禄丰古猿蝴蝶种下第四前臼齿釉质-齿质交界面的三维几何形态

禄丰古猿蝴蝶种 (Lufengpithecus hudienensis) 也称蝴蝶古猿,是重要的早期人科成员,化石产自云南元谋盆地竹棚-小河及雷老两个地点群,其年代为中新世晚期。上世纪八、九十年代的发掘工作共获得幼年个体颅骨1具、残上颌骨10件、残下颌骨17件及1500多枚单个牙齿。受限于当时的技术条件,蝴蝶古猿牙齿内部结构及三维形态一直未有报道和对比研究。本文首次使用高精度CT配合三维几何形态测量方法,对6枚产自小河地点的蝴蝶古猿下颌第四前臼齿的釉质-齿质交界面形态进行了观察和对比,对比材料包括步氏巨猿、猩猩（化石）、大猩猩、黑猩猩及现代人。多变量分析显示,蝴蝶古猿釉质-齿质交界面几何形态接近于本文所涉及的大型猿类对比标本,但并没有表现出与某一特定类群的相似性;咬合面轮廓狭长,前凹尺寸明显小于后凹;整体形态介于齿质尖较高的大猩猩和齿质尖较低、釉质-齿质交界面形态扁平的巨猿、猩猩和黑猩猩之间。本文所观察到的类群之间的异同可能与趋同演化有关,也需要更多数据的进一步验证。将釉质-齿质交界面的三维几何形态和其他牙齿内部结构的信息（如釉质厚度及其三维分布规律等）综合,有助于进一步讨论蝴蝶古猿的分类学、系统发育和食性。     

禄丰古猿(Lufengpithecus lufengensis)牙齿釉质生长线与个体发育问题研究

运用扫描电子显微镜,对4枚禄丰古猿牙齿（恒齿）的釉质结构进行了观察研究。发现：禄丰古猿牙齿釉质表面有明显的釉面横纹结构;釉面横纹的密度向牙颈方向逐渐增大;观察记数了4枚牙齿的釉面横纹数,进而推算出牙冠的形成时间和年龄。与化石人科成员、现代人及现生大猿比较,禄丰古猿牙冠发育模式及时间,与南方古猿纤细种比较接近或相似,明显长于南方古猿粗壮种,有别于现生大猿。     

禄丰古猿牙齿釉质生长线与个体发育问题研究

运用扫描电子显微镜,对４枚禄丰古猿牙齿（恒齿）釉质结构进行了观察研究,发现：禄丰古猿牙齿釉质表面有明显的釉面横纹结构;釉面横纹的密度向牙颈方向逐渐增大;观察记数了４枚牙齿的釉面横纹数,进而推算出牙冠的形成时间和年龄。与化石人科成员,现代人及现生大猿比较,禄丰古猿牙冠发育模式及时间,与南方古猿纤细种比较接近或相似,明显长于南方古猿粗壮种,有别于现生大猿。     

许家窑人幼年个体的釉质发育缺陷

上世纪70年代在许家窑-侯家窑地点发现的人类化石对了解东亚中晚更新世过渡时期古人类的形态演化起到了重要作用。除形态特征外,针对许家窑人病理表现也开展过相关研究,其中许家窑人幼年个体前部牙齿上出现的黄色小坑被认为是患有氟斑牙病的证据,且可能代表世界范围内该牙病的最早实例。然而,经电子显微镜和显微断层扫描显示,这些黄色小坑或凹陷是釉质发育不良表现,而不是代表个体患有氟斑牙病后牙齿受咀嚼压力而产生的物理破损。同步辐射扫描显示,许家窑幼年个体前部牙齿釉质密度均匀,没有出现浅层釉质矿化减小的现象,不支持该个体因釉质矿化过程受影响而患有典型氟斑牙的结论。尽管如此,后部牙齿上大量坑状的釉质缺陷和坑状缺陷底部的加重生长线特征不排除是个体氟摄入过量而影响釉质形成的分泌期而导致的。除表面坑状釉质缺陷外,许家窑幼年个体恒齿不同部位的釉质内部出现缺失（空间结构一般为圆球状）。缺失主要集中在浅层区域,沿齿尖-齿颈方向的密集程度变化与釉质发育不良位置具有一定相关性。釉质内部缺失有时互连并与釉质表面垂直。以上特征显示釉质内部缺失是釉质形成过程受影响所致,且影响因素和发生机理可能与釉质发育不良的类似。许家窑幼年个体不同牙齿在外部釉质缺陷和内部釉质缺失密集程度上的差别可能反映的是个体在发育过程中所需应对的外界扰动因素程度不同。未来研究可对包含许家窑人化石的堆积物中以及许家窑人牙齿中的氟含量进行测定,以进一步研究许家窑人个体的生活环境中是否有过量的氟以及许家窑人是否摄入了过量氟元素,从而对许家窑人的牙齿发育缺陷机理有一个进一步的了解。     

