Limnology and Oceanography

Papers
(The TQCC of Limnology and Oceanography is 7. 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 2022-05-01 to 2026-05-01.)
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Experimental nutrient enrichment of forest streams reduces ecosystem nitrogen and phosphorus storage37
Patchiness of plankton communities at fronts explained by Lagrangian history of upwelled water parcels35
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Ascidians increase in abundance on tropicalized reefs and may enhance benthic nitrous oxide production32
Broad‐scale climate patterns combined with local flow and turbidity disturbances structure the seasonality of gross primary production in an aridland river31
Bottom‐up as well as top‐down processes govern zoobenthic secondary production in a tidal‐flat ecosystem30
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Phytoplankton size distributions in the western North Atlantic and their seasonal variability28
Environmental controls of autotrophic biofilm biomass and community composition in subarctic lakes and streams in Greenland28
Differences in bed elevation shape subtidal mussel bed stability under high‐energy hydrodynamic events27
Phytoplankton community response to a drought‐to‐wet climate transition in a subtropical estuary27
Grazing by an endemic atyid shrimp controls microbial communities in the Hawaiian anchialine ecosystem26
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
Waves and vegetation shape near‐bed turbulent kinetic energy in coastal marshes25
Ecophysiology of two mesophotic octocorals intended for restoration: Effects of light and temperature25
Effects of spatially heterogeneous lakeside development on nearshore biotic communities in a large, deep, oligotrophic lake25
Prolific nitrite reoxidation across the Eastern Tropical North Pacific Ocean24
Role of virus‐mediated lysis in spatiotemporal dynamics of prokaryotic communities in river–estuary–coastal ecosystems24
Urbanization alters river multifunctionality by reducing macroinvertebrate diversity in highly human‐impacted plain river networks24
Nutrient function over form: Organic and inorganic nitrogen additions have similar effects on lake phytoplankton nutrient limitation24
Responses of biogenic dimethylated sulfur compounds to environmental changes in the northwestern Pacific continental sea24
Thermal plasticity of coral reef symbionts is linked to major alterations in their lipidome composition24
Unexpected functional diversity of stream biofilms within and across proglacial floodplains despite close spatial proximity24
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Outwelling of reduced porewater drives the biogeochemistry of dissolved organic matter and trace metals in a major mangrove‐fringed estuary in Amazonia23
In situ aerobic methane oxidation rates in a stratified lake23
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The grazing impact of megaherbivores on sediment accumulation and stabilization functions of seagrass meadows in a subtropical coral reef lagoon23
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Ubiquitous but unique: Water depth and oceanographic attributes shape methane seep communities23
The role of internal nitrogen loading in supporting non‐N ‐fixing harmful cyanobacterial blooms in the water column of a large eutrophic lake23
Sediment depth–dependent fungal community and biogeochemical potentials along the abyssal–hadal transition zone of the Mariana Trench22
Life in turbulent waters: unsteady biota–flow interactions across scales22
Phosphorus enrichment increases the prevalence of a microsporidian parasite in experimental Daphnia populations21
The effects of disturbance on the microbial mediation of sediment stability21
Potential role of submerged macrophytes for oxic methane production in aquatic ecosystems21
Natural and anthropogenic controls on lake water‐level decline and evaporation‐to‐inflow ratio in the conterminous United States21
Multigenerational physiological compensation and body size reduction dampen the effects of warming on copepods21
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Resolving abrupt frontal gradients in zooplankton community composition and marine snow fields with an autonomous Zooglider20
Autonomous instrumentation and big data: New windows, knowledge, and breakthroughs in the aquatic sciences20
Kelp canopy species and forest structure foster distinct faunal assemblages20
Meadow trophic status regulates the nitrogen filter function of tropical seagrasses in seasonally eutrophic coastal waters20
A missing trophic link: Contribution of the microbial loop to the estimation of the trophic position of pelagic consumers20
Net emission of atmospheric volatile organic compounds from ponds in a peatland forest20
The Amazon shelf sediments, a reactor that fuels intense nitrogen cycling at the seabed20
Effect of a tropical cyclone on the pelagic ecosystem of a continental shelf19
Sea ice breakup and nutrient supply regulate the timing and magnitude of algal export over the slopes of the Pacific Arctic region19
Concurrent DNA meta‐barcoding and plankton imaging reveal novel parasitic infection and competition in a diatom19
How marine heatwaves are reshaping phytoplankton in the Northeast Pacific19
Multi‐omics analyses reveal the signatures of metabolite transfers across trophic levels in a high‐CO2 ocean18
