Featured
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Correspondence |
Reply to 'Circadian control of global isoprene emissions'
- C. N. Hewitt
- , K. Ashworth
- & O. Wild
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News & Views |
Mercury in flux
Mercury concentrations in the Arctic atmosphere exhibit a pronounced peak during summer. Model simulations suggest that this can be explained only if boreal rivers deliver large quantities of mercury to the Arctic Ocean.
- Jeroen E. Sonke
- & Lars-Eric Heimbürger
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News & Views |
Earth's titanium twin
A giant impact on the young proto-Earth is thought to explain the formation of the Moon. High-precision analysis of titanium isotopes in lunar rocks suggests that the Moon and Earth's mantle are more similar than existing models permit.
- Matthias M. M. Meier
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Letter |
Abundant Early Palaeogene marine gas hydrates despite warm deep-ocean temperatures
Gas hydrates have been suggested as a carbon source for Palaeogene hyperthermal events, but warm seafloor temperatures are thought to have limited their accumulation. Numerical simulations suggest that enhanced organic carbon sedimentation and methanogenesis could have compensated for the smaller area of hydrate stability.
- Guangsheng Gu
- , Gerald R. Dickens
- & Walter G. Chapman
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Letter |
Acidification of subsurface coastal waters enhanced by eutrophication
Eutrophication increases the acidity of coastal waters. Model simulations suggest that the drop in pH in coastal waters of the northern Gulf of Mexico since pre-industrial times is greater than that expected from eutrophication and ocean acidification alone.
- Wei-Jun Cai
- , Xinping Hu
- & Gwo-Ching Gong
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Correspondence |
Reply to 'Aquifer arsenic source'
- Rebecca B. Neumann
- , Khandaker N. Ashfaque
- & Charles F. Harvey
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News & Views |
Wake-up call for isoprene emissions
Naturally produced hydrocarbons such as isoprene influence air quality and climate. Accounting for circadian control of isoprene emissions helps to bring model simulations of ground-level ozone into closer agreement with observations.
- Alexander T. Archibald
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Letter |
Transient metazoan reefs in the aftermath of the end-Permian mass extinction
Microbes were thought to be the dominant reef constructors following the end-Permian mass extinction. Sponge–microbe reef deposits formed in the Early Triassic from the western United States suggest that instead, metazoan-reef building continued immediately following the extinction wherever marine conditions allowed.
- Arnaud Brayard
- , Emmanuelle Vennin
- & Gilles Escarguel
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Letter |
Strong elemental fractionation of Zr–Hf and Nb–Ta across the Pacific Ocean
Trace elements and their isotopes have been explored as tracers for the movement of water masses. Measurements of the high-field-strength elements Zr, Hf, Nb and Ta along two meridional sections of the Pacific Ocean suggest higher ratios of Zr/Hf and Nb/Ta than expected, suggesting that these ratios will be useful for tracking water masses.
- M. Lutfi Firdaus
- , Tomoharu Minami
- & Yoshiki Sohrin
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Letter |
Hydrogen isotope ratios in lunar rocks indicate delivery of cometary water to the Moon
Water has been found in many lunar rock samples, but its sources are unknown. Isotopic analyses of Apollo samples of lunar mare basalts and highlands rocks suggest that a significant volume of water was delivered to the Moon by comets shortly after its formation by giant impact.
- James P. Greenwood
- , Shoichi Itoh
- & Hisayoshi Yurimoto
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News & Views |
Mid-latitude mercury loss
Bromine facilitates the oxidation of elemental mercury in the lower atmosphere in polar and subpolar regions. Measurements over the Dead Sea suggest that bromine also generates large quantities of oxidized mercury in the mid-latitudes.
- Parisa A. Ariya
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Editorial |
Deep-sea discoveries
The sea floor is emerging as a source of carbon to the overlying ocean. Scientific exploration of the sea bed is essential for a full understanding of the global carbon budget and the safety of deep-sea carbon storage proposals.
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Letter |
Methane hydrate-bearing seeps as a source of aged dissolved organic carbon to the oceans
Marine sediments contain large quantities of carbon, primarily in the form of gas hydrate. Isotopic analyses suggest that carbon derived from fossil methane accounts for up to 28% of the dissolved organic carbon in sea water overlying hydrate-bearing seeps in the northeastern Pacific Ocean.
- John W. Pohlman
- , James E. Bauer
- & N. Ross Chapman
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Letter |
Bromine-induced oxidation of mercury in the mid-latitude atmosphere
In the polar atmosphere, non-reactive gaseous elemental mercury is converted to a highly reactive form of mercury by halogens such as bromine. Measurements over the Dead Sea suggest that bromine also triggers reactive mercury formation over the mid-latitude ocean.
- Daniel Obrist
- , Eran Tas
- & Menachem Luria
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Letter |
Chemosynthetic origin of 14C-depleted dissolved organic matter in a ridge-flank hydrothermal system
Hydrothermal fluids circulate through the upper portion of the oceanic crust. Isotopic analyses suggest that chemosynthetic microbial communities in the crust synthesize dissolved organic carbon in hydrothermal ridge-flank fluids.
