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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >On the potential generality of depth-related ecologic structure in cold-seep communities: Evidence from Cenozoic and Mesozoic examples
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On the potential generality of depth-related ecologic structure in cold-seep communities: Evidence from Cenozoic and Mesozoic examples

机译:冷深群落中与深度有关的生态结构的潜在普遍性:来自新生代和中生代的证据

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摘要

Faunal communities inhabiting hydrocarbon seeps in the deep sea today show a depth-related change in their ecologic structure: the proportion of obligate ('endemic') taxa increases with depth while the abundance of predators and other background taxa decreases. Here the fossil record of seep communities is investigated for similar gradients. The middle Eocene to middle Miocene deep-water cold-seep deposits in western Washington State, USA, are from different depths: those of the middle to late Eocene Humptulips, Bear River and Whiskey Creek sites lived in depths of 500 to 2000. m, those of the late Oligocene to middle Miocene seep communities of the Lincoln Creek and Astoria Formations in depths of 16 to 900. m. These seeps were inhabited by the same taxa that inhabit cold seeps today and like their modern analogs, they show an increasing proportion of obligate taxa and a decreasing abundance of predators and other background taxa with depth. Also among late Mesozoic seep sites a depth-related change in the proportion of obligate taxa is apparent: seep communities in shallow-shelf settings harbor virtually no obligates, while seep communities in outer shelf to slope settings show a high proportion of obligates, although the constituting species have different taxonomic affinities than their Cenozoic and extant counterparts. Unlike in modern examples, differences between seep communities from outer shelf and slope depths were not seen. It is hypothesized that due to the higher Mesozoic sea-levels many seep communities on the continental shelves were located below the photic zone, where an obligate seep fauna could develop. Because an increase in the proportion of obligate taxa with depth can be seen both in the Cenozoic and in the late Mesozoic despite the different taxonomic affinities of the obligate taxa, it is suggested here that this depth-related structure is a general feature of seep faunas independent of the taxa that express this pattern.
机译:今天,居住在深海碳氢化合物渗漏的动物群落显示出与深度有关的生态结构变化:专性(“地方性”)生物分类的比例随深度而增加,而捕食者和其他背景生物的数量减少。在这里,对渗流群落的化石记录进行了类似的梯度研究。美国华盛顿州西部的始新世中期至中新世中期深水冷深沉积物来自不同深度:中新世始末Humptulips,贝尔河和威士忌溪遗址的深度在500至2000年之间。林肯溪和阿斯托里亚岩层的晚渐新世至中新世的渗流群落,深度在16至900米之间。这些渗水的栖息地与当今的冷渗水相同,并且像它们的现代类似物一样,它们显示专性分类的比例不断增加,掠食者和其他背景分类的深度逐渐减少。同样在中生代晚期的渗漏点中,明显的专性类群比例的变化是明显的:浅层架环境中的渗漏群落几乎没有专性,而外陆架至边坡环境中的渗漏群落却表现出很大的专性。组成物种具有与其新生代和现存同类不同的生物分类亲和力。与现代示例不同,未发现外部架子的渗水群落与斜坡深度之间的差异。据推测,由于中生代海平面较高,大陆架上的许多渗流群落位于光合带以下,在这里可以发展专性的渗流动物群。尽管新生代和晚生代的专长类群的亲和力各不相同,但在新生代和中生代后期都可以看到专性类群的比例随着深度的增加而增加,因此在此建议这种与深度有关的结构是渗流动物区系的普遍特征。独立于表达此模式的分类单元。

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