Limnology and Oceanography

Papers
(The median citation count of Limnology and Oceanography is 1. 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 2021-02-01 to 2025-02-01.)
ArticleCitations
Functional structure and diversity of marine benthos reflect food availability and quality, as evidenced by isotopic diversity133
Internal wave resonance, surges, and strong nonlinear damping differentiated in two elongated lakes with the aid of an original Green's function117
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Nutrient pulse scenarios drive contrasting patterns in the functional stability of freshwater phytoplankton48
Supply‐controlled calcium carbonate dissolution decouples the seasonal dissolved oxygen andpHminima in Chesapeake Bay45
Biogeochemical niches and trophic plasticity of shallow and mesophotic corals recovering from mass bleaching45
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Unexpected functional diversity of stream biofilms within and across proglacial floodplains despite close spatial proximity38
Interrelated influence of iron, light, and CO2 on carbon fixation in a Southern Ocean diatom32
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Anaerobic oxidation of methane does not attenuate methane emissions from thermokarst lakes32
Experimental nutrient enrichment of forest streams reduces ecosystem nitrogen and phosphorus storage31
A sprinkling of gold dust: Pine pollen as a carbon source in Baltic Sea coastal food webs30
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Opening the black box of winter: Full‐year dynamics of crustacean zooplankton along a nearshore depth gradient in a large lake26
Variation in sediment and seagrass characteristics reflect multiple stressors along a nitrogen‐enrichment gradient in a New England lagoon26
A coastal N2 fixation hotspot at the Cape Hatteras front: Elucidating spatial heterogeneity in diazotroph activity via supervised machine learning26
Cyclonic eddies modulate temporal and spatial decoupling of particulate carbon, nitrogen, and biogenic silica export in the North Pacific Subtropical Gyre25
Coping with darkness: The adaptive response of marine picocyanobacteria to repeated light energy deprivation25
Denitrification, anammox, and DNRA in oligotrophic continental shelf sediments24
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Zooplankton composition links to climate and salmon survival in a northern temperate fjord24
Synechococcus silicon accumulation in oligotrophic oceans23
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Toward trait‐based food webs: Universal traits and trait matching in planktonic predator–prey and host–parasite relationships22
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Forward and reverse evolution of multivariate responses to cyanobacteria in experimental waterflea populations22
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The role of internal nitrogen loading in supportingnon‐N‐fixing harmful cyanobacterial blooms in the water column of a large eutrophic lake21
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Grazing by an endemic atyid shrimp controls microbial communities in the Hawaiian anchialine ecosystem21
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Response of distributions and emissions of summer biogenic sulfur in the Pacific Arctic to enhanced Pacific Water inflow20
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Carp stocking and climate change are potentially more important factors than nutrient enrichment driving water quality deterioration in subtropical freshwater lakes in China20
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Scallop shells as geochemical archives of phytoplankton‐related ecological processes in a temperate coastal ecosystem20
Calibrating the triple oxygen isotope signature of cultured diatoms19
The interactive effects of temperature and nutrients on a spring phytoplankton community19
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Biogeochemical states, rates, and exchanges exhibit linear responses to large nutrient load reductions in a shallow, eutrophic urban estuary18
Toward resolving disparate accounts of the extent and magnitude of nitrogen fixation in the Eastern Tropical South Pacific oxygen deficient zone18
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Responses of biogenic dimethylated sulfur compounds to environmental changes in the northwestern Pacific continental sea18
Strong hydrodynamic drivers of coral reef fish biodiversity on submerged pinnacle coral reefs18
Wind exposure and sediment type determine the resilience and response of seagrass meadows to climate change18
Cyclical prey shortages for a marine polar predator driven by the interaction of climate change and natural climate variability18
Recovery of denitrification and dissimilatory nitrate reduction to ammonium following reoxygenation of sediments from a periodically hypoxic temperate lagoon18
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Vertical niche occupation and potential metabolic interplay of microbial consortia in a deeply stratified meromictic model lake17
Outwelling of reduced porewater drives the biogeochemistry of dissolved organic matter and trace metals in a major mangrove‐fringed estuary in Amazonia17
No evidence for hybridization in Calanus: Reply to the comment by Parent et al.17
Impact of local rivers on coastal acidification17
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Microbial uptake dynamics of choline and glycine betaine in coastal seawater17
