Fatih
Evrendilek
Department of Landscape Architecture, Mustafa Kemal University, 31034, Antakya-Hatay, Turkey. E-mail: fevrendilek@mku.edu.tr; Fax: +90 326 2455832; Tel: +90 326 2455735
First published on 5th December 2003
Environmental monitoring of national-level comparisons of CO2 emissions is needed to quantify sources and sinks of carbon (C) in national ecosystems. In this study, a national forest inventory database was used to estimate the past and current pools and fluxes of C in deciduous and coniferous forest and woodland ecosystems (20.7 × 106 ha) of Turkey. Growing C stock was 12.63 t C ha−1 in 1960 and 16.55 t C ha−1 in 1995. Total C store in the whole live woody biomass was estimated at 22.77 t C ha−1 in 1996. The total flux of C from the atmosphere into the forest and woodland ecosystems driven by primary productivity was about 1.46 t C ha−1 (or 30.2 Mt C) in 1996. The estimated net release of C from the forest and woodland ecosystems of Turkey to the atmosphere was about 1.34 t C ha−1 (or 21.5 Mt C) in 1996. When C released was taken into account, net ecosystem sequestration (NES) resulted in 0.12 t C ha−1 per year. Such analytical tools as national forest C budgets are needed to improve our preventive and mitigative strategies for dealing with global climate change.
Local human activities modifying C pools and fluxes have the potential to alter the global C cycle and climate. The injection of 480 Pg C into the atmosphere through fossil-fuel combustion and land-use and land-cover (LULC) changes since the Industrial Revolution has disturbed the natural global cycling of C among vegetation, soil, atmosphere, and oceans.6 Deforestation is one of the major LULC changes that released 2.24 Pg C per year to the atmosphere in the 1990s.7 Quantification of C stocks and fluxes of forest ecosystems is of considerable interest in the context of mitigation of global climate change for the following reasons: (1) forest ecosystems store larger quantities of atmospheric CO2 for a longer period of time in vegetation and soil than the other terrestrial ecosystems, (2) countries seek to comply with agreements under the UN Framework Convention on Climate Change; and (3) scientists seek to account for the imbalance in the global C budget (termed as missing sink comprising up to 1.8 Pg C per year in the 1980s).8 National budgets of forest C sequestration may be a practical way of monitoring reductions and increases in atmospheric CO2 concentration and at the same time may contribute to sustainable biological productivity of ecosystems. However, forest C sequestration should be regarded as a component of a mitigation strategy, not as a substitute for the changes required in energy supply, use and technology if atmospheric CO2 concentration is to be stabilized.
Turkey (36–42°N, 26–45°E) has a land area of 779452 km2 with 20 million ha located in arid and 31 million ha located in semi-arid climatic regions. Turkey is a predominantly mountainous country, and true lowland is confined to the coastal fringes, with an average altitude of 1250 m and the highest point of 5137 m (Mount Ararat) above sea level near the Iranian border. Gently rolling, fertile plains cover Thrace and extend along the Black Sea coast of Anatolia. Along the coast of the Aegean Sea are broad, fertile river valleys. A narrow strip of fertile land lies along the Mediterranean Sea. The prevailing climate varies among the Aegean, Mediterranean, Central, East and Southeast regions of Turkey. There are two main climate belts: (1)
‘Temperate’ characterized by cold winters and warm summers with a year-round precipitation, and (2)
‘Mediterranean’ characterized by mild winters and hot and dry summers with more than 65% of the mean annual precipitation occuring in the winter. The temperature reaches a maximum of 45 °C in the south and southeast during the summer and a minimum of −40 °C in the east and central Anatolia during the winter, with a mean annual temperature of 19 °C. Annual precipitation ranges from 250 mm in the central and southeastern regions to 2500 mm in the northeastern coastal plains and mountain regions, with a mean annual precipitation of 650 mm.
