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1.
本文以圆紫菜的绿色突变体(LT)和红色突变体(HT)进行杂交实验,证实了圆紫菜减数分裂发生的时期,并观察了圆紫菜的早期发育和形态建成过程。杂交F1叶状体中,出现了2种亲本色和2种重组色,它们分别为绿色(G,母本色)、红色(R,父本色)、野生色(W)和黄褐色(Y)。4种颜色在F1叶状体中形成了大量由2—4个色块组成的颜色嵌合体,色块出现了分离并呈线性排列。F1叶状体中嵌合体所占比例为82.9%,其中两嵌合最多,三嵌合次之,四嵌合最少。4种颜色在嵌合体的分离比为1G:0.97R:0.88W:0.69Y。上述结果证实圆紫菜的减数分裂发生在壳孢子萌发初期。减数分裂产生的四分子呈线形排列,随后继续发育成叶状体,叶状体发育至7—9个细胞时进行第一次纵向分裂,叶状体形态变宽。随后,圆紫菜梢部开始大量形成和放散单孢子,最终导致圆紫菜的形状为圆形或肾脏形。 相似文献
2.
Journal of Geographical Sciences - This article describes the lake basins of the Jom-Bolok volcanic region in the East Sayan (the largest manifestation of the Holocene eruptions in Central Asia).... 相似文献
3.
劈裂生长的形态发生及内部解剖结构特征的研究 总被引：2，自引：0，他引：2
对绵刺劈裂生长的形态发生及内部解剖结构特征进行了观察,研究结果如下：①绵刺的劈裂生长有两种类型,一种是首先茎从基部到根部发生多次劈裂,以后地上的茎部再相应发生分裂而形成几个独立的植株;另一种是茎基部以上的部位先发生纵裂,而根部后发生分离;②劈裂生长首先在茎基部发生,当绵刺植株生长到5 a以上的时候,这个部位的形成层活动不均匀,出现不规则的木质部排列,形成花环状结构,在相邻的两环状部位进行劈裂;③由于受劈裂生长的影响,劈裂发生后的植株的根部年轮分布不规则,发生劈裂部位的形成层活动不均匀,形成的次生木质部中导管数量少,口径也小,木纤维数量增多,细胞排列紧密而形成缢缩。 相似文献
4.
The species of Epithemia ocellata (Ehr.) Kütz. from Northeastern China were observed by scanning electron microscopy (SEM). The studies on silica valve formation in different stages were made. At the early stage, a Y-shaped raphe sternum was found. Areolae were made from virgae and vimines. In immature valves, the canal formation before the raphe fissure is visible. The raphe system, virgae and vimines (areolae) might be the early siliceous elements of the valve during morphogenesis. The formations of virgae and vimines are similar to that of Gephyria media W. Arnott. Rows of silica papillae formed gradually on the face of the valve. After the areolae were covered with silica and form rows of papillae, the outer valve surface could become mature. Details of the internal costae were observed in mature valves. 相似文献
5.
Song Weibo 《海洋学报(英文版)》1996,15(1):93-99
ＭｏｒｐｈｏｇｅｎｅｔｉｃｓｔｕｄｉｅｓｏｎＵｒｏｎｙｃｈｉａｕｎｃｉｎａｔａ（Ｐｒｏｔｏｚｏａ，Ｃｉｌｉｏｐｈｏｒａ）ｄｕｒｉｎｇｉｔｓａｓｅｘｕａｌｄｉｖｉｓｉｏｎ￥ＳｏｎｇＷｅｉｂｏ（ＲｅｃｅｉｖｅｄＡｕｇｕｓｔ２８，１９９５；ａｃｃｅｐｔｅｄ... 相似文献
6.
研究了史氏尖毛虫（Ｏｘｙｔｒｉｃｈａｓｈｉ）无性生殖周期中核器及纤毛器的发育演化过程。其结果为：１．大核复制带出现后，口原基最早出现在左边第一根横棘毛的左侧，后逐渐向前增生，构成一长形原基带。由口原基的前右角分化出波动膜原基，同时在该处向后组装整齐排列的小膜，构成新的ＡＺＭ，老ＡＺＭ完整地被前仔虫继承。２．额腹横棘毛原基各５列，分别以３∶３∶３∶４∶４方式分化成前后仔虫的额腹横棘毛。３．背触毛８～９列，在第１～３列背触毛中，分别于前后仔虫的中部范围产生第１～３列新原基，每列原基向两端伸展替代老背触毛列，成为前、后仔虫相应的新背触毛。在前、后第３列原基后端发生前、后第４～５或第４～６列原基，它们均偏在第３列原基的右侧，并分别向两端伸展成第４～５或４～６列背触毛；４．在虫体腹面的前、后右缘棘毛原基前方的右边出现第６，７，８或７，８，９列背触毛原基，随后发育为第６，７，８或７，８，９列背触毛，并在演化过程中转位到背面。 相似文献
7.
