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  2. Gondwana - Wikipedia

    en.wikipedia.org/wiki/Gondwana

    Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] was a large landmass, sometimes referred to as a supercontinent.The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian subcontinent.

  3. File:Map of Australia and New Zealand with an inset.svg

    en.wikipedia.org/wiki/File:Map_of_Australia_and...

    Date/Time Thumbnail Dimensions User Comment; current: 12:46, 24 April 2022: 1,205 × 918 (577 KB): Goran tek-en: changed colors and types of lines: 15:47, 19 April 2022

  4. Gondwana Rainforests - Wikipedia

    en.wikipedia.org/wiki/Gondwana_Rainforests

    The Gondwana Rainforests of Australia is a serial property comprising the major remaining areas of rainforest in southeast Queensland and northeast New South Wales. It represents outstanding examples of major stages of the Earth’s evolutionary history, ongoing geological and biological processes, and exceptional biological diversity.

  5. East Gondwana - Wikipedia

    en.wikipedia.org/wiki/East_Gondwana

    The South Polar region of the Cretaceous comprised the continent of East Gondwana–modern day Australia, Zealandia, and Antarctica–a product of the break-up of Gondwana in the Cretaceous Period. The southern region, during this time, was much warmer than it is today, ranging from perhaps 4–8 °C (39–46 °F) in the latest Cretaceous ...

  6. Natural history of Australia - Wikipedia

    en.wikipedia.org/wiki/Natural_history_of_Australia

    Australia separated from Gondwana 99 Ma, and initially remained warm and humid with rainforest vegetation. Inland Australia had systems of rivers and lakes with abundant wildlife. Fossil birds, platypus, frogs and snakes are present from this period. From 30 Ma there was a period of global cooling, and from 15 Ma the Antarctic ice sheet formed.

  7. Natural history of New Zealand - Wikipedia

    en.wikipedia.org/wiki/Natural_history_of_New_Zealand

    The Australia-New Zealand continental part of Gondwana split from Antarctica in the late Cretaceous (95–90 Ma). This was followed by Zealandia separating from Australia (c.85 Ma). The split started from the Southern end and eventually formed the Tasman Sea. By about 70 Ma, the continental crust of Zealandia separated from Australia and ...

  8. Indo-Australian plate - Wikipedia

    en.wikipedia.org/wiki/Indo-Australian_Plate

    Map showing the Indo-Australian plate (IA) and other major plates The Indo-Australian plate, shown as its two subdivisions: the Indian plate (red) and the Australian plate (orange) The Indo-Australian plate is or was a major tectonic plate. It is in the process of separation into three plates, and may be currently separated into more than one ...

  9. Neozealandia - Wikipedia

    en.wikipedia.org/wiki/Neozealandia

    Also, New Zealand has vestiges of ancient temperate rain forests with plant species, such as giant club mosses, tree ferns and Nothofagus trees, dating from the time when the Zealandia subcontinent split off from Gondwana. New Zealand grasslands are dominated by vast spreadings of tussock grass fed upon by the native ground parrots. Most of New ...