青岛潮间带大型底栖海藻群落的研究

在青岛潮间带布设了显浪咀、太平角和石老人3个断面,进行了为期1 a(2006年8月～2007年11月)的大型底栖海藻资源调查研究.结果表明:1. 青岛潮间带大型底栖海藻群落的种类组成中红藻种类最多,其次是褐藻,绿藻最少.2. 群落中大型底栖海藻的生物量有明显的季节变化:春季>夏季>秋季>冬季;生物量在垂直分布上表现出中、低潮带均大于高潮带;在水平分布上无明显差异.3. 底栖藻类群落优势种无季节性变化,第一优势种为孔石莼.4. 采集到大型底栖海藻43种,其中红藻门22属24种,占55.8%;褐藻门9属11种,占25.6%;绿藻门6属8种,占18.6%.     

南长山岛岩岸潮间带底栖藻类群落结构的季节变化格局

南长山岛岩岸潮间带底栖藻类群落的种类组成存在显著的季节差异,4个季节的群落共有种为8种:孔石莼、海黍子、石花菜、江蓠、叉枝藻、小石花菜、叉枝伊谷草和瘤枝凹顶藻。4个季节群落中生物量的变化为:秋季>夏季>冬季>春季。绿藻和褐藻类群主要为暖温性种类,而红藻类群比较复杂,既有暖温带、温带和亚热带性种类,也有寒温带的冷水性种类。4个季节群落的物种优势度序列存在明显的差异,海黍子在春季、夏季和冬季3个群落为第一优势种,瘤枝凹顶藻在秋季为第一优势种。不同季节群落多样性指数变化如下:物种丰富度指数,春季>秋季>冬季>夏季;物种多样性指数,冬季=秋季>春季>夏季;均匀度指数,冬季=秋季>春季>夏季。群落的多样性由红藻类群控制。     

烟台潮间带大型底栖动物群落组成和结构研究

根据2009年11月至2010年8月对烟台3种典型潮间带的大型底栖动物调查,分析了烟台典型潮间带大型底栖动物的群落结构特征,包括群落种类组成、丰度和生物量、优势种、多样性等,采用MDS和CLUSTER分析了大型底栖动物的群落结构,并用AMBI和m-AMBI对底栖群落和环境质量进行了评估。结果表明:本次调查共鉴定出大型底栖动物111种,其中多毛类动物40种,甲壳动物37种,软体动物29种,棘皮动物1种,鱼类2种,其他动物2种(包括纽虫和腔肠动物各1种)。多毛类动物和甲壳动物占据了研究区域底栖群落的主要成分,两者分别占据了群落总种数的36.04%和33.33%。从季节来看,3种类型潮间带物种数均为冬季最低,而秋季则普遍处于较高水平。物种丰度在3种类型潮间带的分布为泥沙质的渔人码头泥质的养马岛沙质的辛安河口,3种类型潮间带的丰度主要贡献者分别为甲壳动物、软体动物和多毛类动物。渔人码头和辛安河口的生物量均以秋季为最高,而养马岛在冬季达到最高,且远高于其他3个季节;软体动物是3种不同类型潮间带生物量的主要贡献者。烟台3种类型潮间带出现的优势种多达15种,但多数优势种仅在某个潮间带的单个季节出现,优势种受季节和潮间带类型的影响明显;日本大螯蜚(优势度为0.29~0.82)是渔人码头全年的优势种,中型阿曼吉虫则是辛安河口的主要优势物种,养马岛的优势物种则为养殖逃逸的菲律宾蛤仔。与以往历史资料相比,烟台潮间带大型底栖动物已经受到了人类活动的深刻影响,原有的潮间带经济种类已经严重退化或消失。     

山东省荣成市月湖海草场底栖藻类群落结构的初步研究

海草生态系统是重要的海洋生态系统之一,而底栖藻类是海草生态系统中的组成部分,具有十分重要的生态功能。2013年1月、4月、7月和10月在荣成月湖草场的三个断面上对其中分布的大型底栖藻类进行了随机取样调查,并对不同季节底栖藻类的群落结构进行比较分析。结果显示,共鉴定出大型藻类16种,隶属3门13属,其中红藻门2属2种,棕色藻门褐藻纲4属4种和绿藻门7属10种;草床和空斑内的藻类季节变化均显著(P=0.000,P=0.008),春季草床内底栖藻类种数最多(13种),秋季S3断面的草床内底栖藻类生物量最高(2191.44±1021.16)g·m~(-2),冬季三个断面的空斑内和夏季S2断面的空斑内为发现底栖藻类;大多数情况下,各断面上草床内Shannon-Wiener多样性、Pielou均匀度和Margalef丰富度指数均大于相应断面上空斑内的值;聚类和排序结果显示,在一年四季中底栖藻类群落结构在草床内和空斑内大都呈显著差异。结果表明,季节变化和海草分布特征对底栖藻类的群落结构有着重要影响。     

