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silica cycle

The content of the article is factually accurate yet sometimes utilizes obscure examples, when simple ones may have been better. For example, the chemical formula for wollastonite was provided, even though quartz is the more recognizable silicate. Additionally, it may be possible that using a common example, such as quartz, may make this more approachable to the general public.

While factually accurate, the tone of the article glosses over complicated concepts, instead of simplifying the language where necessary.

There are 7 total sources, all come from peer-reviewed literature, and initial review indicates that the sources are scientifically sound. Three of the sources are quality, general use articles which provide additional information about the silica cycle. The other sources may be more specific than the citing language strictly requires. For example, the opening statement: "Silicon is considered a bioessential element and is one of the most abundant elements on Earth." is supported by an article entitled A Novel Mechanism by which Silica Defends Grasses Against Herbivory. It may be possible that a more accessible article may provide more useful resources.

The talk page only contains generic Wiki information, indicating that this is a Wiki Education page and a WikiProject page which involves Chemistry and the Environment. Additionally, it has been graded as a C-class in terms of quality, and has been awarded a mid-importance classification. The talk page does not currently include discussion from the contributors.

Silica Cycle Figure

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Silica Cycle
Marine[1] and terrestrial[2][3][4][5][6] contributions to the silica cycle are shown, with the relative movement (flux) provided in units of Tmol Si/yr[7] Marine biological production primarily comes from diatoms[8]. Estuary biological production is due to sponges[9]. Values of flux as published by Tréguer & De La Rocha. Reservoir size of silicate rocks,as discussed in the sources section, is 1.5x10^21 Tmol.[10]


Bibliography to add:

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[1] [6] [5] [8] [11] [2] [12][13]


Bibliography

  1. ^ a b Sarmiento, Jorge Louis (2006). Ocean biogeochemical dynamics. Gruber, Nicolas. Princeton: Princeton University Press. ISBN 9780691017075. OCLC 60651167.
  2. ^ a b Drever, James I. (1993). "The effect of land plants on weathering rates of silicate minerals". Geochemica et Cosmochimica Acta. 58 (10): 2325–2332. doi:10.1016/0016-7037(94)90013-2.
  3. ^ De La Rocha, Christina; Conley, Daniel J. (2017), "The Venerable Silica Cycle", Silica Stories, Springer International Publishing, pp. 157–176, doi:10.1007/978-3-319-54054-2_9, ISBN 9783319540542, retrieved 2019-02-21
  4. ^ Conley, Daniel J. (2002). "Terrestrial ecosystems and the global biogeochemical silica cycle: GLOBAL BIOGEOCHEMICAL SILICA CYCLE". Global Biogeochemical Cycles. 16 (4): 68–1–68-8. doi:10.1029/2002GB001894. S2CID 128672790.
  5. ^ a b Chadwick, Oliver A.; Ziegler, Karen; Kurtz, Andrew C.; Derry, Louis A. (2005). "Biological control of terrestrial silica cycling and export fluxes to watersheds". Nature. 433 (7027): 728–731. doi:10.1038/nature03299. PMID 15716949. S2CID 4421477.
  6. ^ a b Fulweiler, Robinson W.; Carey, Joanna C. (2012-12-31). "The Terrestrial Silica Pump". PLOS ONE. 7 (12): e52932. doi:10.1371/journal.pone.0052932. PMC 3534122. PMID 23300825.
  7. ^ Tréguer, Paul J.; De La Rocha, Christina L. (2013-01-03). "The World Ocean Silica Cycle". Annual Review of Marine Science. 5 (1): 477–501. doi:10.1146/annurev-marine-121211-172346. ISSN 1941-1405. PMID 22809182.
  8. ^ a b Yool, Andrew; Tyrrell, Toby (2003). "Role of diatoms in regulating the ocean's silicon cycle". Global Biogeochemical Cycles. 17 (4). doi:10.1029/2002GB002018. S2CID 16849373.
  9. ^ DeMaster, David (2002). "The accumulation and cycling of biogenic silica in the Southern Ocean: revisiting the marine silica budget". Deep Sea Research II. 49 (16): 3155–3167. doi:10.1016/S0967-0645(02)00076-0.
  10. ^ Sutton, Jill N.; Andre, Luc; Cardinal, Damien; Conley, Daniel J.; de Souza, Gregory F.; Dean, Jonathan; Dodd, Justin; Ehlert, Claudia; Ellwood, Michael J. (2018). "A Review of the Stable Isotope Bio-geochemistry of the Global Silicon Cycle and Its Associated Trace Elements". Frontiers in Earth Science. 5. doi:10.3389/feart.2017.00112. ISSN 2296-6463.
  11. ^ Hartmann, Jens; West, A. Joshua; Renforth, Phil; Köhler, Peter; De La Rocha, Christina L.; Wolf‐Gladrow, Dieter A.; Dürr, Hans H.; Scheffran, Jürgen (2013). "Enhanced chemical weathering as a geoengineering strategy to reduce atmospheric carbon dioxide, supply nutrients, and mitigate ocean acidification". Reviews of Geophysics. 51 (2): 113–149. doi:10.1002/rog.20004. S2CID 722786.
  12. ^ Dugdale, Richard C.; Wilkerson, Frances P.; Minas, Hans J. (1995). "The role of a silicate pump in driving new production". Deep Sea Research I. 42 (5): 697–719. doi:10.1016/0967-0637(95)00015-x.
  13. ^ Berner, Robert A. (August 1992). "Weathering, plants, and the long-term carbon cycle". Geochimica et Cosmochimica Acta. 56 (8): 3225–3231. doi:10.1016/0016-7037(92)90300-8.
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