Paleotropical Kingdom
The Paleotropical Kingdom (Paleotropis) is a floristic kingdom comprising tropical areas of Africa, Asia and Oceania (excluding Australia and New Zealand), as proposed by Ronald Good and Armen Takhtajan. Its flora is characterized by about 40 endemic plant families, e.g. Nepenthaceae, Musaceae, Pandanaceae, Flagellariaceae. Part of its flora, inherited from the ancient supercontinent of Gondwana or exchanged later (e.g. Piperaceae with pantropical distribution and but few warm temperate representatives), is shared with the Neotropical Kingdom, comprising tropical areas of Central and South America. Moreover, the Paleotropical flora influenced the tropical flora of the Australian Kingdom. The Paleotropical Kingdom is subdivided into five floristic subkingdoms according to Takhtajan (or three, according to Good) and about 13 floristic regions. In this article the floristic subkingdoms and regions are given as delineated by Takhtajan.
Contents
Origin
A distinct community of vascular plants evolved millions of years ago, and are now found on several separate areas. Millions of years ago, the warmer and wetter areas supported a tropical adapted flora, including forests of podocarps and southern beech. They were a type of flora characteristic of parts of Gondwana but were present in equivalent ecological areas.
Over millions of years, these type of vegetation present, covered much of the tropics of Earth. Many species are today relicts of a type of vegetation disappeared, which originally covered much of the mainland of Africa, Madagascar, India, South America, Antarctica, Australia, North America, Europe, and other lands when their climate were more humid and warm. Although warm Cloud forests disappeared during the glaciations, they re-colonized large areas every time the weather was favorable again. Most of the Cloud forests are believed to have retroced and advanced during successive geological eras, and their species adapted to warm and wet gradually retreated and advanced, 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.
In the Carboniferous and Permian, New Zealand and New Caledonia were on the periphery of Gondwana, which included Africa, South America, Antarctica, India, New Zealand and Australia. Paleomagnetic data locate New Caledonia originally near the South Pole. In the Triassic and early Jurassic, Gondwana moved northward, warming the eastern margin. New Caledonia separated from Australia and New Zealand during the breakup of the super-continent, separating from Australia at the end of the Cretaceous (66 mya) and probably completing its separation from New Zealand in the mid-Miocene.
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.
Many members of the late Cretaceous - early Tertiary Gondwanan flora survived in islands and Coastal area's equable climate but were eliminated in mainland due to increasingly dry conditions.[1] When the large landmasses became drier and with a harsher climate, this type of forest was reduced to those boundaries areas. Tasmania, Chile, New Zealand and New Caledonia share related species extinct in Australia mainland. The same case occurs in the Atlantic Macaronesia islands and Pacific Taiwan, Hainan, Jeju, Shikoku, Kyūshū, and Ryūkyū Islands. Although some remnants of archaic rich flora still persisted in their coastal mountains and shelter sites, their biodiversity were reduced. The location of Islands in the oceans moderated these climatic fluctuations, and maintained the relatively humid and mild climate which has allowed these communities to persist to the present day.
Plants have limited seed dispersal mobility away from the parent plant and consequently rely upon a variety of dispersal vectors to transport their propagules, including both abiotic and biotic vectors. Seeds can be dispersed away from the parent plant individually or collectively, as well as dispersed in both space and time. Tertiary vegetal species isolated on islands have led to vicariant species and genera and families extinct in the rest of the world have been preserved as endemic in the different islands.
For example genera, Archeria in Ericaceae, or Wollemia in the family Araucariaceae, was known only from fossil remains before the discovery of the living species in 1994 in a temperate rainforest wilderness area of the Wollemi National Park in New South Wales, in a remote series of narrow, steep-sided sandstone gorges near Lithgow.
Fossils dating from before the Pleistocene glaciations show that species of Laurus were formerly distributed more widely around the Mediterranean and North Africa, isolated gave rise to Laurus azorica in Azores Islands, Laurus nobilis in mainland and Laurus novocanariensis in Canary Islands.
Subdivisions
African Subkingdom
10 endemic families (incl. Dioncophyllaceae, Pentadiplandraceae, Scytopetalaceae, Medusandraceae, Dirachmaceae, Kirkiaceae), many endemic genera.
- Guineo-Congolian Province
- Usambara-Zululand Region
- Sudano-Zambezian Region (including tropical Asia west of the Gulf of Khambhat)
- Karoo-Namib Region
- St. Helena and Ascension Region
Madagascan Subkingdom
9 endemic families, more than 450 endemic genera, about 80% endemic species. It ceased to be influenced by the African flora in the Cretaceous, but underwent heavy influence of the Indian Region's flora.
Indo-Malesian Subkingdom
11 endemic families (incl. Degeneriaceae, Barclayaceae, Mastixiaceae) and many endemic genera
Polynesian Subkingdom
No endemic families, many endemic genera. The flora is mostly derivative from that of the Indo-Malesian Subkingdom.
Neocaledonian Subkingdom
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New Caledonia lies on the southernmost edge of the tropical zone, near the Tropic of Capricorn. This flora originated on the supercontinent Gondwana, and persist in current day New Guinea, Australia, New Zealand, New Caledonia and Southamerica. This flora is fossil in Antarctica. The biodiversity of New Caledonia include several endemic families (incl. Amborellaceae, Strasburgeriaceae) and more than 130 endemic genera (incl. Exospermum and Zygogynum). The flora is partially shared with the Indo-Malesian Subkingdom and the Australian Kingdom.
