- Research article
- Open Access
Unexpected link between polyketide synthase and calcium carbonate biomineralization
© Hojo et al.; licensee BioMed Central. 2015
Received: 19 September 2014
Accepted: 15 October 2014
Published: 13 January 2015
Calcium carbonate biominerals participate in diverse physiological functions. Despite intensive studies, little is known about how mineralization is initiated in organisms.
We analyzed the medaka spontaneous mutant, ha, defective in otolith (calcareous ear stone) formation. ha lacks a trigger for otolith mineralization, and the causative gene was found to encode polyketide synthase (pks), a multifunctional enzyme mainly found in bacteria, fungi, and plant. Subsequent experiments demonstrate that the products of medaka PKS, most likely polyketides or their derivatives, act as nucleation facilitators in otolith mineralization. The generality of this novel PKS function is supported by the essential role of echinoderm PKS in calcareous skeleton formation together with the presence of PKSs in a much wider range of animals from coral to vertebrates.
The present study first links PKS to biomineralization and provides a genetic cue for biogeochemistry of carbon and calcium cycles.
Biominerals are produced by living organisms through genetically controlled biological processes, and confer stability, rigidity, defences and functionality to organisms; examples include grass opal (rice; silicate), shell (shellfish; calcium carbonate), and bone/teeth (vertebrate; hydroxyl apatite) [1,2]. The addition of organic components determines organism-specific shape, size, hardness and crystallographic axis orientation of biominerals . Among biominerals, calcium carbonate is the most abundant and is known to play an important role in the global biogeochemical cycles of carbon and calcium through reef building and massive precipitation by calcifying algae in the ocean [4-6], and thus has attracted much attention, together with calcium phosphate mineralization of vertebrate skeleton and teeth.
The biomineral crystallization begins with nucleation through the phase of prenucleation clusters [7,8]. Experimental and modeling studies proposed that nucleation from saturated solution is not a simple event, but is preceded by a phase of amorphous precursors, such as amorphous calcium carbonate (ACC) or amorphous calcium phosphate, depending on the type of biominerals. These precursors then coalesce and rearrange to form nuclei, a core of subsequent crystal growth, a process called ‘nucleation’. Although these processes of biomineralization are well described, the underlying mechanism, particularly regarding the initial nucleation step, remains a mystery.
Otoliths (ear stones) in teleost fish are composed of calcium carbonate and organic materials (0.2–10%) , and primarily function in gravity and motion sensing, providing excellent systems for biochemical and genetic analyses of the mechanisms of calcium carbonate biomineralization. Factors involved in initial step of mineralization have not been definitively identified thus far, except for a report that glycogens are always found in the core of nascent otoliths . This is in part due to the lack of genetic studies targeting otolith mineralization. Indeed, while most zebrafish otolith mutants exhibit defects in the number, shape, and position, only a few completely lack otoliths, and in the cases where the causal gene was identified, its function in the context of mineralization remained unclear [11,12].
To gain insights into the crystallization of calcium carbonate in organisms, we analyzed the medaka spontaneous and homozygous viable mutant, ha, defective in otolith formation. Positional cloning identified a mutation in a novel gene encoding polyketide synthase (pks), named OlPKS, specifically expressed in the otic vesicle at the onset of mineralization. We demonstrate that the compound synthesized by OlPKS is secreted in the endolymph and it acts as a nucleation facilitator in otolith mineralization. Furthermore, sea urchin pks-2 expressed in skeletogenic cells was found to be indispensable for the formation of spicules, calcareous larval skeletons, indicating the generality of a novel link between calcium carbonate biomineralization and animal polyketide synthase.
Materials and methods
Fish strains and mapping
The medaka (Oryzias latipes) d-rR strain was used as a wild-type. ha was isolated as a spontaneous mutant by Tomita . ki79 was isolated from a ENU-mediated mutant screening (at the Tokyo Institute of Technology, Japan). Mapping of the ha locus was carried out as previously described .
