Behling, Hermann

[["dc.bibliographiccitation.artnumber","959914"],["dc.bibliographiccitation.journal","Frontiers in Earth Science"],["dc.bibliographiccitation.volume","10"],["dc.contributor.affiliation","Unkelbach, Julia; \r\nDepartment of Palynology and Climate Dynamics, Albrecht-von-Haller-Institute, University of Goettingen, Goettingen, Germany"],["dc.contributor.affiliation","Behling, Hermann; \r\nDepartment of Palynology and Climate Dynamics, Albrecht-von-Haller-Institute, University of Goettingen, Goettingen, Germany"],["dc.contributor.author","Unkelbach, Julia"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2022-10-04T10:22:03Z"],["dc.date.available","2022-10-04T10:22:03Z"],["dc.date.issued","2022"],["dc.date.updated","2022-11-11T13:14:33Z"],["dc.description.abstract","In palaeoecology, multi-site macro-charcoal analyses provide information on climate–fire–vegetation linkages, their spatial and temporal extent, and the impact of prehistoric human practices. Our multi-site study comprises eight macro-charcoal records from two highly continental forest-steppe regions in western and north-central Mongolia, covering the Holocene. In addition to reviewing macro-charcoal influxes and comparing macro-charcoal morphotype results with arboreal/non-arboreal pollen ratios, our dataset provides the first fire frequency synthesis for two regions in Mongolia. During the early and mid-Holocene, the fire history in western and north-central Mongolia was controlled by the regional climate variability, whereas the fire intensities were higher in the Mongolian Altai. In general, fire frequencies are lower in northern Khangai. Increases in the fire frequency correlate with the potential beginning of a rise in the nomadic population of the Mongolian Altai after 1,100 cal yr BP. In both areas, individual macro-charcoal peaks, a marked site-to-site variability, and a generally very low impact on the forest-steppe distribution may mostly be explained by a strictly local nomadic disturbance."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2022"],["dc.identifier.doi","10.3389/feart.2022.959914"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/114578"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-600"],["dc.publisher","Frontiers Media S.A."],["dc.relation.eissn","2296-6463"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","The reconstruction of Holocene northwestern Mongolian fire history based on high-resolution multi-site macro-charcoal analyses"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Geophysical Research Letters"],["dc.bibliographiccitation.volume","48"],["dc.contributor.author","Wang, Jian"],["dc.contributor.author","Zhou, Xinying"],["dc.contributor.author","Xu, Hai"],["dc.contributor.author","Liu, Junchi"],["dc.contributor.author","Yang, Qingjiang"],["dc.contributor.author","Zhao, Chao"],["dc.contributor.author","Gao, Qiang"],["dc.contributor.author","Zhao, Keliang"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Li, Xiaoqiang"],["dc.date.accessioned","2021-04-14T08:30:19Z"],["dc.date.available","2021-04-14T08:30:19Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1029/2020GL089566"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/83188"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1944-8007"],["dc.relation.issn","0094-8276"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Relationship Between C 4 Biomass and C 4 Agriculture During the Holocene and its Implications for Millet Domestication in Northeast China"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","54"],["dc.bibliographiccitation.journal","Quaternary Science Reviews"],["dc.bibliographiccitation.lastpage","65"],["dc.bibliographiccitation.volume","146"],["dc.contributor.author","Rodrigues, Jackson Martins"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Giesecke, Thomas"],["dc.date.accessioned","2018-11-07T10:10:09Z"],["dc.date.available","2018-11-07T10:10:09Z"],["dc.date.issued","2016"],["dc.description.abstract","At mid to high northern latitudes postglacial vegetation change has often occurred synchronously over large regions triggered mainly by abrupt climate change. Based on 19 pollen diagrams from southern and southeastern Brazil we explore if similar synchronicities in vegetation change were also characteristic for the vegetation dynamics in low latitudes. We used sequence splitting to detect past vegetation change in the pollen diagrams and computed principal curves and rates of change to visually evaluate the changes in composition and dynamics. The results show that vegetation change occurred mostly during the second half of the Holocene with distinct episodes of change. The character of vegetation change is generally consistent with shifts to wetter conditions and agrees with inferred shifts of the South American Monsoon. Speleothems as well as the titanium record from the Cariaco Basin indicate several episodes of rapid shifts in the precipitation regime, which are within the dating uncertainty of the here detected periods of vegetation change (8900, 5900, 2800, 1200 and 550 cal yrs BP). Our results indicate that low latitude vegetation composition follows precession forcing of the hydrology, while change is often triggered and synchronized by rapid climate change much like in high and mid latitudes. Pollen diagrams document changes in the abundance of individual taxa and changes in the amount of woodland cover, while small compositional changes indicate a regional stability of vegetation types during the Holocene. (C) 2016 