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Global pulses of organic carbon burial in deep-sea sediments during glacial maxima
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
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Dynamic biogeochemical provinces in the global ocean
inferredcites →https://doi.org/10.1002/palo.20020openalex-snapshot
The dynamics of the marine nitrogen cycle across the last deglaciation
inferredcites →https://doi.org/10.1007/bf02915395openalex-snapshot
Glacial-interglacial atmospheric CO2 change —The glacial burial hypothesis
inferredcites →https://doi.org/10.1016/0016-7037(82)90110-7openalex-snapshot
Ocean chemistry during glacial time
inferredcites →https://doi.org/10.1016/0079-6611(95)00015-1openalex-snapshot
Seasonal cycles of pelagic production and consumption
inferredcites →https://doi.org/10.1016/j.dsr.2004.06.014openalex-snapshot
Organic carbon content in surface sediments—defining regional provinces
inferredcites →https://doi.org/10.1016/j.epsl.2010.09.022openalex-snapshot
A deeper respired carbon pool in the glacial equatorial Pacific Ocean
inferredcites →https://doi.org/10.1016/j.epsl.2015.03.004openalex-snapshot
Deep circulation changes in the central South Atlantic during the past 145 kyrs reflected in a combined 231Pa/230Th, Neodymium isotope and benthic δ C 13 record
inferredcites →https://doi.org/10.1016/j.margeo.2015.04.005openalex-snapshot
When deep diagenesis in Arctic Ocean sediments compromises manganese-based geochronology
inferredcites →https://doi.org/10.1016/j.quascirev.2012.09.012openalex-snapshot
Simulating atmospheric CO2, 13C and the marine carbon cycle during the Last Glacial–Interglacial cycle: possible role for a deepening of the mean remineralization depth and an increase in the oceanic nutrient inventory
inferredcites →https://doi.org/10.1016/j.quascirev.2014.11.012openalex-snapshot
Deglacial weakening of the oceanic soft tissue pump: global constraints from sedimentary nitrogen isotopes and oxygenation proxies
inferredcites →https://doi.org/10.1016/s0009-2541(99)00041-8openalex-snapshot
Terrestrial organic carbon accumulation on the Amazon deep sea fan during the last glacial sea level low stand
inferredcites →https://doi.org/10.1016/s0277-3791(01)00101-9openalex-snapshot
Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records
inferredcites →https://doi.org/10.1016/s0921-8181(00)00052-7openalex-snapshot
A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy
inferredcites →https://doi.org/10.1016/s0967-0645(01)00091-1openalex-snapshot
Benthic remineralization and burial of biogenic SiO2, CaCO3, organic carbon, and detrital material in the Southern Ocean along a transect at 170° West
inferredcites →https://doi.org/10.1021/cr050347qopenalex-snapshot
Preservation of Organic Matter in Marine Sediments: Controls, Mechanisms, and an Imbalance in Sediment Organic Carbon Budgets?
