Limnology and Oceanography

Papers
(The TQCC of Limnology and Oceanography is 8. 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 2021-08-01 to 2025-08-01.)
ArticleCitations
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Bottom‐up as well as top‐down processes govern zoobenthic secondary production in a tidal‐flat ecosystem33
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Grazing by an endemic atyid shrimp controls microbial communities in the Hawaiian anchialine ecosystem32
Nutrient function over form: Organic and inorganic nitrogen additions have similar effects on lake phytoplankton nutrient limitation32
Phytoplankton size distributions in the western North Atlantic and their seasonal variability32
Unexpected functional diversity of stream biofilms within and across proglacial floodplains despite close spatial proximity32
Outwelling of reduced porewater drives the biogeochemistry of dissolved organic matter and trace metals in a major mangrove‐fringed estuary in Amazonia31
Carbon isotopic constraints on the degradation and sequestration of organic matter in river‐influenced marginal sea sediments31
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Differences in bed elevation shape subtidal mussel bed stability under high‐energy hydrodynamic events30
Phytoplankton community response to a drought‐to‐wet climate transition in a subtropical estuary30
Ubiquitous but unique: Water depth and oceanographic attributes shape methane seep communities30
Role of virus‐mediated lysis in spatiotemporal dynamics of prokaryotic communities in river–estuary–coastal ecosystems29
Experimental nutrient enrichment of forest streams reduces ecosystem nitrogen and phosphorus storage29
Prolific nitrite reoxidation across the Eastern Tropical North Pacific Ocean29
Reference state, structure, regime shifts, and regulatory drivers in a coastal sea over the last century: The Central Baltic Sea case27
Patchiness of plankton communities at fronts explained by Lagrangian history of upwelled water parcels27
Effects of spatially heterogeneous lakeside development on nearshore biotic communities in a large, deep, oligotrophic lake26
The role of internal nitrogen loading in supportingnon‐N‐fixing harmful cyanobacterial blooms in the water column of a large eutrophic lake26
Responses of biogenic dimethylated sulfur compounds to environmental changes in the northwestern Pacific continental sea26
Thermal plasticity of coral reef symbionts is linked to major alterations in their lipidome composition26
Correction to “Cascading, interactive, and indirect effects of climate change on aquatic communities, habitats, and ecosystems”26
Phytoplankton absorb mainly red light in lakes with high chromophoric dissolved organic matter26
Toward trait‐based food webs: Universal traits and trait matching in planktonic predator–prey and host–parasite relationships25
The grazing impact of megaherbivores on sediment accumulation and stabilization functions of seagrass meadows in a subtropical coral reef lagoon25
In situ aerobic methane oxidation rates in a stratified lake24
Temperature‐dependent evolution of cell morphology and carbon and nutrient content in a marine diatom24
Biogeochemical states, rates, and exchanges exhibit linear responses to large nutrient load reductions in a shallow, eutrophic urban estuary24
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Shortcomings of the dissipation rate for understanding the turbulent environment of plankton—And a potential solution23
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Changes to upper‐ocean ecosystems may directly impact abyssal scavenger communities23
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Life in turbulent waters: unsteady biota–flow interactions across scales22
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Applying empirical dynamic modeling to distinguish abiotic and biotic drivers of population fluctuations in sympatric fishes21
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Controls on buffering and coastal acidification in a temperate estuary21
Long‐term nutrient load reductions and increasing lake TN : TP stoichiometry decrease phytoplankton biomass and diversity in a large shallow lake21
A missing trophic link: Contribution of the microbial loop to the estimation of the trophic position of pelagic consumers21
Long‐range transport of littoral methane explains the metalimnetic methane peak in a large lake20
The Amazon shelf sediments, a reactor that fuels intense nitrogen cycling at the seabed20
Potential role of submerged macrophytes for oxic methane production in aquatic ecosystems20
Mechanisms and fluid dynamics of foraging in heterotrophic nanoflagellates20
Natural and anthropogenic controls on lake water‐level decline and evaporation‐to‐inflow ratio in the conterminous United States20
The effects of disturbance on the microbial mediation of sediment stability20
Effect of a tropical cyclone on the pelagic ecosystem of a continental shelf20
Impact of shallow‐water hydrothermal seepage on benthic biogeochemical cycling, nutrient availability, and meiobenthic communities in a tropical coral reef20
High‐resolution water‐quality and ecosystem‐metabolism modeling in lowland rivers20
Oceanic turbulence from a planktonic perspective19
Phosphorus enrichment increases the prevalence of a microsporidian parasite in experimental Daphnia populations19
Multi‐omics analyses reveal the signatures of metabolite transfers across trophic levels in a high‐CO2 ocean19
