139 citations as recorded by crossref.

1. Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model C. Slomp & C. Heinze
2. Geochemical features of fluid in Xiaojiang fault zone, Southeastern Tibetan plateau: Implications for fault activity H. He et al.
3. A model for microbial phosphorus cycling in bioturbated marine sediments: Significance for phosphorus burial in the early Paleozoic A. Dale et al.
4. Phosphorus burial in the ocean over glacial-interglacial time scales F. Tamburini & K. Föllmi
5. Influence of consumer-driven nutrient recycling on primary production and the distribution of N and P in the ocean A. Nugraha et al.
6. Oxygenation of the Earth aided by mineral–organic carbon preservation M. Zhao et al.
7. Transient fertilization of a post-Sturtian Snowball ocean margin with dissolved phosphate by clay minerals E. Fru et al.
8. Marine phosphorus and atmospheric oxygen were coupled during the Great Oxidation Event M. Dodd et al.
9. An intermediate‐complexity model for simulating marine biogeochemistry in deep time: Validation against the modern global ocean S. Romaniello & L. Derry
10. Phosphorus cycling during the Hirnantian glaciation J. Müller et al.
11. Dynamics of nutrient cycles in the Permian–Triassic oceans Y. Sun
12. Solid Earth forcing of Mesozoic oceanic anoxic events T. Gernon et al.
13. Nutrient turnover by large sulfur bacteria on the Namibian mud belt during the low productivity season P. Chuang et al.
14. Black shale formation during the Latest Danian Event and the Paleocene–Eocene Thermal Maximum in central Egypt: Two of a kind? P. Schulte et al.
15. Sedimentary phosphorus cycling and budget in the seasonally hypoxic coastal area of Changjiang Estuary J. Liu et al.
16. Application of δ18O-PO4 analysis to recognize phosphate pollutions in eutrophic water B. Gebus-Czupyt & B. Wach
17. Carbonate-associated phosphate evidence for a small inorganic phosphorus reservoir in the terminal Ediacaran ocean Y. Fan et al.
18. Vivianite is a key sink for phosphorus in sediments of the Landsort Deep, an intermittently anoxic deep basin in the Baltic Sea N. Dijkstra et al.
19. The effects of marine eukaryote evolution on phosphorus, carbon and oxygen cycling across the Proterozoic–Phanerozoic transition T. Lyons et al.
20. Performance of magnetic zirconium-iron oxide nanoparticle in the removal of phosphate from aqueous solution C. Zhang et al.
21. BPOP-v1 model: exploring the impact of changes in the biological pump on the shelf sea and ocean nutrient and redox state E. Lovecchio & T. Lenton
22. Micro-Halocline Enabled Nutrient Recycling May Explain Extreme Azolla Event in the Eocene Arctic Ocean M. van Kempen et al.
23. Iron availability as a dominant control on the primary composition and diagenetic overprint of organic-matter-rich rocks N. Tribovillard et al.
24. Global and regional controls on marine redox changes across the Ordovician-Silurian boundary in South China Y. Liu et al.
25. Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM N. Papadomanolaki et al.
26. Linking carbon cycle perturbations to the Late Ordovician glaciation and mass extinction: A modeling approach J. Zhang et al.
27. The phosphorus cycle and biological pump in Earth’s middle age: Reappraisal of the “Boring Billion” T. Huang et al.
28. Phosphorite deposits: A promising unconventional resource for rare earth elements S. Dar et al.
29. Drivers of the global phosphorus cycle over geological time M. Zhao et al.
30. Biogeochemical effects of atmospheric oxygen concentration, phosphorus weathering, and sea-level stand on oceanic redox chemistry: Implications for greenhouse climates K. Ozaki & E. Tajika
31. Brief and intensive volcanic emissions from Ontong Java Nui heralded Oceanic Anoxic Event 1a H. Matsumoto et al.
32. Enhanced N2‐fixation and NH4+ recycling during oceanic anoxic event 2 in the proto‐North Atlantic I. Ruvalcaba Baroni et al.
33. The eastern Mediterranean phosphorite giants: An interplay between tectonics and upwelling A. Abed
34. Intensified water column hypoxia drives disproportionate benthic P release and N:P imbalance via enhanced sedimentary sulfate reduction S. Baek et al.
