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Rising temperatures and sea-ice-free winters affect the succession of Arctic macrozoobenthic soft-sediment communities (Kongsfjorden, Svalbard)

机译:气温上升和无海冰的冬季影响着北极大型兽足软沉积群落的形成(Kongsfjorden,斯瓦尔巴特群岛)

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摘要

In the Arctic, the currently observed rising air temperature results in more frequent calving of icebergs. The latter derive from tidewater glaciers. Arctic macrozoobenthic soft-sediment communities are considerably disturbed by direct hits and sediment reallocation caused by iceberg scouring. With the aim to describe the primary succession of macrozoobenthic communities following these events, scientific divers installed 28 terracotta containers in the soft-sediment off Brandal (Kongsfjorden, Svalbard, Norway) at 20 m water depth in 2002. The containers were filled with a bentonite-sand mixture resembling the natural sediment. Samples were taken annually between 2003 and 2007. A shift from pioneering species (e.g. Cumacea: Lamprops fuscatus) towards more specialised taxa, as well as from surface detritivores towards subsurface detritivores was observed. This is typical for an ecological succession following the facilitation and inhibition succession model. Similarity between experimental and non-manipulated communities from 2003 was significantly highest after 3 years of succession. In the following years, similarity decreased, probably due to elevated temperatures, which prevented the fjord system from freezing. Some organisms, numerically important in the non-manipulated community (e.g. the polychaete Dipolydora quadrilobata) did not colonise the substrate during the experiment. This suggests that the community had not fully matured within the first 3 years. Later, the settlement was probably impeded by consequences of rising temperatures. This demonstrates the long-lasting effects of severe disturbances on Arctic macrozoobenthic communities. Furthermore, environmental changes, such as rising temperatures coupled with enhanced food availability due to an increasing frequency of sea-ice-free days per year, may have a stronger effect on succession than exposure time.
机译:在北极,目前观察到的气温上升导致冰山崩塌的频率增加。后者来自潮水冰川。北极大型恒河软沉积群落受到冰山冲刷造成的直接撞击和沉积物重新分配的影响。为了描述这些事件之后大型动物群落的主要演替,科学潜水员于2002年在水深20 m的Brandal(挪威挪威斯瓦尔巴特群岛的Kongsfjorden)的软沉积物中安装了28个赤陶容器。这些容器装满了膨润土-类似于天然沉积物的沙子混合物。从2003年到2007年之间,每年进行一次采样。观察到从先驱物种(例如黄瓜花(Cumacea:Lamprops fuscatus))向更专业的类群转变,以及从地表有害物向次表层有害物的转变。这对于遵循促进和抑制演替模型的生态演替来说是典型的。 2003年以来,实验和非操纵社区在连续3年继承后,其相似度最高。在接下来的几年中,相似性下降了,这可能是由于温度升高导致峡湾系统冻结所致。在非操纵群落中具有重要数字意义的某些生物(例如多毛Di Dipolydora quadrilobata)在实验过程中未在底物上定殖。这表明社区在最初的三年内还没有完全成熟。后来,定居可能受到温度上升的影响。这证明了严重干扰对北极大型动物群的长期影响。此外,环境变化,例如温度升高以及每年无海冰天频率的增加导致食物供应量增加,可能比暴露时间对继承的影响更大。

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