To Graze Or Not to Graze: That Is the Question

To graze or not to graze: that is the question J.P.Bakker*, D.Bos and Y. De Vries Laboratory of Plant Ecology, University of Groningen. P.O.Box 14, NL-9750 AA Haren, The Netherlands. fax +31 503632273, e-mail:[email protected], [email protected], [email protected]. *corresponding author Key words: exclosures, long-term monitoring, plant communities, salt-marsh management, species richness, vegetation maps Abstract Changing land use in both natural and artificial salt marshes shifted the focus from coastal protection and agricultural exploitation towards nature conservation interest. Transformation of large areas into nature reserves or national parks included abandoning of livestock grazing by some authorities in charge of management. Succession in natural salt marshes that have never been grazed by livestock, shows a climax of the shrub Atriplex portulacoides at the lower marsh and the tall grass Elymus athericus at the higher marsh of Schiermonnik- oog. As this salt marsh has an age of about 40 years, the long-term climax of natural succession is not known. Exclosure experiments at the always cattle-grazed marsh of Schiermonnikoog, reveals an increase of Atriplex portulacoides at the lower and of Elymus athericus at the higher marsh. The species richness in permanent plots (4 m2) decreases in abandoned areas on the marshes at Schiermonnikoog, Terschelling and Skallingen. The species richness is always higher in grazed plots ranging from 0.01-2500 m2 in artificial marshes in the Netherlands. Long-term (over 20 years) experiments with exclosures and different stocking rates of cattle and sheep in the Netherlands and Germany, show that the Elymus athericus community can get dominant in both natural and artificial marshes. Subsequently, the number of plants communities decreases. Exceptions seem to be related to low rates of sedimentation or inf- luence of fresh water. Experiments lasting less than 10 years show no dominance of the Elymus athericus community. Changes in canopy structure towards a taller vegetation after abandoning or decreasing stocking rate, has negative effects on winter and spring staging geese, and positive effects on some breeding birds. As with natural succession, further changes may take place at the longer term. Continuation of these experiments and monitoring are of vital importance to draw further conclusions. As results of abandoning or reduc- tion of stocking rate may affect various organisms in different ways, the task for salt-marsh management is to define the management goal. After that the means to reach the target can be decided upon, and the question 'to graze or not to graze' can be answered. Nomenclature of plant species follows Van Der Meijden 1990 Introduction grazing over the past twenty years. These changes in landuse have two reasons. Salt marshes could establish in the Locally, farmers are loosing interest in Wadden Sea area since 600 BC as a result these nowadays marginal areas compared of slowing down of the sea-level rise after to the high intensity farming in inland the last Glacial Period (Behre, 1996). areas. Secondly, several authorities in They resulted from sedimentation of silt charge of nature conservation stop all during tidal inundation. As the sediment human interference, including livestock included nutrients, salt marshes harbour grazing. This especially holds for heavily fertile soil with subsequent high plant grazed artificial marshes in Germany, production capacity. Therefore, it is no where the management aim is to turn surprise that salt marshes have been agri- these marshes into more natural salt mars- culturally exploited from their very origin hes (Stock, 1993; Kiehl & Stock, 1994). as grazing ground for livestock. Landuse To understand the effects of cessation by grazing in the entire Wadden Sea area of grazing, we will first discuss the natur- has been practised for about 2600 years al succession on salt marshes and compa- now. Initially it took place on natural salt re these to livestock-grazed marshes. The marshes, but since several centuries also back barrier salt marsh of the Dutch on artificial salt marshes, that mainly island of Schiermonnikoog shows docu- developed along the mainland coast. mented natural succession. The eastern More details on salt-marsh development part continuously extends further east- and its landuse are reviewed by Esselink ward. Salt-marsh development takes place (2000). in the shelter of dunes fringing the North Currently about 50% of the salt-marsh Sea beach. Hence, a chronosequence, area in the international Wadden Sea is representing succession (De Leeuw et al., grazed by livestock (De Jong et al., 1993; Olff et al., 1997) has established 1999). Large areas have been taken out of featuring very young marsh at the east Figure 1. Development of the eastern part of Schiermonnikoog. Different age classes of the vegetation as derived from maps and aerial photographs are indicated. 