inferredcites →https://doi.org/10.1029/2001gb001765openalex-snapshot
Association of sinking organic matter with various types of mineral ballast in the deep sea: Implications for the rain ratio
inferredcites →https://doi.org/10.1029/2003gb002189openalex-snapshot
Isotopic constraints on glacial/interglacial changes in the oceanic nitrogen budget
inferredcites →https://doi.org/10.1029/2004gb002368openalex-snapshot
Burial of terrestrial organic matter in marine sediments: A re‐assessment
inferredcites →https://doi.org/10.1029/2004pa001071openalex-snapshot
A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ 18 O records
inferredcites →https://doi.org/10.1029/2006gb002907openalex-snapshot
A synthesis of global particle export from the surface ocean and cycling through the ocean interior and on the seafloor
inferredcites →https://doi.org/10.1029/2007gl031301openalex-snapshot
Biology‐mediated temperature control on atmospheric pCO2 and ocean biogeochemistry
inferredcites →https://doi.org/10.1029/2009jf001266openalex-snapshot
Real and apparent changes in sediment deposition rates through time
inferredcites →https://doi.org/10.1029/2010gb003935openalex-snapshot
Global calcite cycling constrained by sediment preservation controls
inferredcites →https://doi.org/10.1029/95gb03525openalex-snapshot
The global ocean flux of particulate organic carbon: Areal distribution and magnitude
inferredcites →https://doi.org/10.1029/pa003i003p00361openalex-snapshot
Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years
inferredcites →https://doi.org/10.1038/20859openalex-snapshot
Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica
inferredcites →https://doi.org/10.1038/335529a0openalex-snapshot
Climatically forced organic carbon burial in equatorial Atlantic and Pacific Oceans
inferredcites →https://doi.org/10.1038/35351openalex-snapshot
Influence of oxygen exposure time on organic carbon preservation in continental margin sediments
inferredcites →https://doi.org/10.1038/376755a0openalex-snapshot
Large changes in oceanic nutrient inventories from glacial to interglacial periods
inferredcites →https://doi.org/10.1038/387272a0openalex-snapshot
Evolution of the nitrogen cycle and its influence on the biological sequestration of CO2 in the ocean
inferredcites →https://doi.org/10.1038/nature09149openalex-snapshot
The polar ocean and glacial cycles in atmospheric CO2 concentration
inferredcites →https://doi.org/10.1038/nature10310openalex-snapshot
Southern Ocean dust–climate coupling over the past four million years
inferredcites →https://doi.org/10.1038/nature14059openalex-snapshot
Strong and deep Atlantic meridional overturning circulation during the last glacial cycle
inferredcites →https://doi.org/10.1038/ngeo1324openalex-snapshot
Large inert carbon pool in the terrestrial biosphere during the Last Glacial Maximum
inferredcites →https://doi.org/10.1038/ngeo1352openalex-snapshot
Large climate-driven changes of oceanic oxygen concentrations during the last deglaciation
inferredcites →https://doi.org/10.1038/ngeo1765openalex-snapshot
Processes and patterns of oceanic nutrient limitation
inferredcites →https://doi.org/10.1038/ngeo1832openalex-snapshot
The acceleration of oceanic denitrification during deglacial warming
inferredcites →https://doi.org/10.1038/ngeo2317openalex-snapshot
Glacial–interglacial changes in bottom-water oxygen content on the Portuguese margin
inferredcites →https://doi.org/10.1126/science.1105375openalex-snapshot
Role of Marine Biology in Glacial-Interglacial CO 2 Cycles
inferredcites →https://doi.org/10.1126/science.1141038openalex-snapshot
Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years
inferredcites →https://doi.org/10.1126/science.1150595openalex-snapshot
Covariant Glacial-Interglacial Dust Fluxes in the Equatorial Pacific and Antarctica
inferredcites →https://doi.org/10.1130/0091-7613(1983)11<16:ipitee>2.0.co;2openalex-snapshot
Increased productivity in the eastern equatorial Pacific during the last glacial maximum (19,000 to 14,000 yr B.P)
inferredcites →https://doi.org/10.1130/g31081.1openalex-snapshot
Submarine fans at all sea-level stands: Tectono-morphologic and climatic controls on terrigenous sediment delivery to the deep sea
inferredcites →https://doi.org/10.1163/1570-6664_iyb_sim_org_38804openalex-snapshot
International Hydrographic Organization
inferredcites →https://doi.org/10.5194/bg-10-1131-2013openalex-snapshot
