Incorporação e remodelação de enxertos homólogos na reconstrução alveolar em humanos: análise tomográfica, histológica e histomorfométrica

Enxertos ósseos homólogos congelados têm sido documentados apresentando bons resultados clínicos como substituto ao material autógeno nas reconstruções alveolares. Entretanto, dados referentes à incorporação e remodelação destes enxertos não estão disponíveis na literatura. Este estudo tem por objetivo determinar um período ótimo de espera para instalação de implantes em rebordos reconstruídos com enxertos ósseos homólogos em bloco no que se refere à incorporação e reabsorção. 24 pacientes foram submetidos à reconstrução alveolar óssea homóloga previamente à instalação de implantes. Os indivíduos foram alocados randomicamente em um de 3 grupos de acordo com o tempo de espera para o segundo estágio cirúrgico (4, 6 e 8 meses). Análises tomográficas, histológicas e histomorfométricas foram utilizadas a fim de determinar o grau de reabsorção e incorporação dos enxertos nos diferentes intervalos de tempo para cada grupo. Os dados de reabsorção sofrida pelos enxertos demonstraram diferenças estatisticamente significativas para os três intervalos de espera. Da mesma forma, parâmetros histomorfométricos como contagem de osteócitos e quantificação de remanescentes de osso homólogo nas biópsias apresentaram diferenças significativas entre os grupos. De acordo com os dados do presente trabalho, no que diz respeito à remodelação e incorporação, o período mais favorável à instalação dos implantes a curto prazo após recontruções com enxertos homólogos é de 4 meses.

增强UV-B辐射对暖温带落叶阔叶林下土庄绣线菊水分生理和氮素利用及形态特性的影响

在中国北方大部分地区，水分始终是影响植物生长和分布的最主要限制性因子之一，植物在其生长期经常遭受水分胁迫。不仅如此，随着大气同温层中臭氧浓度的减少，过量的有害紫外辐射（主要是UV-B，280nm-320nm）将穿透大气层达到地球表面。随着全球变化的加剧，这些地区的植物将不可避免地受UV-B和水分胁迫的共同作用。 本实验是在北京东灵山暖温带森林生态系统中，选择常见灌丛土庄绣线菊(Spiraea pubescens)，建立UV-B控制实验。连续三个生长季每天增补9.4kJ•m-2的辐射剂量，模拟臭氧衰减17%时近地表面UV-B辐射的增强。本实验的目的是观测在野外环境下，长时间人工增强UV-B辐射对土庄绣线菊水分生理、氮素利用以及形态特征的影响。具体对以下指标进行测定：叶片的气孔导度、碳同位素比率（δ13 C）、叶含水量、叶面积、水分利用效率（WUE）、叶全氮含量、叶氮素再吸收率。 实验结果表明，增强UV-B辐射显著减少了土庄绣线菊的叶面积（50.1%），提高了叶片全氮含量(102%)，处理植株的氮素再吸收率比对照植株高出50.9%。同时，UV-B辐射还在一定程度上（尽管统计显示不显著）降低了气孔导度(16.1%)、胞间CO2浓度与大气CO2浓度之比(Ci/Ca) (4.0%)、提高了碳同位素比率（δ13 C）(20.5‰)、叶含水量(3.1%)及比叶重（SLW）(5.2%)，从而导致水分利用效率（WUE）的增加(4.1%)，植物的抗旱能力增强。值得注意的是，深层土壤（30-40cm）含水量变化会影响气孔导度、δ13 C、WUE对紫外辐射的响应程度：在土壤干旱的季节（6月和9月），气孔导度、δ13 C、WUE这些指标处理和对照的差异很小，但是当土壤水分充足时（7月和8月），处理和对照的差异就较为显著。另外，随着实验处理时间的延长UV-B的效应变得不显著。相关分析表明，UV-B辐射降低了土壤含水量（30-40cm）与土庄绣线菊叶含水量、δ13 C、Ci/Ca、气孔导度的相关系数，增强了WUE与土壤含水量的相关性，这也许是由于UV-B辐射增强了WUE对土壤水分变化的敏感性。本研究的结果表明UV-B辐射对土庄绣线菊的形态和生长有显著的影响，但对主要水分生理指标影响不显著。

A bone remodelling model coupling micro-damage growth and repair by 3D BMU-activity.

