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Han Lu, Deng Xue, Li Peifeng, Gao Xianchi, Liu Chunying. Effects of temperature on biogenic sulfur production of Ulva prolifera during the decline period[J]. Haiyang Xuebao, 2018, 40(10): 110-118. doi: 10.3969/j.issn.0253-4193.2018.10.011
Citation: Han Lu, Deng Xue, Li Peifeng, Gao Xianchi, Liu Chunying. Effects of temperature on biogenic sulfur production of Ulva prolifera during the decline period[J]. Haiyang Xuebao, 2018, 40(10): 110-118. doi: 10.3969/j.issn.0253-4193.2018.10.011

Effects of temperature on biogenic sulfur production of Ulva prolifera during the decline period

doi: 10.3969/j.issn.0253-4193.2018.10.011
  • Received Date: 2018-03-23
  • Rev Recd Date: 2018-06-13
  • In order to study the characteristics of the release of biogenic sulfur of Ulva prolifera, laboratory simulations were conducted on the Ulva prolifera collected in the middle and late green tides of the Yellow Sea. The effects of different temperatures on the release of biogenic sulfides from Ulva prolifera were investigated. The results are as follows:under the condition of 10-25℃, the increase of temperature can promote the decline of Ulva prolifera. The average release rate of DMS ranged from 2.79-150.70 nmol/(L·g·d), the average release rate of DMSP ranged from 2.16-113.26 nmol/(L·g·d). On the other hand, the high temperature can accelerate the releasing rates of dimethysulfide (DMS) and dimethylsulfonionpropionate (DMSP), and increase the releasing amount. The maximum average release rate of DMS is increased by about 60% at 25℃ compared with 10℃, and the concentration of DMS in culture fluid is increased by 2-3 times. The concentration of DMS and DMSP collected in the culture fluid of Ulva prolifera at the end of green tide was increased compared with that of Ulva prolifera taken during the mid-green tide. The highest concentration of DMS in the culture fluid at the end of green tide of Ulva prolifera was 418.41 nmol/L, which was about 4 times of that in the middle period. The highest concentration of DMS in DMSP was 316.14 nmol/L, which was 3 times of the middle period. The outbreak of the green tide of the Enteromorpha will affect the circulation of the sulfur system in the water body and thus affect the ecological environment of the sea area.
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  • Charlier R H, Morand P, Finkl C W, et al. Green tides on the Brittany coasts[J]. Environmental Research, Engineering and Management, 2007, 3(41):52-59.
    Wang Wenjun, Wang Feijiu, Chen Songlin, et al. PCR amplification and sequence analysis of ITS regions of Enteromorpha prolifera[J]. Marine Fisheries Research, 2008, 29(5):124-129.
    Liu Dongyan, Keesing J K, Dong Zhijun, et al. Recurrence of the world's largest green-tide in 2009 in Yellow Sea, China:Porphyra yezoensis aquaculture rafts confirmed as nursery for macroalgal blooms[J]. Marine Pollution Bulletin, 2010, 60(9):1423-1432.
    钱树本, 刘东艳, 孙军. 海藻学[M]. 青岛:中国海洋大学出版社, 2005:529. Qian Shuben, Liu Dongyan, Sun Jun. Marine Phycology[M]. Qingdao:China Ocean University Press, 2005:529.
    Wang X K, Ma J H, Ye D C, et al. Preliminary study on the life history of Enteromorpha prolifera[J]. Marine Science Bulletin, 2007, 26(5):112-116.
    Liu Feng, Pang Shaojun, Xu Na, et al. Ulva diversity in the Yellow Sea during the large-scale green algal blooms in 2008-2009[J]. Phycological Research, 2010, 58(4):270-279.
    Luo Minbo, Liu Feng. Salinity-induced oxidative stress and regulation of antioxidant defense system in the marine macroalga Ulva prolifera[J]. Journal of Experimental Marine Biology and Ecology, 2011, 409(1/2):223-228.
    Liu Feng, Pang Shaojun, Zhao Xiaobo, et al. Quantitative, molecular and growth analyses of Ulva microscopic propagules in the coastal sediment of Jiangsu province where green tides initially occurred[J]. Marine Environmental Research, 2012, 74:56-63.
    Liu Dongyan, Keesing J K, He Peimin, et al. The world's largest macroalgal bloom in the Yellow Sea, China:Formation and implications[J]. Estuarine, Coastal and Shelf Science, 2013, 129:2-10.
