Behling, Hermann

[["dc.bibliographiccitation.firstpage","679"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Earth System Science Data"],["dc.bibliographiccitation.lastpage","695"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Sánchez Goñi, María Fernanda"],["dc.contributor.author","Desprat, Stéphanie"],["dc.contributor.author","Daniau, Anne-Laure"],["dc.contributor.author","Bassinot, Frank C."],["dc.contributor.author","Polanco-Martínez, Josué M."],["dc.contributor.author","Harrison, Sandy P."],["dc.contributor.author","Allen, Judy R. M."],["dc.contributor.author","Anderson, R. Scott"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Bonnefille, Raymonde"],["dc.contributor.author","Burjachs, Francesc"],["dc.contributor.author","Carrión, José S."],["dc.contributor.author","Cheddadi, Rachid"],["dc.contributor.author","Clark, James S."],["dc.contributor.author","Combourieu-Nebout, Nathalie"],["dc.contributor.author","Mustaphi, Colin. J. Courtney"],["dc.contributor.author","Debusk, Georg H."],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Finch, Jemma M."],["dc.contributor.author","Fletcher, William J."],["dc.contributor.author","Giardini, Marco"],["dc.contributor.author","González, Catalina"],["dc.contributor.author","Gosling, William D."],["dc.contributor.author","Grigg, Laurie D."],["dc.contributor.author","Grimm, Eric C."],["dc.contributor.author","Hayashi, Ryoma"],["dc.contributor.author","Helmens, Karin"],["dc.contributor.author","Heusser, Linda E."],["dc.contributor.author","Hill, Trevor"],["dc.contributor.author","Hope, Geoffrey"],["dc.contributor.author","Huntley, Brian"],["dc.contributor.author","Igarashi, Yaeko"],["dc.contributor.author","Irino, Tomohisa"],["dc.contributor.author","Jacobs, Bonnie"],["dc.contributor.author","Jiménez-Moreno, Gonzalo"],["dc.contributor.author","Kawai, Sayuri"],["dc.contributor.author","Kershaw, A. Peter"],["dc.contributor.author","Kumon, Fujio"],["dc.contributor.author","Lawson, Ian T."],["dc.contributor.author","Ledru, Marie-Pierre"],["dc.contributor.author","Lézine, Anne-Marie"],["dc.contributor.author","Liew, Ping Mei"],["dc.contributor.author","Magri, Donatella"],["dc.contributor.author","Marchant, Robert"],["dc.contributor.author","Margari, Vasiliki"],["dc.contributor.author","Mayle, Francis E."],["dc.contributor.author","McKenzie, G. Merna"],["dc.contributor.author","Moss, Patrick"],["dc.contributor.author","Müller, Stefanie"],["dc.contributor.author","Müller, Ulrich C."],["dc.contributor.author","Naughton, Filipa"],["dc.contributor.author","Newnham, Rewi M."],["dc.contributor.author","Oba, Tadamichi"],["dc.contributor.author","Pérez-Obiol, Ramón"],["dc.contributor.author","Pini, Roberta"],["dc.contributor.author","Ravazzi, Cesare"],["dc.contributor.author","Roucoux, Katy H."],["dc.contributor.author","Rucina, Stephen M."],["dc.contributor.author","Scott, Louis"],["dc.contributor.author","Takahara, Hikaru"],["dc.contributor.author","Tzedakis, Polichronis C."],["dc.contributor.author","Urrego, Dunia H."],["dc.contributor.author","van Geel, Bas"],["dc.contributor.author","Valencia, B. Guido"],["dc.contributor.author","Vandergoes, Marcus J."],["dc.contributor.author","Vincens, Annie"],["dc.contributor.author","Whitlock, Cathy L."],["dc.contributor.author","Willard, Debra A."],["dc.contributor.author","Yamamoto, Masanobu"],["dc.date.accessioned","2019-07-09T11:44:19Z"],["dc.date.available","2019-07-09T11:44:19Z"],["dc.date.issued","2017"],["dc.description.abstract","Quaternary records provide an opportunity to examine the nature of the vegetation and fire responses to rapid past climate changes comparable in velocity and magnitude to those expected in the 21st-century. The best documented examples of rapid climate change in the past are the warming events associated with the Dansgaard–Oeschger (D–O) cycles during the last glacial period, which were sufficiently large to have had a potential feedback through changes in albedo and greenhouse gas emissions on climate. Previous reconstructions of vegetation and fire changes during the D–O cycles used independently constructed age models, making it difficult to compare the changes