福建省主要河口海湾沉积物中甲藻休眠孢囊分类学初步研究

通过对福建省厦门湾、闽江口海域、三沙湾三个主要河口海湾144个站位表层沉积物样品中甲藻休眠孢囊的系统分析,根据甲藻休眠孢囊的形状、外壁结构、颜色、表面修饰物等形态特征共鉴定出9属25种及不定种,并对各孢囊属种的特征进行了分类描述,其中有毒甲藻休眠孢囊2种,即Alexandrium minutun,A. tamarense, 有害种类4 种, 即Alexandrium affine,Lingulodiniumpolyedrum,Scrippsiella trochoide.通过对比表明Alexandrium affine,A. minutum,Diplopelta cf. parva,Polykrikos cf. schwartzii,Protoceratium reticulatum,Protoperidinium minutum,P.cf. minutum,P. cf. americanum以及Alexandrium sp.,Protoperidinium sp.1,P. sp.2等11种甲藻休眠孢囊为本次在福建省海域新发现的种,这些新发现的甲藻种类可能是近年来通过国际间往来的航运船只在我国沿岸海域排放压舱水或贝类引种带来的.     

秋季南黄海表层沉积物中甲藻孢囊分布

2007年秋季(10月)在黄海22个站位采集表层沉积物样品进行甲藻孢囊的种类鉴定与计数,本航次中共鉴定出33种(不包括2个未确定种),优势种是锥状斯克里普藻(Scrippsiella trochoidea)、塔玛亚历山大藻(Alex-andrium tamarense)和膝沟藻属(Gonyaulaxsp.)的种类。与东海和南海甲藻孢囊的同期丰度相比,黄海的相对较低,丰度范围为10~519个/cm3,平均108个/cm3。孢囊丰度总体分布趋势从北向南递增,最高丰度区出现在长江口以北(32°19′59.88″N,122°37′5.16″E),另外,在南黄海调查海域中,中部黄海冷水团区域孢囊丰度较高,膝沟藻成为该区域的优势种,密集中心达101个/cm3。有毒甲藻孢囊在沉积物表层聚集且分布广泛,有爆发赤潮的可能。     

北黄海表层沉积物中甲藻孢囊的分布特征

2009年和2010年采集北黄海15个站位的表层沉积物样品进行甲藻孢囊分析,共鉴定出甲藻孢囊28种(隶属13个属)和2种未定种,优势种为膝沟藻(Gonyaulax spp.)、塔马/链状亚历山大藻(Alexandriumcatenella/tamarense)和微小/相似亚历山大藻(Alexandrium minutu...     

北黄海中部及四十里湾海域甲藻孢囊种类多样性研究

从2008年至2011年,采集了北黄海和烟台四十里湾海域共49个站点的表层沉积物的样品,并对沉积物中的甲藻孢囊进行鉴定。研究发现41种孢囊,隶属于16属：其中,原多甲藻（Protoperidinium?sp.）孢囊Brigantedinium?aymmetricum?Matsuoka为中国海域新记录种。塔马/链状亚历山大藻Alexandrium?tamarense?/?catenella、微小/相似亚历山大藻Alexandrium?minutum?/?affine、网状原角管藻Protoceratium?reticulatum和膝沟藻Gonyaulax?spp.的孢囊是北黄海中部海域孢囊优势种;膝沟藻Gonyaulax?sp.（Spiniferites?bentori?var.?truncata）、具刺膝沟藻Gonyaulax?spinifera（Spiniferites?hyperacanthus）和网状原角管藻P.?reticulatum的孢囊在烟台四十里湾占优势。另外,研究中还发现三种产虾夷扇贝毒素（YTX）甲藻（具刺膝沟藻G.?spinifera、多边舌甲藻Lingulodinium?polyedra和网状原角管藻P.?reticulatum）的孢囊,在芝罘岛到北黄海中部海域都有较高丰度的分布,另三种产麻痹性贝类毒素（PSP）甲藻（塔马/链状亚历山大藻A.?tamarense?/?catenella、微小/相似亚历山大藻A.?minutum?/?affine和链状裸甲藻Gymnodinium?catenatum）的孢囊,在北黄海中部丰度很高。因此,应加强这些海域的甲藻孢囊监测和研究,预防有毒甲藻赤潮的爆发。最后,通过对比分析北黄海中部及烟台四十里湾这两个海域甲藻孢囊分布特征和环境特征的差异,进一步证明了人类活动对近岸海洋生态环境的影响。     

三沙湾海域沉积物中甲藻休眠孢囊的初步研究

通过对福建三沙湾海域50个站位海底沉积物进行研究，共发现9属20种甲藻休眠孢囊。其中，有毒种类2种：Alexandrium minutun、A.tamarense,有害种类4种：Alexandrium affine、Gonyaulax spinifera、Lingulodinium polyedraum、Scripp-siella trochoidea。文中对孢囊的形态与丰度、分布特征进行了初步研究。     

胶州湾表层沉积物中甲藻孢囊的分布

为了解胶州湾表层沉积物中甲藻孢囊的分布特征,于2015年7月采集胶州湾12个站位的表层沉积物进行甲藻孢囊分析,共鉴定甲藻孢囊37种(分属5个类群)和2种未定种,包括自养型20种和异养型17种,优势种为膝沟藻。其Shannon-Wiener多样性指数[H′(log2)]介于2.84—3.91,平均值为3.42;均匀度指数介于0.75—0.98,平均值为0.88,总体值较高。胶州湾海域各站位的甲藻孢囊丰度介于96—969cyst/g DW(干重),平均丰度为401cyst/g DW,呈现出临近湾口处丰度较高,而湾内较低的空间分布差异特征。尤其值得注意的是,有两种产虾夷扇贝毒素(Yessotoxin,YTX)甲藻[具刺膝沟藻(Gonyaulax spinifera)和多边舌甲藻(Lingulodinium polyedrum)]的孢囊和3种产麻痹性贝类毒素(PSP)甲藻[塔玛/链状亚历山大藻(Alexandrium catenella/tamarense)、微小/相似亚历山大藻(A.minutum/affine)和链状裸甲藻(Gymnodinium catenatum)]的孢囊在胶州湾海域大多数站位均有分布,尽管其数量不高,但其广泛的分布范围仍需引起我们的重视。     

