Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome

The biogeochemical cycles of C, N, P and water, the impacts of land use in the stocks and flows of these elements and how they can affect the structure and functioning of Caatinga were reviewed. About half of this biome is still covered by native secondary vegetation. Soils are deficient in nutrients, especially N and P. Average concentrations of total soil P and C in the top layer (0-20 cm) are 196 mg kg–1 and 9.3 g kg–1, corresponding to C stocks around 23 Mg ha–1. Aboveground biomass of native vegetation varies from 30 to 50 Mg ha–1, and average root biomass from 3 to 12 Mg ha–1. Average annual productivities and biomass accumulation in different land use systems vary from 1 to 7 Mg ha–1 year–1. Biological atmospheric N2 fixation is estimated to vary from 3 to 11 kg N ha –1 year–1and 21 to 26 kg N ha–1 year–1 in mature and secondary Caatinga, respectively. The main processes responsible for nutrient and water losses are fire, soil erosion, runoff and harvest of crops and animal products. Projected climate changes in the future point to higher temperatures and rainfall decreases. In face of the high intrinsic variability, actions to increase sustainability should improve resilience and stability of the ecosystems. Land use systems based on perennial species, as opposed to annual species, may be more stable and resilient, thus more adequate to face future potential increases in climate variability. Long-term studies to investigate the potential of the native biodiversity or adapted exotic species to design sustainable land use systems should be encouraged.


General aspects of the caatinga biome
The Caatinga biome covers a large area in Northeast Brazil, about one million square kilometers, mostly overlapping with the semiarid region.Most of the area of the biome presents average annual rainfall lower than 1000 mm.However, the temporal and spatial variability of rainfall is a marked characteristic of the region (Reddy, 1983), rendering averages of little value.In a simplified picture, 20% of the annual rainfall occurs in a single day and 60% in a single month (Sampaio, 1995).Average annual temperatures, on the other hand, are high (23 to 27 °C) and relative humidity usually below 50%.As a consequence, the potential evapotranspiration is high, usually above 1500 mm year -1 , resulting in negative water balances along 7 to 11 months every year.
The average altitude is around 400-500 m but Caatinga reaches the sea in Rio Grande do Norte and Ceará and also covers large plateaus above 1000 m.About 37% of the area is composed of slopes with 4 to 12% inclination and 20% with slopes steeper than 12%, resulting in high erosion risks in cultivated areas (Leprun, 1983).Jacomine (1996) divided the area into three geological types, according to the formation material: 1) areas on top of the crystalline shield; 2) areas where the crystalline shield is covered with sandy material; and 3) areas of sedimentary deposits.Four dominant soil orders, out of a total of 15 orders, form a spatial mosaic covering 66% of the area (Latosols, 19%; Lithosols, 19%; Argisols, 15%; Luvisols, 13%).Over 80% of the area has some soil limitation in relation to agricultural use, which may be related to low fertility, shallow profile, poor drainage or high exchangeable Na (Silva, 2000).
All these climatic and soil variations result in a great diversity of environmental conditions and landscapes.The Caatinga biome spreads over 17 great landscape units, subdivided into 105 geo-environmental units out of a total of 172 for the whole Northeast (Silva et al., 1993).Within this complex region, lives a population of more than 20 million people, making it one of the most densely populated semi-arid regions in the whole world, with 20-30 inhabitants per km 2 .The land tenure system, in which 80% of farms are smaller than 10 ha, creates a condition of extreme vulnerability of the population to climate variability (Sampaio et al., 2009).Therefore, the frequent droughts that occur usually lead to severe negative impacts on the population, the economy and natural resources of the region.

