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1

Bennion, Janet. "Storming Zion: Government Raids on Religious Communities , by STUART A. WRIGHT and SUSAN J. PALMER." Sociology of Religion 77, no. 4 (November 3, 2016): 443–44. http://dx.doi.org/10.1093/socrel/srw046.

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2

Gallagher, Eugene V. "Review: Storming Zion: Government Raids on Religious Communities by Stuart A. Wright and Susan J. Palmer." Nova Religio 20, no. 3 (February 1, 2017): 138–39. http://dx.doi.org/10.1525/nr.2017.20.3.138.

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3

Levin, Yaroslav Aleksandrovich. "«The Palmer raids» - reaction to «The Red Scare» and Edgar Hoover’s role in the actions of the U.S. Department of Justice." Samara Journal of Science 8, no. 3 (August 5, 2019): 211–14. http://dx.doi.org/10.17816/snv201983217.

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The paper is devoted to reaction of the U.S. Department of Justice to the October revolution of 1917 in Russia and the process which received the name The Red Scare in the historiography. The basic changes which happened in Russia, the ideas of radical social justice, the dictatorship of the proletariat and the world revolution during the last stages of the World War I led to an extremely negative perception of the Bolshevik party and its policy in the USA. The general unfriendly spirit was warmed up by various publications accusing V.I. Lenin and his colleagues of communications with Germany (well-known Sissons documents) as well as by various publications in the press. At the same time, the revolution in Russia became an ideological beacon for anarchists and socialists worldwide including America. A special activity was shown by the galleanists organization (followers of the revolutionary and the ideologist of anarchism Luigi Galleani). From April to June 1919 they organized a series of explosions as well as attempts on the life of prominent politicians, businessmen and even the staff of intelligence agencies of the USA. In response to it the Attorney-General Alexander Mitchell Palmer initiated a series of military actions directed against all left-wing parties and groups in the country. The Bureau of investigations became the main body that was occupied in these actions. The paper analyzes the raids that were carried out by BI, their features and effects as well as the career of John Edgar Hoover, who was Palmers personal assistant at that time and later became a director of FBI.
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Ellis, Mark. "J. Edgar Hoover and the “Red Summer” of 1919." Journal of American Studies 28, no. 1 (April 1994): 39–59. http://dx.doi.org/10.1017/s0021875800026554.

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J. Edgar Hoover directed the Bureau of Investigation (BI), later renamed the Federal Bureau of Investigation, from 1924 until his death in 1972. His autocratic style of management, self-mythologising habits, reactionary political opinions and accumulation of secret files on real, imagined and potential opponents have been widely documented. The views and methods he advocated have been variously attributed to values he absorbed as he grew up and to certain peculiarities of his personality. Most biographers trace his rapid rise to prominence in the BI to his aptitude for investigating alien enemies during World War I, and radicals during the subsequent Red Scare. He was centrally involved in the government's response to the alleged threat of Bolshevism in America, and, although he later denied it, he co-ordinated the notorious Palmer raids of January 1920, in which thousands of aliens were rounded up and several hundred were deported.
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5

Worley, Robert. "Q and A with Author: Wright, Stuart A. and Susan J. Palmer, Storming Zion: Government Raids on Religious Communities." Theory in Action 12, no. 3 (July 31, 2019): 173–78. http://dx.doi.org/10.3798/tia.1937-0237.1925.

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6

Popkova, Anna. "Imagining the Russian Community: Novoye Russkoe Slovo, the First Red Scare, and the Palmer Raids, 1919-1920." Journalism History 48, no. 1 (January 2, 2022): 41–60. http://dx.doi.org/10.1080/00947679.2022.2027140.

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7

Matthew May. "From the Palmer Raids to the Patriot Act: A History of the Fight for Free Speech in America (review)." Rhetoric & Public Affairs 12, no. 1 (2009): 130–32. http://dx.doi.org/10.1353/rap.0.0100.

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8

Levin, Y. A., and S. O. Buranok. "Formation of “Red Scare” Concept in USA in First Half of XX Century." Nauchnyi dialog, no. 5 (May 30, 2020): 424–34. http://dx.doi.org/10.24224/2227-1295-2020-5-424-434.

