The chiton stylus canal: An element delivery pathway for tooth cusp biomineralization

A detailed investigation of the stylus canal situated within the iron mineralized major lateral teeth of the chiton Acanthopleura hirtosa was undertaken in conjunction with a row‐by‐row examination of cusp mineralization. The canal is shown to contain columnar epithelial tissue similar to that surrounding the mineralized cusps, including the presence of iron rich particles characteristic of the iron storage protein ferritin. Within the tooth core, a previously undescribed internal pathway or plume is evident above the stylus canal, between the junction zone and mineralizing posterior face of the cusp. Plume formation coincides with the appearance of iron in the superior epithelium and the onset of mineralization at tooth row 13. The plume persists during the delivery of phosphorous and calcium into the tooth core, and is the final region of the cusp to become mineralized. The presence of the stylus canal was confirmed in a further 18 chiton species, revealing that the canal is common to polyplacophoran molluscs. These new data strongly support the growing body of evidence highlighting the importance of the junction zone for tooth mineralization in chiton teeth, and indicate that the chemical and structural environment within the tooth cusp is under far greater biological control than previously considered. J. Morphol. 2009. © 2008 Wiley‐Liss, Inc.     

A new biomineral identified in the cores of teeth from the chiton <Emphasis Type="Italic"> Plaxiphora albida</Emphasis>

The hydrated iron(III) oxide limonite is reported for the first time as a biomineral. In situ laser Raman spectra of the tooth cores from major lateral teeth of the chiton Plaxiphora albida are compared with those of synthetic and mineral iron phosphates and iron oxides. Raman spectra measured on iron phosphate and iron oxide standard materials are shown to be easily distinguishable from one another. The central tooth cores of mature P. albida teeth do not show any evidence for the presence of a separate iron phosphate mineral. Rather, in each tooth a narrow band of the hydrated iron(III) oxide limonite is shown to separate the magnetite of the tooth surface from a central core region comprising both lepidocrocite and limonite. The high concentration of phosphorus in P. albida tooth cores, previously observed by energy dispersive spectroscopy, is not associated with a separate iron phosphate mineral, indicating that this element may be adsorbed onto the surface of the iron oxide minerals present. The failure to detect a separate iron(III) phosphate is discussed with reference to other chiton species that display high levels of iron and phosphorus in the cores of their mature major lateral teeth.     

Proteomic analysis from the mineralized radular teeth of the giant Pacific chiton, Cryptochiton stelleri (Mollusca)

The biomineralized radular teeth of chitons are known to consist of iron-based magnetic crystals, associated with the maximum hardness and stiffness of any biomineral. Based on our transmission electron microscopy analysis of partially mineralized teeth, we suggest that the organic matrix within the teeth controls the iron oxide nucleation. Thus, we used Nano-LC-MS to perform a proteomic analysis of the organic matrix in radular teeth of the chiton Cryptochiton stelleri in order to identify the proteins involved in the biomineralization process. Since the genome sequence of C. stelleri is not available, cross-species similarity searching and de novo peptide sequencing were used to screen the proteins. Our results indicate that several proteins were dominant in the mineralized part of the radular teeth, amongst which, myoglobin and a highly acidic peptide were identified as possibly involved in the biomineralization process.     

In situ Raman spectroscopic studies of the teeth of the chiton Acanthopleura hirtosa

 In situ Raman spectroscopy, in combination with energy dispersive spectroscopy, has been used for the first time to determine the identities and locations, at the micron level, of mineral phases present in single chiton teeth that have been extensively mineralized. At the later stages of development the major lateral teeth of the chiton Acanthopleura hirtosa show characteristic spectroscopic evidence for the presence of lepidocrocite (γ-FeOOH), magnetite (Fe₃O₄), and an apatitic calcium phosphate. Goethite (α-FeOOH) and ferrihydrite (5 Fe₂O₃·9 H₂O), which have been detected previously in teeth at the early stages of mineralization, were not detected in this mature tooth. The spatial distribution of these phases was determined, providing evidence for the presence of a discrete layer of lepidocrocite between the magnetite and apatite regions, illustrating the complexity of the biomineralization process. The technique of laser Raman microscopy is shown to be ideal for the examination of small biomineralized structures in situ, such as chiton teeth. Received: 6 July 1998 / Accepted: 19 August 1998     

