Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798)
Tridacna derasa shells show a crossed lamellar microstructure consisting of three hierarchical lamellar structural orders. The mineral part is intimately intergrown with 0.9 wt% organics, namely polysaccharides, glycosylated and unglycosylated proteins and lipids, identified by Fourier transform inf...
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Online Access: | https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.170622 |
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doaj-25ac9c713acb4b1e8ace1c63b55248b02020-11-25T03:59:24ZengThe Royal SocietyRoyal Society Open Science2054-57032017-01-014910.1098/rsos.170622170622Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798)O. B. A. AgbajeR. WirthL. F. G. MoralesK. ShiraiM. KosnikT. WatanabeD. E. JacobTridacna derasa shells show a crossed lamellar microstructure consisting of three hierarchical lamellar structural orders. The mineral part is intimately intergrown with 0.9 wt% organics, namely polysaccharides, glycosylated and unglycosylated proteins and lipids, identified by Fourier transform infrared spectrometry. Transmission electron microscopy shows nanometre-sized grains with irregular grain boundaries and abundant voids. Twinning is observed across all spatial scales and results in a spread of the crystal orientation angles. Electron backscatter diffraction analysis shows a strong fibre texture with the [001] axes of aragonite aligned radially to the shell surface. The aragonitic [100] and [010] axes are oriented randomly around [001]. The random orientation of anisotropic crystallographic directions in this plane reduces anisotropy of the Young's modulus and adds to the optimization of mechanical properties of bivalve shells.https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.170622bivalviatridacnidaetransmission electron microscopyelectron backscatter diffractionaragoniteyoung's modulus |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
O. B. A. Agbaje R. Wirth L. F. G. Morales K. Shirai M. Kosnik T. Watanabe D. E. Jacob |
spellingShingle |
O. B. A. Agbaje R. Wirth L. F. G. Morales K. Shirai M. Kosnik T. Watanabe D. E. Jacob Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798) Royal Society Open Science bivalvia tridacnidae transmission electron microscopy electron backscatter diffraction aragonite young's modulus |
author_facet |
O. B. A. Agbaje R. Wirth L. F. G. Morales K. Shirai M. Kosnik T. Watanabe D. E. Jacob |
author_sort |
O. B. A. Agbaje |
title |
Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798) |
title_short |
Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798) |
title_full |
Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798) |
title_fullStr |
Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798) |
title_full_unstemmed |
Architecture of crossed-lamellar bivalve shells: the southern giant clam (Tridacna derasa, Röding, 1798) |
title_sort |
architecture of crossed-lamellar bivalve shells: the southern giant clam (tridacna derasa, röding, 1798) |
publisher |
The Royal Society |
series |
Royal Society Open Science |
issn |
2054-5703 |
publishDate |
2017-01-01 |
description |
Tridacna derasa shells show a crossed lamellar microstructure consisting of three hierarchical lamellar structural orders. The mineral part is intimately intergrown with 0.9 wt% organics, namely polysaccharides, glycosylated and unglycosylated proteins and lipids, identified by Fourier transform infrared spectrometry. Transmission electron microscopy shows nanometre-sized grains with irregular grain boundaries and abundant voids. Twinning is observed across all spatial scales and results in a spread of the crystal orientation angles. Electron backscatter diffraction analysis shows a strong fibre texture with the [001] axes of aragonite aligned radially to the shell surface. The aragonitic [100] and [010] axes are oriented randomly around [001]. The random orientation of anisotropic crystallographic directions in this plane reduces anisotropy of the Young's modulus and adds to the optimization of mechanical properties of bivalve shells. |
topic |
bivalvia tridacnidae transmission electron microscopy electron backscatter diffraction aragonite young's modulus |
url |
https://royalsocietypublishing.org/doi/pdf/10.1098/rsos.170622 |
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