Annual Review of Marine Science海洋科学年度综述
Annual Review of Marine Science(英文缩写 ANNU REV MAR SCI),ISSN 1941-1405,eISSN 1941-0611,中文译名:海洋科学年度综述 是一本学术期刊。本页汇总该期刊的最新影响因子、分区信息以及最新收录于 PubMed 的文献,帮助您快速了解期刊全貌。
发文量统计区间：2025-09-28 至 2026-09-28，按本站收录文献的发表日期统计。
期刊介绍
历年影响因子趋势
| JCR 数据年份 | 影响因子 | JCR 分区 |
|---|---|---|
| 2021 | 16.561 | Q1 |
| 2022 | 17.300 | Q1 |
| 2023 | 14.300 | Q1 |
| 2024 | 18.900 | Q1 |
| 2025 | 22.500 | Q1 |
Annual Review of Marine Science 最新收录文献
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1. Learning-Based Methods and the Future of Numerical Ocean and Sea-Ice Modeling.
PMID:日期:2026-09-18The field of operational oceanography is undergoing a significant evolution with the increasing integration of artificial intelligence (AI) methods, which are complementing and, in some cases, redefining traditional numerical modeling approaches. This review explores how AI methods-particularly model-based autoregressive emulators, hybrid modeling, and end-to-end model-free approaches-are reshaping the representation of ocean and sea-ice dynamics in operational systems. We focus on three key objects: sea-ice parameters, near-surface ocean properties, and the 3D ocean state, each of which is characterized by distinct observational and dynamical challenges. While AI-driven innovations offer new opportunities for improved monitoring, forecasting, and uncertainty quantification, their long-term impact on operational systems remains uncertain, especially given the sparsity of subsurface observations and the complexity of ocean dynamics. By synthesizing recent advances and identifying open questions, this article aims to guide the ocean modeling community toward a future where AI and physics-based approaches coexist synergistically.
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2. Cryptic Biogeochemical Cycles in Methanic Marine Sediments.
PMID:日期:2026-09-16Marine sediment biogeochemistry has long been interpreted through the framework of vertical redox zonation, in which organic matter remineralization proceeds through a thermodynamically ordered sequence of terminal electron acceptors. Evidence accumulated over the past two decades has fundamentally challenged this concept. In many marine sediments, multiple metabolic pathways operate simultaneously, linked through rapid recycling of reactive intermediates and sustaining microbial activity without significant expression in net concentration profiles, referred to as cryptic cycling. These cryptic cycles are also prevalent in the deep methanic zone, which has been considered generally inactive. Here, we review cryptic biogeochemical cycles in methanic marine sediments. We discuss methodological approaches for detecting these hidden processes and synthesize evidence from both the base of the sulfate-methane transition zone and the deeper methanic zone. These cycles demonstrate that methanic sediments are far more metabolically active than has been traditionally assumed, with important implications for methane fluxes, nutrient cycling, and mineral diagenesis.
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3. Changes in Ocean Heat, Carbon Content, Ventilation, and Biology: A Review of the Second Decade of GO-SHIP Global Repeat Hydrography.
PMID:日期:2026-09-16Here, we review scientific advances based on the second decade of Global Ocean Ship-Based Hydrographic Investigations Program (GO-SHIP) repeat hydrographic observations, collected between 2014 and 2023, building on an earlier review of GO-SHIP's first decade and its predecessor programs, Climate and Ocean Variability, Predictability, and Change (CLIVAR) and the World Ocean Circulation Experiment (WOCE). During the second decade of GO-SHIP, 50 reference sections were occupied by 10 nations. Scientific advances include continued monitoring of the oceanic uptake of deep heat and anthropogenic carbon associated with climate change, as well as concomitant salinity, oxygen, and nutrient changes. In addition, we present results from new methods to analyze GO-SHIP observations that provide new insights into the patterns of anthropogenic warming in the ocean and water mass inversions that inform full-depth ocean ventilation. Finally, in this decade, GO-SHIP has expanded its scope to incorporate regional seas that represent hotspots of climate-driven change (the Arctic Ocean and Mediterranean Sea) and built a nascent biological component (Bio-GO-SHIP), and we review key results from these efforts.
