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Bacteria abundance, chlorophyll a, ATP and POC concentrations and respiration rates of microorganisms in the Changjiang Estuary and the plume were determined in July 1986. The high values of bacteria abundance occurred in the river mouth in association with suspended matter. It is assumed that bacteria were the major contributor to ATP and the main consumer of dissolved oxygen, and that the relationship between ATP and POC was present in that area. In the dilution zone (salinity; 25-30), instead of bacteria, phytoplankton was the major contributor to ATP and respiration rates, due to diatom bloom. Close relationships between Chi a and ATP, and ATP and POC were observed. Contribution of microbial carbon to POC was also estimated. 相似文献
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Abstract Phosphorus and nitrogen were measured in stream run‐off from the four catchments of the Taita Experimental Basin (41° 11′ S, 174° 58′ E). The land is used as exotic conifer forest, native forest, and hill pasture. Multiple regression analysis was used to estimate chemical losses per unit area in floods and at low flows. At low flows, the hill pasture (fertilised with lime at 630 kg·ba?1·y?1, and superphosphate at 380 kg·ha?1·y?1) tended to lose more phosphorus and nitrate than the forested land, but differences were small, and not always significant. During large floods, the hill pasture (No. 5 Catchment) lost about 3 times as much reactive phosphate and 2–5 times as much total phosphorus as the forested land, and 130–190 times as much nitrate as land in the Exotic Forest and Native Forest 2 Catchments. Nitrate losses from land in the No. 4 Catchment (mainly native forest) were as high as those from the hill pasture, so high nitrate loss is not associated solely with agriculture. Losses of total phosphorus via the catchment streams were estimated as: No. 5 Catchment (hill pasture), 293 g·ha?1·y?1; Native Forest 2 Catchment, 201 g·ha?1·y?1; No. 4 Catchment, 124 g·ha?1·y?1; Exotic Forest Catchment, 71 g·ha?1.y?1. Nitrate‐N losses were estimated to have been 1356 g·ha?1·y?1, 11.5 g·ha?1·y?1, 1436 g·ha?1·y?1, and 44 g·ha?1·y?1 respectively. Phosphorus and nitrate concentrations were similar in the Exotic Forest and Native Forest 2 streams, but the Exotic Forest tended to lose smaller amounts because it yielded about 50% less water per unit area. Over the 2‐y study, an estimated 47–70% of phosphorus losses and up to 83% nitrate losses occurred in large floods; 31% and 48% respectively were apparently lost from the hill pasture catchment in a single flood. Less than 20% of estimated phosphorus losses and as little as 1% of nitrate losses occurred at low flows. Run‐off of phosphorus and nitrate was spasmodic, and this should be considered in assessing the impact of surface run‐off on the biology and chemistry of receiving waters. 相似文献
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Ariyoshi Keisuke Kuwano-Yoshida Akira Chi Wu-Cheng 《Marine Geophysical Researches》2019,40(4):451-451
Marine Geophysical Research - 相似文献
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Abstract A cross‐correlation matrix was computer developed to investigate the statistical dependence of geotechnical properties on other properties as an aid to learning why such dependence exists. Linear correlation coefficients, based on 10,000 data values from borings in four major basins along the axis of the Oslofjorden, and one boring at the south end of the Dramsfjorden, are presented for 17 measured or calculated geotechnical and geochemical parameters. Confidence levels of 99 percent and 99.99 percent were calculated for all parameters, and causative and fortuitous relationships or linkages were investigated using regrouped matrices showing correlations significant at the 99.99 percent confidence level. A table summarizes parameters correlating in both fjords, only in the Oslofjorden, only in the Dramsfjorden, and in neither fjord. Generally, relationships were as expected. Examples of unexpected absence of correlations follow: In the Oslofjorden, the clay‐size fraction and the plastic limit correlated only with the activity and the liquid limit, respectively. The lack of correlation with other parameters may be related to the character of the clay‐size fraction. In the Dramsfjor‐den, the sensitivity did not correlate with any other parameter, which may be related to the anoxic soils found in this fjord. 相似文献
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Saul B. Saila 《Marine Geology》1975,18(3):139-157
A bathymetric survey of the Gilliss Seamount, in the northwest Atlantic Basin, using a multi-beam sonar array system reveals an extremely complex morphologic character of this feature. A new chart provides the most detailed topographic presentation of an Atlantic seamount published to date and highlights the similarity of the Gilliss Seamount with terrestrial strata-volcanoes. Bottom photographs and samples reveal pillow-Iava formation. Seismic profiles show that the volcanic basement is irregularly covered by acoustically transparent deposits that are as much as 668 m thick. Volcanic debris and sediments locally are displaced down the flanks of the seamount. Bottom photographs and cores indicate that the transparent layer has accumulated slowly by deposition from suspensate-rich (mostly clay and planktonic foraminifera) water masses that flow around the mid to lower sectors of this submarine volcano. Bottom-current activity also modifies the abyssal plain turbidite-hemipelagic sequence surrounding the seamount. 相似文献
