Science
- Evolutionary ecology research
- Australian rain forest community assembly
- Australian rain forest through time
- Ecology of Cumberland Plain Woodland
- Bicentenary Plant Diversity Program
- Biodiversity Adaptation Transect
- Botany of Botany Bay
- Conservation genetics
- DNA studies of Elaeocarpaceae
- Ecology of Isopogon prostratus
- Floristic Lists of NSW
- Habitat fragmentation
- Lomatia (Proteaceae)
- Molecular phylogeny of the Australian Lauraceae
- Promiscuous Lomatia
- Promiscuous Proteaceae
- Native plants of Sydney Harbour NP
- Newnes Plateau Shrub Swamps
- Next Generation Sequencing
- Nickel hyperaccumulation in Stackhousia
- NSW Vegetation Classification & Assessment Project
- Plants of the Newnes Plateau
- Plants, vegetation, landscape, country
- Phylogenetic relationships of Ceratopetalum
- Podocarpus elatus
- Rainforest conifer - Podocarpus elatus
- Speciation in Proteaceae
- Testing speciation models
- Horticultural research
- Plant diversity research
- Plant pathology research
- Herbarium & resources
- Scientific publications
Monitoring impacting events - fire, rabbits, rainfall, seasonalityOur research aim at the Australian Botanic Garden, Mount Annan has been to understand the ecology of the woodland as it recovers from nearly two centuries of rural use, and apply this knowledge to conservation management. Our main performance indicator has been the ongoing survival and expansion of all the native plant species present in the woodland, while reducing the abundance of exotic species. Treatments used have been ecological burning, exclosure of herbivores and weed eradication. No plantings of any species have been made.
Some effects of fireThere were no signs of any recent burning in our woodland in 1988, and the area had evidently remained unburnt at least since the early 1980s, and probably much longer, as stock grazing presumably kept the grass low. However there was vigorous regrowth taking place in the early years of our recording, and little evidence of aging or senescent shrubs. Aging or senescent shrubs are often conspicuous in Sydney Sandstone vegetation that has remained unburnt for long periods. However we assumed that fire would be important in Cumberland Plain Woodland ecology, and did want to try out treatments that might remove weed species and benefit native species. With this as an aim we burnt part of the woodland in September 1991. Three plots were burnt in the September 1991 fire. Average native plant species richness dropped slightly immediately after the fire, and then returned to prefire levels (see Figure below). However native species richness at unburnt plots showed similar drops, indicating that this was weather-related rather than fire-related (1992 and 1993 had below average rainfall). Indeed though there was a difference in species richness between burnt and unburnt sites before the fire, these differences were reduced after the fire. Average exotic species richness increased significantly immediately after the fire by over 50% compared with prefire levels 3 years earlier (see figure below), but in the next year it dropped to levels similar to that of unburnt sites and remained similar to them for the next 8 years. In general we did not note any obvious long-term changes in native species composition resulting from the burn and within 3 years the burned area was not noticeably different from adjacent unburnt areas.The main result of the 1991 fire however was that we were able to document the fire responses for a large number of species and demonstrate that the majority of these species could resprout after fire. Ten years later in September 2001 we burnt the same area again, and the following year September 2002 we burnt an adjacent area. Both fires were again Spring burns and of low intensity. Fire has a different dynamic in Cumberland Plain Woodland compared with shrubby woodland vegetation on sandstone. Differences in fuel loads between the two are crucial. In our woodland there is not the heavy fuel build-up that comes from the characteristic shrub-dominated component in woodland on sandstone. In Cumberland Plain Woodland most sticks and persistent leaves come from the widely-spaced eucalypts, shrubs are sparse and make little contribution, and herbs and grasses have soft leaves that decompose faster than the hard leaves of sandstone-growing shrubs. Thus in Cumberland Plain Woodland, fires move rapidly through the groundlayer when it is dry enough, but do not generate high temperatures. These observations were confirmed in our 2005 fires where fires in long unburnt woodland were more patchy and of lower intensity than in adjacent areas of grassland. A surprise from the fires A major finding from the fires surprised us. Immediate responses were slow because of dry conditions, but we discovered that most species responded to subsequent rain in the bare space created by fire, rather than to the direct effects of fire - heat, smoke or ash. We found almost as many different types of seedlings emerging in bare spaces in unburnt areas after rain, as came up in the burnt areas. |
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| Species - Natives | Burnt | Unburnt, | |
| before rain | after rain | after rain | |
| Acacia implexa? | X | ||
| Chloris ventricosa? | X | ||
| Cotula australis | X | X | |
| Cymbonotus lawsonianus | X | X | |
| Cyperus gracilis | XX | ||
| Desmodium brachypodum | X | X | |
| Desmodium varians? | X | ||
| Dichondra repens | XX | XX | XX |
| Dodonaea viscosa | X | X | |
| Einadia hastata | XX | XX | |
| Einadia nutans | XX | XX | |
| Eremophila debilis | XX | X | |
| Erodium crinitum | X | ||
| Eucalyptus crebra? | X | ||
| Euchiton sp. | X | X | |
| Fimbristylis dichotoma | X | ||
| Galium propinquum | X | ||
| Geranium homeanum | X | X | |
| Glycine tabacina | XX | X | |
| Hypericum gramineum? | X | ||
| Mentha satureioides | X | ||
| Microlaena stipoides? | X | ||
| Oxalis perennans | XX | XX | |
| Phyllanthus virgatus | X | ||
| Plectranthus parviflorus | X | X | |
| Poranthera microphylla | X | ||
| Sida corrugata | XX | X | |
| Solanum prinophyllum | XX | XX | |
| Solenogyne dominii | X | ||
| Wahlenbergia gracilis | X | X | |
