深海钻探计划(DSDP)31航次296站晚新生代介形类

本文研究了深海钻探(DSDP)31航次296站晚新生代介形类动物群的性质及其古海洋学意义.此站钻孔上部上新统至全新统以超微浮游生物软泥和粘土为主的16块岩芯中,共分析获得介形类化石8属11种,计有:Poseidonamicus major Benson, P. anteropunctatus Whatley et al., P. punctatus Whatley et al., Pennyella dorsoserrata (Brady), Henryhowella sp., Pterygocythere mucronalatum (Brady), Abyssocythere sp., Abyssocythereis sulcatoperforata (Brady), Pelecocythere sp., Krithe sp. 1和Krithe sp.2.这些介形类属种均为冷海域深海区介形类分子.由此表明,西北太平洋边缘地区在晚新生代曾为一深海区.在第四纪,其深度可能和现今296站的深度大致相当;在上新世,其深度可能更深一些.研究结果证实,深海底栖介形类属种的分布具全球性;在相当长的地质时期内,介形类属种的形态和壳饰都非常稳定,无明显变化.同时,进一步证实,介形类个体大小变化与深度相关,同一种介形类壳体随水域深度加深而增大.     

Ilyocypris bradyi的轮廓分析

本文试图通过对若尔盖盆地晚新生代非海相介形类化石Ilyocypris bradyi(Sars)的轮廓分析来介绍几何形态测量法在介形类化石的形态分析中的应用。分析对比后发现,虽然Ilyocypris bradyi(Sars)居群内的个体在形态上存在或多或少的差异,但这些差异之间存在连续过渡的关系,并未出现明显的分异,说明此种的种内变异是连续的。     

洞庭湖DT01剖面的介形类现生种

本文首次记述了湖南省洞庭湖DT01剖面介形类现生种,包含3属4种,它们为比利时舍氏玻璃介(相似种)Schellencandonacf.belgica(Klie,1937)、布氏土星介Ilyocypris bradyi(Sars,1890)、土星介属(未定种)Ilyocypris sp.和豆形豆形玻璃介Fabaeformiscandona fabaeformis(Fischer,1851)。上述属种在洞庭湖区为首次报道,在湖南省亦是首次。此外,S.cf.belgica在我国还很少报道。本研究可丰富我国介形类现生种数据,同时为利用该类生物定量重建本区域全新世古气候奠定基础。     

武昌东湖的数种介形类甲壳动物

介形类是底栖的切甲类甲壳动物,部分种类的触角上具有发达的游泳刚毛,所以在通常采到的浮游生物标本中亦很常见。早在1903年,G．O．Sars氏曾经报导过采自我国的介形类共三属五新种。1923年,V．Brehm也报导过采自我国广州、北京、四川等地的数种介形类,其中还有一新属,三新种及一新变种。     

角突泥介虫(Ilyocypris angulata Sars)(介形亚纲)雄体的发现

本文报道了角突泥介虫(Ilyocypris angulata Sars)雄体的发现。对此雄体进行了详细的描述,论述了泥介虫属的生活方式,并讨论了介形类有三种生殖方式。     

武昌东湖的数种介形类甲壳动物

介形类是底栖的切甲类甲壳动物,部分种类的触角上具有发达的游泳刚毛,所以在通常采到的浮游生物标本中亦很常见。早在1903年,G.O.Sars 氏曾经报导过采自我国的介形类共三属五新种。1923年,V.Brehm 也报导过采自我国广州、北京、四川等地的数种介形类,其中还有一新属,三新种及一新变种。     

华东地区元荡湖现生介形类新记录

本文首次记述了采自我国东部元荡湖的现生介形类7属9种,分别为:近球形金星介Cypris subglobosa Sowerby,1840、膨大丽神介Cypretta turgida(Sars,1896)、克氏丽星介Cypria kraepelini(G.W.Müller,1903)、无偶斗星介Cypridopsis vidua(O.F.Müller,1776)、塔尔薄丽星介Dolerocypria taalensis Tressler,1937、豆形豆形玻璃介Fabaeformiscandona fabaeformis(Fischer,1851)、弯叶豆形玻璃介F.myllaina Smith et Kamiya,2007、豆形玻璃介(未定种)Fabaeformiscandonasp.和粗糙土星介Ilyocypris salebrosa Stepanaitys,1960。这些属种在太湖流域的淀泖湖群系首次报道,其中F.myllaina和I.salebrosa均首次报道于我国东部湖区。本研究丰富了我国介形类记录,可为介形类地理区系研究提供基础资料。     

