•  Primeval forest structure;
  • Vera hypothesis;
  • forest grazing;
  • large herbivores;
  • pollen analysis;
  • forest conservation policy


  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References
  • 1
    The Vera hypothesis that large herbivores maintained an open landscape in the primeval landscape of lowland Europe is tested using palaeoecological data. The hypothesis suggests that the high abundance of Quercus and Corylus apparent in European pollen diagrams could not have derived from a landscape dominated by closed canopy forests. If natural forest landscapes were indeed more open, current forest conservation management policy across Europe would need to be reconsidered.
  • 2
    Relative proportions of Quercus and Corylus pollen are compared from regions which supported large herbivores with data from Ireland, where large herbivores were excluded. Similarity between the two data sets indicates that large herbivores were not required to maintain these taxa in the primeval landscape.
  • 3
    Fine spatial resolution pollen data from small hollows in Europe and eastern USA were also reviewed. Data from moss polsters show that percentage arboreal pollen is a reliable indicator of canopy openness in theses sites. The palaeoecological data demonstrate that open canopy forest has only ever been maintained by human exploitation.
  • 4
    Large herbivores in Europe do not therefore appear to have maintained an open landscape in primeval times although evidence suggests that they would have influenced the species composition of the forest canopy.
  • 5
    It is proposed that data sources other than pollen should be explored as proxies for past forest structure to test this hypothesis more thoroughly.


  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References

Peterken (1996) has concluded that primeval virgin forest no longer exists in Europe. Despite this, the concept of virgin forest strongly influences nature conservation policy across Europe although, in certain circumstances, cultural exploitation such as coppicing is recognized as an important intervention to be maintained (Peterken 1993). In the absence of true virgin forest in the European temperate zone, the composition and structure of primeval forests in this region has been inferred both from studies of old stands which have received minimal human impact and from palaeoecological data. The image that emerges for lowland temperate Europe is a landscape dominated by closed canopy deciduous forest. This model is challenged by Vera (2000) who considers that large herbivores were instrumental in maintaining a more open landscape and hence prevented the dominance of closed canopy forest.

The significance of Vera's (2000) hypothesis lies in the contention that, if it is valid, then forest conservation policy across much of Europe, and by analogy, parts of North America, is misguided where the conservation aim is to maintain the forest close to its natural condition prior to human impact. The implementation of this policy draws on very significant resources from fiscal and NGO sectors. The publication of Vera's (2000) hypothesis has already prompted a major investigation by English Nature into the future management of large-scale reserves in Britain using naturalistic grazing (Kirby et al. 2004), drawing on the existing experience of this approach at the 5000-ha reserve at Oostvaardersplassen in the Netherlands (Vera 2000). This paper tests the validity of Vera's hypothesis by using palaeoecological data from primeval and modified forests to explore the degree of canopy closure of the primeval forest.

Large herbivores are observed to have significant impacts on forest ecosystems today, such that the control of wild and domestic herbivores is a major conservation management issue (Mitchell & Kirby 1990; Weisberg & Bugmann 2003). In prehistoric times there was greater diversity of large herbivores in Europe; in addition to several species of deer, there were aurochs, tarpan, bison, beaver and wild boar. Vera (2000) proposes a dynamic model in which large herbivores maintained a landscape composed of a mosaic of groves of closed canopy woodland, open parkland and regenerating scrub. Large herbivores grazing and browsing in closed canopy woodland would prevent tree regeneration so that eventually the canopy would open up and ultimately form parkland. The development of browsing resistant thorny scrub (Bakker et al. 2004) would provide protection for regenerating trees in the parkland which would then develop into groves and so complete the cycle. An essential feature of the model is that the landscape is made up of a dynamic mosaic of the components of the cycle in which closed canopy forest exists in groves but that these are not self-perpetuating. The spatial and temporal characteristics of this model have been explored by Kirby (2003, 2005) and the basic elements of the model are illustrated in Fig. 1. Vera confines his model to the geographical region lying between 45° N and 58° N latitude and 5° W and 25° E longitude, and to altitudes below 700 m (Vera 2000, figure 1.5). These limits fall within the principal temperate zone of Europe north of the Alps. By analogy, it is also proposed that the hypothesis applies to the temperate zone of eastern North America.


Figure 1. Vera's model, consisting of the three phases of Open Park, Scrub and Grove, to which a fourth Break-up has been added by Kirby (2003) to represent the transition from woodland grove back to open habitats (Park). Source: Kirby (2003) with the kind permission of English Nature.

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Vera (2000) proposes the following null hypothesis:

‘Pedunculate and sessile oak and hazel survive in a closed forest, and regenerate in gaps in the canopy, in accordance with Watt's ‘gap phase’ model (1947) and Leibundgut's so-called cyclical model. The large herbivores which occurred naturally such as the aurochs, European bison, red deer elk, roedeer and tarpan or European wild horse and the omnivorous wild boar followed the developments in the vegetation. They did not have any influence on the course of the process of the succession and regeneration of forests.’

Vera (2000) tests this null hypothesis using evidence from a very comprehensive review of the literature on modern ecology of forest tress and large herbivores, fossil pollen data and historical information. It is impossible to reconstruct the population densities of large herbivores in prehistoric times (Bradshaw & Mitchell 1999) but Vera (2000) argues that their impact on forest structure is evident from the pollen record. Modern ecological studies suggest that oak (Quercus petraea (Mattuschka) Lieblein and Q. robur L.) and hazel (Corylus avellana L.) require canopy gaps for regeneration (Vera 2000). Pollen records from across Europe are dominated by these taxa in prehistoric times, and this is used as evidence to suggest that the forests must have been more open than today to maintain their regeneration. Vera rejects the null hypothesis in favour of this alternative:

‘The natural vegetation consists of a mosaic of large and small grassland, scrub, solitary trees and groups of trees, in which the indigenous fauna of large herbivores is essential for the regeneration of the characteristic trees and shrubs of Europe. The wood-pasture can be seen as the closest modern analogy for this landscape’ (Vera 2000).