Microbial bioavailability regulates organic matter preservation in marine sediments
inferredcites →https://doi.org/10.5194/bg-7-1973-2010openalex-snapshot
Shelf erosion and submarine river canyons: implications for deep-sea oxygenation and ocean productivity during glaciation
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
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Utilities of Environmental Radioactivity Tracers in Assessing Sequestration Potential of Carbon in the Coastal Wetland Ecosystems
inferred← citeshttps://doi.org/10.1002/2017gl076592openalex-snapshot
The Influence of Water Storage in Marine Sediment on Sea‐Level Change
inferred← citeshttps://doi.org/10.1002/9781119554356.ch5openalex-snapshot
Organic Carbon in Sediments of the Western Indian Margin
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Deep carbon cycle from sediments in subduction zones
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Carbon cycle in tropical peatlands and coastal seas
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Sedimentary diagenesis, depositional environments, and benthic fluxes
inferred← citeshttps://doi.org/10.1016/b978-0-443-15748-6.00094-0openalex-snapshot
Glacial-interglacial carbon cycle dynamics
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Reconstructing organic matter sources and rain rates in the southern West Pacific Warm Pool during the transition from the deglaciation period to early Holocene
inferred← citeshttps://doi.org/10.1016/j.csr.2023.105053openalex-snapshot
Sources of sedimentary organic matter in Arctic fjords: Evidence from lipid molecular markers
inferred← citeshttps://doi.org/10.1016/j.dsr.2020.103341openalex-snapshot
North Pacific deep-sea ecosystem responses reflect post-glacial switch to pulsed export productivity, deoxygenation, and destratification
inferred← citeshttps://doi.org/10.1016/j.dsr.2025.104530openalex-snapshot
The roles of benthic diversity and environmental factors in nutrient and macrofaunal dynamics within the oxygen minimum zone of the British Columbia continental slope
inferred← citeshttps://doi.org/10.1016/j.dsr.2026.104757openalex-snapshot
Spatial heterogeneity of bottom-water redox evolution in the western Pacific marginal seas since the last deglaciation
inferred← citeshttps://doi.org/10.1016/j.dsr2.2017.01.006openalex-snapshot
More reducing bottom-water redox conditions during the Last Glacial Maximum in the southern Challenger Deep (Mariana Trench, western Pacific) driven by enhanced productivity
inferred← citeshttps://doi.org/10.1016/j.dsr2.2017.06.003openalex-snapshot
Aliphatic hydrocarbons and triterpenes of the Congo deep-sea fan
inferred← citeshttps://doi.org/10.1016/j.dsr2.2023.105274openalex-snapshot
A seasonal transition in biological carbon pump efficiency in the northern Scotia Sea, Southern Ocean
inferred← citeshttps://doi.org/10.1016/j.dsr2.2025.105518openalex-snapshot
A large glacial-interglacial shift in carbon burial in the northeast Indian Ocean during the Late Quaternary
inferred← citeshttps://doi.org/10.1016/j.epsl.2016.09.049openalex-snapshot
Disentangling the record of diagenesis, local redox conditions, and global seawater chemistry during the latest Ordovician glaciation
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I/Ca in epifaunal benthic foraminifera: A semi-quantitative proxy for bottom water oxygen in a multi-proxy compilation for glacial ocean deoxygenation
inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117719openalex-snapshot
Multiple S-isotope constraints on environmental changes during the Serpukhovian mass extinction
inferred← citeshttps://doi.org/10.1016/j.epsl.2024.119153openalex-snapshot
Elemental-organic geochemical evidence for the lacustrine metalimnetic oxygen minimum dynamics in the Mid-Late Triassic Chang 7 shales
inferred← citeshttps://doi.org/10.1016/j.epsl.2025.119240openalex-snapshot
Decreased marine organic carbon burial during the Hirnantian glaciation
inferred← citeshttps://doi.org/10.1016/j.epsl.2025.119529openalex-snapshot
Enhanced deoxygenation and carbon storage in the mid-depth subarctic Pacific during the Bølling-Allerød
inferred← citeshttps://doi.org/10.1016/j.epsl.2026.119976openalex-snapshot
Strengthened glacial biological pump revealed by 230Th-normalized biogenic flux in the northern South China Sea
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How soon will landfilled plastics integrate into the geological carbon cycle?
