Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Ecological response to storms Storms elicit an erosion response from the visible portion of all beaches, even the healthy ones. The important thing to remember though, is that most sand is not lost, just put somewhere else within the system. For more information about the beach’s physical response to storms, check out Beach erosion and coastal processes on the Gold Coast information sheet. This information sheet examines the ecological response of the coastal environment to storms. The coastal environment is extraordinarily dynamic. Much habitat can be lost, altered or created in a large storm event. As a result, species composition in these environments tends to fluctuate. The importance of vegetation The integrity of the sand supply on the visible portion of the beach is dependent upon vegetation. This vegetation traps windblown sand, thereby facilitating accretion and the growth of the sand dune, see Figure 1. Vegetation slows down sand particles blown landward by wind, leading to deposition and accumulation of dunes. Without this vegetation, sand will be blown further inland, resulting in a net loss in the sediment budget and a retreating coastline. Figure 2. Ghost Crab (Ocypode cordimanus) (Source: GCCC 2011) Dune plant colonisation Build-up of sand Healthy dune system Figure 1. The process of sand dune formation (GCCM 2011) What about the beach fauna? Disturbances such as storms can have a great effect on the dune and beach fauna. Erosion to the dunes can displace many animals, including crustaceans, reptiles and birds. Naturally, animals would have an opportunity to move away from the eroding escarpment; however, such disturbances in our urban environment can leave them temporarily displaced. Erosion of the sandy beach can lead to the decline in invertebrate populations. There appears to be very few studies of the recovery rates of these invertebrate populations; however, it is known that these invertebrates usually number in the millions, so recovery can be rapid. This recovery is also boosted by an opportunistic immigrant population, which will move in after a storm event to take advantage of reduced levels of competition or predation. Plant succession: the key to recovery from storms Plant succession occurs in response to a disturbance (for example, a storm) and refers to a process of change over time within the ecological community. After a disturbance, particular plant species first colonise the disturbed space followed by a succession of further plant types until the plant community has recovered. Colonising species ♦ Hardy pioneers that survive within the inhospitable, newly formed dunes ♦ Tolerate exposure, poor nutrient conditions, a lack of fresh water and sometimes very high temperatures (McLachlan & Brown, 2006) ♦ Create the structure of the dunal habitat by reducing wind erosion, increasing soil moisture and also increasing nutrient stores within the sand ♦ Example: Spinifex grass (Figure 3), which after a storm hangs over the erosion scarp and starts trapping wind-blown sand Secondary species ♦ Less tolerance to exposure and greater nutrient requirements ♦ Cope with poor water availability and high temperatures ♦ Example: Coastal Wattle, which disperses readily and has in-built mechanisms Figure 3. Sand Spinifex is a valuable coloniser of Gold Coast dunes (Source: GCCC 2006) to cope with water stress (Figure 4) Climax communities ♦ Characterised by mature vegetation, typically dominated by larger, long-lived trees such as Eucalypts, or Pandanus Palm (Figure 5) ♦ Takes much longer to recover from large storm events Our changing coast Storm events are a natural element of the coastal environment. Given time, ecosystems affected by a storm event will recover through processes such as succession. It is important that Council’s coastal management activities work with rather than against these natural processes, and that any management activities do not reduce the ability of natural ecosystems to respond to storm events. Figure 4. Coastal wattle on South Stradbroke Island (Source: GCCC 2007) For more information about these coastal environments, refer to information sheets in the Discovering our Coast series. A healthy dunal system The structural composition of dune vegetation can tell us a lot about the capacity of the ecosystem to respond to a storm event. The presence of colonising species in the fore dunes is a good sign that these oceanfront dunes would be stabilised quickly following a storm disturbance event. In contrast, if the hind dunes experience direct exposure to a storm event, their vegetation composition is less resilient to harsh conditions and recovery is expected to be slower. This is one of the reasons why healthy dune systems feature a combination of fore dunes, secondary dunes and hind dunes – the space gives the beach flexibility to move in accordance with the sand store, and maximise its ability to ecologically and structurally recover from storm events. Figure 5. Established Pandanus Palm on South Stradbroke Island (Source: GCCC 2007) References: Mahony, D. 1978, Beaches: Learning to Live with the Sea. Charden Publications, Summer Hill. McLachlan, A. and Brown, A. 2006, The ecology of sandy shores. Academic Press, Massachusetts.