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首页> 外文期刊>Geo-marine letters >Methane seeps on the outer shelf of the Laptev Sea: characteristic features, structural control, and benthic fauna
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Methane seeps on the outer shelf of the Laptev Sea: characteristic features, structural control, and benthic fauna

机译:Laptev海外架子上的甲烷渗透:特征,结构控制和底栖动物

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Two areas with cold methane seeps on the outer shelf of the Laptev Sea were studied by two interdisciplinary expeditions onboard the RV Akademik Mstislav Keldysh in August-September of 2017 and 2018. These fields lie in water between depths of 63 and 73 m, and in a region of growing interest to the international community. Characteristic features of the methane seeps were obtained, which include their distribution and appearance on the seabed based on acoustic anomalies and seafloor observations. The cold seeps are part of a domain striking in a SW-NE direction along the Laptev Sea Rift System, Khatanga-Lomonosov Fracture Zone, and the Gakkel Ridge junction, and its structure was determined by shallow faults on the outer shelf. These faults are related to subsidence of the outer shelf cutting the caprock formed by permafrost and gas hydrates. Faults serve as conduits for an intense bubble methane discharge at the seabed. Shallow-water methane seep fauna were described for the first time in the Siberian Arctic. The frenulate siboglinid tubeworm Oligobrachia haakonmosbiensis was among the dominant species of the methane seep communities. A newly discovered gastropod species Frigidalvania sp. was also found in abundance at the seeps as well as an ophiuroid Ophiocten sericeum. Significant differences were observed between benthic communities of the two seep fields and background fauna including integral community parameters and the presence/absence of certain species. Development of shallow methane seep communities in the Laptev Sea apparently is related to extremely oligotrophic conditions in this area.
机译:在2017年8月 - 2017年8月 - 2017年8月的RV Akademik Mstislav Keldysh船上,研究了Laptev海上外壳上有两种冷甲烷渗透的区域。这些领域在63和73米的深度之间躺在水中。对国际社会感兴趣的一个地区。获得了甲烷渗透的特征,包括基于声学异常和海底观测的海底上的分布和外观。冷渗透是沿着Laptev海Rift系统,Khatanga-Lomonosov断裂带的SW-NE方向上撞击的域的一部分,并且通过外架上的浅扰确定了它的结构。这些故障与切割多方冻土和天然气水合物形成的外壳的沉降有关。缺陷用作海底上强烈泡沫甲烷排放的导管。浅水甲烷渗漏动物在西伯利亚北极首次描述。细胞纤维素胰蛋白酶oligobrachia haokonmosbiensis是甲烷席席群落的主要种类之一。一个新发现的胃鳞茎SP。也发现渗出物的丰富以及过嘌呤Ophiocten Sericeum。两种席席领域的底栖社区与背景动物区系之间观察到显着差异,包括整体社区参数和某些物种的存在/不存在。 Laptev海中的浅甲烷渗透社区的发展显然与该地区的极其低位营养条件相关。

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