1809 1848 1874 1894 1913 1939 1955 1964 1974 1986 1993 1996 and older marshes more to the west, ran- chronosequence species replacement can ging from zero to about 150-200 years be recorded. The lower salt marsh starts (Figure 1). Increasing age of the marsh with Salicornia spp., Puccinellia mariti- coincides with thicker layer of sediment ma followed by Spergularia maritima, resulting from tidal inundations. The Plantago maritima, Limonium vulgare, thickness of the sediment layer correlates and Atriplex portulacoides at the oldest positively with the nitrogen pool (Olff et stage. The higher marsh features Pucci- al., 1997; Van Wijnen & Bakker, 1997). nellia maritima, Festuca rubra followed The increasing nutrient availability results by Artemisia maritima, and eventually in more plant biomass and a taller canopy Elymus athericus (Olff et al., 1997) (Van De Koppel et al., 1996). In this (Figure 2). Figure 2. Changes in vegetation during salt-marsh succession at Schiermonnikoog. Lower marsh trans- forms into an Atriplex portulacoides marsh. The higher marsh turns from a Puccinellia maritima sward into Festuca rubra, after which Artemisia maritima and eventually Elymus athericus invade. Brent goose grazing pressure is highest towards the younger salt-marsh stages, after which succession evicts the geese (after Drent & Van Der Wal 1999). "ISLANDS" CREEK Goose hours.d-1.km-2 5000 0000 20000 1 1 5000 0 Elymus > 60 yrs Atriplex 40 yrs Festuca Puccinellia 30 yrs Plantago Tr iglochin 15 yrs Salicornia 3 yrs Artemisia The oldest part (150-200 years) of the the international Wadden Sea is possible. salt marsh of Schiermonnikoog has Finally, we will discuss grazing as a tool always been cattle grazed and harbours for salt-marsh management in relation to communities with Salicornia spp., possible targets. Plantago maritima, Limonium vulgare, Puccinellia maritima at the lower marsh and with Festuca rubra, Juncus mariti- Methods mus, and locally Elymus athericus at the higher marsh. Despite the high age, thick Study sites for permanent plots layer of sediment and large nutrient pool All study sites with permanent plots are (Van Wijnen & Bakker, 1997), cattle classified as barrier-connected salt mars- have prevented the tall plant species hes (De Jong et al., 1999). Atriplex portulacoides and Elymus athe- The first study site is located at the ricus from becoming dominant. Instead, island of Schiermonnikoog, The Nether- they have set back the successional clock lands (Table 1). Stocking rates decreased to plant communities harbouring species from 1.5 cattle.ha-1 in the 1970s to 0.5 naturally occurring at younger salt mars- cattle ha-1 from 1995 onwards. Two hes, be it at different abundances (Olff et exclosures (50 x 12.5 m) were erected in al., 1997). We expect under such condi- 1973, one at the transition of a low dune tions, where the successional clock has to the higher salt marsh, the other at the been reset that the cessation of grazing somewhat lower marsh (Bakker, 1989). will quickly result in a vegetation compo- We established 15 paired permanent plots sition that matches the nutrient pool; i.e. a (inside and outside the exclosures). The vegetation that would have occurred wit- vegetation composition in the plots was hout livestock grazing. We will try to recorded annually. place the effects of cessation of livestock The second study site is located at the grazing into the framework of the undis- island of Terschelling, The Netherlands turbed succession at the natural salt marsh (Table 1). The site was grazed for over a of Schiermonnikoog. Several case studies century. The Terschelling marsh 'De on the effects of the cessation of grazing Groede' is grazed with 175 cattle and have been carried out on natural island about 15 horses amounting to 0.5 live- and artificial mainland salt marshes in stock ha-1(authorities in charge of Denmark, Germany and the Netherlands. management, pers. comm.). Two exclos- The scale of recording ranges from per- ures (30 x 30 m) were erected in 1971 manent plots of 4 m2, surveys up to 2500 (Bakker, 1983). One at the transition of a m2 and vegetation mapping of larger low dune to the higher marsh, the other at study sites. the high marsh. Both exclosures were The aim of the present paper is (i) to adjacent to larger dunes systems, hence compare natural succession and secondary received fresh seepage water. The third succession after the cessation of grazing, experimental site was at a transect of higher (ii) to bring together individual studies at to lower marsh. Here the position of the different spatial scale on the effects of fence was changed in such a way that cessation of livestock grazing, (iii) to con- four situations were established: control clude to which extent generalisation for ungrazed, experimentally grazed, control Table 1. Overview of the study sites: substrate, position, area, level with respect to Mean High Tide (MHT), grazing management ( 1 sheep unit equals 2.8 sheep).

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