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The geotechnical consortium 《Marine Georesources & Geotechnology》2013,31(4):297-339
During Leg 75 of the Deep Sea Drilling Project (DSDP) from the D/V Glomar Challenger, a 200‐m deep hole was drilled at Hole 532A on the eastern side of Walvis Ridge at a water depth of 1331 m. Sediment cores were obtained by means of a hydraulic piston corer. All of the cores from this boring were designated for geotechnical studies and were distributed among eight institutions. The results of laboratory studies on these sediment cores were compiled and analyzed. Sediment properties, including physical characteristics, strength, consolidation, and permeability were studied to evaluate changes as a function of depth of burial. It was concluded that the sediment profile to the explored depth of 200 m at Walvis Ridge consists of approximately 50 m of foram‐nannofossil marl (Subunit la) over 64 m of diatom‐nannofossil marl (Subunit 1b) over nannofossil marl (Subunit lc) to the depth explored. All three sediment units appear to be normally consolidated, although some anomalies seem to exist to a depth of 120 m. No distinct differences were found among the sediment properties of the three subunits (la, 1b, and lc) identified at this site. 相似文献
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Four specimens of the thyasirid Conchocele bisecta (Conrad) and one small specimen of the vesicomyid Hubertschenckia ezoensis (Yokoyama), each with a drill hole made by a naticid gastropod, were found at a cold‐seep site in the upper Eocene Poronai Formation of Hokkaido. This is apparently the oldest record not only of drill holes, but also of predation scars, in a cold‐seep fauna. In addition, drilled vesicomyids are known from several Miocene cold‐seep sites in Japan. We suggest that the Eocene and Miocene chemoautotrophic bivalves were drilled only in the shallow‐water settings preferred by most naticids. The lack of drill holes in Oligocene chemoautotrophic bivalves in the northwestern USA suggests that this innovation, which allowed naticids to prey upon highly toxic bivalves, first appeared in the western Pacific during the Eocene. 相似文献
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Gi Hoon Hong Dong Beom Yang Hyun-Mi Lee Sung Ryull Yang Hee Woon Chung Chang Joon Kim Young-Il Kim Chang Soo Chung Yu-Hwan Ahn Young-Je Park Jeong-Eon Moon 《Ocean Science Journal》2012,47(3):387-394
Korean Geostationary Ocean Color Imager (GOCI) and Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua observations of the variation in ocean color at the sea surface were utilized to monitor the impact of nutrient-rich sewage sludge disposal in the oligotrophic area of the Yellow Sea. MODIS revealed that algal blooms persisted in the spring annually at the dump site in the Yellow Sea since year 2000 to the present. A number of implications of using products of the satellite ocean color imagers were exploited here based on the measurements in the Yellow Sea. GOCI observes almost every hour during the daylight period, every day since June 2011. Therefore, GOCI provides a powerful tool to monitor waste disposal at sea in real time. Tracking of disposal activity from a large tanker was possible hour by hour from the GOCI timeseries images compared to MODIS. Smaller changes in the color of the ocean surface can be easily observed, as GOCI resolves images at smaller scales in space and time in comparison to polar orbiting satellites, e.g., MODIS. GOCI may be widely used to monitor various marine activities in the sea, including waste disposal activity from ships. 相似文献
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用紫色蚌和非紫色蚌制取细胞小片,分别插入紫色蚌和非紫色蚌外套膜内,探究三角帆蚌(Hyriopsis cumingii)无核珍珠颜色与制片蚌、育珠蚌的关系;用不同类型制片蚌的不同部位制取细胞小片,分别插入育珠蚌外套膜内,进一步探究珍珠颜色与制片蚌珍珠质颜色的关系。结果表明,以紫色蚌为制片蚌,所产的珍珠为紫色系,珍珠紫色深浅与细胞小片所对应部位的制片蚌珍珠质紫色深浅呈正相关。以非紫色蚌为制片蚌,所产的珍珠有白色系和黄色系,珍珠黄色深浅与细胞小片所对应部位的制片蚌珍珠质黄色深浅呈正相关。三角帆蚌外套膜无核珍珠颜色是由提供细胞小片的制片蚌珍珠质颜色所决定,而与育珠蚌无关。该结论支持珍珠囊表皮细胞来自于移植细胞小片的观点。该结果表明,通过定向选育纯紫、纯白色贝壳珍珠质三角帆蚌新品系,即可培育出纯紫、纯白色无核珍珠。 相似文献
