Featured
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Letter |
Quantification of ocean heat uptake from changes in atmospheric O2 and CO2 composition
An independent estimate based on atmospheric O2 and CO2 measurements suggests that global oceans absorbed about 0.83 watts per square metre of heat over the past three decades—at the high end of previous estimates.
- L. Resplandy
- , R. F. Keeling
- & A. Oschlies
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Letter |
CO2 storage and release in the deep Southern Ocean on millennial to centennial timescales
Analysis of deep-sea coral boron isotope data, as a proxy for pH and thus CO2 chemistry, provides evidence of CO2 storage in the deep Southern Ocean during the last ice age, and its rapid release on millennial to centennial timescales during deglaciation.
- J. W. B. Rae
- , A. Burke
- & B. J. Taylor
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Letter |
Glacial expansion of oxygen-depleted seawater in the eastern tropical Pacific
A downward expansion of oxygen depletion in the eastern Pacific Ocean during the last ice age suggests an increase in the respired carbon reservoir, contributing to the lower levels of atmospheric carbon dioxide during this period.
- Babette A. A. Hoogakker
- , Zunli Lu
- & Eric Galbraith
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Letter |
Widespread seasonal compensation effects of spring warming on northern plant productivity
Widespread but contrasting delayed responses of ecosystem productivity to spring warmth across northern ecosystems is inferred from satellite data, with higher areal fractions of adverse effects than beneficial effects.
- Wolfgang Buermann
- , Matthias Forkel
- & Andrew D. Richardson
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Letter |
Sensitivity of atmospheric CO2 growth rate to observed changes in terrestrial water storage
The growth rate of global atmospheric CO2 concentration is faster in drier years, independently of temperature; this relationship is underestimated in current carbon cycle models.
- Vincent Humphrey
- , Jakob Zscheischler
- & Sonia I. Seneviratne
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Letter |
Reverse weathering as a long-term stabilizer of marine pH and planetary climate
Elevated rates of reverse weathering within silica-rich oceans led to enhanced carbon retention within the ocean–atmosphere system, promoting a stable, equable ice-free climate throughout Earth’s early to middle ages.
- Terry T. Isson
- & Noah J. Planavsky
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Letter |
Global land change from 1982 to 2016
Satellite data for the period 1982–2016 reveal changes in land use and land cover at global and regional scales that reflect patterns of land change indicative of a human-dominated Earth system.
- Xiao-Peng Song
- , Matthew C. Hansen
- & John R. Townshend
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News & Views |
Hyperactive soil microbes might weaken the terrestrial carbon sink
The rate at which carbon dioxide is lost from soil has risen faster than the rate at which it is used by land plants, because soil microbes have become more active — possibly weakening the land surface’s ability to act as a carbon sink.
- Kiona Ogle
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Letter |
Extensive loss of past permafrost carbon but a net accumulation into present-day soils
Comparing the northern permafrost region of the Last Glacial Maximum with the same area today shows that the soil carbon stock has now increased, suggesting that permafrost carbon made no net contribution to preindustrial atmospheric carbon.
- Amelie Lindgren
- , Gustaf Hugelius
- & Peter Kuhry
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Letter |
Globally rising soil heterotrophic respiration over recent decades
Global soil respiration is rising, probably in response to environmental changes, suggesting that climate-driven losses of soil carbon are occurring worldwide.
- Ben Bond-Lamberty
- , Vanessa L. Bailey
- & Rodrigo Vargas
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Letter |
Triple oxygen isotope evidence for limited mid-Proterozoic primary productivity
Triple oxygen isotope measurements of 1.4-billion-year-old sedimentary sulfates reveal a unique mid-Proterozoic atmosphere and demonstrate that gross primary productivity in the mid-Proterozoic was between 6% and 41% of pre-anthropogenic levels.
