Schwendenmann, Luitgard

[["dc.bibliographiccitation.firstpage","327"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Plant and Soil"],["dc.bibliographiccitation.lastpage","335"],["dc.bibliographiccitation.volume","376"],["dc.contributor.author","Meißner, Meik"],["dc.contributor.author","Köhler, Michael"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Hölscher, Dirk"],["dc.contributor.author","Dyckmans, Jens"],["dc.date.accessioned","2017-09-07T11:45:37Z"],["dc.date.available","2017-09-07T11:45:37Z"],["dc.date.issued","2014"],["dc.identifier.doi","10.1007/s11104-013-1970-z"],["dc.identifier.gro","3149058"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5702"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.publisher","Springer Nature"],["dc.relation.issn","0032-079X"],["dc.title","Soil water uptake by trees using water stable isotopes (δ2H and δ18O)−a method test regarding soil moisture, texture and carbonate"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","520"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Ecohydrology"],["dc.bibliographiccitation.lastpage","529"],["dc.bibliographiccitation.volume","2"],["dc.contributor.author","Köhler, Michael"],["dc.contributor.author","Dierick, Diego"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Hölscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:48Z"],["dc.date.available","2017-09-07T11:45:48Z"],["dc.date.issued","2009"],["dc.description.abstract","Water use characteristics of cacao (Theobroma cacao) and Gliricidia sepium shade trees were studied in an agroforest on Sulawesi, Indonesia. The objectives were: (1) to identify environmental and tree structural factors controlling water use, (2) to analyse the effect of shade tree cover on cacao water use and (3) to estimate stand level transpiration. Sap flux density was measured in up to 18 trees per species and described with a Jarvis-type model. Model parameters suggested a 49% higher maximum sap flux density in cacao than in Gliricidia and species differences in the response to vapour pressure deficit and radiation. Tree water use was positively related to tree diameter in both species, but this relationship tended to differ between species. In cacao trees maximal tree water use increased with decreasing canopy gap fraction above the trees (R2adj = 0·39, p = 0·04). This was paralleled by an increase of cacao stem diameter and leaf area with decreasing gap fraction. Maximum water use rate per unit crown area of cacao was 13% higher than that of Gliricidia. At the stand level the average transpiration rate was estimated at 1·5 mm day−1 per unit ground area, 70% of which was contributed to by cacao. We conclude that, in the given stand, species differed substantially in water use characteristics, while estimated stand transpiration is in line with findings from other studies for cacao stands. Shade trees may enhance stand transpiration through own water use and additionally by increasing water use rates of cacao trees"],["dc.identifier.doi","10.1002/eco.67"],["dc.identifier.gro","3149111"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5760"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","1936-0584"],["dc.title","Water use characteristics of cacao and Gliricidiatrees in an agroforest in Central Sulawesi, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","3465"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Biogeosciences"],["dc.bibliographiccitation.lastpage","3474"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Meißner, M."],["dc.contributor.author","Köhler, M."],["dc.contributor.author","Schwendenmann, L."],["dc.contributor.author","Hölscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:39Z"],["dc.date.available","2017-09-07T11:45:39Z"],["dc.date.issued","2012"],["dc.description.abstract","Complementary resource use is considered an important mechanism in the study of biodiversity effects. Here we explore how species identity, species mixture and tree size influence the vertical partitioning of soil water among canopy trees during a soil desiccation period. In the Hainich Forest, Germany, the species Fagus sylvatica, Tilia sp. and Fraxinus excelsior were studied in single- and three-species mixed clusters, each consisting of three co-dominant trees situated within a larger mixed forest stand. Vertical soil water uptake depth was assessed by analyzing the hydrogen stable isotope composition (deuterium, D) of water from depth intervals throughout the soil profile and in tree xylem water. For single species clusters, a mixing model suggested that Fagus distinctively drew water from soil depths of 0.3–0.5 m, Tilia from 0.3–0.5m and 0.5–0.7m and Fraxinus mainly used water from 0.5–0.7 m. In mixed clusters, the uptake patterns of Fagus and Tilia were similar to those of the singlespecies clusters (mainly uptake form 0.3–0.5 m), but Fraxinus showed a different uptake pattern. Fraxinus in mixture had a somewhat homogenously distributed uptake over the soil depths 0.2–0.7 m. For single species clusters, there was no correlation between main soil water uptake depth and tree diameter, irrespective of variations in tree size. In contrast, for mixed clusters there was a significant decrease in the main uptake depth with increasing tree size (P < 0.001, R2 adj = 0.73), irrespective of species mix. In consequence, soil water partitioning was strongest where species were mixed and tree size varied. We further analyzed whether single and mixed-species clusters differed in the level of water uptake, e.g. due to complementarity, but our soil water budgeting did not indicate any such differences. A possible explanation might be that the volume of water used is predominantly governed by properties at the stand level, such as aerodynamic roughness, rather than by processes acting at the meter scale between neighbouring trees. With respect to application, we assume that the upcoming close-to-nature forestry approach for the area, which fosters mixed stands of heterogonous diameters, may result in enhanced complementarity in soil water uptake among canopy trees."