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Theropod dinosaurs are well known for having a ziphodont dentition: serrated, blade-shaped teeth that they used for cutting through prey. Serrations along the carinae of theropod teeth are composed of true denticles, a complex arrangement of dentine, enamel, and interdental folds. This structure would have supported individual denticles and dissipated the stresses associated with feeding. These particular serrations were previously thought to be unique to theropod dinosaurs and some other archosaurs. Here, we identify the same denticles and interdental folds forming the cutting edges in the teeth of a Permian gorgonopsian synapsid, extending the temporal and phylogenetic distribution of this dental morphology. This remarkable instance of convergence not only represents the earliest record of this adaptation to hypercarnivory but also demonstrates that the first iteration of this feature appeared in non-mammalian synapsids. Comparisons of tooth serrations in gorgonopsians with those of earlier synapsids and hypercarnivorous mammals reveal some gorgonopsians acquired a complex tissue arrangement that differed from other synapsids. 相似文献
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Margot Michaud Géraldine Veron Anne-Claire Fabre 《Evolution; international journal of organic evolution》2020,74(12):2681-2702
The skeleton is a complex arrangement of anatomical structures that covary to various degrees depending on both intrinsic and extrinsic factors. Among the Feliformia, many species are characterized by predator lifestyles providing a unique opportunity to investigate the impact of highly specialized hypercarnivorous diet on phenotypic integration and shape diversity. To do so, we compared the shape of the skull, mandible, humerus, and femur of species in relation to their feeding strategies (hypercarnivorous vs. generalist species) and prey preference (predators of small vs. large prey) using three-dimensional geometric morphometric techniques. Our results highlight different degrees of morphological integration in the Feliformia depending on the functional implication of the anatomical structure, with an overall higher covariation of structures in hypercarnivorous species. The skull and the forelimb are not integrated in generalist species, whereas they are integrated in hypercarnivores. These results can potentially be explained by the different feeding strategies of these species. Contrary to our expectations, hypercarnivores display a higher disparity for the skull than generalist species. This is probably due to the fact that a specialization toward high-meat diet could be achieved through various phenotypes. Finally, humeri and femora display shape variations depending on relative prey size preference. Large species feeding on large prey tend to have robust long bones due to higher biomechanical constraints. 相似文献
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The origin of endemic South American canid fauna has been traditionally linked with the rise of the Isthmus of Panama, suggesting that diversification of the dog fauna on this continent occurred very rapidly. Nevertheless, despite its obvious biogeographic appeal, the tempo of Canid evolution in South America has never been studied thoroughly. This issue can be suitably tackled with the inference of a molecular timescale. In this study, using a relaxed molecular clock method, we estimated that the most recent common ancestor of South American canids lived around 4 Ma, whereas all other splits within the clade occurred after the rise of the Panamanian land bridge. We suggest that the early diversification of the ancestors of the two main lineages of South American canids may have occurred in North America, before the Great American Interchange. Moreover, a concatenated morphological and molecular analysis put some extinct canid species well within the South American radiation, and shows that the dental adaptations to hypercarnivory evolved only once in the South American clade. 相似文献
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STEVEN M. HOLLAND 《Palaeontology》2010,53(6):1237-1254
