Genetic and biochemical analysis of an endonuclease encoded by the IncN plasmid pKM101.

The IncN plasmid pKM101 nuc gene encodes a periplasmically localized endonuclease. DNA sequence analysis indicates that this gene encodes a hydrophilic protein of about 19.5 kDa containing a hydrophobic signal sequence. nuc is homologous to a partially sequenced open reading frame adjacent to the sog gene of the plasmid CollB-P9, a plasmid known to encode an endonuclease similar to that of pKM101. A partially sequenced tra gene directly upstream of nuc is homologous to the virB11 gene of Agrobacterium tumefaciens. We have partially purified the pKM101 nuclease by osmotic shock and cation exchange chromatography, and used this enzyme preparation to sequence the protein's amino terminus. The first 13 amino acids of the mature protein match amino acids 23 to 35 of the predicted sequence, indicating that the protein is proteolytically processed to a molecular mass of approximately 17 kDa, probably during export to the periplasmic space. The enzyme was able to attack many sites along an end labelled duplex DNA substrate, but showed clearly preferred cleavage sites, and may cleave preferentially at purine-rich regions.     

The effectiveness of different planting frameworks for recruitment of tropical rainforest species on ex‐rainforest land

A long‐term rainforest restoration experiment was established on abandoned pasture in northeastern Queensland in 1993 to examine the effectiveness of five different restoration planting methods: (T1) control (no plantings); (T2) pioneer monoculture (planting seedlings of one pioneer species, Homalanthus novoguineensis, Euphorbiaceae); (T3) Homalanthus group framework method (H. novoguineensis and eight other pioneer species); (T4) Alphitonia group framework method (Alphitonia petriei, Rhamnaceae, with eight other pioneer species); and (T5) maximum diversity method (planting pioneers, middle‐phase species, and mature‐phase species). We investigated temporal patterns in the (1) fate of seedlings originally planted in 1993; (2) natural recruitment of native plant species; and (3) current habitat structure (canopy cover and ground cover of grasses and invasive plants) within each restoration treatment. A total of 97% of seedlings planted in T2 died within the first 13 years and all had died by 2014. A total of 72% of seedlings planted in T3, 55.5% of seedlings planted in T4, and 55% of seedlings planted in T5 also died by 2014. By 2014, 42 species from 21 families had recruited across the experimental site, and the abundance of recruits was almost twice that recorded in 2001 and 2006. Overall, T3, T4, and T5 had the greatest diversity and abundance of recruits. By 2014, canopy cover was greatest in T3, T4, and T5 but grass cover was least in T5. It is concluded that some restoration success measures increase with planting diversity, but overall the rate of recovery is similar in framework species and maximum diversity method.     

HSP70.1 and -70.3 are required for late-phase protection induced by ischemic preconditioning of mouse hearts

We investigated the role of inducible heat shock proteins 70.1 and 70.3 (HSP70.1 and HSP70.3, respectively) in myocardial ischemic preconditioning (IP) in mice. Wild-type (WT) mice and HSP70.1- and HSP70.3-null [HSP70.1/3(-/-)] mice were subjected to IP and examined 24 h later during the late phase of protection. IP significantly increased steady-state levels of HSP70.1 and HSP70.3 mRNA and expression of inducible HSP70 protein in WT myocardium. To assess protection against tissue injury, mice were subjected to 30 min of regional ischemia and 3 h of reperfusion. In WT mice, IP reduced infarct size by 43% compared with sham IP-treated mice. In contrast, IP did not reduce infarct size in HSP70.1/3(-/-) mice. Absence of inducible HSP70.1 and HSP70.3 had no effect, however, on classical or early-phase protection produced by IP, which significantly reduced infarct size in HSP70.1/3(-/-) mice. We conclude that inducible HSP70.1 and HSP70.3 are required for late-phase protection against infarction following IP in mice.     

Somatic hybrids between Solanum bulbocastanum and potato: a new source of resistance to late blight

 Solanum bulbocastanum, a wild, diploid (2n=2x=24) Mexican species, is highly resistant to Phytophthora infestans, the fungus that causes late blight of potato. However this 1 EBN species is virtually impossible to cross directly with potato. PEG-mediated fusion of leaf cells of S. bulbocastanum PI 245310 and the tetraploid potato line S. tuberosum PI 203900 (2n=4x=48) yielded hexaploid (2n= 6x=72) somatic hybrids that retained the high resistance of the S. bulbocastanum parent. RFLP and RAPD analyses confirmed the hybridity of the materials. Four of the somatic hybrids were crossed with potato cultivars Katahdin or Atlantic. The BC₁ progeny segregated for resistance to the US8 genotype (A-2 mating type) of P. Infestans. Resistant BC₁ lines crossed with susceptible cultivars again yielded populations that segregated for resistance to the fungus. In a 1996 field-plot in Wisconsin, to which no fungicide was applied, two of the BC₁ lines, from two different somatic hybrids, yielded 1.36 and 1.32 kg/plant under a severe late-blight epidemic. In contrast, under these same conditions the cultivar Russet Burbank yielded only 0.86 kg/plant. These results indicate that effective resistance to the late-blight fungus in a sexually incompatible Solanum species can be transferred into potato breeding lines by somatic hybridization and that this resistance can then be further transmitted into potato breeding lines by sexual crossing. Received: 27 October 1997 / Accepted: 11 November 1997     

Methane‐derived carbon flow through microbial communities in arctic lake sediments

