Abstract
Cultivated chrysanthemum (Chrysanthemum morifolium Ramat.) is an economically important ornamental plant species grown worldwide. However, the origin of the genus Chrysanthemum remains unclear. This study was conducted in the Hengduan Mountains, Yunnan Province. We took advantage of a special geographic region where the southernmost species of Ajania and the highest altitude population of Chrysanthemum indicum coexist to investigate their evolutionary origins. Diversity analysis of 9 populations of 5 species that came from 3 genera was carried out based on morphological traits and SRAP markers. Furthermore, topographical and ecological analyses and surveys of the vegetation communities in the plots were carried out for correlation analysis, and past data were used to reconstruct the ancient topography and vegetation to estimate the migration path and divergence time. We found that Chrysanthemum and Ajania were closely related based on the smooth transition states among marginal female florets and their common pollination system. The genetic relationship between Phaeostigma and Chrysanthemum was relatively distant, and Ajania was between them. Low light intensity and relatively humid habitats may be driving the elongation and evolution of marginal female florets. We found that Chrysanthemum and related genera were largely restricted to stony topographies at an altitude of ~3000 m.a.s.l. and in specialized alpine coniferous (Pinus) and broad-leaved (Quercus) mixed forest marginal communities. These stony topographies have become ecological islands of refuge for these species in the current interglacial period. The Hengduan Mountains play a key role in the evolution, divergence, and survival of Chrysanthemum and its allies.
Subject terms: Plant ecology, Plant evolution, Biodiversity, Genetic markers
Introduction
Cultivated chrysanthemum (Chrysanthemum morifolium Ramat.), as one of the most economically important ornamental plants grown worldwide1, has been popular among horticulturists and botanists for a long time2. Most research on cultivated chrysanthemum has focused on breeding, disease control, regulation of horticultural characteristics, and their molecular mechanisms3–9. There are relatively few studies on the evolutionary relationships between the genus Chrysanthemum and its wild relatives, especially with regard to biogeography and ecology, for which the origin of chrysanthemums would be useful information.
Chrysanthemum has 41 species that are widely distributed in Asia (Mongolia, Russia, China, Japan, and Korea) and eastern Europe10. There are approximately 21 species distributed in most parts of China, except Tibet and Northwest China, and most of these species grow in humid areas at low and medium altitudes.
Ajania Poljakov (Anthemideae, Asteraceae) is a sister group closely related to Chrysanthemum that can be distinguished by its disciform capitula; Chrysanthemum, on the other hand, has radiate capitula11. Phaeostigma established by Muldashev12,13 was a genus circumscribing the Chinese endemic species formerly described under Ajania based on palynology and morphology12,14, and this view was supported by molecular phylogeny15. Ajania and Chrysanthemum are not easy to distinguish clearly based on the nuclear ribosomal ITS, chloroplast DNA sequences or single-copy nuclear genes16,17. Hybrids between these taxa are easy to obtain, and their chromosomes are similar to each other. Ohashi and Yonekura18 included Ajania in Chrysanthemum. However, the results of phylogenetic comparisons among different samples and gene sequences are divergent16,17,19. The characteristics of marginal female tubular florets in Ajania can be significantly different from those of ray florets in Chrysanthemum, and more importantly, the geographical distributions of the genera Chrysanthemum and Ajania in China have obvious differences20. According to the records of the Flora of China and the Chinese Virtual Herbarium, Chrysanthemum is usually distributed to the south of China’s 500-mm isoline, whereas Ajania is mainly distributed to the north of China’s 800-mm isoline, and both are distributed between the two isolines. In addition, Chrysanthemum is usually distributed below 3000 m.a.s.l. Hence, the evolutionary relationship and origin of the two genera are still unclear. In particular, the ancestral floret characteristics being the same as those of marginal female florets, either tubular florets or ray florets, is a critical issue.
The evolution of species is driven by the environment. To explore the key issues of evolutionary history, such as the region of origin, divergence time, radiation path, and distribution range, it is necessary to combine fossil21, phytogeographical22, ecological23,24, and other evidence to obtain reasonable and accurate results. In these aspects, there is a paucity of research on Chrysanthemum, Ajania, and their allies (but see Li et al.25), especially on the phytogeography and ecology within their areas.
Mountains contribute disproportionately to the terrestrial biodiversity of Earth26. Mountain regions are unusually biodiverse, with rich aggregations of small-ranged species that form centers of endemism27. Owing to the diversification of habitats and climates, mountains have become refuges and centers of diversity for many species26,28–31. The Hengduan Mountains, located in southwest China, are a hotspot of biodiversity32. The Hengduan Mountains are home to many temperate plant species and are a center of distribution and speciation for many alpine taxa33–35.
The research site of this study was in the Erhai Lake Range, Dali, Yunnan Province, which is located in the southern margin of the Hengduan Mountains. The latitude here is between N25.482° and N26.543°, and the lake-level elevation is 1972 m.a.s.l., whereas the surrounding mountains are almost more than 3000 m.a.s.l. (the highest elevation is more than 4000 m.a.s.l.), which is a typical low-latitude and high-altitude area. As an endemic species of this area, Ajania sericea (A. sericea) is the southernmost recorded species of the genus Ajania in China at present, residing to the south of China’s 800 mm isoline. This special geographical distribution has important significance for the study of biogeography and evolution. However, only one specimen has been collected worldwide, in the collections of Harvard University Herbaria and Libraries, since it was discovered by J. M. Delavay in Yan-in-chan in 1887, and there is a paucity of research on this species. In addition, we found several populations of Chrysanthemum distributed at altitudes over 3000 m.a.s.l. here.
In this study, the main ranges around the Erhai Lake Basin were surveyed comprehensively in different periods for 3 years (2016–2018), and samples of Chrysanthemum and its allies (including A. sericea) were collected along with geomorphologic and geographic information on their habitats. In addition, we surveyed the plant community of the habitats for ecological analysis. Morphological diversity and genetic diversity were analyzed based on traits and sequence-related amplified polymorphism (SRAP) markers, respectively, and the special geographical distribution was documented using geographic information systems (GIS); correlation analysis was performed by combining topography and ecology. Last, the paleogeomorphology, paleovegetation and paleoclimate36 during the upper Eocene and the last glacial of the Quaternary in this study area were reconstructed based on previous studies of paleopalynology and geology to deduce the potential evolutionary relationship and history of the two genera. Our results will provide a new research methodology and perspective for the study of the evolutionary history and origin of Chrysanthemum and its allies through the in-depth study of biogeography and ecology.
