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1.
将南海北部花斑蛇鲻分成南海北部大陆架和北部湾两个不同海域群体，计算花斑蛇鲻的生长与死亡参数。得到的Von Bertalanffy生长方程的相关参数为：南海北部大陆架L∞=45．5cm，K=0．28，t0=-0．460；北部湾L∞=40．0cm，K=0．30，t0=-0．443。计算自然死亡系数得南海北部大陆架为0．63；北部湾为0．67；捕捞死亡系数南海北部大陆架为0．79，北部湾为1．11。据等渔获量曲线建议南海北部大陆架花斑蛇鲻开捕体长由13．3cm增加至20．0cm，同时，捕捞死亡系数可由当前的0．79放宽至1．0；北部湾花斑蛇鲻开捕体长由13．5cm增加至19．0cm的同时，捕捞死亡系数可由当前的1．11放宽至1．5。 相似文献
2.
根据1997年12月至1999年6月在南海北部进行的大规模底拖网渔业资源调查中8个航次4个季节的竹筴鱼(Trachurus japonicus)生物学测定资料,运用FAO开发的最新体长频率数据分析软件FiSATⅡ对竹筴鱼的生长、死亡参数进行估算,并进一步应用Beverton-Holt模式对南海北部竹筴鱼的最新资源状况进行研究.结果表明:(1) 竹筴鱼的叉长和体重的关系式为:W=2.282 8×10-5L2.915 4.(2) 其von Bertalanffy生长方程的各参数为:渐近叉长L∞=31.2 (cm),渐近体重W∞=426.5 (g),生长系数K=0.42,t0=-0.376.(3) 总死亡系数Z=2.15,自然死亡系数M=0.91,捕捞死亡系数F=1.24,开发率E=0.58.在估算结果的基础上,进一步提出南海北部竹筴鱼的最佳可捕规格为叉长14.8 cm. 相似文献
3.
黄梓荣 《广东海洋大学学报》2003,23(1):41-44
采用 4 0 4 ◇/2 0 0mm底拖网 ,在南海北部进行进行 2 0 0nmile专属经济区渔业资源调查 ,测量其渔获 11种经济鱼类的体长数据 ,统计其没达到最小可捕规格所占比例。结果表明 ,渔获中未达到最小可捕规格的幼鱼比例很大 ,北部湾 ,带鱼、短尾大眼鲷和白姑鱼四季平均未达到最小可捕规格的幼鱼超过 30 % ;海南岛以东 ,花斑蛇鲻、带鱼、短尾大眼鲷、长尾大眼鲷和白姑鱼未达到最小可捕规格的幼鱼超过 30 %。同时提出了改进措施 ,即保留该网型 ,放大网目尺寸或将放大后的囊网网目改为方形网目 ;淘汰该网型 ,改囊网网目为方形网目、网目尺寸符合国家标准的四片式拖网网型。 相似文献
4.
黄梓荣 《广东海洋大学学报》2002,22(6):26-31
根据实施休渔前 1997～ 1999年南海北部底拖网调查资料 ,以及实施休渔后 2 0 0 0～ 2 0 0 2年2 0 0nmile专属经济区渔业资源调查 (南海区 )最新资料 ,综合分析南海北部实施休渔前后多齿蛇鲻资源的变动趋势。结果表明 ,实施休渔后 ,海南岛以东和北部湾多齿蛇鲻渔获率分别提高了 5 7.75%和 84 .38% ,并呈现出自然的季节变化 ,渔获群体一龄鱼以下比例减少 ,一龄鱼以上比例增加。并讨论了资源养护的对策。 相似文献
5.