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.quascirev.2016.06.011"],["dc.identifier.isi","000381234000003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/39801"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0277-3791"],["dc.title","Holocene dynamics of vegetation change in southern and southeastern Brazil is consistent with climate forcing"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1243"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","1250"],["dc.bibliographiccitation.volume","22"],["dc.contributor.author","Verissimo, Nuno"],["dc.contributor.author","Safford, Hugh DeForest"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:04:09Z"],["dc.date.available","2018-11-07T09:04:09Z"],["dc.date.issued","2012"],["dc.description.abstract","This study presents a recontruction of the Holocene vegetation and fire history of the Serra do Caparao (Espirito Santo/Minas Gerais, SE Brazil) based on pollen and charcoal analysis from the 130 cm long core Primeiro Rancho I. Radiocarbon dates indicate a complete record of the Holocene (11,400 cal. yr BP to present). At the core site, high elevation grassland (campos de altitude) has been the dominant vegetation throughout the recorded period. In the early Holocene (11,400 to 9000 cal. yr BP), a humid phase was followed by a drier one. Fires occurred continuously during the studied period but were more frequent in the early Holocene. Between 9000 and 2700 cal. yr BP, a gradual increase in the diversity and abundance of Atlantic montane forest taxa indicates an increase in humidity and/or rainfall; campos de altitude taxa still dominated but the montane forest taxon Symplocos was strongly present. Between 2700 and 1200 cal. yr BP, the arboreal Atlantic montane forest taxon Luehea became prominent but forest expansion halted and apparently reversed after 1200 cal. yr BP, possibly because of human activities. Simultaneously, campos de altitude expanded; abrupt variations in the pollen assemblages suggest environmental instability. Campos de altitude are a natural vegetation in Serra do Caparao, but their present extent is likely influenced by anthropogenic activities, as several data suggest an increase of humidity after 1200 cal. yr BP, which should have caused a forest expansion. Reduction in human disturbance at higher elevations would thus probably result in succession to forest in some of the lower campos."],["dc.description.sponsorship","IBAMA [62/97]; CNPq Portaria [368/97]"],["dc.identifier.doi","10.1177/0959683612437864"],["dc.identifier.isi","000309938500005"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/12976"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25051"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Sage Publications Ltd"],["dc.relation.issn","0959-6836"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Holocene vegetation and fire history of the Serra do Caparao, SE Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","138"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Quaternary Research"],["dc.bibliographiccitation.lastpage","148"],["dc.bibliographiccitation.volume","77"],["dc.contributor.author","Hermanowski, Barbara"],["dc.contributor.author","da Costa, Marcondes Lima"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:16:02Z"],["dc.date.available","2018-11-07T09:16:02Z"],["dc.date.issued","2012"],["dc.description.abstract","New pollen, micro-charcoal, sediment and mineral analyses of a radiocarbon-dated sediment core from the Serra Sul dos Carajas (southeast Amazonia) indicate changes between drier and wetter climatic conditions during the past 25,000 yr, reflected by fire events, expansion of savanna vegetation and no-analog Amazonian forest communities. A cool and dry last glacial maximum (LGM) and late glacial were followed by a wet phase in the early Holocene lasting for ca. 1200 yr, when tropical forest occurred under stable humid conditions. Subsequently, an increasingly warm, seasonal climate established. The onset of seasonality falls within the early Holocene warm period, with possibly longer dry seasons from 70,200 to 3400 cal yr BP, and an explicitly drier phase from 9000 to 3700 cal yr BP. Modern conditions with shorter dry seasons became established after 3400 cal yr BP. Taken together with paleoenvironmental evidence from elsewhere in the Amazon Basin, the observed changes in late Pleistocene and Holocene vegetation in the Serra Sul dos Carajas likely reflect large-scale shifts in precipitation patterns driven by the latitudinal displacement of the Inter-Tropical Convergence Zone and changes in sea-surface temperatures in the tropical Atlantic. (C) 2011 University of Washington. Published by Elsevier Inc. All rights reserved."],["dc.identifier.doi","10.1016/j.yqres.2011.10.009"],["dc.identifier.isi","000299242600015"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/27842"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Academic Press Inc Elsevier Science"],["dc.relation.issn","0033-5894"],["dc.title","Environmental changes in southeastern Amazonia during the last 25,000 yr revealed from a paleoecological record"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","447"],["dc.bibliographiccitation.journal","Journal of Asian Earth Sciences"],["dc.bibliographiccitation.lastpage","456"],["dc.bibliographiccitation.volume","114"],["dc.contributor.author","Wang, L."