| Literature DB >> 30327504 |
Hongyi Yang1, Xingyu Zhao1, Changli Liu1, Long Bai1, Min Zhao2, Lili Li3.
Abstract
This study investigated ericoid mycorrhizal fungi (EMF) diversity inEntities:
Mesh:
Substances:
Year: 2018 PMID: 30327504 PMCID: PMC6191440 DOI: 10.1038/s41598-018-33634-1
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Roots of V. uliginosum colonized with fungal endophytes. (A) Micrograph of the root cells stained with trypan blue; a hair root of V. uliginosum coated by loose wefts of fungal hyphae, labeled with arrowhead. (B) A hair root colonized by fungi with coils. *Hyphal coils. (C) A yellowish-brown old root of V. uliginosum colonized by fungi possessing thick hyphae. The arrow indicates the fungal septate. (D) Microsclerotia of dark septate endophytes, labeled with an arrow.
The percent colonization of hair roots by ericoid mycorrhizal fungi (EMF) and dark septate endophytes (DSE).
| EMF | DSE | |
|---|---|---|
| Study area of the Changbai Mountains | 18.6 ± 3.5a | 23.6 ± 3.5c |
| cba study site | 16.2 ± 2.3 | 26.0 ± 2.9 |
| cbb study site | 17.7 ± 2.6 | 22.0 ± 3.0 |
| cbc study site | 21.8 ± 3.0 | 22.8 ± 3.3 |
| Study area of the Greater Khingan Mountains | 12.0 ± 2.6c | 44.3 ± 6.7a |
| ja study site | 11.5 ± 2.9 | 40.5 ± 4.7 |
| jb study site | 12.4 ± 2.4 | 45.3 ± 6.2 |
| jc study site | 12.0 ± 2.3 | 47.2 ± 7.1 |
| Study area of the Lesser Khingan Mountains | 13.0 ± 2.5b | 29.0 ± 5.1b |
| la study site | 13.0 ± 2.2 | 30.4 ± 5.6 |
| lb study site | 14.2 ± 2.8 | 28.0 ± 4.3 |
| lc study site | 11.9 ± 2.0 | 28.4 ± 5.0 |
The numbers represent the mean values ± SD. Different letters indicate significantly different study areas of data (Kruskal-Wallis ANOVA + multiple comparisons, P < 0.05).
The closest relatives of the fungal endophyte isolates based on BLAST analysis in GenBank.
| Fungal isolate& | Best BLAST match | Similarity (%) | ERM* |
|---|---|---|---|
| k5, 6b, | 98–100 | Y | |
|
| 99 | Y | |
| 70,129 | 99–100 | ||
| 99 | Y | ||
| 99 | Y | ||
| 141, | 99 | Y | |
| 7151, | Uncultured | 99 | Y |
| 156, | Uncultured | 98–99 | Y |
|
| 99 | Y | |
| 99 | Y | ||
| 99 | Y | ||
|
| 99 | Y | |
|
| 98 | N | |
|
| Sordariomycetes sp. (KX909156) | 99 | Y |
| f10, | 99 | N | |
| e22, | 99 | N | |
|
| 99 | N | |
|
| 99 | N | |
| 99 | N | ||
|
| 99 | N | |
| h8, h12, | 99–100 | N | |
| 99 | N | ||
|
| 99 | N | |
| 96–98 | Y | ||
| 99 | N | ||
| t1, | 97–99 | N | |
|
| 97 | N |
*Resynthesis trials confirmed the isolates formed ericoid mycorrhizae (Y) or failed to form ericoid mycorrhizae (N). &The isolates used to conduct resynthesis experiments are indicated in bold.
Figure 2Dark septate endophytes (DSE) stained by trypan blue in V. uliginosum root tissue. (A) Intercellular hyphae formed hyphal nets, labeled with an arrow. (B) Intracellular darkly pigmented septate hyphae, labeled with an arrow. (C) Loosely intertwined intracellular hyphae. Arrows indicate the twined regions. (D) Microsclerotia of DSE, labeled with an arrow. (E) DSE, labeled with an arrowhead, colonized the root apex. *Undifferentiated cells.
Figure 3Observation of a section of ericoid mycorrhizal root from V. uliginosum by TEM. (A) Transverse sectional micrograph of an ericoid mycorrhizal root, indicating the epidermal cells fully colonized by the hyphae of O. maius. Two adjacent cells (b,c) in a transverse section had fungal complexes of different ages. (a,b) Cytoplasmic degeneration in the late stage of mycorrhizal colonization. (c) Mature colonization by hyphae that fill the cell. *A detached cell. (B,C) Higher magnified images of two cells (cell c,d in A). (C). PM: plasma membrane; TEW: thickened outer epidermal walls; EH: intracellular fungal hyphae.
