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Scientia Agricola

Print version ISSN 0103-9016

Sci. agric. (Piracicaba, Braz.) vol.69 no.1 Piracicaba Jan./Feb. 2012

http://dx.doi.org/10.1590/S0103-90162012000100005 

ECOLOGY

 

Height-diameter relationships of tropical Atlantic moist forest trees in southeastern Brazil

 

 

Marcos Augusto da Silva ScaranelloI, §; Luciana Ferreira AlvesII, III; Simone Aparecida VieiraI, ; Plinio Barbosa de Camargo1, *; Carlos Alfredo JolyIV; Luiz Antônio MartinelliI

IUSP/ CENA - Lab. de Ecologia Isotópica, C.P. 96 - 13416-000 - Piracicaba, SP - Brasil
IIUniversity of Colorado/Institute of Arctic and Alpine Research (INSTAAR), PO Box 450 - 80309 - Boulder, CO - USA
IIIInstituto de Botânica/Núcleo de Pesquisa em Ecologia, C.P. 3005 - 01031-970 - São Paulo, SP - Brasil
IVUNICAMP/Instituto de Biologia, C.P. 6109 - 13083-970 - Campinas, SP - Brasil

 

 


ABSTRACT

Site-specific height-diameter models may be used to improve biomass estimates for forest inventories where only diameter at breast height (DBH) measurements are available. In this study, we fit height-diameter models for vegetation types of a tropical Atlantic forest using field measurements of height across plots along an altitudinal gradient. To fit height-diameter models, we sampled trees by DBH class and measured tree height within 13 one-hectare permanent plots established at four altitude classes. To select the best model we tested the performance of 11 height-diameter models using the Akaike Information Criterion (AIC). The Weibull and Chapman-Richards height-diameter models performed better than other models, and regional site-specific models performed better than the general model. In addition, there is a slight variation of height-diameter relationships across the altitudinal gradient and an extensive difference in the stature between the Atlantic and Amazon forests. The results showed the effect of altitude on tree height estimates and emphasize the need for altitude-specific models that produce more accurate results than a general model that encompasses all altitudes. To improve biomass estimation, the development of regional height-diameter models that estimate tree height using a subset of randomly sampled trees presents an approach to supplement surveys where only diameter has been measured.

Keywords: tree height, elevation


 

 

Introduction

The Brazilian Atlantic Forest (hereafter referred to as Atlantic Forest) is a biodiversity hotspot considered as one of the global centers of tree diversity and endemism (Guedes-Bruni et al., 2009) and one of the most threatened tropical forest regions in the world (Myers et al., 2000). Although the Atlantic Forest is one of the most diverse biomes on Earth there is limited information regarding the structure and biomass of this forest (Alves et al., 2010; Vieira et al., 2008).

Tree biomass stocks of tropical forests are traditionally estimated using forest inventory data from sample plots (Brown, 1997) and allometric models that relate tree dry mass to easily measurable variables such as diameter at breast height (DBH) and total height (Chave et al., 2005). These variables, along with wood density (Baker et al., 2004), are applied in general allometric models (Chave et al., 2005) when site-specific models are not available. As there are no available allometric models developed destructively for old-growth Atlantic forest sites (Alves et al., 2010; Vieira et al., 2008), a pantropical allometric model developed by Chave et al. (2005) for tropical moist forests has been suggested to estimate the live tree aboveground biomass (AGB) for the coastal tropical Atlantic forest using DBH, wood density and total height (Alves et al., 2010).

Although useful, the measurement of tree height in tropical forest inventories is time-consuming and expensive. As a consequence, there are few forest models that use tree height as an independent variable (Fang and Bailey, 1998). An alternative to height measurement for all individuals is the application of site-specific height-diameter models that relate DBH with measured tree height (Batista et al., 2001). However, height-diameter relationships vary within a geographic region (Peng et al., 2001) due to species composition and local environmental conditions. Hence, there is a growing consensus that the use of site specific height-diameter models fitted using field measures of tree height is an important alternative to reduce uncertainties in forest biomass estimation in tropical forests (Chave et al., 2005; Feldpausch et al., 2010; Nogueira et. al., 2008) and to study forest structure. Therefore, the main objective of this study is to fit and investigate the relation between DBH and tree height across sites located at different altitudes in the Atlantic Forest of the southeast region of Brazil.

