Is it possible to forge a new kind of relationship with the ecological community we in English call, perhaps, unceremoniously, peat bog?
Here in cool Britannic islands, peat has been forming since the last Ice Age, when luminous green mosses took over the quagmire. Fibrous layers of arrested entropy are fuelled by the surfacing of a froth of bryophytes, metabolizing through an exchange of oxygen with carbon dioxide, sunshine for sugar, nutrients, bacteria, and plenty of water. As each generation and their symbiotic partners die down, the decay is slow but sure in locking in carbon. … Read more