共查询到20条相似文献，搜索用时 46 毫秒
1.
2.
3.
江苏沿海开发上升为国家战略,为海安的新一轮发展带来了千载难逢的重大机遇,将为海安的经济社会建设注入新的发展动力、拓展新的发展空间、增添新的发展优势. 相似文献
4.
黄莉新 《海洋与海岸带开发》2009,(12):16-16
沿海地区是江苏发展的潜力和希望所在。党中央、国务院对江苏沿海地区发展高度重视,胡锦涛总书记、温家宝总理作出重要指示、寄予殷切期望。2009年6月,国务院常务会议讨论并通过了《江苏沿海地区发展规划》。这标志着江苏沿海开发已经正式上升到国家层面，成为连接南北、带动中西部地区发展的国家战略。这是江苏人民的多年期盼， 相似文献
5.
江苏省海洋与渔业局办公室 《海洋开发与管理》2009,26(12):76-76
随着国务院批准实施<江苏沿海地区发展规划>,江苏沿海开发上升为国家战略.为加快推进亲一轮沿海开发,江苏省政府于今年8月31日出台了<关于推进海域使用权抵押贷款工作的意见>,此举标志全国海域使用权抵押贷款制度化规范作率先在江苏实施. 相似文献
6.
2008年,江苏沿海开发上升至国家战略层面.作为江苏沿海中部的土地、资源大县射阳县,如何抢抓发展机遇,加快临港工业发展,引领县域经济科学发展,是摆在该县面前的一个迫切需要研究的课题.试从射阳临港工业发展的现状和面临的瓶颈制约入手,提出准确把握临港工业拐点机遇和加快射阳沿海经济发展的几点建议. 相似文献
7.
以连云港为龙头的江苏沿海开发上升到国家战略层面,连云港迎来了千载难逢的历史性机遇.今后将深入实施"以港口为龙头带动、以产业为主攻方向、以城市为有力依托、以基础设施为坚实支撑"的沿海开发策略,构筑大港口,发展大产业,建设大城市,服务大腹地,持续兴起沿海开发热潮,早日昂起江苏沿海开发的龙头,在服务和促进江苏沿海开发以及全国区域共同发展中发挥新的更大的作用. 相似文献
8.
江苏省海洋与渔业局计划财务处渔业处 《海洋开发与管理》2009,26(12):91-94
6月10日,<江苏沿海地区发展规划>经国务院常务会议讨论并原则通过,这标志着江苏省沿海开发已正式成为国家战略.在国务院常务会议上,温总理作了重要讲话并明确指出:在加快江苏沿海地区发展过程中,要大力发展现代农业,做强特色优势农业,提高现代渔业综合生产能力,加快建设农产品加工产业基地等. 相似文献
9.
10.
党中央、国务院从全局和战略的高度,对新一轮沿海地区发展作出了重大部署.胡锦涛总书记、温家宝总理对江苏沿海地区发展高度重视. 相似文献
11.
12.
Soil-sized particulates have been collected on board ship by a mesh technique from the lower troposphere of the North, Equatorial and South Atlantic Ocean, northern and southern Indian Ocean, South and East China Sea and various coastal localities.Spectrographic analysis reveals that, on average, the particulates have concentrations of Mn, Ni, Co, Ga, Cr, V, Ba, and Sr which are of the same order of magnitude as those in average crustal material. In contrast, the average concentrations of Pb, Sn, and Zn are one order of magnitude higher than those in average crustal material.Within this “world-wide” average there are significant geographical variations in the distributions of Pb, Sn, and Zn which may be related to anthropogenic sources.On the basis of trace-element distributions lower tropospheric soil-sized marine particulates have been divided into four genetic components; local, zonal, inter-zonal, and global. The proportions of these components vary geographically, and each component may have both a natural and an anthropogenic fraction. 相似文献
13.
14.
15.
16.
17.
Tautog, Tautoga onitis, is an abundant species of fish in estuaries of the northeastern United States. Planktonic tautog larvae are abundant in summer in these estuaries, but there is little information on rates of growth of tautog larvae feeding on natural assemblages of food in the plankton. We examined abundance and growth of larval tautog and environmental factors during weekly sampling at three sites along a nearshore‐to‐offshore transect in Buzzards Bay, Massachusetts, USA during summer 1994. This is the first study of a robust sample size (336 larvae) to estimate growth rates of field‐caught planktonic tautog larvae feeding on natural diets, using the otolith daily‐growth‐increment method. The study was over the entire summer period when tautog larvae were in the plankton. The sampling sites contrasted in several environmental variables including temperature, dissolved oxygen (DO), and chlorophyll a concentration. There was a temporal progression in the abundance of tautog larvae over the summer, in relation to location and temperature. Tautog larvae were first present nearshore, with a pronounced peak in abundance occurring at the nearshore sites during the last 2 weeks in June. Larvae were absent at this time further offshore. From late June through August, larval abundance progressively decreased nearshore, but increased offshore although never approaching the abundance levels observed at the nearshore sites. The distribution and abundance of tautog larvae appeared to be related to a nearshore‐to‐offshore seasonal warming trend and a nearshore decrease in DO. Otoliths from 336 larvae ranging from 2.3 to 7.7 mm standard length had otolith increment counts ranging from 0 to 19 increments. Growth of larval tautog was estimated at 0.23 mm·day?1, and length of larvae prior to first increment formation was estimated at 2.8 mm indicating that first increment formation occurs 3–4 days after hatching at 2.2 mm. Despite spatial and temporal differences in environmental factors, there were no significant differences in growth rates at any of three given sites over time, or between sites. Because larval presence only occurred at a narrow range of temperature (17–23.5 °C) and DO (6.5–9.3 mg·l?1), in situ differences in growth did not appear to be because of differences in larval distribution and abundance patterns relative to these parameters. 相似文献
18.