The crux of the debate may be simplified thus: the traditional view implies that forest structure dictated herbivore carrying capacity, whereas the Vera hypothesis dictates that herbivore density controls forest structure. Vera's model and hypothesis testing are based on qualitative data drawn from the literature. Kirby (2004) has taken a more quantitative approach to model the spatial and temporal aspects of the hypothesis, whilst palaeoecological data will be used here to quantitatively test Vera's (2000) null hypothesis.

palaeoecological data

Fossil pollen is found in abundance in a variety of sites across the temperate ecotone (Jacobson & Bradshaw 1981). Fossil pollen data have been used to reconstruct changes in vegetation communities over time and can thus be used to infer the impact of large herbivores on temperate forest structure (Vera 2000). By contrast, fossil remains of large herbivores provide qualitative but not quantitative data because they are too rare to enable the reconstruction of population densities (Bradshaw & Mitchell 1999). However, we do have sufficient data to assess whether certain herbivore species were present in particular locations in the past. This provides us with an approach to test Vera's null hypothesis, which is analogous to the manipulation of herbivore grazing using fenced exclosures that is widely used in contemporary forest grazing experiments (Mitchell & Kirby 1990).

Grazing exclusion

Vera argues that large herbivores maintained an open forest structure or mosaic which was necessary to ensure the regeneration of Quercus and Corylus. Review of the European pollen literature confirms the universally high proportions of these taxa throughout the Holocene. It is therefore implied that without the impact of the herbivores, the forest canopy would remain closed, and thus restrict the regeneration of these taxa which would in turn be reflected in the pollen record. This latter hypothesis can be tested by examining pollen data from islands where the herbivore populations have been more restricted than in mainland Europe.

Svenning (2002) discusses the example of the island of Zealand in Denmark where Hannon et al. (2000) have used pollen data to demonstrate that Quercus and Corylus were abundant in the mid Holocene after aurochs and elk had been extirpated. Other deer species and wild boar remained and so the complete exclusion of large herbivores was not maintained. A more convincing case can be made for the island of Ireland. This region is outside the area of lowland temperate Europe defined by Vera (2000, figure 1.5) but shares similar topography and climates and falls within the geographical range of Quercus petraea, Q. robur and Corylus avellana.

Most of Ireland was covered by ice during the last glacial cold stage (Coxon 2001) and so it can be assumed that no large herbivores would have survived from earlier interstadials or interglacials. Migration into Ireland would have been hindered by the isolation of the island during the early Late-glacial and this is also reflected by the depauperate flora compared to the rest of Europe (Mitchell 2002). Early Holocene mammal faunas in Europe have been established from excavations and the data have been collated by Roberts (1998) and Svenning (2002). A subset of these data which relate to large herbivores native to north-west Europe, Britain and Ireland during the early Holocene is presented in Table 1. Ireland had only two large herbivores: wild boar and red deer. The data for red deer in Ireland are remarkable. Red deer bones are absent from early Holocene archaeological sites and no material has been dated from the early Holocene (Woodman et al. 1997). Some bones considered to be those of red deer have been found in early Holocene context at Belfast Lough, but the earliest Holocene radiocarbon dates for red deer in Ireland remain around 4000 bp (where bp refers to radiocarbon years before present) (Woodman et al. 1997). The scarcity or absence of red deer remains of early Holocene age cannot be used as proof of the absence of this herbivore but the available data suggest that, even if red deer was present in Ireland during the early Holocene, it was unlikely to have been very abundant. This is in contrast to wild boar which has been found more widely in both space and time. We can therefore consider the early Holocene forest in Ireland to be almost devoid of large herbivores compared to Britain and the European continent. Ireland can be considered as an early Holocene grazing exclosure, albeit containing wild boar and possibly some isolated red deer populations.

Table 1.  Early Holocene native large herbivores. Data for north-west Europe from Svenning (2002); data for Britain and Ireland from Roberts (1998)
SpeciesNorth- west EuropeBritainIreland
Wild boar (Sus scrofa)XXX
Red deer (Cervus elaphus)XXX
Roe deer (Capreolus capreolus)XX 
Elk (Alces alces)XX 
Reindeer (Rangifer tarandus)XX 
Horse (Equus caballus s.l.)XX 
Aurochs (Bos primigenius)XX 
Beaver (Castor fibre)XX 
Bison (Bison spp.)X  
Fallow deer (Dama dama)X  

Some commentators have considered that the use of fire by Mesolithic hunters to open the forest canopy may confuse the assessment of the impact of large herbivores (e.g. Svenning 2002). With the absence or scarcity of game in Ireland this is unlikely to be an issue. Mesolithic people in Ireland did not have this reason to maintain open forest canopies and this contention is not disputed by the limited archaeological evidence (Woodman 1978; Woodman et al. 1997). Molluscan data do, however, demonstrate that some clearings were created (Preece et al. 1986). Bradshaw & Hannon (2004) also argue that forces like natural fire, windthrow and seasonal flooding would have created forest openness in Europe irrespective of herbivore grazing.

Fine spatial resolution pollen analysis

Traditional pollen analysis from lakes and peat deposits reconstructs vegetation on a spatial scale that is too coarse to reliably reconstruct forest stand structure because these sites collect pollen from a radius of tens of kilometres (Jacobson & Bradshaw 1981; Sugita 1994). The pollen from numerous vegetation communities is mixed before deposition and so the ability to identify dynamics in a single community is restricted. Reconstructing the degree of forest canopy openness or the spatial mosaic of open and wooded patches in the landscape is similarly fraught with uncertainties (Koff et al. 2000). So, although the pollen data from these sites give an indication of the relative proportions of certain tree taxa in the landscape they cannot reveal the structure of the forest with any degree of certainty.

