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 2022-01-01 to 2026-01-01.)
ArticleCitations
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Correction to “Cascading, interactive, and indirect effects of climate change on aquatic communities, habitats, and ecosystems”41
Phytoplankton absorb mainly red light in lakes with high chromophoric dissolved organic matter38
The grazing impact of megaherbivores on sediment accumulation and stabilization functions of seagrass meadows in a subtropical coral reef lagoon37
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Prolific nitrite reoxidation across the Eastern Tropical North Pacific Ocean35
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Experimental nutrient enrichment of forest streams reduces ecosystem nitrogen and phosphorus storage33
Environmental controls of autotrophic biofilm biomass and community composition in subarctic lakes and streams in Greenland32
Ascidians increase in abundance on tropicalized reefs and may enhance benthic nitrous oxide production32
Ubiquitous but unique: Water depth and oceanographic attributes shape methane seep communities30
Bottom‐up as well as top‐down processes govern zoobenthic secondary production in a tidal‐flat ecosystem30
Differences in bed elevation shape subtidal mussel bed stability under high‐energy hydrodynamic events29
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The role of internal nitrogen loading in supporting non‐N ‐fixing harmful cyanobacterial blooms in the water column of a large eutrophic lake27
Responses of biogenic dimethylated sulfur compounds to environmental changes in the northwestern Pacific continental sea27
Urbanization alters river multifunctionality by reducing macroinvertebrate diversity in highly human‐impacted plain river networks26
Broad‐scale climate patterns combined with local flow and turbidity disturbances structure the seasonality of gross primary production in an aridland river26
Ecophysiology of two mesophotic octocorals intended for restoration: Effects of light and temperature26
Outwelling of reduced porewater drives the biogeochemistry of dissolved organic matter and trace metals in a major mangrove‐fringed estuary in Amazonia25
Phytoplankton size distributions in the western North Atlantic and their seasonal variability25
Patchiness of plankton communities at fronts explained by Lagrangian history of upwelled water parcels25
Grazing by an endemic atyid shrimp controls microbial communities in the Hawaiian anchialine ecosystem25
Phytoplankton community response to a drought‐to‐wet climate transition in a subtropical estuary24
Effects of spatially heterogeneous lakeside development on nearshore biotic communities in a large, deep, oligotrophic lake24
Thermal plasticity of coral reef symbionts is linked to major alterations in their lipidome composition24
Waves and vegetation shape near‐bed turbulent kinetic energy in coastal marshes23
Nutrient function over form: Organic and inorganic nitrogen additions have similar effects on lake phytoplankton nutrient limitation23
In situ aerobic methane oxidation rates in a stratified lake23
Carbon isotopic constraints on the degradation and sequestration of organic matter in river‐influenced marginal sea sediments22
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Unexpected functional diversity of stream biofilms within and across proglacial floodplains despite close spatial proximity22
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Biogeochemical states, rates, and exchanges exhibit linear responses to large nutrient load reductions in a shallow, eutrophic urban estuary22
Role of virus‐mediated lysis in spatiotemporal dynamics of prokaryotic communities in river–estuary–coastal ecosystems22
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Sediment depth–dependent fungal community and biogeochemical potentials along the abyssal–hadal transition zone of the Mariana Trench21
Effect of a tropical cyclone on the pelagic ecosystem of a continental shelf21
Life in turbulent waters: unsteady biota–flow interactions across scales21
A missing trophic link: Contribution of the microbial loop to the estimation of the trophic position of pelagic consumers21
Multi‐omics analyses reveal the signatures of metabolite transfers across trophic levels in a high‐CO2 ocean21
Shortcomings of the dissipation rate for understanding the turbulent environment of plankton—And a potential solution20
Changes to upper‐ocean ecosystems may directly impact abyssal scavenger communities20
Phosphorus enrichment increases the prevalence of a microsporidian parasite in experimental Daphnia populations20
High‐resolution water‐quality and ecosystem‐metabolism modeling in lowland rivers20
Kelp canopy species and forest structure foster distinct faunal assemblages20
Multigenerational physiological compensation and body size reduction dampen the effects of warming on copepods20
Applying empirical dynamic modeling to distinguish abiotic and biotic drivers of population fluctuations in sympatric fishes20
The Amazon shelf sediments, a reactor that fuels intense nitrogen cycling at the seabed20
How marine heatwaves are reshaping phytoplankton in the Northeast Pacific20
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The effects of disturbance on the microbial mediation of sediment stability19
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Resolving abrupt frontal gradients in zooplankton community composition and marine snow fields with an autonomous Zooglider19
Autonomous instrumentation and big data: New windows, knowledge, and breakthroughs in the aquatic sciences19
