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Background contextThe ideal tissue-engineered solution for any bone graft substitute is to assist in the rapid formation of bone and facilitate fusion.PurposeThe present study aims to evaluate this E-BMP-2 (Escherichia coli–derived human bone morphogenetic protein-2) in ovine posterolateral lumbar fusion (PLF) to examine the influence of dose and overall performance in a model with similar graft size and diffusive challenges to the human.Study design/settingIn vivo large animal model study.MethodsAn adult ovine PLF was performed in 30 animals with groups of E-BMP-2 with a beta-tricalcium phosphate (β-TCP) carrier at three different dosages, β-TCP alone, and autograft from the iliac crest. The fusions were assessed by radiography (X-ray and microcomputed tomography), mechanical testing, and hard-tissue histology with bone labels at 6, 8, and 10 weeks along with routine paraffin histology at 12 weeks.ResultsResults showed increasing new bone and fusion rate with E-BMP-2 dose, whereas β-TCP alone was largely resorbed and did not achieve fusion in this model at 12 weeks. Autograft showed similar grading for the amount of bone between the transverse processes but a lower fusion rate than β-TCP/E-BMP-2 groups. Bone labels revealed new bone formation at all time points for the E-BMP2 groups, whereas the autograft group showed active bone formation at 10 weeks. Beta-tricalcium phosphate displayed reliable incorporation into the decorticated host bone, whereas limited new bone was found between the transverse processes. At the center of the fusion mass, increased E-BMP-2 dose led to increased incorporation of β-TCP by new bone.ConclusionsThese results suggest that E-BMP-2 was capable of producing posterolateral fusion in the ovine model that is equal to or superior to autologous graft in terms of fusion rate and mechanical strength. E-BMP-2 dose had considerable influence on β-TCP granule resorption.  相似文献   
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Background  

Wound infections are a common complication of surgery that add significantly to the morbidity of patients and costs of treatment. The global trend towards reducing length of hospital stay post-surgery and the increase in day case surgery means that surgical site infections (SSI) will increasingly occur after hospital discharge. Surveillance of SSIs is important because rates of SSI are viewed as a measure of hospital performance, however accurate detection of SSIs post-hospital discharge is not straightforward.  相似文献   
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Antimicrobial susceptibility was analyzed for 354 typhoidal Salmonella isolates collected during 1999–2012 in the Netherlands. In 16.1% of all isolates and in 23.8% of all isolates that showed increased MICs for ciprofloxacin, the MIC for azithromycin was increased. This resistance may complicate empirical treatment of enteric fever.  相似文献   
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Recent findings point to plant root traits as potentially important for shaping the boundaries of biomes and for maintaining the plant communities within. We examined two hypotheses: 1) Thin-rooted plant strategies might be favored in biomes with low soil resources; and 2) these strategies may act, along with fire, to maintain the sharp boundary between the Fynbos and Afrotemperate Forest biomes in South Africa. These biomes differ in biodiversity, plant traits, and physiognomy, yet exist as alternative stable states on the same geological substrate and in the same climate conditions. We conducted a 4-y field experiment to examine the ability of Forest species to invade the Fynbos as a function of growth-limiting nutrients and belowground plant–plant competition. Our results support both hypotheses: First, we found marked biome differences in root traits, with Fynbos species exhibiting the thinnest roots reported from any biome worldwide. Second, our field manipulation demonstrated that intense belowground competition inhibits the ability of Forest species to invade Fynbos. Nitrogen was unexpectedly the resource that determined competitive outcome, despite the long-standing expectation that Fynbos is severely phosphorus constrained. These findings identify a trait-by-resource feedback mechanism, in which most species possess adaptive traits that modify soil resources in favor of their own survival while deterring invading species. Our findings challenge the long-held notion that biome boundaries depend primarily on external abiotic constraints and, instead, identify an internal biotic mechanism—a selective feedback among traits, plant–plant competition, and ecosystem conditions—that, along with contrasting fire regime, can act to maintain biome boundaries.