东亚中更新世古人类下颔第二臼齿釉质-齿质连接面三维形状和釉质厚度分布

东亚中更新世古人类在头骨、下颌骨、牙齿等解剖部位表现出不同程度的形态多样性,中期成员代表为直立人,而晚期成员的演化地位具有较大争议。为进一步了解东亚中更新世古人类内部的形态变异特点和为东亚中更新世晚期古人类分类提供依据,本文使用微分同胚的表面匹配（Diffeomorphic Surface Matching, DSM）和形态测量图（Morphometric map）对下颌第二臼齿（M₂）釉质-齿质连接面的形状和齿冠侧面釉质厚度分布模式进行了量化分析。结果显示：1）东亚中更新世古人类与晚期人属成员（尼安德特人和现代人）存在较明显的形态差别;2）该时段晚期的东亚古人类相对中期直立人在侧面釉质厚度分布规律上具有独特性,并在釉质-齿质连接面的三维形状上与晚期人属成员更加接近。本文在以往对东亚中更新世古人类牙齿内外结构单个性状研究的基础上,使用三维形态测量方法进一步量化了M₂釉质-齿质连接面三维形状和侧面釉质厚度分布模式两项重要特征的变异特点,这对未来该时段同类型牙齿的形态鉴定以及解决东亚中更新世晚期古人类的分类地位具有一定意义。     

广西化石猩猩牙齿釉质厚度研究

华南和东南亚发现大量更新世的猩猩牙齿化石。本研究应用CT扫描三维重建的技术方法研究了广西更新世化石猩猩牙齿釉质厚度,并与现生类人猿、现代人、化石类人猿以及早期人类进行比较分析。结果显示:广西猩猩同类牙齿的釉质厚度与牙齿大小相关性很小;臼齿和前臼齿釉质厚度在上下颌之间不存在显著性差异;来自广西不同地区的猩猩化石牙釉质厚度无显著差异。与早期人科成员相比,广西猩猩的牙釉质相对较薄,平均与相对釉质厚度值都明显小于南方古猿、傍人。与早期人属相比,小于直立人、尼人以及非洲和欧洲的早期人属化石。与现代人和现生灵长类相比,广西化石猩猩釉质厚度明显大于大部分猴类和非洲大猿;平均釉质厚度稍大于现生猩猩,而与现代人更为接近;相对釉质厚度小于现代人,而与现生猩猩差异不大,都属于偏厚型釉质。本文讨论了釉质厚度与系统分类演化、食性适应的相关问题,作者推测釉质厚度可能是物种的特征属性,与牙齿功能适应有密切关联。     

埃迪卡拉纪晚期高家山生物群中瓶状微化石新材料

高家山瓶状微化石为一类发现于陕南宁强高家山生物群Conotubus-Gaojiashania-Protolagena组合带中的微体化石。借助扫描电子显微镜对高家山瓶状微化石的形态特征进行观察,发现在瓶状微化石外壳表面具有浅坑与水滴状构造;运用阴极发光技术研究化石壳壁结构和壳腔内部结构,发现一个瓶状微化石内部存在球状构造。这些化石新材料中的微构造不仅丰富了我们对高家山瓶状微化石形态的认知,还加深了我们对前寒武纪原生生物演化的理解。     

周口店田园洞梅花鹿年龄结构分析

从牙齿主尖釉质层、齿质暴露程度、齿窝封闭情况、齿冠的相对高度、咀嚼面的磨蚀程度及牙冠齿缘釉质层的联合程度等方面对田园洞梅花鹿的年龄结构进行了划分.研究结果显示,中年、青年个体占主体,其次为幼年和老年个体.这表明动物死亡的原因不是自然死亡,很可能是史前人类狩猎造成的灾害性死亡.     