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2012"],["dc.identifier.doi","10.5194/bg-9-3465-2012"],["dc.identifier.gro","3149053"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/8398"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5696"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","1726-4189"],["dc.rights.access","openAccess"],["dc.title","Partitioning of soil water among canopy trees during a soil desiccation period in a temperate mixed forest"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","no"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Ecohydrology"],["dc.bibliographiccitation.lastpage","12"],["dc.bibliographiccitation.volume","8"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Pendall, Elise"],["dc.contributor.author","Sanchez-Bragado, Rut"],["dc.contributor.author","Kunert, Norbert"],["dc.contributor.author","Hoelscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:40Z"],["dc.date.available","2017-09-07T11:45:40Z"],["dc.date.issued","2014"],["dc.description.abstract","We studied tree water uptake patterns, tested for complementary water use among species and analysed controlling factors in a tropical tree diversity experiment. The water uptake depth of five species was investigated across seasons and diversity levels using the natural abundance of water isotopes (δ2H, δ18O) and modelling. Three distinct water acquisition strategies were found for trees growing in monocultures during the dry season: strong reliance (>70%) on soil water from the upper layer (0–30 cm) (Cedrela odorata), uptake from the upper and deeper layers (>30 cm) in equal proportions (Hura crepitans, Anacardium excelsum and Luehea seemannii) and water uptake predominately from deeper layers (Tabebuia rosea). Seasonal shifts in water uptake were most pronounced for T. rosea. The water uptake pattern of a given species was independent of the diversity level underlining the importance of species identity and species characteristics in spatial and temporal tree water use. Statistics did not show a significant effect of diversity on source water fractions, but we did see some evidence for complementary water resource utilization in mixed species plots, especially in the dry season. Our results also demonstrated that the depth of soil water uptake was related to leaf phenology and tree transpiration rates. A higher proportion of water obtained from deeper soil layers was associated with a high percentage foliage cover in the dry season, which explained the higher transpiration rates."],["dc.identifier.doi","10.1002/eco.1479"],["dc.identifier.gro","3149069"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5714"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","1936-0584"],["dc.title","Tree water uptake in a tropical plantation varying in tree diversity: interspecific differences, seasonal shifts and complementarity"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","227"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","New Forests"],["dc.bibliographiccitation.lastpage","240"],["dc.bibliographiccitation.volume","37"],["dc.contributor.author","Derwisch, Sebastian"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Olschewski, Roland"],["dc.contributor.author","Hölscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:39Z"],["dc.date.available","2017-09-07T11:45:39Z"],["dc.date.issued","2009"],["dc.description.abstract","Tropical tree plantations may play an important role in mitigating CO2 emissions through their potential to capture and sequester carbon from the atmosphere. The Clean Development Mechanism (CDM) as well as voluntary initiatives provide economic incentives for afforestation and reforestation efforts through the generation and sale of carbon credits. The objectives of our study were to measure the carbon (C) storage potential of 1, 2 and 10-years old Tectona grandis plantations in the province of Chiriquí, Western Panama and to calculate the monetary value of aboveground C storage if sold as Certified Emission Reduction (CER) carbon credits. The average aboveground C storage ranged from 2.9 Mg C ha−1 in the 1-year-old plantations to 40.7 Mg C ha−1 in the 10-year-old plantations. Using regression analysis we estimated the potential aboveground C storage of the teak plantation over a 20 year rotation period. The CO2-storage over this period amounted to 191.1 Mg CO2 ha−1. The discounted revenues that could be obtained by issuance of carbon credits during a 20 year rotation period were about US60 for temporary CER and US60 for long-term CER, and thus, contribute to a minor extent (1%) to overall revenues, only."],["dc.identifier.doi","10.1007/s11056-008-9119-2"],["dc.identifier.gro","3149054"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/6809"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5697"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","0169-4286"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Estimation and economic evaluation of aboveground carbon storage of Tectona grandis plantations in Western Panama"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","135"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Journal of Applied Ecology"],["dc.bibliographiccitation.lastpage","144"],["dc.bibliographiccitation.volume","49"],["dc.contributor.author","Kunert, Norbert"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Potvin, Catherine"],["dc.contributor.author","Hölscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:43Z"],["dc.date.available","2017-09-07T11:45:43Z"],["dc.date.issued","2012"],["dc.identifier.doi","10.1111/j.1365-2664.2011.02065.x"],["dc.identifier.gro","3149065"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5709"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","0021-8901"],["dc.title","Tree