User:Reke/sandbox: Difference between revisions

Content deleted Content added

Inline

Revision as of 09:23, 17 June 2019

This is the user sandbox of Reke. A user sandbox is a subpage of the user's user page. It serves as a testing spot and page development space for the user and is not an encyclopedia article. Create or edit your own sandbox here.

Other sandboxes: Main sandbox | Template sandbox

Finished writing a draft article? Are you ready to request review of it by an experienced editor for possible inclusion in Wikipedia? Submit your draft for review!

Etymology

History

From prehistory until the 16th century

Taiwan was joined to the mainland in the Late Pleistocene, until sea levels rose about 10,000 years ago. Fragmentary human remains dated 20,000 to 30,000 years ago have been found on the island, as well as later artifacts of a paleolithic culture.^[1]^[2]^: 100^[3]

^ Chang, K.C. (1989). "The Neolithic Taiwan Strait" (PDF). Kaogu. 6. translated by W. Tsao, ed. by B. Gordon: 541–550, 569. Archived from the original (PDF) on 18 April 2012. {{cite journal}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)
^ Olsen, John W.; Miller-Antonio, Sari (1992). "The Palaeolithic in Southern China". Asian Perspectives. 31 (2): 129–160. hdl:10125/17011.
^ Jiao (2007), pp. 89–90.

[1] Chang, K.C. (1989). "The Neolithic Taiwan Strait" (PDF). Kaogu. 6. translated by W. Tsao, ed. by B. Gordon: 541–550, 569. Archived from the original (PDF) on 18 April 2012. {{cite journal}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)

[palaeolithic-2] Olsen, John W.; Miller-Antonio, Sari (1992). "The Palaeolithic in Southern China". Asian Perspectives. 31 (2): 129–160. hdl:10125/17011.

[FOOTNOTEJiao200789–90-3] Jiao (2007), pp. 89–90.

[1]

[2]

[3]

@@ Line 7: / Line 7: @@
 ===From prehistory until the 16th century===
 [[File:Tsou youth of Taiwan (pre-1945).jpg|thumb|upright|A young [[Tsou people|Tsou]] man]]
-Taiwan was joined to the mainland in the Late Pleistocene, until sea levels rose about 10,000 years ago. Fragmentary human remains dated 20,000 to 30,000 years ago have been found on the island, as well as later artifacts of a paleolithic culture.<ref>{{cite journal |last=Chang |first=K.C. |authorlink=Kwang-chih Chang |others=translated by W. Tsao, ed. by B. Gordon |title=The Neolithic Taiwan Strait |journal=Kaogu |year=1989 |volume=6 |pages=541–550, 569 |url=http://http-server.carleton.ca/~bgordon/Rice/papers/App.18ChangKC89.pdf |deadurl=yes |archiveurl=https://web.archive.org/web/20120418153210/http://http-server.carleton.ca/~bgordon/Rice/papers/App.18ChangKC89.pdf |archivedate=18 April 2012}}</ref><ref name="palaeolithic">{{cite journal |last1=Olsen |first1=John W. |last2=Miller-Antonio |first2=Sari |title=The Palaeolithic in Southern China |journal=Asian Perspectives |volume=31 |issue=2 |pages=129–160 |year=1992 |url=http://scholarspace.manoa.hawaii.edu/handle/10125/17011 |hdl=10125/17011}}</ref>{{sfnp|Jiao|2007|pp=89–90}}
+Taiwan was joined to the mainland in the Late Pleistocene, until sea levels rose about 10,000 years ago. Fragmentary human remains dated 20,000 to 30,000 years ago have been found on the island, as well as later artifacts of a paleolithic culture.<ref>{{cite journal |last=Chang |first=K.C. |authorlink=Kwang-chih Chang |others=translated by W. Tsao, ed. by B. Gordon |title=The Neolithic Taiwan Strait |journal=Kaogu |year=1989 |volume=6 |pages=541–550, 569 |url=http://http-server.carleton.ca/~bgordon/Rice/papers/App.18ChangKC89.pdf |deadurl=yes |archiveurl=https://web.archive.org/web/20120418153210/http://http-server.carleton.ca/~bgordon/Rice/papers/App.18ChangKC89.pdf |archivedate=18 April 2012}}</ref><ref name="palaeolithic">{{cite journal |last1=Olsen |first1=John W. |last2=Miller-Antonio |first2=Sari |title=The Palaeolithic in Southern China |journal=Asian Perspectives |volume=31 |issue=2 |pages=129–160 |year=1992 |url=http://scholarspace.manoa.hawaii.edu/handle/10125/17011 |hdl=10125/17011}}</ref>{{rp|100}}{{sfnp|Jiao|2007|pp=89–90}}