The Biological Crystals in Chamid Bivalve Shells: Diversity in Morphology and Crystal Arrangement Pattern
Metadatos
Mostrar el registro completo del ítemEditorial
MDPI
Materia
Bivalves EBSD Biominerals Microstructure/texture Chamidae
Fecha
2024-07-15Referencia bibliográfica
Hoerl, S.; Griesshaber, E.; Checa, A.G.; Schmahl, W.W. The Biological Crystals in Chamid Bivalve Shells: Diversity in Morphology and Crystal Arrangement Pattern. Crystals 2024, 14, 649. https://doi.org/10.3390/cryst14070649
Patrocinador
German Research Council Programmes (GR9/1234, SCHM 930/11-2); Ministerio de Ciencia e Innovación de España (PID2020116660GB-I00)Resumen
Chamid bivalves are marine organisms that live in high-energy environments and are
cemented to hard substrates. To avoid shell damage, the organisms form thick, densely ornamented
shells. Shell material consists of aragonite, and the ornamentation may be either aragonitic or calcitic.
The latter can be developed as scaly spines, rows of blades, or comarginal, radial arched lamellae.
We investigated biological crystal morphology and mode of assembly of Chama arcana and Chama
gryphoides shells. Structural characteristics were obtained from electron backscatter diffraction (EBSD)
measurements, complemented with laser confocal and BSE imaging. We found a wide range of
crystal morphologies and sizes, ranging from irregularly shaped calcite and/or aragonite prisms
to tiny and thin aragonite laths. We observed four different modes of crystal assembly patterns:
1. strongly interlocked dendritic calcite units forming the ornamentation blades; 2. aragonite laths
arranged to lamellae forming the outer shell layer, the layer adjacent to the calcite; 3. aragonite laths
arranged into blocks comprising inner shell layers or aragonitic ornamentations; and 4. shell portions
consisting of aragonite prisms, structured in size and crystal orientation, at muscle attachment sites.
These four different types of crystal arrangements were observed for the shells of the investigated
chamid species; however, they had slightly different strengths of structuring and slight variations
in crystal organisation. Additionally, we observed unique microstructural features in Chama shells:
We report ornamentation crystals resembling idiomorphic calcite and novel, twinned entities found
at the changeover between the aragonitic layers. We highlight and discuss these differences and
anomalies in this contribution.