Structural Organisation of the Cusps of the Radular Teeth of the Chiton Plaxiphora albida

Abstract The structure, morphology and organisation of the cusps of the major lateral radula teeth of the chiton Plaxiphora albida have been examined using light, transmission and scanning electron microscopy, together with energy dispersive X-ray analysis and Mössbauer spectroscopy. In this chiton species, both the anterior and posterior surfaces of the major lateral teeth are composed of magnetite, which is indicated to be non-stoichiometric and associated with some maghemite, together with small amounts of phosphorus and silicon. This outer layer surrounds an inner core region of the tooth, which only reaches the surface through a small window zone on the anterior surface and which contains large amounts of iron and phosphorus presumably in the form of iron(III) phosphate. The organic matrix, on which the teeth are constructed, consists of a zone of densely packed fine fibres at the surface of the tooth, underlain by larger fibres which become sparser deeper into the cusp. The core region is characterized by the presence of densely packed short fibres. In contrast to the situation found in most other species of chiton, large fibres of the organic matrix extend throughout the region of magnetite mineralization, leading to the suggestion that the matrix exerts more control over the mineralization of magnetite than has previously been thought.     

Contribution of Raman spectroscopy to identification of biominerals present in teeth of Acanthopleura rehderi,Acanthopleura curtisiana,and Onithochiton quercinus

Raman spectroscopic investigations of the major lateral teeth of the chitons Acanthopleura rehderi and Acanthopleura curtisiana indicate that, in addition to the magnetite of the cutting surface and a carbonated hydroxyapatite in the central tooth core, these species deposit limonite in place of the lepidocrocite reported for other members of the genus Acanthopleura. A comparison of the spectra from these species with those of Onithochiton quercinus, which also deposits limonite, indicates that the current assignment of these species to Acanthopleura may not be appropriate. Biomineralization of the major lateral teeth may be a useful parameter to include in the taxonomic classification of chiton species.     

The junction zone: Initial site of mineralization in radula teeth of the chiton Cryptoplax striata (Mollusca: Polyplacophora)

Elemental composition and distribution in individual teeth of the whole radula of the chiton Cryptoplax striata were analyzed using energy-dispersive spectroscopy. Both the element deposited and its position within the tooth vary according to the stage of mineralization. The initial site of mineralization is the junction zone, the region between the tooth cusp and base. In this region, the first element to be deposited is iron, followed by phosphorus and then calcium. Iron deposition next commences in the tooth cusp cap, where it proceeds rapidly, being virtually complete within 12 tooth rows. By contrast, mineralization in the core of the tooth cusp does not commence until well down the radula and consists initially of iron and phosphorus with the addition of a small amount of calcium 6 rows later. While mineralization in the tooth base commences early in radula development, it continues right through to the fully mature end of the radula. A number of minor elements are also found at various stages of mineralization. The data obtained have been used to construct a schematic of the progression of mineralization along the length of the radula. © 1996 Wiley-Liss, Inc.     

Fine structure of the mineralized teeth of the chiton Acanthopleura echinata (Mollusca: Polyplacophora)

