Queensland tropical rain forests

The Queensland tropical rain forests are a terrestrial ecoregion located in northeastern Australia and belonging to the Australasian realm. The forest contains the world's best living record of the major stages in the evolutionary history of the world’s land plants.[2] The history of the evolution of marsupials and songbirds is also well represented.

Queensland tropical rain forests
Daintree Rainforest, Queensland
Ecology
Realm	Australasian realm
Biome	tropical and subtropical moist broadleaf forests
Geography
Area	33,129 km^2 (12,791 sq mi)
Countries	Australia
States	Queensland
Conservation
Conservation status	Vulnerable
Global 200	Queensland tropical rain forests
Protected	3,260 km² (10%)[1]

The ecoregion covers 32,700 square kilometers (12,600 sq mi) of northeastern coastal Queensland, from the coast up a series of plateaus and tablelands to the mountains behind the coast. The ecoregion comprises three separate sections. The northern area, which includes Cairns, is the largest, from 15°30’ to 19°25’ south latitude. This northern section is also known as the Wet Tropics bioregion.

Flora

Typical scenery in the Wet Tropics, a walking path with fauna at Josephine Falls, located near Innisfail. Foliage is thin in the photograph due to Cyclone Larry's effects.

Young cassowary in the Daintree Rainforest

The Queensland tropical rain forests are designated one of the Global 200 ecoregions. The ecoregion is the largest remnant of Australia's rain forest flora, home to ancient assemblage of plants, called the Antarctic flora, presently characteristic of New Zealand and southern Chile. Fossil pollen records indicate closed forest covered most of Australia between 50 and 100 million years ago.[3] These forests represent the closest living remnant of the vegetation type from which all of Australia's unique vegetation developed.[3] The vegetation remained across Australia and Antarctica until about 15 million years ago.

Conifers of the southern hemisphere family Araucariaceae are the characteristic tree species. In the northern section of the ecoregion, Kauri commonly form the forest canopy, with Agathis robusta most common at lower elevations, and A. microstachya and A. atropurpurea predominant at higher elevations. In the southern sections, Araucaria cunninghamii is predominant, with Araucaria bidwillii dominant in two small areas. Conifers in the family Podocarpaceae are also present, including genera Podocarpus and Sundacarpus. The forests are thick with vines, ferns, epiphytes, and palms.

These forests are limited to areas of high rainfall and good soils. In waterlogged soils, the rainforest flora gives way to Melaleuca thickets, and on poor soils and in drier areas Eucalyptus becomes dominant. The rainforest flora is intolerant of fire, and where periods of drought have allowed devastating fires, the rainforest flora has retreated, allowing fire-tolerant Eucalyptus to become established. If a relatively wet period persists, the rainforest flora may reestablish itself. It is thought that the land management practices of the aboriginal Australians, which involve setting regular fires to keep the eucalyptus woodlands open, may have encouraged the expansion of eucalyptus forests at the expense of the rainforest flora. These rainforests seem to have retreated considerably since the arrival of the aboriginals' ancestors 50,000 years ago, and are presently limited to isolated pockets comprising less than 2% of the continent's area.

Conservation

These forests are particularly interesting because of their southern location and the high degree of endemism of their plant and animal species. Deforestation caused by logging, road building and farming has led to habitat fragmentation [4] and diminishing populations of species such as spotted-tailed quoll (Dasyurus maculatus), cassowary (Casuarius casuarius), and ring-tail possum (Hemibelideus lemuroides). Introduced species also pose a serious threat to many native species.

In an effort to preserve the Daintree Rainforest north of the Daintree River it was decided by the Government of Queensland in 1993 to halt the spread of the electricity network north of that point, providing a limit to tourist development.[5]

Protected areas include the following:

Homevale National Park Eungella National Park Dryander National Park Conway National Park Whitsunday Islands National Park Paluma Range National Park Halifax Bay Wetlands National Park

Hinchinbrook Island National Park Girringun National Park Edmund Kennedy National Park Hull River National Park Kurrimine Beach National Park Eubenangee Swamp National Park

Ella Bay National Park Wooroonooran National Park Barron Gorge National Park Daintree National Park Cedar Bay National Park Black Mountain National Park

Tourism

View from the Skyrail Rainforest Cableway, 2004

The forests, together with the Great Barrier Reef, have been identified and promoted as a major tourist attraction of Tropical North Queensland, one of five within the state.[6] One of the most significant tourist attractions in the rain forests is the Skyrail Rainforest Cableway.

See also

• Wet Tropics of Queensland

External links

• "Queensland tropical rain forests". Terrestrial Ecoregions. World Wildlife Fund.

References

1. Eric Dinerstein, David Olson, et al. (2017). An Ecoregion-Based Approach to Protecting Half the Terrestrial Realm, BioScience, Volume 67, Issue 6, June 2017, Pages 534–545; Supplemental material 2 table S1b.
2. "Queensland tropical rain forests". Terrestrial Ecoregions. World Wildlife Fund. Retrieved 2 December 2012.
3. McDonald, Geoff; Marcus B. Lane (2000). Securing the Wet Tropics?: A Retrospective on Managing Australia's Tropical Rainforests. Federation Press. p. 14. ISBN 1862873496. Retrieved 3 December 2012.
4. Champion, Neil (2006). Tropical Rain Forests. Black Rabbit Books. p. 18. ISBN 1583405089. Retrieved 2 December 2012.
5. Sharma, K. (2004). Tourism & Economic Development. Sarup & Sons. p. 330. ISBN 8176254967. Retrieved 2 December 2012.
6. Sharma, K. K. (2004). World Tourism Today. Sarup & Sons. p. 172. ISBN 8176255122. Retrieved 2 December 2012.