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Fire History and Soil Gradients Generate Floristic Patterns in Montane Sedgelands and Wet Heaths of Gibraltar Range National Park PDF

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Preview Fire History and Soil Gradients Generate Floristic Patterns in Montane Sedgelands and Wet Heaths of Gibraltar Range National Park

Fire History and Soil Gradients Generate Floristic Patterns in Montane Sedgelands and Wet Heatlis of Gibraltar Range National Park Paul Richard Williams'-^and Peter John Clarke^ 'Botany, SchoolofEnvironmentalSciences andNaturalResources Management, University ofNew Engiand, ArmiDAiE, NSW, 2351 ([email protected]). ^SchoolOFTropicalBiology, James Cook University, and Queensiand Parks andWiidufe Service, PO Box 5597, Townsviue, Queenslwd 4810,Austraua([email protected]). WiiiiAMS, p. AND Clarke P.J. (2006). Fire historyand soilgradients generate Aoristicpatterns inmontane SEDGELWDS ANDWETHEATHS OFGIBRALTARRangeNationalPark.Proceedings oftheLinneanSocietyof NewSouth Wales 111, 27-38. High rainfall escarpment areas along the Great Dividing Range provide habitats for sedgeland and wet heath vegetation in areas with impeded drainage. There are few studies ofthe processes that influence the floristic composition ofmontane sedgelands and heaths in relation to fires that sweep these landscapes. Gibraltar Range National Park contains extensive areas of sedge-heaths that remain mostly fi-ee fi'om anthropogenic disturbance. These areas have a well-known fire history which provides an opportunity to test whether: 1) plant resources are related to time-since-fire; 2) floristic composition is more strongly related to physiographic factors than time-since-fire, and 3) floristic composition ofvegetation is related to fire fi-equency. Physiographic position strongly influenced the vegetation's structure and floristic composition, with taller heaths confined to better-drained edges whereas sedgelands were more common inpoorly drained slopes regardless offire regime. In turn, these patterns were related to soil conductivity reflecting the fertility status ofthe soils. Upper slope heaths were more species rich than those lower in the landscape where soil conductivity was higher Time-since-fire strongly influenced heath structure and species richness declined in the heaths with canopy closure at some sites. Floristic composition across the physiographic gradientwasmoredivergentsoonafterfire andbecamemore similar 15 yearsafterfire. Fire fi'equencyhadno significanteffectonshrub speciesrichness,butfrequentfires decreasedthe abundanceof some woody species. Inter-fire intervals oflessthan sevenyears mayreducethe abundance ofsome shrub species. Boththehistory offire andease ofaccess makethe sedgelands andwetheaths ofGibraltarJlange an ideal locationto assess the long-term effects offire regimes inmontane sedge-heaths. Manuscriptreceived IMay2005, acceptedforpublication 7 December2005. KEYWORDS: Fire ecology, heaths, resource gradients, speciesrichness, time-since-fire. Juncaceae and Restionaceae whilst adjacent wet INTRODUCTION heaths are dominated by shrubs, especially of the families Ericaceae, Fabaceae and Myrtaceae (Keith MontaneplateauxalongtheGreatDividingRange 2004). have high rainfall and low evaporation creating ideal The earliest studies of sedge-heaths identified conditions for sedgelands andwetheath communities that sedgelands dominated the wettest areas, while where drainage is impeded (Keith 2004). Beadle shrubsweremorecommoninbetter-drainedpositions (1981) described the mosaic of sedgelands and wet (Pidgeon 1938). Early descriptions also considered heaths as "sedge-heaths", but more recently Keith sedge-heaths