滴水湖现生介形类与水环境因子间的典范对应关系

滴水湖作为人工新建湖泊,其生态系统形成过程中的跟踪数据对重建其他湖泊生态系统具有重要的参考意义。2013年7月和2014年8月对滴水湖现生介形类分布状况及水环境因子分别进行了调查,结果发现,滴水湖湖水盐度范围介于1.4‰—2.0‰之间,属于微咸水湖。12个采样点共鉴定出现生介形类13种,包括非海相类克氏丽星介Cypria kraepelini(G.W.Müller)和无偶斗星介Cypridopsis vidua(O.F.Müller),海相类中华洁面介Albileberis sinensis Hou、向岛薄丽星介Dolerocypria mukaishimensis Okubo、腹结细花介Leptocythere ventriclivosa Chen、东台新单角介Neomonoceratina dongtaiensis Yang et Chen、长新中华花介Neosinocythere elongata(Hu)、闪光似异口介Paradoxostoma nitida Ho、典型中华美花介Sinocytheridea impressa(Brady)、长中华海花介Sinopontocythere elongata(Gou)、古屋刺花介Spinileberis furuyaensis Ishizaki et Kato、美丽刺面介Spinileberis pulchra Chen和丰满陈氏介Tanella opima Chen。应用典范对应分析(CCA)方法对滴水湖12个样点的8种介形类和9个环境因子进行了相关性研究,结果显示:介形类和环境因子间具有明显的相关性;9个环境因子中叶绿素、总磷和电导率对介形类的分布影响最大,总氮和湖水水温对介形类也有一定影响;从物种分布状况看,相对于低分布频度物种,高分布频度(Y>0.01)物种对环境的耐受性更大,其中Cypria kraepelini和Neomonoceratina dongtaiensis对环境因子的敏感性明显高于其它物种。结合历史资料分析发现,不仅自然环境因子(如电导率、水温等),而且人为干扰因素(如总磷、总氮)都对介形类分布的改变起到重要影响。     

贵州省红枫湖现生介形类新纪录

本文首次记述了采自我国贵州省红枫湖的现生介形类5属7种,分别为:近锐豆形玻璃介Fabae formiscandona subacuta(Yang,1982)、比利时舍氏玻璃介(相似种)Schellencandona cf.belgica(Klie,1937)、亮球星介Cy-clocyprisserena(Kock,1838)、克氏丽星介Cypria kraepelini(G.W.Müller,1903)、条纹薄壳介(相似种)Dolerocypris cf.fasciata(O.F.Müller,1776)、布氏土星介Ilyocypris bradyi Sars,1890、粗糙土星介I.sale-brosa Stepanaitys,1960。这些属种在红枫湖和贵州省均系首次报道,其中S.cf.belgica在我国是首次发现,文内对F.subacuta活体特征的描述在我国尚属首次。     

中国新发现的有关玛利羊齿的材料

The Ostracods studied in this paper were collected by the members of a geologicalparty in 1955 from the yellowish silt-clay in Gansen district,Chaidam Basin.Accord-ing to the collecter's opinion,the geological age of the fossil bearing bed is Pliocene toQuaternary.The Ostracods are found in association with a charophyta,Chara gansenensis Wang(S.Wang,1961),gastropods and some indeterminable fragments of plant and fish bone.The species of Ostracoda described and illustrated in this paper are as follows:Ilyo-cypris gibba(Ramdohr),Eucypris inflata(Sars),Prionocypris gansenensis Huang(sp.nov.),Cypricercus brevis Huang(sp.nov.),Cypridopsis reticulata Huang(sp.nov.),Cyc-locypris serena(Koch),Candona neglecta Sars,C.houae Huang(sp.nov.),Limnocytheredubiosa Daday,L.sancti-patricii Brady et Robertson,L.binoda Huang(sp.nov.)andCyprideis littoralis(Brady).From the geological distribution of this Ostracod assemblage,the fossil bearing bedmay be of Pleistocene in age.     