    刘峰, 逄少军. 黄海浒苔绿潮及其溯源研究进展[J]. 海洋科学进展, 2012, 30(3):441-449. Liu Feng, Pang Shaojun. Research advances on green tides in the Yellow Sea[J]. Advances in Marine Science, 2012, 30(3):441-449.
    丁月旻. 黄海浒苔绿潮中生源要素的迁移转化及对生态环境的影响[D]. 青岛:中国科学院研究生院海洋研究所, 2014. Ding Yuemin. Impacts of Ulva (Enteromorpha) prolifera in the green tide on the Yellow Sea ecological environment-Implications from migration and transformation of biogenic elements[D]. Qingdao:Institute of Oceanology, Chinese Academy of Sciences, 2014.
    Sunda W, Kieber D J, Kiene R P, et al. An antioxidant function for DMSP and DMS in marine algae[J]. Nature, 2002, 418(6895):317-320.
    Karsten U, Kück K, Vogt C, et al. Dimethylsulfoniopropionate Production in Phototrophic Organisms and its Physiological Functions as a Cryoprotectant[M]//Kiene R P, Visscher P T, Keller M D, et al. Biological and Environmental Chemistry of DMSP and Related Sulfonium Compounds. Boston, MA:Springer US, 1996:143-153.
    González J M, Johnston A W B, Vila-Costa M, et al. Genetics and molecular features of bacterial dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) transformations[C]//Timmis K N. Handbook of Hydrocarbon and Lipid Microbiology. Berlin:Springer, 2010.
    Andreae M O. Ocean-atmosphere interactions in the global biogeochemical sulfur cycle[J]. Marine Chemistry, 1990, 30:1-29.
    Andreae M O, Raemdonck H. Dimethyl sulfide in the surface ocean and the marine atmosphere:a global view[J]. Science, 1983, 221(4612):744-747.
    Charlson R J, Lovelock J E, Andreae M O, et al. Oceanic phytoplankton, atmospheric sulfur, cloud albedo and climate[J]. Nature, 1987, 326:655-661.
    Guillard R R L, Ryther J H. Studies of marine planktonic diatoms:Ⅰ. Cyclotella nana Hustedt, and Detonula confervacea (cleve) Gran[J]. Canadian Journal of Microbiology, 1962, 8(2):229-239.
    李瑞香, 吴晓文, 韦钦胜, 等. 不同营养盐条件下浒苔的生长[J]. 海洋科学进展, 2009, 27(2):211-216. Li Ruixiang, Wu Xiaowen, Wei Qinsheng, et al. Growth of Enteromorpha prolifera under different uutrient conditions[J]. Advances in Marine Science, 2009, 27(2):211-216.
    Oremland R S. Biogeochemistry of Global Change:Radiatively Active Trace Gases Selected Papers from the Tenth International Symposium on Environmental Biogeochemistry, San Francisco, August 19-24, 1991[M]. New York:Chapman & Hall, 1993.
    Yang Guipieng, Jing Weiwen, Kang Zhiqiang, et al. Spatial variations of dimethylsulfide and dimethylsulfoniopropionate in the surface microlayer and in the subsurface waters of the South China Sea during springtime[J]. Marine Environmental Research, 2008, 65(1):85-97.
    Steinke M, Wolfe G V, Kirst G O. Partial characterisation of dimethylsulfoniopropionate (DMSP) lyase isozymes in 6 strains of Emilianiahuxleyi[J]. Marine Ecology Progress Series, 1998, 175:215-225.
    Stefels J, van Boekel W. Production of DMS from dissolved DMSP in axenic cultures of the marine phytoplankton species Phaeocystis sp.[J]. Marine Ecology Progress Series, 1993, 97(1):15-18.
