Physiological aspects of the production and conversion of DMSP in marine algae and higher plants
By J. Stefels. 2000
633 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/c1014f2a725ef25608c0ef5ae14ab16f22c0e0d0
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In Atmospheric Science
- M. Puglisi
- M. Rijssel
- W. Gieskes
- L. Hofmann
- K. Bischof
- K. L. Van Alstyne
- Jens C. Nejstgaard
- G. Malin
In Oceanography
- U. Riebesell
- Michael Steinke
- K. Bischof
- L. Hofmann
- Hans-Peter Grossart
- S. Strom
- G. Malin
- M. Allgaier
Citations in the corpus
- Evidence for methane production by the marine algae Emiliania huxleyi (2016, background): “In contrast to the ubiquitous C-source bicarbonate – which can also be used to build Met in algae (Stefels, 2000) – Met is incorporated in specific metabolic pathways.”
- Chemical defense in the microplankton II: Inhibition of protist feeding by β‐dimethylsulfoniopropionate (DMSP) (2003, background): “DMSP is known to act as both an osmolyte and a cryoprotectant in certain algal species (Vairavamurthy et al. 1985; Karsten et al. 1996; Stefels 2000).”
- Vitamin B12 and iron colimitation of phytoplankton growth in the Ross Sea (2007, background): “osmolyte, a cryoprotectant (Stefels 2000), and as an antioxidant (Sunda et al.”
- Coupling of heterotrophic bacteria to phytoplankton bloom development at different pCO 2 levels: a mesocosm study (2008, background): “, 2002) or overflow mechanism (Stefels, 2000).”
- DIMETHYLSULFONIOPROPIONATE CLEAVAGE BY MARINE PHYTOPLANKTON IN RESPONSE TO MECHANICAL, CHEMICAL, OR DARK STRESS1 (2002, background): “DMSP biosynthesis may serve as an overflow mechanism for reducing power (Stefels 2000), with the “excess” DMSP removed by both excretion and cleavage to DMS or by scavenging hydroxyl radicals produced during photosynthesis (Sunda et al. 2001).”
- DMSP in marine macroalgae and macroinvertebrates: Distribution, function, and ecological impacts (2007, background): “Multiple evolutionary origins of DMSP production among all organisms are supported by the existence of at least three different synthetic pathways used in the production of DMSP in algae and vascular plants (reviewed by Stefels, 2000).”
- Effects of environmental factors on dimethylated sulfur compounds and their potential role in the antioxidant system of the coral holobiont (2014, background): “marine algae and bacteria (Stefels 2000), making DMSP a”
- Temperature, light, and the dimethylsulfoniopropionate (DMSP) content of Emiliania huxleyi (Prymnesiophyceae) (2002, background): “DMSP is a compatible solute that contributes to the osmotic balance of algal cells in sea water (Kirst, 1996) and cellular DMSP content is often found to be coupled to salinity (Dickson et al., 1982; Reed, 1983; Vairavamurthy et al., 1985; Dickson and Kirst, 1987a,b; Karsten et al., 1991a, 1992; Kir”
- Diversity, distribution and roles of osmoprotective compounds accumulated in halophytes under abiotic stress. (2015, background): “In addition, the high concentrations of DMSP in the tissues of Spartina species, W. biflora and Saccharum species would contribute to a high baseline osmotic potential, thus giving constitutive tolerance of salinity-related stress (Otte and Morris, 1994; Stefels, 2000).”
- Biofiltering efficiency, uptake and assimilation rates of Ulva clathrata (Roth) J. Agardh (Clorophyceae) cultivated in shrimp aquaculture waste water (2009, background): “Ulvoid algae increase DMSP concentrations as a way of expelling excess sulphur and energy, under conditions of high light, N limitation and unbalanced growth (Stefels 2000).”
- Current understanding of Phaeocystis ecology and biogeochemistry, and perspectives for future research (2007, background): “DMSP has properties in common with the compatible solute glycine betaine, and production of DMSP and DMS may be related to physiological stress (Stefels 2000; Sunda et al. 2002).”
- Ocean acidification effects on calcifying macroalgae (2014, background): “Some calcifying macroalgae have been shown to produce DMSP in a diel cycle, with production highest at night when the carbonate saturation state of the seawater is lowest (Burdett et al. 2013), and under manipulated pCO2 conditions (Burdett et al. 2012).”