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埃德蒙顿龙(恐龙:鸭嘴龙科)的颅生长和变异:对北美洲晚白垩世大型食草动物多样性的启示。

Cranial growth and variation in edmontosaurs (Dinosauria: Hadrosauridae): implications for latest Cretaceous megaherbivore diversity in North America.

机构信息

Department of Ecology and Evolutionary Biology, University of Toronto, Toronto, Ontario, Canada.

出版信息

PLoS One. 2011;6(9):e25186. doi: 10.1371/journal.pone.0025186. Epub 2011 Sep 28.

DOI:10.1371/journal.pone.0025186
PMID:21969872
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3182183/
Abstract

The well-sampled Late Cretaceous fossil record of North America remains the only high-resolution dataset for evaluating patterns of dinosaur diversity leading up to the terminal Cretaceous extinction event. Hadrosaurine hadrosaurids (Dinosauria: Ornithopoda) closely related to Edmontosaurus are among the most common megaherbivores in latest Campanian and Maastrichtian deposits of western North America. However, interpretations of edmontosaur species richness and biostratigraphy have been in constant flux for almost three decades, although the clade is generally thought to have undergone a radiation in the late Maastrichtian. We address the issue of edmontosaur diversity for the first time using rigorous morphometric analyses of virtually all known complete edmontosaur skulls. Results suggest only two valid species, Edmontosaurus regalis from the late Campanian, and E. annectens from the late Maastrichtian, with previously named taxa, including the controversial Anatotitan copei, erected on hypothesized transitional morphologies associated with ontogenetic size increase and allometric growth. A revision of North American hadrosaurid taxa suggests a decrease in both hadrosaurid diversity and disparity from the early to late Maastrichtian, a pattern likely also present in ceratopsid dinosaurs. A decline in the disparity of dominant megaherbivores in the latest Maastrichtian interval supports the hypothesis that dinosaur diversity decreased immediately preceding the end Cretaceous extinction event.

摘要

北美的晚白垩世化石记录样本丰富,仍然是评估恐龙多样性模式的唯一高分辨率数据集,这些模式与白垩纪末期灭绝事件有关。与埃德蒙顿龙关系密切的鸭嘴龙类(恐龙:鸟脚亚目)是北美西部最晚坎潘期和马斯特里赫特期沉积物中最常见的巨型草食动物之一。然而,近三十年来,埃德蒙顿龙物种丰富度和生物地层学的解释一直不断变化,尽管该进化枝通常被认为在马斯特里赫特晚期经历了辐射。我们首次使用几乎所有已知完整的埃德蒙顿龙头骨的严格形态计量学分析来解决埃德蒙顿龙多样性的问题。结果表明,只有两个有效物种,即来自晚坎潘期的埃德蒙顿龙和来自晚马斯特里赫特期的 E. annectens,而先前命名的分类群,包括有争议的 Anatotitan copei,则建立在与个体发育大小增加和异速生长相关的假设过渡形态上。对北美鸭嘴龙类分类群的修订表明,从早马斯特里赫特期到晚马斯特里赫特期,鸭嘴龙类的多样性和差异都有所减少,角龙类恐龙也可能存在这种情况。在马斯特里赫特晚期,主要巨型草食动物的差异减少,这支持了恐龙多样性在白垩纪末期灭绝事件之前就已经减少的假说。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/17110fdb86bf/pone.0025186.g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/e837922dd5dd/pone.0025186.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/a3a55a0e31ed/pone.0025186.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/c5908ff7d482/pone.0025186.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/5cc73e5130a7/pone.0025186.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/9e6168d5cf27/pone.0025186.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/b3446a3a5d7d/pone.0025186.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/17110fdb86bf/pone.0025186.g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/e837922dd5dd/pone.0025186.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/a3a55a0e31ed/pone.0025186.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/c5908ff7d482/pone.0025186.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/5cc73e5130a7/pone.0025186.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/9e6168d5cf27/pone.0025186.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/b3446a3a5d7d/pone.0025186.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9ed1/3182183/17110fdb86bf/pone.0025186.g007.jpg

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