Biology Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, United States of America.
PLoS One. 2012;7(12):e50015. doi: 10.1371/journal.pone.0050015. Epub 2012 Dec 4.
Deep-sea hydrothermal vents are subject to major disturbances that alter the physical and chemical environment and eradicate the resident faunal communities. Vent fields are isolated by uninhabitable deep seafloor, so recolonization via dispersal of planktonic larvae is critical for persistence of populations. We monitored colonization near 9°50'N on the East Pacific Rise following a catastrophic eruption in order to address questions of the relative contributions of pioneer colonists and environmental change to variation in species composition, and the role of pioneers at the disturbed site in altering community structure elsewhere in the region. Pioneer colonists included two gastropod species: Ctenopelta porifera, which was new to the vent field, and Lepetodrilus tevnianus, which had been rare before the eruption but persisted in high abundance afterward, delaying and possibly out-competing the ubiquitous pre-eruption congener L. elevatus. A decrease in abundance of C. porifera over time, and the arrival of later species, corresponded to a decrease in vent fluid flow and in the sulfide to temperature ratio. For some species these successional changes were likely due to habitat requirements, but other species persisted (L. tevnianus) or arrived (L. elevatus) in patterns unrelated to their habitat preferences. After two years, disturbed communities had started to resemble pre-eruption ones, but were lower in diversity. When compared to a prior (1991) eruption, the succession of foundation species (tubeworms and mussels) appeared to be delayed, even though habitat chemistry became similar to the pre-eruption state more quickly. Surprisingly, a nearby community that had not been disturbed by the eruption was invaded by the pioneers, possibly after they became established in the disturbed vents. These results indicate that the post-eruption arrival of species from remote locales had a strong and persistent effect on communities at both disturbed and undisturbed vents.
深海热液喷口受到重大干扰,这些干扰改变了物理和化学环境,消灭了原地栖息的动物群落。喷口场被无法居住的深海海底隔开,因此通过浮游幼虫的扩散进行再殖民对于种群的持续存在至关重要。我们监测了东太平洋隆起 9°50'N 附近的殖民化情况,以解决先驱殖民者和环境变化对物种组成变化的相对贡献、受干扰地点的先驱殖民者在改变该地区其他地方群落结构中的作用等问题。先驱殖民者包括两种腹足纲动物:一种是 Ctenopelta porifera,这是喷口场的新物种;另一种是 Lepetodrilus tevnianus,喷发前数量稀少,但喷发后数量持续增加,延迟并可能竞争过普遍存在的喷发前同属物种 L. elevatus。随着时间的推移,C. porifera 的数量减少,以及后来物种的到来,与喷口流体流量和硫化物与温度比的减少相对应。对于某些物种,这些演替变化可能是由于栖息地要求,但其他物种(L. tevnianus)或物种(L. elevatus)的出现与它们的栖息地偏好无关。两年后,受干扰的群落开始类似于喷发前的群落,但多样性较低。与之前(1991 年)的喷发相比,基础物种(管状蠕虫和贻贝)的演替似乎被延迟了,尽管栖息地化学性质更快地接近喷发前的状态。令人惊讶的是,一个没有被喷发干扰的附近群落被先驱殖民者入侵,可能是在它们在受干扰的喷口建立后。这些结果表明,来自遥远地方的物种在喷发后的到来对受干扰和未受干扰的喷口的群落都产生了强烈而持久的影响。