(b) whether the site meets the floristic descriptors for one or more of the communities.
48 The Council submits that the area identified by one of the witnesses, Dr Andrew Smith, on Figure 10 of his report (Exhibit 3) comprises a combination of the three ecological communities, Swamp Sclerophyll Forest, Subtropical Floodplain Forest and River-Flat Eucalypt Forest. Figure 10 is an aerial photograph on which Dr Smith has superimposed three coloured areas, of which two are relevant being the area coloured mauve and the area coloured green. Dr Smith has also marked the quadrats in which vegetation surveys were undertaken. The Council submits that the mauve coloured area is dominated by the Swamp Sclerophyll Forest community and the green coloured area is dominated by both the Swamp Sclerophyll Forest and River-Flat Eucalypt Forest communities. The Subtropical Coastal Floodplain Forest occurs over both the mauve and green coloured areas. The Council submits that the overlapping and intergrading of each of the three communities on the areas coloured mauve and green is expressly recognised by the Scientific Committee in each of the descriptions of the communities.
49 The applicant submits that the mauve and green coloured areas identified by Dr Smith and marked on Figure 10 of Exhibit 3 do not satisfy the Scientific Committee's descriptions of any of the three communities. The applicant submits the site is not on the landforms identified in the descriptions of the communities and in particular is not on a coastal floodplain. Furthermore, the applicant submits that the floristic composition of the vegetation on the site does not satisfy the floristic descriptors in the Scientific Committee's descriptions of any of the three communities.
The evidence
50 The Court had the advantage of undertaking, on 8 November 2006, a comprehensive view of the site and the control sites in the company of the legal and other representatives of the parties and the parties' experts. The Court had the written and oral evidence of Dr Pam Hazelton, a soil scientist called by the Council, and Dr Christopher Gippel, a geomorphologist called by the applicant, Dr Andrew Smith and Dr Anne Clements, an ecologist and botanist respectively called by the Council and Dr David Robertson and Mr John Travers, both ecologists called by the applicant. In addition, a number of scientific studies were tendered.
Locational descriptors
51 In determining if any one or more of the three communities occur on the site, I need only focus on that part of the site on which the Council contends one or more of the communities occur. This is the part containing the mauve and green coloured areas identified by Dr Smith on Figure 10 of Exhibit 3.
52 The Scientific Committee's Final Determinations for each of the Swamp Sclerophyll Forest, Subtropical Coastal Floodplain Forest and River-Flat Eucalypt Forest communities specify three locational descriptors: the edaphic (soil) requirement, the landform requirement and the required association of the landforms with coastal floodplains.
Edaphic requirement
53 The areas coloured mauve and green on Figure 10 of Exhibit 3 meet the edaphic requirement in the Final Determinations of being associated with clay loams and sandy loams (in para 1 of each description).
54 Dr Hazelton excavated, analysed and described the soils in the areas. Dr Hazelton gave oral evidence that the soil pits were located within the quadrats surveyed by Dr Clements, including quadrats 1-6 which are in the areas coloured mauve and green. The soils included bands of sandy clays, clay silts, silty loams, clay loams, clay sands and sandy clay loams. These soils are characteristic of Quaternary alluvium.
55 Further, the 1:250,000 geological map for the area containing the site identifies part of the areas (towards the north eastern boundary of the site) as supporting Quaternary alluvium. This Quaternary alluvium extends continuously from the site along the watercourse in a southerly direction, across the Pacific Highway and towards Grahamstown Lake. The distribution of the Quaternary alluvium provides a good indication of the extent of the coastal floodplain.
56 The 1:100,000 soil landscape map of the Newcastle mapsheet identifies the site as falling within the Ten Mile Road soil landscape but close to the boundary of the Nungra soil landscape. The Ten Mile Road soil landscape is a colluvial soil landscape while the Nungra soil landscape is an alluvial soil landscape. The Nungra soil landscape is described as being "associated with Quaternary alluvium and deep silty footslope deposits recorded from surrounding hills and overlaying carboniferous rock strata" (L Matthei, Soil Landscapes of 1:100,000 Newcastle Map Sheet , Department of Land and Water Conservation, 1995).
