排序方式： 共有51条查询结果，搜索用时 31 毫秒
31.
蜑螺科 Neritidae 蜑螺属 Nerita 的一些种类形态近似, 形态鉴定上存在种类混淆、同物异名或错误鉴定等现象。作者在整理中国科学院南海海洋生物标本馆和中国科学院海洋生物标本馆历年来采集的蜑螺科标本时, 对4种隶属于蜑螺属的易混淆种进行了比较研究。通过对标本的反复对比, 分别找出了它们之间外部形态、地理分布以及生活习性方面的差异, 澄清了混淆, 确立了其分类地位: 1) 矮狮蜑螺Nerita chamaeleon Linnaeus, 1758和圆蜑螺Nerita histrio Linnaeus, 1758两者贝壳形态相近, 在我国海区分布重叠, 存在混淆以及错误鉴定的现象, 根据螺旋部以及壳面雕刻可将它们区分开, 即前者壳面螺肋光滑, 后者螺肋粗糙, 而前者螺旋部较后者高; 2) 锦蜑螺 Nerita polita Linnaeus, 1758和杂色蜑螺 Nerita litterata Gmelin, 1791两个种常被混淆在一起, 都鉴定为锦蜑螺, 前者在我国见于台湾、海南岛和西沙群岛, 后者在我国见于台湾、福建、广东、广西和西沙群岛, 其中杂色蜑螺此前在我国仅见于台湾, 本文的报道进一步完善了该种的地理分布信息。 相似文献
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Longitudinal patterns of spring-intermonsoon phytoplankton biomass, species compositions and size structure in the Bay of Bengal 总被引：1，自引：0，他引：1
LI Gang KE Zhixin LIN Qiang NI Guangyan SHEN Pingping LIU Huaxue YIN Jianqiang LI Kaizhi HUANG Liangmin TAN Yehui 《海洋学报(英文版)》2012,31(2):121-128
Vertical distributions of phytoplankton biomass, compositions and size structure were investigated during the spring-intermonsoon (April 22 to 30) of 2010 along transact 10°N of the Bay of Bengal, northern Indian Ocean. Surface phytoplankton biomass (Chl a) was (0.065§0.009) μg/L, being greater than 80% of which was contributed by pico-phytoplankton (<3 μm). The Chl a concen- tration vertically increased to the maximal values at deep chlorophyll maximum (DCM) layer that shoaled eastwards from 75 to 40 m. The Chl a biomass at DCM layer generally varied between 0.2 and 0.4 μg/L, reaching the maximum of 0.56 μg/L with micro-phytoplankton cells (>20 μm) accounting for 58% and nano- (3-20 μm) or pico-cells for 15% and 27%, respectively. In particular, the cells concentration coupling well with phosphate level was observed at middle layer (75-100 m) of 87° to 89°E, dominated by micro-cells diatoms (e.g., Chaetoceros atlanticus v. neapolitana, Chaetoceros femur and Pseudonitzschia sp.) and cyanobacteria (i.e., Trichodesmium hildebrandtii), with the cells concentration reached as high as 4.0×104 and 4.3×104 cells/L. At the rest of the trans- act however, dino°agellates (e.g., Amphisdinium carterae and Prorocentrum sp.) were the dominant species, with the cells concentration varying from 0.3×103 to 6.8×103 cells/L. Our results also in- dicate that the regulation of large cells (micro-, nano-) on phytoplankton biomass merely occurred at DCM layer of the Bay. 相似文献
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不同围压下冻结黄土胶结行为的离散元分析 总被引：1，自引：1，他引：0
鉴于冻土中冰的胶结作用在冻土力学性质方面的重要作用,在三维离散元法中,采用黏结发生在有限范围内的模型来考虑冰的胶结作用,对不同围压下冻结黄土的胶结行为进行了数值研究。结果表明：数值模拟的应力-应变曲线与试验数据吻和较好;颗粒接触刚度、平行黏结刚度和强度均随着围压增大而线性增大,但摩擦系数随围压增大而减小;力链、位移和孔隙率与围压的响应关系呈现出统一性。同时,也分析了冰胶结作用影响下的冻土细观变化与宏观力学行为之间的响应关系。这对于促进离散元法在冻土领域内的应用具有积极的作用。 相似文献
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南海东北部浮游植物对氮、磷加富的响应及与不同水团的关系 总被引：3，自引：1，他引：2
2014年5月搭载"实验3"号科考船对南海东北部海区进行氮、磷营养盐现场加富培养实验。水团分析的结果表明,南海东北部海区的环境参数随着空间的变化大体可以分成3个区域:近岸海区、陆架海区和陆坡、海盆海区。加富培养过程中近岸海区和陆坡、海盆海区浮游植物未发生显著变化。陆架海区浮游植物出现显著增长,该海区浮游植物加富氮、磷以后在48h出现反应,同时添加氮、磷显著促进了浮游植物的生长。各培养站位均检测到大量束毛藻,加富培养后迅速减少。营养盐的添加改变了海区浮游植物原有的硅甲藻比例与各粒级叶绿素比例,陆架海区培养后的改变最为明显,同时添加氮磷培养72h后,由甲藻为主的优势种如卡氏前沟藻(Amphidinium carterae)、光亮鳍藻(Dinophysis argus)、原甲藻(Prorocentrumsp.)转变成了以硅藻为主如绕孢角毛藻(Chaetoceros cinctus)、旋链角毛藻(Chaetoceros curvisetus)、放射角毛藻(Chaetoceros radicans)和丹麦细柱藻(Leptocylindrus danicus)。同时,加富实验表明磷酸盐的添加促进了陆架海区微微型浮游植物聚球藻的生长。 相似文献
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Zhixin Ke Yehui Tan Liangmin Huang Chunyu Zhao Xin Jiang 《Marine pollution bulletin》2017,114(1):183-191
Stable isotopic signatures (δ13C and δ15N) and C/N ratios of suspended particulate organic matter (POM) were investigated from the surface water of Daya Bay during summer and winter of 2015. The relatively high δ13CPOM values suggested the input of 13C-depleted terrigenous organic matter was low in Daya Bay. There were significant correlations between δ13CPOM values and chlorophyll a concentrations both during summer and winter, suggesting the δ13CPOM values were mainly controlled by the phytoplankton biomass in the surface water. The distribution of δ15NPOM values was more complicated than that of δ13CPOM and displayed low values in the outer bay and the Dan'ao River estuary. 15N-depleted ammonia originating from industrial wastewater might have strongly influenced the water quality and stable isotopic signatures of POM near the Dan'ao River estuary. The δ13CPOM and δ15NPOM values strongly reflect the influences of anthropogenic activity and eutrophication in Daya Bay. 相似文献
