浙江早古生代孢粉型化石的研究   总被引：1，自引：0，他引：1  

颜铁增  何圣策  尹磊明  秦祥熙  张志芳 《地层学杂志》2011,(1)

在浙江西北部早寒武世荷塘组、晚寒武世华严寺组、早奥陶世宁国组、晚奥陶世长坞组和文昌组、早志留世霞乡组、河沥溪组和康山组、中志留世唐家坞组中发现孢粉型化石,孢粉型化石包括疑源类,隐花(陆生)植物孢子类型等,计66属、112种、31未定种。同时讨论了这9个层位孢粉型化石的组合特征、地质时代及其沉积环境。  相似文献   

不同光质对坛紫菜果孢子和壳孢子萌发的影响          下载免费PDF全文

刘嘉嘉  梁小君  周琳琳  钟晨辉  郭辰涛  唐隆晨  林琪 《应用海洋学学报》2023,42(3):409-415

本研究探究了白、蓝、红、绿光4种光质对坛紫菜（Pyropia haitanensis）果孢子和壳孢子萌发的影响。结果表明，与白光相比，用绿光培养时，果孢子萌发管分枝形成速度、萌发管生长速度，以及壳孢子的细胞分裂速度均相对较快，用红光与蓝光培养时则相对较慢。不同光质对坛紫菜果孢子和壳孢子的存活率无显著影响，但能造成萌发体色泽呈现明显差异。刚从孢子囊释放出来的两种孢子均呈黄褐色，经白光培养的两种孢子以及蓝光培养的果孢子，其萌发体颜色加深至鲜红色，蓝光培养的壳孢子萌发体颜色加深尤为明显，最终呈深紫红色，而红光和绿光培养的两种孢子颜色变浅，最终呈浅黄褐色。研究表明，绿光培养可能不利于坛紫菜孢子萌发过程的色素积累，但有利于孢子萌发及萌发体的生长。  相似文献   

寄生大眼鲷类的大眼鲷匹里虫 Pleistophora priacanthusis（Hua1981），Hua＆Dong1983的光镜和电镜观察＊     

华鼎可  张志宇 《广东海洋大学学报》1986,(1):13-26

前曾报道(Hua 1981，Hua ＆Dong 1983)大眼鲷匹里虫以孢囊型寄生于长尾大眼鲷和短尾大眼鲷的胃、幽门垂、肠道、肠系膜、性腺、肝、脾、腹壁肌肉等部位，孢子有大、中、小三种形态。  相似文献   

A Spore-Pollen Assemblage from the Damoguaihe Formation in the Tamutsag Basin,Mongolia and Its Geological Implication     

WANG Liyan  WAN Chuanbiao  SUN Yuewu 《《地质学报》英文版》2014,88(1):46-61

Based on the palynological data from Well Ta-19-36 and Well Ta-19-37 in the Ta'nan Sag, and Well Ta-22-1 and Well Ta-21-1 in the Bayin Gobi Sag, a spore-pollen assemblage from the Damoguaihe Formation is named as Cicatricosisporites minutaestriatus- Aequitriradites spinulosus-Protopinus sp. assemblage in the Tamutsag Basin, Mongolia. The assemblage is characterized by abundant gymnosperm pollen and diverse fern spores, counted 46.35%–65.57% and 34.43%–52.58% in percentage respectively. Among the gymnosperm pollen, Pinuspollenites sp.(2.66%–16.94%), Protopinus sp.(0–11.38%) and Protopicea sp.(0–10.81%) are dominant; and Alisporites sp., Cerebropollenites sp., Podocarpidites sp., and Abietineaepollenites sp. are common. Some important elements, such as Chasmatosporites sp., Callialasporites prominulus, Parvisaccites sp., Parcisporites sp., Jiaohepollis cf. annulatus, J. bellus, J. verus, Polycingulatisporites sp., Schizaeoisporites certus, Classopollis annulatus are seen. Within the fern spores, Osmundacidites wellamanii(0.85%–4.93%), Appendicisporites sp.(0–4.45%), Baculatisporites comaumensis(0.80%–2.87%), Cicatricosisporites sp.(0.51%–2.66%), C. minor(0–2.14%), Foraminisporis asymmetricus(0–2.40%), Aequitriradites sp.(0– 2.19%) and Cyathidites minor(0–2.13%) are dominant; and some specie of Densoisporites, Cooksonites, Impardecispora, Pilosisporites, Schizaeosprites, Fixisporites, Leptolepidites, Trilobosporites, Kuylisporites, Klukisporites, Hsuisporites, Couperisporites, Maculatisporites are seen. The angiosperm pollen are rare in the assemblage, characterized by Clavatipollenites sp.(0–0.80%) and Songipollis sp.(0–0.27%). The geological age of the Damoguaihe Formation is assigned to Hauterivian – Barremian of Early Cretaceous according to the palynological data, due to the fact that there existed a lot of diverse spores of the family Schizaeaceae and prosperous gymnosperm saccat pollen which the corpus and sacci are differentiated completely, and the presence of early angiosperm pollen of Clavatipollenites. However, the zircon U-Pb isotopic dating of the volcanic rocks in the Nantun Formation indicated that the overlying strata of the Nantun Formation, i.e. the Damoguaihe Formation must be younger than 127.0±2.0–137.9±1.5 Ma. This is consistent with the palynological data. Furthermore, the vegetation reconstructed on the palynological data of the Damoguaihe Formation is conifer forest with shrubs and grassland, belonging to the semi-humid or humid middle to south subtropical climate. Moreover, three new species, namely Biretisporites punctatus sp. nov., Chasmatosporites reticulates sp. nov. and Concentrisporites contractus sp. nov. are described here.  相似文献   

