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Porphyrin
Porphyrin
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Porphine, the parent of porphyrin

Porphyrins (/ˈpɔːrfərɪns/ POR-fər-ins) are heterocyclic, macrocyclic, organic compounds, composed of four modified pyrrole subunits interconnected at their α carbon atoms via methine bridges (=CH−). In vertebrates, an essential member of the porphyrin group is heme, which is a component of hemoproteins, whose functions include carrying oxygen in the bloodstream. In plants, an essential porphyrin derivative is chlorophyll, which is involved in light harvesting and electron transfer in photosynthesis.

The parent of porphyrins is porphine, a rare chemical compound of exclusively theoretical interest. Substituted porphines are called porphyrins.[1] With a total of 26 π-electrons the porphyrin ring structure is a coordinated aromatic system.[2] One result of the large conjugated system is that porphyrins absorb strongly in the visible region of the electromagnetic spectrum, i.e. they are deeply colored. The name "porphyrin" derives from Greek πορφύρα (porphyra) 'purple'.[3]

Structure

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Porphyrin complexes consist of a square planar MN4 core. The periphery of the porphyrins, consisting of sp2-hybridized carbons, generally display small deviations from planarity. "Ruffled" or saddle-shaped porphyrins is attributed to interactions of the system with its environment.[4] Additionally, the metal is often not centered in the N4 plane.[5] For free porphyrins, the two pyrrole protons are mutually trans and project out of the N4 plane.[6] These nonplanar distortions are associated with altered chemical and physical properties. Chlorophyll-rings are more distinctly nonplanar, but they are more saturated than porphyrins.[7]

Complexes of porphyrins

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Concomitant with the displacement of two N-H protons, porphyrins bind metal ions in the N4 "pocket". The metal ion usually has a charge of 2+ or 3+. A schematic equation for these syntheses is shown, where M = metal ion and L = a ligand:

H2porphyrin + [MLn]2+ → M(porphyrinate)Ln−4 + 4 L + 2 H+


Ancient porphyrins

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A geoporphyrin, also known as a petroporphyrin, is a porphyrin of geologic origin.[8] They can occur in crude oil, oil shale, coal, or sedimentary rocks.[8][9] Abelsonite is possibly the only geoporphyrin mineral, as it is rare for porphyrins to occur in isolation and form crystals.[10]

The field of organic geochemistry had its origins in the isolation of porphyrins from petroleum. These findings helped establish the biological origins of petroleum.[11][12] Petroleum is sometimes "fingerprinted" by analysis of trace amounts of nickel and vanadyl porphyrins. Metalloporphyrins in general are highly stable organic compounds, and the detailed structures of the extracted derivatives made clear that they originated from chlorophyll.

Biosynthesis

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In non-photosynthetic eukaryotes such as animals, insects, fungi, and protozoa, as well as the α-proteobacteria group of bacteria, the committed step for porphyrin biosynthesis is the formation of δ-aminolevulinic acid (δ-ALA, 5-ALA or dALA) by the reaction of the amino acid glycine with succinyl-CoA from the citric acid cycle. In plants, algae, bacteria (except for the α-proteobacteria group) and archaea, it is produced from glutamic acid via glutamyl-tRNA and glutamate-1-semialdehyde. The enzymes involved in this pathway are glutamyl-tRNA synthetase, glutamyl-tRNA reductase, and glutamate-1-semialdehyde 2,1-aminomutase. This pathway is known as the C5 or Beale pathway.

Two molecules of dALA are then combined by porphobilinogen synthase to give porphobilinogen (PBG), which contains a pyrrole ring. Four PBGs are then combined through deamination into hydroxymethyl bilane (HMB), which is hydrolysed to form the circular tetrapyrrole uroporphyrinogen III. This molecule undergoes a number of further modifications. Intermediates are used in different species to form particular substances, but, in humans, the main end-product protoporphyrin IX is combined with iron to form heme. Bile pigments are the breakdown products of heme.

