Behling, Hermann

[["dc.bibliographiccitation.firstpage","1647"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","1660"],["dc.bibliographiccitation.volume","16"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Ewah, Carol Teboh"],["dc.contributor.author","Jennerjahn, Tim C."],["dc.contributor.author","Paul, Andre"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T08:42:41Z"],["dc.date.available","2018-11-07T08:42:41Z"],["dc.date.issued","2010"],["dc.description.abstract","High resolution palynological and geochemical data of sediment core GeoB 3910-2 (located offshore Northeast Brazil) spanning the period between 19 600 and 14 500 calibrated year bp (19.6-14.5 ka) show a land-cover change in the catchment area of local rivers in two steps related to changes in precipitation associated with Heinrich Event 1 (H1 stadial). At the end of the last glacial maximum, the landscape in semi-arid Northeast Brazil was dominated by a very dry type of caatinga vegetation, mainly composed of grasslands with some herbs and shrubs. After 18 ka, considerably more humid conditions are suggested by changes in the vegetation and by C(org) and C/N data indicative of fluvial erosion. The caatinga became wetter and along lakes and rivers, sedges and gallery forest expanded. The most humid period was recorded between 16.5 and 15 ka, when humid gallery (and floodplain) forest and even small patches of mountainous Atlantic rain forest occurred together with dry forest, the latter being considered as a rather lush type of caatinga vegetation. During this humid phase erosion decreased as less lithogenic material and more organic terrestrial material were deposited on the continental slope of northern Brazil. After 15 ka arid conditions returned. During the humid second phase of the H1 stadial, a rich variety of landscapes existed in Northeast Brazil and during the drier periods small pockets of forest could probably survive in favorable spots, which would have increased the resilience of the forest to climate change."],["dc.identifier.doi","10.1111/j.1365-2486.2009.02023.x"],["dc.identifier.isi","000277288900002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19761"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1354-1013"],["dc.title","Two-step vegetation response to enhanced precipitation in Northeast Brazil during Heinrich event 1"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","87"],["dc.bibliographiccitation.issue","2-3"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","100"],["dc.bibliographiccitation.volume","16"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Jahns, Susanne"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Kim, Jung-Hyun"],["dc.date.accessioned","2018-11-07T11:07:39Z"],["dc.date.available","2018-11-07T11:07:39Z"],["dc.date.issued","2007"],["dc.description.abstract","The distribution of pollen in marine sediments is used to record vegetation changes over the past 30,000 years on the adjacent continent. A transect of marine pollen sequences from the mouth of the river Congo (similar to 5 degrees S) to Walvis Bay and Luderitz (similar to 25 degrees S) shows vegetation changes in Congo, Angola and Namibia from the last glacial period into the Holocene. The comparison of pollen records from different latitudes provides information about the latitudinal shift of open forest and savannahs (Poaceae pollen), the extension of lowland forest (rain forest pollen) and Afromontane forest (Podocarpus pollen), and the position of the desert fringe (pollen of Caryophyllaceae, Chenopodiaceae and Amaranthaceae). High Cyperaceae pollen percentages in sediments from the last glacial period off the mouth of the river Congo suggest the presence of open swamps rather than savannah vegetation in the Congo Basin. Pollen from Restionaceae in combination with Stoebe-type pollen (probably from Elytropappus) indicates a possible northwards extension of winter rain vegetation during the last glacial period. The record of Rhizophora (mangrove) pollen is linked to erosion of the continental shelf and sea-level rise. Pollen influx is highest off river mouths (10-2000 grains year(-1) cm(-2)), close to the coast (300-6000 grains year(-1) cm(-2)), but is an order of magnitude lower at sites situated far from the continent (< 10 grains year(-1) cm(-2))."],["dc.identifier.doi","10.1007/s00334-006-0080-8"],["dc.identifier.isi","000243004900003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/52614"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1617-6278"],["dc.relation.issn","0939-6314"],["dc.title","Variability in glacial and Holocene marine pollen records offshore from west southern Africa"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","107"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","CLIMATE OF THE PAST"],["dc.bibliographiccitation.lastpage","124"],["dc.bibliographiccitation.volume","4"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Kim, J.