哺乳动物化石牙齿釉质的碳,氧同位素组成与古气候重建方面的研？…

哺乳动物化石牙齿釉质能有效地抵抗成岩作用的影响,并保存原始的碳、氧稳定同位素组成信息。通过对食草类哺乳动物化石牙齿釉质同位素组成的分析可以重建这些动物生存时代的古气候。釉质碳酸盐的碳同位素组成响应于取食植物的碳同位素组成,藉此可以恢复陆地生态系统中Ｃ３和Ｃ４植物的分布比例,这个比例主要受控于大气的ＣＯ２水平、气压和光照等因素,与不同的纬度带和气候带有关,釉质磷酸盐的氧同位素组成响应于饮用水的氧同位     

论非洲叶肢介科的分类

叶肢介化石生长线下缘锯齿状构造曾作为非洲叶肢介科(Afrograptidae)分类的主要特征,通过扫描图像,从比较解剖学研究入手,揭示了现生与化石叶肢介壳瓣的锯齿构造是由于分布于生长线的一排刚毛,基部关节脱落而形成的;分析了生长线刚毛的形态是属于长针形的轴刚毛,主要司触角功能;在5科18属现生叶肢介中,至少3科7属32种具有生长线刚毛,22属化石叶肢介有锯齿构造;作者认为这一构造被视为非洲叶肢介科分类的主要依据是不合适的,壳瓣的放射褶或粗瘤构造在高级分类上更重要,进而对该科的含义进行了厘定;从壳瓣具有多条放射褶这一构造特征来看,它与小叶肢介超科(Estheriellioidea)的成员在发生关系上比较密切,小叶肢介超科可提升为亚目(Estheriellidea),包括小叶肢介超科和非洲叶肢介超科,是中生代初兴起的一个类群。在白垩纪中期消失。     

Postcanine microstructure in Cricodon metabolus,a Middle Triassic gomphodont cynodont from south‐eastern Africa

Cricodon metabolus is a trirachodontid cynodont from the Anisian (Middle Triassic) of eastern and southern Africa. It has labiolingually expanded (gomphodont) postcanines but also a sectorial tooth in the last postcanine locus. In this paper, we examine the crown microstructure of isolated sectorial and gomphodont postcanines belonging to the holotype specimen of this taxon using scanning electron microscopy. The enamel of both teeth is prismless and composed of discontinuous columnar divergence units, supporting the consistent presence of synapsid columnar enamel in cynognathians. Abundant tubules and numerous irregularly spaced incremental lines are also visible in the enamel and dentine layers in each tooth. This study reveals that the enamel thickness varies along the tooth row in Cricodon as the enamel layer of the gomphodont postcanines is 11.5 times thicker than that of the sectorial crown. It is likely that this difference reflects occlusal stresses and fewer replacements in gomphodont postcanines relative to sectorial teeth. Approximately 100 incremental growth lines of von Ebner are present in the dentine layer, indicating that the deposition of the dentine by odontoblasts occurred for three months before the animal's death.     

Enamel in the oral teeth of Latimeria chalumnae (Pisces: Actinistia): a scanning electron microscope study

An investigation with the scanning electron microscope into the microstructure of the surface layer covering the oral teeth of Latimeria chalumnae has shown this tissue to be enamel of the type found in amphibians, reptiles and mammals. It is not comparable with enameloid, cuticular enamel or terminal membrane enamel as described in scanning electron microscope accounts of the teeth of actinopterygians. Equidistant lamellations parallel to the enamel-dentine junction are a distinctive feature, interpreted in this study as phasic appositional growth, a characteristic of the ectodermal type of enamel. These conclusions together with those from histological and microradiographic studies confirm that enamel is present in coelacanths.
The microstructure of enamel in the teeth of Latimeria an extant actinistian compares well with that of fossil crossopterygian teeth described from polarized light studies and indicates that enamel, homologous with the ectodermal type of enamel is found in both actinistians and rhipidistians.     