The following scheme summarizes the biosynthesis of porphyrins, with references by EC number and the OMIM database. The porphyria associated with the deficiency of each enzyme is also shown:

Heme B biosynthesis pathway and its modulators. Major enzyme deficiences are also shown.
Enzyme Location Substrate Product Chromosome EC OMIM Disorder
ALA synthase Mitochondrion Glycine, succinyl CoA δ-Aminolevulinic acid 3p21.1 2.3.1.37 125290 X-linked dominant protoporphyria, X-linked sideroblastic anemia
ALA dehydratase Cytosol δ-Aminolevulinic acid Porphobilinogen 9q34 4.2.1.24 125270 aminolevulinic acid dehydratase deficiency porphyria
PBG deaminase Cytosol Porphobilinogen Hydroxymethyl bilane 11q23.3 2.5.1.61 176000 acute intermittent porphyria
Uroporphyrinogen III synthase Cytosol Hydroxymethyl bilane Uroporphyrinogen III 10q25.2-q26.3 4.2.1.75 606938 congenital erythropoietic porphyria
Uroporphyrinogen III decarboxylase Cytosol Uroporphyrinogen III Coproporphyrinogen III 1p34 4.1.1.37 176100 porphyria cutanea tarda, hepatoerythropoietic porphyria
Coproporphyrinogen III oxidase Mitochondrion Coproporphyrinogen III Protoporphyrinogen IX 3q12 1.3.3.3 121300 hereditary coproporphyria
Protoporphyrinogen oxidase Mitochondrion Protoporphyrinogen IX Protoporphyrin IX 1q22 1.3.3.4 600923 variegate porphyria
Ferrochelatase Mitochondrion Protoporphyrin IX Heme 18q21.3 4.99.1.1 177000 erythropoietic protoporphyria

Laboratory synthesis

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Brilliant crystals of meso-tetratolylporphyrin, prepared from 4-methylbenzaldehyde and pyrrole in refluxing propionic acid

A common synthesis for porphyrins is the Rothemund reaction, first reported in 1936,[13][14] which is also the basis for more recent methods described by Adler and Longo.[15] The general scheme is a condensation and oxidation process starting with pyrrole and an aldehyde.

Potential applications

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Photodynamic therapy

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Porphyrins have been evaluated in the context of photodynamic therapy (PDT) since they strongly absorb light, which is then converted to heat in the illuminated areas.[16] This technique has been applied in macular degeneration using verteporfin.[17]

PDT is considered a noninvasive cancer treatment, involving the interaction between light of a determined frequency, a photo-sensitizer, and oxygen. This interaction produces the formation of a highly reactive oxygen species (ROS), usually singlet oxygen, as well as superoxide anion, free hydroxyl radical, or hydrogen peroxide.[18] These high reactive oxygen species react with susceptible cellular organic biomolecules such as; lipids, aromatic amino acids, and nucleic acid heterocyclic bases, to produce oxidative radicals that damage the cell, possibly inducing apoptosis or even necrosis.[19]

Molecular electronics and sensors

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Porphyrin-based compounds are of interest as possible components of molecular electronics and photonics.[20] Synthetic porphyrin dyes have been incorporated in prototype dye-sensitized solar cells.[21][22]

Biological applications

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Porphyrins have been investigated as possible anti-inflammatory agents[23] and evaluated on their anti-cancer and anti-oxidant activity.[24] Several porphyrin-peptide conjugates were found to have antiviral activity against HIV in vitro.[25]

Toxicology

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Heme biosynthesis is used as biomarker in environmental toxicology studies. While excess production of porphyrins indicate organochlorine exposure, lead inhibits ALA dehydratase enzyme.[26]

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In nature

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Several heterocycles related to porphyrins are found in nature, almost always bound to metal ions. These include

