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| Open AccessKrill and salp faecal pellets contribute equally to the carbon flux at the Antarctic Peninsula
Zooplankton impact Southern Ocean carbon cycling. Here, the authors examine carbon export at the Antarctic Peninsula, finding that krill pellets are efficiently exported, while salp pellets are retained and recycled in surface waters.
- Nora-Charlotte Pauli
- , Clara M. Flintrop
- & Morten H. Iversen
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Article
| Open AccessThawing Yedoma permafrost is a neglected nitrous oxide source
During permafrost thaw, nitrogen can be released as the greenhouse gas nitrous oxide, but the magnitude of this flux is unknown. Nitrous oxide emissions from ice-rich permafrost deposits are reported here, showing that emissions increase after thawing and stabilization and could represent an unappreciated positive climate feedback in the Arctic.
- M. E. Marushchak
- , J. Kerttula
- & C. Biasi
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| Open AccessSubstantial oxygen consumption by aerobic nitrite oxidation in oceanic oxygen minimum zones
Oxygen is fundamental for marine life, yet it is absent from large areas of the ocean. Here the authors demonstrate that microbial nitrite oxidation effectively consumes oxygen where oxygen concentrations are low, playing a pivotal role in these regions.
- J. M. Beman
- , S. M. Vargas
- & S. D. Wankel
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Article
| Open AccessHydrothermal plumes as hotspots for deep-ocean heterotrophic microbial biomass production
Hydrothermal vents are biogeochemically important, but their contribution to the carbon cycle is poorly constrained. Here the authors build a biogeochemical model that estimates autotrophic and heterotrophic production rates of microbial communities within hydrothermal plumes along mid-ocean ridges.
- Cécile Cathalot
- , Erwan G. Roussel
- & Pierre-Marie Sarradin
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| Open AccessAutumn destabilization of deep porewater CO2 store in a northern peatland driven by turbulent diffusion
The CO2 stored in deep peat porewater is viewed as a fixed component of peatland C cycling. Here, the authors reveal a hitherto unknown hydro-physical process that results in sudden losses from this CO2 store every autumn.
- A. Campeau
- , D. Vachon
- & M. B. Wallin
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Article
| Open AccessGlobal predictions of primary soil salinization under changing climate in the 21st century
Excess salt accumulation in the root zone causes soil salinization influencing soil health, biodiversity and food security. Authors used machine learning algorithms to predict global scale soil salinization under changing climate in the 21st century.
- Amirhossein Hassani
- , Adisa Azapagic
- & Nima Shokri
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Article
| Open AccessTemperature effects on carbon storage are controlled by soil stabilisation capacities
The extent to which temperature controls soil carbon storage remains highly uncertain. Here, the authors show that, globally, soil carbon stocks decline strongly with temperature, but the effect is much greater in coarse-textured soils with limited organic matter stabilisation capacities, than in fine-textured soils.
- Iain P. Hartley
- , Tim C. Hill
- & Gustaf Hugelius
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Article
| Open AccessAn abiotic source of Archean hydrogen peroxide and oxygen that pre-dates oxygenic photosynthesis
Hydrogen peroxide (H2O2) has been proposed as an electron donor for photosynthesis before water, however, the amount of H2O2 available on early Earth was thought to be limited. Here the authors propose a new abiotic pathway wherein abrasion of quartz surfaces would have provided enough H2O2.
- Hongping He
- , Xiao Wu
- & Kurt O. Konhauser
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Article
| Open AccessForest defoliator outbreaks alter nutrient cycling in northern waters
Defoliating insects disrupt nutrient cycling of boreal catchments by redistributing carbon and nitrogen from forests to lakes. The resulting shift in lake biogeochemistry exceeds broader between-year trends observed across the boreal and north temperate region.
- Samuel G. Woodman
- , Sacha Khoury
- & Andrew J. Tanentzap
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Article
| Open AccessDistinct methane-dependent biogeochemical states in Arctic seafloor gas hydrate mounds
Archaea in marine sediment control the transfer of methane to the ocean, but microbial dynamics in these environments are poorly understood. Here the authors investigate marine sediments in the high Arctic, showing how methane influx quickly increases abundances of methane-consuming archaea and decreases total microbial community diversity.
