Biophysical Interactions
The biophysical interactions of kelp forest ecosystems include the -
- dynamics of weather and climate,
- geomorphic and hydrologic processes such as earth movements, weathering, erosion, transport and deposition and soil formation,
- biogeographical processes: invasion, succession, modification and resilience,
- adjustments in response to natural stress - vulnerability and resilience.
Biophysical interactions between the atmosphere, biosphere, hydrosphere and lithosphere.
Complex interactions between the atmosphere, biosphere, hydrosphere and lithosphere create and maintain kelp forest ecosystems. Natural processes create change and modification in kelp forests and at times, these ecosystems are resilient to natural change.
Biogeographical processes such as invasion, modification and succession are evident in the growth and decline of kelp forests. Due to the size and complexity of human impacts some kelp ecosystems have disappeared in some parts of the world, including along the east coast of Australia.
The kelp forests along the east coast of Australia are significant to the functioning of the marine environment and are valuable to the Australian economy.
Kelp forests provide
a source of food and habitat for many fish, shellfish and invertebrates
a nursery function for juvenile fish and other species
support for the fishing and seafood industry
support for ecotourism and recreational activities such as scuba diving
and along with other macro-algae and algae produce between 50-70 per cent of earth's oxygen and absorb about 25% of earth's carbon dioxide.
Forests of the Sea - animation - captions included I YouTube I Linchpin I 5:58 https://www.youtube.com/watch?v=UhM6QKGZd_s
The role of the BIOSPHERE
All plant and animal species living in kelp forests make up the biosphere of this ecosystem. These elements are a significant part of the biotic environment and are essential to the existence of kelp forests.
In the kelp forests of the Great Southern Reef (GSR), scientists recognise the high levels of biodiversity and endemism, for example,
“What makes the Great Southern Reef such a distinctive ecosystem is that not only is it incredibly biodiverse, but a high proportion of the species it hosts are found nowhere else on earth” - Stefan Andrews, Ocean Imaging Director and Science Communicator and
The GSR is also a global biodiversity hotspot for bryozoans, chordates, crustaceans, echinoderms, molluscs and sponges. Scientists estimate that between 20–60% of all species are endemic to the GSR.
Read and watch the 'storymap' on the GSR and read the article.
"Kelp forests contain a diversity of marine species on the seafloor, in the understorey and throughout the water column including fish, molluscs (sea snails), bryozoans (lace corals), polychaetes (worms), crustaceans (crabs, isopods, amphipods), echinoderms (sea urchins, sea stars) and sponge." Read more in DPI Macroalgae fact sheet
Figure 11 outlines the important producer and consumer groups and the trophic levels in a kelp forest ecosystem.
Kelp is key to the operation of this ecosystem as kelp produces large amounts of biomass, and supplies food and energy to the entire system.
Kelp forests are also important in recycling nutrients as all parts of the kelp plant absorb nutrients directly from the seawater. When kelp plants lose their grip on the hard subsurface they begin to die and decompose. Many of the microscopic decomposers produce nutrients for kelp and other species like sponges and bryozoans to absorb and consume.
Kelp plants can be considered a keystone species because the whole ecosystem is dependent on kelp being present, and the ecosystem collapses without this species. Scientists have also described kelp as an 'ecosystem engineer' that is, kelp actually builds the ecosystem and creates habitat for species such as marine mammals, fish and invertebrates by providing a source of food and shelter.
Kelp creates habitat by influencing the abiotic and biotic aspects of the environment. Some examples of what kelp does for the ecosystem are -
it oxygenates the water
it absorbs carbon dioxide
it recycles nutrients
it traps and stabilises sediments
it provides a nursery for young plants and fish by reducing water flow and reducing the amount of sunlight which reaches the sea floor.
Figure 10 shows how a kelp forest ecosystem in California functions when sea otters are present and when they are not. The symbiotic relationship between kelp plants and sea otters, is known as mutualism.
In this type of ecological relationship both species depend on each other and benefit each other. Kelp plants need sea otters to eat black urchins. If there are too many black urchins grazing on kelp plants, the kelp forest can completely disappear or be replaced by a much less diverse ecosystem called a turf bed. The sea otter needs the kelp forest as a place for protection during strong currents and a place to find food.
