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Paleolimnological records of nitrogen deposition in shallow, high-elevation lakes of Grand Teton National Park, Wyoming, USA

机译:美国怀俄明州大提顿国家公园浅高海拔湖泊中氮沉积的古植物学记录

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Reactive nitrogen (Nr) from anthropogenic sources has been altering ecosystem function in lakes of the Rocky Mountains, other regions of western North America, and the Arctic over recent decades. The response of biota in shallow lakes to atmospheric deposition of Nr, however, has not been considered. Benthic algae are dominant in shallow, high-elevation lakes and are less sensitive to nutrient inputs than planktonic algae. Because the benthic substrate is typically more nutrient rich than the water column, shallow lakes are not expected to show evidence of anthropogenic Nr. In this study, we assessed sedimentary evidence for regional Nr deposition, sediment chronology, and the nature of algal community response in five shallow, high-elevation lakes in Grand Teton National Park (GRTE). Over 140 diatom taxa were identified from the sediments, with a relatively high species richness of taxa characteristic of oligotrophic conditions. The diatom assemblages were dominated by benthic taxa, especially motile taxa. The GRTE lakes demonstrate assemblage-wide shifts in diatoms, including the following: (1) synchronous and significant assemblage changes centered on ca. A. D. 1960; (2) pre-1960 assemblages differed significantly from post-1960 assemblages; (3) pre-1960 diatom assemblages fluctuated randomly, whereas post-1960 assemblages showed directional change; and (4) changes in delta N-15 signatures were correlated with diatom community composition. These results demonstrate recent changes in shallow high-elevation lakes that are most correlated with anthropogenic Nr. It is also possible, however, that the combined effect of Nr deposition and warming is accelerating species shifts in benthic diatoms. While uncertainties remain about the potential synergy of Nr deposition and warming, this study adds shallow lakes to the growing list of impacted high-elevation localities in western North America.
机译:在过去的几十年中,来自人为来源的反应性氮(Nr)一直在改变洛矶山脉,北美洲西部其他地区和北极地区湖泊的生态系统功能。但是,尚未考虑浅水湖泊中生物区系对Nr大气沉积的响应。底栖藻类在浅水,高海拔湖泊中占主导地位,对营养物输入的敏感性低于浮游藻类。由于底栖底物通常比水柱中养分丰富,因此预计浅湖不会显示出人为Nr的证据。在这项研究中,我们评估了大提顿国家公园(GRTE)的五个浅高海拔湖泊中区域Nr沉积,沉积物年代学以及藻类群落反应性质的沉积证据。从沉积物中鉴定出140多种硅藻类群,其具有富营养条件下的特征性较丰富的类群。底栖生物类群,尤其是活动类群,是硅藻组合的主导。 GRTE湖泊表现出硅藻在整个组合范围内的变化,包括以下几方面:(1)同步且显着的组合变化集中在ca上。公元1960年; (2)1960年前的组合与1960以后的组合有显着差异; (3)1960年前的硅藻组合随机波动,而1960以后的组合显示方向变化。 (4)δN-15标记的变化与硅藻群落组成相关。这些结果表明,与人为污染最相关的浅高海拔湖泊的近期变化。但是,Nr沉积和变暖的综合作用也可能加速底栖硅藻中的物种迁移。尽管关于Nr沉积和变暖的潜在协同作用仍不确定,但这项研究在越来越多的北美西部受影响的高海拔地区中增加了浅湖。

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