| Literature DB >> 17854485 |
David Bass1, Thomas A Richards, Lena Matthai, Victoria Marsh, Thomas Cavalier-Smith.
Abstract
BACKGROUND: It is much debated whether microbes are easily dispersed globally or whether they, like many macro-organisms, have historical biogeographies. The ubiquitous dispersal hypothesis states that microbes are so numerous and so easily dispersed worldwide that all should be globally distributed and found wherever growing conditions suit them. This has been broadly upheld for protists (microbial eukaryotes) by most morphological and some molecular analyses. However, morphology and most previously used evolutionary markers evolve too slowly to test this important hypothesis adequately.Entities:
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Year: 2007 PMID: 17854485 PMCID: PMC2194784 DOI: 10.1186/1471-2148-7-162
Source DB: PubMed Journal: BMC Evol Biol ISSN: 1471-2148 Impact factor: 3.260
Figure 1Comparisons of evolutionary changes in the 18S and the ITS1 sequence. Left tree (black): Maximum likelihood (ML) phylogeny of cercomonad 18S rDNA sequences calculated from an alignment of 15 sequences and 213 nucleotide positions from the hypervariable V4 region. Right tree (grey): ML phylogeny of corresponding ITS1 rDNA (213 positions). Branch lengths and scale bars standardised to illustrate the much greater evolutionary rate of ITS1 than even the most hypervariable 18S rDNA region. Equivalent parsimony analyses using gaps as a 5th character (not shown) showed a parsimony score of 367 (minimum changes) for ITS1 and 120 for the V4 18S rDNA region. Cultures used for ecological and phenotypic character experiments (Table 2) marked by circles.
Figure 2Phylogeny of cercomonads. BioNJ bootstrap tree (1000 replicates; corrected for Γ & I) of a subset of known cercomonad lineages, representing all known main cercomonad clades and genera (Cercomonas, Eocercomonas, and Paracercomonas) as defined by Karpov et al. [14]. The composition and phylogenetic position of the groups α, β, and γ forming the basis of this study are shown. A group-specific primer set was designed for each of these groups (see Methods).
Figure 3Global provenance, biogeography and phylogeny of cercomonads. (A) World map showing major animal biogeographical regions. (B-D) 18S-ITS1 rDNA phylogenies of groups α (278 nucleotide positions), β (414 positions), and γ (335 positions). See Methods for details of each sequence dataset. Coloured discs correspond to hoops on map. Grey arrowheads indicate sequences found in only one biogeographical region. Square black brackets indicate 18S-genotype boundaries. X and Z (bracketed) indicates a possible endemic genotypic radiation. Branches marked a, f, and h in (B) are discussed in relation to additional sampling and ITS-type-specific primer probing. Branches without coloured discs originate from cultures. Sampling range differs among the three groups (Table 1). Key to bootstraps (ML/parsimony) given to right of scale. Bootstraps shown only when equal to or exceeding the value stated, although precise values are shown for clades marked X and Z, as these are discussed in the text as potentially geographically-restricted clades. Branch labels underlined and in bold refer to culture-derived sequences, including those used in the culture experiments. NB: in some cases a single branch corresponds to >1 culture or both environmental and culture-derived sequences. The long branch for 11.7E is not shown in (D) for the sake of clarity. It was not detected in any environmental library.
Sampling and provenance of genotypes sampled
| Australasian | New Zealand | Soil & f/w sediment | 8 (4) | 1 | 4 | 6 | 02.03 |
| Australia | Soil | 4 (1) | 1 | 4 | 12.04 | ||
| Tasmania | Soil | 4 (1) | 1 | 4 | 12.04 | ||
| Neotropical | Peru | Soil | 7 (3) | 1 | 5 | 2 | 07.05 |
| Panama | Freshwater sediment | 4 (4) | 1 | 4 | 03.03 | ||
| Panama | Coastal sediment | 5 (3) | 1 | 2 | 03.03 | ||
| W. Palaearctic | Oxfordshire | Soil | 7 (4) | 1 | 4 | 2 | 07.03 |
| UK | Coastal sediment | 8 (7) | 1 | 4 | 05.02 | ||
| Australasian | New Zealand | Soil & f/w sediment | 8 | 3 | 6 | 4 | 02.03 |
| Coastal sediment | 13 | 1 | 1 | 02.03 | |||
| Tasmania | Soil | 4 (1) | 1 | 1 | 12.04 | ||
| Oriental | Calcutta | Soil | 4 (3) | 1 | 1 | 0 | 02.05 |
| Neotropical | Panama | Freshwater sediment | 7 | 1 | 2 | 0 | 03.03 |
| Panama | Coastal sediment | 8 | 1 | 1 | 03.03 | ||
| Peru | Soil | 12 | 1 | 1 | 07.05 | ||
| W. Palaearctic | UK & Europe | Coastal sediment | 6 | 1 | 1 | 1 | '03 & '04 |
| UK & Europe | Soil | 7 | 1 | 1 | '03 & '04 | ||
| E. Palaearctic | Japan | Freshwater sediment | 6 (5) | 1 | 2 | 0 | 12.04 |
| Nearctic | BC | Coastal sediment | 5 | 1 | 1 | 0 | 06&09.02 |
| Australasian | New Zealand | Soil & f/w sediment | 8 | 1 | 5 | 3 | 02.03 |
| Coastal sediment | 5 | 1 | 2 | 02.03 | |||
| Australia | Soil | 4 | 1 | 4 | 12.04 | ||
| Neotropical | Panama | Soil & f/w sediment | 4 | (11) | (11) | (11) | 03.03 |
| Panama | Coastal sediment | 7 | 1 | 2 | 03.03 | ||
| Ethiopian | South Africa | Soil | 11 | 2 (+21) | 4 (+21) | 2 (+21) | 12.03 |
| W. Palaearctic | UK | Coastal sediment | 11 | 1 | 5 | 1 | 05.02 |
| Oxfordshire | Soil | 4 | 1 | 5 | 07.03 | ||
| E. Palaearctic | Japan | Freshwater sediment | 5 | 1 | 2 | 0 | 12.04 |
| Nearctic | BC | Soil | 6 | 1 | 5 | 0 | 06&09.02 |
(eDNA = environmental DNA sample – see Methods for more details.)
