Ecosystems at risk Limestone Caves Map of Yarrangobilly Caves Fieldwork at Yarrangobilly Caves Map of Australia’s Limestone Caves Page | 1 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre General Information Limestone caves areas are known as “Karst” areas. The caves are a Karst system with about 320 known caves in varying stages of development and differing levels of importance. This Karst is 12kms long and 1.6kms across. Each cave has its own ecosystem functioning and are managed accordingly. The cave ecosystem is part of a larger catchment. The ecosystem within each cave is linked to the upper catchment by the flow of water. What happens above the caves will have an effect on the caves themselves. What is Karst? Karst is the name given to limestone cave systems across the world. They are unique ecosystems with some endemic flora and fauna (found nowhere else in the world) Very little Karst can be found in Australia. The Nullabor plain is the largest Karst system in the Southern Hemisphere Caves are a time capsule of past conditions. Studies of cave decorations have been used to determine past climate change Why is this ecosystem at risk/fragile? The cave system is very susceptible to change. Because it is so stable in terms of abiotoc factors (physical features- temperature, rainfall, humidity, light) it cannot withstand change no matter how small. It is always, moist, dark and humid without diurnal (daily) or seasonal variations so everything has evolved without the ability to cope with change Each system is isolated, we say they are “islands in the sky” The nearest system is the Blue Waterholes. Caves system about 30kms away. So if animals and plants cannot travel from one system to another The caves are affected by the happenings in the surrounding area not just within the caves. For example the upper catchment Pine plantation had a big effect on water flow and hence the caves environment Organisms have become very specialised with reduced capacity to withstand change. Page | 2 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Spatial Patterns and Dimensions Using geographical tools and skills collect data for Site Altitude Latitude Longitude Yarrangobilly Village Site/ Wild cave 35 39S 148 28E North Glory Cave 35 43S 148 29E Biophysical Interactions Dynamics of weather and climate Using the data in the graph above tabulate the monthly temperature data for Kiandra and inside the cave at Yarrangobilly. Jan Feb Mar Apr May June July Aug Sep Oct Nov Dec Mean Daily Temperature at Kiandra Mean Daily Temperature inside cave Page | 3 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Biophysical Interactions Using geographical tools and skills collect data for * Air Temperature *Relative Humidity *Light *Soil pH ( at the entrance only) Characteristic Instrument & Unit Air temperature Thermometer 0 C Relative humidity Hygrometer %RH Light Soil pH Entrance Twilight Dark Meter lux Slightly darker at night than daytime Total Darkness 0 Lux Never varies Universal indicator Strongly Alkaline Strongly Alkaline (gained from historical testing) (gained from historical testing) Animals present Evidence Kangaroos, Wallabys, Lizards, Snakes, Birds Cockroaches, Spiders, Springtails, Cave Cricket Translucent spider, Blind beetle, Cave cricket Plant diversity (number) Quadrat Larger diversity, and numbers Moss, Lichen, Liverworts, Algae Low diversity Lampen Flora- artificially lit areas No natural plants *Mildew also Plant height & % cover Quadrat 5-10cm NIL 50-70% coverage NIL As for surrounding bushland- Mainly shrubs at entrance to 3m 100% coverage Page | 4 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Biophysical Interactions Climate differences exhibited between the three ecosystems. Entrance Twilight Dark Diurnal change Minor Nil Seasonal change Minor Nil Minor Nil Minor Nil Annual change The temperature varies as per the outside surrounds. Significant daily and yearly changes. Air Temp change Overview Dark, damp & always humid. Further into the cave the more stable the climate becomes General rule is that the Temperature in a cave is the average yearly temperature of the surrounding area Page | 5 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Biophysical Interactions Geomorphic and hydrologic processes Many landforms develop from the breaking down of rock (weathering), the removal of the weathered material (erosion) and the deposition of the eroded material. Landforms include hills and valleys, floodplains, beaches, karst (limestone areas) and limestone caves. Steps in Cave Development 1. Rain Water falls 2. Carbon dioxide from soil / air dissolves 3. Formation of acid groundwater 4. Limestone is dissolved by acid groundwater chemical weathering) 5. Caves develop 6. If water table drops the cave stops developing 7. Cave decorations (speleothems) begin to form. The deposition of calcite begins the formation of stalactites and stalagmites. Page | 6 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Nature and rate of change which affects ecosystem functioning Describe the general landscape. Karst system surrounded by granite mountainous wet forest Explain how limestone caves form. The area was under the ocean. Coral reefs formed. About 300000 years ago there was uplift by