福建泉州晚第四纪盆地沉积的孢粉和微体古生物及其古环境意义     

何耀堂 《福建地质》2011,30(3):224-232

福建泉州晚第四纪沉积物中孢粉,晚更新世以气候适应范围较宽的木本植物花粉占优势,适应温暖湿润气候的蕨类植物孢子较少;早全新世二者含量相当;中全新世蕨类植物孢子增多,木本植物花粉退居第二;晚全新世蕨类植物孢子占绝对优势,木本植物花粉相对减少。草本植物花粉浓度始终不高,但随着时代更新,种类增多。区内微体古生物在晚更新世和早全...  相似文献   

A New Triassic Primitive Ichthyosaur from Yuanan, South China     

CHEN Xiaohong  P. Martin SANDER  CHENG Long  WANG Xiaofeng 《《地质学报》英文版》2013,87(3):672-677

Based on the systematic study of two fossil skeleton specimens collected from the top of the third member of the marine Lower Triassic Jialingjiang Formation of Yuanan, Hubei Province, South China, a new Early Triassic primitive ichthyosaur Chaohusaurus zhangjiawanensis sp. nov. is reported and described. The beds yielding the type material are correlated with the Neospathodus homeri-N. triangularis Conodont zone. The new taxon is most similar to Chaohusaurus geishanensis Young and Dong, 1972 in the shape and configuration of the scapula, forefin, pelvic girdle and hindfin, presacral vertebral count and well-developed caudal peak, but distinguished from the latter by its larger size, the position of the pineal foramen in the centre of the parietal, the occurrence of a larger calcaneum in hindfin and the first sacral rib with distal expansion. The new species exhibits common features of primitive ichthyosaurs such as: (1) the prefrontal has an antero-dorsal shelf projecting towards the orbit; (2) the upper temporal fenestra is small; (3) the postorbital and the squamosal meet laterally to the upper temporal fenestra; and (4) cylindrical centra. However, more derived ichthyosaur characters are seen with the frontal separated from the orbital dorsal margin by the contact of the prefrontal and postfrontal, which offer new clues to the early radiation of ichthyosaurs.  相似文献   

鄂西早三叠世南漳-远安动物群地层分布特征          下载免费PDF全文

阎春波  李姜丽  程龙  赵璧  邹亚锐  牛东毅  陈刚  方子晨 《地球科学》2021,46(1):122-135

在区域地质调查的基础上,以远安张家湾嘉陵江组剖面为重点,通过对南漳和远安交界地区下三叠统嘉陵江组剖面测制和多处化石点考察,重新厘定研究区内嘉陵江组岩性特征.认为研究区内的嘉陵江组划分为3个岩性段更为合理,产南漳-远安动物群的纹层状灰岩段位于二段顶部.通过系统化石发掘和张家湾剖面详细描述,初步查明了南漳-远安动物群的垂向分布特征:在30余米厚的纹层状灰岩段中均有海生爬行动物产出,只是丰度和分异度存在一定差异,其中7组岩层相对富集,顶部最为丰富.在此基础上,通过地层对比和所有化石点综合分析,将动物群自北东向南西划分为A~D 4个区带,依次命名为绝缘区、边缘区、相对富集区和富集区,分别对应化石从无到有、丰度逐渐变化及水深逐渐加深的过程,总体上仍处于水体循环受限的台内洼地或潟湖相环境.此次查明动物群的分布特征将为研究动物群生物与环境协同演化及其对早三叠世生物复苏的响应奠定良好的基础.   相似文献   

New Early Cambrian Maikhanellids (Mollusca) from Zhangjiagou Section, South Shaanxi, China     

ZHANG Ya''nan  LIU Yunhuan  SHAO Tiequan  WANG Qi  QIN Jiachen  ZHANG Wei  LIANG Tanxing 《《地质学报》英文版》2022,96(2):440-446