Shortcomings of the dissipation rate for understanding the turbulent environment of plankton—And a potential solution18
Changes to upper‐ocean ecosystems may directly impact abyssal scavenger communities18
Dissolved organic matter mediates the effects of warming and inorganic nutrients on a lake planktonic food web18
Heat stress relief by tidally driven cold‐water bores on a coral reef atoll18
Flow variability and macroinvertebrates jointly regulate stream periphyton and metabolism: Insights from experimental stream mesocosms18
Long‐range transport of littoral methane explains the metalimnetic methane peak in a large lake17
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The influence of environmental parameters on spatial variation in zoobenthic density and stable isotopes (δ13C, δ15N, and δ34S) within17
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Long‐term nutrient load reductions and increasing lake TN : TP stoichiometry decrease phytoplankton biomass and diversity in a large shallow lake17
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Occurrence of small microplastics in the salp Salpa fusiformis in the Kuroshio region17
Summer ecosystem structure in mountain lakes linked to interannual variability of lake ice, snowpack, and landscape attributes17
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A coastal Synechococcus strain is more resilient to iron limitation than an oceanic strain17
Pteropods as early‐warning indicators of ocean acidification16
Limited degradability of dissolved organic carbon, nitrogen, and phosphorus during contrasting seasons in a tropical coastal environment16
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
Terrestrial support of wetland food webs via a dissolved inorganic carbon pathway16
High‐frequency variability dominates potential connectivity between remote coral reefs16
Co‐acquisition of mineral‐bound iron and phosphorus by natural Trichodesmium colonies16
Mass deposition of microbes from wildfire smoke to the sea surface microlayer16
Shifting phenology as a key driver of shelf zooplankton population variability16
Nutritional response of a coccolithophore to changing pH and temperature16
The effect of body size on the feeding current and prey spectrum of the barnacle Amphibalanus improvisus16
Basin‐scale estimates of greenhouse gas emissions from the Mara River, Kenya: Importance of discharge, stream size, and land use/land cover15
Biogeochemical‐Argo data suggest significant contributions of small particles to the vertical carbon flux in the subpolar North Atlantic15
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Variability in lake bacterial growth and primary production under lake ice: Evidence from early winter to spring melt15
Summer sea ice melting enhances phytoplankton and dimethyl sulfide production15
Patterns of siderophore production and utilization at Station ALOHA from the surface to mesopelagic waters15
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Why do algal blooms intensify under reduced nitrogen and fluctuating phosphorus conditions: The underappreciated role of non‐algal light attenuation15
Rapid nitrogen removal in sandy beaches driven by periodic tidal inundations15
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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
Biogeochemical cycling of Cd, Mn, and Ce in the Eastern Tropical North Pacific oxygen‐deficient zone14
Sediment oxygen consumption in Antarctic subglacial environments14
Transport and reactivity of nitrous oxide and methane in two contrasting subterranean estuaries14
Hydrodynamic processes influence nitrous oxide production and emission potential in a mountainous river estuary: Insights from microbial community patterns and model predictions14
Vertical and horizontal variations in phytoplankton chlorophyll a in response to a looping super typhoon14
Wind‐induced near‐inertial motions as a driver of turbulence in a stratified temperate lake14
Contribution of gas concentration and transfer velocity to CO2 flux variability in northern lakes14
Autonomous observations enhance our ability to observe the biological carbon pump across diverse carbon export regimes14
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Methanogens limited to lower rhizosphere and to an atypical salt marsh niche along a pristine intertidal mangrove continuum14
Dynamics of surface accretion and surface elevation differ between river and tide dominated settings in tropical mangroves14
Deep photoautotrophic prokaryotes contribute substantially to carbon dynamics in oxygen‐deficient waters in a permanently redox‐stratified freshwater lake14
Size distribution of aggregates across different aquatic systems around Japan shows that stronger aggregates are formed under turbulence14
Biomass‐to‐volume ratio as a central continuous functional trait for marine zooplankton14
The experimental implications of the rate of temperature change and timing of nutrient availability on growth and stoichiometry of a natural marine phytoplankton community13
Probabilistic assessment of algal nutrient limitation across lakes, leveraging trends with temperature and depth13
Climate change–induced terrestrial matter runoff may decrease food web production in coastal ecosystems13
Hydrology mediates salt marsh belowground biomass response to warming13
