Patterns of anemia and infection from medieval York,England

An assessment of the presence and patterns of porotic hyperostosis and periosteal reactions in the skeletal population (n = 1,014) from St. Helen-on-the-Walls, York, are used to examine health and disease in urban medieval England. The analyses of these two lesions indicate that 58% of the population display evidence of porotic hyperostosis and that 21.5% of the population display periosteal reactions. Through differential diagnosis it is asserted that porotic hyperostosis is associated with iron-deficiency anemia, and that periosteal reactions may be the result of endemic treponematosis and/or non-specific infection, including parasitic infestation. An association between the presence of remodeled lesions and adulthood is noticeable for both porotic hyperostosis and periosteal reactions, as is a pattern of increased average age at death for those displaying both conditions. © 1993 Wiley-Liss, Inc.     

Porotic Hyperostosis and Paleoepidemiology: A Forensic Perspective on Anemia among the Ancient Maya

Porotic lesions caused by childhood anemia are commonly found on ancient Maya crania and have been cited as evidence for extremely poor nutrition during the Classic Period. We reconsider this characterization in the light of recent data on childhood anemia in rural Guatemala and the prevalence of porotic hyperostosis in crania of forensic skeletal remains of rural highland Maya from Plan de Sanchez, Baja Verapaz, which date to 1982. The abundance of porotic hyperostosis in adults from Plan de Sanchez fits well with the number of modern rural children suffering from anemia, but the lesions are very rare compared to archaeological series. Although some minor change in diet and infection may contribute to differences in porotic hyperostosis, it is likely that higher mortality leads to fewer anemic lesions in modern adult crania. We hypothesize that more anemic children survived to adulthood in the past than do today, [iron-deficiency anemia, porotic hyperostosis, Maya, nutrition, forensic anthropology, osteological paradox]     

The causes of porotic hyperostosis and cribra orbitalia: A reappraisal of the iron‐deficiency‐anemia hypothesis

Porosities in the outer table of the cranial vault (porotic hyperostosis) and orbital roof (cribra orbitalia) are among the most frequent pathological lesions seen in ancient human skeletal collections. Since the 1950s, chronic iron‐deficiency anemia has been widely accepted as the probable cause of both conditions. Based on this proposed etiology, bioarchaeologists use the prevalence of these conditions to infer living conditions conducive to dietary iron deficiency, iron malabsorption, and iron loss from both diarrheal disease and intestinal parasites in earlier human populations. This iron‐deficiency‐anemia hypothesis is inconsistent with recent hematological research that shows iron deficiency per se cannot sustain the massive red blood cell production that causes the marrow expansion responsible for these lesions. Several lines of evidence suggest that the accelerated loss and compensatory over‐production of red blood cells seen in hemolytic and megaloblastic anemias is the most likely proximate cause of porotic hyperostosis. Although cranial vault and orbital roof porosities are sometimes conflated under the term porotic hyperostosis, paleopathological and clinical evidence suggests they often have different etiologies. Reconsidering the etiology of these skeletal conditions has important implications for current interpretations of malnutrition and infectious disease in earlier human populations. Am J Phys Anthropol 2009. © 2009 Wiley‐Liss, Inc.     

Porotic hyperostosis: a new perspective.

Porotic hyperostosis is a paleopathologic condition that has intrigued researchers for over a century and a half. It is now generally accepted that anemia, most probably an iron deficiency anemia, is the etiologic factor responsible for lesion production. Although there can be a number of factors involved in the development of iron deficiency anemia, a dietary explanation has often been invoked to explain the occurrence of porotic hyperostosis in past human skeletal populations. In fact, porotic hyperostosis has been referred to as a "nutritional" stress indicator. Traditionally those groups with a higher incidence of porotic hyperostosis have been considered to be less successful in adapting to their environment or more nutritionally disadvantaged than other groups. A new perspective is emerging that is challenging previous views of the role of iron in health and disease, thus having profound implications for the understanding of porotic hyperostosis. There is a new appreciation of the adaptability and flexibility of iron metabolism; as a result it has become apparent that diet plays a very minor role in the development of iron deficiency anemia. It is now understood that, rather than being detrimental, hypoferremia (deficiency of iron in the blood) is actually an adaptation to disease and microorganism invasion. When faced with chronic and/or heavy pathogen loads individuals become hypoferremic as part of their defense against these pathogens, thus increasing their susceptibility to iron deficiency anemia. Within the context of this new perspective porotic hyperostosis is seen not as a nutritional stress indicator, but as a indication that a population is attempting to adapt to the pathogen load in its environment.     

