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Increased vertical decoupling between nutrients in topsoil and water availability in subsoil\/bedrock layers under warming could thereby reduce cumulative nutrient uptake over the growing season.<\/jats:p>\n                      <\/jats:list-item>\n                      <jats:list-item>\n                        <jats:p>\n                          We used a Mediterranean semiarid shrubland as model system to assess the impacts of warming\u2010induced topsoil desiccation on plant water\u2010 and nutrient\u2010use patterns. A 6\u00a0yr manipulative field experiment examined the effects of warming (2.5\u00b0C), rainfall reduction (30%) and their combination on soil resource utilization by\n                          <jats:italic>Helianthemum squamatum<\/jats:italic>\n                          shrubs.\n                        <\/jats:p>\n                      <\/jats:list-item>\n                      <jats:list-item>\n                        <jats:p>A drier fertile topsoil (\u2018growth pool\u2019) under warming led to greater proportional utilization of water from deeper, wetter, but less fertile subsoil\/bedrock layers (\u2018maintenance pool\u2019) by plants. This was linked to decreased cumulative nutrient uptake, increased nonstomatal (nutritional) limitation of photosynthesis and reduced water\u2010use efficiency, above\u2010ground biomass growth and drought survival.<\/jats:p>\n                      <\/jats:list-item>\n                      <jats:list-item>\n                        <jats:p>Whereas a shift to greater utilization of water stored in deep subsoil\/bedrock may buffer the negative impact of warming\u2010induced topsoil desiccation on transpiration, this plastic response cannot compensate for the associated reduction in cumulative nutrient uptake and carbon assimilation, which may compromise the capacity of plants to adjust to a warmer and drier climate.<\/jats:p>\n                      <\/jats:list-item>\n                    <\/jats:list>\n                  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