Modelling exercises suggest that small hollow sites in closed canopy forest collect most of their pollen from within a radius of 50–100 m (Sugita 1994) and this has been supported by empirical data from the USA (Jackson & Wong 1994; Calcote 1995). Small hollow pollen analysis from forested sites can therefore provide data on forest dynamics at the forest stand scale. If the forest canopy opens up then the pollen source area may be greater but the increased light will be registered in the pollen record by enhanced flowering of herbaceous taxa. The pollen of herbaceous taxa are normally poorly represented in traditional larger sites because of their limited pollen transport. Pollen does not travel far to small hollow sites and so forest openness can be detected. This assumption is tested below with empirical data.


  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References

Comparison of Quercus (deciduous) and Corylus pollen abundance between Ireland and the area of Europe defined by Vera (2000, figure 1.5) provides the basis for testing the null hypothesis. The data must be temporally constrained to be late enough in the Holocene to ensure that the taxa would be present in the region but also to predate significant manipulation of the forest structure by human activity. Reference to Huntley & Birks (1983) and Brewer et al. (2002) indicate that the lower date should be 8500 bp. The widespread establishment of Neolithic cultures throughout western Europe after 5500 bp (Roberts 1998) provides the upper time limit for the data set.

The European Pollen Database ( was accessed for all sites that lie within the geographical and altitudinal limits set by Vera (2000) and cover the time period from 8500 bp to 5500 bp. This search delivered 21 sites which are detailed in Table 2. The IPAL data base, which is confined to fossil pollen data from Ireland (R. Marchant, unpublished data), was also accessed and delivered 15 sites covering the desired time period and all below 700 m altitude (Table 2). The raw pollen count data for each site were converted into relative proportions based on a pollen sum of identified terrestrial taxa, including fern spores. The mean relative abundance of Quercus and Corylus pollen in contiguous 500-year time slices was then computed to capture time transgressive changes across the sites. This generated data for six time slices for each taxon at each site. The resulting data matrix for each taxon was then subjected to principal components analysis (PCA) using the canoco 4.5 (Biometrics-Plant Research International, Wageningen, The Netherlands) package to illustrate the relationship between the European and Irish data (ter Braak & Šmilauer 1997–2003). Redundancy analysis (RDA), which is a form of constrained PCA, was then employed with site location (Europe or Ireland) as the single explanatory variable (Lepš & Šmilauer 2003). The data were not transformed prior to analysis. The null hypothesis that there is no difference between the data for Europe and Ireland was tested using a restricted Monte-Carlo permutation test.

Table 2.  Site details for pollen data derived from EPD and IPAL databases
Site nameCountryGrid referenceSource reference
KamenickyCzech Republic49˚44′ N 15˚58′ ERybníčková & Rybníček(1988)
Hockham MereEngland52°30′ N 00°50′ EBennett (1983)
Pannel BridgeEngland50°54′ N 00°41′ EWaller (1987)
Vallie de la VoiseFrance48°25′ N 01°45′ Evan Zeist & van der Spoel-Walvius (1980)
Lake Balaton CentreHungary46°44′ N 17°24′ ENagy-Bodor et al. (1995)
Zsombo-swampHungary46°21′ N 19°59′ ENagy-Bodor et al. (1995)
Tytuvenu tyrelisLithuania55°35′ N 23°18′ EKabailiené (1990)
Błędowo LakePoland52°33′ N 20°40′ EBinka et al. (1991)
KlukiPoland54°42′ N 17°17′ ETobolski (1987)
Lake LednicaPoland52°33′ N 17°23′ EMakohonienko & Walanus (1991)
Lake SkvzetuszewskiePoland52°33′ N 17°21′ ETobolski & Okuniewska-Nowaczyk (1989)
Puścizna RękowiańskaPoland49°29′ N 19°49′ EObidowicz (1989)
SłopiecPoland50°47′ N 20°47′ ESzczepanek (1961, 1982)
SzymbarkPoland49°38′ N 21°06′ ESzczepanek (1989)
TarnowiecPoland49°42′ N 21°37′ EHarmata (1987)
Ageröds MosseSweden55°50′ N 13°25′ ENilsson (1964)
KansjonSweden57°38′ N 14°32′ EG.L. Jacobson (unpublished); Berglund et al. (2002)
Lake SambösjönSweden57°08′ N 12°25′ EDigerfeldt (1982)
Mabo MossSweden58°01′ N 16°04′ EGöransson (1991)
LobsigenseeSwitzerland47°01′ N 07°17′ EAmmann (1989)
Ivano-FrankovskoyeUkraine49°55′ N 23°46′ EArtjushenko et al. (1982)
Arts LoughIreland52°55′ N 06°20′ WBradshaw & McGee (1988)
Ballinloghhig LoughIreland52°12′ N 10°18′ WBarnosky (1988)
Belle LakeIreland52°11′ N 07°02′ WCraig (1978)
Black LoughIreland53°15′ N 07°41′ WHeery (1998)
Borheen LoughIreland52°24′ N 08°12′ WE. Cole (unpublished)
Camclaun LoughIreland52°10′ N 10°24′ WDodson (1990)
Clara BogIreland53°32′ N 07°41′ WConnolly (1999)
Cornaher LoughIreland53°23′ N 07°28′ WHeery (1997)
CregganmoreIreland54°15′ N 09°36′ WMcKeever (1984)
GlendaloughIreland53°00′ N 06°20′ WJ. Maldonado (unpublished)
Kellys LoughIreland52°50′ N 06°15′ WE. Cole (unpublished)
Ladies ViewIreland51°58′ N 09°36′ WVokes (1966)
Lough AnaffrinIreland53°55′ N 09°48′ WBrowne (1986)
Lough ClevalaIreland54°04′ N 09°24′ WBrowne (1986)
Sluggan BogIreland54°48′ N 06°21′ WSmith & Goddard (1991)

