毛冠菊属的系统学研究

　　毛冠菊属是菊科21个“有问题”属中的一个，主要分布于青藏高原地区。按照林镕、陈艺林的概念，它包含了Nannoglottis、．Stereosanthus、Vierhapperia、Senecio和Doronicum5个属的成员。它曾先后被放入旋覆花族、千里光族和紫菀族，在上述三族中的亚族位置也不确定。它的许多重要性状，如舌片颜色、染色体数目等等，人们所知甚少。由于缺乏野外工作以及看不到大多数名字的模式，林镕、陈艺林对该属的修订有待深入的研究。本文研究了该属的外部形态学、微形态学、解剖学、孢粉学、细胞学、生态学以及ITS序列，确定了毛冠菊属的分类位置，并建立了一个新的属下分类系统。 1．外部形态 在检查大量标本（包括大多数模式）和野外居群考察的基础上，分析了主要外部形态学性状的变异式样及其对划定物种范围的价值。共确认以下9个种：青海毛冠菊、厚毛毛冠菊、狭舌毛冠菊、虎克毛冠菊、宽苞毛冠菊、大果毛冠菊、毛冠菊、玉龙毛冠菊和云南毛冠菊。川西毛冠菊被处理成狭舌毛冠菊的异名。 2．微形态学 在光镜下检查了毛冠菊属9种和紫菀族2个代表属的花柱的形状、花药顶端不育附属物、花药基部、花药基部、花盘、花丝领、药室内壁细胞等微形态性状。除了花柱基外，其他的微形态学在属内一致。管状花的花柱形态支持将毛冠菊属放在紫菀族，但其药室内壁细胞两极加厚式样表明它和广义的旋覆花有某些联系。 3．叶表皮研究 在光镜和电镜下检查了毛冠菊属8个种的叶表皮特征。．所有种的气孔器都为不规则型。青海毛冠菊表皮细胞的为多边形，而其他种都为不规则型。青海毛冠菊表皮角质层的加厚方式也与其他种明显不同。 4．扫描电镜下的舌片和花柱分枝特征 在扫描电镜下观察毛冠菊属8种和紫菀族7个代表种的舌片近轴面表皮细胞。发现毛冠菊属的舌片近轴面表皮细胞都为板状，并且沿细胞中央特征性加厚，这与紫菀族类型的表皮细胞一致，但毛冠菊属表皮细胞的角质层主要是纵向条纹或皱纹，而紫菀族总是横向的条纹或皱纹，明显不同。 在扫描电镜下又检查了毛冠菊属8种和紫菀族8个代表种的管状花花柱分枝近轴面的结构，结果在毛冠菊属管状花花柱分枝的近轴面都发现了柱头毛状的突起，而在紫菀族8种中没有发现。从突起的形状和位置判断，它可能是残存的、未充分发育的柱头毛。这表明雌性不育管状花可能刚刚从两性管状花演化而来。 也在扫描电镜下观察了毛冠菊属6种和紫菀族8个代表种的舌状花和丝状花的花柱分枝的远轴面，结果在毛冠菊属4种中发现了类似扫集毛状的突起。从这种突起的位置和形状判断，它可能是残余的扫集毛。这种突起在除雏菊以外的其他紫菀族代表种中缺失。 5．细胞学 检查了毛冠菊属8种的细胞学性状。结果发现毛冠菊属所有种的染色体基数都为x -9。染色体长度大约4um-lOum。核型公式：毛冠菊、厚毛毛冠菊、狭舌毛冠菊、宽苞毛冠菊和云南毛冠菊都为2n=14m+2sm+2st;玉龙毛冠菊、大果毛冠菊和青海毛冠菊都为2n=12m+4sm+2st。A1、A2值在属内没有明显差异。所有种的核型都是2A型。这表明在物种形成的过程中没有多倍化参与，毛冠菊属宜放在紫菀族而不是千里光族。细胞学证据支持毛冠菊属为一单系类群。 6．分子生物学 测定了毛冠菊属7种的ITS序列，并从基因库里下载了46个ITS序列，涵盖紫菀族14个亚属和旋覆花族、春黄菊族、金盏菊族。以旋覆花族、春黄菊族、金盏菊族为外类群。简约性分析显示，毛冠菊属在紫菀族中，并有较高的bootstrap值，在紫菀族中处于基部位置。Olearia和Chiliotrichum两个Hinterhuberinae亚族的代表属与毛冠菊属密切相关。在属下系统发育分析中，Olearia和Chiliotrichum被选做外类群。652个性状中，共有7】个信息位点（31个在ITSI，33个在ITS2，7个在5.8S）。简约性分析时只获得一棵最简约树。树上有两个明显的进化支，一支仅有青海毛冠菊一种，另一支包含其他种类。这种分支方式也得到形态学和生态学证据的支持。 7．毛冠菊属的系统学 从上述结果可以看出，毛冠菊属宜放入紫菀族中，在紫菀族中处于基部位置，与Hinterhuberinae亚族关系密切。综合上述研究结果，提出一个新的属下 分类系统： 毛冠菊属的新系统 组I单头组Sect. Monocephala T.G.Gao et YL.Chen Sect nov. 青海毛冠菊Nannoglottis ravida (C.Winkl.)Y.L.Chen 组II毛冠菊组Sect. Nannoglottis 系1．长舌系Ser. Delavayanae Ling et YL.Chen 厚毛毛冠菊Nannoglottis delavayi(Franch.)Ling et Y.L.Chen 狭舌毛冠菊Nannoglottis gynura(C.Winkl.) Ling et YL.Chen 虎克毛冠菊Nannoglottis hookeri (C.B.Clarke ex Hook.f.)Kitam. 宽苞毛冠菊Nannoglottis latisquama Ling et Y.L.Chen 大果毛冠菊Nannoglottis macrocarpa Ling et YL.Chen 系2．短舌系Ser. Nannoglottis 毛冠菊Nannoglottis carpesioides Maxim. 玉龙毛冠菊Nannoglottis hieraciphylla (Hand.-Mzt.)Ling et YL.Chen 云南毛冠菊Nannoglottis yuennanensis (Hand.-Mzt.) Hand.-Mzt.