- Scott A. Klasek
- , Wei-Li Hong
- & Frederick S. Colwell
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Article
| Open AccessImpact of intensifying nitrogen limitation on ocean net primary production is fingerprinted by nitrogen isotopes
Projected declines in marine primary production are underpinned by a slowdown in nitrogen supplied to surface waters. Here the authors detail a new means to detect this slowdown and describe major shifts in the 21st century oceanic nitrogen cycle.
- Pearse J. Buchanan
- , Olivier Aumont
- & Alessandro Tagliabue
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Article
| Open AccessAltered growth conditions more than reforestation counteracted forest biomass carbon emissions 1990–2020
We combine data from global forest resource assessments with a forest model to quantify the role of major drivers of net carbon fluxes from global forest biomass at national resolution between 1990 and 2020. We find that growth-condition changes, more than reforestation, counteracted forest biomass carbon emissions mostly driven by deforestation.
- Julia Le Noë
- , Karl-Heinz Erb
- & Simone Gingrich
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Article
| Open AccessSpontaneous assembly of redox-active iron-sulfur clusters at low concentrations of cysteine
Iron-sulfur (FeS) proteins are involved in electron transfer and CO2 fixation. Here, the authors show that FeS clusters can form spontaneously in the presence of the amino acid cysteine, in conditions similar those expected in Hadean alkaline hydrothermal vents, suggesting a plausible mechanism of their emergence at the origin of life.
- Sean F. Jordan
- , Ioannis Ioannou
- & Nick Lane
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Article
| Open AccessAntarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
The Antarctic ozone hole has had far-reaching impacts, but effects on geochemical cycles in polar regions is still unknown. Iodine records from the interior of Antarctica provide evidence for human alteration of the natural geochemical cycle of this essential element.
- Andrea Spolaor
- , François Burgay
- & Alfonso Saiz-Lopez
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Article
| Open AccessDiverse sediment microbiota shape methane emission temperature sensitivity in Arctic lakes
Arctic lakes are strong and increasing sources of atmospheric methane, but extreme conditions and limited observations hinder robust understanding. Here the authors show that microbes in the middle of Arctic lakes have elevated methane producing potential, and are poised to release even more in the future.
- Joanne B. Emerson
- , Ruth K. Varner
- & Virginia I. Rich
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Article
| Open AccessRewetting does not return drained fen peatlands to their old selves
Whether rewetting leads to effective restoration of drained peatlands is unclear. Here the authors analyse a large number of near-natural and rewetted fen peatland sites in Europe, finding persistent differences in plant community composition and ecosystem functioning, and higher variance in the restored sites.
- J. Kreyling
- , F. Tanneberger
- & G. Jurasinski
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Article
| Open AccessEcological memory of recurrent drought modifies soil processes via changes in soil microbial community
Legacies of past ecological disturbances are expected but challenging to demonstrate. Here the authors report a 10-year field experiment in a mountain grassland that shows ecological memory of soil microbial community and functioning in response to recurrent drought.
- Alberto Canarini
- , Hannes Schmidt
- & Andreas Richter
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Article
| Open AccessCO2, nitrogen deposition and a discontinuous climate response drive water use efficiency in global forests
Water use efficiency is a key measure of plant responses to climate change. Here, the authors investigate its control by CO2, nitrogen deposition, and water availability using a global tree-ring dataset. They find an aridity threshold and quantify changes in control over the past 50 years.
- Mark A. Adams
- , Thomas N. Buckley
- & Tarryn L. Turnbull
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Article
| Open AccessFire-derived phosphorus fertilization of African tropical forests
Nowhere is biomass burning more abundant than on the African continent, but the biogeochemical impacts on forests are poorly understood. Here the authors show that biomass burning leads to high phosphorus deposition in the Congo basin, which scales with forest age as a result of increasing canopy complexity.
- Marijn Bauters
- , Travis W. Drake
- & Pascal Boeckx
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Article
| Open AccessMethane from microbial hydrogenolysis of sediment organic matter before the Great Oxidation Event
Microbial CH4 kept the early Earth warm under the faint young sun, but clear records are lacking. Here the authors present isotopic evidence that CH4 seepage in the Canadian shield is from hydrogen biodegradation in a Neoarchean ecosystem rather than an abiotic synthesis product.
