Reviews of books

Historia, utopía y ficción de la Ciudad de los Césares. Metamorfosis de un mito. Por FERNANDO AINSA. Madrid: Alianza Editorial, 1992. Pp. 120.

Cultural Diffusion of Spanish Humanism in New Spain: Francisco Cervantes de Salazar's ‘Diálogo de la dignidad del hombre.’ By DIANNE M. BONO. New York: Peter Lang, 1991. Pp. 161.

Soldiers of the Virgin: The Moral Economy of a Colonial Maya Rebellion. By KEVIN GOSNER. Tucson: University of Arizona Press, 1992. Pp. xiv, 227.

La crisis del orden colonial. Estructura agraria y rebeliones populares de la Nueva España, 1750–1821. By ERIC VAN YOUNG. México: Alianza Editorial, 1992. Pp. 515.

Esthetic Recognition of Ancient Amerindian Art. By GEORGE KUBLER. New Haven: Yale University Press, 1991. Pp. xvii, 276.

Books of the Brave: Being an Account of Books and of Men in the Spanish Conquest and Settlement of the Sixteenth‐Century New World. By IRVING A. LEONARD. Introduced by ROLENA ADORNO. Berkeley: University of California Press, 1992. Pp. xlvii, 453.

Family and Frontier in Colonial Brazil: Santana de Parnaíba, 1580–1822. By ALIDA C. METCALF. Berkeley: University of California Press, 1992. Pp. xvi, 280.

Los naufragios. By ALVAR NUÑEZ CABEZA DE VACA. Edición crítica de ENRIQUE PUPO‐WALKER. Madrid: Castalia, 1992. Pp. 334.

Estudios de literatura hispanoamericana. Sor Juana Inés de la Cruz y otros poetas barrocos de la colonia. By GEORGINA SABAT‐RIVERS. Barcelona: PPU, 1992. Pp. 355.

Vida i sucesos de la monja alférez. Autobiografía atribuida a Doña Catalina de Erauso. Edición, introducción y notas de RIMA DE VALLBONA. Tempe: Center for Latin American Studies, Arizona State University, 1992. Pp. 236.     

Reviews

Sans résumé

---

Reviews

     

A late Holocene pollen record from Lake Almalou in NW Iran: evidence for changing land-use in relation to some historical events during the last 3700 years

A pollen diagram was prepared from Lake Almalou, a volcanic crater wetland located on the eastern flanks of the Sahand Volcanic Complex in NW Iran. The core provides a 3700-year record of human activity and environmental change in an upland region. We attempt to relate vegetation changes to both climatic change and historical events. Variations of anthropogenic pollen indicators suggest several phases of intensified human activities. Two strongly expressed agricultural phases are dated at about 2450–2220 cal BP (Achaemenid Empire) and 230–30 cal BP (collapse of Safavid Dynasty to the modern period). Historical rather than climatic events appear to be the main controlling factors for upland land-use dynamics. Fruticulture has been practiced in the region at least since the Iron Age, reaching its maximum importance 1500–1250 cal BP during the reign of Sassanid Empire; it declined by the time of Islamic conquest of Iran (651 AD). The Little Ice Age is tangibly recorded by higher lake water levels most probably due to both lower summer temperatures and higher annual precipitations. Low values of cereal-type and cultivated tree pollen during this period may indicate a change in the lifestyle from the cultivation of fields and orchards to a more nomadic life dominated by summer pasture. The modern period (1850 AD onwards) is characterized by expansion of agricultural activities to upland areas and intensified pastoralism.     

Isotopic analysis of the ecology of herbivores and carnivores from the Middle Pleistocene deposits of the Sierra De Atapuerca,northern Spain

Carbon and oxygen isotope values reveal resource partitioning among the large mammal fauna from three contemporaneous Middle Pleistocene hominid-bearing localities within the Sierra de Atapuerca (northern Spain). Carbon isotope values sampled from the tooth enamel of fauna present during Atapuerca Faunal Unit 6 show that a C₃-dominated ecosystem surrounded the area where fossils were preserved during this time. For the herbivores, Fallow deer isotope values are significantly different from Red deer and horses and show that this species did not forage in open environments at this locality. Red deer and horses show similar feeding strategies with less negative carbon values implying use of more open environments for these taxa. For the carnivores, carbon isotope values for Ursus deningeri are significantly different from either lions (Panthera leo) or foxes (Vulpes vulpes) and support the contention that this species is herbivorous. Special metabolic mechanisms involved in hibernation in U. deningeri might also have influenced its isotope values. The carbon isotope values of remaining carnivores were similar and suggest that each was typically a generalist carnivore, eating a wide variety of prey items. While the isotopic results generally correspond to ecology indicated by previous techniques, this study shows that isotope analyses can provide further insights that alternate techniques do not provide. Isotope analyses can help elucidate the ancient ecology of taxa present in the Sierra de Atapuerca during the Middle Pleistocene allowing for an accurate portrayal of the setting in which humans lived.