Search alternatives:
significant level » significance level (Expand Search), significance levels (Expand Search), significant gender (Expand Search)
level decrease » levels decreased (Expand Search), level increased (Expand Search), teer decrease (Expand Search)
long decrease » point decrease (Expand Search), fold decrease (Expand Search), coping decreased (Expand Search)
nn decrease » _ decrease (Expand Search), a decrease (Expand Search), mean decrease (Expand Search)
significant level » significance level (Expand Search), significance levels (Expand Search), significant gender (Expand Search)
level decrease » levels decreased (Expand Search), level increased (Expand Search), teer decrease (Expand Search)
long decrease » point decrease (Expand Search), fold decrease (Expand Search), coping decreased (Expand Search)
nn decrease » _ decrease (Expand Search), a decrease (Expand Search), mean decrease (Expand Search)
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HFD decreases ITM and alters metabolic homeostasis.
Published 2025“…Two-way ANOVA, n.s., not significant, ** p < 0.01). <b>(F)</b> Long-term memory (LTM) was significantly decreased in the HFD group. …”
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Modeling the relationship between cancer level in hemolymph and MarBTN in tank eDNA.
Published 2025Subjects: -
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Alterations of Ceramides, Acylcarnitines, GlyceroLPLs, and Amines in NSCLC Tissues
Published 2024Subjects: -
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Metabolites with decreasing levels during the development.
Published 2025“…<p>Temporal profiles of polar metabolites and lipids with SCN levels significantly decreasing from E19 to P28. Rhythmicity was determined by eJTK; full or dashed lines depict the profiles that either did or did not pass the significance threshold (FDR-adjusted <i>P</i> < 0.05), respectively.…”
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Graded loading creep stress loading level.
Published 2025“…The results reveal that (1) freeze-thaw cycles exert a significant influence on the rock’s creep behavior, with axial strain, instantaneous strain, and creep strain increasing progressively with the number of freeze-thaw cycles; (2) dual-fractured rock samples with varying fracture angles exhibit distinct differences in creep phenomena, where increased fracture angles result in pronounced increases in instantaneous and creep strains, and higher horizontal stress levels lead to greater strain generation; (3) all rock samples with different pre-existing fractures exhibit rock bridge breakthrough during creep failure, and the variation in fracture angle affects the failure mode; (4) and the long-term strength of the rock varies with changes in fracture angle and freeze-thaw cycle frequency, showing an increasing trend with greater fracture angles but a rapid decrease with increasing freeze-thaw cycles. …”
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