Now showing 1 - 10 of 19
  • 2019Journal Article
    [["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Nature Communications"],["dc.bibliographiccitation.volume","10"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Wolters, Steffen"],["dc.contributor.author","van Leeuwen, Jacqueline F. N."],["dc.contributor.author","van der Knaap, Pim W. O."],["dc.contributor.author","Leydet, Michelle"],["dc.contributor.author","Brewer, Simon"],["dc.date.accessioned","2020-12-10T18:09:52Z"],["dc.date.available","2020-12-10T18:09:52Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1038/s41467-019-13233-y"],["dc.identifier.eissn","2041-1723"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16828"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73783"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Postglacial change of the floristic diversity gradient in Europe"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]
    Details DOI
  • 2010Journal Article Research Paper
    [["dc.bibliographiccitation.firstpage","231"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","244"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Eckstein, Jan"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Bauerochse, Andreas"],["dc.date.accessioned","2018-11-07T08:45:27Z"],["dc.date.available","2018-11-07T08:45:27Z"],["dc.date.issued","2010"],["dc.description.abstract","Excellently preserved subfossil pine and oak tree remains from the bottom layer of raised bog peat were dendroecologically investigated at Venner Moor (northwest Germany). Tree-ring analyses were combined with observations of stem and root morphology, preservation state, mineral soil relief, peat stratigraphy and pollen analysis to reconstruct in great detail environmental changes leading to the start of the raised bog formation. Hydrology was identified as the main determinant influencing tree growth and population dynamics at Venner Moor, as documented by different growth patterns and dying-off dates in relation to the mineral soil elevation. The woodland phase has been dendrochronological dated to the period from 2421-2077 BC (4371-4027 cal BP). In this period, a general change from more or less open landscape with dominating heath to wet pine forest and eventually to open raised bog occurred at the site. Comparisons with pine population dynamics at the nearby Voerdener Moor and with the independent Lower Saxony log yak Chronology (LSBOC) indicate that the reconstructed ecological changes at Venner Moor are mainly triggered by climate variations, in particular wet shifts on the decadal timescale. This example shows the value of subfossil pine layers from northwest German bogs as a high resolution proxy archive of Holocene humidity fluctuations."],["dc.description.sponsorship","German Research Foundation [LE 1805/2-1]"],["dc.identifier.doi","10.1177/0959683609350397"],["dc.identifier.isi","000274900800008"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/13085"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/20445"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0959-6836"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Dendroecological investigations at Venner Moor (northwest Germany) document climate-driven woodland dynamics and mire development in the period 2450-2050 BC"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]
    Details DOI WOS
  • 2010Journal Article
    [["dc.bibliographiccitation.firstpage","259"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","270"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Pidek, Irena A."],["dc.contributor.author","Svitavska-Svobodova, Helena"],["dc.contributor.author","van der Knaap, Willem O."],["dc.contributor.author","Noryskiewicz, Agnieszka M."],["dc.contributor.author","Filbrandt-Czaja, Anna"],["dc.contributor.author","Noryskiewicz, Bozena"],["dc.contributor.author","Latalowa, Malgorzata"],["dc.contributor.author","Zimny, Marcelina"],["dc.contributor.author","Swieta-Musznicka, Joanna"],["dc.contributor.author","Bozilova, Elissaveta"],["dc.contributor.author","Tonkov, Spassimir"],["dc.contributor.author","Filipova-Marinova, Mariana V."],["dc.contributor.author","Poska, Anneli"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Gikov, Aleksander"],["dc.date.accessioned","2018-11-07T08:41:10Z"],["dc.date.available","2018-11-07T08:41:10Z"],["dc.date.issued","2010"],["dc.description.abstract","Annual pollen-accumulation rates (PAR) of Fagus (beech) obtained within the framework of the Pollen Monitoring Programme (PMP) were analyzed in pollen traps along a N-S transect from the Baltic Sea to the Black Sea in different European vegetation units. The study regions are situated in the lowlands of northern Poland, the uplands of SE Poland, the Czech Krkonoe Mts, the Czech umava Mts, the Swiss Jura Mts, the Swiss Alps, the Bulgarian Rila Mts and the Bulgarian Strandzha Mts. Most time series are 10 or 11 years long, some are 5-16 years long. Inter-annual fluctuations in Fagus PAR were analyzed and compared with seed mast years. Years with high Fagus PAR and others with low Fagus PAR occurred most frequently in parallel within each region and often in two neighbouring regions. 