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Hydrothermal Vents and Methane Seeps: Rethinking the Sphere of Influence

机译:热液喷口和甲烷渗出:重新思考影响范围

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Although initially viewed as oases within a barren deep ocean, hydrothermal vent and methane seep communities are now recognized to interact with surrounding ecosystems on the sea floor and in the water column, and to affect global geochemical cycles. The importance of understanding these interactions is growing as the potential rises for disturbance from oil and gas extraction, seabed mining and bottom trawling. Here we synthesize current knowledge of the nature, extent and time and space scales of vent and seep interactions with background systems. We document an expanded footprint beyond the site of local venting or seepage with respect to elemental cycling and energy flux, habitat use, trophic interactions, and connectivity. Heat and energy are released, global biogeochemical and elemental cycles are modified, and particulates are transported widely in plumes. Hard and biotic substrates produced at vents and seeps are used by “benthic background” fauna for attachment substrata, shelter, and access to food via grazing or through position in the current, while particulates and fluid fluxes modify planktonic microbial communities. Chemosynthetic production provides nutrition to a host of benthic and planktonic heterotrophic background species through multiple horizontal and vertical transfer pathways assisted by flow, gamete release, animal movements, and succession, but these pathways remain poorly known. Shared species, genera and families indicate that ecological and evolutionary connectivity exists among vents, seeps, organic falls and background communities in the deep sea; the genetic linkages with inactive vents and seeps and background assemblages however, are practically unstudied. The waning of venting or seepage activity generates major transitions in space and time that create links to surrounding ecosystems, often with identifiable ecotones or successional stages. The nature of all these interactions is dependent on water depth, as well as regional oceanography and biodiversity. Many ecosystem services are associated with the interactions and transitions between chemosynthetic and background ecosystems, for example carbon cycling and sequestration, fisheries production, and a host of non-market and cultural services. The quantification of the sphere of influence of vents and seeps could be beneficial to better management of deep-sea environments in the face of growing industrialization.
机译:尽管最初被视为贫瘠的深海中的绿洲,但现在人们认识到热液喷口和甲烷的渗漏群落可与海床和水柱中的周围生态系统相互作用,并影响全球地球化学循环。随着对油气开采,海底采矿和拖网作业造成干扰的潜在可能性的增加,理解这些相互作用的重要性也越来越高。在这里,我们综合了通气和渗流与背景系统相互作用的性质,程度,时间和空间尺度的当前知识。我们记录了有关元素循环和能量通量,栖息地利用,营养相互作用和连通性的局部发泄或渗漏点之外的扩展足迹。释放热量和能量,改变全球生物地球化学和元素循环,并以羽状形式广泛运输颗粒。在“底栖背景”动物区系中,在通风孔和渗漏处产生的坚硬生物底物被用于附着地层,庇护所,并通过放牧或流过当前位置获得食物,而颗粒物和流体通量则改变了浮游微生物群落。化学合成生产通过水,配子释放,动物运动和演替的多种水平和垂直转移途径,为许多底栖和浮游异养背景物种提供了营养,但这些途径仍然鲜为人知。共有的物种,属和科表明,深海的喷口,渗水,有机物跌落和背景群落之间存在生态和进化上的联系。然而,实际上尚未研究与不活动的通风孔,渗水和背景组合的遗传联系。通风或渗流活动的减弱在空间和时间上产生了重大转变,通常与可识别的过渡带或演替阶段建立了与周围生态系统的联系。所有这些相互作用的性质都取决于水深,区域海洋学和生物多样性。许多生态系统服务与化学合成生态系统和背景生态系统之间的相互作用和过渡相关,例如碳循环和固存,渔业生产以及许多非市场和文化服务。面对不断发展的工业化,对通风孔和渗水的影响范围进行量化可能有助于更好地管理深海环境。

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