Translocation of ferritin and biomineralization of goethite in the radula of the limpet Cellana toreuma reeve

Nonclassical crystallization of goethite nanorods in limpet teeth by self-assembly of silica-rich nanoparticles reveals structure-mechanical property relations

The intricate organization of goethite nanorods within a silica-rich matrix makes limpet teeth the strongest known natural material. However, the mineralization pathway of goethite in organisms under ambient conditions remains elusive. Here, by investigating the multi-level structure of limpet teeth at different growth stages, it is revealed that the growth of goethite crystals proceeds by the attachment of amorphous nanoparticles, a nonclassical crystallization pathway widely observed during the formation of calcium-based biominerals. Importantly, these nanoparticles contain a high amount of silica, which is gradually expelled during the growth of goethite. Moreover, in mature teeth of limpet, the content of silica correlates with the size of goethite crystals, where smaller goethite crystals are densely packed in the leading part with higher content of silica. Correspondingly, the leading part exhibits higher hardness and elastic modulus. Thus, this study not only reveals the nonclassical crystallization pathway of goethite nanorods in limpet teeth, but also highlights the critical roles of silica in controlling the hierarchical structure and the mechanical properties of limpet teeth, thus providing inspirations for fabricating biomimetic materials with excellent properties.

In slow motion: radula motion pattern and forces exerted to the substrate in the land snail Cornu aspersum (Mollusca, Gastropoda) during feeding

The radula is the anatomical structure used for feeding in most species of Mollusca. Previous studies have revealed that radulae can be adapted to the food or the substrate the food lies on, but the real, in vivo forces exerted by this organ on substrates and the stresses that are transmitted by the teeth are unknown. Here, we relate physical properties of the radular teeth of Cornu aspersum (Müller. 1774 Vermium terrestrium et fluviatilium, seu animalium infusoriorum, helminthicorum, et testaceorum, non marinorum, succincta historia. Volumen alterum. Heineck & Faber, Havniæ & Lipsiæ.), a large land snail, with experiments revealing their radula scratching force. The radula motion was recorded with high-speed video, and the contact area between tooth cusps and the substrate was calculated. Forces were measured in all directions; highest forces (106.91 mN) were exerted while scratching, second highest forces while pulling the radula upwards and pressing the food against its counter bearing, the jaw, because the main ingesta disaggregation takes place during those two processes. Nanoindentation revealed that the tooth hardness and elasticity in this species are comparable to wood. The teeth are softer than some of their ingesta, but since the small contact area of the tooth cusps (227 µm²) transmits high local pressure (4698.7 bar) on the ingesta surface, harder material can still be cut or pierced with abrasion. This method measuring the forces produced by the radula during feeding could be used in further experiments on gastropods for better understanding functions and adaptations of radulae to ingesta or substrate, and hence, gastropods speciation and evolution.

From bacteria to mollusks: the principles underlying the biomineralization of iron oxide materials

Various organisms possess a genetic program that enables the controlled formation of a mineral, a process termed biomineralization. The variety of biological material architectures is mind-boggling and arises from the ability of organisms to exert control over crystal nucleation and growth. The structure and composition of biominerals equip biomineralizing organisms with properties and functionalities that abiotically formed materials, made of the same mineral, usually lack. Therefore, elucidating the mechanisms underlying biomineralization and morphogenesis is of interdisciplinary interest to extract design principles that will enable the biomimetic formation of functional materials with similar capabilities. Herein, we summarize what is known about iron oxides formed by bacteria and mollusks for their magnetic and mechanical properties. We describe the chemical and biological machineries that are involved in controlling mineral precipitation and organization and show how these organisms are able to form highly complex structures under physiological conditions.

Cloning and characterization of an IKK homologue from pearl oyster, Pinctada fucata

IkappaB kinase (IKK) play central roles in cell signaling by regulating nuclear factor-kappaB (NF-kappaB) activation, which is involved in inflammatory response, proliferation, development and bone homeostasis. We report here for the first time that an IKK homologue was cloned and functionally characterized in pearl oyster, Pinctada fucata. The full-length cDNA consists of 2546bp with an ORF encoding a 737 amino acids protein. The putative pearl oyster IKK protein (Pf-IKK) possesses the characteristic organization of the mammalian IKK proteins, namely an amino-terminal kinase domain followed by a leucine zipper region and a carboxylterminal helix-loop-helix motif. Real-time PCR (RT-PCR) analysis indicated that Pf-IKK was ubiquitously expressed in pearl oyster. We also found that lipopolysaccharides (LPS) transiently stimulates IkappaBalpha degradation, but not expression levels of Pf-IKK. When transfected into NIH3T3 cells, Pf-IKK activated the expression of NF-kappaB-controlled reporter gene and induced NF-kappaB translocation, whereas the activation was greatly deduced by pyrrolidine dithiocarbamate (PDTC). We also found that overexpression of Pf-IKK increased the alkaline phosphatase (ALP) activity significantly. Based on the results and the homology to the vertebrate NF-kappaB cascade, these studies help to highlight a potentially important regulatory pathway to the study of the related functions in mollusks.

Biomineralization of limpet teeth: A cryo-TEM study of the organic matrix and the onset of mineral deposition

The continuously growing limpet radula contains teeth at various stages of maturity and thus provides an excellent opportunity for studying the processes and mechanisms of their mineralization. We report here on our structural investigations of the pre-formed chitin matrix and the initial deposition and growth of goethite (alpha-FeOOH) crystals within the matrix. By using cryo-techniques, in which unstained sections of the teeth are examined in a frozen-hydrated state in a transmission electron microscope (TEM), we were able to characterize the process without introducing artifacts normally associated with the staining, dehydration, and embedding required for conventional TEM. The unmineralized matrix consists of relatively well ordered, densely packed arrays of chitin fibers, with only a few nanometers between adjacent fibers. There are clearly no pre-formed compartments that control goethite crystal size and shape; rather, crystals must push aside or engulf the fibers as they grow. By examining teeth nearly row-by-row around the onset of mineralization, we were able to image the first-formed mineral within the chitin matrix. These linear deposits of goethite appear to nucleate on the chitin fibers, which thus control the orientation of the crystals. Crystal growth, on the other hand, is apparently not influenced by the matrix, in contrast to many other biomineralization systems.