Independent variations of CH₄ emissions and isotopic composition over the past 160,000 years

During the last glacial cycle, greenhouse gas concentrations fluctuated on decadal and longer timescales. Concentrations of methane, as measured in polar ice cores, show a close connection with Northern Hemisphere temperature variability, but the contribution of the various methane sources and sinks to changes in concentration is still a matter of debate. Here we assess changes in methane cycling over the past 160,000 years by measurements of the carbon isotopic composition delta C-13 of methane in Antarctic ice cores from Dronning Maud Land and Vostok. We find that variations in the delta C-13 of methane are not generally correlated with changes in atmospheric methane concentration, but instead more closely correlated to atmospheric CO2 concentrations. We interpret this to reflect a climatic and CO2-related control on the isotopic signature of methane source material, such as ecosystem shifts in the seasonally inundated tropical wetlands that produce methane. In contrast, relatively stable delta C-13 values occurred during intervals of large changes in the atmospheric loading of methane. We suggest that most methane sources-most notably tropical wetlands-must have responded simultaneously to climate changes across these periods.

Right-handed neutrino production rate at T > 160 GeV

The production rate of right-handed neutrinos from a Standard Model plasma at a temperature above a hundred GeV has previously been evaluated up to NLO in Standard Model couplings (g ~ 2/3) in relativistic (M ~ πT) and non-relativistic regimes (M ≫ πT), and up to LO in an ultrarelativistic regime (M ≲ gT). The last result necessitates an all-orders resummation of the loop expansion, accounting for multiple soft scatterings of the nearly light-like particles participating in 1↔2 reactions. In this paper we suggest how the regimes can be interpolated into a result applicable for any right-handed neutrino mass and at all temperatures above 160GeV. The results can also be used for determining the lepton number washout rate in models containing right-handed neutrinos. Numerical results are given in a tabulated form permitting for their incorporation into leptogenesis codes. We note that due to effects from soft Higgs bosons there is a narrow intermediate regime around M ~g 1/2 T in which our interpolation is phenomenological and a more precise study would be welcome.

Sphingosine kinase 2 deficient mice exhibit reduced experimental autoimmune encephalomyelitis: Resistance to FTY720 but not ST-968 treatments

The immunomodulatory drug FTY720 is presently approved for the treatment of relapsing-remitting multiple sclerosis. It is a prodrug that requires activation by sphingosine kinase 2 (SK-2) to induce T cell homing to secondary lymphoid tissue. In this study, we have investigated the role of SK-2 in experimental autoimmune encephalomyelitis (EAE) in C57BL/6 mice. We show that SK-2 deficiency reduced clinical symptoms of EAE. Furthermore, in SK-2-deficient mice, the protective effect of FTY720 on EAE was abolished, while the non-prodrug FTY720-derivative ST-968 was still fully active. Protection was paralleled by reduced numbers of T-lymphocytes in blood and a reduced blood-brain-barrier leakage. This correlated with reduced mRNA expression of ICAM-1, VCAM-1, but enhanced expression of PECAM-1. A similar regulation of permeability and of PECAM-1 was seen in primary cultures of isolated mouse brain vascular endothelial cells and in a human immortalized cell line upon SK-2 knockdown. In summary, these data demonstrated that deletion of SK-2 exerts a protective effect on the pathogenesis of EAE in C57BL/6 mice and that SK-2 is essential for the protective effect of FTY720 but not of ST-968. Thus, ST-968 is a promising novel immunomodulatory compound that may be a valuable alternative to FTY720 under conditions where SK-2 activity is limited.