Bone as most of living tissues is able, during its entire lifetime, to adapt its internal microstructure and subsequently its associated mechanical properties to its specific mechanical and physiological environment in a process commonly known as bone remodelling. Bone is therefore continuously renewed and micro-damage, accumulated by fatigue or creep, is removed minimizing the risk of fracture. Nevertheless, bone is not always able to repair itself completely. Actually, if bone repairing function is slower than micro-damage accumulation, a type of bone fracture, usually known as "stress fracture", can finally evolve. In this paper, we propose a bone remodelling continuous model able to simulate micro-damage growth and repair in a coupled way and able therefore to predict the occurrence of "stress fractures". The biological bone remodelling process is modelled in terms of equations that describe the activity of basic multicellular units. The predicted results show a good correspondence with experimental and clinical data. For example, in disuse, bone porosity increases until an equilibrium situation is achieved. In overloading, bone porosity decreases unless the damage rate is so high that causes resorption or "stress fracture".

Use of skeletochronological analysis to estimate the age of leatherback sea turtles Dermochelys coriacea in the western North Atlantic

Although growth rate and age data are essential for leatherback management, estimates of these demographic parameters remain speculative due to the cryptic life history of this endangered species. Skeletochronological analysis of scleral ossicles obtained from 8 captive, known-age and 33 wild leatherbacks originating from the western North Atlantic was conducted to characterize the ossicles and the growth marks within them. Ages were accurately estimated for the known-age turtles, and their growth mark attributes were used to calibrate growth mark counts for the ossicles from wild specimens. Due to growth mark compaction and resorption, the number of marks visible at ossicle section tips was consistently and significantly greater than the number visible along the lateral edges, demonstrating that growth mark counts should be performed at the tips so that age is not underestimated. A correction factor protocol that incorporated the trajectory of early growth increments was used to estimate the number of missing marks in those ossicles exhibiting resorption, which was then added to the number of observed marks to obtain an age estimate for each turtle. A generalized smoothing spline model, von Bertalanffy growth curve, and size-at-age function were used to obtain estimates of age at maturity for leatherbacks in the western North Atlantic. Results of these analyses suggest that median age at maturation for leatherbacks in this part of the world may range from 24.5 to 29 yr. These age estimates are much greater than those proposed in previous studies and have significant implications for population management and recovery.

北京东灵山地区森林植物养分利用效率研究

本文选择东灵山地区具有代表性的11种植物，研究了植物叶片养分元素动态特征以及各个层次物种、生活型和生境等对植物叶片养分元素再吸收的影响。主要结论如下： 1、不同物种间、以及相同物种在不同森林类型内的叶片C素含量变化程度较小;11个物种之间叶片N素养分浓度差很大，但各种植物叶片的N素含量的季节变化比较一致，大多数情况下表现为单峰型或双峰变化曲线;各种森林类型中11种植物叶片P的最高含量都出现在生长初期，以后开始下降。 2、在物种水平、养分再吸收是一种重要的养分保存机制，N素和P素再吸收率大约为50%，对这两种养分元素而言，相同生境下生长的不同植物种的养分再吸收率不同，存在显著差异，而同一植物种不同生境下养分再吸收率之间也存在差异，而S素的差异则不显著。 3、同一生活型在不同的森林类型中养分再吸收率差异不明显，同一森林类型中不同生活型的养分再吸收率差异也不明显;高养分再吸收率不是低养分环境所选择的优势性状，低养分环境中的物种主要通过延长叶片寿命和加强低养分浓度状况下的物质合成来适应低养分环境。 4、除了土壤pH值外，土壤容重、土壤有机质、土壤全氮、土壤阳离子交换量在三种生境下都表现出一定的差异性。华北落叶松林生境下的土壤养分含量较丰富，其次是落叶阔叶混交林，辽东栎林相对前二种生境其土壤养分相对低一些，但在三种生境之间养分元素再吸收率差异不显著，植物养分再吸收没有或微弱地受控于土壤养分获得的能力。