Materials and methods
Study site
The research area was the mountains, river valleys, and basins around Erhai Lake, from N25.482° to N26.543° and E99.895° to E100.524°, within a rectangular range of approximately 120 × 65 km in Dali, Yunnan Province, China. Fieldwork analysis was conducted during May–December of 2016–2018; we searched for the species of the genus Chrysanthemum and its allies throughout the study area to obtain comprehensive distribution data. Moreover, the main vegetation types in this study area were recorded to understand vegetation characteristics at different altitudes. Furthermore, for each plot in which target species were found, plant community and topography data were collected in plots for correlation analysis.
Sampling and data collection
Three replicate plots (10 × 10 m) were randomly established within each plot37, and each replicate plot was spaced 10–50 m apart38. The number of target plants in each plot was recorded as the abundance (AB). The species richness of the tree layer (TS, height> 2 m, highly lignified), shrub layer (SS, height <2 m, lignified), and herb layer (HS, height <0.5 m) and the total richness (R, where R = TS + SS + HS) were separately recorded within each plot. TS was determined to the species level because of the significance that presenting detailed descriptions of tree species composition would have for this study, and SS and HS were identified to the genus level. Photos were taken for comparison with herbarium specimens if a species could not be identified in the field39 or had great significance to this study. The percentage cover40,41 of the tree layer (TLC), shrub layer (SLC), and herb layer (HLC) were estimated based on the surface area. The surface rock coverage (SRC) as a topographical factor in this study was estimated by the following formula:
(L(m): maximum length of rock; W (m): maximum width of rock; 0.7: correction factor based on the empirical value obtained after 20 different measurements; p: plot area (100 m2)).
To assess the morphological diversity, based on morphology, 44 qualitative traits (Table S2) were recorded and coded with different levels during the flowering period. We randomly collected 10 replicate plant samples (0–5 samples from each plot) from three replicate plots to measure 12 quantitative traits for principal component analysis (PCA): plant height (PH), stem diameter (SD), maximum leaf length (MLL), maximum leaf width (MLW), petiole length (PL), compound corymb diameter (CCD), capitulum diameter (CD), ray floret length (RFL), involucre length (IL), marginal female tubular floret length (FTL), tubular floret length (TL), and achene length (AL).
To assess the genetic diversity, based on SRAP markers, genomic DNA was extracted from the leaves of each species using a slightly modified version42 of the Murray and Thompson43 hexadecyltrimethylammonium bromide (CTAB) method. The SRAP method followed the protocol described by Zhang et al.44, and analysis was performed as described by Li and Quiros45. Analysis of genetic relationships was performed with NTSYS-pc 2.1 based on UPGMA (unweighted pair-group method with arithmetic means). The sequences of the forward and reverse SRAP primers used in this study are shown in Table S1.
We determined geographical coordinates and altitude (m.a.s.l.) of each sampling area by GPS. To understand the pollination traits, we recorded the florescence and took photos of the pollinating insects of each target population as evidence. The current main vegetation types of the study area were recorded within altitude gradient intervals; according to the previous data of paleopalynological and geological research46–52, the ancient topography and vegetation communities were reconstructed based on time nodes. These data were used to deduce the potential evolutionary relationship and estimate the divergence time between Chrysanthemum and its allies via comparison with the current situation.
Statistical analyses
The digital elevation model (DEM) was based on the Shuttle Radar Topography Mission (SRTM 3, NASA and NIMA, USA) data. We used ArcMap10.5 (Esri USA) to extract the aspect, slope53, and topographic position index for GIS analysis54. To more intuitively and accurately show topographic features, we made DEM profiles for each population. Since most of the mountains in this area are north-south oriented, we adopted east-west cross sections that were parallel to the latitude. In addition to the coefficient of variation (CV), the Shannon-Weaver diversity index (H’)51,55 was calculated based on qualitative traits using the following formula:
(P: populations = 9, Xi: the number of code values within the ith level for a qualitative trait. Level: the average value (A) and standard deviation (S) of all codes of a certain trait were calculated and then divided into 10 levels, from the first level (X < A–2S) to the tenth level (X > A + 2S), where each 0.5S is a level)
The differences between two populations of the species that live in two different plots, based on 11 quantitative morphological indexes, can be assessed by T-tests. To clearly understand the differences among 11 quantitative morphological indexes that form different species and populations, we conducted a principal component analysis (PCA) in Origin 2019 (OriginLab, USA). To account for potential correlations between the target species abundance, plant community structure and topography that could explain differences in the distribution patterns of Chrysanthemum and its allies, a correlation matrix56 was established using R 3.6.1 (R Core Team, 2016).
Results
Altitude and topographic features based on field work
In the study area, three species of Chrysanthemum, one species of Ajania, and one species of Phaeostigma were found in nine independent small-scale alpine areas (Table 1 and Fig. 1). We found that in the study area, Chrysanthemum and its allies were all distributed in high-altitude mountains and displayed a special pattern, being mainly distributed around an elevational range of 3000 m.a.s.l. ±300 m.a.s.l. The altitude range of most populations was relatively narrow, except for Cg–N (Fig. 1). Moreover, the five species were separated from each other by geographical isolation, and there was no overlap in the distribution of the two species in a plot. We observed similar topographic features with large numbers of surface rocks or screes and a thin soil layer in the nine plots (Fig. 2a, b and Fig. S1) in which Chrysanthemum and its allies were observed in this area, which suggests that they have low waterlogging tolerance.
Table 1.
Taxon | Population | Distribution | Florescence |
---|---|---|---|
Chrysanthemum glabriusculum (W. W. Smith) Handel–Mazzetti | Cg | N 25.695° E 100.108° | Late Oct.–Late Dec. |
Cg–N | N 25.727° E 100.094° | Mid Oct.–Early Dec. | |
Chrysanthemum indicum Linnaeus | Ci | N 25.974° E 100.360° | Early Nov.–Mid Dec. |
Chrysanthemum lavandulifolium var. tomentellum (Handel–Mazzetti) | Cl | N 25.556° E 100.435° | Early Nov.–Late Nov. |
Ling et Shih | Cl–N | N 25.567° E 100.430° | Early Nov.–Late Nov |
Ajania sericea Shih | As | N 26.095° E 100.118° | Early Oct.–Mid Nov. |
As–N | N 26.184° E 100.054° | Early Oct.–Mid Nov. | |
Phaeostigma quercifolium (W. W. Smith) Muldashev. | Pq | N 25.853° E 100.045° | Late Sep.–Mid Nov. |
Pq–N | N 26.503° E 100.001° | Late Sep.–Early Nov. |
Diversity and principal component analysis of morphological characteristic data
Although the altitude and topography were similar, the 9 populations showed high morphological diversity based on the 44 qualitative traits (Table S5). The qualitative traits with high diversity mainly focused on the shapes and divisions of leaves, the presence of trichomes on stems and leaves, colors of the scarious margins of phyllaries, ray florets, and marginal female tubular florets. The diversity index of upper stem leaf shapes was the highest (H′ = 1.58) (Fig. S4, Table S5). Subsequently, we found that there were sessile glands (Fig. 2c, Fig. S1) on the corollas57,58 of all five species (H′ = 0.00); in particular, this trait was reported for the first time for A. sericea, Chrysanthemum glabriusculum, and Chrysanthemum lavandulifolium var. tomentellum. Notably, A. sericea exhibited morphological characteristics that suggested that it has very high drought tolerance in comparison to other species. These characteristics included densely packed trichomes all over the plant, completely subdivided leaves, and narrowly elliptical ultimate segments.
