1. Evergreen Closed-Forests

This formation is defined by having the canopies touching or overlapping with a crown cover of > 90%. It includes the rainforests, which in the Hunter Region includes the sub-formations of Subtropical Rainforest, Warm Temperate Rainforest and Cool Temperate Rainforest; as well as the depauperate and lower Dry Rainforest. The closed mangroves are also included in this formation as Low Closed-forest.

Distribution

Rainforests occur mostly around the southern and south-eastern slopes of the Barrington Plateau and in sheltered valleys on the plateau, to the north of Dungog, and in sheltered valleys of the Watagan Mountains. A few isolated patches occur on the Liverpool Range and in the mountains of the southern watershed. Patches of dry rainforest occur in protected sites westwards to the centre of the Valley and further westward to the Widden Valley in the southern mountains. In the driest sites vine thickets occur. They have a different suite of taxa to the dry rainforests. Mangroves are not classified as rainforest, however, they generally have a closed canopy and are included here as low closed-forests. They are confined to coastal enclosures and esturine areas.

Climatic and edaphic factors

They occur in the higher rainfall (1000 - 1500 mm) areas on the rich soils associated with the Tertiary basalts and the Carboniferous shales of the Mt. Royal Range and Liverpool Ranges, and the Permain shales and Tertiary basalts and alluvium in the Watagan Mountains and Hunter Range.

Sub formations

1A. Subtropical Rainforest

In the Subtropical Rainforest the upper canopy averages about 30 m tall with scattered emergents, typically usually of Eucalyptus or Ficus species. A lower sub-canopy, about 7 m tall, may be present, and epiphytes and lianas are common, but the floor is usually relatively open. They occur in the deep valleys, usually with a southern to eastern aspects and at lower altitudes where richer soils have accumulated. Numerous species are present, producing a high species richness, and the trees and shrubs have relatively large and soft mesophytic leaves.


Subtropical Rainforest in the Williams River valley.

1B. Warm Temperate (Submontane) Rainforest

In this sub-formation emergents are fewer, the canapy is not as high and a sub-canopy may also be pesent. Epiphytes are fewer, but lianas are common and ferns are often present on the floor. Tree and shrub leaves are also smaller. They generally occur at altitudes above the STRf and may merge with the CTRf at the upper limit. They also occupy the less favourable areas of lower moisture and/or greater exposure or lower temperatures. Many of the same species that are present in the STRf also occur here but the species richness is reduced.


Warm Temperate Rainforest in Bow Wow Gorge.

1C. Cool Temperate (Montane) Rainforest

The Cool Temperate Rainforest canopy is relatively even, lianas are absent and the floor is often dense with mosses, ferns and tree ferns. They occur in similar aspects to the WTRf but at higher altitudes where the average temperatures are lower. The number of species is few, Nothofagus moorei is dominant, and Doryphora sassafras may be locally common. The tree ferns are Dicksonia antarctica.


Cool Temperate Rainforest in a south facing gully on Barrington Tops.

1D. Dry Rainforest (Low Closed-forest)

In drier sheltered situations with a south-eastern aspect, or amongst rocky outcrops, where there is sufficient moisture Dry Rainforest may be found. The trees are lower, to about 10 m high and the canopy is often dense, emergents are common and there is often a discontinuous shrubby understory. Ground cover may be herbaceous and/or ferny, or open. In the moister areas rainforest species are common, where as in the drier areas the softer mesophytic species are replaced by hardier genera, such as: Trema, Geijera, Ficus, Clerodendrum, Notelaea, Breynia, Citrobatus, Myoporum, Canthium, and Rhagodia. Small vines and twinners, such as species of Cissus, Pandorea, Parsonsia and Marsdenia are common. A few scattered grasses may occur.

 

1E. Mangrove Low Closed-forests

Along waterways and on mud flats in the intertidal zone, mangroves form narrow bands of small trees of uniform height with a dense canopy. One or two species, Avicennia marina and less frequently Aegiceras corniculatum, only are present. Sarcocornia quinqueflora and other halophytes and the sedge Juncus kraussii may occur on the tidal areas to the landward side of the mangroves. Whilst not classified as "rainforest", mangroves usually have a closed canopy.


Avicennia marina mangroves along the Hunter River.

1F. Other Minor Closed Forests

In near coastal areas a number of small areas are occupied by Livistona australis closed forest. These normally contain other co-canopy or emergent species and generally occur on moist sites in the Open-forest formations.

Along some of the streams on the Barrington Tops dense stands of Leptospermum montanum may occur.



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