N4-macrocycle Cofactor name metal comment
chlorin chlorophyll magnesium several versions of chlorophyll exist (sidechain; exception being chlorophyll c)
bacteriochlorin bacteriochlorophyll (in part) magnesium several versions of bacteriochlorophyll exist (sidechain; some use a usual chlorin ring)
sirohydrochlorin (an isobacteriochlorin) siroheme iron Important cofactor in sulfur assimilation
biosynthetic intermediate en route to cofactor F430 and B12
corrin vitamin B12 cobalt several variants of B12 exist (sidechain)
corphin Cofactor F430 nickel highly reduced macrocycle

Synthetic

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A benzoporphyrin is a porphyrin with a benzene ring fused to one of the pyrrole units. e.g. verteporfin is a benzoporphyrin derivative.[27]

Non-natural porphyrin isomers

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Porphycene, first porphyrin isomer, synthesised from bipyrrole dialdehyde through McMurry coupling reaction

The first synthetic porphyrin isomer was reported by Emanual Vogel and coworkers in 1986.[28] This isomer [18]porphyrin-(2.0.2.0) is named as porphycene, and the central N4 Cavity forms a rectangle shape as shown in figure.[29] Porphycenes showed interesting photophysical behavior and found versatile compound towards the photodynamic therapy.[30] This result was followed by the preparation of [18]porphyrin-(2.1.0.1), named it as corrphycene or porphycerin.[31] Other non-natural porphyrins include [18]porphyrin-(2.1.1.0) and [18]porphyrin-(3.0.1.0) or isoporphycene.[32] The N-confused porphyrins feature one of the pyrrolic subunits with the nitrogen atoms facing outwards from the core of the macrocycle.[33][34]

Various reported Isomers of porphyrin

See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Porphyrins are a class of organic heterocyclic compounds characterized by a structure, consisting of four modified rings interconnected by four methine bridges (=CH-) to form a planar, aromatic . This core structure, known as porphin, typically features atoms at positions that can coordinate metal ions, and it often includes various side chains such as methyl, vinyl, or groups in naturally occurring variants. Widely distributed in nature as pigments, porphyrins exhibit intense absorption in the , with characteristic Soret bands around 400 nm and Q-bands between 500–800 nm, imparting colors ranging from red to green. In biological systems, porphyrins play essential roles as cofactors in vital processes; for instance, iron-complexed porphyrins form the in and , enabling oxygen transport and storage in animals. Magnesium-complexed chlorins (porphyrin derivatives) constitute the chlorophylls in and photosynthetic , facilitating light-harvesting and in . These compounds are biosynthesized through a conserved pathway starting from 5-aminolevulinic acid, leading to , which is then metallated to yield functional derivatives. Fossil records indicate porphyrin-like structures persist in ancient sediments and biomolecules, providing insights into over billions of years. Chemically, porphyrins are versatile scaffolds for synthetic modification, with derivatives like chlorins (featuring one reduced ring) expanding their properties for diverse applications. In medicine, porphyrin-based compounds are employed in for , where they accumulate in tumor cells and generate upon light activation to induce . They also serve as sensitizers in systems and agents due to their tunable and biocompatibility.

Structure and Properties

Core Structure

Porphyrin is a heterocyclic macrocycle composed of four pyrrole rings interconnected at their α-carbon atoms via four methine bridges (=CH-), forming a conjugated cyclic array. The parent compound, known as porphine, has the molecular formula C20_{20}H14_{14}N4_4 and features a tetrapyrrolic core with 20 carbon atoms and 4 nitrogen atoms arranged in a nearly planar configuration. In this structure, each pyrrole ring contributes two carbon atoms to the outer perimeter, while the methine bridges link them to create a 20-membered outer ring and a 16-membered inner ring; the nitrogen atoms bear hydrogen atoms (N-H bonds) directed toward the center, enabling potential coordination sites. The conjugated π-electron system in spans the , delocalizing electrons across the alternating double bonds in the units and methine bridges. This system contains 18 π-electrons, adhering to (4n + 2, where n = 4), which imparts aromatic character and enhances the molecule's thermodynamic stability while modulating its reactivity, such as in electrophilic substitutions at the meso positions. The planar geometry facilitates this delocalization, with the inner cavity allowing for interactions that underpin its role in metal complex formation. Crystallographic analysis of porphine reveals a monoclinic crystal structure (space group P21_1/c) with key bond lengths reflecting the partial double-bond character due to conjugation: pyrrolic C-N bonds average approximately 1.37 , while ring C-C bonds are around 1.40 , and methine C-CH bonds measure about 1.37 . These dimensions, determined from data, underscore the uniform electron distribution across the , contributing to its rigidity and photochemical properties.

