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Journal articles on the topic 'Dimethylsulphide'

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Published: 4 June 2021

Last updated: 20 February 2023

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1

Simo, Rafel, Joan O. Grimalt, and Joan Albaigés. "Dissolved dimethylsulphide, dimethylsulphoniopropionate and dimethylsulphoxide in western Mediterranean waters." Deep Sea Research Part II: Topical Studies in Oceanography 44, no. 3-4 (1997): 929–50. http://dx.doi.org/10.1016/s0967-0645(96)00099-9.

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2

Uher, Günther, J. Julian Pillans, Angela D. Hatton, and Robert C. Upstill-Goddard. "Photochemical oxidation of dimethylsulphide to dimethylsulphoxide in estuarine and coastal waters." Chemosphere 186 (November 2017): 805–16. http://dx.doi.org/10.1016/j.chemosphere.2017.08.050.

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3

Bouillon, René-Christian, Peter A. Lee, Stephen J. de Mora, Maurice Levasseur, and Connie Lovejoy. "Vernal distribution of dimethylsulphide, dimethylsulphoniopropionate, and dimethylsulphoxide in the North Water in 1998." Deep Sea Research Part II: Topical Studies in Oceanography 49, no. 22-23 (January 2002): 5171–89. http://dx.doi.org/10.1016/s0967-0645(02)00184-4.

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4

Kwint, RLJ, and KJM Kramer. "Dimethylsulphide production by plankton communities." Marine Ecology Progress Series 121 (1995): 227–37. http://dx.doi.org/10.3354/meps121227.

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5

Buckley, Fiona S. E., and Stephen M. Mudge. "Dimethylsulphide and ocean–atmosphere interactions." Chemistry and Ecology 20, no. 2 (April 2004): 73–95. http://dx.doi.org/10.1080/02757540410001670209.

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6

Shooter, David, and Peter Brimblecombe. "Dimethylsulphide oxidation in the ocean." Deep Sea Research Part A. Oceanographic Research Papers 36, no. 4 (April 1989): 577–85. http://dx.doi.org/10.1016/0198-0149(89)90007-1.

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7

SMITH, ANDREW T., ROBERT C. BRAY, ALASTAIR G. McEWAN, ALAN S. McALPINE, and SUE BAILEY. "Stopped-flow studies on dimethylsulphoxide reductase from Rhodobacter capsulatus: kinetic competence of the dimethylsulphide-reduced intermediate." Biochemical Society Transactions 26, no. 3 (August 1, 1998): S211. http://dx.doi.org/10.1042/bst026s211.

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8

ŠUSTA, J., and P. HAVLOVÁ. "A Study of Dimethylsulphide Formation During Malting." Kvasny Prumysl 42, no. 11 (November 1, 1996): 346–49. http://dx.doi.org/10.18832/kp1996027.

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9

Brimblecombe, Peter, and David Shooter. "Photo-oxidation of dimethylsulphide in aqueous solution." Marine Chemistry 19, no. 4 (September 1986): 343–53. http://dx.doi.org/10.1016/0304-4203(86)90055-1.

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10

Cropp, Roger A., John Norbury, Albert J. Gabric, and Roger D. Braddock. "Modeling dimethylsulphide production in the upper ocean." Global Biogeochemical Cycles 18, no. 3 (July 27, 2004): n/a. http://dx.doi.org/10.1029/2003gb002126.

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11

Kniveton, Dominic R., Martin C. Todd, Jean Sciare, and Nikos Mihalopoulos. "The net effect of ultraviolet radiation on atmospheric dimethylsulphide over the Southern Indian Ocean." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 363, no. 1826 (January 15, 2005): 187–89. http://dx.doi.org/10.1098/rsta.2004.1486.

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Dimethylsulphide (DMS) in the atmosphere may play an important role in the climate system. This study shows an inverse relationship between ultraviolet extremes and atmospheric DMS, independent of changes in wind speed, sea–surface temperature and photosynthetically active radiation, as measured at Amsterdam Island in the Southern Indian Ocean.

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12

Ferek, R. J., R. B. Chatfield, and M. O. Andreae. "Vertical distribution of dimethylsulphide in the marine atmosphere." Nature 320, no. 6062 (April 1986): 514–16. http://dx.doi.org/10.1038/320514a0.