Phaeostigma quercifolium was significantly different from other species, exhibiting qualitative traits that were different from those noted in previous studies, such as a subshrub posture, the presence of cicatricles, lateral expansion of the petiole base, yellow-white tubular florets, an absence of rhizomes, and annular lobules at the petiole (Table S5). However, brownish style branches were found in both P. quercifolium (Fig. S1a) and A. sericea in this study (Fig. 2c), which was a key trait that separated Phaeostigma from Ajania according to Muldashev12.
Ray florets of the Cg–N population showed a high diversity of lengths and a range of characteristics. For example, plants that grew on open stony slopes had shorter ray florets and an obvious tri-denticulate apex, which were similar to the Cg population that grew in dense shrubs (Fig. 2d (2–5)). We compared the morphology between the marginal female florets (A. sericea, As population) (Fig. 2e (1)) and the ray florets (C. glabriusculum, Cg–N population) (Fig. 2e (2–5)), and obvious transition states in the morphology were observed (Fig. 2e (1–5)). Notably, the half-tubular female florets (Fig. 2e (2)) indicated that the ray florets of Chrysanthemum might have originated from the splitting and elongation of the marginal female tubular florets that came from Ajania, which was an important piece of evidence for determination of the evolutionary relationship between Ajania and Chrysanthemum.
There were no significant differences in most quantitative traits between the two different populations of the same species (P < 0.05). The main significant differences came from the PH. However, the RFL of the Cg-N population was significantly higher than that of Cg population (P = 0.014, Table S6), which again supported the differences seen in the qualitative traits.
PCA with 12 quantitative traits from 9 populations generated 3 clusters, namely, the Chrysanthemum cluster, the Ajania cluster and the Phaeostigma cluster (Fig. 3a). For the first principal component, almost all quantitative traits were positively correlated except FTL. We suggest that plant type and organ size constitute the factors for PC1. Since the second principal component was positively correlated with CD, CCD, and LFL, we suggest inflorescence as the significant factor for PC2. Chrysanthemum populations had more significant inflorescences than the other two genera according to the scatter from PC2, and P. quercifolium had larger plant types than PC1. A. sericea was significantly smaller than other species.
Genetic diversity and cluster analysis
From the 24 appropriate SRAP primer combinations, a total of 276 reliable bands were scored, of which 269 (97.46%) were polymorphic (Table S2, Fig. S5). The genetic similarity coefficient among the five genotypes ranged from 0.38 to 0.70, with an average of 0.55 (Fig. 4). The largest genetic distance was recorded between P. quercifolia and C. l. var. tomentellum; the lowest was between C. glabriusculum and C. indicum. The dendrogram of genetic relationships among genotypes revealed by the UPGMA method is presented in Fig. 4, and three main clusters were generated in this tree. P. quercifolia and A. sericea formed a separate cluster, and three species of Chrysanthemum clustered into another group. The genetic relationship between Phaeostigma and Chrysanthemum was relatively distant, and Ajania was between them. This result is similar to the PCA result (Fig. 3a) based on morphology. Therefore, there was homogeneity between morphological diversity and genetic diversity.
Topographic analysis based on GIS
Our results show that there were no Chrysanthemum species or their allies distributed in the valleys and basins that are found in low-altitude regions (Fig. 5a); the 9 populations were all in the mountains, with the highest peak at over 3000 m.a.s.l. Most of the populations were located on the southern, southeastern and southwestern aspects except for Cg-N, which was on the northern aspect, with less light (Fig. 5b). In contrast, two populations of As were on the southern aspect (aspect values: 183.52, 193.06), with the longest light time (Fig. 5b, Table S4). In addition, Cg and Cg–N were very close to each other, with similar elevations and topographies, and the only difference was that Cg was on the eastern aspect (67.75), with more direct light and relatively drier habitats. We hence argue that Chrysanthemum and its allies were most likely heliophilous, especially Ajania, and the northern aspect with lower light intensity and relatively humid habitats may be the key factor driving the elongation and evolution of marginal female florets. The slopes of habitats for all populations were more than 15°, and most of them were more than 30° (Fig. 5c, Table S4). However, in the actual survey, the microtopography of each sampling area was relatively complex, and protruding large rocks and cliffs were often present, which made the slope value larger. Through the topographic position index analysis, we found that all populations lived at high topographic positions in the mountains (index ≥ 2) (Table S4), and most were on the tops of the mountains (Fig. 5d).
The small-scale topographic features of the nine populations displayed two modes based on the cross section (Fig. S2). One mode was located on the middle and upper regions of a high mountain (the altitude of the mountain was greater than 4000 m.a.s.l.), such as those of Cg and Cg–N. Others were located on top of a large mountain area. The similar altitude and small-scale topographic features indicated that the three genera had close relationships and similar developmental histories. However, under the same mode, different slopes and aspects make the microclimate and vegetation community of each plot different, which provides the right conditions for the evolution of more diversity among Chrysanthemum and its allies in this study area.
Correlation analysis based on plot data
There was at least one plot where AB was zero in the Cl, Cl–N, and Aq–N populations (Table S3), which indicated that the distribution range of these three populations was very narrow, as the maximum separation distance was 50 m. We found that the R was low, whereas the TLC was high and the SRC was low, in all plots. As mentioned above, Cg–N was a special population that was located on the northern slope with less light. However, the SRCs of the three plots were high, with values above 20%, and the highest value was 37%. This topography resulted in very low TLC, and the average TLC of the three plots was less than 3%, which reduced the shading of the shrub layer and herb layer from the perspective of the plant community and made up for the lack of light. In all six plots of A. sericea, the TLC was low, whereas the SLC, HLC, and SRC were high, and the average SRC was more than 20%. These stony southern slopes formed a relatively dry microclimate with a small area that provided the specific habitat and vegetation community, which is optimal for A. sericea. The composition of the tree layer displayed a certain consistency, often in the form of coniferous-evergreen, broad-leaved, mixed forest trees, mainly including Pinus yunnanensis, Pinus armandii, Quercus aquifolioides, Quercus rehderiana, and Quercus spinosa.
