南黄海大型底栖生物次级生产力研究

根据2000年秋季和2001年春季在南黄海24个大面站进行的大型底栖生物定量采集样品资料,利用Brey’s(1990)的经验公式对调查海区进行了大型底栖生物栖息密度、生物量、次级生产力和P/B值的研究计算.结果表明,该海域大型底栖生物平均栖息密度在2000年秋季为154.2个/m2,与2001年春季的147.8个/m2相当,平均生物量以去灰干重计,秋季为6.92g/m2,远高于春季的2.81g/m2;年平均次级生产力以去灰干重计,为4.98gm-2a-1.与生物量的分别格局相似,次级生产力在所调查海域的西南和东南部有两个高生产力分布区域,而该二区域正好在黄海冷水团的两侧,由此验证大型底栖生物的生物量和次级生产力受海水温度的影响较大.平均P/B值在研究海域为1.10a-1.与渤海研究结果比较,证明了底栖生物群落生产力随水深增大而下降,P/B值随水温升高而升高.图2表2参31     

南黄海鯷鱼产卵场大型底栖生物次级生产力研究

根据2001至2003年南黄海鯷鱼产卵期在鯷鱼产卵场33个站考察采集的大型底栖生物定量样品资料，利用Brey’s(1990)的经验公式对调查海区进行了大型底栖生物栖息密度、生物量、次级生产力和P/B值的研究计算，结果表明，该海域大型底栖生物平均栖息密度为194．3ind．m^-2，平均生物量以去灰干重计，为4．08gm^-2，平均次级生产力以去灰干重计，为4．09gm^-2a^-1，研究表明，生物量和次级生产力受水深的影响，平均P／B值在研究海域为1．32a^-1，对研究结果与整个南黄海、渤海和东海的结果进行了比较与讨论，证明生产力随水深的加大而降低，P／日值随水漏升高而升高，图2表1参25     

东海大型底栖生物次级生产力研究

根据2000年秋季和2001年春季在东海23个大面站进行的大型底栖生物定量采集样品资料，利用Brey’s（1990）的经验公式对调查海区进行了大型底栖生物栖息密度、生物量、次级生产力和P／B值的研究和计算．结果表明，该海域大型底栖生物平均栖息密度在秋季为87m^-2，远低于春季的138m^-2，而平均生物量以去灰干重计，秋季为1．40gm^-2，高于春季的1．25gm^-2；年平均次级生产力以去灰干重计，为1．62gm^-2a^-1，远低于渤海和南黄海．研究表明，大型底栖生物生物量和次级生产力受水温和水深的影响，平均P／B值在研究海域为1．41a^-1，高于渤海和黄海，表明在东海大型底栖生物中个体小而代谢快、生活史短的种在大型底栖生物中占的比重要大于渤海和南黄海，P／B值随水温升高而升高，图2表2参28     

长江口及毗邻海域大型底栖动物的次级生产力(英文)

根据2005年与2006年在长江口及其毗邻海域,采用改进型0.1m2的Gray-O’Hara箱式采泥器,对85个站位进行的大型底栖动物定量调查资料,利用Brey’s(1990)的经验公式对底栖生物的次级生产力、P/B值及其空间分布状况进行统计和分析.结果表明,该海域共发现大型底栖动物330种,平均栖息密度为(146.4±22.3)indm-2,平均生物量以无灰干重计,为(2.31±0.41)g(ash-free dryweight,AFDW)gm-2.调查海域大型底栖动物的平均次级生产力以无灰干重计,为(2.48±0.38)g(AFDW)m-2a-1.在空间分布上,底栖生物的次级生产力自西向东,或自近岸向外海逐渐升高,并在调查区中部形成垂直于河口并与海岸大致平行且呈带状分布的高生产力中心,之后,次级生产力随水深增加呈现下降趋势.根据地理位置差异,整个研究区域被分为5个亚区,次级生产力在各亚区之间呈现显著差异.其中位于最西侧的河口亚区(HK)与杭州湾亚区(HW),由于受到强大的淡水注入以及污水排放影响,成为整个研究区的低生产力中心.通过与其它研究相比较可以得出,对于理化条件复杂多变的河口区,大型底栖动物通常具有较低的次级生产力.此外,研究区大型底栖动物的平均P/B比为(1.48±0.06)a-1,显示该区域大多数物种通常个体较小且更新率较高.     