2006 was exceptional as it had a very high Fagus sylvatica pollen deposition in all study regions and it was also a mast year. In Bulgaria, the trend in the 5 years of Fagus orientalis PAR in the Strandzha Mts differed from that of F. sylvatica PAR in the Rila Mts. Aiming at establishing the relationship between average Fagus PAR and tree cover, differences in Fagus PAR (averaged per pollen trap) were related in each region to the proportion of beech trees in the vegetation within 2 km of the pollen traps, the distance to the nearest pollinating Fagus tree, regional or local presence of beech forests, the degree of landscape openness, and the size of forest opening in which a trap is situated. Average Fagus PAR was found to track the regional abundance of beech trees in the vegetation, not the distance of the nearest Fagus tree. Regional occurrence of beech-dominated forests was reflected by a Fagus PAR of ca. 1,400 grains cm(-2) year(-1), local abundance very close to pollen traps by ca. 2,400 grains, small patches of forest with admixture of Fagus by ca. 170-220 grains, and scarcity or absence of Fagus by ca. 40 grains or less."],["dc.description.sponsorship","PMP Sheila Hicks"],["dc.identifier.doi","10.1007/s00334-010-0248-0"],["dc.identifier.isi","000280825200003"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/7644"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19409"],["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","Variation in annual pollen accumulation rates of Fagus along a N-S transect in Europe based on pollen traps"],["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 WOS
  • 2020Journal Article
    [["dc.bibliographiccitation.firstpage","1115"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","1128"],["dc.bibliographiccitation.volume","30"],["dc.contributor.author","Álvarez-Barra, Valentina"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Fontana, Sonia L."],["dc.date.accessioned","2020-12-10T18:38:28Z"],["dc.date.available","2020-12-10T18:38:28Z"],["dc.date.issued","2020"],["dc.description.abstract","Natural disturbance processes such as volcanic eruptions, fire and human activities are important vegetation drivers in north Patagonia. Here, we tested the impact of volcanic ash fall and fire on vegetation composition analysing two sediment records, Lake Avutarda and Lake Bruja, located in the forest-steppe transition at 40°S. In addition, our analysis provides the first account on the history of Nothofagus alpina at its eastern distribution limits. Our results comprise the last 3000 years, indicating the persistence of the vegetation despite evident volcanic activity documented by numerous tephra layers in both records. Eleven fire episodes were identified, while redundancy analysis indicates a non-significant influence of fire activity on the vegetation. The population increase of Nothofagus alpina represents the most important change in vegetation composition in the last three millennia. We speculate that the presumed change in climate, which led to the expansion of Austrocedrus chilensis south of the study area, also caused the increase of Nothofagus alpina populations in the region."],["dc.description.sponsorship","Comisión Nacional de Investigación Científica y Tecnológica \t https://doi.org/10.13039/501100002848"],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft \t https://doi.org/10.13039/501100001659"],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft \t https://doi.org/10.13039/501100001659"],["dc.identifier.doi","10.1177/0959683620913920"],["dc.identifier.eissn","1477-0911"],["dc.identifier.issn","0959-6836"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/77332"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.publisher","SAGE Publications"],["dc.relation.eissn","1477-0911"],["dc.relation.issn","0959-6836"],["dc.title","Late-Holocene vegetation dynamics and disturbance regimes in north Patagonia Argentina (40°S)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]
    Details DOI
  • 2010Journal Article
    [["dc.bibliographiccitation.firstpage","271"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","283"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Pardoe, Heather S."],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","van der Knaap, Willem O."],["dc.contributor.author","Svitavska-Svobodova, Helena"],["dc.contributor.author","Kvavadze, Eliso V."],["dc.contributor.author","Panajiotidis, Sampson"],["dc.contributor.author","Gerasimidis, Achilles"],["dc.contributor.author","Pidek, Irena A."],["dc.contributor.author","Zimny, Marcelina"],["dc.contributor.author","Swieta-Musznicka, Joanna"],["dc.contributor.author","Latalowa, Malgorzata"],["dc.contributor.author","Noryskiewicz, Agnieszka M."],["dc.contributor.author","Bozilova, Elissaveta"],["dc.contributor.author","Tonkov, Spassimir"],["dc.contributor.author","Filipova-Marinova, Mariana V."],["dc.contributor.author","van Leeuwen, Jacqueline