Heterochrony in Shell Sculpture Development within the Ostracode Genus Hemicythere

The evolutionary issues of taxonomic significance of the shell sculpture in Ostracoda are addressed. This is a comparative ontogenetic study of three types of lateral sculpture (fossa-mural reticulation, punctation, and foveolation), as well as flanges, ridges, and tubercles is made in different age stages and morphological variations of three ostracode species with different strengths of the expression of sculpture: Hemicythere borealis (Brady, 1868), H. villosa (Sars, 1866), and H. nana (Schornikov, 1974). It is shown that the development of each sculpture type proceeds relatively independently and represents a mosaic; developmental stages are accompanied by numerous heterochronies. This results in many parallelisms, and even the trend of the evolution of a structure can change. The pathways of morphological evolution of Hemicythere species are discussed.     

中国近海海牛亚目(软体动物)的区系分析

中国近海共有海牛亚目(Doridacea)软体动物136种,隶属于23科49属,主要分布在浙江以南的热带、亚热带海区,有些种类向北可以分布到黄、渤海,少数种类仅分布于黄、渤海,属于印度-西太平洋区的中国-日本亚区。     

The Mouthparts in Some North Atlantic Species of the Genus Orchomene Boeck (Crustacea, Amphipoda)

The mouthparts of five North Atlantic species of the genus Orchomene have been studied in detail. The species are: O. serrata (Boeck, 1861), O. amblyops G. O. Sars, 1890, O. crispata (Goes, 1866). O. humilis (A. Costa, 1853) and O. pectinate. G. O. Sars, 1882. The structure of the mandibular molar has been studied with the aid of the scanning electron microscope. Some features of the mouthparts, common to the species examined, are interpreted as generic criteria which should justify retaining the genus Orchomene Boeck, 1870, separated from the closely related genera OrchomeneUa G. O. Sars, 1890, and Orchomenopsis G. O. Sars. 1891.     

依据大规模捕捞统计资料分析东黄渤海白姑鱼种群划分和洄游路线

根据我国10多个主要渔业公司1971-1982年间白姑鱼(Argyrosomus argentatus)捕捞统计资料,从产量分布,鱼群移动等方面,研究了东黄渤海白姑鱼的种群划分和洄游路线。结果显示,我国沿海白姑鱼可分为2个种群。其中,黄渤海种群越冬场主要在黄海中部34°00'N以北水域。每年3-4月份,鱼群陆续进入山东半岛的乳山沿海、渤海各海湾、黄海北部沿岸和海州湾产卵。栖息在渤海的白姑鱼9-11月份在渤海中部索饵,形成越冬群体,11月后绕过成山头向越冬场洄游,12月至1月份到达越冬场;东黄海种群越冬场主要是在东海外海和中南部近海。每年3-4月份东海外海白姑鱼向西进入舟山渔场。在舟山渔场,这部分鱼群与从东海中南部近海北上的产卵群体汇合,向西进入舟山群岛沿海水域产卵。到了5月份,在浙江北部近海形成索饵群体。6-8月份,索饵群体经过长江口北上黄海南部近海索饵,9月份,索饵群体前锋到达34°00'N禁渔线外侧。此后,索饵场的白姑鱼向南做越冬洄游,并在10月份回到长江口。从这里,一部分群体游向外海越冬场,一部分群体继续南下回到东海中南部近海的越冬场。另外,在东海中南部近海越冬群体,部分就近游向沿岸的海湾,河口产卵,产卵后在产卵场外侧索饵,冬季回到就近的越冬场。     

Ostracoda (Crustacea) from Lizard Island,northern Great Barrier Reef,Australia. II. The family Paradoxostomatidae Brady & Norman, 1889

The present paper deals with the taxonomy of the ostracod family Paradoxostomatidae Brady & Norman, 1889 from the coral reefs around Lizard Island, northern Great Barrier Reef, Australia. 18 species were found, all of them belonging to the genusParadoxostoma Fischer, 1855. 2 species had been previously described from Heron Island, southern Great Barrier Reef. 1 species had been described from the Red Sea. 2 species are left in open nomenclature.     