In south east Australia, rock lobsters are the natural predator of urchins. However, the reduction of the population of southern rock lobsters through overfishing, has meant that spiny urchins have been able to invade, modify and overtake the kelp forests of some parts of Victoria and north east Tasmania.
This process is also happening in Victoria Read and watch the video clip. Included is a short news clip uploaded onto Facebook, showing a tv reporter visiting a scientist in Port Phillip Bay.
Black urchins are native to the kelp forests of NSW. Black urchins have not caused the same overgrazing in NSW kelp forests as they have in Tasmania and Victoria.
The kelp forests in NSW seem to be resilient to most changes in the size and density of black urchins as natural predators still exist to keep the population of urchins in check.
Biogeographical processes
The processes of invasion, modification and succession are important biogeographical processes that can be illustrated by examining the effects of invasive spiny urchins on kelp forest ecosystems.
Invasion
In all three locations, California, north-east Tasmania and Victoria, the impacts of the black urchin could be considered an example of a biogeographical process known as invasion.
Invasion refers to when a species is not native to an area but establishes itself and dominates another area or ecosystem. Biological invasions usually have multiple negative effects on ecosystems, usually disrupt the interactions between species and can often impact the whole ecosystem.
(REFER to the section
Human impacts - positive and negative
to know more about this process.)
Modification and Succession
Modification and succession are also biogeographical processes which are evident in kelp forests.
Modification refers to to the changes which take place in an ecosystem after an increase or decrease in a species occurs, or after a new species is introduced.
Some kelp forests in south east Australia have undergone the process of modification due to the impacts of 'tropicalisation.' These kelp forests have also experienced the process of invasion due to the arrival of the spiny urchins which often follow 'tropicalisation'.
The process of 'tropicalisation' refers to the introduction of a number of tropical species to temperate kelp forests. Over the last ten years, the East Australian current has carried species such as spiny urchins further south, as far as north east Tasmania. The spiny urchins consume kelp and algae on the rocky reefs. This creates an 'urchin barren'.
Succession refers to the process of ecological succession, whereby ecosystems regenerate in a structured way after a disturbance. There are two types of ecological succession - primary and secondary. Primary succession occurs over a long period of time for example after a volcanic eruption.
Secondary succession occurs if an ecosystem recovers and re-establishes after a natural disturbance or event. For example, kelp forests can usually regrow after storm damage.
Some kelp forests along the NSW coast have undergone the process of secondary succession after human induced disturbance. Succession has been 'kick-started' and managed by scientists so that kelp forests can regenerate by themselves.
Watch the video and interviews with scientists Dr Verges and Dr Marzinelli - here they explain the complexities of kelp ecosystems, human interactions, tropicalisation and a restoration project called 'Operation Crayweed' .
Refer to the section
Human impacts - positive and negative to learn more about modification, invasion, 'tropicalisation' and restoration.
What is the difference between plants and algae?
Algae and macro-algae (seaweed) are primitive aquatic plants that photosynthesise, that is, they take in the sun's energy and create carbohydrates and oxygen.
However, unlike land plants, algae do not have roots and they do not take in any nutrients from the sea floor. Algae do not have veins or flowers and pollen like land based plants do. Macro-algae obtain all of their nutrients from the water.
From the DPI Macroalgae fact sheet by the Principal Research scientist, Royal Botanic Gardens Sydney.
Concepts and definitions
Biomass, keystone species, abundance, mutualism, predation, competition, succession, symbiotic relationship.
Biodiversity - refers to both the variety of species and how many of each species occurring in the ecosystem.
Endemism - refers to when a species is native to an area or place, and not found anywhere else.
Activities
Watch the 'storymap' on the GSR presentation and video and make a list of the animals and plants named. The quote to the left gives you a hint of what to look out for.
Define predation. Use figure 10 or the Great southern reef photos below to list two examples of a predator and prey in a kelp forest ecosystem.
Define competition. Watch YouTube ' A line in the sand or the photos above to list two examples of two species competing with each other to consume the same food.
Refer to the 'storymap' Mission Blue Why was the GSR listed as a Mission Blue Hope Spot?
Source: Brumbaugh
Figure 11: the pyramid shows the trophic levels of the marine ecosystem, with kelp as the primary producer.
Source: www.sciencelearn.org.nz
Figure 12: shows Kelp growing on a rocky reef and black urchins present.
