Abstract
Fracture is one of the pathological signs most frequently encountered in archaeologically obtained bones. To expand the paleopathological knowledge on traumatic injuries, it is desirable to secure data on long bone fractures from as wide a geographic and temporal range as possible. We present, for the first time, evidence of long bone fractures in a 16th-18th century Joseon skeletal series (n=96). In this study, we found 3 Colles' fractures of the radius in 2 individual cases. The pattern of fractures was unique. Although previous reports show that the ulna is broken more often than the radius, ulnar fracture associated with fending off a blunt attack was rare in our series (1/7 cases). Transverse fractures, typically caused by intentional violence, were also very rare (1/7 cases) in this study. These results may reflect the relatively tranquil lives of the Joseon people in 16th-18th century Korea. We also found post-fracture complications such as deformations, bone length shortening, and osteomyelitis. The present study would be of interest to medical scientists in related fields because it is one of the few studies conducted on long bone fractures among pre-modern societies in East Asian countries, thus far.
Evidence of trauma is one of the most frequently observed medical signs in human skeletons from archaeological sites [1-4]. Osteological studies on traumatic injuries have recently evolved from simple case reports to in-depth, population-level investigations [5, 6]. Some studies have extended this line of inquiry further, investigating trauma patterns in association with socioeconomic conditions. In the process, medical knowledge of long-bone fractures in history has become much more comprehensive [1, 3, 7, 8]. Categories of traumatic injuries in historical skeleton samples include fracture, dislocation, and post-traumatic deformity. [2, 4]. Long bone fractures have been studied over the past several decades. The earliest trauma samples discovered in archaeological sites are Homo erectus bones taken from a Choukoutien cave in China [4, 9], as well as Homo sapiens specimens dating to the Paleolithic through Neolithic periods [9, 10].
The historical literature suggests that fracture hazards are usually determined by cultural, environmental, and socioeconomic conditions prevailing in a given human society. The prevalence and distribution of fractures change with the culture and subsistence base of each human society [2, 4, 7, 10-15]. Securing data from as wide a geographic and temporal range as possible is desirable to expand the paleopathological knowledge base on fractures. However, research on the variances in fracture prevalence relative to temporal and geographic conditions is inadequate. In East Asian countries, where industrialization was delayed until recently, no studies have been conducted on fractures in premodern societies yet.
Over the past several years, we attempted to build a human skeletal sample collection consisting of specimens obtained from 16th-18th century Joseon tombs in Korea. Our investigations of the collection have revealed important information concerning the health and disease status of pre-modern Joseon people [16-21]. We undertook osteological examinations of skeletons from the same collection to determine the prevalence and location of long bone fractures in premodern Korean specimens. The purpose of our study was to contribute to a better understanding of the fracture patterns prevailing in a premodern East Asian population.
We examined the long bones of Joseon Dynasty skeletons, maintained at Seoul National University College of Medicine, Korea, to identify osteological evidence of fractures. Archaeological evidence and carbon dating results confirmed that every skeleton in this study belonged to 16th-18th century Korean people. Although the cases examined in this series were collected from different cemeteries of Joseon period, the tombs that contained these skeletons were of the same type, Hoegwakmyo. This type of Joseon tomb was surrounded by a fortified barrier made of a lime-soil mixture that successfully reduced grave intrusion and robbery.
The long bones examined (n=96) included the humerus, ulna, radius, femur, tibia, fibula, and clavicle. Since 61 bone elements (4.5%) were lost or severely damaged, the total number of elements examined was 1,283. We determined the sex of the individuals by the shape of the sciatic notch or mastoid process. We estimated the age at death following the method of Lovejoy et al. [21]. Briefly, individuals were classified into adolescent (12-20 years), young adult (20-35 years), middle aged (35-50 years), and old (>50 years) groups using osteological indicators such as the degrees of transverse organization, granularity, apical activity, retroauricular activity, and articular surface porosity.
Genuine fractures were differentiated from post-mortem damage after interment by suggestive clues such as the surface coloration in the fracture site distinct from other parts [2, 4, 22]. Affected and unaffected sides of long bones were always compared in the same individual because rotation or abnormal deviation of the bone could not be easily identified in the cases that exhibited other pathologies such as infections [4]. We also determined the type of long bone fractures. Direct trauma causes penetrating, comminuted, transverse, and crush type fractures, while indirect trauma causes spiral, oblique, torus, impacted, burst, and avulsion fractures [2]. Of these, transverse and oblique fractures are especially significant, because transverse fractures are known to result from intentional violence, whereas oblique fractures are mainly sustained in accidents [4]. The position of fracture in the shaft of the long bone, i.e., proximal, middle or distal third, was recorded following the method of Grauer and Roberts [7]. Rotational or linear deformity, healed fracture alignment, bone shortening, presence of osteomyelitis, and callus formation were also examined and described.