Abstract: Using Whittaker’s concepts of alpha, beta, and gamma diversity, Sepkoski asked how global diversity was assembled at scales ranging from the community to the province. In the years since, ecologists have recast diversity in terms of additive partitions where total diversity can be decomposed into sample‐level alpha diversity plus the sum of a series of beta diversity terms that reflect progressively larger spatial scales. Given that marine alpha diversity represents a tiny fraction of global diversity, Phanerozoic global diversity patterns must be dominated by changes in beta diversity at one or more scales. A ballooning ecological literature demonstrates wide variation in beta diversity among ecosystems, regions, and taxa, suggesting that large changes in beta diversity on evolutionary timescales are likely. But the question is which scales are the most important. Several recent palaeontological studies help to constrain beta diversity within sedimentary basins, and the emergence of sample‐based databases puts an answer to Sepkoski’s question within reach. A new method for calculating diversity partitions for richness is introduced, which allows the calculation of each species’ contribution to alpha and beta diversity, as well as the contribution of each sampling unit to beta diversity. 相似文献
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晚古生代瓢叶目植物的古生态学探讨 总被引：2，自引：0，他引：2
对已知瓢叶目植物生态信息较为全面的观察分析表明 ,华夏植物群中瓢叶目植物的生态条件与欧美植物群较为相似。很可能 ,瓢叶目植物在欧美植物区和华夏植物区均可发育于水分充足的低地植物群和排水条件较好的高地植物群。对华夏植物群中某些低地群落的植物古生态样方统计分析结果显示 :一般情况下 ,瓢叶目植物的属种数量与植物群落中其它类群数量相比所占份额较少 (分异度不高 ) ,而它的个别种的数量则在群落中占据的比重较大 ,甚至占据优势地位 (丰度较高 )。从群落结构来看 ,瓢叶目植物所在的群落往往具有较好的分层结构。瓢叶目和某些楔叶纲、真蕨和种子蕨纲植物共同构成群落的林下层植被。群落的中、高层通常是石松纲和科达纲 。 相似文献
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湘西北晚二叠世—早三叠世早期牙形石古生态 总被引：4，自引：0，他引：4
通过对牙形石器官的对称性、相分布和地球化学特征的研究,探讨湘西北晚二叠世至三叠纪初牙形动物的生态分布.按器官所包括不同对称型分子的比例,牙形动物器官的对称性可分为4级,器官的对称性越高,动物运动能力越强.湘西北晚二叠世一三叠纪初地层可分为6种沉积相,即盆地相、盆缘-台坡相、开阔台地相、边缘浅滩相、局限台地相和泥坪相.具不同对称级器官的属种在6种沉积相中的差异分布,反映了牙形动物的3种生态类型:自由游泳型、浮游型和底栖型.牙形石地球化学组分的变化与当时环境演变相吻合.随水深增加,化石中的P含量升高,而Ca、s、sr的含量降低;Al、Fe和Ba在近岸浅水环境的牙形石中富集;而Mg的富集指示高盐环境.基于上述研究,划分了4个牙形石相,建立了一个组合横向替代的牙形动物生态分布模式. 相似文献
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Records of a lake's life in time: the sediments 总被引：2，自引：2，他引：2
Winifred Pennington 《Hydrobiologia》1981,79(3):197-215
The evidence from analysis of cores from lake sediments is used to identify the influences which, acting through time, have brought about changes in the lakes of the English Lake District. These are: i. climatic changes, recorded mainly in microfossil assemblages ii. soil dynamics on catchments — the natural soil development of an interglacial cycle and its effect on water composition, and iii. perturbations of input resulting from activities of man.The present position of each of 14 lakes in a series of increasing eutrophication is shown to be the result of two processes of modification by man. The first was a significant reduction in volume of the hypolimnion of the shallow lakes, consequent on the accelerated rate of sediment accumulation which followed deforestation and cultivation of catchments in all the lakes — this did not affect the biology of the deep lakes. The second has been the introduction of human and animal wastes into some of the lakes during the last 120 years, which imposed on affected lakes a process of more rapid change which was more intense in the shallow lakes. 相似文献
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文中简述了中国的琥珀研究历史,并简要介绍了本专辑的内容.本专辑呈现了近年来我国学者对克钦琥珀内含物研究的部分新进展,包括了来自14个研究单位的26位作者的13篇论文,涵盖了植物、脊椎动物、腹足类和昆虫等类群. 相似文献
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Marc Philippe Gilles Cuny Varavudh Suteethorn Naramese Teerarungsigul Georges Barale Frédéric Thévenard 《Historical Biology》2013,25(1-4):1-6
Published reports of amber predating the Aptian are rare and mention only amber pieces the size of millimetric marbles. Mid Cretaceous amber records, however, show a dramatic increase in number as well as in the size of the pieces, a phenomenon which is still poorly understood. The discovery of the first Jurassic deposit with comparatively large centimetric sized pieces of amber, in southern Thailand, is significant. Taphonomy and palaeobotany indicate a dense forest surrounding a coastal lake dominated by the resin-producing Agathoxylon tree. Since the palaeoecology of other amber-producing Jurassic and Cretaceous deposits is very similar a new hypothesis needs to be sought to explain the mid Cretaceous amber boom. It is suggested here that it was the result of a geological or taphonomic bias because coastal lacustrine environments are much better preserved after the Aptian on a worldwide scale. 相似文献
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生物化石群落在埋葬过程中普遍经历了均时作用的过程。正是这种作用导致了同一生态环境域,但不同时期生物组合相混合的结果。因此,这种化石群落可能为一个连续演化群落的不同阶段的混合体,也可能是环境连续演化过程中不同生态群落的混合组合,这样的化石组合所记录的古生物学信息非常复杂。因此,对化石累积过程中的均时作用的清晰了解,将非常有助于古生物群落的分类学、居群动力学、埋葬学、古生态学、演化古生物学,甚至地层学研究精度的提高。文章根据前人的研究,扼要介绍和讨论均时作用的概念、过程、程度、效应和判别,及受均时作用影响的化石组合的分类。 相似文献