Figure 4Venn diagram showing the specific and shared OTUs of different study areas.
Putative EMF reads originated from different study areas.
| OTU ID | Top hits in GenBank (Accession No.) | Similarity (%) | No. of reads | ||
|---|---|---|---|---|---|
| Changbai Mountains | Greater Khingan Mountains | Lesser Khingan Mountains | |||
| OTU25 | 100 | 7 | 1403 | 1 | |
| OTU335 | 96 | 3 | 1 | 0 | |
| OTU247 | 96 | 4 | 11 | 0 | |
| OTU35 | 96 | 0 | 737 | 0 | |
| OTU181 | 99 | 16 | 0 | 8 | |
| OTU59 | 96 | 41 | 1 | 308 | |
| OTU430 | 99 | 0 | 3 | 0 | |
| OTU49 | 98 | 386 | 0 | 235 | |
| OTU141 | 99 | 10 | 32 | 0 | |
| OTU237 | 96 | 10 | 0 | 0 | |
| OTU53 | 99 | 300 | 90 | 4 | |
| OTU101 | 91 | 0 | 67 | 0 | |
| OTU530 | 92 | 0 | 8 | 0 | |
| OTU73 | 98 | 0 | 179 | 0 | |
| OTU99 | 99 | 1 | 1 | 102 | |
| OTU450 | 100 | 0 | 0 | 4 | |
| OTU28 | 100 | 302 | 896 | 96 | |
| OTU82 | 98 | 5 | 0 | 116 | |
| OTU116 | 91 | 66 | 0 | 2 | |
| OTU150 | 96 | 0 | 8 | 60 | |
| OTU203 | 94 | 0 | 0 | 24 | |
| OTU261 | 100 | 8 | 0 | 15 | |
Top hits in GenBank provided the best match of the representative sequences to GenBank, with accession numbers shown in brackets.
Figure 5Principal coordinate analysis (PCoA) of fungal communities of V. uliginosum from different study areas.
Figure 6Taxonomic composition distribution of genus-level and UPGMA tree for different samples. Only the top 10 genera are shown for taxonomic composition distribution, and other genera were classified as “other”. In the UPGMA tree, samples originated from the Changbai Mountains, the Greater Khingan Mountains, and the Lesser Khingan Mountains, are shown as red, green, and blue, respectively.
Figure 7A putative model of the co-existence between EMF and DSE in the hair roots of V. uliginosum.
Characteristics of the study sites in northeastern China.
| Study site | Changbai Mountains | Greater Khingan Mountains | Lesser Khingan Mountains | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| cba | cbb | cbc | ja | jb | jc | jd | je | jf | la | lb | lc | |
| Location | 128°15′38″E; 42°03′36″N | 128°16′23″E; 42°05′00″N | 128°13′04″E; 42°06′42″N | 124°07′00″E; 50°17′22″N | 124°06′48″E; 50°17′03″N | 124°07′05″E; 50°17′30″N | 124°07′02″E; 50°17′21″N | 124°06′01″E; 50°16′22″N | 124°06′27″E; 50°20′32″N | 129°16′42″E; 48°11′17″N | 129°13′47″E; 48°12′36″N | 129°13′39″E; 48°09′55″N |
| Climate | temperate continental monsoon climate | cold continental monsoon climate | continental monsoon climate | |||||||||
| Frost-free days | 100 | 85–130 | 106 | |||||||||
| Mean annual rainfall | 700–1400 mm | 400–800 mm | 550–600 mm | |||||||||
| Mean annual temperature | 3–7 °C | −2.8 °C | 0–2 °C | |||||||||
| pH | 4.9 | 4.7 | 4.7 | 5.5 | 4.9 | 5.7 | — | — | — | 4.4 | 4.5 | 4.5 |
| Water-soluble salt (μs/cm) | 66 | 224 | 182 | 186 | 93 | 171 | — | — | — | 190 | 294 | 300 |
| CaCO3 (g/kg) | 6.7 | 23.3 | 27.9 | 37.7 | 26.6 | 26.3 | — | — | — | 30.2 | 55.0 | 23.8 |
| Organic matter (g/kg) | 78 | 615 | 661 | 394 | 174 | 294 | — | — | — | 606 | 704 | 575 |
| Total N (g/kg) | 1.30 | 1.40 | 1.39 | 1.53 | 1.47 | 1.33 | — | — | — | 1.27 | 1.30 | 1.30 |
| Total P (g/kg) | 0.18 | 1.21 | 0.88 | 2.28 | 1.31 | 2.24 | — | — | — | 1.09 | 1.22 | 1.15 |
| Total K (g/kg) | 37.20 | 5.82 | 6.14 | 8.32 | 19.60 | 11.10 | — | — | — | 5.67 | 8.97 | 6.21 |
—The values for the samples were not tested.