- Matthew D. McCarthy
- , Steven R. Beaupré
- & Ellen R. M. Druffel
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Editorial |
Trouble at depth
The deep ocean is largely uncharted territory. The aftermath of the BP oil spill has been a poignant reminder that its relative inaccessibility hinders exploration, but does not extend much protection from human interference.
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Commentary |
Short-lived uncertainty?
Short-lived greenhouse gases and black-carbon aerosols have contributed to past climate warming. Curbing their emissions and quantifying the forcing by all short-lived components could both mitigate climate change in the short term and help to refine projections of global warming.
- Joyce E. Penner
- , Michael J. Prather
- & David S. Stevenson
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Letter |
Phanerozoic concentrations of atmospheric oxygen reconstructed from sedimentary charcoal
Varying concentrations of atmospheric oxygen have affected the development of animals and the role of wildfire in ecosystems. Reconstructions of past oxygen concentrations from fossil charcoal constrain atmospheric oxygenation over the past 400 million years.
- Ian J. Glasspool
- & Andrew C. Scott
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Letter |
Warming influenced by the ratio of black carbon to sulphate and the black-carbon source
Black-carbon aerosols absorb solar radiation and are thought to be a significant source of global warming. Surface and aircraft measurements of aerosol plumes in China suggest that solar absorption increases with the ratio of black carbon to sulphate.
- M. V. Ramana
- , V. Ramanathan
- & J. J. Schauer
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News & Views |
Balancing ocean nitrogen
The ocean's nitrogen budget has escaped quantification. A modelling study shows how a small shift in the nitrate-to-phosphate uptake ratio of phytoplankton has a large effect on calculated nitrogen fixation rates.
- Wolfgang Koeve
- & Paul Kähler
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Letter |
Asphalt volcanoes as a potential source of methane to late Pleistocene coastal waters
Natural petroleum seepage emits large volumes of oil and methane to the oceans every year, accompanied by the formation of asphalt volcanoes on the sea floor. The discovery of seven asphalt volcanoes off the coast of southern California may help to explain high methane emissions recorded during the late Pleistocene.
- David L. Valentine
- , Christopher M. Reddy
- & Morgan Soloway
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Letter |
Origin of acidic surface waters and the evolution of atmospheric chemistry on early Mars
The sedimentary deposits at Meridiani Planum on Mars were formed in acidic surface waters. Geochemical calculations show that the oxidation of dissolved iron and the precipitation of oxidized iron minerals in the surface waters could be sufficient to generate the inferred acidity.
- Joel A. Hurowitz
- , Woodward W. Fischer
- & Ralph E. Milliken
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Books & Arts |
Albertan oil
Anna Armstrong reviews Dirty Oil by Leslie Iwerks, Dogwoof: 2010. UK release date: 19 March 2010.
- Anna Armstrong
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Letter |
Hydrothermal contribution to the oceanic dissolved iron inventory
Mineral dust and marine sediment resuspension are generally considered the primary sources of the nutrient iron to the oceans. Numerical model results suggest that iron released by hydrothermal activity is also an important source of dissolved iron, particularly in the Southern Ocean.
- Alessandro Tagliabue
- , Laurent Bopp
- & Catherine Jeandel
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Letter |
Insolation and CO2 contribution to the interglacial climate before and after the Mid-Brunhes Event
The five interglacial periods that occurred after the Mid-Brunhes Event 430,000 years ago were longer and warmer than the preceding interglacials. Climate modelling indicates that a change in the seasonality of insolation following the event, in conjunction with higher greenhouse-gas concentrations, could have caused the relative warmth.
- Q. Z. Yin
- & A. Berger
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Letter |
Atmospheric nanoparticles formed from heterogeneous reactions of organics
Nanoparticles are a key component of atmospheric aerosols, growing rapidly under ambient conditions. Exposure of nanoparticles to organic vapours shows that various organic species can enhance the growth of nanoparticles.
- Lin Wang
- , Alexei F. Khalizov
- & Renyi Zhang
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Letter |
Deforestation driven by urban population growth and agricultural trade in the twenty-first century
Reducing tropical deforestation is at present considered a cost-effective option for mitigating climate change. Satellite-based estimates of forest loss suggest that urban population growth and urban and international demand for agricultural products are key drivers of deforestation in the tropics.
- Ruth S. DeFries
- , Thomas Rudel
- & Matthew Hansen
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Backstory |
Spoilt beauty
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Letter |
Long-term persistence of oil from the Exxon Valdez spill in two-layer beaches
Oil spilt from the tanker Exxon Valdez more than 20 years ago still persists in the gravel beaches of Prince William Sound, Alaska. Field data and numerical modelling indicate that some of the oil was trapped in the anoxic environment of the lower layers of the beaches when the water table was low.
- Hailong Li
- & Michel C. Boufadel
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Editorial |
Digging deeper
Arsenic contamination of groundwater affects millions of people in southern Asia. Water from deep wells could help, but only if used in moderation.
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Commentary |
The socio-economics of arsenic removal
Nearly an eighth of the population in Bangladesh relies on arsenic-contaminated drinking water. Arsenic-removal filters could help to reduce exposure, but their price is high for the poor and their maintenance is cumbersome.
- Richard Bart Johnston
- , Suzanne Hanchett
- & Mohidul Hoque Khan