Людина цзайчанійська (Ukrainian Wikipedia)

Analysis of information sources in references of the Wikipedia article "Людина цзайчанійська" in Ukrainian language version.

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cssn.cn

ethn.cssn.cn

discovery.com

news.discovery.com

doi.org

  • Chang, Chun-Hsiang; Kaifu, Yousuke; Takai, Masanaru; Kono, Reiko T.; Grün, Rainer; Matsu’ura, Shuji; Kinsley, Les; Lin, Liang-Kong (2015). The first archaic Homo from Taiwan. Nature Communications. 6: 6037. Bibcode:2015NatCo...6.6037C. doi:10.1038/ncomms7037. PMC 4316746. PMID 25625212. Older low-sea-level events, 225, 240–280, ?300, 335–360 and 425–450 ka cannot be completely excluded as the age for Penghu 1, but such a situation requires explanation for preservation through repeated sedimentary events and the unusual distribution of Crocuta crocuta ultima. Therefore, Penghu 1 is younger than 450 ka, and most likely 10–70 ka or 130–190 ka.
  • Wu, Xinzhi; Tong, Haowen (2015). Discussions on the significance and geologic age of Penghu 1 Mandible (PDF). Acta Anthropologica Sinica (Chinese та English) . 34 (3). doi:10.16359/j.cnki.cn11-1963/q.2015.0000. Архів оригіналу (PDF) за 4 березня 2016. Процитовано 7 січня 2024.
  • McMenamin, Mark A. S. (2015). Homo tsaichangensis and Gigantopithecus. South Hadley, Massachusetts: Meanma Press. doi:10.13140/2.1.3463.7121. ISBN 978-1-893882-19-5.
  • Chen, Fahu; Welker, Frido; Shen, Chuan-Chou; Bailey, Shara E.; Bergmann, Inga; Davis, Simon; Xia, Huan; Wang, Hui; Fischer, Roman (May 2019). A late Middle Pleistocene Denisovan mandible from the Tibetan Plateau. Nature (англ.). 569 (7756): 409—412. Bibcode:2019Natur.569..409C. doi:10.1038/s41586-019-1139-x. ISSN 1476-4687. PMID 31043746.

harvard.edu

ui.adsabs.harvard.edu

  • Chang, Chun-Hsiang; Kaifu, Yousuke; Takai, Masanaru; Kono, Reiko T.; Grün, Rainer; Matsu’ura, Shuji; Kinsley, Les; Lin, Liang-Kong (2015). The first archaic Homo from Taiwan. Nature Communications. 6: 6037. Bibcode:2015NatCo...6.6037C. doi:10.1038/ncomms7037. PMC 4316746. PMID 25625212. Older low-sea-level events, 225, 240–280, ?300, 335–360 and 425–450 ka cannot be completely excluded as the age for Penghu 1, but such a situation requires explanation for preservation through repeated sedimentary events and the unusual distribution of Crocuta crocuta ultima. Therefore, Penghu 1 is younger than 450 ka, and most likely 10–70 ka or 130–190 ka.
  • Chen, Fahu; Welker, Frido; Shen, Chuan-Chou; Bailey, Shara E.; Bergmann, Inga; Davis, Simon; Xia, Huan; Wang, Hui; Fischer, Roman (May 2019). A late Middle Pleistocene Denisovan mandible from the Tibetan Plateau. Nature (англ.). 569 (7756): 409—412. Bibcode:2019Natur.569..409C. doi:10.1038/s41586-019-1139-x. ISSN 1476-4687. PMID 31043746.

livescience.com

nature.com

nih.gov

pubmed.ncbi.nlm.nih.gov

  • Chang, Chun-Hsiang; Kaifu, Yousuke; Takai, Masanaru; Kono, Reiko T.; Grün, Rainer; Matsu’ura, Shuji; Kinsley, Les; Lin, Liang-Kong (2015). The first archaic Homo from Taiwan. Nature Communications. 6: 6037. Bibcode:2015NatCo...6.6037C. doi:10.1038/ncomms7037. PMC 4316746. PMID 25625212. Older low-sea-level events, 225, 240–280, ?300, 335–360 and 425–450 ka cannot be completely excluded as the age for Penghu 1, but such a situation requires explanation for preservation through repeated sedimentary events and the unusual distribution of Crocuta crocuta ultima. Therefore, Penghu 1 is younger than 450 ka, and most likely 10–70 ka or 130–190 ka.
  • Chen, Fahu; Welker, Frido; Shen, Chuan-Chou; Bailey, Shara E.; Bergmann, Inga; Davis, Simon; Xia, Huan; Wang, Hui; Fischer, Roman (May 2019). A late Middle Pleistocene Denisovan mandible from the Tibetan Plateau. Nature (англ.). 569 (7756): 409—412. Bibcode:2019Natur.569..409C. doi:10.1038/s41586-019-1139-x. ISSN 1476-4687. PMID 31043746.

ncbi.nlm.nih.gov

  • Chang, Chun-Hsiang; Kaifu, Yousuke; Takai, Masanaru; Kono, Reiko T.; Grün, Rainer; Matsu’ura, Shuji; Kinsley, Les; Lin, Liang-Kong (2015). The first archaic Homo from Taiwan. Nature Communications. 6: 6037. Bibcode:2015NatCo...6.6037C. doi:10.1038/ncomms7037. PMC 4316746. PMID 25625212. Older low-sea-level events, 225, 240–280, ?300, 335–360 and 425–450 ka cannot be completely excluded as the age for Penghu 1, but such a situation requires explanation for preservation through repeated sedimentary events and the unusual distribution of Crocuta crocuta ultima. Therefore, Penghu 1 is younger than 450 ka, and most likely 10–70 ka or 130–190 ka.

researchgate.net

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