- Xinyu Xia
- & Yongli Gao
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| Open AccessDecline in plankton diversity and carbon flux with reduced sea ice extent along the Western Antarctic Peninsula
Over the past century, the Western Antarctic Peninsula has experienced rapid warming and a substantial loss of sea ice with important implications for plankton biodiversity and carbon cycling. Using a 5-year DNA metabarcoding dataset, this study assesses how interannual variability in sea-ice conditions impacts biodiversity and biological carbon fluxes in this region.
- Yajuan Lin
- , Carly Moreno
- & Nicolas Cassar
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| Open AccessPurple sulfur bacteria fix N2 via molybdenum-nitrogenase in a low molybdenum Proterozoic ocean analogue
N2 fixation was key to the expansion of life on Earth, but which organisms fixed N2 and if Mo-nitrogenase was functional in the low Mo early ocean is unknown. Here, the authors show that purple sulfur bacteria fix N2 using Mo-nitrogenase in a Proterozoic ocean analogue, despite low Mo conditions.
- Miriam Philippi
- , Katharina Kitzinger
- & Marcel M. M. Kuypers
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Article
| Open AccessTransporter characterisation reveals aminoethylphosphonate mineralisation as a key step in the marine phosphorus redox cycle
Here the authors show that 2-aminoethylphosphonate (2AEP) mineralisation is widespread in the global ocean, operating independently of exogenous inorganic phosphate concentration. They propose 2AEP may be a major route for the regeneration of phosphate required to support marine primary production.
- Andrew R. J. Murphy
- , David J. Scanlan
- & Ian D. E. A. Lidbury
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| Open AccessPlant mixture balances terrestrial ecosystem C:N:P stoichiometry
Plant and soil C:N:P ratios are critical to ecosystem functioning, but it remains uncertain how plant diversity affects terrestrial C:N:P. In this meta-analysis of 169 studies, the authors find that plant mixtures can balance plant and soil C:N:P ratios according to background soil C:N:P.
- Xinli Chen
- & Han Y. H. Chen
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Article
| Open AccessAbove- and belowground biodiversity jointly tighten the P cycle in agricultural grasslands
Relationships between biodiversity and phosphorus cycling and the underlying processes are complex. Here the authors analyse a biodiversity manipulation experiment and an agricultural management gradient to show how plant and mycorrhizal fungal diversity promote phosphorus exploitation.
- Yvonne Oelmann
- , Markus Lange
- & Wolfgang Wilcke
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Article
| Open AccessSedimentary pyrite sulfur isotopes track the local dynamics of the Peruvian oxygen minimum zone
To explore the importance of local vs. global sulfur-cycle controls on variations in pyrite sulfur isotopes, the authors couple carbon-nitrogen-sulfur concentrations and stable isotopes of sediments from the Peruvian oxygen minimum zone, identifying a major role for the local organic carbon loading.
- Virgil Pasquier
- , David A. Fike
- & Itay Halevy
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Article
| Open AccessDiffusion controls the ventilation of a Pacific Shadow Zone above abyssal overturning
The deep North Pacific is the end of the road for global ocean circulation, but the circulation patterns and ventilation are poorly understood. Here the authors show that diffusive transports both along and across density layers play a leading role in returning 1,400 year old water to the surface.
- Mark Holzer
- , Tim DeVries
- & Casimir de Lavergne
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Article
| Open AccessTowards omics-based predictions of planktonic functional composition from environmental data
Advances in omics approaches could enable quantitative predictions of microbial functional composition. Here the authors re-analyze 885 metagenome-assembled genomes from Tara Oceans, and use a network approach to quantify protein functional clusters and explore their biogeography.