Alizarin Red staining for visualizing mineralized otoliths was essentially done as described . Embryos were fixed with 4% PFA/2× PBS (phosphate buffered saline) containing 1% sodium hydroxide for three hours at room temperature. The samples were then washed with PBS several times, and stained with 2% Alizarin Red S/1% sodium hydroxide solution overnight. After quickly washing with 0.5% KOH, samples were mounted in 80% glycerol.
Transmitted electron microscopy
Embryos were fixed with 2% PFA and 2% glutaraldehyde buffered in 0.1 M cacodylate buffer and postfixed in 2% OsO4 in 0.1 M cacodylate buffer. Uranyl acetate and lead stain solution were used for contrast enhancement. The specimens were embedded in Quetol-812. Ultrathin sections (70 nm) were analyzed and documented with an electron microscope (JEOL, JEM-1400 Plus).
Whole-mount in situ hybridization
Immunofluorescence for OMP-1 was performed as previously described Murayama et al. , whereas staining for acetylated α-tubulin, OlPKS and PKC ζ were done as previously described by Kamura et al.  (see Additional file 1). Polyclonal rabbit OlPKS [amino acids 1520–1711] antibodies were raised by immunization of rabbits with bacterially expressed His-tagged truncated proteins.
Morpholino knockdown and mRNA rescue in medaka embryos
The morpholino antisense oligonucleotide (MOs; Gene Tools LLC) for first-Met of OlPKS was as follows: 5'-AACCACGGCTATTCCGTCCTCCATG-3'. in vitro syntheses of mRNAs were conducted as reported previously . Full length of olpks was isolated from the d-rR strain by RT-PCR. The sequences of primers are described in Additional file 1 (Whole-mount in situ hybridization). For injection of olpks mRNA with active site mutation, ki79 fish was used, because it likely carries a null mutation. Amino acid of the active site in each enzymatic domain was substituted as followed (with nucleotide sequences): KS, 173Cys → Asn (TGC → AAC); AT, 608Ser → Ala (TCC → GCA); DH,914His → Ala (CAC → GCC); KR,1859Tyr → Phe(TAC → TTC); ACP, 2010Ser → Ala(TCC → GCC); Loop (interdomain region; control), 435Thr → Ala(ACC → GCC) [20-22]. Microinjection of MO or mRNAs was carried out as previously described .
Animal type I PKS sequences were retrieved by TBLASTN against genome sequences of each species or BLASTP search against nr-protein database using the OlPKS sequence. For each candidates, domain search was done by Pfam sequence search, and amino acid sequences having basic PKS domains KS and AT, and additional domains (e.g., DH, KR, ER, ACP etc.) were defined as an animal type I PKS.
Generation the ha chimeric medaka
Transplantation experiments were performed based on the previous works . [Tg (β-actin:DsRed)] were used as wt-cell donors, whereas ha fish were prepared as hosts. Whether otoliths were formed or not and how many fluorescence cell were contained were confirmed by observations around st. 29 using a confocal fluorescence microscope (Zeiss, LSM710). A transplantation experiment was conducted as a negative control in which [ha −/−; Tg (β-actin:DsRed)] animal was used as the donors (detailed in Additional file 1).
OlPKS expression in A. oryzae and medaka rescue assay
The entire OlPKS ORF was amplified and subcloned into a fungal expression vector, pTAex3. The resulting expression plasmid pTA-olpks was used for transformation of A. oryzae M-2-3 according to the protoplast-PEG method described by Gomi et al. . The mycelia of transformants were extracted with acetone, followed purification using partition between ethyl acetate/H2O two times and the ethyl acetate layer was concentrated to dryness, and partitioned between hexane/90% methanol. The methanol layer was concentrated to dryness to give the material for medaka assay. Each extracts re-dissolved in DMSO was added to the medium in which ha medaka embryos were incubated. (detailed in Additional file 1).