桑沟湾大型底栖动物的次级生产力

根据2009年夏季和冬季在桑沟湾9个大面站进行的大型底栖动物定量采集样品资料,利用Brey(1990)的经验公式对调查海区进行了大型底栖动物丰度、生物量、次级生产力和P/B值的研究计算.结果表明,该海域大型底栖动物年平均丰度为1 226.7 ind m-2,年平均生物量为3.62 g(AFDW)m-2,年平均生产力为4.76 g(AFDW)m-2 a-1,P/B值平均为1.45 a-1.调查期间由湾口到湾底,次级生产力呈明显的梯度升高.相关分析表明,水深和水温是影响次级生产力的重要环境因子.通过比较,发现桑沟湾大型底栖动物次级生产力与南黄海相近,高于东海、长江口和深沪湾,低于渤海、胶州湾、大亚湾和海坛海峡;P/B值低于长江口、海坛海峡和深沪湾,高于其它海区,说明桑沟湾大型底栖动物群落中,个体小、生活史短、代谢快的种类所占比例低于海坛海峡和深沪湾,高于其它海区.图2表3参25     

长江口潮间带大型底栖动物次级生产力及其影响因子

根据2010年8月至2011年5月在崇明东滩潮间带进行的大型底栖动物定量采集样品资料,利用Brey(1990)的经验公式分析了调查区域内大型底栖动物栖息密度、生物量、次级生产力和P/B值.结果表明:以去灰干质量(AFDM)计,5月、8月和11月总平均栖息密度、总平均生物量、总平均次级生产力和总平均P/B值分别为637.83 ind m-2、6.82 gm-2、6.71 g m-2a-1和1.01 a-1.纵向梯度上,总平均栖息密度、总平均生物量、总平均次级生产力三者大小排序均为东旺沙≥捕鱼港>团结沙.分析表明,潮间带次级生产力受软体动物影响明显,其中河蚬(Corbicula fluminea)、黑龙江河蓝蛤(Potamocorbula amurensis)、缢蛏(Sinonovacula constricta)、光滑狭口螺(Stenothyra glabra)、泥螺(Bullactaexarata)和中华拟蟹守螺(Cerithidea sinensis)这6种优势种贡献了崇明东滩潮间带65.24%的次级生产力.调查区域总平均P/B值为1.01 a-1,推测东滩大型底栖动物平均一年更替一代,群落结构不稳定,受外界影响较大.运用主成分分析(PCA)对断面环境状况进行分析,显示团结沙生境状况最稳定,捕鱼港次之,东旺沙最剧烈.对次级生产力影响因子进行相关性分析,发现除生物量、栖息密度外,水体总氮、总磷对其也存在较大影响.采用典范对应分析(CCA)解析断面各季节大型底栖动物群落次级生产力与环境变量的关系,显示断面群落次级生产力环境影响因子不尽一致,东旺沙影响因子为Sal、TP、TOC及DO;捕鱼港影响因子为TN、TOC、Chla及DO;团结沙生境状况极稳定,受环境因子影响极小,分析其次级生产力影响因子可能更偏向于沉积物理化因子.     

东寨港红树林区大型底栖动物多样性研究

于2010年3-12月对海南东寨港红树林区进行4次采样,研究该地大型底栖动物生物量、栖息密度的时空变化规律以及不同季节红树林群落大型底栖动物物种多样性的差异.结果表明,不同季节大型底栖动物的种类、数量差异极大,大型底栖动物种类以冬季为最多(45种),夏季为最少(28种),生物量以秋季为最高(272.78 g·m-2),夏季为最低(165.93 g·m-2),密度以冬季为最大(679.25 m-2),夏季为最小(504.95 m-2).对各站位大型底栖动物的生物量、栖息密度及不同红树群落底栖动物的物种多样性指数、丰富度指数和均匀度指数进行站位-季节间无重复的双因素方差分析,结果显示栖息密度、多样性指数和丰富度指数在季节间差异显著(P＜0.05),生物量、均匀度指数在站位间差异显著(P＜0.05).分析表明温度、盐度、底质和红树种类是导致大型底栖动物物种多样性存在差异的主要因素,东寨港红树林恢复有利于底栖动物生物量及物种多样性的增加.     

