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Bryophytes and their distribution in the Blue Mountains region of ...

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244 Cunn<strong>in</strong>ghamia 10(2): 2007 Down<strong>in</strong>g et al, <strong>Bryophytes</strong> <strong>in</strong> <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s<br />

that time perhaps seen as a sou<strong>the</strong>rn extension <strong>of</strong> <strong>the</strong> <strong>Blue</strong><br />

Mounta<strong>in</strong>s. Most are accepted as alp<strong>in</strong>e species <strong>and</strong> have<br />

been listed by Ramsay et al. (1986) as occurr<strong>in</strong>g <strong>in</strong> <strong>the</strong><br />

alp<strong>in</strong>e areas <strong>of</strong> New South Wales above 1800 m elevation.<br />

The species are: Aulacomnium palustre (Hedw.) Schwägr.,<br />

Bl<strong>in</strong>dia robusta Hampe, Bryum australe Hampe, Catagonium<br />

nitens (Brid.) Cardot, Entosthodon apophysatus (Taylor)<br />

Mitt., Lepyrodon pseudoalgurus B.H.Allen, Notoligotrichum<br />

crispulum (Hook.f. & Wilson) G.M.Sm., Physcomitrium<br />

conicum Mitt., Polytrichastrum alp<strong>in</strong>um (Hedw.) G.L.Sm.<br />

<strong>and</strong> Sanionia unc<strong>in</strong>ata (Hedw.) Loeske. Only two <strong>of</strong> <strong>the</strong>se<br />

species collected by von Mueller, Polytrichastrum alp<strong>in</strong>um<br />

<strong>and</strong> Bl<strong>in</strong>dia robusta, have s<strong>in</strong>ce been recorded from <strong>the</strong> <strong>Blue</strong><br />

Mounta<strong>in</strong>s.<br />

Polytrichastrum alp<strong>in</strong>um has been recorded from Kanangra<br />

Boyd National Park, above 1000 m a.s.l., (by J. Glime <strong>in</strong> 1981)<br />

<strong>and</strong> at Wentworth Falls (by H. Ramsay <strong>in</strong> 1977). This species<br />

has also been recorded from <strong>the</strong> summit <strong>of</strong> Mount Canobolas,<br />

1395 m a.s.l., 130 km north-west <strong>of</strong> Katoomba (Down<strong>in</strong>g,<br />

Oldfield & Fairburn-Wilson 2002), mak<strong>in</strong>g its presence <strong>in</strong> <strong>the</strong><br />

higher areas <strong>of</strong> <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s not surpris<strong>in</strong>g.<br />

Bl<strong>in</strong>dia robusta is a conspicuous species <strong>and</strong> <strong>the</strong>re are two<br />

specimens (<strong>in</strong> <strong>the</strong> John Ray Herbarium, University <strong>of</strong> Sydney<br />

(SYD)) collected <strong>in</strong> 1930 at Wentworth Falls by A. Burges.<br />

There are a number <strong>of</strong> o<strong>the</strong>r moss specimens collected by<br />

Burges at Wentworth Falls on <strong>the</strong> same date, <strong>and</strong> as <strong>the</strong>se<br />

species still commonly occur <strong>in</strong> <strong>the</strong> vic<strong>in</strong>ity <strong>of</strong> Wentworth<br />

Falls, it is apparent that Burges did collect B. robusta from<br />

this location. It is difficult to imag<strong>in</strong>e how its occurrence<br />

along stream banks would have been overlooked by both<br />

earlier <strong>and</strong> later collectors. We have been unable to f<strong>in</strong>d<br />

it anywhere <strong>in</strong> <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s <strong>and</strong> it may have been<br />

destroyed by drought, fire or urban development.<br />

Habitat <strong>and</strong> ecological <strong>in</strong>formation on bryophytes is<br />

generally very limited. Many herbarium packets (although<br />

appropriately labelled with location) bear m<strong>in</strong>imal<br />

<strong>in</strong>formation describ<strong>in</strong>g l<strong>and</strong>form (plateau, ridge, valley, <strong>and</strong><br />

canyon), aspect, moisture or lack <strong>of</strong> it, vegetation type (heath,<br />

woodl<strong>and</strong>, forest, <strong>and</strong> closed forest), degree <strong>of</strong> shad<strong>in</strong>g,<br />

substrate (rock, soil or s<strong>and</strong>, tree trunk, tree branches, tree<br />

fern, fallen log), underly<strong>in</strong>g rock (s<strong>and</strong>stone, shale, basalt,<br />

limestone, <strong>and</strong> granodiorite) or associated bryophytes. Such<br />

specimens have contributed to species lists for locations, but<br />

could not contribute <strong>in</strong>formation concern<strong>in</strong>g habitat.<br />

O<strong>the</strong>r problems relate to identification. In <strong>the</strong> case <strong>of</strong> taxa<br />

that have been viewed by experts <strong>in</strong> recent years, it is<br />

possible to be confident <strong>in</strong> <strong>the</strong> names allocated to specimens,<br />

e.g. Macromitrium specimens determ<strong>in</strong>ed by Vitt & Ramsay,<br />

Papillaria determ<strong>in</strong>ed by H. Streimann, Sphagnum by R.<br />

Seppelt <strong>and</strong> Aneura <strong>and</strong> Riccardia determ<strong>in</strong>ed by H. Hewson.<br />

However, <strong>the</strong>re are many groups, such as Campylopus,<br />

Grimmia <strong>and</strong> Leucobryum, for which identification is<br />

challeng<strong>in</strong>g. Often <strong>the</strong>re are no recent publications <strong>and</strong> it is<br />

not with<strong>in</strong> <strong>the</strong> scope <strong>of</strong> this study to check <strong>the</strong> determ<strong>in</strong>ations<br />