Anemia and childhood mortality: latitudinal patterning along the coast of pre-Columbian Peru

Hrdlicka ([1914] Smithson. Inst. Misc. Collect. 61:1-69) reported that pre-Columbian skeletal material from the coastal lowland Andean region exhibited a high frequency of porotic hyperostosis, a pathological condition of bone that generally is thought to indicate childhood anemia. While subsequent studies tended to reinforce this conclusion, factors implicated in the condition have yet to be fully explored in the region as a whole. This study explores regional and intravalley variation as one step in establishing biocultural variables that increase the apparent risk of childhood anemia. The study sample includes 1,465 individuals: 512 from Peruvian collections housed at the Field Museum of Natural History, and 953 from systematically excavated contexts from Moquegua, Peru. Environmental stressors, such as parasites and disease, rather than specific dietary practices were found to be more likely associated with childhood anemia in these coastal Andean samples. The study supports cribra orbitalia as an earlier expression of porotic hyperostosis and suggests that porotic hyperostosis, as recorded here, cannot be easily dismissed as a result of cranial shape modification. No clear temporal patterns were observed. Finally, the study establishes that comparing data for children and adults can reveal the relative association between childhood anemia and mortality. Childhood mortality associated with anemia was elevated where the presence of tuberculosis or tuberculosis-like conditions was more common and the presence of water-borne pathogens was negligible. In contrast, those buried at lower altitudes, closer to the coast, and consuming mainly marine resources were less likely to die in childhood with anemia than in the other contexts studied.     

Porotic hyperostosis: representative of a childhood condition

Porotic hyperostosis is currently considered to be one of several stress markers available for assessing the health and nutritional status of past human populations. The present study questions one of the basic assumptions underlying its use; that is, that the occurrence of porotic hyperostosis in an individual represents an episode of anemia that was current or had occurred within a relatively short period prior to death. A synthesis of data from a Romano-British site Poundbury Camp, anthropological and clinical studies, and information on bone physiology suggests that lesions of porotic hyperostosis seen in adults are most probably representative of a childhood episode of anemia. Lesions seen in adults are the result of bone changes occurring in the growth period that have not undergone complete remodelling. This viewpoint has implications for future interpretation of data on porotic hyperostosis obtained from skeletal collections.     

Cribra orbitalia,a possible sign of anemia in early historic native populations of the British Columbia coast

Excavated and museum skeletons of the postcontact period revealed cribra orbitalia in four native ethnolinguistic divisions of the British Columbia coast, Haida, Kwakiutl, Nootka, and Coast Salish. Affected skulls were distributed among 25 of 35 localities, indicating widespread occurrence in a mainly heterogeneous population. Manifestations were similar to porotic hyperostosis, and additional lesions in the sample tend to support the concept that cribra orbitalia is related to anemia. Both inherited and acquired disorders may have been involved in the etiology. A uniquely high incidence of 52.9% occurred in immature of the Haida, a relatively homogeneous population. However, marked variability in expression by age group and by sex in the total sample is suggestive of iron-deficiency anemia. The data and historical information parallel modern expectations of susceptibility. Among 454 skulls, cribra orbitalia occurred in 32.7% of growing children and adolescents, 19% of infants and toddlers, 13.3% of adult females, and 4.8% of adult males. Postcontact disruptions and disease may have figured in promoting iron-deficiency anemia, but noted precontact occurrences may also have been due to the disorder.     

