زيلانديا Zealandia

Coordinates: 40°S 170°E / 40°S 170°E / -40; 170
يجب ألا يـُخلـَط بينها وبين Zeelandia (disambiguation).
For other uses, see زيلانديا (توضيح).
طبوغرافيا زيلانديا, outlined in pink. The linear ridges running north-northeast (Colville to the west and Kermadec to the east, separated by the Havre Trough and Lau Basin) and southwest (the Resolution Ridge System) away from New Zealand are not considered part of Zealandia, nor are Australia (left), Vanuatu, or Fiji (top centre).[1]

Zealandia (pronounced /ziːˈlændiə/), also known as Te Riu-a-Māui (Māori)[2] or Tasmantis (from Tasman Sea),[3][4] is an almost entirely submerged mass of continental crust in Oceania that subsided after breaking away from Gondwana 83–79 million years ago.[5] It has been described variously as a submerged continent, continental fragment, and microcontinent.[6] The name and concept for Zealandia was proposed by Bruce Luyendyk in 1995,[7] and satellite imagery shows it to be almost the size of Australia.[8] A 2021 study suggests Zealandia is over a billion years old, about twice as old as geologists previously thought.[9][10]

By approximately 23 million years ago, the landmass may have been completely submerged.[11][12] Today, most of the landmass (94%) remains submerged beneath the Pacific Ocean.[13] New Zealand is the largest part of Zealandia that is above sea level, followed by New Caledonia.

Mapping of Zealandia concluded in 2023.[14] With a total area of approximately 4,900,000 km2 (1,900,000 sq mi),[6] Zealandia is substantially larger than any features termed microcontinents and continental fragments. If classified as a microcontinent, Zealandia would be the world's largest microcontinent. Its area is six times the area of the next-largest microcontinent, Madagascar,[6] and more than half the area of the Australian continent. Zealandia is more than twice the size of the largest intraoceanic large igneous province (LIP) in the world, the Ontong Java Plateau (approximately 1,900,000 km2 or 730,000 sq mi), and the world's largest island, Greenland (2,166,086 km2 or 836,330 sq mi). Zealandia is also substantially larger than the Arabian Peninsula (3,237,500 km2 or 1,250,000 sq mi), the world's largest peninsula, and the Indian subcontinent (4,300,000 km2 or 1,700,000 sq mi). Due to these and other geological considerations, such as crustal thickness and density,[15][16] some geologists from New Zealand, New Caledonia, and Australia have concluded that Zealandia fulfills all the requirements to be considered a continent rather than a microcontinent or continental fragment.[6] Geologist Nick Mortimer commented that if it were not for the ocean level, it would have been recognised as such long ago.[17]

Zealandia supports substantial inshore fisheries and contains gas fields, of which the largest known is the New Zealand Maui gas field, near Taranaki. Permits for oil exploration in the Great South Basin were issued in 2007.[18] Offshore mineral resources include ironsands, volcanic massive sulfides and ferromanganese nodule deposits.[19]

Etymology

GNS Science recognises two names for the landmass. In English, the most common name is Zealandia, a latinate name for New Zealand; the name was coined in the mid-1990s and became established through common use. In the Māori language, the landmass is named Te Riu-a-Māui, meaning 'the hills, valleys, and plains of Māui'.[2]


الجيولوجيا

انظر أيضاً: جيولوجيا زيلانديا, جيولوجيا نيوزيلندا, جغرافيا نيو كاليدونيا, and جيولوجيا نيو كاليدونيا
خريطة طبوغرافية لزيلانديا

Geology of Zealandia

الجغرافيا الحيوية

New Caledonia is at the northern end of the ancient continent, while New Zealand rises at the plate boundary that bisects it. These land masses constitute two outposts of the Antarctic flora, featuring araucarias and podocarps. At Curio Bay, logs of a fossilized forest closely related to modern kauri and Norfolk pine can be seen that grew on Zealandia approximately 180 million years ago during the Jurassic period, before it split from Gondwana.[20] The trees growing in these forests were buried by volcanic mud flows and gradually replaced by silica to produce the fossils now exposed by the sea.

