SILICON METABOLISM IN DIATOMS: IMPLICATIONS FOR GROWTH

By V. Martin‐Jézéquel, M. Hildebrand, M. Brzezinski. 2000

934 citations recorded by the source corpus.

Subfields: Biomaterials, Geochemistry and Petrology, Oceanography

View Paper: https://www.semanticscholar.org/paper/41a569dcc8d4fe95adc7e83af4a14c7fd2da8a28

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Citations in the corpus

Growth dynamics of non-toxic Pseudo-nitzschia delicatissima and toxic P. seriata (Bacillariophyceae) under simulated spring and summer photoperiods (2005, background): “The rate of nutrient uptake or assimilation, and its half saturation constant are variable (Flynn, 1998; Martin-Jézéquel et al., 2000), offering potential advantages to those species most suited to the ambient conditions.”
Marine Bioinorganic Chemistry: The Role of Trace Metals in the Oceanic Cycles of Major Nutrients (2003, background): “A transporter of Si(OH)4 has been isolated and sequenced (Hildebrand et al., 1998; Hildebrand et al., 1997) and the physiology of silicon uptake has been well studied (Martin-Jezequel et al., 2000).”
UNCOUPLING OF SILICON COMPARED WITH CARBON AND NITROGEN METABOLISMS AND THE ROLE OF THE CELL CYCLE IN CONTINUOUS CULTURES OF THALASSIOSIRA PSEUDONANA (BACILLARIOPHYCEAE) UNDER LIGHT, NITROGEN, AND PHOSPHORUS CONTROL1 (2002, background): “…is coordinated with photosynthesis or with some product of photosynthesis (Turpin et al. 1988, Turpin 1991, Vergera et al. 1998), whereas Si metabolism is linked to the cell cycle and not directly to photosynthesis (Brzezinski 1992, Brzezinski and Conley 1994, Martin-Jézéquel et al. 2000).”
A Review of the Stable Isotope Bio-geochemistry of the Global Silicon Cycle and Its Associated Trace Elements (2018, background): “…even within the same species, and is primarily a function of ambient dissolved Si (DSi) concentration and cellular growth rate, whereby the bSiO2 content of a cell decreases during DSi limitation and/or accelerated growth (Martin-Jezequel et al., 2000; Claquin et al., 2002; Baines et al., 2010).”
Growth physiology and fate of diatoms in the ocean: a review (2005, background): “, ms in review) and to the differences between silicon, carbon and nitrogen cyclings (Martin-Jézéquel et al., 2000; Claquin et al., 2002).”
Role of diatoms in regulating the ocean's silicon cycle (2003, background): “The diatoms require both silicic acid and phosphate to grow, and uptake these nutrients in a variable ratio [Martin-Jézéquel et al., 2000].”
Effect of iron deficiency on diatom cell size and silicic acid uptake kinetics (2004, background): “This can be explained by the fact that the incorporation of Si is mainly linked to the duration of the cell wall synthesis phase and does not require concurrent photosynthesis (Martin-Jézéquel et al. 2000).”
Diatom sinkings speeds: Improved predictions and insight from a modified Stokes' law (2010, background): “Instead, most work has focused on silica content (the mass of silica per cell) and how it varies with size and with environmental conditions such as temperature, salinity, light, and nutrient conditions (for a review, see Martin-Jezequel et al. 2000).”
Synergistic effects of iron and temperature on Antarctic phytoplankton and microzooplankton assemblages (2009, background): “Diatom cellular Si quotas have been shown to be inversely related to nutrient-limited growth rates (Martin-Jezequel et al., 2000), such as the Fe-limited conditions found in our control treatments.”
SYNCHRONIZED GROWTH OF THALASSIOSIRA PSEUDONANA (BACILLARIOPHYCEAE) PROVIDES NOVEL INSIGHTS INTO CELL‐WALL SYNTHESIS PROCESSES IN RELATION TO THE CELL CYCLE 1 (2007, background): “Limitation of growth rate in diatoms by a variety of factors can lead to increased incorporation of silica into the cell wall (Taylor 1985, Martin-Jézéquel et al. 2000, Claquin and Martin-Jézéquel 2002), not directly due to the limiting factors but due to prolongation of the cellcycle phase in…”