Porotic hyperostosis: new evidence to support the anemia theory

The etiology of skull lesions known as porotic hyperostosis has long been a matter for speculation. The most widely accepted theory at present suggests that an anemia, either acquired or genetic, is responsible for lesion development. However, acceptance of this theory is not universal and the nature of the relationship between orbital and vault lesions remains a controversial issue. This paper provides a much broader field of supportive evidence on which to base the anemia theory. This involves a synthesis of information from the clinical and anthropological literature as well as new data from two skeletal collections: Poundbury Camp, a Romano-British series, and the Hodgson collection, a 19th century East Asian series. A comparison is made between clinical and anthropological data at the macroscopic, microscopic, radiographic, and demographic levels of analysis. This approach reveals the similarities in expression between clinically diagnosed anemias and porotic hyperostosis.     

Dietary iron-deficiency up-regulates hephaestin mRNA level in small intestine of rats

Hephaestin is a protein, recently found from the study of sla (sex-linked anemia) mouse. Hephaestin is suggested to transport iron from intestinal enterocytes into the circulation. Iron is essential for living and for humans to maintain a constant total iron concentration in whole body. In this study, it was found that dietary iron-deficiency up-regulated hephaestin mRNA level in the proximal small intestine of rats. Therefore, it is suggested that in dietary iron-deficiency, hephaestin gene expression in proximal small intestine is up-regulated to absorb more iron from diet.     

Porotic hyperostosis in a marine-dependent California Indian population

A maize-based iron- and protein-deficient diet is commonly cited as the most important cause of porotic hyperostosis among American Indian agriculturalists. An alternative to this maize dependence hypothesis is suggested by the analysis of 432 crania from the nonagricultural, fish-dependent population of the Channel Island area of southern California. Cribra orbitalia, a form of porotic hyperostosis associated with iron deficiency anemia, is just as common among these fisherpeople, whose diet was rich in iron and essential amino acids, as it is among maize-dependent agriculturalists. Northern Channel Island crania have much more cribra orbitalia than those from the California mainland. The highest incidence is on San Miguel, a small geographically isolated island with a shortage of fresh water and terrestrial resources. The Indians who lived on Santa Cruz, the largest of the northern Channel Islands with the greatest diversity of terrestrial plants and animals, have less cribra orbitalia than those who lived on Santa Rosa or San Miguel Island. This geographical distribution appears to be explained by island-mainland and interisland differences in water contamination, exposure to fish-borne parasites, and nutritional adequacy of the diet. The prevalence of porotic hyperostosis in a population with a heavy dietary dependence on marine resources shows that among prehistoric American Indians, this condition is not always associated with an iron- and protein-deficient diet of cultigens. It seems likely that high nutrient losses associated with diarrheal disease are often more significant in the etiology of porotic hyperostosis than a low dietary intake of essential nutrients.     

Human dietary change.

The transition from hunting and gathering to agriculture and animal husbandry in the Near East and Mediterranean Region began some 12,000 years ago. The ecological changes associated with this change are known to have been related to higher levels of stress from undernutrition and infectious disease. Certain pathologies found in human skeletal remains from this time are indicative of anaemia and osteoporosis, although it is not clear whether they had clear nutritional aetiologies. In this paper, dietary changes associated with changes in subsistence practices in this region are described. In addition, quantitative modelling of possible patterns of dietary and nutrient intakes of adult males before, and soon after, the establishment of agrarian economies is used to examine the proposition that the skeletal pathologies porotic hyperostosis, cribra orbitalia and porotic hyperostosis may have been due to nutritional deficiencies. The results suggest that protein deficiency was only likely if subjects were suffering from chronic energy deficiency (CED) and their diet contained no meat. Dietary calcium deficiency was possible after the transition to cultivation and animal husbandry, in the presence of moderate or severe CED. Anaemias, although present after the transition, were unlikely to have had dietary aetiologies, regardless of the severity of CED.     