绣球族的系统学研究

绣球科绣球族包含9属：草绣球属、叉叶蓝属、Broussaisia、常山属、绣球属、蛛网萼属、赤壁木属、冠盖藤属和钻地风属。到目前为止，绣球族内的属间关系还不清楚，族内的系统发育关系还有争论。本研究的目的是在前人研究的基础上，进一步发现新的系统学性状，为绣球族乃至绣球科补充新的证据;并综合多学科的研究结果进行分析，探讨绣球族的系统学关系。 本文研究了绣球族的外部形态学、花发育形态学、解剖学、分子系统学和分支系统学。 主要内容包括： 1. 形态学 通过标本室研究和野外观察，对绣球族植物的形态分化进行了分析。发现习性、地上茎的生存期限、花冠卷叠式、花瓣联合与否、花柱的联合程度、雄蕊的数目及排列具有系统学价值;放射花和果实是很好的分类性状，但并非可靠的系统学性状。 2. 花发育形态学 在扫描电子显微镜下，研究了绣球族常山属、绣球属、冠盖藤属、蛛网萼属共4种植物花器官发生和发育的全过程。发现它们的花萼均为螺旋式相继发生，花瓣的发生近乎同时。冠盖藤、马桑绣球及常山具两轮雄蕊，第一轮雄蕊发生于花瓣内轮正对萼片中部的位置，随后第二轮雄蕊发生于正对花瓣中部的位置。在第一轮雄蕊略靠内的位置形成第二轮雄蕊的时候，多数情况下，相邻的对萼雄蕊之间只形成1个对瓣雄蕊，但有时却形成2个对瓣雄蕊，使雄蕊群的数目略多于花被的数目。对萼雄蕊与对瓣雄蕊的分化方式基本一致，但它们在花芽中空间取向不同。 蛛网萼雄蕊数目极多，雄蕊群的发生式样较为独特，并不始于对萼三联体。最早的雄蕊于杯状体近基部发生，之后雄蕊的发生大致沿杯状体壁向上，具离心趋势。在雄蕊发生过程中杯状体继续伸长，为众多雄蕊的发生提供了空间。蛛网萼雌蕊的发生明显早于雄蕊，其它3种植物雌蕊的发生晚于雄蕊。4种植物的雌蕊在发生上较为相似，发育却不同。在常山、马桑绣球和蛛网萼中，花柱从开始到发育成熟始终分离，柱头在每个花柱的顶端形成;而冠盖藤属的花柱裂片从开始就是联合的，最终形成单一的花柱，柱头从合生花柱顶端远轴面分化形成。 3. 解剖学 在光学显微镜和扫描电子显微镜下，观察了绣球族9属42种1变种及近缘8属11种共53种1变种的叶表皮特征。发现气孔的分布、气孔器的类型、表皮细胞的形状及其垂周壁式样、毛被等具有一定的系统学意义和分类价值。绣球族各属的气孔仅散生于下表皮;而在绣球族的几个近缘属中，上下表皮均有气孔分布。气孔器在多数类群中为无规则型，仅常山属和绣球属离瓣组的成员为平列型。气孔多为椭圆形，稀近圆形;外拱盖表面通常光滑，仅在钻地风属中具条状纹饰;外拱盖内缘具环状加厚，近全缘、不规则波状或浅波状。表皮细胞在多数种中为不规则形，垂周壁波状、浅波状或深波状;在有些种中为（近）多边形，垂周壁平直或弓形。叶表皮细胞形状、垂周壁式样在绣球族寡种属属级水平比较稳定，但在绣球属中变化较大。表皮角质膜纹饰形态多样，有网纹、粗网纹、浅波状条纹、波状条纹、条纹、粗条纹及丝状条纹;在钻地风属及绣球属的少数种中，角质膜条纹有时汇集呈球形或玫瑰型。表皮毛状附属物有单细胞2分枝毛（黄山梅属）、多细胞星状毛（星毛冠盖藤）、单细胞星状毛（溲疏属）和单细胞不分枝毛四种。对钻地风属所有种的观察结果表明，仅在椭圆钻地风的下表皮细胞中央观察到乳突状结构，而在白背钻地风和圆叶钻地风中并未观察到前人描述的附属物。 4. 叶绿体DNA trnL-F序列的分析 首次对绣球族9属23种及近缘类群3属3种的trnL-F序列进行了测定。序列长度在860 bp~970 bp范围内变化。在以山梅花属、溲疏属和黄山梅属为外类群，基于trnL-F序列构建的系统树上，绣球族作为一个单系群得到很高的支持率。绣球属的种出现在不同的分支上，表明该属不是一个单系群。绣球族被分为两大支：第一支由绣球属离瓣组的中国绣球、绣球、以及常山和Broussaisia arguta组成;第二支由绣球属另外的9个种与草绣球属、叉叶蓝属、蛛网萼属、赤壁木属、冠盖藤属以及钻地风属组成。在第二支中，下列类群的近缘关系得到支持：① 草绣球与叉叶蓝属;② 绣球属挂苦子组的东陵绣球、圆锥绣球和挂苦绣球。③ 钻地风属、赤壁木属和冠盖藤属;④ 蜡莲绣球、莼兰绣球、马桑绣球、粗枝绣球。 5. 分支分析 以山梅花属为外类群，基于形态、解剖、花发育、孢粉等32个性状（或性状状态）对绣球族9属的系统发育关系进行了分支分析。结果表明：草绣球属和叉叶蓝属为基出类群，这两个属有多个共同特征;绣球族其余的成员聚成一支，该支又有5个分支。其中蛛网萼属和绣球属冠盖组各为单独的分支，它们有多个自衍征，可能有各自独立的演化线;绣球属离瓣组与常山属聚成一分支，二者的密切关系得到解剖学证据的支持;绣球属绣球组和星毛组聚成一分支，这两个组包含了绣球属的多数种类;钻地风属、赤壁木属、冠盖藤属、Broussaisia和绣球属挂苦子组聚成一分支。其中钻地风属、赤壁木属与冠盖藤属具多个近裔衍征，表明它们是绣球族的晚出类群。 通过对绣球族植物外部形态、花器官发生、叶表皮微形态特征、叶绿体DNA trnL-F区的研究以及基于形态性状的分支分析，并综合已有的研究结果，我们认为： 1. 绣球族是一个单系群;绣球属不是一个单系群。 2. 在绣球族中，草绣球属和叉叶蓝属关系密切，它们可能是绣球族其余成员的姐妹群。 3. 绣球组和星毛组可能是绣球属的核心成员;离瓣组和常山属关系密切;冠盖组有单独的演化线。 4. 赤壁木属、冠盖藤属和钻地风属为单系群，它们在绣球族处于较高的演化位置。 5. 绣球属需重新界定。

