The fate of the atmospheric CO 2 that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Question

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Answer 1

Question

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

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Answer 2

Question

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

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Answer 3

Question

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

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Answer 4

Question

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

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Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!

Answer 5

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

Answer 6

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

Answer 7

Chapter 12, Problem 1QR

To determine

The fate of the atmospheric CO₂ that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.

Answer 8

Expert Solution & Answer

Answer to Problem 1QR

All the atmospheric CO₂ that was present in earliest Earth has now been stored in physical forms over geological time.

Answer 9

Expert Solution & Answer

Answer 10

Expert Solution & Answer

Answer 11

Explanation of Solution

Early Earth had CO₂ in abundance. With the passing time and geological activities, all this CO₂ has been fixed in different forms. Major part of this CO₂ (about 80%) is now found in chemically bound form in limestone in deep oceans. Limestone is chemically formed of Calcium Carbonate (CaCO₃). During the early times, CO₂ from the atmosphere started dissolving in the ocean water and sediments of CaCO₃ were formed. This decreased the amount of CO₂ in the atmosphere.

When life originated in oceans, the early photosynthesizing organisms also started using CO₂ from the atmosphere, resulting in further decrease in levels of CO₂ in the atmosphere.

Answer 12

Ch. 12 - Prob. 1QR Ch. 12 - Prob. 2QR Ch. 12 - Prob. 3QR Ch. 12 - Prob. 4QR Ch. 12 - Prob. 5QR Ch. 12 - Prob. 6QR Ch. 12 - Prob. 7QR Ch. 12 - Prob. 8QR Ch. 12 - Prob. 9QR Ch. 12 - Prob. 10QR

The fate of the atmospheric CO 2 that was loaded in the intense greenhouse climatic atmosphere of earliest Earth.