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ArticleParkinson's disease protein DJ-1 regulates ATP synthase protein components to increase neuronal process outgrowth(Springer Nature, 2019-06-13) Chen, Rongmin ; Park, Han-A ; Mnatsakanyan, Nelli ; Niu, Yulong ; Licznerski, Pawel ; Wu, Jing ; Miranda, Paige ; Graham, Morven ; Tang, Jack ; Boon, Agnita J. W. ; Cossu, Giovanni ; Mandemakers, Wim ; Bonifati, Vincenzo ; Smith, Peter J. S. ; Alavian, Kambiz N. ; Jonas, Elizabeth A.Familial Parkinson’s disease (PD) protein DJ-1 mutations are linked to early onset PD. We have found that DJ-1 binds directly to the F1FO ATP synthase β subunit. DJ-1’s interaction with the β subunit decreased mitochondrial uncoupling and enhanced ATP production efficiency while in contrast mutations in DJ-1 or DJ-1 knockout increased mitochondrial uncoupling, and depolarized neuronal mitochondria. In mesencephalic DJ-1 KO cultures, there was a progressive loss of neuronal process extension. This was ameliorated by a pharmacological reagent, dexpramipexole, that binds to ATP synthase, closing a mitochondrial inner membrane leak and enhancing ATP synthase efficiency. ATP synthase c-subunit can form an uncoupling channel; we measured, therefore, ATP synthase F1 (β subunit) and c-subunit protein levels. We found that ATP synthase β subunit protein level in the DJ-1 KO neurons was approximately half that found in their wild-type counterparts, comprising a severe defect in ATP synthase stoichiometry and unmasking c-subunit. We suggest that DJ-1 enhances dopaminergic cell metabolism and growth by its regulation of ATP synthase protein components.
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ArticleNoble gas signatures in Greenland : tracing glacial meltwater sources(John Wiley & Sons, 2015-11-06) Niu, Yi ; Castro, M. Clara ; Aciego, Sarah M. ; Hall, Chris M. ; Stevenson, Emily I. ; Arendt, Carli A. ; Das, Sarah B.This study represents the first comprehensive noble gas study in glacial meltwater from the Greenland Ice Sheet. It shows that most samples are in disequilibrium with surface collection conditions. A preliminary Ne and Xe analysis suggests that about half of the samples equilibrated at a temperature of ~0°C and altitudes between 1000 m and 2000 m, with a few samples pointing to lower equilibration altitudes and temperatures between 2°C and 5°C. Two samples suggest an origin as melted ice and complete lack of equilibration with surface conditions. A helium component analysis suggests that this glacial meltwater was isolated from the atmosphere prior to the 1950s, with most samples yielding residence times ≤ 420 years. Most samples represent a mixture between a dominant atmospheric component originating as precipitation and basal meltwater or groundwater, which has accumulated crustal 4He over time.