In some disputed cases, the pattern of fracture was confirmed by radiographic analysis. Following gross inspection, simple radiographs of the fracture were obtained in standard anteroposterior and lateral views. Radiographs in the mediolateral or tangential views were also obtained if necessary. Percentage of fracture was calculated for each element and individual. Multiple fractures were defined by presence of ≥2 fractures, and were calculated for each individual.
To presume the good reasons for arm fractures of Joseon people, we also searched for information in The Diaries of the Royal Secretariat (Seungjeongwon Ilgi), the historical literature of the Joseon Dynasty [23].
The study population included 96 individuals: 56 men (58.3%) and 40 women (41.7%). Of these, 5 individuals (cases nos. 33, 41, 65, 98, and 100) showed fractures (5.2%). The number of bone elements fractured was 7 (0.55%) (Table 1). All of them exhibited signs of healed fractures, but none had evidence of post-mortem changes after interment. Four fractures were found in the upper extremity bone elements, while 3 fractures were identified in the lower extremity elements (Table 1). Fractures were identified in middle-aged (cases nos. 33, 98, and 100) and old (cases nos. 41 and 65) individuals. Four fractures were identified in men (cases nos. 41, 65, 98, and 100) and only 1 in women (case no. 33). Oblique fractures were observed in 6 elements (cases nos. 33, 65, 41, and 100), while a transverse fracture was found only in the left ulna of case 98 (Table 1).
In case no. 33 (middle-aged woman), an oblique fracture was identified in the middle of the left femoral shaft. Marked deformity, axial deviation, and rotation were associated with shortening of the bone length after fracture (Fig. 1A). The marked changes observed on gross examination of the femur suggested that the healing process was atypical. Radiography showed bony irregularities in the medullary cavity (Fig. 1B, C). We also found an opening in the posterior part of the left femur, possibly representing a cloaca penetrating into the marrow space (Fig. 1D). A bony fragment, possibly healed in a malaligned position, was identified on its anterior surface (Fig. 1E, F). All these signs suggest that the individual might have had osteomyelitis as a complication after femur fracture.
Case no. 41 (old man) showed a Colles' fracture in the distal right radius; fracture type was oblique. We observed radial shortening on gross examination (Fig. 2A, B) with dorsal and proximal displacement of the distal fracture fragment (Fig. 2A, D). The distal radius also showed radial angulation with cortical disruption and a sharp edge on the volar side, suggesting that healing occurred without proper reduction (Fig. 2C, E). Callus formation, dorsal tilt, and shortening of the bone were prominent radiographic features in the right radius (Fig. 2F). Case no. 41 probably experienced significantly limited range of motion and loss of function because of the severe angulation and bone length shortening.
Case no. 65 (old man) had fractures in the distal left fibula and tibia, with bony thickening in the distal tibia (Fig. 3A). An oblique fracture line was observed on radiographs of the tibia (Fig. 3B, C). The distal left fibula was also thickened and rotated, and radiographic examination revealed a radiolucent fracture line and cortical thickening (Fig. 3D, G). In case no. 98 (middle-aged man), a transverse fracture was noted in the mid-shaft of the left ulna (Fig. 4A, C), most likely caused by direct intentional force. The lower left ulnar shaft was widened without shortening of the length (Fig. 4A, B). Radiographs showed the radiolucent fracture line and callus formation (Fig. 4B, E). No evidence of malalignment or rotation of the ulnar axis was observed.
Case no. 100 was a middle-aged man with oblique Colles' fractures in both radii. The left radius was shortened (Fig. 4F). Radiographs showed prominent osteosclerotic change in the right radial metaphysis, suggesting recent fracture (Fig. 4G, H). Dorsal angulation was also confirmed by the presence of volar tilt on the lateral view, measured as the angle created by articular surface of distal radius and a line drawn perpendicular to the long axis of the radius (Electronic Supplementary Fig. 1). The distal angulation between the long axis of the radial bone and the distal end of the radius was more prominent in the left radius. Although the fractured area was covered by remodeled bone, significant proximal displacement was not evident (Electronic Supplementary Fig. 1C, D).
