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Germination requirements and seedling responses to water availability and soil type in four eucalypt species

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GAUTHIER-VILLARS/EDITIONS ELSEVIER
DOI: 10.1016/S1146-609X(01)01130-4

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Eucalyptus; leteritic loam; sand; seeds; soil water potential

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We conducted experiments on seed germination, seedling survival and seedling growth of four Eucalyptus species to identify factors that might explain why they are restricted to the two major soil types in southwestern Australia, deep sands (E. macrocarpa, E. tetragona) and lateritic loam (E. loxophleba, E. wandoo). At high temperatures (28 degreesC), germination in darkness was lower for the two 'loam species' than for the 'sand species', while there were no differences in light or at low temperatures (10 degreesC). Germination commenced earlier, and was faster in the sand species than in the loam species, but was almost inhibited in all species by -1.0 MPa. E. tetragona proved the most drought-tolerant in terms of germination level and seedling survival. Seedlings of the sand species had much longer roots two weeks after germination in the absence of water stress, and the roots of more seedlings continued to elongate under moderate water stress (-1.0 MPa), than the two loam species. Roots were longer in all species, except E. macrocarpa, at -0.5 MPa than at -0.1 MPa, despite seedlings having a smaller mass and hypocotyl length. As water availability declined, there was a tendency for the sand species to survive longer on sand than on loam while soil type had no effect on the loam species. Pattern and duration of seedling survival of the loam species was similar to that of the sand species despite their smaller seeds. We conclude that seedlings from the large-seeded sand species are able to penetrate the soil profile faster and deeper, but that they are not less prone to drying soils than seedlings from the small-seeded loam species. Instead, seed size and germination speed are important prerequisites to cope successfully with unstable soil surfaces and to exploit the rapidly descending water in deep sands. (C) 2002 Editions scientifiques et medicales Elsevier SAS. All rights reserved.

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