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Deforestation in Madagascar

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  • 8 chapters
Illegal slash and burn practise in the region west of Manantenina.
Diorit · CC BY-SA 3.0

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Through Environmental issues, Deforestation and Biodiversity

The extent of primary forest loss in Madagascar has been the subject of debate. What is certain is that the arrival of humans on Madagascar some 2000+ years ago began a process of fire, cultivation, logging and grazing that has reduced forest cover. Industrial forest exploitation during the Merina monarchy and French colonialism contributed to forest loss. Evidence from air photography and remote sensing suggest that by c. 2000, around 40% to 50% of the forest cover present in 1950 was lost. Current hotspots for deforestation include dry forests in the southwest being converted for maize cultivation and rain forests in the northeast exploited for tropical hardwoods.

Primary causes of forest loss include slash-and-burn for agricultural land (a practice known locally as tavy) and for pasture, selective logging for precious woods or construction material, the collection of fuel wood (including charcoal production) and, in certain sites, forest clearing for mining.

History of deforestation in Madagascar

Early history

Deforestation by life in Madagascar by human intervention first made an impact on its highland forests as early as AD 600 in the establishment of swidden fields by Indonesian settlers. The creation of swidden fields is a subsistence method of agriculture that has been practiced by humans across the globe for over 12000 years by means of a slash-and-burn technique that clears an area in preparation for crop growth. An increase in the rate of forest removal was seen around AD 1000 with the introduction of cattle from Africa, compelling Malagasy islanders to expand their grassland grazing areas. Historical records point to the importance that this impact has caused with the disappearance of most of Madagascar's highland forest by 1600 AD. Attempts to conserve Madagascar's forests were introduced by rulers in the establishment of environmental regulations, the earliest being seen in 1881 when Queen Ranavalona II placed a ban on using slash-and-burn techniques in agriculture. These efforts aimed to protect the future of the countries rainforests, however, it has been estimated that over 80 percent of Madagascar's original forests are gone with half of this loss occurring since the late 1950s.

Recent history

Early estimates of deforestation in Madagascar were unreliable until using data taken over a 35-year period from a combination of aerial photography, taken in 1950, and more recently data from satellite imagery available since 1972 were used to clearly see the extent of rainforest cleared in the eastern areas of Madagascar. By 1985, only 50 percent of the 7.6 million hectares that existed in 1950 remained equating to an average deforestation rate of over 111,000 hectares per year and by 2005 the country had seen a total of 854,000 hectares of forest lost since 1990. Since the first evidence of human occupation less than 2000 years ago the island of Madagascar's population in 2002 had grown to about 12 million people (McConnell, 2002). Agricultural fires, erosion and soil degradation continue to contribute to the degradation of the countries ecological stability impeding forest regrowth and according to recent data taken over the 2001 – 2012 period the rate of forest loss in Madagascar's has continued to increase.

As shown in the diagram on the left, Madagascar can be divided into four climatic ecoregions with four forest types: moist forest in the East (green), dry forest in the West (orange), spiny forest in the South (red), and mangrove forests along the West coast (blue). Ecoregions were defined following climatic and vegetation criteria. The dark grey areas represent the remaining natural forest cover for the year 2014. Forest types are defined on the basis of their belonging to one of the four ecoregions.

The main figure in the diagram on the right shows the changes in forest cover from 1973 to 2014. Forest cover in 1953 is shown in the bottom-right inset. Two zooms in the western dry (left part) and eastern moist (right part) ecoregions present more detailed views of (from top to bottom): forest cover in 1953, forest cover change from 1973 to 2014, forest fragmentation in 2014 and distance to forest edge in 2014. Data on water bodies (blue) and water seasonality (light blue for seasonal water to dark blue for permanent water) have been extracted from Pekel et al. (2016).

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