In this study, among the many factors possibly influencing fracture frequency, we first considered age and sex. All of our long bone fracture samples were from middle-aged or old individuals. This is understandable, since the long bones from older individuals are likely to be more fragile and prone to injury by even low-energy impacts. Senile osteoporosis is known to significantly increase the vulnerability of bones to trauma [4]. We also observed that long bone fractures were much more common in men than in women. As noted in studies on other human populations [24, 25], this male preponderance might be associated with typical sex-related differences in physical activity. Joseon men typically performed more strenuous work than women, and so would have sustained a higher frequency of fractures.
We also considered the social and economic status of the individuals in our interpretation of the current results. Most skeletons examined in this study were collected from Hoegwakmyo, a unique burial system of the Joseon Dynasty. The people of Joseon society regarded Hoegwakmyo as an ideal tomb because this manner of constructing tombs was highly recommended by Chu Hsi, the grandmaster of Confucianism [26]. Nevertheless, the tomb was only adopted by the rich Joseon elites because its construction was too expensive for lower-class individuals. Therefore, when archaeologists in Korea found Hoegwakmyo tombs in archaeological fields, they assumed that the human remains in these tombs must be from the upper class of Joseon society [26, 27]. Most of the individuals represented in the present study are much more likely to have been landowners than farmers [26].
The fracture type and location, also known to vary by population [14, 15], were also considered in this study. Although a number of investigators have reported a high frequency of clavicular involvement in fractures [13, 28, 29], we could not identify any clavicle fractures in our Joseon skeletal series (Table 1). The pattern of forearm fracture in the present study was unique. In most previous studies, a very high percentage of fractures occurred in the forearm bones, with the ulna broken more often than the radius [10, 29, 30]. One such example is the Monteggia fracture, a fracture of the proximal third of ulna with dislocation of the radius head. Paleopathologists consider the finding of a large number of Monteggia fractures in a skeletal series important because they may have been incurred while fending off a blunt attack, implying that the people lived in an environment where violence was rampant [1, 14, 30]. Although forearm fractures were commonly observed in the present study, each 1 involved the radius, with the exception of 1 element (case no. 98, possibly a Monteggia fracture). We discovered 3 Colles' fractures of different severity in 2 individuals (cases nos. 41 and 100) (Table 1).
The Colles' fracture is generally associated with indirect, accidental falls on the hand (e.g., a short fall caused by a shift in body weight), resulting in angulation, proximal displacement of the distal fragment, and bone length shortening [28, 31, 32]. Similarly, accidents can be considered the cause of the Colles' fractures in this study. The high-class, elite Joseon individuals buried in Hoegwakmyo would naturally have fewer incidents of hard-labor-related accidents that could have caused bone breakage. Some, although not all, Colles' fractures in this study might have been caused by accidents characteristic only of the upper classes in Joseon society. Our search for contemporary articles on fractures in historical documents of Joseon society (Seungjeongwon Ilgi) interestingly showed that many arm injuries of the Joseon elite were caused by accidents such as a fall from a horse (Electronic Supplementary Table 1).
The fracture types also indicate a rarity of injuries possibly induced by intentional violence in our series. Most of the fractured elements were of the oblique type (6/7, 85.7%), suggesting indirect, accidental forces acting from a distance [2, 7]. Transverse fracture, typically associated with intentional violence [4, 33], was identified in only 1 individual (case no. 98). This supports the conclusion that the Joseon individuals examined in this study might not have been commonly subjected to blunt trauma in a violent setting. We can assume that the Joseon elite spent tranquil lives.
Post-fracture complications include infection, tissue necrosis, abnormal or non-union, and bone deformity. Deformations can develop or worsen because individuals living with fractures compensate for their injuries [4]. We observed a variety of fracture-induced complications in this study, for example malalignment (cases nos. 41, 98, and 100) caused by incomplete reduction of the injury. In case no. 33, post-fracture infection appeared to have extended to the medullary space, and this is particularly interesting because although osteomyelitis was a common disorder in centuries prior to the use of antibiotics, it has rarely been traced in archaeological samples [4, 11, 30]. Because of the difficulty in diagnosing osteomyelitis by bone examination alone, researchers worldwide hesitate to definitively declare lesions to be osteomyelitis without very clear, incontrovertible supporting evidence [4]. Our case no. 33 may be 1 such rare example, in which we confirmed the most typical osteological signs of osteomyelitis, including bony proliferation, cloaca opening, and bone marrow involvement.
