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  2. Carbon sequestration - Wikipedia

    en.wikipedia.org/wiki/Carbon_sequestration

    Carbon sequestration is part of the natural carbon cycle by which carbon is exchanged among the biosphere, pedosphere (soil), geosphere, hydrosphere, and atmosphere of Earth. [citation needed] Carbon dioxide is naturally captured from the atmosphere through biological, chemical, or physical processes, and stored in long-term reservoirs.

  3. Mangrove forest - Wikipedia

    en.wikipedia.org/wiki/Mangrove_forest

    Mangrove plants require a number of physiological adaptations to overcome the problems of low environmental oxygen levels, high salinity, and frequent tidal flooding.Each species has its own solutions to these problems; this may be the primary reason why, on some shorelines, mangrove tree species show distinct zonation.

  4. Bioturbation - Wikipedia

    en.wikipedia.org/wiki/Bioturbation

    Walrus bioturbations in Arctic benthic sediments have large-scale ecosystem effects. [ 1 ] Bioturbation is defined as the reworking of soils and sediments by animals or plants. It includes burrowing, ingestion, and defecation of sediment grains. Bioturbating activities have a profound effect on the environment and [ 2 ] are thought to be a ...

  5. Seagrass meadow - Wikipedia

    en.wikipedia.org/wiki/Seagrass_meadow

    Seagrass meadows provide coastal storm protection by the way their leaves absorb energy from waves as they hit the coast. They keep coastal waters healthy by absorbing bacteria and nutrients, and slow the speed of climate change by sequestering carbon dioxide into the sediment of the ocean floor.

  6. Salt marsh - Wikipedia

    en.wikipedia.org/wiki/Salt_marsh

    An estuarine salt marsh along the Ōpāwaho / Heathcote River, Christchurch, New Zealand Salt marsh on Sapelo Island, Georgia, US. Salt marshes occur on low-energy shorelines in temperate and high-latitudes [5] which can be stable, emerging, or submerging depending if the sedimentation is greater, equal to, or lower than relative sea level rise (subsidence rate plus sea level change ...

  7. Carbon sink - Wikipedia

    en.wikipedia.org/wiki/Carbon_sink

    The amount of carbon dioxide varies naturally in a dynamic equilibrium with photosynthesis of land plants. The natural carbon sinks are: Soil is a carbon store and active carbon sink. [8] Photosynthesis by terrestrial plants with grass and trees allows them to serve as carbon sinks during growing seasons.

  8. Soil - Wikipedia

    en.wikipedia.org/wiki/Soil

    Soil, also commonly referred to as earth or dirt, is a mixture of organic matter, minerals, gases, liquids, and organisms that together support the life of plants and soil organisms. Some scientific definitions distinguish dirt from soil by restricting the former term specifically to displaced soil.

  9. Oceanic carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Oceanic_carbon_cycle

    The oceanic carbon cycle (or marine carbon cycle) is composed of processes that exchange carbon between various pools within the ocean as well as between the atmosphere, Earth interior, and the seafloor. The carbon cycle is a result of many interacting forces across multiple time and space scales that circulates carbon around the planet ...