118 citations as recorded by crossref.

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33. 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
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49. The stabilisation of the long-term Cretaceous greenhouse climate: Contribution from the semi-periodical burial of phosphorus in the ocean Y. Huang et al. 10.1016/j.cretres.2012.04.005
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52. Chemical speciation, reactivity, and long-term burial of sedimentary phosphorus in Green Bay, a seasonally hypoxia-influenced freshwater estuary P. Lin et al. 10.1016/j.scitotenv.2024.174957
53. Climate-driven changes in sedimentation rate influence phosphorus burial along continental margins of the northwestern Mediterranean A. Cortina et al. 10.1016/j.palaeo.2018.03.010
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56. Phosphorus recycling and burial in Baltic Sea sediments with contrasting redox conditions H. Mort et al. 10.1016/j.gca.2009.11.016
57. 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
58. Benthic phosphorus cycling in the Peruvian oxygen minimum zone U. Lomnitz et al. 10.5194/bg-13-1367-2016
59. 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
60. Spatial continuous integration of Phanerozoic global biogeochemistry and climate B. Mills et al. 10.1016/j.gr.2021.02.011
61. Temporal responses of coastal hypoxia to nutrient loading and physical controls W. Kemp et al. 10.5194/bg-6-2985-2009
62. 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
63. 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
64. Controls on the Termination of Cretaceous Oceanic Anoxic Event 2 in the Tarfaya Basin, Morocco C. Krewer et al. 10.2475/001c.118797
65. Late Ordovician climate change and extinctions driven by elevated volcanic nutrient supply J. Longman et al. 10.1038/s41561-021-00855-5
66. Spatial stoichiometry: cross‐ecosystem material flows and their impact on recipient ecosystems and organisms J. Sitters et al. 10.1111/oik.02392
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68. The modern phosphorus cycle informs interpretations of Mesoproterozoic Era phosphorus dynamics D. Canfield et al. 10.1016/j.earscirev.2020.103267
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77. Marine redox change and extinction in Triassic–Jurassic boundary strata from the Larne Basin, Northern Ireland A. Bond et al. 10.1016/j.palaeo.2022.111018
78. Geochemical Approach to Determine the Possible Precipitation Parameters of the Coniacian–Santonian Mazıdağı Phosphates, Mardin, Turkey D. Gundogar & A. Sasmaz 10.3390/min12121544
79. Biogeochemistry of the North Atlantic during oceanic anoxic event 2: role of changes in ocean circulation and phosphorus input I. Ruvalcaba Baroni et al. 10.5194/bg-11-977-2014
80. Reconciling atmospheric CO 2 , weathering, and calcite compensation depth across the Cenozoic N. Komar & R. Zeebe 10.1126/sciadv.abd4876
81. Paleoenvironmental implications of Cenozoic sediments from the central Arctic Ocean (IODP Expedition 302) using inorganic geochemistry C. März et al. 10.1029/2009PA001860
82. 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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86. 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
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