| Literature DB >> 27103988 |
Sheng-Hong Wang1, Lei Bao1, Tian-Ming Wang1, Hong-Fang Wang1, Jian-Ping Ge1.
Abstract
Climate oscillations are the key factors to understand the patterns in modern biodiversity. East Asia harbors the most diverse temperate flora, largely because an extensive terrestrial ice cap was absent during repeated Pleistocene glaciation-interglacial cycles. Comparing the demographic histories of species that are codistributed and are close relatives may provide insight into how the process of climate change influences species ranges. In this study, we compared the spatial genetic structure and demographic histories of two coexisting Eleutherococcus species, Eleutherococcus senticosus and E. sessiliflorus. Both species are distributed in northern China, regions that are generally considered to be sensitive to climatic fluctuations. These regions once hosted temperate forest, but this temperate forest was replaced by tundra and taiga forest during the Last Glacial Maximum (LGM), according to pollen records. Using three chloroplast DNA fragments, we assessed the genetic structure of 20 and 9 natural populations of E. senticosus and E. sessiliflorus, respectively. Extremely contrasting genetic patterns were found between the two species; E. sessiliflorus had little genetic variation, whereas E. senticosus had considerably higher levels of genetic variation (15 haplotypes). We speculated that a recent severe bottleneck may have resulted in the extremely low genetic diversity in E. sessiliflorus. In E. senticosus, populations in Northeast China (NEC) harbored all of the haplotypes found in this species and included private haplotypes. The populations in NEC had higher levels of genetic diversity than did those from North China (NC). Therefore, we suggest that both the NC and NEC regions can sustain LGM refugia and that lineage admixture from multiple refugia took place after the LGM elevated the local genetic diversity in NEC. In NEC, multiple genetic hot spots were found in the Changbai Mountains and the Xiaoxing'an Range, which implied that multiple locations in NEC may sustain LGM refugia, even in the Xiaoxing'an Range.Entities:
Keywords: East Asia; Eleutherococcus senticosus; Eleutherococcus sessiliflorus; ecological niche modeling; northern refugia; phylogeography
Year: 2016 PMID: 27103988 PMCID: PMC4833501 DOI: 10.1002/ece3.2118
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
Figure 1The individual plants of Eleutherococcus senticosus (A) and E. sessiliflorus (C), and their fruits (B) (D).
Figure 2(A) Geographic distribution of 15 chloroplast DNA (cpDNA) haplotypes in Eleutherococcus senticosus. The size of the pies is proportional to the contribution of each population to the total gene diversity (C T). The blue dots represent the 9 sampling locations of E. sessiliflorus. (B) Median‐joining network of the 15 cpDNA haplotypes in E. senticosus and one cpDNA haplotype (H16) in E. sessiliflorus. Circle sizes correspond to haplotype frequency. Branch lengths longer than one mutational step are marked on each branch.
Sample locations, sample sizes, haplotypes, and genetic diversity of populations of Eleutherococcus senticosus and E. sessiliflorus
| Population code | Location | Longitude (°E) | Latitude (°N) | Alt. (m) |
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| Haplotype | Private haplotype |
|---|---|---|---|---|---|---|---|---|---|---|---|
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| WYL | Wuyiling, Heilongjiang | 129.65 | 48.73 | 425 | 10 | 0.00053 | 0.00052 | 0.511 | 1.067 | H2 (2), H4 (1), H5 (7) | |
| KDQ | Kundeqi, Heilongjiang | 127.74 | 48.68 | 440 | 9 | 0.00069 | 0.00060 | 0.694 | 1.603 | H3 (1), H5 (5), H9 (2), H15 (1) | H15 |
| LS | Liangshui, Heilongjiang | 128.88 | 47.18 | 414 | 10 | 0.00080 | 0.00073 | 0.844 | 2.133 | H1 (2), H3 (1),H6 (3), H7 (1), H9 (3) | |
| FZ | Fangzheng, Heilongjiang | 128.99 | 45.67 | 297 | 9 | 0.00124 | 0.00154 | 0.722 | 1.563 | H1 (3), H9 (4), H13 (2) | |
| FYQ | Fengyueqiao, Heilongjiang | 130.82 | 44.79 | 728 | 8 | 0.00087 | 0.00094 | 0.821 | 2.000 | H1 (2), H3 (2), H5 (3), H9 (1) | |
| HNH | Huangnihe, Jilin | 128.00 | 43.61 | 650 | 9 | 0.00069 | 0.00065 | 0.639 | 1.317 | H1 (1), H5 (5), H9 (3) | |