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4. New Views on Cobalamin in Marine Microbial Ecosystems.
PMID:日期:2026-09-16Cobalamin (vitamin B) has long been recognized as a key cofactor required for phytoplankton growth and as a basis for ecological interactions between phytoplankton and bacteria in the sea. New findings, however, have revealed new functional roles of microbes in cobalamin production and use and illuminated a diversity of cobalamin-related compounds in the ocean. Recent studies have also made it clear that cobalamin limitation of primary productivity and phytoplankton growth is widespread, with seasonal and regional patterns, and that cobalamin can structure microbial interactions that form the basis of key processes in the marine environment. Here, we review recent progress regarding the ecology, biochemistry, evolution, and biogeochemistry of cobalamin and its impacts on microbial processes in the marine water column. We then highlight priority research directions to better illuminate the impact of cobalamin on the future of marine ecosystems.
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5. Metaproteomics in the Study of Marine Microbial Processes: Opportunities in Ocean Research and Diagnosis.
PMID:日期:2026-09-16Proteins are abundant biomolecules that serve key functions in marine microbial communities, such as enzymes catalyzing biogeochemical reactions and transporters acquiring scarce nutrients. The measurement of proteins in biologically diverse microbial communities, such as those in ocean environments, is called metaproteomics. In recent years, metaproteomics methodologies have matured into powerful and practical approaches that contribute valuable functional and diagnostic information about microbial physiology, metabolism, and biogeochemistry. In this review, we introduce the conceptual foundations and methodological principles of marine metaproteomics; discuss current applications in marine microbiology, ocean biogeochemistry, and ecosystem diagnosis; and evaluate emerging frontiers, including quantitative stoichiometric inference, biomarker development, and global-scale interoperability. We argue that metaproteomics has reached a pivotal stage: poised not only to complement other meta-omics approaches but also to become an accessible central tool for diagnosing marine ecosystem function and understanding microbial responses to environmental change.
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6. Changes in Southern Ocean Circulation Across Climate Transitions and Their Impacts on Carbon and Heat Fluxes.
PMID:日期:2026-09-01Today, the Southern Ocean (SO) is the primary sink of anthropogenic heat and carbon, yet anthropogenic warming and ozone depletion have altered its circulation and stratification, creating uncertainty about the persistence of this sink. Evidence from the last glacial period and deglaciation shows that the SO played a central role in past climate transitions by releasing heat and carbon to the atmosphere through sea-ice retreat and enhanced ventilation of deep and abyssal waters. Antarctic warming during weak Atlantic Meridional Overturning Circulation (AMOC) phases was likely amplified by SO feedbacks, such as increased deep-ocean convection, and a strengthening/poleward shift of Southern Hemisphere westerlies. However, changes in the abyssal circulation, its interaction with North Atlantic Deep Water, and its impact on oceanic carbon during the deglaciation remain debated. Finally, although sediment and modeling evidence suggests that Antarctic Ice Sheet (AIS) discharge can significantly affect climate and biogeochemistry, clear signals remain scarce in existing proxy records-either masked by dominant AMOC-driven variability or unresolved due to limited temporal resolution. Improved model representation and proxy records are needed to clarify the role of abyssal circulation and the interaction between the ocean and AIS.
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7. Beyond an Ocean of Chlorophyll: The Role of Proteorhodopsin Phototrophy in Plankton Ecology.
