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1 January 2020 Forest fragments of the Andean piedmont as carbon sinks
Ana M. Aldana, Pablo R. Stevenson
Author Affiliations +
Abstract

Some tropical countries, such as Colombia, are venturing into the international carbon market by means of avoided deforestation programs, i.e., they seek carbon credits by not cutting down forests. Consequently, basic information about carbon storage in different forest types is urgently needed. We describe the tree community dynamics of forest fragments in cattle ranches of the western Orinoco basin, and their relationship to the forests’ ability to accumulate carbon. We re-sampled three 1-ha vegetation plots after six and seven years of establishment. We found that these forests have different population dynamics; smaller fragments have negative net population change, but the dynamics allow for an annual carbon accumulation rate of around 0.57 Mg ha−1. This rate is similar to the rate reported for some mature Amazon forests and may be attributed to high soil fertility.

Introduction

Carbon storage estimation in different ecosystems has become a central subject in conservation science, because natural ecosystems can mitigate climate change effects by acting as carbon sinks, limiting the availability of this greenhouse gas in the atmosphere (Ashton, Tyrrell, Spalding, & Gentry, 2012; Pan, Birdsey, Phillips, & Jackson, 2013). In tropical forests, which account for 55% of the carbon stored in the world’s forests, 65% of the carbon is stored as biomass in the roots, trunks, and leaves of woody plants (Pan et al., 2011). In Colombia, a tropical country, avoided deforestation initiatives have emerged during the last decade from a variety of stakeholders such as the agriculture and livestock industries, which hope to mitigate the damage of their own productive activities while offering the service of carbon storage to other productive sectors (Fedegan, 2006; Fedepalma, 2013). However, the impact of these initiatives is still unknown, because the carbon stocks in Colombia have been estimated only for primary forests (Alvarez et al., 2012; Phillips et al., 2016; Sierra et al., 2007).

High deforestation rates in Colombia have left vast areas of fragmented and secondary forests (Phillips et al., 2016). These forests, if conserved and restored, could be useful for carbon trade (Saatchi et al., 2011). Research on land-use changes and ecosystem services is still scarce (Etter, McAlpine, Wilson, Phinn, & Possingham, 2006; Rodríguez Eraso, Armenteras-Pascual, & Retana Alumbreros, 2012; Sánchez-Cuervo, Aide, Clark, & Etter, 2012) and is needed for planning conservation strategies in geographic areas dedicated to agriculture and livestock.

Estimations of carbon accumulated in tropical forests depend on climate, soil type (since in cold climates and anoxic conditions carbon usually accumulates in soils), and the structure of plant communities and their productivity (Carvalhais et al., 2014; Lähteenoja, Ruokolainen, Schulman, & Oinonen, 2009). The amount of carbon in plants is divided in two components, above and below ground, which are estimated based on allometric equations (Gibbs, Brown, Niles, & Foley, 2007). However, these equations are more common for aboveground biomass (AGB), using information on the diameter of trees at breast height (DBH) and wood density (Alvarez et al., 2012; Chave et al., 2005). In some cases, equations can also include tree height (Feldpausch et al., 2012; Goodman et al., 2013). The ecosystem service related to carbon storage from the atmosphere may also depend on forest dynamics, because a forest in which the recruitment of new trees is higher than mortality would show high accumulation rates (if variables such as wood density and tree height are kept constant) (Johnson et al., 2016).

Cattle ranching is a productive activity involving deforestation, the use of forest resources, fragmentation, and edge effects associated with high mortality of large trees (Laurance, Delamónica, Laurance, Vasconcelos, & Lovejoy, 2000), which are the main drivers of AGB stocks (Slik et al., 2013). Fragments, especially small or narrow forest fragments, have a strong relationship between perimeter and area, and thus are susceptible to large edge effects (Nascimento & Laurance, 2004). Forest fragments show drastic changes in plant species composition, because there is high recruitment of pioneer species near edges (Laurance et al., 2006). As pioneer trees are characterized by low wood density and usually short stature (Muller-Landau, 2004), it is expected that forest fragments should have greater abundance of low wood density species. In addition, the mortality of large trees caused by more wind exposure and changes in abiotic conditions should exacerbate the pattern (Laurance et al., 2011).

