Please use this identifier to cite or link to this item: https://repositorio.inpa.gov.br/handle/1/19168
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dc.contributor.authorLaurance, William F.-
dc.date.accessioned2020-06-15T22:05:59Z-
dc.date.available2020-06-15T22:05:59Z-
dc.date.issued2000-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/19168-
dc.description.abstractThis paper describes four global-change phenomena that are having major impacts on Amazonian forests. The first is accelerating deforestation and logging. Despite recent government initiatives to slow forest loss, deforestation rates in Brazilian Amazonia have increased from 1.1 million ha yr-1 in the early 1990s, to nearly 1.5 million ha yr-1 from 1992-1994, and to more than 1.9 million ha yr-1 from 1995-1998. Deforestation is also occurring rapidly in some other parts of the Amazon Basin, such as in Bolivia and Ecuador, while industrialized logging is increasing dramatically in the Guianas and central Amazonia. The second phenomenon is that patterns of forest loss and fragmentation are rapidly changing. In recent decades, large- scale deforestation has mainly occurred in the southern and eastern portions of the Amazon - in the Brazilian states of Para, Maranhao, Rondonia, Acre, and Mato Grosso, and in northern Bolivia. While rates of forest loss remain very high in these areas, the development of major new highways is providing direct conduits into the heart of the Amazon. If future trends follow past patterns, land-hungry settlers and loggers may largely bisect the forests of the Amazon Basin. The third phenomenon is that climatic variability is interacting with human land uses, creating additional impacts on forest ecosystems. The 1997/98 El Nino drought, for example, led to a major increase in forest burning, with wildfires raging out of control in the northern Amazonian state of Roraima and other locations. Logging operations, which create labyrinths of roads and tracks in forests, are increasing fuel loads, desiccation and ignition sources in forest interiors. Forest fragmentation also increases fire susceptibility by creating dry, fire-prone forest edges. Finally, recent evidence suggests that intact Amazonian forests are a globally significant carbon sink, quite possibly caused by higher forest growth rates in response to increasing atmospheric CO2 fertilization. Evidence for a carbon sink comes from long-term forest mensuration plots, from whole-forest studies of carbon flux and from investigations of atmospheric CO2 and oxygen isotopes. Unfortunately, intact Amazonian forests are rapidly diminishing. Hence, not only is the destruction of these forests a major source of greenhouse gases, but it is reducing their intrinsic capacity to help buffer the rapid anthropogenic rise in CO2.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 61, Número 1, Pags. 113-122pt_BR
dc.rightsRestrito*
dc.subjectAmazonian Forestsen
dc.subjectCarbon Fluxen
dc.subjectClimate Variabilityen
dc.subjectDeforestationen
dc.subjectGlobal Changeen
dc.subjectHabitat Fragmentationen
dc.subjectTropical Forestsen
dc.subjectClimate Changeen
dc.subjectConservationen
dc.subjectEcosystemsen
dc.subjectEnvironmental Impacten
dc.subjectFire Hazardsen
dc.subjectTropicsen
dc.subjectForestryen
dc.subjectDeforestationen
dc.subjectEnvironmental Impacten
dc.subjectGlobal Changeen
dc.subjectMan-environment Relationsen
dc.subjectEnvironmental Impact Assessmenten
dc.subjectEnvironmental Planningen
dc.subjectEnvironmental Protectionen
dc.subjectForesten
dc.subjectGlobal Climateen
dc.subjectLand Useen
dc.subjectCaesalpinia Ciliataen
dc.subjectRondoniaen
dc.titleMega-development trends in the Amazon: Implications for global changeen
dc.typeArtigopt_BR
dc.identifier.doi10.1023/A:1006374320085-
dc.publisher.journalEnvironmental Monitoring and Assessmentpt_BR
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