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Michalzik, Beate
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Michalzik, Beate
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Michalzik, Beate
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Michalzik, B,
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2007Journal Article [["dc.bibliographiccitation.firstpage","497"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Waste Management"],["dc.bibliographiccitation.lastpage","509"],["dc.bibliographiccitation.volume","27"],["dc.contributor.author","Michalzik, Beate"],["dc.contributor.author","Ilgen, G."],["dc.contributor.author","Hertel, F."],["dc.contributor.author","Hantsch, S."],["dc.contributor.author","Bilitewski, B."],["dc.date.accessioned","2018-11-07T11:07:40Z"],["dc.date.available","2018-11-07T11:07:40Z"],["dc.date.issued","2007"],["dc.description.abstract","Due to their broad industrial production and use as PVC-stabilisers, agro-chemicals and anti-fouling agents, organo-metal compounds are widely distributed throughout the terrestrial and marine biogeosphere. Here, we focused on the emission dynamics of various organo-metal compounds (e.g., di,- tri-, tetra-methyl tin, di-methyl mercury, tetra-methyl lead) from two different kinds of pre-treated mass waste, namely mechanically-biologically pre-treated municipal solid waste (MBP MSW) and municipal waste incineration ash (MWIA). In landfill simulation reactors, the emission of the organo-metal compounds via the leachate and gas pathway was observed over a period of 5 months simulating different environmental conditions (anaerobic with underlying soil layer/aerated/anaerobic). Both waste materials differ significantly in their initial amounts of organo-metal compounds and their environmental behaviour with regard to the accumulation and depletion rates within the solid material during incubation. For tri-methyl tin, the highest release rates in leachates were found in the incineration ash treatments, where anaerobic conditions in combination with underlying soil material significantly promoted its formation. Concerning the gas pathway, anaerobic conditions considerably favour the emission of organo-metal compounds (tetra-methyl tin, di-methyl mercury, tetra-methyl lead) in both the MBP material and especially in the incineration ash. (c) 2006 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.wasman.2006.02.018"],["dc.identifier.isi","000244238900006"],["dc.identifier.pmid","16714103"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/52619"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0956-053X"],["dc.title","Emissions of organo-metal compounds via the leachate and gas pathway from two differently pre-treated municipal waste materials - A landfill reactor study"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]Details DOI PMID PMC WOS2008Journal Article [["dc.bibliographiccitation.firstpage","1829"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE"],["dc.bibliographiccitation.lastpage","1841"],["dc.bibliographiccitation.volume","38"],["dc.contributor.author","le Mellec, Anne"],["dc.contributor.author","Michalzik, Beate"],["dc.date.accessioned","2018-11-07T11:13:17Z"],["dc.date.available","2018-11-07T11:13:17Z"],["dc.date.issued","2008"],["dc.description.abstract","Herbivorous insect infestations significantly alter element and nutrient cycling in forests, thus directly and indirectly affecting ecosystem functioning. In this paper, we report on the herbivore-mediated transfer of carbon (C) and nitrogen (N) from the canopy to the forest floor and its influence on soil microbial activity during a pine tappet (Dendrolimus pini L.) infestation. Over the course of 6 months, we followed C and N fluxes in bulk deposition, throughfall, and green fall (green needle debris dropped during herbivory) together with solid frass (insect faeces) in an 80-year-old Scots pine (Pinits silvestris L.) forest. Compared with the control, herbivore defoliation significantly doubled throughfall inputs of total and dissolved organic C and N over the study period. Frass plus green-fall C and N fluxes peaked in June-July at 110 kg C.ha(-1) and 2.3 kg N.ha(-1), respectively. Randomized intervention analysis revealed no significant effects of herbivory on soil microbial properties, except for adenylate energy charge, which showed slightly higher values under herbivory. This study demonstrates the importance of canopy herbivory on overall C and N inputs to forest ecosystems, particularly in altering the timing and quality of the organic material reaching the forest floor and potentially affecting belowground processes."],["dc.description.sponsorship","erman Research Foundation, DFG [MI 927/1-1]"],["dc.identifier.doi","10.1139/X08-045"],["dc.identifier.isi","000257359600012"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53855"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Natl