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State of the Bay Report 2011-Final.pdf - Anchor Environmental

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No. saltmarsh patches<br />

Saltmarsh area (million m 2 )<br />

<strong>State</strong> <strong>of</strong> Saldanha <strong>Bay</strong> & Langebaan Lagoon <strong>2011</strong><br />

Aquatic macrophytes<br />

6.2 Long term changes in Saltmarshes in Langebaan Lagoon<br />

Saltmarshes in Langebaan are reportedly an important habitat and breeding ground for a range <strong>of</strong><br />

fish, bird and invertebrate species (Christie 1981, Day 1981, Gerrike 2008). Langebaan Lagoon<br />

incorporates <strong>the</strong> second largest salt marsh area in South Africa, accounting for approximately 30% <strong>of</strong><br />

this habitat type in <strong>the</strong> country, being second only to that in <strong>the</strong> Knysna estuary (Allanson et al.<br />

1999).<br />

Long term changes in salt marshes in Langebaan Lagoon were investigated by Gerrike (2008)<br />

using aerial photographs taken in 1960, 1968, 1977, 1988 and 2000. He found that overall saltmarsh<br />

area had shrunk by only a small amount between 1960 and 2000, losing on average 8 000 m 2 per<br />

annum. Total loss during this period was estimated at 325 000 m 2 , or 8% <strong>of</strong> <strong>the</strong> total (Figure 6.3,).<br />

Most <strong>of</strong> this loss has been from <strong>the</strong> smaller patches <strong>of</strong> salt marsh that existed on <strong>the</strong> seaward edge<br />

<strong>of</strong> <strong>the</strong> main marsh. This is clearly evident from <strong>the</strong> change in <strong>the</strong> number <strong>of</strong> saltmarsh patches in <strong>the</strong><br />

lagoon over time, which has declined from between 20 and 30 in <strong>the</strong> 1960s and 70s to less than 10<br />

at present. Gerrike (2008) attributed <strong>the</strong> observed change over time to increases in sea level that<br />

would have drown <strong>the</strong> seaward edges <strong>of</strong> <strong>the</strong> marshes or possibly reduced sediment inputs from <strong>the</strong><br />

terrestrial edge (i.e. reduced input <strong>of</strong> windblown sand due to stabilization by alien vegetation and<br />

development).<br />

20<br />

15<br />

10<br />

5<br />

0<br />

1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005<br />

Figure 6.3. Change in saltmarsh area over time in Langebaan Lagoon. (Data from Gerricke 2008)<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

0<br />

1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005<br />

Figure 6.4.<br />

Change in <strong>the</strong> number <strong>of</strong> discrete saltmarsh patches over time in Langebaan Lagoon. (Data<br />

from Gerricke 2008)<br />

127<br />

ANCHOR<br />

e n v i r o n m en t a l

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