A new maikhanellid genus, Totornatus gen. nov., from the Lower Cambrian (Fortunian Stage) of Zhangjiagou section at Xixiang County, southern Shaanxi Province, South China, is based on a new taxon T. strigatus gen. et sp. nov. Although showing similar morphology with a cap-shaped shell and an oval aperture to other members of the family, the new species differs from previous maikhanellids in its smooth apex. The apical field consists of dense, small, round or oval granules, which gradually merge to bigger, elongated, scale-like protrusions toward the apertural margin. On this basis, we establish Totornatus strigatus, which shows a transverse groove in two-ninths of its shell. This result enriches the diversity of the earliest mollusks and maikhanellids.  相似文献   

Cleaning symbiosis among New Zealand fishes     

A. M. Ayling  R. V. Grace 《新西兰海洋与淡水研究杂志》2013,47(2):205-218

These first observations of cleaning symbiosis amongst New Zealand fishes were made between June 1967 and March 1970. Five species of labrid fishes; Halichoeres sp., Coris picta (Bloch and Schneider, 1801), Coris sandageri (Hector, 1884), Pseudolabrus luculentus (Richardson, 1848) and Pseudolabrus miles (= coccineus) (Bloch and Schneider, 1801) are now known to be facultative cleaners. One is an undescribed species and two others are new records for New Zealand. Halichoeres sp. is a more active cleaner than the other four and is almost an obligate cleaner. Observed behaviour indicates that these species are typical temperate zone cleaners.  相似文献   

民和盆地侏罗系地层划分与对比   总被引：2，自引：0，他引：2  

张虎权  王廷栋  阎存凤  袁剑英 《地层学杂志》2007,31(1):62-67

民和盆地是一个油、煤、气伴生的中新生代陆相盆地,侏罗系地层层序自下而上划分为下侏罗统炭洞沟组(大西沟组)、中侏罗统窑街组、红沟组、上侏罗统享堂组。中侏罗世早、中期气候温暖湿润,形成了以沼泽相煤系地层和湖相暗色泥岩、油页岩为主的生油建造,晚侏罗世至白垩纪气候较为干燥,形成了以河流相为主的砂砾岩储集建造。根据古生物、岩性、电性、含煤性、构造、古气候等地层划分对比标志,重新确立了盆地的地层系统,建立了盆地中新生界地层标准剖面,为盆地石油勘探奠定了坚实的基础。  相似文献   

西秦岭拉尔玛金矿热水硅质岩中的分子古生物学研究   总被引：1，自引：0，他引：1  

林丽  朱利东 《地球科学》1998,23(5):503-507

拉尔玛金矿热水成因硅质岩中的分子古生物学研究表明;其正烷烃以碳数分布于Ｃ１６～Ｃ３６,主峰碳为Ｃ２９为特征,除此,还鉴定出规则类异戊二烯和胡萝卜烷系列化合物,烷基环己烷系列,长链三环萜烷,五环三萜烷,甾类分子化石和烷基噻吩系列化合物,烷基四氢噻吩系列化合物,二苯并噻吩,甲基二苯并噻吩等含硫芳烃以及菲及其同系物等非含硫芳烃分子化石,氯仿沥青“Ａ”族组成Ｑ型聚类分析表明拉尔玛金矿硅质岩与现代蓝绿藻和绿  相似文献   

广东南雄盆地白垩系—古近系界线   总被引：3，自引：0，他引：3  

童永生  李曼英 《地质通报》2002,21(10):668-674

在过去的30年中有数支考察队在广东南雄盆地进行了白垩纪和古近纪地层多学科的系统研究。本文综合了南雄盆地近年的岩石地层学、磁性地层学、地球化学、古生物学方面的研究成果和湖北新洲盆地时代相当于浓山组的地层中得到的同位素年龄,认为上湖组时代大体上与Danian期相当,或相当于北美哺乳动物分期Puercan和Torrejo-nian期,其底界接近于白垩系—古近系界线。  相似文献   

