6 research outputs found
Evaluation of Clinically Relevant Drug-Drug Interactions and Population Pharmacokinetics of Darolutamide in Patients with Nonmetastatic Castration-Resistant Prostate Cancer : Results of Pre-Specified and Post Hoc Analyses of the Phase III ARAMIS Trial
In situ determination of iron(II) in the anoxic zone of the central Baltic Sea using ferene as spectrophotometric reagent
Continuous flow analysis for soluble Fe(II) species in seawater was performed with a colorimetric method using ferene as a spectrophotometric reagent. The method is based on the measurement of absorbance of the [FeII(fer)3]4 --complex at 594 nm. No preconcentration-steps are required. Samples prepared in the laboratory in line with external calibration experiments have been successfully analyzed in the nanomolar range (R2 = 0.959). A detection limit of 20 nM was obtained. Furthermore, investigations were performed in situ with a wet chemical analyzer in the water column of the central Baltic Sea. Finally the results were consistent with measurements made by an independent laboratory based method (ICP-OES)
A Multi-Pumping Flow System for In Situ Measurements of Dissolved Manganese in Aquatic Systems
A METals In Situ analyzer (METIS) has been used to determine dissolved manganese (II) concentrations in the subhalocline waters of the Gotland Deep (central Baltic Sea). High-resolution in situ measurements of total dissolved Mn were obtained in near real-time by spectrophotometry using 1-(2-pyridylazo)-2-naphthol (PAN). PAN is a complexing agent of dissolved Mn and forms a wine-red complex with a maximum absorbance at a wavelength of 562 nm. Results are presented together with ancillary temperature, salinity, and dissolved O 2 data. Lab calibration of the analyzer was performed in a pressure testing tank. A detection limit of 77 nM was obtained. For validation purposes, discrete water samples were taken by using a pump-CTD system. Dissolved Mn in these samples was determined by an independent laboratory based method (inductively coupled plasma–optical emission spectrometry, ICP-OES). Mn measurements from both METIS and ICP-OES analysis were in good agreement. The results showed that the in situ analysis of dissolved Mn is a powerful technique reducing dependencies on heavy and expensive equipment (pump-CTD system, ICP-OES) and is also cost and time effective
Discovery and Characterization of BAY 1214784, an Orally Available Spiroindoline Derivative Acting as a Potent and Selective Antagonist of the Human Gonadotropin-Releasing Hormone Receptor as Proven in a First-In-Human Study in Postmenopausal Women
Investigating hypoxia in aquatic environments: diverse approaches to addressing a complex phenomenon
In this paper we provide an overview of new
knowledge on oxygen depletion (hypoxia) and related phenomena
in aquatic systems resulting from the EU-FP7
project HYPOX (“In situ monitoring of oxygen depletion in
hypoxic ecosystems of coastal and open seas, and landlocked
water bodies”, www.hypox.net). In view of the anticipated
oxygen loss in aquatic systems due to eutrophication and climate
change, HYPOX was set up to improve capacities to
monitor hypoxia as well as to understand its causes and consequences.
Temporal dynamics and spatial patterns of hypoxia were
analyzed in field studies in various aquatic environments, including
the Baltic Sea, the Black Sea, Scottish and Scandinavian
fjords, Ionian Sea lagoons and embayments, and Swiss
lakes. Examples of episodic and rapid (hours) occurrences of
hypoxia, as well as seasonal changes in bottom-water oxygenation
in stratified systems, are discussed. Geologically
driven hypoxia caused by gas seepage is demonstrated. Using
novel technologies, temporal and spatial patterns of watercolumn
oxygenation, from basin-scale seasonal patterns to
meter-scale sub-micromolar oxygen distributions, were resolved.
Existing multidecadal monitoring data were used to
demonstrate the imprint of climate change and eutrophication
on long-term oxygen distributions. Organic and inorganic
proxies were used to extend investigations on past oxygen
conditions to centennial and even longer timescales that
cannot be resolved by monitoring. The effects of hypoxia on
faunal communities and biogeochemical processes were also
addressed in the project. An investigation of benthic fauna is
presented as an example of hypoxia-devastated benthic communities
that slowly recover upon a reduction in eutrophication
in a system where naturally occurring hypoxia overlaps
with anthropogenic hypoxia. Biogeochemical investigations
reveal that oxygen intrusions have a strong effect on the microbially
mediated redox cycling of elements. Observations
and modeling studies of the sediments demonstrate the effect
of seasonally changing oxygen conditions on benthic mineralization
pathways and fluxes. Data quality and access are
crucial in hypoxia research. Technical issues are therefore
also addressed, including the availability of suitable sensor
technology to resolve the gradual changes in bottom-water
oxygen in marine systems that can be expected as a result of
climate change. Using cabled observatories as examples, we
show how the benefit of continuous oxygen monitoring can
be maximized by adopting proper quality control. Finally,
we discuss strategies for state-of-the-art data archiving and
dissemination in compliance with global standards, and how
ocean observations can contribute to global earth observation
attempts