The major lateral teeth of the chiton Acanthopleura echinata are composite structures composed of three distinct mineral zones: a posterior layer of magnetite; a thin band of lepidocrocite just anterior to this; and apatite throughout the core and anterior regions of the cusp. Biomineralization in these teeth is a matrix-mediated process, in which the minerals are deposited around fibers, with the different biominerals described as occupying architecturally discrete compartments. In this study, a range of scanning electron microscopes was utilized to undertake a detailed in situ investigation of the fine structure of the major lateral teeth. The arrangement of the organic and biomineral components of the tooth is similar throughout the three zones, having no discrete borders between them, and with crystallites of each mineral phase extending into the adjacent mineral zone. Along the posterior surface of the tooth, the organic fibers are arranged in a series of fine parallel lines, but just within the periphery their appearance takes on a "fish scale"-like pattern, reflective of the cross section of a series of units that are overlaid, and offset from each other, in adjacent rows. The units are approximately 2 microm wide and 0.6 microm thick and comprise biomineral plates separated by organic fibers. Two types of subunits make up each "fish scale": one is elongate and curved and forms a trough, in which the other, rod-like unit, is nestled. Adjacent rod and trough units are aligned into large sheets that define the fracture plane of the tooth. The alignment of the plates of rod-trough units is complex and exhibits extreme spatial variation within the tooth cusp. Close to the posterior surface the plates are essentially horizontal and lie in a lateromedial plane, while anteriorly they are almost vertical and lie in the posteroanterior plane. An understanding of the fine structure of the mineralized teeth of chitons, and of the relationship between the organic and mineral components, provides a new insight into biomineralization mechanisms and controls.     

Atomic force microscopy study of tooth surfaces

Atomic force microscopy (AFM) was used to study tooth surfaces in order to compare the pattern of particle distribution in the outermost layer of the tooth surfaces. Human teeth and teeth from a rodent (Golden hamster), from a fish (piranha), and from a grazing mollusk (chiton) with distinct feeding habits were analyzed in terms of particle arrangement, packing, and size distribution. Scanning electron microscopy and transmission electron microscopy were used for comparison. It was found that AFM gives high-contrast, high-resolution images and is an important tool as a source of complementary and/or new structural information. All teeth were cleaned and some were etched with acidic solutions before analysis. It was observed that human enamel (permanent teeth) presents particles tightly packed in the outer surface, whereas enamel from the hamster (continuously growing teeth) shows particles of less dense packing. The piranha teeth have a thin cuticle covering the long apatite crystals of the underlying enameloid. This cuticle has a rough surface of particles that have a globular appearance after the brief acidic treatment. The similar appearance of the in vivo naturally etched tooth surface suggests that the pattern of globule distribution may be due to the presence of an organic material. Elemental analysis of this cuticle indicated that calcium, phosphorus, and iron are the main components of the structure while electron microdiffraction of pulverized cuticle particles showed a pattern consistent with hydroxyapatite. The chiton mineralized tooth cusp had a smooth surface in an unabraded region and a very rough structure with the magnetite crystals (already known to make part of the structure) protruding from the surface. It was concluded that the structures analyzed are optimized for efficiency in feeding mechanism and life span of the teeth.     

Effects of Chemical Speciation on the Mineralization of Organic Compounds by Microorganisms

The mineralization of 1.0 to 100 ng each of four complexing compounds—oxalate, citrate, nitrilotriacetate (NTA), and EDTA—per ml was tested in media prepared in accordance with equilibrium calculations by a computer program so that the H, Ca, Mg, Fe, or Al complex (chemical species) was predominant. Sewage microorganisms mineralized calcium citrate more rapidly than iron, aluminum, or hydrogen citrate, and magnesium citrate was degraded slowest. Aluminum, hydrogen, and iron oxalates were mineralized more rapidly than calcium oxalate, and magnesium oxalate was decomposed slowest. Sewage microorganisms mineralized calcium NTA but not aluminum, magnesium, hydrogen, or iron NTA or any of the EDTA complexes. Pseudomonas sp. mineralized calcium and iron citrates but had no activity on hydrogen, aluminum, or magnesium citrate. Pseudomonas pseudoalcaligenes mineralized calcium, iron, hydrogen, and aluminum citrates but had little activity on magnesium citrate. Pseudomonas alcaligenes used calcium, iron, hydrogen, and aluminum oxalates readily, but it used magnesium oxalate at a slower rate. Listeria sp. destroyed calcium NTA but had no effect on hydrogen, iron, or magnesium NTA. Increasing the Ca concentration in the medium enhanced the breakdown of NTA by Listeria sp. The different activities of the bacterial isolates were not a result of the toxicity of the complexes or the lack of availability of a nutrient element. NTA mineralization was not enhanced by the addition of Ca to Beebe Lake water, but it was enhanced when Ca and an NTA-degrading inoculum were added to water from an oligotrophic lake. The data show that chemical speciation influences the mineralization of organic compounds by naturally occurring microbial communities and by individual bacterial populations.     