<strong>of</strong> all <strong>the</strong> specimens held <strong>in</strong> various herbaria.<br />

Discussion<br />

The effect <strong>of</strong> accessibility on bryophyte record<strong>in</strong>g<br />

There was a considerable difference <strong>in</strong> <strong>the</strong> number <strong>of</strong> species<br />

recorded at different locations (Table 5) <strong>and</strong> accessibility has<br />

probably been <strong>the</strong> major factor determ<strong>in</strong><strong>in</strong>g <strong>the</strong> number <strong>of</strong><br />

species recorded from some locations. Follow<strong>in</strong>g construction<br />

<strong>of</strong> <strong>the</strong> railway <strong>in</strong> 1868, visitors were able to travel by tra<strong>in</strong><br />

to Lawson, Wentworth Falls <strong>and</strong> Blackheath (Valder 1988).<br />

Govetts Leap (at Blackheath) <strong>and</strong> Wentworth Falls were <strong>the</strong><br />

most popular <strong>Blue</strong> Mounta<strong>in</strong>s dest<strong>in</strong>ations, accord<strong>in</strong>g to The<br />

Railway Guide <strong>of</strong> <strong>the</strong> day. Cheap tra<strong>in</strong> fares <strong>and</strong> a growth<br />

<strong>in</strong> tourist facilities attracted many visitors. Construction <strong>of</strong><br />

walk<strong>in</strong>g tracks at Wentworth Falls <strong>and</strong> Govetts Leap began<br />

<strong>in</strong> 1890. By 1910, motor coaches facilitated travel from <strong>the</strong><br />

railway to more distant locations (Burke 1988). In 1875,<br />

when <strong>the</strong> Mount Wilson Railway Station (later changed<br />

to Bell) was completed, it became much easier to travel to<br />

Mount Wilson <strong>and</strong> Mount Irv<strong>in</strong>e (Valder 1988).<br />

The early collectors, Whitelegge, Forsyth <strong>and</strong> Watts, all used<br />

rail <strong>and</strong> <strong><strong>the</strong>ir</strong> collections, for example from Gr<strong>and</strong> Canyon at<br />

Blackheath, from Valley <strong>of</strong> <strong>the</strong> Waters at Wentworth Falls,<br />

from Dantes Glen at Lawson, all <strong>in</strong>dicate <strong>the</strong>y used <strong>the</strong> same<br />

walk<strong>in</strong>g paths that we use today. The Rev. W.W. Watts walked<br />

or travelled on horseback to visit parishioners (Ramsay 1980)<br />

but today we still use <strong>the</strong> same road that Watts used, w<strong>in</strong>d<strong>in</strong>g<br />

through closed forest from Mount Wilson to Mount Irv<strong>in</strong>e.<br />

Factors affect<strong>in</strong>g <strong>distribution</strong> <strong>of</strong> bryophytes <strong>in</strong> <strong>the</strong> <strong>Blue</strong><br />

Mounta<strong>in</strong>s: topography <strong>and</strong> geology<br />

Most <strong>of</strong> <strong>the</strong> bryophytes <strong>in</strong> <strong>the</strong> <strong>Blue</strong> Mounta<strong>in</strong>s are found <strong>in</strong> <strong>the</strong><br />

closed forests <strong>of</strong> gullies <strong>and</strong> valleys on s<strong>and</strong>stone <strong>and</strong> shale.<br />

The dense canopies <strong>of</strong> closed forests protect bryophytes<br />

from high light, extreme temperatures <strong>and</strong> desiccation by<br />

strong w<strong>in</strong>ds. Damp rocks, soil, fallen logs <strong>and</strong> tree roots<br />

are <strong>of</strong>ten covered with bryophytes. Unlike many eucalypts,<br />

trees <strong>of</strong> <strong>the</strong> closed forest, such as Doryphora sassafras,<br />

Ceratopetalum apetalum <strong>and</strong> Callicoma serratifolia have<br />

persistent bark, allow<strong>in</strong>g epiphytic bryophytes to colonise<br />

tree trunks, branches <strong>and</strong> twigs. <strong>Bryophytes</strong> that can survive<br />

<strong>in</strong> low light levels <strong>of</strong> closed forest are <strong>of</strong>ten large <strong>and</strong><br />

conspicuous, with growth forms that allow <strong>the</strong>m to access<br />

maximum light levels. For example, pendulous mosses<br />

(Papillaria spp.) hang from tree trunks <strong>and</strong> tree fern trunks,<br />

<strong>and</strong> dendroid mosses <strong>and</strong> liverworts (Hypnodendron vitiense<br />

subsp. australe, Hypopterygium spp. <strong>and</strong> Hymenophyton<br />

flabellatum) grow upwards from wet rocks <strong>and</strong> soil along<br />

creek banks (Figures 4, 5). Tall, upright species, such as<br />

Dawsonia superba (Figure 12) rapidly colonise newly<br />

exposed earth <strong>of</strong> l<strong>and</strong> slips, or gap<strong>in</strong>g holes <strong>in</strong> <strong>the</strong> ground<br />

where mature trees have fallen. Three beautiful mosses,<br />

Neckera pennata, Cyathophorum bulbosum <strong>and</strong> Calomnion<br />

complanatum grow on <strong>the</strong> trunks <strong>of</strong> tree ferns, tree trunks<br />

<strong>and</strong> wet rocks, almost always <strong>in</strong> deep shade close to streams.

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