F. N."],["dc.contributor.author","Kalnina, Laimdota"],["dc.date.accessioned","2018-11-07T08:41:10Z"],["dc.date.available","2018-11-07T08:41:10Z"],["dc.date.issued","2010"],["dc.description.abstract","This paper compares pollen spectra derived from modified Tauber traps and moss samples from a selection of woodland types from Bulgaria, the Czech Republic, Georgia, Greece, Poland, Switzerland and Wales. The study examines the representation of individual taxa in the two sampling media and aims to ascertain the duration of pollen deposition captured by a moss. The latter aim was pursued through the calculation of dissimilarity indexes to assess how many years of pollen deposited in a pollen trap yield percentage values that are most similar to those obtained from the moss. The results are broadly scattered; the majority of moss samples being most similar to several years of pollen deposition in the adjacent trap. For a selection of samples, a comparison of the pollen accumulation rate in pollen traps with the pollen concentration in the moss per unit surface indicates that the entrapment and/or preservation of individual pollen types in the moss differ from that in the pollen trap. A comparison of the proportion of different taxa in the moss with the pollen spectrum of 2 years of pollen deposition in the trap also revealed large differences. There is a tendency for bisaccate grains such as Pinus and Picea to have a higher representation in moss than in traps but there is considerable regional variation. The results indicate that pollen proportions from moss samples often represent the pollen deposition of one area over several years. However, bisaccate pollen grains tend to be over-represented in moss samples compared to both pollen traps and, potentially, lake sediments."],["dc.identifier.doi","10.1007/s00334-010-0258-y"],["dc.identifier.isi","000280825200004"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/7640"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19410"],["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","Comparing pollen spectra from modified Tauber traps and moss samples: examples from a selection of woodlands across Europe"],["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 WOS
  • 2009Journal Article
    [["dc.bibliographiccitation.firstpage","209"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","220"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Seppa, Heikki"],["dc.contributor.author","Alenius, Teija"],["dc.contributor.author","Muukkonen, Petteri"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Miller, Paul A."],["dc.contributor.author","Ojala, Antti E. K."],["dc.date.accessioned","2018-11-07T08:32:08Z"],["dc.date.available","2018-11-07T08:32:08Z"],["dc.date.issued","2009"],["dc.description.abstract","Recent investigations show that the pollen accumulation rate (PAR) of the common tree taxa is directly related to the biomass and, by inference, to the population size of the taxa around the study site. Fossil PAR records preserved in lakes provide therefore a potential proxy for quantitative biomass and population reconstructions. We use the high-resolution PAR records obtained from two accurately dated lake sediment cores in Finland to generate quantitative Holocene biomass records for Pinus, Picea and Betula, the most common tree taxa of the European Boreal forest. PAR values were calibrated to biomass values by comparing the modern PAR values with the modern biomass values and assuming a linear relationship between the past PAR and biomass values. The obtained PAR and biomass values and trends are remarkably coherent between the two records. Pinus has a stable Holocene biomass size and its modern biomass, about 20 t/ha corresponds with the natural Pinus biomass in the study regions. In contrast, Picea immigrated from the East during the mid Holocene, had a maximum biomass, 50-60 t/ha, at 3500-1000 cal. yr BP, and declined strongly during the last 1500-1000 years as a result of increased human activity and related rise of fire frequency. Thus, the modern Picea biomass in the study regions, about 22 t/ha, is only 35-40% of the natural Picea biomass. The results of this pilot study demonstrate the potential of the calibrated PAR data in quantitative biomass and population reconstructions. Such reconstructions can provide fresh insights into the structure of past plant communities and, when combined with records reflecting palaeoclimates, natural disturbances, and human activity, can help to disentangle the long-term importance of different enviromental drivers to changes in plants populations and ecosystems."],["dc.description.sponsorship","Academy of Finland; European Science Foundation [2003-980409]"],["dc.identifier.doi","10.1177/0959683608100565"],["dc.identifier.isi","000264239900004"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/13075"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/17274"],["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","Calibrated pollen accumulation rates as a basis for quantitative tree biomass reconstructions"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]
    Details DOI WOS