as a sere in succession leading to more complex vegetation (Pidgeon 1938; Davis 1941; (2004)hascircumscribedthemas"MontaneBogsand Fens", reserving the term "Montane Heaths" to those Jackson 1968).Withthisfocus,Millington(1954)was heathlandswithwell-drainedsoils onrockysites. The the first to descNriSbeWthe sedge-heaths ofthe Northern Tablelands of describing the cyclic formation more poorly drained sedgelands are dominated by of Sphagnum hummocks and hollows following species of the monocotyledon families Cyperaceae, FIRE HISTORY, SOIL GRADIENTS AND FLORISTIC PATTERNS the European tradition. More recently, Whinam and MATERIALSAND METHODS Chilcott (2002) surveyed the floristic composition and environmental relationships of Sphagnum bogs Study sites in eastern Australia but did not sample those areas Study sites were located in Gibraltar Range where Sphagnum was absent. National ParkinFebruary 1995 by choosingreplicate Contemporary studies have considered geology, sedge-heaths that were widely spaced with different soil depth and soil moisture as interrelated factors firehistories. Fire histories ofdifferent sections ofthe controlling floristic patterns within sedge-heath parkwere determinedthrough consultation with park communities (Burrough et al. 1977; Buchanan 1980; staffandtheirfirehistoryrecords. Firefirequencyover Brown and Podger 1982; Pickard and Jacobs 1983; the last 30 years was found to be similar for many Bowman etal. 1986; Myerscough and Carolin 1986). sedge-heaths of the park, differing only in whether The importance of water level in determining the they had been burnt since 1980 (i.e. differing in the distributionofdominantmontanesedge-heathsspecies time since last fire). was shown by Tremont (1991), who evaluated the Sedge-heaths occur as distinct swampy low- effects ofhydrological changes resulting from a dam lying islands surrounded by eucalypt forest. Six built across a wet heath in Cathedral Rock National sedge-heaths were selected for this survey based Park. Resource-driven processes were highlighted in on certainty and differences in known fire history the detailed studies ofKeith and Myerscough (1993) and ease of access. All six sedge-heaths were burnt who found species richness was inversely related to in wildfires of both 1964 and 1980. Two remained soil resources, consistent with resource competition unbumt since 1980 andwere considered in this study models that predict greatest species diversity with as long unbumt (i.e. 15 years since fire). Two sedge- lowest levels ofresources (Tilman 1982). heaths were burnt in a plarmed bum in 1994 and Fire is a regular event in sedge-heath were considered regenerating communities, having communities, due to the dense graminoid biomass been bumt only half a year prior to this study. The and the fine elevated fuels presented in the leaves of remaining two sedge-heaths had an intermediate age the sclerophyllous shrubs. Both obligate seeder (fire- since lastfire. Onewasbumtinawildfire in 1989, the killed) and resprouting species co-exist within wet other in a plaimed bum in 1990. Therefore ofthe six heaths, although resprouting shrub species are more sedge-heaths surveyed, two were last bumt 15 years, numerous than those killed by fire (Clarke and Knox two 5-6 years, and two were bumt half a year prior 2002). Plant species richness is usually highest in the to the survey (Williams 1995). Following the 1995 initial post-fire community, due to the recruitment survey all study sites were bumtby a landscape-scale of short-lived species (e.g. Specht et al. 1958), with wildfire seven years later in November 2002 and a an inverse relationship between shrub canopy cover subset ofthe original sites were