红条毛肤石鳖齿舌主侧齿中铁还原酶分布及与生物矿化的关系

以红条毛肤石鳖Acanthochiton rubrolineatus(Lischke)齿舌为材料,通过切片和酶组织化学技术,在光镜和电镜下对齿舌主侧齿的微结构及高铁还原酶的存在进行观察,从微观角度了解齿舌主侧齿齿尖的矿化机理。结果显示,成熟主侧齿由齿尖和齿基组成。齿尖结构由外至内分为三层,最外层为磁铁矿层,前后齿面磁铁矿层的厚度不等,后齿面约50μm,前齿面约5-10μm。向内依次为棕红色的纤铁矿层,厚约10μm,及略显黄色的有机基质层,有机基质层占据着齿尖内部的大部分结构。高分辨透射电镜下显示磁铁矿由条状四氧化三铁颗粒组成,长约2-3μm,宽约100-150nm。齿舌的矿化是一个连续过程,不同部段处于不同的矿化阶段,齿舌囊上皮细胞沿囊腔分布,并形成齿片。未矿化的新生主侧齿齿尖中存在由有机基质构成的网状结构。随矿化的进行,有机基质内出现矿物颗粒。初始矿化的齿尖外表面有一个细胞微突层,微突的另一端为囊上皮细胞,矿物质经由微突层达齿尖并沉积于有机基质中,齿尖随之矿化并成熟。初始矿化齿尖的外围有大量的三价铁化物颗粒,稍成熟的齿尖外围同时还出现二价铁化物。新生或初始矿化主侧齿齿尖外围的囊上皮细胞中有大量球形类似于铁蛋白聚集体的内容物,直径0.6-0.8μm,球体由膜包围。齿舌囊上皮组织中存在三价高铁还原酶,此酶分布于上皮细胞的膜表面,可能与齿尖表面磁铁矿的生成有一定的关系。       

Effect of nickel(II) substitution on the resonance Raman and NMR spectra of Alcaligenes xylosoxidans azurin II: implications for axial-ligand bonding interactions in cupredoxin active sites

Assignment of the resonance Raman (RR) spectrum of Ni(II)-substituted azurin II from Alcaligenes xylosoxidans (NCIMB 11015) using Ni isotope substitution reveals an anomalously low Ni-S(Cys) stretching frequency of 349?cm^–1, suggesting the presence of significant axial-ligand bonding interactions. The X-ray crystal structure of Ni(II)-substituted azurin from Pseudomonas aeruginosa shows that there are two potential axial ligands to the Ni ion: a peptide carbonyl O at a distance of 2.46?Å, together with a long-range interaction from a methionine sulfur (S′) at a distance of 3.30?Å. Comparison of the RR properties of Ni(II)-substituted azurin II with stellacyanin (which contains an axial carbonyl ligand, but no methionine) suggests that the interaction from the carbonyl oxygen ligand alone is not sufficient to account for the weak Ni azurin metal-thiolate bond. Instead, it appears that a Ni-methionine bonding interaction is also required to explain the low Ni-S(Cys) stretching frequency in Ni(II)-substituted azurin II. This hypothesis is supported by NMR studies which show a large paramagnetic shift for the protons of the methionine side-chain. Thus, it appears that Ni-substituted azurin II is best described as five-coordinate, and that significant Ni(II)-methionine bonding interactions can occur at a distance of 3.3?Å.     