The AB of Chrysanthemum and its allies had significant positive correlations with SRC (R = 0.59, α = 0.05) and HLC (R = 0.67, α = 0.05) and was negatively related to TLC (R = −0.51, α = 0.05) and TS (R = −0.34, α = 0.05) (Fig. 3b). These findings indicated that all target species in this area were mainly distributed in open stony coniferous–broad-leaved, mixed forest margins, and they hardly grew in the dense woods. These marginal communities were similar to ecological islands, separated by other dense vegetation communities and scattered in small-scale areas formed by special stony topography.
Discussion
Factors affecting the particularity of distribution
The genus Chrysanthemum is generally distributed in the middle-low altitude and middle-low-latitude humid areas of the subtropical and temperate zones of Asia, and a few grow in the high-latitude frigid zones of Russia (Far East) and North America. For C. indicum, the distribution area is relatively wide, but there are few high-altitude populations25. Ajania is usually distributed in mid-latitude arid and semiarid areas, and the altitude is higher than that of Chrysanthemum, with the highest altitude being 5300 m.a.s.l. (A. khartensis). Ci was the highest population of Chrysanthemum indicum (3210 m.a.s.l.) reported in China, with an altitude higher than that of Ajania in this area. This may be mainly due to the relatively warm climate of the low latitudes. In addition, this area is located in the southernmost margin of the Hengduan Mountain Range, which blocks the cold current from the north. The warm and wet current from the south59 easily forms rain and fog at the top of the mountains, which makes the small area relatively warm and humid even in the high-altitude areas above 3000 m.a.s.l., allowing C. indicum to survive. In addition, these particular stony small areas with long light hours and a relatively dry microclimate allowed Ajania to exist in the low-latitude area with 1000 mm annual average precipitation. However, the differences in light hours caused by aspect and vegetation community led to the discrepant florescence of Chrysanthemum in this area. Even for the same species, the florescence of the Cg–N population on the northern aspect occurred earlier than that of the Cg population on the eastern aspect (Table 1).
However, there are many similar stony topographies with relatively low altitudes in this area, so why is there no distribution of Chrysanthemum and its allies? We found that their preferred habitats were highly dependent on the specialized vegetation community: alpine coniferous–broad-leaved mixed forest marginal communities, in which the conifers were mainly from Pinus, whereas the broad-leaved communities were usually alpine evergreen sclerophyllous Quercus and Rhododendron. We highlight that the development of these communities60 is of great significance to the distribution and evolution of Chrysanthemum and its allies, and this region has become an ecological island61 of refuge28,62 for these species in the current interglacial period.
Migration path and divergence time estimation based on paleopalynology, paleobotany, and paleogeography
Based on the data and paleopalynological, paleobotanical, and paleogeographical63 evidence, we reconstructed the ancient topography and vegetation64, ensuring that the estimations of the origin, divergence time65,66, and migration path of these species are as accurate as possible. This study area is the original location of “Tali Glaciation”67–69. A large amount of relevant research data provides strong support for exploring the change in climate and evolutionary history of vegetation in this area. According to the current altitude data, the mountains around Erhai Lake were divided into two types: those with an altitude of more than 3900 m.a.s.l. and those with an altitude of more than 3000 m.a.s.l. but less than 3300 m.a.s.l. We then reconstructed the paleoelevation and paleovegetation of the Upper Eocene (~36 Ma BP)50,51,70,71 and the last Quaternary glaciation (~70–10 Ka BP)46,72,73 for these two types of mountains (Fig. 6).
The ancestral range of Anthemideae Cass. was most likely in Central and South Africa during the Upper Eocene74, approximately 37–36 Ma BP. This study area had a paleoelevation of 1.3–2.6 km above sea level, which would most likely have been associated with a vegetation cover consisting of tropical-subtropical, deciduous, coniferous, broadleaf forests that were mainly composed of Carya, Juglans, Castanea, Alnus, Polypodium, Pinus, Quercus, and Abies (Fig. 6). The reconstructed mean annual air temperature (MAAT) had a value of 16.8–21.7 °C, warmer than the present-day MAAT (~6 °C). However, there was an ancient subtribe, Artemisiinae (Anthemideae), in Jianchuan based on Artemisiaepollenites (Artemisia-type pollen)51. Therefore, we speculated that the ancient Artemisiinae with Artemisia-type pollen was a relatively primitive vernacular Anthemideae group in this region and was the common ancestor of Artemisia, Phaeostigma, Chrysanthemum, and Ajania.
By the last Quaternary glaciation (~70–10 ka BP), the Qinghai–Tibetan Plateau and Hengduan Mountains had been uplifted, and the landform of this area was basically the same as it is now. Affected by glaciation, the climate had become cold and dry, the area above 3900 m.a.s.l. was covered by glaciers all year round, and the lake level had reduced. The climate in the low-altitude basin area was relatively warm and became that of a temperate coniferous–broad-leaved mixed forest dominated by Pinus Cyclobalanopsis, Tsuga, and Quercus46 (Fig. 6), which was similar to the community that Chrysanthemum and its allies is dependent on today. Despite the lack of pollen fossils in this stratum, we inferred that Chrysanthemum and Ajania or their common ancestor already existed in this area based on their present communities. However, the populations were not large, scattered in the open or located in the margins of forests, but they started lateral radiation and migration in the low-altitude and middle-altitude (1900–2500 m.a.s.l.) areas (Fig. 6). In the Holocene (interglacial stage), the climate had become humid and warm, with dense vegetation in low-altitude and medium-altitude areas, forming the current evergreen broad-leaved coniferous mixed forests mainly composed of Pinus, Alnus, and Castanopsis. Owing to competition between populations, the habitat of Chrysanthemum and its allies has become compressed, and the populations have been forced to migrate to high-altitude areas with the coniferous–broad-leaved mixed forest marginal community, thus forming the high-altitude scattered distribution pattern seen at present. The Quaternary has experienced several glacial-interglacial cycles75, but we could not reconstruct the vegetation of the whole Quaternary owing to the lack of data. However, notably, the geodiversity caused by the uplift of the Hengduan Mountains created a small-scale76 alpine topography with diverse microclimates, which provided a refuge for Chrysanthemum and its allies during the interglacial stage and drove the divergence and diversification of their populations. The pollen fossils of Chrysanthemum and Ajania have been found only in the strata of the late Quaternary (~20 Ka Bp) to date. Hence, we estimated that the divergence of the two genera occurred along with the uplift of the Hengduan Mountains and Quaternary glacial-interglacial cycles, from approximately the late Miocene to the late Pleistocene (8–0.1 Ma).
