Macroalgal mariculture is gaining global attention to achieve carbon neutrality due to its important contribution to ocean carbon sequestration.However,some wild macroalgal species(e.g.,Sargassum and Ulva prolifera)ex...Macroalgal mariculture is gaining global attention to achieve carbon neutrality due to its important contribution to ocean carbon sequestration.However,some wild macroalgal species(e.g.,Sargassum and Ulva prolifera)exhibit strong environmental adaptability and can cause large-scale,recurrent blooms in global oceans,fueled by rising atmospheric CO_(2) levels and coastal eutrophication.Notably,massive Ulva prolifera green tides have occurred annually in the Yellow Sea for the past 17 consecutive years.At the late blooming stage,millions of tons of U.prolifera naturally sink to the shallow seafloor.The subsequent intense microbial aerobic degradation of sinking macroalgae results in coastal hypoxia and acidification,with most of the macroalgal carbon returning to the atmosphere.Preventing or reducing the intense degradation of massive sinking U.prolifera could enable more macroalgal carbon storage in the ocean in the long term and alleviate the harmful effects of green tide.Thus,ecological disasters from macroalgal blooms may be transformed into useful natural platforms to increase ocean carbon sequestration.We propose an integrated strategy using environmentally friendly minerals(e.g.,montmorillonite and calcium carbonate)and coagulants(e.g.,polyaluminum chloride),along with natural algicidal bacteria or substances,to induce rapid flocculation and sedimentation of blooming macroalgae,reduce the degradation of sinking macroalgae and its negative environmental impacts,and minimize the generation of macroalgal propagules or seeds and the potential risk for future green tide outbreaks.This integrated approach is potentially a promising approach to tap the carbon sequestration potential of macroalgal blooms to mitigate climate change.展开更多
The China Seas include the South China Sea, East China Sea, Yellow Sea, and Bohai Sea. Located off the Northwestern Pacific margin, covering 4700000 km^2 from tropical to northern temperate zones, and including a vari...The China Seas include the South China Sea, East China Sea, Yellow Sea, and Bohai Sea. Located off the Northwestern Pacific margin, covering 4700000 km^2 from tropical to northern temperate zones, and including a variety of continental margins/basins and depths, the China Seas provide typical cases for carbon budget studies. The South China Sea being a deep basin and part of the Western Pacific Warm Pool is characterized by oceanic features; the East China Sea with a wide continental shelf, enormous terrestrial discharges and open margins to the West Pacific, is featured by strong cross-shelf materials transport; the Yellow Sea is featured by the confluence of cold and warm waters; and the Bohai Sea is a shallow semiclosed gulf with strong impacts of human activities. Three large rivers, the Yangtze River, Yellow River, and Pearl River, flow into the East China Sea, the Bohai Sea, and the South China Sea, respectively. The Kuroshio Current at the outer margin of the Chinese continental shelf is one of the two major western boundary currents of the world oceans and its strength and position directly affect the regional climate of China. These characteristics make the China Seas a typical case of marginal seas to study carbon storage and fluxes. This paper systematically analyzes the literature data on the carbon pools and fluxes of the Bohai Sea,Yellow Sea, East China Sea, and South China Sea, including different interfaces(land-sea, sea-air, sediment-water, and marginal sea-open ocean) and different ecosystems(mangroves, wetland, seagrass beds, macroalgae mariculture, coral reefs, euphotic zones, and water column). Among the four seas, the Bohai Sea and South China Sea are acting as CO_2 sources, releasing about0.22 and 13.86–33.60 Tg C yr^(-1) into the atmosphere, respectively, whereas the Yellow Sea and East China Sea are acting as carbon sinks, absorbing about 1.15 and 6.92–23.30 Tg C yr^(-1) of atmospheric CO_2, respectively. Overall, if only the CO_2 exchange at the sea-air interface is considered, the Chinese marginal seas appear to be a source of atmospheric CO_2, with a net release of 6.01–9.33 Tg C yr^(-1), mainly from the inputs of rivers and adjacent oceans. The riverine dissolved inorganic carbon (DIC) input into the Bohai Sea and Yellow Sea, East China Sea, and South China Sea are 5.04, 14.60, and 40.14 Tg C yr^(-1),respectively. The DIC input from adjacent oceans is as high as 144.81 Tg C yr^(-1), significantly exceeding the carbon released from the seas to the atmosphere. In terms of output, the depositional fluxes of organic carbon in the Bohai