Kalpitiya Dutch Bay mangrove soil redox potential: anaerobic mud and stilt-root lenticels?
How do Rhizophora and Avicennia mangrove roots transport atmospheric oxygen into sulfide-rich waterlogged sediments in Dutch Bay during morning low-tide exposure?
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3 Answers from travellers
The intertidal sediments of Dutch Bay in Kalpitiya are severely anaerobic, characterized by negative redox potential (Eh below -200mV) and toxic hydrogen sulfide generated by sulfate-reducing bacteria. Mangroves survive using specialized root adaptations. Rhizophora mucronata develops looping stilt roots (prop roots) covered in hydrophobic lenticels (gas-exchange pores), while Avicennia marina sends up vertical pencil-like pneumatophores from horizontal roots. During morning low tide, lenticels open to absorb atmospheric oxygen, channeling it through internal sponge-like aerenchyma tissue down to root tips, creating an oxygenated buffer zone that neutralizes toxic sulfides.
Boat fuel spills coat root lenticels in petroleum residues, suffocating subterranean roots and triggering localized tree mortality across lagoon channels.
Fiddler crabs (Uca species) burrow around pneumatophores, aerating dense mud sediments and boosting nutrient cycling around root zones.
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