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Vertical distribution of below‐ground biomass in intensively grazed mesic grasslands
Author(s) -
Rodríguez Miguel A.,
Alvarez Javier,
GómezSal Antonio
Publication year - 1996
Publication title -
journal of vegetation science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.1
H-Index - 115
eISSN - 1654-1103
pISSN - 1100-9233
DOI - 10.2307/3236427
Subject(s) - biomass (ecology) , perennial plant , grassland , environmental science , forb , altitude (triangle) , agronomy , tussock , grazing , ecology , biology , geometry , mathematics
. Previous work has shown that below‐ground biomass is more concentrated in surface soil layers in intensively grazed mesic grasslands than in moderately grazed grasslands. However, since the mesic grasslands previously studied shared similar compositional traits, the question remained whether grasslands with differing species composition, and intensive defoliation, showed similar biomass distribution patterns. Eight grasslands at four sites distributed along an elevational gradient were investigated. The upper and lower zones of a slope were sampled at each site. Four of these grasslands were grazed by livestock and the other four were grazed and mown. Biomass was divided into above‐ground, root crown and three root layers. Species composition varied according to management and topography. Annuals and perennial forbs had relatively more above‐ground biomass at the upper part of the slopes, while perennial grasses dominated the lower parts. The above‐ground biomass and root biomass at 4 — 7 cm depth attained maximum values in the lower, potentially more fertile, parts of the slopes. Crown biomass increased with altitude at the upper part of the slopes. Despite their differences in composition and structure, seven out of the eight stands showed a remarkable concentration of the below‐ground biomass near the soil surface, which decreased drastically with soil depth. This pattern is similar to that observed in the intensively grazed mesic communities studied earlier. This similarity was more evident in the more mesic‐like grasslands, since it increased from the upper, potentially drier parts of the slopes, to the lower parts, and, when each topographic position was considered separately, from low to high elevation.

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