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Past vegetation changes in the Brazilian Pantanal arboreal–grassy savanna ecotone by using carbon isotopes in the soil organic matter
Author(s) -
VICTORIA REYNALDO LUIZ,
FERNANDES FERNANDO,
MARTINELLI LUIZ ANTONIO,
CÁSSIA PICCOLO MARISA,
CAMARGO PLINIO BARBOSA,
TRUMBORE SUSAN
Publication year - 1995
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.1995.tb00018.x
Subject(s) - ecotone , arboreal locomotion , vegetation (pathology) , environmental science , organic matter , δ13c , ecology , transect , soil organic matter , soil carbon , soil water , soil science , stable isotope ratio , biology , habitat , medicine , physics , pathology , quantum mechanics
Measurements of the organic carbon inventory, its stable isotopic composition and radiocarbon content were used to deduce vegetation history from two soil profiles in arboreal and grassy savanna ecotones in the Brazilian Pantanal. The Pantanal is a large floodplain area with grass‐dominated lowlands subject to seasonal flooding, and arboreal savanna uplands which are only rarely flooded. Organic carbon inventories were lower in the grassy savanna site than in the upland arboreal savanna site, with carbon decreasing exponentially with depth from the surface in both profiles. Changes in 13 C of soil organic matter (SOM) with depth differed markedly between the two sites. Differences in surface SOM 13 C values reflect the change from C 3 to C 4 plants between the sites, as confirmed by measurements of 13 C of vegetation and the soil surface along a transect between the upland closed‐canopy forest and lowland grassy savanna. Changes of 13 C in SOM with depth at both sites are larger than the 3–4 per mil increases expected from fractionation associated with organic matter decomposition. We interpret these as recording past changes in the relative abundance of C 3 and C 4 plants at these sites. Mass balances with 14 C and 13 C suggest that past vegetational changes from C 3 to C 4 plants in the grassy savanna, and in the deeper part of the arboreal savanna, occurred between 4600 and 11 400 BP, when major climatic changes were also observed in several places of the South American Continent. The change from C 4 to C 3 , observed only in the upper part of the arboreal savanna, was much more recent (1400 BP), and was probably caused by a local change in the flooding regime.