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Ontogeny affects response of northern red oak seedlings to elevated CO 2 and water stress: II. Recent photosynthate distribution and growth
Author(s) -
TOMLINSON PATRICIA T.,
ANDERSON PAUL D.
Publication year - 1998
Publication title -
new phytologist
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.742
H-Index - 244
eISSN - 1469-8137
pISSN - 0028-646X
DOI - 10.1111/j.1469-8137.1998.00291.x
Subject(s) - photosynthesis , deserts and xeric shrublands , shoot , sink (geography) , biology , growth rate , ontogeny , horticulture , botany , agronomy , ecology , habitat , geometry , cartography , mathematics , genetics , geography
Northern red oak in the western Lake States area of the USA exists on the most xeric edge of its distribution range. Future climate‐change scenarios for this area predict decreased water availability along with increased atmospheric CO 2 . We examined recent photosynthate distribution and growth in seedlings as a function of CO 2 mole fraction (400, 530 and 700 μmol mol −1 CO 2 ), water regime (well watered and water‐stressed), and ontogenic stage. Water stress effects on growth were largely offset by elevated CO 2 . Water stress increased root mass ratio without concurrently increasing allocation of recent photosynthate to the roots. However, apparent sink strength of water‐stressed seedlings at the completion of the third growth stage tended to be greater than that of well watered seedlings, as shown by continued high export, which may contribute carbon reserves to support preferential root growth under water‐stressed conditions. Elevated CO 2 decreased apparent shoot sink strength associated with the rapid expansion of the third flush. Carbon resources for the observed enhanced growth under elevated CO 2 could be provided by enhanced photosynthetic rate over an increased leaf area (Anderson & Tomlinson, 1998, this volume). Increased sink strength of LG seedlings under water‐stressed conditions, together with decreased apparent shoot sink strength associated with growth in elevated CO 2 provide mechanisms for offsetting water stress effects by growth in elevated CO 2 . Careful control of ontogeny was necessary to discern these changes and provides further evidence of the need for such careful control in mechanistic studies.