Source: John Turnbull www.marineexplorer.org
Activities
6. Define the following terms keystone species, abundance, symbiotic relationship, mutualism, and succession.
7. Watch the news-clip from channel 9 - Victoria and describe how the scientist measures the 'abundance' of urchins.
8. Watch the Youtube clip called 'Forests of the sea' made by lynchpin
and explain how the symbiotic relationship between kelp and lobster can be considered an example of 'mutualism'.
9. From the same YouTube describe the modifications to the kelp forest ecosystem as a result of an increase in spiny urchins in eastern Tasmania.
10. Outline at least one interaction between the biosphere and each of the three other 'spheres'.
'A line in the sand' - The Australian Sea Lion I YouTube I 12:37 I Department for Environment and Water (SA) . Transcript
Adjustments in response to natural stress
When thinking about how kelp ecosystems respond to natural stress the concepts of vulnerability and resilience have to be considered.
After storms and flooding events, kelp forests are often severely damaged, with a heavy loss in the numbers of kelp plants. This can be observed in the amount of seaweed washed up on the beach (known as 'wrack').
However, in the past, rapid recovery of the kelp forest has occurred because
each kelp plant has a fast individual growth rate. Kelp are known to have some of the fastest growth rates of any primary producer in any ecosystem.
There is 'frequent recruitment' of young kelp, which means that young kelp plants are usually successful in growing to maturity and becoming part of the kelp forest. This occurs partly, because young kelp plants grow close to, and are therefore protected by, the female kelp plant.
When an ecosystem re- establishes itself after natural stresses, it is considered to be 'resilient'. Kelp ecosystems can be considered to be highly resilient to normal storm damage especially when the conditions needed for its growth eg, ocean temperatures, water quality are in the normal to optimal range.
Some of the kelp forests in NSW seem to be resilient to most changes in the size and density of black urchins as natural predators still exist to keep the population of urchins in check. Scientists recognise that there is a 'boom and bust' cycle between urchin barrens and kelp forests across the world and in many places it is a natural cycle based upon the change in numbers of the primary herbivore, eg, tropical fish.
However, the resilience of kelp forests is much lower to other changes in the abiotic environment such as, water quality and ocean temperatures.
Kelp forests are vulnerable, and have low resilience to an increase in sea temperatures. Modifications to the ecosystem have occurred due to this human stress.
Read more below in 'The hydrosphere' section and in the section Human impacts - positive and negative
The role of the HYDROSPHERE
Elements of the hydrosphere including ocean currents, ocean temperature, water quality, tides and waves provide the conditions for kelp forests to establish and thrive. These elements are part of the abiotic environment and are extremely important to the survival of kelp forests.
Some requirements and preferences of kelp forests include -
cooler ocean water of less than 20 degrees celsius, on average
cool ocean waters often contain nutrient upwellings which assists growth
normal ocean salinity levels
normal seawater chemistry, including normal ocean water pH of approximately 8.2
ocean water quality, including turbidity, should be at least at moderate levels. Kelp are negatively affected when there is polluted water eg, with sewage or sediments.
Shallow water is preferred - Most kelp grow to a depth of up to 30 metres and most kelp grow below the low tide level.
Hydrological Processes
Normal hydrological processes such as ocean currents, flooding or storm waves with high energy impact kelp forests.
Storms create waves with high energy which can damage the holdfasts of kelp plants. A healthy kelp forest can regrow and show resilience to this type of natural stress.
Often storms also produce high levels of precipitation and flooding. Rain, stormwater and floodwaters can erode soil and carry sediment into coastal rivers, bays and seas. Sediment can be deposited and smother kelp plants reducing its ability to photosynthesise.
Ocean currents are a significant element of the hydrosphere and are important because they distribute heat around the globe. Ocean currents generally travel horizontally and are not dependent on tidal flows.
See figure 13 which shows the major ocean currents which flow around Australia.
A more detailed map of ocean currents can be seen in the State of the Environment map.
Biogeographical processes
Modification
The process of modification can be seen in the way both water quality and rising ocean temperatures negatively impact kelp forests. Both of these elements are important aspects of the hydrosphere.
- Water quality
Polluted sewage water which flowed from Sydney's sewerage system directly onto the coast up until the 1990's shows how flows in the hydrosphere can affect kelp forests.
Two large sewage treatment plants in Sydney's east and at north - east discharged primary treated sewage through a short pipeline close to Sydney's coastline. There was substantial community concern and protests about coastal water quality during this time.