农牧交错区主要植物的氮素利用效率

Berendse&Aerts (1987)认为氮素利用效率(nitrogen use efficiency，NUE)可以分为两部分的乘积，即：①氮素生产力(nitrogen productivity，NP)，②氮素的平均滞留时间(mean residencetime，MRT)。本文利用这一概念对处于我国北方农牧交错带的内蒙古自治区多伦县典型植物的氮素利用策略进行了研究。研究假设：植物在贫瘠生境上所采取的氮素适应策略主要是提高对所吸收氮素的保持能力(较长的MRT)，而不是提高NUE。 在不同土壤生境上，属于不同生活型的不同物种其NP和MRT之间存在负相关关系。在不同生境、生活型和物种之间，作为NP与MRT乘积的NUE比NP、MRT的变化相对要小，结果表明植物主要通过延长MRT来适应氮素贫瘠的生境。因为NP与MRT相反的方向变化，二者不能同时增加或减少，所以NP与MRT之间存在相互协调(trade-off)的关系。 在群落和生态系统水平上，NP与MRT之间也存在相互协调关系，不同水平上的NUE之间也存在一定的联系。除了在种间存在这种关系外，通过对多伦县和十三里滩两种针茅（大针茅、克氏针茅）的氮素利用特征的研究，发现在种内，NP与MRT之间也存在这种相互协调关系。NUE与土壤供氮能力有关，随着土壤供氮能力的下降，NUE呈上升趋势。植物的NUE不仅与土壤的供氮能力有关，其它因素如土壤水分供应状况也会对植物的NUE产生影响，例如，与生长在河岸上的植物相比，生长在河滩湿地上的植物具有较高的NP，但MRT却较低。在群落中，不同植物个体的NUE及其组成参数NP和MRT也存在较大的差异，较大的植株具有较高的NP和MRT，因而NUE也高于个体较小的植株。本文研究结果表明，植物的NUE与氮素回收转移特性密切相关，植物提高氮素回收效率(nitrogen resorption efficiency，NRE)可以延长MRT，从而提高NUE。

典型草原优势植物养分回收特性对养分和水分梯度变化的响应

养分回收是植物衰老时，养分从衰老组织向活的组织体转移的一种过程。该过程延长了养分在植物体内的滞留时间，提高了植物保持养分的能力，因此是植物适应养分贫瘠生境的策略之一。全球气候变化，包括降水格局改变和氮（N）沉降增加，改变了生态系统正常的生物地球化学循环，因此可能会对植物的养分回收特性产生影响。研究不同N、磷（P）、水梯度上，植物物种养分回收特性的响应格局，对于预测N沉降增加和降水格局改变对物种养分利用策略的潜在影响，具有一定的理论与实践意义。本研究以中国科学院植物研究所多伦恢复生态学实验站长期施N肥实验（0，1，2，4，8，16，32，64 g N m-2 yr-1等8个水平）为研究平台研究了克氏针茅（Stipa krylovii）群落中优势植物养分回收随N素添加梯度的变化，同时结合三个盆栽控制实验（施N肥实验：0，0.5，1，2，4，8，16，32，64，128 g N m-2等10个水平;施P肥实验：梯度同施N肥实验;控水实验：3600，4000，4500，5143，6000，7200，9000，12000，18000，36000 mL pot-1等10个水平），主要探讨了羊草（Leymus chinensis）养分回收效率（从衰老组织中回收转移的养分百分数，RE）和养分回收度（以枯叶中养分浓度衡量，RP）以及其它叶片养分特性(绿叶养分浓度和比叶面积SLA)对环境因子改变的响应格局。同时，我们还调查了枯叶C:N比和C:P比等参数，研究环境因子改变对凋落物分解的影响。 1）连续4年施N肥显著降低了五个物种叶片N素回收度（NRP），对P素回收度（PRP）的影响在各物种间差异较大，但低N提高了多数物种的PRP;物种间，冷蒿（Artemisia frigida）RP（枯叶N和P浓度分别为14.3±2.0 mg g-1和0.68±0.09 mg g-1）最低，砂韭（Allium bidentatum）（N：5.2±0.2 mg g-1，P：0.12±0.01 mg g-1）最高。沿施N梯度，N素回收效率（NRE）的变化趋势在物种间差异较小但在方法间（叶干重水平，叶面积水平和单株水平）差异较大，而P素回收效率（PRE）的变化在物种间和方法间差别都较大。叶干重水平和叶面积水平上，NRE在四个物种中表现出显著降低的趋势，PRE只在糙隐子草（Cleistogenes squarrosa）和星毛委陵菜（Potentilla acaulis）中显著降低，其它三个物种变化不显著。单株水平上，所有物种NRE（除了克氏针茅）和PRE均与施N量梯度无显著性关系。物种间，砂韭的RE最高（＞80.0%），冷蒿和星毛委陵菜最低（＜60.0%）。方法间，叶片水平上的RE均高于单株水平上。沿施N肥梯度，两个禾本科物种SLA无显著变化规律，而其它三个物种SLA表现出先增加后变化不大的趋势。物种间，最高和最低的SLA分别表现在冷蒿和克氏针茅。沿施N肥梯度，五个物种C:N比呈先显著降低后缓慢降低的趋势。物种间，最大和最小的C:N比分别出现在砂韭和冷蒿。 2）盆栽施N肥实验中，一定范围内，施N肥显著提高了羊草地上地下生物量、SLA和绿叶N浓度，显著降低了C:N比、NRP、NRE和PRE，但对绿叶P浓度、叶片PRP和C:P比无明显影响。平均枯叶N浓度和枯叶P浓度分别为16.2 mg g-1和1.01 mg g-1，平均NRE和PRE分别为46.1﹪和58.1﹪。10月时，地下生物量和养分积累均高于地上部分。 3）盆栽施P肥实验中，一定范围内，施P肥显著地提高了羊草地上地下生物量、SLA、绿叶N浓度和绿叶P浓度，显著降低了C:N比、C:P比、NRP、PRP和PRE，但对NRE无显著影响。平均枯叶N浓度和枯叶P浓度分别为9.9 mg g-1和7.43 mg g-1，平均NRE和PRE分别为58.2﹪，平均PRE为56.1﹪。10月时地下部分生物量和N库积累均高于地上部分，而P库在两个部分间差别不大。 4）盆栽控水实验中，一定范围内，供水量增加显著增加了羊草地上地下生物量、SLA、NRP、PRP、PRE、C:N比和C:P比，显著降低了绿叶N浓度，但对绿叶P浓度和NRE无显著性影响。平均枯叶N浓度和枯叶P浓度分别为10.4 mg g-1和0.32 mg g-1，平均NRE和PRE分别为54.4﹪和76.8﹪。10月时，地下部分生物量和养分积累均高于地上部分。 以上结果表明，N、P和水分因子的改变影响了植物生物量和养分分配、叶片养分特性、养分回收能力以及枯叶分解质量等，且不同梯度影响程度也不同。因此，未来全球变化包括N沉降增加和降水格局改变可能影响植物养分利用策略和凋落物分解特性，进而可能对植被-土壤系统养分循环产生影响。