Influence of tectonics and neotectonics on the morphogenesis of the peak karst of Halong Bay,Vietnam
Pascal Fenart N. N. Cat Claude Drogue Doan Van Canh Sévenn Pistre 《Geodinamica Acta》2013,26(3-4):193-200
AbstractIn northeast Vietnam, the karst of Halong Bay is characterized by very active neotectonics. The directional distribution of fracturing of the calcareous rocks is characterized by the influence of two major fault zones: the Red River fault zone (N140) and the Tan-Lu fault zone (N050). Karst development was favoured by intense fracturing, according to these two major directions, and reactived during recent tectonics by a compressional regime with σ1 N070, followed by an extensional regimes with σ1 near to EW that led to significant vertical movement. These tectonics, coupled with intense erosion, led to genesis and evolution of the spectacular morphology of this peak karst. © Elsevier, Paris 相似文献
8.
NIELS RAMEIL ADRIAN IMMENHAUSER GEORG WARRLICH HEIKO HILLGÄRTNER HENK J. DROSTE 《Sedimentology》2010,57(3):883-911
Lithocodium aggregatum and Bacinella irregularis are now extinct, shallow marine life forms of unknown taxonomic origin. Forming part of the tropical platform biota during much of the Mesozoic, these organisms experienced bloom periods and temporarily replaced rudist–coral assemblages during parts of the Early Aptian. Within the limitations of time resolution, this ‘out‐of‐balance’ facies is coeval with the Oceanic Anoxic Event 1a‐related black shale deposition in oceanic basins but the triggering factors remain poorly understood. Here, a platform‐wide comparison of Lithocodium–Bacinella geobodies and morphotypes from the Sultanate of Oman is presented and placed in its environmental, bathymetric and physiographic context. Lithocodium–Bacinella geobodies reach from kilometre‐scale ‘superstructures’ to delicate centimetre‐sized growth forms. Clearly, scale matters and care must be taken when drawing conclusions based on spatially limited observational data. Whilst the factors that cause Lithocodium–Bacinella expansion should probably be considered in a global context, regional to local factors affected growth patterns in a more predictable manner. Here, the unresolved taxonomic relationship remains the main obstacle in any attempt to unravel the response of Lithocodium–Bacinella to specific or interlinked environmental parameters as different organisms respond differently to changing environment. Acknowledging these limitations, the following tentative patterns are observed: (i) Lithocodium–Bacinella tolerated a wide range of hydrodynamic levels and responded to differences in energy level or physiographic settings (margin, intrashelf basin, inner platform) by obtaining characteristic growth forms. (ii) Lithocodium–Bacinella favoured low‐sediment input but had the ability to react to higher sedimentation rates by enhanced upward growth; a feature perhaps pointing to a phototrophic metabolism. Circumstantial evidence for continuous growth within the upper‐sediment column is debated. (iii) The availability of accommodation space had a direct influence on the maximum size of geobodies formed. (iv) Fluctuating nutrient levels and sea water alkalinity may have affected the growth potential of Lithocodium–Bacinella. Understanding the relationship between Lithocodium–Bacinella morphogenesis on a wide range of scales and local environmental parameters allows for better prediction of the spatial distribution of reservoir properties and also results in an improved interpretation of palaeoenvironments. This study might represent a useful first step in this direction. 相似文献
9.
利用改进的蛋白银染色法，研究了宽四虫（Steiiniasp．）的形态及其无性生殖周期中核器和纤毛器的发育演化过程。其发生过程为：1．大核改组带出现后，口原基出现在老口围带后方之腹棘毛左侧，其内的毛基体组装成整齐排列的小膜，构成新AZM，老AZM后部也发生部分更新的现象。2．颇腹根棘毛原基各5列，分别以3：3。3：4：3方式分化成前、后仔虫的额、腹、横棘毛。3．在第1－3列背触毛中，分别于前、后仔虫的中部范围产生第1—3列新原基，每列原基向两端伸展替代老背触毛列，成为前、后仔虫相应的第一列新背触毛。4．在前后第3列背触毛原基后端发生前、后第4列原基，它稍偏向第3列原基的右侧，向前伸展成第4列背触毛；在虫体腹面，前、后右缘棘毛原基的前方出现第5、6列背触毛原基，后发育为第5、6列背触毛，在虫体演化过程中转位到背面。 相似文献
10.
宋微波 《中国海洋湖沼学报》1993,(2)
Morphogenesis during cell division was investigated in oligotrichous ciliate,Halteria grandinella utilizing protargol impregnated specimens. The cortical morphogenetical pattern of Hdteria grandinella is generally similar to that given by Faure-Fremiet. The prater inherits the parental adoral zone of membranelles (AZM) appar ently unchanged; in the opisthe the oral primordium develops de novo from a single AZM-anlage; somatic cirri for both the proter and opisthe are separately differentiated from 10 (seldom 9) cirral primordia that originate de novo from 10 latitudinal developmental anlagen. The anlage of paroral membrane of opisthe forms just to the right of the posterior end of the oral primordium. Each streak of cirral primordia develops 4 groups of basal body pairs: both of the anterior two consist of only one pair of basal bodies, on the contrary, each of the last two groups has 2 basal body pairs. 相似文献