Research Council Canada-n R C Research Press"],["dc.relation.issn","0045-5067"],["dc.title","Impact of a pine lappet (Dendrolimus pini) mass outbreak on C and N fluxes to the forest floor and soil microbial properties in a Scots pine forest in Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]Details DOI WOS2013Journal Article [["dc.bibliographiccitation.firstpage","253"],["dc.bibliographiccitation.journal","Quaternary International"],["dc.bibliographiccitation.lastpage","264"],["dc.bibliographiccitation.volume","308"],["dc.contributor.author","Niemann, Holger"],["dc.contributor.author","Matthias, Isabelle"],["dc.contributor.author","Michalzik, Beate"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:18:44Z"],["dc.date.available","2018-11-07T09:18:44Z"],["dc.date.issued","2013"],["dc.description.abstract","Late Holocene human impact and environmental changes were reconstructed from a sediment core of the Laguna Daniel Alvarez (2200 m asl) located on the outskirts of the city of Loja, southeastern Ecuador. Palaeoenvironmental changes were investigated by pollen, spore, algae and charcoal analysis in combination with X-Ray Fluorescence (XRF) scanning and element analysis of delta C-13, Total Organic Carbon (TOC), Total Nitrogen (TN) and radiocarbon dating. This multi-proxy study provides in detail the settlement history in the inner-Andean dry valley in southern Ecuador over the last ca. 1400 years. Between 630 and 1470 AD, Zea mays was intensively cultivated around the studied lake by the native Palta culture in the Loja region. After ca. 1470 AD, Z. mays cultivation collapsed, accompanied by an increase in fallow vegetation, such as Mimosa and Poaceae, probably as a result of the Inca invasion and occupation from 1463 to 1531 AD in southern Ecuador. After ca. 1570 AD, Amaranthaceae/Chenopodiaceae markedly increased, reflecting the beginning of the Spanish Conquest. In 1531 AD, Loja became Spanish and, during the first ca. 100 years of the Spanish regime, Loja developed into the fortified capital of the province. In the 17th century, crop growing strongly declined due to the diminished indigenous population that probably suffered from new diseases introduced by the Spanish invaders. Pinus and Eucalyptus as well as Plantago lanceolata were introduced in the Loja region about 220 years ago. (C) 2013 Elsevier Ltd and INQUA. All rights reserved."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft (DFG) [FOR 402/D1]"],["dc.identifier.doi","10.1016/j.quaint.2013.03.017"],["dc.identifier.isi","000325306800025"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/28473"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1040-6182"],["dc.title","Late Holocene human impact and environmental change inferred from a multi-proxy lake sediment record in the Loja region, southeastern Ecuador"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]Details DOI WOS2011Journal Article [["dc.bibliographiccitation.firstpage","393"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Plant and Soil"],["dc.bibliographiccitation.lastpage","403"],["dc.bibliographiccitation.volume","342"],["dc.contributor.author","le Mellec, Anne"],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Michalzik, Beate"],["dc.date.accessioned","2018-11-07T08:56:47Z"],["dc.date.available","2018-11-07T08:56:47Z"],["dc.date.issued","2011"],["dc.description.abstract","Apart from the forest floor, the canopy of forested ecosystems functions as the second most important source for dissolved and particulate fractions of organic and inorganic C and N compounds. However, under mass outbreak situations of insect herbivores this flux path of organic matter is considerably intensified clearly exceeding C and N fluxes from the forest floor. In this paper we report on herbivore-altered C and N fluxes from the canopy to the forest floor and effects on forest floor nutrient fluxes during severe defoliating herbivory of the winter moth (Operophtera brumata) and the mottled umber moth (Eranis defoliaria) in an oak forest in Germany. Over the course of 6.5 months we followed the C and N fluxes with bulk deposition, throughfall solution, insect frass deposits (green-fall together with insect faeces) and with forest floor solution in an 117-yr-old oak (Quercus petraea) forest. Compared to the control, herbivore defoliation significantly enhanced throughfall inputs of total and dissolved organic carbon and nitrogen by a factor of 3 and 2.5 (for TOC and DOC), and by 1.4 and 1.3 times (for TNb and DNb), respectively. Frass plus green-fall C and N fluxes peaked in May with 592 kg C ha(-1) and 33.5 kg N ha(-1) representing 79.6% (for C) and 78.3% (for N) of the total C and N input over 2.5 months. The quantitative and