Ultimately a long term solution was developed which transported the sewage through a much longer pipeline, called the ocean outfall pipeline system. Unfortunately, kelp forests were affected by the poor water quality and much of the kelp died. The impact on Sydney's kelp forest went unnoticed until researchers such Coleman, Verges and Marzinelli measured the impact around 2003.
Much of the kelp forest was modified ( it disappeared) due to the impact of this threat. That is, the kelp forest did not grow back after water quality problems were fixed in the 1990's. So geographers can conclude that the kelp forest had low resilience and was highly vulnerable to threats.
Refer to the section Human impacts - positive and negative to learn more about the disappearance of Sydney's kelp forests.
- Rising ocean temperatures
Ocean currents have an important role in distributing heat around the globe. However, the changing climate has changed some ocean currents like the the Eastern Australian Current (EAC), see figure 13 for its location.
How has the EAC affected kelp forests?
Scientists recognise that as ocean temperatures have risen, the EAC has become stronger and now flows a lot further south than before. The warmer waters of the EAC have impacted kelp forests along NSW coasts eg, near the Solitary islands and even the kelp forests of Tasmania.
The warmer waters bring with them other species eg, tropical fish and urchins which feed off the kelp until there is no kelp left. This process is known as 'tropicalisation' and it leads to a significantly modified ecosystem.
Read more in the previous section on the Biosphere and in the section on
What is the East Australian Current? I YouTube I ABC I 3:57 Transcript
https://www.youtube.com/watch?v=zstqK7dCdyU
Figure 13: shows map of Ocean currents which operate in Australian oceans and seas.
Source: Copyright Marine Science Australia 2012 All rights reserved.
Concepts and definitions
Hydrological processes, ocean currents, sewage, sewerage, photosynthesis, sediment.
Australia's ocean odyssey: A journey down the East Australian current I Official trailerI ABC I YouTube I2:40
https://www.youtube.com/watch?v=ulNOSK2YE7Q
Activities
Draw a simple diagram of the water cycle and include ocean currents and river flows in this diagram.
Explain the difference between the sewerage system and the stormwater system. Simply explain how each system impacts the hydrosphere and kelp forests?
Watch the Youtube videos - What is the East Australian current ?
and the Official trailer of Ocean Odyssey
From these videos, describe the location of the EAC and discuss the importance of the EAC and ocean currents on weather, climate and ecosystems.
Research why ocean levels are rising. Read the article from scientists at the 'Australian Academy of Science'. Refer to the importance of thermal expansion, loss of ice from glaciers, and surface melt from the Greenland ice melt.
Describe one link between the hydrosphere and each of the other 'spheres'.
The role of the ATMOSPHERE
Figure 13: Sunlight reaching a kelp forest
Source: John Turnbull www.marineexplorer.org
The role of the ATMOSPHERE
The role of the atmosphere can be seen in the way
weather and climate influence the growth of kelp forests.
that kelp forests are important in the earth's carbon and oxygen cycles
Temperature and access to sunlight are two elements of the atmosphere, weather and climate, which are important in creating conditions for the optimal growth of kelp forests. These elements are a significant part of the abiotic environment and are extremely important in the survival of kelp forests.
Two climatic aspects of the atmosphere which affect the growth of kelp forests are:
Kelp requires cooler waters to thrive. Kelp can grow in waters which reach up to 26 degrees celsius, but most kelp requires the average annual ocean temperature to be less than 20 degrees Celsius. Atmospheric conditions such as storms, prevailing winds and ocean currents all affect ocean temperature, which in turn impacts kelp forest ecosystems.
Kelp usually attaches its holdfast on the sea floor, (the benthic zone), however kelp grows so that it can reach sunlight.
The zone where sunlight reaches is called the photic zone. Kelp uses sunlight to photosynthesise. That is, kelp plants take in the sun's energy and create carbohydrates and oxygen. The kelp forests of south- eastern Australia grow in the temperate latitudes where air temperatures are not tropical or polar, but cool to warm. Global warming and changing climatic conditions have altered the prevailing seasonal average temperatures which have affected ocean temperatures, which in turn, have impacted kelp forest ecosystems.
