- Research article
- Open Access
Algal MIPs, high diversity and conserved motifs
BMC Evolutionary Biology volume 11, Article number: 110 (2011)
Major intrinsic proteins (MIPs) also named aquaporins form channels facilitating the passive transport of water and other small polar molecules across membranes. MIPs are particularly abundant and diverse in terrestrial plants but little is known about their evolutionary history. In an attempt to investigate the origin of the plant MIP subfamilies, genomes of chlorophyte algae, the sister group of charophyte algae and land plants, were searched for MIP encoding genes.
A total of 22 MIPs were identified in the nine analysed genomes and phylogenetic analyses classified them into seven subfamilies. Two of these, Plasma membrane Intrinsic Proteins (PIPs) and GlpF-like Intrinsic Proteins (GIPs), are also present in land plants and divergence dating support a common origin of these algal and land plant MIPs, predating the evolution of terrestrial plants. The subfamilies unique to algae were named MIPA to MIPE to facilitate the use of a common nomenclature for plant MIPs reflecting phylogenetically stable groups. All of the investigated genomes contained at least one MIP gene but only a few species encoded MIPs belonging to more than one subfamily.
Our results suggest that at least two of the seven subfamilies found in land plants were present already in an algal ancestor. The total variation of MIPs and the number of different subfamilies in chlorophyte algae is likely to be even higher than that found in land plants. Our analyses indicate that genetic exchanges between several of the algal subfamilies have occurred. The PIP1 and PIP2 groups and the Ca2+ gating appear to be specific to land plants whereas the pH gating is a more ancient characteristic shared by all PIPs. Further studies are needed to discern the function of the algal specific subfamilies MIPA-E and to fully understand the evolutionary relationship of algal and terrestrial plant MIPs.
General function and structure of MIPs
Major Intrinsic Proteins (MIPs) are pore forming membrane proteins found in virtually all types of organisms. They have been shown to facilitate the passive transport of a wide range of small, polar molecules such as water, glycerol and urea [1–5]. MIPs are thought to have evolved through an internal gene duplication creating a direct repeat resulting in the twofold quasi symmetry of the structure . Even though the overall pairwise sequence similarities can be low, all MIPs share some structural features such as having six transmembrane helices (H1-H6), connected by five loops (loop A-loop E), and two highly conserved NPA motifs. The NPA motifs are located at the N-terminal end of two half helices, HB and HE, formed by parts of loop B and loop E respectively. These two half helices are inserted from opposite sides of the membrane and meet to form one of two selectivity regions of the pore. The positive charges formed by the helical dipoles of HB and HE are focused on the NPA motifs, thereby effectively obstructing the passage of protons by means of electrostatic repulsion . The second restriction site of the MIP pore is called the aromatic/arginine (ar/R) selectivity filter and consists of four amino acid residues forming the narrowest part of the pore. It is thought that the amino acid residue composition of this constriction site is the major determinant of the substrate specificity of MIPs .
Terrestrial plants have more isoforms and a wider variety of MIPs than any other group of organisms. Even in the genome of a relatively simple land plant like a moss 23 different MIPs, divided on seven subfamilies, are encoded . Little is known on why, when and how all these subfamilies evolved in plants. Land plants are thought to descend from fresh water green algae and thus identification and studies of algal MIPs can potentially provide clues to the origin and early evolution of plant MIPs. The complete set of MIPs in nine algal genomes were therefore identified, analysed and compared to land plant MIPs in this work.
Evolution and phylogeny of green algae
The clade of green plants (viridiplantae) together with the glaucophytes and the red algae (rhodophytes) form the larger monophyletic clade archaeplastida (the plant kingdom) which include all organisms with a chloroplast of primary endosymbiotic origin. The green plants are divided into the chlorophytes (consisting only of algal species) and streptophytes (containing both algae and land plants) and these clades are thought to have split 725-1200 Million Years Ago (MYA) [10–12] (Figure 1). The chlorophytes are further divided into several classes and even though the internal relationship between many of these classes is unresolved, there is a general consensus that mamiellophyceae is basal to chlorophyceae and trebouxiophyceae, which both belong to the well-defined UTC clade . The other group of green plants, streptophytes, consists of a few classes of green algae (collectively known as the paraphyletic group charophyta) and the monophyletic group of land plants (embryophyta). The green algae studied in this work all belong to the chlorophyte clade with the Ostreococcus and Micromonas species belonging to the class mamiellophyceae , Volvox carteri and Chlamydomonas reinhardtii to the class chlorophyceae and Coccomyxa sp. C-169 and Chlorella sp. NC64A to the class trebouxiophyceae (Figure 1).
In this article, we identify 22 algal MIPs that cluster into seven subfamilies whereof two, the Plasma membrane Intrinsic Proteins (PIPs) and GlpF-like Intrinsic Proteins (GIPs), already have been characterized in land plants. All the investigated algal genomes encode at least one MIP, but only three contain more than one subfamily. The characteristics of each of the seven subfamilies are described and the evolution of the wide variety of algal MIPs, and their functions, is discussed.
Identification and annotation of algal MIPgenes
Nine algal genomes available at the Joint Genome Initiative (JGI)  were searched for encoded MIPs using protein sequences from Physcomitrella patens and Chlamydomonas rheinhardtii as queries [9, 15]. This yielded 20 different MIP genes of which only two corresponding complete sequences and one partial sequence were also present in GenBank . Less than half of the identified algal MIP genes had a good model in JGI , hence new gene models were created for the majority of the genes (Additional file 1). In one of the algal genomes (Ostreococcus tauri) no MIP genes were found initially. However, repeating the searches of all genomes using all algal MIPs discovered in the first round of searches as queries revealed two more MIP sequences, whereof one was from this species (OtMIPC1;1), resulting in a total of 22 algae MIPs, see Table 1. Six of these MIPs are found in the five species belonging to the class mamiellophyceae whereas the remaining 16 MIPs are derived from the four species within the UTC clade. Coding sequences for the algae MIPs are provided in FASTA-format (Additional file 2).
To take advantage of the high degree of structural conservation within the MIP family, a three dimensional alignment of MIP structures was constructed and used as a guide in creating a sequence alignment. Representatives of known subfamilies from all three domains of life were then added and manually aligned to the initial structure based sequence alignment. Thereafter the identified algal sequences from the first searches were added and aligned. Finally the number of reference sequences in the alignment was reduced to a more manageable subset still representing a wide variety of MIPs from bacteria, land plants, mammals and viruses. The highly divergent N- and C-terminal regions were excluded in the phylogenetic analyses and therefore no effort was put into aligning these. An overview picture of the alignment showing gaps and the positions of conserved structural elements is shown in Figure 2. Also indicated in the figure are the intron positions in the gene models and their relative position to the reading frame. Since these were not included in the dataset underlying the phylogenetic analysis, the positions can be used to verify the phylogenetic grouping of sequences. The alignment file is provided in Nexus format as Additional file 3.
