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An innovative approach for monitoring abiotic factors influencing mangrove forest biodiversity in an estuarine ecosystem M. Atwell1; M.N. Wuddivira1; J. Gobin2; D.A. Robinson3 1Department of Food Production, University of the West Indies, 2Department of Life Sciences, University of the West Indies, 3Centre for Ecology and Hydrology, Environment Centre, Wales, UK 1 Introduction The UN’s Millennium Ecosystem Assessment (2005) targeted coastal wetlands as environments that “are experiencing some of the most rapid degradation and loss worldwide”. 5 Mangrove wetlands are important because they provide a buffer, protecting vulnerable coastal and marine ecosystems from rising sea levels and storm tides (Ewel et al., 1998). Rhizophora mangle (red), Avicennia germinans (black) and Laguncularia racemosa (white) species of mangroves were identified along the river banks. The red mangroves thrived in areas of adverse water quality conditions and indeed are the hardiest of the three species. In Trinidad West Indies, land-use changes and sea defenses impact water quality and alter mangrove forest distribution and biodiversity. Salinity and water quality parameters play a major role in determining mangrove species diversity in a tropical estuarine ecosystem. This research therefore investigates the abiotic water quality factors influencing mangrove zonation along the South Oropouche River, Godineau Swamp. 2 Summary & Conclusion The novel use of boat-mounted geophysical imaging has therefore proven to be a useful tool in determining saline water intrusion and in the characterization of spatial and temporal patterns of the abiotic factors affecting mangrove zonation pattern. Methodology An innovative measurement campaign using conventional sensors and high spatial resolution geophysical imaging was adopted to monitor the river water quality and salinity patterns. Seasonally at high tide, measurements were obtained from two river channels, a 6km larger main channel and a 2km shorter side channel (Fig. 1). •Electromagnetic Induction (boat-mounted geophysical imaging) was used to spatially map the salinity of the water non-invasively (Plate 1). River b water was spatially tested in situ for pH, dissolve oxygen (DO), conductivity, temperature and turbidity using a U-10 multi parameter water quality checker (Plate 2). 4 •Aerial photos were analyzed using GIS for the years 1962 and 2003 to determine mangrove boundary change (Fig. 2). Species abundance was identified using transects at 5m intervals along both sides of the river banks. Data analysis included geostatistics with SGEMS, graphs and GIS. Discussion Our results showed a significant decrease in mangrove species diversity as adverse water quality conditions prevailed. This is partly due to saline water intrusion particularly in the dry season, which takes place with increased tidal inundation extending as far as 6km upstream (Fig. 1). * 1. References Ewel, K.C., Twilley, L.L. and Ong, J.E. 1998. Different kinds of mangrove forests provide different goods and services. Global Ecology and Biogeography letters. 7:83-94. (a) (b) 2. “South Oropouche, Trinidad.” 2009. 61o29’56”N and 10o13’13”E. Google Earth. August 29, 2009. Accessed August 29 2009. 3. “South Oropouche, Trinidad.” 2010. 61o29’56”N and 10o13’13” E. Google Earth. February 19, 2010. Accessed February 19 2010. 4. Millennium Ecosystem Assessment "Synthesis Report" (2005) 16. Fig. 1: Spatial map of ECa along the main and side channels of the river in (a) wet season and (b) dry season. Blue represents low salinity while red represents high salinity. 20 1 0 0 Distance (m) pH Fig. 4: Percentage species abundance as a function of 0.00 500.00 1000.00 1500.00 2000.00 2500.00 pH (Side channel) 120 8.2 100 8.0 80 7.8 60 7.6 40 7.4 20 0 7.2 White Black 0.00 500.00 1000.00 Black Red DO 1500.00 2000.00 120 100 80 60 40 20 0 Distance (m) pH 2500.00 8 7 6 5 4 3 2 1 0 Distance (m) White Red Fig. 6: Percentage species abundance as a function of Dissolved Oxygen (DO) (Side channel) pH Distance (m) White Black Red 40 DO (mg/l) 6.8 57 18 0 48 22 7.0 41 15 20 33 47 7.2 24 43 40 60 White Black Red This adverse water quality may also be due to low levels of pH and DO in the stagnant side channel as a result of decomposition of organic matter and run-off from acidified mangrove soils (Figs. 4 and 6). In the side channel where adverse water quality conditions were prevalent, only the red mangrove predominates, indicating a loss of mangrove species diversity. DO DO (mg/l) 7.4 5 4 3 2 49 4 11 57 17 27 23 50 26 76 33 47 38 13 43 33 48 22 54 94 60 39 60 80 16 7.6 pH 80 % Abundance of dominant species 100 7.8 8 7 6 16 25 3 49 4 73 0 98 3 12 49 15 35 18 29 20 79 21 59 Fig.2: Aerial extent of mangrove boundary for the years 1962 (pink) and 2003 (pattern) 8.0 % Abundance of dominant species The pH and DO levels showed a marked decrease in the side channel than in the main channel of the river (Figs. 3-6). Rhizophora mangle L. (red) as opposed to Avicennia germinans (black) and Laguncularia racemosa (white) was found under adverse water quality conditions of low DO, pH levels and high levels of salinity (Figs. 3-6). 100 17 27 Aerial photos (Fig.2) showed an overall decrease of more than 10% in mangrove extent from 1962- 2003. The apparent electrical conductivity (ECa) levels were much lower in the main channel than in the side channel both in the wet and dry season (Fig. 1). In the dry season, however, saline water intrusion was very evident as salt water moved further inland (Fig. 1b). 120 73 0 Results 8.2 16 3 Fig. 5: 1000.00 Percentage species abundance as a function 2000.00 3000.00 4000.00 5000.00 6000.00of7000.00 0.00000 0000000 0000000 0000000 Dissolved Oxygen (DO)0000000 (Main 0000000 channel)0000000 0000000 000000 00 00 00 00 00 00 00 120 16 25 3 49 4 73 0 98 12 3 4 15 9 3 18 5 29 20 7 21 9 59 Plate 2. U-10 Water Quality Checker % Abundance of dominant species Plate 1. Boat-mounted geophysical imaging % Abundance of dominant species 1000.00 2000.00 3000.00 4000.00 5000.00 6000.00 7000.00 Fig.3: Percentage species abundance a function of pH 0.00000 0000000 0000000 0000000 0000000as0000000 0000000 0000000 000000 00 00 (Main 00channel) 00 00 00 00