下三横山岛潮间带大型海藻群落构成及季节变化

为发展多营养层级综合养殖系统（IMTA）,2019年对浙江嵊泗列岛下三横山岛养殖海区潮间带底栖大型海藻周年群落构成及时空特征进行调查分析。结果显示：研究区域共采集到36种大型海藻,包含24种红藻、4种绿藻以及8种褐藻,且群落结构季节性变化显著。鼠尾藻（Sargassum thunbergii）、羊栖菜（S. fusiforme）、石莼（Ulva lactuca）、带形蜈蚣藻（Grateloupia turuturu）、复生凹顶藻（Laurencia composita）所有调查站位均有出现,为该海区的优势种,且鼠尾藻四季皆为优势种。大型海藻群落的丰富度指数（D）、多样性指数（H′）、均匀度指数（J′）的年均值分别为0.81、1.85、2.33,且季节变化明显。优势种Pearson相关分析显示：带形蜈蚣藻、复生凹顶藻生物量与叶绿素a、温度和盐度呈极显著相关,舌状蜈蚣藻（G. livida）、角叉菜（Chondrus ocellatus）生物量与溶解氧呈极显著正相关,珊瑚藻（Corallina officinalis）生物量与溶解性无机磷和pH呈极显著正相关,铜藻（S. horneri）生物量与温度呈显著负相关,石莼生物量与化学需氧量、pH、盐度和叶绿素a呈显著相关,羊栖菜生物量与化学需氧量呈极显著正相关。具经济价值的优势种（鼠尾藻、羊栖菜、石莼）可作为IMTA系统大型海藻候选种。     

山东长岛潮间带大型底栖动物生态特征研究

2015年11月(秋季)、2016年2月(冬季)、2016年6月(春季)、2016年9月(夏季)大潮期间对山东长岛列岛中南长山岛和北长山岛的3个不同底质类型的潮间带采样点进行了系统的大型底栖动物调查,研究了其数量特征和季节变化,包括群落种类组成、密度和生物量、优势种、物种多样性等,结果表明:本次调查共鉴定出大型底栖动物隶属7个门,共81种。其中环节动物门多毛类动物25种,软体动物门25种,节肢动物门22种,棘皮动物门6种,其他类群共3种(包括纽虫、腔肠动物和鱼类各1种)。潮间带大型底栖动物平均密度为118.97 ind./m~2,软体动物和甲壳动物占据了研究区域底栖群落的密度主要成分,两者分别占比为39.58%和36.68%。各采样点平均密度为北长山岛(BCS)(141.17 ind./m~2)避险角(NCS1)(122.33ind./m~2)明珠广场东(NCS2)(93.42ind./m~2);各采样点平均生物量为128.03g/m~2,软体动物和甲壳动物占据了研究区域底栖群落的生物量主要成分,两者分别占比为58.56%和35.32%。平均生物量北长山岛(BCS)(234.95g/m~2)避险角(NCS1)(99.99g/m~2)明珠广场东(NCS2)(49.13g/m~2)。从季节来看,各站点的物种数、平均密度和生物量季节变化的规律性不明显,总体为秋、春季较多,夏、冬季较少。3个站点物种多样性指数(H′)、丰富度指数(D)和均匀度指数(J′)平均值分别为2.30、1.99和0.79,各潮区中,均为中潮带低潮带高潮带,各季节变化不明显。优势种受底质类型和季节变化的影响明显,没有在各站点和季节均为优势种的种类,主要的优势种有平背蜞(Gaetice depressus)、绒螯近方蟹(Hemigrapsus penicillatus)、短滨螺(Littorina brevicula)等。与以往历史资料相比,长岛潮间带生物出现了一定变化,种类和数量减少,与烟台近岸潮间带大型底栖动物种类组成差别很大。     

