Deep-sea hydrothermal vents and methane seeps are inhabited by members of the same higher taxa but share few species, thus scientists have long sought habitats or regions of intermediate character that would facilitate connectivity among these habitats. Here, a network analysis of 79 vent, seep, and whale-fall communities with 121 genus-level taxa identified sedimented vents as a main intermediate link between the two types of ecosystems. Sedimented vents share hot, metal-rich fluids with mid-ocean ridge-type vents and soft sediment with seeps. Such sites are common along the active continental margins of the Pacific Ocean, facilitating connectivity among vent/seep faunas in this region. By contrast, sedimented vents are rare in the Atlantic Ocean, offering an explanation for the greater distinction between its vent and seep faunas compared with those of the Pacific Ocean. The distribution of subduction zones and associated back-arc basins, where sedimented vents are common, likely plays a major role in the evolutionary and biogeographic connectivity of vent and seep faunas. The hypothesis that decaying whale carcasses are dispersal stepping stones linking these environments is not supported.
BackgroundThe adaptation to, and colonization of, new habitats is often achieved via geographically or ecologically intermediate 'stepping stones' [1][2][3]. Understanding the nature of these stepping stones is thus crucial for interpreting the history of colonizations and present-day distributions, for the design of protected areas and for predicting vectors of dispersal of invasive species and of infectious diseases [2][3][4][5]. Of particular interest for biogeographers and evolutionary biologists in this context are isolated and extreme habitats with faunas and floras showing endemism and unusual adaptations, such as island archipelagos [6,7], caves [8,9], seamounts [10,11], and deep-sea hydrothermal vents and methane seeps [12][13][14]. Among these, vents and seeps are characterized by harsh environmental conditions and host unique ecosystems in which the dominant species gain their nutrients from symbiotic chemoautotrophic bacteria and are independent of photosynthetic food chains [15,16]. Vents and seeps are inhabited by members of the same higher taxa, notably siboglinid tubeworms, bathymodiolin mussels, and vesicomyid clams, but overlap on the species level is limited. This is thought to result from the different tectonic settings and physical properties of vents and seeps: whereas many vents are located in open ocean settings and are characterized by volcanic rocks and hot, metal-rich fluids, methane seeps occur on continental margins and are characterized by cold fluids, soft sediment, and carbonate rocks [15]. Vents and seeps are thus perceived as two distinct types of ecosystems that have evolutionary connections, but the nature of these connections remains controversial. Because the number of shared species increases in areas where both habitat types occur in close proximity, for example, around Japan and in t...