黑龙江省东部中侏罗世至早白垩世沟鞭藻组合序列   总被引：5，自引：0，他引：5  

祝幼华  何承全 《地层学杂志》2003,27(4):282-288,T001

对近二十年来黑龙江省东部海相侏罗纪—白垩纪沟鞭藻地层资料进行了综合研究 ,首次为该地区建立起侏罗纪—白垩纪沟鞭藻地层序列 ,主要包含 7个组合带 (含 3个高峰带 ) ,其中绥滨地区 Callovian— Valanginian期有 4个带 ;鸡西盆地早白垩世也有 4个带 (其中包括与绥滨地区早白垩世早期同时异相的一个 )。它们自下而上为 :1)绥滨组的 Pareodinia ceratophora- N annoceratopsispellucida组合带 ;　 2 )东荣组下部的 Gonyaulacysta jurassica组合带 (高峰带 ) ;　 3)东荣组上部的 Amphorula delicata组合带 ;　 4 )东荣组最上部的海相 Oligosphaeridium pul-cherrimum组合带 (高峰带 )或鸡西盆地滴道组的微咸水—半咸水的 Vesperopsis didaoensis- L agenorhytis granoru-gosa组合带 ,两者为同时异相关系 ;　 5 )城子河组下部海相层的 Odontochitina operculata- Muderongia tetracantha组合带 (该带可进一步划分出 2个亚组合带 ) ;　 6 )城子河组上部海相层的 Canningia reticulata组合带 ;　 7)穆棱组下段的 Cribroperidinium ?parorthoceras组合带 (高峰带 )。  相似文献   

Co-monitoring bacterial and dinoflagellates communities by denaturing gradient gel electrophoresis(DGGE) and SSU rRNA sequencing during a dinoflagellates bloom     

KAN Jinjun  CHEN Feng 《海洋学报(英文版)》2004,23(3):483-492

Dinoflagellates are unicellular eukaryotic protists that dominate in all coastal waters, and are also present in oceanic waters. Despite the central importance of dinoflagellates in global primary production, the relationship between dinoflagellates and bacteria are still poorly understood. In order to understand the ecological interaction between bacterial and dinoflageUates communities, denaturing gradient gel electrophoresis (DGGE) and SSU rRNA sequencing were applied to monitoring the population dynamics of bacteria and dinoflagellates from the onset to disappearance of a dinoflagellates bloom occurred in Baltimore Inner Harbor, from April 15 to 24, 2002. Although Prorocentrum minimum was the major bloom forming species under the light microscopy, DGGE method with dinoflagellate specific primers demonstrated that Prorocentrum micans, Gymnodinium galatheanum and Gyrodinium uncatenum were also present during the bloom. Population shifts among the minor dinoflagellate groups were observed. DGGE of PCR-amplified 16S rRNA gene fragments indicated that cyanobacteria, α, β, γ-proteobacteria, FlavobacteriumBacteroides-Cytophaga (FBC), and Planctomcetes were the major components of bacterial assemblages during the bloom. DGGE analysis showed that Cytophagales and α-proteobacteria played important roles at different stages of dinoflagellates bloom. DGGE can be used as a rapid tool to simultaneously monitor population dynamics of both bacterial and dinoflagellates communities in aquatic environments, which is demonstrated here.  相似文献   

Ocean urea fertilization for carbon credits poses high ecological risks     

Glibert PM  Azanza R  Burford M  Furuya K  Abal E  Al-Azri A  Al-Yamani F  Andersen P  Anderson DM  Beardall J  Berg GM  Brand L  Bronk D  Brookes J  Burkholder JM  Cembella A  Cochlan WP  Collier JL  Collos Y  Diaz R  Doblin M  Drennen T  Dyhrman S  Fukuyo Y  Furnas M  Galloway J  Granéli E  Ha DV  Hallegraeff G  Harrison J  Harrison PJ  Heil CA  Heimann K  Howarth R  Jauzein C  Kana AA  Kana TM  Kim H  Kudela R  Legrand C  Mallin M  Mulholland M  Murray S  O'Neil J  Pitcher G  Qi Y  Rabalais N  Raine R  Seitzinger S  Salomon PS  Solomon C 《Marine pollution bulletin》2008,56(6):1049-1056

The proposed plan for enrichment of the Sulu Sea, Philippines, a region of rich marine biodiversity, with thousands of tonnes of urea in order to stimulate algal blooms and sequester carbon is flawed for multiple reasons. Urea is preferentially used as a nitrogen source by some cyanobacteria and dinoflagellates, many of which are neutrally or positively buoyant. Biological pumps to the deep sea are classically leaky, and the inefficient burial of new biomass makes the estimation of a net loss of carbon from the atmosphere questionable at best. The potential for growth of toxic dinoflagellates is also high, as many grow well on urea and some even increase their toxicity when grown on urea. Many toxic dinoflagellates form cysts which can settle to the sediment and germinate in subsequent years, forming new blooms even without further fertilization. If large-scale blooms do occur, it is likely that they will contribute to hypoxia in the bottom waters upon decomposition. Lastly, urea production requires fossil fuel usage, further limiting the potential for net carbon sequestration. The environmental and economic impacts are potentially great and need to be rigorously assessed.  相似文献   

