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The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Microbes and the Carbon Cycle01:24

Microbes and the Carbon Cycle

The carbon cycle is a fundamental Earth process involving the transfer of carbon among the biosphere, lithosphere, atmosphere, and hydrosphere. It plays a critical role in regulating the planet’s climate and supporting life by cycling carbon through various chemical forms and reservoirs. Carbon primarily circulates as carbon dioxide (CO₂), representing its oxidized form, while reduced forms such as methane (CH₄) and organic compounds also play essential roles.Microbial activity is central to...
Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
What are Biogeochemical Cycles?00:54

What are Biogeochemical Cycles?

The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
The Calvin Benson Cycle01:46

The Calvin Benson Cycle

Ribulose 1,5- bisphosphate carboxylase/oxygenase (RuBisCo) is a critical enzyme that catalyzes carbon dioxide assimilation during photosynthesis. However, it is an inefficient enzyme, having an extremely slow catalytic rate. A typical enzyme can process about a thousand molecules per second; however, RuBisCo fixes only around three-carbon dioxides per second. Photosynthetic cells compensate for this slow rate by synthesizing very high amounts of RuBisCo, making it the most abundant single...
The Phosphorus Cycle01:21

The Phosphorus Cycle

Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.

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Related Experiment Video

Updated: Jun 7, 2026

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
07:32

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.

Published on: June 4, 2021

A carbon cycle science update since IPCC AR-4.

A J Dolman1, G R van der Werf, M K van der Molen

  • 1Department of Earth Sciences, VU University Amsterdam, The Netherlands. han.dolman@falw.vu.nl

Ambio
|November 9, 2010
PubMed
Summary

Global carbon cycle research shows rising CO2 emissions and increasing methane levels. Uncertainties remain regarding carbon sinks, but forests and permafrost store more carbon than previously estimated.

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Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
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Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

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Last Updated: Jun 7, 2026

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
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Published on: June 4, 2021

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Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
11:19

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses

Published on: October 21, 2016

Area of Science:

  • Earth System Science
  • Climate Science
  • Environmental Science

Background:

  • The global carbon cycle is critical for understanding climate change.
  • Advances since the IPCC AR4 report necessitate a review of current knowledge.
  • Anthropogenic activities significantly impact carbon fluxes.

Purpose of the Study:

  • To review key advances in global carbon cycle understanding since IPCC AR4.
  • To synthesize findings on carbon emissions, sinks, and storage.
  • To identify uncertainties and future research directions.

Main Methods:

  • Literature review of recent scientific publications.
  • Analysis of data on CO2 and methane emissions.
  • Synthesis of findings on ocean and land carbon sinks.
  • Evaluation of carbon storage in permafrost and forests.

Main Results:

  • Fossil fuel CO2 emissions increased near the high end of IPCC scenarios.
  • Methane emissions are rising, with potential increases from northern wetlands.
  • Forests (old-growth and tropical) show higher carbon uptake than expected.
  • Ocean CO2 uptake is better understood, but regional variability exists.
  • Permafrost carbon stores are estimated to be twice as large as previously thought.
  • Large-scale fires and droughts negatively impact carbon uptake.

Conclusions:

  • Preserving marine ecosystems may require CO2 stabilization below 450 ppm.
  • Dynamic Vegetation Models show significant divergence in future carbon trajectories.
  • Key uncertainties include process descriptions, CO2 fertilization, and nitrogen-carbon interactions.