Evolutionary relationships among Chrysanthemum, Ajania, and Phaeostigma
Based on the brownish style branches, erect corolla lobes, and microechinate pollen, Muldeshev12,13 separated Phaeostigma from Ajania. However, there were also brownish style branches in A. sericea, whereas the browning degree was relatively lower than that in P. quercifolium. Two different pollen exine ornamentations have been confirmed for the tribe Anthemideae, namely, the Anthemis-type (echinate, with medium to long spines) and the Artemisia-type (microechinate, with short spinules)77,78. The former was more likely to be related to entomophily, while the latter was more likely to be related to anemophily78,79. Chrysanthemum and most Ajania species Anthemis-type species, while Phaeostigma species were Artemisia-type species15,17,78, and there was no relevant research on A. sericea. In our study, although pollen morphology was not involved, P. quercifolium was more likely related to anemophily, and the other four species, including A. sericea, were more likely related to entomophily based on the pollinators recorded through our long-term field work (Fig. S3), which strongly supported the previous research hypothesis that Phaeostigma and Ajania were split, based on ecological evidence. In addition, our results on the morphological characteristics also supported this hypothesis, with differences in the qualitative traits of P. quercifolium from those reported in previous studies, such as a subshrub structure, the presence of small scars on the stem, lateral expansion of the petiole base, yellow-white tubular florets, erect corolla lobes, the absence of emergent rhizomes, and annular lobules at the petiole. Last, our cluster analysis based on SRAP markers provided genetic evidence for this hypothesis: the genetic relationship between Phaeostigma and Chrysanthemum was relatively distant, and the former formed an independent cluster that was separate from Chrysanthemum and Ajania (Fig. 4).
For Chrysanthemum and Ajania, despite the observation that the populations of Ajania were separated from those of Chrysanthemum, based on our PCA results, we suggest that the two genera were very closely related based on the obvious smooth transition between states for marginal female florets between Chrysanthemum (ray florets) and Ajania (tubular florets) discovered in the Cg–N population (C. glabriusculum) and the fact that they use the same entomophily pollination system. This assumption is also supported by previous molecular biology results15,17, and our dendrogram showed that the genetic distance between Chrysanthemum and Ajania was closer than that between Chrysanthemum and Phaeostigma (Fig. 4).
However, there is a key problem: what were the ancestral characteristics of the marginal female florets, the tubular florets, or ray florets? Previous studies have shown that Artemisia groups (tubular florets) were considered to have evolved secondarily by loss of ray florets19,78,80. However, the discovery of a number of fossil pollen (with short spinules) grains preserved in dinosaur-bearing deposits from the Late Cretaceous (~76–66 Ma) in Antarctica drastically pushes back the timing of assumed origin of Asteraceae65. Therefore, at the family and angiosperm levels, we speculate that the groups that were likely related to anemophily with short spinule pollens were the more ancient and primitive ancestors. Hence, tubular florets corresponding to anemophily may be the ancestral characteristics of marginal female florets. The results of our PCA and qualitative trait analysis indicated that Chrysanthemum had a more significant inflorescence to attract pollinators; in contrast, P. quercifolium was unattractive, with erect whitish corollas, and A. sericea was in the middle of the two. P. quercifolium may be a relic species of Artemisiinae that benefited from the diverse topographies and climate of the Hengduan Mountains, which was a refuge for this species, as it survived through several global climate changes in the Late Tertiary and Quaternary.
Owing to the limitations of species samples, in this study, we were unable to perform a comprehensive analysis of the evolution of the three genera. However, we highlight that Chrysanthemum and its related genera were highly dependent on small-scale special stony topographies and specialized communities in the study area and that the northern aspect (16.28), with less light, may be the key factor for the elongation and evolution of marginal female florets. The uplift of the Hengduan Mountains played a key role in the evolution, divergence, and survival of Chrysanthemum and its allies.
Supplementary information
Acknowledgements
This work was funded by the National Key Research and Development Program of China (2019YFD1001501), the National Natural Science Foundation of China (31730081, 31870306), the Youth Program of Science and Technology Department of Yunnan Province (2016FD070), and a project funded by the Priority Academic Program Development of Jiangsu Higher Education Institution.
Author contributions
X.C. planned and designed the research; conducted the fieldwork, sampling and data collection; carried out analyses; performed the experiments; and wrote the initial draft. G.R., Z.W., and X.D. participated in the data analyses. X.Y. performed the experiments. H.W., J.J., and F.C. revised the manuscript. F.C. planned the research.
Conflict of interest
The authors declare that they have no conflict of interest.
Supplementary information
Supplementary Information accompanies this paper at (10.1038/s41438-020-00407-9).
References
- 1.Hirakawa H, et al. De novo whole-genome assembly in Chrysanthemum seticuspe, a model species of Chrysanthemums, and its application to genetic and gene discovery analysis. DNA Res. 2019;26:195–203. doi: 10.1093/dnares/dsy048. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 2.Stevenson T. Chrysanthemums. Nature. 1912;90:248. [Google Scholar]
- 3.Ministry of Agriculture and Fisheries UK. Control of the Chrysanthemum midge. Nature144, 280 (1939).