35. GEOCLIM reloaded (v 1.0): a new coupled earth system model for past climate change S. Arndt et al.
36. Evolution of the crustal phosphorus reservoir C. Walton et al.
37. C-GEM (v 1.0): a new, cost-efficient biogeochemical model for estuaries and its application to a funnel-shaped system C. Volta et al.
38. Quantifying the effects of nutrient loading on dissolved O2 cycling and hypoxia in Chesapeake Bay using a coupled hydrodynamic–biogeochemical model J. Testa et al.
39. Earth system instability amplified biogeochemical oscillations following the end-Permian mass extinction Z. Li et al.
40. Warming, euxinia and sea level rise during the Paleocene–Eocene Thermal Maximum on the Gulf Coastal Plain: implications for ocean oxygenation and nutrient cycling A. Sluijs et al.
41. Glacial‐interglacial variations in marine phosphorus cycling: Implications for ocean productivity I. Tsandev et al.
42. Global phosphorus retention by river damming T. Maavara et al.
43. Deciphering Middle–Late Eocene Paleoenvironmental Conditions Using Geochemical Trends: Insights from the Beni Suef Area, Northeastern Desert, Egypt M. Sayed et al.
44. Quantifying Phosphorus Sources and Sinks in the Gaoping River-Sea System in Southwestern Taiwan J. Hung & Y. Yeh
45. A model study of warming-induced phosphorus–oxygen feedbacks in open-ocean oxygen minimum zones on millennial timescales D. Niemeyer et al.
46. Developing a new method for analyzing carbonate-associated phosphate through inductively coupled plasma-tandem mass spectrometry (ICP-MS/MS) W. Liu et al.
47. Simulating the biogeochemical effects of volcanic CO2 degassing on the oxygen-state of the deep ocean during the Cenomanian/Turonian Anoxic Event (OAE2) S. Flögel et al.
48. Uncovering the Ediacaran phosphorus cycle M. Dodd et al.
49. Recurring marine phosphorus spikes during major palaeozoic mass extinctions and climate change M. Dodd et al.
50. A nutrient control on expanded anoxia and global cooling during the Late Ordovician mass extinction Z. Qiu et al.
51. Biogeochemical explanations for the world’s most phosphate-rich lake, an origin-of-life analog S. Haas et al.
52. Microbial sequestration of phosphorus in anoxic upwelling sediments T. Goldhammer et al.
53. ECO: A Generic Eutrophication Model Including Comprehensive Sediment-Water Interaction J. Smits et al.
54. Intense biological phosphate uptake onto particles in subeuphotic continental margin waters S. Sokoll et al.
55. iLOSCAR: interactive Long-term Ocean-atmosphere-Sediment CArbon cycle Reservoir model v1.0 S. Li et al.
56. Changes in continental weathering regimes inhibited global marine deoxygenation during the Paleocene-Eocene thermal maximum G. Wei et al.
57. Biogeochemical Controls on Coastal Hypoxia K. Fennel & J. Testa
58. Box-modelling of the impacts of atmospheric nitrogen deposition and benthic remineralisation on the nitrogen cycle of the eastern tropical South Pacific B. Su et al.
59. The stabilisation of the long-term Cretaceous greenhouse climate: Contribution from the semi-periodical burial of phosphorus in the ocean Y. Huang et al.
60. Phosphate removal from aqueous solutions by nano‐alumina for the effective remediation of eutrophication D. Yadav et al.
61. Global negative emissions capacity of ocean macronutrient fertilization D. Harrison
62. Chemical speciation, reactivity, and long-term burial of sedimentary phosphorus in Green Bay, a seasonally hypoxia-influenced freshwater estuary P. Lin et al.
63. Climate-driven changes in sedimentation rate influence phosphorus burial along continental margins of the northwestern Mediterranean A. Cortina et al.
64. Holocene sea-level changes modulate iron-bound phosphorus burial in subtropical coastal sediments Y. Chen et al.
65. CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales K. Ozaki et al.
66. A global reference for black shale geochemistry and the T-OAE revisited: upper Pliensbachian – middle Toarcian (Lower Jurassic) chemostratigraphy in the Cleveland Basin, England I. Jarvis et al.
67. Phosphorus recycling and burial in Baltic Sea sediments with contrasting redox conditions H. Mort et al.
68. Coupling early-diagenesis and pelagic biogeochemical models for estimating the seasonal variability of N and P fluxes at the sediment–water interface: Application to the northwestern Adriatic coastal zone D. Brigolin et al.