基于微形态特征的中国瓦韦属植物分类的再修订

通过野外采集和观察，标本鉴定和实验研究，从植物形态学，叶柄和根状茎的解剖，叶表皮的显微观察，和孢子形态的扫描电镜观察等方面进行研究与分析，对中国瓦韦属（除薄叶组）进行了分类学修订研究。 1. 形态性状分析 研究了国内外重要标本馆的大量瓦韦属植物标本，通过对一些重要的形态性状的观察和分析，判定其变异规律及分类学意义。根状茎上的鳞片和孢子囊上的隔丝的形状和网眼结构是瓦韦属属下分类和种的划分的最主要的形态学性状。其它特征如孢子囊群着生的位置、中脉的颜色、根状茎直立或横走等在种内也具有一定的稳定性，可以帮助种的划分和鉴定。因此，在对瓦韦属植物进行分类时要结合几个相关性状而不是单一的性状进行分类。 2. 叶柄和根状茎的解剖 对瓦韦属（除薄叶组）49 个种的叶柄和根状茎进行解剖观察，发现叶柄中维管束的条数一般为1--7 条不等，排成一字形、三角形或半圆形。两根粗的维管束排列在腹面，较细的维管束排列在背面。叶柄中没有厚壁组织，但是在叶柄和根状茎的连接部位叶足处有厚壁组织的存在。根状茎横切面观察显示除了维管束外还有厚壁组织的存在，在常绿种内厚壁组织较多，落叶类型中厚壁组织较少。 3. 叶表皮形态 观察了瓦韦属51 个种的叶表皮形态和结构，发现该性状对于属下划分具有一定的系统学意义，也有助于疑难物种的鉴别。瓦韦属植物的叶表皮细胞形状通常为多边形、不规则；垂周壁式样为波状和浅波状；气孔器类型比较复杂，在所观察的类群中，气孔器都分布在下表皮上，极细胞型Polocytic type，共环极细胞型Copolocytic type ，腋下细胞型Axillocytic type ，聚腋下细胞型Coaxillocytic 是最常见的类型，不规则型Anomocytic type ，不规则四细胞型Anomotetracytic type，不等细胞型Anisocytic type，辐射状细胞型Actinocytic type 和双环不等四细胞型Amphicycloanisocytic type 也存在于瓦韦属的叶表皮中。属下同一个组的叶表皮特征近似，不同的组具有一定的差别。 4. 孢子形态 在扫描电镜下对瓦韦属50 个种的孢子形态进行了观察。瓦韦属的孢子两侧对称，极面观为椭圆形，赤道面观为肾形、豆形或半圆形。孢子的表面纹饰可以分为6 类，分别是光滑、颗粒状、瘤状、皱状、波状以及疣状的纹饰。瓦韦属的孢子周壁较薄，纹饰由外壁组成。孢子形态具有重要的系统学意义，可以为属下分类提供可靠的证据，对形态近似的物种的划分也有重要参考价值。 通过对大量标本的研究，以及模式标本的考证，结合野外居群观察，综合分析有关分类学资料，主要依据比较稳定的微观性状，对瓦韦属植物进行了新的分类学修订。结果承认中国瓦韦属（除薄叶组）有37 种，可以分为5 个组，有3 个名称被首次处理为异名，另有2 个种暂时存疑。

