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首页> 外文期刊>Deep-Sea Research >Temporal and spatial distributions of cold-water corals in the Drake Passage: Insights from the last 35,000 years
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Temporal and spatial distributions of cold-water corals in the Drake Passage: Insights from the last 35,000 years

机译:德雷克海峡中冷水珊瑚的时空分布:近35,000年的见解

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Scleractinian corals have a global distribution ranging from shallow tropical seas to the depths of the Southern Ocean. Although this distribution is indicative of the corals having a tolerance to a wide spectrum of environmental conditions, individual species seem to be restricted to a much narrower range of ecosystem variables. One way to ascertain the tolerances of corals, with particular focus on the potential impacts of changing climate, is to reconstruct their growth history across a range of environmental regimes. This study examines the spatial and temporal distribution of the solitary scleractinian corals Desmophyllum dianthus, Gardineria antarctica, Balanophyllia malouinensis, Caryophyllia spp. and Flabellum spp. from five sites in the Drake Passage which cross the major frontal zones. A rapid reconnaissance radiocarbon method was used to date more than 850 individual corals. Coupled with U-Th dating, an age range of present day back to more than 100 thousand years was established for corals in the region. Within this age range there are distinct changes in the temporal and spatial distributions of these corals, both with depth and latitude, and on millennial timescales. Two major patterns that emerge are: (1) D. dianthus populations show clear variability in their occurrence through time depending on the latitudinal position within the Drake Passage. North of the Subantarctic Front, D. dianthus first appears in the late deglaciation (~ 17,000 years ago) and persists to today. South of the Polar Front, in contrast, early deglacial periods, with a few modern occurrences. A seamount site between the two fronts exhibits characteristics similar to both the northern and southern sites. This shift across the frontal zones within one species cannot yet be fully explained, but it is likely to be linked to changes in surface productivity, subsurface oxygen concentrations, and carbonate saturation state. (2) at locations where multiple genera were dated, differences in age and depth distribution of the populations provide clear evidence that each genus has unique environmental requirements to sustain its population.
机译:巩膜珊瑚的分布范围从热带浅海到南大洋深处。尽管这种分布表明珊瑚对多种环境条件具有耐受性,但单个物种似乎仅限于生态系统变量范围更窄的范围。确定珊瑚的耐受性的一种方法,特别是关注气候变化的潜在影响,是在一系列环境体系中重建其生长历史。这项研究审查了孤立的巩膜珊瑚石竹,南极的加迪纳,Balanophyllia malouinensis,Caryophyllia spp的时空分布。和Flabellum spp。来自德雷克通道中五个主要站点的站点。快速侦察放射性碳方法被用来对850多个单独的珊瑚进行测年。加上U-Th年代,该地区的珊瑚的年龄范围可以追溯到10万年前。在这个年龄范围内,这些珊瑚的时空分布在深度和纬度以及千禧年尺度上都有明显的变化。出现的两种主要模式是:(1)石竹种群根据德雷克海峡内的纬度位置,其发生的时间具有明显的变异性。在南亚极锋的北部,石竹D. dianthus最早出现在冰期晚期(〜17,000年前),一直持续到今天。相反,在极地线以南,是冰河早期,有一些现代事件。两个前沿之间的海山遗址表现出与北部和南部遗址相似的特征。尚未完全解释一个物种内额叶带的这种变化,但可能与表面生产力,地下氧浓度和碳酸盐饱和状态的变化有关。 (2)在有多个属的年代,种群年龄和深度分布的差异清楚地证明了每个属都具有维持其种群的独特环境要求。

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