Nature Geoscience

Papers
(The TQCC of Nature Geoscience is 21. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-11-01 to 2024-11-01.)
ArticleCitations
Risk of pesticide pollution at the global scale625
Half of global methane emissions come from highly variable aquatic ecosystem sources525
Biochar in climate change mitigation406
Global mapping reveals increase in lacustrine algal blooms over the past decade270
Drivers of PM2.5 air pollution deaths in China 2002–2017249
Current Atlantic Meridional Overturning Circulation weakest in last millennium231
Different climate sensitivity of particulate and mineral-associated soil organic matter224
Recent European drought extremes beyond Common Era background variability208
Managing nitrogen legacies to accelerate water quality improvement173
Control of particulate nitrate air pollution in China162
Ice velocity and thickness of the world’s glaciers151
Rivers as the largest source of mercury to coastal oceans worldwide150
Increased carbon footprint of materials production driven by rise in investments147
Shifts in regional water availability due to global tree restoration140
Phosphorus as an integral component of global marine biogeochemistry123
Eleven-year solar cycles over the last millennium revealed by radiocarbon in tree rings123
Rapid decline in Antarctic sea ice in recent years hints at future change115
High Mountain Asia hydropower systems threatened by climate-driven landscape instability111
Enhanced aerosol particle growth sustained by high continental chlorine emission in India105
Coupled anaerobic methane oxidation and reductive arsenic mobilization in wetland soils105
Co-variation of silicate, carbonate and sulfide weathering drives CO2 release with erosion98
Formation of necromass-derived soil organic carbon determined by microbial death pathways98
A biogeochemical–hydrological framework for the role of redox-active compounds in aquatic systems98
Attribution of global lake systems change to anthropogenic forcing97
Potential CO2 removal from enhanced weathering by ecosystem responses to powdered rock96
Global carbon dioxide efflux from rivers enhanced by high nocturnal emissions95
Global carbon budget of reservoirs is overturned by the quantification of drawdown areas95
Poleward expansion of tropical cyclone latitudes in warming climates93
Deforestation-induced warming over tropical mountain regions regulated by elevation88
Secondary organic aerosol formed by condensing anthropogenic vapours over China’s megacities86
Global water availability boosted by vegetation-driven changes in atmospheric moisture transport84
Atlantic and Pacific tropics connected by mutually interactive decadal-timescale processes83
Scientists from historically excluded groups face a hostile obstacle course82
Fire effects on the persistence of soil organic matter and long-term carbon storage81
Drought self-propagation in drylands due to land–atmosphere feedbacks80
A coupled model of episodic warming, oxidation and geochemical transitions on early Mars78
Past abrupt changes, tipping points and cascading impacts in the Earth system76
Recent recovery of Antarctic Bottom Water formation in the Ross Sea driven by climate anomalies74
Opportunities and challenges in using remaining carbon budgets to guide climate policy74
Substantial carbon drawdown potential from enhanced rock weathering in the United Kingdom73
Global mass of buoyant marine plastics dominated by large long-lived debris73
Imbalance of global nutrient cycles exacerbated by the greater retention of phosphorus over nitrogen in lakes72
Uncertain response of ocean biological carbon export in a changing world72
Global patterns of daily CO2 emissions reductions in the first year of COVID-1970
Birth of a large volcanic edifice offshore Mayotte via lithosphere-scale dyke intrusion70
Rewetting global wetlands effectively reduces major greenhouse gas emissions70
Open ocean and coastal new particle formation from sulfuric acid and amines around the Antarctic Peninsula69
Abrupt changes in the global carbon cycle during the last glacial period69
Shifts in vegetation activity of terrestrial ecosystems attributable to climate trends69
Potential impacts of atmospheric microplastics and nanoplastics on cloud formation processes68
Empirical estimate of forestation-induced precipitation changes in Europe68
Confronting the water potential information gap67
Intensification of El Niño-induced atmospheric anomalies under greenhouse warming65
Increased outburst flood hazard from Lake Palcacocha due to human-induced glacier retreat65
Pacific shoreline erosion and accretion patterns controlled by El Niño/Southern Oscillation63
Synergistic effects of four climate change drivers on terrestrial carbon cycling61
