Ecology of bryophytes along altitudinal and latitudinal ... of bryophytes along altitudinal and latitudinal gradients ... line but also along a longitudinal gradient over a ... (branched

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TROPICAL BRYOLOGY 20 (2001)

Ecology of Bryophytes in New Zealand

Tropical Bryology 20: 117-137, 2001

Ecology of bryophytes along altitudinal and latitudinal gradientsin New Zealand.Studies in austral temperate rain forest bryophytes 15.

Jan-Peter Frahm1 & Ralf Ohlemüller2

1 Botanisches Institut, Meckenheimer Allee 170, D 53115 Bonn, Germany2 present address: Botany dept., University of Otago, P.O.Box 56, Dunedin, New Zealand

Abstract: Six altitudinal transects through temperate rain forests were studied at different latitudesin the South and North Island of New Zealand with respect to species numbers of bryophytes, coverand phytomass of epiphytic bryophytes, composition of life forms and ratio liverworts : mosses.Phytodiversity of bryophytes is almost constant from the lowlands to the high montane belt butdecreases in the subalpine belt. Similarly, phytomass and cover increase with elevation but decreasein the subalpine belt. The percentage of liverworts increases accordingly and can reach maxima of80-90%. The most significant life forms are tails and wefts characteristic for hyperhygric conditions,pendents for cloud belts and cushions for subalpine belts. The altitudinal gradient is much strongerthen the latitudinal gradient, that means the differences between the elevations within a transect aremore important than the differences between the transects. They are attributed to the humidity.The temperate rain forests of New Zealand have similar bryological characteristics as the tropicalrain forests in equatorial latitudes in 2000 – 3000 m altitude but differ in the drier subalpine belt andhigher phytomass.

1. Introduction

Large parts of New Zealand are characterized byan abundance of bryophytes, especially in themoist western side of the Southern Alps on theSouth Islands and at the mountains of the NorthIslands. The mass of bryophytes, which coversnot only the forest floor but also trunks andbranches provides the typical rain forest aspect.Few attempts were made so far to study the

bryophytes as the most characteristic part of therain forests. First studies were undertaken withinthe German BRYOTROP project in different partof the tropics (South America, Africa, SE-Asia,cf. Frahm 1987, 1990, 1994c), where transectstudies from the lowland forest to the forest linewere performed to get a first impression of thefloristic composition on hectare plots, the changesof phytodiversity along the altitudinal gradient,the phytomass, ecological conditions, life

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strategies, morphological adaptations andphytosociology of epiphyte communities. TheBRYOAUSTRAL project was establishedamongst others to collect similar data of thetemperate rainforests of the southern hemisphere.New Zealand provides the best conditions forsuch study. It has still large undisturbed forestareas and for the transect studies, the forest lineis reached all along the south Island and in someparts of the North Islands. Due to a N-S extensionof about 1500 km, New Zealand offers in additionthe interesting chance to determine the speciesdiversity and other parameters not only alongaltitudinal gradients from the lowland to the forestline but also along a longitudinal gradient over along distance from North to South and a W-Egradient, which is characterized by the amountof precipitation. By this way, the bryophytediversity can be determined within athreedimensional model.

The studies should help to find answers forfollowing questions:

A. Evaluations within a single transect:1. how is the species richness expressed byspecies numbers all of the hectare plots studied?2. how is the biodiversity distributed along thetransect? Is there a gradient along the transectand if, is there an increase or a decrease fromlow to high elevations?3. How is the altitudinal zonation of the forestsalong the transect based on bryophytes?

B. Comparison of different transects.1. How are the different transects related to eachother with regard to their species composition,species richness, cover, ratio liverwort : mossesetc. ?2. Are the differences within one transect (alongthe altitudinal gradient) greater than betweendifferent transects at different latitudes? Iselevation or latitude the determining factor ?

C. Comparison with tropical rain forests.1. Are the parameters observed in the temperaterain forests of New Zealand (species number perrelevée, altitudinal gradients, life forms, moss-liverwort index etc.) comparable with tropicalrain forests or are there differences between

tropical and temperate rain forests with regard tothe bryophyte vegetation ?2. Have tropical and temperate rain forestsparameters in common with regard to theirbryophyte vegetation which allows to define theterm rain forest bryologically ?3. Which latitudes in the tropics resemble thetemperate rainforests in New Zealand with regardto their „mossiness“ (cover) or species richness?

A similar study of the same transects and studyareas but based on higher plants was publishedby Ohlemüller & Wilson (2000).

2. Methods

2.1 Study areasField work was carried out in February and March1998. During fieldwork, 34 hectare plots werestudied in forests in 200 m altitudinal intervallsalong 6 transects from the lowland, many to theforest line. The S-N distance between thetransects is approx. 5° = 555 km.The hectare plots were chosen in homogoneousforest sites, which gives a good base forcomparability.

The location of the transects is given in fig. 1,that of the plots in tab. 1.

South IslandTransect 1 (Plots 1-7): Haast Pass Highway (incl.

