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Groundwater and the ecosystems that depend on them are running into a serious global threat, linked to human activities that take place on the surface. Groundwater is the main source of drinking water in the European scale, and in other regions of the planet; and, for this reason substantial, but at the same time anthropocentric, they are monitored from the point of view of physico-chemical and quantity. Although scientific research has finally recognized the ecological dimension of groundwater, there is no legislation at both Community and national level which provide for monitoring the state of biological quality of subterranean ecosystems and those who depend on them. There is a further regulatory gap, largely related to the legal vacuum in the field of bio-monitoring of the quality of the GDE, which concerns the conservation of their biodiversity. Despite this state of affairs, the preservation of the GDE and biodiversity hosting plays a crucial aspect in view of the conservation of habitats and species with high intrinsic value of conservation.

Why is the GDE-dependent fauna so important for the conservation of biodiversity at a global, EU and national level?

The reasons are many:

  1. the subterranean fauna, which is given to strictly dependent GDE, is characterized by a high rate of endemism (up to 90% of the subterranean fauna = stygobitic), is endemic to restricted areas or obvious a point endemism (single known species of a single-site collection of a single area);
  2. the subterranean fauna is often made up of true living fossils, only evidence of life forms more or less widely distributed in surface water in the geological past (at the scale of tens of thousands to millions of years ago) and whose descendants are today the 'only evidence of an extinct fauna in the area now confined to groundwater;
  3. the subterranean fauna plays numerous ecosystem services in the recycling of nutrients and oxygenation of the sediment in which they live.

But what are the main threats which alter the structure and function of the GDE?
Human activities that insist on the surface of the aquifers, springs, river environments are putting at serious risk the survival of the species that make up the biodiversity of the GDE, and because some determinants are generating pressures corresponding to a significant impact on the GDE, resulting in the extinction of species rare both in terms of abundance of geographical distribution, and because the disappearance of the communities who live and make the GDE determines the decline of ecosystem services associated with the presence of diverse animal communities.


Principali determinanti (D) e relative pressioni (P) che incidono sulle acque sotterranee. Lo stato (S) e gli impatti (I) riguardano sia le risorse idriche sotterranee, sia gli ecosistemi acquatici e terrestri connessi e dipendenti. Le risposte (R) sono i programmi d’azione delle norme UE pertinenti (in primo luogo il programma di misure di cui alla Direttiva Quadro sulle Acque) (da: Protezione delle acque sotterranee in Europa. La nuova Direttiva Acque Sotterranee – Consolidare il quadro normativo dell’UE. 2008. DOI 10.2779/86124).

Main determinants (D) and related pressures (P) affecting groundwater. The status (S) and impacts (I) concerns both the groundwater resources, both aquatic and terrestrial ecosystems and associated employees. The responses (R) are the action programs of relevant EU rules (primarily the program of measures set out in the Water Framework Directive) (from: Protection of groundwater in Europe. The new Groundwater Directive - Consolidating the framework EU regulatory. 2008. DOI 10.2779 / 86124).

1) Climate change alters the hydrological cycle thereby resulting in alternating periods of drought and periods of extremely high rainfall, triggering a cascade phenomenon that is leading to drastic reduction of capacity of the aquifers and the ecosystems that depend on it: once perennial rivers in ' Mediterranean area are becoming intermittent, with periods of extreme dry that lasts for more than three months (July-September); sources diminish their scope; sectors river fed directly from groundwater are gradually disconnecting dall'acquifero below, resulting in a lower scope concomitant to the depletion of the aquifer. By contrast, the disastrous floods in other periods of the hydrological year, leading to sharp rises in river flows, with increase in the rate of erosion of the riverbed and instability of the river corridor hyporheic with consequent alteration of its biodiversity.


I fiumi in Abruzzo a rischio: fiumi perenni che diventano intermittenti (per gentile concessione del Dr. A. Di Sabatino, Università dell’Aquila)

The rivers in Abruzzo at risk: perennial rivers that become intermittent (courtesy of Dr. A. Di Sabatino, University of L'Aquila)


Emungimento dall’acquifero e ripercussioni sul regime di portata fluviale (tratto da The Nature Conservancy).

Pumping from river and repercussions on the regime of river discharge (from The Nature Conservancy).



2) Changes in land use
Changes in land use have profound effects on the quality and quantity of underground water and the ecosystems that depend on them. The main determinants in the land-use change are farming, animal husbandry, industrial settlements, particularly concentrated along the coastlines of the Abruzzo region, the presence of urban centers of varying size and Disruptive connectivity environmental presence of purifiers, Imhoff tanks, etc .. Changes are associated with more action to contain the flood risk along the river courses, which lead to the total eradication of riparian strips with the loss of the potential to reduce nitrogen load and increase of 'soil erosion. Changes in land use are also associated with climate warming on a local scale, a situation that underlies water demand accessory for the maintenance of all field activities. The agricultural activity first generates an increase of pollutants in both surface and groundwater, where are found at increasing concentrations nitrogenous compounds, mainly in the oxidized form of nitrogen (nitrate), as the nitrogen-based fertilizers are often used in excess from farms. In recent years it also assists to an alarming increase in the concentration of ammonium in groundwater under hypoxic conditions and in the absence or marked decrease of nitrification processes both physical and biological. The European Union has set the threshold range of concentrations in groundwater but each member state has established its own limits (for Italy: from 0.084 to 52 mg / l of ammonium; European Commission, 2010), although it has been observed that concentrations greater than 0.084 mg / l are lethal for many species of invertebrates and species groundwater threshold value down to 0.035 mg / l. These contaminants are added to pesticides, although in Abruzzo their concentration in groundwater has not yet reached levels of alert.

