Taxonomical and Biogeochemical Investigation of Elements in Holocene Mollusk Shells in the South and Southwestern Marmara Basin, Turkey     

Saday Azadoglu ALIYEV Ali SARI Bahadir KTEN Ankara University  Faculty of Engineering  Department of Geological Engineering  Tandogan  Ankara  Turkey 《《地质学报》英文版》2008,82(6)

Concentrations of some heavy metals and trace elements such as Cr,Ga,Ni,Zn,Mo,Cu, Pb,Yb,Y,Nb,Ti,Sr,Ba,Mn,Sc,Co,V,Zr,Fe,Al,W,Se,Bi,Sb,As,Cd in recent mollusk shells and factors affecting their distribution and deposits collected from various depths in the southern and southwestern parts of the Marmara Sea are investigated.The distribution of the elements in the shells is categorized into four groups.Of these,concentrations of 12 elements(As,Bi,Cd,Co,Ga,Mo,Nb, Sb,Se,Sc,W and Yb)are below zero [(0.053-0.79)×10~(-6)];concentrations of seven elements(Cr,Ni, Pb,V,Y,Zr and Cu)are(1.0-6.0)×10~(-6);concentrations of four elements(Ti,Mn,Ba and Zn)are 10- 20×10~(-6);and concentrations of five elements(Si,Al,Fe,Mg and Sr)are(47.44-268.11)×10~(-6).The taxonomic characteristics of the 29 elements were studied separately in mollusk shells such as Chamalea gallina(Linné),Pitar-rudis(Poll),Nassarius reticulatus(Linné),Venerupis senescens (Coocconi),Mytilus galloprovincialis(Lamarck),Mytilaster lineatus(Gemelin in Linné)and Chlamys glabra.It was found that,in mollusk taxonomy,the elements have unique values.In other words, element concentrations in various mollusk shells depend mainly on the taxonomic characteristics of mollusks.In various bionomic environments different element distributions of the same species are attributed to the different geochemical characters of the each environment.Data obtained in this study indicate that the organisms are the most active and deterministic factors of the environment.  相似文献   

新疆及其毗邻地区荒漠昆虫区系的形成与演变   总被引：1，自引：0，他引：1  

黄人鑫  HU Hong-ying  吴卫  范兆田  索菲娅 《干旱区地理》2005,28(1):38-44

荒漠昆虫区系的形成与演变是昆虫学研究的中心议题之一,在对新疆现代荒漠昆虫区系研究的基础上,结合自侏罗-白垩纪以来新疆及其毗邻地区出现的地质事件、气候变迁、植被演替等研究资料分析表明,荒漠昆虫的祖先主要是中生型昆虫。我国塔里木盆地、东疆诸盆地、贺兰山以西及蒙古等地,被称为中央亚细亚的地区,荒漠昆虫的起源是在侏罗纪和白垩纪的交替时期,其区系形成是在白垩纪末至早第三纪的古新世;而准噶尔盆地、中亚细亚东部地区等的被称为中亚细亚的地区,荒漠昆虫的起源较中央亚细亚为晚,是在白垩纪,区系形成是在早第三纪的始新世。土著种的特化是区系形成的基本途径,物种的迁移也具有重要作用,但主要为由东到西的迁移。早第三纪末期开始的喜马拉雅造山运动使环境走向极度干旱荒漠化,带来了古荒漠昆虫区系的解体和现代荒漠昆虫区系的形成;随着喜马拉雅山的隆起和古地中海的干涸,物种的迁移逐渐变为由西向东。第四纪大冰川活动促使中亚细亚成为强大的物种形成中心,从而给新疆荒漠昆虫区系带来重大影响,致使中亚细亚成分常常占到40％以上。  相似文献   

Eocene fauna of Messel Pit Fossil Site, Germany     

Stephan Schaal 《世界地质(英文版)》2005,8(1)

The paper reports sunthetically the Cocene fauna of the Messel Pit Fossil site of Germany, in detail, including its rich taxanomic composttions, geological and paleogeographic backgroud, and the studying and applying history.  相似文献   

