Landscapes of Power and Identity: Comparative Histories in the Sonoran Desert and the Forests of Amazonia from Colony to Republic

Landscapes of Power and Identity: Comparative Histories in the Sonoran Desert and the Forests of Amazonia from Colony to Republic . Cynthia Radding. Durham, NC: Duke University Press, 2005. 431 pp.     

Post-Boom Logging in Amazonia

Recent analyses of timber exploitation in Amazonia conclude that a variety of socioeconomic and ecological factors in the region make a stable and profitable logging industry virtually impossible. Most of these studies focus on large-scale timber industries and their dependence on over-exploitation of a small number of high-value timbers. In this article we discuss the economic, ecological, and social aspects of Amazonian logging in a region where the timber industry appeared to have collapsed after stocks of high-value timber were exhausted. We show that forestry in a post-boom phase, currently found in many areas of Amazonia, differs from the better-described boom period in its scale of operations, in the range of timbers cut, in management practices employed, and in the costs and benefits of production. Results of a seven-year study show that when sawtimber, poles and firewood are produced in a management system that combines forestry and agriculture they can provide significant additional income for Amazonian smallholders.     

Predicting pre-Columbian anthropogenic soils in Amazonia

The extent and intensity of pre-Columbian impacts on lowland Amazonia have remained uncertain and controversial. Various indicators can be used to gauge the impact of pre-Columbian societies, but the formation of nutrient-enriched terra preta soils has been widely accepted as an indication of long-term settlement and site fidelity. Using known and newly discovered terra preta sites and maximum entropy algorithms (Maxent), we determined the influence of regional environmental conditions on the likelihood that terra pretas would have been formed at any given location in lowland Amazonia. Terra pretas were most frequently found in central and eastern Amazonia along the lower courses of the major Amazonian rivers. Terrain, hydrologic and soil characteristics were more important predictors of terra preta distributions than climatic conditions. Our modelling efforts indicated that terra pretas are likely to be found throughout ca 154 063 km² or 3.2% of the forest. We also predict that terra preta formation was limited in most of western Amazonia. Model results suggested that the distribution of terra preta was highly predictable based on environmental parameters. We provided targets for future archaeological surveys under the vast forest canopy and also highlighted how few of the long-term forest inventory sites in Amazonia are able to capture the effects of historical disturbance.     

Projecting future fire activity in Amazonia

Fires are major disturbances for ecosystems in Amazonia. They affect vegetation succession, alter nutrients and carbon cycling, and modify the composition of the atmosphere. Fires in this region are strongly related to land‐use, land‐cover and climate conditions. Because these factors are all expected to change in the future, it is reasonable to expect that fire activity will also change. Models are needed to quantitatively estimate the magnitude of these potential changes. Here we present a new fire model developed by relating satellite information on fires to corresponding statistics on climate, land‐use and land‐cover. The model is first shown to reproduce the main contemporary large‐scale features of fire patterns in Amazonia. To estimate potential changes in fire activity in the future, we then applied the model to two alternative scenarios of development of the region. We find that in both scenarios, substantial changes in the frequency and spatial patterns of fires are expected unless steps are taken to mitigate fire activity.     

Shamanism, Christianity and Culture Change in Amazonia

Among many indigenous peoples of Amazonia, shamanism and Christianity co-exist as central cultural elements shaping the ways in which people interpret and interact with the world. Despite centuries of co-existence, the relationship between shamanism and Christianity has entered an especially dynamic era as many of Amazonia’s indigenous peoples abandon Catholicism for Evangelical and Sabbatarian churches. Testing the relationship between Christian church affiliation and shamanism in 23 Makushi and Wapishana communities in southern Guyana, we found that Evangelicals and Sabbatarians are less likely to visit shamans or accept their legitimacy than are Anglicans and Catholics. However, conversion does not necessarily imply a complete rejection of indigenous religious systems as many self-identified Evangelicals and Sabbatarians continue to adhere to some indigenous beliefs and practices. We conclude by positing possible implications of religious conversion for natural resource use on indigenous lands.     

Missionary Encounters: Histories and Memoirs

Alexander Merensky: Erinnerungen aus dem Missionsleben in Transvaal (Südafrika) 1859 bis 1882. Ulrich van der Heyden. ed. Cognoscere, 5. Berlin: Edition Ost, 1996.560 pp.
Hate the Old and Follow the New: Khoekhoe and Missionaries in Early Nineteenth-Century Namibia. Tilman Dedering. Stuttgart, Germany: Franz Steiner Verlag, 1997. 205 pp.     

Natural Histories of Discourse

Natural Histories of Discourse. Michael Silverstein and Greg Urban. eds. Chicago: University of Chicago Press, 1996. 352 pp.     