 

Materials and Methods

This study was carried out in the São Paulo State Park of Serra do Mar (PESM), southeast Brazil, and nearby the Picinguaba and Santa Virginia stations (44°48' W, 23° 22' S). The state park contains 47,500 ha of diverse tropical ecosystems, including mangroves, restinga (sandy coastal plain forests), and humid tropical forests from sea level up to 1,200 m a.s.l. (SMA, 1998). According to Veloso et al. (1991), the Atlantic Forest, at the latitude of this study, can be subdivided into vegetation types by altitude as follows: lowland forest, submontane forest and montane forest. Along the coastline, there is another Atlantic forest type known as restinga or coastal seasonally flooded forest (Araújo, 1992). Mean annual rainfall in the study area is c. 2600 mm, and monthly average temperature ranges from 17.6 °C to 24.7 °C (Sentelhas et al., 1999) varying according to altitude.

From 2006 until 2007, 13 one-hectare permanent plots were established along an altitudinal transect at the Serra do Mar state park to evaluate forest diversity and ecosystem function variation within the north coastal Atlantic Forest of São Paulo state (Alves et al., 2010; Joly et al., 2008). Aiming to represent the range of local environmental conditions, four one-hectare permanent plots (100 × 100 m) were established at varying altitudes: in the lowland forest at 100 m altitude, in the submontane forest at 400 m altitude and in the montane forest at 1,000 m altitude. Due to its limited representativeness within the Park relative to the other forest types, only one plot was established at sea level in the restinga forest. All trees > 4.8 cm DBH were tagged and mapped to a horizontal distance of ± 10 cm in each permanent plot, and tree circumference was measured within ± 1 mm (Alves et al., 2010). Soils in lowland, submontane and montane forest sites are classified as Inceptisol (USDA taxonomy) with more than 50 % of sand content and in the restinga forest the soil is classified as Quartzipsamment (USDA taxonomy) with more than 80 % of sand content (Alves et al., 2010). These soils have in common a high sand content, with low pH, low phosphorus concentration, low sum of bases and high aluminum saturation. The density of trees, palms and tree ferns with DBH > 4.8 cm ranged from 1467 up to 1885 stems ha-1 (average of 1,626 stems ha-1) in the restinga forest, 1,170 up to 1,298 stems ha-1 (average of 1,230 stems ha-1) in the lowland forest, 1,517 up to 1,926 stems ha-1 (average of 1,727 stems ha-1) in the submontane forest and 1,454 up to 1,834 stems ha-1 (average of 1,723 stems ha-1) in the montane forest (Alves et al., 2010). The most rich families in these forests sites are: Myrtaceae, Rubiaceae, Fabaceae, and Lauraceae

Common canopy tree species with DBH > 30 cm include: Hieronyma alchorneoides Allemão, Virola bicuhyba (Schott ex Spreng.) Warb, Eriotheca pentaphylla (Vell.) A. Robyns, Sloanea guianensis (Aubl.) Benth, Cryptocaria mandiocanna Meisn., Ecclinusa ramiflora Mart., Licania hoehnei Pilg. and Chrysophyllum viride Mart. & Eichler ex Miq. For a full description of the sampling design and stand site characteristics, see Alves et al. (2010) and Sousa Neto et al. (2010). Hereafter we will refer to these forest types by the altitudes of occurrence.

Using the database generated by Alves et al. (2010), we randomly selected 268 trees stratified by altitude of occurrence and by DBH class to perform tree height measurements. The DBH classes were: < 10 cm, 10-30 cm, 30-50 cm and > 50 cm. We did not include palms in our analysis. Approximately the same number of randomly selected individuals was measured for each diameter class.

Tree height was set as the vertical distance measured from ground to the topmost live leaf. A telescoping measuring rod (Crain Enterprise, model no. 90182) was used to measure the height of trees up to 16 m height. For trees taller than 16 m we used a handheld laser range finder (Impulse-200LR, Laser Technology Inc., Englewood, Colorado) that measures distance and calculates height using an angular measurement from a clinometer integrated into the instrument.

There are numerous studies that relate height and diameter for different species and forest regions. In tropical forests, there are few studies reporting height-diameter models and limited information about their performance (Batista et al., 2001; Fang and Bailey, 1998; Feldpausch et al., 2010). Here, we propose a performance test of the eleven linear and non-linear height-diameter models (Table 1), tested earlier by Fang and Bailey (1998) and Batista et al. (2001) in other tropical forests.

