Corre, Marife D.

[["dc.bibliographiccitation.firstpage","1539"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Biological Reviews"],["dc.bibliographiccitation.lastpage","1569"],["dc.bibliographiccitation.volume","92"],["dc.contributor.author","Dislich, Claudia"],["dc.contributor.author","Keyel, Alexander C."],["dc.contributor.author","Salecker, Jan"],["dc.contributor.author","Kisel, Yael"],["dc.contributor.author","Meyer, Katrin M."],["dc.contributor.author","Auliya, Mark"],["dc.contributor.author","Barnes, Andrew D."],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Darras, Kevin"],["dc.contributor.author","Faust, Heiko"],["dc.contributor.author","Hess, Bastian"],["dc.contributor.author","Klasen, Stephan"],["dc.contributor.author","Knohl, Alexander"],["dc.contributor.author","Kreft, Holger"],["dc.contributor.author","Meijide, Ana"],["dc.contributor.author","Nurdiansyah, Fuad"],["dc.contributor.author","Otten, Fenna"],["dc.contributor.author","Pe'er, Guy"],["dc.contributor.author","Steinebach, Stefanie"],["dc.contributor.author","Tarigan, Suria"],["dc.contributor.author","Tölle, Merja H."],["dc.contributor.author","Tscharntke, Teja"],["dc.contributor.author","Wiegand, Kerstin"],["dc.date.accessioned","2017-09-07T11:44:46Z"],["dc.date.available","2017-09-07T11:44:46Z"],["dc.date.issued","2017"],["dc.description.abstract","Oil palm plantations have expanded rapidly in recent decades. This large-scale land-use change has had great ecological, economic, and social impacts on both the areas converted to oil palm and their surroundings. However, research on the impacts of oil palm cultivation is scattered and patchy, and no clear overview exists. We address this gap through a systematic and comprehensive literature review of all ecosystem functions in oil palm plantations, including several (genetic, medicinal and ornamental resources, information functions) not included in previous systematic reviews. We compare ecosystem functions in oil palm plantations to those in forests, as the conversion of forest to oil palm is prevalent in the tropics. We find that oil palm plantations generally have reduced ecosystem functioning compared to forests: 11 out of 14 ecosystem functions show a net decrease in level of function. Some functions show decreases with potentially irreversible global impacts (e.g. reductions in gas and climate regulation, habitat and nursery functions, genetic resources, medicinal resources, and information functions). The most serious impacts occur when forest is cleared to establish new plantations, and immediately afterwards, especially on peat soils. To variable degrees, specific plantation management measures can prevent or reduce losses of some ecosystem functions (e.g. avoid illegal land clearing via fire, avoid draining of peat, use of integrated pest management, use of cover crops, mulch, and compost) and we highlight synergistic mitigation measures that can improve multiple ecosystem functions simultaneously. The only ecosystem function which increases in oil palm plantations is, unsurprisingly, the production of marketable goods. Our review highlights numerous research gaps. In particular, there are significant gaps with respect to socio-cultural information functions. Further, there is a need for more empirical data on the importance of spatial and temporal scales, such as differences among plantations in different environments, of different sizes, and of different ages, as our review has identified examples where ecosystem functions vary spatially and temporally. Finally, more research is needed on developing management practices that can offset the losses of ecosystem functions. Our findings should stimulate research to address the identified gaps, and provide a foundation for more systematic research and discussion on ways to minimize the negative impacts and maximize the positive impacts of oil palm cultivation."],["dc.identifier.doi","10.1111/brv.12295"],["dc.identifier.fs","621226"],["dc.identifier.gro","3148957"],["dc.identifier.pmid","27511961"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14337"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5600"],["dc.language.iso","en"],["dc.notes.intern","Wiegand Crossref Import"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | B | B10: Landschaftsbezogene Bewertung der ökologischen und sozioökonomischen Funktionen von Regenwald- Transformationssystemen in Sumatra (Indonesien)"],["dc.relation.issn","1464-7931"],["dc.relation.orgunit","Abteilung Ökosystemmodellierung"],["dc.relation.orgunit","Wirtschaftswissenschaftliche Fakultät"],["dc.relation.orgunit","Abteilung Bioklimatologie"],["dc.rights","CC BY-NC 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by-nc/4.0/"],["dc.subject.gro","Elaeis guineensis"],["dc.subject.gro","biodiversity"],["dc.subject.gro","ecosystem functions"],["dc.subject.gro","ecosystem services"],["dc.subject.gro","land-use change"],["dc.subject.gro","oil palm"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","A review of the ecosystem