AFM探测缺铁性贫血病人的红细胞

在纳米量级上探测红细胞生理病理特性对于揭示疾病的起源、早期诊断和有效的治疗是十分重要的。疾病可以从分子水平上扰乱红细胞的形貌和功能。缺铁性贫血病人的红细胞的形貌具有严重的表面畸形。通过高分辨率的原子力显微镜成像研究了健康人和缺铁性贫血病人红细胞的整个形貌和表面膜的差异。结果表明,红细胞的形貌参数（例如细胞的峰、谷、峰谷差、表面起伏和标准方差）可以探测健康和病理的红细胞。因此,红细胞的形貌信息可望成为诊断健康和疾病,以及评估治疗效果的重要指标。     

Recognition of sickle cell anemia in skeletal remains of children

The present study discusses in detail the osteological changes associated with sickle cell anemia in children and their importance in differential diagnosis. Posterior calcaneal and specific articular surface disruptive metacarpal lesions are diagnostic for sickle cell anemia. Calvarial thickening, tibial and femoral cortical bone thickening, and bowing are of more limited utility in differential diagnosis. Granular osteoporosis, pelvic demineralization and rib broadening are nonspecific. Localized calvarial “ballooning,” previously not described, may have diagnostic significance. Bone marrow hyperplastic response (porotic hyperostosis) in sickle cell anemia produces minimal radiologic changes contrasted with that observed in thalassemia and blood loss/hemolytic phenomenon. Two other issues, the osteological criteria for discriminating among the anemias and the purported relationship between porotic hyperostosis and iron deficiency anemia, are also discussed. There is sufficient information to properly diagnose the four major groups of anemias, and further, to establish that iron deficiency is only indirectly associated with porotic hyperostosis. The hyperproliferative bone marrow response (manifest as porotic hyperostosis) to blood loss or hemolysis exhausts iron stores, resulting in secondary iron deficiency. Am J Phys Anthropol 104:213–226, 1997. © 1997 Wiley-Liss, Inc.     

低频交变磁场刺激对缺铁性贫血大鼠贫血改善的作用研究

目的:明确低频正弦波交变电磁场对缺铁性贫血大鼠贫血改善的作用效果,为其未来的临床应用提供实验依据。方法:雄性断乳的SPF级Sprague-Dawley(SD)大鼠,共36只,随机的等分为空白对照组(n=12)、缺铁性贫血组(n=12)和缺铁性贫血+电磁场刺激组(n=12)。缺铁性贫血组和缺铁性贫血+电磁场刺激组的大鼠饲养以低铁饲料和去离子水,每周尾静脉放血1 m L。空白对照组大鼠饲养以常规饲料和普通蒸馏水,且不予尾静脉放血。对缺铁性贫血+电磁场刺激组的12只大鼠施加全身低频交变电磁场刺激,每天刺激2小时,连续刺激10周。实验结束后提取大鼠血液样本,使用氰化高铁血红蛋白法进行测定全血血红蛋白含量,使用专用试剂盒测定血清铁和总铁结合力;提取肝脏和脾脏组织,对肝脏铁和脾脏铁含量进行测定。结果:全身暴露低频交变电磁场刺激显著提高了缺铁性贫血大鼠体重(P0.05),提升了其血清铁含量(P0.05),显著提高全血血红蛋白含量(P0.05),并显著降低了缺铁性贫血大鼠血清总铁结合力(P0.05);同时,电磁刺激也显著提高了缺铁性贫血大鼠肝脏铁和脾脏铁含量(P0.05)。结论:交变电磁场作为一种经济、安全、无创的物理作用方式,具有较为显著的缺铁性贫血的改善效果。     

Amino acid analysis of bone from a possible case of prehistoric iron deficiency anemia from the American southwest