浙江近海后鳃类软体动物的分布及其区系

报道了浙江近海的后鳃类97种,分别隶属于7目30科44属。其中我国沿岸广温广布种14种,主要分布于东海和南海的亚热带种50种,南海的热带种18种,渤、黄海延伸到东海北部的暖温带种15种。     

渤海淡水存留时间分析

利用渤海蒸发量、降水量、入海径流量、渤海及黄海盐度数据,基于淡水比例方法估算了渤海的淡水存留时间,并设计敏感性实验,定量分析了渤海淡水通量对渤海淡水存留时间的影响。结果表明,渤海年平均(1965—1980、1986—1992、1994、1996年)淡水存留时间为2.6年,并呈现弱上升的趋势。20世纪80年代的淡水存留时间(4.6年)与20世纪60年代(3.0年)相比,增加了近50%。渤海淡水存留时间随淡水输入的增加而缩短。与净降水量(降水量与蒸发量之差)相比,渤海淡水存留时间对入海径流量变化更敏感,因而流域调水的环境规划应予以充分关注。     

黄渤海甲壳类的分类多样性

为了解黄渤海甲壳类的分类多样性特征, 我们统计了2010-2015年中国水产科学研究院黄海水产研究所调查捕获的黄渤海甲壳类(软甲纲: 十足目与口足目)物种名录。结合历史文献, 进一步系统整理得到黄渤海甲壳类物种总名录。基于这2个名录, 应用分类阶元包含指数(the inclusion index at taxonomic level, TINCL_i)、平均分类差异指数(average taxonomic distinctness index, Δ⁺)和分类差异变异指数(variation in taxonomic distinctness index, Λ⁺)研究了其分类多样性特征。结果显示: 2010-2015年调查名录中, 甲壳类共93种, 隶属于2目39科66属, 其中10种为新分布种; 对虾科、藻虾科、长臂虾科、梭子蟹科和弓蟹科的物种数最多, 合计占总物种数的38.71%; TINCL_i分别为1.41种/属和2.38种/科; Δ⁺和Λ⁺分别为50.25和35.20。总名录中, 甲壳类共228种, 隶属于2目53科123属, 其中藻虾科、豆蟹科、对虾科、弓蟹科和鼓虾科的物种数最多, 合计占总物种数的30.70%; TINCL_i分别为1.85种/属和4.30种/科, Δ⁺和Λ⁺分别为50.18和30.87。对虾科的相对丰富度指数(the relative richness index, R_r)最高(100), 其次是梭子蟹科(71.43)和长臂虾科(62.50), 豆蟹科最低(6.25)。黄渤海甲壳类的平均分类差异指数(Δ⁺)明显小于鱼类(P < 0.05)。2010-2015年调查的Δ⁺计算值高于理论值, 且在理论值的95%置信区间内, 说明黄渤海甲壳类群落正处在中等程度的干扰中。     

Ecological analysis of benthic ostracods in the northern Japan Sea, based on water properties of modern habitats and late Cenozoic fossil records

The ecology of ostracods in the northern Japan Sea is well documented. These ostracods can be grouped in two assemblages: (1) the Tsushima Warm Current Surface Water Assemblage (TWSA, northern), which lives in an environment where summer temperatures reach up to about 20 °C, winter temperatures up to about 5 °C. Several species in this assemblage, e.g., Loxoconcha optima and Pontocythere subjaponica tolerate seasonally low temperatures, and lived in the region since the early Pleistocene; (2) the Japan Sea Intermediate Proper Water Assemblage (JSI-PA), which lives at greater depths (lower shelf to upper slope). This assemblage lives under stable conditions, with a small annual range in temperature (0–5 °C). The assemblage has a relatively low diversity, contains species such as Acanthocythereis dunelmensis and Robertsonites spp., and has been present in the area since the Pliocene. These data indicate that the presently living species either tolerate seasonally low temperatures (TWSA, northern) or tolerate stable, but very low temperatures (near 0 °C), and therefore, they could survive the Pleistocene environmental fluctuations in the Japan Sea caused by glacio-eustatic changes in sea level. Our data document the survival of ostracod species during past climate change, and thus can be used to speculate on the effect of possible future climate change on the faunas. We predict that some of the cryophilic species in the Japan Sea cannot be expected to survive global warming for more than 2 centuries.