  • 2018Journal Article Editorial Contribution (Editorial, Introduction, Epilogue)
    [["dc.bibliographiccitation.journal","Frontiers in Earth Science"],["dc.bibliographiccitation.volume","6"],["dc.contributor.author","Rull, Valentí"],["dc.contributor.author","Montoya, Encarni"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Morris, Jesse L."],["dc.date.accessioned","2020-12-10T18:44:21Z"],["dc.date.available","2020-12-10T18:44:21Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.3389/feart.2018.00186"],["dc.identifier.eissn","2296-6463"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78422"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.publisher","Frontiers Media S.A."],["dc.relation.eissn","2296-6463"],["dc.rights","http://creativecommons.org/licenses/by/4.0/"],["dc.title","Editorial: Palynology and Vegetation History"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","editorial_ja"],["dspace.entity.type","Publication"]]
    Details DOI
  • 2010Journal Article Research Paper
    [["dc.bibliographiccitation.firstpage","247"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","258"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Fontana, Sonia L."],["dc.contributor.author","van der Knaap, Willem O."],["dc.contributor.author","Pardoe, Heather S."],["dc.contributor.author","Pidek, Irena A."],["dc.date.accessioned","2018-11-07T08:41:09Z"],["dc.date.available","2018-11-07T08:41:09Z"],["dc.date.issued","2010"],["dc.description.abstract","Pollen monitoring has become a standard investigation method for researchers in several disciplines; among them are Quaternary palynologists, who conduct experiments in order to gain insights that will help to interpret the content of pollen in sediments. A review of the literature shows how these experiments diversified during the 1920s and 1930s with an array of different research questions, ranging from pollination biology to hay fever studies. Quaternary palynologists gained renewed interest with the possibility of radiocarbon dating late Quaternary sediments and obtaining accumulation rates. Also, the comprehensive model of pollen deposition and the pollen budget studies by H. Tauber encouraged researchers to conduct similar experiments using the same type of pollen trap, which became the main trapping device for Quaternary palynologists. The high precipitation in the tropics inspired the development of alternative designs. The equipment used to assess the pollen content in the air has evolved from simple gravity devices to different types of apparatus using a vacuum pump or revolving rods that collect the pollen on impact. Silicone impregnated filters exposed perpendicularly to the wind can also yield a volumetric assessment and have proven useful in areas with a low content of pollen in the air. The literature review is followed by a brief account of the developments which established the basis for the formation of a group of scientists monitoring the pollen deposition at a network of sites using standard pollen traps, the Pollen Monitoring Programme (PMP). Over the last 15 years the network has collected a large dataset, which is now available to answer a number of research questions. A summary of selected regions and environments, for which pollen monitoring results are available, is provided to serve as a complement to the investigations mentioned above and to provide an overview that may stimulate new research."],["dc.identifier.doi","10.1007/s00334-010-0261-3"],["dc.identifier.isi","000280825200002"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/4980"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19408"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0939-6314"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","From early pollen trapping experiments to the Pollen Monitoring Programme"],["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"]]
    Details DOI WOS
  • 2009Journal Article
    [["dc.bibliographiccitation.firstpage","417"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","424"],["dc.bibliographiccitation.volume","18"],["dc.contributor.author","Fyfe, Ralph M."],["dc.contributor.author","de Beaulieu, Jacques-Louis"],["dc.contributor.author","Binney, Heather"],["dc.contributor.author","Bradshaw, Richard H. W."],["dc.contributor.author","Brewer, Simon"],["dc.contributor.author","Le Flao, Anne"],["dc.contributor.author","Finsinger, Walter"],["dc.contributor.author","Gaillard, Marie-Jose"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Gil-Romera, Graciela"],["dc.contributor.author","Grimm, Eric C."],["dc.contributor.author","Huntley, Brian"],["dc.contributor.author","Kunes, Petr"],["dc.contributor.author","Kuehl, Norbert"],["dc.contributor.author","Leydet, Michelle"],["dc.contributor.author","Lotter, Andre F."],["dc.contributor.author","Tarasov, Pavel E."],["dc.contributor.author","Tonkov, Spassimir"],["dc.date.accessioned","2018-11-07T11:25:33Z"],["dc.date.available","2018-11-07T11:25:33Z"],["dc.date.issued","2009"],["dc.description.abstract","Pollen stratigraphies are the most spatially extensive data available for the reconstruction