scholarly journals Why Did Great Apes Disappear from Southwestern China?

Eos ◽  
2020 ◽  
Vol 101 ◽  
Author(s):  
Sarah Stanley

Periodic pulses of cooler temperatures may have disrupted the warm, humid, late Miocene climate that sustained the region’s great apes long after most species disappeared elsewhere.

2021 ◽  
Vol 118 (5) ◽  
pp. e2015215118
Author(s):  
Alessandro Urciuoli ◽  
Clément Zanolli ◽  
Sergio Almécija ◽  
Amélie Beaudet ◽  
Jean Dumoncel ◽  
...  

Late Miocene great apes are key to reconstructing the ancestral morphotype from which earliest hominins evolved. Despite consensus that the late Miocene dryopith great apes Hispanopithecus laietanus (Spain) and Rudapithecus hungaricus (Hungary) are closely related (Hominidae), ongoing debate on their phylogenetic relationships with extant apes (stem hominids, hominines, or pongines) complicates our understanding of great ape and human evolution. To clarify this question, we rely on the morphology of the inner ear semicircular canals, which has been shown to be phylogenetically informative. Based on microcomputed tomography scans, we describe the vestibular morphology of Hispanopithecus and Rudapithecus, and compare them with extant hominoids using landmark-free deformation-based three-dimensional geometric morphometric analyses. We also provide critical evidence about the evolutionary patterns of the vestibular apparatus in living and fossil hominoids under different phylogenetic assumptions for dryopiths. Our results are consistent with the distinction of Rudapithecus and Hispanopithecus at the genus rank, and further support their allocation to the Hominidae based on their derived semicircular canal volumetric proportions. Compared with extant hominids, the vestibular morphology of Hispanopithecus and Rudapithecus most closely resembles that of African apes, and differs from the derived condition of orangutans. However, the vestibular morphologies reconstructed for the last common ancestors of dryopiths, crown hominines, and crown hominids are very similar, indicating that hominines are plesiomorphic in this regard. Therefore, our results do not conclusively favor a hominine or stem hominid status for the investigated dryopiths.


2008 ◽  
Vol 148 (1) ◽  
pp. 36-59 ◽  
Author(s):  
Jing-Xian Xu ◽  
David K. Ferguson ◽  
Cheng-Sen Li ◽  
Yu-Fei Wang

2021 ◽  
pp. 1-8
Author(s):  
San-Ping Xie ◽  
Si-Hang Zhang ◽  
Jennifer C. McElwain ◽  
Peng Zhang ◽  
Bing Wang ◽  
...  

Author(s):  
Robin Dunbar

Who were our earliest ancestors? Our lineage can be said to have started when the African great apes of the late Miocene gave rise to a new, more terrestrial group, the australopithecines, some six or seven million years ago. Two important things had happened at...


2007 ◽  
Vol 104 (49) ◽  
pp. 19220-19225 ◽  
Author(s):  
Y. Kunimatsu ◽  
M. Nakatsukasa ◽  
Y. Sawada ◽  
T. Sakai ◽  
M. Hyodo ◽  
...  

Phytotaxa ◽  
2019 ◽  
Vol 393 (1) ◽  
pp. 1
Author(s):  
HUA ZHU

The Yunnan boast three broad-leaved forests, the semi-wet evergreen broad-leaved forest (SWEB) occurring in subtropical plateaus areas, the lower montane evergreen broad-leaved forest (LMEB) in tropical lower montane, and the upper montane evergreen broad-leaved forest (UMEB) in subtropical upper montane regions. Floristic composition and biogeography of these evergreen broad-leaved forests are studied and their diversification and divergence are revealed. I found similarities across the three forest types with species-rich families tending to have cosmopolitan distributions and families with less species exhibiting other distribution types. In biogeographical elements, the SWEB and the UMEB showed similar affinity in the proportion of tropical elements comprising total genera, specifically 45% and 44% respectively, and temperate elements totaling 46% and 48%, of all genera with northern temperate distribution comprising the highest ratio (18% in the SWEB and 20% in the UMEB ). LMEB tropical elements comprised 79% of the total genera, with tropical Asian distributed elements contributing the highest ratio (27%). While the three forest floras comprised of similar families, the same is not true at the genus and species levels. I suggest our results indicate divergence of the three forest floras, possibly from events in the geological history of Yunnan. From recent palaeobotanical studies, the diversification of floras of these evergreen broad-leaved forests in Yunnan occurred during the late Miocene with increased divergence with time in response not only to altitude changes and at the same time global cooling in Yunnan, but also the southeastward extrusion of Indochina geoblock influencing LMEB, and the Himalayan uplift affecting the floras of SWEB and UMEB.


2015 ◽  
Vol 425 ◽  
pp. 14-40 ◽  
Author(s):  
Shu-Feng Li ◽  
Li-Mi Mao ◽  
Robert A. Spicer ◽  
Julie Lebreton-Anberrée ◽  
Tao Su ◽  
...  

2015 ◽  
Vol 60 (20) ◽  
pp. 1768-1777 ◽  
Author(s):  
Yongjiang Huang ◽  
Xueping Ji ◽  
Tao Su ◽  
Li Wang ◽  
Chenglong Deng ◽  
...  

2020 ◽  
Vol 47 (11) ◽  
Author(s):  
Pei Li ◽  
Chunxia Zhang ◽  
Jay Kelley ◽  
Chenglong Deng ◽  
Xueping Ji ◽  
...  

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