Main land use systems in the Caatinga biome
The area annually occupied with agricultural fields comprises about 10% of the whole semiarid region (Sampaio and Menezes, 2002).Less than 2% are permanent crops and most of the annual crops are planted in the slash and burn system.Livestock, mainly cattle but also goats and sheep, are ubiquitous.Native pastures covered 13 × 10 6 ha, while planted pastures covered 6 × 10 6 ha (Sampaio and Salcedo, 1997).However, cattle also feed on the harvested agricultural fields and fallow vegetation and mature Caatinga areas.In the 1990's, fuel wood extraction was the main driver for the annual deforestation of about 1 × 10 6 ha, only in the states of CE, RN, PB and PE (Sampaio and Salcedo, 1997) and the area deforested due to wood extraction has been growing since then.At that time, most of the wood came from new agricultural fields but now it is mostly an independent activity.In the whole region, according to Araújo Filho and Barbosa (2000), the annual deforestation reaches 2.7% of the area and more than 80% of the native vegetation cover corresponds to pioneer and secondary vegetation stages.

Remaining area of native vegetation
In 1984, native Caatinga vegetation covered 68% of its original area, the rest being used for agriculture or greatly altered by anthropic activities (CNRBC, 2004).In 1990, an updated survey conducted by Sudene and Ibama indicated an expressive reduction of the native coverage, to 47%.In 2004, results from 'Projeto de Conservação e Utilização Sustentável da Diversidade Biológica Brasileira' (Probio) showed only a small decrease in this area (to 43%), corresponding to 363115 km 2 .Monitoring in 2008, performed using 111 orbital images from CBERS2B and 52 images from TM Landsat 5, estimated the coverage to be 53.6%(Figure 1).It is possible that most of the difference in the more recent survey resulted from a difference in the methodological approach and not from a real increase in coverage.In a complex mosaic of vegetation with distinct regeneration ages and growth potential due to different environmental characteristics it is difficult to determine the limits of native vegetation, but it is also possible that the area of native vegetation has had an increase due to the recent socio-economic changes that occurred in the region and in Brazil.

Structure and functioning of terrestrial ecosystems
Due to the high demographic density (20 to 30 inhabitants per km 2 ) and the land tenure system, most of the semiarid region of NE Brazil has been subdivided into a large number of small properties, with less than 10 ha each.This high pressure pushed the region beyond its sustainability limit.Irrigation and high input systems are limited to at the most 3% of the area due to low water availability plus soil inadequacy (Sampaio et al., 2009).Therefore, low input systems, subjected to the high climatic variability and characterized by instability of their biogeochemical processes are the rule.Understanding the functioning of these systems requires knowledge of these processes, in order to identify practices capable of increasing regional sustainability.
Figure 2 shows a conceptual model of the main stocks and flows of carbon, water and nutrients in a typical agroecosystem in the Caatinga biome.The main objective of this paper is to present the available information on these stocks and flows.Flows are colored according to their impact on the balance of nutrients: blue are inputs and red are outputs from the system.To maintain productivity, inputs should be maximized and outputs minimized.Green flows indicate recycling and should be managed so as to increase productivity in a sustainable way.The uptake flow from deeper soil layers (dotted line) assumes that resources (water and nutrients) may be tapped in systems with trees or deep rooted perennial grasses and shrubs.

