Grazing activities and biodiversity history in the Pyrénées - new insights on high altitude ecosystems in the framework of a Human-Environment Observatory

Reconstruction of the relationship between pastoral activities and vegetation history in the central Pyrenees demonstrates the importance of grazing pressure in the maintenance of floristic diversity in highland regions that have been abandoned

Science Highlights: Integrative Paleoscience invasive species, and forestalling secondary succession of forests following past anthropogenic activities.For the majority of cases, a return to extensive grazing activities is highly recommended.However, this suggestion is often based on present-day observations with a temporal record spanning no more than 10 years (Canals and Sebastià, 2000).
The potential of incorporating historical ecology and paleoecology in conservation biology is now recognized, including their applicability to biodiversity maintenance, conservation evaluation and changing disturbance regimes.Paleo-studies can provide guidelines for environmental managers (Swetnam et al., 1999;Valsecchi et al., 2010).The effects of long-term, human-induced disturbances (i.e., grazing pressure) on ecosystem dynamics and their biodiversity still need to be further investigated.

A Human-Environment Observatory: Insights on future dynamics
The Upper Vicdessos Valley (Ariège, eastern Pyrenees) is representative of a common scenario in the Pyrenean massif where agro-pastoral activities have reached an extremely low level, now characterized only by extensive grazing.Successional processes involving encroachment of open land and overgrowth by trees are now occurring rapidly at all altitudes.Hill slopes have all been subjected to an overwhelming encroachment of fallow land (Betula, Fraxinus, Corylus) whereas altitude zones used for summer grazing are progressively colonized by heathland (principally Juniperus communis, Calluna vulgaris, Cytisus scoparius).After thousands of years of intense agro-silvo-pastoral activities (going back to the late Neolithic period, Galop and Jalut, 1994), a rapid decline in human activities linked to rural depopulation took place during the first half of the 20 th century.
The Vicdessos Valley is therefore a particularly interesting case study.Since 2009, a Human-Environment Observatory (http://w3.ohmpyr.univ-tlse2.fr/presentation_ohm_pyr.php) headed by the laboratory GEODE was set up by the Institute of Ecology and Environment of the French National Center for Scientific Research (INEE-CNRS).It aims to monitor past and present evolutions of human-environment interactions in order to anticipate future dynamics and consequently to provide a scientific basis for understanding the functioning of social-ecological systems.This implies a close collaboration with local and governmental planners in charge of management and conservation of landscapes and ecosystems.The observatory is a multidisciplinary consortium bringing together scientists to work on integrated micro-regional research (Pyrenean Valley scale).It involves observations and measures of present dynamics (e.g., meteorological and climatic observations, experimental approaches, monitoring of plant and animal communities) and studies of past human activities over long-term timescales.The latter uses instrumental and documentary data sources, tree de-mography (dendrology), old maps, agricultural statistics, aerial photographs, and long-term sedimentary proxy data (e.g., sedimentology, biogeochemistry, pollen and charcoal) from lakes and bogs in the valley.

From over-grazing to abandonment: 200 years of grazing activities
In the Vicdessos Valley, the hanging valley of Bassiès (altitude between 1400 and 2500 m asl) lies one of the study sites of Science Highlights: Integrative Paleoscience the observatory.The research focuses on the impact of grazing activities on highaltitude ecosystems.Paleoecological data, including pollen and charcoal (>150 µm) accumulation rates and loss-on-ignition (LOI), have been retrieved from the small peat bog of Orry de Théo.This sequence illustrates the history of vegetation cover, soil erosion and fire in relation to grazing activities over the last 200 years (Fig. 1).Rarefaction analysis was undertaken on pollen data to estimate the variations of palynological richness assumed to reflect the floristic diversity, and vegetation and landscape dynamics over time (Berglund et al., 2008).The comparison of the palynological richness with documentary sources (demographic data and book records of number of cattle in the valley) provides valuable insights on the role of human-induced disturbances such as grazing activities on floristic and landscape diversity.Figure 1 shows a positive association between grazing pressure and floristic richness.This correlation remains   2).The correspondence between paleoecological data and documentary sources confirms the complementarity of the approaches.
The local case study of the Bassiès Valley gives information on diversity baselines, thresholds, and the resilience of mountainous ecosystems to anthropogenic disturbances.This study is also rich in lessons on the loss of floristic diversity related to the variability or the decline in grazing activities and to pine-dominated secondary succession in a context of under-grazing.This kind of integration of data is already being used by managers to affirm the necessity or futility of restoration actions, and especially to avoid thresholds and to reverse the trajectories of key processes.

Figure 1 :
Figure 1: Trajectories of changes observed since the beginning of the 19 th century in the Bassiès Valley based on historical and paleodata.a) Evolution of the Auzat commune population; b) Comparison between the evolution of grazing pressure recorded in agricultural statistics of the Auzat commune and the estimated palynological richness (E(Tn)) inferred from pollen records from the Orry de Théo peat bog; c) Ash content (mineral fraction; LOI 550°C) recorded in the Orry de Théo peat bog; d) Charcoal (>150 µm) accumulation rate reconstructed in the Orry de Théo peat profile; e) Pollen accumulation rates (g cm -2 a -1 ) of selected taxa recorded in the Orry de Théo peat bog.This reconstruction shows, at a local scale, the change from a scenario of over-grazing to a near-total abandonment of summer pastoral farming activities.In the 1950s, an important period of transition is noted during which grazing pressure can no longer curb the development of heathland species and tree recolonization (dashed gray line).

Figure 2 :
Figure 2: Maps based on aerial photographs (French National Geographic Institute) showing vegetation and land-use changes in the Bassiès Valley between 1962 and 2008.The grazing decline (orange area) is concomitant with increasing forest density, principally dominated by an expansion of Pinus uncinata and birch (aqua and purple areas).This density increase has been particularly rapid during the last 20 years as shown by the repeat photographs taken in the valley' s pastoral zones between 1976 and 2009.
high until around the 1920s despite a decrease in sheep numbers, whereas the presence of cattle leads to soil degradation.A threshold is reached in the 1950s: the decline of flocks associated with a modification of pastoral practices leads to under-grazing and limits the soil erosion.At the same time, the overgrowing of Juniper and Calluna heathlands and the expansion of trees (Pinus and Betula), no longer controlled by browsing, are favored.Fire signatures recorded between 1950 and 1970 may indicate the use of fire by the shepherds to restore and clear their pastures.From the beginning of the 1980s, a significant reduction in the number of farmers in the valley has progressively led to a near-total disappearance of grazing activity.In these previously grazed areas, an inevitable and probably irreversible (except through expensive restoration actions) return to forest has led to a decline in floristic diversity.Landscape dynamics are illustrated by reconstructions based on aerial photographs taken between 1962 and 2008 as well as repeat photographs showing the progression of pinedominated forest between 1976 and 2009 (Fig.