Syllabus Edition

First teaching 2023

First exams 2025

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Abiotic Factors: Marine & Terrestrial (HL IB Biology)

Revision Note

Naomi H

Author

Naomi H

Expertise

Biology

Coral Reef Formation

  • Corals are the result of a symbiotic relationship between an animal known as a coral polyp, and a zooxanthellae algae
    • The polyp provides shelter and protection
    • The algae carry out photosynthesis and produce carbon compounds such as carbohydrates
  • Some species of coral polyps secrete calcium carbonate which builds up in layers to form a hard outer structure; over time these deposits from thousands of individuals can form a coral reef
reef-building-corals-photograph

CC BY 2.0, via Wikimedia Commons

Some coral species secrete layers of calcium carbonate that forms the hard structure of coral reefs

Distribution of coral reefs

  • The distribution of reef-building corals is limited to the topics and subtropics
    • Non reef-building species can be found in other regions
  • The formation of coral reefs is limited by abiotic factors, including: 
    • Water depth
    • pH
    • Salinity (salt concentration)
    • Water clarity
    • Temperature
  • Coral has a narrow range of tolerance for all of these abiotic factors, resulting in its limited distribution

Coral reef distribution mapdistribution-of-hot-and-cold-coral-reefs

The distribution of reef building corals is limited by abiotic factors

Abiotic factors affecting coral reef formation table

Abiotic factor Effect on reef formation
Water depth Corals can only grow at shallow depths where light can penetrate the water at high enough levels for the zooxanthellae to photosynthesise.
pH

The hard outer layer secreted by coral polyps is made from calcium carbonate, which dissolves when the pH is too low.

Corals need carbonate ions to build calcium carbonate. The H+ ions that are present at lower pH levels combine with carbonate ions to form hydrogen carbonate ions, reducing the availability of carbonate ions for reef-building.

Increased carbon dioxide released from the burning of fossil fuels dissolves in the oceans and lowers the pH pf the water, reducing coral growth.
Salinity

Since corals are marine animals they need salty water, within a 32-42 % range, to survive.

Freshwater run-off from land can reduce salt concentrations and limit coral growth.
Water clarity

Water clarity must be good for light to penetrate through the water.

Sediment from land run-off, and water pollution, can reduce water clarity and limit coral growth.
Temperature

Corals have a range of tolerance of roughly 20-28 °C, though they grow best in water temperatures above 23 °C.

While they can withstand short periods of higher temperatures, rising sea temperatures causes the polyps to expel their algae symbionts, leading to coral bleaching.

Terrestrial Biome Distribution

  • The term biome can be defined as follows:

A large community of plants and animals that has occurred as a result of environmental factors

  • Biomes occur over large geographical areas, and are usually named after their dominant vegetation type, e.g. a geographical area dominated by tropical rainforest will be a tropical rainforest biome
  • Examples of biomes include:
    • Temperate rainforest
    • Tropical rainforest
    • Temperate deciduous forest
    • Boreal, or coniferous forest, sometimes known as taiga
    • Grassland, e.g. temperate or savanna
    • Tundra
    • Desert, e.g. hot desert or cold desert
  • Biome distribution is affected by abiotic factors in the environment

Biome distribution map

Biome distribution map

The distribution of biomes is affected by abiotic factors

  • Average temperatures and rainfall patterns are significant factors in determining the development of a biome
    • For any given combination of these two factors, a specific biome will result
  • Biome development can be plotted on a graph known as a climograph, with mean annual rainfall and temperature on its axes

Biome development graph

effect-of-temperature-and-precipitation-on-global-biome-distribution

For any given temperature and rainfall pattern, a particular biome will develop

  • The likely biome at any given rainfall and temperature can be determined from the climograph, e.g.
    • At a mean average rainfall of 200 cm and mean average temperature of 25 °C, tropical seasonal forest will develop
    • At a mean average rainfall of 300 cm and mean average temperatures of 15 °C, temperate rainforest will develop
    • At a mean average rainfall of 100 cm and mean average temperatures of 0 °C, taiga, or boreal forest, will develop
  • Bear the following points about climographs in mind when drawing conclusions:
    • Climographs shows a distinct boundary between biome types, but the reality is that there will be a gradual shift from one biome type to another
    • Rainfall and temperature are not the only factors that influence biome development; the dotted lines in the graph above show situations where other variables, such as soil type and animal grazing, may play an important role
    • Because neither rainfall or temperature can be described as being an independent variable or a dependent variable, the allocation of temperature and rainfall to the graph axes may vary
      • The graph above has rainfall on the x axis and temperature on the y axis, but this could just as correctly be plotted the other way around
      • The graph above has temperature plotted from high to low on the y axis, but this could be plotted from low to high

Exam Tip

Be sure to read the axis labels and values carefully before drawing conclusions from climographs.

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Naomi H

Author: Naomi H

Naomi graduated from the University of Oxford with a degree in Biological Sciences. She has 8 years of classroom experience teaching Key Stage 3 up to A-Level biology, and is currently a tutor and A-Level examiner. Naomi especially enjoys creating resources that enable students to build a solid understanding of subject content, while also connecting their knowledge with biology’s exciting, real-world applications.