diversity enhances tree transpiration in a Panamanian forest plantation"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1568"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Agricultural and Forest Meteorology"],["dc.bibliographiccitation.lastpage","1578"],["dc.bibliographiccitation.volume","150"],["dc.contributor.author","Dierick, Diego"],["dc.contributor.author","Hölscher, Dirk"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.date.accessioned","2017-09-07T11:45:40Z"],["dc.date.available","2017-09-07T11:45:40Z"],["dc.date.issued","2010"],["dc.description.abstract","We studied water use in a common bamboo species (Bambusa blumeana J.A. and J.H. Schultes) in the Philippines with the aim to (1) estimate bamboo water use and its dependence on environmental factors, (2) evaluate internal water storage and water dynamics and (3) compare water use characteristics of this bamboo species with those of co-occurring tree species. Two thermal sap flow methods were applied and complemented with a deuterium tracing experiment. Sap flow measured using the stem heat balance method (SHB) was in agreement with simultaneous flow measurements from thermal dissipation probes (TDP) which were used for long term measurements in this study. Maximal sap flux densities measured at the culm base using the TDP method were up to 25.7 g cm−2 h−1, but can be 2–3 times higher at other positions along the culm due to changes in the culm wall cross-section. Maximal water use rates of bamboo culms were on average 12 kg d−1, corresponding to a maximal transpiration rate of 1.4 mm d−1 at the clump level. These values are in line with those of co-occurring tree species, but bamboo tends to limit water use more under reduced soil water availability than most co-occurring tree species. Deuterium added to the transpiration stream at the culm base travelled upwards more slowly than in trees, leading to maximal deuterium levels in the canopy at the 3rd or 6th day after labelling, whereas this was the 1st or 2nd day for trees. This may indicate higher water storage capacities in bamboo relative to its water use rates, although diurnal patterns of sap flux density did not support this interpretation. Research highlights ▶ TDP and SHB thermal sap flow methods gave comparable estimates of water use in bamboo. ▶ Water use patterns can be explained by the distinct anatomy of bamboo. ▶ Bamboo sap flux and transpiration were within the range found in co-occurring trees. ▶ Isotope tracing suggests redistribution of water among culms."],["dc.identifier.doi","10.1016/j.agrformet.2010.08.006"],["dc.identifier.gro","3149066"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5711"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","0168-1923"],["dc.title","Water use characteristics of a bamboo species (Bambusa blumeana) in the Philippines"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","411"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Agricultural and Forest Meteorology"],["dc.bibliographiccitation.lastpage","419"],["dc.bibliographiccitation.volume","150"],["dc.contributor.author","Kunert, Norbert"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Hölscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:35Z"],["dc.date.available","2017-09-07T11:45:35Z"],["dc.date.issued","2010"],["dc.description.abstract","We studied nine tree species with different leaf phenologies growing in monospecific plantations in the watershed of the Panama Canal. The annual rainfall in the region averages 2350 mm with a pronounced dry season from January to March. The atmospheric evaporative demand is usually higher in the dry season compared to the wet season. Our objectives were to (1) compare water use characteristics among the tree species, (2) analyze the response of sap flux density to changes in environmental conditions, and (3) estimate seasonal and annual tree water use and transpiration rates. Tree sap flux was monitored using the heat dissipation technique according to Granier. Under full foliage, maximum sap flux densities varied more than twofold among species. Time of leaf shedding and duration of leafless periods also varied strongly among species. However, the relationship between percentage of foliage and normalized maximum sap flux densities can be described by a universal non-species-specific function. Species means of maximum transpiration rates on a basis of projected crown area varied more than twofold (1.2–2.8 mm day−1). Transpiration rates between the dry and wet season differed for six of the nine species. Three species (Acacia mangium, Anacardium excelsum, and Gmelina arborea) showed enhanced transpiration in the dry season with dry to wet season ratios between 1.4 and 2.1. In contrast, the dry to wet season ratio of Cedrela odorata, Hura crepitans, and Tectona grandis ranged from 0.4 to 0.8. The results suggest that tree species choice can substantially influence water resource use in plantation forestry under such seasonal climatic conditions."],["dc.identifier.doi","10.1016/j.agrformet.2010.01.006"],["dc.identifier.gro","3149051"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5694"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","0168-1923"],["dc.title","Seasonal dynamics of tree sap flux and water use in nine species in Panamanian forest plantations"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","886"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","Tree