The Qinzhou Bay-Hangzhou Bay joint belt is a significant tectonic zone between the Yangtze and Cathaysian plates, where plentiful hydrothermal siliceous rocks are generated. Here, the authors studied the distribution of the siliceous rocks in the whole tectonic zone, which indicated that the tensional setting was facilitating the development of siliceous rocks of hydrothermal genesis. According...

We used stable isotopes of carbon and nitrogen to examine the diversity of microbial populations consumed as foods at deep-sea hydrothermal vents. Invertebrate consumers at Gorda and Juan de Fuca Ridge vent sites had variable carbon isotope compositions, implying the use of more than one microbial food resource. 6’C values for consumer invertebrates at Gorda ranged between 13.2% (polynoid polyc...

Variation in larval supply to disjunct marine populations can provide insight into larval transport and delivery mechanisms, especially when compared with observations of physical transport. Daily variability in larval supply at two mussel-dominated hydrothermal vents, East Wall and Choo Choo, near 9u509N, East Pacific Rise, was quantified concurrently with hydrodynamic observations to investig...

Alvinellids have long been considered to be endemic Pacific vents until recent discovery of their presence in the Indian Ocean. Here, a new alvinellid is characterized and formally named from recently discovered vents, Wocan, Daxi, northern Both morphological molecular evidences support its placement genus Paralvinella , representing first species out Pacific. The species, described as mira n. ...

S ince their discovery in the 1970s and 1980s, giant tubeworms at hydrothermal vents and cold seeps have fascinated biologists and laymen alike—not only for their alien morphology (Figure 1), but also for epitomizing the perfect animal–microbe symbiosis. They are among the biggest worms on this planet—some over 3 m long— yet they do not eat other organisms. Tubeworms thrive independently of pho...