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The issue of how the an important and multifaceted aspect of domestic and foreign policy formed by US FBI, called the "Red Scare" is addressed in the article. It is shown that this political and ideological concept seemed unacceptable for distribution in the United States, since it created a danger of the penetration of communist ideas and their adherents into all government bodies and major public organizations. Factors that influenced the strengthening of the FBI’s position in the fight against communist ideology in the United States in the 1920s, in particular, terrorist acts carried out by left-wing forces, which allowed the FBI to implement a program of struggle (Palmer raids) with organizations, adhering to communist views are examined. The measures taken by the FBI and its director John Edgar Hoover in the 1930s against Soviet intelligence, which contributed to reinforcing negative perceptions of the “Red Scare” within the agency are highlighted. The authors conclude that the position of the FBI influenced the building of the attitude of the entire US intelligence community in this vein, which in turn had a great impact on the development of the country’s domestic and foreign policy.
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9

Tobey, Kristen. "Wright, Stuart A., and Palmer, Susan J. Storming Zion: Government Raids on Religious Communities. Oxford: Oxford University Press, 2015. xii+288 pp. $29.95 (paper)." Journal of Religion 97, no. 3 (July 2017): 448–50. http://dx.doi.org/10.1086/691821.

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10

Ahmad, Imad A. "Enemy Aliens." American Journal of Islam and Society 21, no. 3 (July 1, 2004): 139–42. http://dx.doi.org/10.35632/ajis.v21i3.1774.

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David Cole, a professor at the Georgetown University Law Center, is a brilliantconstitutional attorney and an outstanding advocate of civil liberty. InEnemy Aliens, he articulates the case that Attorney General John Ashcroft’sabridgements of the civil liberties of non-citizens and alleged “enemy combatants”in the name of the war on terrorism is at once part of an old strategyof establishing such constitutionally questionable actions against thosepeople least politically able to defend themselves and, at the same time, thefirst step to expanding such incursions against civil rights into the populationat large.Cole writes with the meticulous care appropriate to a legal mind ofthe first caliber and with a graceful and literate rhetorical style. “The linebetween citizen and foreigner, so natural during wartime,” he writes (p.5), “is not only easy to exploit when restrictive measures are introduced,but also easy to breach when the government later finds it convenient todo so.” Cole writes with authority on facts of which too many Americansare completely ignorant: selective detention and deportation based onreligion or national origin, secret trials (or no trials), prolonged interrogation“under highly coercive, incommunicado conditions ... and withoutaccess to lawyers,” and “indefinite detention on the attorney general’ssay-so” (p. 5).Cole presents the historical precedents that justify his thesis. In 1988,President Ronald Reagan signed a bill apologizing for the appalling detentionof Japanese-Americans during World War II. However, that internmentwas an extension of the Enemy Alien Act of 1798, “driven by nativist fearsof radical French and Irish immigrants” (p.7), but still on the books. The“Palmer Raids” of the early twentieth century, wherein thousands of for ...
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11

McCrary, Charles. "Storming Zion: government raids on religious communities, by Stuart A. Wright and Susan J. Palmer, New York, Oxford University Press, 2015, xii + 288 pp., ISBN 978 019 539889 2, US$99.00 (cloth); ISBN 978 019 539890 8, US$29.95 (paperback)." Religion 47, no. 3 (October 21, 2016): 530–33. http://dx.doi.org/10.1080/0048721x.2016.1244637.

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12

Kobayashi, Satoru, Tomohiro Oguchi, Simone Tanelli, and Eastwood Im. "Backscattering enhancement on spheroid-shaped hydrometeors: Considerations in water and ice particles of uniform size and Marshall-Palmer distributed rains." Radio Science 42, no. 2 (March 3, 2007): n/a. http://dx.doi.org/10.1029/2006rs003503.

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13

Motta, Javan Pereira, José Tarcísio da Silva Oliveira, Rafael Leite Braz, Ana Paula Coelho Duarte, and Rejane Costa Alves. "Caracterização da madeira de quatro espécies florestais." Ciência Rural 44, no. 12 (December 2014): 2186–92. http://dx.doi.org/10.1590/0103-8478cr20130479.