Physiology"],["dc.bibliographiccitation.lastpage","900"],["dc.bibliographiccitation.volume","30"],["dc.contributor.author","Schwendenmann, L."],["dc.contributor.author","Dierick, D."],["dc.contributor.author","Köhler, M."],["dc.contributor.author","Hölscher, Dirk"],["dc.date.accessioned","2017-09-07T11:45:40Z"],["dc.date.available","2017-09-07T11:45:40Z"],["dc.date.issued","2010"],["dc.description.abstract","Reliable estimates of water use by trees and other woody plants are crucial for an improved understanding of plant physiology and for water resource management. Since the 1980s, the thermal dissipation probe (TDP) method has been widely applied in trees, proved to be fairly accurate but is challenging in remote areas. Also in the 1980s, the deuterium (D(2)O or deuterium oxide) tracing method was proposed, which so far has less often been applied. However, deuterium tracing requires less sophisticated equipment in the field and new analytical methods reduce costs and increase sample throughput. The objectives of this study were (i) to compare plant water use estimates of the TDP and D(2)O method and (ii) to determine whether the D(2)O method is appropriate for assessing absolute magnitudes of plant water use. The two methods were employed on five tropical tree species and a bamboo species growing in a reforestation stand in the Philippines and an agroforestry system in Indonesia. For bamboo, an increase in D(2)O values in neighbouring, non-labelled culms suggests that injected D(2)O was partly redistributed among culms, which would seriously limit the accurate estimation of water use for the target culm. For trees, water use estimates resulting from the D(2)O tracing method were proportional to the TDP results (r(2) = 0.85, P < 0.001), but absolute values were, on average, about seven times higher. This overestimation may be due to the assumptions underlying the D(2)O tracing method, such as the conservation of tracer mass, not being met. Further, it cannot be excluded that underestimation of water use by the TDP method contributed partly to the observed difference. However, when considering known sources of error, a large part of the observed difference remains unexplained. Based on our results, the use of the D(2)O tracing method cannot be recommended without further experimental testing if absolute values of whole-plant water use are a major goal. However, the D(2)O tracing method appears suitable for answering other questions, such as relative differences in water use among trees, water redistribution among neighbours and internal water transport and storage processes in plants."],["dc.identifier.doi","10.1093/treephys/tpq045"],["dc.identifier.gro","3149071"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5716"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","0829-318X"],["dc.title","Can deuterium tracing be used for reliably estimating water use of tropical trees and bamboo?"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","171"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Agroforestry Systems"],["dc.bibliographiccitation.lastpage","187"],["dc.bibliographiccitation.volume","79"],["dc.contributor.author","Moser, G."],["dc.contributor.author","Leuschner, C."],["dc.contributor.author","Hertel, D."],["dc.contributor.author","Hölscher, D."],["dc.contributor.author","Köhler, M."],["dc.contributor.author","Leitner, D."],["dc.contributor.author","Michalzik, B."],["dc.contributor.author","Prihastanti, E."],["dc.contributor.author","Tjitrosemito, S."],["dc.contributor.author","Schwendenmann, L."],["dc.date.accessioned","2017-09-07T11:45:34Z"],["dc.date.available","2017-09-07T11:45:34Z"],["dc.date.issued","2010"],["dc.description.abstract","In South-east Asia, ENSO-related droughts represent irregularly occurring hazards for agroforestry systems containing cocoa which are predicted to increase in severity with expected climate warming. To characterize the drought response of mature cocoa trees, we conducted the Sulawesi Throughfall Displacement Experiment in a shaded (Gliricidia sepium) cocoa agroforestry system in Central Sulawesi, Indonesia. Three large sub-canopy roofs were installed to reduce throughfall by about 80% over a 13-month period to test the hypotheses that (i) cocoa trees are sensitive to drought due to their shallow fine root system, and (ii) bean yield is more sensitive to drought than leaf or stem growth. As 83% of fine root (diameter <2 mm) and 86% of coarse root biomass (>2 mm) was located in the upper 40 cm of the soil, the cocoa trees examined had a very shallow root system. Cocoa and Gliricidia differed in their vertical rooting patterns, thereby reducing competition for water. Despite being exposed for several months to soil water contents close to the conventional wilting point, cocoa trees showed no significant decreases in leaf biomass, stem and branch wood production or fine root biomass. Possible causes are active osmotic adjustment in roots, mitigation of drought stress by shading from Gliricidia or other factors. By contrast, production of cocoa beans was significantly reduced in the roof plots, supporting reports of substantial reductions in bean yields during ENSO-related drought events in the region. We conclude that cocoa possesses traits related to drought tolerance which enable it to maintain biomass production during extended dry periods, whereas bean yield appears to be particularly drought sensitive."],["dc.identifier.doi","10.1007/s10457-010-9303-1"],["dc.identifier.gro","3149046"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/4251"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/5690"],["dc.language.iso","en"],["dc.notes.intern","Hoelscher Crossref import"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.notes.submitter","chake"],["dc.relation.issn","0167-4366"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Response of cocoa trees (Theobroma cacao) to a 13-month desiccation period in Sulawesi, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]