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首页> 外文期刊>Paleobiology >Stable isotope evidence for changes in dietary niche partitioning among hadrosaurian and ceratopsian dinosaurs of the Hell Creek Formation, North Dakota
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Stable isotope evidence for changes in dietary niche partitioning among hadrosaurian and ceratopsian dinosaurs of the Hell Creek Formation, North Dakota

机译:稳定的同位素证据表明北达科他州地狱溪组的鸭嘴龙和角顶龙恐龙的饮食生态位分配发生变化

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摘要

Questions related to dinosaur behavior can be difficult to answer conclusively by using morphological studies alone. As a complement to these approaches, carbon and oxygen isotope ratios of tooth enamel can provide insight into habitat and dietary preferences of herbivorous dinosaurs. This approach is based on the isotopic variability in plant material and in surface waters of the past, which is in turn reflected by carbon and oxygen isotope ratios of animals that ingested the organic matter or drank the water. Thus, it has the potential to identify and characterize dietary and habitat preferences for coexisting taxa. In this study, stable isotope ratios from coexisting hadrosaurian and ceratopsian dinosaurs of the Hell Creek Formation of North Dakota are compared for four different stratigraphic levels. Isotopic offsets between tooth enamel and tooth dentine, as well as taxonomic differences in means and in patterns of isotopic data among taxa, indicate that primary paleoecological information is preserved. The existence of taxonomic offsets also provides the first direct evidence for dietary niche partitioning among these herbivorous dinosaur taxa. Of particular interest is the observation that the nature of this partitioning changes over time: for some localities ceratopsian dinosaurs have higher carbon and oxygen isotope ratios than hadrosaurs, indicating a preference for plants living in open settings near the coast, whereas for other localities isotope ratios are lower, indicating a preference for plants in the understory of forests. In most cases the isotope ratios among hadrosaurs are similar and are interpreted to represent a dietary preference for plants of the forest canopy. The inferred differences in ceratopsian behavior are suggested to represent a change in vegetation cover and hence habitat availability in response to sea level change or to the position of river distributaries. Given our current lack of taxonomic resolution, it is not possible to determine if dietary and habitat preferences inferred from stable isotope data are associated with single, or multiple, species of hadrosaurian/ceratopsian dinosaurs.
机译:单独使用形态学研究可能很难得出与恐龙行为有关的问题。作为这些方法的补充,牙齿珐琅质的碳和氧同位素比可以提供食草恐龙的栖息地和饮食偏好的信息。这种方法基于过去的植物材料和地表水中的同位素变异性,而变异性又可以通过摄入有机物或喝水的动物的碳和氧同位素比来反映。因此,它有可能为共存的生物分类识别和表征饮食和生境偏好。在这项研究中,比较了北达科他州地狱溪组同时存在的鸭嘴龙和角顶龙恐龙的稳定同位素比,用于四种不同的地层水平。牙釉质和牙本质之间的同位素偏移,以及分类单元之间同位素数据的方式和模式的分类学差异,表明已保留了主要的古生态信息。分类学偏移的存在也为这些食草恐龙类群中的饮食生态位分配提供了第一个直接证据。特别令人关注的是,这种划分的性质会随着时间而改变:在某些地区,ceratotopian恐龙的碳和氧同位素比率高于鸭嘴龙,这表明其偏爱生活在沿海附近露天环境中的植物,而对于其他地方的同位素比率而言较低,表明对森林底层植物的偏爱。在大多数情况下,鸭嘴龙之间的同位素比是相似的,并且被解释为代表了对林冠植物的饮食偏好。建议推断出角顶龙行为的差异代表植被覆盖的变化,并因此代表响应海平面变化或河流分流点位置的栖息地可用性。鉴于我们目前缺乏分类学分辨率,无法确定从稳定同位素数据推断出的饮食和栖息地偏好是否与单个或多个鸭嘴龙/鹿角龙恐龙有关。

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