Substituent Variations

Porphyrins can be modified through substitution at the β-positions on the pyrrole rings (carbons 2, 3, 7, 8, 12, 13, 17, 18) or at the meso-positions on the methine bridges (carbons 5, 10, 15, 20), allowing for diverse structural variations while maintaining the core macrocycle. These positions enable the attachment of alkyl, aryl, or functional groups that alter the molecule's overall properties without disrupting the conjugated π-system. In naturally occurring porphyrins, such as protoporphyrin IX, substituents are primarily located at the β-positions, including four methyl groups, two vinyl groups, and two propionate groups, which contribute to its role in biological systems like heme. This unsymmetrical β-substitution pattern distinguishes protoporphyrin IX from the unsubstituted porphine core and facilitates specific interactions in enzymatic environments. Synthetic porphyrins often feature uniform substitutions for controlled reactivity; for example, meso-tetraphenylporphyrin (TPP) bears four phenyl groups at the meso-positions, enhancing synthetic accessibility and versatility in coordination studies. Similarly, octaethylporphyrin (OEP) incorporates eight ethyl groups at the β-positions, providing a model for densely substituted systems closer to natural porphyrins in peripheral crowding. Substituents significantly influence , with hydrophilic groups like carboxylates in propionates improving aqueous solubility, while bulky aryl groups in TPP increase organic solvent solubility compared to β-alkyl variants. They also affect stability, as sterically demanding meso-aryl substituents enhance thermal and oxidative stability by reducing distortion. from meso-aryl groups, such as in TPP, prevent intermolecular aggregation through spatial hindrance, promoting monomeric behavior in solution. Historical nomenclature for substituted porphyrins, developed by , uses (I–IV) to denote the four possible positional isomers of β-substituted patterns, ensuring unambiguous identification of stereochemical arrangements. This system remains relevant for classifying complex natural and synthetic derivatives.

Physical and Spectroscopic Properties

Porphyrins are typically isolated as crystalline solids exhibiting a deep purple to color, resulting from their extensive conjugated π-electron system that enables strong absorption in the . This coloration is a hallmark of the porphyrin , with variations in hue influenced by substituents but consistently tied to the core aromatic structure. Regarding solubility, free-base porphyrins are generally insoluble in due to their hydrophobic nature but readily dissolve in organic solvents such as , , and . Substituent modifications, such as the addition of or groups (e.g., in sulfonated ), significantly improve aqueous solubility by introducing hydrophilic functionalities, enabling applications in polar media. The ultraviolet-visible (UV-Vis) absorption spectrum of porphyrins features a characteristic intense Soret band (B-band) near 400 nm, attributed to a higher-energy π-π* transition, alongside weaker Q-bands in the 500–700 nm range corresponding to lower-energy π-π* excitations. These spectral features are explained by the Gouterman four-orbital model, which posits that the porphyrin UV-Vis spectrum arises from transitions involving two nearly degenerate highest occupied molecular orbitals (HOMO-like a1u and b2u) and two lowest unoccupied molecular orbitals (LUMO-like eg set), with the Soret band's intensity stemming from allowed transitions and the Q-bands from partially forbidden ones due to nodal plane symmetries. Free-base porphyrins display prominent and , with fluorescence quantum yields often around 0.10, emitting in the red region (600–700 nm) following excitation of the Soret or Q-bands; these properties arise from the rigid, conjugated structure minimizing non-radiative decay. In contrast, metal coordination typically quenches by providing alternative decay pathways, such as metal-to-ligand charge transfer, though brief mention of such changes is noted here while detailed complex properties are addressed elsewhere. Nuclear magnetic resonance (NMR) provides diagnostic signatures for porphyrins, with ¹H NMR showing meso protons deshielded at approximately 10 ppm due to the macrocycle's diatropic ring current, β-protons at 8–9 ppm, and inner NH protons strongly shielded at -2 to -3 ppm. (IR) spectra reveal characteristic bands for N-H stretching vibrations around 3300 cm⁻¹ in free-base forms and C=C stretching of the near 1600 cm⁻¹, confirming the presence of the units and extended double bonds. Porphyrins exhibit good thermal stability as crystalline solids, with decomposition typically onsetting above 300–400°C under inert conditions, influenced by substituents that can either enhance or reduce this threshold through steric or electronic effects.