Lake Ellery, Jackson Bay Road),lowland - subalpine (20 - 800 m a.s.l.),43°56´S - 44°07´S , 169°10´W -169°25´W, mixed podocarpbroadleaved beech forest / beech forest/ beech broadleaved forest. Precipitation3455 mm/year.

Transect 2 (Plots 8-14): Franz Josef Glacier area:Alex Knob Track at Franz Josef Glacier,Morraine Walks at Fox Glacier, BruceBay Road, Gillespie Beach Road,lowland - subalpine (30 - 800 m a.s.l.),43°24´S - 43°25´S, 170°09´W -170°10´W, podocarp broadleaved forest/ broadleaved forest. Precipitation 5920mm/year.

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Transect 3 (Plots 15-20): St. Arnaud area: Rangeand Sloop Track, Mt. Robert, lowland -sub alpine (630 - 1400 m a.s.l.), 41°49´S, 172°52´W, beech broadleaved forest /beech forest. Precipitation 1575 mm/year.

Transect 4 (Plots 21-27): Karamea area: Mt.Stormy Track, Oparara - River andKohaihai - River, lowland - montane (20- 1000 m a.s.l.), 41°06°S - 41°12´S172°08´W - 172°12´W, broadleavedforest / mixed podocarp broadleavedbeech forest. Precipitation 2410 mm/year.

North IslandTransect 5 (Plots 28-32): Ohakune Mt. Road on

Mt. Ruapehu, (incl. Rangataua Road),lowland - subalpine (650 - 1450 m a.s.l.),39°19´S - 39°24´S, 175°25´W,podocarp broadleaved forest / mixedpodocarp broadleaved beech forest /beech forest. Precipitation 2845 mm/year.

Transect 6 (Plots 33-38): Urewera National Parkarea: Lake Waikareiti track andManuoha Hut track, lowland - montane(600 - 1150 m a.s.l.), 38°40´S - 44°30´S,177°05´W - 177°09´W, beech forest.Precipitation 2050 mm/year.

2.2. MethodsIn every hectare plot the following parameterwere determined:

a. The number of bryophyte species (speciesrichness, α-diversity, occurrence). Since all studyareas are of the same size, these data can also beused by determining the frequency of species inthe different plots along the transect. Thecommon species were noted in the field, otherspecies were collected and determined afterfieldwork. Specimens are deposited in theherbarium of the author (BONN), duplicates inthe herbarium of Landcare Research Christchurch(CHR).

b. The cover of bryophytes on soil, rock androtten wood as well as on trees.

c. The ratio of the quantity of liverworts andmosses.

d. Percentage of life forms using the a modifiedclassification by Mägdefrau (1982): turfs,dendroids, tails, pendants turfs, wefts, mats andcushions. This list excludes annuals (which is alife strategy), makes no difference between shortand tall turfs as well as tails and fans and includesdendroids (which is a growth form) in the senseof dendroid turfs. A major point is that not toomuch different life forms should bedifferrentiated because too much categories hidethe trends. The life form categories werepreviously much based on their differentmorphology but should express ecologicaladaptations and should also be redefinedecophysiologically. Therefore different life formscan be significant for the same adaptation. Theexact application of life forms is not alwaysunproblematical and requires explanation:Dendroids include here true dendroid speciessuch as Dendroligotrichum dendroides as wellumbrella mosses (Hypopterygium spp.,Hypnodendron spp.), and dendroid liverworts(Plagiochila spp.) or umbrella liverworts(Hymenophyton spp., Symphyogyna sp.).Tails include typical mosses such asCyathophorum bulbosum, but also Hookeriaceae,species of Plagiochila and species ofSchistochila, Lopidium concinnum, Echinodium,Cyrtomnion, Cyrtopus, Hymenodon, Calomnionand species of Symphyogyna. Fans are includedin tails. The differentiation concerns only agrowth form (branched vs. unbranched), whichmakes no difference with regard to the wateruptake and the fact that both have no contact withother plants and are not attached to the substrate.Species with creeping stems and erect branches(Mesotus, Macromitrium, Dicnemon) are alsoincluded here, although they are confined tohigher altitudes and are adapted to dry conditions.Pendants usually consist of Weymouthiacochleariifolia, W. mollis and Papillaria spp. Thislife form is a modification as shown by the factthat these species are found creeping and notpendant in drier conditions. In contrast, speciesof Lepidolaena, Porella, Mesotus, Dicnemon andWijkia are found in pendant forms in humidhabitats

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Turfs include species of Dicranoloma,Ditrichum, Rhizogonium, but also Ptychomnionaciculare and certain species of Plagiochila.Wefts are represented by Lepidozia spp. andTrichocolea spp. The inclusion of Thuidium asproposed by Mägdefrau must be doubted,because it characterizes much drier habitats asthose of Lepidozia or Trichocolea.Mats are attributed to Hypnum spp., Wijkia sp.and other pleurocarps but also thallose hepatics(Monoclea, Aneura). Perennial thalli such asMonoclea were not considered by Mägdefrau.(thallus is a growth form).Cushions are typically formed by Leptostomumin the subalpine.In several cases an exact application of a life formwas difficult, e.g. in species of Riccardia growingupright, species of Bazzania somewhatintermediate between mats and turfs. In addition,turfs and cushions are not always clearly beseparated. Stands of Dicranoloma can be almostcushion-like in drier habitats but form loose turfsin wetter habitats. This concerns also theclassification of “mossballs” consisting ofspecies of Dicranoloma, Herbertus andChandonanthus.Due to the insufficient knowledge,phytogeographical evaluations could not beperformed. Observations of sterility or asexualviz. sexual propagation were begun but notcontinued since they seemed not to give sufficientresults.