PMID:日期:2026-08-27Until the early 2000s, light-driven energy capture in the ocean was viewed almost exclusively through the lens of chlorophyll-based photosynthesis. The discovery of proteorhodopsins (PRs) in marine bacterioplankton fundamentally expanded this paradigm, revealing that the surface ocean is also inhabited by photoheterotrophs that exploit sunlight using simple retinal-bound proton pumps. Over the past 25 years, multiomic and physiological studies have shown that PRs are widespread across marine microorganisms, especially in prokaryotes. Analyzing global ocean metatranscriptomes, we find that PR genes consistently rank among the most highly expressed functions in situ, often rivaling genes for core metabolic processes. The combined evidence suggests that PR-driven phototrophy enables cells to pay essential energetic tolls to maintain membrane potential, enhance substrate uptake and utilization, and sustain motility during carbon scarcity. Spectral tuning and carotenoid antennae further adapt PRs to distinct light niches across productivity gradients. By supporting heterotrophic metabolism across ocean regimes, PR phototrophy likely influences dissolved organic matter processing, underscoring the need to integrate light-driven heterotrophy into marine carbon cycle models.
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8. Predicting Long-Term Trajectories of Coastal Marshes: Processes, Models, and Uncertainty.
PMID:日期:2026-08-27Coastal marshes are ecologically and geomorphologically important environments that are increasingly threatened by climate change and human activities. Anticipating their long-term (decadal to centennial) trajectory is critical for assessing vulnerability and informing restoration strategies. A wide range of process-based models have been developed to represent marsh morphodynamics across spatial scales and levels of complexity, yet persistent challenges remain in translating field observations-such as suspended sediment concentration, settling velocity, and sediment porosity-into effective long-term model parameters. As a result, these models are often more successful at elucidating general mechanisms and feedback than at making site-specific predictions. Data-driven approaches, in contrast, are commonly used to assess marsh drowning and vulnerability at specific locations but typically neglect key feedback associated with evolving landscape geometry and sediment mass conservation. Tracking sediment mass trajectories under different forcing scenarios would facilitate comparison across models and support the transfer of insight between physics-based, exploratory, and data-driven models. In addition, as marsh trajectories are increasingly shaped by restoration and sediment management practices, future outcomes will depend not only on natural processes but also on resource management decisions. Here, we review fundamental considerations and various approaches to modeling marsh trajectory and highlight recent advances and research gaps.
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9. Mammals' Insular Dispersal on Madagascar: Land Bridges and Rafting Theories, a Counterpoint Review.
PMID:日期:2026-08-27Insular faunas and fossil assemblages result from a complex interaction of geodynamical (geological, climatic, and eustatic) and biological, taphonomic, and historical processes. The debate should not be framed as a contest between biology and geodynamics but rather as an effort to reconcile the two. Geodynamic reconstructions must remain independent of biological assumptions, yet they must also be consistent with biological evidence. If faunal dispersal patterns appear to contradict existing geological models to the extent that they require improbable explanations, then the fault likely lies in the geological reconstructions, which should be revisited. We present here how recent geophysical and geological data completely reshape our view of the geodynamic evolution of the Mozambique Channel and provide geodynamic and paleo-biogeographical coherence, leading to more robust and coherent reconstructions of Earth's past.
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10. Decoding the Deep: The Ecology, Biogeography, and Evolution of Deep-Sea Viruses.
PMID:日期:2026-08-13Viruses dominate the deep-ocean biosphere (>200-m depth) yet remain profoundly understudied. As the most abundant biological entities on Earth, they govern the geochemistry, evolution, and ecology of deep-sea prokaryotic and eukaryotic communities across a vast array of deep-sea biomes. The last two decades have witnessed revolutionary advances in deep-sea sampling, sequencing, and computational biology, illuminating viral diversity and function across Earth's largest active biome. Here, we synthesize emerging patterns in deep-sea viral ecology, biogeography, and evolutionary dynamics while identifying critical knowledge gaps and opportunities. This review is pertinent in the face of deep-sea mining and climate change, which threaten to fundamentally alter these ecosystems and cascade through virus-host networks in ways we cannot yet predict. Understanding viral control of deep-sea biogeochemistry and resistance to environmental perturbation is essential for predicting ecosystem resilience in the face of anthropogenic pressures and informing policy on one of Earth's final frontiers.