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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Morphometric variability in the diatom Fragilariopsis kerguelensis: Implications for Southern Ocean paleoceanography
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Morphometric variability in the diatom Fragilariopsis kerguelensis: Implications for Southern Ocean paleoceanography

机译:硅藻Fragilariopsis kerguelensis的形态变异性:对南大洋古海洋学的影响

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摘要

Diatoms play a central role in the ecosystem of the Southern Ocean, where they represent the main producers and carriers of organic carbon and dissolved silicon towards the deep ocean. Variability in space and time of the size of the most abundant species (Fragilariopsis kerguelensis) may directly impact the way this ecosystem functions, and also affect the nutrient balance of the global ocean, as important water masses (e.g. the Antarctic Intermediate Water) get their nutrient signature in this area. We used a biometric approach and analyzed the size variability of F. kerguelensis valves in sixty-four surface sediment samples from the Southern Ocean, in sediment trap samples from a mooring (Site PF3) at the Antarctic Polar Front (APF), and along a nearby piston core (PS1654-2). The average length and valve area of F. kerguelensis displayed a distinct increase in the proximity of the APF, and lower values to the north and south of it, and also changed markedly over seasonal cycles, as diatom blooms and nutrient availability waxe and wane. The last glacial to interglacial transition also witnesses important changes in the general shape and valve size of F. kerguelensis, with specimens from glacial intervals being ca. 30% larger than their interglacial counterparts (195 versus 150 μm2 valve area). A sharp peak in average area and a very specific valve morphology correspond to the first signs of deglaciation and concurring SST (Sea Surface Temperature) increase and sea-ice retreat. The latter, together with melting icebergs, may have contributed dissolved iron to surface waters. The highest average sizes during glacial intervals are higher than what found anywhere in the Southern Ocean today. The newly proposed proxy (valve area and shape of F. kerguelensis) may thus prove useful for the reconstruction of the past position and nutrient characteristics of the APF and “opal belt”, a region characterized by high production and export of biogenic silica, in a particularly sensitive and dynamic area such as the Southern Ocean.
机译:硅藻在南大洋的生态系统中发挥着核心作用,它们代表着有机碳和溶解硅向深海的主要生产者和载体。随着重要水团(例如南极中层水)的吸收,最丰富物种(Fragilariopsis kerguelensis)的大小在空间和时间上的变化可能直接影响该生态系统的运作方式,并影响全球海洋的营养平衡。该区域的营养素特征。我们使用了一种生物特征学方法,并分析了南大洋的64个地表沉积物样本,南极极地(APF)的系泊处(PF3站点)的沉积物陷阱样本中的kerguelensis阀门的大小变异性。附近的活塞芯(PS1654-2)。硅藻的平均长度和瓣膜面积在APF的附近显示出明显的增加,在其北部和南部显示出较低的值,并且随着硅藻的盛开和养分的可利用性的下降而在季节性周期中也发生了显着变化。最后一次冰期至冰期间过渡也见证了美洲鳗(F. kerguelensis)的总体形状和瓣膜大小发生了重要变化,冰川间隔的标本约为。比其间冰期同类产品大30%(195对150μm2的阀门面积)。平均面积的尖峰和非常特殊的瓣膜形态对应于脱冰的最初迹象,并伴随着SST(海表温度)升高和海冰退缩。后者与融化的冰山一起可能将溶解的铁带到了地表水。冰川间隔期间的平均大小最高,超过了当今南大洋的任何地方。因此,新提出的代用物(克尔弗氏菌的瓣膜面积和形状)可能有助于重建APF和“蛋白石带”的过去的位置和养分特征,该地区的特征是高产和高产生物硅的出口。一个特别敏感和充满活力的地区,例如南部海洋。

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