基于连续型时滞差分模型的南大西洋长鳍金枪鱼资源评估

南大西洋长鳍金枪鱼群体是全球资源状况维持较好的金枪鱼群体之一,剩余产量模型(Surplus production model, SPM)、年龄结构模型(Age-structured population model, ASPM)和贝叶斯产量模型(Bayesian surplus production model, BSPM)等都已成功运用于该群体的资源评估。连续型时滞差分模型(Continuous delay-difference model, CTD-DM)是在时滞差分模型(Delay-difference model, D-DM)基础上考虑了生物过程充分时间延迟构建起来的模型,比起ASPM需要较少的数据,并且比SPM更具有生物学意义。本文在离散型D-DM基础上构建了CTD-DM,并应用在南大西洋长鳍金枪鱼渔业数据中。结果显示,CTD-DM评估的最大可持续产量(Maximum Sustainable Yield, MSY) 80%置信区间为21510-23118 t (中值22398 t),较ASPM和SPM等MSY评估结果偏保守。相对生物量B_(2011)/B_(MSY)和相对捕捞死亡系数F_(2011)/F_(MSY)分别为1.45和1.04,当前该群体相对资源量水平较好,但是相对捕捞死亡系数较高;BSPM和CTD-DM的风险评估结果显示,当捕捞死亡率均等于0.2时在2025年取得最大持续产量,考虑到当前渔业持保守态度和预防性策略的理念,建议捕捞死亡率应控制在0.15以内。     

渔业产量和资源生物量数值模型及相关因子的初步研究

对于渔业的中长期预报计算,是渔业种群补充的关键问题。本文在单位补充量产量和单位补充量生物量模型中加入了亲体一补充模型即密度相关过程,并引入了白色噪音以模拟环境变化。结果表明：本研究(1)可以明确地给出渔业种群崩溃的可能性,估计出达到崩溃时的捕捞死亡率;(2)可以估计最大持续产量的绝对值;(3)引入的白色噪音可以模拟环境变化对产量与捕捞死亡率和产量与亲体生物量关系曲线的影响。虽然亲体补充关系仍多是个假设,补充与亲体之间存在的补偿机制需要进一步的研究。     

基于环境因子的西北太平洋秋刀鱼资源量评估研究

太平洋秋刀鱼(Cololabis saira)资源量波动易受海洋环境,尤其是海表温度(SST)变化的影响。本文假设产卵场最适SST范围(P_s)影响环境容纳量(K),索饵场最适SST范围(P_f)影响内禀自然生长率(r),利用2003—2014年西北太平洋渔业数据,建立了基于海表温度的剩余产量模型(EDSP),评估西北太平洋秋刀鱼资源量。研究显示,根据偏差信息准则(DIC)值,基于产卵场海表温度的剩余产量模型(P_s-EDSP)为最优模型。在P_s-EDSP中,最大可持续产量(MSY)为208.56×10~4 t,B_(MSY)水平的生物量为71.46×10~4 t。西北太平洋秋刀鱼的捕捞死亡率为0.15,低于目标水平和MSY水平的捕捞死亡率(F_(tar),F_(MSY)),当前资源生物量高于B_(MSY)。研究结果表明,目前西北太平洋秋刀鱼未遭遇过度捕捞,在其资源评估和管理中应适当考虑产卵场海表温度环境因素。     

厦门海域渔业资源评估

以初级生产力和渔业统计资料为材 ,分别应用Tait沿岸海域生态系能流分析法、营养动态法和Cushing等 3种模式 ,估算厦门沿岸海域的渔业资源自然生产量。同时 ,分别应用Schaefer和Fox两种剩余产量模式估算最大持续产量和最大持续捕捞力量。前 3种模式估算该海域的资源生产量分别为 2 0 1 0 5t,1 8463t和 1 7489t,平均 1 8686t。后两种模式估算最大持续产量平均值分别为 9639t和 91 0 4t。估算的最大持续捕捞力量 :5种作业综合总功率为 1 5976kW ;以厦门机定置渔船单位功率渔捞效率为标准估算的总功率为 2 7351kW ;以厦门机刺网渔船单位功率渔捞效率为标准估算的总功率为 432 1 3kW。 1 997年实际渔获量和捕捞力量均超过了估算的最大持续产量和最大持续捕捞力量。文中还讨论了捕捞力量的调整问题。     

基于环境因子的东海马鲛鱼(Scomberomorus Niphonius)资源量评估

东海马鲛鱼(Scomberomorus Niphonius)的种群动态易受海洋环境条件的影响,在其资源评估和管理中需要考虑海洋环境条件的作用。假设马鲛鱼产卵场最适海表温度10～19℃(Suitable SST,Tsui)范围会影响种群环境容纳量(K),因此分别使用产卵季3月最适表温范围比值(Tsui-Mar)、4月最适表温范围比值(Tsui-Apr)和3、4月份最适表温范围比值的平均值(Tsui-Ave)作为剩余产量模型的环境因子,构建三种基于环境因子的剩余产量模型(environmentally dependent surplus production,EDSP),分别为Tsui-MarEDSP、Tsui-Apr-EDSP和Tsui-Ave-EDSP,利用贝叶斯估计模型参数,结果显示Tsui-Mar、Tsui-Apr、Tsui-Ave三个基于环境因子的EDSP模型偏差信息标准(deviance information criterion,DIC)值小于传统的剩余产量模型的DIC值,其中Tsui-Ave-EDSP模型DIC值最小,精度最高,估计的最大可持续产量(maximum sustainable yield,MSY)的范围为8.125×106～8.371×106 t,资源量(biomass)范围是1.429×106～1.455×106 t,从1994年到2015年,马鲛鱼的捕捞死亡率远低于目标死亡率(Ftar)和MSY水平捕捞死亡率(FMSY),种群资源量高于MSY水平资源量(BMSY)。东海马鲛鱼没有被过度捕捞或未发生过度捕捞,基于EDSP模型中的管理参考点更为保守,建议日后东海马鲛鱼的种群评估和管理应考虑产卵场环境条件。     