Carbon and nutrient stocks in soils
Average total organic carbon (TOC) in the Ap horizon of soils under Caatinga vegetation are generally low, compared to other biomes of Brazil (Table 1).These low values are related primarily to the low organic residue inputs and to the low vegetal biomass formation, which is limited by water and also soil fertility deficiencies.
Table 2 presents more detailed soil data obtained from the surveys of all Northeastern states, except Maranhão and Piaui (Jacomine et al., 1971;1972a, b;1973;1975 a, b;1979).Among the soil orders that occur in the region, Vertisols and Cambisols have the highest TOC (12,3 g C kg -1 ) but occupy only 5% of the semiarid area.Luvisols and Lithosols occupy a larger area (32%), mainly on top of the crystalline shield and have TOC between 10.4 e 11.8 g kg -1 .Latosols and Argisols follow in area (36%), the first ones mainly derived from sedimentary and the second ones from both crystalline and sedimentary material, and have TOC between 9.7 and 8.9 g kg -1 .Flows in gray color represent inputs, those in dashed black lines represent outputs from the system, while those in solid black lines represent internal cycling (adapted from Menezes et al., 2005).(2007).Menezes et al. (2005) compiled data from several soil surveys and reported that 90% of the soil samples of the main orders in the semiarid region of NE Brazil had medium to low extractable p levels.Total p is generally higher in Luvisols and Lithosols than in Latosols and Argisols (Table 2).In general, there is a close relation among TOC and total P (r = 0,89**) and TOC and clay content (r = 0,82**).The lowest TOC and total p values are those of Regolithic Neosols, which frequently receive manure additions when cultivated, due to the extremely low fertility.
Information regarding stocks and availabilities of N, P and other nutrients in soils of the Caatinga biome are relatively scarce, but the available studies are consistent in pointing N and P as the most limiting to plant growth.Cavalcanti et al. (1998) and Guimarães et al. (1998) published surveys of fertility analysis for soils of Pernambuco and Ceará, respectively.Sampaio et al. (1995) reviewed some of the earlier works, including the first approximation of Galvão and Cate Junior (1969) for Rio Grande do Norte, Paraíba, Pernambuco and Alagoas and the evaluation of Oliveira et al. (1988) for the whole Northeast region.They are based on thousands of soil samples and indicate a general deficiency of P and low need for liming, except for Piauí and, in a smaller scale, for Alagoas.This broad panorama confirms that N and P are limiting and that practices to raise soil fertility are needed in the region.

Aboveground biomass of perennial vegetation
The average aboveground biomass of Caatinga vegetation has been estimated to be in the interval between 30 and 50 Mg ha -1 .A better approximation cannot be made because direct measurements are almost non-existent, indirect estimations reveal a very high spatial variability (2 to 156 Mg ha -1 ) and the sampled areas are few and chosen according to preferential criteria.Direct measurement (74 Mg ha -1 ) was made in a single site at Serra Talhada, Pernambuco (Kauffman et al., 1993).Estimates based on botanical surveys tend to fall in the upper part of the range because of the preference for undisturbed vegetation while estimates based on fuel wood production tend to fall in the lower part of the range because they include areas with repeated short cycle (10 to 15 years) clear cutting (Gariglio et al., 2010).Since most of the Caatinga corresponds to vegetation recovering from previous cutting, for fuel wood or part of the slash and burn agriculture system, the regional average must be in the lower third of the range.Of the total aboveground biomass, 5 to 10% (2 to 6 Mg ha -1 ) correspond to leaves (Table 3) and are renewed every year, contrasting with the biomass stocked in stems and branches (Silva, 1998).Most of this leaf biomass is consumed by the ubiquitous domestic herds, either directly from the plants or after falling to the ground (Schacht et al., 1989;Hardesty and Box, 1988).
Data for cultivated areas are fewer than for Caatinga.The area with perennial crops is proportionally small.The only available data is for five year old dwarf cashew plants (Table 3).Other perennial crops, like Prosopis juliflora and Gliricidia sepium, probably have biomasses in the upper range of Caatinga, since they are usually planted in sites with more water availability.The aboveground biomass of annual crops is considered as production and it is eliminated every year, exported as agricultural product, consumed by animals, burned or incorporated to the soil.

Annual aboveground net primary productivity
Papers dealing with annual biomass productivity are scarcer in the literature than those that quantified biomass stocks in the Caatinga biome.The variation is very large due to the enormous variability of water availability, brought about by rainfall variation, topographic differences and different soil depth and water holding capacities (Menezes and Sampaio, 2000).Annual productivities and biomass accumulation are estimated to vary from 1 to 7 Mg ha -1 year -1 and all actual measurements fall in this range (Table 3).This capacity can be expressed as years necessary to rebuild the stocks.The sustainable cycle of fuel wood production has been estimated to vary from 10 to 15 years, with average of 13 years (Gariglio et al.,  (1971, 1972a, b, 1973, 1975a, b, 1977).2) Percentages correspond to proportion in relation to the area of the Northeastern semiarid.3) Weighted average according to the number of samples in each soil order.

