Department of Earth Sciences, University of Oxford, Oxford, United Kingdom.
PLoS One. 2013 May 31;8(5):e65989. doi: 10.1371/journal.pone.0065989. Print 2013.
Pliosaurids were a long-lived and cosmopolitan group of marine predators that spanned 110 million years and occupied the upper tiers of marine ecosystems from the Middle Jurassic until the early Late Cretaceous. A well-preserved giant pliosaurid skull from the Late Jurassic Kimmeridge Clay Formation of Dorset, United Kingdom, represents a new species, Pliosaurus kevani. This specimen is described in detail, and the taxonomy and systematics of Late Jurassic pliosaurids is revised. We name two additional new species, Pliosaurus carpenteri and Pliosaurus westburyensis, based on previously described relatively complete, well-preserved remains. Most or all Late Jurassic pliosaurids represent a globally distributed monophyletic group (the genus Pliosaurus, excluding 'Pliosaurus' andrewsi). Despite its high species diversity, and geographically widespread, temporally extensive occurrence, Pliosaurus shows relatively less morphological and ecological variation than is seen in earlier, multi-genus pliosaurid assemblages such as that of the Middle Jurassic Oxford Clay Formation. It also shows less ecological variation than the pliosaurid-like Cretaceous clade Polycotylidae. Species of Pliosaurus had robust skulls, large body sizes (with skull lengths of 1.7-2.1 metres), and trihedral or subtrihedral teeth suggesting macropredaceous habits. Our data support a trend of decreasing length of the mandibular symphysis through Late Jurassic time, as previously suggested. This may be correlated with increasing adaptation to feeding on large prey. Maximum body size of pliosaurids increased from their first appearance in the Early Jurassic until the Early Cretaceous (skull lengths up to 2360 mm). However, some reduction occurred before their final extinction in the early Late Cretaceous (skull lengths up to 1750 mm).
上龙类是一种生活在海洋中的掠食者,寿命长且分布广泛,存在于 1.1 亿年的时间里,从中侏罗世到早白垩世,占据着海洋生态系统的上层。英国多塞特郡的白垩纪晚期 Kimmeridge Clay 组中保存完好的巨型上龙类头骨代表了一个新物种,即凯瓦纳上龙。本研究详细描述了这个标本,并对晚侏罗世上龙类的分类和系统发育进行了修订。我们基于先前描述的相对完整、保存完好的标本,命名了另外两个新物种,即木匠上龙和韦斯特伯里上龙。大多数或所有晚侏罗世上龙类都代表了一个全球分布的单系群(上龙属,不包括“上龙”andrewsi)。尽管具有较高的物种多样性,分布广泛,出现时间长,但与早期多属上龙类组合(如中侏罗世牛津粘土组)相比,上龙类表现出的形态和生态变化相对较少。与类似上龙类的白垩纪 Polycotylidae 相比,上龙类的生态变化也较少。上龙类具有坚固的头骨、较大的体型(头骨长度为 1.7-2.1 米)和三棱形或近三棱形的牙齿,表明它们具有食肉类的习性。我们的数据支持了通过晚侏罗世时间下颚联合长度逐渐缩短的趋势,如前所述。这可能与对大型猎物的摄食适应有关。上龙类的最大体型从早侏罗世首次出现到早白垩世逐渐增大(头骨长度可达 2360 毫米)。然而,在晚白垩世早期(头骨长度可达 1750 毫米),它们最终灭绝之前,体型出现了一些缩小。