Nutrient uptake and alkaline phosphatase (ec 3:1:3:1) activity of emiliania huxleyi (PRYMNESIOPHYCEAE) during growth under n and p limitation in continuous cultures

By R. Riegman, W. Stolte, A. Noordeloos, D. Slezak. 2000

296 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Oceanography, Pollution

View Paper: https://www.semanticscholar.org/paper/208236a2303d357d11325ab7f83e8cd28c3759b2

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In Environmental Chemistry

In Oceanography

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J. Raven

Citations in the corpus

Coccolithophores and the biological pump: responses to environmental changes (2004, background): “The variability in carbon quota is even higher when cell division of E. huxleyi is limited by phosphorus or nitrogen (Paasche 1998; Riegman et al. 2000).”
Coccolithophore dynamics in non‐bloom conditions during late summer in the central Iceland Basin (July‐August 2007) (2010, background): “16) was originally included as a critical factor (Tyrrell and Merico 2004) based on E. huxleyi showing a high affinity for phosphate (Riegman et al. 2000).”
Phytoplankton nutrient competition under dynamic light regimes (2004, background): “Often, though, nutrient uptake in the dark is still a substantial fraction of the uptake in light (e.g., Riegman et al. 2000).”
ERSEM 15.06: a generic model for marine biogeochemistry and the ecosystem dynamics of the lower trophic levels (2015, background): “As coccolithophores are reported to have generally higher phosphorus affinity but lower nitrogen acquisition capacity with respect to other phytoplankton (Riegman et al., 2000; Paasche, 1998), limitation of these nutrients has an opposed impact on the rain ratio.”
Phytoplankton niches, traits and eco-evolutionary responses to global environmental change (2012, unknown): “Phytoplankton cell size is highly dependent on the levels of nutrients, light, and temperature (Dou cette & Harrison 1990, Riegman et al. 2000, Montagnes & Franklin 2001).”
Modelling phytoplankton succession on the Bering Sea shelf: role of climate influences and trophic interactions in generating Emiliania huxleyi blooms 1997 2000 (2004, background): “5–2:75mmolm 3 determined by Sambroto et al. (1986) in the Bering Sea) and 0:05mmolm 3 for ammonium uptake (Tyrrell and Taylor, 1996).”
Representing key phytoplankton functional groups in ocean carbon cycle models: Coccolithophorids (2002, background): “…in diatoms [Grime, 1979; Raven, 1997], and lack of storage vacuoles and low nutrient uptake rates in coccolithophorids [Eppley et al., 1969; Riegman et al., 2000] may explain the glacial-interglacial transition in the relative abundance of carbonate/silicate deposited in marine sediments…”
Environmental controls on coccolithophore calcification (2012, background): “Riegman et al. (2000) showed that Emiliania huxleyi has the highest affinity for PO43– ever recorded in a phytoplankton species.”
Novel copper‐binding and nitrogen‐rich thiols produced and exuded by Emiliania huxleyi (2004, background): “Despite a reportedly low uptake rate for nitrate (Riegman et al. 2000) and the lack of a vacuole that permits nutrient storage, E.”