Our main objective is to describe the tree community dynamics of forest fragments in cattle ranches of the Orinoco Basin, located in the Andean piedmont, and to determine their relationship to carbon accumulation. Specifically, we want to: 1. Determine growth, mortality, and recruitment rates of woody plant species in these forest fragments; 2. Quantify the variation in wood density of tree species in these fragments; and 3. Estimate the carbon stocks and carbon accumulation rates of the forest fragments. Considering the predictable changes in the tree community, we expected to find a low estimate of carbon storage in the forest fragments and a negative balance of carbon accumulation over time.

Methods

Field study

The municipality of San Martín (Meta, Colombia) is one of the oldest cities in the region, founded in 1585. The surrounding region has since been used for extense cattle ranching in large areas. The original landscape was mainly continuous forest from the foothills of the Andes, with some natural savannas to the southeast. Land-use change estimations from the Colonia (Etter, 2015; Etter, Sarmiento, & Romero, 2010) show that fragmentation has been occurring since the late 1600s, resulting in a landscape of riparian forest fragments (Appendix 1).

The remaining forest in the area has been categorized as tropical moist forest (Romero Ruíz, García, García, i Pascual, & Ruíz, 2004). The mean temperature is 27.5°C, ranging from 19 to 35°C (Stevenson, 2011). Annual rainfall in the region is usually between 2,600 and 3,000 mm and is seasonal, with two dry months with less than 100 mm (usually January and February) (Stevenson, Castellanos, Cortés, & Link, 2008). During the last three decades cattle ranches have been increasingly replaced with oil palm plantations, making the Meta Department the most extensive producer in Colombia (Wagner, Castro, & Stevenson, 2007). It has been observed that when grasslands are free from human intervention, a secondary forest is established (Stevenson, 2011).

We re-sampled three forest plots (1 ha) in forest fragments in three cattle ranches in San Martín (Appendix 1). We established the plots during the first semester of 2005 (Stevenson & Aldana, 2008) and the second semester of 2009. Fragment 1 has an approximate area of 28 ha, and the 1-ha plot (3°36′30.40″N, 73°38′20.72″W) was re-sampled six years after establishment (second semester of 2011); Fragment 2 has an approximate area of 23 ha, and the 1-ha plot (3°37′42.02″N, 73°38′19.86″W) was re-sampled seven years after establishment (second semester of 2012); Fragment 3 is the biggest remaining fragment in the municipality, 1,000 ha in area; the 1-ha plot (3°34′54.9″N, 73°27′14.7″W) was re-sampled six years after establishment (second semester of 2015).

During the re-sampling of the plots we measured the increased DBH of trees greater than 10 cm, recording the number of dead individuals and new recruits. We measured height of 76% of the individuals in our database, using a laser clinometer. We collected wood cores to determine wood density, here measured as Wood Specific Gravity (WSG sensu, Williamson & Wiemann, 2010), of at least one individual from the most abundant species, following the protocol proposed by Chave (2005). Green volume was calculated using the dimensional method, and wood cores were oven dried at 103°C for 72 hours.

Data analysis

We compared the census data from 2005 (Stevenson & Aldana, 2008) and 2009 with census data from 2011 – 2015 to determine annual growth, mortality, and recruitment rates for each plot using the formulae presented by Sherman and collaborators (Sherman, Fahey, Martin, & Battles, 2012).

We calculated above ground biomass (AGB) for each sampling year, using the allometric equations for Tropical Moist Forest of the type I, which take into account DBH, height and wood density. We used the best predictive model for neotropical moist forests (Type I.3) (Alvarez et al., 2012). Biomass calculations for other woody life forms were done using different allometric equations to minimize errors; for palms we calculated the biomass using the equations proposed by Goodman et al. (2013), and for lianas we calculated the biomass using the equation proposed by Schnitzer, DeWalt, and Chave (2006).

For cases where the WSG was not measured by us (33% of species), we used information on species measured by our research group, following the same protocols (Casas et al., 2016), and values reported in the Dryad global database (Chave et al., 2009; Zanne et al., 2009). For species with no reported WSG values in either of the databases, we used the mean for the genus or family (using a combined database with the three sources mentioned previously), assuming that this trait is phylogenetically conserved (Chave et al., 2006). To evaluate whether mean WSG was different among plots we performed an ANOVA and a Tukey test, using the information from the year of re-sampling.