functions in oil palm plantations, using forests as a reference system"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","25"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Plant and Soil"],["dc.bibliographiccitation.lastpage","38"],["dc.bibliographiccitation.volume","336"],["dc.contributor.author","Guckland, Anja"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Flessa, Heiner"],["dc.date.accessioned","2018-11-07T08:37:48Z"],["dc.date.available","2018-11-07T08:37:48Z"],["dc.date.issued","2010"],["dc.description.abstract","The mixture of other broadleaf species into beech forests in Central Europe leads to an increase of tree species diversity, which may alter soil biochemical processes. This study was aimed at 1) assessing differences in gross rates of soil N cycling among deciduous stands of different beech (Fagus sylvatica L.) abundance in a limestone area, 2) analyzing the relationships between gross rates of soil N cycling and forest stand N cycling, and 3) quantifying N2O emission and determining its relationship with gross rates of soil N cycling. We used N-15 pool dilution techniques for soil N transformation measurement and chamber method for N2O flux measurement. Gross rates of mineral N production in the 0-5 cm mineral soil increased across stands of decreasing beech abundance and increasing soil clay content. These rates were correlated with microbial biomass which, in turn, was influenced by substrate quantity, quality and soil fertility. Leaf litter-N, C:N ratio and base saturation in the mineral soil increased with decreasing beech abundance. Soil mineral N production and assimilation by microbes were tightly coupled, resulting in low N2O emissions. Annual N2O emissions were largely contributed by the freeze-thaw event emissions, which were correlated with the amount of soil microbial biomass. Our results suggest that soil N availability may increase through the mixture of broadleaf species into beech forests."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft (DFG) [Graduiertenkolleg 1086]"],["dc.identifier.doi","10.1007/s11104-010-0437-8"],["dc.identifier.isi","000283367600004"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/7634"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/18622"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","0032-079X"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Variability of soil N cycling and N2O emission in a mixed deciduous forest with different abundance of beech"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","6318"],["dc.bibliographiccitation.issue","15"],["dc.bibliographiccitation.journal","Proceedings of the National Academy of Sciences"],["dc.bibliographiccitation.lastpage","6322"],["dc.bibliographiccitation.volume","108"],["dc.contributor.author","Powers, J. S."],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Twine, T. E."],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:34Z"],["dc.date.available","2017-09-07T11:43:34Z"],["dc.date.issued","2011"],["dc.identifier.doi","10.1073/pnas.1016774108"],["dc.identifier.gro","3150178"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/7064"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6914"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.relation.issn","0027-8424"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Geographic bias of field observations of soil carbon stocks with tropical land-use changes precludes spatial extrapolation"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","yes"],["dc.type.version","submitted_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","123"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","SOIL"],["dc.bibliographiccitation.lastpage","137"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","de Blécourt, Marleen"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Paudel, Ekananda"],["dc.contributor.author","Harrison, Rhett D."],["dc.contributor.author","Brumme, Rainer"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2020-12-10T18:47:55Z"],["dc.date.available","2020-12-10T18:47:55Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.5194/soil-3-123-2017"],["dc.identifier.eissn","2199-398X"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78945"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Spatial variability in soil organic carbon in a tropical montane landscape: associations between soil organic carbon and land use, soil properties, vegetation, and topography vary across plot to landscape scales"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2311"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Biogeosciences"],["dc.bibliographiccitation.lastpage","2325"],["dc.bibliographiccitation.volume","7"],["dc.contributor.author","Koehler, B."],["dc.contributor.author","Zehe, E."],["dc.contributor.author","Corre, M. D."],["dc.contributor.author","Veldkamp, E."],["dc.date.accessioned","2017-09-07T11:43:41Z"],["dc.date.available","2017-09-07T11:43:41Z"],["dc.date.issued","2010"],["dc.description.abstract","Soil respiration is the