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Any attempt to enhance rock lobster production by increasing survival after settlement, or by ongrowing or outplanting young juveniles, requires knowledge of the shelter preferences of young juveniles. For juvenile Jasus edwardsii in the wild these are not well known. Information available suggests that juveniles up to c. 35 mm carapace length (CL) occupy shelters that generally conform closely to their body dimensions but that larger juveniles use shelters of more variable dimension, often much larger than their body size. We investigated mainly physical factors important in shelter choice by 15–59 mm CL (c. 2–24‐month‐old juveniles) in laboratory tank experiments. In overnight tests, all sizes of juvenile lobster chose to occupy holes (shelters with sides) over open horizontal gaps. Preference for open horizontal gaps versus horizontal crevices (where the height reduces from a maximum at the mouth to zero at the opposite end) was much less clear‐cut; choice varied according to lobster size. For the number of entrances into holes, there was evidence for an ontogenetic shift in preference, small lobsters preferring two openings over one, whereas those >30 mm CL (c. 9 months old) preferred one over two. For lobsters <40 mm CL, the hole size and gap size preferences revealed were generally consistent with the field evidence for J. edwardsii in that there was a close and proportional relationship between lobster size and shelter size; what differed was that the open gaps chosen in the tanks by the smallest lobsters (15–19 mm CL) were larger than the holes used in the tank experiments and 30–50% larger than those reportedly used in the field. For lobsters >40 mm CL, the holes and gaps chosen in the tanks were generally larger and more variable in size, as in the field. 相似文献
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Ocean Color Satellite Imagery and Shipboard Measurements of Chlorophyll a and Suspended Particulate Matter Distribution in the East China Sea 总被引：1，自引：0，他引：1
Satellite-derived ocean color data of Coastal Zone Color Scanner (CZCS) on board the Nimbus-7 and Ocean Color and Temperature Scanner (OCTS) on board the Advanced Earth Observing Satellite (ADEOS) are jointly used with historical in situ data to examine seasonal and spatial distributions of chlorophyll a (Chl-a) and suspended particulate matter (SPM) concentrations in the East China Sea. Ocean color imagery showed that Chl-a concentrations on the continental shelf were higher than those of the Kuroshio area throughout the year. Satellite-derived Chl-a concentrations are generally in good accordance with historical in situ values during spring through autumn (although no shipboard in situ measurement was conducted at nearshore areas). In contrast, ocean color imagery in winter indicated high Chl-a concentrations (4–10 mg m–3) on the continental shelf where bottom depth was less than 50 m when surface water was turbid (2–72 g m–3 of SPM at surface), while historical in situ values were usually less than 1 mg m–3. This suggests that resuspended bottom sediment due to wind-driven mixing and winter cooling is responsible for the noticeable overestimation of satellite-derived Chl-a concentrations. The algorithm for ocean color needs to be improved urgently for turbid water. 相似文献
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叙述了目前海水现场水色测量的弊端 ,指出数字化海洋水色的潜在应用价值 ;根据色度学及色度学的三原色基本理论 ,确定海洋现场水色的色度要素 ,使海洋现场水色标号统一为物理学中严格的颜色物理量。结合 1 996年渤海水域光谱反射测量 ,对渤海水域 4个典型站位的反射光谱做了水色色度分析 ,并进行了 2种测量方法的比较 相似文献
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We examined the effects of the presence of larval conspecifics on larval vertical distribution of four‐arm and six‐arm plutei of Strongylocentrotus droebachiensis and bipinnaria of Asterias rubens, in laboratory experiments, by manipulating population density. Larvae were introduced to experimental columns (10 × 10 × 30 cm) at one of two or three population densities (S. droebachiensis: 0.1 and 10 larvae·ml?1; A. rubens: 0.1, 1 and 10 larvae·ml?1). Subsequent changes in vertical distribution were determined from images of the larvae in the columns illuminated by a 532‐nm laser and captured by a high‐resolution camera. Larvae of both species were found higher in the water column in the high than in the low and intermediate population densities. The relationship between vertical swimming velocity and nearest neighbour distance (NND) was measured for four‐arm plutei of S. droebachiensis, and used to determine a range in distances among individuals that may affect potential interactions. The variation in swimming velocity decreased with increasing proximity below a threshold distance among individuals of 10 mm, which was greater than the estimated distance in the high population density. We suggest that the increased larval aggregation near the water surface under high population density is the result of a behavioural response to conspecifics. 相似文献