Spatiotemporal variability of dissolved inorganic macronutrients along the northern Antarctic Peninsula (1996–2019)17
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Thiamine limitation of periphyton in Adirondack Mountain streams16
Phytoplankton size distributions in the western North Atlantic and their seasonal variability16
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Harmonizing marine zooplankton trait data toward a mechanistic understanding of ecosystem functioning16
Nutrient function over form: Organic and inorganic nitrogen additions have similar effects on lake phytoplankton nutrient limitation16
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Eutrophication and predation mediate zooplankton diversity and network structure16
Phytoplankton community response to a drought‐to‐wet climate transition in a subtropical estuary16
Spectrophotometrically derived seawater CO2‐system assessments: Parameter calculations using pH do not require measurements at standard temperatures15
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Trophic mediation and ecosystem stability: An assessment using qualitative network models15
Strong marine heatwaves trigger flowering in seagrass15
Krill availability in adjacent Adélie and gentoo penguin foraging regions near Palmer Station, Antarctica15
Ingestion and respiration rates of a common coastal mysid respond differently to diurnal temperature fluctuation15
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Brownification reduces oxygen gross primary production and community respiration and changes the phytoplankton community composition: An in situ mesocosm experiment with high‐frequency sensor measurem15
Summer dynamics drive the microbial response to carbon and nutrient additions in a high‐altitude lake15
Pelagic and ice‐associated microalgae under elevated light and pCO2: Contrasting physiological strategies in two Arctic diatoms14
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Effects of spatially heterogeneous lakeside development on nearshore biotic communities in a large, deep, oligotrophic lake14
Water aging and the quality of organic carbon sources drive niche partitioning of the active bathypelagic prokaryotic microbiome14
Future warming stimulates growth and photosynthesis in an Arctic microalga more strongly than changes in light intensity or pCO214
P inputs determine denitrifier abundance explaining dissolved nitrous oxide in reservoirs14
Elemental content allometries and silicon uptake rates of planktonic Rhizaria: Insights into their ecology and role in biogeochemical cycles14
Diazotrophy modulates cyanobacteria stoichiometry through functional traits that determine bloom magnitude and toxin production14
Nitrous oxide production in the Chesapeake Bay14
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Glacial meltwater and sediment resuspension can be important sources of dissolved and total dissolvable aluminum and manganese to coastal ocean surface waters14
Ocean acidification may mitigate negative effects of warming on carbon burial potential in subtidal unvegetated estuarine sediments14
Microscopy and DNA‐based characterization of sinking particles at the Bermuda Atlantic Time‐series Study station point to zooplankton mediation of particle flux13
Different temperature sensitivities of key physiological processes lead to divergent trait response patterns in Arctic phytoplankton13
The importance of source data in river network connectivity modeling: A review13
A simple approach to quantifying whole‐lake methane ebullition and sedimentary methane production, and its application to the Canadian Lake Pulse dataset13
Thermal plasticity of coral reef symbionts is linked to major alterations in their lipidome composition13
Ubiquitous but unique: Water depth and oceanographic attributes shape methane seep communities13
In situ aerobic methane oxidation rates in a stratified lake13
Factors regulating the concentration of particulate iodine in coastal seawater13
Adjusting metabolic rates and critical oxygen tension in planktonic copepods under increasing hypoxia in highly productive coastal upwelling zones13
Highest primary production achieved at high nitrogen levels despite strong stoichiometric imbalances with phosphorus in hypereutrophic experimental systems13
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Size‐specific grazing and competitive interactions between large salps and protistan grazers13
Temperature‐dependent evolution of cell morphology and carbon and nutrient content in a marine diatom13
Bloom compression alongside marine heatwaves contemporary with the Oregon upwelling season13
Relative size matters: Spawning substrate roughness size and spacing affect egg dislodgement and retention in the benthos13
Eavesdropping on plankton—can zooplankton monitoring improve forecasting of biotoxins from harmful algae blooms?13
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Light, ammonium, pH, and phytoplankton competition as environmental factors controlling nitrification13
Influence of settling organic matter quantity and quality on benthic nitrogen cycling13
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Zooplankton grazing reduces the persistence of an anthropogenic pollution marker in lake water13
Local coral connections within an atoll reef system underlie reef resilience and persistence13
Net ecosystem dissolution and respiration dominate metabolic rates at two western Atlantic reef sites13