Morpholino knockdown in sea urchin embryos
Microinjection of MOs was carried out as described previously with some modifications  (see Additional file 1). MOs (Gene Tools LLC) for first-Met blocking and their five-mispair controls were as follows (small letters in control sequences indicate substituted nucleotides).
hppks-1: 5'-CTGGTTTTATTGCTTCCCATGTTGA-3', hppks-2: 5'-CCCTCCAACTATCTTCCATAACTCA-3', hppks-1 control: 5'- CTGcTaTTATTcCTTCCgATcTTGA -3', hppks-2 control: 5'-CCgTgCAAgTATgTTCgATAACTCA-3'.
The ha embryo fails to mineralize otoliths
In ha mutant embryos, the OV, macula and cilia develop normally (Additional file 2A to D, I and J), and seeding particles are floating in the OV (Figure 1A and Additional files 3 and 4). Furthermore, organic materials such as OMP-1, a major soluble organic matrix protein, are secreted into the endolymph (Figure 1B) (other known organic components, starmaker-like and sparc are normally expressed in the OV (Additional file 2E and F)). Nevertheless, in ha mutants, mineralized stones never form (Figure 1A and C), but instead OMP-1-positive particles precipitate in the endolymph (Figure 1A Inset and B). This was further supported by TEM observation; fine substances (Figure 1D and D′, arrows), probably organic substances supplied by seeding particles, were accumulated around the epithelium in ha (Figure 1D Right and 1D’ Right), instead of growing otoliths (Figure 1D Left and D′ Left, asterisks). In wild-type (wt) OVs, fine particles were compacted into a round ‘globule’ (Figure 1D Left, ‘g’; ), and the globules then form otoliths by coalescing near the macula (Figure 1D asterisks; see also Additional file 2G). Taken together, in ha embryos, otolith mineralization is completely inhibited, even though major organic materials are supplied into the endolymph.
ha gene encodes a polyketide synthase
Using positional cloning, we narrowed down the ha locus to a 64.7 kb region in linkage group 20, which contains four open reading frames (ORFs 1–4). Sequencing analysis identified a 9-nucleotide deletion (3-amino acid deletion) in ORF 2 that encodes a type I polyketide synthase (PKS) (Figure 2A). We thereafter named this gene Oryzias latipes polyketide synthase (olpks). The olpks transcript is 6153 nt in length, comprises six exons, and encodes a 2051 amino acid protein. PKSs are multifunctional enzymes mainly found in bacteria, fungi and plant, and catalyze the biosynthesis of a diverse group of second metabolite, polyketides, some of which are used for pharmaceuticals with antibiotic and mycotoxic properties . Type I PKS has a set of distinct enzymatic domains that individually catalyze a series of reactions, to produce a final compound. Likewise, OlPKS contains five distinct domains: ketoacyl synthase (KS), acyl transferase (AT), dehydratase (DH), ketoreductase (KR), and acyl carrier protein domain (ACP) (Figure 2B). Essential amino acid sequence motifs for the function of each domain are conserved in OlPKS (Additional file 5B). The vertebrate fatty acid synthase (FAS), essential for all organisms, is thought to be an evolutionary subset of this family [34,35]. Animal FASs and another iterative type I PKSs share a conserved structure that includes KS, AT and ACP domains. FASs contain additional enzymatic domains such as KR, DH, ER and TE, which are present on different PKSs in different combinations. OlPKS possesses the minimal module (KS, AT and ACP) and additional KR and DH domains (Figure 2B and Additional file 5B).
Otolith formation in MO or mRNA of OlPKS
olpks first-Met MO
Active site mutation
Type I PKSs found in animal lineage
Type 1 PKS?
Corresponding RNA (Unigene or RNA)?
Homo sapiens GRCh37.p13
Bos taurus UMD3.
Canis (lupus) familiaris
Canis lupus familiaris CanFam3.1
Tursiops truncatus turTur1
Mus musculus GRCm38.p1
PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like
mycocerosic acid synthase-like [Sarcophilus harrisii (Tasmanian devil)]
LOC100091954 fatty acid synthase-like [Ornithorhynchus anatinus (platypus)]
LOC100091954 (pseudo gene)
N.A (pseudo gene)
PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like is oformX2 [Gallus gallus].