The small hollow pollen record is sensitive to canopy openness so the relative proportion of arboreal pollen (AP) to nonarboreal pollen (NAP) has been chosen to represent an index of openness. Svenning (2002) has compared pollen data to other proxies of canopy openness, such as beetles, molluscs and plant macrofossils, to demonstrate that the AP : NAP ratio is a reasonable index of openness. The degree of openness represented by AP percentage in small hollows can also be evaluated using pollen data from moss polsters. Pollen extracted from the living parts of moss polsters provides an integrated pollen sample from several previous years. The pollen trapping properties of moss polsters are analogous to those of small hollows and so provide a reasonable contemporary model (Fall 1992) against which present vegetation composition and structure can be compared to pollen representation. Moss polster pollen data from both open (i.e. not forested) and closed canopy forest locations from across Europe have been accessed from the literature. The data are presented as the range of one standard deviation either side of the mean AP percentage.

Published small hollow pollen data were collated from sites which contained early Holocene records within the area of lowland Europe defined by Vera and from Ireland. The pollen data from each site were grouped into consecutive 1000-year time periods. The maximum and minimum percentage arboreal pollen values within each 1000-year time period are plotted as an AP range from 12 sites.


  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References

The PCA plots illustrate that the Irish data lie within the range of the European data for both Quercus and Corylus (Fig. 2). Site location accounted for only 1% of variance in the RDA for Quercus and 7.6% for Corylus. Site location was not a statistically significant source of variation in the analysis of either taxon (F-ratio = 0.335 for Quercus and 2.807 for Corylus). This implies that there was no significant difference in the relative proportions of Quercus and Corylus in the primeval forests of Ireland and Europe despite the differences in large herbivores between the regions. Therefore Vera's null hypothesis can not be rejected, i.e. the presence or absence of large herbivores has little impact on the relative abundance of Quercus and Corylus in primeval woodland in lowland temperate Europe. If this is the case then we should examine the structure of this early Holocene primeval forest more closely.


Figure 2. PCA plots of relative proportions of (a) Quercus pollen and (b) Corylus pollen. Open circles represent sites from within the area of lowland Europe defined by Vera (2000), while closed circles represent sites in Ireland (see Table 2 for site details).

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Contemporary moss polster pollen data indicate that closed canopy forests maintain AP greater than 60% (Fig. 3). These data can be contrasted with data from completely open sites where AP does not exceed 50% (Fig. 4). The data from Spain are an exception because the open sites investigated included arboreal scrub genera such as Quercus and Celtis (Díaz Fernández 1994). Furthermore, Spain is outside the lowland temperate region of Europe as defined by Vera (2000). Data from the forest edge in France and the Spanish Dehesa (parkland) are also included in Fig. 4 as these are rare examples of contemporary pollen data from partially wooded habitats. Significantly, the AP percentage values do not exceed 50% in these latter cases. The contemporary pollen data from moss polsters indicate that AP percentages in excess of 60% are indicative of closed canopy forest while AP percentages less than 50% are indicative of more open habitats. These data confirm that pollen analysis from small hollows in forested catchments can be used to assess the degree of canopy closure.


Figure 3. Mean arboreal pollen (AP) percentage ± 1 SD from moss polsters collected within closed canopy forests. The data sources are Poland: Dąbrowski (1975) and Makohonienko et al. (1998); Germany: Dambach (1998); Ireland: Mitchell (1988) and unpublished data; France: Ruffaldi (1994); Spain: Díaz Fernández (1994) and Andrade Olalla et al. (1994).

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Figure 4. Mean arboreal pollen (AP) percentage ± 1 SD from moss polsters collected from open sites. The data sources are Poland: Makohonienko et al. (1998); Germany: Dambach (1998); Ireland: Hall (1989); France: Ruffaldi (1994); Spain: Díaz Fernández (1994) and Andrade Olalla et al. (1994); France (Forest edge): Ruffaldi (1994); Spain (Dehesa): Díaz Fernández (1994).

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The arboreal pollen remains above 60% at all small hollow sites prior to 3000 years ago (Figs 5–7). Comparison with the contemporary pollen data (Figs 3 and 4) indicates the maintenance of closed canopy forest for the primeval woodland in both Ireland and the rest of Europe. Over the last 3000 years, arboreal pollen falls below 60% at some sites and in each case this is associated with documented human impact on the forest which has resulted in the artificial opening of the canopy (see original papers for details). This independent evidence further strengthens the argument that small hollow pollen sites can be used to investigate forest canopy cover. The temporal resolution of the pollen samples across the sites is variable but there is no indication of open forest canopies at any site prior to human impact irrespective of the presence of large herbivores in the region.


Figure 5. Arboreal pollen (AP) percentage range over 1000-year intervals from small hollow sites in Southern Sweden. The data sources are Mattarps: Björkman (1996); Djaknabygd, Osaby in field, Rashult in field, Osaby out field, Rashult out field: Lindbladh & Bradshaw (1995).

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Figure 6. Mean arboreal pollen (AP) percentage range over 1000-year intervals from small hollow sites in Denmark. The data sources are Glyceria hollow: Andersen (1984); Suserup Skov: Hannon et al. (2000).

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Figure 7. Mean arboreal pollen (AP) percentage range over 1000-year intervals from small hollow sites in Ireland. The data sources are Brackloon: Little et al. (2001); Camillan, Derrycunihy: Mitchell (1988); Uragh: Little et al. (1996).

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  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References

Pollen data have been used to test Vera's hypothesis on two spatial scales. Data from large lakes and bogs show similar records for Quercus and Corylus irrespective of the presence or absence of large herbivores, thus indicating that large herbivores are not a prerequisite for the maintenance of these genera in the primeval landscape, which was a central tenet of Vera's hypothesis.

