REPORT ON PONTONIINE SHRIMPS（CRUSTACEA：DECAPODA）COLLECTED BY JOINT CHINESE—GERMAN MARINE BIOLOGY EXPEDITIONS TO HAINAN ISLAND,SOUTH CHINA SEA i.ANCHISTUS,CONCHODYTES,CORALLIOCARIS     

李新正  刘瑞玉 《中国海洋湖沼学报》2002,20(4):371-377

The present paper reports 7 species of pontoniine shrimps collected from Hainan Island,South China Sea,by the Joint Chinese-German Marine Biology Expeditions,in which,Conchodytes nipponensis(De Haan,1844)and Coralliocaris brevirostris Borradaile,1898 are new records from Chinese waters.  相似文献   

苏拉威西岛北部左旋走滑与俯冲后撤的动力学分析     

张健  董淼  姜程浩  方桂  褚伟  何雨蓓 《地质学报》2023,97(1):1-15

苏拉威西岛北部属于马鲁古海板块,其主体是北苏拉威西海沟俯冲带与帕卢-科洛左旋走滑断裂所围限的岛北支和岛东支。大约5 Ma前,苏拉群岛沿Sorong断层与苏拉威西岛东支碰撞,导致北苏拉威西海沟俯冲后撤,引起了岛北支顺时针旋转约20°～25°,同时,西侧的帕卢-科洛断层发生了约4 cm/a的左旋走滑。本文利用综合地球物理方法,计算了该区三维温度、速度、黏性特征,认为：苏拉威西岛北部在左旋走滑、俯冲后撤过程中,地壳以脆性变形为主,但由于北苏拉威西海沟俯冲带在地壳内形成南向倾斜的软弱层,Moho面和地形“镜像”区域内形成脆、韧变形共存的组合。地幔变形为韧性变形,深度约100 km的上地幔低速流变层是地幔韧性变形的主控层位。在周边板块边界不断移动的动力学背景中,苏拉威西岛北部在地壳尺度以收缩-伸展变形为主,在岩石圈尺度以旋转变形为主。  相似文献   

Spatial scale variability in shoot density and epiphytic leaves of Posidonia oceanica on Kerkennah Island (Tunisia) in relation to current tide effects          下载免费PDF全文

Mounir Ben Brahim  Lotfi Mabrouk  Asma Hamza  Mabrouka Mahfoudhi  Abderahmen Bouain  Lotfi Aleya 《Marine Ecology》2015,36(4):1311-1331

A study was undertaken of the patterns of spatial variability, epiphytic biomass and distribution of epiphytic fauna and flora of Posidonia oceanica. Samples were taken at four stations located approximately 4 km apart, exposed to different current conditions. Stations A and B, situated near the Oued Mimoun tidal channel with its relatively strong bi‐directional flows, were affected by high current tide. The other two stations, North Oued Mimoun (L1) and South Oued Mimoun (L2), were located further from the channel, in low current tide conditions. Sampling was conducted in the Attaya area of Kerkennah Island (Tunisia) in August 2009 at depths between 2 and 3 m, with the results indicating differences among the stations. Shoot density decreased when exposed to high levels of hydrodynamic activity generated by current tides whereas the epiphytic biomass of P. oceanica leaves decreased at sheltered stations located far from the channel. Epiphytic algae such as Heterokontophyta, Rhodophyta and Chlorophyta, and epiphytic fauna represented by Bryozoa, Hydrozoa, Annelida, Porifera and Tunicata, dominated the epiphytic assemblages and were abundant at the station most exposed to high current tide hydrodynamics. Cyanobacteria, however, were dominant in stations exposed to low current tide.  相似文献   

A preliminary study of freshwater meiofaunal communities at Greenwich Island,South Shetland Islands,Antarctica     

Soraya J. Silva  Minerva Cordovés  Nory González  Leinny González 《极地研究(英文版)》2015,(1)

Meiofaunal communities of three small, shallow freshwater habitats sampled during the austral summer of 2013 in Greenwich Island, South Shetland Islands, Antarctica, are reported. Communities are domin...  相似文献   

影响海南岛的台风降水及水汽输送源地分析     

罗婷  王远清  李丽平 《气象与环境学报》2020,36(6):42-49

利用1986—2016年中国气象局台风最佳路径资料、海南岛区域站降水数据以及基于拉格朗日方法的轨迹模式对近30 a影响海南岛的台风降水和大气环流特征进行分析,并探讨了台风影响降水期间水汽输送通道和源地。结果表明：6—10月是台风影响海南岛的主要时段,也是台风降水主要时段。在台风降水偏多(少)年,长江以南地区冷空气影响偏弱(强),副热带高压偏弱(强),南支槽偏强(弱),低层水汽通量场呈现异常气旋性(反气旋性)环流。降水偏多年,海南岛受到来自西北太平洋异常东北气流与印度洋、孟加拉湾的异常偏强西南气流影响;降水偏少年,水汽主要来自西太平洋的偏东气流和南海较弱的西南气流。海南岛台风降水的四个主要水汽源地分别为西太平洋、孟加拉湾、南海和印度洋,在台风降水偏多年,水汽输送贡献最大的是西太平洋和孟加拉湾,分别为33%和30%,来自东西两路的水汽供应充足,而在偏少年西太平洋水汽输送贡献最大,为38%,其余水汽源地贡献均在30%以下,以110°E以东的水汽输送为主。  相似文献   