黄海春季表层叶绿素和初级生产力及其粒径结构研究

根据2006年4月对黄海浮游植物分级叶绿素及初级生产力的调查,研究了黄海叶绿素及初级生产力的水平分布及粒级结构特征,并分析了其主要影响因素。黄海海域调查站位表层叶绿素a质量浓度变化范围为0.20～4.94μg·L-1,平均值为0.96μg·L-1。叶绿素最大值出现在临近长江口的站位。叶绿素分级结果表明黄海春季以粒径〉5μm的浮游植物占优势。黄海表层初级生产力的变化范围为2.03～15.64mg·m-3·h-1,平均值为6.08mg·m-3·h-1。其中南黄海海域初级生产力平均为6.58mg·m-3·h-1,北黄海海域初级生产力平均为4.92mg·m-3·h-1。高值区分布在南黄海中部。受水体透明度的影响,低值区出现在临近长江口的站位。断面站位分析表明浮游植物初级生产力由北向南逐步升高,温度随纬度的变化是南北海域初级生产力水平差异的主要原因。由于粒径较小（〈5μm）的浮游植物单位叶绿素具有较高的碳固定能力,调查期间整个海区初级生产力以粒径〈5μm的浮游植物贡献为主。     

河北昌黎海域大型底栖动物群落特征及青岛文昌鱼资源现状

于2017年春季(5月)和夏季(8月)对河北昌黎黄金海岸国家级自然保护区海域大型底栖动物群落特征及青岛文昌鱼(Branchiostoma belcheri tsingtauense)资源现状进行调查。结果表明,春夏两季分别鉴定出大型底栖动物56和50种,种类组成皆以环节动物为主;大型底栖动物平均栖息密度为87.11 m~(-2),平均生物量为11.13 g·m~(-2);青岛文昌鱼平均栖息密度为31.36 m~(-2),平均生物量为1.44 g·m~(-2),体长为0.50～4.45 cm,Ⅱ、Ⅲ龄青岛文昌鱼占优势地位,体重为0.3～109.4 mg,优势体重组为20～40和0～20 mg,昌黎海域青岛文昌鱼个体偏小,与历史资料对比发现,青岛文昌鱼资源量正在逐年减少。春夏两季大型底栖动物多样性指数变化趋势相似,Shannon-Wiener多样性指数平均值显示该海域大型底栖动物生境一般;采用Bray-Curtis相似性系数聚类分析和多维排列尺度(MDS)分析相结合的方法研究春夏季大型底栖动物群落结构,结果表明春季可分为5个群组,夏季可分为2个群组,群组组成差异较大。     

黄海西部大气湿沉降(降水)中各元素沉降通量的初步研究

本文对黄海西部的千里岩、青岛的麦岛降水(雨+雪)中的H+,NH+4,K +,Na+,Ca2+,Mg2+,F-,Cl-,NO-3,SO2-4 ,SiO2-3,PO3-4进行了测定.计算了除H+以外其他离子的湿沉降通量.1998年千里岩N,P,Si的湿沉降通量分别为:DIN([NH+ 4]+[NO-3])0.611g·m-2.a-1,P 0.002g·m-2 ·a-1,Si 0.078g·m-2·a-1,麦岛N,P,Si的湿沉降通量分别为:DIN 0.776g·m-2.a-1,P 0.008g·m-2·a-1,Si 0 .060g·m-2.a-1,千里岩降水的N/P比(摩尔比)为72 7,远高于海水中的Redfield比值(16),将对该海域的营养盐结构产生一定的影响. 对于忽略小于0.7mm的降水对湿沉降通量所可能产生的误差进行了估算,发现几种主要离子均小于9%.     

胶州湾多毛类环节动物数量分布与环境因子的关系

根据1998~2002年胶州湾10个站各季度大型底栖动物调查结果,讨论了多毛类环节动物在各站出现种数、生物量、栖息密度与环境因子的关系.结果表明,海底底质是影响多毛类数量分布与变化的重要因子,沙质软泥有利于多毛类生长,而粗沙砾石底质多毛类分布较少;春季多毛类种数、生物量和栖息密度均较高;在一定条件下,盐度是多毛类的限制因子,当盐度升高时,其生物量和栖息密度呈增加趋势.图2表6参14     

