NOTE: If you can read this, then you have not entered our site from the proper entry point! In order for all links to function properly, you must start by clicking here.
Carbon moves through our planet over longer time scales as well. For example, over millions of years weathering of rocks on land can add carbon to surface water which eventually runs off to the ocean. Over long time scales, carbon is removed from seawater when the shells and bones of marine animals and plankton collect on the sea floor. These shells and bones are made of limestone, which contains carbon. When they are deposited on the sea floor, carbon is stored from the rest of the carbon cycle for some amount of time. The amount of limestone deposited in the ocean depends somewhat on the amount of warm, tropical, shallow oceans on the planet because this is where prolific limestone-producing organisms such as corals live. The carbon can be released back to the atmosphere if the limestone melts or is metamorphosed in a subduction zone. |
Acidic Ocean Water Impacts Corals and Other Marine Life
A Podcast about how Northern forests and tropical forests play a part in the uptake of carbon.
Carbon is an element. It is part of oceans, air, rocks, soil and all living things. Carbon doesn’t stay in one place. It is always on the move!
Carbon moves through our planet over longer time scales as well. For example, over millions of years weathering of rocks on land can add carbon to surface water which eventually runs off to the ocean. Over long time scales, carbon is removed from seawater when the shells and bones of marine animals and plankton collect on the sea floor. These shells and bones are made of limestone, which contains carbon. When they are deposited on the sea floor, carbon is stored from the rest of the carbon cycle for some amount of time. The amount of limestone deposited in the ocean depends somewhat on the amount of warm, tropical, shallow oceans on the planet because this is where prolific limestone-producing organisms such as corals live. The carbon can be released back to the atmosphere if the limestone melts or is metamorphosed in a subduction zone. |
Acidic Ocean Water Impacts Corals and Other Marine Life
A Podcast about how Northern forests and tropical forests play a part in the uptake of carbon.
Carbon is part of the ocean, air, rocks, soil and all living things. Carbon doesn’t stay in one place. It is always on the move!
|
Acidic Ocean Water Impacts Corals and Other Marine Life
A Podcast about how Northern forests and tropical forests play a part in the uptake of carbon.