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.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","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","939"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","CLIMATE OF THE PAST"],["dc.bibliographiccitation.lastpage","954"],["dc.bibliographiccitation.volume","10"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Fleitmann, Dominik"],["dc.contributor.author","Nowaczyk, N. R."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Wegwerth, Antje"],["dc.contributor.author","Arz, Helge W."],["dc.date.accessioned","2018-11-07T09:46:01Z"],["dc.date.available","2018-11-07T09:46:01Z"],["dc.date.issued","2014"],["dc.description.abstract","High-resolution pollen and dinoflagellate cyst records from sediment core M72/5-25-GC1 were used to reconstruct vegetation dynamics in northern Anatolia and surface conditions of the Black Sea between 64 and 20 ka BP. During this period, the dominance of Artemisia in the pollen record indicates a steppe landscape and arid climate conditions. However, the concomitant presence of temperate arboreal pollen suggests the existence of glacial refugia in northern Anatolia. Long-term glacial vegetation dynamics reveal two major arid phases similar to 64-55 and 40-32 ka BP, and two major humid phases similar to 54-45 and 28-20 ka BP, correlating with higher and lower summer insolation, respectively. Dansgaard-Oeschger (D-O) cycles are clearly indicated by the 25-GC1 pollen record. Greenland interstadials are characterized by a marked increase in temperate tree pollen, indicating a spread of forests due to warm/wet conditions in northern Anatolia, whereas Greenland stadials reveal cold and arid conditions as indicated by spread of xerophytic biomes. There is evidence for a phase lag of similar to 500 to 1500 yr between initial warming and forest expansion, possibly due to successive changes in atmospheric circulation in the North Atlantic sector. The dominance of Pyxidinopsis psilata and Spiniferites cruciformis in the dinocyst record indicates brackish Black Sea conditions during the entire glacial period. The decrease of marine indicators (marine dinocysts, acritarchs) at similar to 54 ka BP and increase of freshwater algae (Pediastrum, Botryococcus) from 32 to 25 ka BP reveals freshening of the Black Sea surface water. This freshening is possibly related to humid phases in the region, to connection between Caspian Sea and Black Sea, to seasonal freshening by floating ice, and/or to closer position of river mouths due to low sea level. In the southern Black Sea, Greenland interstadials are clearly indicated by high dinocyst concentrations and calcium carbonate content, as a result of an increase in primary productivity. Heinrich events show a similar impact on the environment in the northern Anatolia/Black Sea region as Greenland stadials."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2013"],["dc.identifier.doi","10.5194/cp-10-939-2014"],["dc.identifier.isi","000338761600002"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/10124"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/34767"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1814-9332"],["dc.relation.issn","1814-9324"],["dc.rights","CC BY 3.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/3.0"],["dc.title","Orbital- and millennial-scale environmental changes between 64 and 20 ka BP recorded in Black Sea sediments"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","433"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Anais da Academia Brasileira de Ciências"],["dc.bibliographiccitation.lastpage","443"],["dc.bibliographiccitation.volume","80"],["dc.contributor.author","Stefenon, Valdir Marcos"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Gailing, Oliver"],["dc.contributor.author","Finkeldey, Reiner"],["dc.date.accessioned","2018-11-07T11:11:03Z"],["dc.date.accessioned","2020-05-14T07:39:07Z"],["dc.date.available","2018-11-07T11:11:03Z"],["dc.date.available","2020-05-14T07:39:07Z"],["dc.date.issued","2008"],["dc.description.abstract","Up to date. little is known about the relationship between historical demography and the current genetic structure of A. angustifolia. As a first effort towards overcoming this lack, microsatellite data scored in six populations and isozyme allele frequencies published for 11 natural stands of this species were analysed in order to assess molecular signatures of populations demographic history. Signatures of genetic bottlenecks were captured in all analysed populations of southeastern Brazil. Among southern Populations, signatures of small effective population size were Observed in only three out of 13 populations. Southern Populations likely experienced faster recovery of population size after migration onto highlands. Accordingly, current genetic diversity of the Southern populations gives evidence of fast population size recovery. In general, demographic history of A. angustifolia matches climatic dynamics of southern and Southeastern Brazil during the Pleistocene and Holocene. Palynological records and reconstruction of the past climatic dynamics of Southeastern and southern Brazil support the hypothesis of different population size recovery dynamics for populations from these