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Type and referred specimens of Coniasaurus crassidens from the Lower Chalk (Upper Cretaceous; Cenomanian) of southeast England, are re-described. The type is a left maxilla associated with 14 dorsal vertebrae. The maxilla is elongate, bears a low ascending process, and has a long and posteriorly positioned external narial margin. The first maxillary tooth is pointed and bears a groove on the labial face; more posterior maxillary teeth are increasingly rounded and bulbous, and have a single groove on the labial face. Mandibles assigned to Coniasaurus cf. C. crassidens possess teeth of similar form; mandibular bones include the dentary, splenial, angular, coronoid, prearticular, and surangular. A number of features show important similarities to later mosasaurs and contemporaneous groups such as dolichosaurs. These new data provide a very different picture of coniasaurs and their mode of life in the early Upper Cretaceous. The functional morphology of coniasaur teeth is unique and shows occlusion between the lingual platforms of the upper teeth with the crowns of the lower teeth. Coniasaurs can be considered as analgous to small sauropterygians in terms of general morphology, habitats, and trophic structure. Coniasaur distributions in the Cenomanian and Turonian of Europe and North America are similar to the palaeobiogeographic patterns of other organisms living in the Tethys and SuperTethys Seaway. 相似文献
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本文简要叙述南沙海区全新世小孔亚目苔藓虫群体形状和生态环境的关系,对非附着生长的类型进行了初步的分类。 相似文献
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广西隆林祥播中二叠世生物礁的钙藻化石 总被引：1，自引：2，他引：1
本文描述了广西隆林祥播中二叠世茅口期生物礁中的钙藻化石17属18种,其中新属5个:Paralithoporella gen. nov., Guangxilamina gen. nov., Favoporella gen. nov., Sinophyllum gen. nov.,和Monostysisyrinx gen. nov.; 新种9个:Solenopora guangxien sis sp. nov., Paralithoporella sincrisis gen. et sp. nov., Guangxilamina incompta gen. et sp. nov., Favoporella hexagona gen. et sp. nov., Ivanovia permica sp. nov., Anchicodium expressum sp. nov., Sinophyllum hexagonum gen. et sp. nov., Sphaeroporella minima gen. et sp. nov., Monostysisyrinx circula ris gen. et sp. nov.。本文还建立一新科——Monostysi sy rinaceae。在当前生物礁中,钙藻是重要的造礁生物,可以起造架、粘结、障积等作用,也可作为居礁生物或造粒生物 相似文献
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描术贵州西部晚石炭世威宁组的腹足类７属９种（其中２新种）,早石炭世草海组鸭子塘段的腹足类６属６种（其中１新种）。参照黄渤海海域内现生腹足类的生态习性,初步推断鸭子段为早石炭世浅海陆棚沉积。 相似文献
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James O. Farlow 《Historical Biology》2013,25(1-4):49-51
The palaeoecology of a sequence of five closely spaced mammalian assemblages in the English Late Eocene Bembridge Limestone Formation is studied using cladistic, seriation and ecological diversity methods, after assessing the collecting and taphonomic biases. Analysis of this sequence is important as it is temporally close to the terminal Eocene global cooling event. It is concluded that the assemblages probably reflect quite closely the species composition of the original living communities and that they indicate habitats ranging from an open wooded environment to dense forest. The oldest assemblage (limestone facies) indicates open wooded habitat and contains earliest occurrences of certain taxa in the English Eocene; these represent northward dispersal from southwestern Europe in response to changing climate. The more forested habitats occur higher in the sequence and are characterised by ‘Lazarus’ taxa, suggesting reversion to earlier existing environments. Small scale changes appear to relate to local events, whereas more major ones may result from global climate change. Certain pairs of closely related species are segregated in different assemblages which are habitat distinctive, a conclusion not available from their morphologies. 相似文献
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This paper reports on newly developed ecomorphological models for the cervid intermediate phalanx. Using a geometric morphometric approach, we quantitatively assess the overall gracility of the bone, the depth and concavity of the proximal articulation and the roundness and symmetry of the distal articulation in the intermediate phalanx, to establish relationships between morphology, locomotor behavior and environment. The morphology of the phalanx was found to vary along a gradient from gracile phalanges with shallow proximal articulations in forms adapted to yielding substrate, to robust phalanges with deeper proximal articulations in taxa adapted to firm substrate. Phylogeny and allometry are accounted for using regressions and phylogenetic comparative methods. Although the results indicate phylogeny explains part of the morphological variation, overall the shape of the intermediate phalanx appears mainly driven by differences in function. Consequently, this element promises to be a useful palaeoenvironmental proxy that can be applied on fossil assemblages with cervid remains. 相似文献