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Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning
The Antarctic ice sheets contribution to rising sea levels at the end of the last ice age remains a matter of debate. Here, the authors present a suite of ice-sheet modelling experiments and conclude that the retreating Antarctic ice sheet may have contributed as much as 0.7 m per century to meltwater pulse 1A.
- N. R. Golledge
- , L. Menviel
- & R. H. Levy
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Sensitive response of the Greenland Ice Sheet to surface melt drainage over a soft bed
The delivery of meltwater to the base of the Greenland Ice Sheet has been shown to regulate ice flow, yet the role of soft basal sediment is unknown. Here, the authors use a three-dimensional ice sheet model to assess the impact of seasonal meltwater delivery on subglacial sediment shear strength and ice flow.
- M. Bougamont
- , P. Christoffersen
- & S. P. Carter
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Sea-level variability over five glacial cycles
Detailed sea-level records beyond ~150,000 years ago are limited. Here, the authors present a radiometrically constrained sea-level record from the Red Sea, spanning five glacial cycles and examine sea-level rise rates and the effects of past global ice-volume changes on monsoon intensity.
- K. M. Grant
- , E. J. Rohling
- & F. Williams
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How shorter black carbon lifetime alters its climate effect
Unlike most aerosols, black carbon absorbs solar radiation, potentially warming the atmosphere, yet its total climate effect remains uncertain. Here, the authors use a chemical transport and global circulation model to investigate the impact of black carbon emissions on global, annual mean radiative forcing.
- Øivind Hodnebrog
- , Gunnar Myhre
- & Bjørn H. Samset
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Real-time QEXAFS spectroscopy measures rapid precipitate formation at the mineral–water interface
Geochemical reactions at the mineral–water interface are complicated, yet a molecular-scale understanding of their kinetics is critical. Here, Siebecker et al.conduct real-time measurements in a flow-through cell to show the rapid formation of layered double hydroxides at a clay mineral surface.
- Matthew Siebecker
- , Wei Li
- & Donald Sparks
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Subduction of the oceanic Hikurangi Plateau and its impact on the Kermadec arc
Large igneous province subduction is a rare process with many unknowns. Timm et al.present geochemical and geophysical data providing insights into the Hikurangi Plateau subduction and its impact on arc volcanism, identifying a missing piece of the Ontong Java–Manihiki–Hikurangi super plateau.
- Christian Timm
- , Bryan Davy
- & John A. Gamble
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Persistence of pressure patterns over North America and the North Pacific since AD 1500
Synoptic-scale atmospheric pressure patterns control moisture delivery and thus drought occurrence across western North America, yet long-term records are lacking. Here, the authors use a novel combination of tree-ring data and self-organizing maps to reconstruct and analyse pressure patterns since AD 1500.
- Erika K. Wise
- & Matthew P. Dannenberg
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Chemo-mechanics of salt damage in stone
Growth of salt crystals in pores is one of the most damaging weathering mechanisms for stone in ornamental structures and historical buildings. Here, the authors present a simple yet powerful treatment for predicting when salt damage will occur, quantifying this susceptibility to salt crystallization.
- Robert J. Flatt
- , Francesco Caruso
- & George W. Scherer
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Validation of climate model-inferred regional temperature change for late-glacial Europe
Comparison of climate model hindcasts with proxy data is essential to improve model reliability, yet standardized palaeoclimate data sets are lacking. Here, Heiri et al. compare chironomid-based palaeotemperature records with the ECHAM-4 atmospheric general circulation model, showing excellent agreement.
- Oliver Heiri
- , Stephen J. Brooks
- & André F. Lotter
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Aridity threshold in controlling ecosystem nitrogen cycling in arid and semi-arid grasslands
Understanding the relationship between aridity and ecosystem N-cycling is important in predicting the effects of global climate change. Here, the authors present N isotopes across an aridity gradient and identify a tipping point, which marks a divergence in N-cycling controlling factors and mechanisms.