As sea levels drop during glacial periods, more of Zealandia becomes a terrestrial environment rather than a marine environment. Originally, it was thought that Zealandia had no native land mammal fauna, but the discovery in 2006 of a fossil mammal jaw from the Miocene in the Otago region demonstrates otherwise.[21]

التقسيمات السياسية

Exclusive economic zone of New Zealand and continental shelf boundaries for much of Zealandia

The total land area (including inland water bodies) of Zealandia is 286,660.25 km2 (110,680.14 sq mi). Of this, New Zealand comprises the overwhelming majority, at 267,988 km2 (103,471 sq mi, or 93.49%) that includes the mainland (North Island and South Island), nearby islands, and most outlying islands, including the Chatham Islands, the New Zealand Subantarctic Islands, the Solander Islands, and the Three Kings Islands (but not the Kermadec Islands or Macquarie Island (Australia), which are parts of the rift).[22]

New Caledonia and the islands surrounding it comprise some 18,576 km2 (7,172 sq mi or 6.48%) and the remainder is made up of various territories of Australia including the Lord Howe Island Group (New South Wales) at 56 km2 (22 sq mi or 0.02%), Norfolk Island at 35 km2 (14 sq mi or 0.01%), as well as the Cato, Elizabeth, and Middleton reefs (Coral Sea Islands Territory) with 5.25 km2 (2.03 sq mi).[22][23]

التعداد

اعتبارا من 2024 the total human population of Zealandia is approximately 5.4 million people. The largest city is Auckland with about 1.7 million people; roughly one-third of the total population of the continent.

