Campbell James A, Mitchell Mark T, Ryan Michael J, Anderson Jason S
Department of Biological Sciences, University of Calgary, Calgary, AB, Canada.
Royal Tyrrell Museum of Palaeontology, Drumheller, AB, Canada.
PeerJ. 2021 Feb 11;9:e10720. doi: 10.7717/peerj.10720. eCollection 2021.
Elasmosaurid plesiosaurian remains have been documented from non-marine to paralic (fluvial to estuarine) sediments of the upper Campanian Dinosaur Park Formation (DPF) of southern Alberta since 1898. Despite this long collection history, this material has received relatively little research attention, largely due to the highly fragmentary nature of most recovered specimens. However, this assemblage is significant, as it constitutes a rare occurrence of plesiosaurian remains in a non-marine depositional environment. This study reports on a recently collected and prepared specimen, which represents the most complete elasmosaurid yet collected from the DPF. This specimen preserves the trunk region, the base of the neck and tail, a partial fore and hind limb, and tooth, and is sufficiently complete to be assigned as the holotype of a new genus and species. This new taxon is diagnosed by a distinctive character state combination including a boomerang-shaped clavicular arch with acute anterior process, convex anterolateral margin, deeply embayed posterior margin, and pronounced ventral keel, together with the presence of 22 dorsal vertebrae, and the anterior dorsal centra bearing a ventral notch. The DPF plesiosaurian fossils were recovered from both estuarine/bay and fluvial palaeochannel sediments. The holotype skeleton represents an osteologically mature individual with an estimated body length of around 5 m, although the largest referred DPF elasmosaurid might have been closer to 7 m, which is considerably larger than other plesiosaurians reported from non-marine deposits. This suggests small-body lengths relative to typical elasmosaurids from marine settings, but is consistent with other plesiosaurians recovered from non-marine sediments. The identification of a distinct elasmosaurid taxon in the DPF might be evidence of niche-partitioning among the predominantly oceanic members of the ubiquitous plesiosaurian clade.
自1898年以来,在艾伯塔省南部上坎帕阶恐龙公园组(DPF)的非海洋至近海(河流至河口)沉积物中已记录到薄板龙科蛇颈龙类化石。尽管有如此长的收集历史,但这些材料受到的研究关注相对较少,主要是因为大多数回收标本的性质高度破碎。然而,这一组合具有重要意义,因为它构成了非海洋沉积环境中罕见的蛇颈龙类化石。本研究报告了一个最近收集并准备好的标本,它是从DPF收集到的最完整的薄板龙科化石。该标本保存了躯干区域、颈部和尾部基部、部分前肢和后肢以及牙齿,完整程度足以被指定为一个新属和新物种的正模标本。这个新分类单元的特征是具有独特的特征状态组合,包括呈回旋镖形状的锁骨弓,前端尖锐,前外侧边缘凸起,后边缘深深凹陷,腹侧龙骨明显,还有22个背椎,以及前背椎体带有腹侧缺口。DPF蛇颈龙类化石是从河口/海湾和河流古河道沉积物中回收的。正模标本骨架代表一个骨骼成熟的个体,估计体长约5米,尽管DPF中最大的被参考的薄板龙科化石可能接近7米,这比从非海洋沉积物中报道的其他蛇颈龙类要大得多。这表明相对于海洋环境中的典型薄板龙科,其体型较小,但与从非海洋沉积物中回收的其他蛇颈龙类一致。在DPF中识别出一个独特的薄板龙科分类单元,可能是无处不在的蛇颈龙类分支中主要海洋成员之间生态位划分的证据。