It is possible that dietary conditions can result in the production of abnormal bone protein. For example, a heavily maize-dependent diet could be deficient in one or more essential amino acids necessary to normal human biochemistry and consequently necessary for normal bone protein synthesis. Amino acid analysis of bone tissues, thus, could provide a useful diagnostic tool in paleopathology. To test this potential we have compared the amino acid analyses of bone samples from a prehistoric Southwest Indian child exhibiting porotic hyperostosis with samples taken from (1) two children's skeletons lacking bone lesions but from the same area and time, (2) a modern child who died from accidental causes, and (3) adult human compact bone. Analytical results of the nonpathological prehistoric specimens were virtually identical to that of the modern infant, indicating remarkable preservation of bone protein. The pathological bone sample differed from the three control specimens by having as much as 25% less of those amino acids containing hydroxyl group and acidic side chains. We interpret the amino acid profile for the diseased child as indicating the presence of a greater proportion of helical protein (or less noncollagenous protein) as well as a lowered degree of hydroxylation of proline and lysine. One explanation for our data is that protein biosynthesis is altered in the child exhibiting porotic hyperostosis, and either some proteins important in the early phases of mineralization are not produced in sufficient quantity, or some necessary enzyme cofactors (e.g., dietary ferrous ions) are missing. We conclude that our data are compatible with, but do not prove, the hypothesis that the porotic hyperostosis exhibited by the Southwest Indian child is the result of iron deficiency anemia.     

Prevalence and etiology of acquired anemia in Medieval York, England

This paper presents three distinct models for the development of acquired anemia: iron-deficiency anemia produced by the inadequate intake and/or absorption of iron, the anemia of chronic disease (ACD) caused by the body's natural iron-withholding defense against microbial invaders, and megaloblastic anemia caused by insufficient intake and/or absorption of vitamin B(12) or folic acid. These etiological models are used to interpret the distribution and etiology of anemia among adult individuals interred at the Medieval Gilbertine Priory of St. Andrew, Fishergate, York (n = 147). This bioarchaeological analysis uncovered not only a strong relationship between decreasing status and increasing prevalence of anemia for both men and women, but also identified clear sex-based differences at this site. Within the high-status group, blood and iron loss as a result of rampant parasitism likely produced an environment ripe for the development of iron-deficiency anemia, while the parasitic consumption of vitamin B(12) may have caused occasional cases of megaloblastic anemia. As status decreases, the interpretation of anemia becomes more complex, with megaloblastic anemia and ACD emerging as viable, potentially heavy contributors to the anemia experiences of low-status people at St. Andrew's. Apart from status effects, women (especially young women) are disproportionately affected by anemia when compared to men within their own status group and, on average, are also more likely to have experienced anemia than their male peers from other status groups. This suggests that high iron-demand reproductive functions helped to make iron-deficiency anemia a chronic condition in many women's lives irrespective of their status affiliation.     

A radiographic study of porotic hyperostosis

Skull lesions known as porotic hyperostosis have been of interest to researchers since the mid-19th century. The etiology of porotic hyperostosis has long been a matter for speculation yet there has never been complete acceptance or substantiation of any one of the many theories proposed. Today the most widely accepted theory suggests that anemias of either acquired or genetic origin are responsible for porotic hyperostosis. The present study tests this hypothesis using criteria which were chosen after the examination of clinical radiographs of patients with various types of anemia. These criteria are: the presence of “hair-on-end” trabeculation, outer table thinning, texture changes, diploic thickening, orbital roof thickening, orbital rim changes, and the underdevelopment of frontal sinuses. A comparison of these criteria from the clinical X-rays with X-rays of skulls with porotic hyperostosis provides a more rigorous, repeatable, and standardized method upon which to base a diagnosis. This approach enables radiography to provide the necessary link between the clinical and anthropological with which to investigate the origin of porotic hyperostosis.     