2010
).The length of the fallow period allowing sufficient nutrient accumulation in the aboveground biomass and the re-initiation of the slash and burn cycle is in this same range.In Araripina, Pernambuco, the fallow period was 12 years (Tiessen et al., 1992).However, the large variability of climate, soil fertility and previous level of soil degradation renders general averages of little value.Herb and small shrub biomass stocks and productions have similar values (2 to 6 Mg ha -1 year -1 ) because most of these plants have annual cycles.Bromelias and small cacti are exceptions.Production values are also similar to those of trees and large shrubs and are inversely related to the biomass stock of these large plants: areas of Caatinga vegetation with tall and dense canopies produce little biomass of small plants and the opposite occurs in areas of open Caatinga vegetation, except if they are in degraded or environmentally limited areas.Selective cutting of plants to reduce density and shading is a management technique used to increase pasture production.One single estimate was made of bromeliad biomass (1.4 Mg ha -1 ) which is very dense in some areas but absent in other ones (Table 3).Within fields of perennial crops, the biomass of weeds has the same variation as that in native vegetation, depending on size and density of the crop plants, except after weeding or herbicide application (Ribeiro et al., 2004).
Many publications refer to annual crops, largely dominant in the semiarid, but most have data only about the commercial products (fruits, foliage, etc) and very few include data on total biomass, in spite of the importance of crop residues as animal fodder.Productions vary greatly (0.2 to 6 Mg ha -1 year -1 ) but, except in irrigated areas, are similar to those of native plants or even smaller, under similar environmental conditions, due to their inferior adaptability, lower biodiversity and shorter life cycle.

Litter deposition
Data about litter deposition and decomposition in areas of Caatinga vegetation are still scarce in the literature ( Sampaio and Silva, 1996).Among the few studies conducted, we may mention Dantas (2003), Santana (2005), Souto (2006), and Costa et al. (2007).On average, litter production in the drier areas of the Caatinga biome falls between 1500 to 3000 kg ha -1 year -1 , on a dry matter basis, but may reach over 6000 kg ha -1 year -1 in the more humid areas of the region (Sampaio and Silva, 1996;Dantas, 2003).These levels of litter production are clearly lower than those observed in other forest formations in Brazil but, similarly to other ecosystems, the period of peak litterfall in areas of Caatinga vegetation occurs at the end of the rainy season and beginning of the dry season.
Data about litter stocks are also rare.Martins (2008) quantified the stocks of litter in areas of Caatinga in Pernambuco and found 6,500 to 20,100 kg ha -1 of dry matter in preserved areas, from 1,900 to 7,200 kg ha -1 in moderately degraded areas, and from 140 to 1.016 kg ha -1 in severely degraded areas.Amorim (2009) studied the carbon cycling in an area of preserved Caatinga in Petrolina, Pernambuco, and observed an average litter stock of 7,000 kg ha -1 .In another study in an area of Caatinga in Paraíba, Souto (2006) estimated an average litter stock of about 1,200 kg ha -1 .
Most of the Caatinga litter biomass corresponds to the leaf fraction, followed by bark, branches and the miscellaneous fractions (Souto, 2006).The nutrient content of the leaf fraction has been reported by Dantas (2003), who found average values of 19.1; 1.0; 15.6 g kg -1 of N, P and K, on a dry matter basis, respectively, while Santana (2005) observed concentrations of 14.5; 0.8; and 7.6 g kg -1 of these elements.