Sea, Yellow Sea, East China Sea, and South China Sea are 2.00, 3.60, 7.40, and 5.92 Tg C yr^(-1), respectively. The fluxes of organic carbon from the East China Sea and South China Sea to the adjacent oceans are 15.25–36.70 and 43.93 Tg C yr^(-1), respectively. The annual carbon storage of mangroves, wetlands, and seagrass in Chinese coastal waters is 0.36–1.75 Tg C yr^(-1), with a dissolved organic carbon(DOC) output from seagrass beds of up to 0.59 Tg C yr^(-1). Removable organic carbon flux by Chinese macroalgae mariculture account for 0.68 Tg C yr^(-1) and the associated POC depositional and DOC releasing fluxes are 0.14 and 0.82 Tg C yr^(-1), respectively. Thus, in total, the annual output of organic carbon, which is mainly DOC, in the China Seas is 81.72–104.56 Tg C yr^(-1). The DOC efflux from the East China Sea to the adjacent oceans is 15.00–35.00 Tg C yr^(-1). The DOC efflux from the South China Sea is 31.39 Tg C yr^(-1). Although the marginal China Seas seem to be a source of atmospheric CO_2 based on the CO_2 flux at the sea-air interface, the combined effects of the riverine input in the area, oceanic input, depositional export,and microbial carbon pump(DOC conversion and output) indicate that the China Seas represent an important carbon storage area.展开更多
To avoid the negative effects of antibiotics,using phage to prevent animal disease becomes a promising method in aquaculture.Here,a lytic phage provisionally named vB_Vca S_HC that can infect the pathogen(i.e.,Vibrio ...To avoid the negative effects of antibiotics,using phage to prevent animal disease becomes a promising method in aquaculture.Here,a lytic phage provisionally named vB_Vca S_HC that can infect the pathogen(i.e.,Vibrio campbellii 18)of prawn was isolated.The phage has an isometric head and a non-contractile tail.During phage infection,the induced host mortality in 5.5 h reached ca.96%,with a latent period of 1.5 h and a burst size of 172 PFU/cell.It has an 81,566 bp circular ds DNA genome containing 121 open reading frames(ORFs),and ca.71%of the ORFs are functionally unknown.Comparative genomic and phylogenetic analysis revealed that it is a novel phage belonging to Delepquintavirus,Siphoviridae,Caudovirales.In the phage genome,besides the ordinary genes related to structure assembly and DNA metabolism,there are 10 auxiliary metabolic genes.For the first time,the pyruvate phosphate dikinase(PPDK)gene was found in phages whose product is a key rate-limiting enzyme involving Embden-Meyerhof-Parnas(EMP)reaction.Interestingly,although the phage has a strong bactericidal activity and contains a potential lysogeny related gene,i.e.,the recombinase(Rec A)gene,we did not find the phage turned into a lysogenic state.Meanwhile,the phage genome does not contain any bacterial virulence gene or antimicrobial resistance gene.This study represents the first comprehensive characterization of a lytic V.campbellii phage and indicates that it is a promising candidate for the treatment of V.campbellii infections.展开更多
We studied the effects of expected end-of-the-century p CO_2(1000 ppm)on the photosynthetic performance of a coastal marine cyanobacterium Synechococcus sp.PCC7002 during the lag,exponential,and stationary growth phas...We studied the effects of expected end-of-the-century p CO_2(1000 ppm)on the photosynthetic performance of a coastal marine cyanobacterium Synechococcus sp.PCC7002 during the lag,exponential,and stationary growth phases.Elevated p CO_2significantly stimulated growth,and enhanced the maximum cell density during the stationary phase.Under ambient p CO_2conditions,the lag phase lasted for 6 days,while elevated p CO_2shortened the lag phase to two days and extended the exponential phase by four days.The elevated p CO_2increased photosynthesis levels during the lag and exponential phases,but reduced them during the stationary phase.Moreover,the elevated p CO_2reduced the saturated growth light(Ik)and increased the light utilization efficiency(α)during the exponential and stationary phases,and elevated the phycobilisome:chlorophyll a(Chl a)ratio.Furthermore,the elevated p CO_2reduced the particulate organic carbon(POC):Chl a and particulate organic nitrogen(PON):Chl a ratios during the lag and stationary phases,but enhanced them during the exponential phase.Overall,Synechococcus showed differential physiological responses to elevated p CO_2during different growth phases,thus providing insight into previous studies that focused on only the exponential phase,which may have biased the results relative to the effects of elevated p CO_2in ecology or aquaculture.展开更多
基金supported by the National Natural Science Foundation of China(nos.U1906216 and 42188102)the National Key Research and Development Program of China(2020YFA0608304)the MOST ONCE project.