Phylogenetic analyses reveal seven groups of MIPs in algae
In order to classify the algal MIPs, their protein sequences were analysed phylogenetically together with the reference set, using both the maximum likelihood method  and the Bayesian method . Results from these analyses are also presented in Figure 2, displaying the Maximum Likelihood tree to the left, where the branch lengths illustrate the sequence divergence, and a consensus tree to the right, summarizing the results of two different stability tests. In this tree the stability of each node is shown by the Maximum Likelihood bootstrap support value together with indications of Bayesian posterior probabilities of at least 90%.
In order to facilitate the interpretation, the phyla from which the plant MIPs are derived are indicated by colour coding of the branches in the consensus tree in Figure 2. The 22 algal MIPs cluster into seven groups whereof two are closely associated with the PIP and GIP subfamilies found in land plants . These two groups of algal MIPs are therefore classified as PIPs and GIPs. Classification of the remaining five novel groups is not as straight forward and hence these groups were arbitrarily named MIPA-MIPE. There is no support for an endosymbiotic origin via the chloroplast of any these subfamilies, since no close homologs are found in cyanobacteria. In the next section the characteristics of each of the seven algal MIP groups are described more in detail.
Two sequences from Coccomyxa sp. C-169 grouped basal to the PIPs of Physcomitrella patens, a grouping with high support from both Maximum Likelihood and Bayesian inference (Figure 2). Aside from a general overall similarity, these sequences display many of the specific features that are characteristic of PIPs, supporting a common origin and function of these proteins. The ar/R filters are almost identical to the highly conserved filter of PIPs in land plants, with the minor difference of the algal MIPs having a cysteine instead of a threonine in the third position (Table 2). In the algal sequences loop A is slightly longer (3-8 amino acids) but still contains the highly conserved cysteine found in plant PIPs  though offset by two amino acids. The D loop, involved in gating of land plant PIPs, has a conserved loop length and the histidine required for pH gating  is also present. However, the two N-terminal acidic residues indicated in calcium gating  are lacking. The phosphorylation site in loop B is conserved (KXSXXR) whereas the C-terminal phosphorylation site specific for PIP2s  is not. Furthermore, the GGGAN motif of loop C is fully conserved in one of the algal sequences but only partially in the other sequence (LGASN). Also at the gene level there is evidence of shared ancestry for all PIPs, with two intron positions being conserved (Figure 2). Considering these specific and the general overall similarities, algal MIPs were classified as PIPs but numbered CcPIP4;1 and CcPIP4;2, to reflect their basal position in this subfamily.
Three sequences, one from Coccomyxa sp. C-169 and one from Chlorella sp. NC64A along with a sequence from the Chlorella virus PbcvMT325 [AQPV1; 23] clustered together with PpGIP1;1 with high support in the clade containing glycerol channels from Gram positive bacteria. The ar/R filters of these algal sequences are very similar to the one of PpGIP1;1, suggesting that they are permeable for glycerol (Table 2). They also contain the among glycerol channels conserved DXXXR motif just after the second NPA box, but are missing the very long C loop unique for PpGIP1;1 as well as any conserved intron positions [Figure 2; 24]. However, similar to PpGIP1;1 these sequences have a shorter loop preceding the first NPA box and also atypical residues compared to other MIPs at positions T72, F89 and Q93 (EcGlpF numbering). These residues have been suggested to be involved in the packing of the core near the first NPA box [6, 24]. In the light of their close association with PpGIP1;1 these MIPs were named CcGIP1;1, CnGIP1;1 and PbcvMT325GIP1;1 respectively. It should be noted that the sequence of H4 is poorly conserved in CnGIP1;1, making the functionality of this particular protein questionable.
The remaining five algal MIP groups were named MIPA-MIPE arbitrarily. A single sequence from Coccomyxa sp. C-169 showed no apparent association with any other sequence and was named CcMIPA1;1. In this MIP the first NPA box is substituted to NPM, a variation that is seen at the second NPA motif in several other isoforms e.g. PpNIP6;1. tBLASTn searches suggest weak similarity to plant HIPs, TIPs and animal AQP8s. In line with this the ar/R filter resembles that of AtTIP2;1 which have been shown to be permeable to water, urea and ammonia (Table 2).
Two sequences from Ostreococcus lucimarinus and Ostreococcus RCC809 form a separate group. Both MIPs have atypical NPA motifs (NPS in HB and NAA in HE) and also lack the highly conserved motif leading up to the first NPA box, suggesting an alternative conformation of this part of loop B. The ar/R filter of these sequences is similar to the one in GLALlac  suggesting that both water and glycerol might be substrates. These sequences were named OlMIPB1;1 and OrMIPB1;1.
Three sequences from Micromonas pusilla CCMP1545, Micromonas RCC299 and Ostreococcus tauri grouped with the PpSIPs and the human AQP11 and AQP12. These MIPs all lack a conserved glycine in H2, suggested to be important in the packing of the helices [26, 27]. All three proteins have unusual substitutions in H3 and H6 where a conserved glutamine is replaced by a threonine or serine and a conserved proline changed to alanine, respectively. The C-terminal regions of the algal sequences are rich in positively charged residues, similar to those of SIPs and AQP11/12 where these residues have been suggested to have a function in ER retention . Overall the ar/R filter is quite different to that of any characterised MIP and despite the fact that the conserved arginine of the ar/R filter is lacking just like in the SIPs and AQP11/12, they are not really comparable (Table 2). Even though these algal sequences firmly grouped with the PpSIPs they showed an even closer association with HsAQP11 and HsAQP12. This, together with the very long branch lengths, led to the classification of these sequences as a separate subfamily and therefore named MpMIPC1;1, MrMIPC1;1 and OtMIPC1;1 instead of being classified as SIPs.