The net change in AGB was calculated as the difference between the AGB in 2011 – 2015 and the AGB in 2005–2009, divided by the number of years between each sampling. We compared the results among plots and between sampling years with a t-test.

Results

Population Dynamics

The three forest fragments have different mortality and recruitment rates (Table 1). Recruitment rate for fragments 1 and 2 was lower than fragment 3, resulting in a negative change in stem densities. Only fragment 3 showed a positive change in stem density, although relative tree growth rate was lower in fragment 3 than fragments 1 and 2.

Table 1.

Community dynamics of forest fragments: Recruitment, mortality, net population change and average relative growth rates of the tree communities of three forest plots (1ha) in fragments located in cattle ranches of the Andean piedmont in Meta, Colombia.

10.1177_1940082916667339-table1.tif

Wood Specific Gravity

The distribution and mean values of Wood Specific Gravity for woody plant species differ among forest fragments (Figure 1). The analysis showed differences among fragments (ANOVA, F = 0.26, P < 0.01) and a Tukey test showed that mean WSG is lower in fragment 1.

Figure 1.

Histogram of the distribution of wood specific gravity values for tree species in three forest fragments of the Andean piedmont in Meta, Colombia. Values were assigned to each individual stem from a species average calculated based on the measurements made by us in the present study and complemented with information from unpublished data (Casas et al., 2016). For species missing in our database (10%) we used information from Global Data Bases (Zanne et al., 2009). Dotted lines represent the mean values for each fragment.

10.1177_1940082916667339-fig1.tif

Above Ground Biomass Change

The estimations of the rate of biomass change were positive for fragments 1 and 3 and negative for fragment 2 (Figure 2). These forests fragments, on average, are accumulating 0.57 Mg of AGB per hectare per year. Sierra et al. (2007) calculated that carbon biomass content in moist tropical forests is around 45%, from which we estimate that, on average, each hectare of these forest fragments is accumulating 0.26 Mg of carbon every year.

Figure 2.

Above Ground Biomass change in three forest plots (1-ha) in fragments located in cattle ranches of the Andean piedmont in Meta, Colombia, after 6 and 7 years of establishment.

10.1177_1940082916667339-fig2.tif

Growth rate and Wood Specific Gravity

Given the surprising result of positive AGB change and negative stem density change in fragments 1, we explored the possibility of the mortality rate being compensated by the rapid growth of some tree species. A negative relationship between growth rates and wood density is expected in contexts of r and K strategies. Although we did not find this relationship, we found high WSG values (WSG > 0.6) for some species with high relative growth rate (RGR) (RGR > 2%). These results are summarized in Figure 3, which was drawn with species that had more than two individuals with observations of RGR in our database.

Figure 3.

Relationship between Relative Growth Rate and Wood Specific Gravity for 63 tree species (species in our data set with more than 2 observations), found in forest fragments located in cattle ranches of the Andean piedmont in Meta, Colombia. Species colored in red may be of interest for native wood production and ecosystem restoration (WSG>0.6, RGR>2%). Species names have been shortened for easier reading, species names from top to bottom are: Eschweilera cabrerana (cabo de hacha), Hieronyma oblonga (candelo), Hirtella americana (moradito), Garcinia madruno (madroño), Eugenia sp., Alchornea discolor, Licania subarachnophylla.

10.1177_1940082916667339-fig3.tif

Discussion

Population Dynamics

We found that the smaller fragments have a negative change in stem densities, due to a mortality rate higher than the recruitment rate. A higher mortality rate can be attributed to selective logging that has been occurring in these fragments in past years. Similarly, a lower recruitment rate may be due to intensive use by the cattle that go daily into the forest to drink water from the streams within these fragments. Although we do not have measurements of the effect of cattle in these forests, cattle presence in the forest may cause high seedling mortality and soil compaction (Hernández-Vargas, Sánchez-Velásquez, Carmona-Valdovinos, & Cuevas-Guzmán, 2000).

This idea is supported by a positive change in stem densities for fragment 3, which is isolated from cattle presence. Also, the negative effect of selective logging may be attenuated by the size of the fragment.

