Soil Moisture and Its Interaction With Temperature Determine Root Metabolomes of a Himalayan Alpine Shrub.

On the other hand, the metabolites that showed an increasing trend with an increase in temperature at low soil moisture content and the opposite under high soil moisture content include beta‐Myrcene (Figure 4b ), myricetin (Figure 4c ) phosphatidylethanolamine (Figure S5e ), taxifolin (Figure S5f ), pyridoxine (Figure S5g ), asparagine (Figure S5h ), and ornithine (Figure S5i ). 3.5.2 Other Metabolites Among the many other metabolites that were not represented in pathways above, primary metabolites, including fatty acids (Figure 5b ) and arginine & derivatives (Figure S6a ), exhibited an increasing trend with rising temperatures and low moisture levels.

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The most strongly climate‐impacted metabolomic pathways (based on bubble color, where red indicates highly significant pathways and yellow represents less significant ones) were valine, leucine, and isoleucine degradation and synthesis (bubble no. 1 and 3), followed by monoterpenoid biosynthesis (bubble no. 4), glycerophospholipid metabolism (bubble no. 5), phenylpropanoid biosynthesis (bubble no. 6), flavonoid biosynthesis (bubble no. 8), and vitamin B6 metabolism (bubble no. 9).

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