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O conhecimento das relações existentes entre a estrutura anatômica da madeira com suas propriedades físicas ou mecânicas é importante para seu uso adequado. Este trabalho teve como objetivo caracterizar a anatomia microscópica e propriedades físicas da madeira de quatro diferentes espécies florestais. A madeira estudada foi proveniente das seguintes espécies: Cedrela fissilis (Cedro), Híbrido clonal Eucalyptus urophylla × Eucalyptus grandis (Eucalipto urograndis), Hovenia dulcis (Uva do Japão) e Gallesia integrifolia (Pau d'alho). Para a determinação da retratibilidade, utilizou-se a norma MB26/40 da ABNT (1940); as dimensões lineares foram obtidas com palmer, precisão de 0,001mm. O estudo da anatomia da madeira seguiu as recomendações da norma de procedimento em estudos de anatomia de madeira, da COPANT (1974) e também da IAWA (1989). Os caracteres anatômicos avaliados foram: diâmetro tangencial (µm) e frequência de vasos (nomm-2); comprimento de fibra (µm), diâmetro de lume (µm) e espessura de parede de fibra (µm); altura (µm), largura (µm) e frequência de raios (nomm-1). Os valores do coeficiente anisotrópico foram de 1,16; 1,77; 1,81 e 1,84 para a madeira de C. fissilis, H. dulcis, Híbrido clonal e G. integrifolia, respectivamente, demonstrando que a madeira de C. fissilis possui elevada estabilidade dimensional e as demais madeiras, valores aceitáveis para esse coeficiente.
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14

Dias, Fellipe Camargo Ferreira, and Luiz Sinesio Silva Neto. "AVALIAÇÃO DA RELAÇÃO ENTRE SARCOPENIA E FUNCIONALIDADE EM IDOSAS QUILOMBOLAS DE BREJINHO DE NAZARÉ – TO." DESAFIOS - Revista Interdisciplinar da Universidade Federal do Tocantins 6, no. 1 (March 30, 2019): 54–59. http://dx.doi.org/10.20873/uft.2359365220196154.

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A sarcopenia está associada a diversas doenças, redução da funcionalidade e prejuízos para qualidade de vida dos gerontes. A associação da sarcopenia com funcionalidade em populações quilombolas tem sido pouco estudada. Este trabalho teve por objetivo verificar a associação entre sarcopenia e funcionalidade em idosas quilombolas e não quilombolas. Estudo transversal realizado com 62 participantes mulheres (variando de 60 a 85 anos), que foram divididas em dois grupos, sendo 39 quilombolas (GQ) e 23 não quilombolas (GC). Para o diagnóstico de sarcopenia foi utilizado o algoritmo proposto pelo European Working Group on Sarcopenia in Older People, a massa muscular foi analisada pelo exame de absortometria de raios-x de dupla energia e a força de preensão palmar por meio do dinamômetro de mão. O desempenho físico foi analisado pelo teste de velocidade de marcha. Para analisar a capacidade funcional os testes de Katz e Lawton foram utilizados. Foi identificada uma prevalência de sarcopenia de 5,12% no GQ e de 8,69% no GC. Há maior proporção de mulheres quilombolas com incapacidade funcional, 100% delas apresentando dependência para ambas as atividades. A condição de ser quilombola demonstrou maiores prejuízos na capacidade funcional, independentemente de ser acometida por sarcopenia.
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15

Symons, Jennifer. "Mechanical Effect of Performance Pressure Boots on Cadaveric Equine Hindlimb Fetlock Biomechanics." Animals 11, no. 4 (March 30, 2021): 958. http://dx.doi.org/10.3390/ani11040958.

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Pressure boots are applied to hind limbs of showjumping horses with the intent to enhance jumping form. Manufacturers claim acupressure points enhance proprioception of hind limbs. With this increased awareness, horses are expected to retract their hind limbs to clear jump rails. This research aimed to investigate a more direct, mechanical effect of pressure boots on hind limb biomechanics. Cadaveric hind limbs (n = 6) were mechanically loaded in axial compression (3 cycles at 0.25 Hz, displacement control ~3300 N) with (2 trials) and without (2 trials) a pressure boot applied. During mechanical loading, fetlock angle was measured using bone fixed pins with retroreflective markers (30 Hz). Changes in limb load and fetlock angle between unloaded and loaded states, as well as average fetlock joint stiffness, were compared between trials with and without the pressure boot via ANOVA. Differences in measured loads between trials with and without the boot were observed in both unloaded (Δ = 6 N, p = 0.05) and loaded states (Δ = 25 N, p = 0.002). Trials with the boot had greater average fetlock stiffness (Δ = 3 N/degree, p = 0.001). Differences in loads with and without boots may increase with greater fetlock angles when cantering and jumping. These mechanical effects of pressure boots may contribute to greater tensile loading of palmar tendons and ligaments, and likelihood of musculoskeletal injury that can be related to animal welfare issues.
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16

Thomas, Z. A., F. Kwasniok, C. A. Boulton, P. M. Cox, R. T. Jones, T. M. Lenton, and C. S. M. Turney. "Early warnings and missed alarms for abrupt monsoon transitions." Climate of the Past Discussions 11, no. 2 (April 13, 2015): 1313–41. http://dx.doi.org/10.5194/cpd-11-1313-2015.

