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11.
One hundred and forty six dinosaur footprints occur on the Cenomanian outcrop of Fenoliga. They are arranged in six trackways and six footprint groups (a–f). Two basic footprint types can be distinguished: firstly, large circular-elliptical sauropod footprints, forming four trackways (I, III, V, VI) and five footprint groups (a–e), and secondly, smaller, tridactyl theropod footprints forming two trackways (II and IV) and one footprint group (f). Three type specimens, one sauropod and two theropod, were determined during the course of the work. Since no dinosaur bones have been discovered in the Cenomanian rocks of Istria so far, these findings are outstandingly important in the analysis of the regional dinosaur fauna.  相似文献   
12.
Present article is on Russian Far East carnivorous dinosaur paleoecology.Described summary is based on detailed study and comparison of isolated shed teeth morphology.  相似文献   
13.
Present article is on Russian Far East carnivorous dinosaur paleoecology. Described summary is based on detailed study and comparison of isolated shed teeth morphology.  相似文献   
14.
本文报道了首次在山东青岛莱西地区晚白垩世红土崖组发现的恐龙蛋化石,蛋化石呈圆形,其直径为11 cm,蛋壳的显微构造研究表明,它属于树枝蛋类,可能为镰刀龙类恐龙所产。沉积环境和岩石地球化学分析显示,该时期研究区主要为河道—河漫滩沉积环境,适宜的古气候条件是恐龙蛋孵化的理想地区;同时镰刀龙类蛋的发现,预示着将来在该地区很有可能发现镰刀类恐龙骨骼化石。  相似文献   
15.
The palynological assemblage from Wulaga dinosaur site in Jiayin from southeastern Zeya-Bureya Basin was studied. The high content of pteridophytes spores is characteristic for this assemblage. The further characters are in decrease of abundance-tricolpate pollen, Ginkgocycadophytus, pollen of Taxodiaceae, Cup ressaceae and Taxaceae ( TCT) , bisaccate pollen of Pinaceae, and triporate pollen. The bone-bearing burials of Wulaga dinosaur site formed under conditions of vast swampy river valley covered by ferns and taxodialeans. Tricolpate pollen, produced by plants, close to those of Platanaceae, Fagaceae, Betulaceae, and Juglandaceae, counts in favor of valley river open canopy forests.  相似文献   
16.
方晓思  常燕生 《地质通报》2011,30(11):1689-1696
越来越多的事实表明,印度板块曾经连续两次撞击了欧亚板块。第一次发生在近200Ma前,通过印度板块将冈 瓦纳大陆上的恐龙动物群带到了亚洲,使中国首次出现了早侏罗世恐龙。确切地说,中国恐龙起源于印度板块的第一 次撞击。侏罗纪之后,印度板块又被引发起顺时针转动,在其东部出现了与泰国之间的断裂,并最终孕育着孟加拉湾 的形成,为第二次撞击拉开了序幕。55Ma前印度板块再次撞向欧亚板块的西藏地区,造就了喜马拉雅山。  相似文献   
17.
Recent geological and paleontological exploration in the Indus basin of Pakistan allowed the discover-ies of numerous remains of non-marine reptiles (titanosaurian sauropod,abelisaurian and noasaurian theropod dinosaurs),and marine reptiles (crocodiles),flying reptiles (pterosaurs),marine and non-marine mammals, fishes,invertebrates,and plants,especially Pakistan is relatively rich in footprints/trackways in the Mesozoic. These vertebrates of Indo-Pakistan are very significant for paleobiogeographic study due to the present-day con-nection of this continent with Asia in Northern Hemisphere,whereas during past (Jurassic and pre-Jurassic)it was connected to the Gondwana.The Mesozoic vertebrates show close affinities with Gondwanan landmasses. The Cenozoic vertebrates show Eurasian affinity and migrated from Indo-Pak subcontinent to Eurasia or vice ver-sa via Paleo Indus River systems along Western Indus Suture,after long journey of about 6 000 km the first col-lision of Indo-Pak subcontinent with Asia occurred at terminal Cretaceous.  相似文献   
18.
The palynological assemblage from Wulaga dinosaur site in Jiayin from southeastern Zeya-Bureya Basin was studied. The high content of pteridophytes spores is characteristic for this assemblage. The further characters are in decrease of abundance-tricolpate pollen, Ginkgocycadophytus, pollen of Taxodiaceae, Cupressaceae and Taxaceae (TCT) , bisaccate pollen of Pinaceae, and triporate pollen. The bone-bearing burials of Wulaga dinosaur site formed under conditions of vast swampy river valley covered by ferns and taxodialeans. Tricolpate pollen, produced by plants, close to those of Platanaceae, Fagaceae, Betulaceae, and Juglandaceae, counts in favor of valley river open canopy forests.  相似文献   
19.
南雄盆地白垩纪-古近纪地层研究进展   总被引:2,自引:3,他引:2  
简要介绍近年来南雄盆地地层研究的主要进展。在始兴陆源浈水组及南雄城南上湖组坪岭段发现窃蛋龙类,后者还见鸭咀龙类;界址、水口、下坪及始兴斜谭等地大凤组产大量以圆形蛋类为主的蛋化石;南雄盆地西区南雄群中发现叶肢介、昆虫、鲎虫、有孔虫等;初步查明阶齿兽在地层中的分布,在大塘剖面其首次出现距上湖组底界约60m,最高层位见于浓山组;利用测定蛋壳的稳定同位素和铱元素富集异常探讨恐龙绝灭;白垩系一古近系界线划分目前存在4种意见:1)划在上湖组近底部(根据恐龙绝灭),2)坪岭段/下惠段之间(根据介形虫),3)坪岭段上部(根据阶齿兽,腹足类)和4)浈水组中上部(根据孢粉)。  相似文献   
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