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On what does the success of bioremediation of oil spills depond? a. Success depends on the presence of only aromatic and highly branched hydrocarbon chain compounds and the temperature. b. Success depends on the presence of less nonvolatile and more aromatic and highly branched hydrocarbon chain compounds and the temperature. c. Success depends on the type of oil compounds, the presence of naturally- occurring oil- solubilizing prokaryotes in the ocean, and the type of water body. d. Success depends on the type of oil compounds, solubilizing prokaryotes in the ocean and the temperature.

Short Answer

Expert verified
The correct answer is c.

Step by step solution

01

- Identify key factors

Analyze the given options to identify the key factors required for successful bioremediation of oil spills. Look for mentions of oil compound types, prokaryotes, water body, and temperature.
02

- Eliminate irrelevant factors

Eliminate options that include irrelevant factors. For instance, options discussing specific hydrocarbon chains or nonvolatile compounds may not cover the broader requirements for bioremediation.
03

- Compare the relevant factors

Compare the remaining options to determine which one encompasses all necessary factors such as type of oil compounds, presence of solubilizing prokaryotes, type of water body, and temperature.
04

- Determine the correct answer

Select the option that contains all identified key factors for the successful bioremediation of oil spills.

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Key Concepts

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

oil compound types
Bioremediation of oil spills heavily depends on the type of oil compounds present. Oil is a complex mixture of various hydrocarbons, including:
  • Saturated hydrocarbons: These are relatively easy to break down by microorganisms.
  • Aromatic hydrocarbons: These compounds have ring structures and are more challenging to degrade but can be broken down by specialized bacteria.
  • Asphaltenes and resins: These are heavier fractions that are very resistant to biodegradation.
Because different microorganisms have varying abilities to degrade specific compounds, the success of bioremediation relies on the presence and balance of these mixed hydrocarbon types. Efficient bioremediation requires identifying the types of hydrocarbons present in the oil spill to tailor the microbial approach accordingly. Recognizing whether the oil contains more biodegradable fractions or more complex substances helps in selecting the right bioremediation strategy.
naturally-occurring oil-solubilizing prokaryotes
Naturally-occurring oil-solubilizing prokaryotes play an essential role in bioremediation. Prokaryotes such as bacteria possess the metabolic pathways needed to break down complex oil compounds. Key genera involved include:
  • Pseudomonas: Known for its ability to degrade a wide array of hydrocarbons.
  • Alcanivorax: Specialized in breaking down alkanes, a major component of crude oil.
  • Mycobacterium: Known for degrading polycyclic aromatic hydrocarbons.
These bacteria either exist naturally in marine environments or can be introduced to aid the bioremediation process. Their efficiency is influenced by factors such as nutrient availability and environmental conditions. For example, nitrogen and phosphate fertilizers are sometimes added to boost microbial growth and activity. Successfully harnessing these microbes requires understanding their ecological roles and optimizing conditions to enhance their oil-degrading capabilities.
environmental conditions
Environmental conditions have a significant impact on the success of oil spill bioremediation. Key factors include:
  • Temperature: Affects the metabolic rates of microorganisms. Both extremely low and high temperatures can hinder microbial activity.
  • Oxygen Levels: Critical for aerobic microbes that require oxygen to break down oil. In oxygen-poor environments, anaerobic microbes can still play a role, but the degradation process is slower.
  • pH Levels: Most oil-degrading microbes prefer neutral to slightly alkaline pH levels.
  • Salinity: Marine oil spills are heavily affected by the salinity of the water, which can influence microbial communities.
Bioremediation efforts need to consider these factors to create conducive conditions for microbial activity. For example, in colder climates, bioremediation might slow down unless specific cold-tolerant bacteria are employed. Similarly, the addition of oxygen or nutrients can enhance microbial growth and accelerate oil degradation. Managing these environmental parameters is crucial for the effective implementation of bioremediation strategies in diverse habitats.