Root biomass stocks and productivity
Only four papers deal with root biomass of native vegetation in the Caatinga biome, two restricted to thin roots in the upper soil layer.The stock of 5 mm thick roots down to 30 cm soil depth varied from 3 to 8 Mg ha -1 in Caruaru, PE (Salcedo et al., 1999), while the total stock down to 1 m reached 12 Mg ha -1 in Araripina, PE (Tiessen et al., 1992).
The production of thin roots (up to 2 mm thick) in the top soil layer, estimated as the stock difference along the year, was 2.4 Mg ha -1 year -1 (Medeiros, 1999).Therefore, the magnitude seems to be the same as that of aboveground biomass productivities.In a 5 year old dwarf cashew crop, roots down to 30 cm soil depth had biomass (0.5 to 0.9 Mg ha -1 ) corresponding to less than 10% of the aboveground biomass (Morais et al., 2004).

Atmospheric deposition of nutrients
Nutrient inputs through rainfall are one of very few processes that provide nutrients to ecosystems in the Caatinga biome.In spite of its low magnitude, this input becomes relevant because of the low natural stocks and the low inputs of other external sources.Perez-Marin and Menezes (2008) quantified nutrients in rainfall water in an agroforestry system and evaluated the effects of tree canopies in the nutrient content of the water reaching the soil.Those authors determined that 32% of the rainfall (TR) was intercepted by the canopies (I), 67% passed as throughfall (T) and only 0.74 reached the soil through stemflow (S).Stemflow only occurred during rain events equal to or larger than 4 mm, a similar value to that reported by Lima and Leopoldo (2000) in a riparian forest (4.2 mm).Although low, the quantities of S are relevant because the water reaches the soil at a low speed and are more easily infiltrated, resulting in a localized water and nutrient distribution around the trees (Oliveira Junior and Dias, 2005;Johnsson, 1990).The concentrations of N and P in S and T were similar and four times higher than those of the rainwater.The concentration of K was 2 times higher in S than in T and seven times higher than in the rainwater.Average N, P and K inputs were 5, 1 and 24 kg ha -1 in the rainwater, 9, 2 and 62 kg ha -1 in the throughfall and 0.12, 0.02 and 1 kg ha -1 in stemflow water, respectively.

Biological nitrogen fixation
The capacity of Caatinga legume species to simbiotically associate with rhizobia is an important issue to their use in agroforestry systems and revegetation programs.However, knowledge on the subject is limited in semiarid Northeast in spite of the high number of total legume species, many of them endemic (Queiroz, 2002).The world literature on legume nodulation (Allen and Allen, 1981;The Bean Bag, 1995, 1996, 1997, 2002;Souza et al., 1994;Faria et al., 1984Faria et al., , 1987Faria et al., , 1989;;Faria and Lima, 1998) refer to approximately 293 species that occur in the semiarid, 216 (73.4%) nodulate, 69 (23.5%) do not and 8 species have conflicting information.
In general, δ 15 N of tropical forests are higher than those of temperate forests (Martinelli et al., 1999).Values of nonfixing species in Caatinga ( 7 a 9‰) are high (Freitas et al., 2010a) compared to those of other Brazilian ecosystems: cerrado, <2‰ (Sprent et al., 1996;Bustamante et al., 2004); and Amazon forest, <5,25‰ (Gehring et al., 2005).But they are similar to those found by Schulze et al. (1991) in semiarid areas of Namibia (7.38‰).A survey of determinations in 118 areas indicates that high values are usually associated with semiarid regions (Handley et al., 1999).The processes that increase δ 15 N signals are associated to soil mineral N losses, usually through leaching or volatilization.Any factor that increases the flow from organic to mineral pools (more susceptible to losses) drives the systems to enrichment of 15 N (Högberg, 1997;Handley et al., 1999).
In Caatinga, trees with high N 2 fixation can be clearly separated from non-fixing ones based on their δ 15 N signals.Several species have been identified as fixing high proportions of their N while others are clearly non-fixing ones (Freitas et al., 2010b;Souza, 2010).Preliminary estimates of N amounts fixed annually in the canopy of Caatinga were made for two sites: in Serra Talhada, PE, they were of 3 kg ha -1 , in mature Caatinga, and 26 kg ha -1 in a regenerating Caatinga; in Remigio, PB, they were 11 and 21 kg ha -1 , respectively (Freitas and Sampaio, 2008).To these amounts must be added the amounts fixed in the wood parts that were estimated only for the regenerating Caatinga in Serra Talhada (22 kg ha -1 ).Apparently, the contribution of biological fixation to mature Caatingas is small but it is, of the same order of magnitude of the only other estimative (7 kg ha -1 year -1 Roggy et al. 1999), found in the literature for a tropical vegetation, a rain forest in French Guyana (Roggy et al. 1 1999).The most important factor for these low amounts is the low proportion of plants of fixing species in the mature vegetation, a fact confirmed by several studies (Sampaio, 1996).In regenerating Caatinga, the large difference comes from the much higher proportion of fixing plants.

