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A paisagem da parte sul do Pantanal é formada por um mosaíco de rios, lagos, brejos, campos úmidos estacionais e florestas que são fortemente influenciados pelos níveis da água no solo. Ao sul do Rio Negro, na região de inundação estacional, desenvolve-se a forma clássica da savana úmida que apresenta como grandes extensões de campo com arbustos e árvores (Curatella americana, Byrsonima orbignyana) os quais são resistentes à inundação.
Boundaries and processes; Forest-savanna boundaries: general considerations; Ecological processes at the forest-savanna boundary; Physical environment at the Boundary; Mapping forest and savannas in sub-Saharan Africa from advanced very high resolution radiometer (AVHRR) imagery; Influence of physical factors on the nature and dynamics of forest-savanna boundaries; Dynamics of the forest-savanna boundary in the Rio Branco-Rupunini region of northern Amazonia. Edaphic changes at the forest-savanna boundary with particular reference to the neotropics; Soil and litter nutrient losses in forest clearings close to a forest-savanna boundary on Maraca Island, Roraima, Brazil; Soil conditions and soil biology in different habitats across a forest-savanna boundary on Maraca Island, Roraima, Brazil; Observations on soils, foliar nutrient concentrations and floristic composition of cerrado sensu stricto and cerradao communities in central Brazil; Soil formation and nutrient dynamics at the woodland-savanna boundary in East Africa; Environmental change and vegetation; Landscape dynamics and surface deposits arising from late quaternary fluctuations in the forest-savanna boundary; The development of rainforest-savanna boundaries in tropical Australia; Ultraviolet V-B insolation and the altitudinal forest limit; How old are South Africa's grasslands? Vegetation structure and dynamics at the boundary; The phytogeography of savanna species of neotropical Chrysobalanaceae; The nature and the dynamics of the forest-savanna boundary in south-western Nigeria; Effects of trees on understorey vegetation and soils at forest-savanna boundaries in East Africa; The forest-savanna boundary on Maraca Island, Roraima, Brazil: an investigation of two contrasting transects; Floristic composition, phytosociology and comparison of cerrado and gallery forests at Fazenda Agua Limpa, Federal District, Brazil; Transitions between cerrado and forest vegetation in Brazil; Observations on the differentiation of woodland and wet savanna habitats in the Pantanal of Mato Grosso, Brazil; The Chaco-Pantanal transition in southern Mato Grosso, Brazil; Animals at the forest-savanna boundary; Soil fauna at the forest-savanna boundary: role of the termite mounds in nutrient cycling; The chemical ecology of forest and savanna termites; The forest-savanna boundary and habitat selection by Brazilian social wasps; The importance of forest edges in the ecology of open country cerrado birds; The role of mammals in neotropical forest-savanna boundaries; Modelling of the Boundary; Modelling energy flows and surface temperatures over forest and savanna; Modelling the location of woody-grassland boundaries; A conceptual model relating environmental factors and vegetation formations in the lowlands of tropical South America.
There are many famous wetlands in the world that have been deemed important for the homeostasis ofthe biosphere and accorded some form ofprotected status in view of the richness of their flora and fauna. T}1e Pantanal, located almost directly in the center ofthe South American continent, is among the largest such wetlands in the world. It is, in fact, the largest wetland that is still in a nearly natural state and has not been extensively modified by man for agriculture. The extent of the region covered by flood waters at the end of each rainy season varies from year to year, sometimes considerably, so estimates of the exact area it occupies have varied enormously. The size of the 2 2 Pantanal has been reported to be between 80,000 km (Bonetto, 1975) and 250,000 km (Tundisi and Matsumura-Tundisi, 1985). The most co~on1y accepted estimates at the present time are approximately 130,000 to 140,000 km , supported by estimates made from Nimbus-7 satellite observations (Hamilton et al. , 1996). However, Por (1995) suggested that the area extending into Bolivia and Paraguay has not been satisfactorily 2 surveyed, leading him to accept the figure of 200,000 km as the area of the entire Pantanal, ineluding all of its extensions. The main reason for the year to year variation in the extent of the flooding is the considerable difference in timing of the rainfall on the watershed.