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Lake Poukawa, a shallow hardwater lake, is situated on calcareous lake silt overlying peat and alluvium. Two tephra layers, Taupo Pumice and Waimihia Lapilli, aged c. 2000 and 3500 calendar years respectively, were present in four cores (c. 6 m long) of the lake sediment. The diatom flora of the cores was studied to find any indication of changes in the lake morphology and to assess the effects of tephra deposition. Increased abundance of small Fragilaria spp. appears to indicate periods when the lake was less extensive, c. 3700–3500 y ago, and c. 2800–3000 y ago. In the recent past, increased abundance of Fragilaria spp. in lake sediment near the present southern margin almost certainly coincides with artificial draining since A.D. 1931. The occurrence of marine sponge spicules in the cores probably indicates that rates of erosion in the catchment were low before 2500 y ago and high 100–0 y ago. Diatom samples taken at close intervals adjacent to the Taupo and Waimihia tephras indicate that above the ash estimated numbers of diatoms per unit dry weight increase, but the proportion of epiphytic species decreases. Some of the possible causes of this increase are discussed. The tephra layers possibly preserved more diatom frustules, or increased diatom growth by supplying silica, phosphorus, and sulphur nutrients directly, or organic matter from vegetation damage in the surrounding catchment. Alternatively, in shallow hardwater lakes, if acids are deposited with the tephra and its fine particles form an impermeable layer on the calcite sediments the lake will become less alkaline and nutrient depleted. 相似文献
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Multiple paternity in the common long‐armed octopus Octopus minor (Sasaki, 1920) (Cephalopoda: Octopoda) as revealed by microsatellite DNA analysis 
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下载免费PDF全文 Multiple paternity was assessed in Octopus minor using microsatellite DNA markers. Octopus minor adults were captured in traps and kept in indoor cement ponds. The females spawned after several days. Ten broods (B1–B10), each containing 15 embryos and the maternal octopus, were maintained until the embryos reached the stage at which DNA could be extracted and used for genotyping. Multiple paternity was tested using five microsatellite DNA markers and the results proved the hypothesis that multiple paternity occurs in O. minor (observed in six out of the 10 broods). Analysis with GERUD software gave the minimum number of fathers and showed that four broods were sired by a single male, three were sired by two different males and three were sired by three different males. In brood B10, the number of fathers identified by the single‐locus method was one fewer than that by the GERUD method. Of the six multiple paternity broods, four (66.7%) showed significant skew from equal paternal contributions, which indicated that sperm competition and/or cryptic female choice may be important for post‐copulatory paternity bias in this species. 相似文献
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海洋蓝洞保留了原始的水体、沉积物、化石残骸和完整的生物骨骼, 是重要的自然遗产和地质奇观, 具有重要的科学研究价值。三沙永乐蓝洞是目前全球已发现的最深海洋蓝洞, 有着独特的洞体结构和水体化学特征, 但其成因仍是未解之谜。本文结合南海的构造演化, 分析了永乐环礁碳酸盐岩台地的发育历史, 认为永乐环礁的形成以加积和退积为主, 其台地边缘属于陡崖型台地斜坡, 有利于发育断层/裂缝; 永乐环礁之上钻井岩心的氧同位素数据表明, 永乐环礁在14.75~168.60m的深度范围内发生了地下水溶蚀作用, 这与实际观测到的158m深洞体转折处之上发生的洞穴垮塌作用相符。通过综合对比分析认为, 三沙永乐蓝洞的形成是断层/裂缝溶蚀机制与深部洞穴垮塌机制综合作用的结果。地下水(淡水、海水)首先沿着台地边缘发育的断层/裂缝进行溶蚀, 在158m以上通过洞穴垮塌作用形成了近垂直的洞穴, 而在158m以下则沿着断层/裂缝继续向下溶蚀形成了略倾斜的深部洞穴结构, 最终由于海平面的上升淹没而形成了蓝洞。本研究可为未来寻找更多海洋蓝洞提供重要的经验与借鉴。 相似文献
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通过异质结界面分析与 AMPS 模拟计算研究了 a-Si:H/c-Si 异质结太阳电池在低温工作、a-Si:H 层低掺杂、高价带补偿以及高界面态时光态 J-V 曲线出现 S-Shape 现象的物理过程,总结了 S-Shape 现象的物理原因.分析结果表明,当空穴输运受到界面势垒的限制时,空穴在 c-Si 界面附近聚集,能带重新分配,c-Si 耗尽区的电场减小,更多的电子从 c-Si 准中性区反转至 c-Si 界面及耗尽区与空穴复合,复合速率显著增大,光电流的损失显著增大,光态 J-V< 相似文献