| CH | Chunhua, Jilin | 131.15 | 43.39 | 690 | 15 | 0.00081 | 0.00100 | 0.867 | 2.269 | H1 (1), H2 (1), H3 (4), H7 (2), H9 (2), H12 (4), H14 (1) | H14 |
| WQ | Wangqing, Jilin | 130.18 | 43.35 | 543 | 7 | 0.00077 | 0.00097 | 0.857 | 2.143 | H1 (2), H2 (1), H3 (2), H4 (2) | |
| SHB | Saihanba, Hebei | 117.50 | 42.27 | 8 | 0 | 0 | 0 | 0 | H6 (8) | ||
| CBS | Changbaishan, Jilin | 127.89 | 42.25 | 1028 | 9 | 0.00138 | 0.00123 | 0.806 | 2.016 | H1 (2), H3 (4), H5 (1), H6 (1), H13 (1) | |
| DS | Dasu, Liaoning | 125.09 | 41.88 | 546 | 4 | 0.00123 | 0.00113 | 0.833 | 2.000 | H5 (2), H11 (1), H12 (1) | H11 |
| DHT | Dahaituo, Hebei | 116.12 | 41.36 | 1611 | 8 | 0.00072 | 0.00064 | 0.821 | 2.000 | H1 (1), H5 (3), H6 (2), H9 (2) | |
| QS | Qianshan, Liaoning | 123.12 | 40.98 | 529 | 9 | 0 | 0 | 0 | 0 | H7 (9) | |
| BS | Baishi, Liaoning | 124.78 | 40.94 | 911 | 10 | 0.00146 | 0.00124 | 0.889 | 2.367 | H1 (1), H5 (2), H7 (3), H8 (1), H9 (2), H10 (1) | H8, H10 |
| WLS | Wulingshan, Hebei | 117.48 | 40.56 | 1165 | 9 | 0.00041 | 0.00044 | 0.389 | 0.722 | H1 (2), H6 (7) | |
| XWT | Xiaowutai, Hebei | 115.42 | 39.98 | 1160 | 13 | 0.00061 | 0.00074 | 0.744 | 1.734 | H1 (3), H3 (2), H5 (6), H6 (2) | |
| LYS | Luyashan, Shanxi | 111.92 | 38.73 | 2060 | 10 | 0.00053 | 0.00058 | 0.689 | 1.476 | H1 (2), H5 (3), H6 (5) | |
| PQG | Pangquangou, Shanxi | 111.46 | 37.85 | 1944 | 10 | 0 | 0 | 0 | 0 | H5 (10) | |
| ZSY | Zhangshiyan, Hebei | 114.03 | 37.46 | 1537 | 8 | 0.00058 | 0.00080 | 0.536 | 0.929 | H1 (3), H5 (5) | |
| LKS | Lingkongshan, Shanxi | 112.13 | 36.58 | 1492 | 10 | 0.00053 | 0.00080 | 0.533 | 0.924 | H1 (6), H5 (4) | |
| Average | 0.00110 | 0.00086 | 0.835 | 2.413 | |||||||
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| FYQ | Fengyueqiao, Heilongjiang | 130.82 | 44.79 | 478 | 1 | – | – | – | – | H16 | – |
| CH | Chunhua, Jilin | 131.15 | 43.39 | 242 | 8 | – | – | – | – | H16 | – |
| DQG | Daqinggou, Neimenggu | 122.17 | 42.8 | 211 | 3 | – | – | – | – | H16 | – |
| CBS | Changbaishan, Jilin | 127.89 | 42.25 | 775 | 8 | – | – | – | – | H16 | – |
| QS | Qianshan, Liaoning | 123.12 | 40.98 | 483 | 10 | – | – | – | – | H16 | – |
| WLS | Wulingshan, Hebei | 117.48 | 40.56 | 899 | 11 | – | – | – | – | H16 | – |
| BSh | Baoshan, Liaoning | 123.78 | 40.42 | 221 | 2 | – | – | – | – | H16 | – |
| XWT | Xiaowutai, Hebei | 115.42 | 39.98 | 859 | 9 | – | – | – | – | H16 | – |
| ZSY | Zhangshiyan, Hebei | 114.03 | 37.46 | 1221 | 9 | – | – | – | – | H16 | – |
| Average | – | – | – | – | |||||||
Sample size (n), Watterson's estimate (θ), nucleotide diversity (π), haplotype diversity (Hd) and allele richness after rarefaction (R S) are shown for each population.
Figure 3The contribution of each population in Eleutherococcus senticosus to the total gene diversity. The black dots on the bars represent the total gene diversity of that population (C T). Gray bars indicate the contribution to interpopulation diversity. White bars indicate the contribution to intrapopulation diversity. Sample locations from different regions were colored green for North China (NC), red for the Changbai Mountains and yellow for the Xiaoxing'an Range. The latter two areas are located in Northeast China (NEC).
Figure 4Rooted consensus trees for cpDNA haplotypes. Values on the branches are bootstrap support values for the posterior probability of the Bayesian analysis. Haplotypes distributed in different areas are marked in different colors. Colors were green for North China (NC), red for the Changbai Mountains, and yellow for the Xiaoxing'an Range.
Figure 5Mismatch distribution for Eleutherococcus senticosus. The solid line represents the simulated mismatch distribution of a stationary population. The dotted line represents the observed mismatch distribution.
Figure 6Results of the predicted distribution probability from ecological niche modeling (ENM) for current climatic conditions of Eleutherococcus senticosus (A) and E. sessiliflorus (B) and for the Last Glacial Maximum (LGM, c. 21,000–18,000 years before present) of E. senticosus (C) and E. sessiliflorus (D) using data from the Model for Interdisciplinary Research on Climate (MIROC).