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沿泥炭地发育的空间换时间序列,有壳变形虫组合的演替变化。

Successional change of testate amoeba assemblages along a space-for-time sequence of peatland development.

作者信息

Zhang H, Väliranta M, Amesbury M J, Charman D J, Laine A, Tuittila E-S

机构信息

ECRU, Ecosystems and Environment Research Programme, Faculty of Biological and Environmental Sciences, University of Helsinki, P.O. Box 65, FI-00014, Finland; Helsinki Institute of Sustainability Science (HELSUS), Finland.

ECRU, Ecosystems and Environment Research Programme, Faculty of Biological and Environmental Sciences, University of Helsinki, P.O. Box 65, FI-00014, Finland; Helsinki Institute of Sustainability Science (HELSUS), Finland.

出版信息

Eur J Protistol. 2018 Oct;66:36-47. doi: 10.1016/j.ejop.2018.07.003. Epub 2018 Jul 24.

Abstract

It is well established that in ombrotrophic bogs, water-table depth (WTD) is the primary environmental control on testate amoeba distribution. However, the environmental controls on testate amoebae in minerotrophic fens are less well known and successional change in their assemblages associated with fen-bog peatland development has been scarcely investigated. Here we investigate a peatland space-for-time sequence resulting from postglacial rebound on the west coast of Finland, to assess successional patterns in testate amoeba communities and their relationships with environmental variables during peatland development. Sample sites along a 10-km transect from coast to inland ranged from a recently emerged wet meadow to a mature bog. Environmental variables (e.g., peat thickness, carbon and nitrogen content, pH, WTD and vegetation) were measured alongside testate amoeba samples. Results showed that even though the distribution of testate amoebae was to some extent determined by the succession stage, many taxa had wide WTD and pH ranges. The primary environmental control for many taxa changed along the succession. In conclusion, the ecological constraints on testate amoebae in minerotrophic systems are more complex than in bogs. The detected patterns also complicate the use of testate amoebae as a primary proxy in palaeoecological reconstructions where fen-to-bog shifts occur.

摘要

众所周知,在雨养泥炭沼泽中,地下水位深度(WTD)是对有壳变形虫分布的主要环境控制因素。然而,对矿质营养型沼泽中有壳变形虫的环境控制了解较少,并且与沼泽 - 泥炭地发育相关的其群落演替变化几乎未被研究。在此,我们研究了芬兰西海岸因冰后期回弹而形成的一个泥炭地时空序列,以评估有壳变形虫群落的演替模式及其在泥炭地发育过程中与环境变量的关系。从海岸到内陆沿着一条10公里长的样带设置的采样点,范围从最近出现的湿草甸到成熟的沼泽。在采集有壳变形虫样本的同时,测量环境变量(例如泥炭厚度、碳和氮含量、pH值、地下水位深度和植被)。结果表明,尽管有壳变形虫的分布在一定程度上由演替阶段决定,但许多分类单元具有较宽的地下水位深度和pH值范围。许多分类单元的主要环境控制因素在演替过程中发生了变化。总之,矿质营养系统中有壳变形虫的生态限制比泥炭沼泽更为复杂。所检测到的模式也使在发生从沼泽到泥炭地转变的古生态重建中,将有壳变形虫用作主要代用指标变得复杂化。

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