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13

Dacey, John W. H., Gary M. King, and Stuart G. Wakeham. "Factors controlling emission of dimethylsulphide from salt marshes." Nature 330, no. 6149 (December 1987): 643–45. http://dx.doi.org/10.1038/330643a0.

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14

Broadbent, Andrew D., and Graham B. Jones. "DMS and DMSP in mucus ropes, coral mucus, surface films and sediment pore waters from coral reefs in the Great Barrier Reef." Marine and Freshwater Research 55, no. 8 (2004): 849. http://dx.doi.org/10.1071/mf04114.

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Concentrations of dimethylsulphide (DMS) and its precursor compound dimethylsulphoniopropionate (DMSP), two sulphur compounds that are involved in the formation of clouds, were measured for mucus ropes, coral mucus, surface films and sediment pore waters collected from three coral reefs in the Great Barrier Reef, Australia. The concentrations of DMS (61–18 665 nm) and DMSP (1978–54 381 nm) measured in mucus rope samples are the highest yet reported in the marine environment. The values exceed concentrations of DMS and DMSP reported from highly productive polar waters and sea ice algal communities. Concentrations of DMSP in coral mucus ranged from 1226 to 25 443 nm, with mucus from Acropora formosa containing the highest levels of DMSP. Dimethylsulphide and DMSP in surface microlayer samples from three coral reefs were two to four times subsurface (0.5 m) concentrations. In coral-reef sediment pore waters, concentrations of DMS and DMSP were substantially higher than water-column concentrations, suggesting that coral sediments may be a significant source of these two compounds to reef waters. Overall, the results strongly suggest that coral reefs in the Great Barrier Reef are significant sources of these two sulphur substances.

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15

SHOOTER, DAVID, NEMINDRA JAYATISSA, and NOEL RENNER. "Volatile reduced sulphur compounds in butter by solid phase microextraction." Journal of Dairy Research 66, no. 1 (February 1999): 115–23. http://dx.doi.org/10.1017/s002202999800329x.

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The reduced sulphur volatiles, methanethiol and dimethyldisulphide (but not dimethylsulphide), have been detected in the headspace of butter samples. Their concentrations in the butter itself were calculated by determination of the distribution coefficient (K) through spiking butter samples with known quantities of methanethiol and dimethyldisulphide. The K values obtained suggest that the dimethyldisulphide had a greater affinity than methanethiol for the lipid phase of the butter. Solid phase microextraction used in conjunction with gas chromatography–mass spectrometry has been shown to be an effective method for headspace analysis and was used for quantifying the butter headspace concentrations of the reduced sulphur compounds. Seasonal variation of both methanethiol and dimethyldisulphide were found in a series of butter samples, the highest concentration being in spring with an overall decrease through the New Zealand summer. Grass type and condition appeared to influence the concentrations of these compounds in the butter. Storage of the series of butter samples at 4°C for 5 weeks resulted in a significant decrease in the concentrations of both methanethiol and dimethyldisulphide. The dimethylsulphide concentration in all butter samples was below the detection limit of the analytical system used.

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16

Garcés, Esther, Elisabet Alacid, Albert Reñé, Katherina Petrou, and Rafel Simó. "Host-released dimethylsulphide activates the dinoflagellate parasitoid Parvilucifera sinerae." ISME Journal 7, no. 5 (January 24, 2013): 1065–68. http://dx.doi.org/10.1038/ismej.2012.173.

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17

Shenoy, Damodar M., K. B. Sujith, Mangesh U. Gauns, Shrikant Patil, Amit Sarkar, Hema Naik, P. V. Narvekar, and S. W. A. Naqvi. "Production of dimethylsulphide during the seasonal anoxia off Goa." Biogeochemistry 110, no. 1-3 (March 18, 2012): 47–55. http://dx.doi.org/10.1007/s10533-012-9720-5.

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18

De Mora, S. J., P. A. Lee, A. Grout, C. Schall, and K. G. Heumann. "Aspects of the biogeochemistry of sulphur in glacial melt water ponds on the McMurdo Ice Shelf, Antarctica." Antarctic Science 8, no. 1 (March 1996): 15–22. http://dx.doi.org/10.1017/s0954102096000041.

