Abstract
Marine Isotope Stage 3 (MIS 3) is characterized by high climatic variability resulting from numerous centennial to millennial scale events. The environmental and climatic reconstruction of this interval is restricted by the sparsity of high-resolution (centennial-scale) terrestrial records in most of South America. This contribution is an attempt to reconstruct the general environmental and climatic conditions of southern South America during MIS 3 by means of continental records located in central Argentina; this is an extensive and heterogeneous region made up of diverse geomorphological settings under different climatic conditions. Therefore, the main features of several aeolian and fluvial records situated in different geomorphological settings across the region are overviewed. The results indicate the predominance of regional aggradation during MIS 3 with differences in the accumulation rates and dominance of either aeolian or fluvial deposits depending on the geomorphological setting. The aggradation process was interrupted by stability intervals evidenced by paleosols in the San Rafael plain, the San Luis paleo-dunefield, the eastern Sierras Pampeanas piedmont and the eastern Pampean plain. The paleosols might represent lapses of decreasing aeolian input and perhaps more humid conditions. In addition, paleobiological indicators from alluvial sequences suggest higher temperatures and water availability between 35 and 31 ka in the Andean piedmont , while dry subhumid or strongly seasonal conditions with alternating subhumid-humid phases were inferred in the eastern Pampean plain during MIS 3. These intervals tend to cluster during the second part of MIS 3, and might reflect the environmental responses to some of the climatic oscillations that occurred during MIS 3. Detailed analysis and a more adjusted chronology are needed to correlate the aeolian and fluvial episodes along with the stability intervals at regional and continental scales.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Akers P, Brook G, Liang F, Wang X, Auler A, Railsback B, Cheng H, Edwards RL, Benedetto C (2014) A 48,000 year record of climate change in west central Argentina from stalagmites in Caverna de las Brujas. Climate Change: The karst record, 7th International Conference, Melbourne, 29 Sept–2 Oct, 2014, Abstract with Programme, p 20–21
Baker SE, Gosse JC, McDonald EV, Evenson EB, Martínez O (2009) Quaternary history of the piedmont reach of Río Diamante, Argentina. J South Amer Earth Sci 28:54–73
Blasi A, Castiñeira Latorre C, Del Puerto L, Prieto AR, Fucks E, De Francesco C. Hanson P, García Rodríguez F, Huarte R, Carbonari J, Young A (2010) Paleoambientes de la cuenca media del río Luján (Buenos Aires, Argentina) durante el último período glacial (EIO 4–2) Lat Am J Sedimentol Basin Anal 17(2):85–111
Bradley R (2015) Paleoclimatology, reconstructing climates of the quaternary, 3rd edn. Elsevier, Amsterdam 675 p
Carignano CA (1999) Late Pleistocene to recent climatic change in Córdoba Province, Argentina: geomorphological evidence. Quat Int 57–58:117–134
De Francesco CG, Zárate MA, Miquel SE (2007) Late Pleistocene mollusc assemblages inferred from paleoenvironments from the Andean piedmont of Mendoza, Argentina. Palaeogeogr Palaeoclimatol Palaeoecol 257:461–469
Frechen M, Seifert B, Sanabria JA, Argüello GL (2009) Chronology of late Pleistocene Pampa loess from the Córdoba area in Argentina. J Quat Sci 24:761–772
Gómez Orellana L, Ramil-Rego P, Muñoz Sobrino C (2007) The Würm in NW Iberia, a pollen record from area Longa (Galicia). Quat Res 67:438–452
Isla F, Schnack E (this volume) Sea level changes during the marine isotopic stage 3 in Argentina
Kemp RA, Toms PS, King M, Kröhling DM (2004) The pedosedimentary evolution and chronology of Tortugas, a late quaternary type-site of the northern Pampa, Argentina. Quat Int 114(1):101–112
Kemp R, Zárate MA, Toms PS, King M, Sanabria J, Arguello G (2006) Late Quaternary paleosols, stratigraphy and landscape evolution in the Northern Pampas, Argentina. Quat Res 66:119–132
Kröhling D (1999) Upper quaternary of the lower Carcarañá basin, North Pampa, Argentina. Quat Int 57(58):135–148
Latrubesse EM, Ramonell CG (2010) Landforms and chronology in the Pampean sand sea, Argentina. Abstracts Volumen, 18 International Sedimentological Congress, Mendoza, Argentina, p 529
Latrubesse EM, Stevaux JC, Cremon EH, May J-H, Tatumi SH, Hurtado MA, Bezada M, Argollo JB (2012) Late megafans, fans and fluvio-aeolian interactions in the Bolivian Chaco, Tropical South America. Palaeogeogr Palaeoclimatol Palaeoecol 356–357:75–88
