Wood growth of Tabebuia barbata (E. Mey.) Sandwith (Bignoniaceae) and Vatairea guianensis Aubl. (Fabaceae) in Central Amazonian black-water (igapó) and white-water (várzea) floodplain forests
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- da Fonseca Júnior, S.F., Piedade, M.T.F. & Schöngart, J. Trees (2009) 23: 127. doi:10.1007/s00468-008-0261-4
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Tree growth is a fundamental indicator for conservation plans of Amazonian floodplain forests. In this study we use dendrochronology to analyze wood growth patterns of Tabebuia barbata and Vatairea guianensis, two tree species occurring in nutrient-rich white-water (várzea, Mamirauá Sustainable Development Reserve, MSDR) and nutrient-poor black-water (igapó, Amanã Sustainable Development Reserve, ASDR) floodplain forests of Central Amazonia. From 20 trees per species and floodplain system (total of 80 trees) growing under a similar flooding regime with a mean inundation height of about 4 m we measured diameter at breast height (dbh). We sampled two cores per tree with an increment corer at the height of dbh to determine wood density (WD), tree age and mean radial increment (MRI) rates. The wood samples were macroscopically analyzed. Both tree species show distinct annual tree rings characterized by marginal parenchyma tissues. MRI was measured by a digital measuring device and WD was determined by the ratio dry mass/fresh volume. MRI of both tree species was significantly higher in the várzea than in the igapó, which can be traced back to the contrasting nutrient status. WD showed no difference comparing both floodplain forest types. Tree ages of a species for the same diameter are more than twofold higher in the igapó than in the várzea. To insure a sustainable harvest, felling cycles in these forests should be adjusted according to rates of growth.
KeywordsAmazonFloodplain forestDendrochronologyForest managementConservation
The Central Amazonian floodplain forests along the large river systems are an aquatic-terrestrial transition zone (Junk et al. 1989), because they alternate annually between a flooded and a non-flooded phase triggered by a monomodal flood-pulse with a mean amplitude of about 10 m (Schöngart and Junk 2007). Forests cover about 50–75% of the floodplain system and are the main vegetation type (Wittmann et al. 2002). Floodplain forests are of extreme importance for the fluvial ecosystems functioning as sinks and sources in the biogeochemical cycles, regulating the hydrological systems, acting as habitats for a high biodiversity of partial endemic plant and animal species and delivering natural resources for the human populations (Wittmann et al. 2006). The floodplain forests can be distinguished by their nutrient status into the igapó and the várzea (Prance 1979). The igapó covers about 100,000 km2 and is influenced by clear-water or black-water rivers draining the geochemically poor watersheds of the Central Brazilian shield and the Guyanas. The water has low pH and nutrient status. The várzea (~200,000 km2) is fed by the white-water rivers originating from the Andean catchments bringing high amounts of nutrient-rich sediments into the Central Amazonian floodplains which is deposited during the flooded period. Therefore the soils of the várzea floodplains contain much higher stocks of macro and micronutrients than the igapó (Furch 1997).
The existence of the monomodal flood-pulse for millions of years (Junk 1989) enabled the adaptation for hundreds of tree species to these extreme flooding conditions resulting in different forest types along hydrological, edaphic and successional gradients (Wittmann et al. 2006). The annual long-term flooding results in phenological, morphological and physiological responses of the trees (Parolin et al. 2004) and triggers the growth rhythm of many floodplain species (Schöngart et al. 2002). Flooding causes anaerobic conditions in the soils (Worbes 1997) leading to a reduction of root activity and root respiration at the beginning of the aquatic phase. During this period, the trees replace their leaves and start flowering and fruiting (Schöngart et al. 2002). Wood growth is mainly restricted to the terrestrial phase (vegetation period). During 3–4 months of the aquatic phase the cambium is dormant leading to the formation of an annual tree ring (Worbes 1988; Schöngart et al. 2002). The analysis of tree-ring sequences (dendrochronology) is a powerful tool for a rapid and accurate assessment of tree growth during the past comprising decades and centuries. This method is of extreme importance to obtain information on tree ages and diameter increment rates (Dünisch et al. 2003). In the Central Amazonian floodplain forests dendrochronology has been successfully applied to model climate–growth relationships (Schöngart et al. 2004, 2005), carbon sequestration (Schöngart 2003) and the definition of species-specific management criteria (Schöngart et al. 2007; Schöngart 2008).
