Introduction
The European silver fir (Abies alba Mill.) is a large tree (the tallest fir specimens in the Black Forest were even 68 m high) found in Central, Southern and Eastern Europe. The tree is regarded as an important species from the perspective of ecology, forest functioning and maintenance of forest biodiversity. Because of the tree’s dimensions, very big numbers of specimens in forest stands, wood with good mechanical properties, and the fact that it is also used for paper production, it is a commercially important species. In its natural condition, it grows in mountainous and sub-mountainous areas and in France and Poland—also in lowlands [1,2,3,4,5].
Silver fir prefers areas with higher humidity and evenly distributed rainfall at the level of 700 to 1800 mm (with exceptions). Usually, such areas are located at an altitude of 500–2000 m above sea level. In favorable conditions (cool and wet habitats) it lives for up to 600 years. In places where firs are concentrated, summer temperatures range from 14 to 19 degrees [1,3,4,6,7]
Silver fir grows on various types of fresh soils and in a wide pH range. The tree avoids very compact and wet soils. At higher altitudes, it forms poor and mixed tree stands with Norway spruce (Picea abies (L.) H.Karst), Scots pine (Pinus sylvestris L.) and, above all, Common beech (Fagus sylvayica L.). At lower altitudes it also occurs in oak-hornbeam forests. It is classified as a shade-tolerant species and the younger generations under the canopy of the main stand often create a so-called ‘seedling bank’ [1,2,3,4,5,6,7].
Silver firs are said not to be resistant to late frosts, fires and industrial air pollution, especially SO2 [3,4,6].
Firs growing in different parts of the present natural range come from different glacial refuges: the Iberian, Balkan and Apennine peninsulas. This fact has a significant impact on their current genetic diversity [8,9].
For various reasons, in many areas silver fir is now on the decline [3,6,10]. In recent years, especially in dendrochronological studies, an improvement in the condition and growth of firs has generally been noted [4,10]. However, the future of this tree, considering, the climatic changes, is not clearly defined. Some studies suggest an increase of its importance in forest resources [11,12], while others predict a regress and a decline in numbers [13,14]. According to Korpel (Jaworski) [3], forests with dominant fir have a development cycle of 400 years. The tree has been subject to numerous studies, including [15,16,17,18,19]. Just one periodical, called ‘Sylwan’, has printed over 40 publications during the last ten years.
The main goal of our research was to answer the question: is there a relationship between a potential natural community developing in specific habitat conditions and the number of potentially natural fir localities?
This article aims to present data that may shed some more light on the position of fir in potential, natural vegetation arrangements (ecosystem types) and provide some new arguments in the discussion about the habitat requirements of the species.
‘Potential natural vegetation’ (PNV) is understood as a hypothetical state of vegetation described by means of phytosociological units of vegetation (communities) that might be achieved by natural primary or secondary succession if anthropogenic influences were eliminated and the plants typical of a given region might make full use of the possibilities created by varied habitats [20].
Potential natural vegetation is determined based on a survey of actual vegetation communities as well as direct and indirect analysis of an abiotic habitat [21].
Knowledge of vegetation diversity in connection with environmental diversity provided the grounds for developing applied phytosociology [22]. The best-known uses of phytosociology are in forestry, where it is used to assess the transformations of the natural environment caused by human activities, e.g., in defining indicator (phytoindicative) properties of communities [23]. The determination of potential natural vegetation is the easiest way to establish the productive capability of a habitat. This constitutes the basis for silvicultural planning and operations [22,23]. Poland was one of the first countries to develop a map of potential natural vegetation—at a scale of 1:300,000 [21]. A map of potential vegetation for Europe, together with a description of the main vegetation formations was presented by Bohn et al. [24].
The study described here complements the findings of the work done in the years 1998–2006 as part of two research projects (grants) that were to form the basis for a program to restitute fir in the Polish part of the Sudetes [25]. The Sudetes are a mountain range about 300 km long, situated in south-western Poland and northern Czechia [26] (more information is provided in the Section 2 below). The program to restitute fir in the Sudetes, which was launched in 1999, aims to raise fir’s share in forests up to 18%. In order to achieve the aim, a number of preservative seed plantations were set up to provide afforestation material at a later stage [27,28].
The studies referred to above assessed the resources of fir in terms of its genetic diversity (isoenzyme studies) [29], the total number of sites and specimens [30], occurrence in various habitat conditions [31], growth rate, crown development and damage in various conditions [32,33], growth during the last decades (dendrochronological studies) [10], natural regeneration [34,35], soil properties at sites where it occurs [36,37], the degree of development of symbiosis with mycorrhizal fungi [25], and the impact of present and future human management on the species [25]. It was found, for instance, that Abies alba used to be common in the Sudetes at an altitude of 350–800 MASL. Firs grow here satisfactorily at sites with different exposure, representing a broad spectrum of vegetation communities and forest habitat types [30,31]. The Sudeten fir woods, significantly reduced (by 70%–80%) as a result of intensive forest management in the 19th c. and the first half of the 20th c. (promoting spruce monocultures) e.g., [25,38,39,40], in the years 1960–1990 were subject to the strong pressure of industrial pollution, especially SO2, whose average concentration in many locations exceeded 60 μg/m3, and periodically even 190 μg/m3 e.g., [25,38,39,41]. These conditions, in combination with commercial activities that failed to account for fir’s specific requirements, led to a situation in which its share in the forest composition was markedly lower than the initial 1% level [25]. The principal factor that hinders the restoration and spreading of the tree in the Sudetes is currently a very significant scattering of its specimens, which makes the exchange of its genetic material difficult (large, hardly airborne pollen grains). When the pollution level dropped, a surprisingly intensive fir revitalization was observed, which usually took place according to the following pattern: development of a regenerative crown on the trunk—regeneration of the trunk thickness growth—regeneration of the primary crown in the upper part of the tree (mainly development of lateral shoots)—increased blooming and cone crops. It turns out that silver fir, regarded as very sensitive to changes in the environment, is able to live in unfavorable conditions for a long time, with a reduced crown and minimum growth, only to greatly increase its growth once the conditions improve. During a period unfavorable to growth for instance, because of a sudden canopy disruption, many trees rebuild their crown from a broad one to a narrower and more compact one, and so become more resistant to industrial pollution [25]. Isoenzyme analyses have shown that there are genetic differences between firs from the Sudetes and the Carpathians, and most of the firs in the Sudetes are native populations (as opposed to, for instance, spruce). The differences were confirmed by later studies [9,42].
