首页> 美国卫生研究院文献>Proceedings of the Royal Society B: Biological Sciences >Bathyal feasting: post-spawning squid as a source of carbon for deep-sea benthic communities
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Bathyal feasting: post-spawning squid as a source of carbon for deep-sea benthic communities

机译:海底盛宴:产卵后的鱿鱼是深海底栖生物群落的碳源

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摘要

In many oceanic carbon budgets there is a discrepancy between the energetic requirements of deep-sea benthic communities and the supply of organic matter. This suggests that there are unidentified and unmeasured food sources reaching the seafloor. During 11 deep-sea remotely operated vehicle (ROV) surveys in the Gulf of California, the remains (squid carcasses and hatched-out egg sheets) of 64 post-brooding squid were encountered. As many as 36 remains were encountered during a single dive. To our knowledge this is one of the largest numbers of natural food falls of medium-size deep-sea nekton described to date. Various deep-sea scavengers (Ophiuroidea, Holothuroidea, Decapoda, Asteroidea, Enteropneusta) were associated with the remains. Although many of the 80 examined ROV dives did not encounter dead squids or egg sheets (n = 69), and the phenomenon may be geographically and temporally restricted, our results show that dead, sinking squid transport carbon from the water column to the seafloor in the Gulf of California. Based on food fall observations from individual dives, we estimate that annual squid carcass depositions may regionally contribute from 0.05 to 12.07 mg C m−2 d−1 to the seafloor in the areas where we observed the remains. The sinking of squid carcasses may constitute a significant but underestimated carbon vector between the water column and the seafloor worldwide, because squid populations are enormous and are regionally expanding as a result of climate change and pressure on fish stocks. In the future, standardized methods and surveys in geographical regions that have large squid populations will be important for investigating the overall contribution of squid falls to regional carbon budgets.
机译:在许多海洋碳预算中,深海底栖生物群落的能量需求与有机物供应之间存在差异。这表明有未确定和无法计量的食物来源到达海底。在加利福尼亚湾进行的11次深海遥控车(ROV)调查中,发现了64只育雏后的鱿鱼的遗体(s体和孵出的卵)。一次潜水中遇到多达36具遗骸。据我们所知,这是迄今为止描述的中型深海尼顿自然食物数量最多的地区之一。各种深海清道夫(蛇皮纲,蛇皮纲,十足目,小行星,肠op虫)与遗骸有关。尽管在经过80次检查的ROV潜水中,许多没有遇到死鱿鱼或卵薄的现象(n = 69),并且该现象可能在地理和时间上受到限制,但我们的结果表明,沉没的鱿鱼将碳从水柱传输到海底。加利福尼亚湾。根据个体潜水的食物下降观察,我们估计鱿鱼的car体年沉积物可能对该区域海底的区域贡献为0.05至12.07 mg C m −2 d -1 。我们观察遗骸的区域。鱿鱼尸体下沉可能构成全球水柱和海底之间重要但被低估的碳载体,因为气候变化和鱼类种群压力的结果,鱿鱼种群数量巨大且正在区域扩张。未来,鱿鱼人口众多的地理区域的标准化方法和调查对于调查鱿鱼落对区域碳预算的总体贡献将非常重要。

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