انظر أيضا

References

  1. ^ "Figure 8.1: New Zealand in relation to the Indo-Australian and Pacific Plates". The State of New Zealand's Environment 1997. 1997. Archived from the original on 18 January 2005. Retrieved 20 April 2007.
  2. ^ أ ب "The origin and meaning of the name Te Riu-a-Māui/Zealandia". www.gns.cri.nz. GNS Science. 2 May 2019. Retrieved 11 August 2020.
  3. ^ Flannery, Tim (2002). The Future Eaters: An Ecological History of the Australasian Lands and People (in الإنجليزية). Grove Press. p. 42. ISBN 978-0-8021-3943-6. Retrieved 26 December 2020.
  4. ^ Danver, Steven L. (22 ديسمبر 2010). Popular Controversies in World History: Investigating History's Intriguing Questions. ABC-CLIO. p. 187. ISBN 978-1-59884-078-0. Archived from the original on 5 أغسطس 2016. Zealandia or Tasmantis, with its 3.5 million square km territory being larger than Greenland, ...
  5. ^ Gurnis, M., Hall, C.E., and Lavier, L.L., 2004, Evolving force balance during incipient subduction: Geochemistry, Geophysics, Geosystems, v. 5, Q07001, https://doi.org/10.01029/02003GC000681
  6. ^ أ ب ت ث خطأ استشهاد: وسم <ref> غير صحيح؛ لا نص تم توفيره للمراجع المسماة mortimer
  7. ^ Luyendyk, Bruce P. (April 1995). "Hypothesis for Cretaceous rifting of east Gondwana caused by subducted slab capture". Geology. 23 (4): 373–376. Bibcode:1995Geo....23..373L. doi:10.1130/0091-7613(1995)023<0373:HFCROE>2.3.CO;2.
  8. ^ Gorvett, Zaria (8 February 2021). "The missing continent it took 375 years to find". BBC. Retrieved 9 February 2021.
  9. ^ Turnbull, R.E.; Schwartz, J.J.; Fiorentini, M.L.; Jongens, R.; Evans, N.J.; Ludwig, T.; McDonald, B.J.; Klepeis, K.A. (2021-08-01). "A hidden Rodinian lithospheric keel beneath Zealandia, Earth's newly recognized continent". Geology (in الإنجليزية). 49 (8): 1009–1014. Bibcode:2021Geo....49.1009T. doi:10.1130/G48711.1. ISSN 0091-7613.
  10. ^ Aylin Woodward (14 Aug 2021). "A fragment of a mysterious 8th continent is hiding under New Zealand - and it's twice as old as scientists thought". Business Insider.
  11. ^ "Searching for the lost continent of Zealandia". The Dominion Post. 29 September 2007. Retrieved 9 October 2007. We cannot categorically say that there has always been land here. The geological evidence at present is too weak, so we are logically forced to consider the possibility that the whole of Zealandia may have sunk.
  12. ^ Campbell, Hamish; Gerard Hutching (2007). In Search of Ancient New Zealand. North Shore, New Zealand: Penguin Books. pp. 166–167. ISBN 978-0-14-302088-2.
  13. ^ Wood, Ray; Stagpoole, Vaughan; Wright, Ian; Davy, Bryan; Barnes, Phil (2003). New Zealand's Continental Shelf and UNCLOS Article 76 (PDF). Institute of Geological and Nuclear Sciences Limited. Institute of Geological and Nuclear Sciences series 56. Wellington, New Zealand: National Institute of Water and Atmospheric Research. p. 16. NIWA technical report 123. Archived from the original (PDF) on 21 فبراير 2007. Retrieved 22 فبراير 2007. The continuous rifted basement structure, thickness of the crust, and lack of seafloor spreading anomalies are evidence of prolongation of the New Zealand land mass to Gilbert Seamount.
  14. ^ Newcomb, Tim. "Earth's Hidden Eighth Continent Is No Longer Lost". Science > Our Planet. Popular Mechanics (in الإنجليزية الأمريكية). ISSN 0032-4558.
  15. ^ خطأ استشهاد: وسم <ref> غير صحيح؛ لا نص تم توفيره للمراجع المسماة MortimerCampbell2014
  16. ^ "Zealandia: Is there an eighth continent under New Zealand?". BBC News (in الإنجليزية البريطانية). 17 فبراير 2017. Archived from the original on 28 مارس 2017. Retrieved 26 مارس 2017.
  17. ^ Sumner, Thomas (2017-03-13). "Is Zealandia a continent?". Science News for Students. Society for Science and the Public. Retrieved 2021-12-22.
  18. ^ "Great South Basin – Questions and Answers". 11 يوليو 2007. Archived from the original on 14 أكتوبر 2008. Retrieved 18 أبريل 2008.
  19. ^ "New survey published on NZ mineral deposits". 30 مايو 2007. Archived from the original on 16 أكتوبر 2008. Retrieved 18 أبريل 2008.
  20. ^ "Fossil forest: Features of Curio Bay/Porpoise Bay". Archived from the original on 17 October 2008. Retrieved 6 November 2007.
  21. ^ Campbell, Hamish; Gerard Hutching (2007). In Search of Ancient New Zealand. North Shore, New Zealand: Penguin Books. pp. 183–184. ISBN 978-0-14-302088-2.
  22. ^ أ ب "The Lost Continent of Zealandia". www.virtualoceania.net. Retrieved 2020-12-15.
  23. ^ Detailed map of Zealandia
  24. ^ "Population | Stats NZ". www.stats.govt.nz. Retrieved 2021-04-21.
  25. ^ "268 767 habitants en 2014". ISEE. Archived from the original on 13 نوفمبر 2014. Retrieved 16 نوفمبر 2014.
  26. ^ "2016 Census QuickStats: Norfolk Island". quickstats.censusdata.abs.gov.au (in الإنجليزية). Archived from the original on 7 May 2019. Retrieved 2021-04-21.
  27. ^ Australian Bureau of Statistics (27 June 2017). "Lord Howe Island (State Suburb)". 2016 Census QuickStats. Retrieved 7 July 2017. Edit this at Wikidata

وصلات خارجية

قالب:Oceanic features of Zealandia قالب:Submerged landmasses


40°S 170°E / 40°S 170°E / -40; 170

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