| Literature DB >> 21639885 |
Lin Sen1, Mario A Fares, Bo Liang, Lei Gao, Bo Wang, Ting Wang, Ying-Juan Su.
Abstract
BACKGROUND: The chloroplast-localized ribulose-1, 5-biphosphate carboxylase/oxygenase (Rubisco), the primary enzyme responsible for autotrophy, is instrumental in the continual adaptation of plants to variations in the concentrations of CO2. The large subunit (LSU) of Rubisco is encoded by the chloroplast rbcL gene. Although adaptive processes have been previously identified at this gene, characterizing the relationships between the mutational dynamics at the protein level may yield clues on the biological meaning of such adaptive processes. The role of such coevolutionary dynamics in the continual fine-tuning of RbcL remains obscure.Entities:
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Year: 2011 PMID: 21639885 PMCID: PMC3129321 DOI: 10.1186/1745-6150-6-29
Source DB: PubMed Journal: Biol Direct ISSN: 1745-6150 Impact factor: 4.540
Figure 1The phylogenetic tree inferred from . Geologic timescale is tagged above the phylogenetic tree (Unit: Million years). The estimated global atmospheric CO2 concentrations from the GEOCARB III model are mapped under the phylogenetic tree according to the geologic timeline. Each node in the tree is numbered. Posterior probability values are shown along the branches and those with posterior probability ≥ 0.9 are heavily thickened. Two time intervals are demonstrated in grey. The six major clades concerned in this research are indicated: Podocarpaceae, Podocarpus I and II, Cephalotaxaceae, Taxus and Torreya. The length of each branch is in proportion to the divergence time estimated by using the UCLD model.
Parameters estimated under the UCLD model
| Posterior | Estimated divergence | Estimated rates | Geologic period | |
|---|---|---|---|---|
| 1 | 100 | 8.62 | 1.52 | Neogene |
| 7 | 99.97 | 29.61 | 2.85 | Paleogene/Neogene |
| 13 | 100 | 49.65 | 2.69 | Paleogene |
| 25 | 95.51 | 52.95 | 1.69 | Paleogene |
| 26 | 100 | 19.98 | 2.06 | Neogene |
| 27 | 99.99 | 66.75 | 2.46 | Paleogene |
| 28 | 99.99 | 61.78 | 1.99 | Paleogene |
| 30 | 100 | 134.19 | 4.66 | Lower Cretaceous |
| 32 | 100 | 9.13 | 2.41 | Paleogene |
| 35 | 99.67 | 31.9 | 1.96 | Paleogene |
| 36 | 100 | 39.88 | 2.94 | Paleogene |
| 38 | 100 | 34.74 | 1.28 | Paleogene |
| 39 | 99.99 | 69.45 | 1.65 | Cretaceous/Paleogene |
| 40 | 96.18 | 8.18 | 1.59 | Neogene |
| 47 | 99.29 | 21.02 | 1.56 | Neogene |
| 49 | 98.09 | 4.12 | 1.48 | Neogene/Quaternary |
| 50 | 98.77 | 21.05 | 1.52 | Neogene |
| 51 | 100 | 30.85 | 2.53 | Paleogene/Neogene |
| 54 | 98.18 | 1.47 | 2.01 | Neogene/Quaternary |
| 55 | 100 | 9.98 | 2.47 | Neogene/Quaternary |
| 64 | 100 | 20.17 | 2.57 | Neogene |
| 65 | 99.76 | 136.64 | 1.58 | Lower Cretaceous |
| 67 | 100 | 168.52 | 2.89 | Middle Jurassic |
| 70 | 99.97 | 174.16 | 1.97 | Middle Jurassic |
Results for the well supported nodes in Figure 1 are shown.
Figure 2Estimated parameters under the M8 model using Selecton web-server. Approximate posterior means of ω are weighted by the posterior probabilities. Sites are numbered according to the reference sequence from Taxus mairei (GenBank accession number: AY450856).