Recent findings (1) have demonstrated striking differences in plant rooting strategies across biomes worldwide, spawning the hypothesis that belowground competition for soil resources may be critical for maintaining biome boundaries (1, 2). This idea differs fundamentally from the historical notion that biomes primarily are delineated by extrinsic abiotic factors such as climate, geological parent material, or topography (38), or the more recent recognition that aboveground plant adaptations can promote fire-determined plant communities (9, 10).Belowground competition introduces a biotic mechanism that is intrinsic to the plant community, emerges from plant–plant contest for resources, and may help explain the puzzling observation that biome boundaries can persist independent of climate–geological factors (4, 10).Of central importance is Ma et al.’s (1) recent observation that root traits that are associated with resource uptake appear to differ across biomes with differing soil resource dynamics. Specifically, Ma et al. hypothesized that thin-rooted plant strategies may be favored in biomes with permanently or seasonally low soil resources. They reasoned that, in those conditions, natural selection would favor absorptive roots [i.e., first-order roots (1, 11)] with low diameter and high specific root length (i.e., root length per unit photosynthetic carbon invested), which, in turn, are traits that allow high root surface area and efficient exploration of resource-poor soils. Conversely, thick roots and low specific root length may remain competitive traits in biomes with abundant soil resources, despite reduced root surface area and less efficient soil exploration.Here we test Ma et al.’s hypothesis (1) using a unique study of root traits and plant–plant resource competition across the boundary of two distinct biomes within the Cape Floristic Region of South Africa: Fynbos and Afrotemperate Forest. We show in Fig. 1 and 12, 13), by slow decomposition and nutrient recycling (14), and by low stores of soil organic matter (15). In contrast, the Afrotemperate Forest biome is defined by a substantial accumulation of soil organic matter and organic-bound nutrients, which, in turn, supports high rates of plant–soil–nutrient recycling. Based on Ma et al.’s hypothesis, we would expect that these sharp differences in soil resource conditions would result in divergent belowground root traits across the biome boundary.Open in a separate windowFig. 1.Sharp differences in biodiversity, aboveground plant traits, and ecosystem properties across the South African Fynbos–Forest boundary. (A) Two neighboring biomes of the Cape Floristic Region—the Fynbos (62) and the Afrotemperate Forest (63)—form a sharp boundary despite perching on the same geological parent material (39). (B) Biodiversity: The hyperdiverse Fynbos harbors >7,000 plant species, of which the majority are endemic to South Africa (64). The Afrotemperate Forest, on the other hand, contains >450 species with less endemism (63). (C) Aboveground plant traits: Fynbos species generally possess thick and small leaves with a high carbon-to-nitrogen (C:N) ratio while Afrotemperate Forest species display thinner and larger leaves with a lower C:N ratio. In addition, Fynbos plant species possess traits that either enhance (e.g., waxes) or resist (e.g., thick bark) fire. For example, Fynbos vegetation contains high concentrations of flammable organic compounds (e.g., crude fat content) that can facilitate very hot fires (65). In contrast, Afrotemperate Forest species tend to be sensitive to fire and possess traits that suppress fire (e.g., high water content). (D) Ecosystem properties: Fynbos soils are exceedingly poor in soil carbon, nitrogen, and phosphorus contents. In contrast, the Afrotemperate Forest soil is characterized by a developed layer rich in carbon, nitrogen, and phosphorus, which facilitates active cycling of nutrients between plant and soil pools (66, 67).Table 1.Comparison of neighboring Fynbos and Afrotemperate Forest
Properties and traitsFynbosAfrotemperate Forest
Ecosystem properties
 Fire return interval, y12∼20*n.a.
 Soil carbon, mg/g23.5(5, 4.9), 9.2(1.4)49.3(5, 4.4)
 Soil nitrogen, mg/g1.07(5, 0.29), 0.15(0.01), 1.3(0.6)§3.24(5, 0.26), 3.9(0.8)§
 Soil phosphorus, mg/kg6.8(5, 2.8), 4.8(0.9)§28.4(5, 2.5), 22.5(8.6)§
 Litter decomposition rate, y−10.07, 0.05#0.24
 Litter half-life time, y10, 14#2.9
 Canopy cover, %20(360, 0.76)**81(9, 0.03)**
Aboveground plant traits
 Maximal height, m0.84(309, 0.05)**17(26, 0.92)**
 Leaf thickness, mm0.44(309, 0.15)**0.19(143, 0.005)**
 Leaf size, cm27.5(309, 1.7)**20.4(143, 1.7)**
 Specific leaf area, cm2/g60(309, 2.2)**105(143, 8.1)**
 Amax, μmol CO2⋅m−2⋅s−118(16–20)††8.6(7.5–9.8)††
 Crude fat content, %4.3–6.7‡‡2.6–4.0‡‡
 Fuel moisture content, %86–15‡‡139–229‡‡
 C:N ratio66,§§ 95§§18¶¶
 Bark thickness, mm7.2##∼3∥∥