(1) These additional genotypes were also detected, and were not recovered from any other site. (Not shown on Fig. 3.)
Figure 4Shared alignment characters supporting putative geographically restricted clades . (A) Paracercomonas group α tree; (B) Paracercomonas group β tree (taken from Fig. 3). Characters at specific alignment positions are coloured black when 0.8 of positions agree; otherwise they are unshaded. Unique clade-specific alignment characters are illustrated with triangles across the bottom of the alignments. Shared sequence motifs in a hyper-variable section are illustrated with an oval across the bottom. Sequence position numbers across the top refer to DB-1002-6 and P101 PANAMA.
Results of culture experiments: ability of clonal cercomonad strains to grow in various marine media and other strain characteristics
| Strain | ||||||||
| XT179 | 1 | 1 | 1 | 5–7 | ||||
| α | NZ1.5C | 1 | 1 | 1 | 5–6 | |||
| α | XT160 | 1 | 1 | 1 | 5–7 | |||
| α | EC | 1 * | 2 * | 1 | 5–7 | X? | ||
| α | 5A | 1 | 2 * | 2 | N/A | 6–8 | X? | |
| α | P111 | 1 | 3 | N/A | N/A | 5–7 | X | |
| α | SCCAP C1h | 1 | N/A | N/A | N/A | 4–10h | N/A | |
| γ | C73 | 1 | 1 | N/A | 4–6 | X | ||
| γ | XT196 | 1 | 2 | N/A | N/A | 5–10 | N/A | |
| γ | C76 | 2 | 3 | N/A | X | 5 | X | |
| γ | 11.7E | 3 | 4 | N/A | 5–7 | |||
N/A = no data
* Although the ITS1 sequences for EC and 5A are identical, and 18S rDNA is identical in the V4 region (on which Fig. 1 is based), EC has an insert near the 3' end of 18S and is therefore clearly a different strain. This is the only strain in this study known to have such an insert.
a see Figs 1, 2, and 3.
b Identical numbers indicate strains with identical sequences.
c Identical numbers indicate strains with strain traits other than size (flagella length:body length, form and frequency of plasmodium formation, propensity to form cell clusters, etc.) which were indistinguishable from others in the same medium under light microscopy (200× phase contrast).
d Overall performance of strains under a range of saline medium regimens, as described in Methods. X means that no living cells were seen.
e Size range determined from 3+ independent cultures observed over a period of 18 months.
f Indicates the propensity of the strain to form cysts in Volvic & grain cultures, summarized from observations of 3+ independent cultures observed over a period of 18 months. X = no cysts seen, = cysts infrequent and sparse, = cysts regular at low to medium densities, = cysts readily formed and seen at high densities.
g A measure of the ability of the strain to form dense cultures in Volvic & grain medium, which persist well over time (2+ months in unmanipulated cultures), summarized from observations of 3+ independent cultures observed over a period of 18 months. = rarely or never reach high density, = may reach medium to high density but do not persist, = usually reach high densities and/or persist for long periods without encysting or disappearing from the culture.
h See ref. 31. Not included on Figs 1 and 3 as there is no ITS1 sequence available. Not included in culture experiments.
Sequence variation within libraries constructed from two clonal cercomonad cultures
| AZ61 | 18S | 545 | 15 | 0.11 | Relatively conserved |
| C-591 | 535 | 11 | 0.09 | ||
| AZ6 | ITS1-5.8S-ITS2-28S (D1/D2 region) | 603 | 11 | 0.08 | Relatively variable |
| C-59 | 609 | 20 | 0.14 | ||
| AZ6 | whole fragment | 1148 | 26 | 0.09 | (average) |
| C-59 | 1144 | 31 | 0.11 |
1 see ref. 14