Losses due to the removal of Caatinga vegetation
Slash-and-burn systems, which still exist in the Caatinga biome, contribute significantly to losses of carbon and nutrients from agroecosystems.However, in NE Brazil, the agricultural phase of the slash-and-burn cycle is losing the significance as the main driver of land clearing, due to the low prices and low productivities of crops in the region.
Instead, the extraction of fuel wood, in many areas of the region, is becoming the main driver of deforestation, in order to supply the widespread domestic, commercial and industrial demands for fuel wood in the region.
The fire used after land clearing eliminates the debris (small branches and leaves) and also promotes a short-term improvement in soil fertility, due to inputs of nutrients in the ash and the elimination of the seed bank of many invasive plant species.However, the fire also leads to the loss of almost 100% of the C and N and part of the P present in the burnt biomass.Kauffman et al. (l993) quantified losses of more than 500 and 20 kg ha -1 of N and P, respectively, after a fire to burn the biomass slashed from an area of Caatinga in Serra Talhada, PE.
In addition to the losses from the slashed vegetation, the fire may also lead to significant losses of C and N from soil organic matter.Salcedo et al. (l993, 1997) worked in the same plots as Kauffman et al. (l993) and observed rapid decreases in nutrient stocks in the soil organic matter during the months following slash and burn.Similarly, Tiessen et al. (1992), who worked in an Oxisol in Araripina, PE, found losses up to 40% of soil C only six years after land clearing.In another study, Fraga and Salcedo (2004) quantified the stocks of C and organic N and P in ten sites in Paraíba and Pernambuco, comparing soils under native Caatinga vegetation and adjacent agricultural or pasture plots.Those authors found that the cultivated areas had only approximately half of the levels of carbon and nutrients compared to the soils under Caatinga.

Nutrient outputs due to crop harvest and grazing
After mineralization, the nutrients in the soil organic matter are converted to labile forms and may be taken up by crops or forage species.Afterwards, a fraction of these nutrients is then exported from the ecosystem due to the sale of crops or animal products.Menezes et al. (2002) quantified the removal of nutrients from subsistence systems in family farms in the semi-arid region of Paraíba and found that cropping fields lost, on average, 16, 1 and 18 kg ha -1 year -1 of N, P and K, respectively, due to the harvest of grains and straw.The results are similar to those reported by Sanchez (2002), which compiled 30 years of data from 37 countries in Africa and found average N, P and K losses of 22, 2.5 and 15 kg ha -1 year -1 from cropping fields.In another study, Menezes et al. (2005) quantified the removal of nutrients in the biomass of prickly pear (Opuntia ficus-indica Mill) cultivated to be used as forage in 50 fields in semi-arid NE Brazil.Since this species is particularly productive in dry lands, nutrient removal was extremely high, averaging up to 300, 107 and 1454 kg ha -1 of N, P and K, respectively, in the 5 most productive fields, which represented 7 and 3% of the total N and P from the top layer of the soils.