of past land-cover change. Detailed knowledge of past land-cover is becoming increasingly important to evaluate the present trends in, and drivers of, vegetation composition. The European Pollen Database (EPD) was established in the late 1980s and developed in the early 1990s to provide a structure for archiving, exchanging, and analysing Quaternary pollen data from Europe. It provides a forum for scientists to meet and engage in collaborative investigations or data analysis. In May 2007 several EPD support groups were developed to assist in the task of maintaining and updating the database. The mapping and data accuracy work group (MADCAP) aims to produce an atlas of past plant distributions as detected by pollen analyses in Europe, in order to meet the growing need for this data from palaeoecologists and the wider scientific community. Due to data handling problems in the past, a significant number of EPD datasets have errors. The initial task of the work group, therefore, was a systematic review of pollen sequences, in order to identify and correct errors. The EPD currently (January 2009) archives 1,032 pollen sequences, of which 668 have age-depth models that allow chronological comparison. Many errors have been identified and corrected, or flagged for users, most notably errors in the pollen count data. The application of spatial analyses to pollen data is related to the number of data points that are available for analysis. We therefore take this opportunity to encourage the submission of pollen analytical results to the EPD or other relevant pollen databases. Only in this way will the scientific community be able to gain a better understanding of past vegetation dynamics."],["dc.description.sponsorship","European Science Foundation EuroCLIMATE programme"],["dc.identifier.doi","10.1007/s00334-009-0215-9"],["dc.identifier.isi","000268729300005"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/3504"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/56646"],["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","The European Pollen Database: past efforts and current activities"],["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 WOS
  • 2010Journal Article
    [["dc.bibliographiccitation.firstpage","309"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","323"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Nielsen, Anne Birgitte"],["dc.contributor.author","Moller, Peter Friis"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Stavngaard, Beth"],["dc.contributor.author","Fontana, Sonia L."],["dc.contributor.author","Bradshaw, Richard H. W."],["dc.date.accessioned","2018-11-07T08:41:11Z"],["dc.date.available","2018-11-07T08:41:11Z"],["dc.date.issued","2010"],["dc.description.abstract","Since 1967 annual pollen deposition has been monitored in the semi-natural mixed deciduous woodland Draved Forest by the Geological Survey of Denmark. In this paper, we analyse the variability in pollen accumulation rates for the eight most common deciduous trees, and their relationships to monthly temperature and precipitation. High summer temperatures in the year before flowering have a positive effect on pollen deposition for several species. A positive correlation between temperatures during the flowering season and pollen accumulation rates is found for Fagus sylvatica, Quercus robur, Fraxinus excelsior and Corylus avellana. The amount of precipitation can have both positive and negative effects on pollen accumulation, depending on species and on time of year. Linear modelling showed that combinations of monthly climate parameters could explain between 10 and 80% of the variation observed in different species. There were marked differences in the time series of pollen accumulation and pollen/climate relationships for some species between traps within the forest related to the location of trees near the traps. This underlines the importance of using multiple traps in a region for this type of study. Time series analyses were used to test for cyclicity in pollen accumulation rates, which could be caused by resource limitations or internal biological factors. No significant autocorrelations were found, although Alnus glutinosa showed a tendency towards 3-year cyclicity. These results indicate that, with the possible exception of Alnus glutinosa, temperature and precipitation are the main factors controlling the annual variability in pollen deposition of the trees in Draved Forest."],["dc.description.sponsorship","Carlsberg Foundation; Danish Research Council; GEUS"],["dc.identifier.doi","10.1007/s00334-010-0253-3"],["dc.identifier.isi","000280825200006"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/4979"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19412"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1617-6278"],["dc.relation.issn","0939-6314"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","The effect of climate conditions on inter-annual flowering variability monitored by pollen traps below the canopy in Draved Forest, Denmark"],["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 WOS