How Coral Reefs are formed - labelled diagram and explanation

Geographer Online
1 Dec 201502:13

Summary

TLDRThis video explores the fascinating process of coral reef formation, highlighting the specific conditions required for their growth. It introduces three main types: fringing reefs that touch land, barrier reefs with a gap from land due to sea level changes or island sinking, and atolls formed when the sea level further exceeds the land mass. The script uses visual examples like the Great Barrier Reef to illustrate these formations, showing how they evolve in sequence in tropical waters.

Takeaways

  • 🐠 Coral reefs are made up of polyps and are considered animals.
  • 🌡️ They require very specific conditions to grow.
  • 🏝️ There are three different types of coral reefs.
  • 🌊 Fringing reefs form next to or touching the land, typically in tropical waters.
  • 📸 Fringing reefs are seen in the photo with no gap between the coral and the land.
  • 🐢 Barrier reefs have a gap between the land and the coral, such as the Great Barrier Reef.
  • 📈 Barrier reefs can form due to rising sea levels or the sinking of an island.
  • 🔄 Atolls form when the sea level rises further or the island sinks completely.
  • ⚪ Atolls have a circular formation with no central landmass, resembling a circular tropical island.
  • ⏳ Coral reefs tend to form in sequence, with each type having distinct characteristics.

Q & A

  • What are coral reefs?

    -Coral reefs are formations made up of polyps, which are small animals that require specific conditions to grow and thrive.

  • What is the meaning of 'fringing reef'?

    -A fringing reef is a type of coral reef that forms next to or adjacent to land, with no gap between the reef and the land.

  • In what type of waters do fringing reefs typically form?

    -Fringing reefs form in tropical waters, specifically in the Coral Sea area, as indicated by the purple marking on the script's map.

  • What is the Great Barrier Reef an example of?

    -The Great Barrier Reef is an example of a barrier reef, which is a type of coral reef that has a separation between the land and the coral.

  • What could cause the formation of a barrier reef?

    -A barrier reef can form due to a rise in sea level or the sinking of an island, resulting in a gap between the land and the coral.

  • How does a barrier reef differ from a fringing reef?

    -A barrier reef differs from a fringing reef in that it has a gap or separation from the land, whereas a fringing reef is in direct contact with the land.

  • What is an atoll?

    -An atoll is a ring-shaped coral reef that forms when the sea level rises further or the island continues to sink, resulting in a circular formation with no land in the middle.

  • What are the conditions necessary for coral to grow upwards from a fringing reef to form a barrier reef?

    -For coral to grow upwards from a fringing reef to form a barrier reef, it needs to maintain the sea surface temperature, light level, and other conditions necessary for its survival.

  • What is the sequence of coral reef formation as described in the script?

    -The sequence of coral reef formation starts with a fringing reef, then potentially evolves into a barrier reef, and finally may form an atoll.

  • What does the script suggest about the relationship between coral reefs and land?

    -The script suggests that the type of coral reef formed is influenced by the relationship between the coral and the land, with different types of reefs forming based on whether the coral is adjacent to the land or separated from it.

  • How does the script illustrate the formation of coral reefs?

    -The script illustrates the formation of coral reefs through the use of photographs and descriptions of the different types of reefs, including fringing reefs, barrier reefs, and atolls.

Outlines

00:00

🌊 Formation of Coral Reefs

This paragraph introduces the video's focus on coral reef formation, explaining that corals are animals with specific growth requirements. It outlines three main types of coral reefs: fringing, barrier, and atoll. Fringing reefs form adjacent to land in tropical waters, as seen in the provided photo with no gap between the reef and the land. Barrier reefs, exemplified by the Great Barrier Reef off Australia, have a gap between the land and the coral, possibly due to sea level rise or island subsidence. Atolls form when the sea level continues to rise or the island sinks further, creating a circular coral structure surrounding a central lagoon without landmass, as depicted in the photo with arrows indicating the sequence of reef formation.

Mindmap

Keywords

💡Coral Reefs

Coral reefs are diverse underwater ecosystems composed of colonies of coral polyps, which are small, living animals. They are integral to the video's theme as the formation and types of coral reefs are the central focus. The script mentions that coral reefs require specific conditions to grow, highlighting their sensitivity to environmental factors.

💡Polyps

Polyps are the fundamental building blocks of coral reefs, being the tiny animals that create the coral structure through their exoskeletons. The script emphasizes that coral reefs are made up of these living organisms, which underscores the biological aspect of coral formation.

💡Fringing Reef

A fringing reef is a type of coral reef that is in direct contact with the shore, as mentioned in the script when discussing the formation next to tropical islands. It is a key concept as it represents the initial stage in the sequence of coral reef development discussed in the video.

💡Tropical Waters

Tropical waters are warm marine environments where coral reefs typically form. The script specifies that fringing, barrier, and atoll reefs form in these waters, indicating the importance of temperature in coral growth and survival.

💡Barrier Reef

A barrier reef is a type of coral reef that has a significant gap between the reef and the shore, as exemplified by the Great Barrier Reef off the coast of Australia. The script explains that barrier reefs form when there is a separation between the land and the coral, usually due to geological events like sea level rise or island subduction.