Natural and anthropogenic controls on lake water‐level decline and evaporation‐to‐inflow ratio in the conterminous United States18
Mechanisms and fluid dynamics of foraging in heterotrophic nanoflagellates18
Controls on buffering and coastal acidification in a temperate estuary18
Potential role of submerged macrophytes for oxic methane production in aquatic ecosystems18
Concurrent DNA meta‐barcoding and plankton imaging reveal novel parasitic infection and competition in a diatom18
Impact of shallow‐water hydrothermal seepage on benthic biogeochemical cycling, nutrient availability, and meiobenthic communities in a tropical coral reef18
Sea ice breakup and nutrient supply regulate the timing and magnitude of algal export over the slopes of the Pacific Arctic region18
Dissolved organic matter mediates the effects of warming and inorganic nutrients on a lake planktonic food web18
Meadow trophic status regulates the nitrogen filter function of tropical seagrasses in seasonally eutrophic coastal waters18
Stability of chironomid community structure during historic climatic and environmental change in subarctic Alaska18
Net emission of atmospheric volatile organic compounds from ponds in a peatland forest18
Long‐range transport of littoral methane explains the metalimnetic methane peak in a large lake18
Flow variability and macroinvertebrates jointly regulate stream periphyton and metabolism: Insights from experimental stream mesocosms18
Long‐term nutrient load reductions and increasing lake TN : TP stoichiometry decrease phytoplankton biomass and diversity in a large shallow lake18
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Nutritional response of a coccolithophore to changing pH and temperature16
Unexpectedly stable soil organic carbon in tidal marshes under combined nitrogen loading and increased inundation compared to individual effects16
Patterns of siderophore production and utilization at Station ALOHA from the surface to mesopelagic waters16
Co‐acquisition of mineral‐bound iron and phosphorus by natural Trichodesmium colonies16
The influence of environmental parameters on spatial variation in zoobenthic density and stable isotopes (δ13C, δ15N, and δ34S) within16
Summer ecosystem structure in mountain lakes linked to interannual variability of lake ice, snowpack, and landscape attributes16
Terrestrial support of wetland food webs via a dissolved inorganic carbon pathway16
Mass deposition of microbes from wildfire smoke to the sea surface microlayer16
Basin‐scale estimates of greenhouse gas emissions from the Mara River, Kenya: Importance of discharge, stream size, and land use/land cover16
Shifting phenology as a key driver of shelf zooplankton population variability16
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Summer sea ice melting enhances phytoplankton and dimethyl sulfide production16
The effect of body size on the feeding current and prey spectrum of the barnacle Amphibalanus improvisus15
Variability in lake bacterial growth and primary production under lake ice: Evidence from early winter to spring melt15
Biogeochemical‐Argo data suggest significant contributions of small particles to the vertical carbon flux in the subpolar North Atlantic15
Limited degradability of dissolved organic carbon, nitrogen, and phosphorus during contrasting seasons in a tropical coastal environment15
High‐frequency variability dominates potential connectivity between remote coral reefs15
Why do algal blooms intensify under reduced nitrogen and fluctuating phosphorus conditions: The underappreciated role of non‐algal light attenuation15
The interaction between vegetation patchiness and tidal flows in a shortleaf seagrass meadow15
Pteropods as early‐warning indicators of ocean acidification15
The role of tides and winds in shaping seed dispersal in coastal wetlands15
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Geochemical focusing and burial of sedimentary iron, manganese, and phosphorus during lake eutrophication15
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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
Sediment oxygen consumption in Antarctic subglacial environments14
Size distribution of aggregates across different aquatic systems around Japan shows that stronger aggregates are formed under turbulence14
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Biogeochemical cycling of Cd, Mn, and Ce in the Eastern Tropical North Pacific oxygen‐deficient zone14
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Biomass‐to‐volume ratio as a central continuous functional trait for marine zooplankton14
Hydrodynamic processes influence nitrous oxide production and emission potential in a mountainous river estuary: Insights from microbial community patterns and model predictions14
Dependency of Arctic zooplankton on pelagic food sources: New insights from fatty acid and stable isotope analyses14
Environment matters: Dominant coastal marsh grasses produce similar biomass carbon pools in a brackish mesocosm experiment13
Methanogens limited to lower rhizosphere and to an atypical salt marsh niche along a pristine intertidal mangrove continuum13
Contribution of gas concentration and transfer velocity to CO2 flux variability in northern lakes13
Hydrology mediates salt marsh belowground biomass response to warming13
Dynamics of surface accretion and surface elevation differ between river and tide dominated settings in tropical mangroves13
Significant impact of lithogenic dissolution from subantarctic volcanic islands on the regional marine silicon cycle13
