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Natural processes of coastal environment
Coastal environments being affected by human activities
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Queensland coastal dunes are an integral part of coastal environment and ecosystems. Queensland beaches are known for a number of its natural icons and prominent features and are widely recognized and appreciated for their breath taking scenery, significant biodiversity, recreation experiences and generation of economic benefits from tourism. With the influx of human influence with beachfront development, mowing and topsoiling dunes, pedestrian and vehicular traffic, weeds and feral animals disturbing the native ecological communities, leads to the destruction of delicate sand dunes creating more damaging problems such as erosion. (reference)
Point cartwright is located on the coast of south east Queensland and stretches 100m. It has a diverse environments such as sand
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dunes and rocky shores that are important for the life of all its inhabitants. Sand dunes are formed through the combination of waves and wind patterns which causes sand to build up. These areas support and sustain plant and animal life and is vital in maintaining a healthy coast line. Stable sand dunes play a dynamic part in protecting the coastline.
They act as a shield against wave damage throughout storms, protecting the land behind from salt water intrusion. This sand barrier allows the growth of more complex plant communities in areas protected from salt water inundation, sea spray and strong winds. Communities of plants that grow on beaches and dunes are known as dune vegetation.
The ecology of these ecosystems plays a key role in mediating many of the functions of dunes, including their growth and stabilization. Similarly, the physical environment of this unique habitat strongly shapes the ecology of the organisms living there.
- explain abiotic changes that happen along a gradient and how do species change as a result.
Zonation is the categorization of biomes into zones based on their distribution or arrangement in a habitat as determined by environmental factors, e.g. altitude, latitude, temperature, other biotic factors, etc. (Collins English Dictionary, n.d.). There are three main zones of dune vegetation that are arranged roughly parallel to the coastline. Closest to the sea is the pioneer zone, extending landward from the debris line at the top of the beach in an area called the foredune or frontal dune as seen in
Table 1. In the pioneer zone of the beach where sediments are covered frequently by water, aquatic organisms thrive. However, in the areas at and just above the high tide zone, conditions are harsh. The lack of water makes life nearly impossible for aquatic or terrestrial organisms, and the dry sand is easy to heat and cool, resulting in strong swings in temperature from too hot to bitterly cold during winter (sunshine coast council, 2016. Foredune or frontal dune areas are more protected from wind, blowing sand and salt spray and this results in increased nutrients and moisture available for plant growth. Such species observed include spinifex (Spinifex sericeus), pig face (Carpobrotus glaucescens) and goat's foot convolvulus (Ipomoea pes-caprae). Weeping horsetail sheoaks (Casuarina equisetifolia) and screw pines (Pandanus tectorius) are common tree species found along the coast and were observed at the point cartwright transect (seen in table 2). All these plants have specialised characteristics that allow them to cope with the extreme conditions as seen in table 4, they have adaptations such as waxy and/or hairy coverings on their stems and leaves, narrow leaves, succulent leaves, extensive and vigorous root systems or other such traits that allow them to cope with little water and nutrients and lots of wind and salt. The array and health of plant life is vital in the strength of food chains and animals in a coastal ecosystem providing shelter and food for surrounding organisms. Organisms living in this zone must have a high tolerance for being blasted with and buried by the constantly moving sand, lack of nutrients and high salinity levels (removal, 2016) . As seen in Table 3 there was a variety of organisms that were observed in the point cartwright dunes such as ghost crabs, ants and grasshoppers.
There are many things working together to ensure Dune stabilization. These include; re-vegetation, fences, poly-mesh fencing, planked walkways, and controlled pedestrian access. This method is a softer option than the rip-rap wall and is used because human land-use, which at this place consists mainly of recreational buildings, is far away from the ocean. Deposition is also being managed at North Cronulla beach. Dune stabilization is being used to prevent deposited material from being eroded away.
Government of South Australia, 2005. Adelaide's Living Beaches. A Strategy for 2005 - 2025, December, pp. 5-27.
We saw that there was vegetation, which had been planted on the sand dunes near Dunwich Heath. There is also fencing around the dunes to stop them being eroded through people walking on them. Coastal Protection At Aldeburgh Text Box: Fig 4.1Text Box: In Aldeburgh however, the types of protection involve 'hard' protection. These are man-made objects. At Aldeburgh, three hard protection methods have been employed, and one soft method.
Purpose: The purpose of this lab is to investigate the various components of different ecosystems in a smaller representation and study the conditions required for the ecosystem’s sustainability as well as the connections between
There are many different types of coasts that exist throughout the United States. The south shore of Long Island has a unique types of coast known as a barrier beach. Barrier beaches are long narrow land forms that are composed of sand and other lose sediments. These sediments are brought together by the actions of waves, currents and storm surges. Barrier beaches are subject to constant changes by the same forces. Sand is constantly eroded in one area an deposited in another. Barrier coasts are important for a number of reasons; they protect the mainland of Long Island from the open ocean and flooding during storms, for recreational use and the unique ecosystems which exist on barrier beaches.
