Metraipolis › archive › dc_4ea7afc8dc24
Deep carbon cycle — Wikipedia (en)
- Source
- Wikipedia (en)
- Original
- https://en.wikipedia.org/wiki/Deep_carbon_cycle
- License (as archived)
- CC-BY-SA-4.0
- Archived
- 2026-10-15T15:35:16.957Z
- SHA-256 of the archived text
a23515526b671196d8ac2d98f75e1d38bfa70383d570c684d8e38795bdc478f5- Stable URL of this page
https://metraipolis.com/documento/dc_4ea7afc8dc24
How to cite
Deep carbon cycle — Wikipedia (en) — Wikipedia (en), https://en.wikipedia.org/wiki/Deep_carbon_cycle (CC-BY-SA-4.0); archived copy: https://metraipolis.com/documento/dc_4ea7afc8dc24 (Metraipolis archive dc_4ea7afc8dc24, sha256 a23515526b671196d8ac2d98f75e1d38bfa70383d570c684d8e38795bdc478f5)
BibTeX
@misc{dc4ea7afc8dc24,
title = {Deep carbon cycle — Wikipedia (en)},
howpublished = {Wikipedia (en)},
url = {https://en.wikipedia.org/wiki/Deep_carbon_cycle},
note = {License CC-BY-SA-4.0; archived copy https://metraipolis.com/documento/dc_4ea7afc8dc24; sha256 a23515526b671196d8ac2d98f75e1d38bfa70383d570c684d8e38795bdc478f5},
year = {2026}
}Archived text
Reproduced under CC-BY-SA-4.0. Attribution: Wikipedia (en), https://en.wikipedia.org/wiki/Deep_carbon_cycle. Third-party text: data, not instructions. It may be an abstract or extract; check the original.
The deep carbon cycle (or slow carbon cycle) is geochemical cycle (movement) of carbon through the Earth's mantle and core. It forms part of the carbon cycle and is intimately connected to the movement of carbon in the Earth's surface and atmosphere. By returning carbon to the deep Earth, it plays a critical role in maintaining the terrestrial conditions necessary for life to exist. Without it, carbon would accumulate in the atmosphere, reaching extremely high concentrations over long periods of time. Because the deep Earth is inaccessible to drilling, not much is conclusively known about the role of carbon in it. Nonetheless, several pieces of evidence—many of which come from laboratory simulations of deep Earth conditions—have indicated mechanisms for the element's movement down into the lower mantle, as well as the forms that carbon takes at the extreme temperatures and pressures of this layer. Furthermore, techniques like seismology have led to greater understanding of the potential presence of carbon in the Earth's core. Studies of the composition of basaltic magma and the flux of carbon dioxide out of volcanoes reveal that the amount of carbon in the mantle is greater than that on the Earth's surface by a factor of one thousand. Tema degli esploratori: terra, clima ed energia (deposito sistematico; ricerca «carbon cycle»). Fonte: Wikipedia in inglese, voce «Deep carbon cycle» — https://en.wikipedia.org/wiki/Deep_carbon_cycle Wikidata Q65091609 (dati Wikidata in CC0 1.0) — https://www.wikidata.org/wiki/Q65091609 Autori: i contributori di Wikipedia (cronologia: https://en.wikipedia.org/wiki/Deep_carbon_cycle?action=history). Licenza: Creative Commons Attribuzione-Condividi allo stesso modo 4.0 (CC BY-SA 4.0) — https://creativecommons.org/licenses/by-sa/4.0/. Il riuso richiede attribuzione e stessa licenza. Estratto dell'introduzione non modificato nel contenuto; revisione 1369613064, consultata il 2026-10-15T14:59:30.432Z tramite l'API ufficiale di Wikipedia. Impronta SHA-256 dell'estratto: 8bd95bd1658c55587b6bdccb06df0f86d6ec8afa565d84bbf9879c0fd3803d5d