Ordovician strata in the Cliefden Caves area,New South Wales: a case study in the preservation of a globally significant paleontological site     

I. G. Percival  B. D. Webby  H. D. T. Burkitt 《Australian Journal of Earth Sciences》2019,66(6):869-877

The Cliefden Caves area in central-western New South Wales includes the scientifically most important and irreplaceable examples of fossiliferous Ordovician rocks in the State. Exposures of the stratigraphically lower parts of the Cliefden Caves Limestone Subgroup on the aptly named Fossil Hill are world-famous among paleontologists and internationally significant for preserving the earliest in situ shell beds documented in the literature. They also contain some of the oldest known rugose corals, and an exceptional example of one of the oldest coralline biostromes, as well as many examples of invertebrate fossils and cyanobacterial mat structures that either are unique to this locality or were first described from here. Other stratigraphic levels throughout the total 363?m-thick Cliefden Caves Limestone Subgroup are similarly endowed with highly significant fossils, such as a globally unique in situ shell bank with rare examples of the trimerellide brachiopod Belubula spectacula, a wealth of shelly fossils and trilobites on Dunhill Bluff (adjacent to Fossil Hill to the east), and the appropriately named Trilobite Hill. Less well known to the general public, but of international importance to paleontologists, is the unique deep-water sponge fauna of the overlying Malongulli Formation that occurs at several levels in limestone lenses within this unit. Fossils from the Cliefden Caves Limestone Subgroup and the Malongulli Formation have been documented in more than 60 scientific papers and monographs since paleontological investigations into the site were first published in 1895. Despite concerted scientific endeavour in the region over the past 50?years, much more study needs to be done to fully document the paleontological riches of the Cliefden Caves area. These sites are interpreted as the remains of a tropical island, fringed by limestone and flanked by deep-water environments in which the Malongulli Formation was deposited. Preservation of such islands is exceptionally rare in the geological record. It is therefore vital for the area to remain accessible to scientific researchers to continue their studies. Flooding of the Belubula Valley by a proposed dam downstream from the Cliefden Caves area would hinder future research work on this unique geoheritage resource. Fortunately, a successful public campaign has led to listing of the site on the State Heritage Register that will provide essential protection of the caves from inundation while ensuring continued access to researchers.  相似文献   

First Record of Hoplictis(Carnivora,Mustelidae) in East Asia from the Miocene of the Ulungur River Area,Xinjiang,Northwest China     

Alberto VALENCIANO  JIANGZUO Qigao  WANG Shiqi  LI Chunxiao  ZHANG Xiaoxiao  YE Je 《《地质学报》英文版》2019,93(2):251-264

The first unequivocal remains of medium to large-sized mustelids from the middle Miocene Halamagai and Kekemaideng formations have been found in the Ulungur River area, Xinjiang, northwestern China. These new fossils are referred to the hypercarnivorous mustelid Hoplictis Ginsburg, 1961 and denote the first record of the genus in East Asia.We define Hoplictis baihu n. sp., for the mustelid from Tieersihabahe(Halamagai Fm.), which represents the smallest species of the genus. This primitive form is closer to H. florancei and H. noueli than to H. anatolicus and later, larger and more derived Hoplictis spp., from Europe and North America. A large toothless mandible from Duolebulejin(Kekemaiden Fm.) is assigned to Hoplictis cf. helbingi, and it presumably might represent the first record of H. helbingi outside Western Europe. The systematic position of Hoplicitis in relation to Ischyrictis with which it is similar is clarified. The occurrence in East Asia of two species of Hoplictis greatly expands the known distribution and diversity of the genus, and supports a Palaearctic Neogene dispersal event of carnivorans between Europe and Asia during the late Shanwangian–early Tunggurian equivalent to MN5–6 in Europe, and indication of another dispersal event from Europe to North America,through Northwest China during the late Tunggurian, equivalent to MN7–8 in Europe.  相似文献