Effet des facteurs physiques de l'environnement sur les premiers stades de la régénération naturelle du sapin pectiné (Abies alba Mill) dans certaines stations du Jura
Abstract:Résumé — Les premières phases de la régénération du sapin ont été analysées en étudiant la germination et le comportement des semis dans des expériences menées à la fois au champ en environnement naturel et au laboratoire en conditions contrôlées. Pour atteindre ces objectifs, le vaste domaine karstique du Jura a constitué un milieu modèle de choix parce que des stations forestières typiques sont observées côte-à-côte, avec des niveaux de régénération, soit très élevés, soit très bas. L'absence de géotro… Show more
“…Silver fir is mainly found in mountainous regions characterized by their high humidity (Rolland et al 1999). Tan and Bruckert (1992) confirmed this trend by showing that soil and atmospheric humidity were the two limiting variables conditioning regeneration survival. At high elevations, the limiting factor is most probably frost (Balcar and Kacálek 2008).…”
Section: Ecology Of Silver Fir Regenerationmentioning
“…Silver fir is mainly found in mountainous regions characterized by their high humidity (Rolland et al 1999). Tan and Bruckert (1992) confirmed this trend by showing that soil and atmospheric humidity were the two limiting variables conditioning regeneration survival. At high elevations, the limiting factor is most probably frost (Balcar and Kacálek 2008).…”
Section: Ecology Of Silver Fir Regenerationmentioning
“…The same conclusion may be drawn from the findings of Š imak (1951), Duchafour and Millischer (1954), Mayer (1960), Korpel' and Vinš (1965), Jaworski (1973) and Schrempf (1978). Here, it is also worth noting that the soil moisture and ectohumus depth acknowledged by some authors to be crucial for successful fir regeneration (Calaone and Giannini, 1971;Grunda, 1972;Tan and Bruckert, 1992;Končer, 1992) could not be restricting factors in the stands sampled for this study. In particular, patches occupied by less hygrophilous and moder/mor humus-indicative plant species exhibited more abundant fir regeneration (Fig.…”
Section: The Spatial Variation Of Seedling Density and Its Probable Cmentioning
“…Currently these forests have disappeared and individuals of Abies are scattered in the abundant P. sylvestris forests. The process causing these changes could result from climatic conditions in the late Holocene being drier than they are at present; Abies is less adapted to drought than P. sylvestris (Aussenac 1980;Tan & Bruckert 1992;Guicherd 1994). However, the Pinus cembra treeline has also been lowered, and P. cembra is better adapted to dry conditions than P. sylvestris (Hättenschwiller & Körner 1995).…”
Section: Tree Limits and Trends Of Changementioning
Abstract. Current land‐use a bandonment and the current rise in temperature in the Alps both suggest that tree limits may change. When it is assumed that the climate of the early mid‐Holocene between 8000 and 5000 yr before present is analogous to that of the predicted climate of the late 21st century, palaeo‐ecological studies of the early Holocene may provide data for the prediction of the vegetation pattern in a century from now. It appears that mid‐Holocene charcoal assemblages can be used to reconstruct the spatial patterns of the vegetation before, or during, the practice of slash‐and‐burn.
Correspondence analysis (CA) of charcoal assemblages shows that an important ecological gradient is determined by elevation. However CA also shows that charcoal assemblages in profiles between 1700 and 2100 m a.s.l. are roughly stratified: the more recent assemblages from the topmost centimetres of soil are intermediate between the lowermost assemblages and assemblages from higher elevations. This suggests that the woody communities at the highest elevation were located at lower elevations at a later date. The taxonomic diversity of the soil charcoal assemblages has been compared to that of present‐day phytosociological relevés after transformation to charcoal‐equivalent data. This comparison revealed that the vegetation pattern along the altitudinal gradient in the mid‐Holocene was different from that at present. The assemblages indicate that some communities disappeared, that Picea is a late‐Holocene invading species, and that there is no strict modern analogue for the vegetation structure prior to that of 3000 yr ago. The past structure of the woody vegetation was also different from that of today. Although past vegetation is not a good analogue for predicting future vegetation patterns, it still has potential as an indicator for the potential presence of tree species where there is none today. If we assume a temperature rise, and take into account current trends of landscape use abandonment, then we can expect strong vegetation dynamics at the upper tree line in the future: Abies alba may expand to occupy elevations of ca. 1800–2000 m in mixed communities with Picea abies, Pinus sylvestris and hardwood species, and Pinus cembra may expand up to 2500–2700 m a.s.l.
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