中国蔷薇属芹叶组（Rosa Sect. Pimpinellifoliae DC. ex Ser.）的分类学研究

本研究通过我国CDBI、 KUN、PE、SZ等主要标本馆约3, 500份馆藏标本的研究和野外考察相结合，对我国蔷薇属（Rosa L.）芹叶组(Sect. pimpinellifoliae DC. ex Ser.）植物以及相关组的一些种进行了性状特征、形态和微形态的研究，对该组的一些种的形态特征描述进行了补充，同时给出详细的地理和海拔范围分布图。综合花粉以及种子（瘦果）形态的研究结果重新制订了分种检索表，同时，对该组一些形态相近容易混淆的种进行了对比研究，特别对一直存在争议的绢毛复合体（绢毛蔷薇R. sericea Lindl.和峨眉蔷薇R. omeiensis Rolfe）进行了大量宏观形态特征的研究，并用光学显微镜（LM）和扫描电镜(SEM)对二者的花粉及种子形态、微形态进行对比研究和分析，主要研究内容包括： 1. 芹叶组孢粉研究 对芹叶组的10个种及相关的4个组共17个种（18个样品）的植物花粉进行了光镜和扫描电镜观察和比较研究。研究结果表明：蔷薇属植物花粉粒大小为中等偏小，极轴长23.98[21.82(R. graciliflora Rehd. et Wils.)～29.18(R. tsinglingensis Pax. et Hoffm.)] μm，赤道轴长28.65[24.15（R. graciliflora）～34.70(R. davidii Crép.)] μm；花粉属辐射对称等极单花粉，花粉形态赤道面观呈球形到超长球形；极面观为三裂圆形或近圆形,三孔沟，孔缘加厚,具中部突起的桥状盖。花粉外壁纹饰为条纹状，光镜下形态特征相差不大；在电镜下外壁条纹和脊沟内穿孔的形状、大小和频度等特征，常具组至种水平上的可见变异，可作为组至种水平划分的依据。 根据花粉外壁条纹特征及穿孔形状和数目等特征，本研究将这些植物的花粉归为5个类型，并编制了分组检索表。同时，根据条纹状的清晰度，排列方式、条纹形状、穿孔大小及其频度等方面的差异，各有特点，对该组的10个种编制了分种检索表。 2. 芹叶组种子形态研究 应用光学显微镜和扫描电镜对我国蔷薇属芹叶组14个种及相关组5个组共36种植物的种子宏观形态及种皮微形态特征进行了观察研究。结果显示，蔷薇属种子形态多样,形状分别为肾形、卵形或锥形等；种子颜色以淡棕色、褐色以及土黄色为主；种子大小种间相差悬殊，相对体积为（长×宽×厚）36.66（4.79～114.47) mm3。光镜下，种子宏观形态特征具组内一致性，在扫描电镜下种子表面结构特征因种而异，其纹饰以网纹为主，可分为3种类型，即近平滑型、负网纹型和网纹型。研究结果表明，蔷薇属种子表面纹饰与地理分布关系不大,具有组及种内稳定性。其种子形态、大小、表而纹饰类型等特征可作为蔷薇属组及种水平上的分类依据。 结合蔷薇属花粉形态研究结果，得出蔷薇属种皮微形态特征与花粉外壁纹饰特征相吻合，在代表组及种的特征上具相关性的结论。同时根据种子形态、微形态结构特征的组间区别和种间差异编制了分组及芹叶组14个种的分种检索表。 3. 绢毛蔷薇复合体的研究 通过对大量标本的研究、野外观察以及扫描电镜对绢毛蔷薇复合体的花粉形态和种皮表面结构进行研究，通过对小叶、花粉及种子的形态定量分析结果支持Rowley (1959)的观点，将峨眉蔷薇处理为绢毛蔷薇的一个变种。 综上研究结果得出，蔷薇属植物的小叶片数目、花被基数以及花粉及种子形态等性状是较为稳定的，这些特征可很好的作为分类学依据。 The morphology, pollen exine sculpture and seed coat structure of the species of Rosa sect. Pimpinellifoliae and related sections were studied.About 3,500 herbarium specimens at CDBI, KUN, PE, and SZ were examined. Field work in Sichuan and Yunnan were conducted. Revisions of some species were carried out and a new key to species of sect. Pimpinellifoliae was proposed based on morphology, pollen exine sculpture and seed coat structure, Detailed morphological descriptions, geographical distributions and the altitudinal ranges of some taxa are given. The systematics of the species complex, the Rosa sericea complex (R. sericea Lindl. & R. omeiensis Rolfe), was emphasized. This thesis focused on the following three aspects: 1. Pollen morphology of Rosa sect. Pimpinellifoliae The pollen morphology of 18 samples representing 10 species of the Eurasian Rosa sect. Pimpinellifoliae and 7 additional species of related sections was investigated under LM and SEM. The pollen grains are monadic, actinomorphic, equipolar, medium-sized, spheroidal to perprolate in equatorial view, 3-lobed circular or semi-circular in polar view, crassimarginate, pontoperculate, and with striate exine sculpture. The striate sculpture varies among sections and species. The equatorial axis ranges from 17.97 