2014
DOI: 10.1016/j.jsames.2014.09.019
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Nine thousand years of upper montane soil/vegetation dynamics from the summit of Caratuva Peak, Southern Brazil

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Cited by 2 publications
(2 citation statements)
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“…The gradual increase in height of such physiognomy is likely a result of the relative thickness of subsurface mineral horizons, below histosol horizons (histic) (Scheer et al 2014). Another strata was observed some 50 cm afar, in which Croton mullerianus, Rhynchospora exaltata and C. triquetrum were dominant.…”
Section: Resultsmentioning
confidence: 95%
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“…The gradual increase in height of such physiognomy is likely a result of the relative thickness of subsurface mineral horizons, below histosol horizons (histic) (Scheer et al 2014). Another strata was observed some 50 cm afar, in which Croton mullerianus, Rhynchospora exaltata and C. triquetrum were dominant.…”
Section: Resultsmentioning
confidence: 95%
“…There is Palaeobotanical evidence that suggests that the mountain ridges of Southeastern Brazil have been uninterruptedly covered by upper montane grasslands since the end of the Pleistocene (Behling 1997a, b). A similar situation must have occurred to the regions immediately to the South, although back then some exposed mountain ridges may have been largely bare or covered only by precursor rupestrian vegetation, being colonized (or recolonized) throughout the Holocene (Scheer et al 2012(Scheer et al , 2014.…”
Section: Introductionmentioning
confidence: 95%