e. The phytomass of epiphytic bryophytes (wetweight) on 0.5 m2. For the determination, theepiphytic bryophytes were scraped off the barkof a representative tree trunk in each plot in 1-2m height. The material was soaked in water for12 hrs and weight with a balance after the excesswater was shaked off. The dry weight could notbe determined in the field because there was nochance to get the bryophytes dried. However,according to our experience in various parts ofthe tropics, the wet weight is generally 3 timeshigher than the dry weight (Frahm1990, 1994c).g. Microclimatic measurements of temperatureand air humidity were made over a period of 3-5days in different altitudes of the transect usingTinytalk (Orion Co.) dataloggers.

3. Results

3.1 PhytomassThe “mossiness” of a rain forest is well expressedby the amount of phytomass produced bybryophytes. It was characterized by the weightof the bryophyte layer on 0.5 m2 of a tree trunkin every relevée. The phytomass depends on thehumidity of a habitat (precipitation = nutrientsupply and length of periods >80% rH duringdaylight = length of photosynthetic period), andsince the precipitation differs in the transectsstudied between 1600 and 6000 mm, it cannotdirectly be compared. Generally an increase ofthe phytomass with elevation can be observed,which corresponds with increasing precipitationand cloud layers (fig. 2). Thus the phytomassincreases along the Haast transect from 630 g/0.5 m2 near sea level to 2800 g/0.5 m2 in 600 melevation. Although the precipitation (based onthe values of the climate station, which can differfrom the relations in the field) is “only” 3450mm/year but almost 6000 mm/year in the FranzJosef Glacier area, the phytomass along the lattertransect is not higher but increases from 250 g/0.5m2 at 200 m elevation to 800 g/0.5m2 at 800m, being considerably higher in two swampforests shortly above sea level, where 540 and580 g were measured. Maximum values arereached at 800 m in the South Island and 1000 –1200 m in the North Island. This is in accordancewith a change in the forest structure from highmontane to subalpine forests. Although thesubalpine forests are much lighter, which couldfavour epiphyte growth, they are apparently muchdrier, which is expressed in a drastic change ofepiphytic bryophyte communities and the lifeforms of their species (Lindlar & Frahm in press).The determination of phytomass per 0.5m2 istherefore also an expression of the different lifeforms composing the bryophyte layer on treetrunks. It cannot be used as parameter for theepiphytic bryophyte production of an altitudinalbelt, because of the uneven distribution ofbryophytes on different trunks and on trunks andcanopy.Phytomass production is, however, controlled bya combination of light, temperature, water andnutrient supply and not correlated with a singleparameter. Thus there was no correlation for

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example between the phytomass and the relativelight intensity measured

3.2 Cover of epiphytic bryophytesThe values for the percentage cover of bryophyteson soil and especially on bark are relativelycharacteristic for the altitudinal belts, which isshown by values derived from different relevéesat the same altitude. Deviations are only possiblee.g. on mountain ridges, which are notcomparable with slopes, in the case that woodswere burnt or host trees infected by fungi. Coverof bryophytes on the forest floor was estimatedbut not evaluated because it varies much andseems to depend much on the competition offlowering plants and ferns, different from tropicalforests, where this effect cannot be observedThe cover of epiphytic bryophytes along thetransects is shown in fig. 3. It is not correlatedwith the precipitation. Transects with higherprecipitation such as Mt. Ruapehu, North Islandhave 35-40% cover between 600 and 1400 mwhereas transects with lower precipitation suchas St. Arnaud, South Island, have higher values,an indication that bryophyte cover of epiphytesis not determined by precipitation but humidity(fog, cloud cover). Generally there is an increaseof the cover of epiphytic bryophytes with thealtitude. Maximum values are reached atelevations with frequent cloud layers or situations(depressions, lake shores) with frequent mist inthe morning, an effect, which can also beobserved in other parts of the world similar tothe elfin forests in the tropics. In the subalpinebelt as in the St. Arnaud transect at 1400 m, thereis a sudden decrease of cover values combinedwith a change of life forms with water storingadaptations as an indication of strongevaporation. Along the Franz-Josef and Karameatransect, high cover values are found alreadyshortly above sea level, which are higher thanthose from the next slopes, which is interpretedby the higher humidity in these stands either byswamp forests or by frequent fog in the coastalplains.The cover values are not directly correlated withthe phytomass, because large covers of thin crustsgive only small phytomass values.

