fix Makiranta_2012_tiol

#239

data/ForC_citations.csv

@@ -988,7 +988,7 @@ Maier_2004_rcua,10.1111/j.1529-8817.2003.00809.x,Maier,2004,Respiratory carbon u
 Major_2010_fosb,10.1111/j.1365-2486.2009.02044.x,Major,2010,"Fate of soil-applied black carbon: downward migration, leaching and soil respiration","MAJOR, J., LEHMANN, J., RONDON, M., & GOODALE, C. (2010). Fate of soil-applied black carbon: downward migration, leaching and soil respiration. Global Change Biology, 16(4), 1366-1379. doi:10.1111/j.1365-2486.2009.02044.x",English,https://onlinelibrary.wiley.com/doi/abs/10.1111/j.1365-2486.2009.02044.x,"Black carbon (BC) is an important pool of the global C cycle, because it cycles much more slowly than others and may even be managed for C sequestration. Using stable isotope techniques, we investigated the fate of BC applied to a savanna Oxisol in Colombia at rates of 0, 11.6, 23.2 and 116.1 t BC ha-1, as well as its effect on non-BC soil organic C. During the rainy seasons of 2005 and 2006, soil respiration was measured using soda lime traps, particulate and dissolved organic C (POC and DOC) moving by saturated flow was sampled continuously at 0.15 and 0.3 m, and soil was sampled to 2.0 m. Black C was found below the application depth of 0-0.1 m in the 0.15-0.3 m depth interval, with migration rates of 52.4±14.5, 51.8±18.5 and 378.7±196.9 kg C ha-1 yr-1 (±SE) where 11.6, 23.2 and 116.1 t BC ha-1, respectively, had been applied. Over 2 years after application, 2.2% of BC applied at 23.2 t BC ha-1 was lost by respiration, and an even smaller fraction of 1% was mobilized by percolating water. Carbon from BC moved to a greater extent as DOC than POC. The largest flux of BC from the field (20-53% of applied BC) was not accounted for by our measurements and is assumed to have occurred by surface runoff during intense rain events. Black C caused a 189% increase in aboveground biomass production measured 5 months after application (2.4-4.5 t additional dry biomass ha-1 where BC was applied), and this resulted in greater amounts of non-BC being respired, leached and found in soil for the duration of the experiment. These increases can be quantitatively explained by estimates of greater belowground net primary productivity with BC addition. ",NAC,NA,0
 Makiranta_2007_sgge,NAC,Makiranta,2007,Soil greenhouse gas emissions from afforested organic soil croplands and cutaway peatlands,NAC,English,NAC,NAC,NAC,1,0
 Makiranta_2008_fcta,10.1016/j.soilbio.2008.01.009,Makiranta,2008,Factors causing temporal and spatial variation in heterotrophic and rhizospheric components of soil respiration in afforested organic soil croplands in Finland,"Makiranta, P., Minkkinen, K., Hytonen, J., & Laine, J. (2008). Factors causing temporal and spatial variation in heterotrophic and rhizospheric components of soil respiration in afforested organic soil croplands in Finland. Soil Biology and Biochemistry, 40(7), 1592-1600. doi:10.1016/j.soilbio.2008.01.009",English,https://linkinghub.elsevier.com/retrieve/pii/S0038071708000631,"Partitioning soil respiration (SR) into its components, heterotrophic and rhizospheric respiration, is an important step for understanding and modelling carbon (C) cycling in organic soils. However, no partitioning studies on afforested organic soil croplands exist. We separated soil respiration originating from the decomposition of peat (SRP), and aboveground litter (SRL) and root respiration (SRR) in six afforested organic soil croplands in Finland with varying tree species and stand ages using the trenching method. Across the sites temporal variation in SR was primarily related to changes in soil surface temperature (-5 cm), which explained 71-96% of variation in SR rates. Decomposition of peat and litter was not related to changes in water table level, whereas a minor increase in root respiration was observed with the increase in water table depth. Temperature sensitivity of SR varied between