-H."],["dc.date.accessioned","2018-11-07T11:19:41Z"],["dc.date.available","2018-11-07T11:19:41Z"],["dc.date.issued","2008"],["dc.description.abstract","ODP Site 1078 situated under the coast of Angola provides the first record of the vegetation history for Angola. The upper 11 m of the core covers the past 30 thousand years, which has been analysed palynologically in decadal to centennial resolution. Alkenone sea surface temperature estimates were analysed in centennial resolution. We studied sea surface temperatures and vegetation development during full glacial, deglacial, and interglacial conditions. During the glacial the vegetation in Angola was very open consisting of grass and heath lands, deserts and semi-deserts, which suggests a cool and dry climate. A change to warmer and more humid conditions is indicated by forest expansion starting in step with the earliest temperature rise in Antarctica, 22 thousand years ago. We infer that around the period of Heinrich Event 1, a northward excursion of the Angola Benguela Front and the Congo Air Boundary resulted in cool sea surface temperatures but rain forest remained present in the northern lowlands of Angola. Rain forest and dry forest area increase 15 thousand years ago. During the Holocene, dry forests and Miombo woodlands expanded. Also in Angola globally recognised climate changes at 8 thousand and 4 thousand years ago had an impact on the vegetation. During the past 2 thousand years, savannah vegetation became dominant."],["dc.identifier.isi","000257303600003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55346"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1814-9332"],["dc.relation.issn","1814-9324"],["dc.title","Thirty thousand years of vegetation development and climate change in Angola (Ocean Drilling Program Site 1078)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","73"],["dc.bibliographiccitation.issue","2-3"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","75"],["dc.bibliographiccitation.volume","16"],["dc.contributor.author","Jahns, Susanne"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Bittmann, Felix"],["dc.contributor.author","Schluetz, Frank"],["dc.date.accessioned","2018-11-07T11:07:39Z"],["dc.date.available","2018-11-07T11:07:39Z"],["dc.date.issued","2007"],["dc.identifier.doi","10.1007/s00334-006-0086-2"],["dc.identifier.isi","000243004900001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/52612"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0939-6314"],["dc.title","A thankful tribute to Hans-Juergen Beug on the occasion of his 75th birthday"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","217"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Quaternary Research"],["dc.bibliographiccitation.lastpage","230"],["dc.bibliographiccitation.volume","69"],["dc.contributor.author","Gonzalez, Catalina"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Wefer, Gerold"],["dc.date.accessioned","2018-11-07T11:18:02Z"],["dc.date.available","2018-11-07T11:18:02Z"],["dc.date.issued","2008"],["dc.description.abstract","We present new palynological information from the anoxic Cariaco Basin, off Venezuela, that provides insight into the response of northernmost South American vegetation to rapid climate changes between 68 and 28 ka, specifically during North Atlantic Heinrich events (HEs) and Dansgaard/Oeschger cycles. We defined three different vegetation modes: (1) an interstadial mode characterized by the highest pollen concentration and the maximum extension of semi-deciduous and evergreen forests; (2) a stadial mode characterized by increases of salt marshes, herbs, and montane forests; and (3) a Heinrich event mode characterized by the lowest pollen concentrations, abrupt increases of salt marshes, and decreased forest abundance. Similarly, indices of C4/C3 plants show increases during stadials with clear peaks during the onset of HEs, though grasslands did not become dominant during these periods. We alternatively propose that these expansions of C4 plants are associated with the expansion of coastal salt marshes. Our vegetation record suggests the prevalence of humid conditions during interstadials, dry and cold conditions during stadials, and dry and cold conditions together with changes in sea level during HEs. This new palynological evidence supports previous interpretations that main environmental changes in northernmost South America were driven by latitudinal displacements of the Intertropical Convergence Zone and sea-level changes. (C) 2007 University of Washington. All rights reserved."],["dc.identifier.doi","10.1016/j.yqres.2007.12.001"],["dc.identifier.isi","000254787600004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/54955"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0033-5894"],["dc.title","Neotropical vegetation response to rapid climate changes during the last glacial period: Palynological evidence from the Cariaco Basin"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1645"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","1646"],["dc.bibliographiccitation.volume","16"],["dc.contributor.author","Haberle, Simon G."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Kirleis, Wiebke"],["dc.date.accessioned","2018-11-07T08:42:41Z"],["dc.date.available","2018-11-07T08:42:41Z"],["dc.date.issued","2010"],["dc.identifier.doi","10.1111/j.1365-2486.2010.02231.x"],["dc.identifier.isi","000277288900001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19760"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1354-1013"],["dc.title","Introduction: Tropical palaeoecology and global change"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","CLIMATE OF THE PAST"],["dc.bibliographiccitation.volume","7"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Kim, J.