The unique points of our study were not limited to fracture type and location. Skeletal series in most countries have revealed fracture rates of 15.1-32.9% (person fracture rates) and 2.4-11.7% (total % of fractured elements). However, the long bone fractures rates in our Joseon sample were only 5.2% (person fracture rate) and 0.55% (total % of fractured elements) (Electronic Supplementary Table 2). The fact that the samples in our skeletal series were collected only from the upper and ruling classes of the Kingdom and not from all strata of Joseon society, may explain the relatively low fracture prevalence observed in this study. The low fracture rate might well have reflected the less strenuous physical labor of the Joseon individuals examined, since performance of heavy physical labor is closely associated with fracture frequency [29]. However, the comparison of disease signs in different skeletal series must be approached discreetly if the research methods used have not been sufficiently standardized [34]. Definitive conclusions cannot be derived while the technical limitations inherent in non-standardized studies on skeletal series persist under different conditions.
Despite its shortcomings, the present study is of interest to scientists in related medical fields. The skeletal series of East Asian societies might manifest unique fracture patterns because of the distinctive lifestyle that they have maintained for many millennia. However, few simple descriptive studies have been conducted on skeletons collected from archaeological fields in Korea or other East Asian countries until now. Our study involves long bone fracture cases evidently representing a 16th-18th century Joseon skeletal series. We have presented the first description of some unique points of fractures observed in these 16th-18th century Joseon skeletons. Further research focusing on different social strata and populations is nevertheless required to gain a clearer understanding of trauma in historic Asian populations.
Figures and Tables
Acknowledgements
This study was supported by Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Education, Science, and Technology (2012-0002118).
References
1. Kilgore L, Jurmain R, Van Gerven D. Palaeoepidemiological patterns of trauma in a medieval Nubian skeletal population. Int J Osteoarchaeol. 1997; 7:103–114.
2. Lovell NC. Trauma analysis in paleopathology. Am J Phys Anthropol. 1997; 104:Suppl 25. 139–170.
3. Judd MA. Comparison of long bone trauma recording methods. J Archaeol Sci. 2002; 29:1255–1265.
4. Ortner D. Identification of pathological conditions in human skeletal remains. 2nd ed. San Diego: Academic Press;2003.
5. Lovejoy CO, Heiple KG. Analysis of fractures in skeletal populations with an example form the Libben site, Ottawa County, Ohio. Am J Phys Anthropol. 1981; 55:529–541.
6. Larsen CS. Bioarchaelolgy: interpreting behavior form the human skeleton. Cambridge: Cambridge University Press;1997.
7. Grauer AL, Roberts CA. Paleoepidemiology, healing, and possible treatment of trauma in the medieval cemetery population of St. Helen-on-the-Walls, York, England. Am J Phys Anthropol. 1996; 100:531–544.
8. Yoon HK, Park C, Jang S, Jang S, Lee YK, Ha YC. Incidence and mortality following hip fracture in Korea. J Korean Med Sci. 2011; 26:1087–1092.
9. Weidenreich F. The duration of life of fossil man in China and the pathological lesions found in his skeleton. Chin Med J. 1939; 55:34–44.
10. Angel JL. Patterns of fractures from neolithic to modern times. Anthropol Kozl. 1974; 18:9–18.
11. Hooton EA. The Indians of Pecos pueblo: a study of their skeletal remains. New Haven: Yale University Press;1930.
12. Hill P. Whithorn and St. Ninian: the excavation of a monastic town 1984-1991. Stroud: Sutton Publishing;1997. p. 519–562.
13. Judd MA, Roberts CA. Fracture patterns at the Medieval Leper Hospital in Chichester. Am J Phys Anthropol. 1998; 105:43–55.
14. Judd MA. Trauma and interpersonal violence in ancient Nubia during the Kerma period (ca. 2500-1500 BC). Edmonon, Alberta: University of Alberta;2000.
15. Djurić MP, Roberts CA, Rakocević ZB, Djonić DD, Lesić AR. Fractures in late medieval skeletal populations from Serbia. Am J Phys Anthropol. 2006; 130:167–178.