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The distribution of dimethylsulphide (DMS), together with the precursor dimethylsulphonio-propionate (DMSP) and the oxidation product dimethylsulphoxide (DMSO), was measured in melt waters on the McMurdo Ice Shelf in the immediate vicinity of Bratina Island. Conductivity in these sulphate dominated ponds was extremely variable, ranging from 0.106–52.3 mS cm−1. Similarly, chlorophyll a concentrations in the pond waters (1–150 μg 1−1) and mats (1.4–33 μg cm−2) differed considerably. The biomass was dominated by benthic felts of phototrophic cyanobacteria, which might act as a source of biogenic sulphur compounds in the ponds. The mean (and ranges) of concentrations of dissolved sulphur compounds (nmol 1−1) were: CS2 0.16 (<0.04–1.29); DMSPd 0.6 (<0.07–8.4); DMS 3.5 (<0.07–183); DMSO 27.9 (15.5–184.5). Very high concentrations of DMSO were ubiquitous in the ponds in the ice-cored moraine region of the ice shelf, with dissolved concentrations having been 1–2 orders of magnitude greater than those of DMS or DMSPd. It is difficult to ascribe the formation of DMSO solely to the conventionally accepted pathways of DMS oxidation by either bacterial activity or photochemical reactions. A direct biosynthetic production from phytoplankton or bacteria might be involved which means that DMSO in aquatic environments could act as a significant source of DMS rather than as a sink as generally supposed.

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19

ČULÍK, J., V. KELLNER, B. ŠPINAR, and Z. RÖSSNEROVÁ. "Quantitative analysis of free dimethylsulphide and its precursors in malt and beer. I. Quantitative analysis of free dimethylsulphide and its precursors in malt." Kvasny Prumysl 37, no. 8 (August 1, 1991): 225–30. http://dx.doi.org/10.18832/kp1991023.

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20

Fogelqvist, Elisabet. "Dimethylsulphide (DMS) in the Weddell Sea surface and bottom water." Marine Chemistry 35, no. 1-4 (November 1991): 169–77. http://dx.doi.org/10.1016/s0304-4203(09)90015-9.

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21

Cerqueira, M. A., and C. A. Pio. "Production and release of dimethylsulphide from an estuary in Portugal." Atmospheric Environment 33, no. 20 (September 1999): 3355–66. http://dx.doi.org/10.1016/s1352-2310(98)00378-1.

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22

Kittler, P., H. Swan, and J. Ivey. "An indicating oxidant scrubber for the measurement of atmospheric dimethylsulphide." Atmospheric Environment. Part A. General Topics 26, no. 14 (October 1992): 2661–64. http://dx.doi.org/10.1016/0960-1686(92)90117-4.

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23

Toumi, Ralf. "BrO as a sink for dimethylsulphide in the marine atmosphere." Geophysical Research Letters 21, no. 2 (January 15, 1994): 117–20. http://dx.doi.org/10.1029/93gl03536.

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24

ČULÍK, J., V. KELLNER, B. ŠPINAR, Z. RÖSSNEROVÁ, and L. VESELÝ. "Quantitative analysis of free dimethylsulphide and its precursors in malt and beer II. Quantitative analysis of free dimethylsulphide and its precursors in wort and beer." Kvasny Prumysl 37, no. 12 (December 1, 1991): 329–34. http://dx.doi.org/10.18832/kp1991032.

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25

Matrai, Patricia A. "Dimethylsulphide: Oceans, atmosphere and climate (G. Restelli and G. Angeletti [eds.])." Limnology and Oceanography 39, no. 6 (September 1994): 1497. http://dx.doi.org/10.4319/lo.1994.39.6.1497.

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26

Gabric, Albert J., Peter H. Whetton, and Roger Cropp. "Dimethylsulphide production in the subantarctic southern ocean under enhanced greenhouse conditions." Tellus B: Chemical and Physical Meteorology 53, no. 3 (January 2001): 273–87. http://dx.doi.org/10.3402/tellusb.v53i3.16596.