Pollen analysis at the fine spatial scale of small hollows has been demonstrated to distinguish open and closed forest canopies but there is no evidence from the available data for open canopies in the primeval forest when large herbivores were present. If large herbivores did not dictate the structure of primeval forests then it is reasonable to assume that the forest structure dictated herbivore carrying capacity.

A review of small hollow pollen data from eastern USA reveals AP values above 80% prior to European settlement and so prompts a similar conclusion (Foster et al. 1992; Schoonmaker 1992; Foster & Zebryk 1993; McLachlan et al. 2000; Foster et al. 2002; Schauffler & Jacobson 2002). The impacts of European settlement in central Massachusetts have been well documented (Foster et al. 1998). Widespread settlement began in the eighteenth century and by 1830 more than 70% of the forest had been converted to agricultural land. Abandonment of agricultural land from the mid nineteenth century onwards resulted in the natural regeneration of forests which cover 85% of the region today (Foster et al. 1998). These landscape scale changes to some extent mimic those proposed by the Vera hypothesis. The forest canopy was gradually reduced to produce a mosaic of open land with isolated copses of woodland associated with each farm. Regional pollen data from small lakes in central Massachusetts detect these changes to the landscape from the original forest with low NAP values, to the expansion of European settlement with higher NAP followed by the recovery of the forest during the twentieth century (Fuller et al. 1998). Similar investigations in coastal Massachusetts also reveal that closed canopy forest was maintained until European settlement (Foster & Motzkin 2003). So although the eastern USA supported a diverse suite of large herbivores, it appears that they did not maintain an open landscape in primeval times as predicted by the Vera hypothesis.

The pollen data from temperate America and Europe indicate that human intervention was the only force that has maintained open canopies in forests over the last 10 000 years. Bradshaw et al. (2003) argue that fire, rather than herbivores, has been a significant factor in opening forest canopies and while human intervention is often associated with fire, it is not always possible to make this connection.

The role of herbivores in maintaining open landscapes cannot be dismissed before considering two critical issues. The first relates to the ecology of oak and hazel and the second to the adequacy of pollen data in developing and testing this hypothesis. The autecology of Quercus and Corylus suggests that they can not regenerate under a closed canopy (Vera 2000), which implies that their maintenance must rely on the more traditional models of gap dynamics (e.g. Watt 1947). Nevertheless, more thorough experimental investigations of the ecology and ecophysiology of these taxa are required to test whether light conditions under closed canopy woodland is actually the principal factor restricting their regeneration in woodland today. Rackham (2003) argues that the introduction of American oak mildew may have made contemporary oak seedlings more light-demanding than their primeval ancestors. Both beech (Fagus sylvatica) and lime (Tilia spp.) were absent from Irish forests in primeval times and so oak would have filled a wider ecological niche than in lowland central Europe. This may account for some enhancement of the pollen values for Ireland but as Vera's hypothesis considers that oak can not regenerate under its own shade, this difference can not explain the strong overlap of the Irish and European pollen data.

Secondly, this review has focused on pollen data because of their central role in the development of Vera's hypothesis. Contemporary data have been used to validate the implications drawn from fossil pollen data although the data are limited, especially for the open and semi-open habitats which the hypothesis proposes (Gaillard et al. 2000). Additional data from these habitats are required for more thorough validation. The availability of small hollow pollen data from the early Holocene is also very limited. Bradshaw & Hannon (2004) stress that these sites bias data towards wetter habitats which may have some influence on the conclusions drawn from them. So the consideration of other independent data sources would be very valuable. To this end, the use of habitat specific coleopteran (beetle) remains preserved in small hollow deposits will provide an additional level of validation due to their ability to infer open and closed forest canopy conditions (Whitehouse & Smith 2004). Results of ongoing research in UK and Ireland are awaited. The same is true for molluscan data (Preece et al. 1986).

The available pollen data reported here forces the rejection of Vera's hypothesis; despite this, large herbivores (natural and domestic) can have a significant impact on contemporary forest structure and composition (Mitchell & Kirby 1990; Humphrey et al. 1998; Vera 2000). The difficulty of quantifying herbivore density has led palaeoecologists to ignore their potential impact in the past, although this is beginning to be redressed (Bradshaw & Mitchell 1999; Bradshaw et al. 2003). Two investigations where details on past herbivore densities are available demonstrate that substantial increases in herbivore grazing influenced tree species composition, but the forest canopies were maintained (Mitchell 1990; Mitchell & Cole 1998). Bradshaw & Hannon (2004) argue that natural fires were probably the principal driver of forest canopy openness during the early Holocene. Their review of pollen and macrofossils implies that factors like fire and windthrow created gaps that herbivores maintained but which they could not create.


  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References

I would like to express my sincere gratitude to Frans Vera for promoting the debate on the role of large herbivores in temperate forests. I would also like to acknowledge the authors who have made their pollen data available through the EPD and IPAL data bases, especially those who have submitted unpublished data. I would like to thank Rob Marchant for his assistance in accessing these data. I also thank John Birks for his comments and advice on statistical analysis, and Keith Kirby, Manel Leira, Peter Moore, George Smith, Nicki Whitehouse and an anonymous referee for their valuable comments on earlier drafts of this paper.