Mechanobiology of bone remodelling

Bone as most of living tissues is able, during its entire lifetime, to adapt its internal microstructure and subsequently its associated mechanical properties to the specific mechanical and physiological environment in a process commonly known as bone remodelling. Bone is therefore continuously renewed and microdamage removed minimizing the risk of fracture. Bone remodelling is controlled by mechanical and metabolical stimuli. In this paper, we introduce a new model of bone remodelling that takes into account both types of influences. The predicted results show a good correspondence with experimental and clinical data. For example, in disuse, bone porosity increases until an equilibrium situation, while, in overloading, decreases unless the damage rate is so high that causes resorption and "stress fracture". This model has been employed to predict bone adaptation in the proximal femur after total hip replacement proving its consistence and good correspondence with well-known clinical experiences.

章古台沙地人工林树木养分再吸收与利用效率

以科尔沁沙地章古台地区人工林树种樟子松（Pinus svlvestris var．mongolica）、油松（Ptabulaeformis）、赤松（Pdensora）和彰武小钻杨（Populusxiaozhuanica）以及11、20、29、45四个年龄樟子松树木为材料，从植物N、P、K、Ca、Mg养分方面探讨了树木对贫痔生境的适应能力。结果表明：针叶树樟子松、赤松、油松叶片N、P、K含量的季节特征相似。叶片N含量各季节变化较小，而叶片P、K含量在2003年总体表现出逐渐增加的趋势。四个年龄樟子松叶片的养分含量季节特征相似。樟子松叶片的平均N和P含量显著（P＜0.05）高于赤松，油松最低，而三者N：P比和K含量无显著差别。彰武小钻杨叶片的N、P、K含量显著高于针叶树。樟子松叶片N、P、K的再吸收效率与能力及利用效率均低于油松和赤松，而Mg的再吸收效率与能力及利用效率均高于两种树种。反映了樟子松对N、P、K养分的保存·利用和减少损失量的能力均低于油松和赤松，而对Mg的保存和利用能力则强于两种树种。结合叶片凋落造成的年养分损失量大小差异，对N、P、K供应不足生境的适应能力大小为：油松＞赤松＞樟子松。针叶树N、P、K、ca、Mg的再吸收能力和利用效率都显著高于落叶树彰武小钻杨，反映出针叶树更能适应贫瘠环境的特点。随着樟子松年龄的增加，叶片的N、P、K、Mg再吸收效率和能力都表现出了下降的趋势，反映了樟子松对贫瘩生境的适应能力随着年龄的增加而下降。同时，随着年龄的增加樟子松叶片单位N、P、K、Mg养分的生产力水平下降，表现了在养分利用上的衰退特征。对树木叶片N:P比、养分再吸收效率与能力及利用效率进行分析和比较，表明研究区最限制树木生长的养分可能为N，P的限制作用还不突出。人为干扰造成大量N、P、K养分从森林生态系统中损失。树木叶片N的年再吸收量与总的N年损失量相当，反映了在剧烈人为干扰条件下，养分再吸收对于树木的生长和生存具有更加重要的作用。

