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The emergent layer contains a small number of very large trees called emergents, which grow above the general canopy, reaching heights of 45–55 m, although on occasion a few species will grow to 70–80 m tall. [21] [22] They need to be able to withstand the hot temperatures and strong winds that occur above the canopy in some areas.
The environmental impact of deep sea mining is controversial. [39] [40] Environmental advocacy groups such as Greenpeace and the Deep Sea Mining Campaign [41] claimed that seabed mining has the potential to damage deep sea ecosystems and spread pollution from heavy metal-laden plumes. [42] Critics have called for moratoria [43] [44] or ...
The structure of a tropical rainforest is stratified into layers, each hosting unique ecosystems. These include the emergent layer with towering trees, the densely populated canopy layer, the understory layer rich in wildlife, and the forest floor, which is sparse due to low light penetration. The soil is characteristically nutrient-poor and ...
Panorama of the rainforest, 2013 16°12′S 145°24′E / 16.2°S 145.4°E / -16.2; The Daintree Rainforest , also known as the Daintree , is a region on the northeastern coast of Queensland , Australia, about 105 km (65 mi), by road, north of the city of Cairns .
The Amazon rainforest, [a] also called Amazon jungle or Amazonia, is a moist broadleaf tropical rainforest in the Amazon biome that covers most of the Amazon basin of South America. This basin encompasses 7,000,000 km 2 (2,700,000 sq mi), [2] of which 6,000,000 km 2 (2,300,000 sq mi) are covered by the rainforest. [3]
[specify] The rainforest is also home to animals such as the Honduran white bat and the common chunk-headed snake (Imantodes cenchoa). The common chunk-headed snake is also called the blunthead snake. It tree-dwelling. Although slightly venomous, the venom is mostly restricted the back teeth to aid the tree snake in eating prey such as small ...
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The soil generally contains a thin but very fertile layer of humus dropped from plants and animals in the forest above, followed by an infertile second layer due to rapid leaching caused by high rainfall. The third level, weathered bedrock, is common to almost all soil types.