Sahul: Difference between revisions
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Sahul was in the south-western [[Pacific Ocean]], located approximately north to south between the [[Equator]] and the [[44th parallel south]] and west to east between the [[112th meridian east|112th]] and the [[152nd meridian east|152nd]] meridians east.{{sfnp|White|O'Connell|1982|p=6}} Sahul was separated from [[Sundaland|Sunda]] to its west by the [[Wallacea|Wallacean Archipelago]].{{sfnp|White|O'Connell|1982|p=6}}{{sfnp|O’Connell|Allen|Hawkes|2010|p=57}} At its largest, when ocean levels were at their lowest, it was approximately {{convert|10600000|km2|sqmi}} in size.{{refn|group=note|The present day area of Australia, New Guinea and Tasmania is approximately {{convert|8500000|km2|sqmi}}.{{sfnp|White|O'Connell|1982|p=6}}}}{{sfnp|White|O'Connell|1982|p=6}} |
Sahul was in the south-western [[Pacific Ocean]], located approximately north to south between the [[Equator]] and the [[44th parallel south]] and west to east between the [[112th meridian east|112th]] and the [[152nd meridian east|152nd]] meridians east.{{sfnp|White|O'Connell|1982|p=6}} Sahul was separated from [[Sundaland|Sunda]] to its west by the [[Wallacea|Wallacean Archipelago]].{{sfnp|White|O'Connell|1982|p=6}}{{sfnp|O’Connell|Allen|Hawkes|2010|p=57}} At its largest, when ocean levels were at their lowest, it was approximately {{convert|10600000|km2|sqmi}} in size.{{refn|group=note|The present day area of Australia, New Guinea and Tasmania is approximately {{convert|8500000|km2|sqmi}}.{{sfnp|White|O'Connell|1982|p=6}}}}{{sfnp|White|O'Connell|1982|p=6}} |
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After |
After the [[Last Glacial Period|last Ice Age]] global temperatures increased and sea levels gradually rose, flooding the land bridge and separating mainland Australia from New Guinea and Tasmania.{{sfnp|Kennett|Chopping|Blewett|2018|p=4}} New Guinea was separated from the Australian mainland approximately 8,000 years ago, and Tasmania approximately 6,000 years ago.{{sfnp|Kennett|Chopping|Blewett|2018|p=4}} |
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Sahul hosted a large variety of unique fauna that changed independently from the rest of the world.{{sfnp|White|O'Connell|1982|p=12}} Most notably nearly all [[mammal]]s on Sahul were [[marsupial]]s including a range of [[Browsing (herbivory)|browsers]], [[Burrowing animals|burrowers]], [[scavenger]]s and [[predator]]s; [[bat]]s and rodents represented the only [[placental mammal]]s.{{sfnp|White|O'Connell|1982|p=12}} |
Sahul hosted a large variety of unique fauna that changed independently from the rest of the world.{{sfnp|White|O'Connell|1982|p=12}} Most notably nearly all [[mammal]]s on Sahul were [[marsupial]]s including a range of [[Browsing (herbivory)|browsers]], [[Burrowing animals|burrowers]], [[scavenger]]s and [[predator]]s; [[bat]]s and rodents represented the only [[placental mammal]]s.{{sfnp|White|O'Connell|1982|p=12}} |
Revision as of 20:48, 2 November 2024
Sahul (/səˈhuːl/), also called Sahul-land, Meganesia, Papualand and Greater Australia,[1] was a paleocontinent that encompassed the modern-day landmasses of mainland Australia, Tasmania, New Guinea, and the Aru Islands.[2][3][4][5][6]
Sahul was in the south-western Pacific Ocean, located approximately north to south between the Equator and the 44th parallel south and west to east between the 112th and the 152nd meridians east.[2] Sahul was separated from Sunda to its west by the Wallacean Archipelago.[2][7] At its largest, when ocean levels were at their lowest, it was approximately 10,600,000 square kilometres (4,100,000 sq mi) in size.[note 1][2]