re-sampled. and understorey species richness (Specht and Specht 1989; Keith and Bradstock 1994). Frequent fires in Sampling design sedge-heath communities also have the potential to Preliminary inspections of the sites suggested alter floristic composition ifthe life cycles ofplants that floristic patterns were likely to vary with the soil are not completed between fire intervals (Keith et al. moisture gradient from the drier outer edge to the 2002). drainage channels flowing through the centre ofeach There are few studies of the processes that sedge-heath, as documented in similar communities mediate the floristic composition of the montane in southemAustralia (e.g. Buchanan 1980; Keith and sedge-heaths in northern NSW, unlike their coastal Myerscough 1993). Therefore a stratified sampling and southern counterparts (see Keith 2004). Gibraltar designwasused, whereeachsedge-heathwas divided Range National Park contains extensive areas of into three habitats: drier outer edge, mid-slope and montane sedge-heaths that remain mostly fi-ee fi-om drainage charmel. To survey spatial variation, three anthropogenic disturbance. These bogs and heaths plots wereplaced in each ofthe three habitats in each also have a well-known fire history which provides ofthe top, central and lower sections ofsedge-heath. an opportunity to test whether: 1) plant resources Therefore 27 plots (3 habitats x 3 plots x 3 sections) (soil and light) are related to time-since-fire; 2) were surveyedineachofthe six sedge-heaths (2 areas floristic composition is more strongly related to X 3 time-since-fire), providing a total of 162 plots. In physiographic factors than time-since-fire, and 3) addition 36 plots (2 habitats x 3 plots x 2 areas x 3 floristic composition is relatedto fire firequency. fire frequencies) were re-sampled in 2003 for woody species. In this sampling, the drier outer edge and 28 Proc. Linn. Soc. N.S.W., 127, 2006 WILLIAMS AND CLARKE p. P.J. drainagechannelwere surveyedineachoftwo sedge- variables of total species, resprouters, obligate heaths for each fire frequency. seeders, woody plants, graminoids, grasses, ferns The quantitative nested quadrat method and forbs. In addition analyses of covariance were (Morrison et al. 1995) was used to document species performed with conductivity as a covariate. A fire- GLM abundance at each plot. This method uses concentric frequency orthogonal analysis was also applied sub-quadrats of increasing size, which were 1, 4, 9, to species richness data collected in 2003 with fire 16 and 25m^ in this study. An abundance score out frequency (3 levels) and habitat (2 levels). APoisson offive was given to each ofthe species at each plot, error structure with a log link function was applied derived fi-om the number of sub-quadrats it was for species richness data, a binomial error structure present within. Plant nomenclature follows Harden with a logistic link function for species presence/ (1990-93) with later modifications adopted by the absence dataandanidentitylinkfunctionwas applied National Herbarium, Sydney, and voucher specimens to normally distributed data. NCW of uncommon species were lodged in the Beadle Herbarium (NE) Herbarium. Fire responses (obligate seeder or resprouter) were documented RESULTS for species within the recently burnt sites. Electrical conductivity and soil pH measurements were taken Effects oftime-since-fire and habitat using electronic meters and a 1:5 ratio of soil to Eighty-nine taxa were recorded from the 162 distilled water. Electrical conductivity is positively plots sampled in 1995 (seeAppendix 1). Shrubs were correlated with soil ionic concentrations and hence the most common growth form (41 spp.) followed A is a crude