tectonic forces. As rainwater flows over the ground it combines with carbon from the plants forming a Carbonic acid which dissolves the limestone as it flows through small cracks. Over millions of years the cracks form into the caves. Explain how speleothems (cave decorations) form. Flow of water is the key. Water drips off leaving a small ring deposit of calcite. Slowly this calcium builds up to lengthen the decoration. As water drips onto the floor it leaves a buildup of calcite forming the stalactite decorations Stalagmites grow from the floor up from the deposition of calcium carbonate from drops of water landing on the cave floor (below left). Stalactites have formed along joint lines in the limestone where water has seeped through (below right). Page | 7 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Vegetation Entrance Native Trees Grevillia, Bursaria Tea Tree, Hakea Native Grasses Poa Wallaby Introduced Trees Liverworts, Moss, Algae Lichen (50-70% coverage) Lampen Flora (near artificial lights) Buttercup Other Introduced Weeds Dark Mountain Gum Mountain Ash Native Shrubs Native Herbs Twilight St Johns Wart Scotch thistle Elm Pine Caves generally: Plant Biomass is 0.2kg/m2 which is very low (Rainforest is 45kg/m2) There is a lack of sun light for photosynthesis so only a few small, specialised plants survive hence only a small number and type of herbivores can live in the ecosystem Page | 8 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Fauna Entrance Twilight Dark Wallaby Cave Cricket Translucent Spider Wombats Cockroaches Blind Beetle Birds Spiders Cave Cricket Lizards Springtails Snakes Thylacine (Tasmania tiger) fossils indicate previous climatic conditions suited its habitation Blind Harvestman Spider only found in the Harry Wood Cave- endemic very endangered Fauna has unique physiological adaptations to survive in the dark, humid, moist cave environment: Long feelers, multiple long limbs are an advantage. They have lost pigmentation, and have poor or no eyesight. A behavioural adaptation is the Crickets move out to the entrance area to feed at night Very specialised with reduced capacity to withstand change Page | 9 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Human Impacts ( positive and negative) Aboriginal history Yarrangobilly means "Teeth water" Groups travelled through the area on way to mountains for summer Caves would have been used for shelter. Wet & damp not suitable for permanent accommodation. Rough terrain made living here difficult European history Late 1800s first Europeans came to the area and discovered the caves Glory farm- cattle farm set up homestead on Yarrangobilly River Introduced Poplar and Elm trees Trout were introduced to the river from Adaminaby area 1920 cave house was constructed for tourism 1950s prison labour from Cooma was used to develop infrastructure for visitation 1967 NPWS took over management. Discouraged visitation because could not handle the sewerage an wastes- was destroying the system Page | 10 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Human Impacts ( positive and negative) Traditional and Contemporary management practices List of the Human Impacts in this ecosystem Complete the table by listing the inadvertent human effects on this ecosystem and the management practices employed (both traditional and contemporary) Human Impact Impact on the functioning of the ecosystem Management Practices Effectiveness of Management Practices Highway Road Old road construction storage and dump site Quarry- disused Buildings, homestead, sewerage Pine tree plantation Page | 11 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Human Impact Impact on the functioning of the ecosystem Management Practices Effectiveness of Management Practices Land clearing Camp ground / Fire places Toilets-sewerage river into Washing in river- Garbage dumping Feral animals Page | 12 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Traditional and contemporary management practices Upper Catchment Area Maintaining the upper catchment area is very important in caves management. Any change in the water cycle will have an effect on the cave ecosystem. The cave ecosystem relies on the water flowing in to the caves for much of the energy and food supply. Reductions in the amount of water will affect cave development. Replacing native vegetation with pine plantations reduced the water entering the caves. Pines use 17% more water than eucalypts. Pollution has a big impact on water quality. Sources of pollution can be sediment from land clearing, animal faeces, sewerage, road dirt and oil, seepage from garbage tips. Natural Sink holes were used as garbage tips in the past How are the caves and catchment being managed on a sustainable basis? The Yarrangobilly caves are managed by National Parks and Wildlife Service (NPWS) under the Kosciuszko National Park Management Plan. Caves are categorised according to their importance and access is determined accordingly. At Yarrangobilly there are 6 categories of caves, varying from “open to public” to “scientifically significant”. NPWS must manage both the caves and the catchment for the Yarrangobilly Karst system. 