second largest flux in the global carbon cycle, yet the underlying below-ground process, carbon dioxide (CO2) production, is not well understood because it can not be measured in the field. CO2 production has frequently been calculated from the vertical CO2 diffusive flux divergence, known as \"soil-CO2 profile method\". This relatively simple model requires knowledge of soil CO2 concentration profiles and soil diffusive properties. Application of the method for a tropical lowland forest soil in Panama gave inconsistent results when using diffusion coefficients (D) calculated based on relationships with soil porosity and moisture (\"physically modeled\" D). Our objective was to investigate whether these inconsistencies were related to (1) the applied interpolation and solution methods and/or (2) uncertainties in the physically modeled profile of D. First, we show that the calculated CO2 production strongly depends on the function used to interpolate between measured CO2 concentrations. Secondly, using an inverse analysis of the soil-CO2 profile method, we deduce which D would be required to explain the observed CO2 concentrations, assuming the model perception is valid. In the top soil, this inversely modeled D closely resembled the physically modeled D. In the deep soil, however, the inversely modeled D increased sharply while the physically modeled D did not. When imposing a constraint during the fit parameter optimization, a solution could be found where this deviation between the physically and inversely modeled D disappeared. A radon (Rn) mass balance model, in which diffusion was calculated based on the physically modeled or constrained inversely modeled D, simulated observed Rn profiles reasonably well. However, the CO2 concentrations which corresponded to the constrained inversely modeled D were too small compared to the measurements. We suggest that, in well-structured soils, a missing description of steady state CO2 exchange fluxes across water-filled pores causes the soil-CO2 profile method to fail. These fluxes are driven by the different diffusivities in inter- vs. intra-aggregate pores which create permanent CO2 gradients if separated by a \"diffusive water barrier\". These results corroborate other studies which have shown that the theory to treat gas diffusion as homogeneous process, a precondition for use of the soil-CO2 profile method, is inaccurate for pore networks which exhibit spatial separation between CO2 production and diffusion out of the soil."],["dc.identifier.doi","10.5194/bg-7-2311-2010"],["dc.identifier.fs","570252"],["dc.identifier.gro","3150209"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/5240"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6948"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.notes.status","final"],["dc.relation.issn","1726-4189"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","CO2 production"],["dc.subject.ddc","570"],["dc.title","An inverse analysis reveals limitations of the soil-CO2 profile method to calculate CO2 production and efflux for well-structured soils"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","42"],["dc.bibliographiccitation.journal","Geoderma"],["dc.bibliographiccitation.lastpage","50"],["dc.bibliographiccitation.volume","284"],["dc.contributor.author","Allen, Kara"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Kurniawan, Syahrul"],["dc.contributor.author","Utami, Sri Rahayu"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:32Z"],["dc.date.available","2017-09-07T11:43:32Z"],["dc.date.issued","2016"],["dc.description.abstract","Forest conversion to agriculture can decrease soil nutrient stocks overtime. However, inherent spatial variability in soil biochemical properties in converted landscapes could be high, and may supersede effects of land-use change on soil nutrient changes. Our aims were to assess changes in soil nutrient stocks with land-use change, and to quantify the proportions of spatial variability and land-use change effects on the overall variance of soil nutrient stocks. This study was conducted in Jambi Province, Sumatra, Indonesia in two distinct landscapes defined by the dominant soil texture and type: loam and clay Acrisol soils. In each landscape, four land-use types were examined: lowland forest and rubber interspersed in naturally regenerating forest (referred here as “jungle rubber”) as reference land uses and smallholder plantations of rubber and oil palm. In the 0–0.5 m soil depth of the reference land uses, the clay Acrisol had higher total N (660.1 ± 63.8–1074.2 ± 158.8 g N m− 2; P ≤ 0.05), exchangeable Ca (24.1 ± 5.7–80.6 ± 22.8 g Ca m− 2; P ≤ 0.06), Mg (4.3 ± 0.6–39.2 ± 16.3 g Mg m− 2; P ≤ 0.02), K (11.7 ± 0.7–34.7 ± 12.1 g K m− 2; P ≤ 0.06), extractable P (1.1 ± 0.1–2.6 ± 0.1 g P m− 2; P ≤ 0.001) and effective cation exchange capacity (ECEC; 11.4 ± 3.1–40.6 ± 11.0 cmolc kg− 1; P = 0.02), illustrating that clay content influenced soil fertility in these highly weathered soils. Compared to the reference land uses, the oil