  1. Top of page
  2. Summary
  3. Introduction
  4. Methods
  5. Results
  6. Discussion
  7. Acknowledgements
  8. References
  • Ammann, B. (1989) Late-Quaternary palynology at Lobsingensee. Regional vegetation history and local lake development. Dissertationes Botanicae, 137, 157 pp.
  • Andersen, S.T. (1984) Forests at Løvenholm, Djursland, Denmark, at present and in the past. Kongelige Danske Videnskabernes Selskab Biologiske Skrifter, 24, 1208.
  • Andrade Olalla, A., Valdeolmillos, A. & Ruiz Zapata, B. (1994) Modern pollen spectra and contemporary vegetation in the Paramera mountain range (Avila, Spain). Review of Palaeobotany and Palynology, 82, 127139.
  • Artjushenko, A.T., Arap, R.Y. & Bezusko, L.G. (1982) History of Vegetation of Western Areas of Ukraine in Quaternary Period. Naukova dumka 136, Kiev.
  • Bakker, E.S., Olff, H., Vandenberghe, C., De Maeyer, K., Smit, R., Gleichman, J.M. & Vera, F.W.M. (2004) Ecological anachronisms in the recruitment of temperate light-demanding tree species in wooded pastures. Journal of Applied Ecology, 41, 571582.
  • Barnosky, C.W. (1988) A Late-glacial and Post-glacial pollen record from the Dingle Peninsula, County Kerry. Proceedings of the Royal Irish Academy, 88B, 2337.
  • Bennett, K.D. (1983) Devensian late-glacial and Flandrian vegetational history at Hockham mere, Norfolk, England. New Phytologist, 95, 489504.
  • Berglund, B.E., Lagerås, P. & Regnéll, J. (2002) Odlingslandskapets historia i Sydsverige en pollenanalytisk syntes. Markens Minnen Landskap Och Odlingshistoria På Småländska Höglandet Under 6000 År (eds B.E.Berglund & K.Börjesson), pp. 153174. Riksantikvarieämbetet, Stockholm.
  • Binka, K., Cieśla, A., Łącka, B., Madeyska, T., Marciniak, B., Szeroczyńska, K. & Więckowski, K. (1991) The development of Błędowo lake (central Poland). A palaeoecological study. Studia Geologica Polonica, 100, 383.
  • Björkman, L. (1996) Long-term population dynamics of Fagus sylvatica at the northern limits of its distribution in southern Sweden: a palaeoecological study. Holocene, 6, 225234.
  • Bradshaw, R. & Hannon, G. (2004) The Holocene structure of north-west European forest induced from palaeoecological data. Forest Biodiversity: Lessons from History for Conservation (eds O.Honnay, K.Verheyen, B.Bossuyt & M.Hermy), pp. 1125. CAB International, Oxford.
  • Bradshaw, R.H., Hannon, G.E. & Lister, A.M. (2003) A long-term perspective on ungulate–vegetation interactions. Forest Ecology and Management, 181, 267280.
  • Bradshaw, R.H.W. & McGee, E. (1988) The extent and time-course of mountain blanket bog erosion in Ireland. New Phytologist, 108, 219224.
  • Bradshaw, R. & Mitchell, F.J.G. (1999) The palaeoecological approach to reconstructing former grazing–vegetation interactions. Forest Ecology and Management, 120, 312.
  • Brewer, S., Cheddadi, R., De Beaulieu, J.L., Reille, M. & Contributors, D. (2002) The spread of deciduous Quercus throughout Europe since the last glacial period. Forest Ecology and Management, 156, 2748.
  • Browne, P.R. (1986) Late glacial and Post glacial pollen stratigraphy and vegetation history of the Nephin Begs, County Mayo. PhD Thesis, Trinity College, University of Dublin.
  • Calcote, R. (1995) Pollen source area and pollen productivity: evidence from forest hollows. Journal of Ecology, 83, 591602.
  • Connolly, A. (1999) The palaeoecology of Clara Bog, Co. Offaly. PhD Thesis, Trinity College, University of Dublin.
  • Coxon, P. (2001) Cenozoic: Tertiary and Quaternary (until 10 000 years before present). The Geology of Ireland (ed. C.H.Holland), pp. 387428. Dunenin Academic Press, Edinburgh.
  • Craig, A.J. (1978) Pollen percentage and influx analyses in south-east Ireland: a contribution to the ecological history of the late-glacial period. Journal of Ecology, 66, 297324.
  • Dąbrowski, M.J. (1975) Tree pollen rain and the vegetation of the Bialowieza National Park. Biuletyn Geologiczny Poloniae, 19, 157172.
  • Dambach, K. (1998) An attempt to quantify land surfaces cleared of forests by means of pollen analysis in Central Europe. Quantification of Land Surfaces Cleared of Forests During the Holocene – Modern Pollen/Vegetation/Landscape Relationships as an Aid to the Interpretation of Fossil Pollen Data (eds M.-J.Gaillard & B.E.Berglund), pp. 1730. Gustav Fischer Verlag, Stuttgart.
  • Díaz Fernández, P.M. (1994) Relations between modern pollen rain and Mediterranean vegetation in Sierra Madrona (Spain). Review of Palaeobotany and Palynology, 82, 113125.
  • Digerfeldt, G. (1982) The Holocene development of Lake Sambösjön. 1. The regional vegetation history. Lundqua Report, 23, 124.
  • Dodson, J.R. (1990) The Holocene vegetation of a prehistorically inhabited valley, Dingle peninsula, Co. Kerry. Proceedings of the Royal Irish Academy, B 90, 151174.
  • Fall, P.L. (1992) Pollen accumulation in a montane region of Colorado, USA  – a comparison of moss polsters, atmospheric traps and natural basins. Review of Palaeobotany and Palynology, 72, 169197.
  • Foster, D.R., Clayden, S., Orwig, D.A., Hall, B. & Barry, S. (2002) Oak, chestnut and fire: climate and cultural controls of long-term forest dynamics in New England, USA. Journal of Biogeography, 29, 13591379.