EXAFS and Mössbauer characterization of the Diiron(III) site in stearoyl-acyl carrier protein Δ9– desaturase

Stearoyl-acyl carrier protein (ACP) Δ⁹-desaturase (Δ9D) from the castor plant is the best characterized soluble acyl-ACP desaturase. This enzyme utilizes a diiron center to catalyze the O₂- and NADPH-dependent introduction of a cis double bond between carbons 9 and 10 of stearoyl-ACP, yielding oleoyl-ACP. In the present study, we have used X-ray absorption spectroscopy to provide the first metrical information for the diferric oxidation state. These studies reveal distinct diiron clusters that have Fe-Fe distances of either 3.12 or 3.41?Å. The species having the 3.12?Å Fe-Fe distance also exhibits a 1.8?Å Fe-O bond and is thus proposed to represent Δ9D molecules containing a (μ-oxo)bis(μ-carboxylato)diiron(III) cluster. The species having the 3.41?Å Fe-Fe distance exhibits no short Fe-O bond, and thus likely represents Δ9D molecules containing a (μ-hydroxo)diiron(III) cluster. Mössbauer studies of the extended X-ray absorption fine structure (EXAFS) samples revealed three quadrupole doublets (ΔE _Q(1)=1.53?mm/s, 72%;ΔE _Q(2)=0.72?mm/s, 21%;ΔE _Q(3)=2.20?mm/s, 7%) that originate from three distinct dinuclear clusters. From analysis of spectral intensities and by comparison with previous studies of (μ-oxo)- and (μ-hydroxo)diiron(III) clusters in both model complexes and proteins, doublet 1, the Mössbauer majority species, is likely associated with the EXAFS majority species having a 3.12?Å Fe-Fe separation and a 1.8?Å Fe-μ-oxo bond, while doublet 2 likely results from one iron site (or both) of a cluster associated with the EXAFS species having a 3.41?Å Fe-Fe separation. The presence of multiple diiron center conformations in diferric Δ9D may reflect the necessity for the active site to allow access of the substrate stearoyl-ACP (～9?kDa) during desaturation catalysis.     

Matrix Heterogeneity in the Radular Teeth of the Chiton Acanthopleura hirtosa

The structure and organization of the organic matrix of the cusps of the major lateral teeth of the chiton Acanthopleura hirtosahave been examined using conventional light and transmission electron microscopy techniques and by using the protein ferritin as an ultrastructural probe. The results show major structural differences in the organic matrix between the surface layers of the anterior (calcified) region and the posterior (magnetite-mineralized) region and their respective underlying regions. In addition, the central (lepidocrocite-mineralized) region of the tooth has been examined and shown to consist of bundles of fibres arranged such that they display a tightly interwoven pattern. It is suggested that while the structural organization of surface fibres readily permits the passage of ions required for mineralization, the architecturally discrete distribution of biominerals found in mature chiton teeth is due mostly to spatial delineation of the tooth by matrix macromolecules in the central region of the tooth.     

Development and microstructure of tooth histotypes in the blue shark,Prionace glauca (Carcharhiniformes: Carcharhinidae) and the great white shark,Carcharodon carcharias (Lamniformes: Lamnidae)

Elasmobranchs exhibit two distinct arrangements of mineralized tissues in the teeth that are known as orthodont and osteodont histotypes. Traditionally, it has been said that orthodont teeth maintain a pulp cavity throughout tooth development whereas osteodont teeth are filled with osteodentine and lack a pulp cavity when fully developed. We used light microscopy, scanning electron microscopy, and high‐resolution micro‐computed tomography to compare the structure and development of elasmobranch teeth representing the two histotypes. As an example of the orthodont histotype, we studied teeth of the blue shark, Prionace glauca (Carcharhiniformes: Carcharhinidae). For the osteodont histotype, we studied teeth of the great white shark, Carcharodon carcharias (Lamniformes: Lamnidae). We document similarities and differences in tooth development and the microstructure of tissues in these two species and review the history of definitions and interpretations of elasmobranch tooth histotypes. We discuss a possible correlation between tooth histotype and tooth replacement and review the history of histotype differentiation in sharks. We find that contrary to a long held misconception, there is no orthodentine in the osteodont teeth of C. carcharias. J. Morphol. 276:797–817, 2015. © 2015 Wiley Periodicals, Inc.     

