878 resultados para van der Meer method
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door H. J. Koenen. Uitgeg. door het Provinciaal Utrechtsche Genootschap van kunsten en wetenschappen
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Palaeoclimatic information can be retrieved from the diffusion of the stable water isotope signal during firnification of snow. The diffusion length, a measure for the amount of diffusion a layer has experienced, depends on the firn temperature and the accumulation rate. We show that the estimation of the diffusion length using power spectral densities (PSDs) of the record of a single isotope species can be biased by uncertainties in spectral properties of the isotope signal prior to diffusion. By using a second water isotope and calculating the difference in diffusion lengths between the two isotopes, this problem is circumvented. We study the PSD method applied to two isotopes in detail and additionally present a new forward diffusion method for retrieving the differential diffusion length based on the Pearson correlation between the two isotope signals. The two methods are discussed and extensively tested on synthetic data which are generated in a Monte Carlo manner. We show that calibration of the PSD method with this synthetic data is necessary to be able to objectively determine the differential diffusion length. The correlation-based method proves to be a good alternative for the PSD method as it yields precision equal to or somewhat higher than the PSD method. The use of synthetic data also allows us to estimate the accuracy and precision of the two methods and to choose the best sampling strategy to obtain past temperatures with the required precision. In addition to application to synthetic data the two methods are tested on stable-isotope records from the EPICA (European Project for Ice Coring in Antarctica) ice core drilled in Dronning Maud Land, Antarctica, showing that reliable firn temperatures can be reconstructed with a typical uncertainty of 1.5 and 2 °C for the Holocene period and 2 and 2.5 °C for the last glacial period for the correlation and PSD method, respectively.
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Aims: The aim of this study is to explore the migration (colonization of new areas) and subsequent population expansion (within an area) since 15 ka cal BP of Abies, Fagus, Picea, and Quercus into and through the Alps solely on the basis of high-quality pollen data. Methods: Chronologies of 101 pollen sequences are improved or created. Data from the area delimited by 45.5–48.1°N and 6–14°E are summarized in three ways: (1) in a selection of pollen-percentage threshold maps (thresholds 0.5%, 1%, 2%, 4%, 8%, 16%, and 32% of land pollen); (2) in graphic summaries of 250-year time slices and geographic segments (lengthwise and transverse in relation to the main axis of the Alps) as pollen-percentage curves, pollen-percentage difference curves, and pollen-percentage threshold ages cal BP graphed against both the length and the transverse Alpine axes; and (3) in tables showing statistical relationships of either pollen-percentage threshold ages cal BP or pollen expansion durations (=time lapse between different pollen-percentage threshold ages cal BP) with latitude, longitude, and elevation; to establish these relationships we used both simple linear regression and multiple linear regression after stepwise-forward selection. Results: The statistical results indicate that (a) the use of pollen-percentage thresholds between 0.5% and 8% yield mostly similar directions of tree migration, so the method is fairly robust, (b) Abies migrated northward, Fagus southward, Picea westward, and Quercus northward; more detail does not emerge due to an extreme scarcity of high-quality data especially along the southern foothills of the Alps and in the eastern Alps. This scarcity allows the reconstruction of one immigration route only of Abies into the southern Alps. The speed of population expansion (following arrival) of Abies increased and of Picea decreased during the Holocene, of Fagus it decreased especially during the later Holocene, and of Quercus it increased especially at the start of the Holocene.
