松科早期球果研究的历史与现状

本文主要对早白垩世到老第三纪渐新世这段时间的松科化石球果的研究作了系统回顾和总结。松科化石球果的研究经历了一个由分散、幼稚到系统、成熟的发展过程,现在将松科化石球果分为三个属：Ｐｉｔｙｏｓｔｒｏｂｕｓ、Ｐｓｅｕｄｏａｒａｕｃａｒｉａ及Ｐｉｎｕｓ。其中Ｐｓｅｕｄｏａｒａｕｃａｒｉａ及Ｐｉｎｕｓ为两个自然属,Ｐｓｅｕｄｏａｒａｕｃａｒｉａ已经绝灭。Ｐｉｔｙｏｓｔｒｏｂｕｓ作为一个器官属,包括那些在松科中分类位置不明的球果。对松科化石球果进行细致的外部形态及内部结构的研究主要目的在于演化关系的探讨上：对于Ｐｉｎｕｓ,主要探讨这个属内各个亚属、组、亚组之间的演化关系;对于Ｐｉｔｙｏｓｔｒｏｂｕｓ和Ｐｓｅｕｄｏａｒａｕｃａｒｉａ,通过绝灭类型的分析,探索松科内各个类群（包括绝灭的）的演化关系进而完成进化树是研究的主要方向,现在这方面已有了Ｐｉｎｕｓ中心说及Ｐｓｅｕｄｏａｒａｕｃａｒｉａ分支说两个假说。     

松科的核型和系统发育研究

松科通常主要依据长、短枝及叶等的形态特征分成冷杉亚科、落叶松亚科和松亚科。该科各属的核型可以划分成5个类型：(1)松型(24(22)m+0(2)sm);(2)冷杉型((22～14)m十(2～l0)sm(st));(3)落叶松型(12m+12sm(st));(4)花旗松型(10m+12sm+4t);(5)金钱松型(4sm+40t(4SC))。本文根据核型资料的比较分析,各属从原始到进化的顺序可能是：松属(松型核型)-银杉属、云杉属、铁杉属、(雪松属)、油杉属、冷杉属(冷杉型核型)→黄杉属、落叶松属(花旗松型核型和落叶松型核型)→金钱松属(金钱松型核型)。这个顺序和亲缘关系在以核型的平均臂比为纵坐标、染色体长度比为横坐标的坐标图上得到清楚反映(不包括金钱松属)。核型为K(2n)＝44＝4sm+40t(4SC)的单型属金钱松属不仅在染色体数目和核型上与其他各属差异明显,而且具有独特的习性和-系列形态学和解剖学的特征,如落叶乔木(仅同落叶松属),短枝之叶簇状密生而辐射平展呈圆盘状,叶枕在落叶后密集成环节状,雄球花多数簇生短枝顶端,种鳞卵状披针形,成熟时与基部贴生的苞鳞连同崩解的球果中轴一起脱落,叶中3个树脂道及其分布,维管束帽缺如以及传输组织铁杉型(仅同铁杉属)等。因此,本文将金钱松属提升为一个新亚科Pseudolaricoideae L.C．Li,并把原来的3个亚科降为相应的族而隶于松亚科。松科里唯一具K(2n)=24＝12m+12sm(st)核型的黄杉属和落叶松属组成落叶松族,而雪松属按其核型与冷杉族更相近而置于该族。本文根据核型资料建立的松科新系统也得到形态、解剖、植化、免疫、生化、胚胎及占植物等学科有关资料的支持。本文还讨论了前人的松科演化系统。     