- Chao Wang
- , Xiaobo Wang
- & Edith Bai
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Weakening of the stratospheric polar vortex by Arctic sea-ice loss
The mechanism behind the severely cold winters experienced by the mid-latitudes of the Northern Hemisphere in recent years is not fully understood. Here, the authors combine observational analyses and model experiments to reveal a dynamic connection between Arctic sea-ice cover and the polar stratosphere.
- Baek-Min Kim
- , Seok-Woo Son
- & Jin-Ho Yoon
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Terrestrial selenium distribution in China is potentially linked to monsoonal climate
Selenium deficiency is a major health problem, particularly in the selenium-poor belt in China, yet its distribution in the terrestrial environment is poorly understood. Here, the authors combine geochemical and palaeoclimate data and show that selenium distribution in China may be related to East Asian monsoon rainfall.
- Tim Blazina
- , Youbin Sun
- & Lenny H.E. Winkel
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| Open AccessA Cenozoic-style scenario for the end-Ordovician glaciation
Claims that the end-Ordovician Earth was characterized by giant ice sheets, yet paradoxically warm oceans and elevated CO2 levels are open to debate. Here, Ghienne et al. examine sedimentary records from low and high palaeolatitude settings and propose a revision of the mechanisms for end-Ordovician events.
- Jean-François Ghienne
- , André Desrochers
- & Jan Veizer
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Magnetic properties of uncultivated magnetotactic bacteria and their contribution to a stratified estuary iron cycle
Magnetotactic bacteria synthesize magnetite or greigite magnetosomes that, when fossilized, can serve as biomarkers of past ocean redox shifts. Here, Chen et al.show that these magnetosome types have very similar coercivity distributions, with implications for the analysis of sedimentary magnetic records.
- A.P. Chen
- , V.M. Berounsky
- & N.G.F. Vella
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Magnetic force microscopy reveals meta-stable magnetic domain states that prevent reliable absolute palaeointensity experiments
Obtaining reliable estimates of the absolute palaeointensity of the Earth’s magnetic field is difficult and many methods induce alteration. de Groot et al.present a means to see and explain changes in magnetization in unreliable samples, explaining why some samples systematically fail paleointensity experiments.
- Lennart V. de Groot
- , Karl Fabian
- & Mark J. Dekkers
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Differentiated availability of geochemical mercury pools controls methylmercury levels in estuarine sediment and biota
Methylmercury in aquatic biota constitutes a severe environmental issue globally, but models struggle to provide accurate quantification. Here, the authors combine experimental approaches to assess contributions from different pools and use the data to interpret the mercury cycle in an estuarine setting.
- Sofi Jonsson
- , Ulf Skyllberg
- & Erik Björn
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Interpreting carbonate and organic carbon isotope covariance in the sedimentary record
To date, covariance of carbonate and organic carbon isotope records has been assumed to denote fidelity of the original signal. This study shows that post-depositional alteration can create strong correlations, raising doubts about the use of correlated records to imply important changes in past global carbon cycling.
- Amanda M. Oehlert
- & Peter K. Swart
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| Open AccessHolocene variations in peatland methane cycling associated with the Asian summer monsoon system
Although it has been widely suggested that the mid-Holocene minimum methane emissions are associated with hydrological change, direct evidence is missing. Here, the authors present evidence from the Tibetan Plateau using tracers of methanogenesis and methanotrophy, in combination with climate simulations.
- Yanhong Zheng
- , Joy S. Singarayer
- & Richard D. Pancost
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Fumigant methyl iodide can methylate inorganic mercury species in natural waters
Methyl iodide is a fumigant registered for use in many countries and its usage is increasing. Here, the authors identify a new pathway of mercury methylation via methyl iodide in sunlit water, suggesting the necessity for a more comprehensive risk assessment for the use of methyl iodide as a fumigant.
- Yongguang Yin
- , Yanbin Li
- & Guibin Jiang
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Formation of recent Pb-Ag-Au mineralization by potential sub-surface microbial activity
Studies suggest almost the same amount of biomass is present in subterranean settings as on Earth’s surface. Here, the authors propose that a large intraterrestrial microbial system was responsible for mineralization in southern Spain, and that microbes may play a major role in sub-surface ore-forming processes.