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Microbial nitrogen removal and recycling in the redox transition zone of a meromictic lake and its coupling to sulfur cycling13
Consistent prokaryotic successional dynamics across contrasting phytoplankton blooms13
Nutrient‐dependent thermal response in growth and stoichiometry of Antarctic phytoplankton13
Unique thermal mixing patterns in Lake Ontario revealed by novel year‐round observations of thermal stratification13
Dependency of Arctic zooplankton on pelagic food sources: New insights from fatty acid and stable isotope analyses13
Environment matters: Dominant coastal marsh grasses produce similar biomass carbon pools in a brackish mesocosm experiment13
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Dynamic benthic oxygen fluxes lessen hypoxia effects on open continental shelves13
Corrigendum: Food sources drive temporal variation in elemental stoichiometry of benthic consumers13
Extreme wildfire conditions shift coastal phytoplankton community structure in California13
Experimental droughts in mesocosms reveal a gradient of tolerance in Alpine stream macroinvertebrates13
Seafloor bioturbation intensity on the deep sea: More complex than organic matter13
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Significant impact of lithogenic dissolution from subantarctic volcanic islands on the regional marine silicon cycle13
Differential impacts of pH on growth, physiology, and elemental stoichiometry across three coccolithophore species13
Blue carbon additionality: New insights from the radiocarbon content of saltmarsh soils and their respired CO213
Responses of microbial communities and greenhouse gas production to land use change in mangrove wetland sediments13
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Increasing acidification does not affect sexual reproduction of a solitary zooxanthellate coral transplanted at a carbon dioxide vent13
Elevated dissolved carbon dioxide and associated acidification delays maturation and decreases calcification and survival in the freshwater crustacean Daphnia magna13
The effect of vorticity on the feeding of a freshwater grazer12
Variability in the phytoplankton response to upwelling across an iron limitation mosaic within the California current system12
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
Tidal control and mangrove dieback impact on methane emissions from a subtropical mangrove estuary12
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Isotopic signatures of biotic and abiotic N2O production and consumption in the water column of meromictic, ferruginous Lake La Cruz (Spain)12
Searching for drivers of the patchy distribution of sympatric deposit‐feeding sea cucumbers: A multi‐scale monitoring study12
Rainstorm regimes modulate cyanobacterial bloom dynamics in deep reservoirs: Synergistic effects of nutrient pulses and hydrological perturbations12
Bacterial biogeography of the Indian Ocean12
Coral rubble dynamics in the Anthropocene and implications for reef recovery12
Calcification increases carbon supply, photosynthesis, and growth in a globally distributed coccolithophore12
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Seasonal drivers of dissolved oxygen across a tidal creek–marsh interface revealed by machine learning12
Grazer‐induced bioluminescence and toxicity in marine dinoflagellates12
Terrigenous inputs link nutrient dynamics to microbial communities in a tropical lagoon12
In situ observations of zooplankton show changes in abundance and swimming speed in response to hypoxia and acidification12
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Do phytoplankton require oxygen to survive? A hypothesis and model synthesis from oxygen minimum zones11
Effect of marine heat waves on carbon metabolism, optical characterization, and bioavailability of dissolved organic carbon in coastal vegetated communities11
An actionable guide to the United Nations' Biodiversity Beyond National Jurisdiction Agreement for research scientists11
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
Climate change scenarios differentially modulate the impact of invasion in a native macrophyte species11
Wind‐driven currents and water masses shape spring phytoplankton distribution and composition in hydrologically complex, productive shelf waters11
Promoting effects of aluminum addition on chlorophyll biosynthesis and growth of two cultured iron‐limited marine diatoms11
Depth and basin shape constrain ecosystem metabolism in lakes dominated by benthic primary producers11
Grazer‐induced toxin production is energetically costly and significantly reduces growth of cylindrospermopsin‐producing cyanobacteria11
On the fundamental additive modes of ocean color absorption11
Co‐occurrence and successional patterns among diatoms, dinoflagellates, and potential parasites in a coastal upwelling experiment11
Dynamics of alongshore current in the Taiwan Strait: A perspective on the southward Kuroshio branch in winter11
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Inorganic carbon dynamics and their relation to autotrophic community regime shift over three decades in a large, alkaline river11
Uncertainty sources for measurable ocean carbonate chemistry variables11
Invertebrate trophic structure on marine ferromanganese and phosphorite hardgrounds11
Epiphyton phenology determines the persistence of submerged macrophytes: Exemplified in temperate shallow lakes11