马尾松雌球果的发生和早期发育研究

采用常规石蜡制片技术对马尾松雌球果的发生和早期发育进行了研究。结果表明：雌球果原基发生时间为10月中旬,不同的树龄和着生部位,其发生时间不同。雌球果原基与营养茎端在外部形态及内部细胞组织学分区结构有明显差异。营养茎端外形扁平,内部顶端分生组织结构有顶端原始细胞区、中央母细胞区、形成层状过渡区、周围分生组织区及肋状分生组织区5个明显的分区;而雌球果原基外形呈圆锥状,内部结构只有套层和髓区。12月初,最初的苞片原基在雌球果原基的鳞片的叶腋处产生,之后其由基部向顶部连续发生。翌年1月初,在苞片原基的叶腋处,珠鳞原基发生,发生方向亦为向顶发育。2月底,苞片体积不再发生变化,珠鳞膨大端的基部的近轴面分化出2个倒生胚珠。从雌球果原基发生到胚珠分化历时4个多月。亚热带的冬季气候对马尾松雌球果的生长发育没有明显的抑制作用。     

中国松科植物的分布型和区系分析

简介松科研究的新进展,根据新近资料划分中国松科植物10属95种的分布型和进行区系分析,结果是北温带分布4属,东亚-北美间断分布2属,中国特有3属和越南-华南分布1属。25个种分布型分属于欧亚温带、东亚和亚洲热带3个植物区域。比较详细分析其4点主要特征;分布的区域差异和不平衡,高的特有性,间断分布和替代分布等。     

松科冷杉属植物的化石历史和现代分布

冷杉是北半球阴暗针叶林的优势种和建群种,现全世界共有52种1亚种12变种,在北半球形成南欧、北美和东亚三个分布中心,这三个地区也是冷杉属化石最丰富的地区。在垂直分布上,冷杉集中分布于1000～2000m（15种）和2500～4000m（13种）两个海拔地段。在中国,冷杉植物呈南北间断分布,集中分布在横断山地区。冷杉属的特有现象和孑遗分布现象都十分突出,有7个种呈孑遗分布。根据冷杉属的地史分布和现代分布的研究并结合最新的系统演化资料,本文推测冷杉属于白垩世中期起源于北半球的中高纬度地区,始新世以后,随着全球气候的变冷,逐步向南迁移,由于喜马拉雅山脉、阿尔卑斯山、落基山脉抬升及东亚季风气候的出现以及第四纪冰期的影响而形成了现代间断的分布格局。冷杉与银杉、金钱松等其它松科植物的形成模式十分相似。     

杉科的细胞分类学和系统演化研究

根据杉科的核型资料,本文(1)提出“1B”可能是一个新的高等植物核型类型;(2)讨论了各属的有关分类学问题及相互亲缘关系,它们的进化顺序可能是柳杉属、水松属、落羽杉属、水杉属、巨杉属、红杉属、杉木属(密叶杉属与之近缘)、台湾杉属;(3)支持金松属分立成金松科,它可能比杉科各属原始; (4)红杉(AAAABB)的亲本可能是二个古代种“水杉”和“巨杉”,它们的直接后裔或留下的近缘是水杉和巨杉;(5)杉科存在A和L两条进化路线,前者包括柳杉属、水松属、落羽杉属、台湾杉属;后者包括水杉属、巨杉属、红杉属、杉木属(密叶杉属);(6)提出一个杉科新系统(包括一个新亚科):Ⅰ.柳杉亚科(柳杉属),Ⅱ.落羽杉亚科(水松属、落羽杉属),Ⅲ.红杉亚科(水杉属、巨杉属、红杉属),Ⅳ.杉木亚科(杉木属、密叶杉属),Ⅴ.台湾杉亚科,新亚科(台湾杉属)。本文还对前人的杉科系统作了讨论。     