- Fernando Tornos
- , Francisco Velasco
- & Juan Manuel Escobar
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A highly unradiogenic lead isotopic signature revealed by volcanic rocks from the East Pacific Rise
Radiogenic isotopes in oceanic basalts provide a window into the different geochemical components making up Earth’s mantle. Here, the authors provide data from volcanic glasses along the East Pacific Rise with an unusual lead signature, suggesting the existence of a novel type of upper mantle reservoir.
- Berengere Mougel
- , Arnaud Agranier
- & Pascal Gente
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| Open AccessAn electromagnetic field disrupts negative geotaxis in Drosophila via a CRY-dependent pathway
The earth’s electromagnetic field has a modest effect on the behaviour of Drosophila melanogaster. Here, Fedele et al. use an assessment of climbing behaviour to describe how the blue-light circadian photoreceptor cryptochrome mediates a negative movement response to gravity in flies.
- Giorgio Fedele
- , Edward W. Green
- & Charalambos P. Kyriacou
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Southern Annular Mode-like changes in southwestern Patagonia at centennial timescales over the last three millennia
The Southern Annular Mode (SAM) strongly impacts modern Southern Hemisphere climate, yet insight into its pre-industrial behaviour is lacking. Here, the authors present a high-resolution lake record and show that SAM variability coincided with major centennial-scale climate changes over the past 3,000 years.
- Patricio I. Moreno
- , I. Vilanova
- & R. De Pol-Holz
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| Open AccessClinopyroxene precursors to amphibole sponge in arc crust
Studies have suggested amphibole to be a major phase in the lower crust based on trace element geochemistry of volcanic suites, although the formation of these lithologies remains cryptic. Here, the author suggests a reaction-replacement mechanism to explain how this cryptic fractionation may occur.
- Daniel J. Smith
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Differentiating moss from higher plants is critical in studying the carbon cycle of the boreal biome
Satellite-derived indices used to estimate gross primary production and carbon cycling rarely differentiate between boreal mosses and vascular plants, despite differences in photosynthetic capacity. Here, the authors show that this may have led to an overestimation of the boreal carbon budget.
- Wenping Yuan
- , Shuguang Liu
- & Timo Vesala
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Natural snowfall reveals large-scale flow structures in the wake of a 2.5-MW wind turbine
Models of turbulent flows are often simulated in the laboratory, in sampling areas with dimensions <1 m. Here, the authors exploit a natural snowstorm to quantify turbulent flows, exploring the complex dynamics of the atmospheric boundary layer around a 2.5-MW utility-scale wind turbine.
- Jiarong Hong
- , Mostafa Toloui
- & Fotis Sotiropoulos
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Bimodal magmatism produced by progressively inhibited crustal assimilation
The origin of bimodal (mafic–felsic) rock suites is a fundamental question in volcanology. Here, the authors present a new model for magmatic differentiation in continental igneous provinces and explain how large volumes of granitic magma can be produced in otherwise basaltic systems.
- F. C. Meade
- , V. R. Troll
- & I. Klonowska
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Source identification of the Arctic sea ice proxy IP25
The organic geochemical biomarker IP25 has been widely applied in the reconstruction of Arctic sea ice, yet its source remains undetermined. Here, the authors report the identification of IP25in common pan-Arctic sea ice diatoms, thus establishing its applicability as a palaeo Arctic sea ice proxy.
- T. A. Brown
- , S. T. Belt
- & C. J. Mundy
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| Open AccessIntensification of the meridional temperature gradient in the Great Barrier Reef following the Last Glacial Maximum
The Great Barrier Reef (GBR) is under threat from rising ocean temperatures, yet its response to past temperature change is poorly known. Felis et al. show that the GBR experienced a much steeper temperature gradient during the last deglaciation, suggesting it may be more resilient than previously thought.
- Thomas Felis
- , Helen V. McGregor
- & Jody M. Webster
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| Open AccessEvidence for global cooling in the Late Cretaceous
The Late Cretaceous experienced significant cooling, yet a lack of low-latitude records mean the regional extent of this cooling is poorly constrained. Linnert et al. present a TEX86sea surface temperature record from a palaeolatitude of ~35 °N and show that Late Cretaceous cooling was global in nature.