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Perspectives on provenance and alteration of suspended and sedimentary organic matter in the subtropical Pearl River system, South China
inferred← citeshttps://doi.org/10.1016/j.gca.2019.09.025openalex-snapshot
Multi-elemental composition of authigenic carbonates in benthic foraminifera from the eastern Bering Sea continental margin (International Ocean Discovery Program Site U1343)
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Hydrodynamic processes and source changes caused elevated 14C ages of organic carbon in the East China Sea over the last 14.3 kyr
inferred← citeshttps://doi.org/10.1016/j.gca.2022.07.022openalex-snapshot
Beyond anoxia: Exploring sedimentary thallium isotopes in paleo-redox reconstructions from a new core top collection
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103917openalex-snapshot
What triggered the Late Ordovician mass extinction (LOME)? Perspectives from geobiology and biogeochemical modeling
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104542openalex-snapshot
Last glacial burial of woody debris in deep-sea sediments and its carbon cycling significance
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104644openalex-snapshot
Effects of climate change and methane-rich fluid activity on sedimentary sulfur geochemical records in the northern South China Sea since mid-Pleistocene
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104660openalex-snapshot
Dual carbon isotopes constrain the sources and age variations of terrestrial organic carbon in the middle Okinawa Trough since the last deglaciation
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104771openalex-snapshot
Organic matter burial and degradation in the southern South China Sea since the last glaciation
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105467openalex-snapshot
Southern component water-driven carbonate dissolution and carbon storage during the Last Glacial Maximum in the western South Atlantic
inferred← citeshttps://doi.org/10.1016/j.gr.2018.12.012openalex-snapshot
Arido-eustasy: A new example of non-glacial eustatic sea level change
inferred← citeshttps://doi.org/10.1016/j.jenvrad.2024.107464openalex-snapshot
Utilities of environmental radioactivity tracers in assessing sequestration potential of carbon in the coastal wetland ecosystems
inferred← citeshttps://doi.org/10.1016/j.jhazmat.2025.137537openalex-snapshot
Unveiling the deep-sea microplastic Odyssey: Characteristics, distribution, and ecological implications in Pacific Ocean sediments
inferred← citeshttps://doi.org/10.1016/j.jngse.2016.09.046openalex-snapshot
Estimation of pore space methane hydrate in marine sediments of Cascadia Margin
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Characterizing organic carbon source, age, and degradation state in Northern Patagonia fjord surface sediments
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Using deep-sea images to examine ecosystem services associated with methane seeps
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Variability in zoobenthic blue carbon storage across a southern polar gradient
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Effect of sea-level on organic carbon preservation in the Okinawa Trough over the last 91 kyr
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Testing spatial interpolation methods for deep-time organic carbon burial in epicontinental seas by taking Sunda Shelf as an example
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Middle to Late Pleistocene deep-water ventilation evolution in the Western Tropical South Atlantic
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The Modern Yellow River Delta as a vast and dynamic sedimentary carbon reservoir
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Different pacemakers of marine organic carbon burial in the North Yellow Sea from the early to late Holocene
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Organic carbon burial in a middle Eocene East Asian paleolake: Response to global and regional climate changes
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Changes in the particulate organic carbon pump efficiency since the Last Glacial Maximum in the northwestern Philippine Sea
