Aerial image of a tidal marsh at Bird Island Reserve, NC. Tidal marshes occur worldwide, and store large amounts of carbon in their soils. This type of carbon is called blue carbon – named for the color of the ocean and can store carbon for millennia.
Soil scientists use augers to collect soil “cores” for study. This one was collected from a tidal marsh in the Albemarle-Pamlico Sound, NC. The darker material is decaying plant material – stored carbon – contained in the marsh. The lighter color is mineral soil further down in the soil profile.
L. Gorczynski (blue shirt) examines soil in a tidal salt marsh soil on Pea Island National Wildlife Refuge, NC with B. Parrish (orange shirt). A root mat can be seen at the right end of the yellow measuring tape as labeled. The grey layer, mineral soil, has less carbon.
Newswise — October 3, 2022 – “Blue carbon” is a term for carbon captured by the world’s oceans and coastal ecosystems. Mangrove forests, tidal marshes, and seagrass beds are the main vegetated coastal areas that store vast amounts of blue carbon. It’s not really blue – it’s named after the color of the ocean. The Soil Science Society of America’s (SSSA) October 3rd Soils Matter blog explores how blue carbon is an important tool in reducing the effects of climate change.
According to soil scientist and blogger Lori Gorczynski, carbon moves through a cycle on the Earth. It is exchanged between the atmosphere, oceans, and land surface in different forms. Carbon dioxide (CO2) in the atmosphere is used by plants for their metabolism. Plants then store the carbon in various forms of carbohydrates and proteins. When they decompose, the carbon is released back into the atmosphere, creating a carbon cycle.
Terrestrial forests have long been recognized for their role in the carbon cycle. Despite their small global extent, blue carbon ecosystems store much larger quantities of carbon per unit area compared to upland forests!
Blue carbon ecosystems are highly productive in storing carbon. They capture and store carbon in their living, above-ground biomass (stems, leaves, and branches), like an upland forest. It’s what goes on below the surface that makes coastal ecosystems more efficient at carbon storage than their terrestrial counterparts.
In a terrestrial forest, the plant litter on the ground is exposed to air and decomposes like typical plant litter. In oceans and coastal ecosystems, the soil is often under water all the time, or exposed to continuous tidal wetting. These soils are deficient in oxygen, which is needed to decompose the plant litter.
So, plant litter in blue carbon ecosystems doesn’t decompose as fast as its terrestrial counterparts. Without oxygen, the soil microorganisms responsible for the breakdown of organic matter are not able to work as efficiently. This allows carbon to build up and be locked away in the soils over longer periods of time – making them great at carbon storage.
Between half and 99% of the blue carbon stored within mangrove forests, tidal marshes, and seagrass beds, is located belowground in the soils and sediments. If undisturbed, these areas act as long-term carbon sinks. Here carbon can be sequestrated for millennia!
Blue carbon ecosystems are also influenced by ocean tides and currents (i.e., “blue” comes from the color of the ocean), which can carry organic carbon from outside sources into the ecosystem to be buried and stored.
In addition to their valuable role in the global carbon cycle, blue carbon ecosystems provide many additional ecosystem services. These include flood and storm surge protection as well as filtration of pollutants and sediments. They are an essential habitat that supports biodiversity and fisheries. Despite this, they are among the most threatened ecosystems in the world.
One-third of mangrove, tidal marsh, and seagrass areas over the past several decades to dredging, filling, development, and pollution are already lost. In addition, climate change and associated sea level rise has the potential to flood and erode tidal marshes and mangrove forests. When these ecosystems are damaged or eroded, the carbon that was once stored is released back into the carbon cycle, where it can enter the atmosphere as CO2. Because of this, it’s important to restore and protect these ecosystems so they may continue to store blue carbon and act as a carbon “sink.”
If you are wondering how much blue carbon is stored in these coastal areas, the Natural Resource Conservation Service (NRCS) Coastal Zone Soil Survey Focus Team (CZSS) is one group working to determine just that. Moving forward, as climate change and its effects are addressed, knowledge of blue carbon will be essential.
To read the entire blog visit here: https://soilsmatter.wordpress.com/2022/10/01/what-is-blue-carbon-and-why-is-it-important/
Follow SSSA on Facebook at https://www.facebook.com/SSSA.soils, Twitter at SSSA_Soils. SSSA has soils information on www.soils.org/discover-soils, for teachers at www.soils4teachers.org, and for students through 12th grade, www.soils4kids.org.
The Soil Science Society of America (SSSA) is a progressive international scientific society that fosters the transfer of knowledge and practices to sustain global soils. Based in Madison, WI, and founded in 1936, SSSA is the professional home for 6,000+ members and 1,000+ certified professionals dedicated to advancing the field of soil science. The Society provides information about soils in relation to crop production, environmental quality, ecosystem sustainability, bioremediation, waste management, recycling, and wise land use.
MEDIA CONTACT
Register for reporter access to contact detailsArticle Multimedia
Credit: B. Parrish
Caption: Aerial image of a tidal marsh at Bird Island Reserve, NC. Tidal marshes occur worldwide, and store large amounts of carbon in their soils. This type of carbon is called blue carbon – named for the color of the ocean and can store carbon for millennia.
Credit: L. Gorczynski
Caption: Soil scientists use augers to collect soil “cores” for study. This one was collected from a tidal marsh in the Albemarle-Pamlico Sound, NC. The darker material is decaying plant material – stored carbon – contained in the marsh. The lighter color is mineral soil further down in the soil profile.
Credit: M. Ricker
Caption: L. Gorczynski (blue shirt) examines soil in a tidal salt marsh soil on Pea Island National Wildlife Refuge, NC with B. Parrish (orange shirt). A root mat can be seen at the right end of the yellow measuring tape as labeled. The grey layer, mineral soil, has less carbon.
RSS