- Christian Linnert
- , Stuart A. Robinson
- & Ernest E. Russell
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Impact-induced shock and the formation of natural quasicrystals in the early solar system
The first-reported natural quasicrystal, found in the meteorite Khatyrka, has posed many questions regarding the extraterrestrial processes that led to its formation. Here, the authors suggest how the metallic Al- and Cu-bearing phases formed and report the discovery of other new minerals.
- Lincoln S. Hollister
- , Luca Bindi
- & Paul J. Steinhardt
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Silicate deposition during decomposition of cyanobacteria may promote export of picophytoplankton to the deep ocean
The contribution of picophytoplankton to particle transport in the marine environment is relatively unknown. Here, the authors perform incubation experiments and show that decomposing picophytoplankton provides an efficient transport pathway for silica-enriched marine particles.
- Tiantian Tang
- , Kim Kisslinger
- & Cindy Lee
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Carbon storage and potential methane production in the Hudson Bay Lowlands since mid-Holocene peat initiation
Peatlands both store and emit potent greenhouse gases, yet their contribution to carbon dynamics during the past is poorly constrained. Here, Packalen et al.present new age constraints for peat development in the Hudson Bay Lowlands and quantify carbon storage and methane emissions during the Holocene.
- Maara S. Packalen
- , Sarah A. Finkelstein
- & James W. McLaughlin
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| Open AccessRift migration explains continental margin asymmetry and crustal hyper-extension
During continental rifting, various stages and structures are observed, the least understood being hyper-extended continental crust at magma-poor margins. Here, the authors use finite-element thermomechanical models to investigate the mechanism causing observed margin asymmetry and crustal hyper-extension.
- Sascha Brune
- , Christian Heine
- & Stephan V. Sobolev
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Evidence for a difference in rupture initiation between small and large earthquakes
Being able to predict the final size of an earthquake while rupture is ongoing is a largely debated scientific problem. Here, the authors suggest that the evolution of P-wave peak displacement holds information regarding the early stage of the rupture process and may be a proxy for the final size of the event.
- S. Colombelli
- , A. Zollo
- & M. Picozzi
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| Open AccessEnhanced role of eddies in the Arctic marine biological pump
Arctic sea ice has been in rapid decline in recent decades, yet the impact on biogeochemical cycling is unknown due to insufficient sampling. Watanabe et al.combine year-long mooring observations with numerical models to show that an eddy-induced biological pump would be enhanced by sea ice retreat.
- Eiji Watanabe
- , Jonaotaro Onodera
- & Michio J. Kishi
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| Open AccessDirect contribution of the seagrass Thalassia testudinum to lime mud production
Seagrass beds are effective blue-carbon sinks, yet their role as a lime mud source in the tropical carbonate factory is less well known. Here, the authors demonstrate that the species Thalassia testudinumcan significantly contribute to carbonate production via the precipitation of aragonite needles.
- Susana Enríquez
- & Nadine Schubert
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| Open AccessIce sheets as a significant source of highly reactive nanoparticulate iron to the oceans
Glacial meltwaters may help fertilize the iron-limited Polar Oceans, yet the contribution is poorly constrained. Hawkings et al.monitor iron fluxes during a full-melt season in Greenland, and propose that ice sheets provide highly reactive and potentially bioavailable iron, comparable with aeolian dust fluxes.
- Jon R. Hawkings
- , Jemma L. Wadham
- & Jon Telling
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Impacts of El Niño Southern Oscillation on the global yields of major crops
El Niño Southern Oscillation affects seasonal climate worldwide; however, it is uncertain how it impacts global crop yields. Here, the authors present a global assessment of the impacts of El Niño Southern Oscillation on crop productivity and show large differences among regions, crop types and cropping technologies.
- Toshichika Iizumi
- , Jing-Jia Luo
- & Toshio Yamagata
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| Open AccessThe effectiveness of coral reefs for coastal hazard risk reduction and adaptation
The risks of flooding to coastal communities are increasing due to coastal development and climate change. Here, the authors use meta-analyses to quantitatively show that coral reefs can significantly reduce risks from natural hazards, and that reef defences can be enhanced cost effectively.