东海北部三疣梭子蟹资源评估与管理决策分析

三疣梭子蟹(Portunus trituberculatus)是中国东海北部海域重要的经济蟹类,对三疣梭子蟹资源开展评估是其可持续利用的基础。本文运用基于贝叶斯方法的Schaefer剩余产量模型,对东海北部海域的三疣梭子蟹资源进行评估,确定了当前三疣梭子蟹资源的开发利用状态,估算了在不同收获率水平下未来10年三疣梭子蟹的生物量和年总可捕捞量,分析了管理策略实施后三疣梭子蟹资源崩溃的风险。研究显示,在基准方案和敏感性分析方案下模型参数预测值以及生物学参考点估计值比较相近。使用两种方案估算得到的最大可持续产量(MSY)均约为24×10⁴ t, MSY对应的生物量B_MSY均约为252×10⁴ t。在基准方案下,MSY对应的捕捞死亡系数F_MSY为0.096;在敏感性分析方案下,MSY对应的捕捞死系数F_MSY为0.097。在2001—2020年间,捕捞死亡系数均低于F_MSY,且生物量基本在B_MSY水平之上,表明近年来三疣梭子蟹未出现过度捕捞的情...     

中国近海三种重要渔业资源的生物学参考点评估

中国近海大多数渔业都属于数据有限渔业,用对数据要求较高的复杂模型无法对这些渔业资源做出有效评估,因此用数据有限评估模型评估渔业资源的研究具有重要意义。本文使用经典剩余产量模型(CEDA和ASPIC)和两种新型有限数据评估模型(贝叶斯Schaefer剩余产量模型(BSM)和蒙特卡洛MSY估算模型(CMSY)),评估了黄渤海鳀鱼(Engraulis japonicus)、东海带鱼(Trichiurus lepturus)和南海金线鱼(Nemipterus virgatus)这三种重要渔业资源的生物学参考点和资源现状。研究表明:黄渤海鳀鱼MSY估计值为80×10~4～83×10~4 t,生物学参考点F/F_(MSY)估计值小于1.0而B/B_(MSY)略小于1.0,表明这种渔业捕捞强度适中但资源尚未得到完全恢复。东海带鱼MSY估计值为58×10~4～64×10~4 t,F/F_(MSY)估计值大于1.0而B/B_(MSY)估计值小于1.0,表明这种渔业存在过度捕捞且资源已经衰退。南海金线鱼MSY为30×10~4～32×10~4 t,F/F_(MSY)估计值大于1.0而B/B_(MSY)估计值小于1.0,表明这种渔业存在过度捕捞且资源已经衰退。以上4种模型均可适用于中国近海数据有限的渔业资源,但两种经典剩余产量模型对三种渔业数据的拟合不够稳定(相关系数R~2波动较大),因此取BSM和CMSY模型的评估结果作为重要参考,但这两种有限数据评估模型的拟合效果尚需进行深入研究。     

牙鲆种群动态及其资源管理

本文根据1980—1986年间鱼类生物学参数测定,结合体长分布资料的模拟分析,研究黄、渤海区牙鲆种群年龄结构、死亡动态以及在不同年龄和死亡率条件下世代资源生物量变化的规律。模型分析结果表明,当F=1.0和t_c=6.0a时,单位补充量最大群体产量为1492g。由此认为,现阶段牙鲆资源利用的最佳策略是通过增殖放流,增加资源补充;同时应适当控制捕捞压力,减少渔具对幼鱼资源的破坏并增设繁殖保护区,以追求最大持续产量。     

剩余产量模型在不同渔业中的应用

剩余产量模型因其简单和所需数据较少的特点为渔业资源评估广泛采用.本文应用目前常用的四种剩余产量模型对五种渔业下的渔业生物种群及北大西洋箭鱼种群xiphias gladius评估效果作了比较.四种剩余产量模型在渔业1中的评估效果较好,而在渔业2中的效果较差;Schnute模型在充分捕捞的渔业,如渔业3、4、5,尤其是在低生物量的渔业3中评估效果较好,但不适合评估未充分捕捞的渔业.Walters-Hilborn模型(W-H模型)适用于各种渔业,尤其是渔业1、4、5.在过度捕捞渔业中如渔业3、4,模型对参数q的估计较其它参数接近真值.在北大西洋箭鱼(xiphias gladius)渔业的评估中,W-H模型对MSY的估计约为14000吨,接近于Prager(1996)的结果.     

南海北部金线鱼最大可持续产量和总可捕量的研究

限额捕捞试点工作逐步展开,预示着我国海洋渔业管理进入全面有序的管理时代。文章根据2008—2017年南海北部渔港渔业生产抽样调查数据,统计出南海北部金线鱼的产量主要来自刺网,占累计总产量的72.90%。剩余产量模型分析认为南海北部金线鱼的最大可持续产量在168 632.99~31 0518.85 t,平均为251 765.59 t。2017年实施最严格的休渔制度后,当年的捕捞努力量投入和渔业产量均未超过最适值,当前总可捕量可设为158 515 t。文章研究结果可为该鱼种限额捕捞政策实施提供参考。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

A Review of Some Environmental Issues Affecting Marine Mining

This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement.     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments.     

Deep-Sea Sediment Compression Curves: Some Controlling Factors, Spurious Overconsolidation, Predictions, and Geophysical Reproduction

Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.