16. Kim MJ, Oh CS, Lee IS, Lee BH, Choi JH, Lim DS, Yi YS, Han WJ, Kim YS, Bok GD, Lee SD, Shin DH. Human mummified brain from a medieval tomb with lime-soil mixture barrier of the Joseon Dynasty, Korea. Int J Osteoarchaeol. 2008; 18:614–623.
17. Han SS, Baek KW, Shin MH, Kim J, Oh CS, Lee SJ, Shin DH. Dental caries prevalence of medieval Korean people. Arch Oral Biol. 2010; 55:535–540.
18. Kim DK, Lee IS, Kim WL, Lee JS, Koh BJ, Kim MJ, Youn MY, Shin MH, Kim YS, Lee SS, Oh CS, Shin DH. Possible rheumatoid arthritis found in the human skeleton collected from the tomb of Joseon Dynasty, Korea, dating back to the 1700s AD. Int J Osteoarchaeol. 2011; 21:136–149.
19. Kim YS, Oh CS, Lee SJ, Park JB, Kim MJ, Shin DH. Sex determination of Joseon people skeletons based on anatomical, cultural and molecular biological clues. Ann Anat. 2011; 193:539–543.
20. Shin DH, Oh CS, Kim YS, Hwang YI. Ancient-to-modern secular changes in Korean stature. Am J Phys Anthropol. 2012; 147:433–442.
21. Lovejoy CO, Meindl RS, Pryzbeck TR, Mensforth RP. Chronological metamorphosis of the auricular surface of the ilium: a new method for the determination of adult skeletal age at death. Am J Phys Anthropol. 1985; 68:15–28.
22. Ubelaker DH, Adams BJ. Differentiation of perimortem and postmortem trauma using taphonomic indicators. J Forensic Sci. 1995; 40:509–512.
23. Royal Secretariat. The daily records of the Royal Secretariat of Chosun Dynasty (1623-1894). Seoul: National Institute of Korean History;1970.
24. Pratt DS, Marvel LH, Darrow D, Stallones L, May JJ, Jenkins P. The dangers of dairy farming: the injury experience of 600 workers followed for two years. Am J Ind Med. 1992; 21:637–650.
25. Stueland DT, Lee BC, Nordstrom DL, Layde PM, Wittman LM, Gunderson PD. Case-control study of agricultural injuries to women in central Wisconsin. Women Health. 1997; 25:91–103.
26. Shin MH, Yi YS, Bok GD, Lee EJ, Spigelman M, Park JB, Min SR, Shin DH. How did mummification occur in bodies buried in tombs with a lime soil mixture barrier during the Joseon Dynasty in Korea. In : Peña PA, Martin CR, Rodríguez MA, editors. Mummies and Science: World Mummies Research. Santa Cruz de Tenerife: Academia Canaria de la Historia;2008. p. 105–113.
27. Kim MJ, Lee IS, Kim YS, Oh CS, Park JB, Shin MH, Shin DH. Diffuse idiopathic skeletal hyperostosis cases found in Joseon Dynasty human sample collection of Korea. Int J Osteoarchaeol. 2012; 22:235–244.
28. Judd MA, Roberts CA. Fracture trauma in a medieval British farming village. Am J Phys Anthropol. 1999; 109:229–243.
29. Hamilton FH, Boardman J. Fracture tables, with a supplement compiled from Dr. Hamilton's notes by John Boardman comprising in all an analysis of 461 cases of fractures. Buffalo: Jewett, Thomas & Co.;1853.
30. Wood-Jones F. Fractured bone and dislocations. In : Eliot-Smith G, Wood-Jones F, editors. The Archaeological Survey of Nubia for 1907-1908. Vol. II. Report on the Human Remains. Cairo: National Printing Department;1910. p. 293–342.
31. Mays SA. A palaeopathological study of Colles' fracture. Int J Osteoarchaeol. 2006; 16:415–428.
32. Adams JC. Adam's outline of fractures: including joint injuries. Edinburgh: Churchill Livingstone;1983.
33. Wesolowski V. Caries prevalence in skeletal series: is it possible to compare? Mem Inst Oswaldo Cruz. 2006; 101:Suppl 2. 139–145.
34. Burrell LL, Mass MC, Van Gerven DP. Patterns of long-bone fracture in two Nubian cementeries. Hum Evol. 1986; 1:495–506.
Electronic Supplementary Materials
Supplementary data including two tables and one figure can be found with this article online at http://www.acbjournal.org/src/sm/acb-46-203-s001.pdf.