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Abstract. Palaeo-records from China (Cheng et al., 2009; Wang et al., 2008, 2001) demonstrate the East Asian Summer Monsoon (EASM) is dominated by abrupt and large magnitude monsoon shifts on millennial timescales, switching between periods of high and weak monsoon rains. It has been hypothesised that over these timescales, the EASM exhibits two stable states with bifurcation-type tipping points between them (Schewe et al., 2012). Here we test this hypothesis by looking for early warning signals of past bifurcations in speleothem records from Sanbao Cave and Hulu Cave, China (Wang et al., 2008, 2001), spanning the penultimate glacial cycle, and in multiple model simulations derived from the data. We find hysteresis behaviour in our model simulations with transitions directly forced by solar insolation. We detect critical slowing down prior to an abrupt monsoon shift during the penultimate deglaciation consistent with long-term orbital forcing. However, such signals are only detectable when the change in system stability is sufficiently slow to be detected by the sampling resolution of the dataset, raising the possibility that the alarm was missed and a similar forcing drove earlier EASM shifts.
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17

Norström, E., M. E. Kylander, S. R. Sitoe, and J. M. Finch. "Chronostratigraphic palaeo-climate phasing based on southern African wetlands: From the escarpment to the eastern seaboard." South African Journal of Geology 124, no. 4 (December 1, 2021): 977–94. http://dx.doi.org/10.25131/sajg.124.0063.

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Abstract This paper aims to identify chronostratigraphic palaeo-climatic boundaries based on proxy indications from mountain- and coastal wetlands in eastern South Africa and Lesotho. Phase boundaries were identified from timing of climate change inferred by proxies, as well as regime shifts in climate variability. Sometimes magnitude and/or frequency of change was also considered. Summarizing the common palaeo-climatic indications suggest the following chronostratigraphic climate phases: 25 to 18 ka, 18 to 15 ka, 15 to 11.5, 11.5 to 8 ka, 8 to 5.5 ka, 5.5 to 2 ka and 2 to 0 ka. The most robust boundaries were identified at 18 ka, 15 ka and 2 ka, i.e. these boundaries were supported by several proxies/sites. The other boundaries were less clearly detected from available proxies/sites and should be regarded tentative. The timing of a climate shift often coincides at coast and mountain sites. However, the climate conditions within each chronostratigraphic phase sometimes vary between coast and inland sites. The 25 to 18 ka phase was cool and dry with strong and frequent storms, followed by the ca. 18 to 15 ka period when conditions were less severe but still generally cool and dry. At ca. 15 to 11.5 ka several proxies infer warmer climate, with less winter rains. During 11.5 to 8 ka a general increase in wetness is inferred, followed by warming over the 8 to 5.5 ka phase. Between 5.5 and 2 ka a successive change towards wetter is indicated, although timing differ between sites. After 2 ka generally a more variable climate is seen, often with high magnitude shifts between dry and wet. The data resolution, i.e. the number of available wetland records, increases with time from very low during glacial times, to highest resolution during late Holocene. Geographically, sites in the mountain region are overrepresented compared to coastal sites. A comparison with coastal lake records suggests a more variable climate at coastal sites compared to mountain sites during mid- and late Holocene, although different proxy resolution and methodology cannot be ruled out as an explanation. A case study compares multiproxy records from Drakensberg (Sekhokong, Ntsikeni) and the coast (Mfabeni), discussing advantages and problems associated with proxy-comparisons within and between sites.
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18

Thomas, Z. A., F. Kwasniok, C. A. Boulton, P. M. Cox, R. T. Jones, T. M. Lenton, and C. S. M. Turney. "Early warnings and missed alarms for abrupt monsoon transitions." Climate of the Past 11, no. 12 (December 8, 2015): 1621–33. http://dx.doi.org/10.5194/cp-11-1621-2015.