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Three cores of marine sediments from the Shenhu area in the northern part of the South China Sea were analyzed by XANES analysis for sulfur speciation. The area has been investigated for the presence of hydrocarbons and potential gas hydrate formations. Cored samples of site 4B showed a specific profile of sulfur speciation with sharp and frequent variations in relative contents of sulfate and sulfide, which differed greatly from the profiles obtained for the sediments taken at sites 5B and 6A. The upper part of core 4B (of 0–95 cm) was soft and rich in pore water, containing mainly coarse silt sand. The lower part of the core (i.e., depth > 95 cm) was relatively dryer and darker in color, and dominated by silts and clay resembling sediments from mud volcanoes. The sulfur speciation results revealed that sulfate makes up almost 100 percent of all sulfur species in the upper part of the core 4B, which indicates strong oxidizing conditions, whereas the lower part of the same core has high relative contents of sulfide, sometimes close to 100% S2−. In the lower part of the core, the relative content of sulfide and sulfate changes rapidly and frequently, indicating rapid changes of oxidizing and reducing conditions. On the other hand, the vertical profiles of sulfur species for the cores from sites 5B and 6A are relatively consistent with lower sulfide contents indicative of stable and weaker reducing conditions. We hypothesize that the frequent and sharp variations in the ratios of sulfide to sulfate at site 4B may indicate some intermittent eruption of methane with clay from petroleum reservoirs underneath the sea floor over a relatively short period of time. 相似文献
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华贵栉孔扇贝壳色和闭壳肌颜色具有多态性,其中贝壳的桔黄色表型和闭壳肌的黄色表型具有重要的经济价值,是选择育种中的重要目标性状,对这些性状遗传规律的研究可为选择育种提供理论依据。采用自交、正反杂交和卡方检验方法对华贵栉孔扇贝的桔黄色与枣褐色等2个壳色和黄色与白色等2个闭壳肌颜色的遗传规律进行了研究。结果表明,华贵栉孔扇贝贝壳颜色和闭壳肌颜色均属质量性状,受基因控制,可以遗传,不受环境影响;贝壳桔黄色表型对枣褐色表型为显性;闭壳肌白色表型对黄色表型为显性;壳色和闭壳肌颜色为两个互不连锁的独立性状,在后代遗传过程中可以自由组合,独立遗传,不受母性影响;枣褐色贝壳或黄色闭壳肌个体均为隐性纯合体,其后代性状均与亲代相同;由于不能确定桔黄色贝壳或白色闭壳肌个体属于显性纯合还是杂合,显性纯合家系的获得必须通过建立家系并繁育2代才能实现。 相似文献
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B. K. Diggles 《新西兰海洋与淡水研究杂志》2013,47(4):705-713
A number of pathological abnormalities previously unrecorded in New Zealand fishes are described. A silver trevally (Pseudocaranx dentex) captured from the Bay of Islands exhibited swim bladder ectasia. Black oreo (Allocyttus niger) and smooth oreo (Pseudocyttus maculatus) had cysts of unknown aetiology (CUEs) in the gills at prevalences up to 76% and 81%, respectively, in some fishing areas. The CUEs appear long lived and may have some utility for stock discrimination. A hoki (Macruronus novaezelandiae) with X‐cell pseudotumours in the gill was recorded from the Chatham Rise. Alfonsino (Beryx splendens) had conspicuous Kudoa sp. cysts in the gills at prevalences of up to 28%. Smelt (Retropinna retropinna) from the Waikato River were infected with a xenoma forming, Glugea‐like microsporidian. 相似文献
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J. A. Mills 《新西兰海洋与淡水研究杂志》2013,47(2):326-328
The standard body measurements of 165 freshly killed adult Red‐billed Gulls (Larus novaehollandiae scopulinus) from breeding colonies on the Kaikoura Peninsula are presented. A discriminant function, calculated from bill length and depth at gonys measurements of sexed specimens, applied to captured gulls can correctly sex 90.1% of the gulls which fall within the range of overlap of male and female measurements. 相似文献
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Studying interactions between excavating sponges and massive corals by the use of hybrid cores 下载免费PDF全文
下载免费PDF全文 James K. H. Fang Robert A. B. Mason Christine H. L. Schönberg Ove Hoegh‐Guldberg Sophie Dove 《Marine Ecology》2017,38(1)
Excavating sponges often compete with reef‐building corals. To study sponge–coral interactions, we devised a design of hybrid cores that allows sponges and corals to be arranged side by side with similar size and shape, mimicking the situation of neighbouring organisms. Compared to earlier methods that attached sponge cores onto coral surfaces, hybrid cores provide an opportunity to study organism interactions under conditions more equal to the interacting partners. The use of hybrid cores was demonstrated for the excavating sponge Cliona orientalis and the massive coral Porites, which commonly interact on the Great Barrier Reef. Cliona orientalis and massive Porites were cut into half‐moon shaped explants and combined as hybrid cores under replicate