μm (R. sikangensis) to 29.18 μm (R. tsinglingensis) with an average of 23.98 μm in length, while polar axis varies from 24.15 μm (R. gracilifolra) to 34.70 μm (R. davidii) with an average of 28.65 μm in length. The pollens can be divided into five types based on striate sculpture and a key to the sections sampled was proposed accordingly. The pollen morphology of species of sect. Pimpinellifoliae is more homogeneous and different from other sections sampled and did not support the two-series subdivisions in sect. Pimpinellifoliae. A key is also provided based on characers of pollen morphology among species in sect. Pimpinellifoliae. 2. Seed coat structure of Rosa sect. Pimpinellifoliae The seed coat structure of 39 samples representing 14 species of Rosa sect. Pimpinellifoliae and 12 additional species of related sections was investigated under LE and SEM. The seed relative volume (Length × width × thickness) ranges from 4.79 to 114.47 mm3 with an average of 36.66. mm3. The seeds are reniform, ovate or oblong in shape, with orange-brown, light brown or deep brown color. Seed coat sculpture was reticulate or striate-like reticulate. There was no difference in sculpture character of various speices under LM, while three types of seed coat sculpture were identified under SEM and a key to species based on the seed coat sculpture was provided. The three types of seed coat sculpture were nearly smooth, areolate and reticulate. The study of the seed coat sculpture of same species sampled from different populations showed that characters on the seed coat are stable, and thus the size, shape and seed coat sculpture can be used in species level identification. Interestingly, characters in the seed coat sculpture and the pollen morphology in sect. Pimpinellifoliae are consistent at in specific or sectional levels. A key to the 14 species sampled was given based on seed coat sculpture. 3. The study on Rosa sericea complex The Rosa sericea complex contains R. omeiensis and R. sericea. They are morphologically similar to one another and the systematic status of R. omeiensis has been controversial. In this study we examined large numbers of herbarium specimens of R. omeiensis and R. sericea and conducted field observations in the Hengduan Mts.. We also performed SEM study of pollen morphology and seed coat structure of R. omeiensis and R. sericea. We further carried out intensive morphometric study on the leaflet, pollen, and seed morphology. Our results showed that R. omeiensis should be sunk to be a variety of R. sericea, just as Rowley’s treatment in 1959. In conclusion, the features in the number of leaflet and petal, and the morphological character on pollen and seed are relatively stable. Therefore these characters are very useful in taxon delimition.

