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Effects of Pediococcus parvulus 2.6 and its exopolysaccharide on plasma cholesterol levels and inflammatory markers in mice
Beyond the neutron drip line: The unbound oxygen isotopes O-25 and O-26
RIFM fragrance ingredient safety assessment, 2,6-nonadienenitrile, CAS Registry Number 67019-89-0
Crystal structure and substrate interactions of an unusual fungal non-CBM carrying GH26 endo-β-mannanase from Yunnania penicillata
The neutrophil-mobilizing cytokine interleukin-26 in the airways of long-term tobacco smokers
Long-term tobacco smokers with chronic obstructive pulmonary disease (COPD) or chronic bronchitis display an excessive accumulation of neutrophils in the airways; an inflammation that responds poorly to established therapy. Thus, there is a need to identify new molecular targets for the development of effective therapy. Here, we hypothesized that the neutrophil-mobilizing cytokine interleukin (IL)
TLR4-mediated release of heparin-binding protein in human airways : a co-stimulatory role for IL-26
β-Mannanase BoMan26B from Bacteroides ovatus produces mannan-oligosaccharides with prebiotic potential from galactomannan and softwood β-mannans
Complex Involvement of Interleukin-26 in Bacterial Lung Infection
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β -delayed proton emission from P 26 and S 27
Overexpression of ST6GalNAcV, a ganglioside-specific alpha2,6-sialyltransferase, inhibits glioma growth in vivo
β decay of26Ne
Screening of yeast species for the stereo-selective reduction of bicyclo[2.2.2]octane-2,6-dione
Vanin-1 T26I polymorphism, hypertension and cardiovascular events in two large urban-based prospective studies in Swedes.
Bicyclo[3.3.1]nonane-2,6-dione and its utilization as a core building block in supramolecular architectures
Late Pleistocene glacial history of Jameson Land, central East Greenland, derived from cosmogenic (10)Be and (26)Al exposure dating
Abstract in Undetermined Previous work has presented contrasting views of the last glaciation on Jameson Land, central East Greenland, and still there is debate about whether the area was: (i) ice-free, (ii) covered with a local non-erosive ice cap(s), or (iii) overridden by the Greenland Ice Sheet during the Last Glacial Maximum (LGM). Here, we use cosmogenic exposure ages from erratics to reconc
