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根据1986~1987年逐月调查和1987年以来结合教学实习采集的朱家尖海滨底栖无脊椎动物资料,并参考前人对该岛的调查,叙述了朱家尖岛海滨底栖无脊椎动物10门257种,分析了生活潮区、栖息底质等,提出了该岛潮间带生物资源保护的建议。 相似文献
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Yonghua Wu Xuefa Shi Jianjun Zou Zhenbo Cheng Kunshan Wang Shulan Ge Fengdeng Shi 《科学通报(英文版)》2014,59(24):3066-3074
A total of six d13C minimum events,i.e.,VI,V,IV,III,II,and I,were observed via a stable carbon and oxygen isotope analysis of infaunal benthic foraminifera Uvigerina spp.in gravity core OS03-1 in the southeastern Okhotsk Sea over the last 180 ka.These events occurred at112–109,102–90,85–76,57–54,44–40,and 17–10 ka BP.The largest negative excursions reached 2.5%in event V and were greater than 1%in the other events.We proposed that all d13C minimum events were caused by the increase in sea surface water productivity,the weakened formation of Okhotsk Sea intermediate water,and the enhancement of the oxygen minimum zone.The negative excursions were unaffected by methane hydrate destabilization and subsequent methane release based on the results obtained by using archaeal lipid markers. 相似文献
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A Bayesian approach to seafloor classification using multi-beam echo-sounder backscatter data 总被引:2,自引:0,他引:2
Dick G. Simons 《Applied Acoustics》2009,70(10):1258-520
Seafloor classification using acoustic remote sensing techniques is an attractive approach due to its high-coverage capabilities and limited costs. The multi-beam echo-sounder (MBES) system provides high-resolution bathymetry and backscatter information with 100% coverage. In this paper, we present a seafloor classification method that employs the MBES backscatter data. The method uses the averaged backscatter data per beam. It, therefore, is independent on the quality of the MBES calibration. Also, its performance is insensitive to seafloor type variation along the MBES swathe and corrections for the angular dependence of the backscatter are not needed. The method accounts for the ping-to-ping variability of the backscatter intensity. It estimates both the number of seafloor types present in the survey area and the probability density function for the backscatter strength at a certain angle for each of the seafloor types. Application of the method to MBES backscatter data acquired in a well-known test area in the North Sea shows very good agreement with available ground truth. The method’s discriminatory performance for this area is demonstrated to be comparable to that of taking samples of the sediment. All seafloor types known to be present in the area are resolved for. Application of the method to the Stanton bank data set shows clearly separable areas that differ in seafloor composition. 相似文献
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Research on the disappearance causes of the Tenghualuo Site in Lianyungang,Jiangsu Province, China 总被引:2,自引:0,他引:2
《科学通报(英文版)》2008,(Z1):161-176
With brilliant civilization during the transitional period from a original clan society to a state society in prehistory,the Neolithic Tenghualuo Site in Lianyungang was discovered by archaeological survey in 1989,which was titled as‘one of the nation’s ten great archeological discoveries in 2000’.However,the transgression and the anthropogenic environment deterioration have ever been employed to explain the abandonment of the site.Based on a dynasty framework established by the 14 C dating,and using the experimental methods such as micro-paleontology identification in foraminifera and charophytes, the content test of