the different respiration components: SRP was less sensitive to changes in soil surface temperature than SRL or SRR. Factors explaining spatial variation in SR differed between different respiration components. Annual SRP correlated positively with peat ash content while that of SRL was found to correlate positively with the amount of litter on the forest floor, separately for each tree species. Root respiration correlated positively with the biomass of ground vegetation. From the total soil respiration peat decomposition comprised a major share of 42%; the proportion of autotrophic respiration being 41% and aboveground litter 17%. Afforestation lowered peat decomposition rates. Nevertheless the effect of agricultural history can be seen in peat properties for decades and due to high peat decomposition rates these soils still loose carbon to the atmosphere.",NAC,NA,0
-Makiranta_2012_tiol,10.1016/j.soilbio.2012.01.005,Makiranta,2012,The impact of logging residue on soil GHG fluxes in a drained peatland forest,"Makiranta, P., Laiho, R., Penttila, T., & Minkkinen, K. (2012). The impact of logging residue on soil GHG fluxes in a drained peatland forest. Soil Biology and Biochemistry, 48, 1-9. doi:10.1016/j.soilbio.2012.01.005",English,https://linkinghub.elsevier.com/retrieve/pii/S0038071712000181,"Northern peatlands contain substantial reservoirs of carbon (C). Forestry activities endanger the C storages in some of these areas. While the initial impacts of forestry drainage on peatland greenhouse gas (GHG) balance have been studied, the impacts of other silvicultural practices, e.g. logging residue (LR) retention or removal, are not known. We measured the CH4, N2O and CO2 fluxes between peat soil and atmosphere with and without decomposing LR over three (2002-2004) seasons (May-Oct) following clearfelling in a drained peatland forest, along with the mass loss of LR. Seasonal average CO2 efflux from plots with LR (3070 g CO2 m-2 season-1) was twice as high as that from plots without LR (1447 g CO2 m-2 season-1). Less than 40% of this difference was accounted for by the decay of logging residues (530 g CO2 m-2 season-1), so the majority of the increased CO2 efflux was caused by increased soil organic matter decomposition under the LR. Furthermore LR increased soil N2O fluxes over 3-fold (0.70 g N2O m-2 season-1), compared to plots without LR (0.19 g N2O m-2 season-1), while no change in CH4 emissions was observed. Our results indicate that LR retention in clearfelled peatland sites may significantly increase GHG emissions and C release from the soil organic matter C storage. This would make the harvesting of LR for biofuel more beneficial, in the form of avoided emissions. Further investigations of the sources of CO2 under logging residues are, however, needed to confirm this finding.",NAC,NA,0
+Makiranta_2012_tiol,10.1016/j.soilbio.2012.01.005,Makiranta,2012,The impact of logging residue on soil GHG fluxes in a drained peatland forest,"Makiranta, P., Laiho, R., Penttila, T., & Minkkinen, K. (2012). The impact of logging residue on soil GHG fluxes in a drained peatland forest. Soil Biology and Biochemistry, 48, 1-9. doi:10.1016/j.soilbio.2012.01.005",English,https://linkinghub.elsevier.com/retrieve/pii/S0038071712000181,"Northern peatlands contain substantial reservoirs of carbon (C). Forestry activities endanger the C storages in some of these areas. While the initial impacts of forestry drainage on peatland greenhouse gas (GHG) balance have been studied, the impacts of other silvicultural practices, e.g. logging residue (LR) retention or removal, are not known. We measured the CH4, N2O and CO2 fluxes between peat soil and atmosphere with and without decomposing LR over three (2002-2004) seasons (May-Oct) following clearfelling in a drained peatland forest, along with the mass loss of LR. Seasonal average CO2 efflux from plots with LR (3070 g CO2 m-2 season-1) was twice as high as that