69. Benthic phosphorus cycling in the Peruvian oxygen minimum zone U. Lomnitz et al.
70. Granulation and ferric oxides loading enable biochar derived from cotton stalk to remove phosphate from water J. Ren et al.
71. Spatial continuous integration of Phanerozoic global biogeochemistry and climate B. Mills et al.
72. Temporal responses of coastal hypoxia to nutrient loading and physical controls W. Kemp et al.
73. Quasi-steady uptake and bacterial community assembly in a mathematical model of soil-phosphorus mobility I. Moyles et al.
74. Sedimentary phosphorus and iron cycling in and below the oxygen minimum zone of the northern Arabian Sea P. Kraal et al.
75. In Situ Vivianite Formation in Intertidal Sediments: Ferrihydrite-Adsorbed P Triggers Vivianite Formation L. Kubeneck et al.
76. Controls on the Termination of Cretaceous Oceanic Anoxic Event 2 in the Tarfaya Basin, Morocco C. Krewer et al.
77. Late Ordovician climate change and extinctions driven by elevated volcanic nutrient supply J. Longman et al.
78. Spatial stoichiometry: cross‐ecosystem material flows and their impact on recipient ecosystems and organisms J. Sitters et al.
79. Redox-controlled carbon and phosphorus burial: A mechanism for enhanced organic carbon sequestration during the PETM N. Komar & R. Zeebe
80. The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics D. Canfield et al.
81. Volcanism-driven marine eutrophication in the end-Ordovician: Evidence from radiolarians and trace elements of black shale in South China X. Wu et al.
82. Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling J. Zhang et al.
83. The marine phosphorus cycle driven by an unlikely microbe S. Lin & A. Francoeur
84. Comparison of Ediacaran platform and slope δ238U records in South China: Implications for global-ocean oxygenation and the origin of the Shuram Excursion M. Cao et al.
85. Redox sensitivity of P cycling during marine black shale formation: Dynamics of sulfidic and anoxic, non-sulfidic bottom waters C. März et al.
86. Impact of changes in river fluxes of silica on the global marine silicon cycle: a model comparison C. Bernard et al.
87. Modeling hyperthermal events in the Mesozoic-Paleogene periods: a review Y. Zhang et al.
88. Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing S. van de Velde et al.
89. Simulating the long-term carbon cycle in the Phanerozoic: Current status and future developments Y. Zhang et al.
90. Marine redox change and extinction in Triassic–Jurassic boundary strata from the Larne Basin, Northern Ireland A. Bond et al.
91. Geochemical Approach to Determine the Possible Precipitation Parameters of the Coniacian–Santonian Mazıdağı Phosphates, Mardin, Turkey D. Gundogar & A. Sasmaz
92. Biogeochemistry of the North Atlantic during oceanic anoxic event 2: role of changes in ocean circulation and phosphorus input I. Ruvalcaba Baroni et al.
93. Lacustrine Phosphorite in Late Cretaceous Nenjiang Formation of Songliao Basin and the Paleoenvironment Significance J. Liu et al.
94. Phosphorus species in surface sediments of the Kermadec Trench: Distribution and controlling factors Z. Xiong et al.
95. Reconciling atmospheric CO 2 , weathering, and calcite compensation depth across the Cenozoic N. Komar & R. Zeebe
96. Geochemical evidence for the potential extinction mechanisms of the floating fern Azolla in the early Eocene Arctic X. Fan et al.
97. Paleoenvironmental implications of Cenozoic sediments from the central Arctic Ocean (IODP Expedition 302) using inorganic geochemistry C. März et al.
98. Solid phase phosphorus species and preservation of fish remains in marine sediments of areas of high primary productivity and oxygen seasonality (36°S, central South Chile) J. DÍAZ-OCHOA & S. PANTOJA
99. Conditions required for oceanic anoxia/euxinia: Constraints from a one-dimensional ocean biogeochemical cycle model K. Ozaki et al.
100. Drivers, mechanisms and long-term variability of seasonal hypoxia on the Black Sea northwestern shelf – is there any recovery after eutrophication? A. Capet et al.
101. Evolution of the global phosphorus cycle C. Reinhard et al.
102. The mechanism of sapropel formation in the Mediterranean Sea: insight from long-duration box model experiments J. Dirksen & P. Meijer
103. Local and global perspectives on carbon and nitrogen cycling during the Hirnantian glaciation D. LaPorte et al.
104. Environmental changes in the Late Ordovician-early Silurian: Review and new insights from black shales and nitrogen isotopes M. Melchin et al.
