Global Crystallographic Texture of Freshwater Bivalve Mollusks of the Unionidae Family from Eastern Europe Studied by Neutron Diffraction

被引:6
|
作者
Pakhnevich, Alexey [1 ,2 ]
Nikolayev, Dmitry [2 ]
Lychagina, Tatiana [2 ]
Balasoiu, Maria [2 ,3 ]
Ibram, Orhan [4 ]
机构
[1] Russian Acad Sci, Borissiak Paleontol Inst, Moscow 117647, Russia
[2] Joint Inst Nucl Res, Frank Lab Neutron Phys, Dubna 141980, Russia
[3] Horia Hulubei Natl Inst R&D Phys & Nucl Engn, Bucharest 077125, Romania
[4] Danube Delta Natl Inst Res & Dev, Tulcea 820112, Romania
来源
LIFE-BASEL | 2022年 / 12卷 / 05期
关键词
crystallographic texture; pole figures; neutron diffraction; freshwater bivalve mollusk shells; Unionidae family; SHELLS; MICROSTRUCTURES;
D O I
10.3390/life12050730
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
The crystallographic texture of the whole valves of bivalve mollusks from the family Unionidae Unio pictorum Linnaeus, 1758 and Anodonta cygnea Linnaeus, 1758 is studied using pole figures measured using neutron diffraction. The use of neutron diffraction, in contrast to X-rays, makes it possible to study the valves without destroying them. Thus, we can discuss the study of the global texture of the entire valve. It was revealed that the pole figures of aragonite in the valves repeat their shape. The pole density maxima for U. pictorum from the Danube Delta and the Gulf of Finland in the Baltic Sea, living at different salinities and temperatures, differs by 0.41 mrd. The maximum value of the crystallographic texture for A. cygnea from the Danube Delta was also measured (5.07 mrd). In terms of texture sharpness, it surpasses the shell of marine bivalve mollusks, which are partially or completely composed of aragonite. Although U. pictorum and Mya arenaria Linnaeus, 1758 have different microstructures, their pole figures are very similar in isolines pattern, but differ in pole density maxima. No relationship was found between the crystallographic texture and the microstructure in U. pictorum. In addition, we report good qualitative agreement between aragonite X-ray pole figures of Sinanodonta woodiana Lea, 1834 from the Czech river Luznice, and neutron pole figures of U. pictorum from the Danube Delta.
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页数:11
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