Skip to main content

Geology, Stratigraphy, and Chronology of the Pilauco Site

  • Chapter
  • First Online:
Pilauco: A Late Pleistocene Archaeo-paleontological Site

Abstract

The Pilauco site is located in north-western Chilean Patagonia, Region de Los Lagos (40°34′12″S, 73°06′12″W). The stratigraphy of the site comprises of two distinct Pleistocene units. The lower unit corresponds to the sequence San Pablo of MIS5e age and consists of clastic and volcanoclastic sediments (PB-1 to PB-5). The upper unit includes the strata PB-6 to PB-9 with age constraints between 17,370 and 4,340 cal. year BP. The strata bearing fossil mammals and archaeological evidence (PB-7 and PB-8; 16,400–12,800 cal. year BP) correspond to layers of sand derived by means of colluvial transport from the nearby hills to the north of the site, in a fine-grained matrix of organic anoxic material and dispersed gravel clasts deposited in a seasonal wetland. The contact between the layers PB-8 and PB-9 is characterized by an erosional unconformity, a drastic increase in charcoal particles coeval with the nearly complete disappearance of pollen and other plant remains. Moreover, layer PB-9 lacks paleontological and archaeological remains. The discordance has been dated on ~12,800 cal. year BP, which coincides with the Younger Dryas Northern Hemisphere climatic oscillation. The local geological characteristics are concordant with regional geomorphological interpretations that have identified several terraces formed during the last glaciation and the Holocene.

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

Access this chapter

eBook
USD 16.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 16.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 109.99
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

Notes

  1. 1.

    http://calib.qub.ac.uk/calib/, consulted in July 2015.

  2. 2.

    http://calib.qub.ac.uk/calib/, consulted in July 2015.

References

  • Abarzúa A, Gajardo-Pichincura A (2008) ¿Y qué nos cuentan los polen?: Reconstruyendo la historia climática y vegetacional del sitio Pilauco. in: Pino M (ed.) Pilauco: Un sitio complejo del Pleistoceno tardío. Osorno, Norpatagonia chilena. Universidad Austral de Chile. Imprenta América, Valdivia, Chile, pp 49–53

    Google Scholar 

  • Andersson G (1896) Svenska växtvärldens historia. P. A. Norstedt & Söner, Stockholm

    Book  Google Scholar 

  • Arenas M, Milovic J, Pérez Y, Troncoso R, Behlau J, Hanisch J, Helms F (2005). Geología para el ordenamiento territorial: área de Valdivia, Región de Los Lagos. Servicio Nacional de Geología y Minería, Carta Geológica de Chile, Serie Geología Ambiental, No. 8, 71 p., 6 mapas escala 1:100.000 y 1 mapa escala 1:25.000

    Google Scholar 

  • Bentley JM (1997) Relative and radiocarbon chronology of two former glaciers in the Chilean Lake District. J Quat Sci 12(1):25–33

    Article  Google Scholar 

  • Björck S (2007) Younger Dryas oscillation, global evidence. In: Mock CJ, Scott E (eds) The encyclopedia of quaternary sciences. Elsevier, pp 1995–1983

    Google Scholar 

  • Boës X, Fagel N (2008) Timing of the late glacial and Younger Dryas cold reversal in southern Chile varved sediments. J Paleolimnol 39(2):267–281

    Article  Google Scholar 

  • Barnosky AD, Lindsey EL (2010) Timing of Quaternary megafaunal extinction in South America in relation to human arrival and climate change. Quat Int 217:10–29

    Article  Google Scholar 

  • Brüggen J (1945) Miscelánea geológica de las provincias de Valdivia y Llanquihue. Rev Chil Hist Geogr 2:90–113

    Google Scholar 

  • Corvalán N (1974) A new lahar in the central south Chile at the latitude of the Osorno (41oS). In: Abstracts of the IAVCEI symposium, Santiago, 4–6 June 1974

    Google Scholar 

  • Denton GH, Lowell TV, Heusser CJ, Schlüchter C, Andersen BG, Heusser LE, Moreno PI, Marchant DR (1999) Geomorphology, Stratigraphy, and radiocarbon chronology of Llanquihue driftin the area of the southern Lake District, Seno Reloncaví, and Isla Grande de Chiloé, Chile. Geogr Ann A 81(2):167–229

