Open AccessA phylogeny for grasshoppers of the genus Chitaura (Orthoptera: Acrididae) from Sulawesi, Indonesia, based on mitochondrial DNA sequence data
Author(s) -
Walton C.,
Butlin R. K.,
Monk K. A.
Publication year - 1997
Publication title -
biological journal of the linnean society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.906
H-Index - 112
eISSN - 1095-8312
pISSN - 0024-4066
DOI - 10.1111/j.1095-8312.1997.tb01631.x
Subject(s) - biology , vicariance , land bridge , ecology , genus , biological dispersal , endemism , biogeography , taxon , phylogenetic tree , phylogeography , zoology , evolutionary biology , population , biochemistry , demography , sociology , gene
The Indonesian island of Sulawesi occupies a central position within the biogeographically complex region known as Wallacea. Its fauna is characterised by a high rate of endemism and a patchwork distribution of taxa within the island. The grasshopper genus Chitaura is a good example having at least ten endemic species with predominantly parapatric distributions. It can be used as a model for determining the origins of Sulawesi taxa and the within‐island evolution that has led to the present patterns of distribution. Here we present a phylogenetic hypothesis for 28 individuals within the genus, including individuals of one species from Java and two from the Moluccas, based on DNA sequences of the mitochondrial cytochrome oxidase 1 gene. Frequent sequence heteroplasmy was observed. The phylogenetic hypothesis is consistent with recent interpretations of the geological history of Sulawesi suggesting separate evolution on the island for 7–14 Myr, possibly since South Sulawesi was connected to Borneo. Within the island, the pattern of genetic divergence is dominated by a strong correlation with geographic distance, with exceptions indicating past or present barriers to dispersal. Colonisation of the Moluccas from North or Central Sulawesi is implied. Levels of genetic divergence are compared with distribution patterns of colour morphs and with possible effects of tectonic movements in the Cenozoic, or Pleistocene climatic, vegetational and sea‐level changes.