palm plantations had higher soil pH (4.2 ± 0.0–4.6 ± 0.1; P ≤ 0.04), base saturation (8.9 ± 1.6–6.5 ± 1.3%; P ≤ 0.07) and extractable P (0.8 ± 0.1–6.1 ± 3.2 g P m− 2; P ≤ 0.01) in the top 0.5 m depth, which was probably due to the legacy effect of biomass burning and fertilization. We were unable to detect significant effects of land-use change on other soil biochemical characteristics (i.e., ECEC, stocks of exchangeable bases, soil organic carbon (SOC), total N). Based on variance components analysis, a large proportion of the variance of these parameters was accounted by the variation among replicate plots (26–91%) rather than by land-use types (only 0–6%). Power analysis showed that the optimum number of replicate plots to detect land-use change effects on these parameters ranged from 5 to 7. Our results suggest that spatial variability must be represented in the experimental design in order to detect land-use change effects on soil nutrient changes through stratifying the area of inference (i.e., landscape or region) based on known drivers of soil fertility and determining the optimal number of experimental units."],["dc.identifier.doi","10.1016/j.geoderma.2016.08.010"],["dc.identifier.gro","3150168"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6903"],["dc.language.iso","en"],["dc.notes.status","public"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | A | A05: Optimierung des Nährstoffmanagements in Ölpalmplantagen und Hochrechnung plot-basierter Treibhausgasflüsse auf die Landschaftsebene transformierter Regenwälder"],["dc.relation.issn","0016-7061"],["dc.subject","Soil nutrient stocks; Lowland forest; Rubber; Oil palm; Land-use change"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","Spatial variability surpasses land-use change effects on soil biochemical properties of converted lowland landscapes in Sumatra, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","117522"],["dc.bibliographiccitation.journal","Forest Ecology and Management"],["dc.bibliographiccitation.volume","451"],["dc.contributor.author","Tchiofo Lontsi, Rodine"],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","van Straaten, Oliver"],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2019-12-13T16:52:30Z"],["dc.date.available","2019-12-13T16:52:30Z"],["dc.date.issued","2019"],["dc.description.abstract","Although disturbances associated with selective logging can cause pronounced changes in soil characteristics and nutrient stocks, such information is very limited for highly weathered soils in Africa. We assessed the effects of reduced impact logging (RIL, with a 30-year rotation management plan) and conventional logging (CL, without a management plan) on physical and biochemical characteristics of Ferralsol soils that developed on pre-Cambrian rocks in rainforests of Cameroon. Five to seven months after the logging operations were completed, we mapped the CL and RIL sites and quantified the disturbed areas: felling gaps, skidding trails, logging decks and roads. We selected four replicate plots at each site that encompassed these four disturbed strata and an adjacent undisturbed area as the reference. At each disturbed stratum and reference area per plot, we took soil samples down to 50 cm, and quantified soil physical and biochemical characteristics. Nutrient exports with timber harvest were also quantified. The logging intensity was very low with removals of 0.2 and 0.3 tree per hectare, and the ground area disturbed accounted only 5.2% and 4.0% of the total area in CL and RIL, respectively. In terms of area disturbance for each harvested tree, CL had 753 m 2 tree −1 more affected ground area than RIL. Roads and logging decks were the most affected by logging operations, where effective cation exchange capacity, soil organic carbon (SOC), total nitrogen (N), Bray-extractable phosphorus (P) and exchangeable aluminum decreased whereas pH, 15 N natural abundance and exchangeable manganese increased compared to the undisturbed reference area (P < 0.01-0.04). The disturbed area showed overall reductions of 21-29% in SOC, N and P stocks relative to the reference areas (P = 0.02-0.07). The amounts of C, N, P and base cations exported with harvested timber were only 0.4-5.9% of the changes in stocks of these elements in the disturbed strata. Nutrient reductions in the soil and exports through timber harvest were comparable between CL and RIL, after one logging event in this very low intensity logging systems. Our results suggest that unplanned operations together with frequent re-logging inherent to CL can increase area damage and enhance changes in SOC and nutrients as opposed to RIL, which may affect the recovery of the succeeding vegetation."],["dc.identifier.doi","10.1016/j.foreco.2019.117522"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62756"],["dc.language.iso","en"],["dc.relation.issn","0378-1127"],["dc.title","Changes in soil organic carbon and nutrient stocks in conventional selective logging versus reduced-impact logging in rainforests on highly