文摘Macroalgal mariculture is gaining global attention to achieve carbon neutrality due to its important contribution to ocean carbon sequestration.However,some wild macroalgal species(e.g.,Sargassum and Ulva prolifera)exhibit strong environmental adaptability and can cause large-scale,recurrent blooms in global oceans,fueled by rising atmospheric CO_(2) levels and coastal eutrophication.Notably,massive Ulva prolifera green tides have occurred annually in the Yellow Sea for the past 17 consecutive years.At the late blooming stage,millions of tons of U.prolifera naturally sink to the shallow seafloor.The subsequent intense microbial aerobic degradation of sinking macroalgae results in coastal hypoxia and acidification,with most of the macroalgal carbon returning to the atmosphere.Preventing or reducing the intense degradation of massive sinking U.prolifera could enable more macroalgal carbon storage in the ocean in the long term and alleviate the harmful effects of green tide.Thus,ecological disasters from macroalgal blooms may be transformed into useful natural platforms to increase ocean carbon sequestration.We propose an integrated strategy using environmentally friendly minerals(e.g.,montmorillonite and calcium carbonate)and coagulants(e.g.,polyaluminum chloride),along with natural algicidal bacteria or substances,to induce rapid flocculation and sedimentation of blooming macroalgae,reduce the degradation of sinking macroalgae and its negative environmental impacts,and minimize the generation of macroalgal propagules or seeds and the potential risk for future green tide outbreaks.This integrated approach is potentially a promising approach to tap the carbon sequestration potential of macroalgal blooms to mitigate climate change.
基金supported by the National Key Research and Development Program of China (Grant No. 2016YFA0601400)the National Natural Science Foundation of China (Grant Nos. 91751207, 91428308, 41722603, 41606153 and 41422603)+1 种基金the Fundamental Research Funds for the Central Universities (Grant No. 20720170107)CNOOC Projects (Grant Nos. CNOOC-KJ125FZDXM00TJ001-2014 and CNOOCKJ125FZDXM00ZJ001-2014)
文摘The China Seas include the South China Sea, East China Sea, Yellow Sea, and Bohai Sea. Located off the Northwestern Pacific margin, covering 4700000 km^2 from tropical to northern temperate zones, and including a variety of continental margins/basins and depths, the China Seas provide typical cases for carbon budget studies. The South China Sea being a deep basin and part of the Western Pacific Warm Pool is characterized by oceanic features; the East China Sea with a wide continental shelf, enormous terrestrial discharges and open margins to the West Pacific, is featured by strong cross-shelf materials transport; the Yellow Sea is featured by the confluence of cold and warm waters; and the Bohai Sea is a shallow semiclosed gulf with strong impacts of human activities. Three large rivers, the Yangtze River, Yellow River, and Pearl River, flow into the East China Sea, the Bohai Sea, and the South China Sea, respectively. The Kuroshio Current at the outer margin of the Chinese continental shelf is one of the two major western boundary currents of the world oceans and its strength and position directly affect the regional climate of China. These characteristics make the China Seas a typical case of marginal seas to study carbon storage and fluxes. This paper systematically analyzes the literature data on the carbon pools and fluxes of the Bohai Sea,Yellow Sea, East China Sea, and South China Sea, including different interfaces(land-sea, sea-air, sediment-water, and marginal sea-open ocean) and different ecosystems(mangroves, wetland, seagrass beds, macroalgae mariculture, coral reefs, euphotic zones, and water column). Among the four seas, the Bohai Sea and South China Sea are acting as CO_2 sources, releasing about0.22 and 13.86–33.60 Tg C yr^(-1) into the atmosphere, respectively, whereas the Yellow Sea and East China Sea are acting as carbon sinks, absorbing about 1.15 and 6.92–23.30 Tg C yr^(-1) of atmospheric CO_2, respectively. Overall, if only the CO_2 exchange at the sea-air interface is considered, the Chinese marginal seas appear to be a source of atmospheric CO_2, with a net release of 6.01–9.33 Tg C yr^(-1), mainly from the inputs of rivers and adjacent oceans. The riverine dissolved inorganic carbon (DIC) input into the Bohai Sea and Yellow Sea, East China Sea, and South China Sea are 5.04, 14.60, and 40.14 Tg C yr^(-1),respectively. The DIC input from adjacent oceans is as high as 144.81 Tg C yr^(-1), significantly exceeding the carbon released from the seas to the atmosphere. In terms of output, the depositional fluxes of organic carbon in the Bohai Sea, Yellow Sea, East China Sea, and South China Sea are 2.00, 3.60, 7.40, and 5.92 Tg C yr^(-1), respectively. The fluxes of organic carbon from the East China Sea and South China Sea to the adjacent oceans are 15.25–36.70 and 43.93 Tg C yr^(-1), respectively. The annual carbon storage of mangroves, wetlands, and seagrass in Chinese coastal waters is 0.36–1.75 Tg C yr^(-1), with a dissolved organic carbon(DOC) output from seagrass beds of up to 0.59 Tg C yr^(-1). Removable organic carbon flux by Chinese macroalgae mariculture account for 0.68 Tg C yr^(-1) and the associated POC depositional and DOC releasing fluxes are 0.14 and 0.82 Tg C yr^(-1), respectively. Thus, in total, the annual output of organic carbon, which is mainly DOC, in the China Seas is 81.72–104.56 Tg C yr^(-1). The DOC efflux from the East China Sea to the adjacent oceans is 15.00–35.00 Tg C yr^(-1). The DOC efflux from the South China Sea is 31.39 Tg C yr^(-1). Although the marginal China Seas seem to be a source of atmospheric CO_2 based on the CO_2 flux at the sea-air interface, the combined effects of the riverine input in the area, oceanic input, depositional export,and microbial carbon pump(DOC conversion and output) indicate that the China Seas represent an important carbon storage area.