index of soil fertility. light reading was by graminoids (21 spp.), forbs (13 spp.), grasses taken at the soil surface at each plot and calculated and trees (5 spp. each) and ferns (4 spp.). Among all as a percentage ofa reading taken above the canopy. growth forms, 19 species were killed by fire and 70 Aspect, degree ofslope and canopy height were also were recorded as resprouting. Ofthose species killed recorded at eachplot. byfire, onlyBanksiamarginatahadcanopy-heldseed banks. Analyses Ordination of sample sites in two dimensions The species composition and abundance data showed distinct clustering ofsites in relation to time- for each plot were correlated with environmental since-fire and physiography (Fig. 1). The strongest variables using a canonical correspondence analysis effects were time-since-fire with 15 years at the top (CCA) through the CANOCO program. The CCA of the ordination and the more recently burnt sites is calculated in two stages. Firstly the similarity of at the base, whilst the drier edge site to the wetter the 162 plots, based on species composition and chaimel sites are distributed left to right (Fig. 1). This abundance, is calculated to display the relative floristic gradient is initially wide in the short time- ordering of sites (i.e. ordination). The ordination is since fire sites but converges with longer time-since undertaken using a correspondence analysis (CA), fire (Fig. 1). Bothlightandsoilresourceswererelated which is a modal response model, which assumes stronglytophysiographicpositionandtime-since-fire species reach a maximum abundance at a point (Fig. 1) andwhen examinedusingunivariate analyses along an environmental gradient. The second step they show the effect ofcanopy closure on light levels CCA in the is a multiple regression technique that (Table 1, Fig. 2). Univariate analyses also show a evaluates the link between environmental variables strong resource gradient with soil conductivity being at each plot and the initial ordination ofplots based higher along the charmels with corresponding lower on species abundance. In addition, the 36 plots (2 pH(Fig. 2). BothconductivityandpHwere, however, habitats x 3 plots x 2 areas x 3 fire frequencies) that not consistently related to time-since-fire (Table 1, werere-sampledin2003 forwoody species onlywere Fig. 2). analysed using CCA with fire frequency and habitat There was significant negative correlation = as environmental variables. between conductivity and species richness (r The relationships between environmental - 0.53, P < 0.001) (Fig. 3). The relationship between variables of canopy height, light, pH and soil species richness, fire response and growth form conductivity, and habitat and time-since-fire were groups were further examined using GLM which examined using a general linear model (GLM) with showed inconsistent patterns of time-since-fire and habitat (3 levels) and time-since-fire (3 levels) as habitats with a significant interaction term (Table orthogonal factors. This orthogonal design was also 2). The drier outer edge plots contained a greater GLM applied in analyses for the richness response Proc. Linn. Soc. N.S.W., 127, 2006 29 FIRE HISTORY, SOIL GRADIENTS AND FLORISTIC PATTERNS and Lepidosperma limicola remained the most abundant, but the grass Time-Since-Fire Canopy Amphipogon strictus was replaced by the obligate seeding twiner, Cassytha glabella.Therecentlyburntedgeplots contained a total of62 species whilst 48 species were documented in plots unbumt for 15 years. In these edge plots the mean number of obligate seeding species and resprouting species decreased over time, as did richness of herbaceous species (Fig. 4). The mid slope and channel plots in