For oviparous species with little or no parental care, oviposition site choice may be a powerful agent of natural selection, playing an important role in the evolution of species fitness and life history. Identifying ...For oviparous species with little or no parental care, oviposition site choice may be a powerful agent of natural selection, playing an important role in the evolution of species fitness and life history. Identifying and clarifying the microhabitat characteristics of oviposition sites are key to understanding life history strategies and local adaptations for amphibians with complex biphasic life cycles. However, oviposition strategies for amphibians in alpine streams remain poorly understood. Here, we focused on oviposition site selection for the Chinting alpine toad(Scutiger chintingensis) on Mount Wawu on the eastern margin of the Qinghai-Xizang Plateau. We identified the microhabitat differences between oviposition sites and non-oviposition sites for this species, predicted oviposition site selection patterns,and evaluated the relative importance of each microhabitat variable as well as the effects of the variables on the model prediction probabilities. This study revealed that the microhabitat characteristics of oviposition sites in this species included high water velocity, shallow water, and high-water surface coverage. Water velocity and rock volume were the most important variables explaining the categories of oviposition sites. Additionally, we observed nearly half the proportion of overlapping oviposition in this species, and the benefits of this behavior in terms of microhabitat characteristics need to be explored in the future. Our study revealed an oviposition site selection strategy for amphibians within alpine streams, and contributed to understanding the life history and environmental adaptation strategies of an endemic alpine stream species, and thereby providing guidance for effective conservation strategies for alpine stream amphibians under global change.展开更多
The EC (electrical conductivity), pH and concentrations of major anions, cations and dissolved silica were determined in the stream meltwater draining from the glacier. Stream meltwater samples were sampled during Jun...The EC (electrical conductivity), pH and concentrations of major anions, cations and dissolved silica were determined in the stream meltwater draining from the glacier. Stream meltwater samples were sampled during June and October 1997 from Dudu glacier, Bhngirathi valley, Garhwal Himalaya. This study is an attempt to reveal the hydrochemical processes operating in the glacialized regime of Garhwal Himalaya. The results show that the abundance order of cations and anions in the meltwater is c(Ca2+ )>c(Na+ )>c(Mg2+ ) >c(K+ ) and c(SO42- ) >c>(HCO3-) >c(NO3- ) >c(CI- ). The rock weathering is the most important mechanism controlling the water chemistry in the basin. Pyrite oxidation and carbonation are the main hydrogen ion supply reactions contributing to the chemical weathering in the basin. There is a distinct difference between the solute concentrations in samples collected during June and October.展开更多
Fifteen microsatellite DNA markers were developed from a transcriptome assembly of the alpine stream frog （Scutiger boulengeri）.To characterize these loci, we genotyped 23 individuals collected from two sites. Eleve...Fifteen microsatellite DNA markers were developed from a transcriptome assembly of the alpine stream frog （Scutiger boulengeri）.To characterize these loci, we genotyped 23 individuals collected from two sites. Eleven loci were variable, with the number of alleles ranging from one to six within each population. The expected and observed heterozygosities ranged from 0 to 0.78 and from 0 to 0.64, respectively. None of the loci was in linkage disequilibrium and one locus for one population was deviated from will offer useful tools in detecting population structure Tibetan Plateau, where the species resides. the Hardy-Weinberg equilibrium. We hope that these markers of S. boulengeri and in monitoring the fragile ecosystem of the展开更多
基金supported by the National Natural Science Foundation of China (32271737, 32071544)the Interdisciplinary Innovation Team of the Chinese Academy of Sciences (CAS) “Light of West China” Program (xbzg-zdsys-202207)+1 种基金the Shenzhen Zhilan Foundation (2023010291A)Nature Science Foundation of Sichuan Province (24NSFSC2934)。
文摘For oviparous species with little or no parental care, oviposition site choice may be a powerful agent of natural selection, playing an important role in the evolution of species fitness and life history. Identifying and clarifying the microhabitat characteristics of oviposition sites are key to understanding life history strategies and local adaptations for amphibians with complex biphasic life cycles. However, oviposition strategies for amphibians in alpine streams remain poorly understood. Here, we focused on oviposition site selection for the Chinting alpine toad(Scutiger chintingensis) on Mount Wawu on the eastern margin of the Qinghai-Xizang Plateau. We identified the microhabitat differences between oviposition sites and non-oviposition sites for this species, predicted oviposition site selection patterns,and evaluated the relative importance of each microhabitat variable as well as the effects of the variables on the model prediction probabilities. This study revealed that the microhabitat characteristics of oviposition sites in this species included high water velocity, shallow water, and high-water surface coverage. Water velocity and rock volume were the most important variables explaining the categories of oviposition sites. Additionally, we observed nearly half the proportion of overlapping oviposition in this species, and the benefits of this behavior in terms of microhabitat characteristics need to be explored in the future. Our study revealed an oviposition site selection strategy for amphibians within alpine streams, and contributed to understanding the life history and environmental adaptation strategies of an endemic alpine stream species, and thereby providing guidance for effective conservation strategies for alpine stream amphibians under global change.
文摘The EC (electrical conductivity), pH and concentrations of major anions, cations and dissolved silica were determined in the stream meltwater draining from the glacier. Stream meltwater samples were sampled during June and October 1997 from Dudu glacier, Bhngirathi valley, Garhwal Himalaya. This study is an attempt to reveal the hydrochemical processes operating in the glacialized regime of Garhwal Himalaya. The results show that the abundance order of cations and anions in the meltwater is c(Ca2+ )>c(Na+ )>c(Mg2+ ) >c(K+ ) and c(SO42- ) >c>(HCO3-) >c(NO3- ) >c(CI- ). The rock weathering is the most important mechanism controlling the water chemistry in the basin. Pyrite oxidation and carbonation are the main hydrogen ion supply reactions contributing to the chemical weathering in the basin. There is a distinct difference between the solute concentrations in samples collected during June and October.
基金supported by a scholarship from the China Scholarship Council to Z.DU
文摘Fifteen microsatellite DNA markers were developed from a transcriptome assembly of the alpine stream frog （Scutiger boulengeri）.To characterize these loci, we genotyped 23 individuals collected from two sites. Eleven loci were variable, with the number of alleles ranging from one to six within each population. The expected and observed heterozygosities ranged from 0 to 0.78 and from 0 to 0.64, respectively. None of the loci was in linkage disequilibrium and one locus for one population was deviated from will offer useful tools in detecting population structure Tibetan Plateau, where the species resides. the Hardy-Weinberg equilibrium. We hope that these markers of S. boulengeri and in monitoring the fragile ecosystem of the