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Strong solar influence on multi-decadal periodic productivity changes in the central-western Bay of Bengal
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Quantitative reconstruction of primary productivity in low latitudes during the last glacial maximum and the mid-to-late Holocene from a global Florisphaera profunda calibration dataset
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Late Quaternary change in sources and burial of organic carbon off Northeastern Brazil
inferred← citeshttps://doi.org/10.1016/j.quascirev.2026.110306openalex-snapshot
Decoupling of surface productivity and organic carbon preservation in the southeastern Arabian Sea during the last two glacial-interglacial cycles
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Microbiological and environmental significance of metal-dependent anaerobic oxidation of methane
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inferred← citeshttps://doi.org/10.1029/2018jg004674openalex-snapshot
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The Middle to Late Miocene “Carbonate Crash” in the Equatorial Indian Ocean
inferred← citeshttps://doi.org/10.1029/2019gc008382openalex-snapshot
Organic Matter Sources in North Atlantic Fjord Sediments
inferred← citeshttps://doi.org/10.1029/2020gb006769openalex-snapshot
Global Ocean Sediment Composition and Burial Flux in the Deep Sea
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inferred← citeshttps://doi.org/10.1029/2021jg006514openalex-snapshot
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Spatial Discrepancy of Hydrodynamics‐Driven Impacts on Organic Biomarkers Deposition and ′ and TEX86 Temperature Proxies Applications
inferred← citeshttps://doi.org/10.1029/2022gl100638openalex-snapshot
Carbon Sequestration of the Middle Miocene Sunda Shelf Facilitated Global Climate Change
inferred← citeshttps://doi.org/10.1029/2022pa004577openalex-snapshot
Carbon Cycle Responses to Changes in Weathering and the Long‐Term Fate of Stable Carbon Isotopes
inferred← citeshttps://doi.org/10.1029/2023av001000openalex-snapshot
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inferred← citeshttps://doi.org/10.1029/2024pa005072openalex-snapshot
Environmental Controls on Green Bands in Marine Sediments
inferred← citeshttps://doi.org/10.1029/2025av002024openalex-snapshot
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inferred← citeshttps://doi.org/10.1029/2025jg008948openalex-snapshot
Significant Decrease in Sedimentary Organic Carbon Sequestration in the Lower Bengal Fan During the Last Sea Level Rise
inferred← citeshttps://doi.org/10.1038/ngeo2914openalex-snapshot
A lower limit to atmospheric CO2 concentrations over the past 800,000 years
inferred← citeshttps://doi.org/10.1038/ngeo2939openalex-snapshot
Rise of Earth’s atmospheric oxygen controlled by efficient subduction of organic carbon
inferred← citeshttps://doi.org/10.1038/s41467-019-12549-zopenalex-snapshot
Marine nitrogen fixers mediate a low latitude pathway for atmospheric CO2 drawdown
inferred← citeshttps://doi.org/10.1038/s41467-022-35112-9openalex-snapshot
Transfer efficiency of organic carbon in marine sediments
inferred← citeshttps://doi.org/10.1038/s41467-023-40452-1openalex-snapshot
Indian Ocean glacial deoxygenation and respired carbon accumulation during mid-late Quaternary ice ages
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Cycling and persistence of iron-bound organic carbon in subseafloor sediments
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Materials and pathways of the organic carbon cycle through time
inferred← citeshttps://doi.org/10.1038/s41561-026-02120-zopenalex-snapshot
Transient variability in global oceanic oxygen during the Last Interglacial Period
inferred← citeshttps://doi.org/10.1038/s41586-022-05413-6openalex-snapshot
Neogene burial of organic carbon in the global ocean
inferred← citeshttps://doi.org/10.1038/s43017-020-00116-wopenalex-snapshot
Evolution of the structure and impact of Earth’s biosphere
inferred← citeshttps://doi.org/10.1038/s43247-024-01508-2openalex-snapshot
High rates of marine organic carbon burial on the southwest Greenland margin induced by Neoglacial advances
inferred← citeshttps://doi.org/10.1073/pnas.1702953114openalex-snapshot
Glacial weathering, sulfide oxidation, and global carbon cycle feedbacks
inferred← citeshttps://doi.org/10.1073/pnas.1802438115openalex-snapshot