Explanation for Micromorphologies Around Broken Fibers in Fiber-Reinforced Composites

Experimental observations on micromorphologies around broken fibers in glass-fiber-reinforced epoxy matrix composites reveal different kinds of highly oriented patches at the circumambience of broken fibers, whereas the bulk of the matrix has been observed to be largely isotropic. These patches are interpreted to correlated areas where the stress gradients of the matrix are formed after fiber breaking, but the underlying cause for the orientation is still unknown. The authors have modified an embedded cell model to explain the experimental phenomena. The finite element simulation indicates that the surfaces around broken fibers display a change from an extension micromorphology to a mixed tension and shear micromorphology with the increase of applied strain.

Mineralogy of smectites in the surface sediments from the East Pacific and its significance

XRD, TEM, SEM and EDS are employed to analyze smectites in the clay fraction of the surface sediments from the East Pacific. It is shown from the XRD results that the clay fraction consists of about 20% smectites. Three types of smectites are identified, Fe-rich (Type I), Fe, Mg-rich (Type II) and Na,Ca smectite (Type III), and most of them are not well-crystallized. Type I is widely distributed in sediments, showing honeycomblike in the SEM, and aggregated or dispersive hairlike, or cloudy assemblage with a bit curl near its edge in the TEM. This type is considered to be typomorphic type of authigenic smectite in the East Pacific. Type II is similar to Type I in micromorphology in the TEM, showing a transition micronite, while Type III is tabletlike in the TEM with an unclear edge. Type I may be altered from volcanics and some of them even precipitated from the low subthermal water. Type II could also be formed in the ocean floor, while Type III comes from dry and distant continental area. This study suggests that the characteristic of chemical composition and morphology of smectite may give a clue to understand sediment source, origin of minerals and sedimentation in the deep sea.

Characteristics of clay minerals in the northern South China Sea and its implications for evolution of East Asian monsoon since Miocene