丹江口水库底栖动物群落次级生产力空间分布

于2007年7月—2008年5月,分季度对丹江口水库底栖动物群落及水环境进行为期一年的调查。运用经验公式估算丹江口水库大型底栖动物群落的生产力,并分析底栖动物密度、生物量、生产力及P/B系数的空间分布,探讨环境因子与底栖动物群落生产力空间分布的关系。结果显示,丹江口水库底栖动物年平均密度、生物量及生产力分别为4 761 ind·m~(-2)、1.61 g DM·m~(-2)和35.45 g DM·m~(-2)·y~(-1),P/B系数为22.0 y~(-1)。不同区域生产力差异很大,湖泊区达61.80 g DM·m~(-2)·y~(-1),而支流区仅有5.48 g DM·m~(-2)·y~(-1)。P/B系数同样在湖泊区达到最大,为34.0 y~(-1);在丹江过渡区最低,为13.1 y~(-1)。颤蚓是生产力的主要贡献者,周年生产力为31.85 g DM·m~(-2)·y~(-1),占总生产力的90%。湖泊区由于其稳定的水动力条件,为颤蚓提供了非常适宜的生境,因此具有很高的生产力水平。与之相反,支流区由于水体扰动较大,底栖动物生物量及生产力水平均较低。从生产力的角度研究丹江口水库底栖动物群落的空间分布规律及影响因子,对丹江口水库的生态管理具有参考价值。     

Annual biomass and production of the oceanic copepod community off Discovery Bay,Jamaica

Monthly samples were collected in oceanic waters off Discovery Bay, Jamaica, in 60- and 200-m vertical hauls, using 200- and 64-m mesh plankton nets, from June 1989 to July 1991. Length-weight regressions were derived for twelve genera of copepods (R²=0.79 to 0.97). For eight occasions spanning the study period, biomass estimates generated from these length-weight regressions differed by only 3% from direct weight determinations. The mean ash content of copepods was 7.1%, and the energy density was 20.8 kJ g^-1 ash-free dry weight (AFDW). Mean annual biomass of the total copepod community in the upper 60 m was 1.83 mg AFDW m^-3 (range 1.14 to 2.89 mg AFDW m^-3), and for the 200-m water column was 0.96 mg AFDW m^-3 (range 0.12 to 1.99 mg AFDW m^-3). Estimates of generation times for five common taxa ranged from 16.1 to 33.4 d. None of the taxa investigated displayed isochronal development; in general, stage duration increased in later copepodite stages. Weight increments showed a significant decrease in later copepodite stages, but with strong reversal of the trend from stage 5 to adult female in most species. Daily specific growth rates also declined in later copepodite stages, and ranged from 1.49 d^-1 in stage 1–2 Paracalanus/Clausocalanus spp. to 0.04 in stage 5-female of Oithona plumifera. Progressive food limitation of somatic copepodite growth and egg production is postulated. Naupliar production was 50.4 to 59.5% of copepodite production, and egg production was 35.1 to 27.7% of copepodite production in the 60-and 200-m water columns, respectively. Total annual copepod production, including copepodites, nauplii, eggs and exuviae, was 160 kJ m^-2 yr^-1 for the upper 60 m and 304 kJ m^-2 yr^-1 for the upper 200 m. Secondary production of the copepod community in oceanic waters off Discovery Bay approaches 50% of the corresponding value in tropical neritic waters.     

Secondary production ofPrionospio caspersi (Annelida: Polychaeta: Spionidae)

The annual somatic production ofPrionospio caspersi Laubier was estimated, between July 1986 and 1987, at a sandy shallow-bottom station in the area facing the Po River Delta, Italy, where this species is one of the most abundant. Primary recruitment occurs in summer, and maturation of gametes the following spring. Body sizes were estimated from the surface area of the anterior end of worms, projected onto a monitor and recorded using a digitizer tablet. Measurements, to the tenth setiger, were correlated with total length, total body surface area and AFDW. The annual production was 8.06 g m^–2 yr^–1 (AFDW) and the production:biomass (P:B) ratio 4.09. The results are discussed in relation to some physical and chemical features of the environment, stressing differences with the life cycle of other coexisting populations.     

