26 research outputs found
Quantification of characterization of biologically active components of Actaea racemosa L. (black cohosh) for identifying desirable plants for cultivation
Actaea racemosa, more commonly known as black cohosh, is a medicinal plant used for
the suppression of menopausal symptoms. The growing popularity of black cohosh
extract is leading to extensive wild harvesting of the perennial plant. The main purpose of
this research is to use high-pressure liquid chromatography evaporative light scattering
detection analysis of 20 accessions of black cohosh from Bent Creek Germplasm
Repository to quantify the compounds with desirable biological activities. Plants
identified as having desirable properties may be used to produce a superior hybrid plant.
Cultivation of the hybrid plant may help black cohosh’s sustainability. This research
showed that there were significant differences in phytochemical concentrations among
the accessions
Alternating chemotherapy and fractionated radiotherapy as a modality for the treatment of primary liver cancer
Nausea in advanced cancer: relationships between intensity, burden, and the need for help
How does pain experience relate to the need for pain relief? A secondary exploratory analysis in a large sample of cancer patients
Effects of rituximab-based B-cell depletion therapy on skin manifestations of lupus erythematosus – report of 17 cases and review of the literature
Prednisone treatment inhibits the differentiation of B lymphocytes into plasma cells in MRL/MpSlac-lpr mice
Proximate controls on semiarid soil greenhouse gas fluxes across 3Â million years of soil development
© 2015 Springer International Publishing Switzerland Soils are important sources and sinks of three greenhouse gases (GHGs): carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O). However, it is unknown whether semiarid landscapes are important contributors to global fluxes of these gases, partly because our mechanistic understanding of soil GHG fluxes is largely derived from more humid ecosystems. We designed this study with the objective of identifying the important soil physical and biogeochemical controls on soil GHG fluxes in semiarid soils by observing seasonal changes in soil GHG fluxes across a three million year substrate age gradient in northern Arizona. We also manipulated soil nitrogen (N) and phosphorus availability with 7 years of fertilization and used regression tree analysis to identify drivers of unfertilized and fertilized soil GHG fluxes. Similar to humid ecosystems, soil N2O flux was correlated with changes in N and water availability and soil CO2 efflux was correlated with changes in water availability and temperature. Soil CH4 uptake was greatest in relatively colder and wetter soils. While fertilization had few direct effects on soil CH4 flux, soil nitrate was an important predictor of soil CH4 uptake in unfertilized soils and soil ammonium was an important predictor of soil CH4 uptake in fertilized soil. Like in humid ecosystems, N gas loss via nitrification or denitrification appears to increase with increases in N and water availability during ecosystem development. Our results suggest that, with some exceptions, the drivers of soil GHG fluxes in semiarid ecosystems are often similar to those observed in more humid ecosystems