Yes (brain; connective, blood)
PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like [Taeniopygia guttata].
PREDICTED: Taeniopygia guttata phthioceranic/hydroxyphthioceranic acid synthase-like
PREDICTED: probable polyketide synthase 1-like [Falco peregrinus].
PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like [Anolis carolinensis].
PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like [Anolis carolinensis].
PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like [Anolis carolinensis].
Green sea turtle
Phthioceranic/hydroxyphthioceranic acid synthase [Chelonia mydas].
Polyketide synthase Pks N [Chelonia mydas]
PREDICTED: uncharecterized protien LOC101936604 [Chrysemys picta bellii]
PREDICTED: uncharecterized protien LOC101937174 [Chrysemys picta bellii]
Chinese soft shell turtle
Scaffold no. JH209275.1
Xenopus (Silurana) tropicalis
Tropical clawed toad
Xenopus (Silurana) tropicalis build 1 genome database (v4.2 assembly)
OIPKS (PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase-like [Oryzias latipes])
Oryzias latipes ASM31367v1
OIPKS-2 (PREDICTED: phthioceranic/hydroxyphthioceranic acid synthase type I P ps D-like [Oryzias latipes])
OIPKS-3 (PREDICTED: probable polketide synthase 1-like [Oryzias latipes])
Danio rerio wu:fc01d11 (wu: fc01d11),mRNA
Danio rerio Zv9
phthioceranic/hydroxyphthioceranic acid synthase-like
PREDICTED: Takifugu rubripes lovastatin nonaketide synthase-like (LOC101079519), mRNA
hypothetical protien BRAFLDRAFT_205831, partial [Branchiostoma floridae].
Branchiostoma floridae v1.0
hypothetical protien BRAFLDRAFT_247081 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_90481 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_96868 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_96863 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_87472 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_125690 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_91451 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_87410 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_89867 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_87413 [Branchiostoma floridae]
hypothetical protien BRAFLDRAFT_125650 [Branchiostoma floridae]
Gene ID: 7207596
hypothetical protien BRAFLDRAFT_71890 [Branchiostoma floridae]
Gene ID: 7224978
PREDICTED: fatty acids synthase-like
Ciona intestinalis KH
Strongy locentrotus purpuratus
Purple sea urchin
LOC588806 probable polyketide synthase 1-like [Strongylocentrotus purpuratus (purple sea urchin)]
LOC592147 polyketide synthase 2
Nematostella vectensis v1.0
Protein C41A3.1 [Caenorhabditiselegans]
Drosophila melanogasterRelease 5
Based on above results, we conclude that OlPKS is only required for the early step of otolith mineralization and that the mutation in olpks is responsible for the ha phenotype.
OlPKS produces lipophilic substances secreted into the endolymph
We hypothesized that, similar to other PKSs, OlPKS synthesizes polyketide-related small compounds in the OV epithelium, which are then secreted into the endolymph for the initial step of otolith mineralization.
Next, we performed a chimera experiment in which DsRed-expressing wt cells was transplanted into mutant blastula, and examined for otolith formation when wt donor cells colonized mutant OVs (Figure 3B). Remarkably, irrespective of their number and localization within the OV, wt cells effectively restored otolith formation at the appropriate time and location, the macula region, in ha embryos. Only a few cells, located at any region of the vesicle, were found to be sufficient (Figure 3C and Additional file 6A and B).