Rapid population growth, increased human consumption, conversion of forests to agricultural and urban-industrial lands, overgrazing, overharvesting, prevailing semi-arid conditions, poverty, economic crises, rapid urbanization-industrialization, and migration of rural populations to urban areas have had significant adverse impacts on conservation and sustainable management of forest resources, thus causing an increase in degradation and destruction of forest ecosystem productivity. Many forests are exploited by the rural population as a source of fuelwood and charcoal for their domestic needs. The percentage of total roundwood production consumed for fuel was 44% in Turkey.4 About 2000 fires have occurred in Turkey in the last ten years, burning about 12500 ha annually.9 The land area of forests degraded due to overexploitation and urban-industrial expansions was estimated at 11.7 Mha.10 Conversion of forest, pasture, and wetlands into agricultural lands between 1948 and 1994 has amounted to 21.5 Mha.10,11 Regenerating and C sequestration capacities of forest in Turkey are restricted by soil erosion and shallow soils in that 75% of the total land area is prone to different levels of erosion, and only 14% of the total land area has a soil depth of 90 cm or more.10
Sharp et al. (1975) calculated forest biomass of North Carolina in the USA, based on forest inventory data and a constant biomass expansion factor (BEF) of 2.0 t m−3.12 Brown and Lugo (1984) used two different BEF values of 1.6 for closed tropical forests and 3.0 for open tropical forests.13 Kauppi et al. (1992) quantified a C budget of European forests by applying a BEF range of 0.6 to 0.8.14 Turner et al. (1995) estimated C budget for forests in the USA by using a constant ratio of whole-tree C to merchantable-bole C across age classes within a forest type.15 In the work presented here, carbon budget for forest and woodland ecosystems in Turkey was calculated separately for coniferous and deciduous tree groups, based on UN-ECE/FAO national forest inventory data in 1996.16
Turkey is an important center of floristic diversity where three phytogeographical regions of Euro-Siberian, Mediterranean and Irano-Turanian meet, with approximately 8792 vascular and 4734 non-vascular plant species, 2656 endemic plant species, and 1889 animal species identified.18 Dominant dry forest species of the Irano-Turanian floristic region include Pinus nigra subsp. Pallasiana, P. sylvestris, Quercus cerris, Q. pubescens, and Juniperus oxycedrus.19 Dominant sub-humid forest species of the Euro-Siberian or Euxine floristic region include Fagus orientalis, Castanea sativa, Carpinus spp., Picea orientalis, Pinus nigra, P. brutia, P. sylvestris, Abies bornmulleriana, A. equi-trojani.18 Sclerophyllous forest species of the Mediterranean floristic region include Quercus ilex, Q. calliprinos, Pistacia lentiscus, Cercis siliquastrum, Ceratonia siliqua, Pinus brutia, P. pinea, P. halepensis, Cupressus sempervirens, and Cedrus libani.11,19
The present total area of nature conservation constitutes 4.8%
(3.7 Mha) of the country's land area.10 Since 1955, reforestation of 2.5 Mha, erosion control of 284000 ha, and range improvement of 80
000 ha have been carried out, and the current annual anti-desertification activities are 50
000 ha for reforestation and 25
000 ha for erosion control.9 The National Afforestation and Erosion Control Mobilization law passed in 1995 increased the rate of afforestation for industrial and protective purposes in addition to fuelwood and charcoal production to around 300
000 ha annually.9 The share of the forestry sector in the gross national product (GNP) is about 0.9% which would increase to 1.8% if undeclared firewood consumption, and private sector wood production were included in the calculation. Nevertheless, this calculation excludes intangible benefits from the ecosystem services of forests such as regulation of hydrological cycle, sequestration of greenhouse gases (GHGs), soil stability, recreation, and scientific information as well as their role in generating higher income and employment for 7.2 million forest-dependent villagers living in or close to the natural forests.
