AI Article Synopsis

  • The study investigates the phylogeography and demographic history of an ectoparasite found on the Amur minnow in East Asia's cold freshwater, revealing significant geographic distribution patterns among haplotypes.
  • Genetic analysis of 79 individual parasites yielded 25 haplotypes, indicating a purifying selection, with distinct levels of haplotype and nucleotide diversity in the Qinling Mountains.
  • Findings suggest that geological events and climate changes during the Pleistocene influenced the evolutionary history of the ectoparasite, with all populations showing signs of contraction during this period.

Article Abstract

is an ectoparasite on the Amur minnow () that is widely distributed in the cold fresh waters of East Asia. In the present study, the phylogeography and demographic history of and the distribution of its host in the Qinling Mountains are examined. A total of 79 individual parasites was sequenced for a 528 bp region of the mitochondrial NADH dehydrogenase subunit 5 (ND5) gene, and 25 haplotypes were obtained. The substitution rate (dN/dS) was 0.068 and indicated purifying selection. Haplotype diversity () and nucleotide diversity () varied widely in the Qinling Mountains. Phylogenetic trees based on Bayesian inference (BI), maximum likelihood (ML), and maximum parsimony (MP) methods and network analysis revealed that all haplotypes were consistently well-supported in three different lineages, indicating a significant geographic distribution pattern. There was a significant positive correlation between genetic differentiation ( ) and geographic distance. The results of mismatch distribution, neutrality test and Bayesian skyline plot analyses showed that whole populations underwent population contraction during the Pleistocene. Based on the molecular clock calibration, the most common ancestor was estimated to have emerged in the middle Pleistocene. Our study suggests for the first time that a clearly phylogeography of was shaped by geological events and climate fluctuations, such as orogenesis, drainage capture changes, and vicariance, during the Pleistocene in the Qinling Mountains.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7029060PMC
http://dx.doi.org/10.1002/ece3.6000DOI Listing

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