qualitative C and N input via faeces and litter deposition significantly differ between the insect affected and non-affected site. However, the C and N fluxes with throughfall did not significantly correlate with forest floor leachates. In this context, forest floor fluxes of TOC, DOC and NO3-N were significantly lower at the infested site compared to the control, whereas fluxes of NH4-N together with DON were significantly higher. The study demonstrates the importance of linking the population and associated frass dynamics of herbivorous insects with the cycling of nutrients and organic matter in forest ecosystems, highlighting the remarkable alterations in the timing, amounts and nature of organic matter dynamics on the ecosystem level. Consequently, the ecology of phytophagous insects allows partly to explain temporal-spatial alterations in nutrient cycling and thus ecosystem functioning."],["dc.description.sponsorship","German Research Foundation (DFG) [MI 927/1-3]"],["dc.identifier.doi","10.1007/s11104-010-0704-8"],["dc.identifier.isi","000289562000031"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/6662"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/23233"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1573-5036"],["dc.relation.issn","0032-079X"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Insect herbivory, organic matter deposition and effects on belowground organic matter fluxes in a central European oak forest"],["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"]]Details DOI WOS2009Journal Article [["dc.bibliographiccitation.firstpage","255"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Plant and Soil"],["dc.bibliographiccitation.lastpage","262"],["dc.bibliographiccitation.volume","325"],["dc.contributor.author","Mellec, Anne"],["dc.contributor.author","Habermann, Michael"],["dc.contributor.author","Michalzik, Beate"],["dc.date.accessioned","2019-07-09T11:52:24Z"],["dc.date.available","2019-07-09T11:52:24Z"],["dc.date.issued","2009"],["dc.description.abstract","Herbivorous insects can affect ecological processes in forested ecosystems such as nutrient and matter cycling especially during outbreak situations. However, the knowledge about their contribution to the quality and flows of energy and matter in forests is still imperfect. In this paper we report on the herbivore-affected C to N ratios in different fractions of organic matter cascading from the canopy to the forest floor during a pine lappet (Dendrolimus pini L.) mass infestation. Throughout a four months period we monitored the C and N fluxes with throughfall, and the C/N ratios of insect excrements (faeces) and pine needles in an 80-year-old Scots pine forest. Compared to the control, herbivore defoliation significantly magnifies C and N input fluxes by two to three times amounting to 95 kg TOC and 5.9 kg TN ha−1 in addition. Concurrently NO3-N fluxes diminished and the C/N ratios in throughfall solutions increased during peaking frass activity. Compared to fresh needle biomass, the C/N ratios in insect faeces triple during peaking frass activity resulting in values between 70 and 100. This study demonstrates the importance of herbivorous insect’s pests on element cycling as they act as a short-time phenomenon altering the nutrient quality and quantity reaching the forest floor and potentially affecting below-ground processes."],["dc.identifier.doi","10.1007/s11104-009-9976-2"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/3957"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60177"],["dc.notes.intern","Merged from goescholar"],["dc.publisher","Springer"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject.ddc","570"],["dc.title","Canopy herbivory altering C to N ratios and soil input patterns of different organic matter fractions in a Scots pine forest"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]Details DOI2008Journal Article [["dc.bibliographiccitation.firstpage","408"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Land Degradation and Development"],["dc.bibliographiccitation.lastpage","420"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Heitkamp, Felix"],["dc.contributor.author","Glatzel, Stephan"],["dc.contributor.author","Michalzik, Beate"],["dc.contributor.author","Fischer, Elisabeth"],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2018-11-07T11:13:40Z"],["dc.date.available","2018-11-07T11:13:40Z"],["dc.date.issued","2008"],["dc.description.abstract","Decline of heathlands in Central Europe raises the question of successful restoration of degraded heathlands. We examined the impact of different restoration techniques oil soil microbial biomass carbon (C(mic)) and nitrogen (N(mic)) and enzyme activity on an abandoned military training site in the Luneburger Heaths. The aim was to determine which technique resulted