- Emile Faure
- , Sakina-Dorothée Ayata
- & Lucie Bittner
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Matters Arising
| Open AccessReply to: “Questions remain about the biolability of dissolved black carbon along the combustion continuum”
- Yuanzhi Qi
- , Wenjing Fu
- & Xuchen Wang
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Matters Arising
| Open AccessQuestions remain about the biolability of dissolved black carbon along the combustion continuum
- Sasha Wagner
- , Alysha I. Coppola
- & Hongyan Bao
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Article
| Open AccessGlobal distribution patterns of marine nitrogen-fixers by imaging and molecular methods
Nitrogen fixation by diazotrophs is critical for marine primary production. Using Tara Oceans datasets, this study combines a quantitative image analysis pipeline with metagenomic mining to provide an improved global overview of diazotroph abundance, diversity and distribution.
- Juan José Pierella Karlusich
- , Eric Pelletier
- & Rachel A. Foster
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Article
| Open AccessParticulate organic matter as a functional soil component for persistent soil organic carbon
The fate of soil carbon is controlled by plant inputs, microbial activity, and the soil matrix. Here the authors extend the notion of plant-derived particulate organic matter, from an easily available and labile carbon substrate, to a functional component at which persistence of soil carbon is determined.
- Kristina Witzgall
- , Alix Vidal
- & Carsten W. Mueller
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Article
| Open AccessSuppressing peatland methane production by electron snorkeling through pyrogenic carbon in controlled laboratory incubations
Warmer and drier conditions are increasing the frequency of forest fires, which in turn produce pyrogenic carbon. Here the authors show that accumulation of pyrogenic carbon can suppress post-fire methane production in northern peatlands and can effectively buffer fire-derived greenhouse gas emissions.
- Tianran Sun
- , Juan J. L. Guzman
- & Largus T. Angenent
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Article
| Open AccessQuantifying nitrogen fixation by heterotrophic bacteria in sinking marine particles
N2 fixation by heterotrophic bacteria has recently been found to take place on sinking marine particles, but an understanding of its regulation and importance is lacking. Here the authors develop a trait-based model for this N2 fixation, finding that this once overlooked process could have global importance.
- Subhendu Chakraborty
- , Ken H. Andersen
- & Lasse Riemann
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| Open AccessThe Great Oxygenation Event as a consequence of ecological dynamics modulated by planetary change
The Great Oxygenation Event (GOE) 2.4 billion years ago is believed to have been critical for the evolution of complex life. Here, Olejarz et al. propose a model suggesting that competition between major bacterial groups could have triggered the GOE in a feedback loop with geophysical processes.
- Jason Olejarz
- , Yoh Iwasa
- & Martin A. Nowak
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Article
| Open AccessStorage and export of microbial biomass across the western Greenland Ice Sheet
Microbes that colonise ice sheet surfaces are important to the carbon cycle, but their biomass and transport remains unquantified. Here, the authors reveal substantial microbial carbon fluxes across Greenland’s ice surface, in quantities that may sustain subglacial heterotrophs and fuel methanogenesis.
- T. D. L. Irvine-Fynn
- , A. Edwards
- & A. Hubbard
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Article
| Open AccessIndia-Asia collision as a driver of atmospheric CO2 in the Cenozoic
“Earth degassing is a critical carbon source, but its contribution to Cenozoic atmospheric CO2 variations is not well known. Here, the authors analyse CO2 fluxes on the Tibetan Plateau and suggest that the India-Asia collision was the primary driver of changes in atmospheric CO2 over the past 65 Ma.”
- Zhengfu Guo
- , Marjorie Wilson
- & Jiaqi Liu
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Article
| Open AccessCo-benefits of protecting mangroves for biodiversity conservation and carbon storage
Conserving mangrove biodiversity has numerous co-benefits, including climate change-mitigation. Here the authors demonstrate that blue carbon storage in mangroves can be best sustained by combining site-specific dominant species with other species with contrasting functional traits.
- Md Mizanur Rahman
- , Martin Zimmer
- & Ming Xu
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Article
| Open AccessEcology of inorganic sulfur auxiliary metabolism in widespread bacteriophages
Some bacteriophage encode auxiliary metabolic genes (AMGs) that impact host metabolism and biogeochemical cycling during infection. Here the authors identify hundreds of AMGs in environmental phage encoding sulfur oxidation genes and use their global distribution to infer phage-mediated biogeochemical impacts.