One group showed a weak association with the PpXIPs. This was the most numerous group containing eight MIPs with representatives from Coccomyxa sp. C-169, Chlorella sp. NC64A, Volvox carteri and Chlamydomonas reinhardtii. Consistent with the high bootstrap value for this clade the corresponding genes share one or more conserved intron positions in all except one case. The members of this group display variation from an otherwise conserved proline in H6 and instead have glutamine, glutamate, or in one case histidine at this position. They are also distinguished by the unusually short H1 and H2 and by two strictly conserved cysteines in loop C and in the loop after HE respectively. None of these features are found in XIPs, except for a conserved cysteine in the variable C-loop that can be aligned at a corresponding position. Based upon their ar/R filter these algal sequences can be divided into two groups (Table 2). One group have filters similar to that of CrMIPD1;1, which has already been shown to be permeable to glycerol  and one group similar to OsTIP4;1  suggesting water and glycerol as substrate for these. The MIPs in the two groups were named MIPD1 and MIPD2 to MIPD4, respectively, in accordance with the phylogenetic classification (Figure 2; VcMIPD4;1, data not shown). It should be noted that VcMIPD4;1 has a unique substitution in the ar/R filter where the arginine is replaced by histidine.
The group containing three sequences from Chlorella sp. NC64A and one from Ostreococcus RCC809 was named MIPE. They all have ar/R filters identical to that of algal PIPs and also share a conserved motif in loop E (DGCS, where the cysteine is situated at LE1 of the ar/R filter) with these (Figure 3). Furthermore, phylogenetic analyses of the C-terminal region show that these parts of the MIPEs and algal PIPs are closely related (data not shown). The MIPEs also share a motif in loop C with the mammalian classical aquaporins (LXXN). In addition, OrMIPE1;1 shares significant sequence similarity with OlMIPB1;1 and OrMIPB1;1 in loop E (Figure 4). It should be noted that CnMIPE1;3 is missing sequence information corresponding to half of H4, loop D and most of H5 due to a gap in the available genomic sequence.
To investigate if there is any support for a horizontal gene transfer (HGT) event in the evolution of plant MIPs a divergence dating was performed. Of particular interest is the timing of the split between chlorophyte and streptophyte PIPs and the split between chlorophyte/virus and streptophyte GIPs. The PIP split was estimated to 765 MYA (geometric mean, 95% Highest Posterior Density (HPD): 543-1055 MYA) and the GIP split to 704 MYA (geometric mean, 95% HPD: 428-1054 MYA). In light of the similarity of the C-terminal part of the algal PIPs and MIPEs a divergence dating where this part was excluded from all sequences was also performed. The split of the PIPs was then estimated to 737 MYA (geometric mean, 95% HPD: 547-987 MYA). For further details see supplemented log-files (Additional files 4 and 5).
Land plants contain more isoforms and subfamilies of MIPs than other organisms, but how and when this diversity evolved is presently not known. In an attempt to resolve these issues we identified and analysed all MIPs encoded in nine publicly available algal genomes. These algae belong to the chlorophyte clade, making them all equally distant relatives of land plants. At the present there are unfortunately no available genomes of the charophyte algae, which are more closely related to terrestrial plants. In total 22 MIPs were identified and divided into seven subfamilies representing a wide range of variation. Five of the subfamilies, MIPA to MIPE, are specific for algae whereas two, GIPs and PIPs, have previously only been known from terrestrial plants. In the next paragraphs the subfamilies are discussed in detail. The MIPEs are discussed together with the PIPs and MIPBs since they seem to be partially interconnected.
Evolution of PIPs and MIPEs
The algal PIPs show many similarities with the PIPs of land plants and it is tempting to make the assumption that PIPs, with those shared features, were present already some 1000 MYA at the split of the chlorophytes and the streptophytes [10–12]. Land plant PIPs are known to be regulated by pH, Ca2+ and phosphorylation and a molecular gating mechanism has been suggested. In this, several of the residues have overlapping functions in controlling the D-loop conformation in response to the different signals. However, the evolution of the gating mechanism is likely to have been a stepwise process, starting out from a primitive regulatory mechanism and then sequentially adding further functionality. The presence of an among all PIPs conserved histidine crucial for pH gating [H193 in SoPIP2;1; 20, 21] in the algal PIPs, implies that this regulatory feature might be such a primitive mechanism. Contrary to this, the acidic amino acid residues responsible for Ca2+ binding (D28 and E31 in SoPIP2;1) are not found in the algal PIPs, suggesting that the Ca2+-dependent gating is a later acquired trait. This is intriguing as the proposed pH gating mechanism postulates that a salt bridge between H193 and D28 is stabilizing the closed conformation, hinting at an alternative pH dependent interaction in the algal PIPs. Such an alternative interaction might instead include a salt bridge to a phosphorylated serine located in the conserved phosphorylation motif of the B-loop (S115 in SoPIP2;1). In the C-termini of PIP2s there is a second phosphorylation motif, also regulating the gating. The fact that this motif is only found in PIP2s and that the algal PIPs are basal to the PIPs identified in land plants, suggests that this regulation is the most recent addition to the gating mechanism.
PIPs are only present in one of the nine analysed species but an additional partial PIP sequence was found in Parietochloris incise, a relative to Chlorella NC64A (data not shown). However, their absence in all but two of the analysed species means that they have been lost not just once but at least three times in the chlorophytes if a strict vertical inheritance is assumed. An alternative explanation of the observed erratic distribution of PIPs would be a HGT between ancestors of embryophytes and the chlorophyceae, a scenario that would only require two steps.
The fact that the C-terminal part of the algal PIPs, after an among PIPs conserved intron, is more closely related to the corresponding part of the MIPEs might suggest shuffling of DNA between the different MIP genes (Figures 2 and 3). The ar/R filters suggest that both algal PIPs and MIPEs are water specific channels and thus functionally redundant in this aspect, which also is consistent with the finding that MIPEs and PIPs are not detected in the same genome of extant organisms. Regardless of inclusion of the MIPE-like part, the divergence dating indicates that the split between algal and embryophyte PIPs happened some 750 MYA long before the evolution of terrestrial plants, when the two lineages still might have shared an aquatic habitat . The presence of a MIP in a Chlorella virus (PbcvMT325GIP1;1, former AQPV1)  suggests a possible vector for HGT. However, a vertical inheritance of PIPs cannot be excluded since the estimated divergence (547-987 MYA) overlap with the suggested time range for the split of chlorophytes and streptophytes (725-1200 MYA). Nonetheless, the dating propose that an ancestral PIP was present in the early streptophyte algal lineage leading to land plants, suggesting that extant species in the sister clade of terrestrial plants, e.g. Chara corallina, could encode PIPs with some of the common characteristics found in algal and embryophyte PIPs. Thus pH gating would be expected in algal PIPs but perhaps not Ca2+ inhibition. In the presently known algal PIPs there is a cysteine in the ar/R filter predicting that these water channels are sensitive to inhibition by mercury , consistent with experimental findings in charophytes . However, since this residue is in the C-terminal part of the protein, which appears to be more related to MIPEs than PIPs, the ancestral state at this position in early algal PIPs remains uncertain.