between different sites and regions. Here, we present the ACER (Abrupt Climate Changes and Environmental Responses) global database, which includes 93 pollen records from the last glacial period (73–15 ka) with a temporal resolution better than 1000 years, 32 of which also provide charcoal records. A harmonized and consistent chronology based on radiometric dating (14C, 234U=230Th, optically stimulated luminescence (OSL), 40Ar=39Ar-dated tephra layers) has been constructed for 86 of these records, although in some cases additional information was derived using common control points based on event stratigraphy. The ACER database compiles metadata including geospatial and dating information, pollen and charcoal counts, and pollen percentages of the characteristic biomes and is archived in Microsoft AccessTM at https://doi.org/10.1594/PANGAEA.870867."],["dc.identifier.doi","10.5194/essd-9-679-2017"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14712"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58991"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY 3.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/3.0"],["dc.title","The ACER pollen and charcoal database: a global resource to document vegetation and fire response to abrupt climate changes during the last glacial period"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","265"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Journal of Paleolimnology"],["dc.bibliographiccitation.lastpage","277"],["dc.bibliographiccitation.volume","44"],["dc.contributor.author","Enters, Dirk"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Mayr, Christoph"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Zolitschka, Bernd"],["dc.date.accessioned","2018-11-07T08:42:52Z"],["dc.date.available","2018-11-07T08:42:52Z"],["dc.date.issued","2010"],["dc.description.abstract","Environmental changes of the last 9,300 years were reconstructed by geochemical and pollen analyses of a 14-m-long, laminated sediment core from Lago Aleixo, south-eastern Brazil. Fossil pollen assemblages indicate open savannah vegetation (campo cerrado) and gallery forests until approximately 6,900 cal. BP. During that time, siderite laminae were deposited under anoxic conditions at the lake bottom. Then, increased rainfall and a shorter annual dry period allowed gallery forests and semi-deciduous forests to expand, leading to more closed cerrado vegetation. High-intensity rainfall events during this period are recorded as peaks in K and Ti concentrations. The sediment facies during this period consists of alternating layers of diatoms and minerogenic matter. C/N ratios imply that algae and perhaps soils, too, were the main contributors to sediment organic matter. Biogenic silica and delta C-13(org) variations indicate increasing primary productivity, which was related to higher nutrient flux from intensified leaching of soils, as shown by rising K/Al ratios. Around 800 cal. BP, a closed, semi-deciduous forest developed under present-day climate conditions. Slope stabilization diminished erosion processes in the catchment and caused reduced input of minerogenic matter into the basin. Human impact is evident in the topmost homogeneous sediments, as removal of the stabilizing forest cover amplified soil erosion. The continuous trend to more humid conditions during the Holocene probably reflects increased influence of the Amazon Basin as a moisture source. We conclude that the Lago Aleixo sediment archive was a sensitive recorder of environmental dynamics in tropical South America, which were mainly controlled by changes in precipitation patterns."],["dc.identifier.doi","10.1007/s10933-009-9402-z"],["dc.identifier.isi","000277939200020"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/6807"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19804"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1573-0417"],["dc.relation.issn","0921-2728"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Holocene environmental dynamics of south-eastern Brazil recorded in laminated sediments of Lago Aleixo"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]