recently biimt sedge-heaths contained atotalof40species.Themostabundant species in the wetter mid slope and channel plots ofrecently burnt sedge- Light heaths were Lepidosperma limicola, Baeckea omissa, Gymnoschoenus sphaerocephalus and Drosera binata. Lepidosperma limicola, Baeckea omissa and Gymnoschoenus 1.0 1.0 sphaerocephalus were also the most abundant species in the sedge-heaths Figure 1. Biplot from the canonical correspondence analy- unbumt for 15 years. By this stage sis. Symbols represent plots, arrows represent environmen- the herb, Drosera binata, was much tal gradients. Top cluster = 15 year old plots, middle cluster 5 year old, bottom cluster 0.5 year old plots. Circles = edge less abundant and was replaced by plots, squares = mid slopes, triangles = drainage channel plots. Epacris obtusifolia, an obligate seeder subshrub. In the chaimel plots resprouterrichness decreasedthrough number of species compared with the other plots time whilst obligate seeder richness increased (Fig. (Fig. 4a). Species richness decUned with time-since- 4b,c). On the bog slopes species richness appearedto fire in these outer edge plots and reached a peak peaksixyears afterfirethendeclinemainlyduetothe some five years later on the slopes (Fig. 4a). The decrease in grass and sedge species (Fig. 4a,e). four most abundant species in drier edge plots of recently burnt sedge-heaths were Ptilothrix deusta, Effects offire frequency on shrub species Amphipogon strictus, Leptospermum arachnoides No significant trend in species composition with and Lepidosperma limicola. In areas unbumt for 15 firefrequencywasdetectedforshmbspeciesintheCCA years, Ptilothrix deusta, Leptospermum arachnoides analyses,which are shown. Similarly, no effect offire Table 1. Summary results for two factor general linear models fortime-since-fire and habitat for environmental variables.All models have a Poisson error structures with a log-link function and have scale estimated using Pearson Chi-squared. Factor df Canopyheight %Light pH Conductivity F ratio Fratio Fratio Fratio Time-Since-Fire 2 141.7 *** 244.9 *** 2.9 * 2.6 ns Habitat 2 30.0 *** 27.0 *** 8.3 *** 65.9 *** TSF XHabitat 4 2.3 ns 2.5 ns 3.7 *** 3.3 * Residual 153 30 Proc. Linn. Soc. N.S.W., 127, 2006 I WILLIAMS AND CLARKE p. PJ. Channel Midslope Outeredge Channel Mid slope Outer edge 25-1 d) 20 15 10 to 0-" Channel Mid slope Outer edge Channel Midslope Outer edge % Figure 2. Mean (+se) for a) canopy height, b) full sunlight, c) pH, and d) conductivity for each ofthree physiographic positions in the sedge-heaths and among three time-since-fire locations. 35 Channel ^p ^ # Mid slope 30 i CM Outer edge in 25 - 20 - U ^151 Ol 10 H —————————————————————————————— —I I I I I I I I I I I I I I 1 I I I I I I I I I I I I I I I 5 10 15 20 25 30 35 Conductivity Figure 3. Relationship between conductivity (dS/m), species richness and topograph- ic position across the sedge-heaths at Gibraltar Range. Lowness Une fitted. Proc. Linn. Soc. N.S.W., 127, 2006 31 FIRE HISTORY, SOIL GRADIENTS AND FLORISTIC PATTERNS frequency on species richness was detected (Table H 3). However, six common resprouting species had X f3O significantly different abundances across sites with ^5' oTPl different fire frequencies (Table 3, Fig. 5). Ofthese, ao> O•-t Leptospermum gregarium, Hibbertia rufa, Boronia ^>^' H polygalifolia and Grevillea acanthifolia had lower ft 3Oa &29 abundances in sites with the highest fire frequency (Fig. 5). en i>> BT • K) &> CeZl DISCUSSION -<l rt 3 S9 3 n ON ^ ^zn ^ Distinctfloristicpatternsoccurinthesedge-heaths tu ao> Wol* 3 of Gibraltar Range representing both physiographic s en and fire-regime effects. Firstly, floristic composition ** "0 o33ft'" ow••1s