Global Biogeochemical Cycles

Papers
(The H4-Index of Global Biogeochemical Cycles is 29. 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 2021-05-01 to 2025-05-01.)
ArticleCitations
Temporal Variability of Air‐Sea CO2 flux in the Western Tropical North Atlantic Influenced by the Amazon River Plume153
The Diel Cycle of Surface Ocean Elemental Stoichiometry has Implications for Ocean Productivity80
Issue Information76
Issue Information74
Simultaneous Production and Consumption of Soil N2O Creates Complex Effects on Its Stable Isotope Composition72
Direct and Indirect Drivers of Energy and Nutrient Availability in Freshwater Ecosystems Across Spatial Scales60
Refractory Dissolved Organic Matter has Similar Chemical Characteristics but Different Radiocarbon Signatures With Depth in the Marine Water Column56
Global Contrasts Between Oceanic Cycling of Cadmium and Phosphate54
Influence of Changes in pH and Temperature on the Distribution of Apparent Iron Solubility in the Oceans49
Atmospheric Oxygen Abundance, Marine Nutrient Availability, and Organic Carbon Fluxes to the Seafloor47
Meltwater Discharge From Marine‐Terminating Glaciers Drives Biogeochemical Conditions in a Greenlandic Fjord44
Carbon and Greenhouse Gas Budgets of Europe: Trends, Interannual and Spatial Variability, and Their Drivers42
The Global Biogeochemical Cycle of Arsenic41
Quantifying Soil Gaseous Nitrogen Losses From Nitrification and Denitrification Based on Nitrogen Isotope Model36
Bioactive Trace Metals and Their Isotopes as Paleoproductivity Proxies: An Assessment Using GEOTRACES‐Era Data36
Organic Carbon Burial With Reactive Iron Across Global Environments36
Centennial‐Scale Storage of DOC Within Arctic Ocean Deep Waters Controlled by Subzero Temperatures36
Tracing Pan‐Canadian Arctic Water Masses and Dissolved Inorganic Carbon Cycling Using Stable and Radiocarbon Isotopes35
South Asia's Ecosystems Are a Net Carbon Sink, But the Region Is a Major Net GHG Source to the Atmosphere34
Biological Carbon Pump Sequestration Efficiency in the North Atlantic: A Leaky or a Long‐Term Sink?34
Effects of Afforestation on Soil Carbon and Nitrogen Accumulation Depend on Initial Soil Nitrogen Status33
Remote Sensing Soil Freeze‐Thaw Status and North American N2O Emissions From a Regional Inversion32
Influence of Seasonal Variability in Flux Attenuation on Global Organic Carbon Fluxes and Nutrient Distributions32
Issue Information32
Issue Information31
Why are Surface Ocean pH and CaCO3 Saturation State Often out of Phase in Spatial Patterns and Seasonal Cycles?31
Global Patterns of Surface Ocean Dissolved Organic Matter Stoichiometry30
Enhanced Biogeochemical Cycling Along the U.S. West Coast Shelf30
Issue Information30
Bottom‐Up Evaluation of the Methane Budget in Asia and Its Subregions29
How Is the Ocean Anthropogenic Carbon Reservoir Filled?29
Asymmetric Impacts of Diurnal Warming on Vegetation Carbon Sequestration of Marshes in the Qinghai Tibet Plateau29
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