Enamel and dentine ultrastructure in the early Jurassic therian Kuehneotherium

Three fragmentary molars of Kuehneotherium from Wales were progressively abraded by grinding and studied by scanning electron microscopy. A fourth molar was reduced to small blocks, thin sections of which were examined by transmission electron microscopy. Enamel showed a 'preprismatic' pattern, consisting of columns of crystals disposed as pinnae but not separated by an interprismatic substance. No enamel tubules were observed. Incremental lines were present. Inner dentine was permeated by numerous tubules not surrounded by peritubular dentine but a peripheral dentine layer adjacent to the enamel-dentine junction was atubular. Calcified deposits were occasionally observed in the lumen of dentine tubules, some of which were interpreted here as dentinal sclerosis consecutive to masticatory wear.     

Observations on the polyphyodont dentition of Hemiphractus proboscideus (Anura: Hylidae)

In Hemiphractus fang–like teeth are ankylosed to the premaxilla, maxilla and prevomer, and bony odontoids are found on the dentary, angular and palatine bones. The odontoids are small, but a larger pair at the front of the lower jaw project upwards and backwards into the mouth and fit into a diastema between the anterior premaxillary teeth when the mouth is closed.
The teeth are unipartite and monocuspid, and each consists of a strongly recurved and elongated cone of orthodentine, capped at the tip by a thin layer of enamel. The inner circumpulpal layer of the dentine is tubular, but no tubules are present in the outer pallial layer. During tooth development, dentine is formed before the enamel matrix is produced, and the tooth germs lie horizontally beneath the ventral surface of each dentigerous bone. On eruption, the tooth germs migrate horizontally and become ankylosed to the outer edge of the jaw bone by a layer of cellular cementum.
During tooth replacement, the vast majority of the dentine of each tooth, and the cementum at the tooth base, are resorbed by osteoclasts. It is not clear whether the tips of the teeth are shed or not.     

Visualization of initial bacterial colonization on dentine and enamel in situ

Bacterial colonization of dentine is of high relevance in cariology, endodontology and periodontology. The aim of the present in situ study was to establish recent methods for visualization and quantification of initial bacterial adherence to dentine in comparison to enamel. For this purpose, bovine enamel and dentine slabs were fixed on buccal sites of individual upper jaw splints worn by 6 subjects for 30 min, 120 min and 360 min, respectively. Adherent bacteria on the slabs were visualized and quantified with DAPI-staining (4′,6-diamidino-2-phenylindole) and fluorescence in situ hybridization (FISH) of streptococci and eubacteria using the CLSM (confocal laser scanning microscopy) as well as an epifluorescence microscope. In addition, the number of colony forming units was quantified after desorption. Representative samples were processed for SEM (scanning electron microscopy) and TEM (transmission electron microscopy). All methods clearly indicated that a significantly higher number of bacteria adhered to dentine than to enamel. Furthermore, the amount of bacteria on the dentine increased with increasing oral exposure time, but remained rather constant on the enamel. The CLSM allowed visualization of bacteria in the dentinal tubules. Bacteria were found preferentially at the openings of the dentine tubules, but were distributed randomly on the enamel.In conclusion, the adopted methods are suitable for visualization and quantification of bacterial adhesion to dentine. Even the initial bacterial colonization of dentine is much more pronounced than bacterial adherence to the enamel.     