57 As Dr Smith explains, an alluvial landscape is one in which soils are deposited by water and are typically present in layers including layers of fine silts and water sorted particles of different sizes in different layers. Colluvial landscapes are ones in which soils have developed from rock (lithic substrate) in situ or by being deposited by gravity. Colluvial soils typically do not show water sorted layering and typically do not have a podsolic profile and a large gravel content with increasing proximity to bedrock.
58 Dr Hazelton's soil sampling and analysis has established that the soils in the areas meet the description of alluvial not colluvial soils. Dr Hazelton concludes that the soils are those described in the Nungra soil landscape which, in this location, could be seen as an included soil landscape in the Ten Mile Road soil landscape. An included soil landscape is a small area of soil landscape within a predominate landscape. Dr Hazelton concludes that the site has not been mapped as an included Nungra soil landscape because soil landscape units of less than 40 hectares are generally not mapped. Dr Smith corroborates Dr Hazelton's evidence on this point.
59 The Scientific Committee, in a letter to the Council on 12 October 2005, notes that "mapping of soils is scale-dependent, and that small occurrences of shallow alluvial soil may be expected to occur within areas mapped as having lithic substrates". This too corroborates Dr Hazelton's evidence.
60 I accept both Dr Hazelton and Dr Smith's evidence that the soils in the areas are alluvial not colluvial and that the areas are properly to be classified as being of the Nungra soil landscape.
61 The most recent geological mapping is by A Troedson and T R Hashimoto as part of the New South Wales Coastal Quaternary Geology Data Package in 2005. That geological mapping does not show the Quaternary alluvium extending into the site as had the earlier 1:250,000 geological map. However, this geological mapping was done after the works to the Pacific Highway and the Balickera canal unlike the earlier geological mapping which preceded such works. Further, there is no evidence that specific geological surveys were done on the site so as to complete the recent mapping. In contrast, Dr Hazelton has carried out soil surveys which establish the presence of alluvial soils on the site.
Landform requirement
62 The areas coloured mauve and green occur on landforms of the type identified in the Scientific Committee's descriptions of each of the communities. The areas are aptly described as containing alluvial flats and drainage lines.
63 As I have noted, Dr Hazelton found alluvial soils in these areas. Further, she found that the subsoils in the areas were mottled indicating water logging. Dr Hazelton stated that the alluvial soils in the areas have been formed by sediments deposited by streams and an alluvial plain has developed. Dr Hazelton's oral evidence was that the floodplain of Nine Mile Creek (to the north east of the site) extended to the site, at least to the spot height of 21m shown on the topographical map (this spot height is located uphill of the mauve and green coloured areas and to the west of quadrat 1 and to the north of quadrat 6).
64 Dr Smith corroborates Dr Hazelton's evidence that the soils of the areas are alluvial in nature consistent with fluvial and overbank deposits.
65 Dr Smith gave further evidence of flooding, waterlogging and periodic inundation of the areas on the site. Dr Smith stated that he and other consultants had observed flooding and inundation of the areas. (I should interpolate here that inundation was evident in parts of the areas on the day the Court undertook the view). Dr Smith notes that the vegetation in the areas includes many species characteristic of swamps, wetlands and inundated flats including three species of paperbark ( Melaleuca decora , M. linariifolia and M. styphelioides ) and the swamp sedge (G ahnia clarkei ). Emergent old growth Redgum and Melaleuca decora trees are consistent with the site having been periodically inundated for a long period of time (hundreds of years). Dr Smith notes that holes of the freshwater crayfish or yabbie ( Cherax spp) are widespread across the low lying areas. This crustacean needs permanent water or periodic inundation for breeding. Dr Smith notes that there is a gully through the areas. This gully has a defined drainage area in its upper reaches but becomes less defined downstream where flat swampy areas occur and the main channel diverts into a number of smaller drainage channels and ponds.
66 Dr Smith also gave evidence of the low lying, flat nature of the site consistent with it being an alluvial flat on a coastal plain. The geological map of the site shows that Quaternary alluvium extends north from the lower Hunter River coastal floodplain into the north east corner of the site, including part of the areas coloured mauve and green. Swamps are shown consistent with a coastal floodplain. The Karuah 1:25,000 topographic map for the site shows that all of the mauve coloured area and most of the green coloured area is below 30m. A spot height of 21m (at a location just uphill of the areas coloured mauve and green, and to the west of quadrat 1 and north of quadrat 6) shows that much of the area is very low lying and flat. A distance of 400m separates this spot height and the 20m contour which occurs just at the entrance to the site. This reveals a slope of about 1.3%. This is a sufficiently low slope to make the description of an alluvial flat apposite.