- Filippo Ferrario
- , Michael W. Beck
- & Laura Airoldi
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Reactive nitrogen requirements to feed the world in 2050 and potential to mitigate nitrogen pollution
As global population and food demand rises, it is increasingly unclear how reactive nitrogen pollution will be mitigated. Bodirsky et al.run a series of model simulations and show that even under ambitious mitigation, reactive nitrogen pollution is likely to exceed critical environmental thresholds in the year 2050.
- Benjamin Leon Bodirsky
- , Alexander Popp
- & Miodrag Stevanovic
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Two-stroke scooters are a dominant source of air pollution in many cities
Primary and secondary organic aerosols emitted by road vehicles are hazardous to health and climate, with diesel trucks and cars considered the main offenders. Platt et al.show that, despite constituting a small fraction of the fleet, two-stroke scooters can dominate vehicular pollution in some cities.
- S.M. Platt
- , I.El. Haddad
- & A.S.H. Prévôt
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| Open AccessCascading ecological effects of eliminating fishery discards
Discards from fishing vessels are food for scavenging species, so ending the practice may have ecological consequences. Here, Heath et al. show that improving selectivity so that unwanted fish are not caught, achieves conservation benefits, while simply requiring that vessels land their entire catch, does not.
- Michael R. Heath
- , Robin M. Cook
- & Douglas C. Speirs
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Inner gorges cut by subglacial meltwater during Fennoscandian ice sheet decay
Whether the origins of inner gorges were fluvial or subglacial has been debated for decades. Here, Jansen et al. present new evidence, in the form of a suite of cosmogenic nuclide exposure ages and a deglaciation map, which suggests a subglacial meltwater origin for inner gorges in northern Sweden.
- J.D. Jansen
- , A.T. Codilean
- & S. Xu
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Plasma irregularities in the D-region ionosphere in association with sprite streamer initiation
Sprites are spectacular optical emissions in the mesosphere with an enigmatic filamentary nature. Qin et al.present high-speed video and modelling data revealing sub-millisecond dynamics to reconstruct the structures on a km-scale, showing that pre-existing plasma irregularities are responsible for their initiation.
- Jianqi Qin
- , Victor P. Pasko
- & Hans C. Stenbaek-Nielsen
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| Open AccessArctic tree rings as recorders of variations in light availability
Tree rings are widely used to reconstruct historical records of surface temperature. Here, Stine and Huybers analyse tree-ring records north of 50°N and show that changes in the light environment associated with both volcanic eruptions and global dimming significantly influence tree-ring growth.
- A. R. Stine
- & P. Huybers
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| Open AccessMadden–Julian Oscillation prediction skill of a new-generation global model demonstrated using a supercomputer
Prediction of the Madden–Julian Oscillation using complex cloud-resolving models has been limited by computational power. Here, Miyakawa et al.run a series of simulations using the newly developed 10 peta-flop ‘K computer’ and demonstrate a Madden–Julian Oscillation predictive window of 27 days.
- Tomoki Miyakawa
- , Masaki Satoh
- & Kunio Yoneyama
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Chemodiversity of dissolved organic matter in lakes driven by climate and hydrology
Lakes play an important role in the global carbon cycle and understanding their organic matter cycling is vital. Kellerman et al.apply an ultrahigh-resolution technique to 120 lakes across Sweden and show that the molecular composition is shaped by water dynamics and temperature.
- Anne M. Kellerman
- , Thorsten Dittmar
- & Lars J. Tranvik
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Orbital control of western North America atmospheric circulation and climate over two glacial cycles
A palaeoclimate record from Devils Hole, North America, has long called into question the theory of orbital-scale climate variability. Lachniet et al.present a new, well-dated, speleothem record and reveal evidence for strong orbital forcing of palaeoclimate in this region for at least the past 175 kyrs.
- Matthew S. Lachniet
- , Rhawn F. Denniston
- & Victor J. Polyak