-H."],["dc.date.accessioned","2018-11-07T09:00:27Z"],["dc.date.available","2018-11-07T09:00:27Z"],["dc.date.issued","2011"],["dc.format.extent","115"],["dc.identifier.doi","10.5194/cp-7-115-2011"],["dc.identifier.isi","000288992700010"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/24164"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Copernicus Gesellschaft Mbh"],["dc.relation.issn","1814-9324"],["dc.title","Thirty thousand years of vegetation development and climate change in Angola (Ocean Drilling Program Site 1078) (vol 4, pg 107, 2008)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["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","22"],["dc.bibliographiccitation.journal","Quaternary International"],["dc.bibliographiccitation.lastpage","31"],["dc.bibliographiccitation.volume","161"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Safford, Hugh DeForest"],["dc.contributor.author","Wefer, Gerold"],["dc.date.accessioned","2018-11-07T11:05:36Z"],["dc.date.available","2018-11-07T11:05:36Z"],["dc.date.issued","2007"],["dc.description.abstract","Late Quaternary vegetation, fire and climate dynamics were studied by pollen and charcoal analysis in the Serra da Bocaina, in the coastal ranges of southeastern Brazil, Rio de Janeiro and S (a) over tildeo Paulo States. Samples were taken from two cores, Serra da Bocaina I and 2. Seven radiocarbon dates indicate deposits of Late Pleistocene to Holocene age. During the period between 18,570 and 14,570 cal BP wide-spread grassland (\"campos\") with frequent fires existed in the higher Serra da Bocaina; taken together with other evidence, this indicates relatively dry and cold climatic conditions for this period. Upper montane forest occurred in protected valleys or on slopes at lower elevations. The conifer Araucaria angustifolia has been present in the Serra da Bocaina since the Late Pleistocene, but populations have fluctuated. An erosion hiatus in the Late-glacial period, evidenced by reworked deposits lacking pollen, was probably caused by increased rainfall during the Younger Dryas period. Upper montane forest taxa expanded during the Holocene, especially after 7260 cal BP. Indications are that the early and mid Holocene were dry and relatively warm, with an annual dry season longer than present day. Modern patches of campos in the Serra da Bocaina are remnants of more expansive grasslands during glacial times. (c) 2006 Elsevier Ltd and INQUA. All rights reserved."],["dc.identifier.doi","10.1016/j.quaint.2006.10.021"],["dc.identifier.isi","000244919200003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/52106"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1040-6182"],["dc.title","Late Quaternary vegetation and climate dynamics in the Serra da Bocaina, southeastern Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2882"],["dc.bibliographiccitation.issue","21-22"],["dc.bibliographiccitation.journal","Quaternary Science Reviews"],["dc.bibliographiccitation.lastpage","2899"],["dc.bibliographiccitation.volume","29"],["dc.contributor.author","Hessler, Ines"],["dc.contributor.author","Dupont, Lydie M."],["dc.contributor.author","Bonnefille, Raymonde"],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Gonzalez, Catalina"],["dc.contributor.author","Helmens, Karin F."],["dc.contributor.author","Hooghiemstra, Henry"],["dc.contributor.author","Lebamba, Judicael"],["dc.contributor.author","Ledru, Marie-Pierre"],["dc.contributor.author","Lezine, Anne-Marie"],["dc.contributor.author","Maley, Jean"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Vincens, Annie"],["dc.date.accessioned","2018-11-07T08:38:57Z"],["dc.date.available","2018-11-07T08:38:57Z"],["dc.date.issued","2010"],["dc.description.abstract","To reconstruct the response of vegetation to abrupt climate changes during the last glacial we have compiled pollen records from the circum-Atlantic tropics between 23 degrees N and 23 degrees S from both marine and terrestrial sediment cores. Pollen data were grouped into mega-biomes to facilitate the comparison between the different records. Most tropical African records do not appear to register Dansgaard-Oeschger (D-O) variability, although there are vegetation changes during Heinrich Stadials (HS). There is a stronger signal of D-O and HS variability in the South American records. Records close to the modern northern and southern limits of the Intertropical Convergence Zone (ITCZ) show opposite trends in vegetation development during HS and D-O cycles. The pollen data from tropical South America corroborate the hypothesis of a southward shift in the migration pattern of the ITCZ and a reduction in the Atlantic Meridional Overturning Circulation (AMOC) during HS. (C) 2009 Elsevier Ltd. All rights reserved."],["dc.description.sponsorship","NERC; DFG"],["dc.identifier.doi","10.1016/j.quascirev.2009.11.029"],["dc.identifier.isi","000282851600005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/18873"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0277-3791"],["dc.title","Millennial-scale changes in vegetation records from tropical Africa and South America during the last glacial"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]