- Peter W. Crockford
- , Justin A. Hayles
- & Boswell A. Wing
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Letter |
Atmosphere–soil carbon transfer as a function of soil depth
This study of whole-soil carbon dynamics finds that, of the atmospheric carbon that is incorporated into the topmost metre of soil over 50 years, just 19 per cent reaches the subsoil, in a manner that depends on land use and aridity.
- Jérôme Balesdent
- , Isabelle Basile-Doelsch
- & Christine Hatté
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Review Article |
Antarctic and global climate history viewed from ice cores
A discussion of past Antarctic and global climate history as seen from Antarctic ice cores, with an outlook on future goals and drilling priorities.
- Edward J. Brook
- & Christo Buizert
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Article |
Euryhaline ecology of early tetrapods revealed by stable isotopes
An approach using multiple stable isotopes reveals that early tetrapods of the Devonian period were euryhaline animals that inhabited aquatic environments of highly variable salinity.
- Jean Goedert
- , Christophe Lécuyer
- & Min Zhu
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News & Views |
Will ocean zones with low oxygen levels expand or shrink?
Computer simulations show that areas of the ocean that have low levels of dissolved oxygen will expand, but then shrink, in response to global warming — adding to an emerging picture of the finely balanced processes involved.
- Laure Resplandy
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Letter |
Carbon dioxide addition to coral reef waters suppresses net community calcification
In situ carbon dioxide enrichment experiments show that ocean acidification poses a threat to coral reefs by reducing the saturation state of aragonite and the concentration of carbonate ions and that this impairs community calcification.
- Rebecca Albright
- , Yuichiro Takeshita
- & Ken Caldeira
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Letter |
Carbonate-sensitive phytotransferrin controls high-affinity iron uptake in diatoms
Phytotransferrin, a functional analogue of transferrin, has an obligate requirement for carbonate to bind iron, which suggests that acidification-driven declines in the concentration of seawater carbonate ions may negatively affect diatom iron acquisition.
- Jeffrey B. McQuaid
- , Adam B. Kustka
- & Andrew E. Allen
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Letter |
Pervasive phosphorus limitation of tree species but not communities in tropical forests
In lowland tropical forests in Panama, widespread species-level phosphorus limitation of tree growth is not reflected in community-wide growth or biomass owing to the presence of a few species tolerant of low phosphorus availability.
- Benjamin L. Turner
- , Tania Brenes-Arguedas
- & Richard Condit
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Letter |
Pursuing sustainable productivity with millions of smallholder farmers
Millions of Chinese smallholder farmers were persuaded to adopt enhanced management practices, which led to a greater yield, reduced nitrogen fertilizer use and improved environmental performance throughout China.
- Zhenling Cui
- , Hongyan Zhang
- & Zhengxia Dou
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Brief Communications Arising |
Predicting soil carbon loss with warming
- Natasja van Gestel
- , Zheng Shi
- & Bruce A. Hungate
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Brief Communications Arising |
Crowther et al. reply
- T. W. Crowther
- , M. B. Machmuller
- & M. A. Bradford
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Letter |
Fire frequency drives decadal changes in soil carbon and nitrogen and ecosystem productivity
A meta-analysis and field data show that frequent fires in savannas and broadleaf forests decrease soil carbon and nitrogen over many decades; modelling shows that nitrogen loss drives carbon loss by reducing net primary productivity.
- Adam F. A. Pellegrini
- , Anders Ahlström
- & Robert B. Jackson
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Letter |
Large emissions from floodplain trees close the Amazon methane budget
Methane fluxes from the stems of Amazonian floodplain trees indicate that the escape of soil gas through wetland trees is the dominant source of methane emissions in the Amazon basin.
- Sunitha R. Pangala
- , Alex Enrich-Prast
- & Vincent Gauci
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News & Views |
Ocean hotspots of nitrogen loss
Microbial activity in the sea results in a loss of bioavailable nitrogen. It emerges that the climate phenomenon called the El Niño–Southern Oscillation has a surprisingly large effect on the size of this loss.