Contrasting life histories and secondary production of populations of Munnopsurus atlanticus (Isopoda: Asellota) from two bathyal areas of the NE Atlantic and the NW Mediterranean

The isopod Munnopsurus atlanticus occupies bathyal depths in both the Bay of Biscay (NE Atlantic; between 383 and 1022 m) and in the Catalan Sea (Northwestern Mediterranean; between 389 and 1859 m). The species was dominant in both assemblages, reaching bathymetric peaks of abundance on the upper part of the continental slope (400 m depth) in the Bay of Biscay and at ˜600 m in the Catalan Sea. Both the Atlantic and the Mediterranean populations are bivoltines. Demographic analysis of the Bay of Biscay population revealed the production of two generations per year with different potential longevity (5 mo for G₁ and 11 mo for G₂). The mean cohort-production interval (CPI) was estimated at 8 mo, and results of the demographic analysis were also used to estimate production for the Catalan Sea populations. Mean annual density (D) and biomass (B) were higher in the Bay of Biscay (D = 356.7 individuals 100 m⁻²; B = 0.803 mg dry wt m⁻² yr⁻¹) than in the Mediterranean (D = 16.3 individuals 100 m⁻²; B = 0.078 mg dry wt m⁻² yr⁻¹). Also, mean annual production was an order of magnitude higher in the Atlantic (between 4.063 and 4.812 mg dry wt 100 m⁻² yr⁻¹ depending on the method used) than in the Catalan Sea (between 0.346 and 0.519 mg dry wt 100 m⁻² yr⁻¹). M. atlanticus feeds on a wide variety of benthic and pelagic food sources. In both study areas, phytodetritus was not important in the diet of M. atlanticus. In contrast, gut-content data suggested an indirect coupling with phytoplankton production in both areas via foraminiferans. The life history and the recorded production are considered in respect to both the dynamics and levels of primary production and the total mass flux in the respective study areas. Differences in the secondary production of both populations seemed to be more consistently explained by differences in total mass flux than by differences in the primary production levels; this is also consistent with the variety of food sources exploited by M. atlanticus. Received: 22 February 1999 / Accepted: 3 February 2000     

江苏省植被NPP时空特征及气候因素的影响

利用2000—2006年的EOS/MODIS卫星遥感资料,对江苏省植被净初级生产力（NPP）时空特征及气候变化对其影响进行分析。在ArcGIS软件中,建立线性回归方程获得NPP的变化斜率,分析7 a间各像元NPP的空间变化趋势。计算各像元的NPP数值与气候要素的线性相关系数,为定量阐述气候变化对植被生长的影响提供依据。结果表明,江苏省植被NPP 7 a平均值为506.6 g.m-2.a-1（以C计）,比全国同期NPP数值高出约40%。NPP表现出明显的年际变化,2004年植被年均NPP最大为530.6 g.m-2.a-1（以C计）,2000年最小,为481.1 g.m-2.a-1（以C计）。空间分布上NPP表现为东南高于西北,沿海高于内陆。2000—2006年江苏省有76%的区域植被NPP表现为显著增加,仅江苏南部少数区域表现出减少的趋势。除苏南少数区域外,气候因素控制着NPP的时空变化规律。其中气温的升高和太阳辐射的增加促进NPP提高,而降水量的增加引起NPP的降低。     

Succession and growth limitation of phytoplankton in the Gulf of Bothnia (Baltic Sea)

A one year field study of four stations in the Gulf of Bothnia during 1991 showed that the biomass was ca. two times, and primary productivity ca. four times, lower in the north (Bothnian Bay) than in the south (Bothnian Sea) during the summer. Nutrient addition experiments indicated phosphorus limitation of phytoplankton in the Bothanian Bay and the coastal areas in the northern Bothnian Sea, but nitrogen limitation in the open Bothanian Sea. A positive correlation between the phosphate concentration and the production/biomass ratio of phytoplankton was demonstrated, which partly explained the differences in the specific growth rate of the phytoplankton during the summer. Differences in photosynthetic active radiation between the stations also showed a covariation with the primary productivity. The relative importance of nutrient or light limitation for photosynthetic carbon fixation could not, however, the conclusively determined from this study. Marked differences in phytoplankton species composition from north to south were also observed. The number of dominating species was higher in the Bothnian Sea than in the Bothnian Bay. The distribution of some species could be explained as due to nutrient availability (e.g. Nodularia spumigena, Aphanizomenon sp.), while salinity probably limits the distribution of some limnic as well as marine species. The potentially toxic phytoplankton N. spumigena, Dinophysis acuminata and Chrysochromulina spp. were common in the Bothnian Sea but not in the Bothnian Bay. The pico- and nanoplankton biomass during late summer was higher than previously reported due to a revised carbon/volume ratio.