Carbon and nitrogen cycling in Yedoma permafrost controlled by microbial functional limitations60
Marsh resilience to sea-level rise reduced by storm-surge barriers in the Venice Lagoon59
Tropical tree growth driven by dry-season climate variability59
Fluvial organic carbon cycling regulated by sediment transit time and mineral protection58
A record of plume-induced plate rotation triggering subduction initiation58
Calcium carbonate dissolution patterns in the ocean57
Siberian carbon sink reduced by forest disturbances56
Orange hydrogen is the new green56
A tree of Indo-African mantle plumes imaged by seismic tomography56
Underestimated mass loss from lake-terminating glaciers in the greater Himalaya56
Arctic sea-ice loss fuels extreme European snowfall56
Suppression of surface ozone by an aerosol-inhibited photochemical ozone regime55
Global increase in biomass carbon stock dominated by growth of northern young forests over past decade55
Global crop production increase by soil organic carbon54
Slip rate deficit and earthquake potential on shallow megathrusts54
Global cycling and climate effects of aeolian dust controlled by biological soil crusts54
Large-scale thermal unrest of volcanoes for years prior to eruption53
Drought resistance enhanced by tree species diversity in global forests53
Projections of tropical heat stress constrained by atmospheric dynamics53
Microbial methylation potential of mercury sulfide particles dictated by surface structure52
A UK perspective on tackling the geoscience racial diversity crisis in the Global North51
Global chemical weathering dominated by continental arcs since the mid-Palaeozoic51
Dominant role of mineral dust in cirrus cloud formation revealed by global-scale measurements49
Manage fire regimes, not fires49
Half of global agricultural soil phosphorus fertility derived from anthropogenic sources49
Reservoir CO2 and CH4 emissions and their climate impact over the period 1900–206048
Amplified warming of extreme temperatures over tropical land48
Biogenic particles formed in the Himalaya as an important source of free tropospheric aerosols47
Persistent orbital influence on millennial climate variability through the Pleistocene47
Disproportionate control on aerosol burden by light rain47
Sinking enhances the degradation of organic particles by marine bacteria47
Decolonizing geoscience requires more than equity and inclusion47
Impact of warmer climate periods on flood hazard in the European Alps46
Late Ordovician climate change and extinctions driven by elevated volcanic nutrient supply45
Increased night-time oxidation over China despite widespread decrease across the globe45
Soil organic matter formation and loss are mediated by root exudates in a temperate forest45
Agricultural drought over water-scarce Central Asia aggravated by internal climate variability45
Long-distance atmospheric transport of microplastic fibres influenced by their shapes45
Explosive or effusive style of volcanic eruption determined by magma storage conditions45
Winter particulate pollution severity in North China driven by atmospheric teleconnections44
Global patterns of water storage in the rooting zones of vegetation44
Temperature control on CO2 emissions from the weathering of sedimentary rocks44
Earth’s Great Oxidation Event facilitated by the rise of sedimentary phosphorus recycling44
The role of environmental factors in the long-term evolution of the marine biological pump43
Distinct slab interfaces imaged within the mantle transition zone42
Calibrating the marine turbidite palaeoseismometer using the 2016 Kaikōura earthquake41
A further source of Tokyo earthquakes and Pacific Ocean tsunamis41
Effect of tectonic processes on biosphere–geosphere feedbacks across a convergent margin41
Spatiotemporal clustering of great earthquakes on a transform fault controlled by geometry41
Heinrich Stadial aridity forced Mediterranean-wide glacier retreat in the last cold stage40
Conservation slows down emission increase from a tropical peatland in Indonesia40
A world view of pesticides40
Newly formed craters on Mars located using seismic and acoustic wave data from InSight40
Decline in bulk deposition of air pollutants in China lags behind reductions in emissions40
Carbon fixation rates in groundwater similar to those in oligotrophic marine systems40
Superionic iron oxide–hydroxide in Earth’s deep mantle40
Vertical decoupling in Late Ordovician anoxia due to reorganization of ocean circulation39
Slab-derived devolatilization fluids oxidized by subducted metasedimentary rocks38
Springtime arctic ozone depletion forces northern hemisphere climate anomalies38
Twentieth-century Azores High expansion unprecedented in the past 1,200 years38
