The Carbon Cycle, or: Where Does a Tree Go When It Goes
A six-atom dance through oceans, leaves, and the occasional diesel engine.
Every carbon atom in your body was once, in some older life, folded into rock. Before that, perhaps air. Before that, the hot breath of a star. The carbon cycle is not so much a cycle as a dense, slow-motion traffic pattern across a dozen reservoirs: atmosphere, forests, soils, the shallow and the deep ocean, shells and shoots and bones and bones.
In photosynthesis, plants pluck CO2 from the air and thread it into sugars. Animals eat the sugars and exhale the carbon back out, slightly rearranged. Some carbon falls into the soil and, given the right geological patience, reappears millions of years later as a lump of coal, or a seam of graphite, or — with sufficient pressure — a diamond.
Humans have accelerated the cycle's fastest loop considerably. Since 1750 we have transferred roughly 700 gigatonnes of carbon from the slow reservoirs into the fast ones. The planet is noticing. The carbon, for its part, is indifferent. It has been through worse eras than this one, and will outlast us whether we apologize or not.
What is beautiful about the element, if "beautiful" is the word, is its patience. Four valences, one modest atomic number, and an almost infinite capacity for self-combination. From these simple rules come pencils, petroleum, proteins, and the sentence you are reading right now.
Last edited: 2026-04-18
Contributors: 4
Revision: #0x1F4C