Parameter estimates from tests for selection
| Model | ℓ | Parameters | Positively selected sites | |
|---|---|---|---|---|
| M0: One ratio | 137 | -5654.77 | None | |
| M1a: Nearly neutral | 138 | -5539.34 | Not allowed | |
| M2a: Positive selection | 140 | -5529.73 | K30Q | |
| M3: Discrete | 139 | -5536.84 | A11V, Q14K, E28Q, K30Q, G86D, S95N, V99A, I133L, L225I, I251M, K305R | |
| M7: β | 138 | -5547.37 | Not allowed | |
| M8: β & | 140 | -5527.82 | A11V, Q14K, K30Q, S95N, V99A, I133L, L225I | |
| Model A: | 139 | -5533.19 | Not allowed | |
| Model A: | 140 | -5530.95 | A11V, V99A, I133L | |
| Model A: | 139 | -5535.98 | Not allowed | |
| Model A: | 140 | -5533.12 | K30Q | |
| Model A: | 139 | -5538.23 | Not allowed | |
| Model A: | 140 | -5538.33 | None | |
| Model A: | 139 | -5527.9 | Not allowed | |
| Model A: | 140 | -5523.16 | A11V, G86D, V99A, I133L | |
| Model A: | 139 | -5537.56 | Not allowed | |
| Model A: | 140 | -5533.91 | None | |
| Model A: | 139 | -5530.31 | Not allowed | |
| Model A: | 140 | -5526.95 | S143A, T262V | |
| ℓ | ||||
| Model A: | 139 | -5537.3 | Not allowed | |
| Model A: | 140 | -5536.84 | None | |
Positive selection sites are identified with posterior probability higher than 95%.
Tests for selection with Bonferroni correction
| Model | 2Δℓ | Sig. α = 0.05 | Bonferroni correction | Sig. α = 0.05 | ||
|---|---|---|---|---|---|---|
| M0-M3 | 235.86 | 2 | 0 | ● | No need | |
| M1a-M2a | 19.22 | 2 | 0.0001 | ● | No need | |
| M7-M8 | 39.1 | 2 | 0 | ● | No need | |
| M8a-M8 | 4.86 | 1 | 0.0275 | ● | No need | |
| A-A1 test | ||||||
| Taxaceae-Cephalotaxaceae | 4.48 | 1 | 0.0343 | ● | 0.0686 | ○ |
| 5.72 | 1 | 0.0168 | ● | 0.084 | ○ | |
| 0.2 | 1 | 0.6547 | ○ | 3.2735 | ○ | |
| Cephalotaxaceae | 0.92 | 1 | 0.3375 | ○ | 1.6875 | ○ |
| Podocarpaceae | 9.48 | 1 | 0.0021 | ● | 0.0105 | ● |
| 7.3 | 1 | 0.0069 | ● | 0.0345 | ● | |
| 6.72 | 1 | 0.0095 | ● | 0.0475 | ● | |
In the branch-site model, the relevant hypotheses are verified under the Bonferroni correction to avoid false positive conclusion. The sign ● denotes the results that pass the statistical significance tests, while ○ stands for the opposite.
Figure 3Positively selected sites in the RbcL subunit of the Podocarpaceae ancestor. Four positive selected sites of the Podocarpaceae ancestor are highlighted in red arrows. The 3D imagines of the ancestral and current amino acid residues are represented in purple and cyanine, respectively. The ancestral amino acid residues are inferred by the DAMBE package and the ancestral state reconstruction (ASR) molecule on Datamonkey 2010 website for the Podocarpaceae ancestral node [28,82]. The three domains are colour coded differently. Positively selected sites are indicated with lines, whereas the potential ones are with black dotted lines.
Figure 4Coevolutionary networks in the RbcL subunit of the three gymnosperm families. Residues in the networks are sorted clockwise in an ascending order depending on the number of coevolutionary interactions that each amino acid residue establishes. The domains to which these amino acid sites belong are colour-coded. Nodes (amino acid residues) are connected through edges differently according to the nature and characteristics of their coevolution.
Figure 5Coevolving sites within the N-terminal structure of the RbcL subunit. Amino acid residues involving in the coevolutionary network are highlighted red in the 3D structural diagram. And the residues are connected differently according to the nature and characteristics of their coevolution.
Functional roles of the amino acid sites under adaptive evolution
| Location | ||||
|---|---|---|---|---|
| Site | Domain | Interface | Functional roles | References |
| A11V | loop 1 | To contribute to the holoenzyme thermal stability, catalytic efficiency, and CO2/O2 specificity | Kellogg and Juliano (1997) [ | |
| Q14K | Ott | |||
| K30Q | loop 2 | LSU dimers | Du and Spreitzer (2000) [ | |
| I133L | βE | Spreitzer and Salvucci (2002) [ | ||
| S143A | αD | Spreitzer | ||
| L225I | α2 | LSUs and SSUs | Makowski | |
| T262V | β4 | |||
| G86D | βC | Rubisco and its activase | To affect the contacts between the Rubisco and its activase | Du |
| S95N | βD | Portis (2003) [ | ||
| V99A | Portis | |||
All positively selected amino acid sites in Table 3 are included.
Species and GenBank accession numbers for the rbcL gene sequences analysed in this study
| Family | Genus | Species | GenBank Acc. No. |
|---|---|---|---|
| Taxaceae | |||
| Cephalotaxaceae | |||
| Podocarpaceae | |||
| Outgroup | |||
The sign * denotes sequences experimentally determined in the present study.