Correspondence Härdtle, W. (1995) On the theoretical concept of Potential Natural Vegetation and proposals for an up-to-date modification. Folia Geobotanica et Phytotaxonomica, 30, 263–276. Lobo, A., Ibáñez, J.J. & Carrera, C. (1997) Regional scale hierarchical classification of temporal series of AVHRR vegetation index. International Journal of Remote Sensing, 18, 3167–3193. Loidi, J. (1999) Preserving biodiversity in the European Union: the Habitats Directive and its application in Spain. Plant Biosystems, 133, 99–106. Loidi, J. (2007) La evolución del paisaje vegetal del centro-norte de la Penı́nsula Ibérica a lo largo de la historia. Boletı́n de la RSBAP, 11, 11–51. Moravec, J. (1998) Reconstructed natural versus potential natural vegetation in vegetation mapping. Applied Vegetation Science, 1, 173–176. Rivas-Martı́nez, S. (1987) Mapa de series de vegetación de España. ICONA Serie Técnica, Madrid. Rivas-Martı́nez, S. (2007) Mapa de series, geoseries y geopermaseries de vegetación de España. Parte I. Itinera Geobotánica, 17, 5–435. Rivas-Martı́nez, S., Penas, A., Asensi, A., Costa, M., Llorens, L., Pérez de Paz, P.L., Loidi, J., Dı́az, T.E., Izco, J., Ladero, M., Fernández-González, F., Masalles, R. & Sánchez-Mata, D. (2003) Atlas y manual de los hábitat de España. Dirección General de la Conservación de la Naturaleza, Ministerio de Medio Ambiente, Madrid. Rodrigues Tarroso, J.P. (2007) Late-Quaternary landscape dynamics in the Iberian Peninsula and Balearic Islands. Universidade do Porto, Porto. Tüxen, R. (1956) Die heutige potentielle natürliche Vegetation als Gegenstand der Vegetationskartierung. Angewandte Pflanzensoziologie, 13, 5–55. Editor: John Lambshead doi:10.1111/j.1365-2699.2010.02302.x The power of potential natural vegetation (and of spatialtemporal scale): a response to Carrión & Fernández (2009) ABSTRACT A commentary by Carrión & Fernández (Journal of Biogeography, 2009, 36, 2202– Journal of Biogeography 37, 2209–2215 ª 2010 Blackwell Publishing Ltd 2203) compared Holocene pollen records with models of potential natural vegetation (PNV) proposed in the phytosociological literature and concluded that the predicted PNV resulted from anthropogenic disturbance. However, the authors misinterpreted PNV, leading to two serious flaws in their assumptions: (1) PNV is not defined as a pre-anthropic or climax plant community; and (2) PNV is not a concept restricted to the phytosociological method. Therefore we criticize the conclusions expressed in the commentary, and we stress the need for an interdisciplinary approach based on multi-temporal and multi-spatial scales to achieve a modern framework for the study of plant communities. Keywords Climax concept, ecological restoration, Holocene vegetation, landscape dynamics, phytosociology, potential natural vegetation, secondary succession, vegetation classification, vegetation science. In a commentary regarding Holocene pollen deposits from the Canary Islands, Carrión & Fernández (2009) argued that the discovery of Quercus and Carpinus pollen is noteworthy because Ôthe prevailing concepts of natural potential vegetation in the study region imply that the pre-anthropic (mature phase or climax) vegetationÕ would be an evergreen forest dominated by species of Lauraceae. Inferences of pre-anthropic vegetation made by palynologists were also compared with the potential natural vegetation (PNV; incorrectly quoted in the commentary as Ônatural potential vegetationÕ) proposed in the phytosociological literature at a number of sites in the Iberian Peninsula. The results of the two models indicated that, in many instances, the dominant species differed. Therefore they concluded that the PNV types determined in previous studies were the result of anthropogenic disturbance. Consequently, the authors polemically argued that there is a bias Ôin the conceptualization of the vegetational dynamicsÕ by Ôtraditional vegetation scienceÕ, and resistance to abandon this bias Ôhas little to do with scientific evidenceÕ, in front of Ôa growing body of work questioning the floristic-phytosociological approachÕ. Unfortunately, this line of reasoning is based on two serious misunderstandings regarding the PNV concept. First and foremost, PNV is not defined by vegetation scientists as Ôpre-anthropic (mature phase or climax) vegetationÕ. On the contrary, PNV is defined as the plant community that Ôwould become established if all successional sequences were completed without interference by man under the present climatic and edaphic conditions (including those created by man)Õ (MuellerDombois & Ellenberg, 1974, p. 422; our emphasis; see also: Westhoff & van der Maarel, 1973; Ellenberg, 1988; Ricotta et al., 2002). European landscapes exhibit present soil conditions that