Wood Specific Gravity

We found that fragment 1 has a lower WSG mean value, which is possibly an effect of selective logging and low species richness (67 species per hectare). Fragment 2 is not richer in species (69), but some species are not shared, which allows for a higher frequency of species with higher WSG values (Figure 1). Fragment 3 is the most diverse in species (127) and it is also the fragment with the greatest frequency of species with high WSG values. This result is consistent with the reduction in fragment size. However, in our study system selective logging may have eliminated individuals of some old-growth species from the fragments, specially fragment 1 (Stevenson & Aldana, 2008).

Biomass Stocks and Above Ground Biomass Change

Comparing our results with previous estimations, based on extrapolations (Phillips et al., 2011), we found that these forests have lower biomass stocks than previously estimated.

We found that fragment 2 had a negative change in AGB which maybe a consequence of a negative change in stem density; opposite to this pattern, fragment 1 had a negative stem density change, but a positive rate of AGB accumulation, which may be due to a high RGR (see below). Although fragment 3 is more conserved than the other two fragments, it has not reached a neutral carbon balance as have primary forests of the Amazon (Phillips et al., 1998) and it accumulated more AGB per year than the other fragments. In the tropics, the Amazon region has been subject of many studies of AGB accumulation, which show that Amazon primary forests tend to be on an equilibrium state in terms of carbon storage (Hernández-Vargas et al., 2000). Therefore, this result can be explained by past removal of large trees for domestic wood use, which allows for growth and recruitment of competing trees. Fragments 1 and 2 also have a higher RGR than fragment 3, which means that some tree species in these fragments may have high growth rates and high WSG values (see below).

Because these three forest plots may not be representative of all the forest fragments in the Orinoco Basin, the results of this study should be compared with other studies from the same region, in order to reach sound conclusions about the carbon dynamics of forests fragments of the region.

Growth rate and Wood Specific Gravity: Promising Tree Species

The tree species we highlight in Figure 3: Eschweilera cabrerana (cabo de hacha), Hieronyma oblonga (candelo), Hirtella americana (moradito), Garcinia madruno (madroño), Eugenia sp., Alchornea discolor, Licania subarachnophylla could be considered promising for restoration and reforestation programs in the Andean piedmont, as these are native species that grow fast and could enhance the ecosystem services of the forest by accumulating more carbon in their trunks (given their wood density).

Implications for conservation

Although AGB stocks in these forest fragments are lower than in Amazonian primary forests (Baraloto et al., 2013), we found that these forests are capable of accumulating at least 0.26 Mg of carbon every year, very similar to many primary forests in the Neotropics (Phillips, Lewis, Baker, Chao, & Higuchi, 2008). We believe this accumulation rate is due to fertile soils and could be enhanced by reducing selective logging and cattle use of the forest. If well managed and protected, these fragments could be used by cattle ranchers, oil palm producers, and other productive sectors of the region either to compensate for the impacts of their activities or to receive payment for ecosystem services that enhance forest cover and connectivity between forest fragments. Connectivity among these forest fragments would not only benefit tree species populations, but also populations of big mammals like Panthera onca and other native fauna. We found some native tree species that have high values of WSG and are faster growing than other native species; these species should be studied for their potential for timber production, and if successful, may be used to replace Eucalyptus pellita (eucalipto – Red Mahogany) and Pinus caribea (pino - Caribbean Pine). Plantations of the latter species are replacing natural forest and savanna ecosystems in the region.

Appendix 1

Detail of the study area in the municipality of San Martín (Meta, Colombia) in the western Orinoco Basin. Yellow squares show the location of the three 1-ha vegetation plots in the forest fragments. Areas shaded in orange are oil palm plantations, which may be confused with forest fragments. Light green areas are pastures for cattle ranching. Images were created using GoogleEarthPro in June 2016.

10.1177_1940082916667339-fig4.tif

Acknowledgements

The Sánchez-Rey family and the Enciso family were very kind to let us work on their premises; they also helped with fieldwork logistics. Sasha Cárdenas, Marcela Córdoba, Indira León, Camila Monje, Ángela Perilla, Erika Rodríguez, Vanessa Rubio, Luis Francisco Henao, Eduardo Pinel, Diana Acosta, Edna Beltrán, Efraín Rincón, Camilo Quiroga, Maria Juliana Pardo, Felipe Aramburo and Ángela Sánchez helped with the re-sampling of the plots and wood specific gravity measurements. We thank an anonymous reviewer who helped us improve the quality of the manuscript.