海南岛冬季暴雨的时空分布及大尺度环流场特征分析          下载免费PDF全文

曾敏  王咏青  冯文 《气象科学》2023,43(5):589-599

利用海南岛气象观测站逐日降水整编资料和欧洲中期天气预报中心（European Centre for Medium-Range Weather Forecasts，ECMWF） ERA5再分析资料，分析了1991—2020年海南岛冬季暴雨的时空分布及环流特征。结果表明：海南岛冬季暴雨在月际分布（12月—次年2月）上存在较大差异性，降雨量级越大，差异越明显；在空间分布上也存在显著的地域性，东部地区发生频次最高，总体上呈现东多西少的分布特征。海南岛冬季暴雨的水汽输送主要以偏东方向为主，气流来自副高南侧的偏东气流和大陆冷高压东南侧的东北气流。海南岛冬季暴雨发生期间，相对气候平均态而言，偏东低空急流较为强劲，中南半岛南支槽形态明显，副高偏北偏西偏强，南亚高压西北向的出流偏强，且南海海域存在显著的海温正距平。  相似文献   

居民对海岛旅游影响感知的实证研究     

陈金华 《广东海洋大学学报》2007,27(5):20-25

采用实地考察、问卷调查与访谈的方法对我国旅游型海岛东山岛进行调查发现,当地居民对旅游影响的正面感知较强,突出表现在旅游经济影响方面,反映了当地旅游业发展处于起步阶段;居民对旅游的负面影响感知较弱,反映了当地经济转型时期居民对旅游业的期望较高;居民人口统计学的差异对旅游影响感知总体差异不大,但在某些方面存在一定差异。  相似文献   

First cosmogenic 10Be constraints on LGM glaciation on New Zealand's North Island: Park Valley,Tararua Range     

Martin S. Brook  James Shulmeister  Tyne V. H. Crow  Albert Zondervan 《第四纪科学杂志》2008,23(8):707-712

We report the first direct ages for late Quaternary glaciation on the North Island of New Zealand. Mt Ruapehu, the volcanic massif in the North Island's centre, is currently glaciated and probably sustained glaciers throughout the late Quaternary, yet no numeric ages have been reported for glacial advances anywhere on the North Island. Here, we describe cosmogenic ¹⁰Be ages of the surface layers of a glacially transported boulder and glacially polished bedrock from the Tararua Range, part of the axial ranges of the North Island. Results indicate that a limited valley glaciation occurred, culminating in recession at the end of the last glacial coldest period (LGCP, ca. 18 ka). This provides an initial age for deglaciation on the North Island during the last glacial–interglacial transition (LGIT). It appears that glaciation occurred in response to an equilibrium‐line altitude (ELA) lowering of ～1400 m below the present‐day mean summer freezing level. Ages for glaciation in the Tararua Range correspond closely to exposure ages for the last glacial maximum (LGM) from the lateral moraines of Cascade Valley in the South Island, and in Cobb Valley, in northern South Island. The corollary is that glaciation in the Tararua Range coincided with the phase of maximum cooling during MIS 2, prior to the Antarctic Cold Reversal (ACR), during the LGCP. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献   

Report of Pontoniinae Shrimps (Crustacea: Decapoda) Collected by Joint Chinese-German Marine Biology Expeditions to Hainan Island, South China Sea. Ⅲ. Periclimenes     

李新正  刘瑞玉 《中国海洋湖沼学报》2004,(1)

1　INTRODUCTIONInthefirstandsecondpapersofthisseries (LietLiu ,2 0 0 2 ,2 0 0 3) ,wereported 9genera 1 6speciesofPontoniinae ,collectedbytheJointChinese GermanMa rineBiologyExpeditionstoHainanIsland (winterof1 990andspringof 1 992 ) .ThepresentpaperreportsonthespeciesofgenusPericlimenesfromHainanIslandcollectedbytheexpedition.ThematerialsstudiedherearealldepositedintheInstituteofOceanology ,ChineseAcademyofSciences,Qingdao,China (IOCAS) .Inthispaper,“Materialexamined”and“RN…  相似文献   

The deglaciation of Clyde Inlet,northeastern Baffin Island,Arctic Canada     

Jason P. Briner  Irina Overeem  Gifford Miller  Robert Finkel 《第四纪科学杂志》2007,22(3):223-232

The behaviour of ice sheets as they retreated from their Last Glacial Maximum (LGM) positions provides insights into Lateglacial and early Holocene ice‐sheet dynamics and climate change. The pattern of deglaciation of the Laurentide Ice Sheet (LIS) in arctic fiord landscapes can now be well dated using cosmogenic exposure dating. We use cosmogenic exposure and radiocarbon ages to constrain the deglaciation history of Clyde Inlet, a 120 km long fiord on northeastern Baffin Island. The LIS reached the continental shelf during the LGM, retreated from the coastal lowlands by 12.5 ± 0.7 ka (n = 3), and from the fiord mouth by 11.7 ± 2.2 ka (n = 4). Rapid retreat from the outer fiord occurred 10.3 ± 1.3 ka (n = 6), with the terminus reaching the inner fiord shortly after 9.4 ka (n = 2), where several moraine systems were deposited between ca. 9.4 and ca. 8.4 ka. These moraines represent fluctuations of the LIS during the warmest summers since the last interglaciation, and this suggests that the ice sheet was responding to increased snowfall. Before retreating from the head of Clyde Inlet, the LIS margin fluctuated at least twice between ca. 7.9 and ca. 8.5 ka, possibly in response to the 8.2 ka cold event. Copyright © 2006 John Wiley & Sons, Ltd.  相似文献