News & Views |
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News & Views |
Unexpectedly abiotic
Sulphur cycling on early Earth is commonly linked to microbial activity. However, sulphur isotope values from 3.2–3.5-billion-year-old rocks indicate a central role for the breakdown of volcanic sulphur dioxide by ultraviolet radiation instead.
- Boswell Wing
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Letter |
Dust- and mineral-iron utilization by the marine dinitrogen-fixer Trichodesmium
Blooms of the nitrogen-fixing cyanobacterium Trichodesmium, which fuel primary production in tropical and subtropical waters, require large quantities of iron. Laboratory incubations suggest that Trichodesmium accelerates the dissolution of iron oxides and dust, increasing the rate of iron uptake.
- Maxim Rubin
- , Ilana Berman-Frank
- & Yeala Shaked
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Article |
Influence of subsurface biosphere on geochemical fluxes from diffuse hydrothermal fluids
Hydrothermal vents along mid-ocean ridge systems host highly productive communities of microbes. Measurements along the Juan de Fuca ridge suggest that subsurface microbes consume hydrogen in low-temperature hydrothermal fluids, before discharge of these fluids at the sea floor.
- Scott D. Wankel
- , Leonid N. Germanovich
- & Peter R. Girguis
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Letter |
Sedimentary membrane lipids recycled by deep-sea benthic archaea
Archaea are prevalent in the deep sea, and comprise a major fraction of the biomass in marine sediments. 13C-labelling experiments on the sea floor suggest that benthic archaea use sedimentary organic compounds to construct their membranes.
- Yoshinori Takano
- , Yoshito Chikaraishi
- & Naohiko Ohkouchi
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Backstory |
Methane-munching microbes
Nardy Kip, Julia F. van Winden, Huub J. M. Op den Camp and an array of colleagues braved hostile acidic peat bogs around the world in a feat of truly collaborative research.
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Letter |
Global prevalence of methane oxidation by symbiotic bacteria in peat-moss ecosystems
The degradation of submerged Sphagnum mosses generates significant quantities of methane in peat bogs. A global survey of these mosses reveals the presence of an active population of methane-oxidizing bacteria.
- Nardy Kip
- , Julia F. van Winden
- & Huub J. M. Op den Camp
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News & Views |
Phosphorus burial
The formation and burial of calcium phosphate minerals removes large quantities of phosphorus from the ocean. Radiotracer experiments reveal that bacteria in marine sediments mediate the production of these mineral phases at remarkably fast rates.
- Ellery D. Ingall
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Letter |
Microbial sequestration of phosphorus in anoxic upwelling sediments
Organic phosphorus is removed from the ocean by its conversion to phosphorite. Laboratory incubations suggest that bacteria catalyse phosphorite formation, and that the rate of conversion is greatest under anoxic conditions.
- Tobias Goldhammer
- , Volker Brüchert
- & Matthias Zabel
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Letter |
Extracellular electron transfer through microbial reduction of solid-phase humic substances
The decay of soil and sedimentary organic matter yields organic compounds with a high molecular weight, termed humic substances. Sediment-incubation experiments suggest that microbial reduction of solid-phase humics can accelerate iron(III) oxide reduction in wetland soils.
- Eric E. Roden
- , Andreas Kappler
- & Huifang Xu
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Letter |
Magnitude of oceanic nitrogen fixation influenced by the nutrient uptake ratio of phytoplankton
The ratio of nitrogen to phosphorus in phytoplankton varies greatly with taxa and growth conditions. An ecosystem model suggests that the relative abundance of fast- and slow-growing phytoplankton controls the amount of new nitrogen added to the ocean.
- Matthew M. Mills
- & Kevin R. Arrigo
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Letter |
Soil-carbon response to warming dependent on microbial physiology
The loss of carbon dioxide from soils increases initially under climate warming, but tends to decline to control levels within a few years. Simulations of the soil-carbon response to warming with a microbial-enzyme model show that a decline in both microbial biomass and the production of degrading enzymes can explain this attenuation response.
- Steven D. Allison
- , Matthew D. Wallenstein
- & Mark A. Bradford
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