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Peat deposits in Greenland and Denmark were investigated to show that high-resolution dating of these archives of atmospheric deposition can be provided for the last 50 years by radiocarbon dating using the atmospheric bomb pulse. (super 14) C was determined in macrofossils from sequential one cm slices using accelerator mass spectrometry (AMS). Values were calibrated with a general-purpose curve derived from annually averaged atmospheric (super 14) CO (sub 2) values in the northernmost northern hemisphere (NNH, 30 degrees -90 degrees N). We present a through review of (super 14) C bomb-pulse data from the NNH including our own measurements made in tree rings and seeds from Arizona as well as other previously published data. We show that our general-purpose calibration curve is valid for the whole NNH producing accurate dates within 1-2 years. In consequence, (super 14) C AMS can precisely date individual points in recent peat deposits within the range of the bomb-pulse (from the mid-1950s on). Comparing the (super 14) C AMS results with the customary dating method for recent peat profiles by (super 210) Pb, we show that the use of (super 137) Cs to validate and correct (super 210) Pb dates proves to be more problematic than previously supposed. As a unique example of our technique, we show how this chronometer can be applied to identify temporal changes in Hg concentrations from Danish and Greenland peat cores.
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OBJECTIVE To systematically review the reporting of MII (MII) oocyte development after xenotransplantation of human ovarian tissue. DESIGN Systematic review in accordance with the guidelines of the Preferred Reporting Items for Systematic Reviews and Meta-analyses (PRISMA). SETTING Not applicable. PATIENT(S) Not applicable. INTERVENTION(S) Formation of MII oocytes after xenotransplantation of human ovarian tissue. MAIN OUTCOME MEASURE(S) Any outcome reported in Pubmed. RESULT(S) Six publications were identified that report on formation of MII oocytes after xenotransplantation of human ovarian tissue. CONCLUSION(S) Xenografting of human ovarian tissue has proved to be a useful model for examining ovarian function and follicle development in vivo. With human follicles that have matured through xenografting, the possibility of cancer transmission and relapse can also be eliminated, because cancer cells are not able to penetrate the zona pellucida. The reported studies have demonstrated that xenografted ovarian tissue from a range of species, including humans, can produce antral follicles that contain mature (MII) oocytes, and it has been shown that mice oocytes have the potential to give rise to live young. Although some ethical questions remain unresolved, xenotransplantation may be a promising method for restoring fertility. This review furthermore describes the value of xenotransplantation as a tool in reproductive biology and discusses the ethical and potential safety issues regarding ovarian tissue xenotransplantation as a means of recovering fertility.
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INTRODUCTION The aim of the study was to identify the appropriate level of Charlson comorbidity index (CCI) in older patients (>70 years) with high-risk prostate cancer (PCa) to achieve survival benefit following radical prostatectomy (RP). METHODS We retrospectively analyzed 1008 older patients (>70 years) who underwent RP with pelvic lymph node dissection for high-risk prostate cancer (preoperative prostate-specific antigen >20 ng/mL or clinical stage ≥T2c or Gleason ≥8) from 14 tertiary institutions between 1988 and 2014. The study population was further grouped into CCI < 2 and ≥2 for analysis. Survival rate for each group was estimated with Kaplan-Meier method and competitive risk Fine-Gray regression to estimate the best explanatory multivariable model. Area under the curve (AUC) and Akaike information criterion were used to identify ideal 'Cut off' for CCI. RESULTS The clinical and cancer characteristics were similar between the two groups. Comparison of the survival analysis using the Kaplan-Meier curve between two groups for non-cancer death and survival estimations for 5 and 10 years shows significant worst outcomes for patients with CCI ≥ 2. In multivariate model to decide the appropriate CCI cut-off point, we found CCI 2 has better AUC and p value in log rank test. CONCLUSION Older patients with fewer comorbidities harboring high-risk PCa appears to benefit from RP. Sicker patients are more likely to die due to non-prostate cancer-related causes and are less likely to benefit from RP.
