Aquatic Biomes & Carbon Cycle
Water covers most of our planet, creating diverse habitats for life! Aquatic biomes are divided into freshwater (wetlands, streams, rivers, ponds, lakes) and marine (intertidal zones, estuaries, coral reefs, open ocean). Unlike terrestrial biomes that are defined by temperature and precipitation, aquatic biomes are characterized by depth, oxygen levels, light penetration, and nutrient availability.
Wetlands include marshes non−woodyplants, swamps (wooded areas), and bogs (acidic areas with sphagnum moss). In oceans, the photic zone receives sunlight allowing photosynthesis, while the aphotic zone is too deep for light to penetrate. Coral reefs and estuaries have high primary productivity and biodiversity because of their nutrient-rich waters.
The carbon cycle moves carbon atoms between different reservoirs on Earth. This biogeochemical cycle is self-regulating but can be disrupted by human activity. Carbon moves through fast cycles (biological processes like photosynthesis and respiration) and slow cycles (geological processes like sedimentation and fossil fuel formation).
During photosynthesis, producers convert carbon dioxide and water to glucose and oxygen. Through respiration, organisms break down glucose to release energy, producing carbon dioxide and water. Decomposition returns carbon to the atmosphere through respiration and to soil through breakdown of organic matter.
Fun fact: The ocean sediment and fossil fuels are Earth's largest carbon reservoirs, storing carbon for millions of years until released by combustion or weathering!