共查询到18条相似文献，搜索用时 31 毫秒
1.
2002年8月以来,江西省萍乡市博物馆考古专业人员在萍乡市开发区、白源镇、芦溪镇和安源镇等多处建设工地的上白垩统紫红色粉砂岩中,发现258枚大小不同、形状各异的恐龙蛋化石;2008年5月底又在开发区发现和收集到一些残破恐龙骨骼化石。萍乡发现的这些恐龙蛋化石基本上是成窝或部分呈窝状保存,说明在晚白垩世时期,有多种恐龙曾在这里繁衍生息。 相似文献
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河南淅川盆地的恐龙蛋 总被引：4，自引：2，他引：4
记述了河南淅川盆地10个地点发现的恐龙蛋化石计6种,分属于4个科6个属．其中新属1个、新种2个。新属、新种滔河扁圆蛋（Placoolithustaohensis）以其特有的壳单元分枝特征成为树枝蛋科的新型分子;另一新种渐川树枝蛋（Dendroolithusxichuanensis）与湖北安陆王店树枝蛋（D．wandianensis）性质相似,两者时代应彼此相当;含滔河扁圆蛋的马家村组下部应与其下含淅川树枝蛋的高沟组划归同一时段为宜,即晚白垩世早期;含副圆形蛋、椭圆形蛋、长形蛋、南雄蛋的马家村组中、上部和其上的寺沟组,时代应属晚白垩世中、晚期。 相似文献
3.
山东莱阳晚白垩世恐龙蛋化石一新类型 总被引：4，自引：0，他引：4
山东莱阳是中国最早发现的含有丰富的晚白垩世恐龙及恐龙蛋化石产地。上个世纪50～60年代,周明镇(1951,1954)及杨钟健(1954,1959,1965)对莱阳首次发现的恐龙蛋化石进行了研究。1974年,赵资奎、蒋元凯在前人工作基础上,采用显微镜技术方法重新研究了莱阳恐龙蛋壳的显微结构,结果发现它们的显微结构有很大差异。根据赵资奎(1975)提出的恐龙蛋分类方法(Parataxonomy),将莱阳地区已发现的恐龙蛋分别归入圆形蛋科(spheroolithidae)、椭圆形蛋科(Ovaloolithidae)和长形蛋科(Elongatoolithidae)等3个科,共5个属12个种(赵资奎,1979,1993)。最近,大连自然博物馆在整理馆存的化石标本时,发现有4枚形状为扁圆形的恐龙蛋化石是1973年10月从山东莱阳将军顶采集到的。根据目前有关莱阳地区晚中生代地层划分修订的标准(胡承志等,2001),这些标本的出土层位应为上白垩统王氏群将军顶组。我们的初步观察表明,蛋化石的形状、大小及其蛋壳显微结构特征与上述已报道的莱阳恐龙蛋3个类群的明显不同,在此简单记述,以期对莱阳地区晚白垩世恐龙蛋群的综合研究提供些许资料。 相似文献
4.
浙江天台盆地晚白垩世恐龙蛋新类型(英文) 总被引：1，自引：0，他引：1
浙江天台盆地上白垩统赖家组和赤城山组是我国最重要的恐龙蛋化石产出地层之一。近年来,我们对天台盆地陆相红层中的恐龙蛋化石层位进行了详细厘定,对恐龙蛋类型进行了系统描述,并对前人报道的一些属种进行了分类订正。研究显示,天台恐龙蛋化石群基本上可分为7蛋科、12蛋属和15蛋种,代表了我国晚白垩世早期的恐龙蛋化石组合。本文简要报道了主要产自天台盆地赤城山组的双塘似蜂窝蛋(新蛋属、新修订种)、木鱼山半蜂窝蛋(新蛋属、新蛋种)、国清寺副蜂窝蛋(新修订种)、天台棱柱形蛋(新修订种)和张头槽马赛克蛋(新蛋属、新修订种)等3新蛋属、5新蛋种和修订种的主要鉴定特征,并建立一新蛋科——似蜂窝蛋科。 相似文献
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记述了江西省上高县发现的一窝不完整蛋窝的恐龙蛋。根据恐龙蛋宏观形态和蛋壳显微结构特征将其归入石嘴湾珊瑚蛋(Coralloidoolithus shizuiwanensis)。该窝恐龙蛋为近圆形球体,平均长径11.8 cm,平均赤道直径9.8 cm,蛋壳厚度可达2.5 mm;蛋壳由锥体层与柱状层组成,锥体层较薄,柱状层可分为内层、中间层和外层,内层发育致密的水平生长纹,中间层结构松散,含有大量暗色物质,中间层和外层发育次生壳单元。依据新标本的观察,明确珊瑚蛋属在石笋蛋科中以柱状层中间层结构松散为主要分类特征。上高新标本的发现,丰富了石嘴湾珊瑚蛋的古地理分布,同时也为上高地区晚白垩世含恐龙蛋红层的对比提供了新的证据。 相似文献
7.
