The Marsh’s Membrane: A Key-Role for a Forgotten Structure
Recent imaging methods applied to the growing edge of the Pinctada margaritifera shell allow for a better appreciation of ancient structural data. Growth of the Pinctada shell (both lateral extension and thickness increase) is a coordinated mechanism involving a series of clearly identified steps in contrast to the prevailing concept of a direct “self-assembly” process.
KeywordsPeriostracal transit Flexible shell Layered growth mode Marsh membrane
In such models, no place exists for the “innermost shell lamella” described by Marsh and Sass (1983) as “a single continuous layer which forms the inner surface of the shell … firmly attached to the mineral in the underlying calcified layer”.
Here, through a microstructural approach of the growing edge of a prismatic shell layer, an attempt is made to establish a junction between the several decade-old observations clearly neglected in current literature.
37.2 Material and Methods
Adult pearl oysters (Pinctada margaritifera) were collected alive in Tuamotu archipelago. Young samples come from the hatchery of the Direction des Ressources Marines et Minières (DRMM, the Polynesian governmental office for pearl cultivation).
Observations were carried out with optical microscopy (natural and polarized light), scanning electron microscopy in both secondary and backscattered electron modes, and atomic force microscopy in tapping mode. X-ray diffraction measurements were performed at the ID13 beam line of the ESRF (Grenoble).
37.3.1 Structure of the Flexible Shell Initiated and Developed in the Periostracal Grove
On the internal side of the periostracal film, numerous nonadjacent mineral disks are visible and regularly distributed (Fig. 37.1b, c). Every disk is growing around a non-mineralized center (Fig. 37.1d, arrows). The concentric mode of growth of the disks is visible of the outer side (Fig. 37.1e), whereas their inner side reveals a continuous granular structure (Fig. 37.1f). Using transmitted polarized light, the disks appear homogenous, each of them with a specific nuance always in the gray levels of the Newton scale (Fig. 37.1g). The single-crystal behavior of the disks is well established by the perfect superposition of the spots in a series of 27 X-ray diffractions in a single disk (Fig. 37.1h, i). Through their concentric growth mode during their transportation by the periostracum acting as a conveyor belt, the disks reach their maximal size, becoming in close contact at the distal end of the periostracal grove (Fig. 37.1j–m). Their thickness remains about 3–4 μm (Fig. 37.1m, n, black arrow).
37.3.2 Transition from Flexible to Rigid Shell: Occurrence of a New Growth Mode
SEM view of the internal side in the same area reveals the polygonal morphology of the mineral building units (Fig. 37.2b) whose single crystal behavior is obvious in transmitted polarized light (Fig. 37.2c). Transition from discoid to polygonal morphology of the mineral units is well illustrated by transmitted polarized light (Fig. 37.2d). The limits of the previously discoid units are still visible (Fig. 37.2d: blue arrows), while the mineral phase has been extended up to become in contact to the neighboring units (Fig. 37.2d: red arrows). This close contact between the newly formed polygonal units ensures the shell rigidity.
This developmental step shows the first occurrence of an additional component of the shell: the internal side of the crystal-like polygonal units is now covered by a continuous organic membrane (Fig. 37.2b: Mm) so that the mineral phase is sandwiched between the external periostracum and this internal organic membrane. Simultaneously, a completely different biomineralization pattern can be observed. Instead of an individual lateral extension of the disks, mineralization occurs as a synchronic process insuring a simultaneous increase of shell thickness (Fig. 37.2e). Once more, the organic film is visible at the internal side of the polygonal units (Fig. 37.2e, arrows). It is still present (Fig. 37.2f, arrows) when the repeated layered growth process leads the thickness of these calcareous units to be superior to their lateral dimensions, justifying the term “prism.” Closer observations of the basal surface of the prisms leave no doubt about the presence of this well-individualized membrane (Fig. 37.2g, arrows). This membrane, permanently present at the internal surface of the prisms, exhibits a granular structure rather similar to the granular structure of the mineral phase of the prisms (Fig. 37.2h–j).
37.4.1 Inadequacy of the “Direct Crystallization” Model to Account for Formation of the Prismatic Layer in the Pinctada Shell
The “molecular self-assembly process” underlying recent schemes and explicitly formulated by Calvo-Iglesias et al. (2016) cannot be applied to the outer shell layer of the Pinctada margaritifera. The two-phase mechanism briefly described in the present report was suggested by Wada (1961, Figure 8) and Wilbur (1964, Figure 10), who observed circular crystalline units growing “in oolitic aggregation” becoming progressively polygonal by mutual contact. The crystalline properties of the mineral units forming the “flexible shell” were established by Suzuki et al. (2013), but the presence of a non-mineralized center in each of these calcareous units basically modifies the interpretation of their formation and role.
