Question: How does life contribute to the stability of the environment and especially through the sequestering of Carbon.
PLEASE ANSWER the questions correlty and please answer all the questions with what it regards in saying exactly, please and thank you take your time. Ive read the guide lines and honor code that i can have up to Submit only one question at a time under the appropriate subject. A question can have up to 3 subparts (i.e. part a, b, and c). If you dont belive me here is the link of barthleby saying exactly that thanks: https://bartleby.zendesk.com/hc/en-us/articles/360017462394-How-can-I-ensure-my-questions-get-answered-as-quickly-as-possible-
Answer correctly and read the questions corretly, this is all one quesiton if done correclty and organized I will write a very nice review about you! Answer in 20 mintues just a few sentence would do for each question thanks


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