An intense precipitation event causes a temperate forested drainage network to shift from N2O source to sink13
Transport and reactivity of nitrous oxide and methane in two contrasting subterranean estuaries13
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Blue carbon additionality: New insights from the radiocarbon content of saltmarsh soils and their respired CO213
Organic carbon dynamics and microbial community response to oyster reef restoration13
Autonomous observations enhance our ability to observe the biological carbon pump across diverse carbon export regimes13
Deep‐sea wooden shipwrecks influence sediment microbiome diversity13
Differential impacts of pH on growth, physiology, and elemental stoichiometry across three coccolithophore species13
Vertical and horizontal variations in phytoplankton chlorophyll a in response to a looping super typhoon13
Unique thermal mixing patterns in Lake Ontario revealed by novel year‐round observations of thermal stratification13
“Slow” and “fast” in blue carbon: Differential turnover of allochthonous and autochthonous organic matter in minerogenic salt marsh sediments13
Nitrogen stable isotopes (δ15N) and tissue nitrogen in shallow‐water and mesophotic macroalgae differ between the Main Hawaiian Islands and the Northwestern Hawaiian Islan13
Climate change–induced terrestrial matter runoff may decrease food web production in coastal ecosystems13
The experimental implications of the rate of temperature change and timing of nutrient availability on growth and stoichiometry of a natural marine phytoplankton community13
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Tidal control and mangrove dieback impact on methane emissions from a subtropical mangrove estuary12
Seasonal drivers of dissolved oxygen across a tidal creek–marsh interface revealed by machine learning12
Fluorescence as a tracer of the susceptibility of dissolved organic matter to photodegradation in the Arctic Ocean12
Dynamic benthic oxygen fluxes lessen hypoxia effects on open continental shelves12
Isotopic signatures of biotic and abiotic N2O production and consumption in the water column of meromictic, ferruginous Lake La Cruz (Spain)12
Wind‐induced near‐inertial motions as a driver of turbulence in a stratified temperate lake12
Responses of microbial communities and greenhouse gas production to land use change in mangrove wetland sediments12
Nutrient‐dependent thermal response in growth and stoichiometry of Antarctic phytoplankton12
Calcification increases carbon supply, photosynthesis, and growth in a globally distributed coccolithophore12
Bacterial biogeography of the Indian Ocean12
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Corrigendum: Food sources drive temporal variation in elemental stoichiometry of benthic consumers12
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Deep photoautotrophic prokaryotes contribute substantially to carbon dynamics in oxygen‐deficient waters in a permanently redox‐stratified freshwater lake12
Variability in the phytoplankton response to upwelling across an iron limitation mosaic within the California current system12
Elevated dissolved carbon dioxide and associated acidification delays maturation and decreases calcification and survival in the freshwater crustacean Daphnia magna12
Rainstorm regimes modulate cyanobacterial bloom dynamics in deep reservoirs: Synergistic effects of nutrient pulses and hydrological perturbations12
Increasing acidification does not affect sexual reproduction of a solitary zooxanthellate coral transplanted at a carbon dioxide vent12
Searching for drivers of the patchy distribution of sympatric deposit‐feeding sea cucumbers: A multi‐scale monitoring study12
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Seafloor bioturbation intensity on the deep sea: More complex than organic matter11
Holocene climate change shifted Southern Ocean biogeochemical cycling and predator trophic dynamics11
On the fundamental additive modes of ocean color absorption11
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Climate change scenarios differentially modulate the impact of invasion in a native macrophyte species11
Extreme wildfire conditions shift coastal phytoplankton community structure in California11
Invertebrate trophic structure on marine ferromanganese and phosphorite hardgrounds11
Grazer‐induced bioluminescence and toxicity in marine dinoflagellates11
In situ observations of zooplankton show changes in abundance and swimming speed in response to hypoxia and acidification11
The effect of vorticity on the feeding of a freshwater grazer11
Co‐occurrence and successional patterns among diatoms, dinoflagellates, and potential parasites in a coastal upwelling experiment11
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Coral rubble dynamics in the Anthropocene and implications for reef recovery11
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Terrigenous inputs link nutrient dynamics to microbial communities in a tropical lagoon11
Experimental droughts in mesocosms reveal a gradient of tolerance in Alpine stream macroinvertebrates11
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Dynamics of alongshore current in the Taiwan Strait: A perspective on the southward Kuroshio branch in winter11
Carbon production at shallow‐water artificial reef ecosystems relies on water column primary productivity11
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Depth and basin shape constrain ecosystem metabolism in lakes dominated by benthic primary producers11
Consistent prokaryotic successional dynamics across contrasting phytoplankton blooms11