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Abstract. Palaeo-records from China demonstrate that the East Asian Summer Monsoon (EASM) is dominated by abrupt and large magnitude monsoon shifts on millennial timescales, switching between periods of high and weak monsoon rains. It has been hypothesized that over these timescales, the EASM exhibits two stable states with bifurcation-type tipping points between them. Here we test this hypothesis by looking for early warning signals of past bifurcations in speleothem δ18O records from Sanbao Cave and Hulu Cave, China, spanning the penultimate glacial cycle. We find that although there are increases in both autocorrelation and variance preceding some of the monsoon transitions during this period, it is only immediately prior to the abrupt monsoon shift at the penultimate deglaciation (Termination II) that statistically significant increases are detected. To supplement our data analysis, we produce and analyse multiple model simulations that we derive from these data. We find hysteresis behaviour in our model simulations with transitions directly forced by solar insolation. However, signals of critical slowing down, which occur on the approach to a bifurcation, are only detectable in the model simulations when the change in system stability is sufficiently slow to be detected by the sampling resolution of the data set. This raises the possibility that the early warning "alarms" were missed in the speleothem data over the period 224–150 kyr and it was only at the monsoon termination that the change in the system stability was sufficiently slow to detect early warning signals.
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19

Bowman, DMJS. "Diversity Patterns of Woody Species on a Latitudinal Transect From the Monsoon Tropics to Desert in the Northern Territory, Australia." Australian Journal of Botany 44, no. 5 (1996): 571. http://dx.doi.org/10.1071/bt9960571.

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A belt transect, made up of 15 contiguous cells (width, 3.5° of longitude; length, 1° of latitude), was established from the monsoon tropics on the central north coast of the Northern Temtory (11°S) to the central Australian desert on the South Australian border (26°S). On this transect, mean annual rainfall was found to have a negative exponential decay with latitude, with arid conditions commencing at around 18"s-the limit of the monsoonal rains. The mean elevation of each cell steadily increased from the north coast to reach a maximum average elevation of 700 m at around 23°S. The mean alphadiversity (quadrat species richness), and mean beta-diversity (turnover of species along an environmental gradient) was determined for each of the 15 cells by sub-sampling a large 20 × 20 m quadrat data set (N > 2000) collected during the course of the Northern Territory 1:106 vegetation mapping program. It was found that there was little within-cell variation of beta-diversity of woody species which occurred in at least five quadrats, as approximated by the first axis of a detrended correspondence analysis (DCA) of these data. The mean first axis DCA scores were strongly correlated with latitude (r = 0.99); thus, there is no evidence for a floristic disjunction in the composition of common woody species between the monsoon tropics and desert. Mean alpha-diversity had a bimodal distribution on the latitudinal transect, with the maximum mean quadrat richness in the monsoon tropics and a second smaller peak occurred in central Australia, with the lowest levels of alpha-diversity to the south of the limit of the monsoon rains. This pattern was mirrored by the mean number and mean Shannon-Wiener diversity of 1:106 vegetation map units on the transect. It was found that 81% of the variance of mean alpha-diversity was explained by mean annual rainfall and mean elevation for the 15 cells. The increase in mean alpha-diversity in central Australia appears to be related to environmental heterogeneity associated with mountainous terrain. It is possible that the central Australian mountains are a refuge for plants that were more widespread during the last ice-age. It is unknown whether the woody species diversity patterns are in equilibrium with the prevailing climate. More data on the palaeo-environments of the Northern Territory are required to answer this question.
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20

Schittek, K., B. Mächtle, F. Schäbitz, M. Forbriger, V. Wennrich, M. Reindel, and B. Eitel. "Holocene environmental changes in the highlands of the southern Peruvian Andes (14° S) and their impact on pre-Columbian cultures." Climate of the Past Discussions 10, no. 2 (April 11, 2014): 1707–46. http://dx.doi.org/10.5194/cpd-10-1707-2014.

