2018
DOI: 10.1360/n972018-00569
|View full text |Cite
|
Sign up to set email alerts
|

Evolutionary hotspot of Cenozoic fish: Paleogene ichthyofauna from the onshore basins around Beibu Gulf

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

3
1
0

Year Published

2021
2021
2021
2021

Publication Types

Select...
3
3

Relationship

1
5

Authors

Journals

citations
Cited by 6 publications
(4 citation statements)
references
References 19 publications
3
1
0
Order By: Relevance
“…The cyprinid fossils Nanningocyprinus wui and Huashancyprinus robustispinus found in Oligocene formations of the Nanning and Ningming Basins are also consistent with our results (31). Other biological and geological evidence suggests that the palaeo-Jinshajiang once owed southward and probably connected through the palaeo-Red River into the South China Sea (Supplementary Table S1).…”
Section: Resultssupporting
confidence: 90%
“…The cyprinid fossils Nanningocyprinus wui and Huashancyprinus robustispinus found in Oligocene formations of the Nanning and Ningming Basins are also consistent with our results (31). Other biological and geological evidence suggests that the palaeo-Jinshajiang once owed southward and probably connected through the palaeo-Red River into the South China Sea (Supplementary Table S1).…”
Section: Resultssupporting
confidence: 90%
“…The cyprinid fossils Nanningocyprinus wui and Huashancyprinus robustispinus found in Oligocene formations of the Nanning and Ningming Basins are also consistent with our results (29). Other biological and geological evidence suggests that the palaeo-Jinshajiang once owed southward and probably connected through the palaeo-Red River into the South China Sea (SI Appendix, Table S1).…”
Section: Resultssupporting
confidence: 90%
“…The cyprinid fossils Nanningocyprinus wui and Huashancyprinus robustispinus found in the Oligocene Formation of the Nanning and Ningming Basins are also in agreement with our results (30). Other biological and geological evidence also suggests that the palaeo-Jinshajiang once owed southward and probably owed through the palaeo-Red River into the South China Sea (Supplementary Table 1).…”
Section: The Palaeo-jinshajiang Owing Southward In the Oligocenesupporting
confidence: 91%