Contribution of photic and aphotic N2 fixation to production in an oligotrophic sea13
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Role of food web interactions in promoting resilience to nutrient enrichment in a brackish water eelgrass (Zostera marina) ecosystem13
Minerogenic salt marshes can function as important inorganic carbon stores13
Respiration regimes in rivers: Partitioning source‐specific respiration from metabolism time series12
Ecological stoichiometry of functional traits in a colonial harmful cyanobacterium12
Tidal pumping and intertidal groundwater springs create pronounced spatiotemporal thermal variability in a coastal lagoon12
Potential competition between marine heterotrophic prokaryotes and autotrophic picoplankton for nitrogen substrates12
Small wetland‐fringed estuaries deliver disproportionately large carbon loads to the ocean12
Prolific nitrite reoxidation across the Eastern Tropical North Pacific Ocean12
Nutrient availability influences the thermal response of marine diatoms12
Bottom‐up as well as top‐down processes govern zoobenthic secondary production in a tidal‐flat ecosystem12
Measurement of microplastic settling velocities and implications for residence times in thermally stratified lakes12
Geographic variation in organic carbon storage by seagrass beds12
Spatial microheterogeneity and selective microbial consumption of dissolved free amino acids in an oligomesotrophic lake12
Differential effects of elevated pCO2 and warming on marine phytoplankton stoichiometry12
The contribution of intraspecific variation to future climate responses of brown algae12
Sediment organic carbon stocks were similar among four species compositions in a tropical seagrass meadow12
Synchrony dynamics of dissolved organic carbon in high‐mountain streams: Insights into scale‐dependent processes12
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Carbon isotopic constraints on the degradation and sequestration of organic matter in river‐influenced marginal sea sediments12
Effect of a dense inflow on the stratification of a steep‐sided lake12
Efficient oxidation attenuates porewater‐derived methane fluxes in mangrove waters12
Patchiness of plankton communities at fronts explained by Lagrangian history of upwelled water parcels12
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Deterministic processes drive national‐scale patterns in lake surface sediment bacteria and eukaryotic assemblage composition12
Chronically elevated sea surface temperatures revealed high susceptibility of the eelgrass Zostera marina to winter and spring warming11
Dispersal, location of bloom initiation, and nutrient conditions determine the dominance of the harmful dinoflagellateAlexandrium catenella: A meta‐ecosystem study11
Co‐occurrence of browning and oligotrophication in a boreal stream network11
Control of a phytoplankton bloom by wind‐driven vertical mixing and light availability11
Spatial variability of prokaryotic and viral abundances in the Kermadec and Atacama Trench regions11
Predicting river phytoplankton blooms and community succession using ecological niche modeling11
Multi‐omics reveal the pathways involved in induced defensive colony formation of Tetradesmus obliquus in response to Daphnia grazing cues11
Terrestrial input of herbicides has significant impacts on phytoplankton and bacterioplankton communities in coastal waters11
Controls on turnover of marine dissolved organic matter—testing the null hypothesis of purely concentration‐driven uptake: Comment on Shen and Benner, “Molecular properties are a primary control on th11
Tipping points and multiple drivers in changing aquatic ecosystems: A review of experimental studies11
Zooplankton‐derived dissolved organic matter composition and its bioavailability to natural prokaryotic communities11
Alkalinity export to the ocean is a major carbon sequestration mechanism in a macrotidal saltmarsh11
A significant loop of lake sedimentation state links catchment eco‐surroundings and lake biogenic regime shifts11
Microzooplankton grazers induce chain length plasticity in colonial diatoms11
Two temperate seagrass meadows are negligible sources of methane and nitrous oxide11
Elevated temperature relieves phosphorus limitation of marine unicellular diazotrophic cyanobacteria11
Hypoxia dynamics and spatial distribution in a low gradient river11
Controls on methylmercury concentrations in lakes and streams of peatland‐rich catchments along a 1700 km permafrost gradient11
Cascading, interactive, and indirect effects of climate change on aquatic communities, habitats, and ecosystems11
What we do in the dark: Prevalence of omnivorous feeding activity in Arctic zooplankton during polar night11
Remarkably high and consistent tolerance of a Red Sea coral to acute and chronic thermal stress exposures11
Emerging harmful algal blooms caused by distinct seasonal assemblages of a toxic diatom11
Predicting the presence of hypoxic hypolimnia in lakes at large spatial scales11
Reference state, structure, regime shifts, and regulatory drivers in a coastal sea over the last century: The Central Baltic Sea case11
Prairie stream metabolism recovery varies based on antecedent hydrology across a stream network after a bank‐full flood11
A missing trophic link: Contribution of the microbial loop to the estimation of the trophic position of pelagic consumers10
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Distinct drivers of two size fractions of operationally dissolved iron in a temperate river10
