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191.
The diffusion attenuation coefficient for downwelling irradiance, Ka(490), is an important optical parameter of seawater. The optical property, Kd(490), around Nansha Islands in the South China Sea was analyzed based on optical data profiles measured with SPMR (SeaWiFS Profiling Multichannel Radiometer) and SMSR ( SeaWiFS Multichannel Surface Reference ) instrument in April and May, 1999. The results show that Kd(490) is closely correlated with chlorophyll-a concentration, Ccgka, and that the vertical distribution of Kd(490) shows the strong stratification of the water column in this area. Kd(490) has a similar vertical co-variation as KL(490), the diffusive attenuation coefficient for upwelling radiance.Both coefficients increase with depth in the upper layer, where KL(490) is greater than Kd(490); and after a depth, approximatively at the chlorophyll maximum, they decrease with depth, with the former being smaller than the latter. 相似文献
192.
193.
本文根据1987.12~1989.4对舟山朱家尖岛南沙沙滩逐月采集标本进行研究。结果表明,等边浅蛤Gomphina veneriformis的性腺发育可分为5期:增殖期、生长期、成熟期、排放期和休止期。在舟山海区,等边浅蛤一年中为一个繁殖周期,繁殖期为8月下旬至9月中旬。有雄性早熟现象。 相似文献
194.
南沙群岛海域泻湖及礁外沉积物间隙水中的-2价硫 总被引:1,自引:1,他引:1
于1993年5月和1994年3-4月通过调查,用硫离子选择电极法研究南沙群岛海域泻湖及礁外沉积物间隙水中的∑S(-Ⅱ)及SO~(2-)_4,探讨泻湖内及礁外间隙水中-2价硫的分布特征,沉积物-海水界面间硫的扩散转移通量和-2价硫的热力学平衡控制体系。结果表明,该海区∑S(-Ⅱ)含量,泻湖间隙水中远比礁外高,人为活动剧烈的礁内泻湖高于人为活动少的泻湖,离礁近的礁外间隙水中的高于远离礁的间隙水中的。在礁外沉积物间隙水中-2价硫含量呈垂向增加的趋势,沉积物-海水界面间HS-,S2-均是从沉积物向上覆海水扩散,SO反之。礁内泻湖的扩散量远高于礁外的,HS-扩散总平均为61.34μmol/(m2·d),SO为-0.41mmol/(m2·d);礁外泻湖的HS-总平均为14.96μmol/(m2·d),SO为-0.35mmol/(m2·d)。该海区的-2价硫主要由S+2e→S2-氧化还原电对控制,平衡时Eh计算值与实测值接近,单质疏作为亚稳态可存在于沉积物中,并可与溶解铁继续形成自生黄铁矿(FeS2)沉淀。 相似文献
195.
E. Kokinou E. Papadimitriou V. Karakostas E. Kamberis F. Vallianatos 《Marine Geophysical Researches》2006,27(4):241-252
Information concerning two seismic lines, the first located northwest of the Lefkada Island and the second from the deep Ionian basin to the gulf of Patras, is used to trace the Kefalonia Transform Zone (KTZ) and to explore its relation with the sedimentary sequences and the deeper geologic structures in the study area. In addition, sea bottom topography and fault plane solutions are combined in order to explore the prolongation of the KTZ into the Ionian Abyssal Plain (IoAP) and to describe its properties. The boundary between the subduction of the eastern Mediterranean oceanic crust under the overriding continental crust and the KTZ is well constrained by the seismic data in association with seismicity and regional stress field. The southern prolongation of the KTZ is located in the IoAP towards the direction between Kefalonia and Zakynthos Islands at depth greater than 15 km. The southern part of the KTZ exhibits a strike–slip motion with a thrust component according to fault plane solutions of moderate and strong earthquakes. The seismic section mostly confirms the existence of the thrust component and gives information about the tectonic status east and west of the KTZ. 相似文献
196.
Yohei Nakamura Hiroyuki Kawasaki Mitsuhiko Sano 《Estuarine, Coastal and Shelf Science》2007,71(3-4):559-568
Habitat choice of reef fish larvae at settlement is one of the mechanisms proposed to explain spatial patterns in the distribution of fishes and the corresponding spatial structure of communities. Field experiments using Pomacentridae were conducted at Iriomote Island, southern Japan, in order to determine if rare recruitment of coral reef fishes in seagrass beds is due to larval settlement preference. When three types of natural patch treatments (branching coral patch, seagrass patch, and control without patches) were established in cleared seagrass squares in the center of a seagrass bed, four pomacentrid species, Amblyglyphidodon curacao, Dischistodus prosopotaenia, Cheiloprion labiatus, and Dascyllus aruanus, recruited exclusively onto the coral patches, indicating that larvae distributed in the seagrass bed may have preferred a coral rather than seagrass substrate as a settlement habitat. The effects of differences in physical shape (grid structure for branching coral vs. vertical structure for seagrass leaves) and rigidity (rigid substrate for coral vs. flexible substrate for seagrass) between coral and seagrass substrates on such recruitment patterns were investigated using artificial coral and seagrass units. When artificial habitat units with predator exclusion cages were established in the cleared seagrass squares as above, high densities of A. curacao and D. prosopotaenia recruits were observed on the rigid rather than flexible habitat units (both unit types having similar shape), whereas differences in recruit numbers of the two species were unclear in differently shaped units. These results demonstrated that even though pomacentrid larvae are distributed in the seagrass bed, they do not settle on the seagrass substrate owing to their habitat choice being partially based on a preference for substrate rigidity. Moreover, non-recruitment of C. labiatus and D. aruanus on artificial habitat units suggested that the presence of living coral substrates rather than physical shape/rigidity of substrates are an important cue for habitat choice of these fishes. 相似文献
197.
Abstract. .The absorption efficiencies of the intertidal mangrove dwelling mollusk Melampus coffeus and the rocky intertidal dwelling mollusk Acanthopleura granulata were calculated by a modification of CONOVER'S (1966) equation. M. coffeus tended to consume fresh mangrove leaves indicating that M. coffeus may obtain much of its energy from the actual substrate material rather than from associated bacteria and meiofauna on decaying leaves. Obtaining energy directly from the substrate may be a mechanism for M. coffeus to utilize its food source more efficiently. In contrast, chitons (A. granulata) may utilize the higher energy components of their limited intertidal microflora! food source. Using the high energy component of a food source may be an additional mechanism by which organisms efficiently utilize a food source. 相似文献
198.
199.
ZhouWcihua WuYunhua ChenShaoyong YinKedong 《海洋通报(英文版)》2003,5(2):14-21
Concentrations of organic matter, iron and manganese in the deep sea surface sediments in the Nansha Islands sea area, South China Sea are measured, Horizontal and vertical distributions of iron and manganese are discussed. The vertical distribution of iron and manganese in the sediments results from reduction, diffusion, and redeposition of manganese (or iron) oxide and hydroxide in the sediment. There are the maxima of iron and manganese in solid phase in the top of the sediment, which is caused by the penetration of O2 and the upward flux of Mn^2 ( or Fe^2 ). Manganese bacteria play a very important role in the cycle of solid-phase iron and manganese in the ocean environment. Manganese bacteria oxidize Mn^2 ( or Fe^2 ) in dissolved state to Mn^4 ( or Fe^3 ) in oxidized state under the aerobic condition, whereas they reduce iron and manganese in anaerobic conditions. 相似文献
200.