GIPs are found in mosses but not in seed plants. Due to the similarities between P. patens GIP and GLPIIs of bacteria a HGT event has been suggested. Based on sequence divergence this event is thought to have occurred about 1000 MYA . A second HGT event between algae provides the simplest explanation of the sparse distribution of GIPs among plants. However, just as for the PIPs, the divergence dating of algal and P. patens GIPs is unable to discern a vertical inheritance from a scenario involving a second HGT event.
In any case, it appears that both a water channel and a glycerol uptake facilitator were acquired early on in the algal lineages leading to trebouxiophyceae and land plants.
There is only one unique sequence representing the proposed new subgroup of MIPA. This protein appears to be fully functional since, apart from the substitution in the first NPA box, all hallmarks of a typical MIP are present. Thus it is unlikely to be a freely evolving pseudogene and might rather be a MIP distantly related to HIPs, AQP8s or TIPs as suggested by the ar/R filter. The finding of three additional subfamilies (PIPs, GIPs, and MIPDs) in the same organism (Coccomyxa C-169), whereof two are also present in land plants, supports the classification of this sequence as belonging to a separate evolving subfamily rather than being a distant member, diverged by speciation from any of the other subfamilies.
MIPBs and MIPEs
The two sequences in the MIPB subfamily are highly similar, consistent with them being derived from closely related algae. Both these proteins have unusual NPA boxes where the first and second motifs are substituted to NPS and NAA, respectively. In most other MIPs both prolines are strictly conserved indicating that they are crucial for the formation of the pore as they hold the N-terminal ends of helices HB and HE together by van der Waals interactions. The recently solved structure of PfAQP which has NLA and NPS instead of the NPA motifs suggests that the loss of van der Waals interactions between the NPA boxes in MIPBs is compensated for by formation of a hydrogen bond, from the amide nitrogen of the alanine replacing proline, to the hydroxyl group of the serine in the NPS motif . The relatively rare occurrence of MIPs with alternative NPA motifs, having this type of interaction, indicates that the two kinds of interactions may not be completely functionally equivalent. Based on the interspersed distribution among the subfamilies of the alternative interaction it appears as if it has evolved independently several times. This might therefore be an example of convergent evolution resulting in similar functional characteristics. In this context it is also interesting to note that another algal MIP, CnMIPE1;2, has NAA and NPT at the first and second NPA motif, respectively. In this MIP, the ar/R selectivity region deviates from the canonical water specific filter found in the other MIPEs, supporting a different transport function.
Although MIPBs are distinctly different from all other MIPs they also share some of the characteristics found in the MIPEs. As can be seen in Figure 2, the loop connecting HE and H6 is extra long in MIPBs and OrMIPE1;1. The high level of sequence similarity suggests that part of the OrMIPE1;1 gene, encoding this loop and half of HE, derive from a MIPB gene since none of the other MIPEs have this sequence (Figure 4).
In addition MIPBs and some MIPEs share unusual substitutions at positions that are part of a structurally conserved network of hydrogen bonds indirectly anchoring the short cytosolic C-terminal helix in AQP5 and the D-loop in the closed conformation of SoPIP2;1 . At two positions in this network, at the beginning of H3, all MIPBs and MIPEs have unusual substitutions where glutamine and asparagine replace arginine and tyrosine, respectively. Furthermore, an among most MIPs conserved histidine in the B loop is replaced by glutamine in MIPBs, OrMIPE1;1 and CnMIPE1;1. These substitutions suggest that a different network of interactions can be expected in MIPBs and MIPEs (Figure 5), possibly causing changes in the properties of the cytosolic portion of the pore by affecting the conformation of the B-loop preceding the first NPA box.
MIPCs - superaquaporins?
The MIPCs form a well-supported subfamily which associates closely with AQP11/12 and the SIPs. It might be argued that they should all be classified as one subfamily, the superaquaporins . There are a few common features supporting such a classification, they are for example all rich in positively charged residues in the C-terminal, a property thought to be important for ER retention and all have a non-standard first NPA motif. However, except for these similarities no other common conserved motifs can be identified and there is a possibility that this grouping is due to long branch attraction, i.e. they are united by their dissimilarity to all other MIPs (see Figure 2), instead of by an actual shared ancestry. This might also explain why the MIPCs seem to be more closely related to AQP11/12 than the SIPs. Another more speculative explanation would be that AQP11/12 in fact originated from an algal MIPC via HGT. The uncertain evolutionary relationship of MIPCs and the other MIP groups in this clade might in fact be one of the strongest arguments for the classification of MIPCs as a separate subfamily. One unusual feature that is found in the MIPCs but not in the associated groups is the lack of the highly conserved Q and P in H3 and H6 respectively, a characteristic they share with the MIPDs (see MIPD discussion below), possibly suggesting an alternative packing of the helices in the monomer.
MIPDs are more symmetric
As previously mentioned all MIPs have an internal symmetry believed to derive from a duplication of an ancestral gene encoding only half of the present MIP sequence. According to this evolutionary hypothesis the first and second half of the protein were initially identical but have later diverged. Beside the NPA motifs there are symmetrically conserved residues in all corresponding transmembrane helices in the first and second half of the MIPs . However, during evolution functional constraints have also selected and conserved residues that create some asymmetries in the protein. The ar/R filter is one such asymmetric feature that is now present in all MIPs. Another less studied feature is found in helices HB-H3 of the first repeat and the corresponding helices HE-H6 of the second repeat (Figure 6). In H6 there is a conserved proline preventing the formation of a hydrogen bond in the α-helix and resulting in a backbone carbonyl oxygen pointing towards the nitrogen of the proline in the NPA box. At the corresponding position in H3 there is a conserved glutamine that appears to occupy the same position as the backbone carbonyl group in H6. These features are conserved in MIP structures, but interestingly some algal MIPs display a subfamily specific variation at these two sites. MIPCs, but not SIPs or AQP11/12, have serine or threonine in H3 and alanine in H6, suggesting a different interaction in this part of the protein. Another variation is found in GIPs that have a glutamate or an asparagine in H3, conservative replacements that might not change the interactions in these areas much. However, in MIPDs the glutamine in H3 is conserved but the proline in H6 is substituted to glutamine, glutamate and in one case to histidine. This suggests that MIPDs are more symmetrical than other MIPs and thus in this regard, possibly more similar to an ancestral MIP. The fixation of the asymmetry in all other MIPs indicates a functional advantage, however the effect of this substitution is not clear and has not to our knowledge been addressed experimentally.
