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  • 1
    Digitale Medien
    Digitale Medien
    Amsterdam : Elsevier
    Journal of Chromatography B: Biomedical Sciences and Applications 272 (1983), S. 359-365 
    ISSN: 0378-4347
    Quelle: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    ISSN: 1432-0843
    Schlagwort(e): Key words rHuG-CSF ; CD rats
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Medizin
    Notizen: Abstract  Recent studies in human bone-marrow culture and healthy human volunteers suggest that lenograstim [glycosylated, recombinant human granulocyte colony-stimulating factor (rHuG-CSF) produced in Chinese hamster ovary (CHO) cells] has greater in vivo potency than filgrastim [nonglycosylated, methionine-extended recombinant human granulocyte colony-stimulating factor (r-metHuG-CSF) produced in Escherichia coli]. To confirm and extend these results we investigated thein vivopotency of both products in normal rats and neutropenic CD rats as an animal model of chemotherapy-induced neutropenia. In normal rats, groups of eight normal male CD rats received four subcutaneous doses of 10, 30, or 100 μg/kg filgrastim or lenograstim on days 1 – 4 of the study, whereas a control group received the vehicle. Blood samples were collected from each animal before treatment (day  – 5) and on days 2, 3, 5, 8, and 12 of the study for determination of red blood cell (RBC), platelet, white blood cell (WBC), and differential counts. rHuG-CSF and r-metHuG-CSF produced increased WBC counts, principally due to elevated absolute neutrophil counts (ANCs); on days 2, 3, and 5, all groups receiving rG-CSF had ANCs that increased in a progressive and dose-related manner. With the exception of a single value, mean ANCs obtained on days 2, 3, and 5 in lenograstim-treated groups were higher (statistically significant on day 3 at 30 and 100 μg/kg and on day 5 at 10, 30, and 100 μg/kg) than the respective values obtained in filgrastim-treated groups. No compound-related effect was noted in RBC or platelet parameters. Neutropenia was induced in male CD rats (12 animals/group) with a single intraperitoneal dose of 50 mg/kg cyclophosphamide (CPA) on day 0. On days 1 – 4, CPA-treated groups were treated with the vehicle (control) or with filgrastim or lenograstim at 30 or 100 μg/kg per day. An additional group was not treated with CPA and served as the absolute control group. Blood was collected from alternating subgroups on study day  – 5 (pretest) and on days 2, 3, 4, 5, 6, 8, 9, and 12 for determination of RBC, platelet, WBC, and differential counts. No major adverse in-life effect was noted in neutropenic rats. Maximal depression of WBCs and ANCs occurred on day 5, followed by recovery to normal values by days 9 (ANC) and 12 (WBC). On day 3 and days 5 – 9, rHuG-CSF- and metHuG-CSF-treated groups had marked and dose-related increases in WBCs as compared with CPA-treated controls, principally due to elevated ANCs. With the exception of a few values, mean ANC values obtained in lenograstim-treated groups were consistently higher than the respective values obtained in filgrastim-treated groups; the difference was statistically significant on day 3 (30-μg/kg groups) and on days 6 and 8 (100-μg/kg groups). In conclusion, treatment of normal and neutropenic CD rats with lenograstim resulted in a dose-related elevation of ANCs that was consistently and significantly higher than the response to identical doses of filgrastim. These results suggest that lenograstim, the glycosylated form of rG-CSF, has superior in vivo potency in normal and neutropenic animals as compared with filgrastim, the nonglycosylated form of rG-CSF.
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-02-07
    Beschreibung: The Southern Ocean greatly contributes to the regulation of the global climate by controlling important heat and carbon exchanges between the atmosphere and the ocean. Rates of climate change on decadal timescales are therefore impacted by oceanic processes taking place in the Southern Ocean, yet too little is known about these processes. Limitations come both from the lack of observations in this extreme environment and its inherent sensitivity to intermittent processes at scales that are not well captured in current Earth system models. The Southern Ocean Carbon and Heat Impact on Climate programme was launched to address this knowledge gap, with the overall objective to understand and quantify variability of heat and carbon budgets in the Southern Ocean through an investigation of the key physical processes controlling exchanges between the atmosphere, ocean and sea ice using a combination of observational and modelling approaches. Here, we provide a brief overview of the programme, as well as a summary of some of the scientific progress achieved during its first half. Advances range from new evidence of the importance of specific processes in Southern Ocean ventilation rate (e.g. storm-induced turbulence, sea-ice meltwater fronts, wind-induced gyre circulation, dense shelf water formation and abyssal mixing) to refined descriptions of the physical changes currently ongoing in the Southern Ocean and of their link with global climate.This article is part of a discussion meeting issue 'Heat and carbon uptake in the Southern Ocean: the state of the art and future priorities'.