  • Foster, D.R. & Motzkin, G. (2003) Interpreting and conserving the openland habitats of coastal New England: insights from landscape history. Forest Ecology and Management, 185, 127150.
  • Foster, D.R., Motzkin, G. & Slater, B. (1998) Land-use history as long-term broad-scale disturbance: regional forest dynamics in central New England. Ecosystems, 1, 96119.
  • Foster, D.R. & Zebryk, T.M. (1993) Long-term vegetation dynamics and disturbance history of a Tsuga-dominated forest in New England. Ecology, 74, 982998.
  • Foster, D.R., Zebryk, T., Schoonmaker, P. & Lezberg, A. (1992) Post-settlement history of human land-use and vegetation dynamics of a Tsuga canadensis (hemlock) woodlot in central New England. Journal of Ecology, 80, 773786.
  • Fuller, J.L., Foster, D.R., McLachlan, J.S. & Drake, N. (1998) Impact of human activity on regional forest composition and dynamics in central New England. Ecosystems, 1, 7695.
  • Gaillard, M.-J., Sugita, S., Broström, A., Eklöv, M. & Pilesjö, P. (2000) Long term land-cover changes on regional to global scales inferred from fossil pollen – how to meet the challenges of climate research? IGBP PAGES Newsletter, 8 (3), 3032.
  • Göransson, H. (1991) Vegetation and man around lake Björsjöholmssjön during prehistoric time. Lundqua, Report, 31.
  • Hall, V.A. (1989) A study of the modern pollen rain from a reconstructed 19th Century farm. Irish Naturalists’ Journal, 23, 8292.
  • Hannon, G.E., Bradshaw, R.H.W. & Emborg, J. (2000) 6000 years of forest dynamics in Suserup Skov, a seminatural Danish woodland. Global Ecology and Biogeography, 9, 101114.
  • Harmata, K. (1987) Late-Glacial and Holocene History of vegetation at Roztoki and Tarnowiec near Jaslo (Jasło-Sanok Depression). Acta Palaeobotanica, 27, 4365.
  • Heery, A. (1997) The vegetation history of two lake sites adjacent to eskers in central Ireland. Quaternary Newsletter, 82, 3336.
  • Heery, A. (1998) The vegetation history of the Irish midlands: palaeoecological reconstructions of two lake sites adjacent to eskers. PhD Thesis, Trinity College, University of Dublin.
  • Humphrey, J., Gill, R. & Claridge, J.E. (1998) Grazing as a Management Tool in European Forest Ecosystems. Forestry Commission Technical Paper 25. Forestry Commission, Edinburgh.
  • Huntley, B. & Birks, H.J.B. (1983) An Atlas of Past and Present Pollen Maps for Europe: 0–13 000 Years Ago. Cambridge University Press, Cambridge.
  • Jackson, S.T. & Wong, A. (1994) Using forest patchiness to determine pollen source areas of closed-canopy assemblages. Journal of Ecology, 82, 8999.
  • Jacobson, G.L. & Bradshaw, R.H.W. (1981) The selection of sites for paleovegetational studies. Quaternary Research, 16, 8096.
  • Kabailiené, M. (1990) Holocene of Lithuania. Mokslas, Vilnius.
  • Kirby, K.J. (2003) What Might British Forest-Landscape Driven by Large Herbivores Look Like? English Nature Report no. 530. English Nature, Peterborough.
  • Kirby, K.J. (2004) A model of a British forest-landscape driven by large herbivore activity. Forestry, 77, 406420.
  • Kirby, K.J., Robertson, H.J. & Isted, R. (2004) Fresh woods and pastures new: from site-gardening to hands-off landscapes. ECOS, 25, 2633.
  • Koff, T., Punning, J.-M. & Kangur, M. (2000) Impact of forest disturbance on the pollen influx in lake sediments during the last century. Review of Palaeobotany and Palynology, 111, 1929.
  • Lepš, J. & Šmilauer, P. (2003) Multivariate Analysis of Ecological Data Using Canoco. Cambridge University Press, Cambridge.
  • Lindbladh, M. & Bradshaw, R. (1995) The development and demise of a mediaeval forest-meadow system at Linnaeus’ birthplace in southern Sweden: implications for conservation and forest history. Vegetation History and Archaeobotany, 4, 153160.
  • Little, D.J., Boyle, G.M., Ryan, D. & Farrell, E.P. (2001) Intensive Monitoring of an Oak Woodland in Western Ireland. COFORD, Dublin.
  • Little, D.J., Mitchell, F.J.G., Von Engelbrechten, S.S. & Farrell, E.P. (1996) Assessment of the impact of past disturbance and prehistoric Pinus sylvestris on vegetation dynamics and soil development in Uragh Wood, S.W. Ireland. Holocene, 6, 9099.
  • Makohonienko, M. & Walanus, A. (1991) Analizy numeryczne wyników badán palinologicznych osadów Jeziora Lednickiego. Wstep do Paleoecologi Lednideiego Parku Krajobvazowego (ed. K.Tobolski), pp. 6370. Wydawn Nauk Uniwersytetuim Adama Mickiewicza, Poznań.
  • Makohonienko, M., Gaillard, M.-J. & Tobolski, K. (1998) Modern pollen/land-use relationships in ancient cultural landscapes of north-western Poland, with an emphasis on mowing, grazing, and crop cultivation. Quantification of Land Surfaces Cleared of Forests During the Holocene – Modern Pollen/Vegetation/Landscape Relationships as an Aid to the Interpretation of Fossil Pollen Data (eds M.-J.Gaillard & B.E.Berglund), pp. 8598. Gustav Fischer Verlag, Stuttgart.
  • McKeever, M.H. (1984) Comparative palynological studies of two lake sites in western Ireland and north-western Spain. MSc Thesis, Trinity College, University of Dublin.
  • McLachlan, J., Foster, D.R. & Menalled, F. (2000) Anthropogenic origins of late-successional structure and composition in four New England hemlock stands. Ecology, 81, 717733.
  • Mitchell, F.J.G. (1988) The vegetational history of the Killarney Oakwoods, S.W. Ireland: evidence from fine spatial resolution pollen analysis. Journal of Ecology, 76, 415436.