in typical heathland soil conditions. The training site was ill use for about 50 years. Vegetation and soils were degraded in large areas. Restoration actions were: (1) spreading of heath plaggen (sods, containing the organic layer and a few centimetres mineral soil), (2) spreading of heath plaggen and grass seeds (Festuca filiformis Pourr.). (3) spreading of F. filiformis-seeds and (4) succession (episodical tree removal). Ten years after restoration. we measured pH, bulk density, abundance of roots, soil organic carbon (SOC), nitrogen (N(1)), phosphorus (P(1)) C(mic), N(mic) and acid phosphatase activity (AcP) in the first 10cm of the mineral soil. Four restoration treatments were compared with one reference site. The reference site is heathland located near the training site, where no military actions took place. At all disturbed sites, bulk density and pH proved to be higher than oil the reference site. Relative to the reference site, SOC storage reached from 37 to 91 per cent, regeneration of N(1) was slightly lower. In contrast to the advanced development of SOC and Nt, the regeneration of C(mic) and N(mic) was much lower (15-44 per cent). The succession site showed a low pool of SOC, Nt, C(mic) and N(mic), but microbial ratios indicated a less disturbed C- and N-cycle. AcP pronounced differences in nutrient demand between disturbed sites and reference. On this base, recommendations for restoration management were given. Copyright (C) 2008 John Wiley & Soils, Ltd."],["dc.identifier.doi","10.1002/ldr.848"],["dc.identifier.isi","000258557600005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53951"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1085-3278"],["dc.title","Soil microbiochemical properties as indicators for success of heathland restoration after military disturbance"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]Details DOI WOS2016Journal Article [["dc.bibliographiccitation.firstpage","343"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Plant and Soil"],["dc.bibliographiccitation.lastpage","360"],["dc.bibliographiccitation.volume","403"],["dc.contributor.author","Schwarz, Martin T."],["dc.contributor.author","Bischoff, Sebastian"],["dc.contributor.author","Blaser, Stefan"],["dc.contributor.author","Boch, Steffen"],["dc.contributor.author","Grassein, Fabrice"],["dc.contributor.author","Klarner, Bernhard"],["dc.contributor.author","Schmitt, Barbara"],["dc.contributor.author","Solly, Emily F."],["dc.contributor.author","Ammer, Christian"],["dc.contributor.author","Michalzik, Beate"],["dc.contributor.author","Schall, Peter"],["dc.contributor.author","Scheu, Stefan"],["dc.contributor.author","Schöning, Ingo"],["dc.contributor.author","Schrumpf, Marion"],["dc.contributor.author","Schulze, Ernst-Detlef"],["dc.contributor.author","Siemens, Jan"],["dc.contributor.author","Wilcke, Wolfgang"],["dc.date.accessioned","2017-09-07T11:47:48Z"],["dc.date.available","2017-09-07T11:47:48Z"],["dc.date.issued","2016"],["dc.identifier.doi","10.1007/s11104-016-2798-0"],["dc.identifier.gro","3146767"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/4568"],["dc.notes.status","final"],["dc.publisher","Springer Nature"],["dc.relation.issn","0032-079X"],["dc.title","Drivers of nitrogen leaching from organic layers in Central European beech forests"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]Details DOI2005Conference Paper [["dc.bibliographiccitation.firstpage","227"],["dc.bibliographiccitation.issue","3-4"],["dc.bibliographiccitation.journal","Geoderma"],["dc.bibliographiccitation.lastpage","236"],["dc.bibliographiccitation.volume","127"],["dc.contributor.author","Michalzik, Beate"],["dc.contributor.author","Stadler, B."],["dc.date.accessioned","2018-11-07T08:46:05Z"],["dc.date.available","2018-11-07T08:46:05Z"],["dc.date.issued","2005"],["dc.description.abstract","Few studies deal with the origin and contribution of organic matter (OM) fluxes from forest canopies to the variability of DOM and nutrient dynamics in the forest floor. Recent studies indicate a microbial and phytophages origin of OM in the throughfall of temperate forest ecosystems and reported inputs of dissolved (< 0.45 mu m) organic carbon (DOC) with throughfall range between 40 and 160 kg C ha(-1) year(-1). Data on particulate organic matter (0.45 mu m < POM < 2 mm) associated with throughfall fluxes are rare and not often considered in terrestrial ecosystem element budgets. Using field and laboratory experiments, we investigated the direct effects of canopy infestation by two functional groups of herbivores (sap and leaf feeders) on dissolved and particulate organic matter fluxes in throughfall and their impact on forest floor processes. Throughfall fluxes of particulate amino-nitrogen beneath infested spruce were about 60% and those of bexosecarbon beneath infested