Coordination Chemistry

Metal Complex Formation

Porphyrins form metal complexes through coordination at the central cavity defined by their four nitrogen atoms, which create a square-planar with a of approximately 2.0 , optimally suited for divalent transition metals and certain main group elements. This N₄ donor set provides a stable dianionic environment after of the inner N-H bonds, enabling the metal ion to occupy the core and adopt specific geometries based on its electronic configuration and size. The cavity's rigidity and conjugation facilitate strong σ- and π-bonding interactions, making porphyrins versatile ligands for a wide range of metals. The binding process begins with the approach of the metal ion to the porphyrin, often involving initial outer-sphere association followed by deformation of the to accommodate insertion. Deprotonation of the two N-H bonds is crucial, releasing (up to 191 kJ/mol in some cases) as the metal coordinates to all four nitrogens and moves into the plane; this step is typically base-assisted and can be rate-limiting for certain metals. For many complexes, axial ligation occurs subsequently or concurrently, with ligands binding perpendicular to the porphyrin plane. Equilibrium constants for metal insertion reflect the stability of these complexes, with log K values for Cu²⁺ ranging from approximately 10 to 15 depending on the porphyrin substituents and conditions. Common metals incorporated into porphyrins span first-row transition elements such as Fe, Co, and Ni, which form stable complexes due to favorable size matching and electronic compatibility with the N₄ cavity. Second-row transition metals like Ru and Pd also readily coordinate, often exhibiting enhanced stability from stronger metal-ligand bonds. Recent advances have extended this to main group elements, particularly Group 15, with phosphorus(V) complexes synthesized and characterized between 2023 and 2025, including a phosphorus(V)-centered porphyrin with - and air-stable axial P–H bonds, highlighting expanded reactivity and potential applications in and materials. In biological systems, this chemistry is exemplified by , where Fe²⁺ or Fe³⁺ coordinates within . The resulting coordination geometry varies with the metal: d⁸ ions like Ni²⁺ and Pd²⁺ typically adopt a square-planar arrangement (CN=4), remaining low-spin and diamagnetic without axial ligands. For metals like Fe²⁺/³⁺ or Co²⁺, the geometry is often octahedral (CN=6) due to axial ligation by substrates or solvents, which modulates electronic properties. Saddle-shaped distortions of the porphyrin core can arise in complexes with larger metals or bulky substituents, leading to out-of-plane pyrrole tilting and altered bonding, as seen in certain Fe(III) or Ni(II) derivatives. Synthetic methods for metallation emphasize direct insertion, where free-base porphyrins react with metal salts (e.g., acetates or chlorides) under in polar aprotic solvents like DMF, often with added base to facilitate and achieve high yields (up to 90% for Cu and Ni). Template synthesis represents an alternative, particularly for challenging metals, where the ion templates the cyclization of porphyrin precursors during macrocycle assembly, enhancing selectivity and incorporating the metal . These approaches allow precise control over complex formation while avoiding harsh conditions.