conditions. After 90 days in an aquarium setting, positive growth of Cl. orientalis along with net bioerosion were observed in sponge control cores that combined Cl. orientalis with blank substrate. However, when Cl. orientalis and massive Porites were in contact in interaction cores, the sponge displayed negative growth and undetectable bioerosion, and was slightly overgrown by the coral. Cliona orientalis may have developed tissue extension beneath the living coral tissue, but growth and net calcification rates of massive Porites were apparently not affected by Cl. orientalis when comparing the interaction cores to coral control cores that combined massive Porites with blank substrate. Overall, the present work demonstrated that hybrid cores can be used to generate conditions suitable for studying sponge–coral interactions in the laboratory, which can also be applied in the field. 相似文献
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Spatial scales of mesoscale eddies from GOCI Chlorophyll-a concentration images in the East/Japan Sea 总被引：2，自引：0，他引：2
The spatial scales of mesoscale eddies are of importance to understand physio-biogeochemical processes in the East/Japan Sea. Chlorophyll-a concentration images from the Geostationary Ocean Color Imager (GOCI) revealed numerous eddies during the phytoplankton bloom in spring. These eddies were manually digitized to obtain geolocation information at the peripheries from GOCI images and then least-square fitted to each ellipse. The elliptic elements were the geolocation position of the eddy center, the rotation angle from due east, the eccentricity, the lengths of the semi-major and semi-minor axes, and the mean radius of the ellipse. The spatial scales of eddies had a mean radii ranging from 10 km to 75 km and tended to be smaller in the northern region. The scales revealed a linear trend of about ?7.26 km/°N as a function of the latitude. This tendency depended on the latitudinal variation of the internal Rossby radius of deformation, which originates from the substantial difference in the density structure of the water column. The scales from the sea surface temperature image were larger by 1.30 times compared to those from ocean color image. This implies that physical processes along the periphery of the eddy affect the nutrient dynamics. 相似文献
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Abstract The San Diego Trough Geotechnical Test Area, located about 24 km southwest of San Diego in a water depth of about 1.2 km, lies near the base of the Coronado Escarpment directly north of the Coronado Fan. A new bathymetric map delineates a shallow basin in the soft, highly plastic, clayey silts flooring the Test Area. Measurements of shear strength by vane and static cone pene‐trometer, and bulk density by nuclear densitometer, were made in place from the submersible Deep Quest. Sixteen short (< 1.6 m) gravity cores were collected from ships. The geotechnical properties show little areal variation and generally change uniformly with depth within the 55 km2 Test Area. Silt is the predominant grain size, averaging about 62%. In‐place bulk density shows little change with increasing depth, values range from 1.23 to 1.26 Mg/m3; laboratory density values increase with depth, ranging from 1.30 to 1.52 Mg/m3 between the surface and a depth of about 1.1 m. The difference between the in place and laboratory values may indicate sampling densification of the cored sediment. Water content in the cores decreases uniformly within the range of 249 to 43% dry weight. Shear strength increases linearly with depth. The laboratory shear strength values are lower than the in place values, which range from 4 kPa at the surface to about 29 kPa at a depth of 3.27 m. Predictor equations relate Atterberg limits, bulk density, water content, and laboratory and in place shear strength to depth. Sedimentation‐compression e log p curves have an equivalent compression index of 1.5 to nearly 2. Excluding rurbidite layers and sampling disturbance effects, all cores indicate a uniform depositional environment in the surface to 1.6 m of sediment sampled. The geotechnical properties indicate that the sediments in the west central and southwest parts of the Test Area exhibit vertical heterogeneity due to thin silt‐sand layers, presumably of turbidity current origin, that originated from the Coronado Canyon. 相似文献