Distribution and function of subfamilies
The distribution of all the MIP subfamilies in different phylogenetic groups of plants is summarized in Figure 7. Compared to terrestrial plants, chlorophyte algal species in general have fewer subfamilies. Based on this limited dataset trebouxiophyceae have the highest number of subfamilies (3-4), followed by mamiellophyceae (1-2) whereas chlorophyceae only have a single subfamily. Still the diversity of MIPs in chlorophytes at large appears to be higher than that of land plants, resulting in a large number of subfamilies with an interspersed species distribution. A similarly complex picture was seen in a study of the ammonium transporters (AMT) presenting several chlorophyte specific subfamilies . The reason for the variation is not clear but it is possible that a more careful comparison of lifestyle or habitat will reveal a logical pattern that can provide clues to the MIPs physiological function. Interestingly, trebouxiophyceae algae are not only found as free living organisms in aquatic habitats but also as symbionts in protozoa and lichen, and as a part of aeroterrestrial biofilms . More specifically, some Coccomyxa species are free living terrestrial algae , whereas Chlorella NC64A is an endosymbiont of the ciliate Paramecium bursaria . We speculate that the large number of MIP subfamilies found in members of trebouxiophyceae is part of an adaptation to these particular lifestyles. For an endosymbiont it is easy to envision that a facilitated exchange of solutes with the host would be beneficial, whereas the solute concentrations possible in terrestrial environments might favour a passive mode of uptake in free living non-aquatic plants.
It has been suggested that the capability to accumulate polyols, such as glycerol, is a prerequisite for algae to endure the harsh conditions in aeroterrestrial habitats . In yeast, that might also experience variable conditions, it has been shown that glycerol can function as an osmoprotectant. Interestingly the opening of a glycerol facilitator, belonging to the MIP family, mediates adaptation to hypo-osmotic conditions by the rapid release of intracellular glycerol . Thus, it is plausible that the physiological role of GIPs is to provide algae with the same ability to adapt to the extreme hypo-osmotic challenges in aeroterrestrial habitats posed by e.g. rain or melting snow.
Regarding the free living aquatic algae of this study we note that in some species of fish, MIPs have an important physiological function, regulating the buoyancy of the egg by adjusting the water content and thereby controlling the depth and hence the milieu for the developing egg [41, 42]. It seems possible that a similar regulation can occur in free living algae in order to find optimal conditions for photosynthesis, uptake of nutrients, transport by currents or possibly to escape predators.
Studies on membrane localization and of substrate specificity will be important tools to discern the functions of the different subfamilies. At the present, we can only speculate that for example in Coccomyxa, MIPA could functionally correspond to TIPs in land plants and thus has a different function than the GIPs and PIPs encoded in the same alga.
As mentioned before, PIPs and MIPEs are likely to have the same or very similar functions and that might be an explanation to why they have not been found in the same organism.
MIPB and MIPC are only found in mamiellophyceae and MIPD only in chlorophyceae and trebouxiophyceae. This might indicate that these MIPs have a shared ancestry and subfamilies only reflect the evolutionary distance between the different species. Although, the phylogenetic tree presented in Figure 2 is consistent with an orthologous relationship between these algal MIPs, there is no significant support for the nodes connecting these three subfamilies. Furthermore, the ar/R selectivity filters are distinctly different, suggesting differences in substrate specificity and hence physiological function. For the plant MIPs shared between different phyla, our current understanding suggests several HGT events in the evolution of MIPs as the simplest explanation for the observed distribution and complex MIP families found in some algae and land plants. However, this could easily change as more algal genomes become available. Genomes of charophyte algae will be especially informative, bridging the gap between chlorophyte algae and land plants to give a clearer picture of the evolution of the plant MIPs.
In this article the first extensive identification and classification of algal MIPs is presented. 22 different MIPs from nine species are analysed and classified into seven distinct subfamilies, representing the wide variation of MIPs found in green algae. None of the analysed species lack MIPs completely but most of them only contain a single subfamily. The multitude of subfamilies found is less likely to have been present in a common ancestor of green algae, but rather appears to have evolved later in the different algal lineages by a combination of vertical inheritance, HGT, and recombination between MIP genes. In this work, algal members of two of the seven subfamilies present in land plants are identified for the first time, suggesting that these subfamilies had formed long before land plants appeared. We also suggest that concentration gradients posed by terrestrial habitats favoured the accumulation of the many variants of passive transporters, i.e. MIPs, found in extant land living algae and embryophytes.
Identification and annotation of algal MIP genes
The genomes of the algae Chlamydomonas reinhardtii, Volvox carteri, Coccomyxa sp. C-169, Chlorella NC64A, Micromonas pusilla CCMP1545, Micromonas RCC299, Ostreococcus lucimarinus, Ostreococcus RCC809 and Ostreococcus tauri, available at the Joint Genome Initiative  were searched for MIP encoding genes using tBLASTn. First the Coccomyxa genome was searched using amino acid sequences of MIPs from Physcomitrella patens and Chlamydomonas rheinhardtii as queries. The MIPs identified in this search were then also included as queries in tBLASTn searches of the other genomes.
Genome sequences around hits were inspected for existing gene models, which were evaluated and kept if found to accurately represent a MIP gene. If models were missing or likely to be incorrect, new models were made by manual annotations of the genomic sequences. When satisfactory models neither existed nor could be built, hits were believed to be pseudogenes and were excluded from the analysis. Gene models were evaluated by comparing their amino acid sequences to these of known MIPs, emphasizing the existence of conserved residues and constraints on the lengths of transmembrane and loop regions.
Initially a structural alignment was done using DeepView/Swiss-PdbViewer v4.0.1 and the structures of BtAQP1 (1J4N ), EcGLPF (1LDA, ), EcAQPZ (1RC2, ), SoPIP2;1 (1Z98, ), RnAQP4 (2D57, ), MmAQPM (2F2B, ), PfAQP (3C02, ), HsAQP5 (3D9S, ) and BtAQP0 (2B6P, ). This structural alignment was then used as reference when building the alignment used for phylogenetic analyses in MEGA4 . The sequence alignment used for the phylogenetic analysis was constructed by reducing the number reference sequences while trying to maintain the diversity, and by removing the highly variable N- and C-terminal regions of the sequences. The GI-numbers and amino acid sequence alignment (Nexus format) are provided as Additional files 6 and 3.
