Abstract
Mechanisms for making and breaking the heme b cofactor (heme) are more diverse than previously expected. Biosynthetic pathways have diverged at least twice along taxonomic lines, reflecting differences in membrane organization and O2 utilization among major groups of organisms. At least three families of heme degradases are now known, again differing in whether and how O2 is used by the organism and possibly the purpose for turning over the tetrapyrrole. Understanding these enzymes and pathways offers a handles for antimicrobial development and for monitoring heme use in organismal and ecological systems.
Introduction
Heme biosynthesis and degradation are important and highly regulated processes due to the significance of the cofactor and its breakdown products to cellular and organismal health. Over the past two decades, it has become clear that the biosynthetic steps for making heme are not universal [1]. The canonical pathway is limited to eukaryotic organisms and gram-negative bacteria, while gram-positive bacteria, archaea, and denitrifying and sulfate-reducing bacteria possess partly unique and more ancient ways to produce heme [2,3•] (Figure 1). By the same token, different groups of organisms break the heme tetrapyrrole under a variety of conditions using different catalytic strategies. Many discoveries along the heme synthesis and degradation pathways have been made fairly recently due to genome sequencing. Some significant ones are highlighted in this minireview.
Multiple Routes to Heme b
All known pathways to heme commence with the irreversible synthesis of 5-aminolevulinic acid (ALA), are the same up to the intermediate uroporphyrinogen III, and then diverge along taxonomic lines. The “Alternate heme biosynthesis” (Ahb) pathway [3•], used by archaea/sulfate-reducing/denitrifying bacteria, was the first non-canonical pathway to be discovered (Figure 1). Uroporphyrinogen III is converted on this pathway to siroheme, the prosthetic group of sulfite and nitrite reductases. Siroheme is further processed into heme by AhbA, AhbB, AhbC, and AhbD (Figure 1) [3•]. The Ahb pathway offers a fully anaerobic route to heme and several of its intermediates for ancient organisms dwelling in anaerobic niches.
Coproporphyrinogen III, the product of the decarboxylation of uroporphyrinogen III by uroporphyrinogen decarboxylase (UroD), is the last common intermediate for the other two pathways. These begin with either a decarboxylation to yield protoporphyrinogen IX (protoporphyrin-dependent [(PPD) branch] or an oxidation step to yield coproporphyrin III (coproporphyrin-dependent [(CPD) branch]. The PPD branch is found in eukaryotes and gram negative bacteria, which make use of membrane-enclosed compartments to protect and steer toxic reactants (e.g., light-sensitive porphyrins, O2, H2O2, and Fe(II)). The CPD branch is used by gram positive bacteria, which lack either mitochondria or inner/outer membranes but must nonetheless exert control over similar substrates. Notably, the PPD branch has both O2-dependent and –independent catalysts for its two oxidative steps, suggesting that it can function under anaerobic conditions. One of the oxidative reactions of the CPD branch depends on H2O2 (ChdC); the electron acceptor for the other reaction (CgoX) has not been verified.
Decarboxylation of the Ring A- and B- Propionate Groups (CgdC, CgdH, and ChdC).
The first chemical transformation in the PPD branch is the oxidative decarboxylation of the ring A- and B- propionate groups to yield protoporphyrinogen IX (Figure 2). This reaction can be catalyzed by coproporphyrinogen decarboxylase (CgdC) or coproporphyrinogen dehydrogenase (CgdH) in an oxygen-dependent or -independent manner, respectively.
CgdC, found almost exclusively in mitochondria, is a dimeric membrane-bound enzyme [4] (Figure 3a). Its conserved active site base Asp is thought to facilitate direct, cofactor-independent reactions between the propionate side chains of coproporphyrinogen III and 2O2 [5••,6••·]. The reactions occur in a sequential and clockwise manner, yielding 2CO2 and 2H2O2. By contrast, CgdH is a soluble, monomeric, radical SAM (S-adenosylmethionine)/[4Fe-4S]-dependent enzyme that is exclusive to gram-negative bacteria and is structurally and mechanistically unrelated to CgdC (Figure 3) [7,8•, 9]. The 5’-deoxyadenosyl radical initiates the decarboxylation by stereospecific hydrogen-atom abstraction at the beta-position of the propionate side chains, producing a carbon radical [10]. This reaction requires an electron donor at the start of the reaction (to fill the iron-sulfur cluster electron hole) and an electron acceptor at the end (to quench the radical), neither of which has been identified [7]. As with CgdC, the decarboxylations are sequential and clockwise, generating 2CO2.