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Kao, Shuh-Ji"],["dc.contributor.author","Li, Hong-Chun"],["dc.contributor.author","Selvaraj, Kandasamy"],["dc.contributor.author","Hsieh, Meng-Long"],["dc.contributor.author","Chang, Yuan-Pin"],["dc.date.accessioned","2018-11-07T09:47:28Z"],["dc.date.available","2018-11-07T09:47:28Z"],["dc.date.issued","2015"],["dc.description.abstract","We used multi-decadal pollen and diatom records from sediment core TFL-1 from Tsuifong Lake to reconstruct the vegetation dynamics and hydroclimate in northeastern Taiwan during the past 3500 cal BP. Coarse grained sediments in association with higher percentages of wetland pollen (Cyperaceae) and upper conifer pollen (Tsuga and Pinus) in the lower part of the core indicate low lake levels and a relatively cold/dry climate between 3500 and 2030 cal BP, reflecting a decline of the East Asian summer monsoon (EASM). Muddy sediments coupled with reduction of wetland pollen represent the rise of lake levels, implying the re-strengthening of the EASM during the past 2000 years. Paleotemperature was inferred from the variation of pollen origin from the upper and lower mountain forest, indicating the global temperature anomalies of the Medieval Warm Period (MWP) and the Little Ice Age (LIA). In comparison to the main climate forces in the North Pacific, we suggest that the long-term climatic trend in Taiwan was controlled by variations in EASM intensity, while increased precipitation over the past 2000 years may also be linked to warmer sea surface temperature (SST) of the western Pacific Warm Pool (WPWP) and increased El Nino-Southern Oscillation (ENSO) events, which increased typhoon intensity. Higher diatom-inferred pH during 2930-2030 cal BP and the LIA suggest strong hydrological disturbances, reflecting more typhoons passing over Taiwan. The frequent typhoon events could be linked by an abrupt shift of typhoon track, due to the reduction of the WPWP and expansion of the Northwestern Pacific High, which move typhoons in a more westerly direction. (c) 2015 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.jseaes.2015.03.037"],["dc.identifier.isi","000367857800002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/35121"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","1878-5786"],["dc.relation.issn","1367-9120"],["dc.title","Late Holocene environment of subalpine northeastern Taiwan from pollen and diatom analysis of lake sediments"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","69"],["dc.bibliographiccitation.journal","Quaternary International"],["dc.bibliographiccitation.lastpage","76"],["dc.bibliographiccitation.volume","333"],["dc.contributor.author","Wang, L."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Chen, Yue-Ming"],["dc.contributor.author","Huang, Mmeng-Shen"],["dc.contributor.author","Chen, Chen-Tung Arthur"],["dc.contributor.author","Lou, Jiann-Yuh"],["dc.contributor.author","Chang, Yuan-Pin"],["dc.contributor.author","Li, Hong-Chun"],["dc.date.accessioned","2018-11-07T09:39:55Z"],["dc.date.available","2018-11-07T09:39:55Z"],["dc.date.issued","2014"],["dc.description.abstract","The aim of this study is to improve the understanding of environmental changes and the linkages with the dynamics of the East Asian Monsoon (EAM) during the Holocene in the western North Pacific. We analyzed the pollen, diatom, and weak acid-leachable fractions associated with extracted organic compounds of lacustrine sediments retrieved from the subalpine Retreat Lake in northwestern Taiwan. During the early Holocene (10,100-8600 cal BP), cool climate was inferred by the dominance of grass pollen with poor preservation of diatom valves in the record. At that time, derived biomarkers were also dominated by long-chain alkanes originating from herbs. The following Holocene Optimum (8600-6400 cal BP) was characterized by a remarkable increase of tree pollen, indicating the warmer and humid climate and a stronger summer EAM. The possible enhanced monsoon-driven precipitation resulted in higher contents of total organic carbon buried in sediments. However, the climate and precipitation of the alpine area in Taiwan might have been unstable. The high variability of wetland pollen and diatom abundance reveals weak periods of EAM during the late Holocene Optimum (6400-4500 cal BP). The hiatus in the deposit during 4500-2100 cal BP suggests the continuously decline of the EAM. During the last 2100 years, dominated wetland plant pollen accompanying stable diatom abundance indicated humid climatic conditions and a stable increase of the EAM. The climatic condition of study area was similar with modern situation during this late Holocene. (C) 2014 Elsevier Ltd and INQUA. All rights reserved."],["dc.identifier.doi","10.1016/j.quaint.2014.02.014"],["dc.identifier.isi","000336442200009"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/33401"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","1873-4553"],["dc.relation.issn","1040-6182"],["dc.title","Holocene monsoonal climate changes tracked by multiproxy approach from a lacustrine sediment core of the subalpine Retreat Lake in Taiwan"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1251"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","1262"],["dc.bibliographiccitation.volume","22"],["dc.contributor.author","Jeske-Pieruschka, Vivian"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:04:09Z"],["dc.date.available","2018-11-07T09:04:09Z"],["dc.date.issued","2012"],["dc.description.abstract","We present new palaeoenvironmental data from a 281 cm long sediment core studied by means of pollen and charcoal analyses from Rincao das Cabritas of the Sao Francisco de Paula area, which lies in the wettest region of southern Brazil at the present time. The high-resolution record, dated with seven AMS dates, spans the last 16 700 cal. BP. The continuous presence