Iron-Deficiency Anemia is Associated with Altered Characteristics of Sleep Spindles in NREM Sleep in Infancy

Objective To determine the effects of iron-deficiency anemia on the development of non-rapid-eye-movement (NREM) sleep stages, as indexed by sleep spindles. Study design Patterns of sleep spindles during NREM sleep stages 2 and 3–4 (slow-wave-sleep, SWS) were compared in 26 otherwise healthy 6-month-old Chilean infants with iron-deficiency anemia and 18 non-anemic control infants. From polygraphic recordings, EEG activity was analyzed for sleep spindles to assess their number (density), duration, frequency, and inter-spindle interval. Results Iron-deficient anemic infants differed from the control group by having sleep spindles with reduced density, lower frequency, and longer inter-spindle intervals in NREM sleep stage 2 and SWS. Conclusions These results provide evidence of delayed sleep spindle patterns in iron-deficient anemic infants, suggesting that iron is an essential micronutrient for the normal progression of NREM sleep pattern development in the human. Special issue dedicated to Dr. Moussa Youdim.     

Diet, residential origin, and pathology at Machu Picchu, Peru

Pathological conditions in human skeletal remains provide a wealth of information about archaeological populations, but many are limited in their interpretive significance by their nonspecific etiologies. This study analyzes three common pathological conditions known to manifest in infancy and childhood in the skeletal population from Machu Picchu, Peru (N = 74) with published carbon, nitrogen, oxygen, strontium, and lead isotopic data (Turner et al.: J Archaeol Sci 36 (2009) 317–332; Turner et al.: Chungara: Revista de Antropología Chilena 42 (2010) 515–524) to distinguish early‐life diet from residential origins as significantly associated with pathologies among the site's inhabitants. Analyses of variance indicate highly significant variation between enamel δ¹⁸O values, which serve as a rough proxy of local environment, and both cribra orbitalia (CO) and porotic hyperostosis (PH), generally understood to be markers of anemia. Results tentatively suggest that individuals manifesting these lesions may have lived closer to the arid coasts; however, no significant variation was found in parameters of diet (enamel δ¹³C_carbonate, dentin δ¹³C_collagen, dentin δ¹⁵N) by either CO or PH, suggesting that the primary factors causing anemia may have been more significantly related to residential origin rather than diet. Linear enamel hypoplasia (LEH) frequency significantly varied by both dietary and residential parameters, supporting models of LEH formation from a synergy of dietary and environmental factors. These results support previous research on the etiology of PH in the Andes; they also represent a useful approach to refining site‐specific interpretations of pathological conditions in archaeological populations, and exploring etiological variation between populations. Am J Phys Anthropol, 2012. © 2012 Wiley Periodicals, Inc.     

Randomized Placebo-Controlled Trial of Helicobacter pylori Eradication for Iron-Deficiency Anemia in Preadolescent Children and Adolescents

Background. A few cases relating H. pylori infection to iron-deficiency anemia have been described recently. We investigated the role of H. pylori infection in iron-deficiency anemia in preadolescent children and adolescents.
Patients and Methods. We conducted a double-blind, placebo-controlled therapeutic trial in 43 subjects (mean age, 15.4 years) with iron-deficiency anemia. Endoscopy was performed, and biopsy specimens were examined by urease test and histological analysis. Twenty-two of 25 H. pylori –positive patients were assigned randomly to three groups. Group A patients were given oral ferrous sulfate and a 2-week course of bismuth subcitrate, amoxicillin, and metronidazole. Group B patients were given placebo for iron and a 2-week course of triple therapy. Group C patients were given oral ferrous sulfate and a 2-week course of placebo. Iron status was reassessed 4 weeks and 8 weeks after the 2-week regimen ended.
Results. Of the 43 subjects with iron-deficiency anemia, 25 (58.1%) had H. pylori in the antrum. Group A and B subjects, who received eradication therapy, showed a significant increase in hemoglobin level as compared with group C subjects at 8 weeks after therapy ( p = .0086).
Conclusions. Treatment of H. pylori infection was associated with more rapid response to oral iron therapy as compared with the use of iron therapy alone. Such treatment also led to enhanced iron absorption even in those subjects who did not receive oral iron therapy.