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Abstract. Within palaeoenvironmental studies, high-altitude peatlands of the Andes still remain relatively unexploited, although they offer an excellent opportunity for high-resolution chronologies, on account of their high accumulation rates and abundant carbon for dating. Especially in the central Andes, additional high-quality proxy records are still needed due to the lack of continuous and well-dated records, which show a significant variability on sub-centennial to decadal precision scales. To widen the current knowledge on climatic and environmental changes in the western Andes of southern Peru, we present a new, high-resolution 8600 year-long record from Cerro Llamoca peatland, a high-altitude Juncaceous cushion peatland in the headwaters of Río Viscas, a tributary to Río Grande de Nasca. A 10.5 m core of peat with intercalated sediment layers was examined for all kinds of microfossils, including fossil charred particles. We chose homogeneous peat sections for pollen analysis at a high temporal resolution. The inorganic geochemistry was analysed in 2 mm resolution using an ITRAX X-ray fluorescence (XRF) core scanner. We interpret the increase of Poaceae pollen in our record as an expansion of Andean grasslands during humid phases. Drier conditions are indicated by a significant decrease of Poaceae pollen and higher abundances of Asteraceae pollen. The results are substantiated by changes in arsenic contents and manganese/iron ratios, which turned out as applicable proxies for in situ palaeo-redox conditions. The mid-Holocene period of 8.6–5.6 ka is characterized by a series of episodic dry spells alternating with spells that are more humid. After a pronounced dry period at 4.6–4.2 ka, conditions generally shifted towards a more humid climate. We stress a humid/relatively stable interval between 1.8–1.2 ka, which coincides with the florescence of the Nasca culture in the Andean foreland. An abrupt turnover to a sustained dry period occurs at 1.2 ka, which coincides with the collapse of the Nasca/Wari society in the Palpa lowlands. Markedly drier conditions prevail until 0.75 ka, providing evidence for the presence of a Medieval Climate Anomaly. Moister but hydrologically highly variable conditions prevailed again after 0.75 ka, which allowed the re-expansion of tussock grasses in the highlands, increased discharge into the Andean foreland and the re-occupation of the settlements in the lowlands during this so-called Late Intermediate Period. On a supraregional scale, our findings can ideally be linked to and proofed by the archaeological chronology of the Nasca-Palpa region as well as other high-resolution marine and terrestrial palaeoenvironmental records. Our findings show that hydrological fluctuations, triggered by the changing intensity of the monsoonal tropical summer rains emerging from the Amazon Basin in the north-east, have controlled the climate in the study area.
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21

Hall, John R. "Storming Zion: Government Raids on Religious Communities. By Stuart A. Wright and Susan J. Palmer." Journal of Church and State, December 19, 2016, csw119. http://dx.doi.org/10.1093/jcs/csw119.

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22

"From the Palmer Raids to the Patriot Act: a history of the fight for free speech in America." Choice Reviews Online 45, no. 07 (March 1, 2008): 45–3963. http://dx.doi.org/10.5860/choice.45-3963.

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23

Silva Neto, Luiz Sinésio, Fabiane Aparecida Canaan Rezende, Daniella Pires Nunes, Erika Da Silva Maciel, Andreia Travassos, and Neila Barbosa Osório. "Associação de força de preensão palmar e osteoporose avaliada por densitometria óssea (DXA) em idosos quilombolas." Acta Fisiátrica 25, no. 4 (December 31, 2018). http://dx.doi.org/10.11606/issn.2317-0190.v25i4a163868.

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Objetivo: Verificar a associação de força de preensão palmar e osteoporose em idosos quilombolas. Método: Trata-se de um estudo seccional com 70 participantes (idade 65,58 ± 6.67 anos) de ambos os sexos. A densidade mineral óssea (DMO), massa muscular (MM) e o percentual de gordura foram analisados pela absortometria de raios-x de dupla energia (DXA) e a força de preensão palmar (FPP) por meio do dinamômetro de mão. O ponto de coorte adotado para identificação de osteoporose foi o da Organização Mundial de Saúde (OMS). A identificação do status da sarcopenia foi realizado para caraterização da amostra e para o diagnóstico foi utilizado os critérios propostos pelo European Working Group on Sarcopenia in Older People (EWGSOP). A FPP foi associada positivamente e significativamente com a DMO. Resultados: A osteopenia foi identificada em 42,8% da amostra e a osteoporose em 20%, sem diferença entre as frequências segundo o sexo (p = 0,161). Conclusão: Nos idosos quilombolas a baixa FPP esteve positivamente associada com baixa DMO. Portanto, sugerindo que a FPP pode ser considerada um fator de risco importante de estado ósseo em idosos quilombolas.
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