37.4.2 Origin of the Crystallographic Individuality of the Calcite Prisms of the Pinctada Shell
From the deeper parts of the periostracal grove, the calcareous disks transported on the internal side of the periostracum exhibit a non-mineral center, suggesting that this organic glomerule was deposited in close vicinity to the group of cells dedicated to the formation of the periostracum itself (see histological sections in Jabbour et al. 1992). Polarization microscopy and multiple X-ray diffractions show that, in conformity to the results of Suzuki et al. (2013), the disks are crystal-like units, each of them with a specific crystalline orientation (assessed by the distinct gray levels corresponding to a 3–4 μm thickness measured by SEM; Fig. 37.1m). It can be assumed that these specific crystalline orientations take origin in the slightly diverse orientations of the organic substrates of the disks.
From this very early origin of crystallographic orientation in the transitional phase from flexible to rigid shells (Fig. 37.2d), the crystallographic orientation of the first mineral polygons forming the rigid shell relies on the crystallographic orientation of the disks after their upside-down movement. In further growth steps of the prisms, crystallographic orientation of every newly formed polygon is repeated.
Thus, conclusion arises that the long-recognized crystal-like behavior of the prisms forming the outer shell layer of the Pinctada is determined in the deeper part of the periostracal grove and is by no means the result of a “self-assembly process.”
37.4.3 The Crystal-Like Disks as Examples of Non-Ion-by-Ion Crystallization
In the search of evidences for a biological control of crystallization, we must note that all along their growth, the freely and independently crystallizing disks exhibit a concentric layering as obvious traces of their stepping growth mode. If disk crystallization was based on an ion-by-ion mechanism, the presence of calcite faces oriented in conformity with those of crystals produced by purely chemical precipitation should appear in these distant and freely growing units. This is not the case: no exception has been observed to the circular morphology and concentric mode of growth for the crystal-like units. This provides a contrario evidence for a nonionic but biochemically controlled mode of crystallization (i.e., non-purely chemical).
37.4.4 The Marsh’s Membrane as Coordinator of the Layered Growth Mode of the Prisms
Occurrence of the organic membrane covering the newly formed polygons (Fig. 37.2e) and its persistency during further development of the prisms introduce a new factor to be taken into account in the crystallization process. Its granular structure was noted from the early descriptions (Fig. 37.2k) and among the very rare mentions that have been made of this shell component. Yan et al. (2008) have well noted the time-based variability in the development of these grains, leading these authors to qualify the Marsh’s membrane as a “dynamic structure.” This means that the Marsh’s membrane is involved in the mineralization process, a conclusion here confirmed (Fig. 37.2g–j) and by previous observations (Cuif et al. 2014).
One of the most striking features of the calcite prisms in Pinctada margaritifera is the microstructural change that regularly occurs after about 150 μm growth length. After an initial stage with a single crystal structure (Fig. 37.2l), the prisms become polycrystalline (Fig. 37.2m) (Cuif et al. 2011, 2014; Checa et al. 2013).
Such a coordinated change contradicts the theory of “crystal growth competition” that postulates a selection of the best oriented crystals leading to a progressive increase of the mean diameter in a given shell.
37.4.5 The Key Role of the Marsh’s Membrane in Microstructural Evolution of the Prisms
Pinctada calcite prisms are submitted to microstructural changes during aging (Cuif et al. 2014), and composition of both the mineral and organic phases is modified before the occurrence of nacre deposition (Cuif et al. 2011). Microstructural variations of the prisms during shell growth provide evidence for time-based genetically programmed secretion process.
What is remarkable is that the repeated back-and-forth movements of the mantle due to the rhythmic mode of life of the animal leave no trace in prism microstructure. This contrast epitomizes the key role of the Marsh’s membrane in shell formation. When the animal withdraws its mantle for shell closure, the Marsh’s membrane stays in place at the basis of the prismatic layer. Thus, when the mantle returns to an actively mineralizing position, growth of the microstructural units (each of them with its specific crystalline orientation) can restart without any apparent interruption.
Under many respects understanding the Marsh’s membrane as an active interface between mantle secretions and shell is an important issue for both microstructural analysis and any attempt to create biomimetic materials.
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