are often dramatically different from their original state, due to recent or ancient but irreversible human disturbance (cf. Dupouey et al., 2002). Consequently, it is an essential part of the PNV theory that the potential vegetation of a site can be very different from the preanthropic vegetation at the same site (e.g. Mueller-Dombois & Ellenberg, 1974; Chytrý, 1998; Moravec, 1998; Zerbe, 1998; Gamisans, 1999). The PNV concept was introduced (Tüxen, 1956) to express the present (ÔheutigeÕ) potential of a region or site as a useful reference to define a target for restoration ecology and ecological engineering projects, or for landscape management purposes (e.g. to forecast and manage landscape evolution on a time-scale of a few decades) (Rodwell & Patterson, 1994; Härdtle, 1995; Miyawaki, 1998; Zerbe, 1998; Verheyen et al., 2006; Dostalek et al., 2007). It is quite surprising that Carrión & Fernández (2009) completely ignored the large body of works addressing and defining PNV theory. Furthermore, it is perplexing they assumed that Ôclimax vegetationÕ and PNV are considered synonyms in vegetation science. On the contrary, it is well known that the idea of PNV arose as an outcome of (and reaction to) the long-lasting debate on the ÔclimaxÕ concept (Zerbe, 1998; Ricotta et al., 2002). European vegetation scientists have questioned the concept of climax for decades (Mueller-Dombois & Ellenberg, 1974; Chytrý, 1998; Schulze et al., 2005), and we now acknowledge that vegetation is not returning to an alleged, past equilibrium, but is adapting continuously to a changing abiotic environment and biotic interactions. In addition, the inferred climax phase requires a long period of succession, which introduces not only the effects of long-term climatic changes, but also those of vegetation-induced soil modifications. Finally, the climax concept was developed to study the phytogeography of North America, a continent featuring abiotic homogeneity over large areas, a condition rarely verified in Europe. 2211 Correspondence The second fundamental mistake in Carrión & Fernández (2009) was their assumption that PNV is a concept exclusive to the phytosociological school (i.e. of the Braun-Blanquet approach to plant community entitation, sampling and classification; see e.g. Westhoff & van der Maarel, 1973). Although originally developed by phytosociologists, the PNV model does not stem from the assumptions of phytosociology, nor do the Ôpotential communitiesÕ need to be defined and classified through the phytosociological system. PNV-based models can be usefully applied even if vegetation is classified on a purely physiognomic basis (e.g. Liu et al., 2009). Furthermore, despite the fact that PNV arose in a historical context, when succession had a linear deterministic interpretation, it is interesting that even in modern ÔchaoticÕ models of succession, the PNV hypothesis is supported, as it can be viewed as the strange attractor where succession trajectories converge (Anand & Orloci, 1997; Ricotta et al., 2002). Thus the comparison between the distribution of actual vegetation patterns and PNV types is presently integrated in the most current applied ecological research, for example: to assess the effects of disturbance on pattern and diversity in landscape ecology studies (Ricotta et al., 2002; Bajocco et al., 2010); to study the effectiveness of protected area networks (Rosati et al., 2008); and to contribute to habitat monitoring (Mücher et al., 2009). As a consequence, the use of PNV concepts is definitely not restricted to a few Ôacademic refuges [of phytosociology]Õ in Spain or Italy (Carrión & Fernández, 2009). PNV-based methods are largely adopted today in countries where the phytosociological approach is not traditionally applied, such as the USA and China (e.g. Küchler, 1964; Brohman & Bryant, 2004; Liu et al., 2009; Zou et al., 2009), and⁄or within disciplines not related to phytosociology, including forestry and wildlife ecology (e.g. Lexer et al., 2002; Aubry et al., 2007; Kennedy & Wimberly, 2009; Strand et al., 2009). Recently, PNV concepts were integrated in major vegetation-mapping projects, based on extensive international collaboration (Bohn et al., 2004; Walker et al., 2005). Therefore it is unclear why any shortcomings in the PNV model (see Zerbe, 1998 for limitations and caveats) should Ôquestion the floristic-phytosociological approachÕ and why any flaws of the phytosociological approach should weaken the usefulness 2212 of the PNV concept. Incidentally, it should be noted that the conflicts between the assumptions of the phytosociological method and the latest views in ecology form a complex and long-lasting debate (see e.g. Dengler et al., 2008 and references therein), which cannot be