Tomaga-River Inter-Tidal Wetlands
Hydrosphere
River/creek flow provides rich alluvial soil, with nutrients
lithospher provides ground water to woodlands
Water body moderates temperatures
tidal flow waterlogs soil twice daily necessitating mangrove pneumatophors
open delta allows free movement of the tides and deposition of sand sediment
Flood/ storm events may erode the upstream lithosphere increasing turbidity and threatening the photosynthesis
Atmosphere
insolation can reduce soil moisture
Local landforms (mts) increase likelihood of orographic rainfall, may effect shade and exposure on Tidal Wetlands and influence humidity levels.
Lithosphere
lithospher is affected by the amount of tidal erosion
Biosphere
lithosphere is a habitat for high Biodiversity eg, semiphore and soldier crabs
Decomposing flora/fauna increase soil fertility. Crabs/whelks airate the soil allowing for increased decomposition
certain plants must adopt to soil conditions
samphire turns red and drops leaves to combat hypersalinity eg Grey mangrove absorbs and salt through leaves