wS!" vlairnikeesd awliotnhg ignrcardieeanstesd ienlescotirlicamloisctounrdeu,ctiwvhiitcyh aanrde c ^ nutrient accumulation along the drainage lines. « O M These drainage-driven patterns are similar to those ^ o' 2O.i^£ W^s! o"591^* FdoersecsrtibeodnbythKeeistohuathnedrMnyeSrysdcnoeuyghpl(a1t9e9a3u) oatfDNarSkWe.s * en S. Despite these structural similarities, major floristic ** ^3 » SfnD differences separate central and southern NSW from £, northern regions (Keith 1995; Keith 2004), but more n CfQ o o ^b^\ S ^ cst^; ?NS^r* r»st dTeatbalielleadndssurvaenydscoofmtphaerasteidvgee-haenaatlhysseisnatrhee Nreoqrutihreerd.n o' o' era •^ •t 33- Sft. ss 3o Initial comparative analyses oflife-history attributes *** 3 ^3 5w5 fDffttt. (os-f- o!ML. rseusggpeosntsessiyminldarromgersowttohotfhoerrmeasctomcpooasstithieoanthsan(dKefiitrhe "-t a&s» s"1* et al. 2002). to tLoo o-B15' gooQ. <cr 3?FN^^> towarSpdectiheesourtiecrhneesdsgevaolfuetshewehreaethgsenaenradlllyowheirghoenr 3. r»t9 IKS/M)* the slopes and drainage channel corresponding to o n 3 "0 33" 5r patterns at Darkes Forest. This inverse relationship fwt rs nS"th between species richness and electrical conductivity (positively correlated with soil fertility) was similar 3 s 00 U) "1 ^pt- a. to that found in other heaths (Keith and Myerscough fafi S»aT 1993; Myerscough et al. 1996), suggesting a II e «> f^ widespread resource-competition effect in heaths ft 3 5* &9 S 2. withresourcegradients. However, the overallnumber * ^ a. tra oi?> of species encountered was much smaller than the (O ^ Q "Wo9&19 Sns' haingdhMsypeercsiecsourgichhn1e9s9s3)f.ound in coastal heaths (Keith 4i- a n o Lu Habitat segregation of serotinous shrub species o' Br a o33^. A^2* CTQ along gradients ofmoisture and soil fertilityhas been * 3 e oi-S explored in manipulative experiments by Williams * ft B * CC/O3 &•>t "a and Clarke (1997) who suggest that a combination of faB vi • seedlingestablishmentandseedlingsurvivalinrelation • 3^ 0\ U) "-t TOl to moisture gradients segregates species within these ON sedge-heaths. Patterns of seedling establishment are o' 3o. initiated by fire and the effect oftime-since-fire was prominent in our analyses. Following the passage of * ^ ft fire, the sedge-heath canopy is openedup and ground level insolation peaks, but as plants grow taller, 32 Proc. Linn. Soc. N.S.W., 127, 2006 WILLIAMS AND CLARKE p. PJ. a) Total b) Resprouters 28 - 24 - ^20 in £12 a. w ° 8 d - Channel Mid slope Outer edge Channel Mid slope Outer edge c) Obligate seeders d) Woody species 14 n 14 -I 12 12 - E 10 ID <N 10 -(S^I c M in ^ 8 o aat. 6 - w £ 6 o 4 - Q. 6 4i 'S - 2 - Channel Mid slope Outer edge Channel Mid slope Outer edge 14 14 e) Grasses and sedges f) Forbs and ferns 12 - 12 - CM 10 <gl0 E in in ^(SI 8 .1 '3 6 - o ^6 Of S. a. v\ tA *o•- 4 - o 4 d miilln - 2 o-' Channel Mid slope Outer edge Channel Mid slope Outer edge Figure 4. Mean (+se) for species richness a) total, b) resprouters, c) obligate seeders, d) woody species, e) grasses and sedges, f) forbs and ferns for each ofthree physiographic positions and among three time-since-fire locations. Proc. Linn. Soc. N.S.W., 127, 2006 33 « FIRE HISTORY, SOIL GRADIENTS AND FLORISTIC PATTERNS O A7 PAo P O tI o — L^ o C n CD O"pn efnt Do ft po c o^ c <o^-f 03 f3t X 3 o o © S"H t &9 ta Sn-^n o"-* « "ot 1«. w «ML ^ i-ti B8 o- &29 "J . s»r fT o a^. inomi Sum N) Di-t.i < < » 3 » • 00 ^u aSn^i ^^t^o> »esa « S to o *n Og3.^>SoT3n a3 B33 ^ »s v^> <e» 'xj i s- 5'•>^s s: s n <rBt^- ^«O» f-•f(1i AwB"s_ ^-^-< oto 00 too ?< t^o •c^t«^ fM^ ^o I.S io to 2 s^* ??• i^a^.,01:05 ^sa-^ «S-T "a1s raoe> rBt- s^^ ^ inal ksia ©to5IriT* "0 25' V9 •1 (» a e<Mr»a. J&^S» Cao 3 n»rt- 3o Ssir an 0^ ?