【目的】调查闽江口龙头鱼资源,估算其生物学参数。【方法】于2015年1月、5月、8月、11月在福建闽江口11个采样点(25.85°―26.29°N,119.65°―119.87°E)采集龙头鱼3 770尾,测量其体长、体质量,用Fi SATⅡ软件中的ELEFAN I方法,估算龙头鱼的生长、死亡参数及其开捕体长和单位补充量渔获量。【结果】闽江口渔场龙头鱼体长(L)体质量(m)关系为:m=0.000 7 L~(3.804 2) (R~2=0.961 1);龙头鱼Von Bertalanffy生长方程估算的生长参数K、L_∞、m_∞、t_0分别为0.52、28.7 cm、246.1 g和-0.317龄;由生长方程推算出龙头鱼的拐点年龄约为2.252龄,拐点体长约为21.2 cm,拐点体质量约为77.1 g;根据长度变换渔获曲线法估算龙头鱼的总死亡系数为1.67,由Pauly经验公式估算自然死亡系数为1.04,捕捞死亡系数为0.63,开发率为0.377;由动态综合模型估算出龙头鱼的开捕年龄为0.712龄,对应开捕体长为11.9 cm。【结论】闽江口龙头鱼资源处未过度开发状态。 相似文献
6.
黄梓荣 《广东海洋大学学报》2003,23(1):41-44
采用404^◇／200mm底拖网，在南海北部进行进行200n mile专属经济区渔业资源调查，油量其渔获11种经济鱼类的体长数据，统计其没达到最小可捕规格所占比例。结果表明，渔获中末达到最小可捕规格的幼鱼比例很大，北部湾，带鱼、短尾大眼鲷和白姑鱼四季平均末达到最小可捕规格的幼鱼超过30％；海南岛以东，花斑蛇鲻、带鱼、短尾大眼鲷、长尾大眼鲷和白姑鱼未达到最小可捕规格的幼鱼超过30％。同时提出了改进措施，即保留该网型，放大网目尺寸或将放大后的囊网网目改为方形网目；淘汰该网型，改囊网网目为方形网目、网目尺寸符合国家标准的四片式拖网网型。 相似文献
7.
北部湾二长棘鲷生长、死亡及其群体组成 总被引：6，自引：1，他引：5
利用2006年7月至2008年3月北部湾渔业商业捕捞底拖网和刺网渔获物中采集的样本,对北部湾二长棘鲷的生长、死亡及其群体组成进行了初步研究。结果表明,北部湾二长棘鲷优势体长70～140 mm,占82.2%;优势体重为20～60 g,占54.29%;ARSS分析表明雌雄生长不存在显著性差异(P>0.05),繁殖期性比为1.21∶1;von Bertalanffy生长方程的主要参数分别为:L∞=292.8 mm,K=0.167,t0=-1.116;体重的生长拐点为5.463龄;总死亡系数、自然死亡系数和捕捞死亡系数分别为1.041 4、0.282 8和0.752 6,当前开发率为0.728。 相似文献
8.
方目网囊对蓝圆鲹和多齿蛇鲻的选择性比较 总被引：1，自引：0，他引：1
为检测方目网囊对蓝圆鱼参和多齿蛇鲻的选择作用 ,2 0 0 0年 1 1～ 1 2月在南海北部海域试验了 4种目大的方目网囊。结果表明 ,方形网目网囊有利于释放纺缍形 (如蓝圆 鱼参)、圆形或近圆形 (如多齿蛇鲻 )两种形体鱼类的小、幼鱼 ,且对后者的释放效果更好。当网囊目大分别为 45、5 0mm时 ,蓝圆鱼参的5 0 %选择体长 (L0 .5)分别为 1 2 1 2 2、1 2 8 77mm ;当网囊目大分别为 40、45、5 0mm时 ,多齿蛇鲻的L0 5分别为 1 2 4 1 2、1 2 6 75、1 3 9 3 2mm。通过不同目大网囊对蓝圆鱼参、多齿蛇鲻选择性比较分析 ,发现 5 0mm目大方目网囊的选择效果好于 40、45mm目大的网囊 ,因此 ,在南海区拖网渔业中采用 5 0mm目大的方目网囊是必要的 ,同时建议将 1 5 0mm作为蓝圆鱼参、多齿蛇鲻的最小可捕叉长标准。 相似文献
9.