3.3 Ratio liverworts : mosses

The estimation of the ratio between liverwortsand mosses is an easy tool to determine therelative humidity of a stand and to comparedifferent relevées in this respect. It is based onthe experience that liverworts increase withincreasing humidity, either on a continental scale,a regional scale or along a transect. In Europe,there is a distinct increase of liverworts from Eto W (Düll1984). In the Chocó region, one of theregions in the world with the highest precipitationof 15 m/year, liverworts count for 80% of thebryophytes (Frahm 1994a). Liverworts alsoincrease with the altitude in the tropical rainforests (Frahm 1994b). Reason is the lowerdrought tolerance of liverworts.Liverworts generally show a distinct increasealong the altitudinal transects (fig. 4), from 35viz. 40% to 80% along the Haast and Franz-Joseftransects and from 50% to 90% in the Karameatransect. This correlates with high precipitation(Haast: 3455 mm/year, Franz-Josef 5920 mm/year) They are distinctly less represented intransects with lower precipitation as in the drierSt. Arnaud transect (1545 mm/year), whereliverworts do not exceed 10%.

3.4 Species diversitySpecies numbers do not vary much along thetransects (fig. 5). They range between 30 and 50at elevations up to 1000 m. Above 1000 m thereis a sudden decrease of diversity which correlateswith lower cover values as well as phytomassvalues and indicates a major climatic change.

3.5 Life formsThe composition of life forms characterizes muchthe appearance of the bryophyte vegetation. Alife form spectrum allows to obtain a realisticimpression of the habitat (e.g. a lowland forestwith 40% pendants on branches, 30% dendroidsin the forest floor in contrast to a subalpine forestwith 60% cushions). Life forms reflectfurthermore much the different ecologicalconditions of a region (different altitudinal belt,different latitudes), they are a response of thevegetation to the ecological parameters. Life

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forms are mostly correlated with the humidityfactor (water uptake, water retention).The transects are characterized as follows:

1. Haast Pass (fig. 6b)As in the previous transect, dendroids (umbrellashaped Hypnodendron spp. and Hypopterygiumspp.) are most characteristic for low altitudes.They disappear above 400 m. Cushions areconfined to high altitudes (600 – 800 m). Weftshave a maximum at 600 m, where Lepidoziapendulina is dominant on the forest floor as wellas lower tree trunks. Pendants are less frequentas in the Franz-Josef Glacier transect, perhapsbecause of the less frequent mist.

2. Franz-Josef Glacier (fig. 6a)Dendroids is the predominant and highlycharacteristic life form in the lowlands. Theyconsist of species of Hypnodendron andHypopterygium. The percentage is graduallyreduced to 400 m alt. The dendroids at 800 m,however, consist of Dendroligotrichumdendroides. In contrast, pendants are representedat lower altitudes with only small percentages andreach their maximum at 600 m but disappearalmost totally at 800 m. They are significant forcloud forests. Turfs lack in the coastal lowlandforest but increase slightly with altitude and reachtheir maximum at 800 m. Wefts, mats and tailsare represented at all altitudes with low andvarying percentages but no distinct trends.

3. St. Arnaud transect (fig. 6d)The driest transect of all transects studied ischaracterized by a high percentage of turfs(mainly of Dicranoloma spp.), even considerableamounts of cushions through the transectreaching a maximum in the subalpine forest at1400 m, almost lack of pendants, almost constantpresence of mats through the transect as well astails until 1000 m. The distribution of dendroids(here only Dendroligotrichum) is inconstantbecause determined by chance. This speciesforms large clones and can reach high covervalues as here at 1200 m. It is also to beconsidered that this transect starts at 600 m andnot at sea level as the previous ones, which isexpressed in the lack of pendants (except for800 m, a cloud layer), low values for tails and

wefts and lack of umbrella bryophytes.

4. Karamea (fig. 6c)Also here the dendroids are well represented inthe lowlands by umbrella mosses, vanishing atmedium altitudes and being replaced byDendroligotrichum at higher altitudes. Similar tothe previous transects, pendants have also theirmaximum at lower altitudes but disappear above600 m. Wefts increase with altitude with amaximum at 800 and 1000 m and cushions arefound only in the subalpine (1000 m).

5. Ruapehu transect (fig. 6e)The Mt. Ruapehu transect starts also at 600 mand is – like the St. Arnaud transect - no moresituated along the coast, although has a higherprecipitation as transect 4. Both is expressed bythe higher percentage of cushions, especiallyabove 1000 m, decrease of wefts with increasingaltitude, decreasing tails (only up to 1000 m) andincreasing mats.

6. Urewera transect (fig. 6f)This transect starts also at 600 m like bothprevious transects but is more humid. This isexpressed a smaller percentage of cushions anda higher percentage of turfs. The higher altitudesare moister as in the Ruapehu transect, asexpressed by increasing percentages of wefts andhigher percentages of pendants (although not ashigh as in the coastal transects 1-3 along the SouthIsland).

