Niu Yi

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Niu
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Yi
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  • Article
    Parkinson'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.
  • Article
    Noble 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.