The data regarding the locations of the firs used in this paper also come from the period in which the studies referred to above were conducted. As already mentioned, from the early 19th c. the Sudetes were subject to intensive forest management promoting solid spruce stands. Until the 1970s, firs were practically not planted there. The period following WWII, was connected with strong industrial pollution and the belief that in such conditions firs, sensitive to this type of pollution, [3,4,6] would have no chance to survive. Consequently, it was assumed [25,27,28,29] that the fir locations surveyed as part of the studies done in the years 2000–2001, and so before the implementation of the restitution program, were largely remains of the natural sites that had existed there before the introduction of intensive forest management practices. In our opinion, this means that the location data we have are well suited for comparison with potential natural vegetation. The artificial cultivation of a species, which we do in Europe in the case of a majority of commercially important trees, may distort their original distribution and habitat preferences, which is probably the reason for the lack of studies similar to ours.
Discussion
When compared to typical phytosociological studies, we have tried to quantify the differences between individual communities in terms of their usefulness for growing firs.
The earlier phytosociological studies of selected fir sites in the Sudetes and a review of the phytosociological literature regarding the region [31] indicate that A. alba has a broad ecological scale, is a component of many forest communities, and that it is found most frequently at potential sites of acidophilic beech forests, whose vegetation is now strongly transformed because of spruce planting. Typical, mainly acidophilic beech forests take second place (in respect of frequent occurrence). Oak-hornbeam forest takes the third position. This agrees with the findings of our study.
The fact that we recorded the highest share of fir in the fertile beech communities in the Sudetes goes against the opinion that the species plays a minor role in Sudeten fertile beech forests [53]. On the other hand, however, Carpathian fertile beech forests are regarded as the optimum place for fir growth, and according to Zarzycki [53], fertile Carpathian beech forests may even be regarded as the center of the occurrence of A. alba. Its role in individual subunits of this area and in its various parts may differ [53]. On the other hand, phytosociological units whose names originate from ‘fir’ (e.g., Abietetum polonicum) occur on soils with slightly poorer fertility, and in studies devoted to natural regeneration of fir, habitats with mesotrophic soils are assessed particularly well [20,23,53]. In Jaworski’s research [3], fir seedlings survived better in mesotrophic than in eutrophic habitats. According to this author, the pathogenic fungus Cylindrocarpon destructans (Zinss) Scholten was to be responsible for the greater mortality of seedlings in fertile habitats.
Both the very variable share of fir in fertile beech sites and the locally recorded problems with its natural regeneration may be linked to the view that suggests the existence of a natural crop rotation involving fir and beech [1,2,3,4,5,6,7]. As Vrška’s et al. [54] research suggests, the historically recorded changes in the shares of beech and fir in fertile lower-montane forests in large areas of the Carpathians are principally attributable to changes in forest management. However, this does not mean that periodical changes in the shares of beech and fir that occur locally in relatively small areas are not natural in character [3,55,56,57,58,59,60]. If the natural crop rotation referred to above is a common phenomenon, this means that the operating cycle of fertile lower-montane forests may be more complex than we thought and longer than 300–400 years. The fact that studies are conducted at various phases of the cycle, which is additionally modified by various human activities, may account for apparently divergent findings.
The results of our studies indicate a strong position of fir in fertile beech habitats also in the Sudetes, i.e., in a region whose firs, just like the Alpine ones, are closely connected to the Apennine glacial refugium than those in the Carpathians [9]. Consequently, the strong position of fir in eutrophic lower-montane forests and submontane oak-hornbeam forests seems to have a universal character.
A relatively small share in the Sudetes of eutrophic beech communities may indicate that in this region, the original resources of fir may have been relatively smaller than those in the Carpathians. This has been suggested by, for instance, Barzdajn et al. [27]. The historical data show, however, that the percentage was definitely not lower than 20% [25,27,61].
In our opinion, determining the frequency of natural fir localities (FL) within areas of potential plant communities that develop under certain habitats under natural conditions is of great importance to the ecological characteristics of the species, including its potential role in the composition of fertile submontane and lower montane forests. Before conducting the study, when analyzing the literature data, we expected smaller differences and that they would mainly occur between beech and hornbeam forests, while the fertility of the habitat turned out to be the main differentiating factor. Unlike most other members of the Pinace family, which naturally occur in poorer habitats, Abies alba successfully competes with angiosperm deciduous trees in fertile habitats under stable climatic conditions (no severe frosts and prolonged droughts).
That this is the case—we have known for a long time. But the particular strength of this competition, as suggested by our results, is a novelty. Our research, like any other in this field, is contributory in nature. Its results shift the main center of the natural occurrence of silver fir towards fertile habitats. To us, it is interesting and important.