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However, we have in these two situations done the following: To represent the concentrations of TotHg and MeHg in the 8-10 m depth area in 2011 we used the mean concentrations of the 6.5 and 10.5 m depth measurements and we used half the concentrations in the 2-4 m depth area to represent the 0-2 m depth area in 2012.
For example, no measurement was done in the 8-10 m depth area in 2011 or in the 0-2 depth area in 2012.
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These results match the tree branching patterns with the highest Chondrichthyan diversity seen in the 300 600 m depth areas and the lowest seen at depth.
Since the carbon content has remained at a high value from 3.5 m depth onwards, the area was probably covered with rich vegetation.
The regional aquifer was identified at about 100 m depth around lowland areas, although prone to polluting effects from farming activities, erosion and weathering processes.
While the initial stage specific abundance is known from the survey results for the areas >60 m depth, the abundance for the area <60 m depth was set to be 0. The initial horizontal distributions as obtained by the first surveys were entered into the model as a tracer and the exchange rates between the areas were calculated over time.
The bipartite graphs show the occurrence of each phototrophic OTU in the algal farms of herbivorous cichlid species (upper bipartite graphs), and the occurrence of those OTUs in the stomachs of the cichlid species (lower bipartite graphs) living in the shallower area (2.4 ± 1.6 m depth, Figure 4A) and deeper area (11.2 ± 5.4 m depth, Figure 4B).
Furthermore, a number of scour holes of around 0.5 m depth found in the area throughout all MBES surveys do not indicate any lateral mounds (Fig. 3c,d).
Due to their small aperture (0.5 1 m width, 0.15 1 m depth) and limited surface area covered, they could underestimate loads of rarer and larger plastic objects such as bottles, buoys and fishing nets.
Specific correlations include a second order polynomial relationship between Hmax at the 100 m depth contour and inundation area as well as linear relationships between Hmax at the 100 m depth contour and up-river attenuation rates for runup and maximum water levels.
Map a (25 m depth) shows the small area of the shallow, low resistivity (< 30 Ωm, colored orange) anomaly at Fang Hot Springs.
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