阿根廷深海冷渗漏的发现承载着奇特的营养联系和生物多样性

IF 2.3 3区 地球科学 Q2 OCEANOGRAPHY
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引用次数: 0

摘要

化合生态系统拥有独特的地质、生物地球化学、微生物和动物环境,为人类福祉提供关键的生态系统服务。在阿根廷大陆边缘,化合生态系统的存在仍然未知。我们首次在阿根廷深海发现了化合生态系统。我们对马尔维纳斯盆地和科罗拉多盆地的冷渗漏以及科罗拉多盆地的对照地点(无气体)的生物和地质环境进行了评估和比较。我们发现了两个冷渗漏点,它们的地貌特征(坑痕)直径分别为 500 米和 1000 米,深度⁓500 米。两个冷渗漏点的甲烷气泡都被困在海底表面,其中一个渗漏点的甲烷气泡渗入了水体。冷渗漏区栖息着大量底栖大型无脊椎动物(≥300 μm),主要由多毛类、近甲壳类和软体动物组成。阿根廷渗漏区的动物群表现出 δ13C 和 δ15N 稳定同位素特征,表明其具有多个营养级,并由化学合成和光合作用两种能量来源支持。向水体冒泡的差异与化学合成能量来源的不同营养级输入无关,这表明气体输入是由被困在海底沉积物中的气泡介导的。由于海底表层沉积物中存在气泡,因此可以探测到活跃化合生态系统的生态和营养特征。与气体羽流相比,整合海底下维度有助于以更可靠的方式增进我们对化合生态系统与海底流体流动之间相互作用的了解。这些冷渗漏具有重要的生物多样性和深海生态系统功能。它们位于石油和天然气工业开发的招标区域内,但迄今为止尚未成为保护工作的重点。这里提供的信息可以为有效的保护行动提供依据,并提高我们对全球化合生态系统分布的认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Discovery of deep-sea cold seeps from Argentina host singular trophic linkages and biodiversity

Chemosynthetic ecosystems host unique geological, biogeochemical, microbial and faunistic settings, which provide key ecosystem services for human wellbeing. In the Argentine continental margin, the existence of chemosynthetic ecosystems is still unknown. We present the first finding of chemosynthetic ecosystems in the Argentine deep sea. We assessed and compared biological and geological settings for cold seeps at Malvinas Basin and Colorado Basin and a control site (no gas) at Colorado Basin. We found two cold seeps with crater-like geomorphic features (pockmarks) of 500-m and 1000-m diameter at depths of ⁓500 m. Both cold seeps exhibited methane gas bubbles trapped at the surface of the seafloor, one exhibited seepage into the water column. Cold seeps hosted dense benthic macroinvertebrates (≥300 μm) assemblages consisting mainly of polychaetes, peracarid crustaceans and mollusks. The fauna from Argentinean seeps exhibited δ13C and δ15N stable isotope signatures indicative of multiple trophic levels, supported by both chemosynthetic and photosynthetic sources of energy. The difference in bubbling to the water column was not associated with different trophic input of chemosynthetically-derived sources of energy, suggesting that gas input is mediated by the bubbles trapped in the seafloor sediments. The presence of gas bubbles trapped in the surface sediments of the ocean floor allowed the detection of ecological and trophic characteristics of active chemosynthetic ecosystems. Integration of the sub-bottom dimension can help improve our understanding of the interactions of chemosynthetic ecosystems with seafloor fluid flow in a more reliable manner than the gas plumes. These cold seeps host significant biodiversity and ecosystem functions of the deep ocean. They fall within areas tendered for oil and gas industry development, but have not been a focus of conservation efforts to date. Information provided here can inform effective conservation actions and improve our understanding of the distribution of chemosynthetic ecosystems worldwide.

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来源期刊
CiteScore
4.60
自引率
4.20%
发文量
144
审稿时长
18.3 weeks
期刊介绍: Deep-Sea Research Part I: Oceanographic Research Papers is devoted to the publication of the results of original scientific research, including theoretical work of evident oceanographic applicability; and the solution of instrumental or methodological problems with evidence of successful use. The journal is distinguished by its interdisciplinary nature and its breadth, covering the geological, physical, chemical and biological aspects of the ocean and its boundaries with the sea floor and the atmosphere. In addition to regular "Research Papers" and "Instruments and Methods" papers, briefer communications may be published as "Notes". Supplemental matter, such as extensive data tables or graphs and multimedia content, may be published as electronic appendices.
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