Maximum Likelihood analysis was carried out using the software PHYML (Version 2.4.4) . In the analysis the JTT amino acid substitution model was used, the proportion of invariable sites was set to be estimated, the number of substitution rate categories was set to 4 and the gamma distribution parameter was set to be estimated. To assess the robustness of the best tree bootstrapping with 1000 replicates was performed. For the remaining parameters the default settings were used.
For Bayesian Inference analysis, the program MrBayes (Version 3.1.2) was used [18, 50]. The analysis was run with default setting with the following changes: (1) In the likelihood model used, a portion of the sites were invariable while the rate variation of other sites were assumed to be gamma distributed, (2) The rate matrix for amino acid substitution was set to "mixed model", in which the Markov chain samples each model according to its probability, (3) The analysis was set to include 5 chains per run with a temperature of 0.2 and for each chain to run for 2 000 000 generations, sampling every 100th tree. The first 25% of the sampled trees were discarded as burn in for the analysis.
IceLogos for positions 196-233 (SoPIP2;1 numbering) of the MIPEs, the algal PIPs and for P. patens PIPs were created in the iceLogo program (Version 1.2)  using the sampling mode. Corresponding positions from all sequences of the sequence alignment were used as the reference set. The sampling type was set to terminal with the terminal index 1 (N-terminus) and the iteration size to 500.
Divergence dating was performed using the BEAST software package under a relaxed molecular clock . The age of nine nodes was constrained by fossil evidence with prior probabilities distributed lognormally between a strict lower bound and a "soft" higher bound set as the 95% confidence interval. The protostomia/deuterostomia split was set to 531.5-551.9 MYA, the actinoptergyii/sarcopterygii split was set to 416.0-421.8 MYA, the archosauria/mammalian split to 312.3-330.5 MYA  and the bryophyte/polysporangiophyta split was set to 443.0-490.2 MYA . The alignments used were similar to the one used for the phylogenetic analyses but some sequences were added to encompass all of the calibration points and some were removed to reduce complexity. The analysis was based on amino acid sequences. For further details concerning in-data and settings consult the XML-files (Additional files 7 and 8).
Preston GM, Carroll TP, Guggino WB, Agre P: Appearance of water channels in Xenopus oocytes expressing red cell CHIP28 protein. Science. 1992, 256 (5055): 385-387. 10.1126/science.256.5055.385.
Echevarria M, Windhager EE, Tate SS, Frindt G: Cloning and expression of AQP3, a water channel from the medullary collecting duct of rat kidney. Proc Natl Acad Sci USA. 1994, 91 (23): 10997-11001. 10.1073/pnas.91.23.10997.
Ishibashi K, Kuwahara M, Gu Y, Kageyama Y, Tohsaka A, Suzuki F, Marumo F, Sasaki S: Cloning and functional expression of a new water channel abundantly expressed in the testis permeable to water, glycerol, and urea. J Biol Chem. 1997, 272 (33): 20782-20786. 10.1074/jbc.272.33.20782.
Ishibashi K, Sasaki S, Fushimi K, Uchida S, Kuwahara M, Saito H, Furukawa T, Nakajima K, Yamaguchi Y, Gojobori T, et al: Molecular cloning and expression of a member of the aquaporin family with permeability to glycerol and urea in addition to water expressed at the basolateral membrane of kidney collecting duct cells. Proc Natl Acad Sci USA. 1994, 91 (14): 6269-6273. 10.1073/pnas.91.14.6269.
Ma T, Frigeri A, Hasegawa H, Verkman AS: Cloning of a water channel homolog expressed in brain meningeal cells and kidney collecting duct that functions as a stilbene-sensitive glycerol transporter. J Biol Chem. 1994, 269 (34): 21845-21849.
Fu D, Libson A, Miercke LJ, Weitzman C, Nollert P, Krucinski J, Stroud RM: Structure of a glycerol-conducting channel and the basis for its selectivity. Science. 2000, 290 (5491): 481-486. 10.1126/science.290.5491.481.
de Groot BL, Frigato T, Helms V, Grubmuller H: The mechanism of proton exclusion in the aquaporin-1 water channel. J Mol Biol. 2003, 333 (2): 279-293. 10.1016/j.jmb.2003.08.003.
Beitz E, Wu B, Holm LM, Schultz JE, Zeuthen T: Point mutations in the aromatic/arginine region in aquaporin 1 allow passage of urea, glycerol, ammonia, and protons. Proc Natl Acad Sci USA. 2006, 103 (2): 269-274. 10.1073/pnas.0507225103.
Danielson JA, Johanson U: Unexpected complexity of the aquaporin gene family in the moss Physcomitrella patens. BMC Plant Biol. 2008, 8: 45-10.1186/1471-2229-8-45.
Hedges SB, Blair JE, Venturi ML, Shoe JL: A molecular timescale of eukaryote evolution and the rise of complex multicellular life. BMC Evol Biol. 2004, 4: 2-10.1186/1471-2148-4-2.
Yoon HS, Hackett JD, Ciniglia C, Pinto G, Bhattacharya D: A molecular timeline for the origin of photosynthetic eukaryotes. Mol Biol Evol. 2004, 21 (5): 809-818. 10.1093/molbev/msh075.
Zimmer A, Lang D, Richardt S, Frank W, Reski R, Rensing SA: Dating the early evolution of plants: detection and molecular clock analyses of orthologs. Mol Genet Genomics. 2007, 278 (4): 393-402. 10.1007/s00438-007-0257-6.
Marin B, Melkonian M: Molecular phylogeny and classification of the Mamiellophyceae class. nov. (Chlorophyta) based on sequence comparisons of the nuclear- and plastid-encoded rRNA operons. Protist. 2010, 161 (2): 304-336. 10.1016/j.protis.2009.10.002.
DOE Joint Genome Institute. [http://www.jgi.doe.gov]
Anderca MI, Suga S, Furuichi T, Shimogawara K, Maeshima M, Muto S: Functional identification of the glycerol transport activity of Chlamydomonas reinhardtii CrMIP1. Plant & cell physiology. 2004, 45 (9): 1313-1319. 10.1093/pcp/pch141.
Guindon S, Gascuel O: A simple, fast, and accurate algorithm to estimate large phylogenies by maximum likelihood. Syst Biol. 2003, 52 (5): 696-704. 10.1080/10635150390235520.