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Journal of Oceanology and Limnology - Relatively few studies have investigated the community structure of zooplankton in the atolls of the central South China Sea. Zooplankton were sampled at nine... 相似文献
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Latitudinal changes (6°S-20°N) of summer ciliate abundance and species compositions in surface waters from the Java Sea to the South China Sea 总被引：1，自引：0，他引：1
Ciliates play a curial role in energy transfer from pico-and nano-phytoplankton to mesozooplankton in marine ecosystems. In order to visualize their geographical distributions from the Java Sea to the South China Sea (6°S to 20°N), the authors investigated the ciliate abundance and species composition in surface waters during May 18 to 27 of 2010. The ciliate abundance decreased latitudinally from 3 080 ind./L (～6°S) to 40 ind./L (～3°N), and then increased to 1 180 ind./L (～16°N) at the end of the survey. A total of 22 ciliates belonging to 15 genera were identified with the tintinnids accounted for 50% (11 species); and the species number showed a same spatial change as the ciliate abundance. Moreover, the Strombidium occupied over 50% of total ciliate abundance in most stations and Mesodinium and Tintinnopsis contributed to about 18.7% and 11.4%, respectively. In particular, our results indicate that the geographical changes in ciliate abundance were positively regulated by larger nano-and micro-phytoplankton biomass, rather than smaller pico-phytoplankton in the investigated waters. 相似文献
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Phytoplankton growth and microzooplankton grazing in the continental shelf area of northeastern South China Sea after Typhoon Fengshen 总被引：1，自引：0，他引：1
Linbin Zhou Yehui Tan Liangmin HuangJianrong Huang Huaxue LiuXiping Lian 《Continental Shelf Research》2011,31(16):1663-1671
Dilution experiments were used to investigate the phytoplankton growth and microzooplankton grazing in the continental shelf area of northeastern South China Sea during 30 June and 7 July, 2008, occurring about a week after Typhoon Fengshen. We detected negative phytoplankton growth rates (−0.03 to −2.02 d−1) and measured grazing rates of microzooplankton on phytoplankton in size-fractionations of 20-200 μm (1.25±0.44 d−1), 3-20 μm (1.48±0.63 d−1) and <3 μm (1.02±0.42 d−1). Results showed significant correlations between phytoplankton growth and microzooplankton grazing rates, between phytoplankton and ciliate abundance, and between the dominant phytoplankton Thalassionema nitzschioides and the dominant ciliate Helicostomella longa (p<0.05). Phytoplankton decay, due to nutrient-limited conditions occurring with the fading of upwelling and spreading of freshwater plume after Typhoon Fengshen, may account for negative phytoplankton growth rates in this study. Synergism in the specific size-selective grazing of various species, including ciliates and heterotrophic dinoflagellates, may contribute to similar grazing rate on phytoplankton in different size-fractionations, at the integrated level. Interactions between phytoplankton and microzooplankton, including grazing selectivity, top-down and bottom-up control between phytoplankton and microzooplankton may contribute to these findings. Our results indicate that under conditions of negative phytoplankton growth microzooplankton grazing may reduce energy loss from the epipelagic waters by retrieving energy from the decaying phytoplankton community. 相似文献