No high Tibetan Plateau until the Neogene

The Late Paleogene surface height and paleoenvironment for the core area of the Qinghai-Tibetan Plateau (QTP) remain critically unresolved. Here, we report the discovery of the youngest well-preserved fossil palm leaves from Tibet. They were recovered from the Late Paleogene (Chattian), ca. 25.5 ± 0...

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Detalles Bibliográficos
Autores principales: Su, T., Farnsworth, A., Spicer, R. A., Huang, J., Wu, F.-X., Liu, J., Li, S.-F., Xing, Y.-W., Huang, Y.-J., Deng, W.-Y.-D., Tang, H., Xu, C.-L., Zhao, F., Srivastava, G., Valdes, P. J., Deng, T., Zhou, Z.-K.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6402856/
https://www.ncbi.nlm.nih.gov/pubmed/30854430
http://dx.doi.org/10.1126/sciadv.aav2189

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6402856/
https://www.ncbi.nlm.nih.gov/pubmed/30854430
http://dx.doi.org/10.1126/sciadv.aav2189

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