The bio-geochemical cycle of carbon is one of the most
important research theme. This is because carbon dioxide in the
atmosphere has a greenhouse effect. The history of the terrestrial carbon cycle is also the history of climate change. It shows
where and how much carbon is stored, as well as where it is moving and how fast
it is doing so. The carbon in fossils lying dormant in the crust is released
into the atmosphere as carbon dioxide, and part of it is stored in the ocean,
used by living things, and returned to the atmosphere again. This kind of material circulation influenced by biological activity is called the bio-geochemical cycle.