The kelp forests of south eastern Australia are regularly affected by winter storms. The strong, often southerly winds produce high levels of wave energy. Strong waves often rip and dislodge the holdfasts so that kelp breaks away and is carried onto shore. In most cases kelp forests can adapt to this natural stress. This is called resilience. A healthy kelp forest has kelp plants which will reproduce and repopulate the patches in the kelp forests.
Kelp forests are integral to the functioning of the carbon and oxygen cycles of earth. Kelp along with other macro-algae and micro-algae produce up to 70 per cent of the earth's oxygen. Kelp forests are extremely important in the earth's oxygen cycle and the survival of all marine and terrestrial ecosystems.
Kelp plants absorbs carbon dioxide during the process of photosynthesis. Kelp plants actually remove carbon dioxide from the oceans and kelp forests are known as 'carbon sinks.' Kelp forests have been found to absorb approximately 25 per cent of the earth's carbon dioxide.
Some carbon dioxide when it reaches the ocean actually dissolves and forms carbonic acid. This is why oceans are becoming acidic. The process is known as ocean acidification. Many animals with shells, like lobsters and abalone that are part of the kelp forest ecosystem are affected by this process.
Unfortunately acidic ocean water prevents these animals from absorbing calcium carbonate, which is the basis of their shells. Scientists have found the shells of some young lobsters to be much thinner, with consequently poor survival rates. The Australian government recognised the risk of ocean acidification to rocky reefs and their ecosystems in this document.
Figure 14 : View of the ocean
Source: John Turnbull www.marineexplorer.org
Concepts and definitions
carbon cycle, oxygen cycle, benthic zone, pelagic zone, photic zone, photosynthesise, global warming, carbon sink, sequestration, ocean acidification.
Figure 16: The role of kelp in the carbon cycle
Activities
Describe how latitude affects the temperature of the ocean and influences the location of kelp forests.
Outline two ways a cold, southerly storm might affect the kelp forest ecosystems off the NSW south coast.
Describe how a storm could be considered a natural stress to a kelp plant.
Discuss the role of kelp in the carbon and oxygen cycles.
Explain how kelp can sequester (absorb) carbon dioxide.
Explain how the process of ocean acidification operates and its impact on kelp forest ecosystems.
Outline at least one interaction between the atmosphere and each of the three other 'spheres'.
The role of the LITHOSPHERE
The essential role of the lithosphere can be seen in the way that rocky reefs and rock platforms are fundamental to the survival of kelp plants.
Kelp forests of south east Australia grow on the rocky reefs which are found along the coastline. The rocky reefs are part of the lithosphere and provide the foundation for kelp forests to establish and thrive. These elements are a significant part of the abiotic environment and are extremely important in the survival of kelp forests.
The Department of Primary Industries (DPI) in NSW recognises the importance of rocky reefs. DPI states -
"Rocky reefs refers to all areas of rocky outcrops or boulders occurring within marine and estuarine waters below the highest astronomical tide level. Macroalgae and invertebrates contribute to the physical structure of rocky reef habitats and are therefore considered part of these habitats."
The recent recognition of the Great Southern Reef recognises the chain of rocky reefs and kelp habitats which continue for 8000km along the south east, eastern, southern and south western coastlines of Australia.
All kelp plants have a holdfast which act like tree roots in attaching the kelp to a hard surface. The rocky reefs create hard surfaces of different heights for kelp to attach to and hard surfaces which are closer to the surface of the water, thus improving access to sunlight for kelp plants.
Rocky reefs support thousands of kilometres of kelp forests which in turn provide food, shelter and refuge for a wide variety of species. Small fish can escape predators among caves and crevices, while carnivorous species, such as black cod and bream, can use the rocky habitat to find prey. Rocky reefs are a significant part of the habitat that kelp forests provide to invertebrates, fish and marine mammals. Scientists describe these habitats and communities as complex benthic habitats and complex benthic communities.
Geomorphological processes
The Marine Education Society of Australasia (MESA) note that rocky reefs are found where rocks occur above or below the waterline. The rocks are eroded by the action of water and waves and cracks and holes appear which may decrease the surface area available for kelp and increase the availability of shelter for living things.
Geomorphological processes include the processes which shape and change the earth's surface, including its seafloor. All processes which create landforms such as beaches, headlands, bays and rocky reefs are geomorphological processes.
Geomorphological processes can be broken up into three categories and include
weathering - this involves the breaking down and breaking up of the lithosphere and includes both physical and chemical processes.
