Synchrotron µ-XRF mapping analysis of trace elements in in-situ cultured Japanese red coral, Corallium japonicum

PeerJ

article

Nozomu Iwasaki¹  Hiroshi Hasegawa²  Yusuke Tamenori³  Mutsuro Kikunaga⁴  Toshihiro Yoshimura⁵  Hikaru Sawai⁶ 

[1] Faculty of Geo-Environmental Science, Rissho University;Institute of Science and Engineering, Kanazawa University;Japan Synchrotron Radiation Research Institute;Fukada Salvage & Marine Works Co., Ltd.;Research Institute for Marine Resources Utilization, Japan Agency for Marine-Earth Science and Technology;Ibaraki College, National Institute of Technology

关键词: Synchrotron radiation spectroscopy;    µ-XRF/XAS;    Japanese red coral;    Corallium;    Growth rate;    Biogenetic carbonate;   

DOI  :  10.7717/peerj.13931

学科分类：社会科学、人文和艺术（综合）

来源: Inra

【 摘 要 】

Precious corals belong to the family Coralliidae (Cnidaria, Octocorallia), and their axis, which consists of high magnesian calcium carbonate, has long been used in jewelry. With its low growth rate and long lifespan, precious coral is a representative taxon of the vulnerable marine ecosystem. Due to years of overfishing, coral fishery has become a controversial issue. To estimate the growth rate and clarify the uptake process of trace elements in relation to the growth of the carbonate axis, Japanese red coral (Corallium japonicum) was cultured at a depth of 135 m off Takeshima Island, Kagoshima, Japan for 98 months and analyzed by microscopic X-ray fluorescence/soft X-ray photoabsorption (µ-XRF/XAS) speciation mapping. The growth rate was estimated to be 0.37 mm/year in diameter, and 10–11 growth rings were observed in a cross section of the axis. This estimated growth-rate value is the first ever to be obtained from the in-situ culture of Japanese precious coral. The fluctuation in water temperature near the in-situ-culture site was recorded for part of the culture period and then compared with the changes in the growth ring and the distribution of trace elements in a cross section of the coral axis during the same period. When the water temperature was increasing, the growth ring was light in color, sulfur and phosphorus concentrations were low, and magnesium was high. Conversely, a dark band in the growth ring, high sulfur and phosphorus, and low magnesium concentrations were observed when the water temperature was decreasing. In a cross section of the coral axis, the distribution of sulfur and magnesium from the center to the surface corresponded, respectively, to dark and light bands in the annual growth ring. Sulfur concentration was high in the dark band and low in the light band, while magnesium was negatively correlated with sulfur.

【 授权许可】

CC BY