Abrupt global-ocean anoxia during the Late Ordovician–early Silurian detected using uranium isotopes of marine carbonates
inferred← citeshttps://doi.org/10.1073/pnas.2014787118openalex-snapshot
Appraisal of sedimentary alkenones for the quantitative reconstruction of phytoplankton biomass
inferred← citeshttps://doi.org/10.1073/pnas.2016896118openalex-snapshot
A unified theory for organic matter accumulation
inferred← citeshttps://doi.org/10.1073/pnas.2107034118openalex-snapshot
Persistent deep water anoxia in the eastern South Atlantic during the last ice age
inferred← citeshttps://doi.org/10.1073/pnas.2427236122openalex-snapshot
Sensitivity of simulations of Plio–Pleistocene climate with the CLIMBER-2 Earth System Model to details of the global carbon cycle
inferred← citeshttps://doi.org/10.1073/pnas.2511585122openalex-snapshot
Warming substantially amplifies Antarctic coastal polynyas as key carbon sinks
inferred← citeshttps://doi.org/10.1073/pnas.2526409123openalex-snapshot
Shelf-invading low-oxygen waters control Cenozoic organic carbon burial rates
inferred← citeshttps://doi.org/10.1080/09670262.2017.1362593openalex-snapshot
The possible roles of algae in restricting the increase in atmospheric CO 2 and global temperature
inferred← citeshttps://doi.org/10.1111/gcb.71098openalex-snapshot
Status of Polar Blue Carbon: Toward Recognition and Integration in Marine Policy
inferred← citeshttps://doi.org/10.1126/sciadv.aav7337openalex-snapshot
Mid-Pleistocene transition in glacial cycles explained by declining CO 2 and regolith removal
inferred← citeshttps://doi.org/10.1126/sciadv.adk2506openalex-snapshot
Global oceanic oxygenation controlled by the Southern Ocean through the last deglaciation
inferred← citeshttps://doi.org/10.1130/focus062018.1openalex-snapshot
Sea level, climate, and ocean poisoning by sulfide all implicated in the first animal mass extinction
inferred← citeshttps://doi.org/10.1144/sp475.7openalex-snapshot
Processes influencing differences in Arctic and Antarctic trough mouth fan sedimentology
inferred← citeshttps://doi.org/10.1146/annurev-marine-032223-103626openalex-snapshot
The Global Turbidity Current Pump and Its Implications for Organic Carbon Cycling
inferred← citeshttps://doi.org/10.1155/2020/8814545openalex-snapshot
Effect of Sea-Level Change on Deep-Sea Sedimentary Records in the Northeastern South China Sea over the past 42 kyr
inferred← citeshttps://doi.org/10.1175/jcli-d-21-0713.1openalex-snapshot
Carbon Fluxes during Dansgaard–Oeschger Events as Simulated by an Earth System Model
inferred← citeshttps://doi.org/10.1360/csb-2026-1015openalex-snapshot
Terrestrial organic carbon burial in marginal sea during geological warm periods and its carbon cycle negative feedback
inferred← citeshttps://doi.org/10.1360/tb-2021-0535openalex-snapshot
Geological evidences and mechanisms for oceanic anoxic events during the Early Paleozoic
inferred← citeshttps://doi.org/10.1371/journal.pclm.0000434openalex-snapshot
Carbon and carbon-13 in the preindustrial and glacial ocean
inferred← citeshttps://doi.org/10.1515/jbnst-2022-0022openalex-snapshot
A Welfare Economic Approach to Planetary Boundaries
inferred← citeshttps://doi.org/10.1575/1912/67246openalex-snapshot
From the atmosphere to the abyss: tracing organic carbon deposition, cadmium isotopes, and iron cycling using marine
inferred← citeshttps://doi.org/10.2110/jsr.2018.58openalex-snapshot
Topographic Controls On the Development of Contemporaneous but Contrasting Basin-Floor Depositional Architectures
inferred← citeshttps://doi.org/10.21203/rs.3.rs-5022150/v1openalex-snapshot
Sedimentary organic carbon burial in marine oxic sediments modulated by anticyclonic eddy
inferred← citeshttps://doi.org/10.2139/ssrn.5177799openalex-snapshot
Biogeochemical Dynamics of Deep-Sea Sediments Off Bay of Bengal: Implications for Carbon and Nitrogen Cycling in Marginal Marine Systems
inferred← citeshttps://doi.org/10.2475/10.2020.03openalex-snapshot
Redox constraints on a Cenozoic imbalance in the organic carbon cycle
inferred← citeshttps://doi.org/10.31223/x5437bopenalex-snapshot
Reactive iron as an important reservoir of marine organic carbon over geological timescales
inferred← citeshttps://doi.org/10.3389/feart.2022.886120openalex-snapshot