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The achievement progresses of investigation and studies on marine hazardous geology are summarized and presentsd in the late 20 century in China. The importance, research value and presentday studies of marine hazardous geology, a newly developing branch of geoscience, are well expatiated.Several often confused concepts and theories are explained and redefined here. The comment on the means of investigations, assessment of marine hazardous geology, as well as its evolution, innovation,existing questions and future tasks are also introduced and presented. The concepts of “hazard geology“,“geohazard“, “map of marine hazard geology“, “integrated evaluaton on seafloor stablity“ are respectively discussed, including their definition, research objects, methods and contents. The types and classification of marine hazardous geology, principles and methods of marine hazardous geology map compilation, the assessment methods and models of marine hazardous geology environment and seafloor stability and so on are also discussed. 相似文献
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Nitrous oxide concentration and nitrification and denitrification in Zhujiang River Estuary, China 总被引：1，自引：0，他引：1
1 Introduction Estuaries have been subject to intense anthro- pogenic influences over recent decades by inputs of ni- trogen as a consequence of fertilizer usage and sewage/waste input (Howarth et al., 1996). Thus, the capacity of an estuary to buffer or alleviate additional nutrients is of importance in modifying the load of ni- trogen in the marine ecosystem. The role of microor- ganisms in regulating fluxes of nitrogen from land to sea through estuaries has received increased attention (Ni… 相似文献
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Genetic diversity and specific markers in four scallop species, Patinopecten yessoensis,Argopecten irradians, Chlamys nobilis and C.farreri 总被引：1，自引：0，他引：1
The AFLP （amplified fragrnent length polymorphism）technique was used to analyse the genetic diversity in four scallop species, Patinopecten yessoensis, A rgopecten irradians, Chlamys nobilis and C. farreri. The genetic similarity indexes of these four species are 0.8415, 0.7863, 0.7190 and 0.6731, while Shannon diversity indexes are 43.52, 58.87, 80.16 and 92.83, respectively. As analyzed, the genetic diversities in two native species, i.e., C, farreri and C. nobilis, are higher than those in other two introduced species, A. irradians and P. yessoensis. The results also showed that C. nobilis and C, farreri shared the most common loci. The genetic distance indicated that C. nobilis and C. farreri are closely related. Moreover, out of 510 AFLP markers, 21 specific bands are found to distinguish the four species scallops and these markers may be applied to the specific germplasm characterization and molecular assistant classification in scallops. 相似文献
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Barremian–Aptian organic-rich shales from Abu Gabra Formation in the Muglad Basin were analysed using geochemical and petrographic analyses. These analyses were used to define the origin, type of organic matters and the influencing factors of diagenesis, including organic matter input and preservation, and their relation to paleoenvironmental and paleoclimate conditions. The bulk geochemical characteristics indicated that the organic-rich shales were deposited in a lacustrine environment with seawater influence under suboxic conditions. Their pyrolysis hydrogen index (HI) data provide evidence for a major contribution by Type I/II kerogen with HI values of >400 mg HC/g TOC and a minor Type II/III contribution with HI values <400 mg HC/g TOC. This is confirmed by kerogen microscopy, whereby the kerogen is characterized by large amounts of structured algae (Botryococcus) and structureless (amorphous) with a minor terrigenous organic matter input. An enhanced biological productivity within the photic zone of the water columns is also detected. The increased biological productivity in the organic-rich shales may be related to enhanced semi-arid/humid to humid-warm climate conditions. Therefore, a high bio-productivity in combination with good organic matter preservation favoured by enhanced algae sizes are suggested as the OM enrichment mechanisms within the studied basin. 相似文献
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The European Common Fisheries Policy (CFP) has failed to deliver on social, economic and ecological goals. This failure is in part the result of a number of social–ecological feedback mechanisms. The policy is currently undergoing reform, with unknown practical outcomes. Here, relatively successful fisheries policies outside the European Union are reviewed. Through interviews and workshops with scientists, managers and other stakeholders, complemented with literature reviews, practices that can create incentives for long-term sustainability are investigated. The focus is on how the provision of clear and trusted scientific evidence can stimulate defensible decisions, in turn creating incentives for compliance, leading to positive social–ecological outcomes. Despite differences between Europe and the investigated case studies, the prospects of an increased regionalization within the European CFP provides the best starting point for implementing best practice identified in this study. 相似文献