Losses due to soil erosion and water runoff
In addition to the losses due to mineralization and nutrient removal in the harvested crops and pastures, soil erosion is also one of the main processes responsible for the soil fertility decreases in the Caatinga biome (Menezes e Sampaio, 2002;Sampaio et al., 1995).Studies about soil losses following the conversion of native vegetation into cropping fields or pastures present alarming data about these processes (Albuquerque et al., 2001;Margolis et al., 1985b).The severe soil losses reported due to land use change are also related to great water losses due to runoff and, as a consequence, to lower water infiltration and lower water availability for plant growth.The severe rates of erosion and runoff in agroecosystems of the Caatinga biome are a result of the combination of the relief, with most soils presenting moderate to severe slopes, and the rainfall pattern, characterized by short, but intense rainfall events (Sampaio et al., 1995).
The influence of the soil cover type on soil erosion in the Caatinga biome is well reported in the study conducted by Albuquerque et al. (2001).These authors conducted an 8-year study in which quantified soil losses in large field plots with different land covers (native vegetation, crops or pastures) and observed average soil losses of 3 and 30 t ha -1 year -1 in pastures and cropping fields, respectively, while losses under native vegetation averaged only 0,1 t ha -1 year -1 .This study also reported data on the inter-annual variability of these processes, demonstrating that 40% of the soil losses occurred in a single year and other 50% in three other years.In another study, Fraga and Salcedo (2004) used the 137 Cs technique to estimate soil erosion during a 35-year period after removal of the native Caatinga to implement pastures or cropping fields and estimated that during that period, 57% of the C and N lost from the soil in the deforested areas were due to mineralization, while the remaining 43% were due to soil erosion (up to 500 t ha -1 of soil loss during the whole period).Therefore, it is evident the need for the implementation of soil management and conservation practices in agroecosystems of the Caatinga biome in order to avoid soil erosion and the severe depletion of carbon and nutrients after the removal of the native vegetation.Studies that evaluated the impacts of the implementation of soil management practices, such as terraces, countour planting, construction of countour barriers vegetation or stones, etc, have reported 80 to 100% reductions of soil losses compared to reference areas (Silva et al., 1986;Margolis et al., 1985a;Freitas et al., 1981).

Potential impacts of future land use and climate variability
The environmental degradation in many areas of the Caatinga biome has been classified as desertification, which may strongly affect biogeochemical cycling in the region.The desertification processes have both anthropogenic and natural drivers.As discussed previously, the human induced degradation is mostly rooted on deforestation and inadequate soil management, such as slash-and-burn systems, overgrazing and intensive fuel wood extraction.Soil erosion processes are also important drivers of desertification in the Caatinga biome, since it decreases soil fertility and water availability, affecting most ecosystem processes.
Nowadays, there are about 1,300,000 km 2 of land in the biome that are susceptible to desertification, which include areas within 1,488 municipalities of nine Brazilian states (Brasil, 2007).It is evident, therefore, the need for the establishment of actions to prevent deforestation, to improve soil management techniques, and to develop sustainable land use systems in the biome.It is also important to mention that the success of such actions will depend on effective long-term commitment from the many agencies and institutions related to this issue, both at the federal, state and municipal levels.
In addition to unsustainable land use practices, future changes in climate patterns also have strong potential to cause significant impacts in the biogeochemical cycles in the Caatinga biome.In fact, among all biomes in Brazil, the Caatinga is the one with the strongest projected impacts related to climate change.Higher temperatures, lower amounts and increased variability in precipitation patterns are some of the expected changes in the region, which may lead to more intense and frequent droughts, floods, biodiversity loss and lower production of food and energy generation (Brasil, 2004).

Figure 2 .
Figure 2. Conceptual model of the main stocks and flows of C, N, P and water in agroecosystems of the Caatinga biome.Flows in gray color represent inputs, those in dashed black lines represent outputs from the system, while those in solid black lines represent internal cycling (adapted fromMenezes et al., 2005).

Table 1 .
Soil organic carbon stock in areas under native vegetation or anthropic use in Brazilian biomes.

Table 2 .
Characteristics of the Ap horizon of the main soil orders in the Caatinga biome.

Table 3 .
Biomass stocks and production in perennial crop areas or areas with native Caatinga vegetation.