- 4.Cockshull KE, Hughes AP. Distribution of dry matter to flowers in Chrysanthemum morifolium. Nature. 1976;215:780–781. doi: 10.1038/215780a0. [DOI] [Google Scholar]
- 5.Courtney-Gutterson N, et al. Modification of flower color in florist’s Chrysanthemum: production of a white–flowering variety through molecular genetics. Nat. Biotechnol. 1994;12:268–271. doi: 10.1038/nbt0394-268. [DOI] [PubMed] [Google Scholar]
- 6.Gamalero E. Effects of Pseudomonas putida S1Pf1Rif against Chrysanthemum yellows phytoplasma infection. Phytopathology. 2010;100:805–813. doi: 10.1094/PHYTO-100-8-0805. [DOI] [PubMed] [Google Scholar]
- 7.Wei Q, et al. Control of chrysanthemum flowering through integration with an aging pathway. Nat. Commun. 2017;8:829. doi: 10.1038/s41467-017-00812-0. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 8.Yang L, Wen X, Fu J, Dai S. ClCRY2 facilitates floral transition in Chrysanthemum lavandulifolium by affecting the transcription of circadian clock-related genes under short-day photoperiods. Hortic. Res. 2018;5:58. doi: 10.1038/s41438-018-0063-9. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 9.Su J, et al. Current achievements and future prospects in the genetic breeding of chrysanthemum: a review. Hortic. Res. 2019;6:109. doi: 10.1038/s41438-019-0193-8. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 10.Kubitzki, K. The families and genera of vascular plants, Vol. VIII Flowering Plants・Eudicots (eds Kadereit, J. W. & Jeffrey, C.) Compositae (eds. Anderberg, A. A. et al.) (Springer-Verlag Berlin Heidelberg, 2007).
- 11.Poljakov PP. Duo genere novae fam. Compositae. Not. Syst. Herb. Inst. Bot. Akad. Sci. URSS. 1955;17:418–431. [Google Scholar]
- 12.Muldashev AA. A new genus Phaeostigma (Asteraceae) from the East Asia. Botanischeskii Zh . 1981;66:584–588. [Google Scholar]
- 13.Muldashev AA. A critical review of the genus Ajania (Asteraceae-Anthemideae) Botanischeskii Zh . 1983;68:207–214. [Google Scholar]
- 14.Bremer K, Humphries CJ. The generic monograph of the Asteraceae-Anthemideae. Bull. Nat. Hist. Mus. Lond. 1993;23:71–177. [Google Scholar]
- 15.Huang Y, An YM, Meng SY, Guo YP, Rao GY. Taxonomic status and phylogenetic position of Phaeostigma in the subtribe Artemisiinae (Asteraceae) J. Syst. Evol. 2017;55:426–436. doi: 10.1111/jse.12257. [DOI] [Google Scholar]
- 16.Zhao HB, Chen FD, Chen SM, Wu GS, Guo WM. Molecular phylogeny of Chrysanthemum, Ajania and its allies (Anthemideae, Asteraceae) as inferred from nuclear ribosomal ITS and chloroplast trnL-F IGS sequences. Plant Syst. Evol. 2010;284:153–169. doi: 10.1007/s00606-009-0242-0. [DOI] [Google Scholar]
- 17.Liu PL, Wan Q, Guo YP, Yang J, Rao GY. Phylogeny of the Genus Chrysanthemum L.: evidence from single-copy nuclear gene and chloroplast DNA sequences. PLoS ONE. 2012;7:e48970. doi: 10.1371/journal.pone.0048970. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 18.Ohashi H, Yonekura K. New combinations in Chrysanthemum (Compositae-Anthemideae) of Asia with a list of Japanese Specie. J. Jpn. Bot. 2004;79:186–195. [Google Scholar]
- 19.Sanz M, et al. Molecular phylogeny and evolution of floral characters of Artemisia and allies (Anthemideae, Asteraceae): evidence from nrDNA ETS and ITS sequences. Taxon. 2008;57:1–13. [Google Scholar]
- 20.An, Y. M. Studies on the Phylogeny and Biogeography of the Genus Ajania and Its Allies. Master’s thesis. Peking University (2012).
- 21.Barreda VD, et al. Eocene Patagonia fossils of the daisy family. Science. 2010;329:1621–1621. doi: 10.1126/science.1193108. [DOI] [PubMed] [Google Scholar]
- 22.Wefferling KM, Hoot SB. Dated phylogeography of western North American subalpine marshmarigolds (Caltha spp. Ranunculaceae): Miocene-Pliocene divergence of hexaploids, multiple origins of allododecaploids during the Pleistocene, and repeated recolonization of Last Glacial Maxim. J. Biogeogr. 2018;45:1077–1089. doi: 10.1111/jbi.13204. [DOI] [Google Scholar]
- 23.Wiens JJ. Speciation and ecology revisited: phylogenetic niche conservatism and the origin of species. Evolution. 2004;58:193–197. doi: 10.1111/j.0014-3820.2004.tb01586.x. [DOI] [PubMed] [Google Scholar]
- 24.Ricklefs RE. Evolutionary diversification and the origin of the diversity-environment relationship. Ecology. 2006;87:S3–S13. doi: 10.1890/0012-9658(2006)87[3:EDATOO]2.0.CO;2. [DOI] [PubMed] [Google Scholar]
- 25.Li J, Wan Q, Guo YP, Abbott RJ, Rao GY. Should I stay or should I go: biogeographic and evolutionary history of a polyploid complex (Chrysanthemum indicum complex) in response to Pleistocene climate change in China. N. Phytol. 2014;201:1031–1044. doi: 10.1111/nph.12585. [DOI] [PubMed] [Google Scholar]
- 26.Rahbek C, et al. Humboldt’s enigma: What causes global patterns of mountain biodiversity? Science. 2019;365:1108–1113. doi: 10.1126/science.aax0149. [DOI] [PubMed] [Google Scholar]
- 27.Rahbek C, et al. Building mountain biodiversity: Geological and evolutionary processes. Science. 2019;365:1114–1119. doi: 10.1126/science.aax0151. [DOI] [PubMed] [Google Scholar]
- 28.Cosacov A, Sérsic AN, Sosa V, Johnson LA, Cocucci AA. Multiple periglacial refugia in the Patagonian steppe and post-glacial colonization of the Andes: the phylogeography of Calceolaria polyrhiza. J. Biogeogr. 2010;37:1463–1477. [Google Scholar]
- 29.García-Aloy S, et al. North-west Africa as a source and refuge area of plant biodiversity: a case study on Campanula kremeri and Campanula occidentalis. J. Biogeogr. 2017;44:2057–2068. doi: 10.1111/jbi.12997. [DOI] [Google Scholar]