- Katja Fennel
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Letter |
Nutrient co-limitation at the boundary of an oceanic gyre
Nutrient amendment experiments at the boundary of the South Atlantic gyre reveal extensive regions in which nitrogen and iron are co-limiting, with other micronutrients also approaching co-deficiency; such limitations potentially increase phytoplankton community diversity.
- Thomas J. Browning
- , Eric P. Achterberg
- & C. Mark Moore
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Letter |
Early trace of life from 3.95 Ga sedimentary rocks in Labrador, Canada
The authors provide evidence for the existence of life on Earth in the earliest known sedimentary rocks and suggest that the presence of organic carbon, and low stable-isotope values of graphite from sedimentary rocks in Labrador pushes back the existence of organic life to beyond 3.95 billion years.
- Takayuki Tashiro
- , Akizumi Ishida
- & Tsuyoshi Komiya
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News & Views |
Volcanism caused ancient global warming
A study confirms that volcanism set off one of Earth's fastest global-warming events. But the release of greenhouse gases was slow enough for negative feedbacks to mitigate impacts such as ocean acidification. See Letter p.573
- Katrin J. Meissner
- & Timothy J. Bralower
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Letter |
Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum
Boron and carbon isotope data, used in an Earth system model, show that the Palaeocene–Eocene Thermal Maximum was associated with a much greater release of carbon than thought, most probably triggered by volcanism in the North Atlantic.
- Marcus Gutjahr
- , Andy Ridgwell
- & Gavin L. Foster
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Letter |
Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event
Measurements from Antarctic ice suggest that geological methane emissions are much lower than previously thought, and that methane emissions from hydrates and permafrost in response to climate warming are minimal.
- Vasilii V. Petrenko
- , Andrew M. Smith
- & Jeffrey P. Severinghaus
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News & Views |
Food for early animal evolution
A revised timeline for when algae became ecologically important among plankton in the ancient oceans reveals a link between chemical changes in those waters and the emergence of animals in marine ecosystems. See Letter p.578
- Andrew H. Knoll
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Letter |
The rise of algae in Cryogenian oceans and the emergence of animals
Steroid biomarkers provide evidence for a rapid rise of marine planktonic algae between 659 and 645 million years ago, establishing more efficient energy transfers and driving ecosystems towards larger and increasingly complex organisms.
- Jochen J. Brocks
- , Amber J. M. Jarrett
- & Tharika Liyanage
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News & Views |
Trends in ecosystem recovery from drought
An analysis suggests that the time taken for ecosystems to recover from drought increased during the twentieth century. If the frequency of drought events rises, some ecosystems might never have the chance to fully recover. See Letter p.202
- Sonia I. Seneviratne
- & Philippe Ciais
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News & Views |
Arctic plants take up mercury vapour
Trace elements are enriched in plants by natural processes, human activities or both. An analysis of mercury in Arctic tundra vegetation offers fresh insight into the uptake of trace metals from the atmosphere by plants. See Letter p.201
- William Shotyk
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Letter |
Tundra uptake of atmospheric elemental mercury drives Arctic mercury pollution
A two-year study of mercury deposition in the Arctic finds that the main source of mercury is gaseous elemental mercury, which is deposited throughout the year and leads to very high soil mercury levels.
- Daniel Obrist
- , Yannick Agnan
- & Detlev Helmig
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Research Highlight |
Plug pulled on ocean carbon sink
Organic particle behaviour may predict less carbon stored in the sea bed.
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Letter |
Surface tension prevails over solute effect in organic-influenced cloud droplet activation
A phase-separation mechanism is proposed for the dominance of the surface tension effect over the solute effect in the observed activation of ultrafine cloud condensation nuclei.
- Jurgita Ovadnevaite
- , Andreas Zuend
- & Colin O’ Dowd
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News |
Methane exploded from Arctic sea-floor as Ice Age ended
Huge ocean-floor craters were caused by the expulsion of pressurized greenhouse gas thousands of years ago.