Martinson DG, Pisias NG, Hays JD, Imbrie JD, Moore TC, Shackleton NJ (1987) Age Dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year chronostratigraphy. Quat Res 27:1–29
Marwan N, Trauth MH, Vuille MM, Kurths M (2003) Comparing modern and Pleistocene ENSO-like influences in NW Argentina using nonlinear time series analysis methods. Clim Dyn 21(3–4):317–326
Mehl AE, Zárate MA (2012) Late Quaternary alluvial records and environmental conditions in the eastern of Mendoza (33–34° S) Argentina. J South Amer Earth Sci 37:41–59
Messager G (2010) Signatures geomorphologiques de l’activite tectonique Plio-Quaternaire dans le sud des Andes Centrales, Argentine. Unpublished PhD thesis, Université de Pau et des Pays de L’Adour
Pepin E (2010) Interactions géomorphologiques et sédimentaires entre bassin versant et piedmont alluvial. Modélisation numérique et exemples naturels dans les Andes. Unpublished PhD thesis, Université de Toulouse, 282
Pisias NG, Martinson DG, Moore TC Jr, Shackleton NJ, Prell W, Hays J, Boden G (1984) High resolution stratigraphic correlation of benthic oxygen isotopic records spanning the last 300,000 years. Marine Geol 56:119–136
Rabassa J (2008) Late Cenozoic glaciations in Patagonia and Tierra del Fuego. In: Rabassa J (ed), The late Cenozoic of Patagonia and Tierra del Fuego, pp 157–198
Siddall M, Rohling EJ, Thompson WG, Waelbroeck W (2008) Marine isotope stage 3 sea level fluctuations: data synthesis and new outlook Rev Geophys 46:RG4003
Tripaldi A, Forman SL (2007) Geomorphology and chronology of Late Quaternary dune fields of western Argentina. Palaeogeogr Palaeoclimatol Palaeoecol 251:300–320
Tripaldi A, Zárate MA, Brook G, Li Giang G (2011) Late Quaternary paleoenvironments and paleoclimatic conditions in the distal Andean piedmont, southern Mendoza, Argentina. Quat Res 76:253–263
Tripaldi A, Zárate MA (2014) A review of late quaternary dune systems for tropical and subtropical South American east of the Andes. Quat Int. doi:10.1016/j.quaint.2014.06.069
Trauth MH, Bookhagen B, Marwan N, Strecker MR (2003) Multiple landslide clusters record quaternary climate changes in the northwestern Argentine Andes. Palaeogeogr Palaeoclimatol Palaeoecol 194:109–121
Veres D, Bazin L, Landais A, Toyé Mahamadou Kele B, Lemieux-Dudon B, Parrenin F, Martinerie P, Blayo E, Blunier T, Capron E, Chappellaz J, Rasmussen SO, Severi M, Svensson A, Vinther B, Wolff EW (2013) The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years. Clim Past 9:1733–1748
Voelker AHL (2002) Global distribution of centennial-scale records for marine isotope stage (MIS) 3: a database. Quat Sci Rev 21:1185–1212
Wolff EW, Chappellaz J, Blunier T, Rasmussen SO, Svensson A (2010) Millennial-scale variability during the last glacial: the ice core record. Quat Sci Rev 29:2828–2838
Zárate MA (2009) El paisaje pampeano a través del tiempo. In: Berón M, Luna L, Bonomo M, Montalvo C, Aranda C, Carrera Aizpitarte M (eds.), V Congreso de Arqueología de la Región Pampeana. Mamul Mapu. Pasado y Presente desde la Arqueología Pampeana. Editorial Libros del Espinillo, Buenos Aires, p 19–32
Zárate MA, Tripaldi A (2012) The aeolian system of central Argentina. J Aeolian Res 3(4):401–417
Zárate M, Kemp R, Toms P (2009) Late Quaternary landscape reconstruction and geochronology in the northern Pampas of Buenos Aires province, Argentina. J South Am Earth Sci 27:88–99
Acknowledgments
The authors wish to express their gratitude to Jorge Rabassa and Eduardo P. Tonni for the invitation to one of authors (MZ) to participate at the La Plata MIS 3 symposium. We also want to thank Germán M. Gasparini for his help and patience during the preparation of this paper. Financial support was provided by EXA 234-UNLPam, PIP CONICET-2011 and UBA (UBACyT 20620100100009).
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2016 Springer International Publishing Switzerland
About this chapter
Cite this chapter
Zárate, M., Mehl, A., Tripaldi, A. (2016). The Continental Record of Marine Isotope Stage 3 (MIS 3; ~60–25 ka) in Central Argentina: Evidence from Fluvial and Aeolian Sequences. In: Gasparini, G., Rabassa, J., Deschamps, C., Tonni, E. (eds) Marine Isotope Stage 3 in Southern South America, 60 KA B.P.-30 KA B.P.. Springer Earth System Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-40000-6_10
Download citation
DOI: https://doi.org/10.1007/978-3-319-40000-6_10
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-39998-0
Online ISBN: 978-3-319-40000-6
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)