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CerradoThe Cerrado is the second largest of Brazil's major biomes (after Amazonia), originally covering some 2 031 990 km2, and representing the most extensive woodland-savanna region in South America. It is entirely tropical, its core occupying the central Brazilian Plateau, although it extends also marginally into eastern Paraguay. Rainfall is typically high (between 1 100 and 1 600 mm annually), but is concentrated in a period of six to seven months (April to October), the dry season being pronounced and, in some places, resulting in water stress. Many of the typical Cerrado plant species are drought-adapted.
Fire, both natural and human-induced, is an important feature of Cerrado ecology. The flora displays a number of adaptations to fire, including thick bark, leathery leaves, and a rapid regeneration capacity. Fire maintains the balance between grasses and woody vegetation; in its absence, trees predominate, resulting in dry forest. Seed germination is fire-dependent in a number of species. The Cerrado is one of the richest of all tropical savanna regions and has high levels of endemism. Mendonça et al. (1997) listed 6 387 angiosperms, and total plant diversity is estimated at around 10 000 species, of which 4 400 are endemic. The herbaceous species are almost totally endemic. A conservative estimate for diversity of fungi (Dianese et al. 1997) gives 24 000 species, but, being based on six species per host plant, and considering only 4 000 vascular plant species, it is likely an underestimate. Several non-endemic plant species stand out as flagships for this hotspot: for example, the conspicuous palms Mauritia vinifera (locally known as buritís), which grow along the swampy headwaters of streams and rivers (known as veredas) that flow through the Cerrado's open grasslands. Trees of the genus Tabebuia (Bignoniaceae), known as ipê, are also spectacular and widespread inhabitants of the Cerrado; their brilliant yellow, pink, and purple flowers are a common sight.
There are 33 endemic reptiles (of a total of 225 species), six in the snake genus Apostolepis. As with the Atlantic Forest, the genus Amphisbaena is well represented, with at least 26 species present. Very little is known about the ecology of amphisbaenians, as they are largely subterranean. One species that has been well studied is the widespread giant worm lizard (A. alba), which can grow to 70 cm in length; feeds on beetles, ants, and spiders; and has a clutch size ranging from 8–16 eggs, one of the largest known for the family (Colli and Zamboni 1999). Among amphibians, some 289 species have been recorded, of which 26 are endemic, including two species endemic to Serra da Canastra National Park: the Canastra snouted tree frog (Scinax canastrensis) and Zagaia tree frog (Hyla sazimai).
The Cerrado has been occupied by humans for at least 11 000 years (Barbosa and Nascimento 1993), and perhaps as long as 30 000 (Schmitz 1993). Hunter-gatherer societies subsisted on game and native plants, as clearly indicated by the impressive Holocene rock paintings of animals found especially in the dry areas around the Rio São Francisco in Bahia and Minas Gerais and in Goiás and Piauí (Schmitz 1993). During the colonization of Brazil in the early 1500s, the Portuguese avoided the interior of the country because of treaties between Spain and Portugal, and also a cultural predisposition to settle near the sea (Holanda 1936). The first incursions, in search of gold and precious stones, were in the eighteenth century (Alho and Martins 1995), and opened the way for cattle-ranching, the primary economic activity until the mid-1950s, when the government began its plans for a new capital in Goiás, in the heart of the Cerrado, to stimulate the colonization and development of the region. Improved transport and infrastructure, a major commitment to the automobile industry, and agricultural and soil research over the ensuing years, resulted in the Cerrado becoming the major agribusiness (soybean, corn, and irrigated rice) frontier of the country. Following major failures in large-scale development programs in Amazonia, as of the 1970s the World Bank considered the Cerrado to be the alternative for Brazil's agricultural expansion (Goodland and Irwin 1975). Today, nearly one-quarter of all grain produced in Brazil comes from the Cerrado (Alho and Martins 1995).
In spite of its large size and great importance for biodiversity conservation, the Cerrado is poorly represented in Brazil's protected area system. The World Database on Protected Areas indicates that only 1.4% is conserved in protected areas in IUCN categories I to IV, increasing to 5.5% when including other forms of reserves and parks. In Brazil, 62 strictly protected areas (state and federal parks, biological reserves, and ecological stations), mostly limited in size, cover 42 676 km2—only 2.1% of the hotspot's original extent. The most important parks include Chapada dos Guimarães (330 km2), Serra da Canastra (2 000 km2, although only about 720 km2 are currently protected), Emas (1 330 km2), and Grande Sertão Veredas (840 km2), and in 2001 a large and valuable area of the Cerrado in the State of Tocantins was secured as the Jalapão State Park (1 588 km2). Including protected areas of sustainable use (mainly Environmental Protection Areas), this number increases to 102 areas covering 83 520 km2 or 4.1% of the Cerrado (Rylands et al. 2004).
The Brazilian Government held an expert-based Regional Priority Setting Workshop for the Cerrado and Pantanal in 1998 (Fundação Pró-Natureza-FUNATURA et al. 2000). Seventy priority areas for conservation were identified, ranging from the central highlands of the country, at the headwaters of Brazil's major rivers, through the savannas of Amazonia, to the Pantanal of southwestern Brazil, down to fragmented Cerrado remnants in the states of São Paulo and Paraná. The meeting concluded with recommendations for immediate action, with suggestions for changes in legislation in order to create incentives to preserve biodiversity together with water sources, consolidate existing parks and reserves, establish new protected areas, and more intensively survey this vast region that is still so little known to science. < previous section < index > next section >
‹Preface: CEMEX› ‹Preface: Peter A. Seligmann› ‹Preface: Patricio Robles Gil› ‹Foreword: Harrison Ford› ‹Introduction› ‹An Update of Existing Hotspots› ‹Tropical Andes› ‹Tumbes-Chocó-Magdalena› ‹Atlantic Forest› ‹Cerrado› ‹Chilean Winter Rainfall-Valdivian Forests› ‹Mesoamerica› ‹Caribbean Islands› ‹California Floristic Province› ‹Guinean Forests of West Africa› ‹Cape Floristic Region› ‹Succulent Karoo› ‹Madagascar and the Indian Ocean Islands› ‹Mediterranean Basin› ‹Caucasus› ‹Western Ghats and Sri Lanka› ‹Mountains of Southwest China› ‹Sundaland› ‹Wallacea› ‹Philippines› ‹Southwest Australia› ‹New Zealand› ‹New Caledonia› ‹Polynesia-Micronesia› ‹Madrean Pine-Oak Woodlands› ‹Maputaland-Pondoland-Albany› ‹Coastal Forests of Eastern Africa› ‹Eastern Afromontane› ‹Eastern Arc Mountains and Southern Rift› ‹Albertine Rift› ‹Ethiopian Highlands› ‹Horn of Africa› ‹Irano-Anatolian› ‹Mountains of Central Asia› ‹ Himalaya› ‹Indo-Burma› ‹Japan› ‹East Melanesian Islands› ‹Taiwan› ‹Queensland Wet Tropics› ‹References› ‹Addresses› ‹Acknowledgements› ‹Image Captions and Photographer Credits›
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