| TOTAL NATIVES 30 | 3 | 26 | 18 |
| Species - Exotics | Burnt | Unburnt | |
| Before rain | After rain | After rain | |
| *Anagallis arvensis | XX | XX | |
| *Ciclospermum leptophyllum | X | X | |
| *Cirsium vulgare | X | X | X |
| *Gomphocarpus fruticosus | X | ||
| *Heliotropium amplexicaule | XX | XX | |
| *Hypericum perforatum | X | ||
| *Hypochaeris microcephala | X | ||
| *Hypochaeris radicata | X | ||
| *Medicago lupulina? | XX | ||
| *Modiola caroliniana | X | X | |
| *Phytolacca indica | X | X | |
| *Plantago lanceolata | XX | X | |
| *Senecio madagascariensis | XX | XX | |
| *Setaria gracilis | X | ||
| *Sida rhombifolia | XX | XX | XX |
| *Solanum nigrum | X | XX | XX |
| *Sonchus oleraceus | X | X | |
| *Trifolium (incl. 3 species) | XX | XX | |
| *Verbena bonariensis | X | ||
| TOTAL EXOTICS 18-21 | 4-5 | 16-19 | 14-17 |
| Unidentified dicotyledons | 3 species | ||
| Unidentified monocotyledons | 3+species | ||
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Notes from the 2002 droughtThe drought in 2002 occurred at just the right time in our recording sequence. Our monthly recording had begun in 2001 and had given us a year of average year effects. This was followed by the drought year - there was virtually no rain from the end of March to December 2002. Some rain came in late Summer and Autumn 2003, with really good rain in May. (Rainfall 2001: 631 mm, 2002: 524 mm, 2003: 644 mm, longterm average 828 mm)
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The importance of rainfallWhile we were well aware that rainfall was important for the successful growth of woodland species we had not truly realised its importance in the initiation of growth and particularly seedling growth events. We had always assumed that rainfall was distributed more or less throughout the year and was not generally a limiting factor, rather that triggering factors like fire or increasing temperatures were most important in regulating growth and recruitment. Rainfall in the late 1980s and early 1990s was generally average or above. However since 2000 there have been a series of dry and sometimes hot years. 2002 was a particularly dry and hot year, with record high temperatures in December. In the area burnt in our 2002 burn there was little regeneration because of the lack of rainfall, so in summer 2002-2003 we took soil samples and watered them in the glasshouse to see what might be in the soil seedbank. What came up in the soil samples was an impressive array of seedlings many of which we had never seen in the field, though we were familiar with the adult plants there. We also got seedlings of one species Ranunculus sessiliflorus, which we had recorded once back in 1990, and, but for the fact that we had kept a small specimen of it, we would have regarded as an error of identification. As it was, we regarded the species as likely to be extinct in the woodland. Subsequent rain in March 2003 (drought-breaking) resulted in the germination of many seedlings in the woodland, including Ranunculus sessiliflorus and Daucus glochidiatus which has also been recorded only once before. Seedlings of both species, and many others, were recorded in both burnt and unburnt areas, indicating that it was particular site conditions not the effect of fire that allowed seedling establishment, though the open conditions in some burnt areas may have helped by providing locally higher soil temperatures or reduced competition from established plants. Table Number of woodland species with seedlings recorded in burnt (September 2001) or unburnt sites before and/or after good rain (February-March 2002), the Australian Botanic Garden, Mount Annan . Seedlings observed October 2001-August 2002
Short-lived ephemeral species We have been able to compile a list of species, almost all short-lived ephemerals, that recruited well in drought-breaking conditions, ie substantial rain following a long hot dry period. The list includes Ranunculus sessiliflorus, Daucus glochidiatus,*Conyza sumatrensis. While some of these species will occur at other times, generally in smaller numbers, we suggest that factors relating to drought conditions such as temperature may play a part in their dormancy breaking mechanisms. Further work is needed. As a result of these observations we are convinced that the main force driving processes in the woodland is rainfall rather than fire or temperature. The decreased rainfall events expected as climate change takes hold may have a significant impact on the long term floristic composition of the woodland. |
Seasonality - annual and short-term changes 2001-2002Any patch of ground in Cumberland Plain Woodland is likely to change the way it looks during the year. The herbs and grasses grow during favourable weather and die back when it’s hot and dry, or when it’s too cold. In recording species presence in our plots, the number of species has varied from as low as 2 per square metre during a very dry time to 27 after rain has stimulated growth. The number of species one can find varies over space as well as time. In our 5 m x 5 m plots, the total number of species recorded as present at some time has varied from 34 to 53. Changes over a two year period 2001-2002, based on individual species abundance (frequency) from the monthly recording of Plots 4 and 9, show the following features:
Our picture of the Cumberland Plain Woodland flora at the Australian Botanic Garden is of a flora of species with characteristics that enable persistence in the face of fluctuating seasonal rainfall and temperature conditions. Most species are perennial and able to survive severe dry periods at ground level as rootstocks or soil stored seed. These characteristics also allow them to survive fire events. Growth cycles are aligned with longterm annual rainfall patterns, with most species being autumn-winter growing and flowering. Under good rainfall conditions growing and flowering will extend into spring with a slight mid Winter hiatus in very cold years. This is different to the Sandstone flora where spring flowering and growth is the main response. Some difficulties in monitoring Cumberland Plain Woodland
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