In Central and Western Amazonia 60–90% of the timber originates from floodplain forests (Kvist and Nebel 2001; Worbes et al. 2001; Lima et al. 2005), due to the easy access and the low costs for harvesting, skidding and transport of the logs (Higuchi et al. 1994; Barros and Uhl 1995). However, such timber extraction concentrates on a few tree species such as Cedrela odorata, Calophyllum brasiliense, Ceiba pentandra, Virola surinamensis and Platymicium ulei. Timber harvesting in the floodplains is unsustainable because of the gaps of knowledge on growth rates and regeneration patterns of these species (Schöngart et al. 2007; Schöngart 2008). Diameter increment rates are a robust indicator for the dynamical processes of a forest ecosystem (Brienen and Zuidema 2006). Such data are important for the development of conservation plans by sustainable management or preservation. In this study we apply dendrochronology to determine tree age and mean diameter increment rates of the tree species Vatairea guianensis and Tabebuia barbata, which occur in both floodplain forest types.
Materials and methods
We selected the tree species T. barbata (Bignoniaceae) and V. guianensis (Fabaceae) for our study, because they are of commercial importance and occur in both floodplain forest types achieving high abundances (Ferreira 1997; Schöngart 2003; Parolin et al. 2004; Wittmann et al. 2006). Both species are deciduous, shedding their leaves at the beginning of the aquatic phase (February/March) and remaining bare for several weeks (Schöngart et al. 2002). Flowering occurs during December to May (T. barbata) and February/March (V. guianensis), while fruiting is restricted to the flooded period during March to June (T. barbata) and April to June (V. guianensis) (Schöngart et al. 2002; J. Schöngart, personal observation). T. barbata, known as capitarí in Central Amazonia, occurs in late successional stages, but occasionally appears also in earlier successional stages (Worbes 1988) of the low várzea inundated between 3 and 6 m on average per year (Wittmann et al. 2002). In the igapó the species establishes in old-growth forests under similar hydrological conditions. Local people use the wood as posts and lumber for construction (Wittmann et al. 2008). V. guianensis, known as faveira in the Central Amazon region, is a non-pioneer species dominating late successional stages in the low várzea and old-growth forests in the igapó (Parolin and Ferreira 1998; Schöngart 2003). The wood is used and commercialized mainly for house construction (Loureiro et al. 2000).
Fieldwork was realized during two excursions in February 2006 and August 2006. At each site 20 trees of a species with diameter at breast height (dbh) >20 cm were selected in old-growth forests at similar elevations of the várzea and igapó yielding a total number of 80 trees. From every tree dbh, measured 1.30 m above the ground, and the flood-height of every tree, visible as a distinct mark of the last high-water period on the trunk, were recorded. Two wood samples per tree were taken from 1.30 m with an increment corer (5 mm in diameter) to determine tree age and mean radial increment (MRI) as well as wood density (WD).
Sample preparation, ring-width measurements and data treatment
Mean flood-height, sample size, diameter at breast height (dbh), tree age, mean radial increment (MRI) and wood density (WD) of V. guianensis and T. barbata from Central Amazonian floodplain forests of várzea (nutrient-rich) and igapó (nutrient-poor)
n = 20
n = 20
n = 20
n = 20
Mean flood-height (m)
Inundation period (days)
Mean dbh (cm) (min–max)
MRI (mm) (mean ± SD)
1.71 ± 0.51
2.88 ± 1.00
2.29 ± 0.70
3.59 ± 1.53
Tree age (years) (mean ± SD)
92 ± 33
84 ± 28
102 ± 45
91 ± 37
WD (g cm−3) (mean ± SD)
0.83 ± 0.08
0.80 ± 0.08
0.65 ± 0.04
0.66 ± 0.03
Cross-correlations between diameter at breast height (dbh), and wood growth parameters (tree age, MRI, WD) of V. guianensis and T. barbata from the igapó and várzea (bold numbers)
The existence of annual tree rings of many tree species in Amazonian floodplain forests has been indicated by several independent dendrochronological methods such as wood anatomical descriptions, cambial wounding, measurements of the cambial resistance by a shigometer, phenological observations, dendrometers, densitometry, radiocarbon dating and climate–growth relationships (Worbes 1988, 1989, 1997; Worbes et al. 1995; Schöngart et al. 2002, 2004, 2005). In this study we apply dendrochronology to show how wood growth of a tree species varies in forest types of Amazonian floodplains with different nutrient status. Since both tree populations grow under a similar flooding regime, these differences can be traced back to the differing nutrient supply between várzea and igapó (Furch 1997), also shown for the study area at Lake Amanã (Rodrigues 2007). In the alluvial soils of the várzea, nutrient concentrations of macroelements such as P, K, Ca and Mg as well as micronutrients such as Fe, Zn, Mn are 5–15 times higher than in the igapó. This difference is also reflected in the living aboveground biomass of trees comparing the two floodplain types where the nutrient stocks are up to four times higher in the várzea than in the igapó.