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27

Zemmelink, H. J., J. WH Dacey, and E. J. Hintsa. "Direct measurements of biogenic dimethylsulphide fluxes from the oceans: a synthesis." Canadian Journal of Fisheries and Aquatic Sciences 61, no. 5 (May 1, 2004): 836–44. http://dx.doi.org/10.1139/f04-047.

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This paper provides a brief overview of the state-of-the-art of techniques that are currently used for field measurements of trace gas fluxes and the subsequent derivation of gas transfer rates over the oceans. Special attention is given to the relaxed eddy accumulation (REA) and gradient flux (GF) techniques, which rely on empirical functions thus far mainly validated over land. The universality of these functions and their application at sea have not yet been fully evaluated. New experiments have shown that the emission of dimethylsulphide (DMS) can be measured by the REA and GF techniques. Moreover, these measurements have provided parameterizations of gas exchange rates that are within the range of relationships between wind speed and gas transfer that have recently been derived from eddy correlation (EC) and deliberate tracer measurements. Using DMS as a model, gas is potentially a powerful approach to intercalibrate the REA, GF, and EC techniques, test their applicability in the marine environment, and investigate processes that determine trace gas exchange across the ocean surface.

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28

GABRIC, ALBERT J., PETER H. WHETTON, and ROGER CROPP. "Dimethylsulphide production in the subantarctic southern ocean under enhanced greenhouse conditions." Tellus B 53, no. 3 (June 2001): 273–87. http://dx.doi.org/10.1034/j.1600-0889.2001.01244.x.

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29

Limão-Vieira, P., S. Eden, P. A. Kendall, N. J. Mason, and S. V. Hoffmann. "High resolution VUV photo-absorption cross-section for dimethylsulphide, (CH3)2S." Chemical Physics Letters 366, no. 3-4 (December 2002): 343–49. http://dx.doi.org/10.1016/s0009-2614(02)01651-2.

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30

Haimi, Piia, Petri Uusi-Kyyny, Juha-Pekka Pokki, Minna Pakkanen, Juhani Aittamaa, and Kari I. Keskinen. "Isothermal binary vapour–liquid equilibrium for butanes and butenes with dimethylsulphide." Fluid Phase Equilibria 266, no. 1-2 (April 2008): 143–53. http://dx.doi.org/10.1016/j.fluid.2008.01.030.

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31

Cropp, Roger A., Albert J. Gabric, Grant H. McTainsh, Roger D. Braddock, and Neil Tindale. "Coupling between ocean biota and atmospheric aerosols: Dust, dimethylsulphide, or artifact?" Global Biogeochemical Cycles 19, no. 4 (October 7, 2005): n/a. http://dx.doi.org/10.1029/2004gb002436.

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32

Randby, Å. "Effect of propanol and dimethylsulphide in grass silage on organoleptic milk quality." Journal of Animal and Feed Sciences 16, Suppl. 1 (January 26, 2007): 102–7. http://dx.doi.org/10.22358/jafs/74122/2007.

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33

Adedapo, Adebusayo E., Nsikak U. Benson, Akan B. Williams, and Kei Toda. "Field Assessment and determination of concentration levels of Dimethylsulphide in Tropical Seawater." Journal of Physics: Conference Series 1299 (August 2019): 012132. http://dx.doi.org/10.1088/1742-6596/1299/1/012132.

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34

Cropp, Roger, John Norbury, and Roger Braddock. "Dimethylsulphide, clouds, and phytoplankton: Insights from a simple plankton ecosystem feedback model." Global Biogeochemical Cycles 21, no. 2 (June 2007): n/a. http://dx.doi.org/10.1029/2006gb002812.

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35

Steinke, M., G. Malin, S. M. Turner, and P. S. Liss. "Determinations of dimethylsulphoniopropionate (DMSP) lyase activity using headspace analysis of dimethylsulphide (DMS)." Journal of Sea Research 43, no. 3-4 (August 2000): 233–44. http://dx.doi.org/10.1016/s1385-1101(00)00024-1.

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36

Jensen, N. R., J. Hjorth, C. Lohse, H. Skov, and G. Restelli. "Products and mechanism of the reaction between NO3 and dimethylsulphide in air." Atmospheric Environment. Part A. General Topics 25, no. 9 (January 1991): 1897–904. http://dx.doi.org/10.1016/0960-1686(91)90272-9.

