The unusual distribution of arowanas in both Asia and Australia (last connected during the
Mesozoic), despite their freshwater habits, is unique and the subject of several competing hypotheses about when the
ancestor of the Australian arowanas diverged from the ancestor of the Asian arowanas. Kumazawa & Nishida (2000) hypothesized that the two clades diverged about 140
million years ago, during the
Early Cretaceous period, as a product of continental
vicariance, when
Insular India (containing the Asian
Scleropages) &
Madagascar broke off from the
Australian &
Antarctic landmass, fragmenting a population of ancestral
Scleropages that inhabited
East Gondwana during the Early Cretaceous. Lavoue (2015) also found evidence for a Cretaceous divergence between these two clades, but found it to post-date the fragmentation of East Gondwana, suggesting that the ancestral
Scleropages dispersed over marine habitats to its present range during the
Late Cretaceous. More recently, Cioffi
et al (2019) firmly found that the divergence between the Asian and Australian arowanas only dates to the
late Eocene, about 35 million years ago, suggesting that the current distribution of
Scleropages is best explained by a late
Paleogene marine dispersal between Asia and Australia, followed by extirpation of the genus in marine habitats, leaving only the freshwater species. However, fossils of this genus have not yet been definitively identified from marine deposits. The genus had a much wider
distribution during the early
Cenozoic, with
fossil remains known from the
Paleocene of
Niger and
Belgium, and from the
Eocene of
China and
Indonesia. ==Species==