After the last Ice Age global temperatures increased and sea levels gradually rose, flooding the land bridge and separating mainland Australia from New Guinea and Tasmania.[8] New Guinea was separated from the Australian mainland approximately 8,000 years ago, and Tasmania approximately 6,000 years ago.[8]
Sahul hosted a large variety of unique fauna that changed independently from the rest of the world.[9] Most notably nearly all mammals on Sahul were marsupials including a range of browsers, burrowers, scavengers and predators; bats and rodents represented the only placental mammals.[9]
It is estimated humans first colonized Sahul between 4000 and 4500 years ago, making the ocean crossing from Sunda through Wallacea.[10] From Sahul humans spread throughout Oceania.[3]
The name Sahul is used by archeologists, while the name Meganesia tends to be used by zoogeographers.[4] The name Greater Australia has been used, but it has been criticised as "cartographic imperialism" because it places greater emphasis upon what is now Australia at the expense of New Guinea.[6]
See also
- Arafura Sea – Marginal sea between Australia and Indonesian New Guinea
- List of paleocontinents
- Wallace Line
Notes
References
Citations
- ^ Gillespie, Richard (January 2002). "Dating the First Australians". Radiocarbon. 44 (2): 455–472. Bibcode:2002Radcb..44..455G. doi:10.1017/S0033822200031830.
- ^ a b c d e White & O'Connell (1982), p. 6.
- ^ a b O'Connor & Hiscock (2018), p. 26.
- ^ a b Groves (1996), p. 83.
- ^ Oliver (1961), p. 5.
- ^ a b Ballard (1993), p. 20.
- ^ O’Connell, Allen & Hawkes (2010), p. 57.
- ^ a b Kennett, Chopping & Blewett (2018), p. 4.
- ^ a b White & O'Connell (1982), p. 12.
- ^ O’Connell, Allen & Hawkes (2010), pp. 57–58.
Bibliography
- Ballard, Chris (1993). "Stimulating minds to fantasy? A critical etymology for Sahul". In Smith, M. A.; Spriggs, M.; Fankhouser, B. (eds.). Sahul in review: Pleistocene archaeology in Australia, New Guinea and island Melanesia (PDF). Canberra: Australian National University. pp. 17–23. ISBN 0-7315-1540-4.
- Groves, Colin P. (1996). "Hovering on the brink: nearly but not quite getting to Australia". In Rousham, Emily; Freedman, Leonard (eds.). Perspectives in human biology: volume 2 humans in the Australasian region. Singapore: World Scientific Publishing Co, Pte Ltd. pp. 83–87. ISBN 981-02-3023-0. ISSN 1038-5762.
- Kennett, B. L. N.; Chopping, R.; Blewett, R. (2018). The Australian continent: a geophysical synthesis. Canberra: Australian National University Press. ISBN 9781760462475.
- O’Connell, James F.; Allen, Jim; Hawkes, Kristen (2010). "Pleistocene Sahul and the origins of seafaring". In Anderson, Athol; Barrett, James H.; Boyle, Katherine V. (eds.). The global origins and development of seafaring. Cambridge: MacDonald Institute for Archeological Research. pp. 57–68. ISBN 978-1-902937-52-6.
- O'Connor, Sue; Hiscock, Peter (2018). "The people of Sahul and near Oceania". In Cochrane, Ethan E.; Hunt, Terry L. (eds.). The Oxford Handbook of Prehistoric Oceania. New York: Oxford University Press. pp. 26–45. ISBN 978-0-19-992507-0.
- Oliver, Douglas L. (1961). The Pacific Islands. New York: The American Museum of Natural History.
- Thomas, Nicholas (June 2021). "From Sunda to Sahul: the first crossings and early settlement of the Pacific". Natural History. Research Triangle Park: Natural History Magazine, Inc. ISSN 0028-0712. Retrieved 7 January 2022.
- White, J. Peter; O'Connell, James F. (1982). A prehistory of Australia, New Guinea and Sahul. Sydney: Academic Press Australia. ISBN 0-12-746750-5.