On the coast, an example of a physical process includes the physical force of waves which break up rocks and headlands. An example of a chemical process includes the action of saltwater in breaking down particles in a rock pool.
erosion - this involves the transportation of weathered materials by wind and water. An example of water erosion is the action of waves which move weathered rock from a headland to a rocky reef off the coast.
deposition processes include the processes whereby material is deposited (or dropped) by water and wind. An example on the coast is the movement of waves and currents which deposit sand and create a beach.
Different types of rock influence the way the rocky reef is weathered and eroded. Some rocks like basalt are weathered by waves more easily than rocks such as sandstone. When this happens the crevices and cracks are larger and provide shelter and refuge and may support more fish and mobile animals such as the Pacific octopus.
Sandstone on the other hand may be weathered more slowly by the action of waves and currents and become undercut with crevices worn into it. The surfaces of sandstone reefs often teem with sponges, urchins and anemones. For more information read Living on the edge, Geoscience Australia
Surrounding the mainland is an extension of the landmass known as the continental shelf. This shelf is relatively shallow, up to 200 metres deep, compared to the open ocean which can be thousands of metres deep. This shelf extends outward to the continental slope where the deep ocean begins.
Kelp forests grow on the rocky reefs found on the shallower part of the continental shelf. As the water gets deeper, kelp cannot survive and the crevices and surfaces of the continental shelf become covered with many species of sponges and soft corals.
The rocky reefs which make up the Great Southern Reef have experienced relatively stable climatic and geological conditions over the past 50 million years. This stability is thought to explain its high biodiversity and endemism.
Most of the landforms and marine reefs that comprise the Australian coast were caused by the Gondwana break up in the Cretaceous era and Paleogene era (155 million years ago and 34 million years ago). The Australian coast and continental shelf have not changed much since the formation of the island continent because there has been little tectonic activity or large scale erosion to change the coastal margins, especially in the southern part of Australia.
Paleoshoreline data complied by 'Geoscience Australia' suggests that continental plate activity has created a southern mainland shoreline which is uplifting at a modest rate each year whilst the northern edge of the mainland is actually subsiding near the northern subduction zone. For more information, read Living on the edge, Geoscience Australia
Scientists also recognise how the diverse rocky reef ecosystems affect the other parts of the lithosphere on the sea floor. Scientists such as Dr Cayne Layton explains how kelp forests and rocky reef communities act as the trophic foundation of food-webs by providing food for a suite of grazers, detritivores, (species that consume decaying matter like echinoderms) and microbes. The effects can reach the adjacent seagrass and soft sediment communities, ie, the species that live in the sandy or muddy sea floor.
Weathering and erosion of soil and sand on land is transported by rivers and currents in estuaries to the marine environment. When run-off from land holds too much sediment and ends up in a body of water, the water can become turbid. When floodwaters or large volumes of stormwater enter the ocean the sediment load can be high and can cause temporary damage to kelp forests.
In a normal functioning kelp forest ecosystem, kelp can adjust to this natural stress and regrow. However, high levels of turbidity may affect kelp forests because kelp plants need sunlight to photosynthesise. As well, the small particulates may interfere with the small cells involved in reproduction. If seawater becomes turbid then kelp forests may reduce in size or density. Scientists such as Dr Cayne Layton states that this is why the kelp forest made up of 'Ecklonia radiata' off the coast of Adelaide changed to an 'algal turf bed' - with a different species, size and density of kelp. See the photos shown in the Activities section.
Figure 17: shows a rock platform with kelp growing in the intertidal zone.
Source: John Turnbull www.marineexplorer.org
Concepts and definitions
geomorphological processes, temperate rocky reefs, benthic, continental shelf, turbidity, weathering, erosion, deposition, endemism.
Figure 18: Seabed habitats and depth of sea bed off the coast of Sydney.
Source: OEH environment.nsw seabed mapping
Activities
Soil, sediments and sand are part of the lithosphere. Outline the processes that transport them into the seas and oceans.
Use figure 18 to describe the depth and features of the seafloor off the coast of Sydney.
Consult one of the data rich 'e maps' such as environment.nsw seabed mapping , eAtlas , The NationalMap or the seed map .
Choose a location, eg, Towra Point, Botany Bay or a location that you know, and go to 'Marine environment' and view maps such as bathymetry, high tide and low tide satellite images.