regions."],["dc.identifier.doi","10.1590/S0001-37652008000300005"],["dc.identifier.isi","000259122400005"],["dc.identifier.pmid","18797796"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/7860"],["dc.identifier.scopus","2-s2.0-51749088788"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/65411"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53343"],["dc.identifier.url","http://www.scopus.com/inward/record.url?eid=2-s2.0-51749088788&partnerID=MN8TOARS"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0001-3765"],["dc.title","Evidences of delayed size recovery in Araucaria angustifolia populations after post-glacial colonization of highlands in Southeastern Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1857"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Climate of the Past"],["dc.bibliographiccitation.lastpage","1869"],["dc.bibliographiccitation.volume","10"],["dc.contributor.author","Wang, L."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Lee, T-Q"],["dc.contributor.author","Li, H-C"],["dc.contributor.author","Huh, C-A"],["dc.contributor.author","Shiau, L-J"],["dc.contributor.author","Chang, Y-P"],["dc.date.accessioned","2018-11-07T09:45:42Z"],["dc.date.available","2018-11-07T09:45:42Z"],["dc.date.issued","2014"],["dc.description.abstract","We reconstructed paleoenvironmental changes from a sediment archive of a lake in the floodplain of the Ilan Plain of NE Taiwan on multi-decadal resolution for the last ca. 1900 years. On the basis of pollen and diatom records, we evaluated past floods, typhoons, and agricultural activities in this area which are sensitive to the hydrological conditions in the western Pacific. Considering the high sedimentation rates with low microfossil preservations in our sedimentary record, multiple flood events were. identified during the period AD 100-1400. During the Little Ice Age phase 1 (LIA 1 - AD 1400-1620), the abundant occurrences of wetland plant (Cyperaceae) and diatom frustules imply less flood events under stable climate conditions in this period. Between AD 500 and 700 and the Little Ice Age phase 2 (LIA 2 - AD 1630-1850), the frequent typhoons were inferred by coarse sediments and planktonic diatoms, which represented more dynamical climate conditions than in the LIA 1. By comparing our results with the reconstructed changes in tropical hydrological conditions, we suggested that the local hydrology in NE Taiwan is strongly influenced by typhoon-triggered heavy rainfalls, which could be influenced by the variation of global temperature, the expansion of the Pacific warm pool, and the intensification of El Nino-Southern Oscillation (ENSO) events."],["dc.description.sponsorship","Open Access Publikationsfonds 2014"],["dc.identifier.doi","10.5194/cp-10-1857-2014"],["dc.identifier.isi","000344734800015"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11392"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/34685"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Copernicus Gesellschaft Mbh"],["dc.relation.issn","1814-9332"],["dc.relation.issn","1814-9324"],["dc.rights","CC BY 3.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/3.0"],["dc.title","Late Holocene environmental reconstructions and their implications on flood events, typhoon, and agricultural activities in NE Taiwan"],["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.artnumber","51"],["dc.bibliographiccitation.firstpage","51"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","BMC Ecology and Evolution"],["dc.bibliographiccitation.volume","22"],["dc.contributor.author","Carneiro de Melo Moura, Carina"],["dc.contributor.author","Setyaningsih, Christina A."],["dc.contributor.author","Li, Kevin"],["dc.contributor.author","Merk, Miryam Sarah"],["dc.contributor.author","Schulze, Sonja"],["dc.contributor.author","Raffiudin, Rika"],["dc.contributor.author","Grass, Ingo"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Tscharntke, Teja"],["dc.contributor.author","Westphal, Catrin"],["dc.contributor.author","Gailing, Oliver"],["dc.date.accessioned","2022-08-12T12:09:48Z"],["dc.date.available","2022-08-12T12:09:48Z"],["dc.date.issued","2022"],["dc.date.updated","2022-07-29T12:00:29Z"],["dc.description.abstract","Intense conversion of tropical forests into agricultural systems contributes to habitat loss and the decline of ecosystem functions. Plant-pollinator interactions buffer the process of forest fragmentation, ensuring gene flow across isolated patches of forests by pollen transfer. In this study, we identified the composition of pollen grains stored in pot-pollen of stingless bees, Tetragonula laeviceps, via dual-locus DNA metabarcoding (ITS2 and rbcL) and light microscopy, and compared the taxonomic coverage of pollen sampled in distinct land-use systems categorized in four levels of management intensity (forest, shrub, rubber, and oil palm) for landscape characterization."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2022"],["dc.identifier.citation","BMC Ecology and Evolution. 