Parolin and Ferreira (1998) found for some tree species a lower WD in the igapó than in the várzea and suggested that the higher WD in the igapó is an adaptation to low nutrient conditions in their study. The WD of T. barbata was significantly higher in the nutrient-poor igapó (WD = 0.65 ± 0.02 g cm−3) than in the nutrient-rich várzea (WD = 0.78 ± 0.07 g cm−3) (see also Worbes et al. 1995). However, what Parolin and Ferreira (1998) did not consider was that the trees of T. barbata from the igapó grew in an old-growth forest, while those from the várzea originated from a young successional stage. Schöngart (2003) compared growth patterns of T. barbata between várzea forests of different successional stages and found a significantly lower WD in the young successional stage (WD = 0.65 ± 0.07 g cm−3) than in an old-growth forest (WD = 0.84 ± 0.10 g cm−3). Within the floodplain forests of the várzea, the MRI of T. barbata were about twice as high in young successional stages as in the climax stage (Worbes et al. 2001). However, in this study we compare tree growth of T. barbata in old-growth forests at both floodplain types subjected to an almost identical hydrological regime, and we do not find any significant differences in WD. The same holds for V. guianensis indicating no significant differences when comparing trees from igapó and várzea. Schöngart et al. (2005) showed that the legume tree species Macrolobium acaciifolium (Benth.) Benth. (Fabaceae) showed a significantly lower WD in the igapó than in the várzea comparing old-growth forests established at similar elevations. Thus it seems that no general conclusions can be made regarding whether WD of a tree species is higher in the igapó or in the várzea.
However, MRI differs significantly when comparing tree growth of T. barbata and V. guianensis in both floodplain types (Fig. 3). This finding is congruent with earlier studies comparing tree growth of M. acaciifolium in both systems (Schöngart et al. 2005). MRI of 45 tree species in the igapó (MRI = 1.7 mm) was less than the half the MRI of 158 species from the várzea (MRI = 3.5 mm) (Worbes 1997). Also at the stand level a recent study confirmed much lower carbon sequestration rates in the aboveground coarse woody biomass of old-growth forests in the igapó when compared to old-growth forests at identical elevations in the várzea (Stadtler 2007). The lower increment rates of tree species and the lower productivity of stands in the igapó system indicate a different forest dynamic, which has to be considered in conservation plans for preservation and sustainable management.
For centuries, the Amazonian floodplains have been used and settled by a human population of high density that carried out agriculture, pasture, fishing and hunting, as well as the extraction of timber and non-timber products (Nebel and Meilby 2005; Schöngart et al. 2007) and floodplain forests are one of the most threatened forest ecosystems in the Amazon. One of the biggest obstacles in the sustained management of tropical forests is obtaining reliable data on the growth and yield of trees. Achieving sustainable yields requires species-specific management of timber resources, in which the different growth strategies of tree species and the varying site conditions are considered. Unfortunately, species-specific and site-specific management criteria based on wood growth data in the tropics are quite rare (Stahle et al. 1999; Schwartz et al. 2002; Sokpon and Biaou 2002; Nebel and Meilby 2005; Schöngart et al. 2008). For Amazonian forests, the restrictions in felling cycles and MLDs established in IN number 5 of IBAMA are estimations which are not derived from scientific data. The application of inadequate management criteria for a certain tree species under certain site conditions due to missing data on tree growth and natural regeneration can have negative effects on population structures. In this study, estimates for felling cycles vary almost fourfold between 14.0 years (V. guianensis at várzea site) and 55.6 years (T. barbata at igapó site) (Fig. 6). Consequently, polycyclic systems operating with fixed felling cycles of 25–35 years would tend to over-harvest the timber stocks in the igapó and to under-harvest timber stocks in the várzea.
The igapó forests are especially vulnerable to inadequate timber management due to the slow dynamical processes reflected by the significantly lower MRI when compared to the várzea. The sustainable use of timber stocks in the nutrient-poor igapó is, under current management options, not sustainable due to low productivity. It is arguable, therefore, that a better use for floodplain forests of the igapó is to exclude them from timber-resource management for permanent protection as habitat for their highly diverse and partially endemic flora and fauna. In the várzea, however, a sustainable timber harvest is possible, but requires species-specific information on tree growth.
This study was financed by the FEPIM Project 044/2003, GEOMA (Áreas Alagáveis), the INPA/Max-Planck Project as well as the Project 680021/2005–1 of the Brazilian Research Council (CNPq) “Studies to sustain the community-based production in floodplain forests of the Mamirauá and Amanã Reserves”. We are thankful for the comments of an anonymous reviewer.
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