[meteorite-list] Lago Strobel and fractal craters on 1 km el balsitic plateau, Argentina, full text of 2009 research on Holocene water levels and prehistoric culture: Cox: Barron: Murray 2011.07.21
From: Rich Murray <rmforall_at_meteoritecentral.com>
Date: Wed, 20 Jul 2011 23:33:47 -0700 Message-ID: <CAHqJ8pYGYWKcZ9TU7Dsmz_p0HpKwSG+g6np+nGn1vkMZ3zB1WQ_at_mail.gmail.com> Lago Strobel and fractal craters on 1 km el balsitic plateau, Argentina, full text of 2009 research on Holocene water levels and prehistoric culture: Rich Murray 2011.07.21 Lago Strobel, Argentina -48.439649 -71.158664 .722 km el 10 km size many ground views on Google Earth http://www.climategeology.ethz.ch/publications/2010_Ariztegui_et_al_JQS.pdf Lake-level changes in central Patagonia (Argentina): crossing environmental thresholds for Lateglacial and Holocene human occupation DANIEL ARIZTEGUI, 1 * ADRIAN GILLI, 2 FLAVIO S. ANSELMETTI, 3 RAFAEL A. GON? I, 4 JUAN B. BELARDI 5 and SILVANA ESPINOSA 5 1 Section of Earth and Environmental Sciences, University of Geneva, Geneva, Switzerland 2 Geological Institute, ETH Zu? rich, Zu? rich, Switzerland 3 Eawag, Swiss Federal Institute of Aquatic Science and Technology, Duebendorf, Switzerland 4 Instituto Nacional de Antropolog??a y Pensamiento Latinoamericano, Universidad de Buenos Aires, UNCPBA, Buenos Aires, Argentina 5 CONICET/Universidad Nacional de la Patagonia Austral, R??o Gallegos, Santa Cruz, Argentina Ariztegui, D., Gilli, A., Anselmetti, F. S., Gon? i, R. A., Belardi, J. B. and Espinosa, S. 2010. Lake-level changes in central Patagonia (Argentina): crossing environmental thresholds for Lateglacial and Holocene human occupation. J. Quaternary Sci., Vol. 25 pp. 1092?1099. ISSN 0267-8179. Received 30 May 2008; Revised 18 September 2009; Accepted 22 September 2009 ABSTRACT: The role and extent of climate as a cause of the expansion and decline of human cultures is still debatable. It is clear, however, that human?environment interactions are enhanced and interplay more closely in climatically sensitive areas such as around hydrologically closed basins. Lago Cardiel is located at 498 S in the very arid rain shadow east of the Andes, providing an exceptionally receptive system to changes in hydrological balance. Results of a geophysical survey combined with sedimentological and geochemical studies provide a continuous Lateglacia-?Holocene record of substantial water-level changes. These variations, combined with archaeological results from the catchment area, offer a unique possibility to explore the pattern of peopling within this remote area of the globe and its possible relation to climate change. Human occupation in Patagonia is well documented towards the Andes throughout the entire Holocene. Archaeological data from the Lago Cardiel basin, however, show an apparent lack of human activity during the ?rst part of this period, which coincides with well-constrained high lake levels. Our results show an intriguing coincidence between low lake level and increasing human occupation, suggesting that the Lago Cardiel basin has focused human use during intervals with relatively lower effective moisture such as during the Late Pleistocene, but its evidence may have been submerged. This interpretation is con?rmed by archaeological remains from Lago Strobel, another perennial lake with a comparable catchment located in the same climatic region and thus sharing the same climatic history as Lago Cardiel. Copyright # 2009 John Wiley & Sons, Ltd. KEYWORDS: eastern Patagonia; Late Pleistocene; Holocene; archaeology; limnogeology; human occupation. [ free full text ] Received on Thu 21 Jul 2011 02:33:47 AM PDT |
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