The Biological Crystals in Chamid Bivalve Shells: Diversity in Morphology and Crystal Arrangement Pattern

• Published in: Crystals (Basel) 2024-07, Vol.14 (7), p.649
• Main Authors: Hoerl, Sebastian, Griesshaber, Erika, Checa, Antonio G., Schmahl, Wolfgang W.
• Format: Article
• Language: English
• Subjects: Aragonite; Assembly; biominerals; bivalves; Blades; Calcite; Calcite crystals; Carbonates; Chamidae; Composite materials; Crystal morphology; Crystal structure; Damage patterns; Diffraction patterns; EBSD; Electron back scatter; Lamellar structure; Marine biology; Microstructure; microstructure/texture; Mollusks; Morphology; Prisms; Scanning electron microscopy; Shells; Substrates; Twinning (Crystallography); Valves
• ISSN: 2073-4352; 2073-4352
• DOI: 10.3390/cryst14070649

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.