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Die sportmotorische Leistungsfähigkeit (SMLF) gilt in jüngster Zeit als ein Prädiktor für schulische Leistung (SL) (Diamond, 2013). Um die Frage zu beantworten, wie denn zwei auf den ersten Blick so distale Merkmale zusammenhängen sollen, werden unterschiedliche erklärende Variablen diskutiert, wobei die kognitive Stimulationshypothese die exekutiven Funktionen (EF) als mediierende Variable im Zusammenhang zwischen SMLF und SL postuliert. Die Annahme hierbei ist, dass die mit komplexen motorischen Kontrollprozessen einhergehende kognitive Beanspruchung bei einem wiederholten Ausführen von nicht-automatisierten sportbezogenen Handlungen zu einer Aktivierung und somit Förderung der EF führt (Best, 2010). Der mediierende Effekt der EF im Zusammenhang zwischen der SMLF und der SL wird seit einigen Jahren in der Literatur diskutiert und wird im Folgenden innerhalb einer längsschnittlichen Untersuchung getestet. Im Rahmen der Studie SpuK wurden 237 Primarschulkinder (52.3% ♀; 11.31 ± 0.62 Jahre) zu drei Messzeitpunkten in ihrer SMLF (T1) und ihren EF (T2) getestet. Zur Ermittlung der SMLF wurden drei sportmotorische Tests in den Bereichen Koordination, Ausdauer und Schnellkraft durchgeführt. Die EF Inhibition, kognitive Flexibilität und Arbeitsgedächtnis wurden computerbasiert über den N-Back- und Flanker-Test operationalisiert. Zusätzlich wurde die SL (T3) mittels objektiver Schulleistungstests erhoben. Um die Hauptfragestellung zu prüfen, wurde eine bootstrapping basierte Mediationsanalyse in AMOS durchgeführt. Das Strukturgleichungsmodell (2 (22, N=237)=30.357, p=.110; CFI=.978) weist eine zufriedenstellende Anpassungsgüte auf. Erwartungsgemäss zerfällt der Zusammenhang innerhalb des Mediationsmodells zwischen der SMLF und der SL, alsbald die EF ins Modell aufgenommen werden (β=.16, p= .634). Sowohl der Zusammenhang zwischen der SMLF und den EF (β=.38, p= .039), als auch der Zusammenhang zwischen den EF und der SL fallen signifikant aus (β=.91, p=.001) und ergeben dabei eine volle Mediation über den indirekten (p=.021) und totalen Effekt (p=.001). Die vorliegenden längs-schnittlichen Daten bestätigen den Zusammenhang zwischen SMLF und SL bei einer Mediation über die EF und bestätigen somit die aus querschnittlichem Design stammenden Resultate von van der Niet et al. (2014). Literatur Best, J. R. (2010). Effects of physical activity on children’s executive function: Contributions of ex-perimental research on aerobic exercise. Developmental Review, 30, 331-351. Diamond, A. (2013). Executive functions. Annual Review of Psychology, 64, 135-168. van der Niet, A. G., Hartmann, E., Smith, J. & Visscher, C. (2014). Modeling relationships between physical fitness, executive functioning, and academic achievement in primary school chil-dren. Psychology of Sport & Exercise, 15(4), 319-325.
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L. van der Tonge
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Hendrik van der Spyck
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Mit Porträtmedaillon eines Feldherrn
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Drilling at site 207 (DSDP Leg 21), located on the broad summit of the Lord Howe Rise, bottomed in rhyolitic rocks. Sanidine concentrates from four samples of the rhyolite were dated by the 40Ar/39Ar total fusion method and conventional K-Ar method, and yielded concordant ages of 93.7 +/- 1.1 my, equivalent to the early part of the Upper Cretaceous. At this time the Lord Howe Rise, which has continental-type structure, is thought to have been emergent and adjacent to the eastern margin of the Australian-antarctic continent. Subsequent to 94 my ago and prior to deposition of Maastrichtian (70-65 myBP) marine sediments on top of the rhyolitic basement of the Lord Howe Rise, rifting occurred and the formation of the Tasman Basin began by sea-floor spreading with rotation of the Rise away from the margin of Australia. Subsidence of the Rise continued until Early Eocene (about 50 myBP), probably marking the end of sea-floor spreading in the Tasman Basin. These large scale movements relate to the breakup of this part of Gondwanaland in the Upper Cretaceous.