floodplains survive <strong>the</strong>re because <strong>the</strong>y have evolved strategies <strong>for</strong> lowwater use.In contrast, aquatic and wetland plants rarely have water-conservingstrategies. Submerged plants, <strong>for</strong> example, have leaves rarely more thana few cells thick and virtually no protective outer cuticle, so <strong>the</strong>ydehydrate rapidly in <strong>the</strong> sun. Wetland plants with aerial leaves, such asemergent and floating-leafed macrophytes, have a thick or waxy cuticleon <strong>the</strong>ir leaves but transpire readily.Most aquatic plants ‘ride out’ <strong>the</strong> dry inter-flood periods by strategieso<strong>the</strong>r than physiological adaptations. One strategy that is typical <strong>of</strong>annuals is avoidance, exemplified by short life-span and setting seeds,hence reliance on <strong>the</strong> seed-bank. Ano<strong>the</strong>r strategy, typical <strong>of</strong> perennials,is to enter a low-activity or no-growth phase. In this, water loss isrestricted by leaf-shedding, or by complete canopy senescence and dieback.The plant survives with its sensitive generative tissues buried in<strong>the</strong> sediment, or as hard-coated seeds or some o<strong>the</strong>r propagules.Aquatic plants have a wider range <strong>of</strong> propagules than do terrestrialspecies, with rhizomes, corms, tubers, turions, spores and nodalfragments as well as seeds.The long-term survival <strong>of</strong> <strong>the</strong>se propagules depends on being buried inprotective sediments and on <strong>the</strong> sediments being protected fromdisintegration by trampling or machinery. In general, water-conservingstrategies are better developed in shrub and tree species occurring on<strong>the</strong> infrequently-flooded parts <strong>of</strong> floodplains.Adaptations, tolerance and stressDifferences in adaptation to resource availability means species arefound in particular sequences, ie. at different positions on <strong>the</strong>environmental gradient from ‘flooded’ to ‘dry’. This is evident inzonation (Figure 7), <strong>the</strong> concentric patterns <strong>of</strong> species in <strong>the</strong> littoralzone around a billabong or up a riverbank. On a larger scale, a similardistribution can be seen across a floodplain.The degree <strong>of</strong> adaptation can be described as obligate or facultative;and adapted or tolerant. In <strong>the</strong> floodplain wetland context, speciesdependent on aquatic conditions to provide resources, support andopportunity <strong>for</strong> regeneration are obligate species, whereas those thatcan survive on wet muds (at least temporarily) after flood recession andstill flower and set seed, are facultative. Thus, submerged plants such asVallisneria which die <strong>of</strong> desiccation on flood recession are obligate <strong>for</strong>inundation, whereas many species <strong>of</strong> milfoil, Myriophyllum spp., thatcan grow on wet muds, especially during cooler conditions, arefacultative. Similarly, species may be flood-adapted, meaning <strong>the</strong>y havespecific adaptations that allow growth under flooded conditions,whereas species that survive but are not adapted to grow are floodtolerant.An equivalent situation occurs in relation to dry conditions on<strong>the</strong> higher parts <strong>of</strong> a floodplain, where plants may be drought-adaptedor drought-tolerant.The tolerance range <strong>of</strong> a species to a particular component <strong>of</strong> <strong>the</strong> waterregime, such as depth, can be inferred in various ways, includingspecific investigations. Descriptive generalisations such as growth-<strong>for</strong>mcan be helpful (Figure 8).22 <strong>Estimating</strong> <strong>the</strong> <strong>Water</strong> <strong>Requirements</strong> <strong>for</strong> <strong>Plants</strong> <strong>of</strong> <strong>Floodplain</strong> <strong>Wetlands</strong>
<strong>Floodplain</strong> vegetationEcological rangeThe array <strong>of</strong> plants on floodplains includes species that are adapted todry, almost terrestrial, conditions, to aquatic conditions, and to <strong>the</strong>various intermediate conditions. Words used in this guide to refer to<strong>the</strong>se plants are given below:Aquatic plants usually refers to those plants that are adapted togrowing in, on or under water. Definitions vary, and while it is easy toagree that submerged species are aquatics, it is not always accepted thatmedium–tall sedges such as Eleocharis acuta and E. dulcis fromintermittent or seasonal wetlands are aquatics. Aquatic plants may alsobe known as water plants, or hydrophytes.Amphibious plants are those plants that grow or survive on wetexposed mud flats. These may be aquatic plants such as Ludwigiapeploides, stranded by falling water levels, or a completely differenttype <strong>of</strong> plant, <strong>the</strong> semi-terrestrial ones that germinate and grow rapidlyin <strong>the</strong>se conditions (Figure 9).Wetland plants are those found growing in a wetland. In wet–dryfloodplains, <strong>the</strong>y include amphibious and terrestrial and, arguably, alsoexotic species. The definition <strong>of</strong> wetland plants is probably <strong>the</strong> leastprecise <strong>of</strong> <strong>the</strong> definitions listed here.Macrophyte means literally ‘large plant’, a name coined originally todistinguish <strong>the</strong>se from microphytes such as phytoplankton. It is nowused