早中新世沟鞭藻模特地理区系   总被引：1，自引：0，他引：1  

茅绍智  黄奇瑜 《现代地质》2000,14(3):273-280

对早中新世的沟鞭藻植物地理作了初步研究,提出北半球在当时可划争为３以鞭藻地理区,即热带区、亚热带－温带区和北方区。热带区以典型的热带、亚热带种Ｐｏｌｙｓｐｈａｅｒｉｄｉｕｍｚｏｈａｒｙｉ丰富并存在偏胺热带、亚热带的种Ｔｕｂｅｒ ｃｅｕｌｌｄｉｎｉｕｍｄｉｎｉｕｍ ｖａｎｃａｍｐｏａｅ为特征,亚热带一温带区以同时存在Ｔｕｂｅｒｃｕｌｏｄｉｎｉｕｍｄｉｍｉｕｍ ｖａｎｃａｍｐｏａｅ和温带种Ｂｉｔｅｃｔ  相似文献   

早中新世沟鞭藻植物地理区系     

茅绍智  黄奇瑜  雷作淇 《现代地质》2000,14(3)

对早中新世的沟鞭藻植物地理作了初步研究 ,提出北半球在当时可划分为 3个沟鞭藻地理区 ,即热带区、亚热带—温带区和北方区。热带区以典型的热带、亚热带种 Polysphaeridiumzoharyi丰富并存在偏爱热带、亚热带的种 Tuberculodiniumdinium vancampoae为特征 ,亚热带—温带区以同时存在 Tuberculodiniumdinium vancampoae和温带种 Bitectatodinium tepikiense,但缺失 Polysphaeridium zoharyi为特征 ,而北方区则以缺失 Polysphaeridium zoharyi和 Tuberculo-diniumdinium vancampoae二者且组合较贫乏为特征 ,亚热带—温带区的北界大致位于现今 68°N一线 ,此界线可随气温升高而北推 ,例如最温暖的早中新世晚期 ( 1 7～ 1 4 .5Ma)此界线可达 70°N。该带南界大致位于现今 4 5°N处 ,随着气候的转暖可能会变得模糊不清。北方区的海水此时凉而不结冰 ,即此时北极不存在冰盖。本文研究证实了前人根据大植物化石所得出的结论。  相似文献   

快速光响应曲线的优化及在底栖甲藻光适应特性研究中的应用     

黄凯旋  陈亨  徐帅帅  刘莎莎  吕颂辉 《海洋科学》2020,44(1):106-112

利用快速光响应曲线(RLCs)技术研究了不同光背景下的底栖甲藻Cooliatropicalis的光合作用特性,比较了RLCs的不同序列(正序、反序和非序)和不同光照时间(10, 30和60 s)对光合参数的影响。结果表明:正序RLCs由于序列内非光化学淬灭(NPQ)的快速累积,造成曲线的不饱以及光合参数最大相对电子传递速率(rETRmax)和半饱和光强(Ek)的高估。反序和非序RLCs均出现光饱和或光抑制,步长30s和60s的光合参数在不同光背景下的趋势基本一致。在底栖甲藻的光合生理研究中,可考虑采用步长30 s的反序RLCs进行测定。  相似文献   

Phytoplankton variation and its relation to nutrients and allochthonous organic matter in a coastal lagoon on the Gulf of Mexico     

Jos A. Ak-Castillo  Gabriela Vzquez 《Estuarine, Coastal and Shelf Science》2008,78(4):705-714

In tropical and subtropical zones, coastal lagoons are surrounded by mangrove communities which are a source of high quantity organic matter that enters the aquatic system through litter fall. This organic matter decomposes, becoming a source of nutrients and other substances such as tannins, fulvic acids and humic acids that may affect the composition and productivity of phytoplankton communities. Sontecomapan is a coastal lagoon located in the southern Gulf of Mexico, which receives abundant litter fall from mangrove. To study the phytoplankton composition and its variation in this lagoon from October 2002 to October 2003, we evaluated the concentrations of dissolved folin phenol active substances (FPAS) as a measure of plant organic matter, salinity, temperature, pH, O₂, N-NH₄⁺, N-NO₃⁻, P-PO₄³⁻, Si-SiO₂, and phytoplanktonic cell density in different mangrove influence zones including the three main rivers that feed the lagoon. Nutrients concentrations depended on freshwater from rivers, however these varied seasonally. Concentrations of P-PO₄³⁻, N-NH₄⁺ and FPAS were the highest in the dry season, when maximum mangrove litter fall is reported. Variation of these nutrients seemed to depend on the internal biogeochemical processes of the lagoon. Blooms of diatoms (Skeletonema spp., Cyclotella spp. and Chaetoceros holsaticus) and dinoflagellates (Peridinium aff. quinquecorne, Prorocentrum cordatum) occurred seasonally and in the different mangrove influence zones. The high cell densities in these zones and the occurrence of certain species and its ordination along gradient of FPAS in a canonical correspondence analysis, suggest that plant organic matter (i.e. mangrove influence) may contribute to phytoplankton dynamics in Sontecomapan lagoon.  相似文献   