湖北郧县青龙山恐龙蛋化石群被列入国家级地质遗迹自然保护区 总被引：1，自引：0，他引：1
近日 ,经国务院批准 :湖北省十堰市所辖的郧县青龙山恐龙蛋化石群被列为国家级地质遗迹自然保护区 ,这是此批经国务院批准的全国１６个国家级自然保护区中唯一的一个古生物地质遗迹自然保护区。郧县青龙山恐龙蛋化石群自１９９５年初被发现以来 ,经武汉中国地质大学、国家地质博物馆、中科院古脊椎动物研究所等有关专家考察鉴定 ,确认该化石系中生代白垩纪晚期胡岗组红粉沙岩地层的恐龙蛋化石 ,距今６７００万年至１３５００万年 ,其恐龙蛋化石群主要分布在郧县柳陂镇青龙山北坡和南坡、红寨子北坡、土庙岭、贺家村一组附近、磨石为、郑家沟… 相似文献
8.
广东南雄晚白垩世恐龙蛋孵化期的微环境 总被引：1，自引：1，他引：1
本文通过测量南雄盆地晚白垩世的三种恐龙蛋的蛋壳结构,估算了胚胎在正常发育的情况下蛋壳对水蒸汽和呼吸气体的传导率.结果发现,同现生鸟蛋的有关量相比,南雄恐龙蛋的气体传导率很高,蛋窝微环境具有湿度高、氧气含量低和二氧化碳含量高的特点.笔者推测这三种恐龙蛋是埋藏孵化的.从蛋壳结构来看,导致高气体传导率的直接因素是蛋壳上单个气孔的平均横截面积较大.南雄的这三种恐龙蛋的气体传导率与蒙古"原角龙"的蛋的相应值很接近,而与法国恐龙蛋的相差很多. 相似文献
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辽宁昌图上白垩统泉头组恐龙蛋化石的分类订正 总被引：1，自引：0，他引：1
重新描述了20世纪20年代发现于辽宁省昌图地区的恐龙蛋化石。通过对这些标本的宏观和微观形态特征的观察与测量数据分析,将其归入圆形圆形蛋(Spheroolithus spheroides)和厚皮圆形蛋(Spheroolithus megadermus),这是目前这两个蛋种的第二次化石记录。这两个蛋种首次发现于山东莱阳上白垩统将军顶组,根据昌图及其邻近地区恐龙蛋化石与山东莱阳恐龙蛋化石群的对比,结合松辽盆地近年来泉头组的研究成果,认为泉头组的地质时代为晚白垩世早、中期。 相似文献
11.
<正>As dinosaurs were oviparous animals, incubation of their eggs was the essential procedure during their reproduction. Physiologically. eggshell microstructures were bound to adapt to the nest environments during incubation if embryos normally developed. Gas conductance estimated from eggshell morphology can provide evidence for the environment conditions in nests. Seymour (1979) first estimated gas coaductance of dinosaur eggs from France and Mongolia and indicated that the nest environments of these eggs were all high in humidity, low in oxygen and high in carbon dioxide. Such conditions most likely occurred underground or within incubation mounds. Williams et al. (1984) found similar nest environments of four kinds of dinosaur eggs from Aix Basin in southern France. 相似文献
12.
Gerard D. Gierliński 《Ichnos》2015,22(3-4):220-226
The Late Cretaceous track assemblage of southeastern Poland includes intriguing ichnotaxa with Asian or North American affinities. New finds of the ceratopsian-like ichnite and small hadrosauroid track refer directly to this problem, whereas the re-evaluation of foraminifer taxa estimates the stratigraphic positions of the track-bearing horizon and allowed to understand paleogeographic context of the studied and adjacent areas. The results demonstrate that during the Late Cretaceous times, migration of dinosaurs was possible from Asia through the East European Land to Kukeritz Island and the islands at peri-Tethys area. 相似文献
13.
Julio Company 《Historical Biology》2019,31(2):203-210
Fieldwork carried out recently in the southeastern branch of the Iberian Range (Valencia Province, Spain) has led to the collection of a large volume of dinosaur eggshell fragments of unusual thickness. These specimens, up to 4.9 mm thick, were recovered from palustrine grey marls of the upper Campanian-lower Maastrichtian Sierra Perenchiza Formation, which comprises a wetland paleoenvironment deposit. These eggshell fragments have a characteristic compactituberculate ornamentation, dinosauroid-spherulitic organisation, and exhibit a complex canaliculate respiratory system. The external tuberculate surface of the shell as well as the internal microstructure enable referral to Megaloolithus aff. siruguei, the most common megaloolithid oospecies known from the Iberian Peninsula and southern France. The biostratigraphic range of M. siruguei matches the temporal distribution of titanosaurid dinosaurs across the Iberian Range, tentatively considered to be potential producers. 相似文献
14.
