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The bacterial abundance and community composition in four types of soils and their associated Fe-Mn nodules from Queyu (QY) in Shandong Province, Zaoyang (ZY), Wuhan (WH) in Hubei Province and Guiyang (GY) in Hunan Province, China were investigated using real-time PCR, cloning and sequencing approaches. It was found that the bacterial 16S rRNA gene copy numbers in the soils were almost 3 magnitudes greater than those in their corresponding nodules and positively correlated with OM. The bacterial diversity as indicated by Simpson and Shannon indices, were significantly lower in the nodules than in the soils. Remarkable divergence in bacterial community structure was observed between the soils and the nodules, and the difference was the mainly explained by OM. In contrast, the differences within the soils and within the nodules were minor, suggesting significant habitat filtering for the bacterial community composition in the nodules.Acidobacteriawas the most abundant group (accounting for 28.6%–51.6%) in soil bacterial community while nodule bacterial community was predominated byProteobacteria(accounting for 62.8%– 90.5%). A number of clones closely related to well-known Mn-oxidizing, Fe-oxidizing and Fe-reducing bacteria withinProteobacteriawere retrieved mainly from nodules. [ABSTRACT FROM PUBLISHER]

The growth of molluscan shell crystals is generally thought to be initiated from the extrapallial fluid by matrix proteins, however, the cellular mechanisms of shell formation pathway remain unknown. Here, we first report amorphous calcium carbonate (ACC) precipitation by cellular biomineralization in primary mantle cell cultures of Pinctada fucata. Through real-time PCR and western blot analyses, we demonstrate that mantle cells retain the ability to synthesize and secrete ACCBP, Pif80 and nacrein in vitro. In addition, the cells also maintained high levels of alkaline phosphatase and carbonic anhydrase activity, enzymes responsible for shell formation. On the basis of polarized light microscopy and scanning electron microscopy, we observed intracellular crystals production by mantle cells in vitro. Fourier transform infrared spectroscopy and X-ray diffraction analyses revealed the crystals to be ACC, and de novo biomineralization was confirmed by following the incorporation of Sr into calcium carbonate. Our results demonstrate the ability of mantle cells to perform fundamental biomineralization processes via amorphous calcium carbonate, and these cells may be directly involved in pearl oyster shell formation.