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41.
阐明了东山湾重矿物组合规律,物质来源,自生黄铁矿的富集与形成环境。研究表明,湾内重矿物含量<1%,来自漳江及周边水系。东山湾西部的沉积环境有利于自生黄铁矿的形成。 相似文献
42.
大亚湾海域锥状斯氏藻赤潮及其与孢囊的关系 总被引:22,自引:0,他引:22
用沉积物捕捉器取样,研究了大亚湾海域2000年6~9月孢囊(Cyst)种群动态,同时 分析了浮游植物种群动态。研究期间(8~9月)该海域发生了一起大规模的锥状斯氏藻赤潮。 赤潮前一个月,锥状斯氏藻孢囊的平均日形成率为2.05× 105cysts/(m2·d),丰度为50.22%, 该时期以有性生殖产生的静止期孢囊为主;在赤潮盛期的8,9月初,孢囊的平均日形成率达到 2.01 ×106cysts/(m2·d),丰度为96.97%,此时期的孢囊多为营养细胞所形成的暂时性孢囊; 赤潮结束后,由于环境条件的恶化,暂时性孢囊的形成达到高峰,平均日形成率为1.24×l07 cysts/( m2·d),丰度为99.53%。结果表明大亚湾丰富的孢囊是潜在的种源(Seed bed),2000年 的夏季、秋李持续高温(>25℃),台风减少及风力减弱等有利锥状斯氏藻的环境条件诱发孢 囊萌发,开始了该种类的赤潮。 相似文献
43.
44.
采用金属潜在生态危害系数和危害指数的评估方法,评价了大亚湾海域重金属对海洋生态系统的潜在危害。结果表明,大亚湾海域重金属潜在生态危害轻微,而养殖海区和近岸海区的重金属潜在生态危害则相对较重,大亚湾海域重金属的潜在生态危害较珠江口外浅海轻。 相似文献
45.
The Amphipod Community as a Bioindicator in Algeciras Bay (Southern Iberian Peninsula) Based on a Spatio-Temporal Distribution 总被引:2,自引:0,他引:2
Abstract. The amphipod population associated with Bugula neritina (L.), a verycommon bryozoan species in Algeciras Bay (Strait of Gibraltar), was studied on a spatio-temporal scale, in order to define its role as a bioindicator. Samples were collected in December, March, June and September along a transect running from the external to the internal sampling stations.
Fifty-three species belonging to 22 families were identified; the most abundant species were Jassa marmorata H olmes , Ischyrocerus inexpectatus (R uffo ) and Phtisica marina S labber .
The spatial evolution of the amphipod community reflected the physico-chemical conditions of Algeciras Bay, yielding a clear gradient from the outer to the inner stations. The stations located at the mouth of the bay, characterised by high hydrodynamism and low sedimentation, had a higher diversity and species richness than the inner stations with low water movement and higher sedimentation. Eight species preferred for the outer stations, while another nine species were typical of the inner harbours.
The most notable aspect of the seasonal evolution was the increased dominance of the tube-builder and deposit-suspension feeder Jassa marmorota .
Structural and ordination analyses corroborate the outer-inner gradient in the bay and illustrate the importance of hydrodynamic forces and sedimentation in the amphipod community. 相似文献
Fifty-three species belonging to 22 families were identified; the most abundant species were Jassa marmorata H olmes , Ischyrocerus inexpectatus (R uffo ) and Phtisica marina S labber .
The spatial evolution of the amphipod community reflected the physico-chemical conditions of Algeciras Bay, yielding a clear gradient from the outer to the inner stations. The stations located at the mouth of the bay, characterised by high hydrodynamism and low sedimentation, had a higher diversity and species richness than the inner stations with low water movement and higher sedimentation. Eight species preferred for the outer stations, while another nine species were typical of the inner harbours.
The most notable aspect of the seasonal evolution was the increased dominance of the tube-builder and deposit-suspension feeder Jassa marmorota .
Structural and ordination analyses corroborate the outer-inner gradient in the bay and illustrate the importance of hydrodynamic forces and sedimentation in the amphipod community. 相似文献
46.
