Global Biogeochemical Cycles

Papers
(The H4-Index of Global Biogeochemical Cycles is 32. 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 2021-11-01 to 2025-11-01.)
ArticleCitations
South Asia's Ecosystems Are a Net Carbon Sink, But the Region Is a Major Net GHG Source to the Atmosphere205
Tracing Pan‐Canadian Arctic Water Masses and Dissolved Inorganic Carbon Cycling Using Stable and Radiocarbon Isotopes83
The Role of Sediments in Modulating Nitrous Oxide Production in the Southern Benguela Upwelling System: Insights From Stable Isotopic Tracers80
Simultaneous Production and Consumption of Soil N2O Creates Complex Effects on Its Stable Isotope Composition73
Remote Sensing Soil Freeze‐Thaw Status and North American N2O Emissions From a Regional Inversion71
Organic Carbon Burial With Reactive Iron Across Global Environments68
Biological Carbon Pump Sequestration Efficiency in the North Atlantic: A Leaky or a Long‐Term Sink?61
Issue Information60
Direct and Indirect Drivers of Energy and Nutrient Availability in Freshwater Ecosystems Across Spatial Scales52
The Diel Cycle of Surface Ocean Elemental Stoichiometry has Implications for Ocean Productivity52
Influence of Changes in pH and Temperature on the Distribution of Apparent Iron Solubility in the Oceans52
Issue Information49
Centennial‐Scale Storage of DOC Within Arctic Ocean Deep Waters Controlled by Subzero Temperatures45
Refractory Dissolved Organic Matter has Similar Chemical Characteristics but Different Radiocarbon Signatures With Depth in the Marine Water Column45
Carbon and Greenhouse Gas Budgets of Europe: Trends, Interannual and Spatial Variability, and Their Drivers44
The Role of Ballasting, Seawater Viscosity and Oxygen‐Dependent Remineralization for Export and Transfer Efficiencies in the Global Ocean43
Quantifying Soil Gaseous Nitrogen Losses From Nitrification and Denitrification Based on Nitrogen Isotope Model43
Effects of Afforestation on Soil Carbon and Nitrogen Accumulation Depend on Initial Soil Nitrogen Status42
Meltwater Discharge From Marine‐Terminating Glaciers Drives Biogeochemical Conditions in a Greenlandic Fjord41
The Global Biogeochemical Cycle of Arsenic39
Influence of Seasonal Variability in Flux Attenuation on Global Organic Carbon Fluxes and Nutrient Distributions39
The Pan‐Arctic Continental Slope as an Intensifying Conveyer Belt for Nutrients in the Central Arctic Ocean (1985–2015)37
Bioactive Trace Metals and Their Isotopes as Paleoproductivity Proxies: An Assessment Using GEOTRACES‐Era Data37
Atmospheric Oxygen Abundance, Marine Nutrient Availability, and Organic Carbon Fluxes to the Seafloor37
Issue Information36
Issue Information36
Issue Information36
Bottom‐Up Evaluation of the Methane Budget in Asia and Its Subregions35
More Foxes than Hedgehogs: The Case for Nitrogen Fixation in Coastal Marine Sediments34
The Impact of Zooplankton Calcifiers on the Marine Carbon Cycle33
Contrasting Responses of Soil Inorganic Carbon to Afforestation in Acidic Versus Alkaline Soils33
The Biotic‐Abiotic Control of Si Burial in Marine Carbonate Systems of the Pre‐Eocene Si Cycle32
Biological, Biogeochemical, Bio‐Optical, and Physical Variability of the Southern Ocean Along 150°W and Its Relevance to the Great Calcite Belt32
Off‐Shelf Transport and Biogeochemical Cycling of Terrestrial Organic Carbon Along the East Siberian Continental Margin32
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