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37

Malin, Gillian, Suzanne Turner, Peter Liss, Patrick Holligan, and Derek Harbour. "Dimethylsulphide and dimethylsulphoniopropionate in the Northeast atlantic during the summer coccolithophore bloom." Deep Sea Research Part I: Oceanographic Research Papers 40, no. 7 (July 1993): 1487–508. http://dx.doi.org/10.1016/0967-0637(93)90125-m.

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38

Ibberson, R. M., P. J. McDonald, and M. Pinter-Krainer. "The crystal structure determination of dimethylsulphide by high-resolution neutron powder diffraction." Journal of Molecular Structure 415, no. 3 (October 1997): 259–66. http://dx.doi.org/10.1016/s0022-2860(97)00102-6.

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39

Tománková, J., J. Bořilová, I. Steinhauserová, and L. Gallas. " Volatile organic compounds as biomarkers of the freshness of poultry meat packaged in a modified atmosphere." Czech Journal of Food Sciences 30, No. 5 (July 25, 2012): 395–403. http://dx.doi.org/10.17221/408/2011-cjfs.

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The volatile organic compounds (VOCs) in the packing of chicken meat in a modified atmosphere was qualitatively and quantitatively evaluated. The total number of 72 samples of chicken hindquarters were stored under two different modified atmospheres (70% O<sub>2</sub>, 30% CO<sub>2</sub>, and 70% argon, 30% CO<sub>2</sub>) for 20 days. Analyses were performed on Days 0, 4, 8, 12, 16, and 20. VOCs in the headspace samples were detected and quantified by gas chromatography/mass spectrometry (GC/MS) every fourth day of storage. Pentamethylheptane, dimethylsulphide, dimethyl disulphide, dimethyl trisulphide, dimethyl tetrasulphide, hydrogen sulphide and ammonia were detected. Pentamethylheptane and ammonia had similar values for both modified atmospheres (MA). The other compounds were found only in argon MA from the Day 16 of storage with a subsequent increase of values. The measured values for dimethylsulphide were 10.7 and 13.8 mg/l, for dimethyl disulphide they were 1.9 and 10.7 mg/l, dimethyl trisulphide levels were 15.7 and 19.3 mg/l and dimethyl tetrasulphide levels were 93.2 and 418.3 mg/l for Day 16 and 20. The hydrogen sulphide level was detected from 80 to 370 mg/l after the 8<sup>th</sup> day of storage. We showed that the argon MA is less suitable for packaging raw chicken parts than the oxygen MA in view of the increased amount of microflora and unpleasant odour as assessed by sensory analysis. Oxygen prolonged the shelf life by about four days in comparison with argon. Sensory evaluation was similar for both atmospheres after air exhaustion. The argon MA did not extend the shelf life as compared to the oxygen MA.  

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40

Bopp, Laurent, Olivier Aumont, Sauveur Belviso, and Stéphane Blain. "Modelling the effect of iron fertilization on dimethylsulphide emissions in the Southern Ocean." Deep Sea Research Part II: Topical Studies in Oceanography 55, no. 5-7 (March 2008): 901–12. http://dx.doi.org/10.1016/j.dsr2.2007.12.002.

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41

Legrand, M., C. Feniet-Saigne, E. S. Sattzman, C. Germain, N. I. Barkov, and V. N. Petrov. "Ice-core record of oceanic emissions of dimethylsulphide during the last climate cycle." Nature 350, no. 6314 (March 1991): 144–46. http://dx.doi.org/10.1038/350144a0.

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42

Franklin, DJ, M. Steinke, J. Young, I. Probert, and G. Malin. "Dimethylsulphoniopropionate (DMSP), DMSP-lyase activity (DLA) and dimethylsulphide (DMS) in 10 species of coccolithophore." Marine Ecology Progress Series 410 (July 14, 2010): 13–23. http://dx.doi.org/10.3354/meps08596.

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43

Adedapo, A. E., N. U. Benson, A. B. Williams, and K. Toda. "VAPOUR GENERATION CHEMILUMINESCENCE DETECTION SYSTEM FOR DETERMINATION OF DIMETHYLSULPHONIOPROPIONATE AND DIMETHYLSULPHIDE IN TROPICAL SEAWATER." Rasayan Journal of chemistry 13, no. 01 (2020): 44–50. http://dx.doi.org/10.31788/rjc.2020.1315432.