Clay mineral assemblages, crystallinity, chemistry, and micromorphology of clay particles in sediments from ODP Site 1146 in the northern South China Sea (SCS) were analyzed, and used to trace sediment sources and obtain proxy records of the past changes in the East Asian monsoon climate since the Miocene, based on a multi-approach, including X-ray diffraction (XRD) and scanning electron microscopy combined with energy dispersive X-ray spectrometry (SEM-EDS). Clay minerals consist mainly of illite and smectite, with associated chlorite and kaolinite. The illite at ODP Site 1146 has very well-to-well crystallinity, and smectite has moderate-to-poor crystallinity. In SEM the smectite particles at ODP Site 1146 often appear cauliflower-like, a typical micromorphology of volcanic smecites. The smectite at ODP Site 1146 is relatively rich in Si element, but poor in Fe, very similar to the smectite from the West Philippine Sea. In contrast, the chemical composition of illite at ODP Site 1146 has no obvious differences from those of the Loess plateau, Yellow River, Yangtze River, and Pearl River. A further study on sediment source indicates that smectite originates mainly from Luzon, kaolinite from the Pearl River, and illite and chlorite from the Pearl River, Taiwan and/or the Yangtze River. The clay mineral assemblages at ODP Site 1146 were not only controlled by continental eathering regimes surrounding the SCS, but also by the changing strength of the transport processes. The ratios of (illite+chlorite)/smectite at ODP Site 1146 were adopted as proxies for the East Asian monsoon evolution. Relatively higher ratios reflect strongly intensified winter monsoon relative to summer monsoon, in contrast, lower ratios indicate a strengthened summer monsoon relative to winter monsoon. The consistent variation of this clay proxy from those of Loess plateau, eolian deposition in the North Pacific, planktonic, benthic foraminifera, and black carbon in the SCS since 20 Ma shows that three profound shifts of the East Asian winter monsoon intensity, and aridity in the Asian inland and the intensity of winter monsoon relative to summer monsoon, occurred at about 15 Ma, 8 Ma, and the younger at about 3 Ma. The phased uplift of the Himalaya-Tibetan plateau may have played a significant role in strengthening the Asian monsoon at 15 Ma, 8 Ma, and 3 Ma.

甘肃临夏盆地龙担剖面晚新生代磁性地层与古环境

Linxia Basin, situated in the northeast belt of the Tibetan Plateau, is a late Cenozoic depression basin bounded by the Tibetan Plateau and the Chinese Loess Plateau. The Cenozoic deposition, spanning over 30Ma, in which very abundant mammal fossils were discovered, is very suitable for study of uplift processes and geo-morphological evolution of the Tibetan Plateau. The Longdan section (35°31′31.6″N，103°29′0.6″E) is famous for the middle Miocene Platybelodon fauna and the late Miocene Hipparion fauna for a long time and is also one of the earliest known places for wooly rhino, which lies on the east slope of Longdan, a small village of township Nalesi in the south of the Dongxiang Autonomous County, Linxia Hui Nationallity Autonomous Prefecture. The Longdan mammal fauna was discovered at the base of the Early Pleistocene loess deposits at Dongxiang, where the lithology is different from the typical Wucheng Loess on the Chinese Loess Plateau. The rich fossils contain many new species and the major two layers of fossils are in the loess beds. Geologically the fossiliferous area is located in the central part of the Linxia Cenozoic sedimentary basin. Tectonically the Linxia Basin is an intermountain fault basin, bordered by the Leijishan major fault in the south and the north Qinling and Qilianshan major faults in the north. The section is 51.6m thick above the gravel layer, including the 1.6m Late Pleistocene Malan Loess on the top and the other loess-paleosol sequences in the middle of the section. The base of the section is the Jishi Formation, consisting of gravel layer of 13 ~ 17m thick. In this study, 972 bulk samples were collected with an interval of 5cm and other 401 orientied samples were taken with a magnetic compass. In the laboratory, the paleomagnetism, medium grain size, susceptibility, color, micromorphology, anisotropy of magnetic susceptibility were analyzed. From the stratigraphic analysis, the Longdan section from the top 0.3m to the bottom 51.6m, containing 5 normal polarities (N1-N5) and 5 reversal polarities (R1-R5). The paleomagnetic results show N3 is the Olduvai subchron in the middle of the Matuyama chron, and then the chronology of the Longdan mammal fauna is constructed along the section. The Matuyama-Gauss boundary is 45m and N5 enters Gauss chron. The Olduvai subchron with the age of 1.77 ~ 1.95Ma is found just in the upper fossiliferous level of Longdan mammal fauna. Taking the deposit rate of the section into account, the geological age of the upper fossiliferous level of Longdan mammal fauna is estimated to be about 1.9Ma. The lower fossiliferous level is just below the Reunion subchron and its age is estimated to be 2.25Ma. In addition, anisotropy of magnetic susceptibility of the loess-paleosol and other climatic indexes were used for discussing the late Cenozoic paleoenvironmental changes at Longdan, from which the Longdan area should have been an area of predominantly steppe the same as the Longdan mammal fauna.