杉科的细胞分类学和系统演化研究

根据杉科的核型资料,本文(1)提出“1B”可能是一个新的高等植物核型类型;(2)讨论了各属的有关分类学问题及相互亲缘关系,它们的进化顺序可能是柳杉属、水松属、落羽杉属、水杉属、巨杉属、红杉属、杉木属(密叶杉属与之近缘)、台湾杉属;(3)支持金松属分立成金松科,它可能比杉科各属原始;(4)红杉(AAAABB)的亲本可能是二个古代种水杉”和“巨杉”,它们的直接后裔或留下的近缘是水杉和巨杉;(5)杉科存在A和L两条进化路线,前者包括柳杉属、水松属、落羽杉属、台湾杉属,后者包括水杉属、巨杉属、红杉属、杉木属(密叶杉属);(6)提出一个杉科新系统(包括一个新亚科)：I．柳杉亚科(柳杉属),II．落羽杉亚科(水松属、落羽杉属),III．红杉亚科(冰杉属、巨杉属、红杉属),Ⅳ.杉木亚科(杉木属、密叶杉属),V．台湾杉亚科,新亚科(台湾杉属)。本文还对前人的杉科系统作了讨论。     

雪胆属植物化学研究历史和现状

葫芦科雪胆属植物在亚州东南部,中国和靠近中国南部的印度、越南、缅甸均有分布。五十年代初期发现该属植物约七种。1970年云南民间用小蛇莲(俗名)、又名曲莲、园果雪胆(H.amabilis Diels)的地下茎治疗肠炎、菌痢效果良好。我们从中分离到结晶的苦味质称为雪胆素(为两个成分的混晶),具有良好的抗菌作用。对于该属植物当时未见文献记载其化学研究和任何利用价值。因此合同中科院上海有机化学研究     

On Pseudoaraucaria Fliche emend., a Genus of Fossil Pinaceous Cones

The type material of some fossil Pinaceous cones (from the Albianof France) originally described by Fliche in 1896 under thename Pseudoaraucaria is here redescribed in detail. The conesare similar in form to one from the English Lower Greensandhitherto called Pityostrobus benstedi (Mantell) Seward whichis also redescribed here. This newly recognized group of conesdiffers from the cones of any of the recent members of the Pinaceaechiefly by (a) the massive ridge of scale tissue lying betweenthe seeds so that these are deeply embedded in the basal partof the scale, and (b) the presence of a cushion of parenchymaat the chalazal end of the seed. The probable significance ofthese and certain other characters is discussed.     

化石燃料生物脱有机氮研究展望

化石燃料中与有机硫相似的另一类孤对电子含氮有机化合物的存在对生产和环境造成许多危害。石油中的含氮有机化合物是影响炼油工艺、产品性能质量的主要因素。含氮有机化合物具有致癌、致突变性 ,燃烧后则以NOx的形式释放污染大气。化石燃料中所含的有机氮较有机硫更难以去除 ,常规的化学脱有机氮技术高压加氢法处理燃油能耗高 ,处理效果不理想等方面的缺陷使人们思考生物脱氮的可能性。考察了国内外近十多年来化石燃料生物脱有机氮工作的研究进展 ,包括模式有机氮化合物微生物的代谢途径 ,以及相应的代谢途径中的关键酶及其编码基因等方面的研究。     

Fossil ovipositions of dragonflies: Review and interpretation

The paper deals with the stratigraphic range and morphology of fossil formations on plants interpreted as insect ovipositions. Our analysis of the insect fossil record has shown that the endophytic ovipositions probably belong to the Kennedyina and Triadophlebiina (in the Paleozoic and Lower Mesozoic) and to the Calopterygina (in the Upper Mesozoic and Cenozoic).     

Some Fossil Plants from Early Jurassic in Western Hubei With the Relative Problem Between Fossil Plants and Coal-Bearing

Coniopteris magnifica sp. nov., Ctenophyllum chenyuanense sp. nov., C. laxilobum sp. nov., Mironeura dakengensis Zhou, are derived from the Xiangxi Formation (s.s.), Western Hubei. According to the aspect and characteristic of the Xiangxi flora, author considers the Xiangxi Formation as Early Jurassic in age. In this paper, the relative problem between the coal-bearing and the fossil plants is briefly discussed also.     