- 30.Pérez-Escobar OA, et al. Recent origin and rapid speciation of Neotropical orchids in the world’s richest plant biodiversity hotspot. N. Phytol. 2017;215:891–905. doi: 10.1111/nph.14629. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 31.Zhao YP, et al. Resequencing 545 ginkgo genomes across the world reveals the evolutionary history of the living fossil. Nat. Commun. 2019;10:4201. doi: 10.1038/s41467-019-12133-5. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 32.Xing Y, Ree RH. Uplift-driven diversification in the Hengduan mountains, a temperate biodiversity hotspot. Proc. Natl Acad. Sci. USA. 2017;114:E3444. doi: 10.1073/pnas.1616063114. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 33.Sun H. 2002. Evolution of arctic-tertiary flora in Himalayan-Hengduan mountains. Acta Bot. Yunnanica. 2002;24:671–688. [Google Scholar]
- 34.Sun H, Li ZM. Qinghai-Tibet Plateau uplift and its impact on Tethys flora. Adv. Earth. Sci. 2003;18:852–862. [Google Scholar]
- 35.Zhang DC, Zhang YH, Boufford DE, Sun H. Elevational patterns of species richness and endemism for some important taxa in the Hengduan mountains, southwestern China. Biodivers. Conserv. 2009;18:699–716. doi: 10.1007/s10531-008-9534-x. [DOI] [Google Scholar]
- 36.Royer DL, McElwain JC, Adams JM, Wilf P. Sensitivity of leaf size and shape to climate within Acer rubrum and Quercus kelloggii. N. Phytol. 2008;179:808–817. doi: 10.1111/j.1469-8137.2008.02496.x. [DOI] [PubMed] [Google Scholar]
- 37.Opedal ØH, Armbruster WS, Graae BJ. Linking small-scale topography with microclimate, plant species diversity and intra-specific trait variation in an alpine landscape. Plant Ecol. Divers. 2015;8:305–315. doi: 10.1080/17550874.2014.987330. [DOI] [Google Scholar]
- 38.Tölgyesi C. Tree-herb co-existence and community assembly in natural forest-steppe transitions. Plant Ecol. Divers. 2018;11:465–477. doi: 10.1080/17550874.2018.1544674. [DOI] [Google Scholar]
- 39.Rumpf SB. Range dynamics of mountain plants decrease with elevation. Proc. Natl Acad. Sci. USA. 2018;115:1848–1853. doi: 10.1073/pnas.1713936115. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 40.Camarero JJ, Gutiérrez E, Fortin MJ. Spatial patterns of plant richness across treeline ecotones in the Pyrenees reveal different locations for richness and tree cover boundaries. Glob. Ecol. Biogeogr. 2006;15:182–191. doi: 10.1111/j.1466-822X.2006.00211.x. [DOI] [Google Scholar]
- 41.Liang E, et al. Species interactions slow warming-induced upward shifts of treelines on the Tibetan Plateau. Proc. Natl Acad. Sci. USA. 2016;113:4380–4385. doi: 10.1073/pnas.1520582113. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 42.Li P, et al. Genetic diversity, population structure and association analysis in cut chrysanthemum (Chrysanthemum morifolium Ramat.) Mol. Genet. Genomics. 2016;291:1117–1125. doi: 10.1007/s00438-016-1166-3. [DOI] [PubMed] [Google Scholar]
- 43.Murray MG, Thompson WF. Rapid isolation of high molecular weight plant DNA. Nucleic Acids Res. 1980;8:4321–4325. doi: 10.1093/nar/8.19.4321. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 44.Zhang F, et al. SRAP-based mapping and QTL detection for inflorescence-related traits in chrysanthemum (Dendranthema morifolium) Mol. Breed. 2011;27:11–23. doi: 10.1007/s11032-010-9409-1. [DOI] [Google Scholar]
- 45.Li G, Quiros C. Sequence-related amplified polymorphism (SRAP), a new marker system based on a simple PCR reaction: its application to mapping and gene tagging in Brassica. Theor. Appl. Genet. 2001;103:455–461. doi: 10.1007/s001220100570. [DOI] [Google Scholar]
- 46.Shen J, et al. Lake sediment records on climate change and human activities since the Holocene in Erhai catchment, Yunnan Province, China. Sci. China Ser. D. Earth Sci. 2005;48:353–363. doi: 10.1360/03yd0118. [DOI] [Google Scholar]
- 47.Hoorn C, et al. Eocene palynological record of climate change and Tibetan Plateau uplift (Xining Basin, China) Palaeogeogr. Palaeoclimatol. Palaeoecol. 2012;344–345:16–38. doi: 10.1016/j.palaeo.2012.05.011. [DOI] [Google Scholar]
- 48.Cao X, Ni J, Herzschuh U, Wang Y, Zhao Y. A late Quaternary pollen dataset from eastern continental Asia for vegetation and climate reconstructions: Set up and evaluation. Rev. Palaeobot. Palyno. 2013;194:21–37. doi: 10.1016/j.revpalbo.2013.02.003. [DOI] [Google Scholar]
- 49.Li S, et al. Magnetostratigraphy of the Dali Basin in Yunnan and implications for late Neogene rotation of the southeast margin of the Tibetan Plateau. J. Geophys. Res-Sol. Ea. 2013;118:791–807. doi: 10.1002/jgrb.50129. [DOI] [Google Scholar]
- 50.Gourbet L, et al. Reappraisal of the Jianchuan Cenozoic basin stratigraphy and its implications on the SE Tibetan plateau evolution. Tectonophysics. 2017;700–701:162–179. doi: 10.1016/j.tecto.2017.02.007. [DOI] [Google Scholar]
- 51.Wu J, et al. Paleoelevations in the Jianchuan Basin of the southeastern Tibetan Plateau based on stable isotope and pollen grain analyses. Palaeogeogr. Palaeoclimatol. Palaeoecol. 2018;510:93–108. doi: 10.1016/j.palaeo.2018.03.030. [DOI] [Google Scholar]
- 52.Li Q, Wu H, Yu Y, Sun A, Luo Y. Large-scale vegetation history in China and its response to climate change since the Last Glacial Maximum. Quat. Int. 2019;500:108–119. doi: 10.1016/j.quaint.2018.11.016. [DOI] [Google Scholar]
- 53.Mutanga O, et al. Explaining grass-nutrient patterns in a savanna rangeland of southern Africa. J. Biogeogr. 2004;31:819–829. doi: 10.1111/j.1365-2699.2004.01072.x. [DOI] [Google Scholar]
- 54.Rowe RJ. Elevational gradient analyses and the use of historical museum specimens:a cautionary tale. J. Biogeogr. 2005;32:1883–1897. doi: 10.1111/j.1365-2699.2005.01346.x. [DOI] [Google Scholar]