    Materialart: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2019-10-04
    Beschreibung: Since 2004, several hundreds of diving marine animals, mainly Antarctic and Arctic seals, were fitted with a new generation of Argos-CTD tags developed by the Sea Mammal Research Unit of the University of St. Andrews in Scotland. These tags can be used to investigate simultaneously the at-sea ecology of these animals while collecting valuable oceanographic data. Some of these species are able to travel thousands of kilometres, continuously diving to great depths (590 ± 200 m, with maxima around 2000m). Through the years, these animals have become an essential source of temperature and salinity profiles (MEOP-CTD database available at http://www.meop.net), especially for the polar oceans, complementing efficiently the Argo array. One region where the use of instrumented seals has been particularly successful is the Antarctic continental shelf. Recent contributions to the study of the Antarctic Bottom Water production area near Prydz Bay, the rapidly-thinning ice shelves in Amundsen Bay, or the stratification in the marginal ice zone, are demonstrating the rapidly growing value of these data for Polar Research.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2019-07-17
    Beschreibung: Due to the low accessibility of the region, most of the seasonally ice-covered Southern Ocean remains unobserved during winter. Here we show that southern elephant seals (Mirounga leonina), equipped with oceanographic sensors, can measure winter hydrography with unprecedented temporal and spatial resolution. Seals provided a 30-fold increase in hydrographic profiles from the sea ice zone, allowing the major fronts to be mapped south of 60°S. Sea-ice formation rates in the East Antarctic sector were estimated from salinity increase in the upper water column and compared to simulations with a circumpolar finite-element sea-ice ocean model. From the observations, peak freezing rates of 2.5-3 cm/d were estimated for the period from late April to early May during the rapid northward expansion of the ice cover. While the pack ice becomes more compact, sea ice formation declines to 1 cm/d in June/July, and virtually stops by the end of August, when the maximum ice extent is reached. Modeled and observed freezing rates agree remarkably well, so that the model can be used to complete the seasonal cycle. By sampling the ocean during winter, elephant seals fill a blind spot in our sampling coverage, bringing us closer to a truly global ocean observing system.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2019-07-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    facet.materialart.
    Unbekannt
    In:  EPIC3Proceedings of OceanObs 09: Sustained Ocean Observations and Information for Society (Vol. 2), Venice, Italy, 21-25 September 2009, Hall, J., Harrison D.E. & Stammer, D., Eds., ESA Publication WPP-306
    Publikationsdatum: 2019-07-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , peerRev
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    facet.materialart.
    Unbekannt
    In:  EPIC3Proceedings of OceanObs 09: Sustained Ocean Observations and Information for Society (Vol. 2), Venice, Italy, 21-25 September 2009, Hall, J., Harrison D.E. & Stammer, D., Eds., ESA Publication WPP-306.
    Publikationsdatum: 2019-07-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , peerRev
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publikationsdatum: 2023-08-09
    Beschreibung: In contrast with the atmosphere, which is heated from below by solar radiation, the ocean is both heated and cooled from above. To drive a deep-reaching overturning circulation in this context, it is generally assumed that either intense interior mixing by winds and internal tides, or wind-driven upwelling is required; in their absence, the circulation is thought to collapse to a shallow surface cell. We demonstrate, using a primitive equation model with an idealized domain and no wind forcing, that the surface temperature forcing can in fact drive an inter-hemisphere overturning provided that there is an open channel unblocked in the zonal direction, such as in the Southern Ocean. With this geometry, rotating horizontal convection, in combination with asymmetric surface cooling between the north and south, drives a deep-reaching two-cell overturning circulation. The resulting vertical stratification closely resembles that of the real ocean, suggesting that wind-driven pumping is not necessary to produce a deep-reaching overturning circulation contrary to common belief, and that buoyancy forcing plays a much more active role than is usually assumed.
    Sprache: Englisch
    Materialart: info:eu-repo/semantics/conferenceObject
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publikationsdatum: 2023-06-13
    Beschreibung: The data loggers attached to marine mammals represent an instrumentation type which provided a significant amount of temperature profiles for the moderate and polar regions since the 2000s. In the World Ocean Database WOD18 marine mammal data contribute ~60% of temperature profiles south of 50〈sup〉o〈/sup〉S for 2005 – 2018 and ~40% of profiles north of 40〈sup〉o〈/sup〉N being a significant data source for the estimation of the global ocean warming along with the data from ship-based CTDs and Argo floats. Use of the marine mammal data for the ocean heat content estimation requires the assessment of possible instrumental biases. For the first time we assess temperature biases in marine mammal data by comparing these data with temporarily and spatially collocated reference temperature profiles from Argo floats and ship-based CTDs. For the SRDL recorders implemented mostly in the Southern Ocean our estimates indicate a prevailing time- and sensor type dependent thermal negative temperature bias within the range -0.01 to -0.04〈sup〉o〈/sup〉C. The less accurate TRD recorders implemented earlier on mammals in the North Pacific are characterized by a different bias pattern, showing the predominantly positive bias of about 0.08 to 0.10〈sup〉o〈/sup〉C below 100 m. The derived total TRD bias can be decomposed into a small positive thermal bias (~0.02〈sup〉o〈/sup〉C) and the bias due to the systematic error in pressure (depth). Based on the results of the study we provide corrections for instrumental temperature biases both in SRDL and TRD recorders.
    Sprache: Englisch
    Materialart: info:eu-repo/semantics/conferenceObject
    Standort Signatur Einschränkungen Verfügbarkeit
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