Huelsenbeck JP, Ronquist F: MRBAYES: Bayesian inference of phylogenetic trees. Bioinformatics. 2001, 17 (8): 754-755. 10.1093/bioinformatics/17.8.754.
Kukulski W, Schenk AD, Johanson U, Braun T, de Groot BL, Fotiadis D, Kjellbom P, Engel A: The 5A structure of heterologously expressed plant aquaporin SoPIP2;1. J Mol Biol. 2005, 350 (4): 611-616. 10.1016/j.jmb.2005.05.001.
Tournaire-Roux C, Sutka M, Javot H, Gout E, Gerbeau P, Luu DT, Bligny R, Maurel C: Cytosolic pH regulates root water transport during anoxic stress through gating of aquaporins. Nature. 2003, 425 (6956): 393-397. 10.1038/nature01853.
Tornroth-Horsefield S, Wang Y, Hedfalk K, Johanson U, Karlsson M, Tajkhorshid E, Neutze R, Kjellbom P: Structural mechanism of plant aquaporin gating. Nature. 2006, 439 (7077): 688-694. 10.1038/nature04316.
Johansson I, Karlsson M, Johanson U, Larsson C, Kjellbom P: The role of aquaporins in cellular and whole plant water balance. Biochim Biophys Acta. 2000, 1465 (1-2): 324-342. 10.1016/S0005-2736(00)00147-4.
Gazzarrini S, Kang M, Epimashko S, Van Etten JL, Dainty J, Thiel G, Moroni A: Chlorella virus MT325 encodes water and potassium channels that interact synergistically. Proc Natl Acad Sci USA. 2006, 103 (14): 5355-5360. 10.1073/pnas.0600848103.
Gustavsson S, Lebrun AS, Norden K, Chaumont F, Johanson U: A novel plant major intrinsic protein in Physcomitrella patens most similar to bacterial glycerol channels. Plant physiology. 2005, 139 (1): 287-295. 10.1104/pp.105.063198.
Froger A, Rolland JP, Bron P, Lagree V, Le Caherec F, Deschamps S, Hubert JF, Pellerin I, Thomas D, Delamarche C: Functional characterization of a microbial aquaglyceroporin. Microbiology (Reading, England). 2001, 147 (Pt 5): 1129-1135.
Ishibashi K: Aquaporin subfamily with unusual NPA boxes. Biochim Biophys Acta. 2006, 1758 (8): 989-993. 10.1016/j.bbamem.2006.02.024.
Johanson U, Gustavsson S: A new subfamily of major intrinsic proteins in plants. Mol Biol Evol. 2002, 19 (4): 456-461.
Nozaki K, Ishii D, Ishibashi K: Intracellular aquaporins: clues for intracellular water transport?. Pflugers Arch. 2008, 456 (4): 701-707. 10.1007/s00424-007-0373-5.
Li GW, Peng YH, Yu X, Zhang MH, Cai WM, Sun WN, Su WA: Transport functions and expression analysis of vacuolar membrane aquaporins in response to various stresses in rice. Journal of plant physiology. 2008, 165 (18): 1879-1888. 10.1016/j.jplph.2008.05.002.
Becker B, Marin B: Streptophyte algae and the origin of embryophytes. Ann Bot. 2009, 103 (7): 999-1004. 10.1093/aob/mcp044.
Preston GM, Jung JS, Guggino WB, Agre P: The mercury-sensitive residue at cysteine 189 in the CHIP28 water channel. J Biol Chem. 1993, 268 (1): 17-20.
Schutz K, Tyerman SD: Water channels in Chara corallina. J Exp Bot. 1997, 48 (313): 1511-1518. 10.1093/jexbot/48.313.1511.
Newby ZE, O'Connell J, Robles-Colmenares Y, Khademi S, Miercke LJ, Stroud RM: Crystal structure of the aquaglyceroporin PfAQP from the malarial parasite Plasmodium falciparum. Nat Struct Mol Biol. 2008, 15 (6): 619-625. 10.1038/nsmb.1431.
Horsefield R, Norden K, Fellert M, Backmark A, Tornroth-Horsefield S, Terwisscha van Scheltinga AC, Kvassman J, Kjellbom P, Johanson U, Neutze R: High-resolution x-ray structure of human aquaporin 5. Proc Natl Acad Sci USA. 2008, 105 (36): 13327-13332. 10.1073/pnas.0801466105.
Heymann JB, Engel A: Structural clues in the sequences of the aquaporins. J Mol Biol. 2000, 295 (4): 1039-1053. 10.1006/jmbi.1999.3413.
McDonald SM, Plant JN, Worden AZ: The mixed lineage nature of nitrogen transport and assimilation in marine eukaryotic phytoplankton: a case study of micromonas. Molecular biology and evolution. 2010, 27 (10): 2268-2283. 10.1093/molbev/msq113.
Darienko T, Gustavs L, Mudimu O, Menendez CR, Schumann R, Karsten U, Friedl T, Proschold T: Chloroidium, a common terrestrial coccoid green alga previously assigned to Chlorella (Trebouxiophyceae, Chlorophyta). Eur J Phycol. 2010, 45 (1): 79-95. 10.1080/09670260903362820.
Gustavs L, Eggert A, Michalik D, Karsten U: Physiological and biochemical responses of green microalgae from different habitats to osmotic and matric stress. Protoplasma. 2010, 243 (1-4): 3-14. 10.1007/s00709-009-0060-9.
Hoshina R, Kato Y, Kamako S, Imamura N: Genetic evidence of "American" and "European"' type symbiotic algae of Paramecium bursaria Ehrenberg. Plant Biology. 2005, 7 (5): 526-532. 10.1055/s-2005-865912.
Luyten K, Albertyn J, Skibbe WF, Prior BA, Ramos J, Thevelein JM, Hohmann S: Fps1, a yeast member of the MIP family of channel proteins, is a facilitator for glycerol uptake and efflux and is inactive under osmotic stress. EMBO J. 1995, 14 (7): 1360-1371.
Cerda J: Molecular pathways during marine fish egg hydration: the role of aquaporins. J Fish Biol. 2009, 75 (9): 2175-2196. 10.1111/j.1095-8649.2009.02397.x.
Fabra M, Raldua D, Power DM, Deen PM, Cerda J: Marine fish egg hydration is aquaporin-mediated. Science. 2005, 307 (5709): 545-10.1126/science.1106305.
Sui H, Han BG, Lee JK, Walian P, Jap BK: Structural basis of water-specific transport through the AQP1 water channel. Nature. 2001, 414 (6866): 872-878. 10.1038/414872a.