47.
针对杭州湾独特的喇叭型强潮河口湾的特点,基于Blumberg等(1996)的ECOMSED模式,引入动边界技术,建立杭州湾三维动边界的潮流模型.模型以正交曲线坐标下三维非线性水动力方程为基本方程,应用Mellor和Yamada的2.5阶湍流闭合模型计算紊动黏滞系数,嵌入Grant和Madsen的底边界层模型考虑波浪对底部应力的作用,采用干湿网格法模拟潮流漫滩过程;综合考虑径流,风应力,密度流和M2,S2,K1,O1四个主要分潮和M4,S4,MS4三个浅水分潮的作用,从而提高杭州湾潮流模拟的精度.通过验潮站调和常数和多次海流连续观测资料的验证,表明该文建立的模型可以更好的用于杭州湾流场的预报模拟. 相似文献
48.
Vertical and seasonal characteristics of biogenic silica (BSi) dissolution in seawater were investigated by multiple dissolution experiments using seawater collected from surface and mesopelagic layers in Suruga Bay during the period 2002–2004. The dissolution rate coefficients calculated based on temporal changes of BSi concentration varied with the season of sample collection. They ranged from 0.023–0.057 day− 1 for surface samples and 0.0018–0.0025 day− 1 for mesopelagic samples for temperatures approaching in situ conditions. Experiments at various temperatures confirmed that BSi dissolution depends on temperature in natural seawater. Dissolution rate coefficient (day− 1) of BSi correlated significantly with temperature (°C), and Q10 was 2.6. Addition of bioavailable organic matter to low-bioactivity seawater enhanced the protease activity and abundance of bacteria, and increased BSi dissolution rate by a factor of 1.4–2.0. There is clear evidence that BSi dissolution is accelerated by bacterial activity and potentially limited by bioavailable organic matter in natural seawater. Dissolution rates and total decreases of BSi concentration were lower during experiments using mesopelagic samples than in those using surface samples. This suggests that dissolution of BSi varies with depth and that BSi in the mesopelagic water is more resistant to the dissolution than that in the surface water. This lower dissolution rate was caused by lower temperature and lower bacterial activity due to less bioavailable organic matter in mesopelagic water. Our results provide a mechanistic understanding of variations in silica cycling within the seasonally and vertically differing marine environment. 相似文献
49.
合浦珠母贝两个野生种群的生化遗传变异 总被引:12,自引:0,他引:12
用聚丙烯酰胺梯度凝胶垂直平板电泳技术测定了大亚湾和北部湾合浦珠母贝Pinctadamartensi野生种群12种同工酶26个基因座位的遗传变异。结果表明,两个种群的平均杂合度分别为0.1243±0.0377和0.0999±0.0441,与已报道的珠母贝属的其他种很接近。两个种群的杂合子缺失系数分别为-0.278和-0.346;遗传相似度(I)和遗传距离(D)分别为0.9842和0.0159;基因分化系数GST为0.0253,表明2个种群之间有较强的基因流。 相似文献
50.
南极普里兹湾气旋的生消发展 总被引:3,自引:4,他引:3
利用1989~2000年现场观测的气象资料,特别是自1997年以来在南极考察船上接收的NOAA卫星极轨高分辨的卫星云图,研究了普里兹湾气旋的生消发展;提出了夏季绕极气旋进入普里兹湾内也会发展加强,在湾内东风带里也能生成气旋的新观点,修正了普里兹湾仅是气旋墓地的不全面说法,从而进一步完善了南极西风带绕极气旋和东风带上气旋生消发展的理论;研究了普里兹湾冰-气-海相互作用的机理,解释了气旋发生、发展的物理过程.用整体动力学输送法计算了进入普里兹湾980205号绕极气旋爆发性发展的能量交换,指出气旋在超过冰坝进入冰间湖可以获得巨大的热量,使气旋迅速发展成为具有南极特色的强风暴,风力达12级以上,平均风速为38m/s;瞬时最大风速达100m/s. 相似文献