In conclusion, tails, wefts, dendroids, pendantsand cushions have proved to be the mostsignificant life forms along the studied transects.Tails, wefts and possibly also dendroids seem toindicate surplus water supply. These life formshave no mechanisms for water retention, inopposite, they have a maximal surface and thusa maximal evaporation, which is only possiblein hyperhygric conditions. Pendants have localsignificance for altitudes with frequent clouds ormist. In contrast, cushions indicate the drierconditions.

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3.6 Microclimatic measurements

Microclimatic measurements especially of therelative humidity can give a good illustration ofthe habitat conditions of bryophytes. Althoughonly periods of 2-4 days were measured, the datashow characteristics of the habitats, which givegood explanations for the life form spectra in thedifferent transects and elevations.

Along the Haast transect, the humidity was sohigh that the humidity dataloggers did notproperly work. The range of temperatures wassimilarly low along the Haast transect and was10–14°C at 50 m alt. (fig. 7d) but 8-12°C at 400m during the same period, showing a lowdecrease with altitude due to the high humidity.The difference between day and night was 4°Con two sunny days but only 1°C on a rainy day.

Measurements were taken along the Franz-JosefGlacier transect in 200 m and 400 m. At 200 m,the humidity went not below 90% even at noonat a more open microhabitat (fig. 7a) and reachedalmost consistently the dew point in a less openhabitat as well as in 400 m (fig. 7b). Thus thebryophytes are consistently wetted and haveconsistently photosynthesis over the light period.The habitats are also characterized by highnutrient input by high precipitation (around 6000mm/year), which results in high phytomassproduction. Permanent humidity and highrainfall has, however, physiological problemswith regard to gas exchange. Bryophytes attachedto the ground or growing in mats can be coveredby water which reduces much the gas exchange.Therefore the prevailing life forms are umbrellamosses, wefts and tails providing a maximum ofsurface.The temperatures varied during the same periodbetween 8°C in the early morning hours and 14°Cat noon but 11° C and 14°C at 400 m (fig. 7c).(Temperature measurements were taken in thesame spots as the humidity measurements). Itshows considerably low day/night differences of6°C viz. 3°C typically for oceanic climates.All humidity dataloggers along the St. Arnaudtransect at 600, 800 and 1000m showed also abreakdown during the same period but allregistered humidities between 90 and 100%

during the other periods. The temperatures variedbetween 14 and 16°C at all elevations duringcloudy days and reached 22° during a sunny day(fig. 7g). The temperatures in the inland are thushigher even at higher altitudes as along the coast.Also along the Karamea transect, the humiditywas most parts of days and nights above 90%during a period of five days and equally in 200,400 and 600 m alt. (fig. 7e), interrupted only byshort periods at noon, when the humidity droppedto 50% for only a short while. Reason weresudden increases of temperature to almost 20°Cor more (fig. 7f) during sunny seasons. Thehighest values of rH were measured at 200 m alt.The temperature dropped not down below 10°due to the more northern location of the transectas compared to the previous transects.The daily temperatures along the Ruapehutransect in 650, 100 and 1450 m varied muchmore due to the location in the interior of theNorth Island, between 8°C and 2°C in clear nightsand 13°C and 15°C in cloudy nights, 16°C and20°C during sunny days and 6°C and 10°C duringcloudy days, thus more “continental” relationsas compared with the transects along the westcoast of the South Island.Similar ranges were found along the Ureweratransect, where the temperatures in 600m and1000 m varied between 7°C and 15°C at day andnight but reached 22°C on a sunny day (fig. 7h).Conspicuously the temperatures, although takenin 400 m altitudinal difference, showed only fewdifferences, which illustrates that themicroclimate can compensate much differencesin altitude

4. Discussion

Although obtained with relatively simplemethods, this study allows the outline bryologicalcharacteristics of the temperate rainforests ofNew Zealand, the variation along altitudinal andlatitudinal gradients and also a comparison withtropical rain forest in different parts of the worldstudied during the BRYOTROP projects.

Common bryological characteristics of thetemperate rainforests of New Zealand are:1. High phytomass values of epiphytic

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bryophytes with maximum values of 5.6 kg/m2.2. An increase of bryopyhte phytomass from thelowland to the high montane belt but a decreasein the subalpine belt.3. High epiphyte cover values.4. High percentage of liverworts5. High species numbers per area with a decreasein the subalpine.6. Tails, dendroids, wefts as characteristic lifeforms from the lowland to the submontane belt,pendants characteristic in foggy or cloudy areasand cushions in the subalpine belt.

Humidity seems to be the most important factorfor bryophytes: it determines phytomass, coverand percentage of liverworts. These parametersare generally lower along the transects with lowerrain fall. The altitude has also effects on thesefactors, but seems to be correlated with thehumidity (increasing rain fall, cloud cover andmist frequency) with elevation. Latitude ( adifference of 5°) has only small influence on thebryophyte vegetation; it raises the forest lineabout 400 m and causes a drier climate becauseof higher temperatures and higher evaporation.Therefore the different relations along the transecton the North Islands are more attributed to thehumidity than to the latitude. Species richness isnot effected by latitude or altitude but generallyonly lower in the subalpine belt. The speciesrichness of higher plants was also determinedmuch more by altitude than by latitude(Ohlemüller & Wilson 2000).Our results are in accordance with those of Vitt(1991), who studied a transect over 40° in thesame region from Campbell Island S of mainlandNew Zealand to Vanuatu in Oceania. He foundthat species richness is constant over the latitudes,however, increasing with elevation, which couldnot be confirmed in New Zealand, perhapsbecause Vitt´s study was based only on mosses.