Ultrastructure and the importance of wear in the dentition of the halfbeak (Pisces: Hemiramphidae) pharyngeal mill

To assess how tooth microstructure and composition might facilitate the pharyngeal mill mechanism of halfbeaks, apatite structure and iron content were determined by scanning electron microscopy and energy dispersive X‐ray analysis for Hyporhamphus regularis ardelio, Arrhamphus sclerolepis krefftii, and Hemiramphus robustus. Iron was present in developing teeth and was concentrated along the shearing edge of spatulate incisiform teeth, which dominate the occlusive wear zone in all three species. A model based on tooth structure and wear rate is proposed to explain how halfbeaks maintain a fully functional occlusion zone throughout growth and consequent tooth addition and replacement. Replacement teeth erupt and wear rapidly so that a constant occlusion plane is always present. Iron within the tooth tissue reduces the wear rate of the cutting edge while simultaneously maintaining its sharpness and efficiency. J. Morphol. 2009. © 2008 Wiley‐Liss, Inc.     

Iron coordination geometry in full-length, truncated, and dehydrated forms of human tyrosine hydroxylase studied by Mössbauer and X-ray absorption spectroscopy

Full-length human tyrosine hydroxylase 1 (hTH1) and a truncated enzyme lacking the 150 N-terminal amino acids were expressed in Escherichia coli and purified either with or without (6×histidine) N-terminal tags. After reconstitution with ⁵⁷Fe(II), the Mössbauer and X-ray absorption spectra of the enzymes were compared before and after dehydration by lyophilization. Before dehydration, >90% of the iron in hTH1 had Mössbauer parameters typical for high-spin Fe(II) in a six-coordinate environment [isomer shift δ(1.8–77?K)=1.26–1.24?mm s^–1 and quadrupole splitting ΔE _Q=2.68?mm s^–1]. After dehydration, the Mössbauer spectrum changed and 63% of the area could be attributed to five-coordinate high-spin Fe(II) (δ=1.07?mm s^–1 and ΔE _Q=2.89?mm s^–1 at 77?K), whereas 28% of the iron remained as six-coordinate high-spin Fe(II) (δ=1.24?mm s^–1 and ΔE _Q=2.87?mm s^–1 at 77?K). Similar changes upon dehydration were observed for truncated TH either with or without the histidine tag. After rehydration of hTH1 the spectroscopic changes were completely reversed. The X-ray absorption spectra of hTH1 in solution and in lyophilized form, and for the truncated protein in solution, corroborate the findings derived from the Mössbauer spectra. The pre-edge peak intensity of the protein in solution indicates six-coordination of the iron, while that of the dehydrated protein is typical for a five-coordinate iron center. Thus, the active-site iron can exist in different coordination states, which can be interconverted depending on the hydration state of the protein, indicating the presence or absence of a water molecule as a coordinating ligand to the iron. The present study explains the difference in iron coordination determined by X-ray crystallography, which has shown a five-coordinate iron center in rat TH, and by our recent spectroscopic study of human TH in solution, which showed a six-coordinated iron center.     

Do all geckos hatch in the same way? Histological and 3D studies of egg tooth morphogenesis in the geckos Eublepharis macularius Blyth 1854 and Lepidodactylus lugubris Duméril & Bibron 1836