    Article  Google Scholar 

  • Faegri K, Iversen J (1989) Textbook of pollen analysis. Wiley, Londres

    Google Scholar 

  • González-Guarda E, Domingo L, Tornero C, Pino M, Fernández MH, Sevilla P, Agustí J (2017) Late Pleistocene ecological, environmental and climatic reconstruction based on megafauna stable isotopes from northwestern Chilean Patagonia. Quat Sci Rev 170:188–202

    Article  Google Scholar 

  • Hajdas I, Bonani G, Moreno PI, Ariztegui D (2003) Precise radiocarbon dating of Late-Glacial cooling in mid-latitude South America. Quat Res (Orlando) 59:70–78

    Article  Google Scholar 

  • Hartz N, Milthers V (1901) Det senglacie ler i Allerød tegelværksgrav. Medd Dansk Geol Føren 8:31–60

    Google Scholar 

  • Hogg AG, Hua Q, Blackwell PG, Niu M, Buck CE, Guilderson TP, Heaton TJ, Palmer JG, Reimer PJ, Reimer RW Turney CSM, Zimmerman SRH (2013) Shcal13 Southern Hemisphere calibration, 0–50,000 years cal BP. Radiocarbon 55(4):1889–1903

    Article  Google Scholar 

  • Illies H (1970) Geología de los alrededores de Valdivia y Volcanismo y Tectónica en márgenes del Pacífico en Chile Meridional. Universidad Austral de Chile, Valdivia

    Google Scholar 

  • International Unión of Geological Sciences (2009) Request for IUGS ratification to establish the quaternary as a system/period of the cenozoic and revise the associated base of the Pleistocene Series. http://www.iugs.org/

  • Laugénie C (1982) La région des Lacs, Chili méridional, recherches sur l’évolution géomorphologique d’un piémont glaciaire quater-naire andin. Dissertation, University of Bordeaux III

    Google Scholar 

  • Lauer W (1968) Die glaziallandschaft des südchilenischen Seengebietes. Acta Geogr 20:215–236

    Google Scholar 

  • Latorre C, Moreno P, Vargas G, Maldonado A, Villa-Martínez R, Armesto J, Villagrán C, Pino M, Núñez L, Grosjean M (2007) Quaternary environments and landscape evolution. In: Moreno T, Gibbons W (eds) Geology of Chile. Geological Society Press, London, pp 309–328

    Chapter  Google Scholar 

  • Lowell TV, Heusser CJ, Anderson BG, Moreno PI, Heusser LE, Heusser C, Slucter S, Marchant DR, Denton GH (1995) Interhemispheric correlation of Late Pleistocene glacial events. Science 269:1541–1549

    Article  Google Scholar 

  • Macías C (2012) Análisis de posible icnita en el Sitio Pilauco, Pleistoceno tardío, Osorno, Centro-Sur de Chile, Undergraduate Dissertation. Universidad Austral de Chile

    Google Scholar 

  • Massaferro JI, Moreno PI, Denton GH, Vandergoes M, Dieffenbacher-Krall A (2009) Chironomid and pollen evidence for climate fluctuations during the Last Glacial Termination in NW Patagonia. Quat Sci Rev 28:517–525

    Article  Google Scholar 

  • Mercer JH (1976) Glacial history of southernmost South America. Quat Res (Orlando) 6:125–166

    Article  Google Scholar 

  • Moreno PI (1997) Vegetation and climate change near Lago Llanquihue in the Chilean Lake District between 20,200 and 9500 14C yr BP. J Quat Sci 12:485–500

    Article  Google Scholar 

  • Moreno PI (2000) Climate, fire, and vegetation between about 13,000 and 9200 14C year BP in the Chilean Lake District. Quat Res (Orlando) 54:81–89

    Article  Google Scholar 

  • Moreno PI (2004) Millennial‐scale climate variability in northwest Patagonia over the last 15 000 yr. J Quat Sci 19(1):35–47

    Article  Google Scholar 

  • Moreno PI, León AL (2003) Abrupt vegetation changes during the last glacial to Holocene transition in mid-latitude South America. J Quat Sci 18:787–800