Tajkhorshid E, Nollert P, Jensen MO, Miercke LJ, O'Connell J, Stroud RM, Schulten K: Control of the selectivity of the aquaporin water channel family by global orientational tuning. Science. 2002, 296 (5567): 525-530. 10.1126/science.1067778.
Savage DF, Egea PF, Robles-Colmenares Y, O'Connell JD, Stroud RM: Architecture and selectivity in aquaporins: 2.5 Å X-ray structure of aquaporin Z. PLoS Biol. 2003, 1 (3): E72-
Hiroaki Y, Tani K, Kamegawa A, Gyobu N, Nishikawa K, Suzuki H, Walz T, Sasaki S, Mitsuoka K, Kimura K, et al: Implications of the aquaporin-4 structure on array formation and cell adhesion. J Mol Biol. 2006, 355 (4): 628-639. 10.1016/j.jmb.2005.10.081.
Lee JK, Kozono D, Remis J, Kitagawa Y, Agre P, Stroud RM: Structural basis for conductance by the archaeal aquaporin AqpM at 1.68 Å. Proc Natl Acad Sci USA. 2005, 102 (52): 18932-18937. 10.1073/pnas.0509469102.
Gonen T, Cheng Y, Sliz P, Hiroaki Y, Fujiyoshi Y, Harrison SC, Walz T: Lipid-protein interactions in double-layered two-dimensional AQP0 crystals. Nature. 2005, 438 (7068): 633-638. 10.1038/nature04321.
Tamura K, Dudley J, Nei M, Kumar S: MEGA4: Molecular Evolutionary Genetics Analysis (MEGA) software version 4.0. Mol Biol Evol. 2007, 24 (8): 1596-1599. 10.1093/molbev/msm092.
Ronquist F, Huelsenbeck JP: MrBayes 3: Bayesian phylogenetic inference under mixed models. Bioinformatics. 2003, 19 (12): 1572-1574. 10.1093/bioinformatics/btg180.
Colaert N, Helsens K, Martens L, Vandekerckhove J, Gevaert K: Improved visualization of protein consensus sequences by iceLogo. Nat Methods. 2009, 6 (11): 786-787. 10.1038/nmeth1109-786.
Drummond AJ, Rambaut A: BEAST: Bayesian evolutionary analysis by sampling trees. BMC Evol Biol. 2007, 7: 214-10.1186/1471-2148-7-214.
Benton MJ, Donoghue PC: Paleontological evidence to date the tree of life. Mol Biol Evol. 2007, 24 (1): 26-53.
Kenrick P, Crane PR: The origin and early diversification of land plants: a cladistic study. 1997, Washington, D.C.; London: Smithsonian Institution Press
Johanson U, Karlsson M, Johansson I, Gustavsson S, Sjovall S, Fraysse L, Weig AR, Kjellbom P: The complete set of genes encoding major intrinsic proteins in Arabidopsis provides a framework for a new nomenclature for major intrinsic proteins in plants. Plant physiology. 2001, 126 (4): 1358-1369. 10.1104/pp.126.4.1358.
Sakurai J, Ishikawa F, Yamaguchi T, Uemura M, Maeshima M: Identification of 33 rice aquaporin genes and analysis of their expression and function. Plant & cell physiology. 2005, 46 (9): 1568-1577. 10.1093/pcp/pci172.
Sade N, Vinocur BJ, Diber A, Shatil A, Ronen G, Nissan H, Wallach R, Karchi H, Moshelion M: Improving plant stress tolerance and yield production: is the tonoplast aquaporin SlTIP2;2 a key to isohydric to anisohydric conversion?. New Phytol. 2009, 181 (3): 651-661. 10.1111/j.1469-8137.2008.02689.x.
Daniels MJ, Chaumont F, Mirkov TE, Chrispeels MJ: Characterization of a new vacuolar membrane aquaporin sensitive to mercury at a unique site. The Plant cell. 1996, 8 (4): 587-599.
Liu LH, Ludewig U, Gassert B, Frommer WB, von Wiren N: Urea transport by nitrogen-regulated tonoplast intrinsic proteins in Arabidopsis. Plant physiology. 2003, 133 (3): 1220-1228. 10.1104/pp.103.027409.
Loque D, Ludewig U, Yuan L, von Wiren N: Tonoplast intrinsic proteins AtTIP2;1 and AtTIP2;3 facilitate NH3 transport into the vacuole. Plant physiology. 2005, 137 (2): 671-680. 10.1104/pp.104.051268.
Lebrun AS: Towards functional and structural characterization of maize ZmSIP proteins belonging to a divergent aquaporin subfamily. 2010, Louvain-la-Nouve: Université catholique de Louvain
Ma JF, Tamai K, Yamaji N, Mitani N, Konishi S, Katsuhara M, Ishiguro M, Murata Y, Yano M: A silicon transporter in rice. Nature. 2006, 440 (7084): 688-691. 10.1038/nature04590.
Ma JF, Yamaji N, Mitani N, Xu XY, Su YH, McGrath SP, Zhao FJ: Transporters of arsenite in rice and their role in arsenic accumulation in rice grain. Proc Natl Acad Sci USA. 2008, 105 (29): 9931-9935. 10.1073/pnas.0802361105.
Daniels MJ, Mirkov TE, Chrispeels MJ: The plasma membrane of Arabidopsis thaliana contains a mercury-insensitive aquaporin that is a homolog of the tonoplast water channel protein TIP. Plant physiology. 1994, 106 (4): 1325-1333. 10.1104/pp.106.4.1325.
We are grateful to the U.S. Department of Energy Joint Genome Institute for sequencing the algal genomes and making the sequences available to the public. We would also like to thank Prof. Per Kjellbom for valuable discussions on the PhD loop. This work was supported by grants from the Swedish Research Council.
JÅHD and UJ conceived and designed the study, JÅHD collected and prepared the primary dataset, HIA did all divergence dating, JÅHD and HIA contributed equally to the phylogenetical analyses. All authors participated in drafting and writing of the final manuscript.
Hanna I Anderberg, Jonas ÅH Danielson contributed equally to this work.
Electronic supplementary material
Authors’ original submitted files for images
Below are the links to the authors’ original submitted files for images.
About this article
Cite this article
Anderberg, H.I., Danielson, J.Å. & Johanson, U. Algal MIPs, high diversity and conserved motifs. BMC Evol Biol 11, 110 (2011) doi:10.1186/1471-2148-11-110
- Land Plant
- High Posterior Density
- Horizontal Gene Transfer Event
- Plasma Membrane Intrinsic Protein