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Explain how prokaryotes, which were the first known living organisms on Earth, could live despite the lack of oxygen.

Short Answer

Expert verified
Prokaryotes survived by using anaerobic respiration and fermentation, which don't require oxygen.

Step by step solution

01

Understanding Ancient Earth

Around 3.5 billion years ago, the Earth's atmosphere lacked oxygen. Life had to adapt to this anoxic (oxygen-free) environment in order to survive.
02

Metabolic Pathways in Prokaryotes

Prokaryotes developed metabolic pathways that did not rely on oxygen. One primary method is anaerobic respiration, which uses molecules other than oxygen, such as nitrate or sulfate, as the final electron acceptor in the electron transport chain.
03

Fermentation as an Alternative

Besides anaerobic respiration, prokaryotes also use fermentation, which allows for energy production without any electron transport chain. They convert glucose to energy by breaking it down into simpler substances like lactic acid or ethanol.
04

Energy Production Under Anoxic Conditions

Both anaerobic respiration and fermentation enable prokaryotes to extract energy from nutrients. Despite being less efficient than aerobic respiration, these processes were sufficient to support life when oxygen was absent.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Anaerobic Respiration
Anaerobic respiration is a fascinating process that allows organisms to live without oxygen. This type of respiration utilizes different molecules, such as nitrate or sulfate, to take the place of oxygen as the final electron acceptor in the electron transport chain. This means that prokaryotes, which were the first life forms on Earth, could still extract energy from nutrients despite the lack of oxygen.

Here's how it works in a nutshell:
  • Prokaryotes consume organic molecules, such as glucose, for energy.
  • The energy extraction occurs through a series of reactions known as the electron transport chain.
  • Instead of using oxygen at the end of the chain, they use alternative molecules like nitrate or sulfate.
Though anaerobic respiration is less energy-efficient than aerobic (oxygen-based) respiration, it has helped prokaryotes survive billions of years ago when Earth's atmosphere lacked oxygen.
Fermentation
Fermentation is an alternative energy pathway that does not require any oxygen or electron transport chain to produce energy. This process involves converting glucose into simpler substances like lactic acid or ethanol while extracting energy in the form of ATP.

Key aspects of fermentation include:
  • No need for oxygen or electron transport chain steps.
  • Produces less energy compared to aerobic respiration but is crucial for survival in anoxic conditions.
  • Provides essential byproducts like lactic acid (in muscles) or ethanol (in yeast).
Fermentation allowed ancient prokaryotes to efficiently use available resources for energy production, thus enabling their survival and evolution in early Earth's oxygen-free environment.
Anoxic Environment
An anoxic environment is an ecosystem devoid of any oxygen, which was the scenario on early Earth around 3.5 billion years ago. Since there was no oxygen in the atmosphere, early life forms needed to find alternative ways to sustain life.

Characteristics of anoxic environments include:
  • No free oxygen available for metabolic processes.
  • Presence of alternative electron acceptors like nitrate and sulfate.
  • Reliance on anaerobic processes for energy production.
Prokaryotes thrived in these conditions by developing anaerobic respiration and fermentation strategies. These processes enabled them to adapt and survive despite the seemingly inhospitable conditions.
Earth's Ancient Atmosphere
Earth's ancient atmosphere was vastly different from today's air which is rich in oxygen. Around 3.5 billion years ago, the atmosphere was primarily composed of gases like carbon dioxide, methane, and ammonia but lacked free oxygen.

Some important features of Earth's ancient atmosphere include:
  • No free oxygen, posing challenges for life as we know it today.
  • Existence of other gases that influenced the planet's climate and life forms.
  • Pressure on the first life forms to evolve methods like anaerobic respiration to survive.
This lack of oxygen required early prokaryotic life to develop unique metabolic processes that did not depend on oxygen. These adaptations contributed to their success in surviving the primordial Earth.

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Most popular questions from this chapter

Between 300 and 250 million years ago, plate movement assembled all the previously separated landmasses together to form the supercontinent Pangaea. The formation of Pangaea resulted in deeper ocean basins and a drop in sea level, causing shallow coastal areas to dry up. Thus, in addition to rearranging the geography of our planet, continental drift had a major impact on life on Earth. Use the accompanying diagrams and the information above to answer the following: a. Which of the following types of habitats would likely diminish in size during the formation of a supercontinent: deep-ocean habitats, wetlands, shallow marine environments, or terrestrial (land) habitats? Explain. b. During the breakup of a supercontinent, what would happen to sea level- would it remain the same, rise, or fall? c. Explain how and why the development of an extensive oceanic ridge system that forms during the breakup of a supercontinent affects sea level.

Contrast the eastern and western margins of North America during the Cenozoic era in terms of their relationships to plate boundaries.

Suggest a geologic reason why the rift valley system of East Africa is so rich in human ancestor fossils.

Describe two ways in which the sudden appearance of oxygen in the atmosphere about 2.5 billion years ago influenced the development of modern life-forms.

If life on Earth originated from simple chemical compounds such as methane and ammonia, or hydrogen sulphide, why don't we observe the origin of new forms of life today?

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