The egg tooth of squamates evolved to facilitate hatching from mineralized eggshells. Squamate reptiles can assist their hatching with a single unpaired egg tooth (unidentates) or double egg teeth (geckos and dibamids). Egg tooth ontogeny in two gekkotan species, the leopard gecko Eublepharis macularius and the mourning gecko Lepidodactylus lugubris, was compared using microtomography, scanning electron microscopy, and light microscopy. Investigated species are characterized by different hardnesses of their eggshells. Leopard geckos eggs have a relatively soft and flexible parchment (leathery) shell, while eggshells of mourning geckos are hard and rigid. Embryos of both species, like other Gekkota, have double egg teeth, but the morphology of these structures differs between the investigated species. These differences in shape, localization, and spatial orientation were present from the earliest stages of embryonic development. In mourning gecko, anlagen of differentiating egg teeth change their position on the palate during embryonic development. Initially they are separated by condensed mesenchyme, but later in development, their enamel organs are connected. In leopard geckos, the localization of egg tooth germs does not change, but their spatial orientation does. Egg teeth of this species shift from inward to outward orientation. This is likely related to differences in structure and mechanical properties of eggshells in the studied species. In investigated species, two hatching mechanisms are possible during emergence of young individuals. We speculate that mourning geckos break the eggshell through puncturing action with egg teeth, similar to the pipping phase of chick and turtles embryos. Egg teeth of leopard geckos cut egg membranes similarly to most squamates. Our results also revealed differences in egg tooth implantation between Gekkota and Unidentata: gekkotan egg teeth are subthecodont (in shallow sockets), while those in unidentates are acrodont (attached to the top of the alveolar ridge). © 2020 Wiley Periodicals LLC     

Chondrichthyan and actinopterygian remains from theLower Permian Copacabana Formation of Bolivia

Two horizons of the marine Lower Permian (Leonardian) Copacabana Formation have yielded fish remains, on the south-western slope of the Jacha Khatawi Hill, Yaurichambi, La Paz department, Bolivia. This fish fauna consists of teeth and scales of chondrichthyans (Eugeneodontida, Petalodontida, ? Bradyodonti, Elasmobranchii) and actinopterygians (? Plastysomidae). The Eugeneodontida are represented by a new species of a large Agassizodontidae, Parahelicoprion mariosuarezi n.sp., based on a large symphysial tooth series which resembles P. clerci from the Lower Permian Arta beds of the Urals. The Petalodontida are represented by a fragment of a large symphysial tooth which may be referred to the pristodontid genus Megactenopetalus, known else-where from the Lower Permian of the U.S.A. and China. Some isolated crushing teeth may questionably be referred to a bradyodont, possibly Helodus or Lagarodus. Some elasmobranch teeth of «Cladodus type also occur in this locality. Some hemispherical teeth of «phyllodont type and some scales are tentatively referred to the actinopterygian family Platysomidae. These findings are the first record of determinable marine Permian fishes in the Andean region of South America. The overall composition of this fauna agrees fairly well with the fish fauna known from the Marine Lower Permian of United States and eastern Asia.     

Structural characterization of the mononuclear iron site in Pseudomonas cepacia phthalate DB01 dioxygenase using X-ray absorption spectroscopy

Phthalate dioxygenase (PDO) from Pseudomonas cepacia contains a Rieske-like [2Fe-2S] cluster and a mononuclear non-heme Fe(II) site. The mononuclear iron can be replaced by a variety of divalent metal ions, although only Fe(II) permits catalytic activity. We used X-ray absorption spectroscopy to characterize the structural properties of the mononuclear iron site and to follow the structural changes in this site as a function both of Rieske site oxidation state and of phthalate binding. Data for the mononuclear site have been measured directly for PDO substituted with Co or Zn in the mononuclear site, and by difference for the native 3-Fe protein. The mononuclear site was modeled well by low Z-ligation (oxygen or nitrogen) and showed no evidence for high-Z ligands (e.g., sulfur). The relatively short average first shell bond lengths and the absence of significant outer shell scattering suggest that the mononuclear site has several oxygen ligands. With Zn in the mononuclear site, the average bond length (2.00?Å) suggests a 5-coordinate site under all conditions. In contrast, the Co- or Fe-containing mononuclear site appeared to be 6-coordinate and changed to 5-coordinate when substrate was bound, since the first shell bond length changed from 2.08 to 2.02?Å (Co) or 2.10 to 2.06?Å (Fe). The implications of these findings for the PDO mechanism are discussed.