- Jeff Tollefson
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News & Views |
Large rise in carbon uptake by land plants
A proxy for the amount of carbon dioxide taken up by plants for photosynthesis has been used to estimate historical global uptake, revealing a large increase that might partly offset the rise in atmospheric CO2 levels. See Letter p.84
- Dan Yakir
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Letter |
Large historical growth in global terrestrial gross primary production
Long-term records of global carbonyl sulfide levels reveal that terrestrial gross primary production (GPP) increased by around 30% during the twentieth century—a finding that may aid understanding of the connection between GPP growth and climate change.
- J. E. Campbell
- , J. A. Berry
- & M. Laine
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News & Views |
A plan for efficient use of nitrogen fertilizers
A global analysis finds that nitrogen fertilizers could be used more efficiently if their international distribution across croplands was altered — a measure that would also decrease nitrogen pollution.
- Xin Zhang
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Letter |
Paleoproterozoic sterol biosynthesis and the rise of oxygen
Steranes in ancient rocks have been used as ‘molecular fossils’, but the very earliest records of steranes have been shown to be contaminants; here, the presence of two key sterol biosynthesis enzymes in eukaryotes and bacteria suggests at least one gene transfer between bacteria and the earliest eukaryotes occurred some 2.3 billion years ago.
- David A. Gold
- , Abigail Caron
- & Roger E. Summons
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Article |
Evidence for early life in Earth’s oldest hydrothermal vent precipitates
Perhaps the earliest known signs of life have been found in Quebec, where features such as haematite tubes suggest that filamentous microbes lived around hydrothermal vents at least 3,770 million years ago.
- Matthew S. Dodd
- , Dominic Papineau
- & Crispin T. S. Little
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Review Article |
The integral role of iron in ocean biogeochemistry
The recent expansion of observational data has changed our understanding of the ocean iron cycle and its linkages with nutrients such as carbon and nitrogen.
- Alessandro Tagliabue
- , Andrew R. Bowie
- & Mak A. Saito
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News & Views |
Ocean circulation drove increase in CO2 uptake
The ocean's uptake of carbon dioxide increased during the 2000s. Models reveal that this was driven primarily by weak circulation in the upper ocean, solving a mystery of ocean science. See Letter p.215
- Sara E. Mikaloff Fletcher
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Letter |
Recent increase in oceanic carbon uptake driven by weaker upper-ocean overturning
Modelling of ocean carbon uptake for the 1980s to the 2000s shows that stronger upper-ocean overturning caused less carbon to be absorbed by the oceans in the 1990s, but that as the overturning circulation weakens more carbon is now being absorbed.
- Tim DeVries
- , Mark Holzer
- & Francois Primeau
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Letter |
Onset of the aerobic nitrogen cycle during the Great Oxidation Event
Nitrogen isotope data from sediments deposited during the earliest stage of the Great Oxidation Event show evidence for the emergence of a pervasive aerobic marine nitrogen cycle.
- Aubrey L. Zerkle
- , Simon W. Poulton
- & Christopher K. Junium
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News & Views |
Vast peatlands found in the Congo Basin
The discovery of what is potentially the world's largest continuous tropical peat complex has great implications for global carbon stocks, land management and scientific investment in central Africa. See Letter p.86
- Lola Fatoyinbo
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Letter |
Elevation alters ecosystem properties across temperate treelines globally
Examination of the ecosystem properties of treeline ecotones in seven temperate regions of the world shows that the reduction in temperature with increasing elevation does not affect tree leaf nutrient concentrations, but does reduce ground-layer community-weighted plant nitrogen levels, leading to a strong stoichiometric convergence of ground-layer plant community nitrogen to phosphorus ratios across all regions.
- Jordan R. Mayor
- , Nathan J. Sanders
- & David A. Wardle
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Letter |
Compensatory water effects link yearly global land CO2 sink changes to temperature
A study of how temperature and water availability fluctuations affect the carbon balance of land ecosystems reveals different controls on local and global scales, implying that spatial climate covariation drives the global carbon cycle response.
- Martin Jung
- , Markus Reichstein
- & Ning Zeng