Open in a separate windowThough sharing similar climatic and geological conditions, the Fynbos and Afrotemperate Forest biomes differ in their ecosystem properties and plant traits. Values in parentheses identify the sample size and SE from our study.  n.a., not applicable.*Estimate from ref. 68Soil total carbon, total nitrogen, and available phosphorus were derived from five pairs of Forest–Fynbos sites immediately neighboring each other at the Orange Kloof site in the Table Mountain National Park of Cape Town (Materials and Methods).Zero- to 10-cm soil of sandplain lowland Fynbos of Cape Province (69).§Direct comparison of neighboring Forest and Fynbos across four sites in Swartboskloof (42).Based on a 3-y field incubation study using the common species Leucospermum parile (70).#Based on a 2.5-y field incubation study using the common species P. repens (71).Based on the evergreen tree Pterocelastrus tricuspidatus (50).**Plant traits compiled by our group.††Mean (95% CI) digitizer from figure 1a of ref. 72 and rounded to double significant digits. Five Forest species (D. whyteana, K. africana, Olea capensis, Olea europaea, and Rapanea melanophloeos) and four Fynbos species (Berzelia lanuginosa, Erica versicolor, Phylica ericoides, and Searsia lucida) were used.‡‡Crude oil includes oils, fats, waxes, and terpenes that are extracted using the Soxhlet extraction approach (65). For both crude fat content and fuel moisture content, we derived the Fynbos value from the simple mean of the dominant Fynbos species (P. neriifolia, Cliffortia cuneata, B. nodiflora, and Erica plukenetii) and derived the Forest values from six Forest species (C. capensis, Ilex mitis, K. africana, Maytenus oleoides, Brachylaena neriifolia, and Brabejum stellatifolium) (65).§§The first value is derived from table 3 of ref. 73 using the simple mean of four Fynbos elements (proteoid, ericoid, restioid, and other sclerophylls) across coastal and mountain habitats. The second value is the average C:N ratio of the dominant canopy proteoid species.¶¶The simple mean leaf nitrogen concentration of 107 Afrotemperate Forest species across South Africa from ref. 74 is first calculated (25.95 mg/g). Assuming the average carbon concentration is equal to the global average leaf carbon content [476 mg/g (75)], the average C:N ratio is derived.##Bark thickness data of Fynbos species standardized at 5-cm trunk diameter are from woody Protea species that are resistant to fire (76). Restioids, ericoids, grass growth forms, and non–fire-resistant Protea species are pyrophilic. (Forest bark thickness data of Afromontane Forest from Knysna area are from unpublished data.)We further hypothesize that these differences in root traits, when combined with plant–plant competition for belowground resources, may offer a mechanism that acts to reinforce the boundary between the Fynbos and Afrotemperate Forest biomes. Central to such a mechanism is the emergence of a trait-by-resource feedback (2, 16), in which a plant species possesses traits that can impact the local conditions and recycling of soil resources. A biotic feedback can emerge if, in turn, the resulting resource regime acts to promote the resident plant species and/or to prohibit the invasion by nonresident species. In this way, a trait-by-resource feedback can in theory (16) maintain a biome boundary independent of differences in geological parent material or climate factors.An important (but not sufficient) part of this trait-by-resource feedback is that plant root traits must be systematically coupled to plant characteristics that can influence resource dynamics at the ecosystem scale. A notable example is the Fynbos biome (Fig. 1), in which plant species possess traits that promote fires at return times of ∼10 to 40+ y (17, 18). These fires, in turn, are hot enough to induce severely nutrient-poor soil conditions by volatilizing soil and plant organic nitrogen (19, 20) and by increasing the likelihood that phosphorus can leach from the soil profile following rain events (21). However, the feedback can only function if aboveground fire-adapted traits are systematically coupled with belowground traits that allow Fynbos plant species to outcompete any invading plants from the nearby Afrotemperate Forest. Conversely, the Afrotemperate Forest plant community depends on conditions that favor the significant accumulation of an organic soil nutrient pool (Fig. 1), which, in turn, can facilitate the active cycling of nitrogen and phosphorus between the plant and soil components of the ecosystem.We experimentally tested the belowground component of this Fynbos trait-by-resource feedback idea, using a 4-y field experiment in which we manipulated 1) the supply of the potentially growth-limiting resources nitrogen and phosphorus, and 2) the ability of plants to compete for nitrogen and phosphorus belowground. Specifically, we asked whether Afrotemperate Forest tree species could successfully invade the Fynbos plant community, across differing conditions of soil resources and belowground competition. In the field, we established a full factorial manipulation of nitrogen and phosphorus across 40 plots in two separate locations within the native Fynbos plant community (Materials and Methods and SI Appendix, Fig. S2). We transplanted forest tree seedlings into all experimental plots and evaluated their ability to grow across the different soil nutrient and competition scenarios (SI Appendix, Fig. S3).Overall, our project was designed to evaluate whether Fynbos plants possess root traits that are consistent with a high capacity to compete for scarce nutrients and, in turn, whether these traits translate into the ability to outcompete plant species that seek to invade the Fynbos plant community—as predicted by the trait-by-resource feedback mechanism.  相似文献   
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