Museo delle Scienze - MUSE, Limnology and Phycology Section, Corso del Lavoro e della Scienza 3, I-38123 Trento, Italy.
Emilia-Romagna Region, Geological Seismic & Soil Survey, Bologna, Italy; University of Parma, Dept. Physics & Earth Sciences, Parma, Italy.
Sci Total Environ. 2016 Oct 15;568:624-637. doi: 10.1016/j.scitotenv.2016.02.105. Epub 2016 Mar 4.
Springs are biodiversity hotspots and unique habitats that are threatened, especially by water overdraft. Here we review knowledge on ambient-temperature (non-geothermal) freshwater springs that achieve sufficient oversaturation for CaCO3 -by physical CO2 degassing and activity of photoautotrophs- to deposit limestone, locally resulting in scenic carbonate structures: Limestone-Precipitating Springs (LPS). The most characteristic organisms in these springs are those that contribute to carbonate precipitation, e.g.: the mosses Palustriella and Eucladium, the crenophilous desmid Oocardium stratum, and cyanobacteria (e.g., Rivularia). These organisms appear to be sensitive to phosphorus pollution. Invertebrate diversity is modest, and highest in pools with an aquatic-terrestrial interface. Internationally, comprehensive legislation for spring protection is still relatively scarce. Where available, it covers all spring types. The situation in Europe is peculiar: the only widespread spring type included in the EU Habitat Directive is LPS, mainly because of landscape aesthetics. To support LPS inventorying and management to meet conservation-legislation requirements we developed a general conceptual model to predict where LPS are more likely to occur. The model is based on the pre-requisites for LPS: an aquifer lithology that enables build-up of high bicarbonate and Ca(2+) to sustain CaCO3 oversaturation after spring emergence, combined with intense groundwater percolation especially along structural discontinuities (e.g., fault zones, joints, schistosity), and a proper hydrogeological structure of the discharging area. We validated this model by means of the LPS information system for the Emilia-Romagna Region (northern Italy). The main threats to LPS are water diversion, nutrient enrichment, and lack of awareness by non-specialized persons and administrators. We discuss an emblematic case study to provide management suggestions. The present review is devoted to LPS but the output of intense ecological research in Central Europe during the past decades has clearly shown that effective conservation legislation should be urgently extended to comprise all types of spring habitats.
泉水是生物多样性热点和独特的栖息地,尤其受到水资源过度开采的威胁。在这里,我们回顾了有关环境温度(非地热)淡水泉的知识,这些泉水通过物理 CO2 脱气和光自养生物的活动实现了足够的碳酸钙过饱和,从而沉淀出石灰石,局部形成风景优美的碳酸盐结构:石灰沉淀泉(LPS)。这些泉水中最具特色的生物是那些有助于碳酸盐沉淀的生物,例如:苔藓科的 Palustriella 和 Eucladium、喜钙的双星藻属(Oocardium stratum)和蓝藻(例如,Rivularia)。这些生物似乎对磷污染很敏感。无脊椎动物的多样性适中,在具有水生-陆地界面的水池中最高。在国际上,全面的泉水保护立法仍然相对稀缺。在有立法的地方,它涵盖了所有的泉水类型。欧洲的情况很特殊:唯一被纳入欧盟生境指令的广泛分布的泉水类型是 LPS,主要是因为景观美学。为了支持 LPS 的清查和管理,以满足保护立法的要求,我们开发了一个通用的概念模型来预测 LPS 更可能出现的地方。该模型基于 LPS 的先决条件:含水层岩性允许高碳酸氢盐和 Ca(2+) 的积累,以维持泉水涌出后碳酸钙的过饱和,同时伴随着地下水的强烈渗透,特别是沿着构造不连续带(例如,断层带、节理、片理),以及排泄区的适当水文地质结构。我们通过意大利艾米利亚-罗马涅地区(意大利北部)的 LPS 信息系统验证了该模型。对 LPS 的主要威胁是引水、养分富化以及非专业人员和管理人员缺乏意识。我们讨论了一个典型的案例研究,以提供管理建议。本综述致力于 LPS,但过去几十年中欧密集的生态研究成果清楚地表明,应迫切扩大有效的保护立法,以涵盖所有类型的泉水生境。