为检测方目网囊对蓝圆Shen和多齿蛇鲻的选择作用，2000年11－12月在南海北部海域试验了4种目大的方目网囊。结果表明，方形网目网囊有利于释放纺缍形（如蓝圆Shen），圆形或近圆形（如多齿蛇鲻）两种形体鱼类的小，幼鱼，且对后者的释放效果更好。当网囊目大分别为45，50mm时，蓝圆Shen的50％选择体长（L0．5）分别为121.22,128.77mm；当网囊目大分别为40，45，50mm时，多齿蛇鲻的L0．5分别为124.12,126.75,139.32mm。通过不同目大网囊对蓝圆Shen，多齿蛇鲻选择性比较分析，发现50mm目大方目网囊的选择效果效果优于40，45mm目大的网囊，因此，在南海区拖网渔业中采用50mm目大的方目网囊是必要的，同时建议将150mm作为蓝圆Shen，多齿蛇鲻的最小可捕叉长标准。 相似文献
10.
为检测方目网囊对蓝圆鱼参和多齿蛇鲻的选择作用,2000年11～12月在南海北部海域试验了4种目大的方目网囊.结果表明,方形网目网囊有利于释放纺缍形(如蓝圆鱼参)、圆形或近圆形(如多齿蛇鲻)两种形体鱼类的小、幼鱼,且对后者的释放效果更好.当网囊目大分别为45、50 mm时,蓝圆鱼参的50%选择体长(L0.5)分别为121.22、128.77 mm;当网囊目大分别为40、45、50 mm时,多齿蛇鲻的L0.5分别为124.12、126.75、139.32 mm.通过不同目大网囊对蓝圆鱼参、多齿蛇鲻选择性比较分析,发现50 mm目大方目网囊的选择效果好于40、45 mm目大的网囊,因此,在南海区拖网渔业中采用50 mm目大的方目网囊是必要的,同时建议将150 mm作为蓝圆鱼参、多齿蛇鲻的最小可捕叉长标准. 相似文献
11.
As one of the biggest marginal seas in the western Pacific margin, the South China Sea (SCS) experienced continental rifting and seafloor spreading during the Cenozoic. The northern continental margin of the SCS is classified as a passive continental margin. However, its depositional and structural evolution remains controversial, especially in the deep slope area. The lack of data hindered the correlation between continental shelf and oceanic basin, and prevented the establishment of sequence stratigraphic frame of the whole margin. The slope basins in the mid-northern margin of SCS developed in the Cenozoic; the sediments and basin infill recorded the geological history of the continental margin and the SCS spreading. Using multi-channel seismic dataset acquired in three survey cruises during 1987 to 2004, combined with the data of ODP Leg 184 core and industrial wells, we carried out the sequence stratigraphic division and correlation of the Cenozoic in the middle-northern margin of SCS with seismic profiles and sedimentary facies. We interpreted the seismic reflection properties including continuity, amplitude, frequency, reflection terminals, and 15 sequence boundaries of the Cenozoic in the study area, and correlated the well data in geological age. The depositional environment changed from river and lake, shallow bay to open-deep sea, in correspondence to tectonic events of syn-rifting, early drifting, and late drifting stages of basin evolution. 相似文献
12.
南海北部鱼类石油烃含量地理差异原因浅析 总被引：1，自引：0，他引：1
比较了南海北部海洋鱼类石油烃含量的地理差异,结果表明：被研究的5个海区中,广州湾海洋鱼类的石油烃含量明显高于北部湾（p＜0.05）和红海湾（P＜0．05）,该3个海区和珠江口明显高于台湾浅滩（p＜0.01）,其余的两两之间没有统计学差异（p＞0．05）。利用海洋环境质量调查和监测资料进行分析,说明这种地理分布特征与南海北部近岸海域的石油烃污染有直接关系。 相似文献
13.
Ma Hong 《中国海洋湖沼学报》1987,5(1):9-21
The nonwind-driven mechanism of the winter circulation in the northern South China Sea is discussed.
Linked by the Bashi Strait to the Pacific Ocean, the northern South Cnina Sea is treated as a part of the Pacific western
boundary where the circulation variation (except the very thin surface layer) is closely related to that of the ocean interior
and the effect of local wind might be neglected (at least for some seasons).
Based on the assumption that the thick and strong westward current which flows in through the Bashi Strait can effectively
prevent water exchange between the northern and southern South China Seas, the model sea only includes the northern part.
Barotropic numerical experiments show that part of this westward current is deflected by the continental slope and forms the
slope area NE current—the South China Sea Warm Current. Besides, the topographical flow fed by the extension of the western
boundary current and the anticyclonic eddy born near the eastern boundary are also fundamental components of the South China
Sea Warm Current. The reflection of the incident Rossby waves by the continental slope is found to be of significance in the
intensification of the South China Sea Warm Current.
