and Proteaceae colonized New Zealand and New Caledonia, from South America, along the Antarctic margin of Gondwana. At the beginning of the Tertiary, New Zealand and New Caledonia moved north to a warmer climate. This led to a long period of evolution in near complete isolation. New Caledonia's natural heritage includes species whose ancestors were present on New Caledonia when it broke away from Gondwana; not only species but entire genera and even families are unique to the island. Evolution and history The species of the archipelago of New Caledonia are relicts of a type of vegetation which earlier covered much of the tropics of the Earth, including much of the mainland of Australia, South America, Antarctica, South Africa, and North America. Although tropical cloud forests disappeared during the glaciations, they re-colonized large areas during successive geological eras when the weather was favorable again. At other times they were replaced by more cold-tolerant or drought-tolerant sclerophyll plant communities. Many of the then existing species became extinct because they could not cross the barriers posed by new oceans, mountains and deserts, but others found refuge as species relict in coastal areas and islands. When the large landmasses became drier and with a harsher climate, this type of forest was reduced to those boundary areas. Although some remnants of archaic rich flora still persisted in coastal mountains and sheltered sites, their biodiversity was reduced. The location of the New Caledonian Islands in the Pacific Ocean moderated these climatic fluctuations, and maintained the relatively humid and mild climate which has allowed these communities to persist to the present day. The ecological requirements of many of the species are those of the laurel forest, and like most of their counterparts laurifolia in the world, they are vigorous species with a great ability to populate the habitat that is conducive. The geographical isolation and special edaphic conditions helped to preserve it too. Some species are even specialized in nickel hyperaccumulation such as the Sapotaceae Sebertia acuminata. Some geologists assert that, as the island moved north due to the effects of continental drift, it submerged at various intervals, extinguishing its terrestrial flora and fauna. Botanists counter that some areas must have remained above sea-level, serving as refugia. Many members of the late Cretaceous – early Tertiary Gondwanan flora survived in New Caledonia's equable climate but were eliminated in Australia due to increasingly dry conditions. The isolation