Finally, we adopted a heterologous expression system to characterize substances synthesized by OlPKS. Since large-scale expression of PKSs has been established in Aspergillus oryzae , we introduced the olpks cDNA into A. oryzae, expecting that exogenous PKS (i.e., OlPKS) could work using endogenous substrates such as acetyl-CoA and malonyl-CoA in fungal cells like their own PKSs (Figure 3D). OlPKS expression in transformed fungi was confirmed by western-blotting (Additional file 6C). Since polyketide-derivatives exhibit moderate hydrophobic nature, we extracted cultivated mycelia with acetone, followed by purification using partition between ethyl acetate/H2O and subsequent purification. We then attempted a simple in vivo assay in which ha mutant embryos were cultured with an aliquot of the extracts (Figure 3D). Remarkably, these extracts restored otolith mineralization in ha embryos, while no such rescue was observed with control extracts (Figure 3E). Taken together, these data demonstrate that it is not OlPKS but ethyl-acetate extractable substances synthesized by OlPKS and secreted into the endolymph that nucleate otolith mineralization.
Broad distribution and conserved roles of polyketide synthases in animals
We hypothesized that like medaka PKSs, some of the other animal PKSs participate in biomineralization, more specifically calcium carbonate mineralization. To test this idea, we focused on echinoderm pks-2 because its reported expression is in primary mesenchyme cells (PMCs) that give rise to spicules, larval skeletons made of calcium carbonate [38,43]. We first confirmed the PMC-specific expression of pks-2 in our experimental system, Hemicentrotus pulcherrimus (hppks-2). Importantly, the expression of sea urchin pks-2 disappears around late gastrula stage just after PMCs begin to form spicules (Figure 4B Lower Panel). We then examined the function of HpPKS-2 by injecting HpPKS-2 MO. As shown in Figure 4C, HpPKS-2 morphants exhibited severe defects in spicule formation while control MO-injected embryos appeared normal (Figure 4C and Additional file 7C). Another echinoderm pks gene, hppks-1 was found to contribute to pigmentation as previously reported  (Figure 4B Upper Panel and C, and Additional file 7C). We thus conclude that echinoderm pks-2 plays a critical role in the formation of calcareous skeletal elements in larva.
We here show that olpks encoded by the ha locus is essential for the early step of otolith biomineralization in medaka. In ha mutant embryos, mineralized stones never form, but instead OMP-1-positive particles precipitate in the endolymph. Our TEM observation confirmed that crystal growth is never initiated in ha OV despite the accumulation of otolith materials (Figure 1D), suggesting that the product of OlPKS participates in the initial step, in particular, nucleation of mineralization. The expression pattern of olpks supports its early function; the expression is transient and disappears by the onset of otolith formation (Figure 2D). This pattern of expression contrasts sharply with that of other essential genes identified so far. For instance, otolin-1 and omp-1 expression begins at st. 25 and persists into adulthood as these proteins continue to be deposited on growing otoliths throughout life [44,45]. Furthermore, the expression of medaka starmaker (called starmaker-like), a key regulator of the crystal lattice of calcium carbonates , is detected at st. 21 and is again maintained at later stages . Intriguingly, ha fry develop an otolith-like stone (Additional file 2H), and some adult ha fish finally have otolith-like stones, albeit with abnormal shape and size . This does not occur in zebrafish ‘no-otolith’-type mutants such as backstroke and keinstein . These facts further suggest that the endolymph of ha only lacks a trigger. In ha, continuous supply of otolith materials without crystallization could lead to abnormal development of the inner ear and irregular stone formation at later stages. Together with these phenotypic and expression analyses, we conclude that the product of OlPKS functions as a nucleation trigger (facilitator).
Despite our efforts to identify the product of OlPKS, it remains elusive; we failed to detect any specific peak of the synthesized compound in HPLC analysis using extracts of A. oryzae transformed with olpks, probably due to low production of the compound. However, the active substance could have amphiphilic nature like other polyketide (e.g., phenolic lipids ) because it was re-solved in medaka culture medium and penetrates into the otic vesicle of the embryo in the rescue experiment (Figure 3D). Given its amphiphilic nature, the product of OlPKS could serve as a bridge between ACC and organic components such as soluble matrix protein (e.g., OMP-1) and/or insoluble scaffold matrices (e.g., Otolin-1)(the possible functions of these organic compounds in biomineralization were proposed by Nagasawa ). Supporting this idea, in studies of High-resolution Cryo-TEM imaging, monolayers of fatty acids (arachidic acid or stearic acid) that are also amphiphilic in nature, have been used to artificially induce crystal nucleation [7,51]. Further investigation using cell-free systems [52,53] will be necessary to address at which step of biomineralization PKS products actually work.