67 Collectively, Dr Smith's evidence establishes that the areas on the site meet the descriptions of containing "waterlogged or periodically inundated alluvial flats and drainage lines" (para 1 of description of Swamp Sclerophyll Forest community) and "periodically inundated alluvial flats, drainage lines…" (para 1 of descriptions of Subtropical Coastal Floodplain Forest and River-Flat Eucalypt Forest communities).
68 Dr Robertson originally accepted that areas on the site around the creeks [which correspond with the mauve and green coloured areas] did satisfy the locational descriptor for the Swamp Sclerophyll Forest community of being "associated with humic clay loams and sandy loams, on waterlogged or periodically inundated alluvial flats and drainage lines associated with coastal floodplains" (Species Impact Statement, April 2006 at p 6.2).
69 Although Dr Gippel remained steadfast in his opinion that the areas on the site could not be classified as a floodplain, he ultimately conceded in cross examination that the soils on the site have the characteristics of soils of an alluvial floodplain, there were drainage lines on the site, there was active erosion within relevant areas of the site, there were aggradations by channelled and overbank stream flow and that overbank stream flow occurs with an average recurrence interval of 100 years or less. These correspond with the factors in the Scientific Committee's description of floodplains in the Final Determinations.
Association with coastal floodplains
70 The landforms of alluvial flats and drainage lines, which the areas coloured mauve and green contain, are "associated with coastal floodplains". The applicant sought to establish that the areas on the site could not be described as being on a coastal floodplain. The evidence of Dr Gippel, Dr Roberston and Mr Travers had this as its central thesis. However, the evidence missed the mark.
71 The definition of coastal floodplain posited by Dr Gippel, and embraced by Dr Robertson and Mr Travers, did not accord with the meaning of that term in the Scientific Committee's Final Determinations for each of the communities. Dr Gippel, Dr Robertson and Mr Travers trawled through the geomorphological scientific literature and dictionaries in an endeavour to define what is a coastal floodplain and then to demonstrate that the areas on the site did not meet this definition of a coastal floodplain. This endeavour by the applicant's experts was fruitless because the relevant enquiry could only ever be to ascertain the meaning of the term "associated with coastal floodplains" as used by the Scientific Committee in its descriptions of each of the communities in the Final Determinations.
72 An "endangered ecological community" is defined in s 4 of the Threatened Species Conservation Act as meaning an endangered ecological community specified in Schedule 1 of the Act. Part 3 of Schedule 1 of the Act specifies the listed endangered ecological communities to date, including the three of relevance in this case, adding after each the words "(as described in the Final Determination of the Scientific Committee to list the ecological community)". Hence, the enquiry was required to be directed to the description of the Scientific Committee in each of the Final Determinations to list each community.
73 Focusing on the particular concept of a floodplain, the enquiry was required to be directed to the Scientific Committee's intended meaning of floodplain in each of the descriptions of the communities in the Final Determinations. The Scientific Committee's intended meaning can be gleaned from a number of indicators.
74 First, the Scientific Committee in each Final Determination defines "floodplains" as "level landform patterns on which there may be active erosion and aggradation by channelled and overbank stream flow with an average recurrence interval of 100 years or less" (para 1 of each description). As I have earlier noted, the Scientific Committee states that this definition has been adapted from a reference by Speight. However, it is different to Speight's definition, in the ways I have earlier explained. It is wrong in principle to substitute for the Scientific Committee's definition, Speight's definition itself or to seek to qualify in any way the Scientific Committee's definition by reference to Speight's work. Dr Gippel, Dr Robertson and Mr Travers' attempts to do just this were therefore misguided.
75 Secondly, the Scientific Committee does not just rest in its explanation of what it intended to mean by its use of the term floodplain on the definition it provides. The Scientific Committee expands that definition and hence what it intended to mean by the term floodplain by reference to particular landforms that might be "associated" with coastal floodplains.
