scholarly journals Unique phage–bacterium interplay in sponge holobionts from the southern Okinawa Trough hydrothermal vent

Author(s):  
Kun Zhou ◽  
Pei‐Yuan Qian ◽  
Ting Zhang ◽  
Ying Xu ◽  
Rui Zhang
Extremophiles ◽  
2012 ◽  
Vol 16 (2) ◽  
pp. 245-253 ◽  
Author(s):  
Hiroshi Izumi ◽  
Takuro Nunoura ◽  
Masayuki Miyazaki ◽  
Sayaka Mino ◽  
Tomohiro Toki ◽  
...  

Viruses ◽  
2022 ◽  
Vol 14 (1) ◽  
pp. 108
Author(s):  
Wang Liu ◽  
Xiaowei Zheng ◽  
Xin Dai ◽  
Zhenfeng Zhang ◽  
Wenyan Zhang ◽  
...  

Viruses are far more abundant than cellular microorganisms in the marine ecosystem. However, very few viruses have so far been isolated from marine sediments, especially hydrothermal vent sediments, hindering the understanding of the biology and ecological functions of these tiny organisms. Here, we report the isolation and characterization of a temperate bacteriophage, named PVJ1, which infects Psychrobacillus from a hydrothermal vent field in Okinawa Trough. PVJ1 belongs to the Myoviridae family of the order Caudovirales. The tailed phage possesses a 53,187 bp linear dsDNA genome, with 84 ORFs encoding structural proteins, genome replication, host lysis, etc. in a modular pattern. The phage genome is integrated into the host chromosome near the 3′-end of deoD, a gene encoding purine nucleoside phosphorylase (PNP). The phage integration does not appear to disrupt the function of PNP. The phage DNA is packaged by the headful mechanism. Release of PVJ1 from the host cell was drastically enhanced by treatment with mitomycin C. Phages encoding an MCP sharing significant similarity (≥70% identical amino acids) with that of PVJ1 are widespread in diverse environments, including marine and freshwater sediments, soils, artificial ecosystems, and animal intestines, and primarily infect Firmicutes. These results are valuable to the understanding of the lifestyle and host interactions of bacterial viruses at the bottom of the ocean.


2006 ◽  
Vol 3 (0) ◽  
pp. 1-8 ◽  
Author(s):  
Makoto Watanabe ◽  
Kenichi Hoshino ◽  
Ryota Shiokawa ◽  
Yuki Takaoka ◽  
Hideo Fukumoto ◽  
...  

2019 ◽  
Vol 11 (1) ◽  
pp. 929-947
Author(s):  
Siyi Hu ◽  
Zhigang Zeng ◽  
Xue Fang ◽  
Bowen Zhu ◽  
Xiaohui Li ◽  
...  

Abstract The sediment sources in the southern Okinawa trough (SOT) are still controversial and few studies have focused on the effects of transport processes on the elemental composition of initial terrigenous materials. Here we present rare earth element (REE) and trace element data on siliciclastic sediments from 14C age-dated Core S3, which was collected from the SOT, to provide reliable evidence for illustrating the modified effects of marine environments on terrigenous sediments deposited at different stages and exposing changes in sediment source over the past 3 ka. Compared with bulk sediments, the siliciclastic sediments in S3 have more variable REE fractionation parameters and lower middle REE (MREE) contents. Our REE data indicate that during river-sea processes, MREE-enriched fractions such as Fe–Mn oxides and carbonate were added to the original terrigenous sediments before deposition, weakening the degree of REE fractionation in the initial sediments; thus, care should be taken when using REE data from bulk samples to decipher source changes. The temporal changes in sediment source in S3 can be broadly identified based on the REE fractionation parameters of the residual fractions, and the results are largely consistent with the findings obtained by heavy mineral examinations. Units 1 and 3 are dominated by reworked shelf sediments of Changjiang origin,while the proportion of Taiwan-derived sediment is notably higher in Units 2 and 4. The sediment flux of Taiwan origin in the SOT was much smaller than previously thought. Huanghe-derived sediments and volcanic materials did not contribute significantly to the late Holocene sedimentation in the SOT. The large variations in sediment sources in S3 were possibly caused by changes in transport patterns driven by time-dependent changes in oceanic currents.


2003 ◽  
Vol 372 (3-4) ◽  
pp. 167-177 ◽  
Author(s):  
Mamoru Nakamura ◽  
Hiroshi Katao

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