基金supported by the open task of Qingdao National Laboratory for Marine Science and Technology(QNLM2016ORP0311)the NSFC projects (41876174, U1906216)+4 种基金the Senior User Project of RV KEXUE (KEXUE2019GZ03) supported by Center for Ocean Mega-Science,Chinese Academy of Sciencesthe DICP&QIBEBT (DICP&QIBEBT UN201803)the QIBEBT (QIBEBT ZZBS 201805)Dalian National Laboratory For Clean Energy (DNL),CASCentral Public-interest Scientific Institution Basal Research Fund,CAFS (No. 2017HY-ZD1002)。
文摘To avoid the negative effects of antibiotics,using phage to prevent animal disease becomes a promising method in aquaculture.Here,a lytic phage provisionally named vB_Vca S_HC that can infect the pathogen(i.e.,Vibrio campbellii 18)of prawn was isolated.The phage has an isometric head and a non-contractile tail.During phage infection,the induced host mortality in 5.5 h reached ca.96%,with a latent period of 1.5 h and a burst size of 172 PFU/cell.It has an 81,566 bp circular ds DNA genome containing 121 open reading frames(ORFs),and ca.71%of the ORFs are functionally unknown.Comparative genomic and phylogenetic analysis revealed that it is a novel phage belonging to Delepquintavirus,Siphoviridae,Caudovirales.In the phage genome,besides the ordinary genes related to structure assembly and DNA metabolism,there are 10 auxiliary metabolic genes.For the first time,the pyruvate phosphate dikinase(PPDK)gene was found in phages whose product is a key rate-limiting enzyme involving Embden-Meyerhof-Parnas(EMP)reaction.Interestingly,although the phage has a strong bactericidal activity and contains a potential lysogeny related gene,i.e.,the recombinase(Rec A)gene,we did not find the phage turned into a lysogenic state.Meanwhile,the phage genome does not contain any bacterial virulence gene or antimicrobial resistance gene.This study represents the first comprehensive characterization of a lytic V.campbellii phage and indicates that it is a promising candidate for the treatment of V.campbellii infections.
基金supported by the National Key Research and Development Program of China (Grant No. 2016YFA0601402)the China SOA Grant Associated with Task (Grant No. GASI-03-01-02-05)+1 种基金the CNOOC Zhanjiang Branch (Grant No. CNOOC-KJ 125 FZDXM 00 ZJ 001-2014)the National Natural Science Foundation of China (Grant Nos. 41606092 & 41676156)
文摘We studied the effects of expected end-of-the-century p CO_2(1000 ppm)on the photosynthetic performance of a coastal marine cyanobacterium Synechococcus sp.PCC7002 during the lag,exponential,and stationary growth phases.Elevated p CO_2significantly stimulated growth,and enhanced the maximum cell density during the stationary phase.Under ambient p CO_2conditions,the lag phase lasted for 6 days,while elevated p CO_2shortened the lag phase to two days and extended the exponential phase by four days.The elevated p CO_2increased photosynthesis levels during the lag and exponential phases,but reduced them during the stationary phase.Moreover,the elevated p CO_2reduced the saturated growth light(Ik)and increased the light utilization efficiency(α)during the exponential and stationary phases,and elevated the phycobilisome:chlorophyll a(Chl a)ratio.Furthermore,the elevated p CO_2reduced the particulate organic carbon(POC):Chl a and particulate organic nitrogen(PON):Chl a ratios during the lag and stationary phases,but enhanced them during the exponential phase.Overall,Synechococcus showed differential physiological responses to elevated p CO_2during different growth phases,thus providing insight into previous studies that focused on only the exponential phase,which may have biased the results relative to the effects of elevated p CO_2in ecology or aquaculture.