Editorial |
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News & Views |
Enriched carbon source detected
Estimates of carbon in the deep mantle vary by more than an order of magnitude. Coupled volcanic CO2 emission data and magma supply rates reveal a carbon-rich mantle plume source region beneath Hawai'i with 40% more carbon than previous estimates.
- Peter H. Barry
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News & Views |
Ocean dissolved organics matter
Large quantities of organic carbon are stored in the ocean, but its biogeochemical behaviour is elusive. Size–age–composition relations now quantify the production of tiny organic molecules as a major pathway for carbon sequestration.
- Rainer M. W. Amon
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News & Views |
Carbon losses in the Alps
Soil carbon stocks depend on inputs from decomposing vegetation and return to the atmosphere as CO2. Monitoring of carbon stocks in German alpine soils has shown large losses linked to climate change and a possible positive feedback loop.
- Guy Kirk
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News & Views |
Bacterial bloom and crash
Microbes quickly consumed much of the methane released in the 2010 Gulf of Mexico oil spill. Time-series measurements now suggest that, after a steep rise, methane oxidation rates crashed while hydrocarbon discharge was still continuing at the wellhead.
- Evan A. Solomon
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Review Article |
The biogeochemical cycle of iron in the ocean
Iron controls phytoplankton growth in large tracts of the global ocean, and thereby influences carbon dioxide drawdown. Recent advances reveal the importance of iron-binding ligands and organic matter remineralization in regulating ocean iron levels.
- P. W. Boyd
- & M. J. Ellwood
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Letter |
Photolytic degradation of methylmercury enhanced by binding to natural organic ligands
Methylmercury is a neurotoxin that accumulates in food webs and poses a significant risk to human health. Laboratory experiments suggest that complexation of methylmercury with sulphur-containing ligands can stimulate its degradation.
- Tong Zhang
- & Heileen Hsu-Kim
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Letter |
Mass-independent fractionation of mercury isotopes in Arctic snow driven by sunlight
In the Arctic spring, sunlight-induced reactions convert gaseous elemental mercury into compounds that are rapidly deposited on the snowpack. Analysis of the isotopic composition of mercury in snow samples collected during an atmospheric mercury depletion event suggests that sunlight triggers the re-emission of mercury from the snowpack.
- Laura S. Sherman
- , Joel D. Blum
- & Thomas A. Douglas
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