MarketMudflat
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Mudflat

Mudflats or mud flats, also known as tidal flats or, in Ireland, slob or slobs, are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers. A global analysis published in 2019 suggested that tidal flat ecosystems are as extensive globally as mangroves, covering at least 127,921 km2 (49,391 mi2) of the Earth's surface. They are found in sheltered areas such as bays, bayous, lagoons, and estuaries; they are also seen in freshwater lakes and salty lakes alike, wherein many rivers and creeks end. Mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and aquatic animal detritus. Most of the sediment within a mudflat is within the intertidal zone, and thus the flat is submerged and exposed approximately twice daily.

Ecology
on Stewart Island, New Zealand Tidal flats, along with intertidal salt marshes and mangrove forests, are important ecosystems. They support a large population of wildlife, and are a key habitat that allows tens of millions of migratory shorebirds to migrate from breeding sites in the northern hemisphere to non-breeding areas in the southern hemisphere. They are often of vital importance to migratory birds, as well as certain species of crabs, mollusks and fish. In the United Kingdom mudflats have been classified as a Biodiversity Action Plan priority habitat. The maintenance of mudflats is important in preventing coastal erosion. However, mudflats worldwide are under threat from predicted sea level rises, land claims for development, dredging due to shipping purposes, and chemical pollution. It is estimated that up to 16% of the world tidal flats have disappeared since the mid-1980s. The associated growth of coastal sediment deposits can be attributed to rates of subsidence along with rates of deposition (example: silt transported via river) and changes in sea level. Barren zones extend from the lowest portion of the intertidal zone to the marsh areas. Beginning in close proximity to the tidal bars, sand dominated layers are prominent and become increasingly muddy throughout the tidal channels. Common bedding types include laminated sand, ripple bedding, and bay mud. Bioturbation also has a strong presence in barren zones. Marshes contain an abundance of herbaceous plants while the sediment layers consist of thin sand and mud layers. Mudcracks are a common as well as wavy bedding planes. Marshes are also the origins of coal/peat layers because of the abundant decaying plant life. Salt pans can be distinguished in that they contain thinly laminated layers of clayey silt. The main source of the silt comes from rivers. Dried up mud along with wind erosion forms silt dunes. When flooding, rain or tides come in, the dried sediment is then re-distributed. File:ISS013-E-75163 - View of Tunisia.jpg|alt=Satellite view of the Kneiss Islands, Tunisia|Satellite view of the Kneiss Islands, Tunisia. File:Skagit_Bay_6308.JPG|Gulls feeding on mudflats in Skagit Bay, Washington, United States Image:brewster mudflat.jpg|Mudflats in Brewster, Massachusetts, United States, extending hundreds of yards offshore at the low tide. The line of Wrack (seaweed) and seashells in the foreground indicates the high-water mark. ==Cultural Services==
Cultural Services
Tidal flats provide cultural services that reflect a sense of place, foster social interactions, and support well-being. Intergenerational practices of tidal flat gleaning and fishing are central to tidal flat-dependent communities. Hence, enabling cultural preservation and identity for the coastal communities, which are intricately linked with the tidal flats ecosystem. ==Selected example areas==
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