summarised here, and have little to do with the issues raised by Carrión & Fernández (2009). Furthermore, it is not clear why Carrión & Fernández (2009) quoted the Willis & Birks (2006) review to support the claim that Ôthe palaeoecological literature is full of overwhelming evidence against [the phytosociological] notions of vegetational dynamicsÕ. Instead, the need for a multimethod approach to a modern, integrated framework for the study of plant communities (as advocated by Willis & Birks, 2006) should be stressed. We believe in a multidisciplinary approach to community ecology, where short-term secondary succession studied by vegetation scientists and longterm dynamics reconstructed by palynologists are two views of the same process studied at two different spatial-temporal scales, both of which should contribute to the development of a unified, multi-scale model of vegetation dynamics (Davis et al., 2005; Willis et al., 2007; Pickett et al., 2009; Zou et al., 2009). Emmanuele Farris1, Goffredo Filibeck2*, Michela Marignani3 and Leonardo Rosati4 1 Dipartimento di Scienze Botaniche, Ecologiche e Geologiche, Università degli Studi di Sassari, Via Piandanna 4, I-07100 Sassari, Italy 2 Dipartimento di Ecologia e Sviluppo Economico Sostenibile, Università degli Studi della Tuscia, Largo dellÕUniversità snc, I-01100 Viterbo, Italy 3 Dipartimento di Biologia Vegetale, Università degli Studi di Roma ‘‘Sapienza’’, Piazzale Aldo Moro 5, I-00185 Roma, Italy 4 Dipartimento di Biologia, Difesa e Biotecnologie Agro-forestali, Università degli Studi della Basilicata, Viale dellÕAteneo Lucano 10, I-85100 Potenza, Italy *E-mail: [email protected] REFERENCES Anand, M. & Orloci, L. (1997) Chaotic dynamics in a multispecies community. Environmental and Ecological Statistics, 4, 337–344. Aubry, K.B., McKelvey, K.S. & Copeland, J.P. (2007) Distribution and broadscale habitat relations of the wolverine in the contiguous United States. 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Editor: John Lambshead doi:10.1111/j.1365-2699.2010.02323.x The concepts of potential natural vegetation (PNV) and other abstractions (trying to pick up fish with wet hands) ABSTRACT This note follows from an earlier Commentary published in Journal of Biogeography (Carrión & Fernández, 2009, 36, 2202–2203), which provided palaeoecological data, and two replies in the form of Correspondence (Loidi et al., 2010, 37, 2209–2211; Farris et al., 2010, 37, 2211– 2213). The latter papers attempt to invalidate the palaeoecological database as a source of comparison with the maps of potential vegetation. Here, some of the different interpretations of the term Ôpotential natural vegetationÕ (PNV), as used by the floristic phytosociological school, are discussed. It is suggested that there is a conceptual impasse that will not have a solution until a terminological consensus is reached. This terminology will open new methodological avenues that will facilitate the entry of new information derived from historical biogeography, palaeoecology, ecology, phylogeography, and niche and community modelling. One of the main sources of conflict arises from the link made between habitats and floristically-determined associations, a confusion that has crucial repercussions in biological conservation, including in respect of the EU Habitats Directive. Keywords Climax concept, conservation, historical biogeography, palaeoecology, phytosociology, potential natural vegetation. This paper is a response to two papers authored by sixteen phytosociologists from Spain and Italy. The first, Loidi et al. (2010), presents what could be seen as the phytosociological schoolÕs consensus position as already published, for example, by Loidi (1998) in reaction to Blanco et al. (1997). The latter, among others (e.g. Spribille & Ceska, 2001), claim that potential natural vegetation (PNV) has the following weaknesses: (1) the subjective character of sampling, (2) the inefficient description of human-disturbed areas, (3) the lack of regard to the role of structure in the definition of communities, (4) the confused system of nomenclature and the instability of the classification, (5) impoverished, outdated methodology, (6) lack of experimental field studies, and (7) a strong tendency to use ad hoc taxonomy to name phytosociological taxa. Loidi et al. (2010) argue that by seeking a comparison with pristine vegetation, Carrión & Fernández (2009) are using an inexact interpretation of the concept of potential natural vegetation (PNV), even though this comparison is common in applied forestry (Higgins et al., 2004). In practice, it is difficult to determine which interpretation of PNV should be adopted given that there are 2213
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