hardwood trees up to 70% higher compared to uninfested control trees. Corresponding fluxes to filtered samples showed no statistically significant differences. In column irrigation experiments, different levels of aphid infestation (uninfested, moderately, heavy infested) were simulated by adding honeydew to the irrigation solution. Forest floor solution chemistry from forest floor showed a significant reduction in NH4-N and NO3-N fluxes, slightly reduced DON fluxes and significantly increased CO2 effluxes following honeydew application. We suggest that the amount of POM compounds transported with throughfall solution and its subsequent effects on forest floor processes depend on the herbivore functional group and on the level of infestation. From both a quantitative and qualitative point of view, our data indicate that herbivory-mediated organic matter in particulate and dissolved forms contribute considerably to the overall throughfall input of organic substances into the forest floor. (c) 2004 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.geoderma.2004.12.006"],["dc.identifier.isi","000230546600007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/20601"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.publisher.place","Amsterdam"],["dc.relation.conference","9th Meeting of the Nordic-Chapter-of-the-International-Humic-Substances-Society"],["dc.relation.eventlocation","Mid Sweden Univ, Sundswall, SWEDEN"],["dc.relation.issn","0016-7061"],["dc.title","Importance of canopy herbivores to dissolved and particulate organic matter fluxes to the forest floor"],["dc.type","conference_paper"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]Details DOI WOS2010Journal Article [["dc.bibliographiccitation.firstpage","1515"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","1530"],["dc.bibliographiccitation.volume","16"],["dc.contributor.author","Schwendenmann, Luitgard"],["dc.contributor.author","Veldkamp, Edzo"],["dc.contributor.author","Moser, Gerald"],["dc.contributor.author","Hölscher, Dirk"],["dc.contributor.author","Köhler, Michael"],["dc.contributor.author","Clough, Yann"],["dc.contributor.author","Anas, Iswandi"],["dc.contributor.author","Djajakirana, Gunawan"],["dc.contributor.author","Erasmi, Stefan"],["dc.contributor.author","Hertel, Dietrich"],["dc.contributor.author","Leitner, Daniela"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Michalzik, Beate"],["dc.contributor.author","Propastin, Pavel"],["dc.contributor.author","Tjoa, Aiyen"],["dc.contributor.author","van Straaten, Oliver"],["dc.date.accessioned","2017-08-25T10:13:31Z"],["dc.date.accessioned","2020-05-11T13:19:25Z"],["dc.date.available","2017-08-25T10:13:31Z"],["dc.date.available","2020-05-11T13:19:25Z"],["dc.date.issued","2010"],["dc.description.abstract","Agroforestry systems may play a critical role in reducing the vulnerability of farmers' livelihood to droughts as tree-based systems provide several mechanisms that can mitigate the impacts from extreme weather events. Here, we use a replicated throughfall reduction experiment to study the drought response of a cacao/Gliricidia stand over a 13-month period. Soil water content was successfully reduced down to a soil depth of at least 2.5 m. Contrary to our expectations we measured only relatively small nonsignificant changes in cacao (−11%) and Gliricidia (−12%) sap flux densities, cacao leaf litterfall (+8%), Gliricidia leaf litterfall (−2%), soil carbon dioxide efflux (−14%), and cacao yield (−10%) during roof closure. However, cacao bean yield in roof plots was substantially lower (−45%) compared with control plots during the main harvest following the period when soil water content was lowest. This indicates that cacao bean yield was more sensitive to drought than other ecosystem functions. We found evidence in this agroforest that there is complementary use of soil water resources through vertical partitioning of water uptake between cacao and Gliricidia. This, in combination with acclimation may have helped cacao trees to cope with the induced drought. Cacao agroforests may thus play an important role as a drought-tolerant land use in those (sub-) tropical regions where the frequency and severity of droughts is projected to increase."],["dc.identifier.doi","10.1111/j.1365-2486.2009.02034.x"],["dc.identifier.gro","3150086"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6815"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.issn","1354-1013"],["dc.subject","cacao yield; CO2 efflux; fine root biomass; leaf litterfall; plant water uptake; sap flux; shade trees; soil water; throughfall reduction"],["dc.title","Effects of an experimental drought on the functioning of a cacao agroforestry system, Sulawesi, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","no"],["dspace.entity.type","Publication"]]Details DOI