reef sediments - ορισμός. Τι είναι το reef sediments
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Τι (ποιος) είναι reef sediments - ορισμός

RIDGE OF ROCK IN THE SEA FORMED BY THE GROWTH AND DEPOSIT OF CORAL
Barrier Reef; Coral reefs; Coral Reef; Fringing Reef; Ribbon reef; Deltaic reef; Barrier reefs; Coral-Reefs; Lagoonal reef; Cresentic reef; Planar reef; Coral reef destruction; Apron reef; Formation of coral reefs; Darwin's paradox; Reef habitat zones; Habili; Coral Reef Ecology; Coral reef ecology; Barrier reef; Platform reef; Table reef; Bank reef; Tropical coral reef
  • isotherms]]. Most corals live within this boundary. Note the cooler waters caused by upwelling on the southwest coast of Africa and off the coast of Peru.
  • Ancient coral reefs
  • Deep-water [[cloud sponge]]
  • bay Islands]] are part of the mesoamerican coral reef system. Due to this, the authorities have made huge investments for its preservation.
  • Barrier reef
  • A major coral bleaching event took place on this part of the [[Great Barrier Reef]] in Australia
  • 250px
  • A diversity of corals}}
  • NOAA]] Ocean Education Service. Retrieved January 9, 2010.</ref>
  • Formation of an atoll according to [[Charles Darwin]]
  • Close up of polyps arrayed on a coral, waving their tentacles. There can be thousands of polyps on a single coral branch.
  • Coral fragments growing on nontoxic concrete
  • polyp]] anatomy
  • The three major zones of a coral reef: the fore reef, reef crest, and the back reef
  • Locations of coral reefs
  • [[Coralline algae]] ''[[Lithothamnion]] sp.''
  • Fringing reef at [[Eilat]] at the southern tip of [[Israel]]
  • Table coral, ''[[Acropora]] sp.''
  • Inhabited [[cay]] in the [[Maldives]]
  • A small [[atoll]] in the [[Maldives]]
  • The colour of corals depends on the combination of brown shades provided by their [[zooxanthellae]] and pigmented proteins (reds, blues, greens, etc.) produced by the corals themselves.
  • url=https://www.theguardian.com/environment/interactive/2009/sep/02/coral-world-interactive}}</ref>
  • [[Eastern oyster]]s (''Crassostrea virginica'')
  • Platform reef
  • Coral polyps}}
  • shoals]], that is, it slows down and the wave height increases.
  • Fringing reef
  • Most coral polyps are nocturnal feeders. Here, in the dark, polyps have extended their tentacles to feed on zooplankton.
  • sessile]] and take root on the ocean floor. But unlike plants, corals do not make their own food.<ref>[https://oceanservice.noaa.gov/facts/coral.html Are corals animals or plants?] ''NOAA:  National Ocean Service''. Accessed 11 February 2020. Updated: 7 January 2020.</ref>
  • This map shows areas of [[upwelling]] in red. Coral reefs are not found in coastal areas where colder and nutrient-rich upwellings occur.
  •  [[Zooxanthellae]], the microscopic algae that lives inside coral, gives it colour and provides it with food through photosynthesis

Reef shark         
  • Caribbean reef shark
WIKIMEDIA DISAMBIGUATION PAGE
Reef Shark; Reef sharks; Reef shark (disambiguation); Reef shark (SIA)
This article lists several species of reef-associated sharks which are known by the common name reef sharks.
Cyclic sediments         
  • High Atlas middle liassic carbonate platform of Morocco and succession of regressive, autocyclic, "shallowing upward" metric sequences.
  • Model of a virtual "shallowing upward" metric sequence observed on carbonate platforms all along the south tethyan margin (about 10.000km) during the Liassic. (Micro)fossils are identical from the Maghreb till Oman and furtheron.
  • "shallowing upward" sequences from two sections distant of 230 km; note the hurricane (tempestites and tsunami ?)levels with abundant displaced foraminifera on supratidal flat. Middle Liassic, Morocco.
  • 268x268px
SEQUENCES OF SEDIMENTARY ROCKS THAT ARE CHARACTERISED BY REPETITIVE PATTERNS OF DIFFERENT ROCK TYPES (STRATA) OR FACIES WITHIN THE SEQUENCE
Cyclic sedimentation; Cyclic sediment; Rhythmic sediment; Rhythmic sediments; Depositional cycle
Cyclic sediments (also called rhythmic sediments) are sequences of sedimentary rocks that are characterised by repetitive patterns of different rock types (strata) or facies within the sequence. Processes that generate sedimentary cyclicity can be either autocyclic or allocyclic, and can result in piles of sedimentary cycles hundreds or even thousands of metres thick.
Amazon Reef         
  • Map of the Amazon Reef, relative to [[Brazil]], [[French Guiana]] and [[Suriname]], with main reef structures highlighted in orange
  • abbr=on}} depth</small>
  • Atlantic]] represents a fifth of the outflow into the Earth's [[ocean]]s.
  • RV ''Atlantis'']], upon which the discovery team conducted research
Amazonian Reef
The Amazon Reef, or Amazonian Reef, is an extensive coral and sponge reef system, located in the Atlantic Ocean off the coast of French Guiana and northern Brazil. It is one of the largest known reef systems in the world, with scientists estimating its length at over , and its area as over .

Βικιπαίδεια

Coral reef

A coral reef is an underwater ecosystem characterized by reef-building corals. Reefs are formed of colonies of coral polyps held together by calcium carbonate. Most coral reefs are built from stony corals, whose polyps cluster in groups.

Coral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most reefs grow best in warm, shallow, clear, sunny and agitated water. Coral reefs first appeared 485 million years ago, at the dawn of the Early Ordovician, displacing the microbial and sponge reefs of the Cambrian.

Sometimes called rainforests of the sea, shallow coral reefs form some of Earth's most diverse ecosystems. They occupy less than 0.1% of the world's ocean area, about half the area of France, yet they provide a home for at least 25% of all marine species, including fish, mollusks, worms, crustaceans, echinoderms, sponges, tunicates and other cnidarians. Coral reefs flourish in ocean waters that provide few nutrients. They are most commonly found at shallow depths in tropical waters, but deep water and cold water coral reefs exist on smaller scales in other areas.

Coral reefs have declined by 50% since 1950, partly because they are sensitive to water conditions. They are under threat from excess nutrients (nitrogen and phosphorus), rising ocean heat content and acidification, overfishing (e.g., from blast fishing, cyanide fishing, spearfishing on scuba), sunscreen use, and harmful land-use practices, including runoff and seeps (e.g., from injection wells and cesspools).

Coral reefs deliver ecosystem services for tourism, fisheries and shoreline protection. The annual global economic value of coral reefs has been estimated at anywhere from US$30–375 billion (1997 and 2003 estimates) to US$2.7 trillion (a 2020 estimate) to US$9.9 trillion (a 2014 estimate).