) Geological studies in the Baalsrudfjellet nunatak and Wohlthat Mountains to establish the continuation of the East Antarctic Orogen (EAO) in the central Dronnn g Maud land. In: Pant NC, Dasgupta S (eds) Crustal evolution of India and Antarctica: the supercontinent connection. Geological Society, London, p 457. https://doi.org/10.1144/SP457.14

    Chapter  Google Scholar 

  • Sengupta S (1986) Precambrian rocks of the Schirmacher Range, East Antarctica. Z Geol Wiss 16:647–660

    Google Scholar 

  • Sharma C, Chauhan MS, Sinha R (2007) Studies on Holocene climatic changes from Priyadarshini Lake sediments, East Antarctica: the palynological evidence. J Geol Soc India 69:92–96

    Google Scholar 

  • Srivastava D, Kaul MK, Singh RK, Mukerji S, Jayaram S (1988) Some observations on the glacial geomorphological features of Wohlthat Mountains, Central Dronning Maud Land, Antarctica, Technical Publication No. 5. Department of Ocean Development, New Delhi, India

    Google Scholar 

  • Shrivastava PK, Asthana R, Beg MJ, Singh J (2009) Climatic fluctuation imprinted in quartz grains of lake sediments from Schirmacher Oasis and Larsemann Hills area, East Antarctica. Ind J Geosci 63(1):87–96

    Google Scholar 

  • Shrivastava PK, Asthana R, Roy SK, Swain AK, Dharwadkar A (2012) Provenance and depositional environment of epi-shelf lake sediment from Schirmacher Oasis, East Antarctica, vis-a-vis scanning electron microscopy of quartz grain, size distribution and chemical parameters. Elsevier. Pol Sci 6(2):165–182

    Article  Google Scholar 

  • Srivastava A, Kirtikumar R, Khare N (2013) Mineralogical and geochemical studies of glacial sediments from Schirmacher Oasis, East Antarctica. Quat Int 292:205–216. https://doi.org/10.1016/j.quaint.2012.07.028

    Article  Google Scholar 

  • Srivastava HB, Shrivastava PK, Roy SK et al (2018) Transition in late quaternary paleoclimate in Schirmacher region, East Antarctica as revealed from Lake sediments. J Geol Soc India 91(6):651–663. https://doi.org/10.1007/s12594-018-0920-z

    Article  Google Scholar 

  • Sinha R, Chatterjee A (2000) Lacustrine sedimentology in the Schirmacher Range Area, East Antarctica. J Geol Soc India 56:39–45

    CAS  Google Scholar 

  • Sinha R, Chatterjee A, Panda AK, Mitra A (1999) Thermal structure and heat budget of Priyadarshini Lake, Schirmacher Oasis, East Antarctica. Curr Sci 76(5):680–683

    Google Scholar 

  • Sinha R, Sharma C, Chauhan MS (2000) Sedimentological and pollen studies of Lake Priyadarshini, Eastern Antarctica. Palaeobotanist 49:1–8

    Google Scholar 

  • Stern RJ (1994) Arc assembly and continental collision in the Neoproterozoic East African Orogen: implications for the consolidation of Gondwana land. Annu Rev Earth Planet Sci 22:19–351

    Article  Google Scholar 

  • Warrier AK, Mahesh BS, Mohan R, Shankar R, Asthana R, Ravindra R (2014) Glacial interglacial climatic variations at the Schirmacher Oasis, East Antarctica: the first report from environmental magnetism. Palaeogeogr Palaeoclimatol Palaeoecol 412:249–260

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2020 Springer Nature Switzerland AG

About this chapter

Check for updates. Verify currency and authenticity via CrossMark

Cite this chapter

Ravindra, R. (2020). Glacial Sediments of Schirmacher Oasis, East Antarctica and their Characteristics. In: Goel, P., Ravindra, R., Chattopadhyay, S. (eds) Climate Change and the White World. Springer, Cham. https://doi.org/10.1007/978-3-030-21679-5_4

Download citation

Publish with us

Policies and ethics