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44

Trevena, Anne J., and Graham B. Jones. "Dimethylsulphide and dimethylsulphoniopropionate in Antarctic sea ice and their release during sea ice melting." Marine Chemistry 98, no. 2-4 (February 2006): 210–22. http://dx.doi.org/10.1016/j.marchem.2005.09.005.

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45

Eyice, Özge, Motonobu Namura, Yin Chen, Andrew Mead, Siva Samavedam, and Hendrik Schäfer. "SIP metagenomics identifies uncultivated Methylophilaceae as dimethylsulphide degrading bacteria in soil and lake sediment." ISME Journal 9, no. 11 (March 27, 2015): 2336–48. http://dx.doi.org/10.1038/ismej.2015.37.

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46

Gabric, Albert J., Patricia A. Matrai, and MaríA Vernet. "Modelling the production and cycling of dimethylsulphide during the vernal bloom in the Barents Sea." Tellus B: Chemical and Physical Meteorology 51, no. 5 (January 1999): 919–37. http://dx.doi.org/10.3402/tellusb.v51i5.16505.

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47

Marandino, C. A., S. Tegtmeier, K. Krüger, C. Zindler, E. L. Atlas, F. Moore, and H. W. Bange. "Dimethylsulphide (DMS) emissions from the western Pacific Ocean: a potential marine source for stratospheric sulphur?" Atmospheric Chemistry and Physics 13, no. 16 (August 26, 2013): 8427–37. http://dx.doi.org/10.5194/acp-13-8427-2013.

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Abstract. Sea surface and atmospheric measurements of dimethylsulphide (DMS) were performed during the TransBrom cruise in the western Pacific Ocean between Japan and Australia in October 2009. Air–sea DMS fluxes were computed between 0 and 30 μmol m−2 d−1, which are in agreement with those computed by the current climatology, and peak emissions of marine DMS into the atmosphere were found during the occurrence of tropical storm systems. Atmospheric variability in DMS, however, did not follow that of the computed fluxes and was more related to atmospheric transport processes. The computed emissions were used as input fields for the Lagrangian dispersion model FLEXPART, which was set up with actual meteorological fields from ERA-Interim data and different chemical lifetimes of DMS. A comparison with aircraft in situ data from the adjacent HIPPO2 campaign revealed an overall good agreement between modelled versus observed DMS profiles over the tropical western Pacific Ocean. Based on observed DMS emissions and meteorological fields along the cruise track, the model projected that up to 30 g S per month in the form of DMS, emitted from an area of 6 × 104 m2, can be transported above 17 km. This surprisingly large DMS entrainment into the stratosphere is disproportionate to the regional extent of the area of emissions and mainly due to the high convective activity in this region as simulated by the transport model. Thus, if DMS can cross the tropical tropopause layer (TTL), we suggest that the considerably larger area of the tropical western Pacific Ocean can be a source of sulphur to the stratosphere, which has not been considered as yet.

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48

GABRIC, ALBERT J., PATRICIA A. MATRAI, and MARIA VERNET. "Modelling the production and cycling of dimethylsulphide during the vernal bloom in the Barents Sea." Tellus B 51, no. 5 (November 1999): 919–37. http://dx.doi.org/10.1034/j.1600-0889.1999.t01-4-00005.x.

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49

Franklin, Daniel J., Alex J. Poulton, Michael Steinke, Jeremy Young, Ilka Peeken, and Gill Malin. "Dimethylsulphide, DMSP-lyase activity and microplankton community structure inside and outside of the Mauritanian upwelling." Progress in Oceanography 83, no. 1-4 (December 2009): 134–42. http://dx.doi.org/10.1016/j.pocean.2009.07.011.

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50

Hatton, Angela D. "Influence of photochemistry on the marine biogeochemical cycle of dimethylsulphide in the northern North Sea." Deep Sea Research Part II: Topical Studies in Oceanography 49, no. 15 (January 2002): 3039–52. http://dx.doi.org/10.1016/s0967-0645(02)00070-x.

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