State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 3663 North Zhongshan Road, 200062 Shanghai, PR China.
Anal Chem. 2011 Oct 15;83(20):7870-5. doi: 10.1021/ac2017663. Epub 2011 Sep 20.
The presence and localization of organic matrix associated with the aragonite phase in the fibers of blue coral Heliopora coerulea skeletons were studied by in situ microRaman mapping spectra, with a spatial resolution of ~0.3 μm. Spatial variations in the amounts and chemical compositions of the fibers were imaged. The results showed that the amide I and the α-helix of amide III were perpendicular to the c-axis of fibers' growth, whereas the β-turns/sheet of amide III was in the parallel conformation. Visible S-S and C-S bonds were consistent with the XANES results, which indicated the existence of organic sulfur in coral skeletons. Regular cyclic changes between aragonite and organic matrix refined a stepping growth mode of the fibers' biomineralization. An inorganic PO(4) bond was detected and exhibited the same concentration variation trends as the v(4) aragonite bands. Instead of providing an ocean P proxy on the subseasonal to centennial scale by LA-ICPMS, the possibility was raised of producing high resolution surface ocean phosphorus records on daily environmental variation via P/Ca variation cycles determined from Raman mapping data.
通过原位微拉曼图谱,对蓝珊瑚骨骼纤维中与方解石相相关的有机基质的存在和定位进行了研究,空间分辨率约为 0.3μm。成像了纤维数量和化学成分的空间变化。结果表明,酰胺 I 和酰胺 III 的α-螺旋垂直于纤维生长的 c 轴,而酰胺 III 的β-转角/片层呈平行构象。可见的 S-S 和 C-S 键与 XANES 结果一致,表明珊瑚骨骼中存在有机硫。方解石和有机基质之间的规则循环变化细化了纤维生物矿化的阶跃生长模式。检测到无机 PO(4)键,其浓度变化趋势与 v(4)方解石带相同。通过拉曼图谱数据确定的 P/Ca 变化循环,提出了通过 Raman 图谱数据产生高分辨率的海洋磷记录的可能性,而不是通过 LA-ICPMS 在亚季节性到百年尺度上提供海洋磷的代用指标。