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The observation and estimation of directional spectra of sea waves is one of the essential subjects of study of oceanic dynamics. On the basis of the irregular linear wave theory, estimation methods for i/UV, PUV and VV directional wave spectra are derived. By using ij and PUV data measured in-situ, directional wave spectra are estimated, meanwhile the virtues and defects of various spectra are comparied. This method provide a basis for the observations of sea waves. 相似文献
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A study of coccolith assemblages from a box core from the central South Yellow Sea(SYS) was performed revealing fluctuations on their relative abundance(%) that can be related to climatic and hydrographic changes over the last 230 years(1780–2011). Total coccolith abundances ranged from 7.0 to 55.1×10~6 coccoliths·g~(-1)sediment. Although the abundance of different species varied widely throughout the core, seven taxa dominated the assemblage. Among these species, Gephyrocapsa oceanica was the most dominant species, and it showed an average percentage of 50.1%. The pattern of G. oceanica(eutrophic species) was opposite to that of the combined percentage of Braarudosphaera bigelowii and Umbilicosphaera sibogae(both oligotrophic species), indicating that in the Yellow Sea(YS), the distribution pattern of G. oceanica might be characteristic of nutrient availability.Similar patterns between G. oceanica and the Siberian High were observed on an inter-decadal time scale,indicating that the East Asian Winter Monsoon(EAWM) may be an important driver of ecological changes in the YS. When the EAWM prevails, both the Yellow Sea Coastal Current(YSCC) and Yellow Sea Warm Current(YSWC)strengthen, and the increasing nutrient availability and warmer water brought by the strengthened YSWC favor eutrophic and warm-water coccolithophore species, such as G. oceanica. This likely mechanism demonstrates that coccolith assemblages can be used as benign and reliable proxy for climate change and surface oceanography. 相似文献
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The Bonnet Carré Spillway, located 28 miles northwest of New Orleans, was constructed in the early 1930s as part of an integrated
flood-control system for the lower Mississippi River system. From 11 April to 8 May 2008, Mississippi River water was diverted
through the spillway into the 629-square-mile Lake Pontchartrain, which is hydraulically connected to the Gulf of Mexico.
On 8 April, prior to the opening of the spillway, water-quality instruments were deployed and recorded hourly measurements
of water temperature, dissolved oxygen, specific conductance, pH, and nitrate. Discrete water-quality and phytoplankton (algae)
samples were collected in Lake Pontchartrain from 8 April to 3 October 2008 to assess the water-quality nutrient enrichment
effects of the diversion on the lake. The maximum influence of river water in the southern portion of the lake was captured
with continuous (hourly) monitoring of nitrate concentrations, and field measurements such as of specific conductance during
the critical period in late April to early May. By late May, the deployed instruments had recorded the arrival, peak, and
decline of selected constituents associated with the freshwater influx from the Mississippi River/Bonnet Carré Spillway diversion.
The continuous monitoring data showed the short-term interactions of high-nitrate, low-specific conductance river water and
low-nitrate, high-specific conductance lake water. The phytoplankton community composition, as an indicator of water quality,
illustrated an extended response from the river water evident even after the continuous and discrete samples indicated that
the lake had returned to pre-diversion conditions. The initial phytoplankton community response to nutrient increases was
related to accumulations of diatoms. During periods of low nutrient concentrations, accumulations of blue-greens occurred
by July and August. As blue-green algae cell densities and biovolumes increased in the summer, so did the species richness
of blue-green algae, particularly the harmful algae bloom taxa. Cell densities and biovolume of the phytoplankton lake indicator
taxa Skeletonema costatum, Anabaena sp., and Cylindrospermopsis raciborskii were highest and dominated the diatom and blue-green algae communities during the period of most river water influence on
the lake and immediately following the freshwater inflows. The dominance and recession of these indictor taxa reflect the
dramatic changes that occurred in the phytoplankton community in response to an increase in nutrient-rich freshwater from
the diversion into the lake, and not normal seasonal phytoplankton compositional differences. Water-quality data indicated
a gradual reversion to pre-diversion lake conditions by June to July, but shifts in the phytoplankton composition were still
evident through August 2008. Observations from this study were similar to results from previous studies of Mississippi River/Bonnet
Carré Spillway diversion opening in 1997. 相似文献
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Demidov A. B. Gagarin V. I. Artemiev V. A. Arashkevich E. G. Makkaveev P. N. Shchuka S. A. Khrapko A. N. Grigoriev A. V. Vorobieva O. V. Konyukhov I. V. Fedorov A. V. 《Oceanology》2020,60(2):189-204
Oceanology - The vertical distribution of phytoplankton primary production (PP) and chlorophyll a (Chl) was studied based on the data carried out in August–September 2015, 2017, and 2018. The... 相似文献