- Kristopher Kieft
- , Zhichao Zhou
- & Karthik Anantharaman
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Article
| Open AccessNanomolar phosphate supply and its recycling drive net community production in the subtropical North Pacific
Primary productivity in the oligotrophic ocean sustains Earth’s ecosystems, but nutrient concentrations are vanishingly low. Here the authors measure nanomolar macronutrient concentrations in the North Pacific and find that net community production is sustained through high rates of phosphorus recycling.
- Fuminori Hashihama
- , Ichiro Yasuda
- & Masao Ishii
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Article
| Open AccessNutrients cause consolidation of soil carbon flux to small proportion of bacterial community
The fate of soil carbon depends on microbial processes, but whether different microbial taxa have individualistic effects on carbon fluxes is unknown. Here the authors use 16 S amplicon sequencing and stable isotopes to show how taxonomic differences influence bacterial respiration and carbon cycling across four ecosystems.
- Bram W. Stone
- , Junhui Li
- & Bruce A. Hungate
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Article
| Open AccessLateral advection supports nitrogen export in the oligotrophic open-ocean Gulf of Mexico
The middle of the Gulf of Mexico is stratified and highly oligotrophic, yet there are anomalously high fluxes of sinking particulate matter from the euphotic zone. Here the authors show that lateral advection of organic matter supports nitrogen export in the Gulf of Mexico’s open ocean.
- Thomas B. Kelly
- , Angela N. Knapp
- & Michael R. Stukel
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Article
| Open AccessSmall sinking particles control anammox rates in the Peruvian oxygen minimum zone
Up to 40% of the ocean’s fixed nitrogen is lost in oxygen minimum zones (OMZs) by anammox, but despite the importance of this process, nitrogen loss patterns in OMZs are difficult to predict. Here the authors show that ammonium release from small particles is a major control of anammox in the Peruvian OMZ.
- Clarissa Karthäuser
- , Soeren Ahmerkamp
- & Marcel M. M. Kuypers
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Article
| Open AccessA tighter constraint on Earth-system sensitivity from long-term temperature and carbon-cycle observations
Earth-system sensitivity (ESS) describes the long-term temperature response for a given change in atmospheric CO2 and, as such, is a crucial parameter to assess future climate change. Here, the authors use a Bayesian model with data from the last 420 Myrs to reduce uncertainties and estimate ESS to be around 3.4 °C.
- Tony E. Wong
- , Ying Cui
- & Klaus Keller
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Article
| Open AccessGlobal health effects of future atmospheric mercury emissions
Mercury is a neurotoxin and pollutant with enhanced emissions from anthropogenic activities. Here, the authors develop a global emissions, transport, and human risk model and find substantial future losses in revenue and public health if emission reductions proposed by the Minamata Convention are delayed.
- Yanxu Zhang
- , Zhengcheng Song
- & Ping Li
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Article
| Open AccessNutrient content and stoichiometry of pelagic Sargassum reflects increasing nitrogen availability in the Atlantic Basin
The macroalgae Sargassum has grown for centuries in the oligotrophic North Atlantic supported by natural nutrient sources and cycling. Here the authors show that changes in tissue nutrient contents since the 1980s reflect global anthropogenic nitrogen enrichment, causing blooms in the wider Atlantic basin.
- B. E. Lapointe
- , R. A. Brewton
- & P. L. Morton
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Article
| Open AccessThe 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
A large fraction of ice sheet discharge enters the ocean subsurface from underneath large floating ice-tongues. Here the authors show that associated nutrient export may be governed by shelf circulation and, especially for Fe, particle-dissolved phase exchanges, which is largely independent from freshwater Fe content.
- Stephan Krisch
- , Mark James Hopwood
- & Eric Pieter Achterberg
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Article
| Open AccessThe kaolinite shuttle links the Great Oxidation and Lomagundi events
Expanded phosphorus availability possibly triggered a marine bioproduction boom after 2.3 billion years ago, but its delivery mechanisms remain unclear. Here we propose a kaolinite shuttle which efficiently adsorbs phosphorus in continental weathering settings and releases it under marine conditions.
- Weiduo Hao
- , Kaarel Mänd
- & Kurt O. Konhauser