2022 Apr 26;22(1):51"],["dc.identifier.doi","10.1186/s12862-022-02004-x"],["dc.identifier.pii","2004"],["dc.identifier.pmid","35473550"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/112719"],["dc.identifier.url","https://publications.goettingen-research-online.de/handle/2/107375"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-561"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | A | A01: Langzeitliche Vegetationsveränderungen, Pflanzenphänologie und Pflanzen-Bestäuber-Interaktionen in Regenwald und Regenwaldtransformationen in Zentral-Sumatra"],["dc.relation","SFB 990 | B | B09: Oberirdische Biodiversitätsmuster und Prozesse in Regenwaldtransformations-Landschaften"],["dc.relation","SFB 990 | B | B14: Phylogenetische Rekonstruktion von Artengemeinschaften mittels DNA-Barcoding – Zusammenhang zwischen phylogenetischer und funktionaler Diversität im Landschaftskontext"],["dc.relation.eissn","2730-7182"],["dc.relation.issn","2730-7182"],["dc.relation.orgunit","Zentrum für Biodiversität und Nachhaltige Landnutzung"],["dc.rights","CC BY 4.0"],["dc.rights.holder","The Author(s)"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.subject","Environmental DNA"],["dc.subject","Biodiversity"],["dc.subject","Taxonomic composition"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","Biomonitoring via DNA metabarcoding and light microscopy of bee pollen in rainforest transformation landscapes of Sumatra"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1257"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","1268"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Proske, Ulrike"],["dc.contributor.author","Hanebuth, Till J. J."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Nguyen, Van Lap"],["dc.contributor.author","Ta, Thi Kim Oanh"],["dc.contributor.author","Diem, Bui Phat"],["dc.date.accessioned","2018-11-07T08:36:14Z"],["dc.date.available","2018-11-07T08:36:14Z"],["dc.date.issued","2010"],["dc.description.abstract","Three radiocarbon-dated sediment cores from the northeastern Vietnamese Mekong River Delta have been analysed with a multiproxy approach (grain size, pollen and spores, macro-charcoal, carbon content) to unravel the palaeoenvironmental history of the region since the mid Holocene. During the mid-Holocene sea-level highstand a diverse, zoned and widespread mangrove belt (dominated by Rhizophora) covered the extended tidal flats. The subsequent regression and coeval delta progradation led to the rapid development of a back-mangrove community dominated by Ceriops and Bruguiera but also represented locally by e. g. Kandelia, Excoecaria and Phoenix. Along rivers this community seems to have endured even when the adjoining floodplain had already shifted to freshwater vegetation. Generally this freshwater vegetation has a strong swamp signature but locally Arecaceae, Fabaceae, Moraceae/Urticaceae and Myrsinaceae are important and mirror the geomorphological diversity of the delta plain. The macro-charcoal record implies that natural burning of vegetation occurred throughout the records, however, the occurrence of the highest amounts of macro-charcoal particles is linked with modern human activity."],["dc.description.sponsorship","APSA; DFG [HA4317\\2-1]"],["dc.identifier.doi","10.1177/0959683610374884"],["dc.identifier.isi","000284467600007"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/13076"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/18263"],["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","The palaeoenvironmental development of the northeastern Vietnamese Mekong River Delta since the mid Holocene"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","191"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","206"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Brunschoen, Corinna"],["dc.contributor.author","Haberzettl, Torsten"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T08:43:55Z"],["dc.date.available","2018-11-07T08:43:55Z"],["dc.date.issued","2010"],["dc.description.abstract","A lake sediment record from Laguna Campana at 2,488 m a.s.l. in the eastern Ecuadorian Andes allows the reconstruction of local environmental conditions over the past similar to 500 years. A high-resolution multi-proxy approach using pollen, spore, charcoal and XRF analyses provides information about lake genesis, hydrological variations and the development of the surrounding vegetation. Results suggest that Laguna Campana originated from a landslide, which are naturally common and anthropogenically promoted in the study area. Human activities, e.g. deforestation or slash and burn cultivation, impacted the local vegetation development and biodiversity during the recorded period. After a first dense layer of pioneer grasses developed on open soil around the small lake, successional stages of secondary upper mountain rainforest forest mainly composed of Alnus and Weinmannia were observed. The record shows no signs of dense forest regeneration but rather open vegetation with trees and a grassy understory. Especially since ca. a.d. 1980, the proportion of forest in the area was reduced, most probably by fire use for pastures, cultivation and wood extraction. Hydrological variability was derived from differences in minerogenic input and variations in Botryococcus braunii and Sphagnum occurrence. After wettest conditions at the study site, probably triggering the landslide, humid conditions persisted until a time of drier conditions between a.d. 1900 and 1960. A subsequent return to wetter conditions was