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
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Relative depths of the subsurface peaks of phytoplankton abundance conserved over ocean provinces11
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Uncertainty sources for measurable ocean carbonate chemistry variables10
P inputs determine denitrifier abundance explaining dissolved nitrous oxide in reservoirs10
Heterotrophy of particulate organic matter subsidies contributes to divergent bleaching responses in tropical Scleractinian corals10
Ingestion and respiration rates of a common coastal mysid respond differently to diurnal temperature fluctuation10
Variation in sediment and seagrass characteristics reflect multiple stressors along a nitrogen‐enrichment gradient in a New England lagoon10
Synchrony dynamics of dissolved organic carbon in high‐mountain streams: Insights into scale‐dependent processes10
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Inorganic carbon dynamics and their relation to autotrophic community regime shift over three decades in a large, alkaline river10
Epiphyton phenology determines the persistence of submerged macrophytes: Exemplified in temperate shallow lakes10
Effect of increased CO2 on calcium homeostasis and signaling in a marine diatom10
Grazer‐induced toxin production is energetically costly and significantly reduces growth of cylindrospermopsin‐producing cyanobacteria10
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
Differential effects of elevated pCO2 and warming on marine phytoplankton stoichiometry10
An actionable guide to the United Nations' Biodiversity Beyond National Jurisdiction Agreement for research scientists10
Hydrological variability and connectivity shape floodplain microbial community dynamics10
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Wind‐driven currents and water masses shape spring phytoplankton distribution and composition in hydrologically complex, productive shelf waters10
Recovery trends of reef carbonate budgets at remote coral atolls 6 years post‐bleaching10
Do phytoplankton require oxygen to survive? A hypothesis and model synthesis from oxygen minimum zones10
Food web structure and intraguild predation affect ecosystem functioning in an established plankton model10
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Nutrient availability influences the thermal response of marine diatoms10
Cyclical prey shortages for a marine polar predator driven by the interaction of climate change and natural climate variability10
Spatiotemporal variability of dissolved inorganic macronutrients along the northern Antarctic Peninsula (1996–2019)10
Insights on adaptive strategies and evolution of cable bacteria in saline lakes10
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Drivers of phytoplankton responses to summer wind events in a stratified lake: A modeling study10
Effect of marine heat waves on carbon metabolism, optical characterization, and bioavailability of dissolved organic carbon in coastal vegetated communities10
Promoting effects of aluminum addition on chlorophyll biosynthesis and growth of two cultured iron‐limited marine diatoms10
Factors regulating the concentration of particulate iodine in coastal seawater9
The relative importance of environmental heterogeneity and dispersal limitation on spatial patterns of phytoplankton communities varies across seasons9
Effects of Atlantification and changing sea‐ice dynamics on zooplankton community structure and carbon flux between 2000 and 2016 in the eastern Fram Strait9
Fish predation cues induce drifting and emergence in an experimental stream mesocosm system9
Bridging the gap between field and lab: Applicability and performance of the Sylt mesocosms facility to simulate climate change scenarios on intertidal benthic communities9
Can intense storms affect sinking particle dynamics after the North Atlantic spring bloom?9
Gross oxygen production and microbial community respiration in the oligotrophic ocean9
Coral reef erosion: In situ measurement on different dead coral substrates on a Caribbean reef9
Distinct drivers of two size fractions of operationally dissolved iron in a temperate river9
The influence of mountain streamflow on nearshore ecosystem metabolism in a large, oligotrophic lake across a drought and a wet year9
Temporal variation in ecological and evolutionary contributions to phytoplankton functional shifts9
Warming seas: Native Sargassum species at risk9
Strain‐dependent and host genotype–dependent priority effects in gut microbiome assembly affect host fitness in Daphnia9
Biological sources and sinks of dimethylsulfide disentangled by an induced bloom experiment and a numerical model9
Nutrient inversion but not warming drive changes in periphyton biomass and composition in shallow lake mesocosms9
Microplastics stress alters microorganism community structure and reduces the production of biogenic dimethylated sulfur compounds9
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Seasonal hypoxia and temperature inversions in a tropical bay9
Seasonally migrating zooplankton strongly enhance Southern Ocean carbon sequestration9
Successful acclimation of marine diatoms Chaetoceros curvisetus/pseudocurvisetus to climate change9
Seasonal patterns in nutrient bioavailability in boreal headwater streams9
Higher alpha and gamma, but not beta diversity in tropical than in Mediterranean temporary ponds: A multi‐taxon spatiotemporal approach9
Geographic variation in organic carbon storage by seagrass beds9
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