Stability of chironomid community structure during historic climatic and environmental change in subarctic Alaska19
Meadow trophic status regulates the nitrogen filter function of tropical seagrasses in seasonally eutrophic coastal waters19
New evaluation of species‐specific biogenic silica flux of radiolarians (Rhizaria) in the western Arctic Ocean using microfocus X‐ray computed tomography19
Sea ice breakup and nutrient supply regulate the timing and magnitude of algal export over the slopes of the Pacific Arctic region19
Dissolved organic matter mediates the effects of warming and inorganic nutrients on a lake planktonic food web19
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Resolving abrupt frontal gradients in zooplankton community composition and marine snow fields with an autonomous Zooglider18
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Autonomous instrumentation and big data: New windows, knowledge, and breakthroughs in the aquatic sciences18
Multigenerational physiological compensation and body size reduction dampen the effects of warming on copepods18
Concurrent DNA meta‐barcoding and plankton imaging reveal novel parasitic infection and competition in a diatom18
Mechanisms underlying lack of functional compensation by insect grazers after tadpole declines in a Neotropical stream17
The influence of environmental parameters on spatial variation in zoobenthic density and stable isotopes (δ13C, δ15N, and δ34S) within17
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Nutritional response of a coccolithophore to changing pH and temperature17
Patterns of siderophore production and utilization at Station ALOHA from the surface to mesopelagic waters17
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The role of tides and winds in shaping seed dispersal in coastal wetlands17
Investigating transport in a tidally driven coral atoll flow using Lagrangian coherent structures17
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Why do algal blooms intensify under reduced nitrogen and fluctuating phosphorus conditions: The underappreciated role of non‐algal light attenuation16
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Terrestrial support of wetland food webs via a dissolved inorganic carbon pathway16
Co‐acquisition of mineral‐bound iron and phosphorus by natural Trichodesmium colonies16
Limited degradability of dissolved organic carbon, nitrogen, and phosphorus during contrasting seasons in a tropical coastal environment16
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Summer ecosystem structure in mountain lakes linked to interannual variability of lake ice, snowpack, and landscape attributes16
High‐frequency variability dominates potential connectivity between remote coral reefs16
The interaction between vegetation patchiness and tidal flows in a shortleaf seagrass meadow16
Unexpectedly stable soil organic carbon in tidal marshes under combined nitrogen loading and increased inundation compared to individual effects16
Summer sea ice melting enhances phytoplankton and dimethyl sulfide production16
Geochemical focusing and burial of sedimentary iron, manganese, and phosphorus during lake eutrophication16
Mass deposition of microbes from wildfire smoke to the sea surface microlayer15
Basin‐scale estimates of greenhouse gas emissions from the Mara River, Kenya: Importance of discharge, stream size, and land use/land cover15
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Biogeochemical‐Argo data suggest significant contributions of small particles to the vertical carbon flux in the subpolar North Atlantic15
Variability in lake bacterial growth and primary production under lake ice: Evidence from early winter to spring melt15
Shifting phenology as a key driver of shelf zooplankton population variability15
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Pteropods as early‐warning indicators of ocean acidification15
Role of particle dynamics in processing of terrestrial nitrogen and phosphorus in the estuarine mixing zone15
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Methanogens limited to lower rhizosphere and to an atypical salt marsh niche along a pristine intertidal mangrove continuum14
Hydrology mediates salt marsh belowground biomass response to warming14
A simple‐wave damping model for flexible marsh plants14
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Organic carbon dynamics and microbial community response to oyster reef restoration14
Contribution of gas concentration and transfer velocity to CO2 flux variability in northern lakes14
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Differential impacts of pH on growth, physiology, and elemental stoichiometry across three coccolithophore species14
Biogeochemical cycling of Cd, Mn, and Ce in the Eastern Tropical North Pacific oxygen‐deficient zone14
Size distribution of aggregates across different aquatic systems around Japan shows that stronger aggregates are formed under turbulence14
An intense precipitation event causes a temperate forested drainage network to shift from N2O source to sink14
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Corrigendum: A trait‐based carbon export model for mesopelagic fishes in the Gulf of Mexico with consideration of asynchronous vertical migration, flux boundaries, and feeding guilds14
Vertical and horizontal variations in phytoplankton chlorophyll a in response to a looping super typhoon14
Deep‐sea wooden shipwrecks influence sediment microbiome diversity13
