首页> 外文期刊>Deep-Sea Research. PART I, Oceanographic Research Papers >Gouge marks on deep-sea mud volcanoes in the eastern Mediterranean: Caused by Cuvier's beaked whales?
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Gouge marks on deep-sea mud volcanoes in the eastern Mediterranean: Caused by Cuvier's beaked whales?

机译:地中海东部深海泥火山上的凿痕:是居维叶喙鲸造成的吗?

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Enigmatic seafloor gouge marks at depths of 1700-2100m have been observed from submersible during geological survey work studying mud volcanoes in the eastern Mediterranean Sea. The marks consist of a central groove (about 10 cm deep and 1-2 m long), superimposed on a broader bowl-shaped depression (1-2 m long by about 50 cm wide) with raised rims (up to 10cm high) to either side of the central groove. We discuss the potential biological causes of these marks, and conclude that they are probably created by Cuvier's beaked whales (Ziphius cavirostris) during foraging dives to these depths. The mud volcanoes have a comparatively rich and diverse benthic ecology associated with methane-rich fluid seeps and thus could be the base of food chains that reach top predators like the deep-diving whales. The characteristic high acoustic backscatter of the mud volcanoes would facilitate their detection by the echolocation system of these whales.
机译:在研究地中海东部泥火山的地质调查工作中,从潜水器中观察到了1700-2100m深度的神秘海底凿痕。标记由中央凹槽(深约10 cm,长1-2 m)组成,该凹槽重叠在较宽的碗状凹陷处(长度为1-2 m,宽约50 cm),边缘凸起(最大10 cm)。中央凹槽的任一侧。我们讨论了这些标记的潜在生物学原因,并得出结论,它们可能是居维叶喙鲸(Ziphius cavirostris)在觅食潜水至这些深度时造成的。泥火山具有相对丰富和多样的底栖生态学,与富含甲烷的流体渗漏有关,因此可能成为食物链的基础,这些食物链可以到达深海捕鲸等顶级捕食者。泥火山的特征性高声学反向散射将有助于通过这些鲸鱼的回声定位系统对其进行检测。

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