from plots without LR (1447 g CO2 m-2 season-1). Less than 40% of this difference was accounted for by the decay of logging residues (530 g CO2 m-2 season-1), so the majority of the increased CO2 efflux was caused by increased soil organic matter decomposition under the LR. Furthermore LR increased soil N2O fluxes over 3-fold (0.70 g N2O m-2 season-1), compared to plots without LR (0.19 g N2O m-2 season-1), while no change in CH4 emissions was observed. Our results indicate that LR retention in clearfelled peatland sites may significantly increase GHG emissions and C release from the soil organic matter C storage. This would make the harvesting of LR for biofuel more beneficial, in the form of avoided emissions. Further investigations of the sources of CO2 under logging residues are, however, needed to confirm this finding.",NAC,1,0
 Maldague_1963_ofem,NAC,Maldague,1963,Observations fauntistique et microbiologiques dans quelques biotopes forestiers equatoriaux,NAC,French,NAC,NAC,NAC,0,0
 Malhi_1998_cdto,10.1029/98JD02647,Malhi,1998,Carbon dioxide transfer over a Central Amazonian rain forest,"Malhi, Y., Nobre, A. D., Grace, J., Kruijt, B., Pereira, M. G. P., Culf, A., & Scott, S. (1998). Carbon dioxide transfer over a Central Amazonian rain forest. Journal of Geophysical Research: Atmospheres, 103(D24), 31593-31612. doi:10.1029/98jd02647",English,https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/98JD02647,"Tropical rain forests are among the most important and least monitored of terrestrial ecosystems. In recent years, their influence on atmospheric concentrations of carbon dioxide and water vapor has become the subject of much speculation. Here we present results from a yearlong study of CO2 fluxes at a tropical forest in central Amazonia, using the micrometeorological technique of eddy covariance. The diurnal cycle of CO2 flux was consistent with previous short-term studies in tropical rain forests, implying that the Amazonian rain forest shows a fair degree of spatial uniformity in bulk ecophysiological characteristics. Typical peak daytime photosynthesis rates were 24-28 µmol CO2 m-2 s-1, and respiration rates were 6-8 µmol CO2 m-2 s-1. There was significant seasonality in peak photosynthesis over the year, which appeared strongly correlated with soil moisture content. On the other hand, there was no evidence of strong seasonality in soil respiration. Central Amazonia has only a short, 3-month dry season, not atypical of tropical rain forest, and it is therefore likely that large areas of Amazonia exhibit significant seasonality in photosynthetic capacity. The gross primary production was calculated to be 30 t C ha-1 yr-1. An analysis of data quality is included in the appendix. ",NAC,NA,0
 Malhi_1999_tcbo,10.1046/j.1365-3040.1999.00453.x,Malhi,1999,"The carbon balance of tropical, temperate and boreal forests","MALHI, Y., BALDOCCHI, D. D., & JARVIS, P. G. (1999). The carbon balance of tropical, temperate and boreal forests. Plant, Cell and Environment, 22(6), 715-740. doi:10.1046/j.1365-3040.1999.00453.x",English,https://onlinelibrary.wiley.com/doi/full/10.1046/j.1365-3040.1999.00453.x,"Forest biomes are major reserves for terrestrial carbon, and major components of global primary productivity. The carbon balance of forests is determined by a number of component processes of carbon acquisition and carbon loss, and a small shift in the magnitude of these processes would have a large impact on the global carbon cycle. In this paper, we discuss the climatic influences on the carbon dynamics of boreal, temperate and tropical forests by presenting a new synthesis of micrometeorological, ecophysiological and forestry data, concentrating on three case-study sites. Historical changes in the carbon balance of each biome are also reviewed, and the evidence for a carbon sink in each forest biome and its likely behaviour under future global change are discussed. We conclude that there have been significant advances in determining the carbon balance of forests, but there are still critical uncertainties remaining, particularly in the behaviour of soil carbon stocks. ",NAC,NA,0