Nitrogen stable isotopes (δ15N) and tissue nitrogen in shallow‐water and mesophotic macroalgae differ between the Main Hawaiian Islands and the Northwestern Hawaiian Islan13
Transport and reactivity of nitrous oxide and methane in two contrasting subterranean estuaries13
“Slow” and “fast” in blue carbon: Differential turnover of allochthonous and autochthonous organic matter in minerogenic salt marsh sediments13
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Autonomous observations enhance our ability to observe the biological carbon pump across diverse carbon export regimes13
Blue carbon additionality: New insights from the radiocarbon content of saltmarsh soils and their respired CO213
Deep photoautotrophic prokaryotes contribute substantially to carbon dynamics in oxygen‐deficient waters in a permanently redox‐stratified freshwater lake13
Responses of microbial communities and greenhouse gas production to land use change in mangrove wetland sediments13
Corrigendum: Food sources drive temporal variation in elemental stoichiometry of benthic consumers13
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Sediment oxygen consumption in Antarctic subglacial environments13
The experimental implications of the rate of temperature change and timing of nutrient availability on growth and stoichiometry of a natural marine phytoplankton community13
Dependency of Arctic zooplankton on pelagic food sources: New insights from fatty acid and stable isotope analyses13
Dynamics of surface accretion and surface elevation differ between river and tide dominated settings in tropical mangroves13
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Climate change–induced terrestrial matter runoff may decrease food web production in coastal ecosystems13
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Coral rubble dynamics in the Anthropocene and implications for reef recovery12
Variability in the phytoplankton response to upwelling across an iron limitation mosaic within the California current system12
Consistent prokaryotic successional dynamics across contrasting phytoplankton blooms12
Dissolved organic compounds with synchronous dynamics share chemical properties and origin12
Increasing acidification does not affect sexual reproduction of a solitary zooxanthellate coral transplanted at a carbon dioxide vent12
Tidal control and mangrove dieback impact on methane emissions from a subtropical mangrove estuary12
In situ observations of zooplankton show changes in abundance and swimming speed in response to hypoxia and acidification12
Calcification increases carbon supply, photosynthesis, and growth in a globally distributed coccolithophore12
Plankton community composition and productivity near the Subantarctic Prince Edward Islands archipelago in autumn12
Oxygen‐deficient water zones in the Baltic Sea promote uncharacterized Hg methylating microorganisms in underlying sediments12
Isotopic signatures of biotic and abiotic N2O production and consumption in the water column of meromictic, ferruginous Lake La Cruz (Spain)12
Enhanced benthic nitrous oxide and ammonium production after natural oxygenation of long‐term anoxic sediments12
Nutrient‐dependent thermal response in growth and stoichiometry of Antarctic phytoplankton12
Seafloor bioturbation intensity on the deep sea: More complex than organic matter12
Bacterial biogeography of the Indian Ocean12
Elevated dissolved carbon dioxide and associated acidification delays maturation and decreases calcification and survival in the freshwater crustacean Daphnia magna12
Fluorescence as a tracer of the susceptibility of dissolved organic matter to photodegradation in the Arctic Ocean12
Relative depths of the subsurface peaks of phytoplankton abundance conserved over ocean provinces12
Searching for drivers of the patchy distribution of sympatric deposit‐feeding sea cucumbers: A multi‐scale monitoring study12
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Seasonal drivers of dissolved oxygen across a tidal creek–marsh interface revealed by machine learning12
Co‐occurrence and successional patterns among diatoms, dinoflagellates, and potential parasites in a coastal upwelling experiment11
Promoting effects of aluminum addition on chlorophyll biosynthesis and growth of two cultured iron‐limited marine diatoms11
Grazer‐induced toxin production is energetically costly and significantly reduces growth of cylindrospermopsin‐producing cyanobacteria11
Quantitative visual analysis of marine barite microcrystals: Insights into precipitation and dissolution dynamics11
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Invertebrate trophic structure on marine ferromanganese and phosphorite hardgrounds11
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Depth and basin shape constrain ecosystem metabolism in lakes dominated by benthic primary producers11
Inorganic carbon dynamics and their relation to autotrophic community regime shift over three decades in a large, alkaline river11
Correction to “A 7‐yr spatial time series resolves the island mass effect and associated shifts in picocyanobacteria abundances near O'ahu, Hawai'i”11
Different forms of carbon, nitrogen, and phosphorus influence ecosystem stoichiometry in a north temperate river across seasons and land uses11
Carbon production at shallow‐water artificial reef ecosystems relies on water column primary productivity11
Dynamics of alongshore current in the Taiwan Strait: A perspective on the southward Kuroshio branch in winter11