Lars-Göran Danielsson 《Marine Chemistry》1980,8(3):199-215
Results of trace-metal analyses of water samples obtained during a cruise with the Soviet R.V. “Akademik Kurchatov” in the Indian Ocean are presented. The determinations were performed on board with atomic absorption spectrophotometry after a two-stage dithiocarbamate—Freon extraction procedure. Trace-metal concentrations found are in the same range as those found recently for similar open-ocean areas by other workers. The values for lead and zinc are probably high due to contamination. Vertical profiles indicate biogenic processes as controlling factors for the increase of cadmium, copper and nickel concentrations with depth. Iron shows an irregular depth distribution as a result of large random variations in concentration. 相似文献
19.
Klaus Kremling 《Marine Chemistry》1983,13(2):87-108
In June 1981, dissolved Zn, Cd, Cu, Ni, Co, Fe, and Mn were determined from two detailed profiles in anoxic Baltic waters (with extra data for Fe and Mn from August 1979). Dramatic changes across the O2H2S interface occur in the abundances of Cu, Co, Fe, and Mn (by factors of ?100). The concentrations of Zn, Cd, and Ni at the redox front decrease by factors between 3 to 5.Equilibrium calculations are presented for varying concentrations of hydrogen sulfide and compared with the field data. The study strongly supports the assumption that the solubility of Zn, Cd, Cu, and Ni is greatly enhanced and controlled by the formation of bisulfide and(or) polysulfide complexes. Differences between predicted and measured concentrations of these elements are mainly evident at lower ΣH2S concentrations.Cobalt proved to be very mobile in anoxic regions, and the results indicate that the concentrations are limited by CoS precipitation. The iron (Fe2+) and manganese (Mn2+) distribution in sulfide-containing waters is controlled by total flux from sediment-water interfaces rather than by equilibrium concentrations of their solid phases (FeS and MnCO3). The concentrations of these metals are therefore expected to increase with prolonged stagnation periods in the basin. 相似文献
20.
P.N. Froelich L.W. Kaul J.T. Byrd M.O. Andreae K.K. Roe 《Estuarine, Coastal and Shelf Science》1985,20(3):239-264
Concentrations of dissolved nutrients (NO3, PO4, Si), germanium species, arsenic species, tin, barium, dimethylsulfide and related parameters were measured along the salinity gradient in Charlotte Harbor. Phosphate enrichment from the phosphate industry on the Peace River promotes a productive diatom bloom near the river mouth where NO3 and Si are completely consumed. Inorganic germanium is completely depleted in this bloom by uptake into biogenic opal. The ratio taken up by diatoms is about 0·7 × 10?6, the same as that provided by the river flux, confirming that siliceous organisms incorporate germanium as an accidental trace replacement for silica. Monomethylgermanium and dimethylgermanium concentrations are undetectable in the Peace River, and increase linearly with increasing salinity to the seawater end of the bay, suggesting that these organogermanium species behave conservatively in estuaries, and are neither produced nor consumed during estuarine biogenic opal formation or dissolution. Inorganic arsenic displays slight removal in the bloom. Monomethylarsenic is produced both in the bloom and in mid-estuary, while dimethylarsenic is conservative in the bloom but produced in mid-estuary. The total production of methylarsenicals within the bay approximately balances the removal of inorganic arsenic, suggesting that most biological arsenic uptake in the estuary is biomethylated and released to the water column. Dimethylsulfide increases with increasing salinity in the estuary and shows evidence of removal, probably both by degassing and by microbial consumption. An input of DMS is observed in the central estuary. The behavior of total dissolvable tin shows no biological activity in the bloom or in mid-estuary, but does display a low-salinity input signal that parallels dissolved organic material, perhaps suggesting an association between tin and DOM. Barium displays dramatic input behavior at mid-salinities, probably due to slow release from clays deposited in the harbor after catastrophic phosphate slime spills into the Peace River. 相似文献