  • Mitchell, F.J.G. (1990) The impact of grazing and human disturbance on the dynamics of woodland in S.W. Ireland. Journal of Vegetation Science, 1, 245254.
  • Mitchell, F.J.G. (2002) Natural invaders: the Postglacial tree colonisation of Ireland. Biology Invaders: the Impact of Exotic Species (eds C.Moriarty & D.A.Murray), pp. 212. Royal Irish Academy, Dublin.
  • Mitchell, F.J.G. & Cole, E. (1998) Reconstruction of long-term successional dynamics of temperate woodland in Białowieża Forest, Poland. Journal of Ecology, 86, 10421061.
  • Mitchell, F.J.G. & Kirby, K.J. (1990) The impact of large herbivores on the conservation of semi-natural woods in the British uplands. Forestry, 63, 333353.
  • Nagy-Bodor, E., Cserny, T. & Nagy, E. (1995) Report on the study performed for the European Pollen Database. European Pollen Database, Arles.
  • Nilsson, T. (1964) Standard pollen diagramme und C14 datiengen aus dem Ageröds mosse in mittleren schonen. Lunds Universitets Årsskrift NF, 259, 152.
  • Obidowicz, A. (1989) Type Region P-a: Inner West Carpathians-Nowy Targ Basin. Acta Palaeobotanica, 29, 1115.
  • Peterken, G.F. (1993) Woodland Conservation and Management, 2nd edn. Chapman & Hall, London.
  • Peterken, G.F. (1996) Natural Woodland: Ecology and Conservation in Northern Temperate Regions. Cambridge University Press, Cambridge.
  • Preece, R.C., Coxon, P. & Robinson, J.E. (1986) New biostratigraphic evidence for the Post-Glacial colonisation of Ireland and for mesolithic forest disturbance. Journal of Biogeography, 13, 487509.
  • Rackham, O. (2003) Ancient Woodland: Its History, Vegetation and Uses in England, 2nd edn. Castlepoint Press. Dalbeattie, Kirkudbrightshire.
  • Roberts, N. (1998) The Holocene An Environmental History, 2nd edn. Blackwell, Oxford.
  • Ruffaldi, P. (1994) Relationship between recent pollen spectra and current vegetation around the cerin peat bog (Ain, France). Review of Palaeobotany and Palynology, 82, 97112.
  • Rybníčková, E. & Rybníček, K. (1988) Holocene palaeovegetation and palaeoenvironment of the Kameničská kotlina basin (Czechoslovakia). Folia Geobotanica et Phytotaxonomica, 23, 285302.
  • Schauffler, M. & Jacobson, G.L. Jr (2002) Persistence of coastal spruce refugia during the Holocene in northern New England, USA, detected by stand-scale pollen stratigraphies. Journal of Ecology, 90, 235250.
  • Schoonmaker, P.K. (1992) Long-term vegetation dynamics in southwestern New Hampshire. PhD Thesis, Harvard University.
  • Smith, A.G. & Goddard, I.C. (1991) A 12 500 year record of vegetational history at Sluggan Bog, Co. Antrim, N. Ireland (incorporating a pollen zone scheme for the non-specialist). New Phytologist, 118, 167187.
  • Sugita, S. (1994) Pollen representation of vegetation in Quaternary sediments: theory and method in patchy vegetation. Journal of Ecology, 82, 881897.
  • Svenning, J.-C. (2002) A review of natural vegetation openness in north-west Europe. Biological Conservation, 104, 133148.
  • Szczepanek, K. (1961) Póżnoglacjalna i holoceńska historia rośalinnoaści Gór Świętokrzyskich. The history of the Late-Glacial and Holocene vegetation of the Holy Cross Mountains (summary). Acta Palaeobotanica, 2, 145.
  • Szczepanek, K. (1982) Development of the peat-bog at Słopiec and the vegetational history of the Świętokrzyskie (Holy Cross) Mts. in the last 10 000 years. Acta Palaeobotanica, 22, 117130.
  • Szczepanek, K. (1989) Type region P-c: Low Beskidy Mts. Acta Palaeobotanica, 29, 1723.
  • Ter Braak, C.J.F. & Šmilauer, P. (19972003) canoco for Windows, Version 4.51 Biometrics Plant Research International, Wageningen.
  • Tobolski, K. (1987) Holocene vegetational development based on the Kluki reference site in the Gardno-Łeba plain. Acta Palaeobotanica, 28, 179222.
  • Tobolski, K. & Okuniewska-Nowaczyk, I. (1989) Type Region P-r: Poznań-Gniezno-Kujawy Lake Districts. Acta Palaeobotanica, 29, 7780.
  • Vera, F.W.M. (2000) Grazing Ecology and Forest History. CABI, Wallingford.
  • Vokes, E. (1966) Late-glacial and Post-glacial vegetation of Killarney, Co. Kerry. MSc Thesis, Trinity College, University of Dublin.
  • Waller, M. (1987) The Flandrian vegetational history and environmental development of the Brede and Panel Valleys East Sussex. PhD Thesis, Polytechnic of North London, London.
  • Watt, A.S. (1947) Pattern and process in plant communities. Journal of Ecology, 35, 122.
  • Weisberg, P.J. & Bugmann, H. (2003) Forest dynamics and ungulate herbivory: from leaf to landscape. Forest Ecology and Management, 181, 112.
  • Whitehouse, N.J. & Smith, D.N. (2004) ‘Islands’ in Holocene forests: implications for forest openness, landscape clearance and ‘culture-steppe’ species. Environmental Archaeology9, 203212.
  • Woodman, P.C. (1978) The Mesolithic in Ireland: Hunter-Gatherers in an Insular Environment. BAR British Series no. 58, British Archaeological Reports, Oxford.
  • Woodman, P., McCarthy, M. & Monaghan, N. (1997) The Irish Quaternary fauna project. Quaternary Science Reviews, 16, 129159.
  • Van Zeist, S. & Van Der Spoel-Walvius, M.R. (1980) A palynological study of the Late-Glacial and the Postglacial in the Paris basin. Palaeohistoria, 22, 67109.