Declaration of Conflicting Interests

The author(s) declared no potential conflicts of interest with respect to the research, authorship, and/or publication of this article.

Funding

The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: The authors received finantial support from Fondo de Investigaciones of the Facultad de Ciencias at Universidad de Los Andes. AMA received support from the Lóréal – Unesco grant For Women in Science.

References

1.

Alvarez, E., Duque, A., Saldarriaga, J., Cabrera, K., de las Salas, G., del Valle, I., Rodríguez, L., (2012) Tree above-ground biomass allometries for carbon stocks estimation in the natural forests of Colombia. Forest Ecology and Management 267: 297–308. Google Scholar

2.

Ashton, M., Tyrrell, M., Spalding, D., & Gentry, B. (2012). Managing forest carbon in a changing climate (M. S. Ashton, M. L. Tyrrell, D. Spalding, & B. Gentry Eds.). Dordrecht, Netherlands: Springer Netherlands. Google Scholar

3.

Baraloto, C., Molto, Q., Rabaud, S., Hérault, B., Valencia, R., Blanc, L., Thompson, J., (2013) Rapid simultaneous estimation of aboveground biomass and tree diversity across neotropical forests: A comparison of field inventory methods. Biotropica 45: 288–298. Google Scholar

4.

Carvalhais, N., Forkel, M., Khomik, M., Bellarby, J., Jung, M., Migliavacca, M., Reichstein, M., (2014) Global covariation of carbon turnover times with climate in terrestrial ecosystems. Nature 514: 213–217. Google Scholar

5.

Casas, L., Aldana, A.M., Henao-Diaz, F., Villanueva, B., & Stevenson, P. R. (2016). Specific gravity of woody tissue from lowland Neotropical plants: Variance among forest types. Manuscript submitted for publication. Google Scholar

6.

Chave, J. (2005). Measuring wood density for tropical forest trees: A field manual for the CTFS sites. Pan-Amazonia. Retrieved from  http://www.rainfor.net/upload/ManualsEnglish/wood_density_english[1].pdfGoogle Scholar

7.

Chave, J., Andalo, C., Brown, S., Cairns, M. A., Chambers, J. Q., Eamus, D., Yamakura, T., (2005) Tree allometry and improved estimation of carbon stocks and balance in tropical forests. Oecologia 145: 87–99. Google Scholar

8.

Chave, J., Coomes, D., Jansen, S., Lewis, S. L., Swenson, N. G., Zanne, A. E., (2009) Towards a worldwide wood economics spectrum. Ecology Letters 12: 351–366. Google Scholar

9.

Chave, J., Muller-Landau, H. C., Baker, T. R., Easdale, T. A., Hans Steege, T. E. R., Webb, C. O., (2006) Regional and phylogenetic variation of wood density across 2456 neotropical tree species. Ecological Applications 16: 2356–2367. Google Scholar

10.

Etter, A. (2015). La transformación del uso de la tierra y los ecosistemas durante el periodo colonial en Colombia (1500–1800). La Economía Colonial de la Nueva Granada, (pp. 1–44). Bogotá, Colombia: Fondo de Cultura Económica; Banco de la República. Google Scholar

11.

Etter, A., McAlpine, C., Wilson, K., Phinn, S., Possingham, H., (2006) Regional patterns of agricultural land use and deforestation in Colombia. Agriculture, Ecosystems & Environment 114: 369–386. Google Scholar

12.

Etter, A., Sarmiento, A., Romero, M., (2010) Land use changes (1970–2020) and carbon emissions in the Colombian Llanos. In: Hill, M., Hanna, N., (eds) Ecosystem function in Savannas, Boca Raton, FL: CRC Press, pp. 383–402. Google Scholar

13.

Fedegan (2006) Plan Estratégico De La Ganadería Colombiana 2019, Bogotá, Colombia: Author, pp. 1–296. Google Scholar

14.

Fedepalma (2013) Conservación de la Biodiversidad en las Zonas de Cultivos de Palma, Bogotá, Colombia: Author. Google Scholar

15.

Feldpausch, T. R., Lloyd, J., Lewis, S. L., Brienen, R. J. W., Gloor, M., Monteagudo Mendoza, A., Phillips, O., (2012) Tree height integrated into pantropical forest biomass estimates. Biogeosciences 9: 3381–3403. Google Scholar

16.

