| Q59789133 | Anoxia pre-dates Frasnian–Famennian boundary mass extinction horizon in the Great Basin, USA |
| Q46326311 | Bacteriohopanepolyols along redox gradients in the Humboldt Current System off northern Chile |
| Q57859549 | Barium in sediments off northwest Africa: A tracer for paleoproductivity or meltwater events? |
| Q49965920 | Biogeochemistry: Ocean hotspots of nitrogen loss |
| Q59094671 | Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr |
| Q39493400 | Changes in North Atlantic nitrogen fixation controlled by ocean circulation. |
| Q29299791 | Climate-Forced Variability of Ocean Hypoxia |
| Q58054953 | Consistent relationship between global climate and surface nitrate utilization in the western subarctic Pacific throughout the last 500 ka |
| Q58385631 | Deglacial nitrogen isotope changes in the Gulf of Mexico: Evidence from bulk sedimentary and foraminifera-bound nitrogen in Orca Basin sediments |
| Q60559455 | Denitrification in marine sediments: A model study |
| Q105426796 | Detailed sedimentary N isotope records from Cariaco Basin for Terminations I and V: Local and global implications |
| Q58392022 | Distribution of dinoflagellate cysts in surface sediments of the northern North Atlantic in relation to nutrient content and productivity in surface waters |
| Q59813751 | Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes |
| Q56523041 | Evolution of the nitrogen cycle and its influence on the biological sequestration of CO2 in the ocean |
| Q37654788 | First evidence of denitrification vis-à-vis monsoon in the Arabian Sea since Late Miocene |
| Q43908481 | Glacial--interglacial stability of ocean pH inferred from foraminifer dissolution rates |
| Q58054962 | Glacial-interglacial modulation of the marine nitrogen cycle by high-latitude O2supply to the global thermocline |
| Q60145694 | Glacial-interglacial variability in atmospheric CO2 |
| Q33923693 | Glacial/interglacial variations in atmospheric carbon dioxide |
| Q59080088 | Glacialá¤-interglacial changes in nutrient utilization in the equatorial Pacific Ocean |
| Q59140659 | Global constraints on net primary production and inorganic carbon supply during glacial and interglacial cycles |
| Q31049820 | Global pulses of organic carbon burial in deep-sea sediments during glacial maxima |
| Q46135469 | Impact of glacial/interglacial sea level change on the ocean nitrogen cycle |
| Q59095022 | Is the ocean losing nitrate? |
| Q59789108 | Is δ15N of sedimentary organic matter a good proxy for paleodenitrification in coastal waters of the eastern Arabian Sea? |
| Q105426798 | Isotopic constraints on glacial/interglacial changes in the oceanic nitrogen budget |
| Q58054936 | Large climate-driven changes of oceanic oxygen concentrations during the last deglaciation |
| Q34634817 | Large, omega-3 rich, pelagic diatoms under Arctic sea ice: sources and implications for food webs |
| Q59792617 | Late Quaternary variability of sedimentary nitrogen isotopes in the eastern South Pacific Ocean |
| Q90640038 | Marine nitrogen fixers mediate a low latitude pathway for atmospheric CO2 drawdown |
| Q36700424 | Methods for measuring denitrification: diverse approaches to a difficult problem |
| Q57949332 | Modeling the geochemical cycle of iron in the oceans and its impact on atmospheric CO2concentrations |
| Q58825491 | Modelling nitrogen and oxygen isotope fractionation during denitrification in a lacustrine redox-transition zone |
| Q63965085 | Nitrogen cycling on the Namibian shelf and slope over the last two climatic cycles: Local and global forcings |
| Q57949412 | Nitrogen isotope evidence for water mass denitrification during the Early Toarcian (Jurassic) oceanic anoxic event |
| Q59951260 | Nitrogen isotope record of a perturbed paleoecosystem in the aftermath of the end-Triassic crisis, Doniford section, SW England |
| Q57865903 | Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific |
| Q47325352 | Oceanic Cd/P ratio and nutrient utilization in the glacial Southern Ocean |
| Q55869054 | Oceanic sinks for atmospheric CO2 |
| Q60153235 | On the preservation of laminated sediments along the western margin of North America |
| Q58206735 | Organic-rich sediments in ventilated deep-sea environments: Relationship to climate, sea level, and trophic changes |
| Q28651360 | Paleoceanographic insights on recent oxygen minimum zone expansion: lessons for modern oceanography |
| Q58825500 | Preservation of organic matter and alteration of its carbon and nitrogen isotope composition during simulated and in situ early sedimentary diagenesis |
| Q57722079 | Productivity and sedimentaryδ15N variability for the last 17,000 years along the northern Gulf of Alaska continental slope |
| Q58419627 | Rates and regulation of microbially mediated aerobic and anaerobic carbon oxidation reactions in continental margin sediments from the northeastern Arabian Sea (Pakistan Margin) |
| Q43530705 | Reduced nitrogen fixation in the glacial ocean inferred from changes in marine nitrogen and phosphorus inventories |
| Q58073133 | Remote forcing at the Last Glacial Maximum in the tropical Pacific Ocean |
| Q101625161 | Stable Isotope Constraints on Marine Productivity Across the Cretaceous‐Paleogene Mass Extinction |
| Q106957655 | Subdecadally resolved paleoceanography of the Peru margin during the last two millennia |
| Q62516823 | Surface sediment distribution along the Chilean continental slope related to upwelling and productivity |
| Q57878423 | The acceleration of oceanic denitrification during deglacial warming |
| Q56771566 | The sequence of events surrounding Termination II and their implications for the cause of glacial-interglacial CO2 changes |
| Q60136575 | Tracking nutrient and productivity variations over the Last Deglaciation in the Arctic Ocean |
| Q58320486 | What caused the glacial/interglacial atmospheric pCO2 cycles? |