Plant Communities of Western Amazonia

In this review I focus on the socially and ecologically important western Amazon basin and its associated plant communities. I delineate this vast area as between the Andes to the west and the confluence of the Amazon and its first major black-water river, the Rio Negro, to the east. Although scientists have explored here, and local people have lived here for years, we still have—unfortunately—only a most basic understanding of its plant communities. This review is motivated by that lack of knowledge, and attempts both to add a level of organization to what we do know and to suggest future avenues of research. I do this by first realizing that plant communities here must be fundamentally differentiated by the degree of flooding they experience, the kind of water involved, and how regularly that flooding occurs. Within that context, plant communities can then be further defined by such characteristics as soil type, micro-topological relief, and human-induced disturbance regime. After completing the review, I suggest that the diversity of plant communities, not just the plants themselves, is large and likely to grow substantially as we sample more and more, that is to say the peak of the plant community-sampling area curve has not yet been reached. I close with basic questions to help guide future efforts, ideas on how plant communities could be defined quantitatively, and a call for more research funding of the Western Amazon.     

Leaf functional traits and monodominance in Southern Amazonia tropical forests

Tropical monodominant forests are rare communities with low tree species diversity. Species monodominance is not the product of a single mechanism, but the result of a set of not yet fully understood integrated ecological factors acting together. We compared populations of Brosimum rubescens in monodominant and mixed forests in Southern Amazonia to test whether leaf functional traits are ecological factors related to monodominance. Individuals of B. rubescens in the mixed forest invest in conservative strategies, while those in the monodominant forest invest in acquisitive strategies. Leaf functional traits, such as petiole length and adaxial cuticle thickness, could be associated with the monodominance of B. rubescens. Our study highlights for the first time the power of integrating leaf functional traits as a component of the set of ecological conditions to explain species monodominance. B. rubescens showed different functional strategies to establish and maintain its population in different forests, which makes it a strong competitor for resources, such as water and light, through variation in its leaf functional traits. We also suggest that such high plasticity can be an important condition for the persistence of the species over time.

     

Dynamics, patterns and causes of fires in Northwestern Amazonia

According to recent studies, two widespread droughts occurred in the Amazon basin, one during 2005 and one during 2010. The drought increased the prevalence of climate-driven fires over most of the basin. Given the importance of human-atmosphere-vegetation interactions in tropical rainforests, these events have generated concerns over the vulnerability of this area to climate change. This paper focuses on one of the wettest areas of the basin, Northwestern Amazonia, where the interactions between the climate and fires are much weaker and where little is known about the anthropogenic drivers of fires. We have assessed the response of fires to climate over a ten-year period, and analysed the socio-economic and demographic determinants of fire occurrence. The patterns of fires and climate and their linkages in Northwestern Amazonia differ from the enhanced fire response to climate variation observed in the rest of Amazonia. The highest number of recorded fires in Northwestern Amazonia occurred in 2004 and 2007, and this did not coincide with the periods of extreme drought experienced in Amazonia in 2005 and 2010. Rather, during those years, Northwestern Amazonia experienced a relatively small numbers of fire hotspots. We have shown that fire occurrence correlated well with deforestation and was determined by anthropogenic drivers, mainly small-scale agriculture, cattle ranching (i.e., pastures) and active agricultural frontiers (including illegal crops). Thus, the particular climatic conditions for air convergence and rainfall created by proximity to the Andes, coupled with the presence of one of the most active colonisation fronts in the region, make this region differently affected by the general drought-induced fire patterns experienced by the rest of the Amazon. Moreover, the results suggest that, even in this wet region, humans are able to modify the frequency of fires and impact these historically well preserved forests.     

Natural hybridization betweenSaimiri taxa in the Peruvian Amazonia

A wild population situated in the border of the distributions ofSaimiri sciureus macrodon andS. boliviensis peruviensis, in the Peruvian Amazonia, was studied in relation to 22 protein loci. These genetic markers provided indications of secondary intergradation between these two taxa, reinforcing previous morphological and cytogenetic evidences. Continued studies in this region on the hybrids' viability and fertility may be important for decisions related to the taxonomy of this genus.     

Agricultural intensification increases deforestation fire activity in Amazonia

Fire-driven deforestation is the major source of carbon emissions from Amazonia. Recent expansion of mechanized agriculture in forested regions of Amazonia has increased the average size of deforested areas, but related changes in fire dynamics remain poorly characterized. We estimated the contribution of fires from the deforestation process to total fire activity based on the local frequency of active fire detections from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors. High-confidence fire detections at the same ground location on 2 or more days per year are most common in areas of active deforestation, where trunks, branches, and stumps can be piled and burned many times before woody fuels are depleted. Across Amazonia, high-frequency fires typical of deforestation accounted for more than 40% of the MODIS fire detections during 2003–2007. Active deforestation frontiers in Bolivia and the Brazilian states of Mato Grosso, Pará, and Rondônia contributed 84% of these high-frequency fires during this period. Among deforested areas, the frequency and timing of fire activity vary according to postclearing land use. Fire usage for expansion of mechanized crop production in Mato Grosso is more intense and more evenly distributed throughout the dry season than forest clearing for cattle ranching (4.6 vs. 1.7 fire days per deforested area, respectively), even for clearings >200 ha in size. Fires for deforestation may continue for several years, increasing the combustion completeness of cropland deforestation to nearly 100% and pasture deforestation to 50–90% over 1–3-year timescales typical of forest conversion. Our results demonstrate that there is no uniform relation between satellite-based fire detections and carbon emissions. Improved understanding of deforestation carbon losses in Amazonia will require models that capture interannual variation in the deforested area that contributes to fire activity and variable combustion completeness of individual clearings as a function of fire frequency or other evidence of postclearing land use.