of grassland vegetation (Campos) throughout the glacial period reflects cold and markedly drier climatic conditions than today. Nowadays, remote areas of Campos on the highlands represent remnants of an early and widely expanded vegetation of glacial times that was gradually replaced by forest ecosystems during the late Holocene. Araucaria forest began to develop after 3200 cal. BP, with its expansion over Campos starting at about 2950 cal. BP. This was probably due to the presence of a somewhat wetter climate after about 4600 cal. BP, which supported the initial development of forest ecosystems and allowed Atlantic rainforest to spread from the lower regions upwards to higher elevations. The maximum expansion of Araucaria forest took place during the last 1000 years, when it started to be the prevailing vegetation type. This vegetational change coincides with increased precipitation and continuously wetter climatic conditions since 1050 cal. BP. The reconstructed fire history indicates a presence of human-related fires on the highlands from the Late Pleistocene until the mid Holocene. Fire activity was markedly reduced after about 3000 cal. BP when forest expanded continuously under regional wetter climatic conditions."],["dc.identifier.doi","10.1177/0959683611414930"],["dc.identifier.isi","000309938500006"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/12981"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25052"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Sage Publications Ltd"],["dc.relation.issn","0959-6836"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Palaeoenvironmental history of the Sao Francisco de Paula region in southern Brazil during the late Quaternary inferred from the Rincao das Cabritas core"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","387"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","403"],["dc.bibliographiccitation.volume","25"],["dc.contributor.author","Rodrigues, Jackson Martins"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Giesecke, Thomas"],["dc.date.accessioned","2018-11-07T10:12:31Z"],["dc.date.available","2018-11-07T10:12:31Z"],["dc.date.issued","2016"],["dc.description.abstract","In south and southeast Brazil land use caused profound changes in natural vegetation and consequently the value of the pollen composition in surface samples as modern analogues. In order to test the capability of modern pollen to represent the natural vegetation, three different time slices of pollen assemblages from 27 sites spread over southern and south-eastern Brazil and the Misiones Province in Argentina were collated. Pollen samples from the pre-colonization period, selected from the moment just before abrupt changes evidenced on pollen diagrams caused by the colonization process throughout the last 500 years, were assumed to represent the natural vegetation conditions once the climate remained stable within this period. Thus we used pre-colonization assemblages to compare with modern samples to explore to what extent surface pollen may be biased in representing the natural vegetation types. Furthermore, to compare man made vegetation change to climate driven vegetation change we also compared to these 20 out of 27 samples dated to 3,000 years bp. Guided by ordination and cluster analysis, but using abundance thresholds of indicator taxa we classified the pollen spectra of pre-colonization time into seven groups consistent with the main vegetation types in the area. Ordination analyses capture the differentiation between grassland and forested vegetation and between tropical and subtropical vegetation types. Comparing the pre-colonization with other time slices we observed that based on Poaceae abundance, 70 and 85 % respectively of sites from 3,000 bp and modern assemblages maintained their classification. Based on finer classification criteria these values decreased to 40 and 52 % respectively. Square chord dissimilarity indicates that colonization impact altered the pollen composition as strongly as 3,000 years of climate induced vegetation change. The surface samples still represent important environmental gradients; however, their use as modern analogue requires careful treatment and eventual exclusion of highly impacted sites."],["dc.identifier.doi","10.1007/s00334-016-0558-y"],["dc.identifier.isi","000377460700006"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/40251"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1617-6278"],["dc.relation.issn","0939-6314"],["dc.title","Differentiating vegetation types from eastern South American ecosystems based on modern and subfossil pollen samples: evaluating modern analogues"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","24"],["dc.bibliographiccitation.journal","Agriculture, Ecosystems & Environment"],["dc.bibliographiccitation.lastpage","33"],["dc.bibliographiccitation.volume","264"],["dc.contributor.author","Marzinzig, Birgit"],["dc.contributor.author","Brünjes, Lisa"],["dc.contributor.author","Biagioni, Siria"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Link, Wolfgang"],["dc.contributor.author","Westphal, Catrin"],["dc.date.accessioned","2020-12-10T14:14:56Z"],["dc.date.available","2020-12-10T14:14:56Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1016/j.agee.2018.05.003"],["dc.identifier.issn","0167-8809"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/71552"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Bee pollinators of faba bean (Vicia faba L.) differ in their foraging behaviour and pollination efficiency"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]