四川长宁双河晚奥陶世赫南特贝动物群及其对环境变化的响应     

李贵鹏  詹仁斌  吴荣昌 《高校地质学报》2009,15(3)

晚奥陶世赫南特贝动物群在空间上随水深和温度等环境梯度变化的分布型式已经得到广泛而深入的研究,但对该动物群在纵向上演变型式的研究还比较缺乏.以四川长宁双河上奥陶统观音桥组的赫南特贝动物群为研究对象,分析了该动物群的腕足动物个体密度和多样性演变趋势以及与水深、氧含量和生物扰动等环境因子的协同变化,探讨了动物群演变与环境变化之间的关系.研究表明,多样性和个体密度在观音桥组整体上呈上升趋势,最后整个动物群快速消亡,而氧含量和生物扰动强度总体上睛也呈增加趋势.奥陶纪末冈瓦纳大陆冰川的扩张所导致的全球海平面下降可能是影响赫南特贝动物群演变的主要环境因素,但氧含量的突然降低和生物扰动强度的增加也会对群落的一些特征产生影响,有时甚至成为重要的控制因子.赫南特贝动物群多样性在观音桥组顶部达到峰值,但随着海平面的突然下降迅速消亡,相比较其从下而上多样性逐渐增加的过程而言要迅速得多.  相似文献   

甘肃兰州盆地的第三纪地层及哺乳动物群   总被引：10，自引：1，他引：9  

颉光普 《地层学杂志》2004,28(1):67-80

介绍近二十多年来兰州盆地第三系研究的新成果 ,将兰州盆地的第三系和地方哺乳动物群重新进行了划分 ,将咸水河组提升为咸水河群 ,时代自早渐新世晚期至晚中新世。咸水河群中新建八个组 ,从下往上为 :韩家井组(E1 - 23) ,产南坡坪动物群 ;甘家滩组 (E23) ,产峡沟动物群 ;皋兰山组 (N1 1 ) ,产兰州动物群 ;瞿家川组 (N21 ) ,产庙嘴子动物群 ;黄羊头组 (N31 ) ,产张家坪动物群 ;饲马沟组 (N4 1 ) ,产对亭沟动物群 ;下街组 (N51 ) ,产泉头沟动物群 ;龙骨山组(N6 1 ) ,产邢家湾动物群  相似文献   

甘肃第四纪地层的划分   总被引：4，自引：0，他引：4       下载免费PDF全文

曹兴山  屈君霞  赫明林  曹炳媛 《甘肃地质》2004,13(1):16-37

本文依据新构造运动特征与地层接触关系、古地理环境与岩石地层特征、哺乳动物化石种属与产出层位、古地磁与14C测试成果,用多重地层划分概念对第四纪各统进行划分。厘定第四纪下限为2 48Ma·B·P;中更新世下限为0 73Ma·B·P;晚更新世下限为0 20Ma·B·P;早全新世下限为12 0Ka·B·P;中全新世下限为7 0Ka·B·P;晚全新世下限为2 5Ka·B·P。  相似文献   

河北省石家庄地区晚更新世晚期古菱齿象-披毛犀动物群及其古气候          下载免费PDF全文

董明星  张祥信  牛树银  庞其清  边鸿浩  张倩 《古地理学报》2011,13(4):419-425

河北省石家庄市郊区地下7～24m的古滹沱河沉积物中产出丰富的大型哺乳类化石:诺氏古菱齿象(Palaeoloxodon naumanni)、原始牛(Bos primigenius)、杨氏水牛(Bubalus youngi)、披毛犀(Coelodonta antiquitatis)、鹿(Cervus sp.)、四不像鹿(E...  相似文献   

The non-native seaweed Asparagopsis armata supports a diverse crustacean assemblage     

Pacios I  Guerra-García JM  Baeza-Rojano E  Cabezas MP 《Marine environmental research》2011,71(4):275-282

