|
The island’s unique shape results from the submarine collision between the Oriental and Gondwanic geological plates as a consequence of the continuous northern movement of the Gondwanic Plate millions of years ago. This collision forced the welding and buckling of the geologically disparate ‘arms’ of Sulawesi, with the major contact zone for this ‘welding’ process occurring in Central Sulawesi. This puts Central Sulawesi, and Lore Lindu National Park in particular, at the hub of the biodiversity integrity of Sulawesi. This is because it is in Central Sulawesi that the diverse habitat types and richly biodiverse mountains from two previous land masses connect from the north, south and south eastern regional provinces. Most of Sulawesi lies above 500 m in altitude; about 20% of the total land area is above an altitude of 1000 m. The highest mountains ranges are in Central and Northern Sulawesi. The fauna and flora of Sulawesi show a generally closer affinity with islands to the east. The Sulawesi bird fauna is exceptional in that 67% of the species have affinities with Sundaland (Mayr 1944). The mountain flora of Sulawesi is derived from autochonous speciation (endemics) and species that have migrated from other places in the world, mainly from cold climes (van Steenis 1972). Sulawesi butterflies and moths are most strongly associated with the Philippines (Hollaway 1987).
|
|
|---|
|
|---|