3) Over-exploitation of water resources
The uncontrolled use of groundwater resources for agricultural and industrial is leading rapidly to a severe depletion of aquifers. In the coastal floodplains, islands and in many countries bordering the Mediterranean, this phenomenon is leading to the well known phenomenon of salt intrusion resulting salinization of coastal groundwater leaking in this way every potential use.


L’intrusione salina da sovrasfruttamento di acquiferi alluvionali costieri porta alla desertificazione e alla salinizzazione dei suoli.

The saltwater intrusion from overexploitation of coastal alluvial aquifers leads to desertification and soil salinization.


4) Pollution of groundwater
The pollution of groundwater is becoming one of the most pressing threats not only to the quality status of the resource (referred to Legislative Decree 152/2006, as amended) as well as the below-ground biodiversity and ecosystem services. Nitrate pollution is widespread, mainly in agricultural areas, but also in the vicinity of urban settlements provided purifiers undersized or obsolete. Is the increase in ammonium concentration in groundwater that reaches higher concentrations of 0.080 mg / l in the groundwater is proper, both in the environment hyporheic river. The presence of organochlorine compounds are common in coastal and inland alluvial aquifers in the vicinity of industrial sites, together with PAHs (polycyclic aromatic hydrocarbons). Heavy metals are found mainly in shallow alluvial aquifers and the environment hyporheic river where are chelated, remaining in situ for a long time.

Schema tratto da Millennium EcosystemAssessment (MA, 2005): per le acque interne in generale sono indicati i determinanti più rilevanti

Diagram taken from Millennium EcosystemAssessment (MA, 2005): for inland waters in general shows the most significant determinants.


Useful References

Batubara et al. (2014) Science-policy interfacing on the issue of groundwater and groundwater-dependent ecosystems in Europe: implications for research and policy. WIREs Water 2014. doi: 10.1002/wat2.1041.

Bertrand G. et al. (2012) Review: From multi-scale conceptualization to a classification system for inland groundwater-dependent ecosystems. Hydrogeology Journal 20: 5–25 DOI 10.1007/s10040-011-0791-5

Caschetto M., M. Barbieri, D.M.P. Galassi, L. Mastrorillo, S. Rusi, F. Stoch, A. Di Cioccio, M. Petitta (2014) Human alteration of groundwater–surface water interactions (Sagittario River, Central Italy): implication for flow regime, contaminant fate and invertebrate response. Environ. Earth Sci. DOI 10.1007/s12665-013-2584-2588.

Di Lorenzo, T., Cifoni, M., Lombardo, P., Fiasca, B., Galassi, D.M.P. (2014) Ammonium threshold values for groundwater quality in the EU may not protect groundwater fauna: evidence from an alluvial aquifer in Italy. Hydrobiologia, DOI: 10.1007/s10750-014-2018-y.

Eamus D., FroendR. (Groundwater-dependent ecosystems: the where, what and why of GDEs. Australian Journal of Botany, 2006, 54, 91–96

European Commission, 2010. Commission Staff Working Document accompanying the Report from the Commission in accordance with Article 3.7 of the Groundwater Directive 2006/118/EC on the establishment of groundwater threshold values Brussels, SEC(2010) 166 final.

Fiasca, B., Stoch, F., Olivier, M.-J., Maazouzi, C., Petitta, M., Di Cioccio, A., Galassi, D.M.P. (2014) The dark side of springs: What drives small-scale spatial patterns of subsurface meiofaunal assemblages? J. Limnol., DOI: 10.4081/jlimnol.2014.848.

Kløve B. et al. (2011a) Groundwater dependent ecosystems: Part I – Hydroecology, threats and status of ecosystems. Environ. Sci. Policy 14, 770–781.

Kløve B. et al. (2011b) Groundwater dependent ecosystems: Part II – ecosystem services and management under risk of climate change and land-use management. Environ. Sci. Policy 14, 782–793.

Kløve B. et al. (2014) Climate change impacts on groundwater and dependent ecosystems. Journal of Hydrology 518: 250–266.

Serov P, Kuginis L, Williams J.P., May 2012, Risk assessment guidelines for groundwater dependent ecosystems, Volume 1 – The conceptual framework, NSW Department of Primary Industries, Office of Water, Sydney.

UNEP, IGRAC, IWMI, UNESCO-IHPE (2014) Ecosystem-based Adaptation in Groundwater Management. 29 pp. Disponibile al link: http://www.un-igrac.org/dynamics/modules/SFIL0100/view.php?fil_Id=265.