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Offwell Wetland Survey


Diagram of Interrupted Line Transect 2, East/West across the Wetlands.
Measurements taken every other metre.


The diagram below illustrates all the plants which touched the transect line. Click here for an overview of the transect position in the Wetland. This transect is marked by the yellow line on the photograph.

The plants are diagrammatically represented In the illustration below. The horizontal scale is in metres. Click here for the  Key to SpeciesThe water levels are illustrated at the bottom of the diagram. Blue indicates standing water, marked with the approximate depth. Areas without standing water are indicated by the colour olive. Where the areas are adjacent a gradient exists, except on the stream bank which is at 37.5 metres. Marked water levels are not absolute, but will fluctuate according to the amount of water entering the wetland.

Photographs have been used to give a general idea of the vegetation at particular points. The photographs were not necessarily taken at exactly the same time of the survey. Therefore certain species, although present, may not be conspicuous.

Maximise your screen now to view this diagram. Windows users can press the F11 key to alternate the screen between full screen and normal.

     

Dry Land

Marsh

Swamp

Marsh

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EAST . .

10cms depth

2cms

6cms

1cm

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4cms

2cms

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. . .

4cms

7cms

15cms

22cms

60cms

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WEST.
 

The diagram above illustrates plant zonation patterns across the wetland.

There is a very narrow dry land zone on the eastern section of this transect (1-6m mark). The plant species here are those which prefer drier conditions. They include species such as Silver Birch and Rhododendron. Willow also grows here, although it is mainly found in the marsh region. (This does not show up in this diagram because of the large recording interval. See the continuous line transect diagram to compare.) The Rhododendron, which originally covered the entire area, still occurs in a narrow band down both the East and West sides of the wetland and in the Northern dry land area. It is prevented from encroaching further by the wet, marsh conditions in the adjacent areas.

The dry land areas grades very quickly into marsh (6-28m). The marsh zone is characterised by water-logged sediments and levels of standing water which vary with the topography of the zone. Dips and hollows fill with water, while higher mounds are dry. It must be stressed that  the water levels marked on the diagram above were correct at the time of the survey. However, they will fluctuate according to the amount of rainfall and stream water which is entering the wetland.

The marsh zone is characterised by species such as Willow, Wood Clubrush,  Greater Tussock Sedge, Reedmace, Yellow Iris, Marsh Bedstraw and Branched Bur-reed. Water Mint is also very prevalent in this area, but as an anomaly, due to the two metre recording interval, it has not been picked up at all (see the continuous line transect). The Silver Birch at the 17m mark was on a mound raised above the general level of the marsh. It was therefore dry enough at this point for the Silver Birch to survive.

As the water level begins to rise (29m mark), the marsh plants begin to die out. Branched Bur-reed is the last to die out. As the marsh plants disappear and water depth increases, swamp plants such as Bog Bean take over (35-37m).

The swamp ends adjacent to the incoming stream channel. The western bank of the stream very abruptly marks the end of the deep water zone (38m). The west bank of the stream is raised and Alder trees have grown up here. Marsh species, such as Willow and Yellow Iris occur to the west of this region. The species here are actually slightly different to the marsh species in the centre of the wetland, although this is not clear in this diagram. Due to the 2m recording interval, the difference has been missed in this transect. Soft Rush, Pendulous Sedge, Monkey Flower (a non-native species), Water Plantain and Lesser Spearwort are all common species in this area (continuous line transect).

The  E/W continuous line transect  is valuable in that it picks up most of the species present in the transect area (36 species in this case). However, the great number of plants which have to be diagrammatically represented along the line makes the illustration quite difficult to look at and extract information from. There is a great deal of 'clutter' taking the eye away from general patterns of distribution.

Patterns of zonation are somewhat clearer in the interrupted line transect where records were taken every metre. This is because a lot of the less dominant species have been removed from the picture. However, this transect diagram does not show the patterns of zonation as clearly as the corresponding transect diagram for the N/S transect. This is because the 1m transect interval in this E/W transect picks up only about half of the species present (19, as opposed to 36 for the continuous line transect). In other words, rather too much 'clutter' has been removed.

This is even more marked in the diagram above where records were taken every two metres. Only one third of the species present (12, as opposed to 36 found in the continuous line transect) were recorded.. Rather than making zonation patterns clearer, it has tended to obscure them because the records are insufficient to reveal trends in different areas.

There is an added disadvantage with both interrupted line transects in that they are likely to underestimate the range of each species. This is the total region through which the species can be found. As records are only being taken at every metre mark, or at every other metre, plants will only be recorded if they happen to touch the line at the right point. This is illustrated by the apparent absence of Water Mint in the marsh zone, when in fact it is very common there (see the continuous line transect diagram).

The range of a number of the more important plant species distributed along the East/West line transect is shown here. This diagram was derived from the continuous line transect data, for the reason noted just previously.

Why use line transects? - the merits of different types of line transect.

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