Gibbs, H. K., Brown, S., Niles, J. O., Foley, J., (2007) Monitoring and estimating tropical forest carbon stocks: Making REDD a reality. Environmental Research Letters 2: 045023. Google Scholar

17.

Goodman, R. C., Phillips, O. L., del Castillo Torres, D., Freitas, L., Cortese, S. T., Monteagudo, A., Baker, T. R., (2013) Amazon palm biomass and allometry. Forest Ecology and Management 310: 994–1004. Google Scholar

18.

Hernández-Vargas, G., Sánchez-Velásquez, L., Carmona-Valdovinos, T., Cuevas-Guzmán, R., (2000) Efecto de la ganadería extensiva sobre la regeneración arbórea de los bosques de la Sierra de Manantlán. Madera y Bosques 6: 13–28. Google Scholar

20.

Lähteenoja, O., Ruokolainen, K., Schulman, L., Oinonen, M., (2009) Amazonian peatlands: An ignored C sink and potential source. Global Change Biology 15: 2311–2320. Google Scholar

21.

Laurance, W. F., Camargo, J. L. C., Luizão, R. C. C., Laurance, S. G., Pimm, S. L., Bruna, E. M., Vasconcelos, H. L., (2011) The fate of Amazonian forest fragments: A 32-year investigation. Biological Conservation 144: 56–67. Google Scholar

22.

Laurance, W. F., Delamónica, P., Laurance, S. G., Vasconcelos, H. L., Lovejoy, T. E., (2000) Rainforest fragmentation. Nature 404: 836. Google Scholar

23.

Laurance, W. F., Nascimento, H. E. M., Laurance, S. G., Andrade, A., Ribeiro, J. E. L., Giraldo, J. P., Angelo, S, (2006) Rapid decay of tree-community composition in Amazonian forest fragments. Proceedings of the National Academy of Sciences 103: 19010–19014. Google Scholar

24.

Muller-Landau, H. C., (2004) Interspecific and inter-site variation in wood specific gravity of tropical trees. Biotropica 36: 20–32. Google Scholar

25.

Nascimento, H. E. M., Laurance, W. F., (2004) Biomass dynamics in Amazonian forest fragments. Ecological Applications 14: 127–38. Google Scholar

26.

Pan, Y., Birdsey, R. A., Fang, J., Houghton, R., Kauppi, P. E., Kurz, W. A., Hayes, D., (2011) A large and persistent carbon sink in the world’s forests. Science 333: 988–993. Google Scholar

27.

Pan, Y., Birdsey, R. A., Phillips, O. L., Jackson, R. B., (2013) The structure, distribution, and biomass of the World’s forests. Annual Review of Ecology, Evolution, and Systematics 44: 593–622. Google Scholar

28.

Phillips, J. F., Duque, A., Cabrera, K., Navarrete, D. A., Garcia, M. C., Alvarez, E., Vargas, D. M., (2011) Estimación de las Reservas Potenciales de Carbono Almacenadas en la Biomasa Aérea en Bosques Naturales de Colombia, Bogotá, Colombia: Instituto de Hidrología, Meteorología, y Estudios Ambientales-IDEAM. Google Scholar

29.

Phillips, J. F., Duque, Á., Scott, C., Wayson, C., Galindo, G., Cabrera, E., Yepes, A., (2016) Live aboveground carbon stocks in natural forests of Colombia. Forest Ecology and Management 374: 119–128. Google Scholar

30.

Phillips, O., Lewis, S. L., Baker, T. R., Chao, K.-J., Higuchi, N., (2008) The changing Amazon forest. Philosophical Transactions of the Royal Society B: Biological Sciences 363: 1819–1827. Google Scholar

31.

Phillips, O., Malhi, Y., Higuchi, N., Laurance, W. F., Vargas, P. N., Vásquez, R., Grace, J., (1998) Changes in the carbon balance of tropical forests: Evidence from long-term plots. Science 282: 439–442. Google Scholar

32.

Rodríguez Eraso, N., Armenteras-Pascual, D., Retana Alumbreros, J., (2012) Land use and land cover change in the Colombian Andes: Dynamics and future scenarios. Journal of Land Use Science 8: 154–174. Google Scholar

33.

