Investigation of the response of coral microbial communities to seasonal ecological environment at the microscale will advance our understanding of the relationship between coral-associated bacteria community and coral health. In this study, we examined bacteria community composition from mucus, tissue and skeleton of Porites lutea and surrounding seawater every three months for 1 year on Luhuitou fringing reef. The bacterial communities were analyzed using pyrosequencing of the V1-V2 region of the 16S rRNA gene, which demonstrated diverse bacterial consortium profiles in corals. The bacterial communities in all three coral compartments studied were significantly different from the surrounding seawater. Moreover, they had a much more dynamic seasonal response compared to the seawater communities. The bacterial communities in all three coral compartments collected in each seasonal sample tended to cluster together. Analysis of the relationship between bacterial assemblages and the environmental parameters showed that the bacterial community correlated to dissolved oxygen and rainfall significantly at our study site. This study highlights a dynamic relationship between the high complexity of coral associated bacterial community and seasonally varying ecosystem parameters.

Summary: Production and release of outer‐membrane vesicles (OMVs) is known in many bacteria including human pathogens. To date, OMV release has not been reported in coral‐associated bacteria. We discovered that Vibrio shilonii AK1, a well‐studied coral pathogen, produces OMVs in culture. Transmission electron microscopy showed that V. shilonii cultures release two types of vesicles, with a single membrane or two membranes, as well as vesicle chain‐like morphotype in purified vesicle fraction. No significant difference was observed in the amount of OMVs produced by cultures grown at 20°C or 30°C. OMV proteomic analysis, never before done in a coral isolate, showed that a large number of low abundance proteins were exclusively detected in OMVs released by 20°C cultures. Further, the OMVs purified from AK1 cultures grown at both 20°C and 30°C carry N‐acylhomoserine lactone quorum sensing signals, as well as alkaline phosphatase, lipase and chitinase activities. Our results show that V. shilonii OMVs are conduits of signalling molecules, active enzymes and other proteins to its environment. These findings suggest important ecophysiological roles of OMVs in coral reef environment. We discuss the importance of OMV release for V. shilonii fitness and propose several hypotheses as well as a conceptual model.

The deep-sea environment creates the largest ecosystem in the world with the largest biological community and extensive undiscovered biodiversity. Nevertheless, these ecosystems are far from well known. Deep-sea equipment is an indispensable approach to research life in extreme environments in the deep-sea environment because of the difficulty in obtaining access to these unique habitats. This work reviewed the historical development and the state-of-the-art of deep-sea equipment suitable for researching extreme ecosystems, to clarify the role of this equipment as a promoter for the progress of life in extreme environmental studies. Linkages of the developed deep-sea equipment and the discovered species are analyzed in this study. In addition, Equipment associated with researching the deep-sea ecosystems of hydrothermal vents, cold seeps, whale falls, seamounts, and oceanic trenches are introduced and analyzed in detail. To clarify the thrust and key points of the future promotion of life in extreme environmental studies, prospects and challenges related to observing equipment, samplers, laboratory simulation systems, and submersibles are proposed. Furthermore, a blueprint for the integration of in situ observations, sampling, controllable culture, manned experiments in underwater environments, and laboratory simulations is depicted for future studies.

Pseudonocardians A–C (2–4), three new diazaanthraquinone derivatives, along with a previously synthesized compound deoxynyboquinone (1), were produced by the strain SCSIO 01299, a marine actinomycete member of the genus Pseudonocardia, isolated from deep-sea sediment of the South China Sea. The structures of compounds 1–4 were determined by mass spectrometry and NMR experiments (¹H, ¹³C, HSQC, and HMBC). The structure of compound 1, which was obtained for the first time from a natural source, was confirmed by X-ray analysis. Compounds 1–3 exhibited potent cytotoxic activities against three tumor cell lines of SF-268, MCF-7 and NCI-H460 with IC₅₀ values between 0.01 and 0.21 μm, and also showed antibacterial activities on Staphylococcus aureus ATCC 29213, Enterococcus faecalis ATCC 29212 and Bacillus thuringensis SCSIO BT01, with MIC values of 1–4 μg mL⁻¹.

Three new napyradiomycins (1–3) were isolated from the culture broth of a marine-derived actinomycete strain SCSIO 10428, together with six known related analogues napyradiomycin A1 (4), 18-oxonapyradiomycin A1 (5), napyradiomycin B1 (6), napyradiomycin B3 (7), naphthomevalin (8), and napyradiomycin SR (9). The strain SCSIO 10428 was identified as a Streptomyces species by the sequence analysis of its 16S rRNA gene. The structures of new compounds 1–3, designated 4-dehydro-4a-dechlorona pyradiomycin A1 (1), 3-dechloro-3-bromonapyradiomycin A1 (2), and 3-chloro-6, 8-dihydroxy-8-α-lapachone (3), respectively, were elucidated by comparing their 1D and 2D NMR spectroscopic data with known congeners. None of the napyradiomycins 1–9 showed antioxidative activities. Napyradiomycins 1–8 displayed antibacterial activities against three Gram-positive bacteria Staphylococcus and Bacillus strains with MIC values ranging from 0.25 to 32 μg mL⁻¹, with the exception that compound 3 had a MIC value of above 128 μg mL⁻¹ against Staphylococcus aureus ATCC 29213. Napyradiomycins 2, 4, 6, and 7 exhibited moderate cytotoxicities against four human cancer cell lines SF-268, MCF-7, NCI-H460, and HepG-2 with IC₅₀ values below 20 μM, while the IC₅₀ values for other five napyradiomycins 1, 3, 5, 8 and 9 were above 20 μM.