An isolated, large recurved and finely serrated tooth found associated with the prosauropodEuskelosaurus from the Late Triassic part of the Elliot Formation is described here. It is compared to the Triassic thecodonts and carnivorous
dinosaurs and its possible affinity is discussed. The tooth possibly belongs to a basal theropod and shows some features similar
to the allosauroids. This tooth is of significance, as dinosaur remains except for some footprints and trackways, are poorly
known in the Late Triassic horizons of southern Africa. 相似文献
15.
Abstract: We describe bones from the Late Cretaceous of Alberta – including bones of large dinosaurs, a femur from the aquatic reptile Champsosaurus, and a dentary from the marsupial Eodelphis– that bear tooth marks made by animals with opposing pairs of teeth. Of the animals known from the Late Cretaceous of North America, only mammals are capable of making such tooth marks. In particular, multituberculates, which have paired upper and lower incisors, are the most likely candidates for the makers of these traces. The traces described here represent the oldest known mammalian tooth marks. Although it is possible that some of these tooth marks represent feeding traces, the tooth marks often penetrate deep into the dense cortices of the bone. This raises the possibility that, much as extant mammals gnaw bone and antler, some Cretaceous mammals may have consumed the bones of dinosaurs and other vertebrates as a source of minerals. However, none of the tooth marks described here resemble the extensive gnaw traces produced by Cenozoic multituberculates or rodents. This suggests that specialized gnawing forms may have been rare or absent in the Late Cretaceous of North America. 相似文献
16.
浙江天台盆地晚白垩世网形蛋类新类型及网形蛋类的分类订正(英文) 总被引：3，自引：1，他引：3
记述了产自浙江省天台盆地的网形蛋类新材料,建立一新蛋属——拟网形蛋属(Paradictyoo lithusoogen.nov.),两个新蛋种:庒前拟网形蛋(Paradictyoolithus zhuangqianensis oogen.etoosp.nov.)和下西山拟网形蛋(P.xiaxishanensis oogen.et oosp.nov.)。在此基础上,重新系统描述其他已知4种网形蛋属成员的结构特征,并对网形蛋类的分类进行了订正:网形蛋属(Dictyoolithus)仅保留红坡网形蛋(D.hongpoensis Zhao,1994)一个蛋种;建立一新蛋属:原网形蛋属(Protodictyoolithus oogen.nov.),将发现于河南西峡盆地的内乡网形蛋(D.neixiangensis Zhao,1994)和发现于山东莱阳盆地的蒋氏网形蛋(D.jiangi Liu&Zhao,2004)分别修订为:内乡原网形蛋(修订种)(Protodictyoolithus neixiangensis(Zhao,1994)comb.nov.)和蒋氏原网形蛋(修订种)(P.jiangi(Liu&Zhao,2004)comb.nov.);此外,发现于吉林公主岭早白垩世的公主岭网形蛋(D.gongzhulingensis Wang et al.,2006)并不属于网形蛋类,而应归入似蜂窝蛋类(Similifaveoolithus),将其修订为公主岭似蜂窝蛋(修订种)(Similifaveoolithus gongzhulingensis(Wangetal.2006)comb.nov.)。 相似文献
17.
Qing He Shukang Zhang Lida Xing Qin Jiang Xiaoli Wang Zhenghua Pan 《Historical Biology》2019,31(2):168-176
Well-preserved dinosaur eggs from the Cretaceous Huizhou Formation in the Xiuning Basin, Anhui Province, China, are analysed in this paper. We describe a new oospecies, Similifaveoloolithus qiyunshanensis, based on several distinct characters of external morphology, size, eggshell thickness, and internal microstructure. Radial sections of this new oospecies show branched eggshell units with a fused layer near the outer surface, while numerous irregular pores and cones constitute a honeycomb pattern in tangential sections. The discovery of S. qiyunshanensis expands the distribution of Similifaveoloolithidae dinosaur eggs in China and provides new fossils for researching dinosaur eggshell formation mechanisms which are different from those of the currently known oofamilies. The dinosaur-egg-bearing strata in the Huizhou Formation have been dated to the early Late Cretaceous (Cenomanian-Turonian) on the basis of a similar dinosaur egg assemblage in the Tiantai Basin in Zhejiang Province. The eggs described in this paper are thought to have been laid in a buried nest while enrichment of trace elements in eggshells may have been caused by their ingestion into the body of the dinosaur producer. We suggest that the paleoclimate of this habitat was semi-arid to arid and that this environment was favourable for the preservation of eggs.http://zoobank.org/LSIDurn:lsid:zoobank.org:pub:9D63A51F-5A4B-4249-901D-42A33E9FA933 相似文献
18.
《Ichnos》2012,19(1-2):43-49
Cretaceous bird tracks assigned to the ichnogenera Aquatilavipes and Koreanaornis are reported for the first time from Sado Island in the Yeosu Island archipelago, Korea, an area already known for multiple dinosaur track-bearing horizons. The Koreanaornis tracks are associated with many small Cochlichnus trails attributed to nematode worms, on which the birds were likely feeding in a lake shoreline environment. The Koreanaornis and Aquatilavipes assemblages occur at different, albeit close, stratigraphic levels. The Aquatilavipes report is the first from Korea. 相似文献