Microplastics stress alters microorganism community structure and reduces the production of biogenic dimethylated sulfur compounds10
Biogeochemical cycling of trace elements and nutrients in ferruginous waters: Constraints from a deep oligotrophic ancient lake10
Connectivity between Siberian river runoff and the lower limb of the Atlantic Meridional Overturning Circulation10
The microorganisms associated with doliolids in a productive coastal upwelling system10
Modeling carbon export mediated by biofouled microplastics in the Mediterranean Sea10
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Oceanographic controls on Southern Ocean dimethyl sulfide distributions revealed by machine learning algorithms10
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Hydrology controls the carbon mass balance of a mountain lake in the eastern European Alps10
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Iron and phosphorus limitations modulate the effects of carbon dioxide enrichment on a unicellular nitrogen‐fixing cyanobacterium10
Synergistic impacts of nutrient enrichment and climate change on long‐term water quality and ecological dynamics in contrasting shallow‐lake zones10
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High‐frequency dynamics of bottom dissolved oxygen in temperate shelf seas: The joint role of tidal mixing and sediment oxygen demand10
Modeled approaches to estimating blue carbon accumulation with mangrove restoration to support a blue carbon accounting method for Australia10
Seasonal patterns in nutrient bioavailability in boreal headwater streams9
Can intense storms affect sinking particle dynamics after the North Atlantic spring bloom?9
The Ocean's labile DOC supply chain9
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New evaluation of species‐specific biogenic silica flux of radiolarians (Rhizaria) in the western Arctic Ocean using microfocus X‐ray computed tomography9
Seasonal life strategy of Prorocentrum minimum in Chesapeake Bay, USA: Validation of the role of physical transport using a coupled physical–biogeochemical–harmful algal b9
A chemosynthetic ecotone—“chemotone”—in the sediments surrounding deep‐sea methane seeps9
Mechanisms and fluid dynamics of foraging in heterotrophic nanoflagellates9
Reconstructing primary production in a changing estuary: A mass balance modeling approach9
Food web structure in relation to environmental drivers across a continental shelf ecosystem9
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Persistence of bioconvection‐induced mixed layers in a stratified lake9
Plant traits determining biogeomorphic landscape dynamics: A study on clonal expansion strategies driving cliff formation at marsh edges9
Correction to “Zooplankton in northern lakes show taxon‐specific responses in fattyacids across climate‐productivity and ecosystem size gradients”9
Aerobic methane synthesis and dynamics in a river water environment9
Tight association between microbial eukaryote and giant virus communities in the Arctic Ocean9
Impact of increasing carbon dioxide on dinitrogen and carbon fixation rates under oligotrophic conditions and simulated upwelling9
Interplay between microbial community composition and chemodiversity of dissolved organic matter throughout the Black Sea water column redox gradient9
Disturbance is complicated: Headward‐eroding saltmarsh creeks produce multiple responses and recovery trajectories9
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Impact of shallow‐water hydrothermal seepage on benthic biogeochemical cycling, nutrient availability, and meiobenthic communities in a tropical coral reef9
High ebullitive, millennial‐aged greenhouse gas emissions from thermokarst expansion of peatland lakes in boreal western Canada9
Biofilm pigments in temporary streams indicate duration and severity of drying9
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Reconciling the importance of meiofauna respiration for oxygen demand in muddy coastal sediments9
Effect of a tropical cyclone on the pelagic ecosystem of a continental shelf9
Corrigendum: Associations between cyanobacteria and indices of secondary production in the western basin of Lake Erie9
Seasonal hypoxia and temperature inversions in a tropical bay9
The effects of dissolved organic matter supplements on the metabolism of corals under heat stress9
Applying empirical dynamic modeling to distinguish abiotic and biotic drivers of population fluctuations in sympatric fishes9
High variability in organic carbon sources and microbial activities in the hadopelagic waters9
Warming exacerbates the impact of nutrient enrichment on microbial functional potentials important to the nutrient cycling in shallow lake mesocosms9
Typical relationships between phytoplankton biomass and transport time in river‐dominated coastal aquatic systems9
Eutrophication alters bacterial co‐occurrence networks and increases the importance of chromophoric dissolved organic matter composition9
Temporal variation in ecological and evolutionary contributions to phytoplankton functional shifts9
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Periphyton as a key diet source of essential fatty acids for macroinvertebrates across a nutrient and dissolved organic carbon gradient in boreal lakes9
Net community metabolism of a Posidonia oceanica meadow9
Both biotic and abiotic predictors explain significant variation in cyanobacteria biomass across lakes from temperate to subarctic zones8
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