Table 2_A novel α-conotoxin [D1G, ΔQ14] LvIC decreased mouse locomotor activity.xls by Wen Wang (6570)

“…</p>Results<p>The injection of [D1G, ΔQ14] LvIC led to a decrease in locomotor activity in mice. This treatment also resulted in reduced expression of neuronal calcium sensor 1 (NCS-1) and neuroligin 3 (NLGN-3) in the prefrontal cortex (PFC), hippocampus (Hip), and caudate putamen (CPu). …”

Fluorescence Imaging of Neuroblastocyte Differentiation and Parkinson’s Brain Tissue Lesions Examined by a Norepinephrine-Activated Molecular Probe by Huming Yan (9917374)

“…Compared to the previously developed probe <i><b>SXU-NEQ</b></i>, the self-fluorescence intensity of probe <i><b>DQF</b></i> decreased significantly (I<i>_<b>DQF</b></i>/I<i>_{<b>SXU‑NEQ</b>}</i> = 35%). …”

Intracellular retention, but not shedding of NKp65 molecules containing threonine at amino acid position 131 causes decreased surface expression. by Julian Leonard Lino Heller (22049674)

Flow diagram representing bromeliad death by overcrowding within the Bromeliad-death procedure. by Alexandra M. Campbell (3284094)

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PRCC values (with <i>p</i>-values in parentheses) for the median final population size and difference in mean MSI at the final time, without weevil predation and with weevil predat... by Alexandra M. Campbell (3284094)

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Estimated parameters for distribution of basal area. by Alexandra M. Campbell (3284094)

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MRSP Tree Host Data. by Alexandra M. Campbell (3284094)

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Distribution of population at final time (left) and change in mean MSI at final time (right) from simulations across 1000 parameter sets when weevils are absent (red) and with weev... by Alexandra M. Campbell (3284094)

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<i>Tillandsia utriculata</i> death rate data by size class. by Alexandra M. Campbell (3284094)

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Parameter sets generated through Latin hypercube sampling. by Alexandra M. Campbell (3284094)

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Wear morphology: (a) UT, (b) SP1, (c) SP2, and (d) SP3. by Huashen Guan (20454677)

Residual stress of various samples: (a) surface residual stress and (b) residual stress in the depth direction. by Huashen Guan (20454677)

Mean daily sediment transport (g m^-2 day^-1) under different vegetation types and soil cover in southeastern Utah, USA, 2004 to 2018. by Andrew Kulmatiski (833256)

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”

Enhanced Reaction Kinetics in Stationary Two-Phase Flow through Porous Media by Xueyi Zhang (2019148)

“…The global kinetics initially increase before experiencing a monotonic decrease with significant fluctuations caused by the displacement of the nonwetting phase. …”