- 55.Barbo DN, Chappelka AH, Somers GL, Miller-Goodman MS, Stolte K. Diversity of an early successional plant community as influenced by ozone. N. Phytol. 1998;138:653–662. doi: 10.1046/j.1469-8137.1998.00138.x. [DOI] [Google Scholar]
- 56.Liang J, et al. Positive biodiversity-productivity relationship predominant in global forests. Science. 2016;354:aaf8957. doi: 10.1126/science.aaf8957. [DOI] [PubMed] [Google Scholar]
- 57.Vermeer J, Peterson RL. Glandular trichomes on the inflorescence of Chrysanthemum morifolium cv. Dramatic (Compositae). II. Ultrastruct. Histochem. Can. J. Bot. 1979;57:705–713. [Google Scholar]
- 58.Ren JB, Guo YP. Behind the diversity: Ontogenies of radiate, disciform, and discoid capitula of Chrysanthemum and its allies. J. Syst. Evol. 2015;53:520–528. doi: 10.1111/jse.12154. [DOI] [Google Scholar]
- 59.Li J, Guo Y, Romane F. Environmental heterogeneity and population variability of Sclerophyllous Oaks (Quercus Sec. suber) in East Himalayan region. Forestry Stud. China. 2000;2:1–15. [Google Scholar]
- 60.Wright AJ, et al. Plants are less negatively affected by flooding when growing in species-rich plant communities. N. Phytol. 2017;213:645–656. doi: 10.1111/nph.14185. [DOI] [PubMed] [Google Scholar]
- 61.Hughes CE, Atchison GW. The ubiquity of alpine plant radiations: from the Andes to the Hengduan mountains. N. Phytol. 2015;207:275–282. doi: 10.1111/nph.13230. [DOI] [PubMed] [Google Scholar]
- 62.Pfister CA, Hay ME. Associational plant refuges: convergent patterns in marine and terrestrial communities result from differing mechanisms. Oecologia. 1988;77:I18–I129. doi: 10.1007/BF00380934. [DOI] [PubMed] [Google Scholar]
- 63.Zhang YC, Shi GR, Shen SZ. A review of Permian stratigraphy, palaeobiogeography and palaeogeography of the Qinghai–Tibet plateau. Gondwana Res. 2013;24:55–76. doi: 10.1016/j.gr.2012.06.010. [DOI] [Google Scholar]
- 64.Zhou X, et al. Vegetation change and evolutionary response of large mammal fauna during the mid-Pleistocene transition in temperate northern East Asia. Palaeogeogr. Palaeoclimatol. Palaeoecol. 2018;505:287–294. doi: 10.1016/j.palaeo.2018.06.007. [DOI] [Google Scholar]
- 65.Barreda VD, et al. Early evolution of the angiosperm clade Asteraceae in the Cretaceous of Antarctica. Proc. Natl Acad. Sci. USA. 2105;112:10989–10994. doi: 10.1073/pnas.1423653112. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 66.Huang, C. H. et al. Multiple polyploidization events across asteraceae with two nested events in the early history revealed by nuclear phylogenomics. Mol. Biol. Evol. 33, 2820–2835 (2016). [DOI] [PMC free article] [PubMed]
- 67.Credner, W. Geography Investigation Report in 1931. In: Report Collecton of Department of Geography, Vol. 1, 1–35 (National Sun Yat-sen University, 1931).
- 68.Credner W. Observation on geology and morphology of Yunnan. Geol. Surv. Kwangtung Kwangshi, Spec. Publ. 1932;No. X:51. [Google Scholar]
- 69.Yang JQ, Cui ZJ, Yi CL, Sun JM, Yang LR. “Tali Glaciation” on Massif Diancang. Sci. China Ser. D. 2007;50:1685–1692. doi: 10.1007/s11430-007-0114-9. [DOI] [Google Scholar]
- 70.Hoke GD, Zeng JL, Hren MT, Wissink GK, Garzione CN. Stable isotopes reveal high southeast Tibetan Plateau margin since the Paleogene. Earth Planet. Sc. Lett. 2014;394:270–278. doi: 10.1016/j.epsl.2014.03.007. [DOI] [Google Scholar]
- 71.Li S, Currie BS, Rowley DB, Ingalls M. Cenozoic paleoaltimetry of the SE margin of the Tibetan Plateau: constraints on the tectonic evolution of the region. Earth Planet. Sc. Lett. 2015;432:415–424. doi: 10.1016/j.epsl.2015.09.044. [DOI] [Google Scholar]
- 72.Kuang M, et al. Study on the Palaeovegation and Palaeoclimate Since Late Pleistocene in the Dianchang Mountain Area in Dali of YunNan Province. J. Southwest China Norm. Univ. 2002;27:759–765. [Google Scholar]
- 73.Xiao X, et al. Latest Pleistocene and Holocene vegetation and climate history inferred from an alpine lacustrine record, northwestern Yunnan Province, southwestern China. Quat. Sci. Rev. 2014;86:35–48. doi: 10.1016/j.quascirev.2013.12.023. [DOI] [Google Scholar]
- 74.Mandela JR, et al. A fully resolved backbone phylogeny reveals numerous dispersals and explosive diversifications throughout the history of Asteraceae. Proc. Natl Acad. Sci. USA. 2019;116:14083–14088. doi: 10.1073/pnas.1903871116. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 75.Sheldon ND. Quaternary glacial-interglacial climate cycles in Hawaii. J. Geol. 2006;114:367–376. doi: 10.1086/500993. [DOI] [Google Scholar]
- 76.Milbau A, Shevtsova A, Osler N, Mooshammer M, Graae BJ. Plant community type and small-scale disturbances, but not altitude, influence the invasibility in subarctic ecosystems. N. Phytol. 2013;197:1002–1011. doi: 10.1111/nph.12054. [DOI] [PubMed] [Google Scholar]
- 77.Wang WM. On the origin and development of Artemisia (Asteraceae) in the geological past. Bot. J. Linn. Soc. 2004;145:331–336. doi: 10.1111/j.1095-8339.2004.00287.x. [DOI] [Google Scholar]
- 78.Pellicer J, et al. Palynological study of Ajania and related genera (Asteraceae, Anthemideae) Bot. J. Linn. Soc. 2009;161:171–189. doi: 10.1111/j.1095-8339.2009.00998.x. [DOI] [Google Scholar]
- 79.Friedman J, Barrett SCH. Wind of change: new insights on the ecology and evolution of pollination and mating in wind-pollinated plants. Ann. Bot.-Lond. 2009;103:1515–1527. doi: 10.1093/aob/mcp035. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 80.Watson LE, Bates PL, Evans TM, Unwin MM, Estes RJ. Molecular phylogeny of Subtribe Artemisiinae (Asteraceae), including Artemisia and its allied and segregate genera. BMC Evol. Biol. 2002;2:17–28. doi: 10.1186/1471-2148-2-17. [DOI] [PMC free article] [PubMed] [Google Scholar]
Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.