AI Article Synopsis

  • The study examines the evolution of tree form in Daphniphyllum macropodum, focusing on its two varieties: a tree and a shrub, adapted to different temperate climates in Japan.
  • Genetic analysis shows that the two varieties have diverged, but maintain some gene flow, particularly in areas where their ranges overlap, suggesting that environmental factors like snowfall influence their differentiation.
  • Findings propose that the evolution of these varieties aligns with historical climate changes, particularly since the middle Quaternary, which impacted snowfall patterns in their habitats.

Article Abstract

Tree form evolution is an important ecological specialization for woody species, but its evolutionary process with adaptation is poorly understood, especially on the microevolutionary scale. Daphniphyllum macropodum comprises two varieties: a tree variety growing in a warm temperate climate with light snowfall and a shrub variety growing in a cool temperate climate with heavy snowfall in Japan. Chloroplast DNA variations and genome-wide single-nucleotide polymorphisms across D. macropodum populations and D. teijsmannii as an outgroup were used to reveal the evolutionary process of the shrub variety. Population genetic analysis indicated that the two varieties diverged but were weakly differentiated. Approximate Bayesian computation analysis supported a scenario that assumed migration between the tree variety and the southern populations of the shrub variety. We found migration between the two varieties where the distributions of the two varieties are in contact, and it is concordant with higher tree height in the southern populations of the shrub variety than the northern populations. The genetic divergence between the two varieties was associated with snowfall. The heavy snowfall climate is considered to have developed since the middle Quaternary in this region. The estimated divergence time between the two varieties suggests that the evolution of the two varieties may be concordant with such paleoclimatic change.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10462706PMC
http://dx.doi.org/10.1038/s41437-023-00637-2DOI Listing

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