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Most popular questions from this chapter

68\. In an experiment, researchers grew plant seedlings in soils to which one of two strains of bacteria were added. A control group had no bacteria added to the soil. The seedlings’ uptake of the nutrient potassium increased dramatically in the soil with Strain 1 and decreased dramatically in the soil with Strain 2. What specific and broad inferences about the relationship between the bacteria, the seedlings, and available nutrients can you make? a. The Strain 2 bacteria increased the availability of potassium in the soil and this nutrient was needed and used by the seedlings in the soil. The Strain 1 bacteria decreased the availability of potassium in the soil. b. The soil with Strain 1 bacteria must have had more potassium in comparison to soil with Strain 2 bacteria. The seedlings took up more potassium in Soil 1 than in 2 due to this. c. The Strain 1 bacteria increased the availability of potassium in the soil and this nutrient was needed and used by the seedlings in the soil. The Strain 2 bacteria decreased the availability of potassium in the soil. d. The Strain 1 bacteria decreased the availability of potassium in the soil and this nutrient was needed and used by the seedlings in the soil. The Strain 2 bacteria increased the availability of potassium in the soil

In a hypothetical research situation, scientists discover bacterial endospores in silt at the bottom of a marsh that has been contaminated with a pollutant for 25 years. The silt of the marsh was deposited in annual layers. The age of the endospores can be estimated, then, by identifying the layer of silt in which the endospores are found. In flask A, researchers place 20-year-old endospores along with growth medium and the pollutant. In flask B, researchers place 100-year-old endospores along with growth medium and the pollutant. Explain why you would expect to see more growth in one particular flask than in the other. a. Because endospores formed 20 years ago would be more dormant compared to endospores formed 100 years ago, before the marsh was polluted. b. Because endospores formed 20 years ago would be less adapted to polluted conditions compared to endospores formed 100 years ago, before the marsh was polluted. c. Because endospores formed 20 years ago would be more adapted to polluted conditions compared to endospores formed 100 years ago, before the marsh was polluted. d. Because endospores formed 20 years ago would be less dormant compared to endospores formed 100 years ago, before the marsh was polluted.

Which best defines bioremediation? a. the use of microbial metabolism to clean up oil spills b. the use of microbial metabolism to ferment food c. the use of microbial metabolism to remove pollutants d. the use of microbial metabolism to fix nitrogen

Explain the relationship between Earth's ancient atmosphere and the evolution of some of the first life forms on Earth. Use the terms anaerobicandphototrophic, and explain the effect of cyanobacteria on the atmosphere. a. Phototrophic organisms appeared during the first two billion years of Earth's existence. Anaerobic organisms appeared within one billion years of Earth's formation. From these organisms evolved the cyanobacteria which produce oxygen as a by-product of photosynthesis, leading to the oxygenation of the atmosphere. b. For the first two billion years of Earth's existence, the atmosphere had no molecular oxygen. Thus, the first organisms were anaerobic. Cyanobacteria appeared within one billion years of Earth's formation. From these evolved the phototrophic organisms which produce oxygen as a by-product of photosynthesis, leading to the oxygenation of the atmosphere. c. For the first two billion years of Earth’s existence, the atmosphere had no molecular oxygen. Thus, the first organisms were anaerobic. Phototrophic organisms appeared within one billion years of Earth’s formation. From these organisms evolved the cyanobacteria, which produce oxygen as a byproduct of photosynthesis, leading to the oxygenation of the atmosphere. d. For the first two billion years of Earth’s existence, the atmosphere had no molecular oxygen. Thus, the first organisms were anaerobic. Cyanobacteria which produce oxygen as a by-product of photosynthesis, leading to the oxygenation of the atmosphere, appeared within one billion years of Earth’s formation. From these organisms evolved phototrophic organisms

Which is a macronutrient needed by prokaryotes? a. phosphorus b. iron c. chromium d. boron

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