The international journal Ecohydrology & Hydrobiology (E&H) has been created to promote the concept of Ecohydrology, which is defined as the study of the functional interrelations between hydrology and biota at the catchment scale. Ecohydrology extends from the molecular level to catchment-scale processes and is based on three principles: • framework (hydrological principle) - quantification and integration of hydrological and ecological processes at a basin scale; • target (ecological principle) - necessity of enhancing ecosystem absorbing capacity and ecosystem services; and • management tool (ecological engineering) – the use of ecosystem properties for regulation the interplay between hydrology and biota. The journal encourages the submission of manuscripts which adopt an integrative approach to aquatic sciences, explaining ecological and hydrological processes at a river-basin scale or propose practical applications of this knowledge. It will also consider papers in other hydrobiological fields. Especially welcome are papers on regulatory mechanism within biocenosis and the resistance and resilience of freshwater and costal zones ecosystems. There is no page charge for published papers. All submitted papers, written exclusively in English, should be original works, unpublished and not under consideration for publication elsewhere. All papers are peer-reviewed. The following types of papers are considered for publication in E&H: • original research papers • invited or submitted review papers, • short communications
The massive grasslands of Brazil -- known as the cerrados -- which cover roughly a quarter of its land surface and are among the most threatened regions in South America, have received little media attention. This book brings together leading researchers on the area to produce the first detailed account in English of the natural history and ecology of the cerrado/savanna ecosystem. Given their extent and threatened status, the richness of their flora and fauna, and the lack of familiarity with their unique ecology at the international level, the cerrados are badly in need of this important and timely work.
We often envision the New World before the arrival of the Europeans as a land of pristine natural beauty and undisturbed environments. However, David Lentz offers an alternative view by detailing the impact of native cultures on these ecosystems prior to their contact with Europeans. Drawing on a wide range of experts from the fields of paleoclimatology, historical ecology, paleontology, botany, geology, conservation science, and resource management, this book unlocks the secret of how the Western Hemisphere's indigenous inhabitants influenced and transformed their natural environment. A rare combination of collaborators uncovers the changes that took place in North America, Mexico, Central America, the Andes, and Amazonia. Each section of the book has been comprehensively arranged so that a botanical description of the natural vegetation of the region is coupled with a set of case studies outlining local human influences. From modifications of vegetation, to changes in soil, wildlife, microclimate, hydrology, and the land surface itself, this collection addresses one of the great issues of our time: the human modification of the earth.
A ground breaking study of primates that live in flooded habitats around the world.
Until now there has never been a monograph devoted to the Pantanal, the world's largest wetland. The subject has received scant attention in the international literature, so a number of scattered Portuguese papers are reviewed for an English-language readership. The book presents a broad treatment of the Pantanal, ranging from geology to flora, fauna, and the human presence. The publication of this book is most timely, and will be of crucial importance in decisions affecting the ambitious project for a second South American inland Waterway.
With a complex assemblage of largely intact ecosystems that support the earth's greatest diversity of life, the Amazon basin is a focal point of international scientific interest. And, as development and colonization schemes transform the landscape in increasing measure, scientists from around the world are directing attention to questions of regional and global significance. Some of these qustions are: What are the fluxes of greenhouse gases across the atmospheric interface of ecosystems? How mush carbon is stored in the biomass and soils of the basin? How are elements from the land transferred to the basin's surface waters? What is the sum of elements transferred from land to ocean, and what is its marine "fate"? This book of original chapters by experts in chemical and biological oceanography, tropical agronomy and biology, and the atmospheric sciences will address these and other important questions, with the aim of synthesizing the current knowledge of biochemical processes operating within and between the various ecosystems in the Amazon basin.