核心概念
Geographic population structure and local extinctions can explain the observed declines in Neanderthal effective population size over the last 20,000 years, without requiring an actual decline in the number of individuals.
摘要
The article explores mathematical models of geographic population structure to explain the observed patterns in Neanderthal and Denisovan effective population size (Ne) estimates over time.
Key insights:
- The roughly 5-fold decline in Neanderthal Ne over the last 20,000 years is likely an artifact of sampling two genes from the same local deme within a structured population, rather than a real decline in the overall Neanderthal metapopulation.
- Modest rates of local extinction and gene flow between demes can produce substantial reductions in heterozygosity and Ne, even without changes in the total number of individuals.
- Simulations using the island and circular stepping-stone models show that the Neanderthal data are consistent with structured populations, without requiring a real decline in population size.
- The Denisovan data do not show the same decline, but this does not necessarily mean the Denisovan population lacked structure, as such patterns can be variable.
- The results support the hypothesis that the Neanderthal population was geographically structured, as suggested by previous studies using runs of homozygosity.
統計資料
"If two genes are drawn at random from the population as a whole, their expected coalescence time is 2Nd/(2Nm + 1)."
"The mean coalescence time for a pair of lineages i steps apart is (d - i)i/(M + X)."
引述
"Not only does Ne change in response to changes in gene flow [17, 20, 33], it may also exhibit a prolonged decline even when there has been no change either in the number of individuals or in the rate or pattern of gene flow [18, 20]."
"If demes never went extinct, the asymptote, Ne(∞), is even larger than Nd, the size of the metapopulation."
"Consequently, the census size of the metapopulation would be larger than Nd."