112 citations as recorded by crossref.

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31. 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. 10.1016/j.jmarsys.2014.05.018
32. 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. 10.5194/cp-10-1421-2014
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52. Phosphorus recycling and burial in Baltic Sea sediments with contrasting redox conditions H. Mort et al. 10.1016/j.gca.2009.11.016
53. 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. 10.1016/j.jmarsys.2011.04.006
54. Benthic phosphorus cycling in the Peruvian oxygen minimum zone U. Lomnitz et al. 10.5194/bg-13-1367-2016
55. Granulation and ferric oxides loading enable biochar derived from cotton stalk to remove phosphate from water J. Ren et al. 10.1016/j.biortech.2014.09.071
56. Spatial continuous integration of Phanerozoic global biogeochemistry and climate B. Mills et al. 10.1016/j.gr.2021.02.011
57. Temporal responses of coastal hypoxia to nutrient loading and physical controls W. Kemp et al. 10.5194/bg-6-2985-2009
58. Quasi-steady uptake and bacterial community assembly in a mathematical model of soil-phosphorus mobility I. Moyles et al. 10.1016/j.jtbi.2020.110530
59. Sedimentary phosphorus and iron cycling in and below the oxygen minimum zone of the northern Arabian Sea P. Kraal et al. 10.5194/bg-9-2603-2012
60. Controls on the Termination of Cretaceous Oceanic Anoxic Event 2 in the Tarfaya Basin, Morocco C. Krewer et al. 10.2475/001c.118797
61. Late Ordovician climate change and extinctions driven by elevated volcanic nutrient supply J. Longman et al. 10.1038/s41561-021-00855-5
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63. Redox-controlled carbon and phosphorus burial: A mechanism for enhanced organic carbon sequestration during the PETM N. Komar & R. Zeebe 10.1016/j.epsl.2017.09.011
64. The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics D. Canfield et al. 10.1016/j.earscirev.2020.103267
65. Volcanism-driven marine eutrophication in the end-Ordovician: Evidence from radiolarians and trace elements of black shale in South China X. Wu et al. 10.1016/j.jseaes.2023.105687
66. Marine eutrophication within the Tarim Platform in sync with Middle to Late Ordovician climatic cooling J. Zhang et al. 10.1144/jgs2023-078
67. 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. 10.1016/j.gca.2020.04.035
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78. 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 10.2343/geochemj.2.0286
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80. 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. 10.5194/bg-10-3943-2013
81. Evolution of the global phosphorus cycle C. Reinhard et al. 10.1038/nature20772
82. The mechanism of sapropel formation in the Mediterranean Sea: insight from long-duration box model experiments J. Dirksen & P. Meijer 10.5194/cp-16-933-2020
83. Local and global perspectives on carbon and nitrogen cycling during the Hirnantian glaciation D. LaPorte et al. 10.1016/j.palaeo.2009.03.009
84. Environmental changes in the Late Ordovician-early Silurian: Review and new insights from black shales and nitrogen isotopes M. Melchin et al. 10.1130/B30812.1
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