In the CPD branch, decarboxylation of the A- and B-ring propionate groups, by contrast, occurs at the end of the pathway. This reaction, catalyzed by coproheme decarboxylase (ChdC), occurs with ferric coproheme III acting as both substrate and cofactor, yielding heme as the final product (Figure 2) [2,12,13]. ChdC is evolutionarily and structurally unrelated to either CgdC or CgdH and is exclusive to gram-positive bacteria (Figure 3c). It is a member of the chlorite dismutase (Cld) family of proteins, which share a homopentameric structure [12]. Each ChdC monomer ChdC binds a coproheme III molecule. Oxidative decarboxylation is mediated by H2O2 and a conserved Tyr residue in the active site which forms a reactive radical, via a high-valent Fe(IV)=O(coproprophyrin▪+) intermediate [11,14,15]. Analogous to the 5’deoxyadenosyl radical in CgdH, the Tyr radical performs a hydrogen-atom abstraction at the beta-position of each reactive propionate, producing a radical in that position that leads to decarboxylation and formation of a vinyl group. Decarboxylation of the two propionates by ChdC also occurs in a clockwise fashion, generating 2CO2 and 4H2O. H2O2 is an unusual cellular substrate, particularly in catalase-rich organisms. Its source remains to be elucidated.
Oxidation of the Tetrapyrrole Rings (PgoX, PgdH1, PgdH2 and CgoX).
Diversity is most pronounced for the enzymes catalyzing oxidations of the tetrapyrrole ring. This penultimate step in the PPD branch is catalyzed by either PgoX, PgdH1, or PghH2, isofunctional enzymes that are non-homologous and structurally dissimilar [16].
Protoporphyrinogen oxidase (PgoX) catalyzes the six-electron oxidation of the protoporphyrinogen IX ring to protoporphyrin IX (PPIX) using O2. A total of 3O2/6H+ are consumed in three sequential rounds of oxidation, generating 3H2O2 and double bonds at all the meso-carbon positions [17,18•]. PgoX is a homodimeric, membrane-associated enzyme with a single FAD acting as a 2e- cofactor (Figure 4a). It is found almost exclusively in eukaryotes and a few gram-negative bacteria [19,20].
Protoporphyrinogen can also be oxidized by the O2-independent enzymes protoporphyrinogen dehydrogenase 1 and 2 (PgdH1, PgdH2). PgdH1 is found mainly in γ-proteobacteria. It is a membrane-bound member of the long-chain flavodoxin family whose members use FMN to mediate electron transfer reactions [20]. PgdH1 is thought to use respiratory electron carriers such as menadione and ubiquinone for catalysis, in lieu of O2 [5••, 19]. PgdH2 is present in heme-synthesizing, non-enteric gram-negative bacteria such as Acinetobacter (γ-proteobacteria) and Synechocystis (cyanobacteria), which lack both pgoX and pgdH1 [5••,19,21]. Although PgdH2 is the most abundant of the three isofunctional enzymes, little is known about its mechanism. No cofactor has been identified for PgdH2 and it has been reported that PgdH2 is not able to complement a PgdH1-deficient E. coli strain, emphasizing its distinction from PgdH1 [5••,20].
Along the CPD branch, oxidative conversion of coproporphyrinogen III to coproporphyrin III by coproporphyrinogen oxidase (CgoX) is the first committed step. CgoX bears strong similarities in sequence and structure to PgoX, including a non-covalently bound FAD molecule [16,22•]. However, CgoX is monomeric instead of dimeric and is reported to be cytoplasmic instead of membrane-associated [2,22•,23]. The most widely studied CgoX is from Bacillus subtilis. Comparison of its crystal structure (PDBID: 3I6D) [24] with PgoX structures from Myxococcus xanthus (PDBID: 3NKS) [25] and Nicotana tabacum (PDBID: 1SEZ) [17] showed that the CgoX active site is 2-3 times larger (1173 Å vs 450-550 Å) and significantly more positively charged, allowing it to accommodate its larger and more negatively charged substrate [22•]. CgoX has been described as having the same reaction mechanism as PgoX. However, studies on CgoX have been conducted with a protoporphyrinogen IX substrate, and the requirement for O2 as the electron acceptor has not been experimentally validated [24,26]. This begs the question of whether CgoX may catalyze its reaction in an O2-independent manner, particularly in the facultative anaerobes in which it is sometimes found as the only coproporphyrinogen-converting enzyme. Interestingly, the PgoX in Plasmodium falciparium catalyzes its reaction using NAD(P) as an electron acceptor under anaerobic conditions [27]. It is possible that the much larger active site in CgoX can accommodate an electron acceptor such as NAD(P); pi-stacking between FAD and the inhibitor acifluoren in the B.subtilis CgoX alludes to this possibility (Figure 4b).
