Massive actions have been and are being taken into protecting the world’s primates from extinction,while the study of the properties of genetic diversity,demographic history,and ecological relationships will benefit t...Massive actions have been and are being taken into protecting the world’s primates from extinction,while the study of the properties of genetic diversity,demographic history,and ecological relationships will benefit the understand-ing of the long-term survival of a species.The Taihangshan macaque(Macaca mulatta tcheliensis),a subspecies of rhesus macaque(Macaca mulatta),is endemic to China and currently restricted to southern Mt.Taihangshan area.Herein,we evaluated the genetic diversity,population structure,and demographic history of this subspecies using mitochondrial(Cytb and high variable region I:HVR I)and nuclear markers(microsatellite loci)of 131 in-dividuals collected from 9 localities covering the distribution range of this subspecies.Both phylogenetic analyses and genetic assignment revealed that the wild populations of Taihangshan macaques could be divided into 2 major highly divergent clades,THS-east and THS-west.Low genetic diversity(π:0.00266±0.00016)but high haplotype diversity(Hd:0.80352±0.015)were detected in the Taihangshan macaques,particularly in THS-east.Analyses of demographic history suggested that the Taihangshan macaques experiencedfirst a stable historical population size from Holocene to early 19th century but a subtle decline and then slight growth in the recent 200 years.We suggest that bridging the neighbor populations(i.e.setting corridors)would facilitate the male-mediated geneflow and subsequently increase the genetic diversity of the Taihangshan macaque populations.展开更多
Among mammals,mothers provide maternal care and protection starting from gestation and they ensure nutritional supply via lactation after birth(Clutton-Brock 1991).However,in social mammals,infants may also be cared f...Among mammals,mothers provide maternal care and protection starting from gestation and they ensure nutritional supply via lactation after birth(Clutton-Brock 1991).However,in social mammals,infants may also be cared for by a variety of other group members,such as fathers,siblings,a host of more distant relatives,and even unrelated individuals.Care by individuals other than the mother is known as allomaternal care(nonmaternal care)(Ishizuka 2020).Moreover,adoption of an orphaned infant is a special case of allomaternal care(Chaves et al.2020).展开更多
There are five major geological events in Precambrian complex, Taihangshan region determined by researching into geology and isotopic chronology of the complex. Basaltic magma erupted and quartz-dioritic to tonalitic ...There are five major geological events in Precambrian complex, Taihangshan region determined by researching into geology and isotopic chronology of the complex. Basaltic magma erupted and quartz-dioritic to tonalitic magma intruded in earlier neo-Archaean, which formed hornblende-plagiogneiss of Fuping gneiss complex and metamorphic mafic rock enclaves in TTGgneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-Archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Lüliang movement. gneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-Archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Lüliang movement.展开更多
基金financially supported by the Cultivation Fund for Young Teachers in Natural Science Basic Research of Zhengzhou University(JC2020043029)the National Natural Science Foundation of China(Nos.31672302 and 32070446).
文摘Massive actions have been and are being taken into protecting the world’s primates from extinction,while the study of the properties of genetic diversity,demographic history,and ecological relationships will benefit the understand-ing of the long-term survival of a species.The Taihangshan macaque(Macaca mulatta tcheliensis),a subspecies of rhesus macaque(Macaca mulatta),is endemic to China and currently restricted to southern Mt.Taihangshan area.Herein,we evaluated the genetic diversity,population structure,and demographic history of this subspecies using mitochondrial(Cytb and high variable region I:HVR I)and nuclear markers(microsatellite loci)of 131 in-dividuals collected from 9 localities covering the distribution range of this subspecies.Both phylogenetic analyses and genetic assignment revealed that the wild populations of Taihangshan macaques could be divided into 2 major highly divergent clades,THS-east and THS-west.Low genetic diversity(π:0.00266±0.00016)but high haplotype diversity(Hd:0.80352±0.015)were detected in the Taihangshan macaques,particularly in THS-east.Analyses of demographic history suggested that the Taihangshan macaques experiencedfirst a stable historical population size from Holocene to early 19th century but a subtle decline and then slight growth in the recent 200 years.We suggest that bridging the neighbor populations(i.e.setting corridors)would facilitate the male-mediated geneflow and subsequently increase the genetic diversity of the Taihangshan macaque populations.
基金supported by the National Natural Science Foundation of China(No.31472018,31672302).
文摘Among mammals,mothers provide maternal care and protection starting from gestation and they ensure nutritional supply via lactation after birth(Clutton-Brock 1991).However,in social mammals,infants may also be cared for by a variety of other group members,such as fathers,siblings,a host of more distant relatives,and even unrelated individuals.Care by individuals other than the mother is known as allomaternal care(nonmaternal care)(Ishizuka 2020).Moreover,adoption of an orphaned infant is a special case of allomaternal care(Chaves et al.2020).
文摘There are five major geological events in Precambrian complex, Taihangshan region determined by researching into geology and isotopic chronology of the complex. Basaltic magma erupted and quartz-dioritic to tonalitic magma intruded in earlier neo-Archaean, which formed hornblende-plagiogneiss of Fuping gneiss complex and metamorphic mafic rock enclaves in TTGgneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-Archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Lüliang movement. gneiss complex. Granulite facies metamorphism and emplacement of biotite-plagiogneiss occurred in late neo-Archaean. Extension and uplifting from the end of neo-Archaean to Paleoproterozoic era formed Chengnanzhuang large extensional deformation zones and metamorphic mafic veins emplaced into the deformation zones. Remobilization of Precambrian complex and tectonic uplifting in late Paleoproterozoic era formed Longquanguan ductile shear zone and emplacement of Nanying gneiss. Occurrence of regional granite pegmatite at the end of Paleoproterozoic era means the end of the Lüliang movement.