Glacial-Interglacial Variations in Organic Carbon Burial in the Northwest Pacific Ocean Over the Last 380 kyr and its Environmental Implications
inferred← citeshttps://doi.org/10.3389/fmars.2016.00259openalex-snapshot
Perspectives on the Terrestrial Organic Matter Transport and Burial along the Land-Deep Sea Continuum: Caveats in Our Understanding of Biogeochemical Processes and Future Needs
inferred← citeshttps://doi.org/10.3389/fmars.2024.1331940openalex-snapshot
Organic carbon burial and their implication on sea surface primary productivity in the middle Okinawa Trough over the past 200 ka
inferred← citeshttps://doi.org/10.3389/fmicb.2019.00849openalex-snapshot
The Biogeochemical Sulfur Cycle of Marine Sediments
inferred← citeshttps://doi.org/10.3389/fmicb.2020.572017openalex-snapshot
Impact of Terrestrial Input on Deep-Sea Benthic Archaeal Community Structure in South China Sea Sediments
inferred← citeshttps://doi.org/10.3390/jmse10050682openalex-snapshot
Organic Matter Burial in Deep-Sea Fans: A Depositional Process-Based Perspective
inferred← citeshttps://doi.org/10.5194/bg-15-507-2018openalex-snapshot
Glacial–interglacial changes and Holocene variations in Arabian Sea denitrification
inferred← citeshttps://doi.org/10.5194/bg-16-3997-2019openalex-snapshot
N 2 O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N 2 O stable isotopes in ice cores
inferred← citeshttps://doi.org/10.5194/bg-19-1421-2022openalex-snapshot
Ideas and perspectives: Sea-level change, anaerobic methane oxidation, and the glacial–interglacial phosphorus cycle
inferred← citeshttps://doi.org/10.5194/cp-14-1819-2018openalex-snapshot
Carbon burial in deep-sea sediment and implications for oceanic inventories of carbon and alkalinity over the last glacial cycle
inferred← citeshttps://doi.org/10.5194/cp-15-849-2019openalex-snapshot
Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data
inferred← citeshttps://doi.org/10.5194/cp-21-1043-2025openalex-snapshot
Closing the Plio-Pleistocene 13 C cycle in the 405 kyr periodicity by isotopic signatures of geological sources
inferred← citeshttps://doi.org/10.5194/cp-21-571-2025openalex-snapshot
Sediment fluxes dominate glacial–interglacial changes in ocean carbon inventory: results from factorial simulations over the past 780 000 years
inferred← citeshttps://doi.org/10.5194/cp-22-1085-2026openalex-snapshot
Glacial-interglacial shifts in dominant climate forcing over the last 33 ka in the northern South China Sea
inferred← citeshttps://doi.org/10.5194/egusphere-2024-1754-rc1openalex-snapshot
Comment on egusphere-2024-1754
inferred← citeshttps://doi.org/10.5194/egusphere-2024-1754-rc2openalex-snapshot
Comment on egusphere-2024-1754
inferred← citeshttps://doi.org/10.5194/esd-8-1-2017openalex-snapshot
Climate engineering by mimicking natural dust climate control: the iron salt aerosol method
inferred← citeshttps://doi.org/10.5194/essd-12-1053-2020openalex-snapshot
Integrating palaeoclimate time series with rich metadata for uncertainty modelling: strategy and documentation of the PalMod 130k marine palaeoclimate data synthesis
inferred← citeshttps://doi.org/10.5194/gchron-8-85-2026openalex-snapshot
Global and regional Pleistocene benthic δ 18 O stacks with a comparison of different age modeling strategies
inferred← citeshttps://doi.org/10.5194/gmd-12-1491-2019openalex-snapshot
Ocean carbon and nitrogen isotopes in CSIRO Mk3L-COAL version 1.0: a tool for palaeoceanographic research
inferred← citeshttps://doi.org/10.5194/gmd-18-977-2025openalex-snapshot
FESOM2.1-REcoM3-MEDUSA2: an ocean–sea ice–biogeochemistry model coupled to a sediment model
inferred← citeshttps://doi.org/10.70675/a758f51ez989az424az8dc6z71db49478059openalex-snapshot
Transport et accumulation de matière organique dans le système turbiditique de l'Ogooué (Gabon)
inferred← citeshttps://doi.org/10.70675/e65396c0zbad9z4f15z857bza43ea4ee8a6eopenalex-snapshot
The effect of riverine particulate material on primary productivity and the global organic carbon cycle
inferred← citeshttps://doi.org/10.70675/fb87b693z07e2z4ac4z9fbfz0c8b3e4ae719openalex-snapshot
Role of Southern Ocean sea ice on deep ocean circulation and carbon cycle at the Last Glacial Maximum
inferred← citeshttps://doi.org/10.7185/geochemlet.1732openalex-snapshot
Climate driven carbon and microbial signatures through the last ice age
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