Fossil Plants and Their Assemblages from the Early Carboniferous in Guangdong

This paper deals with the Lower Carboniferous fossil plants, 19 genera and 41 species including 10 new species, such as Sublepidodeneron wcwgtanense, Lepidodendron sophoroides, Adiantites lianpingensis, A. matouensis, Archaeopteridium shaoguanense, Rhacopteris angusta, Rhodeites lanceolata, Neuropteris shaoguanensis, Potoniea turbinata and P. racemicarpa. According to the distributive regularity of those fossils in stratigraphic section of Early Carboniferous from Guangdong area, the authors propose to divide the flora into three assemblages from lower to upper, namely, 1, Sublepidodendron mirabile assemblage; 2. Cardiopteridium spetsbergense-Adiantites gothanii assemblage; 3. Archaeopteridium-Sphenopteris obtusiloba assemblage, which separately represent the dispositions of Dahu Formation (the 1st assemblage), the lower part of Ceshui Formation (the 2nd assemblage) and upper part of Ceshui Formation or middle part of Zhongxin Formation (the 3rd assemblage).     

评介T.P.琼斯和N.P.罗合编的《化石植物和孢粉的现代技术》

二十世纪后半叶以来,由于国际上对能源需求的急剧增长,使地质勘探,特别是石油勘探事业迅猛发展,这刺激了孢粉分析技术的改进和一些新技术的出现。尤其是二十世纪六十年代中期起,显微技术的创新(特别是扫描电镜、透射电镜和共聚焦显微技术)、地球化学(特别是生物地球化学)手段的革新、化石植物中基因物质的提取以及计算机数据分析的应用,使古植物学的研究方法和技术从根本上改变了原来的面貌。     

Review of the Fossil Evidence for the Origin and Earliest Evolution of the Seed-plants

The earliest identified seed-plants are found in Latest Devonian aged sediments from Northwest Europe and North America and are believed to have evolved from within the progymnosperms, a group of anatomically advanced pteridophytic plants. However, current evidence makes it problematic to determine from which particular progynmospermous lineage the seed-plants evolved, with the major contender being the Aneurophytalean progymnosperms. The evidence for the ancestral stock to the seed-plants is summarised and the morphologies of the earliest known seed-plants are considered. From their first geological occurrence, the seed-plants are morphologically diverse to such an extent that the identification of a single potential ancestral morphology is impossible. In the light of the evidence so far presented, the precise origin of the seed-plants is unresolved and in need of new evidence relating to the progynmosperm/seed-plant transition. Future lines of research are also suggested.     

Literature Review: The Scanning Electron Microscopy of Fossil Seeds

The monograph on Miocene fruits and seeds from Denmark by E.M. Friis (1985) is reviewed. Many of the SEM pictures in thiswork show varying stages of degradation of the exotesta whichraise problems in the interpretation of surface features ofthe fossil seeds revealed by SEM. The stages of exotesta degradationhave been produced experimentally with ultrasonics on Recentseeds of the Theaceae, and show how surface features which areregarded as taxonomically useful may be affected by such treatment.     

Fossil evidence for a herbaceous diversification of early eudicot angiosperms during the Early Cretaceous

Eudicot flowering plants comprise roughly 70% of land plant species diversity today, but their early evolution is not well understood. Fossil evidence has been largely restricted to their distinctive tricolpate pollen grains and this has limited our understanding of the ecological strategies that characterized their primary radiation. I describe megafossils of an Early Cretaceous eudicot from the Potomac Group in Maryland and Virginia, USA that are complete enough to allow reconstruction of important life-history traits. I draw on quantitative and qualitative analysis of functional traits, phylogenetic analysis and sedimentological evidence to reconstruct the biology of this extinct species. These plants were small and locally rare but widespread, fast-growing herbs. They had complex leaves and they were colonizers of bright, wet, disturbance-prone habitats. Other early eudicot megafossils appear to be herbaceous rather than woody, suggesting that this habit was characteristic of their primary radiation. A mostly herbaceous initial diversification of eudicots could simultaneously explain the heretofore sparse megafossil record as well as their rapid diversification during the Early Cretaceous because the angiosperm capacity for fast reproduction and fast evolution is best expressed in herbs.