Over the past two decades, it has been reported that CgoX, unlike PgoX, is a cytosolic enzyme [2,5••,23,28]. However, studies with recombinant B. subtilis CgoX have shown that CgoX is found in the cell membrane fraction when expressed in E. coli [24,26], and its purification required detergent and denaturing conditions to maintain the enzyme in solution [24]. These observations, along with the fact that CgoX contains the membrane-binding “Domain II” that is also found in PgoX enzymes [22•], suggest that CgoX may be membrane-associated.
Tetrapyrrole Metalation (PpfC, CdfC).
Insertion of Fe(II) into the oxidized tetrapyrrole occurs as the final step in the PPD branch, catalyzed by protoporphyrin IX ferrochelatase (PpfC) (Figure 2). PpfC is homodimeric and thought to localize to the inner mitochondrial membrane of eukaryotes and the inner cellular membrane of gram-negative bacteria [29]. Each monomer contains a [2Fe-2S] cluster that does not participate in catalysis [6••,29,30]. Notably, the PpfC structure has a so-called “active site lip” that assumes an open state in the apo-protein and a closed state upon PPIX binding. In the absence of substrate or upon product formation, the active-site lip reopens, becoming solvent-exposed for substrate entry or product egress (Figure 5a).
The PpfC reaction mechanism requires Fe(II) and PPIX binding, deprotonation of two pyrrole ring nitrogens in PPIX, Fe(II)-insertion into the macrocycle, and product release [5••,29,31,32]. Fe(II) is directly delivered to PpfC by frataxin (Frda in human, Yfh1 in yeast), a homotrimeric membrane-bound enzyme involved in iron storage and delivery to [Fe-S]-cluster and heme biosynthetic enzymes [33]. Frataxin directly interacts with PpfC and transfers Fe(II) to conserved His and Glu residues in the active site (Figure 6) [31,32]. Upon binding PPIX, the active site lip closes in, causing rearrangement of an active site hydrogen-bonding network and distortion to the planarity of the PPIX ring [5••,29,34]. Both conformational changes trigger pyrrole deprotonation via a well-conserved His residue, and facilitating metal insertion into the porphyrin. Protonation of the His also reorients its side-chain and causes the final conformational change in the PpfC reaction cycle: opening of the active site lip for product release [5••,29]. The mechanism of PpfC is assumed to be the same in eukaryotes and gram-negative bacteria; however, further characterization of bacterial enzymes is required to address known differences in the ligation and metal content of their [Fe-S] clusters [5••,30].
Metalation of the oxidized tetrapyrrole is the penultimate step of the CPD branch. Coproporphyrin ferrochelatase (CpfC) catalyzes insertion of iron into coproporphyrin III. CpfC has significantly lower binding affinities and reaction rates with PPIX, relative to PpfC [26,31]. Moreover, instead of a membrane-bound dimer, CpfC is a cytosolic monomer, and although similar in structure, CpfC shares less than 15% sequence identity with PpfC (Figure 5b) [2,26,29,31]. CpfC contains all of the conserved active site residues found in PpfC but lacks the active site lip, perhaps allowing for accommodation of its larger substrate, which binds in a different location than in PpfC (rotated ~100° and ~4.5Å further from the inside of the active site, leaving two propionate groups exposed to solvent). The porphyrin in CpfC still interacts with the conserved active site His, and CpfC binds Fe(II) in a similar manner with its His-Glu residues [31,32]. In the gram-positive B. subtilis, Fe(II) is directly delivered to CpfC by Fra, the B. subtilis frataxin homolog [33•,35] and metalation is thought to occur through a similar mechanism to PpfC, although further work with this enzyme and its substrate is needed.
Multiple ways to break heme
There are multiple reasons to degrade heme, and organisms from different taxonomic groups have evolved unique enzymes and pathways for doing so. Tetrapyrrole degradation allows for iron utilization or resorption in humans (during erythrocyte recycling) and in pathogenic bacteria (during infection through hemolysis and heme sequestration). In animals, heme turnover produces bilirubin and CO, which act systemically as signaling molecules. Heme is also a source of PPIX, used as a precursor for synthesis of photoactive compounds called phytochromes in cyanobacteria, red algae, and plants. Lastly, heme is a redox- and photo- active molecule which can cause oxidative stress. Complete degradation of heme and isolation of the iron is essential to not only pathogens, but also serves a self-protective function.
Heme as an iron source.