Otolith formation shares many features with the formation of vertebrate bones consisting of calcium phosphate (hydroxyapatite) minerals, the best characterized calcification process to date . Intriguingly, in bone formation, phospholipid such as phosphatidylserine (PS) has been implicated in an inducer of hydroxyapatite mineralization and most likely acts as a nucleation facilitator [52,55,56]. Since PS is a small substance with amphiphilic nature, the product of OlPKS could be a functional counterpart in calcium carbonate mineralization, interacting with calcium ions, ACC and matrix proteins.
The phylogenetic analysis based on the KS domain demonstrates the topology in which animal PKSs are separated from the animal FAS clade (Additional file 7A). Unlike the fas gene, the distribution of pks genes in animals is irregular; they are not found in some animal groups, for examples, fly, frog, and mammal, which represent some of the most intensively studied model animals (Figure 4A). These facts complicate the evolutionary origin of animal pks genes, while a single origin of animal fas has been repeatedly supported. Horizontal gene transfer, gene duplications and gene losses could have occurred during evolution, as proposed in bacteria/fungi PKSs [57-59]. Among those animal pks genes, sea urchin pks-2 could be functionally equivalent to olpks because of its early and transient expression in the calcifying cell lineage and its knockdown phenotype, although the domain architecture of sea urchin PKS-2 differs to some degree from that of OlPKS, being KS-AT-DH-ER-KR-ACP-TE and KS-AT-DH-KR-ACP, respectively .
Given the conserved role of medaka and sea urchin PKSs, calcium carbonate biomineralization could generally require the products of PKSs for nucleation. PKSs could participate in the production of coral skeletons and calcification of algae in the ocean. For instance, Emiliania huxleyi [58,60] has some pks genes (e.g., fgeneshEH_pg.50__74, protein ID103465, Joint Genome Institute (http://genome.jgi-psf.org/pages/search-for-genes.jsf?organism=Emihu1)). Intriguingly, the presence of PKS in Cnidaria appears to be associated with biomineraliztion; coral (A. digitifera) has a couple of pks genes, whereas Hydra magnipapillata and Nematostella vectensis do not. Furthermore, pks genes of bird and reptile might be involved in production of egg shells. In frogs and mammals, however, pks genes were no longer needed and lost during evolution, although their inner ears still contain calcium carbonate biominerals. This inconsistency may be explained by the fact that their biominerals do not form large stones, but instead small grains called otoconia. However, further intense search in those animals which appear to have lost pks genes will definitely be needed.
The present study addresses the function of the vertebrate pks gene and demonstrates its vital role in calcium carbonate biomineralization. Further functional analyses of newly identified PKSs will uncover a long-overlooked world of polyketides and their derivatives in animals. Our finding also provides genetic and molecular cues for the geochemical study of global carbon and calcium cycles.
pks genes reported herein have been deposited in GenBank with accession numbers as follow: olpks [AB923905], hppks-1 [AB923906] and hppks-2 [AB923907].
We thank Dr. Hiromichi Nagasawa for providing anti- O. mykiss OMP-1 serum; Dr. Joachim Wittbrodt for providing the cDNA of pax2; Dr. Akira Kudo for providing the ki79 fish; Yasuko Ozawa for excellent fish care; Sayaka Tayama for her contribution to the chimeric experiment. Members of the Yasuo Ohnishi laboratory, past and present, are acknowledged, particularly Adeline Muliandi, Takayuki Hayashi and Takuya Makino.
This work was supported in part by Exploratory Research ("Houga Kenkyu") Grant-in-Aid for Scientific Research from the Ministry of Education, Culture, Sports, Science and Technology.
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