Caatinga


Caatinga is a type of desert vegetation, and an ecoregion characterized by this vegetation in interior northeastern Brazil. The name "Caatinga" is a Tupi word meaning "white forest" or "white vegetation".
The Caatinga is a xeric shrubland and thorn forest, which consists primarily of small, thorny trees that shed their leaves seasonally. Cacti, thick-stemmed plants, thorny brush, and arid-adapted grasses make up the ground layer. Most vegetation experiences a brief burst of activity during the three-month long rainy season.
Caatinga falls entirely within earth's tropical zone and is one of 6 major ecoregions of Brazil. It covers 850,000 km², nearly 10% of Brazil's territory. It is home to 26 million people and over 2000 species of plants, fish, reptiles, amphibians, birds, and mammals.

Geography

The Caatinga covers the interior portion of northeastern Brazil bordering the Atlantic seaboard, extending across eight states: Piauí, Ceará, Rio Grande do Norte, Paraíba, Pernambuco, Alagoas, Sergipe, Bahia, and parts of Minas Gerais. Altogether, the Caatinga comprises 850,000 km², about 10% of the surface area of Brazil. By comparison, it is over nine times the surface area of Portugal, whence came Brazil's early European settlers, and 20% larger than the U.S. state of Texas.Located between 3°S 45°W and 17°S 35°W, the Caatinga experiences irregular winds from all directions. Rainfall is thus intermittent but intense, totalling on average. Although the climate is typically hot and semi-arid, the Caatinga includes several enclaves of humid tropical forest, with trees tall.
in Bahia state, in Brazil
To the northwest, the Caatinga is bounded by the Maranhão Babaçu forests; to the west and southwest, the Atlantic dry forests and Cerrado savannas; to the east, the humid Atlantic coastal forests; and to the north and northeast, the Atlantic Ocean.

Climate

The Caatinga has only two distinguishable seasons: a hot and dry winter, and a cold and rainy summer. During the dry winter periods there is no foliage or undergrowth, as plants try to conserve water. Roots protrude through the surface of the stony soil, to absorb water before it is evaporated. Leaves fall off the trees to reduce transpiration. With all the foliage and undergrowth dead during the drought periods and all the trees having no leaves the Caatinga has a yellow-grey, desert-like look. During the peak periods of drought the Caatinga's soil can reach temperatures of up to 60 °C.
The drought usually ends in December or January, when the rainy season starts. Immediately after the first rains, the grey, desert-like landscape starts to transform and becomes completely green within a few days. Small plants start growing in the now moist soil and trees grow back their leaves. Rivers that are mostly dry during the past 6 or 7 months start to fill up and streams begin to flow again.

Ecology

Caatinga harbors a unique biota, with thousands of endemic species. Caatinga contains over 1,000 vascular plant species in addition to 187 bees, 240 fish species, 167 reptiles and amphibians, 516 birds, and 148 mammal species, with endemism levels varying from 9 percent in birds to 57 percent in fishes.

Vegetation

The Caatinga does not correspond to a single type of vegetation, but rather a broad mosaic. Nonetheless, all vegetative structure is adapted to the xeric climate. Succulent and crassulaceous species dominate; non-succulents exhibit small, firm leaves and intense branching at the base, akin to shrubs. Palm stands usually contain carnaúba or babaçu palms, but occasionally tucumã and macaúba.
The Caatinga has enough endemic species to constitute a floristic province. ''
Most authors divide the Caatinga into two different subtypes: dry and humid, but categorizations vary to as many as eight different vegetative regimes.

Fauna

The Caatinga is home to nearly 50 endemic species of birds, including Lear's macaw ', Spix's macaw ', moustached woodcreeper , Caatinga parakeet,
Caatinga antwren, Sao Francisco black tyrant and Caatinga cacholote.
Endemic mammal species include:
Based on radiocarbon dating of potsherds, proponents of historical ecology such as William Denevan and William Balee have suggested that large sections of the Caatinga region may be of anthropogenic origin. Over 1000 years ago, native peoples may have unintentionally created the environment of the modern-day Caatinga through constant slash-and-burn agriculture, thereby stymying plant succession and preventing major rainforests from growing within the region.
Conversely, fossil evidence suggests that the Caatinga may historically have been part of a much larger dry belt.

Conservation

The Caatinga is poorly represented in the Brazilian Conservation Area network, with only 1% in Integral Protection Conservation Areas and 6% in Sustainable Use Conservation Areas. Protected areas include Chapada Diamantina National Park, Serra da Capivara National Park, and Serra das Confusões National Park.
Economic developed has fragmented the native biome. Estimates on the amount of Caatinga transformed affected by economic development range 25-50%, making Caatinga the most degraded ecosystem in Brazil, following the Atlantic Forest, which has lost over 80% of its original cover.

Economic exploitation

The local population lives in extreme poverty, and many rely on extraction of natural resources for a livelihood. There are few drinkable water sources, and harvesting is difficult because of the irregular rainfall.

Agriculture

Native plants are used in local agriculture, much of it slash-and-burn. Pilocarpus jaborandii appears to exhibit medicinal properties. The fruits of umbú and mangabá are used as food directly, and other species are used for forage. Local palms produce commercial-grade lauric and oleic oils, which undergirds much of the economy of northeast Brazil.
Meliponiculture is also a well-developed and traditional activity in the region. One of the most productive species, Melipona subnitida, known locally as jandaíra, produces up to 6 liters a year, resulting in economic profit for the population.
Irrigation along the São Francisco River promises to turn the region into a breadbasket. The soil is very fertile, and existing irrigation infrastructure already supports the export of grapes, papayas and melons. At the same time, irrigation threatens to salinize the soil.

Grazing

and goat farming are popular and very productive in the region. Overgrazing and timbering for fuelwood have decimated local vegetative populations; outside irrigated regions, the area has begun to desertify à la Sahara and Sahel.

On Caatinga