    Article  Google Scholar 

  • Moreno H, Varela J (1985) Geología, volcanismo y sedimentos piroclásticos cuaternarios la región central y sur de Chile. In Tosso J (ed) Suelos volcánicos de Chile. Capítulo 6. Instituto de Investigaciones Agropecuarias (INIA), pp 491–526

    Google Scholar 

  • Moreno PI, Jacobson GL, Andersen BG, Lowell TV, Denton GH (1999) Abrupt vegetation and climate changes during the last glacial maximum and the last Termination in the Chilean Lake District: a case study from Canal de la Puntilla (41°S). Geogr Ann A: Series A, Phy Geogr 81A:285–311

    Article  Google Scholar 

  • Moreno PI, Denton GH, Moreno H, Lowell TV, Putnam AE, Kaplan MR (2015) Radiocarbon chronology of the last glacial maximum and its termination in northwestern Patagonia. Quat Sci Rev 122:233–249

    Article  Google Scholar 

  • Moreno K, Bostelmann JE, Macías C, Navarro-Harris X, De Pol-Holz R, Pino M (2019). A late Pleistocene human footprint from the Pilauco archaeological site, Northern Patagonia, Chile. PLOS ONE PONE-D-18-03927R2 in press

    Article  Google Scholar 

  • Pérez Y, Milovic J, Troncoso R, Hanish F, Helms F, Toloczky M (2003) Geología para el ordenamiento territorial: Área de Osorno, Región de los Lagos. Servicio Nacional de Geología y Minería, Carta Geológica de Chile, Serie Geológica Ambiental No 6, 62 p, 7 mapas escala 1:100.000. Santiago

    Google Scholar 

  • Pino M, Miralles C (2008) La geología cuaternaria de Pilauco. In: Pino M (ed.). Pilauco, un Sitio complejo del Pleistoceno tardío. Osorno, Norpatagonia Chilena. Universidad Austral de Chile. Imprenta América, Valdivia, Chile, p 37–42

    Google Scholar 

  • Pino M, Chavez M, Navarro X, Labarca R (2013) The late Pleistocene Pilauco site, south central Chile. Quat Int 299:3–12

    Article  Google Scholar 

  • Pino, M., Martel-Cea, A., Astorga, G., Abarzúa, A.M., Cossio, N., Navarro, X., Lira, M.P., Labarca, R., Lecompte, M.A., Adedeji, V., Moore, C.R., Bunch, T.E., Mooney, C., Wolbach, W. S., West, A., Kennett, J.P. (2019). Sedimentary record from Patagonia, southern Chile supports cosmic- impact triggering of biomass burning, climate change, and megafaunal extinctions at 12.8 Ka. Sci Rep 9(1):4413

    Google Scholar 

  • Porter S (1981) Pleistocene glaciation in the Southern District of Chile. Quat Res (Orlando) 16:262–292

    Google Scholar 

  • Soto-Bollmann K (2014) Origen de la fracción arenosa de la capa portadora de megafauna del Sitio Pilauco, Osorno, Norpatagonia de Chile. Undergraduate Dissertation, Universidad Austral de Chile

    Google Scholar 

  • Stockmarr J (1971) Tablets with spores used in absolute pollen analysis. Pollen Spores 13:615–621

    Google Scholar 

  • Stuiver M, Reimer PJ (1993) Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35:215–230

    Article  Google Scholar 

  • Tello F, Elgueta M, Abarzúa AM, Torres F, Pino M (2017) Fossil beetles from Pilauco, south-central Chile: An Upper Pleistocene paleoenvironmental reconstruction. Quat Int 449:58–66

    Article  Google Scholar 

  • Whitlock C, Larsen C (2001) Charcoal as a proxy fire. In: Smol JP, Birks HJB, Last WM (eds) Tracking environmental change using Lake Sediments: Terrestrial, Algal, and Siliceous indicators. Kluwer Academic Publishers, Dordrecht, The Netherlands, pp 75–97

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Mario Pino .

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

Pino, M., Martel-Cea, A., Vega, R.M., Fritte, D., Soto-Bollmann, K. (2020). Geology, Stratigraphy, and Chronology of the Pilauco Site. In: Pino , M., Astorga, G. (eds) Pilauco: A Late Pleistocene Archaeo-paleontological Site. The Latin American Studies Book Series. Springer, Cham. https://doi.org/10.1007/978-3-030-23918-3_3

Download citation

Publish with us

Policies and ethics