The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Question

Want to see the full answer?

Answer 1

Question

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Expert Solution & Answer

Want to see the full answer?

Check out a sample textbook solution

See solution

Students have asked these similar questions

Give two examples of those bacteria that can survive in hot sulphur springs.

Filtration to remove protozoa occurs in: Question 5 options: A) anaerobic sludge digestion. B) primary sewage treatment. C) secondary sewage treatment. D) water treatment.

Are coliform bacteria dangerous in the water?

Answer 2

Question

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Expert Solution & Answer

Want to see the full answer?

Check out a sample textbook solution

See solution

Answer 3

Question

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Expert Solution & Answer

Want to see the full answer?

Check out a sample textbook solution

See solution

Answer 4

Question

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Expert Solution & Answer

Want to see the full answer?

Check out a sample textbook solution

See solution

Answer 5

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Answer 6

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Answer 7

Chapter 20.13, Problem 1MQ

Summary Introduction

The lowest layer in the ocean that exists just above the seabed and below the thermocline is called as deep sea and its depth of 1000 fathoms or more. The addition to deep sea waters, another most and vast unexpected microbial biosphere that is present below the sea floor is called as deep sea sediments. The sea sediment materials are naturally occurring that is broken down by the processes of erosions and weathering. It is eventually transported by the cation of water, ice and wind through the force of gravity that are acting on the particle.

Answer 8

Expert Solution & Answer

Answer 9

Expert Solution & Answer

Answer 10

Want to see the full answer?

Check out a sample textbook solution

See solution

Answer 11

Ch. 20.1 - Prob. 1MQ Ch. 20.1 - Prob. 2MQ Ch. 20.1 - Prob. 3MQ Ch. 20.1 - How does a microbial population differ from a...Ch. 20.1 - Prob. 1CR Ch. 20.2 - Prob. 1MQ Ch. 20.2 - What is a biogeochemical cycle? Give an example...Ch. 20.2 - Prob. 1CR Ch. 20.3 - Prob. 1MQ Ch. 20.3 - Prob. 2MQ

Solution Summary: The author explains the microbial biosphere of deep sea sediments, which is broken down by erosions and weathering. The reduction of sulfate is one of the vital forms of anaerobic respiration

Concept explainers

Videos

Want to see the full answer?

Chapter 20 Solutions