Aerobic methane (CH₄) oxidation mitigates CH₄ release and is a significant pathway for carbon and energy flow into aquatic food webs. Arctic lakes are responsible for an increasing proportion of global CH₄ emissions, but CH₄ assimilation into the aquatic food web in arctic lakes is poorly understood. Using stable isotope probing (SIP) based on phospholipid fatty acids (PLFA‐SIP) and DNA (DNA‐SIP), we tracked carbon flow quantitatively from CH₄ into sediment microorganisms from an arctic lake with an active CH₄ seepage. When 0.025 mmol CH₄ g^?1 wet sediment was oxidized, approximately 15.8–32.8% of the CH₄‐derived carbon had been incorporated into microorganisms. This CH₄‐derived carbon equated to up to 5.7% of total primary production estimates for Alaskan arctic lakes. Type I methanotrophs, including Methylomonas, Methylobacter and unclassified Methylococcaceae, were most active at CH₄ oxidation in this arctic lake. With increasing distance from the active CH₄ seepage, a greater diversity of bacteria incorporated CH₄‐derived carbon. Actinomycetes were the most quantitatively important microorganisms involved in secondary feeding on CH₄‐derived carbon. These results showed that CH₄ flows through methanotrophs into the broader microbial community and that type I methanotrophs, methylotrophs and actinomycetes are important organisms involved in using CH₄‐derived carbon in arctic freshwater ecosystems.     

Patient-centered outcomes of high-velocity, low-amplitude spinal manipulation for low back pain: A systematic review

Low back pain (LBP) is a well-recognized public health problem with no clear gold standard medical approach to treatment. Thus, those with LBP frequently turn to treatments such as spinal manipulation (SM). Many clinical trials have been conducted to evaluate the efficacy or effectiveness of SM for LBP. The primary objective of this paper was to describe the current literature on patient-centered outcomes following a specific type of commonly used SM, high-velocity low-amplitude (HVLA), in patients with LBP. A systematic search strategy was used to capture all LBP clinical trials of HVLA using our predefined patient-centered outcomes: visual analogue scale, numerical pain rating scale, Roland-Morris Disability Questionnaire, and the Oswestry Low Back Pain Disability Index. Of the 1294 articles identified by our search, 38 met our eligibility criteria. Like previous SM for LBP systematic reviews, this review shows a small but consistent treatment effect at least as large as that seen in other conservative methods of care. The heterogeneity and inconsistency in reporting within the studies reviewed makes it difficult to draw definitive conclusions. Future SM studies for LBP would benefit if some of these issues were addressed by the scientific community before further research in this area is conducted.     

Diversity of active aerobic methanotrophs along depth profiles of arctic and subarctic lake water column and sediments

Methane (CH₄) emitted from high-latitude lakes accounts for 2–6% of the global atmospheric CH₄ budget. Methanotrophs in lake sediments and water columns mitigate the amount of CH₄ that enters the atmosphere, yet their identity and activity in arctic and subarctic lakes are poorly understood. We used stable isotope probing (SIP), quantitative PCR (Q-PCR), pyrosequencing and enrichment cultures to determine the identity and diversity of active aerobic methanotrophs in the water columns and sediments (0–25 cm) from an arctic tundra lake (Lake Qalluuraq) on the north slope of Alaska and a subarctic taiga lake (Lake Killarney) in Alaska''s interior. The water column CH₄ oxidation potential for these shallow (∼2 m deep) lakes was greatest in hypoxic bottom water from the subarctic lake. The type II methanotroph, Methylocystis, was prevalent in enrichment cultures of planktonic methanotrophs from the water columns. In the sediments, type I methanotrophs (Methylobacter, Methylosoma and Methylomonas) at the sediment-water interface (0–1 cm) were most active in assimilating CH₄, whereas the type I methanotroph Methylobacter and/or type II methanotroph Methylocystis contributed substantially to carbon acquisition in the deeper (15–20 cm) sediments. In addition to methanotrophs, an unexpectedly high abundance of methylotrophs also actively utilized CH₄-derived carbon. This study provides new insight into the identity and activity of methanotrophs in the sediments and water from high-latitude lakes.     

Metamorphosis of the olfactory organ of the sea lamprey (Petromyzon marinus L.): Morphological changes and morphometric analysis

In larval sea lampreys (Petromyzon marinus), a small, relatively inconspicuous olfactory organ sac contains small, densely packed olfactory receptor neurons and sustentacular cells. During metamorphosis, the larval organ transforms into a prominent lamellar structure with large distinct olfactory epithelial cells that is characteristic of the adult lamprey. In the present study, scanning electron microscopy and light microscopy are used to examine changes during the seven stages (1–7) of metamorphosis. The magnitude of growth over the course of metamorphosis is evident from the doubling of the relative weight of the nasal sac. During early metamorphosis (stages 1 and 2), the larval olfactory organ enlarges, and by stage 3 specific adult structures begin to form, namely a nasal valve between the nasal tube and the organ, lamellar folds, and diverticuli of the accessory olfactory organ. Subsequent development involves widening of the cells lining the lamellar folds to the form characteristic of postmetamorphic lampreys. Although the cells in the troughs initially retain numerical density values that are significantly higher than those on the lamellar surfaces, by stage 7 values decline both in troughs and along lamellar surfaces to those observed in adults. These results show that although expansion of the olfactory organ is ongoing throughout metamorphosis, remodeling occurs early (by stage 3). This timing provides space for extensive olfactory receptor neuron neurogenesis and differentiation and correlates with the transformation of some organs that were previously examined. This is the first report in any species of olfactory receptor neuron zonation based on morphometric characteristics. J. Morphol. 231:41–52, 1997. © 1997 Wiley-Liss, Inc.