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Fig. 1 Components of carbon (C) budget of Turkish forest and woodland in 1996. The boxes and arrows refer to C stocks in t C ha−1 and fluxes in t C ha−1 per year, respectively. GPP = gross primary productivity = NPP/0.5 = 1.46; Ra = plant respiration = 0.73; NPP = net primary productivity = GPP − Ra = 0.73; Rh = soil respiration = 0.30; NEP = net ecosystem productivity = NPP − Rh = 0.43; NES = net ecosystem sequestration = NEP − Removal = 0.12; and total forest and woodland area = 20.713 Mha. |
Since the UN-ECE/FAO data did not distinguish between coniferous and deciduous woodlands, the relative proportions of the reported stock or flux figures of coniferous (VEF) and deciduous (VDF) trees on forest were assumed to be the same on woodland (VEDW), and the total coniferous and deciduous C stocks/fluxes (TCED) of forest and woodland were estimated as follows:
![]() | (2) |
![]() | (3) |
![]() | (4) |
![]() | (5) |
To complete the C budgets, initial carbon stocks in soil and wood products, and total litterfall rate were estimated from the relevant literature data. The carbon in wood products from the forests is brought back to the atmosphere by product decomposition in long-term. The total amount of C in wood products was assumed to be constant, and thus, the average amount of C removed is equal to the amount of C released in product decomposition.22 Soil organic C (SOC) pool was assumed to be in steady-state and contained the average forest SOC stock of 27 European countries of 47 t C ha−1 to a depth of 30 cm.23 Decomposition rate of the SOC pool was assumed to be in steady state with the flow rate of litterfall into the soil. Total litterfall rate from above- and below-ground woody biomass of living trees was estimated by multiplying woody biomass by compartment-specific turnover rates (r) as follows:
LFTB-EF = (AGBEF × rAGB-EF) + (BGBEF × rBGB-EF) | (6) |
LFTB-DF = (AGBDF × rAGB-DF) + (BGBDF × rBGB-DF) | (7) |
Year | Area/Mha | Annual increment (AI)/t C ha−1 per year | Annual felling (AF)/t C ha−1 per year | Net C increment (NCA)/t C ha−1 per year | Growing C stock (GS)/t C ha−1 |
---|---|---|---|---|---|
a The ratios of oven dry above-ground woody biomass to volume and of C to oven dry above-ground woody biomass for all tree species were assumed as 0.6 and 0.5, respectively. Mha = 106 ha. | |||||
1960 | 20.199 | 0.39 | 0.22 | 0.17 | 12.63 |
1965 | 20.199 | 0.40 | 0.26 | 0.14 | 13.14 |
1970 | 20.199 | 0.41 | 0.33 | 0.08 | 13.67 |
1975 | 20.199 | 0.42 | 0.37 | 0.05 | 14.25 |
1980 | 20.308 | 0.43 | 0.37 | 0.06 | 14.75 |
1985 | 20.399 | 0.44 | 0.35 | 0.09 | 15.30 |
1990 | 20.458 | 0.45 | 0.28 | 0.18 | 15.91 |
1995 | 20.559 | 0.46 | 0.25 | 0.21 | 16.55 |
Best-fitted regression lines | y = −3.5 + 0.002x | y = −1780 + 1.8x − 0005x2 | y = 1851 − 1.9x + 0.0005x2 | y = −205.3 + 0.11x | |
r 2 = 0.99 | r 2 = 0.94 | r 2 = 0.94 | r 2 = 0.99 | ||
AI = 0.082 × GS0.617 | |||||
r 2 = 0.99 |
Total C storage in living woody biomass of coniferous and deciduous trees was estimated at 471.6 Mt C, with about 91% on forest and 9% on woodland. Coniferous trees make up about 60% of the total C stock of forest and woodland. Total tree C density was 39.8 t C ha−1 for the coniferous forest, 49.2 t C ha−1 for the deciduous forest, 5.5 t C ha−1 for the coniferous woodland, 2.8 t C ha−1 for the deciduous woodland, and 22.8 t C ha−1 for the whole forest and woodland ecosystems. Above-ground C density was estimated at 36.8 t C ha−1 on forest and 3.4 t C ha−1 on woodland, and below-ground C density at 6.2 t C ha−1 on forest and 0.6 t C ha−1 on woodland. The world and European averages for above- and below-ground C density of forest were about 86 t C ha−1 in 1994 and 53.5 t C ha−1 in 1995, respectively.5,23 Carbon budgets for deciduous and evergreen forest and woodland ecosystems in Turkey are shown separately in Table 2.