This is the first study describing the crustacean fauna associated to Asparagopsis armata, a non-native, red seaweed widely distributed along western Mediterranean coasts. First found in Australia and New Zealand, it was introduced naturally through the Strait of Gibraltar and rapidly spread out. A one-year spatio-temporal study (Feb 08-Feb 09) was carried out in the Strait of Gibraltar to characterize the spatio-temporal patterns of the associated crustacean fauna. Maximum biomass of A. armata was measured during April-June, whereas the maximum crustacean abundances were registered from June-October. In total 41 crustacean species were identified. The caprellid Caprella penantis, traditionally associated to non-polluted areas, was more abundant on Tarifa Island (higher values of dissolved oxygen and pH) than in Algeciras (lower oxygen and pH). The gammarid Podocerus variegatus was dominant in Algeciras Bay while Hyale schmidti and Apherusa mediterranea were the most abundant on Tarifa Island. Among isopods, Synisoma nadejda was only found on Tarifa Island. When compared with literature of native algae of the intertidal and shallow sublittoral, the species richness of associated crustaceans was similar in A. armata and the natives. Very little is known about the influence of this algae on altering marine communities, so complete faunistic studies dealing with other groups such as polychaetes or molluscs are necessary to properly address biogeographical, ecological and management programmes dealing with this non-native species.  相似文献   

桑沟湾大型底栖动物生物多样性研究     

王宗兴  孙丕喜  刘彩霞  刘新杰  连岩  徐玉珊 《中国海洋大学学报(自然科学版)》2011,(Z2):79-84

为了解桑沟湾大型底栖动物多样性现状,作者于2009年7月和12月对桑沟湾9个站位进行2个航次的采样,以种类组成、生物量和栖息密度为基础,采用物种多样性指数(Shannon-Wiener index)、物种丰富度指数(Species richnessindex)以及物种均匀度指数(Species evenness index)对大型底栖动物多样性及其影响因子进行了分析。结果表明:共采到大型底栖动物83种,其中多毛类45种,占种类总数的54.22%,软体动物11种(占13.25%),甲壳类23种(占27.71%),其他4种(占4.82%)。各站获得平均种类数在2～28种之间,种类最少的出现在夏季的C8站,最多的出现在夏季的C4站。不同养殖区生物多样性指数差异也很大,物种多样性(H′)和物种丰富度指数(D)均以贝类养殖区最高,藻类养殖区最低,而物种均匀度指数(J′)以贝藻混养区最高,藻类养殖区最低。生物多样性除了受种的数量及其个体密度的影响外,还与多种环境因素有关,相关性分析结果表明:水温、盐度、沉积物类型和硫化物含量是影响桑沟湾大型底栖动物生物多样性的主要环境因子。  相似文献   

ESR,U-series and paleomagnetic dating of Gigantopithecus fauna from Chuifeng Cave,Guangxi, southern China     

Qingfeng Shao  Wei Wang  Chenglong Deng  Pierre Voinchet  Min Lin  Antoine Zazzo  Eric Douville  Jean-Michel Dolo  Christophe Falguères  Jean-Jacques Bahain 《Quaternary Research》2014

Several Gigantopithecus faunas associated with taxonomically undetermined hominoid fossils and/or stone artifacts are known from southern China. These faunas are particularly important for the study of the evolution of humans and other mammals in Asia. However, the geochronology of the Gigantopithecus faunas remains uncertain. In order to solve this problem, a program of geochronological studies of Gigantopithecus faunas in Guangxi Province was recently initiated. Chuifeng Cave is the first studied site, which yielded 92 Gigantopithecus blacki teeth associated with numerous other mammalian fossils. We carried out combined ESR/U-series dating of fossil teeth and sediment paleomagnetic studies. Our ESR results suggest that the lower layers at this cave can be dated to 1.92 ± 0.14 Ma and the upper layers can be dated to older than 1.38 ± 0.17 Ma. Correlation of the recognized magnetozones to the geomagnetic polarity timescale was achieved by combining magnetostratigraphic, biostratigraphic and ESR data. The combined chronologies establish an Olduvai subchron (1.945–1.778 Ma) for the lowermost Chuifeng Cave sediments. We also analyzed the enamel δ¹³C values of the Gigantopithecus faunas. Our results show that southern China was dominated by C₃ plants during the early Pleistocene and that the Gigantopithecus faunas lived in a woodland-forest ecosystem.  相似文献