Chapter 6 – Dynamics of DOP

By David M. Karl, K. Björkman. 2002

177 citations recorded by the source corpus.

Subfields: Biochemistry, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/44bd0317bcbec427d7350989964b1af7e7ba8259

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Citations in the corpus

Lack-of P-limitation of phytoplankton and heterotrophic prokaryotes in surface waters of three anticyclonic eddies in the stratified Mediterranean Sea (2011, background): “DOP and arsenate (reviewed by Karl and Björkman, 2002).”
Presence and regulation of alkaline phosphatase activity in eukaryotic phytoplankton from the coastal ocean: Implications for dissolved organic phosphorus remineralization (2006, background): “Not only are DOP and DON often available to phytoplankton, but their concentrations can exceed those of dissolved inorganic phosphate (DIP) and nitrogen (DIN) in some instances, particularly in the photic zone (Monaghan and Ruttenberg 1999; Karl and Björkman 2002; Ruttenberg and Dyhrman 2005).”
Dynamics of Dissolved Organic Phosphorus (2015, background): “This chapter is an update of Karl and Björkman (2002), which appeared in the first edition of this volume.”
Zinc availability and alkaline phosphatase activity in Emiliania huxleyi: Implications for Zn‐P co‐limitation in the ocean (2006, background): “However, organic P concentrations always ex- ceed those of SRP (Benitez-Nelson 2000; Karl and Bjorkman 2002) with typical values (measured as soluble nonreactive phosphorus [SNP]) in oligotrophic regions ranging between 30 and 300 nmol L21 (e.g., Wu et al. 2000; Bjorkman and Karl 2003; Van Den…”
Polyphosphate in Trichodesmium from the low‐phosphorus Sargasso Sea (2010, background): “Others have hypothesized that polyP could accumulate in phytoplankton from oligotrophic, low-P regions, as part of an overplus-type response (Karl and Björkman 2002).”
Alkaline phosphatase activities in the central Atlantic Ocean indicate large areas with phosphorus deficiency (2003, background): “Irrespective of origin, AP facilitates the breakdown of P from organic molecules which constitute an important P pool in the oligotrophic ocean, where phosphate concentrations are low (Vidal et al. 1999, Karl & Björkman 2002).”
Harmful algal blooms: How strong is the evidence that nutrient ratios and forms influence their occurrence? (2012, background): “There are significant pools of dissolved organic N and P (DON and DOP) in coastal waters (Antia et al., 1991; Bronk, 2002; Karl and Björkman, 2002; Lønborg et al., 2009a).”
Alkaline phosphatase activity in the subtropical ocean: insights from nutrient, dust and trace metal addition experiments (2014, background): “Phosphorus is an essential macronutrient for all life on earth due to its role in key cellular components such as genetic biomolecules (DNA and RNA), energy transfer molecules (ATP) and cell structure (phospholipids) (Karl and Björkman, 2002).”
Alkaline phosphatase activity and regulation in the North Pacific Subtropical Gyre (2010, background): “Measuring the presence of APA alone, without complementary data on the physiological or genetic regulation of this enzyme, makes interpretation of the nutrient status of the population challenging (Karl and Björkman 2002; Dyhrman and Ruttenberg 2006).”