Heme can be non-enzymatically and non-stereospecifically degraded in the presence of either H2O2 or O2 with a reducing agent like ascorbate, releasing Fe(II), CO, and 4 isomers of the green product verdoheme [36,37]. By contrast, enzymes whose cellular role is to degrade heme (heme oxygenase, HO break the heme ring stereospecifically in an O2-dependent manner, usually producing α-verdoheme and CO [37,38•]. Reduction and addition of 2O2 yields α-biliverdin and Fe(II) (Figure 7). Mammalian isoform 1 of HO (HO1) is most abundant in the spleen, at the site of erythrocyte degradation and iron recycling. Soon after the discovery of HO1, prokaryotic homologs were found to catalyze the same reaction in pathogenic bacteria (e.g., HmuO in Corynebacterium and PigA/HemO in proteobacteria), this time as a way to harvest host-derived heme as a source of nutritional iron [37]. Termed canonical HOs, these enzymes have highly conserved α-helical structures, active sites with extensive hydrogen-bonding, and an α-helical loop that interacts with the distal side of the porphyrin and is responsible for stereospecific cleavage of heme at the α-meso carbon (Figure 8a) [39]. Because the heme ring is rotated ~100° in the PigA/HemO active site relative to the other HOs, this enzyme produces the β- and γ-products in a 3:7 ratio (Figure 8b) [36,37].
Conceivably as a way to avoid production of CO, an immune system activator, some organisms such as Staphylococcus aureus and Mycobacterium tuberculosis have a different mechanism for degrading heme. Known as IsdG-like HOs, IsdG or IsdI and MhuD are dimeric enzymes that have ferredoxin-like α-/β-folds that form a β-barrel at the monomer interface (Figure 8C and 8D, respectively) [37,40••]. Each monomer binds heme, distorting the planarity of the ring. Porphyrin ruffling is believed to promote stereospecific cleavage at the β- and δ- positions or the α-position in IsdG/I or MhuD, respectively [41,42]. The products of IsdG/I are β- and δ-staphylobilin, Fe(II), and formaldehyde, while cleavage by MhuD (where the heme ring is rotated ~90° relative to the heme in IsdG/I) forms a different linear tetrapyrrole, α-mycobilin, Fe(II), and no 1-carbon product (Figure 7). Interestingly, the major chlorophyll breakdown pathway in green plants uses O2 and a Rieske-type monooxygenase, pheophorbide a oxygenase, to generate a structural analog of α-mycobilin called red chlorophyll catabolite, Mg(II), and no 1-carbon product [43,44]. This enzyme bears no sequence or structural similarity to MhuD.
The IsdG-like HOs exhibit further diversity among the species yet studied. The pathogen L. monocytogenes, in addition to its IsdG-like HO, encodes another IsdG-like protein called Isd- LmHde. This protein shares structural similarity to IsdG, and binds and degrades heme at both domains and folds as a monomer instead of a dimer [37]. By contrast, S. aureus expresses both IsdG and IsdI, paralogous proteins where the former is believed to carry out “housekeeping” heme degradation, while the latter serves a regulatory function.
Heme degradation in photosynthetic organisms.
Phytochromes are a class of photoreceptors in plants and photosynthetic bacteria. These molecules are synthesized via the conversion of heme to α-biliverdin by HO1 and the subsequent reduction of α-biliverdin to species specific phytochrome in a ferredoxin-dependent manner [45]. Cyanobacterial and plant HO1 is homologous to canonical HOs of non-photosynthetic organisms and similarly releases Fe(II) and CO during catalysis.
O2-independent heme degradation.
Organisms residing under anoxic conditions also have a mechanism to degrade heme. ChuW is a radical SAM methytransferase which degrades heme in an O2-independent manner. Using the 5’-deoxyadenosyl radical, a methyl group from a second molecule of SAM is transferred to heme, yielding the linear tetrapyrrole anaerobilin and Fe(II) [8•] (Figure 7). ChuW contains a [4Fe-4S] cluster and uses flavodoxin as an electron source. Heme degradation in the absence of O2 and without the concomitant production of immunogenic CO makes sense not only for obligate anaerobic pathogens, but also enteric commensal bacteria, where it may support nutritional iron absorption and/or relief from oxidative stress.
Conclusions
The diverse means by which organisms make and break heme speak to the importance of the tetrapyrrole scaffold and iron ion that is harbored inside it. Pathway diversity appears to have had both ecological and cell-biological drivers. It seems likely that, as genomes and ecosystems are further explored, tetrapyrrole biology will continue to be a locus for future discovery.
Highlights.
Pathways for heme biosynthesis and degradation are not universally conserved
Pathway diversification may have been both ecologically and biologically driven
Unique molecules from each pathway may serve as therapeutic targets or biomarkers
Footnotes
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