桂山岛海域甲藻孢囊的分布与浮游植物休眠体萌发研究

为了了解珠江口桂山岛海域甲藻孢囊的分布及浮游植物休眠体的萌发状况,以揭示赤潮发生潜势,于2009年1月采集了珠江口桂山岛海域表层沉积物样品,对沉积物中甲藻孢囊的种类和数量进行分析,并对浮游植物休眠体进行了萌发试验。结果表明,桂山岛海域甲藻孢囊有21种,原多甲藻类孢囊在种类数上占优势。甲藻孢囊密度较低,为110~315个/g,平均为202个/g,养殖区密度高于非养殖区。异养型甲藻孢囊百分比含量较高,表明了该海域较高的富营养化程度。活体孢囊密度百分比达61.8%,说明表层沉积物中存在大量未萌发的活性孢囊,为赤潮暴发埋下了隐患。萌发的浮游植物种类数较少,为19属22种。20 d和40 d萌发的浮游植物细胞平均密度分别为490个/g和264个/g。萌发的甲藻优势种为Biecheleriopsis adriatica,其次为锥状斯氏藻(Scrippsiella trochoidea);萌发的硅藻主要以中肋骨条藻(Skeletonema costatum)、旋链角毛藻(Chaetoceros curvistus)和舟形藻(Navicula sp.)占优势。桂山岛海域有毒有害甲藻孢囊的广泛分布以及潜在赤潮种类的大量萌发,表明该海域有较高的赤潮发生风险。     

闽江口海域表层沉积物中甲藻休眠孢囊的初步研究

对福建闽江口50个站位的海底沉积物样品进行分析,共鉴定出甲藻孢囊17种,隶属7属,主要的种类有锥状斯氏藻(Scrippsiella trochoidea),科夫／无纹多沟藻(Polykrikos kofoidii／schwartzii)、斯氏膝沟藻(G．scrippsae)和具刺膝沟藻(Gonyaulax spinifera)：锥状斯氏藻为最丰富的种：并检出有毒种塔玛亚历山大藻(Alexandrium tamarense)。研究结果表明,闽江口表层沉积物中的甲藻休眠孢囊主要分布在砂-粉砂-粘土沉积物类型中;有毒甲藻塔玛亚历山大藻有可能在每年5-6月、10-11月对该海域的海洋生物和人类健康及生命安全构成潜在威胁,应加强监测。     

舟山港4艘商船压舱箱沉积物中甲藻孢囊种群结构的分析

为了解商船压舱箱沉积物在海洋水生生物入侵过程中扮演的潜在媒介作用,本文利用光学显微镜观察法,研究了停泊于我国舟山港4艘商船压舱箱沉积物中甲藻孢囊的种类组成、孢囊密度、香农-威纳指数(H′)和PSP原因种,并对甲藻孢囊种群结构进行了相关性分析。结果表明,鉴定出的甲藻孢囊隶属于5大类,共24种,4份样品中甲藻孢囊的种群结构各有差异,但均检测出能产生麻痹性贝毒(Paralytic Shellfish Poisons,PSP)的甲藻孢囊,如亚历山大藻Alexandriumspp.和链状裸甲藻Gymnodium catenatum。在4艘商船的压舱箱沉积物中均检测出有硅藻分布,其中在富成轮压舱箱沉积物中还检测出3种未知种孢囊。通过相关性分析可知,甲藻孢囊H′值与PSP甲藻孢囊密度占总甲藻孢囊密度的比率呈负相关。甲藻可以通过商船压舱箱沉积物为传播媒介,以孢囊形式来扩大其生物地理分布,提高甲藻物种多样性可有助于降低PSP甲藻的破坏风险。因此,有效处理船只压舱箱沉积物、积极保护当地海洋生物物种多样性,对于降低外来甲藻物种(特别是一些有毒有害种)的赤潮风险和保持当地海洋生态系统的平衡,具有十分重要的意义。     

湄洲湾海域甲藻孢囊的时空分布初步调查

为了解湄洲湾海域表层沉积物中甲藻孢囊的时空分布特征,于2018年5月(春)、8月(夏)、11月(秋)和2019年2月(冬)采集湄洲湾海域7个站位表层沉积物样品,进行甲藻孢囊分析,共鉴定出甲藻孢囊6大类42种和2种未知种。异养型甲藻孢囊种类数和丰度均高于自养型甲藻孢囊,其中又以原多甲藻类孢囊的种类和丰度最高。季节间差异不明显:种类数介于34～38种之间,丰度则在397.8～569.5 cysts/g之间变化,全年平均丰度448.0 cysts/g。工业区附近的站位种类数和丰度均低于养殖区附近的站位和对照点。优势种高达16种,原多甲藻类占绝对优势,但全部优势种优势度均不大。多样性指数、丰富度指数和均匀度指数均较高,全年的平均值分别为3.45、1.55和0.92。与历史资料对比,新发现19种孢囊,但丰度相差不大。另需注意的是,在湄洲湾海域共发现6种有毒甲藻孢囊,虽然全年丰度均不高,但仍有暴发有毒赤潮的危险,需引起重视。     

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.     

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.     

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.