New and important roles for DMSP in marine microbial communities
By R. Kiene, L. Linn, J. Bruton. 2000
578 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography, Process Chemistry and Technology
View Paper: https://www.semanticscholar.org/paper/a49201b8e45d0adfd266fa2845471e0cfd322ce6
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In Atmospheric Science
In Oceanography
- U. Riebesell
- Hans-Peter Grossart
- D. Thornton
- M. Allgaier
- Michael Steinke
- M. Vogt
- R. Thyrhaug
- M. Rijssel
In Process Chemistry and Technology
Citations in the corpus
- Dissolved organic matter (DOM) release by phytoplankton in the contemporary and future ocean (2014, background): “Compiling data from a range of in situ experiments and culture work, Kiene et al. (2000) concluded that DMSP forms <1 to 39% of the cell carbon quota of phytoplankton, with most values lying in the range of 1–5%.”
- Linking a Bacterial Taxon to Sulfur Cycling in the Sea: Studies of the Marine Roseobacter Group (2003, background): “Thus the DMSP cleavage pathway has important implications for global climate regulation while the DMSP demethylation pathway plays an important role in supplying carbon and sulfur to the marine food web (Kiene et al. 2000; Simó et al. 2002).”
- Environmental constraints on the production and removal of the climatically active gas dimethylsulphide (DMS) and implications for ecosystem modelling (2007, background): “Kiene et al. (2000) also stipulated that it is not necessary for the DMSP d concentration to be high, but that it is the bacterial sulphur demand relative to the DMSP d availability that is critical.”
- Coupling of heterotrophic bacteria to phytoplankton bloom development at different pCO 2 levels: a mesocosm study (2008, background): “Furthermore, marine bacteria can satisfy almost all their sulphur demand through DMSP consumption (e.g. Kiene et al., 2000).”
- Temperature, light, and the dimethylsulfoniopropionate (DMSP) content of Emiliania huxleyi (Prymnesiophyceae) (2002, background): “Especially when the bloom collapses and the DMSP is released into the water column, a mismatch in DMSP availability and the bacterial reduced sulphur demand occurs and superfluous DMSP is cleaved into DMS and acrylate facilitating escape of DMS to the atmosphere (Kiene et al., 2000).”