Environmental Biophysics and Molecular Ecology Program, Department of Marine and Coastal Sciences, Rutgers University, 71 Dudley Road, New Brunswick, NJ 08901, USA.
Department of Chemistry, Rutgers University, 73 Warren Street, Newark, NJ 07102, USA.
Science. 2017 Jun 2;356(6341):933-938. doi: 10.1126/science.aam6371.
Little is known about how stony corals build their calcareous skeletons. There are two prevailing hypotheses: that it is a physicochemically dominated process and that it is a biologically mediated one. Using a combination of ultrahigh-resolution threedimensional imaging and two-dimensional solid-state nuclear magnetic resonance (NMR) spectroscopy, we show that mineral deposition is biologically driven. Randomly arranged, amorphous nanoparticles are initially deposited in microenvironments enriched in organic material; they then aggregate and form ordered aragonitic structures through crystal growth by particle attachment. Our NMR results are consistent with heterogeneous nucleation of the solid mineral phase driven by coral acid-rich proteins. Such a mechanism suggests that stony corals may be able to sustain calcification even under lower pH conditions that do not favor the inorganic precipitation of aragonite.
关于石珊瑚如何构建其钙质骨骼,人们知之甚少。有两种流行的假说:一种是物理化学主导的过程,另一种是生物介导的过程。我们使用超高分辨率三维成像和二维固态核磁共振(NMR)光谱技术的组合,表明矿物的沉积是由生物驱动的。无定形纳米颗粒最初随机排列在富含有机物质的微环境中;然后,它们通过颗粒附着的晶体生长聚集并形成有序的霰石结构。我们的 NMR 结果与富含珊瑚酸的蛋白质驱动的固相矿物质异质成核一致。这种机制表明,即使在不利于霰石无机沉淀的较低 pH 值条件下,石珊瑚也可能能够维持钙化。