76 Dr Gippel sought to restrict the meaning of the term "associated with" to make it synonymous with "on". Thus, he expressed the view that a landform such as a drainage line could only ever be "associated with" a coastal floodplain if the drainage line was on the coastal floodplain. I reject Dr Gippel's construction.
77 The Scientific Committee in the Final Determinations describes each community by reference to its association with specified edaphic conditions and its location on specified landforms. The landforms specified are alluvial flats (that might be either waterlogged or periodically inundated) and drainage lines. The Scientific Committee narrows the class of alluvial flats and drainage lines to those that are "associated with" coastal floodplains. However, the Scientific Committee chose not to narrow the class further by specifying that the landforms of alluvial flats and drainage lines be "on" or "be part of" the coastal floodplains. Use of the preposition "on" would have demanded that the landforms be in a position of immediate proximity to the coastal floodplains while use of the phrase "be part of" would have demanded that the landforms be constituent elements of the coastal floodplains. The Scientific Committee chose not to so restrict the connection between the landforms and the coastal floodplains but instead used the phrase "associated with" thereby signifying a wider connection.
78 The relation by which the landforms might be connected with the coastal floodplains can vary but may include a relation of physical proximity, hydrological connection or ecological interrelationship.
79 Landforms might be connected by a relation of physical proximity. Landforms on or that are part of the coastal floodplain obviously have such a relation. But landforms which are separate from the coastal floodplains still could have a relation of physical proximity. At their closest, they could adjoin (abut or be in contact with) coastal floodplains or, slightly further removed, they could be adjacent (lying near or close) to coastal floodplains. But again the Scientific Committee did not limit the relation between the landforms and the coastal floodplains by these words but allowed a greater latitude of relation by employing the phrase "associated with". As a general rule, however, the greater the distance becomes between the landforms and the coastal floodplains, the weaker the physical connection becomes. Perhaps the elevation parameter (up to 50m for the Swamp Sclerophyll Forest community and up to 250m for the Subtropical Coastal Floodplain Forest and River-Flat Eucalypt Forest communities) may set an outer limit.
80 Landforms might have a direct hydrological connection. A site containing a discrete alluvial flat or drainage line with a fluvial connection to the coastal floodplain, such as where the drainage line might have onto the floodplain. Waters on the floodplain may in times of flood back up the drainage line or onto the alluvial flat causing inundation. A groundwater connection may be yet another example.
81 Landforms may have an ecological relationship with the coastal floodplain. There may be a relationship between the vegetation and soils of the floodplain and those of the relevant landform such as an alluvial flat or a drainage line. Fingers of alluvial soils may extend from the floodplain up drainage lines and into alluvial flats and the vegetation may follow resulting in the same vegetation communities on the floodplain and the alluvial flats and drainage lines. Provided there is a means of linkage (such as vectors for pollen, seed and fruit transportation and corridors for wildlife) vegetation communities can straddle physical obstructions to form discontinuous but linked communities.
82 Dr Robertson accepted in oral evidence that there could be discrete and discontinuous locations of the community. He prepared an illustrative sketch showing different locations of floodplains on different order watercourses. He gave as an example a floodplain on a small upper catchment creek at higher elevation (Perennial Creek near Grafton).
83 Dr Smith referred to a reference cited by the Scientific Committee in each of the Final Determinations of D A Keith, "Ocean shores to desert dunes: the native vegetation of New South Wales and the ACT", NSW Department of Conservation, Sydney, 2004 that stated that "the best remnants of this vegetation class [coastal floodplain wetlands] are now found not on the open plains but further up valleys on small flats amid undulating terrain that mostly supports grassy woodlands. In these areas fingers of alluvium extend up intermittent creek lines and carry distinctive forest of C asuarina glauca as well as various Melaleuca (paperbark) species up to 20m tall".
84 The fact that the Scientific Committee intended that areas with the relevant landforms can be associated with coastal floodplains, notwithstanding that they might be separated from and/or discontinuous with coastal floodplains, is also evident from the Scientific Committee's identification for the Subtropical Coastal Floodplain Forest and River-Flat Eucalypt Forest that they may occur on "localised" River-Flats that may occur at an elevation high above the coastal floodplain (up to 250m above sea level).