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The effect of vorticity on the feeding of a freshwater grazer11
Food web structure and intraguild predation affect ecosystem functioning in an established plankton model11
Uncertainty sources for measurable ocean carbonate chemistry variables11
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Wind‐driven currents and water masses shape spring phytoplankton distribution and composition in hydrologically complex, productive shelf waters11
Holocene climate change shifted Southern Ocean biogeochemical cycling and predator trophic dynamics11
Effect of increased CO2 on calcium homeostasis and signaling in a marine diatom11
Epiphyton phenology determines the persistence of submerged macrophytes: Exemplified in temperate shallow lakes11
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Drivers of phytoplankton responses to summer wind events in a stratified lake: A modeling study11
Recovery trends of reef carbonate budgets at remote coral atolls 6 years post‐bleaching11
Nutrient availability influences the thermal response of marine diatoms10
Heterotrophy of particulate organic matter subsidies contributes to divergent bleaching responses in tropical Scleractinian corals10
Differential effects of elevated pCO2 and warming on marine phytoplankton stoichiometry10
Net ecosystem dissolution and respiration dominate metabolic rates at two western Atlantic reef sites10
Recovery of denitrification and dissimilatory nitrate reduction to ammonium following reoxygenation of sediments from a periodically hypoxic temperate lagoon10
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On the fundamental additive modes of ocean color absorption10
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P inputs determine denitrifier abundance explaining dissolved nitrous oxide in reservoirs10
A sprinkling of gold dust: Pine pollen as a carbon source in Baltic Sea coastal food webs10
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Microplastics stress alters microorganism community structure and reduces the production of biogenic dimethylated sulfur compounds10
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Factors regulating the concentration of particulate iodine in coastal seawater10
Variation in sediment and seagrass characteristics reflect multiple stressors along a nitrogen‐enrichment gradient in a New England lagoon10
Terrestrial input of herbicides has significant impacts on phytoplankton and bacterioplankton communities in coastal waters10
Synchrony dynamics of dissolved organic carbon in high‐mountain streams: Insights into scale‐dependent processes10
Do phytoplankton require oxygen to survive? A hypothesis and model synthesis from oxygen minimum zones10
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Cyclical prey shortages for a marine polar predator driven by the interaction of climate change and natural climate variability10
Distinct drivers of two size fractions of operationally dissolved iron in a temperate river10
Spatiotemporal variability of dissolved inorganic macronutrients along the northern Antarctic Peninsula (1996–2019)10
Highest primary production achieved at high nitrogen levels despite strong stoichiometric imbalances with phosphorus in hypereutrophic experimental systems10
Ingestion and respiration rates of a common coastal mysid respond differently to diurnal temperature fluctuation10
Geographic variation in organic carbon storage by seagrass beds10
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Effect of marine heat waves on carbon metabolism, optical characterization, and bioavailability of dissolved organic carbon in coastal vegetated communities10
Scallop shells as geochemical archives of phytoplankton‐related ecological processes in a temperate coastal ecosystem10
High rates of erosion on a wave‐exposed fringing coral reef9
Highly mobile pelagic species co‐occur with fine‐scale ocean fronts9
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Seasonally migrating zooplankton strongly enhance Southern Ocean carbon sequestration9
Strain‐dependent and host genotype–dependent priority effects in gut microbiome assembly affect host fitness in Daphnia9
Predicting larval alewife transport in Lake Michigan using hydrodynamic and Lagrangian particle dispersion models9
Biological sources and sinks of dimethylsulfide disentangled by an induced bloom experiment and a numerical model9
Higher alpha and gamma, but not beta diversity in tropical than in Mediterranean temporary ponds: A multi‐taxon spatiotemporal approach9
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Gross oxygen production and microbial community respiration in the oligotrophic ocean9
Copepod egg production estimates are biased by female mortality9
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Successful acclimation of marine diatoms Chaetoceros curvisetus/pseudocurvisetus to climate change9
Can intense storms affect sinking particle dynamics after the North Atlantic spring bloom?9
Seasonal hypoxia and temperature inversions in a tropical bay9
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Nutrient inversion but not warming drive changes in periphyton biomass and composition in shallow lake mesocosms9
Coral reef erosion: In situ measurement on different dead coral substrates on a Caribbean reef9
Seasonal patterns in nutrient bioavailability in boreal headwater streams9
Dark carbon fixation in stream carbon cycling9
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