Contribution No. 1362 from Institute of Oceanology, Academia 相似文献
14.
Diatom assemblages in surface sediments from the South China Sea as environmental indicators 总被引：1，自引：0，他引：1
We studied diatom distribution from 62 samples from the uppermost 1 cm of sediment in the South China Sea (SCS), using grabs or box corers in three cruises between 2001–2007. Fifty six genera, 256 species and their varieties were identified. Dominating species included Coscinodiscus africanus, Coscinodiscus nodulifer, Cyclotella stylorum, Hemidiscus cuneiformis, Melosira sulcata, Nitzschia marina, Roperia tesselata, Thalassionema nitzschioides, Thalassiosira excentrica, and Thalassiothrix longissima. Most surface sediments in the SCS were rich in diatoms, except for a few coarse samples. Average diatom abundance in the study area was 104 607 valve/g. In terms of the abundance, ecology, and spatial distribution, seven diatom zones (Zones 1–7) were recognized. Zone 1 (northern continental shelf) is affected by warm currents, SCS northern branch of the Kuroshio, and northern coastal currents; Zone 2 (northwestern continental shelf) is affected by intense coastal currents; Zone 3 (Xisha Islands sea area) is a bathyal environment with transitional water masses; Zone 4 (sea basin) is a bathyal-to-deep sea with stable and uniform central water masses in a semi-enclosed marginal sea; Zone 5 (Nansha Islands marine area) is a pelagic environment with relatively high surface temperature; Zone 6 (northern Sunda Shelf) is a tropical shelf environment; and Zone 7 (northern Kalimantan Island shelf area) is affected by warm waters from the Indian Ocean and coastal waters. The data indicate that these diatom zones are closely related to topography, hydrodynamics, temperature, nutrients and especially the salinity. Better understanding of the relationship between diatom distribution and the oceanographic factors would help in the reconstruction of the SCS in the past. 相似文献
15.
Using a Finite-Volume Community Ocean Model, we investigated the dynamic mechanism of the South China Sea Warm Current(SCSWC) in the northern South China Sea(NSCS) during winter monsoon relaxation. The model reproduces the mean surface circulation of the NSCS during winter, while model-simulated subtidal currents generally capture its current pattern. The model shows that the current over the continental shelf is generally southwestward, under a strong winter monsoon condition, but a northeastward counter-wind current usually develops between 50-and 100-m isobaths, when the monsoon relaxes. Model experiments, focusing on the wind relaxation process, show that sea level is elevated in the northwestern South China Sea(SCS), related to the persistent northeasterly monsoon. Following wind relaxation, a high sea level band builds up along the mid-shelf, and a northeastward current develops, having an obvious vertical barotropic structure. Momentum balance analysis indicates that an along-shelf pressure gradient provides the initial driving force for the SCSWC during the first few days following wind relaxation. The SCSWC subsequently reaches a steady quasi-geostrophic balance in the cross-shelf direction, mainly linked to sea level adjustment over the shelf. Lagrangian particle tracking experiments show that both the southwestward coastal current and slope current contribute to the northeastward movement of the SCSWC during winter monsoon relaxation. 相似文献
16.
Wang Haoyin Li Guangxue Zhang Yang Liu Yong Liu Dongsheng Ding Dong Xu Jishang Ma Yanyan Qiao Lulu Wang Liyan Li Qian 《中国海洋大学学报(英文版)》2020,19(4):827-836
The sediments in core YS01 recovered from the South Yellow Sea mud deposit zone contain abundant benthic foraminifera, particularly shallow continental shelf species, but rare of planktonic foraminifera. The benthic foraminifera are dominated by stenohaline cold shallow-water species and euryhaline brackish-water species. In this paper, the palaeoenvironmental changes were discussed based on the grain-size compositions and benthic foraminiferal assemblages. Six different benthic foraminiferal assemblages were discriminated by species analysis from the foraminiferal fauna. According to AMS~(14)C dating data in core YS01, we identified four main stages of marine environmental changes since the last deglaciation: a near-shore depositional stage(13.1 – 9.5 kyr B.P.), a transitional stage from near-shore deposition to shallow-sea deposition(9.5 – 5.6 kyr B.P.), a high sea level stage with shallow-sea deposition(5.6–2.9 kyr B.P.), and a stable shallow-sea depositional stage(2.9 kyr B.P. to the present). 相似文献
17.