105. Cretaceous oceanic anoxic events prolonged by phosphorus cycle feedbacks S. Beil et al.
106. Phosphorus diagenesis in deep-sea sediments: Sensitivity to water column conditions and global scale implications I. Tsandev et al.
107. Fish scales in sediments from off Callao, central Peru J. Díaz-Ochoa et al.
108. Eco-environment of reservoirs in China J. Chen et al.
109. Large closed-basin lakes sustainably supplied phosphate during the origins of life C. Walton et al.
110. Nitrogen cycle suppression and enhanced carbon burial during the Paleocene-Eocene thermal maximum, recorded from Tarfa section, Egypt (Tethys Ocean) A. Salman et al.
111. Phosphorus cycling from the margin to abyssal depths in the proto-Atlantic during oceanic anoxic event 2 P. Kraal et al.
112. Ocean deoxygenation, the global phosphorus cycle and the possibility of human-caused large-scale ocean anoxia A. Watson et al.
113. COPSE reloaded: An improved model of biogeochemical cycling over Phanerozoic time T. Lenton et al.
114. A case study of 10 years groundwater radon monitoring along the eastern margin of the Tibetan Plateau and in its adjacent regions: Implications for earthquake surveillance Y. Zhao et al.
115. Bio-irrigation Promotes Reactive Phosphorus Recycling in an Oxidized Sedimentary Environment S. Benelli et al.
116. Electrochemical oxidation of glyphosate coupled with induced crystallization for simultaneous phosphorus recovery J. Liu et al.
117. Orbitally paced phosphogenesis in Mediterranean shallow marine carbonates during the middle Miocene Monterey event G. Auer et al.
118. Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2 M. Clarkson et al.
119. Long-term controls on ocean phosphorus and oxygen in a global biogeochemical model V. Palastanga et al.
120. Stepwise Earth oxygenation is an inherent property of global biogeochemical cycling L. Alcott et al.
121. The development of deep-ocean anoxia in a comprehensive ocean phosphorus model J. Donohue et al.
122. Atlantic meridional overturning circulation and phosphate-classified bottom-up control of Atlantic pelagic ecosystems through the 20th century D. Kamykowski
123. Insights from a dynamical system approach into the history of atmospheric oxygenation M. Fakhraee & N. Planavsky
124. Shelf erosion and submarine river canyons: implications for deep-sea oxygenation and ocean productivity during glaciation I. Tsandev et al.
125. Continental weathering and redox conditions during the early Toarcian Oceanic Anoxic Event in the northwestern Tethys: Insight from the Posidonia Shale section in the Swiss Jura Mountains J. Montero-Serrano et al.
126. Periodic ocean oxygenation events during the mid-Ediacaran Z. Li et al.
127. Modeling phosphorus cycling and carbon burial during Cretaceous Oceanic Anoxic Events I. Tsandev & C. Slomp
128. Iron and manganese shuttles control the formation of authigenic phosphorus minerals in the euxinic basins of the Baltic Sea T. Jilbert & C. Slomp
129. The spread of marine anoxia on the northern Tethys margin during the Paleocene-Eocene Thermal Maximum A. Dickson et al.
130. Soda lake phosphorus fluxes controlled by biological uptake imply abundant phosphate in plausible origin-of-life environments S. Haas et al.
131. Integrating sediment biogeochemistry into 3D oceanic models: A study of benthic-pelagic coupling in the Black Sea A. Capet et al.
132. The impact of transport processes on rare earth element patterns in marine authigenic and biogenic phosphates G. Auer et al.
133. Sedimentary organic carbon to phosphorus ratios as a redox proxy in Quaternary records from the Mediterranean P. Kraal et al.
134. Bioturbation has a limited effect on phosphorus burial in salt marsh sediments S. van de Velde et al.
135. Rates of seafloor and continental weathering govern Phanerozoic marine phosphate levels S. Sharoni & I. Halevy
136. Sea surface carbonate dynamics at reefs of Bolinao, Philippines: Seasonal variation and fish mariculture-induced forcing R. Isah et al.
137. Regional environmental degradation after mid-2010s, possible links with flow pattern change in a semi-enclosed sea (Ise Bay, Japan) K. Aoki et al.
138. Coastal hypoxia and sediment biogeochemistry J. Middelburg & L. Levin
139. Stability of the marine nitrogen cycle over the past 165 million years L. Godfrey et al.