A comparison with studies from tropical rainforests (Frahm 1987, 1990, 1994c) shows thatonly altitudes above about 2000 m in the tropicscan be compared with temperate rain forests inNew Zealand (fif. 8). This is presumably due tothe different climatic conditions in the tropicallowland and (sub)montane regions. Although theprecipitation may be comparable, the

temperatures are much higher in the tropics,causing physiological problems for thebryophytes. The rain forest in 0-1000m in thetemperate regions is thus comparable to themontane to subalpine forest in the tropics. Thisis confirmed by the fact that several species(Lepyrodon tomentosus, Monoclea gottschei)found in the temperate rain forests in southernChile have migrated north into the Andes andare found again in Colombia and Venezuela 2000m higher, according to the relative habitatconsistency of species. Other temperate rainforest species such as Dicranoloma billardieriare found again in the mountains of CentralAfrica. This is also confirmed by the fact thatmany genera typical for temperate rain forestsare found in tropical rain forests at altitudes above2000 m such as liverwort species of Lepicolea,Chandonanthus, Herbertus, Bazzania,Plagiochila or Lepidozia.Above 2000 m we have similar climaticconditions as well as bryophyte vegetation in bothrain forests types. This includes similar life formspectra, phytomass and cover. Thus the montaneforest of the tropical rainforest in equatoriallatitudes can be compared with the lowland rainforest in 40°S, the high montane tropical withthe montane temperate and the subalpine tropicalwith the high montane temperate forest (fig. 8).This becomes not so evident from theclimatological data: the mean annualtemperatures in New Zealand vary between 8°and 11°C at the base of the transects. Thiscorresponds to 2900 – 3300 m alt. at Mt. Kahuziin Zaire (Frahm 1994a), however, the temperaturein New Zealand is much depressed because ofthe oceanic influence and not directly comparablewith the situation in the midth of the Africancontinent.

There is, however, a distinct differences betweenthe both rain forest types:Whereas the values for cover and phytomass intropical rain forests increase towards the forestline, there is a decrease in the temperate rainforests of New Zealand in the subalpine belt. Thiseffect is attributed to the drought at this elevation,which is expressed by drought tolerant life forms.It corresponds with the scheme in fig. 8, in whichthe subalpine temperate forest is comparable with

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the regions in the tropics above the forest line.

The phytomass of epiphytic bryophytesdetermined in Central Africa (Frahm 1994c, herecalculated for wet weight) was 60 g/m2 at 900 malt., 210 g/m2 at 1900 m, 300 g/m2 at 2900 and1800 g at 3300 m and thus distinctly lower thanin all transects in New Zealand. Maximum valuesin Borneo (Frahm 1990) were 1360 g/m2 wetweight at 3300 m alt. and thus comparable to St.Arnaud 800 m or Haast 1300 m.

The bryological parameters indicate the followingaltitudinal zonation of the temperate rain forestsin New Zealand:1. A lowland zone > 200 m which is weaklydistinguished by lower phytomass and cover (notin swamp forests in the Franz-Josef glaciertransect), lower percentage of liverworts (not inthe Karamea transect) and composition of lifeforms.2. The montane zone from 200 to 800 – 1400 m,which can hardly be differentiated in any sub- orhigh montane zone. The varying upper limitdepends on the latitude and humidity. It is lowestin the southernmost transect in the South Islandand raises with increasing latitude and decreasingprecipitation.3. The subalpine zone above 800 – 1400 mcharacterized by dramatical reduced values forcover, phytomass, species numbers, liverwortpercentage and change of the composition of lifeforms.

Acknowledgements.We would like to thank the German ResearchFoundation (DFG) for financial support of the BRYOAUSTRAL project by grants to J.-P. Frahm (Fr 491/9-1) and W. Frey (Fr 404/3-1). We also thank theDepartments of Conservation in Tongariro, Nelson,Gisborne and Hokitika in New Zealand for permissionto collect bryophytes and also our colleagues Dr.Jessica Beever (Auckland) and Dr. Allan Fife(Christchurch) for help and support.

Literature

Düll, R. 1984. Computerized Evaluation of theDistribution of European Liverworts.Journal of the Hattori Botanical Laboratory56: 1-5.

Frahm, J.-P. 1987. Ökologische Studien über dieepiphytische Moosvegetation in Regen-wäldern NO-Perus. Beih. Nova Hedwigia88: 143-158.

Frahm, J.-P. 1990. The ecology of epiphyticbryophytes on Mt. Kinabalu, Sabah (Malay-sia). Nova Hedwigia 51: 121-132.

Frahm, J.-P. 1994a. A contribution to the bryofloraof the Chocó region, Colombia. I. Mosses.Tropical Bryology 9: 89-110.

