2/19/2024 0 Comments Clima en highland california![]() Cambridge, MA: Peabody Museum Bulletin 6, 181-196. “Measures of Mobility and Occupational Intensity in Highland Peru.” In Identifying Seasonality and Sedentism in Archaeological Sites: Old and New World Perspectives, ed. London: BAR International Series 427, 154-166. “Hunting and Herding Economies on the Junin Puna.” In Economic Prehistory of the Central Andes, ed. “Preceramic Transhumance in the Callejón de Huaylas, Peru.” American Antiquity 36: 139-148. “Excavations at Quishqui Puncu in the Callejón de Huaylas, Peru.” Occasional papers of the Idaho State University Museum 26. Beiträge zur Kenntnis der Lithischen Perioden in der Puna Junins, Peru. “Lauricocha: Fundamentos para una Prehistória de los Andes Centrales.” Studia Praehistórica 3. “Ancient Human Remains from Central Peru.” American Antiquity 46: 167-178.Ĭardich, A. Cuenca, Ecuador: La Universidad de Cuenca.īeynon, D. El Hombre Temprano en la Región del Ilaló, Sierra del Ecuador. New York: Cambridge University Press, 3-40. ![]() “The Character and Context of Highland Preceramic Society.” In Peruvian Prehistory, ed. Lima: Instituto Andino de Estudios Arqueológicos. Cronologia, Clima, y Subsistencia en el Precerámico Peruano. “Paleoindian and Archaic Cultural Periods in the Arid and Semiarid Regions of Northern Chile.” Advances in World Archaeology, 2: 161-203. Prehistory of the Ayacucho Basin, Peru: vol. “The Nature of the Andean Preceramic.” Occasional Papers of the Idaho State Museum 21. Paris: Institut Francais D’Études Andines. Telarmac-hay: Chasseurs et Pasteurs Préhistoriques des Andes, I. Lauricocha: Fundamentos para una Prehistória de los Andes Centrales. “Los Yacimientos de Lauricocha y la Nueva Interpretación de la Prehistoria Peruana.” Studia Praehistórica 1.Ĭardich, A. ![]() Iowa City: University of Iowa Press.Ĭardich, A. Montane Foragers: Asana and the South-Central Andean Archaic. Finally, the paper evaluates the application of non-pollen palynomorphs, especially coprophilous fungal spores, at Prato Spilla ‘A’ (Emilia Romagna) and concludes that greater caution must be used when interpreting middle Holocene human activity based upon pollen data alone.Aldenderfer, M. Throughout the middle Holocene, Abies woodland fl uctuates, with marked declines between 6488-6318 cal yrs BP and 5287-4835 cal yrs BP, although the cause remains uncertain. Fagus woodland becomes established sometime before 6488-6318 cal yrs BP, but never becomes a major component of the woodland cover. During the early Holocene, mixed coniferous-deciduous woodland is dominant with Quercus, as well as Abies, Fagus and Corylus. The ‘Younger Dryas’ is possibly represented by an increase in Betula and Artemisia. This is succeeded by Betula and Pinus woodland, and the expansion of thermophilous taxa, namely Abies, Corylus and Quercus during the Late Würm Lateglacial Interstadial. The record indicates the transition from open Pinus woodland to Artemisia dominated grassland, and finally Juniperus shrubland during the late Würm. An enhanced radiocarbon-dated pollen-stratigraphical record from Rovegno (Liguria, 812m asl), northern Apennines (Italy), has provided a history of vegetation succession from before 17,056-16,621 cal yrs BP to the present day.
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