Properties of Complexes

Metalloporphyrin complexes exhibit distinct electronic properties compared to free-base porphyrins, primarily due to metal-ligand interactions that introduce charge transfer transitions. In particular, metal-to-ligand charge transfer (MLCT) bands appear in the UV-Vis spectra of certain metalloporphyrins, such as those with iron or centers, where shifts from the metal d-orbitals to the porphyrin π* orbitals, often observed in the visible region around 400-500 nm. These MLCT transitions contribute to the intense coloration and photochemical reactivity of the complexes. Additionally, the incorporation of metals shifts the potentials of the porphyrin ring and metal center; for example, the Fe³⁺/Fe²⁺ couple in proteins like has a midpoint potential of approximately +0.028 V vs. NHE, modulated by axial ligands and the protein environment to facilitate in biological systems. The reactivity of metalloporphyrins is notably enhanced by their ability to bind axial ligands, with binding affinities varying based on the ligand's nucleophilicity and the metal's coordination preferences. Imidazole ligands bind more strongly to iron(III) porphyrins than water, with formation constants for bis(imidazole) complexes around 10⁵-10⁶ M⁻² in aqueous media, reflecting the preference for nitrogen donors in mimicking heme active sites. This axial coordination influences reactivity, as seen in cobalt(II) porphyrins, which reversibly bind O₂ with affinities comparable to cobalt-substituted myoglobin (equilibrium constant K_O2 ≈ 10³-10⁴ torr⁻¹ at low temperatures), enabling model studies of oxygen transport without irreversible oxidation. Stability of metalloporphyrin complexes is governed by high thermodynamic formation constants, reflecting the strong of the tetradentate porphyrin to the metal ion. For iron(II) tetraphenylporphyrin, the overall stability constant (β₄) exceeds 10³⁰, indicating exceptional robustness under physiological conditions, though sensitivity to oxidation can lead to ring degradation upon exposure to strong oxidants. These complexes are generally stable to reduction but may undergo metal extrusion under extreme or reductive conditions. Spectroscopic properties of metalloporphyrins differ markedly from free-base forms due to metal-induced perturbations. The Soret band, a characteristic π-π* transition, shifts to longer wavelengths in zinc(II) porphyrins, typically appearing at ~423-430 nm, compared to ~418 nm in the free base, arising from the filled d¹⁰ configuration that stabilizes the excited state. For paramagnetic metals like Cu²⁺, electron paramagnetic resonance (EPR) spectroscopy reveals g-values around 2.0-2.2 and hyperfine splitting from nitrogen nuclei, providing insights into the square-planar geometry and unpaired electron delocalization over the porphyrin ring. Recent advances highlight unique properties in main group metal complexes of modified porphyrins, such as phosphaporphyrins, where phosphorus substitution introduces σ-π interactions that alter electronic delocalization and enhance stability for optoelectronic applications. These systems exhibit tunable potentials and , with coordination to metals like aluminum or yielding complexes stable under ambient conditions and showing potential in sensing due to their distinct charge transfer characteristics.

Synthesis Methods

Biological Biosynthesis

The biological biosynthesis of porphyrins primarily occurs through the biosynthetic pathway, a conserved enzymatic process in most organisms that produces as a key intermediate, which is then modified into or other derivatives. This pathway begins in the mitochondria and involves shuttling intermediates to the , comprising eight enzymatic steps that convert simple precursors into the macrocyclic structure. The process is essential for generating , a cofactor in proteins like and , and shares early steps with the synthesis of in photosynthetic organisms. The pathway initiates with the condensation of glycine and succinyl-CoA to form δ-aminolevulinic acid (ALA), the first committed precursor, catalyzed by ALA synthase (ALAS), which is the rate-limiting enzyme. This reaction occurs in the mitochondria and releases CO₂ and CoA as byproducts: glycine+succinyl-CoAALA synthaseδ-aminolevulinic acid (ALA)+CO2+CoA\text{glycine} + \text{succinyl-CoA} \xrightarrow{\text{ALA synthase}} \delta\text{-aminolevulinic acid (ALA)} + \text{CO}_2 + \text{CoA}
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