Early development of Chondrus ocellatus Holm （Gigartinaceae, Rhodophyta）     

王爱华  王继成  段德麟 《中国海洋湖沼学报》2006,24(2):129-133

1 INTRODUCTION Red algae C. ocellatus lives in temperate zone of coastal area, and inhabits at substrates from high tide to low tide regions. Its life history is composed of three phases: tetrasporophyte, gametophyte and carposporophyte. Chondrus is one o…  相似文献   

Preliminary study on the spore-pollen assemblages found in the Cenozoic sedimentary rocks in Grove Mountains, east Antarctica and its climatic implications     

方爱民刘小汉  王伟铭李潇丽俞良军  黄费新 《极地研究(英文版)》2005,16(1):23-32

Glaciogene sedimentary rocks have been found in modem tills of the Grove Mountains, east Antarctica during the 1998 - 1999 Chinese National Antarctic Research Expedition （CHNARE）. Based on the lithilogic and sedimentary features, these sedimentary rocks are correlated with Cenozoic sedimentary strata of the Pagodroma Group in the neighboring Prince Charles Mountains and the Sorsdal Formation in VestFold Hills. Sedimentary clasts contain sparsely Late Tertiary spores and pollens, including ： Toroisporis （ Lygodiaceae）, Osmunda, Granulatisporites （ Pteridaceae？） , Polypodiaceae, Podocarpus , Araucariaceae, Artemisia , Rhus , Nothofagidites , Proteacidites （Proteaceae） , Quercus , Fraxinoipollenites （ Oleaceae ） , Oleoidearumpollenites（ Oleaceae ）, Operculumpollis, and Tricolpopollenites. Most of the pollen and spores contained in these samples originate from local sources according to the conditions of their preservations as well as correlations with the microfossil assemblages found in the neighboring areas. The majority of the pollen assemblages, as represented by Podocarpus and Nothofagus, belong to the Weddellian biogeocenose, however some exotic components from the old sedimentary basement rocks may have been included during erosion of the proximal ice sheet. If the source areas of glaciogenic sedimentary rocks that bear the pollen and spores are assumed to be local, or in the up glacier areas, the pollen assemblages in these samples might represent an inland flora during a warmer period of the ice-sheet evolutionary history. The finding of the Artemisia and Chenopodiaceae in the pollen assemblages implies that they may belong to late Tertiary （most probably Pliocene）. The absence of diatoms in the samples analyzed may indicate that there are no Cenozoic marine strata in the interior of the east Antarctica beyond the Grove Mountains. The significances of the finding of the Nothofagus in these pollen assemblages are discussed on the basis of current knowledge about the age, distribution and ecological conditions of this kind of fossils found in Sirius Group or other strata outcropped in Antarctica. As a preliminary conclusion, we think that the existence of the Cenozoic glaciogenenic rocks and their pollen assemblages present new evidence for a large scale glacial retreat history in Grove Mountains of east Antarctica, and thus support a dynamic East Antarctic Ice Sheet （EAIS）. This is consistent with the interpretations of Webb et al. （1984）.  相似文献   

NEW OBSERVATIONS ON THE MEIOTIC PROCESS IN THE MARINE DINOFLAGELLATE NOCTILUCA SCINTILIANS （NOCTILUCALES, DINOPHYCEAE）     

周成旭  严小军 《中国海洋湖沼学报》2002,20(1):67-73

The meiotic process in Noctiluca scintillans were observed under light microscope.Some abnormal cell divisions, incompletely separated “zoospores” and the changes of the zoospores are described in this paper. Together with the fmdings of field samplings and the previous results by other researchers, the process of meiosis in N. scintillans was supposed to be a pathway to reduce the extra high density of NH3-N within the cell in order to ensure normal population growth.  相似文献   

早白垩世Ruffordia goepperti的原位孢子及与分散孢子的关系   总被引：2，自引：0，他引：2  

邓胜徽 《地质论评》1998,44(3):243-248

海金沙特的Ｒｕｆｆｏｒｄｉａ ｇｏｅｐｐｅｒｔｉ（Ｄｕｎｋｅｒ）Ｓｅｗａｒｄ是世界上早白垩世极为重要的蕨类植物。通过对比发现,Ｒｕｆｆｏｒｄｉａ ｇｏｅｐｐｅｒｔｉ原位孢子的形态和细微纹饰与地层中分散孢子Ｃｉｃａｔｒｉｃｏｓｉｓｐｏｒｉｔｅｓ ａｕｓｔｒａｌｉｅｎｓｉｓ（Ｃｏｏｋｓｏｎ）Ｐｏｔｏｎｉｅ和Ｃ．ｍｉｎｏｒ（Ｂｏｌｃｈ．）Ｐｏｃｏｃｋ一致,而且大化石与分散孢子的地史、地理分布范围也相同,  相似文献   

塔里木盆地西部巴参1井晚泥盆世孢子的发现及意义     

高联达  何卓生 《中国区域地质》1998,17(2):147-148

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伶仃洋L＿2和L＿（16）孔第四纪有孔虫群与孢粉化石带特征及其地质意义   总被引：5，自引：0，他引：5  

陈木宏  赵焕庭  温孝胜  张乔民  宋朝景 《海洋地质与第四纪地质》1994,(1)

本文所依据的分析样品是取自珠江最大的一个河口湾伶仃洋中部的水下钻孔岩芯，其底部到达花岗岩基底。通过对第四纪有孔虫群与孢粉化石带特征的分析，阐明在相同的钻孔岩芯中，有孔虫分布变化所反映的古沉积环境特征与孢粉分析的古气候特征较为吻合，并与相应的沉积相对应，结合￣（１４）Ｃ和￣（２３０）Ｔｈ／￣（２３２）Ｔｈ比值法测年数据，从而较好地重塑本区晚更新世中期以来的地质历史。  相似文献