Antarctic ice-shelf advance driven by anomalous atmospheric and sea-ice circulation38
Equal abundance of summertime natural and wintertime anthropogenic Arctic organic aerosols38
Sea spray as an obscured source for marine cloud nuclei38
Rates of protoplanetary accretion and differentiation set nitrogen budget of rocky planets38
Amazonian forest degradation must be incorporated into the COP26 agenda38
Lunar compositional asymmetry explained by mantle overturn following the South Pole–Aitken impact37
Large subglacial source of mercury from the southwestern margin of the Greenland Ice Sheet37
Quantifying the physical processes leading to atmospheric hot extremes at a global scale37
Surface characteristics of the Zhurong Mars rover traverse at Utopia Planitia37
Machine learning reveals climate forcing from aerosols is dominated by increased cloud cover37
Rapid glacier retreat rates observed in West Antarctica36
Sub-aerial talik formation observed across the discontinuous permafrost zone of Alaska36
The vertical structure of CO in the Martian atmosphere from the ExoMars Trace Gas Orbiter36
Contrasting effects of aridity and seasonality on global salinization36
Shortwave absorption by wildfire smoke dominated by dark brown carbon36
Direct astronomical influence on abrupt climate variability36
Pyrogenic carbon decomposition critical to resolving fire’s role in the Earth system36
Eruptive activity of the Santorini Volcano controlled by sea-level rise and fall35
Constraint on net primary productivity of the global ocean by Argo oxygen measurements35
Methane hydrate dissociation across the Oligocene–Miocene boundary35
Atlantic circulation change still uncertain35
Drivers of river reactivation in North Africa during the last glacial cycle34
Carbon concentration increases with depth of melting in Earth’s upper mantle34
Oxygen priming induced by elevated CO2 reduces carbon accumulation and methane emissions in coastal wetlands34
Southeast Asian ecological dependency on Tibetan Plateau streamflow over the last millennium33
Possible link between Earth’s rotation rate and oxygenation33
Acceleration of a large deep-seated tropical landslide due to urbanization feedbacks33
Risks to carbon storage from land-use change revealed by peat thickness maps of Peru32
Atmospheric CO2 control of spontaneous millennial-scale ice age climate oscillations32
Fault strength and rupture process controlled by fault surface topography32
Fluid migration in low-permeability faults driven by decoupling of fault slip and opening32
Influence of biogenic emissions from boreal forests on aerosol–cloud interactions32
A poorly mixed mantle transition zone and its thermal state inferred from seismic waves32
Arctic Ocean stratification set by sea level and freshwater inputs since the last ice age32
Cyclical geothermal unrest as a precursor to Iceland’s 2021 Fagradalsfjall eruption32
Mapping peat thickness and carbon stocks of the central Congo Basin using field data31
Postseismic geodetic signature of cold forearc mantle in subduction zones31
Neogene South Asian monsoon rainfall and wind histories diverged due to topographic effects31
Implications of the iron oxide phase transition on the interiors of rocky exoplanets31
Rapid retreat of Thwaites Glacier in the pre-satellite era31
Multi-decadal trends in Antarctic sea-ice extent driven by ENSO–SAM over the last 2,000 years31
Boosting geoscience data sharing in China30
The global contribution of soil mosses to ecosystem services30
A century of groundwater accumulation in Pakistan and northwest India30
Persistent late Permian to Early Triassic warmth linked to enhanced reverse weathering30
Oceanic transform fault seismicity and slip mode influenced by seawater infiltration30
Phosphorus availability on the early Earth and the impacts of life30
Upper-plate controls on subduction zone geometry, hydration and earthquake behaviour30
Fire enhances forest degradation within forest edge zones in Africa30
Forest vulnerability to drought controlled by bedrock composition29
A pole-to-equator ocean overturning circulation on Enceladus29
Decreasing subseasonal temperature variability in the northern extratropics attributed to human influence29
Archaean seafloors shallowed with age due to radiogenic heating in the mantle28
Recent strengthening of snow and ice albedo feedback driven by Antarctic sea-ice loss28
Enhanced dust emission following large wildfires due to vegetation disturbance28
Global dominance of tectonics over climate in shaping river longitudinal profiles28
Uncertainty in US forest carbon storage potential due to climate risks28
High water content of arc magmas recorded in cumulates from subduction zone lower crust27
Submarine melting of glaciers in Greenland amplified by atmospheric warming27
