Garros Christiana W, Powers Mark J, Dyer Aaron D, Currie Philip J
Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada.
Department of Ecology and Evolutionary Biology, University of Toronto, Toronto, Ontario, Canada.
J Anat. 2025 Sep-Oct;247(3-4):736-764. doi: 10.1111/joa.14262. Epub 2025 Apr 19.
Troodontidae is a family of small-bodied theropods known predominantly from Asia but are comparatively scarce in North America. In the Dinosaur Park Formation (DPF) of Alberta, Canada, they are known predominantly from isolated material, precluding taxonomic and ontogenetic precision for this clade. Previously never sampled histologically within the DPF, here we attempt to fill in gaps in our knowledge about the life histories of the clade in this formation by histologically surveying metatarsals, which are among the most abundant and identifiable troodontid elements in the DPF. We sampled 11 metatarsals (three metatarsal IIs, three metatarsal IIIs and five metatarsal IVs) of varying sizes and included three pathological individuals to describe the microanatomy of both healthy and pathological metatarsals, determine the ontogenetic status of each element and graph their pattern of growth. Osteohistology reveals that troodontid metatarsals grew and remodelled asymmetrically within the cortex, ceasing growth and remodelling primarily along articular surfaces and entheses. Pathological individuals ranged from displaying features of response to localised stress (chronic callus formation and avulsion/chip fracture) to extreme modification in response to trauma and inflammation at the distal joint. Only the latter appeared to be related to overall growth, suggesting the condition either developed early and stunted growth or another underlying cause was responsible for both the stunted growth and the resulting pathological features observed. Overall, tracking the growth of the specimens reveals that there are at least two growth trajectories within the DPF differentiated by the timing of major growth spurts and growth plateaus. Whether this represents sexual dimorphism, taxonomic diversity, or another form of variation warrants further investigation.
伤齿龙科是一类小型兽脚亚目恐龙,主要分布于亚洲,但在北美相对较少。在加拿大艾伯塔省的恐龙公园组地层(DPF)中,伤齿龙科化石主要是零散的,这使得对该类群进行精确的分类和个体发育研究变得困难。此前从未对DPF地层中的伤齿龙科化石进行过组织学采样,在此我们通过对跖骨进行组织学研究,试图填补我们对该地层中伤齿龙科恐龙生活史认识的空白,跖骨是DPF地层中最丰富且易于识别的伤齿龙科化石元素之一。我们采集了11根不同大小的跖骨(3根第二跖骨、3根第三跖骨和5根第四跖骨),其中包括3个病理个体,以描述健康和病理状态下跖骨的微观解剖结构,确定每个元素的个体发育状态,并绘制其生长模式图。骨组织学研究表明,伤齿龙科的跖骨在皮质内不对称生长和重塑,主要沿关节面和附着点停止生长和重塑。病理个体表现出从对局部压力的反应特征(慢性骨痂形成和撕脱/碎片骨折)到远端关节创伤和炎症引起的极端变化。只有后者似乎与整体生长有关,这表明这种情况要么是早期出现并阻碍了生长,要么是另一个潜在原因导致了生长发育迟缓以及所观察到的病理特征。总体而言,对标本生长情况的追踪表明,DPF地层中的伤齿龙至少有两种生长轨迹,主要区别在于主要生长突增和生长平台期的时间。这是否代表性别二态性、分类多样性或其他形式的变异,还有待进一步研究。