25% of revenue generated by tourism to the caves is returned into cave care programs. Water flow is critical to the caves so its management is extremely important. The general belief is that once you allow visitation you sacrifice the cave. However due to historical visitation, there is an obligation to continue visitation into the caves. NPWS have included an education component with guided tours that play a critical role in the ongoing management of this fragile and at risk ecosystem. Pathing has been installed outside cave entrances to help reduce the amount of dirt entering the cave via the feet of visitors. Lighting systems are continually being replaced with automatic energy efficient light system NPWS staff must balance environmental and cultural heritage issues. For this reason they have retained the introduced Elms and Pines. NPWS produce their own Hydropower on site replacing old diesel generators that use to leak oil into river. A new sewerage system (costing $1.5 million) which uses no chemicals was recently installed and it is located on granite site nearby- not on Karst. Local Poa grass uses up nutrients and provides a seed bank for regeneration works. Feral Brumbies are kept away for the caves area with an active trapping and removal program in place. Page | 13 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Cave Tour Notes: Pure Limestone is milky or white Limestone turns into marble when gets volcanic heat Red colour is from iron picked up as water passes over rock with iron in it Black colour is caused by bushfires. Some black staining from early visitors using kerosene lamps Black bands caused by fires used to date age of cave Moonmilk- bacteria reacts with limestone to form white growth Water levels fluctuate Calcite floats on water Straws 6mm in diameter, hollow as water drips off leaves ring of calcite which is new growth. 98% turn into stalactites Bacon water comes from side of cave and runs down wall Bacon grows into Shawl and Shawl grows into Blanket Helicitite turn up and around from roof Column is Stalactite and Stalactite joined 392 Known caves 6 show caves with 5000 visitors per year Jillabenan is most decorated cave in Australia 2 million years old Small cave with limited air flow. Tour groups increase temperature and co2 which speeds up Lampenflora growth. When temperature increases the cave is closed Jersey Cave 1.5 million years old Glory Caves Page | 14 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre 100000 years old Least developed so self-guided tours in South Glory Past Exam Questions & Examiner notes: 2013 HSC Geography Question 25 – Ecosystems at Risk “Assess the human impacts on the functioning of TWO ecosystems at risk” General observations: Almost all students named 2 ecosystems. Many included spatial dimensions ( location, size, etc) The majority of answers were quite detailed Students seem to have found it easy to outline / describe human impacts on ecosystems and managed to include several for each ecosystem Discriminators: Human impacts: These are many and varied and directly relevant to the ecosystems chosen Simplistic coverage of impacts – list human actions eg. Dirt access roads, accommodation & buildings, sewerage pollution, farming, forestry, More comprehensive coverage of impacts; human action effects of action eg. Tourism sacrifice of caves loss of ecosystem Human impacts on the functioning A lot of students didn’t address the term “functioning” Requires a greater depth of knowledge / understanding Explicitly talks about how the actions of humans impacts on the functioning of an ecosystem Functioning = energy flows, nutrient cycle’s, chemical transfer, photosynthesis, food chains, food webs, trophic levels, linkages, biodiversity, interdependence, stability, structure, biophysical interactions, seral progression, succession, dynamic equilibrium Assess Judgement Simplistic judgement – a statement like “ this impacts on the functioning of the ecosystem” with no follow up given Implied impact on the functioning of the ecosystem – not explicitly stated More comprehensive – makes a judgment about the impact of one human action on the functioning of an ecosystem – but doesn’t carry it through all examples of human impacts Explicit, comprehensive judgement supported by evidence about the impact of human actions on the functioning of the ecosystem. Impacts are: positive, negative, devastating, destructive, minimal, extensive, damaging, disturbing, constructive…. Caves Ecosystem at Risk: Lotus Diagram Page | 15 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre Ecosystems at Risk: Caves Study Lotus Diagram 1 2 Spatial Patterns Weather & Climate 4 Bio geographical processes 1. 2 Spatial Patterns Weather & Climate 3 4 Geomorphic and Hydrological processes 5 ALPINE ECOSYSTEM AT RISK Yarrangobilly Caves Bio geographical processes 6. . Nature and rate of change which affects ecosystem function 6. Nature and rate of change which affects ecosystem function 3 Geomorphic and Hydrological processes 7 Human impacts Positive & negative Adjustments in response to natural stress 5 Adjustments in response to natural stress 8 Traditional and contemporary management practices 7 Human impacts Positive & negative 8 Traditional and contemporary management practices Page | 16 Ecosystems at Risk: Caves Study Riverina Environmental Education Centre