Scanning electron microscope study of cat and dog enamel structure

Scanning electron microscopy revealed several similarities as well as significant differences in the enamel structure between cat and dog teeth. Three enamel layers were present in both species; a surface rodless (aprismatic) layer, an outer layer of parallel rods (only at some sites), and an inner layer with prominent Hunter-Schreger bands. In the inner layer of both carnivores, the diameter of individual rods varied significantly and frequently their course changed abruptly with respect to neighboring rods. In dog teeth the cross-sectional shape of inner enamel rods was pleomorphic, but hexagonal in outer enamel. In contrast, cat enamel rods were rounded in both inner and outer enamel layers. Hunter-Schreger bands of cats circumscribed the teeth in relatively straight segments, but these bands showed pronounced waviness in dog teeth. In cats and dogs the surface rodless layer was structurally continuous with subjacent interrod enamel and covered all tooth surfaces with the exception of the cervical areas. The data show that the structure of inner and outer enamel layers differ between these two carnivore species and that the enamel structure of the cat was most similar to that described in humans. One principal difference between carnivore and human teeth is that the growth lines of carnivores do not terminate at perikymata on the tooth surface.     

Development of larval and transformed teeth in Ambystoma mexicanum (Urodela, Amphibia): an ultrastructural study

Odontogenesis of early larval non-pedicellate teeth, late larval teeth with a more or less distinct dividing zone and fully transformed pedicellate teeth in Ambystoma mexicanum (Urodela) was studied to obtain insights into the development of differently structured teeth in lower vertebrates. Using transmission electron microscopy we investigated five developmental stages: (1) papilla; (2) bell stage (secretion of the matrix begins); (3) primordium (mineralization and activity of ameloblasts starts); (4) replacement tooth (young, old); and (5) established, functional tooth. Development of the differently structured teeth is largely identical in the first three stages. Mineralization takes place in apico-basal direction up to the (prospective) pedicel (early and some late larvae) or up to the zone that divides the late larval and transformed tooth in pedicel and dentine shaft (pedicellate condition). Mineralization starts directly at the collagen and by means of matrix vesicles. First odontoblasts develop small processes that extend to the basal lamina of the inner epithelial layer of the enamel organ. The processes are small and lack organelles in early larval teeth, but become larger, arborescent, and contain some organelles in late larval and transformed teeth. The processes are surrounded by unmineralized matrix (predentine). Odontoblasts at the basis of the teeth, at the pedicel, and in the zone of division do not develop significant cytoplasmic processes that extend into the matrix. Cells of the inner enamel epithelium differentiate to ameloblasts that secrete the enamel. In the early larval tooth they show an extensive basal labyrinth that becomes regressive when the enamel layer is completed. In late larval and transformed teeth, however, a large cavity arises between the basal ruffled border of ameloblasts and their basal lamina. This cavity appears to mediate amelogenesis. A small apical zone in early, but not in late larval teeth directly below the thin enamel layer consists of enameloid and is free of dentine channels.     

Oxalate solution and collagen-oxalate solution as protective liners for dentine.

The aim of the present study was to evaluate under scanning electron microscopy the ability of different chemically reactive solutions to form a protective layer on dentine. The materials selected were an oxalate solution, a collagen-oxalate solution, a collagen-oxalate solution plus glutaraldehyde and a saline control solution. Small dentine fragments, obtained from extracted human teeth, were treated with the various chemical solution for 60 seconds. All samples were then examined in a Jeol scanning electron microscope. The preliminary observations suggest that dentine may be covered by a mixture of oxalate crystals and collagen producing a homogeneous layer of reactive agents.     

Quantitative, qualitative and topographic distribution of lead, zinc, iron and copper in hard teeth tissues

The objectives of the paper included a quantitative evaluation qualitative and topographic distribution of four microelements, namely lead, zinc, iron and copper, within enamel prisms, interprismatic region, tubular dentine, and intertubular dentine. The studies were carried out with the use of an X-ray microanalyser and an electron scanning microscope. The values of lead, zinc, iron and copper were higher in the enamel. Topographic curves for all the elements were similar within the enamel and dentin, characterized by unevenly distributed flat zero segments along with several peaks of diversified amplitude, being somewhat denser in the enamel. Qualitative distribution of the elements was also similar, and slightly denser within the enamel, the grains being unevenly scattered.