Carbon production at shallow‐water artificial reef ecosystems relies on water column primary productivity11
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Holocene climate change shifted Southern Ocean biogeochemical cycling and predator trophic dynamics11
Effect of increased CO2 on calcium homeostasis and signaling in a marine diatom10
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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Fish predation cues induce drifting and emergence in an experimental stream mesocosm system10
Heterotrophy of particulate organic matter subsidies contributes to divergent bleaching responses in tropical Scleractinian corals10
Hydrological variability and connectivity shape floodplain microbial community dynamics10
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Rising temperatures increase fish nitrogen excretion: Evidence from a meta‐analysis10
Dark carbon fixation in stream carbon cycling10
Bridging the gap between field and lab: Applicability and performance of the Sylt mesocosms facility to simulate climate change scenarios on intertidal benthic communities10
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Distinct drivers of two size fractions of operationally dissolved iron in a temperate river10
Cyclical prey shortages for a marine polar predator driven by the interaction of climate change and natural climate variability10
Synchrony dynamics of dissolved organic carbon in high‐mountain streams: Insights into scale‐dependent processes10
Insights on adaptive strategies and evolution of cable bacteria in saline lakes10
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P inputs determine denitrifier abundance explaining dissolved nitrous oxide in reservoirs10
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Recovery of denitrification and dissimilatory nitrate reduction to ammonium following reoxygenation of sediments from a periodically hypoxic temperate lagoon10
Microplastics stress alters microorganism community structure and reduces the production of biogenic dimethylated sulfur compounds10
Spatiotemporal variability of dissolved inorganic macronutrients along the northern Antarctic Peninsula (1996–2019)10
Nutrient availability influences the thermal response of marine diatoms10
Factors regulating the concentration of particulate iodine in coastal seawater10
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Kinetics of sulfate‐ and iron‐dependent anaerobic methane oxidation in freshwater lake sediment9
Strain‐dependent and host genotype–dependent priority effects in gut microbiome assembly affect host fitness in Daphnia9
Carbon dioxide emissions across contrasting urban freshwater ecosystems9
Warming seas: Native Sargassum species at risk9
The influence of mountain streamflow on nearshore ecosystem metabolism in a large, oligotrophic lake across a drought and a wet year9
Predicting larval alewife transport in Lake Michigan using hydrodynamic and Lagrangian particle dispersion models9
Seasonal hypoxia and temperature inversions in a tropical bay9
Temporal variation in ecological and evolutionary contributions to phytoplankton functional shifts9
Effects of Atlantification and changing sea‐ice dynamics on zooplankton community structure and carbon flux between 2000 and 2016 in the eastern Fram Strait9
Copepod egg production estimates are biased by female mortality9
High rates of erosion on a wave‐exposed fringing coral reef9
Gross oxygen production and microbial community respiration in the oligotrophic ocean9
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Nutrient inversion but not warming drive changes in periphyton biomass and composition in shallow lake mesocosms9
Highly mobile pelagic species co‐occur with fine‐scale ocean fronts9
Biological sources and sinks of dimethylsulfide disentangled by an induced bloom experiment and a numerical model9
Seasonally migrating zooplankton strongly enhance Southern Ocean carbon sequestration9
Can intense storms affect sinking particle dynamics after the North Atlantic spring bloom?9
From barrier to gateway: Climate‐facilitated expansion of thaliaceans in the Arctic Ocean9
The relative importance of environmental heterogeneity and dispersal limitation on spatial patterns of phytoplankton communities varies across seasons9
Successful acclimation of marine diatoms Chaetoceros curvisetus/pseudocurvisetus to climate change9
Higher alpha and gamma, but not beta diversity in tropical than in Mediterranean temporary ponds: A multi‐taxon spatiotemporal approach9
Epixylic microbial communities as key regulators of methane emissions from submerged wood in a tropical hydroelectric reservoir9
Coral reef erosion: In situ measurement on different dead coral substrates on a Caribbean reef9
Diel vertical migration and seamount stepping stones promote species connectivity from coastal to offshore insular systems in the Tropical Southwestern Atlantic8
Iron and nitrogen stress controls summertime biogeochemistry in the high‐latitude North Atlantic8
Marine nutrient subsidies promote biogeochemical hotspots in undisturbed, highly humic estuaries8
A model of algal‐virus population dynamics reveals underlying controls on material transfer8
Benthic bacterial communities are shaped by browning in boreal headwater streams8
Three‐dimensional swimming behavior and activity of a mesopelagic fish8
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