Stress, rigidity and sediment strength control megathrust earthquake and tsunami dynamics27
Dynamic history of the inner core constrained by seismic anisotropy27
A solar wind-derived water reservoir on the Moon hosted by impact glass beads27
Paleofloods stage a comeback27
End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia27
Dynamics of the abrupt change in Pacific Plate motion around 50 million years ago27
Fracturing and healing of basaltic magmas during explosive volcanic eruptions26
Distinct sources of interannual subtropical and subpolar Atlantic overturning variability26
Continuum of earthquake rupture speeds enabled by oblique slip26
Sustained emission reductions have restrained the ozone pollution over China26
Nonlinear forcing of climate on mountain denudation during glaciations26
Regulation of ionospheric plasma velocities by thermospheric winds25
Impaired viral infection and reduced mortality of diatoms in iron-limited oceanic regions25
Correlation of porosity variations and rheological transitions on the southern Cascadia megathrust25
Abrupt episode of mid-Cretaceous ocean acidification triggered by massive volcanism25
Increased interglacial atmospheric CO2 levels followed the mid-Pleistocene Transition25
Pleistocene climate variability in eastern Africa influenced hominin evolution25
Emergence of Southern Hemisphere stratospheric circulation changes in response to ozone recovery25
Diminishing lake area across the northern permafrost zone25
Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean25
Transient ocean oxygenation at end-Permian mass extinction onset shown by thallium isotopes25
An unshakable carbon budget for the Himalaya25
Simple shear origin of the cross-faults ruptured in the 2019 Ridgecrest earthquake sequence25
Astronomically controlled aridity in the Sahara since at least 11 million years ago25
Temporal patterns of soil carbon emission in tropical forests under long-term nitrogen deposition25
Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO225
Muted multidecadal climate variability in central Europe during cold stadial periods24
Asthenospheric low-velocity zone consistent with globally prevalent partial melting24
Accrual of widespread rock damage from the 2019 Ridgecrest earthquakes24
Brittle fragmentation by rapid gas separation in a Hawaiian fountain24
Penultimate deglaciation Asian monsoon response to North Atlantic circulation collapse24
Climate-driven decoupling of wetland and upland biomass trends on the mid-Atlantic coast24
Subslab heterogeneity and giant megathrust earthquakes24
Crater population on asteroid (101955) Bennu indicates impact armouring and a young surface24
Substantial contribution of iodine to Arctic ozone destruction23
The biogeochemical balance of oceanic nickel cycling23
Limited carbon cycling due to high-pressure effects on the deep-sea microbiome23
The diverse meteorology of Jezero crater over the first 250 sols of Perseverance on Mars23
Shutdown of Southern Ocean convection controls long-term greenhouse gas-induced warming23
Recovery from microplastic-induced marine deoxygenation may take centuries23
Topographic stress control on bedrock landslide size23
Jurassic greenhouse ice-sheet fluctuations sensitive to atmospheric CO2 dynamics23
Bedrock weathering contributes to subsurface reactive nitrogen and nitrous oxide emissions23
Oxygenation of the Earth aided by mineral–organic carbon preservation22
Dissolved organic phosphorus concentrations in the surface ocean controlled by both phosphate and iron stress22
Reduced phosphorus availability in paddy soils under atmospheric CO2 enrichment22
Increased typhoon activity in the Pacific deep tropics driven by Little Ice Age circulation changes22
Global patterns in marine organic matter stoichiometry driven by phytoplankton ecophysiology22
The future lifespan of Earth’s oxygenated atmosphere22
Machine learning in Earth and environmental science requires education and research policy reforms22
Dominant role of soil moisture in mediating carbon and water fluxes in dryland ecosystems22
Antarctic basal environment shaped by high-pressure flow through a subglacial river system21
Underestimated burden of per- and polyfluoroalkyl substances in global surface waters and groundwaters21
Earth-like lithospheric thickness and heat flow on Venus consistent with active rifting21
Fluid transport and storage in the Cascadia forearc influenced by overriding plate lithology21
Geometric controls on cascading rupture of the 2023 Kahramanmaraş earthquake doublet21
Glacial deep ocean deoxygenation driven by biologically mediated air–sea disequilibrium21
Nitrogen isotopic constraints on nutrient transport to the upper ocean21
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