💡Sea Level Rise

Sea level rise is a geological process that increases the depth of the ocean, which can affect coral reefs by causing them to grow upwards to maintain optimal living conditions. The script uses this term to explain how barrier reefs form when corals adapt to higher sea levels.

💡Island Subduction

Island subduction refers to the geological process where an island sinks due to tectonic activity. The script mentions this as a possible reason for the formation of barrier reefs when the corals attempt to grow upwards to reach the light and optimal water temperature.

💡Atoll

An atoll is a ring-shaped coral reef or a series of islets that encircle a lagoon, partially or completely. The script describes atolls as formations that occur when the island continues to sink or the sea level rises further, exceeding the land mass and creating a circular coral structure.

💡Coral Sea Area

The Coral Sea Area is a region in the tropical waters where coral reefs are known to form, as indicated by the script. This geographical reference is important as it provides a specific context for the types of coral reefs being discussed.

💡Sequence

The term 'sequence' in the script refers to the developmental stages of coral reefs, from fringing to barrier to atoll. It illustrates the evolutionary process of coral reef formation over time and geological changes.

💡Environmental Conditions

Environmental conditions such as sea surface temperature and light levels are critical for coral growth, as highlighted in the script. These conditions are the non-geological factors that influence the health and development of coral reefs.

Highlights

Coral reefs are formed by polyps, which are small animals with specific growth conditions.

Three main types of coral reefs are discussed: fringing, barrier, and atoll.

Fringing reefs form adjacent to land in tropical waters, as seen in the Coral Sea area.

Fringing reefs have no gap between the coral and the land, as illustrated in the provided photo.

Barrier reefs, like the Great Barrier Reef, form with a separation from the land due to geological events.

Geological events such as sea level rise or island subduction can lead to the formation of barrier reefs.

Barrier reefs grow upwards from fringing reefs to maintain optimal sea surface temperature and light levels.

Atolls form when the sea level continues to rise or the land sinks further, exceeding the land mass.

Atolls have a circular formation with no land, resembling a tropical coral island.

The formation of coral reefs tends to occur in a sequence, starting from fringing to atoll.

The video provides visual examples of each coral reef type, aiding understanding of their formation and characteristics.

Coral reefs require specific environmental conditions to thrive, emphasizing the fragility of these ecosystems.

The video explains the importance of sea surface temperature and light for coral growth.

Geological changes play a crucial role in the transformation from one type of coral reef to another.

The formation process of coral reefs is a dynamic and ongoing interaction between the corals and their environment.

Understanding the formation of coral reefs is vital for conservation efforts and environmental protection.

The video offers insights into the complex processes behind the creation of these diverse and vital ecosystems.

Coral reefs are not only biologically diverse but also play a significant role in coastal protection and tourism.

Transcripts

play00:00

hello everyone in this video we're going

play00:02

to be looking at the formation of coral

play00:03

reefs

play00:04

remember coral reefs are polyps and they

play00:07

are animals and they require very very

play00:09

specific conditions for them to grow

play00:12

now as you can see we get three

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different types of coral reefs

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to begin with we're going to start with

play00:17

a fringing wreath

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now the word fringing means next to or

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adjacent to or you know touching

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so fringing reef is going to form in the

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tropical waters in the coral sea area

play00:29

in these areas that are marked by this

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purple and they're going to form right

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next to say a tropical island or

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something like that

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and they're going to be touching the

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land

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you can also see this in the photo above

play00:42

there's no gap between the coral reef

play00:44

and the land

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the second type of coral reef we're

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going to look at are barrier reefs

play00:50

an example of this obviously the very

play00:51

famous example of this is a great

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barrier reef just over the coast of

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australia

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again these form in tropical waters

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in this case though something must have

play01:00

occurred for the coral to to have this

play01:02

gap to have a separation between the

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land and the coral

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what can happen is one of maybe two

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different types of events

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um the sea level could rise meaning that

play01:13

the coral needs to then grow upwards

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or the island could have sunk due to

play01:17

some element of subduction

play01:19

in both of these instances the coral

play01:21

would have tried to grow upward safe

play01:23

from a fringing reef to replace or to

play01:26

get sorry to the leveled sea level and

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sea surface temperature and the light

play01:30

level that it needs to survive

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you can see in the photo that a barrier

play01:34

reef is obviously creates a barrier and

play01:36

separates the land from the coral

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number three you get the formation of an

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atoll

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again these can form because the island

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has continued to sink or the sea level

play01:45

has risen even further

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and in this case the coral

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or the sea level sorry exceeds the

play01:52

land mass and uh you get this kind of

play01:55

formation circular formation as you can

play01:57

see in the photo with no land and it

play02:00

looks like a nice little circular

play02:01

tropical coral island

play02:03

as you can see by the arrows these tend

play02:05

to form in sequence

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Related Tags
Coral ReefsTropical WatersPolypsFringing ReefsBarrier ReefsAtollsSea LevelIsland SinkingCoral GrowthMarine EcologyEnvironmental Science