OOIR: Observatory of International Research

Papers

(The H4-Index of Global Biogeochemical Cycles is 33. 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 2022-01-01 to 2026-01-01.)

Article	Citations
The Role of Ballasting, Seawater Viscosity and Oxygen‐Dependent Remineralization for Export and Transfer Efficiencies in the Global Ocean	218
Influence of Seasonal Variability in Flux Attenuation on Global Organic Carbon Fluxes and Nutrient Distributions	82
The Role of Sediments in Modulating Nitrous Oxide Production in the Southern Benguela Upwelling System: Insights From Stable Isotopic Tracers	78
Influence of Changes in pH and Temperature on the Distribution of Apparent Iron Solubility in the Oceans	75
Direct and Indirect Drivers of Energy and Nutrient Availability in Freshwater Ecosystems Across Spatial Scales	74
Issue Information	67
The Diel Cycle of Surface Ocean Elemental Stoichiometry has Implications for Ocean Productivity	64
Centennial‐Scale Storage of DOC Within Arctic Ocean Deep Waters Controlled by Subzero Temperatures	62
Quantifying Soil Gaseous Nitrogen Losses From Nitrification and Denitrification Based on Nitrogen Isotope Model	58
Simultaneous Production and Consumption of Soil N₂O Creates Complex Effects on Its Stable Isotope Composition	57
Atmospheric Oxygen Abundance, Marine Nutrient Availability, and Organic Carbon Fluxes to the Seafloor	56
Meltwater Discharge From Marine‐Terminating Glaciers Drives Biogeochemical Conditions in a Greenlandic Fjord	55
Issue Information	50
Divergent Microbial Nitrogen‐Limitation Dynamics Between Primary and Secondary Succession in Subalpine Ecosystems of the Eastern Tibetan Plateau	49
Carbon and Greenhouse Gas Budgets of Europe: Trends, Interannual and Spatial Variability, and Their Drivers	46
South Asia's Ecosystems Are a Net Carbon Sink, But the Region Is a Major Net GHG Source to the Atmosphere	45
Refractory Dissolved Organic Matter has Similar Chemical Characteristics but Different Radiocarbon Signatures With Depth in the Marine Water Column	44
The Global Biogeochemical Cycle of Arsenic	43
Biological Carbon Pump Sequestration Efficiency in the North Atlantic: A Leaky or a Long‐Term Sink?	42
Tracing Pan‐Canadian Arctic Water Masses and Dissolved Inorganic Carbon Cycling Using Stable and Radiocarbon Isotopes	42
Effects of Afforestation on Soil Carbon and Nitrogen Accumulation Depend on Initial Soil Nitrogen Status	42
Remote Sensing Soil Freeze‐Thaw Status and North American N₂O Emissions From a Regional Inversion	41
Organic Carbon Burial With Reactive Iron Across Global Environments	40
The Pan‐Arctic Continental Slope as an Intensifying Conveyer Belt for Nutrients in the Central Arctic Ocean (1985–2015)	40
Issue Information	39

Issue Information	39
Issue Information	38
Enhanced Biogeochemical Cycling Along the U.S. West Coast Shelf	37
More Foxes than Hedgehogs: The Case for Nitrogen Fixation in Coastal Marine Sediments	35
Global Patterns of Surface Ocean Dissolved Organic Matter Stoichiometry	34
Asymmetric Impacts of Diurnal Warming on Vegetation Carbon Sequestration of Marshes in the Qinghai Tibet Plateau	34
Bottom‐Up Evaluation of the Methane Budget in Asia and Its Subregions	34
Underestimated Carbon Losses as Dissolved Organic Carbon in Forested Headwater Streams	33