Rb and Sr,susceptibility analysis as well as granularity and sedimentary facies analysis,some researches on the sediments from the two exploration layers at Tenghualuo Site were conducted,and the following new findings have been gained:Firstly,foraminifera which are relevant to the marine environment were not found in the sediment layer,however,25 charales,which usually live in the freshwater environment,in 07LTT1 exploration samples were found.Among them,3 charales were found in the samples from the forth sediment layer below the late Longshan Cultural layer and 22 charates were from the second sediment layer above the late Longshan Cultural layer.Furthermore,5 plant seeds and 41 fungal spores,together with many carbonation holes,plant seed shells,as well as their roots and stems were also found in the second sediment layer above the late Longshan Cultural layer.Secondly,the cumulative probability curves of the sediments’granularity in both the last and its overlying culture intermittent layers have characteristics of three-phase river sediment curve,and the ratios between Rb and Sr are both quite high in samples from two layers sedimented during the disappearing time of the site.All above-mentioned evidences indicate that disappearance of the Tenghualuo Site was not related to the transgression.The late Longshan Culture of the site could be completely abandoned after a relatively long-ter 相似文献
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系统分析北海外沙泻湖CK10钻孔岩芯的硅藻、有孔虫、介形虫化石, 并进行14C年代测定, 探讨硅藻、有孔虫组合特征、沉积相演化和地层年代。该孔全新世地层硅藻化石群自下而上划分为: Ⅰ. 波缘曲壳藻(Athnanthescrenulata)—亲缘桥弯藻(Cym bella affinis) —披针桥弯藻(Cym . lanceolata) ,Ⅱ.亲缘桥弯藻—波缘曲壳藻—卵形菱形藻(Nitzschia cocconeiformis) , Ⅲ. 亲缘桥弯藻—波缘曲壳藻—史密斯双壁藻(Diploneissm ithii),Ⅳ. 波缘曲壳藻—亲缘桥弯藻—条纹小环藻(Cyclotella striata), Ⅴ.卵形菱形藻—具槽直链藻(Melosira sulata)—柱状小环藻(Cyc. stytorum ), Ⅵ.条纹小环藻—柱状小环藻, Ⅶ. 具槽直链藻—条纹小环藻—卵形菱形藻, Ⅷ. 柱状小环藻等8 个硅藻组合带。有孔虫群自下而上划分为: Ⅰ. 毕克卷转虫变种(Am m onia beccarii var.) —瘦瘪雅得虫(Jadam mina m acrescens) , Ⅱ. 毕克卷转虫变种—异地希望虫(Elphidium advenum )—球室 相似文献
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分别采用不同的地层学方法对西藏贡扎地区的两条相邻上白垩统剖面进行了年代地层划分.根据将建立在贡扎Ⅰ上白垩统剖面上的锶同位素演化曲线与W. H .Burke等的同时代锶同位素演化曲线对比,剖面上岗巴村口组顶界年龄值约为81.4 Ma;根据在贡扎Ⅱ剖面上划分出的12个浮游有孔虫化石带确定的岗巴村口组顶界年龄值约为67.0 Ma.作者认为岗巴村口组顶界年龄值存在明显差别是受诸多因素影响,在对地层进行年代地层研究中,要不断提高各种地层学方法的分辨率,并尽可能采用综合的地层学方法. 相似文献
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Discovery of Late Cretaceous foraminifera in the Songliao Basin: Evidence from SK-1 and implications for identifying seawater incursions 总被引:3,自引:0,他引:3
DangPeng Xi XiaoQiao Wan ZhiQiang Feng Shun Li ZiHui Feng JianZhong Jia Xia Jing WeiMin Si 《科学通报(英文版)》2011,56(3):253-256
The Songliao Basin is the largest oil-bearing basin in China.In the absence of sufficient evidence,the possibility of seawater incursion(s) into the Songliao Basin remains controversial.Recently,we discovered relatively abundant foraminifera fossils from units 1 and 2 of the Nenjiang Formation of borehole SK-1.Benthic foraminifera (Gavlinella sp.,Anomalinoides sp.,Pullenia sp.,Haplophragmoides sp.,Karrorulina hokkaidoana,Clavulinoides sp.),as well as planktonic foraminifera (Archaeoglobigerina blowi,Archaeoglobigerina cretacea and Hedbergella flandrini),were identified.These fossils were widely distributed in the marine Cretaceous.According to the global distribution of the above-mentioned planktonic foraminifera,the age of these fossil bearing strata appears to be Late Coniacian to Santonian.More importantly,these foraminifera provide direct evidence for marine water incursions into the Songliao Basin during deposition of the Lower Nenjiang Formation. 相似文献