Abstract

Testate amoebae are one of the most studied groups of microorganisms in Sphagnum peatland ecosystems and, therefore, one of the most reliable bioindicators of their ecological status. Peatland ecosystems are supported by a delicate biogeochemical balance that leads to the formation of peat, one of the main sinks of C, as a result of soil–atmosphere interaction, but currently they are one of the most threatened wetland types at their southern distribution limit. In the European continent, where climatic conditions limit peat formation, they have endured significant anthropic pressure for centuries, and the risk of loss of biodiversity linked to these ecosystems is critical. In addition, peatlands are poorly known ecosystems in the Iberian Peninsula compared with other wetlands; therefore, we have studied the chemical parameters of water and the diversity patterns of testate amoebae in the western Iberian Peninsula to better understand the current status of these ecosystems. The analysis of testate amoeba communities showed an inverse relationship between the diversity and conservation status of these peatlands, both in relation to chemical parameters (i.e., pH, electrical conductivity, phosphates) and to the proportion of anthropized area, with a marked geographical pattern in the degree of anthropogenic disturbance.

Highlights

  • Peatland ecosystems develop as a result of a complex biogeochemical balance, generating a sink for atmospheric C as a result of the soil–atmosphere interaction [1,2,3]

  • The loss of peatland ecosystems has a direct impact on the biodiversity associated with these ecosystems [7]; for this reason, they have been catalogued as a priority habitat of community interest by the Habitats Directive 92/43/EEC of the European Union [8] in order to establish protection areas and promote monitoring programs that guarantee their conservation, especially compromised by climatic conditions in southern Europe due to the greater fragility of the balance that allows for peat formation and due to the limited size and high fragmentation of this type of habitat [9,10]

  • Experiments on Swedish peatland ecosystems showed that increases in pH, electrical conductivity, dissolved inorganic nitrogen, and phosphorus are associated with the degree of anthropogenic transformation of peatland ecosystems; a decrease in these parameters has been observed in long-term peatland restoration programs [50]

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Summary

Introduction

Peatland ecosystems develop as a result of a complex biogeochemical balance, generating a sink for atmospheric C as a result of the soil–atmosphere interaction [1,2,3]. The disruption of peat generation processes due to changes in climatic conditions (e.g., droughts or high temperatures) or anthropic impact (e.g., drainage, nutrient input, peat extraction, and construction of infrastructures) leads to the release of greenhouse gasses due to peat mineralization [4,5]. This is especially critical in the context of climate change because of its positive feedback effect on global warming [6]. Testate amoebae are widely used for paleoecology inferences in peatland studies [22,28,29,30,31]

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