85 As I have noted earlier, the Scientific Committee has specified in the Final Determinations that the communities include other specific vegetation communities identified in other vegetation surveys and mapping. One such vegetation community is Riparian Melaleuca Swamp Woodland (Map Unit 42) identified and mapped in the LHCCREMS. The Final Determination for the Swamp Sclerophyll Forest community identifies the MU42 community to be included within the Swamp Sclerophyll Forest community. The LHCCREMS mapping of the distribution of the MU42 community shows that it comprises disjunct patches of habitat along drainage lines several kilometres distant from Grahamstown Lake or other alluvial floodplains. Some of these drainage lines are not on alluvial soil landscapes or Quaternary floodplain alluvium, but extend up valleys on intermittent creeks draining ultimately into Grahamstown Lake. Notwithstanding the locations of the MU42 community, the Scientific Committee has incorporated that community into the Swamp Sclerophyll Forest community. This reveals that the Scientific Committee did not intend that the Swamp Sclerophyll Forest community must occur "on" coastal floodplains or on sites that abut or are continuous with coastal floodplains.
86 I note that the above construction of the locational descriptors in the Final Determinations was also reached by the Scientific Committee. The Scientific Committee in a letter to the Council dated 12 October 2005, observed that it did not construe the description of Swamp Sclerophyll Forest in the Final Determination as stipulating "that all stands of the community must be continuous with coastal floodplains, only that the drainage lines are associated with coastal floodplains. Thus, a discrete alluvial flat or drainage line would be associated with a coastal floodplain if the drainage line flowed onto the floodplain and the site was in proximity to the floodplain, irrespective of whether the assemblage was continuous throughout its occurrence along the drainage line. In the context of the entire NSW coastline to which the Determination applies, flats separated from major floodplains by distances of a few hundred metres would also be consistent with the intent of the Determination".
87 Insofar as the decision of Commissioner Bly in CBD Prestige Holdings Pty Ltd v Lake Macquarie City Council [2005] NSWLEC 367 (12 July 2005) paras 45-47 held to the contrary of the construction of the Final Determination for the Swamp Sclerophyll Forest community that I have explained, I am of the opinion that it was wrongly decided and should not be followed.
88 Hence, the evidence of Dr Gippel, embraced by Dr Roberston and Mr Travers, that the areas coloured mauve and green on the site were not "on" a coastal floodplain did not and could not establish that the areas were not "associated with" a coastal floodplain.
89 In this case, the areas of the site have the necessary association with the identified soils (clay loams and sandy loams) and occur on the identified landforms of waterlogged or periodically inundated alluvial flats and drainage lines. Furthermore, these identified landforms are "associated with" a coastal floodplain. As I have noted, on the north eastern corner of the site, the underlying geology is that of Quaternary alluvium. Quaternary alluvium is associated with a floodplain. That Quaternary alluvium continues down drainage lines and creeks to the Grahamstown Lake.
90 The areas on the site coloured mauve and green are associated with this floodplain. These areas contain alluvial soils, which have been deposited by fluvial action. The alluvial soils are, in fact, continuous with the Quaternary alluvium in the north east corner of the site and down the water courses towards the Grahamstown Lake. The drainage line and the drainage across the site have a fluvial connection to the floodplain.
91 For these reasons, the areas coloured mauve and green on the site meet each of the locational descriptors of each of the three communities.
Floristic descriptors
92 The vegetation in the areas coloured mauve and green on Figure 10 of Exhibit 3 meet the floristic descriptors in the Scientific Committee's Final Determinations for each of the Swamp Sclerophyll Forest, Subtropical Coastal Floodplain Forest and River-Flat Eucalypt Forest communities. There are five sets of reasons.
Characteristic species
93 The areas contain a significant number of the flora species listed as characteristic species in the descriptions of the community. There have been, over the years, numerous vegetation surveys of the site, including by the current experts for the parties. When the data of these surveys are aggregated, the total number and percentage of characteristic species of the communities recorded on the site, as calculated by Dr Smith, is as follows:
Community Number of Species Percentage of Species
River-Flat Eucalypt Forest 42 55
Swamp Sclerophyll Forest 29 52
Sub-tropical Coastal Floodplain Forest 39 48