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Pathology or expected morphology? Investigating patterns of cortical porosity and trabecularization during infancy
Hayley Welsh1, Megan B Brickley2
1Department of Anthropology, University of Toronto, Toronto, Ontario, Canada.
Insights
Cortical bone porosity in infants increases with growth and weight-bearing activities, then decreases as children approach homeostasis. This transient porosity is a normal part of early skeletal development.
Area of Science:
- Paleopathology
- Pediatric Bone Biology
- Bioarchaeology
Background:
- Cortical porosity increases skeletal fragility in adults.
- Etiology of cortical porosity in pediatric populations is understudied.
- Understanding childhood bone development is crucial for bioarchaeological interpretation.
Purpose of the Study:
- To investigate age-related changes in femoral midshaft cortical porosity in infants and young children.
- To determine the influence of femoral growth and locomotor development on cortical porosity.
- To establish a baseline for normal skeletal development in early childhood.
Main Methods:
- Analysis of 48 individuals (fetal to 3.99 years) from a 10th-13th century French cemetery.
- Preparation and light microscopy of femoral midshaft histological sections.
- Calculation of geometric variables (total area, cortical area, pore area) using BoneJ software.
Main Results:
- Significant association between increased cortical porosity/trabecularization and age.
- Peak porosity observed in individuals aged 0.5-1.99 years, coinciding with accelerated growth and femoral loading.
- Reduced porosity in individuals aged 2.0-3.99 years suggests adaptation and approaching homeostasis.
Conclusions:
- Transient midshaft cortical porosity in infancy and early childhood is a normal developmental pattern.
- This porosity is likely driven by bone reorganization due to rapid growth and the onset of weight-bearing activities.
- Findings provide essential data for interpreting skeletal development in bioarchaeological studies.
Abstract:
Increased cortical porosity is associated with a heightened risk of skeletal fragility due to bone loss and structural decay in adults. However, few studies have examined the etiology of cortical porosity in infants and children. This study examines whether age-related changes in femoral growth and locomotor development influence femoral midshaft cortical porosity in a sample of 48 individuals (fetal to 3.99 years) from the 10th-13th century cemetery of St. Étienne de Toulouse, France. Histological sections were prepared and imaged using light microscopy. Midshaft geometric variables such as total area, cortical area, and pore area were calculated using BoneJ. Increased porosity and cortical trabecularization were found to be significantly associated with age, being almost exclusively present in individuals aged 0.5-1.99 years. At approximately 6 months of age infants typically begin engaging in regular femoral loading and experience an acceleration in growth. The observed increase in midshaft porosity and trabecularization, therefore, likely results from the reorganization and redistribution of cortical bone, stimulated by increased growth velocity and the onset of weight-bearing activities. The reduction in cortical porosity and trabecularization in individuals aged 2.0-3.99 years indicates that children are approaching some sort of homeostasis as growth velocity slows and their femora adapt to consistent loading. Understanding what expected skeletal development looks like is necessary when conducting bioarcheological studies and this study provides evidence for a pattern of transient midshaft porosity during infancy and early childhood.
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