 

 

The non-linear and linear models were fitted using the functions "Nonlinear Least Squares" and "Fitting linear models" of the R statistical software packages (R Development Core Team, 2011). To assess the performance of height-diameter models and then to test the effect of altitude on estimates, we applied the Akaike Information Criterion (AIC) (Burnham and Anderson, 2002; Chave et al., 2005). The formula of AIC used as the criterion for model selection (Chave et al., 2005) is:

AIC = -2 Log(L) + 2p

where L is the likelihood of the fitted model and p is the total number of parameters in the model. The best model of the eleven tested models of this database will minimize the AIC value (Burnham and Anderson, 2002). Our analysis was structured as follows: (i) first, we pooled the data (using the subset of 268 trees with measured heights) to select the best model as described above; (ii) second, using the best overall model(s) we fitted the best site-specific height diameter model and calculated the AIC value for each altitude; (iii) finally, we compared the pooled AIC value with the AIC from the sum of the site-specific height-diameter models to test the altitudinal effect (because the data came from the same source; see Burnham and Anderson, 2002). This sum matches the performance of the selected height-diameter model taking into account the site-specific altitude effect, and so can be compared with the pooled model AIC value (Burnham and Anderson, 2002). If the pooled model has a smaller AIC value, there is no altitudinal effect on tree height estimates. The maximum tolerance used to select the best models using the AIC value was equal to Log8 or 2 (Burnham and Anderson, 2002). Although our data apparently show some degree of heteroscedasticity (Figure 1), we decided to acknowledge it and then proceed with our model selection and tests since AIC is not sensitive to the heteroscedasticity (Burnham and Anderson, 2002).

 

Results and Discussion

For the pooled data set the non-linear Weibull and Chapman-Richards models performed best (Table 2). All parameters of the best fit models were significant (p < 0.01), with the exception of the b parameter of the Chapman-Richards model in the 100 m and 400 m forests (Table 3). Consequently, we will analyze the height-diameter relationships variation using only the Weibull height estimates. The height-diameter fits are shown in Figure 1 separated by site/altitude.

 

 

Non-linear height-diameter models have biological interpretations and are less sensitive to individual points, making them more stable and more reliable for data extrapolation (Batista et al., 2001). Batista et al. (2001) and Fang and Bailey (1998) also found better performance of non-linear height-diameter models in other tropical forests. The Weibull model has been widely used to describe tree allometric relationships, especially for modeling height-diameter relationships (Batista et al., 2001; Fang and Bailey, 1998; Muller-Landau et al., 2006).

The site specific height-diameter Weibull and Chapman-Richards models (AIC from pooled model with the altitude effect in the Table 3) had better performance than the pooled model fit using the full database (AIC from pooled model without the altitude effect in the Table 2). The latter model had the highest AIC value (Table 2 and Table 3), indicating the effect of altitude on tree height estimates and demonstrating the difficulty of extrapolation using a single height-diameter model along the altitudinal gradient. The same result was found by Tasissa et al. (1997) and (Trincado et al., 2007) probably because the use of site-specific equations accounts for local geographic effects in growth patterns of tree communities. This could be especially true along our altitudinal gradient, where slopes are steeper at 400 m and 1,000 m than at sea level or at 100 m altitude (Alves et al., 2010).

The height-diameter relationship was marginally different among forest types up to a DBH of approximately 30 cm (Figure 2). Above this DBH the relationship for the sea level forest was distinct from the other forests. For a given DBH greater than 30 cm, trees at the sea level are shorter than trees at higher altitudes (Figure 2). However, for a constant DBH of 100 cm, tree heights decrease with increasing altitude (Figure 2) if the sea level forest is excluded.

 

 

At sea level, trees are seasonally flooded during heavy rain events and particularly during the wet season when the soil remains flooded for several weeks (Scarano, 2002). Additionally, soils at the sea level have the highest sand content and the lowest nutrient content among all soils along the altitudinal gradient (Sousa Neto et al., 2011). Possibly, these stress factors contribute to the small stature of trees established in this forest type. With exception to the sea level, large DBH tree heights tend to decline with increasing altitudes (Figure 2). The same trend was found by Lieberman et al. (1996), studying an altitudinal gradient in North of Barva Vulcan, Costa Rica.