almost interchangeably with aquatic plants, and includes <strong>the</strong>stoneworts Chara and Nitella in <strong>the</strong> family Characeae because, eventhough <strong>the</strong>se are algae, <strong>the</strong>y have a herb-like <strong>for</strong>m.These terms, being difficult to define satisfactorily <strong>for</strong> all conditions andall plants, are flexible. When buying or using books to identify wetlandand floodplain or aquatic plants, it is advisable to check <strong>the</strong> definitionsbeing used. Only State or national floras are fully comprehensive.The plants may be short- or long-lived perennials, biennials or shortlivedannuals; <strong>the</strong>y may be small or simple <strong>for</strong>ms, such as duckweedsand charophytes, or large woody species, such as trees.Temporal changesOn wet–dry floodplains, <strong>the</strong> changes that result from flooding and laterfrom flood recession, provide a brief but distinct growing opportunity.Short-lived and dormant herbs and <strong>for</strong>bs, that is herbaceous plants o<strong>the</strong>rthan grasses, grow quickly; rapid growth alters <strong>the</strong> appearance <strong>of</strong> aperennial community.A lignum shrubland may have an understorey <strong>of</strong> short sedges, aquaticherbs or terrestrial grasses, depending on time since flooding, but is stilla lignum shrubland. If, however, <strong>the</strong> lignum is removed, <strong>the</strong>n what was<strong>the</strong> understorey now appears as a dynamic, constantly changingwetland plant community.It would be a mistake to interpret all herb–<strong>for</strong>b wetland plantcommunities as <strong>the</strong> result <strong>of</strong> disturbance. The aquatic herbs thatgerminate or regrow on lagoon floors after flooding are a transient plantcommunity; as <strong>the</strong> wetland dries out, <strong>the</strong> plants in this community die.Section 2: Introducing <strong>the</strong> Vegetation 23
- Page 1 and 2: Estimating the WaterRequirements fo
- Page 3 and 4: ContentsPreface 7Acknowledgments 8G
- Page 5: List of Tables1 Spatial variability
- Page 8 and 9: Note that the guide is concerned pr
- Page 10 and 11: ecomes a matter of how to use what
- Page 12 and 13: Figure 1. Floodplain featuresThe fl
- Page 14 and 15: Figure 4.Wanganella Swamps, souther
- Page 16 and 17: Floodplain wetlands, being a mosaic
- Page 18 and 19: Section 2:Introducing theVegetation
- Page 20 and 21: size and vigour rarely reach their
- Page 24 and 25: The lagoon floor is then colonised
- Page 26 and 27: Note 11Growth-formsField guides to
- Page 28 and 29: identical conditions. PFTs differ f
- Page 30 and 31: Note 13Changes in depthSome herbace
- Page 32 and 33: Focusing on depthWater regime analy
- Page 34 and 35: Note 15Internet dataEnvironmental d
- Page 36 and 37: Step 3: Vegetation-hydrologyrelatio
- Page 38 and 39: Note 19Modelling and time-stepsIn s
- Page 40 and 41: Section 4: Old andNew DataOne of th
- Page 42 and 43: see Figure 15), despite a three-fol
- Page 44 and 45: frequency. This is rather limiting,
- Page 46 and 47: Figure 13. Lippia, a floodplain wee
- Page 48 and 49: single measure of the vegetation to
- Page 50 and 51: Section 5:ObtainingVegetation DataW
- Page 52 and 53: However, if the chosen species has
- Page 54 and 55: Figure 15. Range of tree condition
- Page 56 and 57: Figure 16. Spatial-temporal sequenc
- Page 58 and 59: Note 26Canopy condition indexA visu
- Page 60 and 61: Note 27Mapping floodplainwetland ve
- Page 62 and 63: Shape of species responseThe shape
- Page 64 and 65: Figure 18. Heat pulse sensorHeat pu
- Page 66 and 67: section, using storage volume and i
- Page 68 and 69: Figure 20. Crack volume and drying
- Page 70 and 71: Figure 21. The relationshipbetween
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epresentative, there should be no m
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All of the curves are described by
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monitoring, precision levels, scali
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sites of significant recharge and d
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Figure 24. Degraded channelPart of
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and so depth estimates are inaccura
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Section 7:PredictingVegetationRespo
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AEAM and the Macquarie Marshes. An
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Category 3: hydraulic/empiricalAppr
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For example, changes in surface and
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ReferencesPrefaceArthington AH and
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Section 3Roberts J and Marston F (1
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Kunin WE and Gaston KG (1993). The
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Singh VP (1995).“Computer models
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Web ListingsNote 40Data on the WebM
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flood. This has not been attempted,
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Seven points over the flow range is
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used as exclusions; or can be quant
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Table A1 - 4. A flooding overlay ch
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Table A2 - 1.(cont’d) K c and K s