Determining spatial changes in the diet of nearshore suspension-feeders along the South African coastline: Stable isotope and fatty acid signatures     

E. Louise Allan  Shan T. AmbroseNicole B. Richoux  P. William Froneman 《Estuarine, Coastal and Shelf Science》2010

Mesoscale oceanographic features, such as upwellings, are known to play an important role in regulating the structure and productivity of nearshore marine communities. Stable isotope (δ¹³C and δ¹⁵N) and fatty acid analyses were employed to assess the influence of an upwelling cell along the south-eastern coastline of southern Africa on the diet of the mussel, Perna perna. Eight sites were sampled: two upstream, three in the vicinity and three downstream of the upwelling cell. Stable isotope and fatty acid signatures indicated that the mussels consumed a diet of detritus derived mainly from macroalgae, diatoms and dinoflagellates. One-way ANOVA on the δ¹³C and δ¹⁵N signatures and the principal component analysis of the fatty acid profiles of the mussels identified distinct groups corresponding to the above mentioned regions. The proportion of diatom biomarkers in the fatty acid profiles decreased downstream of the upwelling region while the proportion of dinoflagellate biomarkers increased. Upwelling regions are typically associated with elevated levels of productivity; however, these systems usually become silicon depleted and result in the replacement of diatoms with dinoflagellates. The highest proportions of the dinoflagellate markers were recorded in the two furthest sites downstream of the upwelling cell. The spatial variation in the diet of the mussels, therefore, appears to reflect the presence of the upwelling cell in the nearshore biology of the region.  相似文献   

两种甲藻和两种硅藻脂肪酸组成的比较研究   总被引：3，自引：0，他引：3  

刘梦坛  李超伦  孙松 《海洋科学》2010,34(10):77-82

研究了4种海洋微藻的脂肪酸组成。研究结果显示,锥状斯氏藻(Scrippsiella trochoidea)和海洋原甲藻(Prorocentrum micans)的主要脂肪酸有16:0、18:4ω3、18:5ω3、20:3ω6、22:6ω3,中肋骨条藻(Skeletonema costatum)和角毛藻(Chaetoceros sp.)的主要脂肪酸为14:0、16:0、16:1ω7、20:5ω3。两种甲藻和两种硅藻分别都表现出典型的甲藻门和硅藻门的脂肪酸特征。从总脂肪酸、PUFA、ω3和ω6脂肪酸的含量来看,单位干质量的两种甲藻能够比两种硅藻提供更多的脂肪酸类营养物质。但是某些动物生长发育所必需的脂肪酸(如20:5ω3)在硅藻中的含量却高于甲藻。因此实际应用中单种饵料往往不能提供足够的营养物质,通常需要将不同饵料混合以获得营养价值更高的饵料。对4种微藻的脂肪酸组成进行聚类分析和主成分分析,结果不仅反映了4种微藻在分类上亲缘关系的远近,也反映了几种微藻各自的脂肪酸组成特征。  相似文献   

Spatio-temporal variation in density of microphytoplankton genera in two tropical coral reefs of Mauritius     

《African Journal of Marine Science》2013,35(4):423-438

Spatial and temporal (seasonal and interannual) variation in microphytoplankton was investigated at two tropical coral reef sites off Mauritius (Belle Mare [BM] and Flic-en-Flac [FEF]), from 2010 to 2012. Each site was divided into three zones: coast, lagoon and reef. Microphytoplankton, nutrient and chlorophyll a samples were collected, and physico-chemical parameters were measured in situ. A total of 56 microphytoplankton genera were identified (43 diatoms, 8 dinoflagellates and 5 cyanobacteria). Total microphytoplankton density exhibited spatial and temporal variation, being higher at BM and near the coast, and mostly high in summer. Nutrient concentrations were highest near the coast as a result of run-off events and anthropogenic inputs, especially during heavy rainfall, and this resulted in elevated total microphytoplankton density. There were no clear diversity patterns at the two sites or within the different zones. At both sites, Navicula, Cocconeis and Fragilaria were the dominant diatoms, and Gymnodinium, Alexandrium and Protoperidinium were the dominant dinoflagellates. There was a shift in dominance from Navicula in summer to Fragilaria in winter. This seasonal shift may reflect how these species respond differently to environmental change, which could have implications for primary production at spatial and temporal scales.  相似文献