庙子湖岛和黄兴岛夏季岩礁潮间带大型底栖动物群落格局

于2009年8月21-22日期间同步调查庙子湖岛和黄兴岛两个岩礁潮间带断面的大型底栖动物种类组成,并分析其群落格局。结果表明,庙子湖岛采集的样品中共有4门28种大型底栖动物,黄兴岛的则有5门37种大型底栖动物;两断面底栖动物群落以广温广布种和亚热带种为主,软体动物作为绝对优势类群主导其分布特征;总平均栖息密度、总平均生物量表现为庙子湖岛＞黄兴岛,种类数及生物量分布均表现为中潮带＞低潮带＞高潮带,栖息密度分布则表现为中潮带＞高潮带＞低潮带;物种多样性指数和物种丰富度指数均为黄兴岛＞庙子湖岛,两断面高潮带的群落生态指数相对中、低潮带较低;大型底栖动物ABC曲线分析表明,庙子湖岛底栖动物群落未受到污染或扰动,黄兴岛底栖动物群落则受到了中等程度的污染或扰动。     

青岛三种岩礁海藻附植小型底栖生物的初步研究

2013年6月-2014年6月对青岛岩礁潮间带鼠尾藻、孔石莼、蜈蚣藻附植小型底栖生物进行了连续13个月的逐月采样,对小型底栖生物的丰度、生物量、生产量、类群组成及其季节动态进行了研究。共鉴定出小型底栖生物16个类群。鼠尾藻附植小型底栖生物的年平均丰度和生物量分别为7×103 ind·g-1 dwt algae·a-1和56×103μg·g-1 dwt algae·a-1。孔石莼附植小型底栖生物的年平均丰度和生物量分别为2×103 ind·g-1 dwt algae·a-1和8×103μg·g-1 dwt algae·a-1。蜈蚣藻附植小型底栖生物的年平均丰度和生物量分别为3×103 ind·g-1 dwt algae·a-1和16×103μg·g-1 dwt algae·a-1。三种藻类附植小型底栖生物平均丰度和生物量的高低依次为:鼠尾藻蜈蚣藻孔石莼。附植小型底栖生物及其主要类群的丰度具有明显的季节变化,其中鼠尾藻、孔石莼附植小型底栖生物丰度与海水温度和盐度显著相关。附植小型底栖生物的丰度还可能与藻类生长周期关系密切,三种藻类附植小型底栖生物的丰度的最高值均出现在藻类的快速生长期之前。三种藻类附植小型底栖生物群落差异显著,鼠尾藻上线虫为最优势类群,孔石莼和蜈蚣藻上底栖桡足类为最优势类群。藻类形态和藻类生活周期是影响附植小型底栖生物类群组成、丰度和生物量的关键因素。     

辽河口潮间带大型底栖动物摄食功能群特征研究

2020年对辽河口潮间带7条断面46个站位开展了春、秋两季大型底栖动物调查,并进行摄食功能群划分,研究了其潮间带大型底栖动物摄食功能群的组成及特征。共发现46种大型底栖动物,以软体动物、环节动物和节肢动物为主。肉食者功能群种类数最多,且主要为环节动物类群;浮游生物食者功能群则在丰度及生物量方面占优势地位,且主要为软体动物类群。大型底栖动物各摄食功能群丰度及生物量(除肉食者外)均表现出春季高于秋季,且在断面间无显著性差异,但浮游生物食者在靠近辽河入海口的断面(B和C断面)占据绝对优势。双因素方差分析显示,各摄食功能群的种类数、丰度和生物量在季节变化上均无显著差异。本研究结果有助于揭示辽河口潮间带大型底栖动物摄食功能群的变化规律,并为生物资源保护和修复提供基础数据。     

浙南潮间带大型底栖藻类时空分布及多样性研究

在浙南地区布设10条断面开展春秋航次潮间带大型底栖藻类调查, 重点对大型底栖藻类的时空分布及多样性进行研究.共鉴定出大型底栖藻类61种, 其中包括绿藻门8种, 褐藻门16种, 红藻门36种, 蓝藻门1种, 区系特征明显, 大型底栖藻类的季节演替也非常明显, 春季的物种数(53种)明显高于秋季(25种), 而两个季节都出现的物种只有17种.浙南大型底栖藻类平均生物量为540.16g·m-2, 春季(722.18g·m-2)明显高于秋季(358.14g·m-2);从垂直分布来看, 秋季与春季各断面生物量也并不相同, 秋季低潮区739.45g·m-2>中潮区334.95g·m-2>高潮区0g·m-2;春季中潮区1 943.30g·m-2>低潮区965.03 g·m-2>高潮区290.41g·m-2.从物种优势度可以看出, 两个季节的主要优势种有相同之处, 但它们在群落的功能地位上随着季节有着较大的变化, 如春季鼠尾藻Sargassum thunbergii (Mert.) O. Kuntze是第1优势种, 而秋季却成第2优势种.Shannon-Winner指数(H')、Margalef 物种丰富度指数(d)和Pielou均匀度指数(J') 的平均值秋季分别为1.38±0.66、0.70±0.38、0.93±0.41,春季分别为1.65±1.09、1.07±0.63、0.80±0.38.各断面多样性相差较大, 这与浙南各断面的大型底栖藻类的稳定和复杂性有很大关系, 这一点从群落结构聚类分析也得到验证.     