【目的】研究南海北部近海区域柱状沉积物多环芳烃组成及分布特征,讨论全新世早期火历史及气候变化。【方法】利用AMS 14C定年技术结合有机地球化学分析手段对全新世早期南海北部近海沉积物柱状样品中多环芳烃(PAHs)分布特征进行研究。【结果】南海北部近海沉积物中16种PAHs总浓度范围为8.58~17.48 ng/g,在约10000 a B.P.的全新世早期呈现先增大后减小波动变化,与TOC变化基本同步。【结论】沉积物中多环芳烃主要来源于南海北部近海陆源区域自然火灾产生的焦炭残渣。PAHs的沉积浓度变化间接指示了全新世早期东亚季风的强度变化。 相似文献
18.
TIAN Xu JIANG Zuzhou GAO Wei LIU Zhaoqing LIU Xiling FAN Ying QIN Shengjie JING Chunlei XU Yue LIU Baohua XU Fangjian 《中国海洋大学学报(英文版)》2019,(5)
The concentrations of rare earth elements(REEs) in the bulk sediment of Core X2, which was collected from southeastern Hainan Island, were analyzed to investigate the relative contributions of various provenance regions since mid-Holocene. The results show that sediments in Core X2 were primarily derived from Hainan Island with lesser amounts from Taiwan and limited input from the Pearl River. Based on the application of quantitative inversion to model the REE data, the average contributions of river materials from southeastern Hainan Island and southwestern Taiwan to the study area were 68% and 32%, respectively. Furthermore, starting at 4.0 kyr BP, the transport of fluvial sediments from Taiwan to the study region increased due to enhanced hydrodynamics in South China Sea(SCS). These results indicate that the contributions of mountain river materials from Hainan Island and Taiwan to the continental shelf of northern SCS are non-negligible. Furthermore, these results demonstrate that mountain rivers can play an important role in the material cycle of continental margins and may feature a greater impact than large river systems in specific continental shelf areas. 相似文献
19.
Large amplitude internal solitary waves (ISWs) often exhibit highly nonlinear effects and may contribute significantly to
mixing and energy transporting in the ocean. We observed highly nonlinear ISWs over the continental shelf of the northwestern
South China Sea (19°35′N, 112°E) in May 2005 during the Wenchang Internal Wave Experiment using in-situ time series data from
an array of temperature and salinity sensors, and an acoustic Doppler current profiler (ADCP). We summarized the characteristics
of the ISWs and compared them with those of existing internal wave theories. Particular attention has been paid to characterizing
solitons in terms of the relationship between shape and amplitude-width. Comparison between theoretical prediction and observation
results shows that the high nonlinearity of these waves is better represented by the second-order extended Korteweg-de Vries
(KdV) theory than the first-order KdV model. These results indicate that the northwestern South China Sea (SCS) is rich in
highly nonlinear ISWs that are an indispensable part of the energy budget of the internal waves in the northern South China
Sea. 相似文献
20.
孙传香 《广东海洋大学学报》2010,30(2):6-10
中日东海划界历经旷日持久而未能解决,中国主张尊重《联合国海洋法公约》(以下简称《公约》)中大陆架之自然延伸原则,采取不同于专属经济区的方法对大陆架进行划界,而日本则始终坚持采用中间线对中日东海大陆架和经济专属区作一揽子划界。无论从逻辑角度还是法理视角,日本主张在中日东海划界中适用中间线将混淆《公约》中专属经济区与大陆架两种制度。基于中日东海大陆架的地质与地貌特点以及公约对上述两种权利的不同规定,中日难以通过中间线对东海的海洋权益作出公平划分。中日两国应以《公约》为依据,分别对专属经济区和大陆架的划界作出安排,同时兼顾处理钓鱼岛群岛的主权归属问题,使中日东海划界问题得到妥善解决。 相似文献