observed over the last decades. XRF analyses suggest an increase in deposition of atmospherically derived lead since the formation of the lake."],["dc.identifier.doi","10.1007/s00334-010-0236-4"],["dc.identifier.isi","000277183200003"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/4238"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/20088"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","0939-6314"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","High-resolution studies on vegetation succession, hydrological variations, anthropogenic impact and genesis of a subrecent lake in southern Ecuador"],["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","3459"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","3479"],["dc.bibliographiccitation.volume","28"],["dc.contributor.affiliation","Jennerjahn, Tim; 2\r\nDepartment of Biogeochemistry and Geology\r\nLeibniz Centre for Tropical Marine Research (ZMT)\r\nBremen Germany"],["dc.contributor.affiliation","Nugroho, Septriono Hari; 4\r\nResearch Center for Geotechnology\r\nNational Research and Innovation Agency (BRIN)\r\nBandung Indonesia"],["dc.contributor.affiliation","Yulianto, Eko; 4\r\nResearch Center for Geotechnology\r\nNational Research and Innovation Agency (BRIN)\r\nBandung Indonesia"],["dc.contributor.affiliation","Behling, Hermann; 1\r\nDepartment of Palynology and Climate Dynamics\r\nUniversity of Goettingen\r\nGoettingen Germany"],["dc.contributor.author","Hapsari, K. Anggi"],["dc.contributor.author","Jennerjahn, Tim"],["dc.contributor.author","Nugroho, Septriono Hari"],["dc.contributor.author","Yulianto, Eko"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2022-04-01T10:03:26Z"],["dc.date.available","2022-04-01T10:03:26Z"],["dc.date.issued","2022"],["dc.date.updated","2022-06-14T22:18:39Z"],["dc.description.abstract","Abstract Southeast Asian peatlands, along with their various important ecosystem services, are mainly distributed in the coastal areas of Sumatra and Borneo. These ecosystems are threatened by coastal development, global warming and sea level rise (SLR). Despite receiving growing attention for their biodiversity and as massive carbon stores, there is still a lack of knowledge on how they initiated and evolved over time, and how they responded to past environmental change, that is, precipitation, sea level and early anthropogenic activities. To improve our understanding thereof, we conducted multi‐proxy paleoecological studies in the Kampar Peninsula and Katingan peatlands in the coastal area of Riau and Central Kalimantan, Indonesia. The results indicate that the initiation timing and environment of both peatlands are very distinct, suggesting that peat could form under various vegetation as soon as there is sufficient moisture to limit organic matter decomposition. The past dynamics of both peatlands were mainly attributable to natural drivers, while anthropogenic activities were hardly relevant. Changes in precipitation and sea level led to shifts in peat swamp forest vegetation, peat accumulation rates and fire regimes at both sites. We infer that the simultaneous occurrence of El Niño‐Southern Oscillation (ENSO) events and SLR resulted in synergistic effects which led to the occurrence of severe fires in a pristine coastal peatland ecosystem; however, it did not interrupt peat accretion. In the future, SLR, combined with the projected increase in frequency and intensity of ENSO, can potentially amplify the negative effects of anthropogenic peatland fires. This prospectively stimulates massive carbon release, thus could, in turn, contribute to worsening the global climate crisis especially once an as yet unknown threshold is crossed and peat accretion is halted, that is, peatlands lose their carbon sink function. Given the current rapid SLR, coastal peatland managements should start develop fire risk reduction or mitigation strategies."],["dc.description.abstract","Our interdisciplinary research shows how the changes in precipitation and sea level influenced the dynamics of coastal peatlands in Indonesia. It was inferred that the simultaneous occurrence of El Niño‐Southern Oscillation (ENSO) events and sea level rise (SLR) synergized in the past which led to the occurrences of severe forest fires, although it did not interrupt peat accretion. In the future, intensified ENSO and SLR can potentially magnify human‐induced peat fires in the coastal area, worsening global climate crisis. Coastal peatland managements should anticipate such hidden risk of current rapid SLR. image"],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659"],["dc.identifier.doi","10.1111/gcb.16131"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/106169"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-530"],["dc.relation.eissn","1365-2486"],["dc.relation.issn","1354-1013"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.rights","This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes."],["dc.rights.uri","http://creativecommons.org/licenses/by-nc/4.0/"],["dc.title","Sea level rise and climate change acting as interactive stressors on development and dynamics of tropical peatlands in coastal Sumatra and South Borneo since the Last Glacial Maximum"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]