Outline what bathymetry refers to and how it links to rocky reefs and the location of kelp forests.
Outline one interaction between the lithosphere of the kelp forest ecosystems and each of the other three spheres.
Extended response
Discuss the biophysical interactions operating in kelp forest ecosystems. In your answer refer to biogeographical, geomorphological and hydrological processes.
Investigating biophysical interactions through fieldwork
Fieldwork is an essential component of geography. It provides students an experience of active research when investigating geographical phenomena.
Complete the following activities to guide fieldwork in the investigation of kelp forest characteristics, functioning and interactions.
Key fieldwork inquiry questions:
How do the four components of the biophysical environment interact to form a kelp forest ecosystem?
What fieldwork methodologies and equipment can be used to investigate kelp forest ecosystems? Will your investigation be primarily land based ?
How will your results be recorded?
How do we draw conclusions?
For further assistance in conducting fieldwork contact:
NSW Department of Education Environmental and Zoo Education Centres
Sydney Institute of Marine Science SIMS
Pre-work
Prior to fieldwork identify the location of your kelp forest ecosystem using digital maps.
Access Six Maps to view aerial maps. These maps will provide opportunities to locate your site and estimate the size of your fieldwork site.
Access Atlas of Living Australia or ReefLifeSurvey to view the distribution of kelp species such as 'Ecklonia radiata' and 'Phyllospora comosa'.
Compare the distribution of these kelp species to name the kelp species at your fieldwork location.
Compare these maps with either Six Maps or eAtlas or The NationalMap ( Look under 'Map - Australian topography map' or Map - 3 -d terrain ) to determine the location of the continental shelf, the rocky reefs, rock platforms and the depth of the ocean (bathymetry). Outline the effect that ocean depth has on the location of kelp forest ecosystems.
Access weather and climate information from the Bureau of Meteorology.
Explain how the location is influenced by latitude, ocean depth and bathymetry.
Read and view the video from biology online to view two methods (methodologies ) which demonstrate how to use quadrats and transects to collect data collection in the field.
Figure 19 : choose a safe site to investigate the elements of a kelp forest ecosystem.
Source: Observatory Hill EEC
Measuring abiotic factors
Abiotic factors are important to measure as they are the primary determinant of species abundance and distribution. In kelp forest ecosystems, the interactions within the atmosphere, hydrosphere, biosphere and lithosphere that occur lead to its unique character. The maintenance of optimal conditions such as water temperature, water quality and water depth are essential for proper functioning.
To investigate the nature and functioning of kelp forest ecosystems measure the abiotic factors in and near a kelp forest.
Your fieldwork site should be chosen so that you can measure and record abiotic factors safely.
View the gallery of images to identify the equipment and methodologies used to measure and record abiotic factors.
Use the gallery of images and categorise techniques and data according atmosphere, biosphere, hydrosphere and lithosphere.
What does figure 19 suggest about recent atmospheric conditions at this beach ?
Predict the differences between the abiotic factors in a healthy kelp forest and one which is degraded or one which has almost disappeared.
Figure 20 : Carousel photos show common equipment and methodologies used to measure abiotic factors.
Source : NPS California, World Water Monitoring Challenge, ReefLifeSurvey and Observatory Hill EEC.
Figure 20a : Small seaweed bed in Sydney harbour.
Source : Observatory Hill EEC.
Measuring biotic factors
The living components within an ecosystem all interact and play an important role in shaping the environment.
An investigation of the size of the kelp forest and its composition informs an understanding of the nature of the ecosystem. The interactions between species explains the proper functioning of the system. Land managers and scientists are able to determine kelp forest resilience and stress by measuring and recording biotic factors.
View the gallery of images to describe the methodologies used to measure and record biotic factors.
Whys are identification charts, books or Apps required in ecosystem fieldwork ?
Identify secondary sources that support biotic investigations in the field.
Explain how fieldwork informs our understanding of ecosystem functioning. In your answer refer to kelp forest productivity, ecosystem engineers and energy flows.
Explain the importance of ethical fieldwork practices.
Read more about fieldwork techniques in Traditional and contemporary management practices
Figure 20b : Carousel photos show elements of a kelp ecosystem and common equipment and methodologies used to measure biotic factors.
Source : ReefLifeSurvey, Mosman Council, UTS, theconversation.com and Observatory Hill EEC.