Frahm, J.-P. 1994b. Scientific results of theBRYOTROP Expedition to Zaire andRwanda 2. The altitudinal zonation of thebryophytes on Mt. Kahuzi, Zaire. TropicalBryology 9: 153-167.

Frahm, J.-P. 1994c. Scientific results of theBRYOTROP Expedition to Zaire andRwanda 1. The ecology of epiphyticbryophytes on Mt. Kahuzi (Zaire). TropicalBryology 9: 137-152.

Gradstein, S.,R., Frahm, J.-P. 1987. Die floristischeHöhengliederung der Moose entlang desBryotrop-Transekts in NO-Peru. Beih. Novahedwigia 88: 105-114.

Lindlar, A., Frahm, J.-P. (in press) Epiphyticbryophyte communities in New Zealandtemperate rainforests along selectedaltitudinal transects. Studies in australtemperate rainforest bryophytes 13.Phytocoenologia.

Mägdefrau, K. 1982. Life-forms of bryophytes. Pp.45-58 in A.J.E. Smith (ed.), BryophyteEcology, London (Chapman & Hall).

Ohlemüller, R., Wilson, J.B. 2000. Vascular plantspecies richness along latitudinal andaltitudinal gragients: a contribnution fromNew Zealand temperate rainforests. EcologyLetters 3: 262-266.

Vitt, D.H. 1991. Distribution patterns, adaptivestrategies, and morphological changes ofmosses along elevational and latitudinalgradients on South Pacific Islands. Pp. 205-231 in: P.L. Nimis & T.J. Crovello (eds.),Quantitative Approaches to Phytogeo-graphy. Amsterdam (Kluwer).

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Tab. 1: Location of the study areas

Plot Date Lat. [S] Long. [E] Transect Altitude1 26.02.1998 44° 04' 168° 40' 1 202 26.02.1998 44° 01' 168° 46' 1 203 22.02.1998 43° 58' 169° 10' 1 404 25.02.1998 44° 03' 169° 22' 1 2005 25.02.1998 44° 02' 169° 25' 1 4006 21.02.1998 44° 07' 169° 21' 1 5907 24.02.1998 44° 07' 169° 21' 1 8008 20.02.1998 43° 40' 169° 35' 2 309 19.02.1998 43° 25' 169° 51' 2 5011 15.02.1998 43° 25' 170° 10' 2 19012 18.02.1998 43° 24' 170° 10' 2 42013 18.02.1998 43° 24' 170° 10' 2 60014 16.02.1998 43° 24' 170° 09' 2 80015 08.03.1998 41° 48' 172° 51' 3 63016 08.03.1998 41° 49' 172° 52' 3 80017 07.03.1998 41° 49' 172° 48' 3 85018 06.03.1998 41° 49' 172° 52' 3 100019 06.03.1998 41° 49' 172° 52' 3 125020 06.03.1998 41° 49' 172° 52' 3 140021 03.03.1998 41° 07' 172° 06' 4 2022 02.03.1998 41° 10' 172° 10' 4 20023 02.03.1998 41° 10' 172° 10' 4 20024 04.03.1998 41° 17' 172° 13' 4 35025 04.03.1998 41° 17' 172° 13' 4 60026 01.03.1998 41° 17' 172° 13' 4 80027 01.03.1998 41° 17' 172° 13' 4 100028 15.03.1998 39° 24' 175° 25' 5 65029 16.03.1998 39° 23' 175° 27' 5 80030 14.03.1998 39° 21' 175° 29' 5 102031 14.03.1998 39° 20' 175° 30' 5 122032 14.03.1998 39° 19' 175° 31' 5 145033 21.03.1998 38° 45' 177° 10' 6 60034 21.03.1998 38° 44' 177° 11' 6 80035 19.03.1998 38° 44' 177° 10' 6 95036 22.03.1998 38° 41' 177° 7' 6 68037 22.03.1998 38° 41' 177° 7' 6 100038 20.03.1998 38° 41' 177° 7' 6 1150

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Table 2. Studied transects.Precipitation and temperature was determined from climatological datasets (obtained from ClimateResearch and Information Services, Wellington, NZ) of the nearest available station. Values givenhere are therefore only approximate.

No. Transect Altitudinal range Precipitation Temperature[m a.s.l.] [mm/year] [mean annual ºC]

1 Haast Pass 20 - 800 3455 < 82 Franz Josef Glacier 30 - 800 5920 93 St. Arnaud 630 - 1400 1575 94 Karamea 20 - 1000 2410 115 Mt. Ruapehu 650 - 1450 2845 96 Urewera 600 - 1200 2050 10

Map 1. Location of transects.

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Frahm & Ohlemüller

0

500

10001500

2000

2500

3000

20 200

400

600

800

1000

1200

1400

m alt.

g/0.

5qm

HaastFranz JosefSt. ArnaudKarameaRuapehuUrewera

Fig. 2: Phytomass of epiphytic bryophytes (wet weight) in different altitudes along the sixtransects.

020406080

100

20 200

400

600

80010

0012

0014

00

m alt.