Abiotic factors are things that are nonliving that influence an environment and it's inhabitants. Some of the abiotic factors that are attributed to coastal erosion in Louisiana are hurricanes, tropical storms, elevation, sunlight, overnutrition, sea-level rise, and deposition. Hurricanes bring about larger waves which cause dune erosion or beach erosion (Clark et al., 1998). This is significant because beaches and/or the dunes of the beach serve as buffers to the coastline and the ecosystem. As the beach or dunes recede from the erosion caused by these large waves and an increased sea-level the flora and fauna that help sustain the area die off or retreat to a more habitable zone leaving the wetlands in a critical state often resulting in a total loss of the area (Stockdon et al., 2012). Due to the nature of the Gulf of Mexico large destructive storms such as hurricanes or tropica...
Longshore drift is a process by which sediments are transported from one place to another. When this process occurs, beaches, spits and sandbars are accreted over time. If the process of longshore drift is altered by factors such as stronger winds and stronger currents, beach erosion begins at a faster rate and this may result in many serious problems. The main stakeholders of longshore drift are resort owners. They rely on people to visit their resorts and enjoy the beach. However, if longshore drift erodes t...
Because of farm fertilizer, an excess quantity of nitrogen and phosphorus can be wash down becoming runoff into rivers. From this, marine algal blooms cause the water to turn green from the chlorophyll (Reed, 2011). Eutrophication then becomes a dilemma in the system causing either an increase of primary production or an expansion of algae. An enormous expansion of phytoplankton on the water’s surface is then established. At the same time the water column is also stratified, meaning things such as the temperature and salinity are not sync from top to bottom. The seasonal warm surface water has a low density forming a saltier layer above while the cooler and more dense water masses near the bottom layer is isolated from the top cutting off oxygen supply from the atmosphere (Overview, 2008).
Not only has urban development faced damage from these coastal changes, however by changing coastal stability, development itself has increased erosion. Buildings, roads and homes built too close to the beach have become vulnerable to erosion due to extreme weather conditions. Furthermore, during storms, large waves cause severe erosion to this beach. Consequently, wave patterns change as they are are not naturally rolling onto the beach. Instead, they are smashing against built surfaces/structures (causing more erosion) and then are being violently pushed back.
Leading scientists advise climate change will cause increases to the frequency and intensity of extreme weather events. Rising sea levels pose a significant risk to coastal communities, while the world’s oceans could become too acidic to support coral reefs and other calcifying marine organisms. Coral reefs contain only six per cent of the area of the Great Barrier Reef, yet they provide critical habitat and food for numerous species in the ecosystem. However, climate change has already impacted coral reefs in the Great Barrier Reef as corals are very helpless against its potential impacts. Eight mass coral bleaching events has occurred since 1979, triggered by unusually high water temperatures. And because of this, zooxanthellae (photosynthetic algae) leave their tissues and corals will have no more colours hence ‘bleaching’. Without the zooxanthellae, the corals that remain gradually starve to death. Once the coral dies, fish and a multitude of other marine species are soon affected. Rising sea levels and more frequent and intense storm surges will see more erosion of Australia’s coastline, causing community and residential
The very high zone with a deep slope is found in the south-west part of the quadrangle with UTM coordinates from 4623040 meters to 4629000 meters North, and 342760 meters to 349000 meters East. On the other hand, this zone
The coastal wetlands are very important too. The loss of coastal wetlands are being destroyed twice as fast than they are being restored (“Coastal Wetlands”). Coastal wetlands include bottomland hardwood and mangrove swamps, salt and freshwater marshes, and shrubby depressions that are called “pocosins” mostly found in the southeast part of the United States. Coastal wetlands have many functions. They play a role in flood protection, erosion control, wildlife food and habitat, commercial fisheries, water quality, recreation, and even carbon sequestration (“Coastal Wetlands”). So as you can see, coastal wetlands have many functions just as any other wetland.
in a habitat, changes in climate, the development or destruction of a mountain range, river
In many parts of the world, ecosystems’ temperatures begin to rise and fall to extreme levels making it very difficult for animals and plants to adapt in time to survive. Climate has never been stable here on Earth. Climate is an important environmental influence on ecosystems. Climate changes the impacts of climate change, and affects ecosystems in a variety of ways. For instance, warming could force species to migrate to higher latitudes or higher elevations where temperatures are more conducive to their survival. Similarly, as sea level rises, saltwater intrusion into a freshwater sys...
People from all over the world go to beautiful beaches that are filled with water as clear as ice or as beautiful as diamonds. But, what will happen if we do not conserve the appealing sites that draw attraction to the public? Contaminated beaches has become a controversial issue to the public because of the causal problem, the harm to the people and marine animals, the government agencies supporting or opposing pollution, and the industries involved in creating such unlawful decisions. To create and find a solution, we must first find the core to the problem.