data/ForC_measurements.csv

@@ -25750,7 +25750,7 @@ measurement.ID,sites.sitename,plot.name,stand.age,dominant.life.form,dominant.ve
 26617,Baotianman Natural Reserve,Temperate Deciduous Forest. Stand established around 1958,50,woody,2TDB,NA,Quercus aliena,LAI,2008,8,2007.5,7.5,2008.5,7.5,3.5,NAC,NAC,NA,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,R,1389,NA,NA,NA,NA,NA,NA,Luan_2012_roba,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4911.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0
 26618,Baotianman Natural Reserve,Temperate Deciduous Forest. Stand established around 1958,50,woody,2TDN,NA,Pinus armandii,soil_C2N,2008,8,2007.5,7.5,2008.5,7.5,14.92,NAC,NAC,NA,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,R,1678,NA,NA,NA,NA,NA,NA,Luan_2012_roba,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4912.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0
 26619,Baotianman Natural Reserve,Temperate Deciduous Forest. Stand established around 1958,50,woody,2TDN,NA,Pinus armandii,LAI,2008,8,2007.5,7.5,2008.5,7.5,2.96,NAC,NAC,NA,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,R,1389,NA,NA,NA,NA,NA,NA,Luan_2012_roba,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4912.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0
-26620,Vesijako Research Forest,Boreal Evergreen Forest. Stand established around 1950,55,woody,2TEN,NA,Pinus sylvestris; Picea abies; Betula pubescens,biomass_ag_C,NAC,9,NAC,9,NAC,9,132.4,NAC,NAC,NAC,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NAC,NA,NAC,NA,NA,NA,NA,NA,I,NA,NA,NA,NA,NA,NA,NA,Makiranta_2012_tiol,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4919.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",1
+26620,Vesijako Research Forest,Boreal Evergreen Forest. Stand established around 1950,55,woody,2TEN,NA,Pinus sylvestris (81%); Picea abies (10%); Betula pubescens (9%). ,biomass_OM,2001,8,NAC,9,NAC,9,132.4,NAC,NAC,NAC,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NAC,NA,NAC,NA,NA,NA,NA,NA,I,NA,NA,NA,NA,NA,NA,NA,Makiranta_2012_tiol,Bond-Lamberty_2004_corr,Table 2,SRDB Record_number:4919.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,1,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0
 26623,Hesse,Temperate Deciduous Forest. Stand established around 1963,40,woody,2TDB,NA,Fagus sylvatica,soil_C2N,2003.5,8,2002.5,7.5,2004.5,7.5,10.9,NAC,NAC,NA,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,R,1679,NA,NA,NA,NA,NA,NA,Ngao_2012_svos,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4943.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0
 26624,Hesse,Temperate Deciduous Forest. Stand established around 1963,40,woody,2TDB,NA,Fagus sylvatica,LAI,2003.5,8,2002.5,7.5,2004.5,7.5,6.9,NAC,NAC,NA,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,R,1390,NA,NA,NA,NA,NA,NA,Ngao_2012_svos,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4943.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0
 26625,Hesse,Temperate Deciduous Forest. Stand established around 1963,40,woody,2TDB,NA,Fagus sylvatica,soil_C2N,2003.5,8,2002.5,7.5,2004.5,7.5,11.7,NAC,NAC,NA,NAC,NAC,NAC,NAC,NAC,NAC,NA,NA,NA,NA,NA,NA,NA,NA,NA,NA,R,1679,NA,NA,NA,NA,NA,NA,Ngao_2012_svos,Bond-Lamberty_2004_corr,NAC,SRDB Record_number:4944.,NA,Ben Bond-Lamberty; R script: Bond-Lamberty,0,Ben Bond-Lamberty,"Bond-Lamberty_2004_corr, Anderson-Teixeira_2018_fagd",0

data/ForC_sites.csv

@@ -2856,7 +2856,7 @@ site.ID,sites.sitename,network,alt.names,super.site,city,state,country,lat,lon,c
 2961,NHM,NAC,NAC,NA,NAC,Missouri,USA,37.1,-91.2,(minutes rounded),NAC,NA,13.3,NAC,NAC,1120,NA,NAC,NAC,NAC,NAC,Alfisols and Ultisols,Alfisols and Ultisols,Soil Drainage:  Dry,NA,1044,North America,Nearctic,Cfa,Temperate continental forest,NA,Li_2012_rcli,Li_2012_rcli,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
