Interactive comment on “Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model” by V. Palastanga et al
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This model was designed to look at the P cycle and therefore, the most important results are the changes in the P cycle between the different simulations. The removal of P from the ocean is messy it can be removed in multiple phases, which have complex relationships with the redox and biotic conditions near the sediment-water interface. Therefore, the discussion should really focus on these removal processes, which is very novel.
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Interactive comment on “Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model” by V. Palastanga et al
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Interactive comment on “Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model” by V. Palastanga et al
متن کامل
Interactive comment on “Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model” by V. Palastanga et al
To test this hypothesis we present a series of experiments with an ocean biogeochemical model of the glacial ocean with and without inclusion of these particulate fluxes. Our work builds on previous box modeling studies by Tsandev et al. (2010) and Filippelli et al. (2007) for the glacial ocean and our own work on carbon (C), oxygen and phosphorus cycling in the present-day (pre-industrial) oce...
متن کاملInteractive comment on “Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model” by V. Palastanga et al
The paper describes changes in marine oxygen and phosphorus fields obtained for glacial and interglacial environmental conditions with a global ocean circulation model. A main result is that reasonable patterns of glacial oxygen and reactive P burial can only be obtained with the input of terrigenous particulate organic C and P. This hypothesis is of great scientific interest, and the manuscrip...
متن کاملInteractive comment on “Glacial-interglacial variability in ocean oxygen and phosphorus in a global biogeochemical model” by V. Palastanga et al
[. . .] The main problems are the lack of mechanistic insight, data constraints, or testable predictions. The model is used to calculate things, and the results of the calculations are presented with little discussion for the underlying processes. Although interesting, I am left uncertain as to whether the results have any relevance to reality. I would suggest a thorough rewrite of the paper th...
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تاریخ انتشار 2012