Cov

er % Haast

Franz JosefSt. ArnaudKarameaRuapehuUrewera

Fig.

Fig. 3: Cover of epiphytic bryophytes (%) in the relevées along the transects.

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0

20

40

60

80

100

m alt.

perc

enta

ge o

f liv

erw

orts

HaastFranz JosefSt. ArnaudKarameaRuapehuUrewera

Fig. 4: Percentage of liverworts along the transects.

0102030405060

520

040

060

080

010

0012

0014

00

m alt.

spec

ies

num

ber

St. ArnaudKarameaHaastFranz JosefRuapehuUrewera

Fig. 5: Species numbers in hectare plots along the altitudinal transects

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Frahm & Ohlemüller

0% 50% 100%

5

200

400

600

800

Alti

tude

(m) Dendroids

TailsPendantsTurfsMatsWefts

Fig. 6a: Composition of life forms along the Franz-Josef Glacier transect.

0% 50% 100%

5

20

200

400

600

800 DendroidsTailsPendantsTurfsMatsWeftsCushions

Fig. 6b: Composition of life forms along the Haast transect.

131



0% 20% 40% 60% 80% 100%

600

800

1000

1200

1400DendroidsTailsPendantsTurfsMatsWeftsCushions

Fig. 6d: Composition of life forms along the St. Arnaud transect.

Fig. 6c: Composition of life forms along the Karamea transect.

0% 20% 40% 60% 80% 100%

200

400

600

800

1000 DendroidsTailsPendantsTurfsMatsWeftsCushions

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Frahm & Ohlemüller

0% 20% 40% 60% 80% 100%

600

800

1000

1200


Fig. 6e: Composition of life forms along the Ruapehu transect.

0% 20% 40% 60% 80% 100%

600

800

1000


Fig. 6f: Composition of life forms along the Urewera transect.

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RH2

S/N 21650 Zeit (Start 18.02.98 09:59:39)

18.2 09:59 15:59 21:59 19.2 03:59 09:59 15:59

Hum

idity

(%R

H)

20,0

30,040,0

50,060,0

70,0

80,090,0

100,0110,0

120,0

Fig. 7a: Franz-Josef Glacier transect, curve of air humidity in an open (!) site at 200 m alt. Valuesabove 100% are caused by condensation of water on the electrode.

RH3

S/N 39365 Zeit (Start 18.02.98 09:59:32)

18.2 09:59 15:59 21:59 19.2 03:59 09:59 15:59

Hum

idity

(%R

H)

-20,0

0

20,0

40,0

60,0

80,0

100,0

120,0

140,0

Fig. 7b: Franz-Josef Glacier transect, curve of air humidity in 400 m alt.

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Frahm & Ohlemüller

T4

S/N 49393 Zeit (Start 18.02.98 10:59:05)

18.2 10:59 16:59 22:59 19.2 04:59 10:59 16:59 22:59 20.2 04:59

Tem

pera

ture

°C

8,0

10,0

12,0

14,0

16,0

18,0

20,0

22,0

Fig. 7c: Franz-Josef Glacier transect, curve of temperature at 400 m alt.

T3

S/N 17978 Zeit (Start 21.02.98 18:19:39)

21.2 18:19 22.2 06:19 18:19 23.2 06:19 18:19 24.2 06:19 18:19 25.2 06:19

Tem

pera

ture

°C

8,0

9,0

10,0

11,0

12,0

13,0

14,0

15,0

16,0

17,0

Fig. 7d: Haast Transect. Curve of temperature at 50 m. alt.

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RH3

S/N 39365 Zeit (Start 01.03.98 11:24:06)

1.3 11:24 2.3 3.3 4.3 5.3

Hum

idity

(%R

H)

40,0

50,0

60,0

70,0

80,0

90,0

100,0

110,0

120,0

Fig. 7e: Karamea transect. Curve of humidity in 600 m alt.

T2

S/N 17938 Zeit (Start 01.03.98 11:17:18)

1.3 11:17 2.3 3.3 4.3 5.3

Tem

pera

ture

°C

6,08,0

10,012,014,016,018,020,022,024,026,028,0

Fig. 7f: Karamea transect. Curve of temperature over a period of five days.

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Frahm & Ohlemüller

15So 16Mo 17DiZeit (Start 14.03.98 10:31:29)

-5,0

0

5,0

10,0

15,0

20,0

25,0

30,0

35,0

Tem

pera

ture

°C

Fig. 7g: Ruapehu-Transect. Curves of temperature in 650, 100 and 1450 m alt.

19Do 20Fr 21Sa 22So 23MoZeit (Start 18.03.98 18:17:09)

0

5,0

10,0

15,0

20,0

25,0

30,0

Tem

pera

ture

°C

Fig. 7h: Urewera transect. Curves of temperatures in 600 m and 1000 m alt.

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Fig. 8: Comparison of altitudinal zonation of bryophytes in Peru and New Zealand

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Ecology of bryophytes along altitudinal and latitudinal ... of bryophytes along altitudinal and latitudinal gradients ... line but also along a longitudinal gradient over a ... (branched