 2962,UAM,NAC,NAC,NA,NAC,Missouri,USA,37.1,-91.2,(minutes rounded),NAC,NA,13.3,NAC,NAC,1120,NA,NAC,NAC,NAC,NAC,Alfisols and Ultisols,Alfisols and Ultisols,Soil Drainage:  Dry,NA,1044,North America,Nearctic,Cfa,Temperate continental forest,NA,Li_2012_rcli,Li_2012_rcli,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
 2963,EAM,NAC,NAC,NA,NAC,Missouri,USA,37.1,-91.2,(minutes rounded),NAC,NA,13.3,NAC,NAC,1120,NA,NAC,NAC,NAC,NAC,Alfisols and Ultisols,Alfisols and Ultisols,Soil Drainage:  Dry,NA,1044,North America,Nearctic,Cfa,Temperate continental forest,NA,Li_2012_rcli,Li_2012_rcli,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
-2964,Vesijako Research Forest,NAC,NAC,NA,NAC,NAC,Finland,61.36667,25.11667,NAC,NAC,NA,NAC,NAC,NAC,NAC,NA,NAC,NAC,NAC,NAC,Histosol,Histosol,Soil Drainage:  Dry,NA,905,Europe,Palearctic,Dfc,Boreal coniferous forest,NA,Makiranta_2012_tiol,Makiranta_2012_tiol,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
+2964,Vesijako Research Forest,NAC,NAC,NA,NAC,NAC,Finland,61.36666667,25.11666667,minute,NAC,NA,NAC,NAC,NAC,NAC,NA,NAC,NAC,NAC,NAC,Histosol,Histosol,Soil Drainage:  Dry,NA,905,Europe,Palearctic,Dfc,Boreal coniferous forest,NA,Makiranta_2012_tiol,Makiranta_2012_tiol,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
 2965,Nikiema_2012_igge research site in Michigan USA,NAC,NAC,NA,NAC,Michigan,USA,46.6,-87.45,NAC,290,NA,NAC,NAC,NAC,NAC,NA,NAC,NAC,NAC,NAC,Sandy loam,"Sandy loam, Bulk density =  0.89 g cm-3.",Soil Drainage:  Dry,NA,1045,North America,Nearctic,Dfb,Temperate continental forest,NA,Nikiema_2012_igge,Nikiema_2012_igge,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
 2966,US-NC1,NAC,NAC,NA,NAC,North Carolina,USA,35.8,-76.667,NAC,5,NA,NAC,NAC,NAC,1320,NA,NAC,NAC,NAC,NAC,"Fluvial, surface loam","Fluvial, surface loam",Soil Drainage:  Dry,NA,540,North America,Nearctic,Cfa,Subtropical humid forest,NA,Noormets_2012_troh,Noormets_2012_troh,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
 2967,US-NC2,NAC,NAC,NA,NAC,North Carolina,USA,35.8,-76.667,NAC,5,NA,NAC,NAC,NAC,1320,NA,NAC,NAC,NAC,NAC,"Fluvial, muck layer","Fluvial, muck layer",Soil Drainage:  Dry,NA,540,North America,Nearctic,Cfa,Subtropical humid forest,NA,Noormets_2012_troh,Noormets_2012_troh,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,0,0,NAC,0,NA,NA,NA
@@ -5233,4 +5233,4 @@ site.ID,sites.sitename,network,alt.names,super.site,city,state,country,lat,lon,c
 3296,HJ Andrews Experimental Forest,NAC,NAC,NA,NAC,Oregon,USA,NA,NA,NAC,NAC,NA,NAC,NAC,NAC,2100,NA,NAC,NAC,NAC,NAC,Clay loam,Clay loam,Soil Drainage:  Dry,NA,NA,NA,NAC,NA,NA,NA,NAC,Campbell_2005_fsra,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,NA,NA,NAC,NA,NA,NA,NA
 3297,Metolius Basin,NAC,NAC,NA,NAC,Oregon,USA,NA,NA,NAC,NAC,NA,NAC,NAC,NAC,520,NA,NAC,NAC,NAC,NAC,Sandy loam,Sandy loam,Soil Drainage:  Dry,NA,NA,NA,NAC,NA,NA,NA,NAC,Campbell_2005_fsra,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,NA,NA,NAC,NA,NA,NA,NA
 3305,Vedrova_1997_omdi research site in Russia,NAC,NAC,NA,NAC,NAC,Russia,NA,NA,NAC,NAC,NA,NAC,NAC,NAC,NAC,NA,NAC,NAC,NAC,NAC,Sandy loam,Sandy loam,Soil Drainage:  Dry,NA,NA,NA,NAC,NA,NA,NA,NAC,Vedrova_1997_omdi,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,NA,NA,NAC,NA,NA,NA,NA
-3322,Antonov_1990_dosr research site in Bulgaria,NAC,NAC,NA,NAC,NAC,Bulgaria,NA,NA,NAC,1810,NA,NAC,NAC,NAC,NAC,NA,NAC,NAC,NAC,NAC,Mountainous-forest soil,Mountainous-forest soil,Soil Drainage:  Dry,NA,NA,NA,NAC,NA,NA,NA,NAC,Antonov_1990_dosr,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,NA,NA,NAC,NA,NA,NA,NA
+3322,Antonov_1990_dosr research site in Bulgaria,NAC,NAC,NA,NAC,NAC,Bulgaria,NA,NA,NAC,1810,NA,NAC,NAC,NAC,NAC,NA,NAC,NAC,NAC,NAC,Mountainous-forest soil,Mountainous-forest soil,Soil Drainage:  Dry,NA,NA,NA,NAC,NA,NA,NA,NAC,Antonov_1990_dosr,NA,NA,Bond-Lamberty_2004_corr,R script: Bond-Lamberty,NA,NA,NAC,NA,NA,NA,NA