    Li Hongmei, Zhang Yongyu, Tang Hongjie, et al. Spatiotemporal variations of inorganic nutrients along the Jiangsu coast, China, and the occurrence of macroalgal blooms (green tides) in猠灴桨敥爠楳捯?摴楨浥敲瑮栠祙汥獬畬汯晷椠摓敥??慊敝爮漠獈潡汲獭?慵湬搠?捬汧潡略搬?挲漰渱搷攬渠猶愳琺椱漶渴?渱男挲氮攼楢孲?嵛?‵?漠畈牵渠慌汩?潮晢??攠潈灵栠祃獨極捡慮汭?剮攬猠效慥爠捍桩??瑸浩潡献瀠桒敥牭敯獴?????????どは????????????ㄠ?????戾牕?孶??嵰??敬杩杦???????攠牭敡正?副?????漠扩扮猠?偨?嘠??敬瑬?慷氠???楛浊敝琮栠祒汥?獯畴汥映楓摥敮?慩湮摧?捯汦漠畅摮?捩潲湯摮敭湥獮慴琬椠漲渰?渷甬挠氱改甲猺′挱漷爭爲攲氷愮琼楢潲渾獛′椶湝?璛桞攬?渴潟狉琬栠攘慨猬琠?倮愠揺榎晈楊挭?佁振攱慂溄嬲?崱???潷畷狟湒懔汾?濶智??敛潊灝栮礠獷椋揑慦氬?刲攰猱收愬爠挴栰??琩洺漱猱瀵栭攱爲攳献????????????????????????????扡牮?嬬??嵴??敬搮礠慓牰摡???????楤挠牴潥扭楰慯汲?捬礠捶污楲湩条?潩晬???匠偯?愠渼摩 ̄??卶?椠湰?捯潬慩獦瑥慲污?愯湩搾?潩汮椠杴潨瑥爠潙灥桬楬捯?猠敓慥睡愬琠敃牨孩?嵡???椠洲渰漱水潛杊祝?愠湍摡?佩据敥愠湓潣杩牥慮灣桥祳?????????????????????戮爼?孲??崲?噝愠湨??甬礠汵???????椮攠猶母攴猟?坩?埂?????漆瀖??????斅琡?愔汶???椮漠汿漰柑楦挬愠氲‰挱漶測琠爱漴氨?漩昺?猳栲漭爸琳?琮攠牚浨?癵愠牌楩慮瑦楥潩測猠?楨湡?琠桙敡?捷潥湮挬攠湇瑵牡慮琠楘潩湵?潩普???協偨?愠湩摮???卲?摳畩牭極湬条?慩??椠?側桵慤敹漠捯祮猠瑣楨獡??楥??獦瀠牰楨湹杳?扣污潬漠浡孮?崠???潭畩牣湡慬氠?潮晤?卣敡慴?割敳猠敯慦爠捷桡?????????ぴ????????ㄠ??????扯牳?孴??嵮??楲敯湣敥?剳?偯???楩湸渠???????楦猠瑡牱極扡畴瑩楣漠湰?慡湮摴?瑛畊牝渮漠癗敥牴?潡普?搠楓獣獩潥汮癣敥搬???匱倶?愠渱搴?椶琩猺?爳攲氭愸琳椹漮渼獢桲椾灛′眸楝琠栠?戬愠掓琕敿爬椠憋氜?瀬爠潉搮甠挍琌椩澦湡?愋溒撇?撉椴洍敩瑐棂秹氊玆甴汓昭椥摻旐?榦溄?瓍桛敊??甠水晄?濝暤??攲砰椱挱漬嬠?崷???椺洲渲漭氲漶朮礠?慨湡摮?传捊敵愬渠潄来牮慧瀠案祵???ふちの????????????????et al. Impacts of decomposition of submerged plants on nutrient concentrations in overlying water in Tuhai River under different temperatures[J]. Water Resources Protection, 2011, 27(4):22-26.
    Nguyen B C, Belviso S, Mihalopoulos N, et al. Dimethyl sulfide production during natural phytoplanktonic blooms[J]. Marine Chemistry, 1988, 24(2):133-141.
    Yang Guipeng, Song Yizhu, Zhang Hai, et al. Seasonal variation and biogeochemical cycling of dimethylsulfide (DMS) and dimethylsulfoniopropionate (DMSP) in the Yellow Sea and Bohai Sea[J]. Journal of Geophysical Research:Oceans, 2015, 119(12):8897-8915.
    许高宾. 浒苔爆发对海水中生源硫代谢产物的影响[D]. 青岛:中国海洋大学, 2016. Xu Gaobin. Study on the effect of the outbreak of enteromorpha on biogenic sulfur production[D]. Qingdao:Ocean University of China, 2016.
    Andreae M O. The ocean as a source of atmospheric sulfur compounds[M]//Buat-Ménard P. The Role of Air-Sea Exchange in Geochemical Cycling. Dordrecht:Springer, 1986:331-362.
    Andreae M O, Elbert W, De Mora S J. Biogenic sulfur emissions and aerosols over the tropical South Atlantic:3. Atmo
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