What are the possible causes for this variation in height-diameter relationships along the altitudinal gradient? Soils at 100 m, 400 m and 1,000 m are Inceptisols, with no significant depth difference along the altitudinal gradient (Alves et al., 2010), and with low nutrient content. They are less sandy and have higher nutrient content than soils at sea level (Sousa Neto et al., 2010). More important, there are no differences in soil depth along the altitudinal gradient (Sousa Neto et al., 2010). However, at higher altitudes, air and soil temperatures are lower, with a high incidence of low level clouds and fog formation that reduces annual irradiance (Sousa Neto et al., 2010). These conditions and strong winds are commonly cited as environmental characteristics that distinguish montane from lowland tropical rain forests (Grubb, 1977; Tanner, 1980) and could be the cause of lower tree heights at higher altitudes. Frequently, strong winds cause decrease of tree stature in tropical forests at high altitude (Lawton, 1982). Exposed trees that grow under stress caused by strong winds tend to grow more in diameter than in height, increasing stem strength (Lawton 1982, 1984).

As well as the difference in slope of the terrain is a plausible cause, the local topographic variation among forest types in this altitudinal gradient (see Alves et al., 2010) might be a factor controlling light availability and ultimately, tree height. Montane and submontane forest are located in steeper terrains when compared to the other forest types, so that the vertical distribution of light is expected to be more asymmetric than in flat areas (Alves et al., 2010). As the trees have the crown exposed to more light, they are shorter, reach larger diameters and have also larger crowns (Alves and Santos, 2002).

While we are not able to pinpoint which of these climate conditions is the cause for the observed altitudinal gradient in tree heights we speculate that all of these conditions as well as the difference in the slope of the terrain are plausible causes.

Finally, the tallest statured forest (100 m altitude) was compared with height-diameter models from other studies within the tropical Amazon forest and showed extensive differences in tree stature among these forests (Figure 3). For trees of or above 20 cm DBH, the tropical Atlantic forest had smaller stature than Amazonian forests in Brazil (Asner et al., 2002; Nogueira et al., 2008). For trees with 100 cm DBH, this difference reached 76 % when compared with trees in central Amazon. This result supports the need to use tree height as an independent variable in biomass allometric models used to compare different tropical forests, especially in sites where regional site specific biomass models are not available (Chave et al., 2005; Feldpausch et al., 2010; Nogueira et al., 2008). This is especially important in the case of the coastal Atlantic forest of southeastern Brazil due to various limitations resulting in vegetation suppression. Therefore, an alternative solution to the development of biomass allometric equations based on destructive measurements (harvested trees) is the application of general pantropical models including height to estimate live above ground biomass (Vieira et al., 2008).

 

 

Conclusions

The effect of altitude on tree height estimates was evident and emphasize the need for altitude-specific models that produce more accurate results than a general model that encompasses all altitudes. Tree height has a strong influence on the estimate of live aboveground biomass made by allometric models. To improve biomass estimation, the development of regional height-diameter models that estimate tree height using a subset of randomly sampled trees presents an approach to supplement surveys where only diameters have been measured.

 

Acknowledgements

This work was supported by FAPESP, through a master's scholarship provided to M.A.S. Scaranello (proc. nº. 07/06821-5) and as part of the Thematic Project Functional Gradient (Process Number 03/12595-7), within the BIOTA/FAPESP Program - The Biodiversity Virtual Institute (www.biota.org.br). COTEC/IF 41.065/2005 and IBAMA/CGEN 093/2005 permit. We thank Eliana Simões and João Paulo Villani for their logistic support at Picinguaba and Santa Virgínia field stations. We thank Edmar A. Mazzi for field assistance. Especially thanks to Michael Keller for the use of the laser range finder for height measurements, and helpful comments in an earlier draft. We also thank João L.F. Batista for helpful comments in an earlier draft. Maria Hunter kindly reviewed the English language in the final version of this manuscript.

 

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* Corresponding author
pcamargo@cena.usp.br

§Present address: UNICAMP/Instituto de Biologia, C.P. 6109 – 13083-970 – Campinas, SP – Brasil.
Present address: UNICAMP/Núcleo de Estudos e Pesquisas Ambientais – R. dos Flamboyants, 155 – 13083-867 – Campinas, SP – Brasil.

Edited by: Eros Artur Bohac Francisco / Luís Reynaldo Ferracciú Alleoni

Received June 18, 2010 Accepted September 30, 2011

 

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