Romero Ruíz, M., García, G., García, G. O., i Pascual, J. A., & Ruíz, D. M. R. (2004). Ecosistemas de la cuenca del Orinoco colombiano (p. 187). Bogotá, Colombia: Instituto de Investigación de Recursos Biológicos Alexander von Humboldt (IAVH); Instituto Geográfico Agustín Codazzi. Google Scholar

34.

Saatchi, S. S., Harris, N. L., Brown, S., Lefsky, M., Mitchard, E. T. A., Salas, W., Morel, A., (2011) Benchmark map of forest carbon stocks in tropical regions across three continents. Proceedings of the National Academy of Sciences of the United States of America 108: 9899–9904. Google Scholar

35.

Sánchez-Cuervo, A. M., Aide, T. M., Clark, M. L., Etter, A., (2012) Land cover change in Colombia: Surprising forest recovery trends between 2001 and 2010. PLoS ONE 7: e43943. Google Scholar

36.

Schnitzer, S. A., DeWalt, S. J., Chave, J., (2006) Censusing and measuring lianas: A quantitative comparison of the common methods. Biotropica 38: 581–591. Google Scholar

37.

Sherman, R. E., Fahey, T. J., Martin, P. H., Battles, J. J., (2012) Patterns of growth, recruitment, mortality and biomass across an altitudinal gradient in a Neotropical Montane forest, Dominican Republic. Journal of Tropical Ecology 28: 483–495. Google Scholar

38.

Sierra, C. A., del Valle, J. I., Orrego, S. A., Moreno, F. H., Harmon, M. E., Zapata, M., Benjumea, J. F., (2007) Total carbon stocks in a tropical forest landscape of the Porce region, Colombia. Forest Ecology and Management 243: 299–309. Google Scholar

39.

Slik, J. W. F., Paoli, G., Mcguire, K., Amaral, I., Barroso, J., Bastian, M., Zweifel, N., (2013) Large trees drive forest aboveground biomass variation in moist lowland forests across the tropics. Global Ecology and Biogeography 22: 1261–1271. Google Scholar

40.

Stevenson, P. R., (2011) The abundance of large ateline monkeys is positively associated with the diversity of plants regenerating in neotropical forests. Biotropica 43: 512–519. Google Scholar

41.

Stevenson, P. R., Aldana, A. M., (2008) Potential effects of ateline extinction and forest fragmentation on plant diversity and composition in the Western Orinoco Basin, Colombia. International Journal of Primatology 29: 365–377. Google Scholar

42.

Stevenson, P. R., Castellanos, M. C., Cortés, A. I., Link, A., (2008) Flowering patterns in a seasonal tropical lowland forest in Western Amazonia. Biotropica 40: 559–567. Google Scholar

43.

Wagner, M., Castro, F., Stevenson, P. R., (2007) Habitat characterization and population status of the Dusky Titi (C allicebus ornatus) in fragmented forests, Meta, Colombia. Neotropical Primates 16: 621–627. Google Scholar

44.

Williamson, G. B., Wiemann, M. C., (2010) Measuring wood specific gravity correctly. American Journal of Botany 97: 519–524. Google Scholar

45.

Zanne, A. E., Lopez-Gonzalez, G., Coomes, D. A. A., Ilic, J., Jansen, S., Lewis, S. L., … , Chave, J. (2009). Global wood density database. Dryad Digital Repository. Retrieved from  http://dx.doi.org/10.5061/dryad.234Google Scholar
© The Author(s) 2016 This article is distributed under the terms of the Creative Commons Attribution-NonCommercial 3.0 License (http://www.creativecommons.org/licenses/by-nc/3.0/) which permits non-commercial use, reproduction and distribution of the work without further permission provided the original work is attributed as specified on the SAGE and Open Access pages (https://us.sagepub.com/en-us/nam/open-access-at-sage).
Ana M. Aldana and Pablo R. Stevenson "Forest fragments of the Andean piedmont as carbon sinks," Tropical Conservation Science 9(4), (1 January 2020). https://doi.org/10.1177/1940082916667339
Received: 26 May 2016; Accepted: 12 July 2016; Published: 1 January 2020
KEYWORDS
above ground biomass accumulation rate
forest dynamics
wood specific gravity
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