Quasi-3D Cytoskeletal Dynamics of Osteocytes under Fluid Flow

Osteocytes respond to dynamic fluid shear loading by activating various biochemical pathways, mediating a dynamic process of bone formation and resorption. Whole-cell deformation and regional deformation of the cytoskeleton may be able to directly regulate this process. Attempts to image cellular deformation by conventional microscopy techniques have been hindered by low temporal or spatial resolution. In this study, we developed a quasi-three-dimensional microscopy technique that enabled us to simultaneously visualize an osteocyte's traditional bottom-view profile and a side-view profile at high temporal resolution. Quantitative analysis of the plasma membrane and either the intracellular actin or microtubule (MT) cytoskeletal networks provided characterization of their deformations over time. Although no volumetric dilatation of the whole cell was observed under flow, both the actin and MT networks experienced primarily tensile strains in all measured strain components. Regional heterogeneity in the strain field of normal strains was observed in the actin networks, especially in the leading edge to flow, but not in the MT networks. In contrast, side-view shear strains exhibited similar subcellular distribution patterns in both networks. Disruption of MT networks caused actin normal strains to decrease, whereas actin disruption had little effect on the MT network strains, highlighting the networks' mechanical interactions in osteocytes.

新增生岩石圈与软流圈的相互作用：来自地幔橄榄岩捕虏体的证据

The petrology and geochemistry of peridotites entrained in Beiyan Cenozoic alkaline basalts within the middle segment of Tan-Lu fault zone and clinopyroxene megacrysts in the late Mesozoic and Cenozoic alkaline basaltic rocks from the North China Craton, have been systematically investigated. The main conclusions are obtained as follows. The peridotites entrained in alkaline basalts at Beiyan, Shandong Province, China are comprised of dominantly spinel lherzolites and spinel wehrlites with porphyroclastic, granuloblastic textures to resorption textures. The xenoliths are fertile in major element compositions (High CaO, TiO2, Low MgO, Cr2O3). The olivine Fo (= 100×Mg / (Mg+Fe) possesses a low and very large range of 81.0 to 91.0. The peridotites contain high percentages (Lherzolites: 10 - 19% in volume; Wehrlites: 24 - 28% in volume) of clinopyroxene with spongy textures. The Sr and Nd isotopic ratios of clinopyroxene separates from peridotites and pyroxenite xenoliths have a depleted and small range fall within the area of MORB, similar to newly-accreted lithospheric mantle. However, the appearance of many wehrlites and highly enriched LREE pattern suggest that this newly-accreted lithospheric mantle was considerably modified and reconstructed recently through the peridotite-asthenospheric melt interaction. The upwelling of asthenosphere from late Cretaceous to Eogene and upper mantle shearing of the Tan-Lu fault played an important role in the modification and reconstruction of the newly-accreted lithospheric mantle. The clinopyroxene megacrysts in the late Mesozoic and Cenozoic alkaline basaltic rocks from the eatern North China Craton are different in aspects of major elements, trace elements and isotopic composition. The characteristics of texture, mineral compositions and geochemistry as well as the Fe-Mg partitioning between the crystal and the melt indicates that the Al-augites in the Cenozoic basalts represent high-pressure crystallization products of alkaline basaltic melts. Thus, both of clinopyroxene megacrysts and host basalts could be derived from a same primitive magma. However, the Al-augites in the late Mesozoic basaltic rocks represent accidentally-included xenocrysts of basaltic components which had crystallized in the depth from a previously melting episode. The more depleted Sr-Nd isotopic compositions of Cenozoic megacrysts compared with those of host alkaline basalts and tholeiites demonstrate that even the alkali basalts could not completely represent primitive magma initiating in asthenosphere. That is to say, the Cenozoic alkaline basalts were more or less modified by some enriched Sr-Nd isotopic components during their eruption. Meanwhile, the tholeiites were not the products formed only by fractional crystallization of alkaline basaltic magma or different degrees of partial melting. It may result from the contribution of lithospheric mantle materials or crust contamination in magma chamber to alkali basaltic magmas.

Elevação do seio maxilar versus colocação de implantes curtos

Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Medicina Dentária

A osteonecrose associada ao uso de bisfosfonatos

Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Medicina Dentária

Elevação do seio maxilar versus implantes zigomáticos

Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Medicina Dentária

A importância clínica da vitamina D

Projeto de Pós-Graduação/Dissertação apresentado à Universidade Fernando Pessoa como parte dos requisitos para obtenção do grau de Mestre em Ciências Farmacêuticas