weathered soils in Southern Cameroon"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","59"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Nutrient Cycling in Agroecosystems"],["dc.bibliographiccitation.lastpage","79"],["dc.bibliographiccitation.volume","124"],["dc.contributor.author","Quiñones, Cecille Marie O."],["dc.contributor.author","Veldkamp, Edzo"],["dc.contributor.author","Lina, Suzette B."],["dc.contributor.author","Bande, Marlito Jose M."],["dc.contributor.author","Arribado, Arwin O."],["dc.contributor.author","Corre, Marife D."],["dc.date.accessioned","2022-09-01T09:49:21Z"],["dc.date.available","2022-09-01T09:49:21Z"],["dc.date.issued","2022"],["dc.description.abstract","Abstract\n \n Field-based quantification of soil greenhouse gas emissions from the Philippines’ agriculture sector is missing for vegetable production systems, despite its substantial contribution to agricultural production. We quantified soil N\n 2\n O emission, CH\n 4\n uptake, and CO\n 2\n efflux in vegetable farms and compared these to the secondary forest. Measurements were conducted for 13 months in 10 smallholder farms and nine forest plots on Andosol soil in Leyte, Philippines using static chambers. Soil N\n 2\n O and CO\n 2\n emissions were higher, whereas CH\n 4\n uptake was lower in the vegetable farms than in the forest. Vegetable farms had annual fluxes of 12.7 ± 2.6 kg N\n 2\n O-N ha\n −1\n  yr\n −1\n , −1.1 ± 0.2 kg CH\n 4\n -C ha\n −1\n  yr\n −1\n , and 11.7 ± 0.7 Mg CO\n 2\n -C ha\n −1\n  yr\n −1\n , whereas the forest had 0.10 ± 0.02 kg N\n 2\n O-N ha ha\n −1\n  yr\n −1\n , −2.0 ± 0.2 kg CH\n 4\n -C ha\n −1\n  yr\n −1\n , and 8.2 ± 0.7 Mg CO\n 2\n -C ha\n −1\n  yr\n −1\n . Long-term high N fertilization rates in vegetable farms resulted in large soil mineral N levels, dominated by NO\n 3\n –\n in the topsoil and down to 1-m depth, leading to high soil N\n 2\n O emissions. Increased soil bulk density in the vegetable farms probably increased anaerobic microsites during the wet season and reduced CH\n 4\n diffusion from the atmosphere into the soil, resulting in decreased soil CH\n 4\n uptake. High soil CO\n 2\n emissions from the vegetable farms suggested decomposition of labile organic matter, possibly facilitated by plowing and large N fertilization rates. The global warming potential of these vegetable farms was 31 ± 2.7 Mg CO\n 2\n -eq ha\n −1\n  yr\n −1\n (100-year time frame)."],["dc.identifier.doi","10.1007/s10705-022-10222-4"],["dc.identifier.pii","10222"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/113399"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-597"],["dc.relation.eissn","1573-0867"],["dc.relation.issn","1385-1314"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Soil greenhouse gas fluxes from tropical vegetable farms, using forest as a reference"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","5243"],["dc.bibliographiccitation.issue","21"],["dc.bibliographiccitation.journal","Biogeosciences"],["dc.bibliographiccitation.lastpage","5262"],["dc.bibliographiccitation.volume","17"],["dc.contributor.author","Formaglio, Greta"],["dc.contributor.author","Veldkamp, Edzo"],["dc.contributor.author","Duan, Xiaohong"],["dc.contributor.author","Tjoa, Aiyen"],["dc.contributor.author","Corre, Marife D."],["dc.date.accessioned","2021-04-14T08:31:02Z"],["dc.date.available","2021-04-14T08:31:02Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.5194/bg-17-5243-2020"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/17656"],["dc.identifier.url","https://publications.goettingen-research-online.de/handle/2/83463"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.notes.intern","Merged from goescholar"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | A | A05: Optimierung des Nährstoffmanagements in Ölpalmplantagen und Hochrechnung plot-basierter Treibhausgasflüsse auf die Landschaftsebene transformierter Regenwälder"],["dc.relation.eissn","1726-4189"],["dc.rights","CC BY 4.0"],["dc.rights.uri","http://creativecommons.org/licenses/by/4.0/"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","Herbicide weed control increases nutrient leaching compared to mechanical weeding in a large-scale oil palm plantation"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","3802"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","3813"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Matson, Amanda L."],["dc.contributor.author","Corre, Marife D."],["dc.contributor.author","Veldkamp, Edzo"],["dc.date.accessioned","2017-09-07T11:43:42Z"],["dc.date.available","2017-09-07T11:43:42Z"],["dc.date.issued","2014"],["dc.identifier.doi","10.1111/gcb.12668"],["dc.identifier.gro","3150204"],["dc.identifier.pmid","24965673"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6943"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.relation.issn","1354-1013"],["dc.title","Nitrogen cycling in canopy soils of tropical montane forests responds rapidly to indirect N and P fertilization"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]