Model of the post-Cenozoic evolution of the cryolithozone of the shelf of the western part of the Laptev Sea

The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ～200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ～380 km from the coast at a depth of ～250 m above the sea level.     

Investigation of the mechanism of the long-term evolution of the carbon cycle in the ecosystem of the Sevastopol bay

We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative abundances of organic and inorganic carbon as an index of the carbon cycle stability.     

Contemporary state of the investigation of the influence of the discharge of rivers on the hydrologic structure of the Black Sea

We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic regime of the sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

双壳贝类血淋巴中儿茶酚胺的检测方法初步研究

研究的目的是探索一种检测双壳贝类血淋巴中儿茶酚胺含量的方法。以栉孔扇贝(Chlamysfarreri)和长牡蛎(Crassostreagigas)为实验对象,研究了取样、抗氧化剂、氧化铝用量以及Tris缓冲液用量等对实验结果的影响。结果表明,高效液相色谱电化学检测器法(HPLC-ECD)可以灵敏高效地对双壳贝类血淋巴中儿茶酚胺进行定性、定量检测。实验表明,取样时间最长不超过1.5min;还原性谷胱甘肽作抗氧化剂效果较好;前处理各试剂与血样量的最适配比为血样量1.5mL,Tris缓冲液(1.5mol/L,pH8.6)1mL和氧化铝25mg;水洗后离心并尽可能吸干氧化铝中的水分。去甲肾上腺素、肾上腺素和多巴胺的回收率分别为53%~69%、47%~73%和48%~56%。     

Modelling of the ecosystem of the Black-Sea shelf zone near the estuary of the Danube

We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the shelf zone and open sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

黄河入海径流对河口海域盐度影响研究

为研究黄河入海径流变化条件下河口附近海域盐度扩散特征,以更好地保护河口海域生物资源多样性,本文以黄河下游利津水文站的长序列实测径流数据资料为基础,利用近海水动力模型FVCOM,分析径流变化对黄河口海域盐度的影响规律。结果表明：黄河口与莱州湾之间存在顺时针的环流系统,在余流作用以及涨落潮方向的影响下,黄河冲淡水长期向莱州湾扩散;丰水期黄河冲淡水几乎影响了整个莱州湾,27盐度锋可以到达莱州湾中部,27等盐线的表层包络面积为2 665.61 km²,占莱州湾的1/4左右,枯水期低盐度水只有向南扩散的趋势,27以下的低盐度水集中分布在黄河口门附近,27等盐线的表层包络面积只有199.65 km²;5月份,随着入海径流量增加,27等盐线扩散的范围、距离、方向都会发生明显变化。在对近海生物资源有迫切保护需求的情景下,适当减少其他用水户供水量以增加入海生态径流量,可以有效改善黄河口海域附近的盐度情况,为生物资源的生长繁殖创造良好条件。     

The influence of the bottom contour on the deformed state of the ice cover due to the motion of the submarine

The authors have previously determined that the effectiveness and failure pattern of the ice cover caused by flexural-gravity waves generated by a submerged body motion near the bottom ice can greatly depend on the depth of the water area. In its turn, the presence of a ledge on the ice surface may affect a wave propagation pattern. This paper presents an experimental study of the bottom contour influence on the deflection and length of flexural-gravity waves. The authors describe a numerical model for the analysis of the deformed state of ice caused by hydrodynamic loads due to a submarine motion, taking into account the bottom contour. The experiments are carried out in the ice tank. The results of calculations and experiments are compared.     

Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state.     

Dynamics of the ice cover and peculiarities of the ice transportation of the sediments at the tidal flats of the Kandalaksha Gulf of the White Sea

Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m³ from 1 km of coast in the wide tidal flats and <50 m³ on the steep coasts) are delivered to the water area.     

Parameters of the sediments of the deep-water basin of the Black Sea

The methodology and the first results of the computations of the volumes, masses, and growth rates of the sedimentary body of the buried Black Sea basin are presented. Their temporal evolution reflects the regional paleogeodynamics, in particular, the reorientation of the vector of the relative movement of the Arabian and Eurasian lithospheric plates and the related intensification of their collision in the late Miocene-Pliocene.