Ecosystem C stock and flux | Forest | Woodland | Grand total | ||||
---|---|---|---|---|---|---|---|
EF | DF | Total | EF | DF | Total | ||
a EF = coniferous trees; DF = deciduous trees; TB = total biomass; AGB = aboveground biomass; BGB = belowground biomass; GPP = gross primary productivity; NPP = net primary productivity; NEP = net ecosystem productivity; NES = net ecosystem sequestration. The ratios of NPP to GPP, and C to dry biomass were assumed to be 0.5 Mt = 106 t. | |||||||
Area/×103 ha | 6492 | 3462 | 9954 | 4617 | 6142 | 10 759 | 20 713 |
C stock in TB/Mt C | 258.6 | 170.4 | 429.0 | 25.6 | 17.0 | 42.6 | 471.6 |
C stock in AGB/Mt C | 221.2 | 145.8 | 367.0 | 21.9 | 14.5 | 36.4 | 403.4 |
C stock in BGB/Mt C | 37.4 | 24.6 | 62.0 | 3.7 | 2.5 | 6.2 | 68.2 |
GPPTB/Mt C per year | 13.8 | 11.0 | 24.8 | 3.0 | 2.4 | 5.4 | 30.2 |
NPPTB/Mt C per year | 6.9 | 5.5 | 12.4 | 1.5 | 1.2 | 2.7 | 15.1 |
NPPAGB/Mt C per year | 5.9 | 4.7 | 10.6 | 1.3 | 1.0 | 2.3 | 12.9 |
NPPBGB/Mt C per year | 1.0 | 0.8 | 1.8 | 0.2 | 0.2 | 0.4 | 2.2 |
NEP/Mt C per year | 3.6 | 3.7 | 7.3 | 0.9 | 0.8 | 1.7 | 9.0 |
NES/Mt C per year | 0.8 | 1.1 | 1.9 | 0.4 | 0.3 | 0.7 | 2.6 |
The total flux of C from the atmosphere into the forest and woodland ecosystems driven by primary productivity was about 30.2 Mt C per year. Plant respiration of C accounted for half of this gross primary productivity (GPP),21 thus leaving total net primary productivity (NPP) of 15.1 Mt C per year (0.73 t C ha−1 per year), with a ratio of total NPP of forest to that of woodland of 4.6. Approximately 85% and 15% of NPP were sequestered in the above- and below-ground woody biomass of Turkish forest and woodland, respectively. About 48% of the total NPP was felled, and 36% was transferred into the soil organic C (SOC) pool through litterfall and natural losses. The remaining 16% (0.12 t C ha−1 per year) was sequestered in the live woody biomass of the forest and woodland. About 88.5% of fellings (0.35 t C ha−1 per year) were removed from the forest and woodland, and the remaining 11.5% was transferred as felling residues to the SOC pool.
Soil respiration (Rh) was assumed to be equal to the total input rate of plant residues of 0.30 t C ha−1 per year. Net ecosystem productivity (NEP) as the difference between NPP and soil respiration was estimated at 0.43 t C ha−1 per year. The estimated net release of C was about 1.34 t C ha−1 (or 21.5 Mt C) from plant and soil respirations and decay of wood products of the forest and woodland ecosystems of Turkey to the atmosphere in 1996. When biomass removed out of the forest ecosystems was taken into account, net ecosystem sequestration (NES) resulted in 0.12 t C ha−1 per year (Fig. 1). Total C stock in wood products in 2001 was estimated at 0.64 t C ha−1.4 Karjalainen et al.23 found in the calculation of the C budget of 27 European countries between 1995 and 2000 that average NPP, Rh, NEP and NES were 3.18 t C ha−1 per year, 1.9 t C ha−1 per year, 1.28 t C ha−1 per year, and 0.66 t C ha−1 per year, respectively. For only productive forests of Turkey, Nabuurs and Schelhaas26 reported, on average, a C stock in vegetation of 24.73 t C ha−1, NEP of 0.53 t C ha−1 per year, and NES of 0.25 t C ha−1 per year. The above average values reported by Karjalainen et al., and Nabuurs and Schelhaas may be used as a proxy for the estimation of the magnitude of uncertainties involved in this study.
Reducing vulnerability to human-induced disturbances of forests, and speeding their recovery from the disturbances require the continued monitoring of the structure and function of forest ecosystems to update risk assessments and actions in an adaptive management system. Actions needed to be undertaken for sustainable forest management and conservation in Turkey range from forest policy reviews, new legal instruments, restructuring of institutions, and public participation to implementation of ecological indicators, quantification of the ecosystem services including C sequestration capacity of forests, and rehabilitation of damaged forest ecosystems.
This journal is © The Royal Society of Chemistry 2004 |