确定陆地-水生连通性对北冰洋湖泊过去气候古生态推断的影响

IF 2.4 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Boreas Pub Date : 2021-12-09 DOI:10.1111/bor.12572
Alannah M. Niemeyer, Andrew S. Medeiros, Anthony Todd, Brent B. Wolfe
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引用次数: 0

摘要

由于陆地和地下水流的变化以及沉积物和溶解营养物质的运输,永久冻土退化导致的水文连通性增加可能会对亚北极景观常见的浅水系统产生重大影响。在这里,我们基于对位于因纽维克(加拿大西北地区)附近的两个湖泊的多参数古湖沼学分析,探讨了连通性增加对水生生产力的影响。我们将周围地区几乎没有永久冻土退化证据的湖泊(PG03湖)与通过湖泊集水区的解冻多边形网络与陆地景观有多重联系的湖泊(PG 09湖)进行了对比。生物指标(指令学)和有机碳氮元素和同位素组成的比较揭示了最近不同的湖泊历史。PG03湖的摇蚊组合遵循预期的温度梯度,自1970 CE以来,变暖信号明显,而PG09湖的摇蝇组合主要对营养物质的可用性和栖息地的变化做出反应,这可能是由于与景观的水文连通性增加。在约1960年CE之后,在PG09湖观察到快速的集合和栖息地变化,以及摇蚊丰度的显著增加,随后陆地环境的输入量增加,如高C:N比(>15)和低δ13Org(−30‰)所示。高异地添加(~1960–2014 CE)后水生生产力的提高得到了C:N减少和有机质快速增加(Corg,N)的支持。这些结果表明,湖泊陆水界面连通性的增强可能会促进未来生产力的提高。同样,产量的增加也对对次级梯度弹性较低的湖泊的7月气温重建提出了挑战,因为与温度梯度正交的指标的主导地位发生了变化,可能会出现类似的失配。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Identifying the influence of terrestrial–aquatic connectivity on palaeoecological inferences of past climate in Arctic lakes

Identifying the influence of terrestrial–aquatic connectivity on palaeoecological inferences of past climate in Arctic lakes

Increased hydrological connectivity due to permafrost degradation is likely to have substantial implications for shallow aquatic systems common to sub-arctic landscapes due to changes to overland and subsurface flow of water and transport of sediments and dissolved nutrients. Here, we explore the influence of increased connectivity on aquatic productivity based on multi-parameter palaeolimnological analysis of two lakes located near Inuvik (Northwest Territories, Canada). We contrast a lake with little evidence of permafrost degradation in the surrounding area (Lake PG03) to one that has multiple connections to the terrestrial landscape through a network of thaw polygons in the lake catchment (Lake PG09). Comparisons of biological indicators (chironomids) and organic carbon and nitrogen elemental and isotope composition reveal recent divergent lake histories. The chironomid assemblage of Lake PG03 followed an expected temperature gradient, with a warming signal evident since ˜1970 CE, whereas the chironomid assemblage of Lake PG09 was found to primarily respond to nutrient availability and changes in habitat, likely as a result of increasing hydrological connectivity to the landscape. Rapid assemblage and habitat change along with a prominent increase in chironomid abundance were observed at Lake PG09 after ˜1960 CE, following a shift to greater inputs from the terrestrial environment as indicated by high C:N ratios (>15) and low δ13Corg (−30‰). Increased aquatic productivity following high allochthonous additions (˜1960–2014 CE) is supported by decreased C:N and rapidly increasing organic matter (Corg, N). These results demonstrate that increased connectivity along the terrestrial–aquatic interface for lakes is likely to foster elevated productivity in the future. Likewise, increased production poses a challenge to chironomid-inferred July air temperature reconstructions in lakes that are less resilient to secondary gradients, where analogue mismatches can occur due to shifts in dominance of indicators that are orthogonal to the temperature gradient.

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来源期刊
Boreas
Boreas 地学-地球科学综合
CiteScore
5.90
自引率
4.50%
发文量
36
审稿时长
>12 weeks
期刊介绍: Boreas has been published since 1972. Articles of wide international interest from all branches of Quaternary research are published. Biological as well as non-biological aspects of the Quaternary environment, in both glaciated and non-glaciated areas, are dealt with: Climate, shore displacement, glacial features, landforms, sediments, organisms and their habitat, and stratigraphical and chronological relationships. Anticipated international interest, at least within a continent or a considerable part of it, is a main criterion for the acceptance of papers. Besides articles, short items like discussion contributions and book reviews are published.
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