< . s s^^^B2Kr. <pb1o bo ^M 0^Oa^5q ^^^'t^- (o^^Q^". wo"<' ipari bber ? >! (t 'TS a =ar. oa3 «»3 TJ S NSWri" SnS> 2-1«^ SBS»fBi ?^^ ag Ci iTn£3 CrBt CT\ ?^to 3c&3> «Bav«ns;> sS- ^S ar*2.ts^» f^>is!i. 51?SSai a' 13 Sar a 6»?S^ aB" "Ta i •0ftf9Ji BSaiT* ' K 2^ ff 05 a* SM* Si "25 s^." a f>-K p ^K. S^d" Sa3 ib p ^M ^s?s; ^^ F&i-9t- 3 .^raS^ c?">>? sted mod « >XS- ^~Ks- e. "13 a 5'^ * ^ a- to o ?^^ o ?<^ ^ ^ to to £; a ^B. •galifo oronia S: ^ a td ^3 a' 34 Proc. Linn. Soc. N.S.W., 127, 2006 WILLIAMS AND CLARKE p. P.J. 0o) c (0 c 3 < CD CO CO CO CO CO 1•S i 1 1 .CO s i 5 i CD CD c 1 O) C t CO 2 -Q0Q} & 1 a CO CO 2 CD CD 1 ^^ CO i 1 CCD 1 O0Q) '5 i CO o CQ 1 CD 1 CD i 1 & 1 1 -J BCO CD UJ OQ Figure 5. Total abundance scores (frequency score) for the ten most common woody plantsrecorded in sedge-heaths in 2003, eight months after a fire among areas that been burnt 2, 3, and 5 times since 1964. ground layer insolation subsequently decreases. and then became less variable at 15 years time-since- Neither soil pH nor conductivity showed consistent fire. This may reflect the lack of strong competitive trends with time-since-fire although it is likely that exclusion in the drainage channel heaths, possibly post-fire soil nutrients peaked immediately after fire. due to their narrow and patchy distribution. We Hence it is thought that competition for light is the think the alternative explanation ofthe lack ofshort- main driver for differences in floristic composition lived species immediately after fire unlikely because with time-since-fire (Specht and Specht 1989; Keith short-lived species were common along creek banks. and Bradstock 1994) or alternatively the differences Unfortunately, studies of long-unbumt sedge-heaths simplyreflect species' life spans. Decreases inwoody were halted in 2003 when all long-unbumt sedge- species richness with time-since fire are prominent in heaths wereburnt in wildfires. thebetter-drained, outer-edge heaths. Hencewe think Fire frequency appears to have much less that competition rather than variation in the life span influence on composition than time-since-fire, ofplants is the causal factor. although only shrub data were sampled. When shrub There were no major decreases in species species abundances were examined individually richness in the channel or slope plots, which may several dominant species had reduced abundances reflect the slower growth dynamics of montane under frequent fire regimes. This is consistent with sedge-heaths compared with coastal systems. patterns in the adjacent dry sclerophyll forests Overall, variation in floristic composition along the (Knox and Clarke in this volume) where higher fire drainage gradientwas greatest immediately afterfire. frequencies reduced plant performance. We would Proc. Linn. Soc. N.S.W., 127, 2006 35 ' FIRE HISTORY, SOIL GRADIENTS AND FLORISTIC PATTERNS A predict, however, that if the intervals between fires moorlandexample fromTasmaniaandmainland were less than eight years then the dominance and Australia. Proceedings oftheLinneanSocietyofNew composition would change. South Wales 115, 61-75. Keith, D.A. (2004). 'Ocean shores to desertdunes: the nativevegetation ofNew SouthWales andtheACT'. ACKNOWLEDGEMENTS (NSWDepartment ofEnvironment andConservation, Sydney). Keith, D.A. andBradstock, R.A. (1994). Fire and NSW The Director ofthe National Parks andWildlife competition inAustralianheath: aconceptual model ServiceisthankedforallowingustodothisworkinGibraltar andfieldinvestigations. JournalofVegetation Range National Park under permit No. 1601. The Service Science 5, 347-354. staffatGlenInnes arethankedfortheirencouragementand Keith, D.A. andMyerscough, P. J. (1993). 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