[["dc.bibliographiccitation.firstpage","391"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Bibliotheksdienst"],["dc.bibliographiccitation.lastpage","405"],["dc.bibliographiccitation.volume","52"],["dc.contributor.affiliation","Achterberg, Inke;"],["dc.contributor.affiliation","Bertelmann, Roland;"],["dc.contributor.affiliation","Elger, Kirsten;"],["dc.contributor.affiliation","Hübner, Andreas;"],["dc.contributor.affiliation","Pfurr, Norbert;"],["dc.contributor.affiliation","Schüler, Mechthild;"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Bertelmann, Roland"],["dc.contributor.author","Elger, Kirsten"],["dc.contributor.author","Hübner, Andreas"],["dc.contributor.author","Pfurr, Norbert"],["dc.contributor.author","Schüler, Mechthild"],["dc.date.accessioned","2022-11-28T11:11:16Z"],["dc.date.available","2022-11-28T11:11:16Z"],["dc.date.issued","2018-04-04"],["dc.date.updated","2022-11-27T10:28:37Z"],["dc.description.abstract","Der Fachinformationsdienst Geowissenschaften der festen Erde (FID GEO), betrieben durch die Niedersächsische Staats- und Universitätsbibliothek (SUB) Göttingen und die Bibliothek des Wissenschaftsparks Albert Einstein am GeoForschungsZentrum (GFZ) Potsdam, entwickelt diverse Angebote in den Bereichen E-Publizieren, Forschungsdaten und Digitalisierung. Auf der Homepage www.fidgeo.de sind die Services zusammengestellt. Auf dem Publikationsserver des FID GEO, GEO-LEOe-docs, werden Inhalte dauerhaft frei zugänglich angeboten. Für die Publikation von Forschungsdaten über den FID GEO steht das Repositorium GFZ Data Services zur Verfügung. FID GEO kooperiert eng mit den geowissenschaftlichen Fachgesellschaften."],["dc.description.abstract","The Specialised Information Service for Solid Earth Geosciences (FID GEO), run by the Göttingen State and University Library and the Bibliothek des Wissenschaftsparks Albert Einstein at the GFZ German Research Centre for Geosciences Potsdam, offers services for E-publishing, research data publishing, and digitisation. All services are presented on the website www.fidgeo.de. Texts and maps are permanently accessible on the repository GEO-LEOe-docs; research data are published in cooperation with GFZ Data Services. FID GEO cooperates closely with learned societies."],["dc.identifier.doi","10.1515/bd-2018-0045"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/117653"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.publisher","De Gruyter"],["dc.relation","Fachinformationsdienst Geowissenschaften"],["dc.relation.eissn","2194-9646"],["dc.relation.issn","0006-1972"],["dc.title","Der Fachinformationsdienst Geowissenschaften der festen Erde (FID GEO):"],["dc.title.alternative","The Specialised Information Service for Solid Earth Geosciences (FID GEO): Promoting digital transformation and Open Access in geoscience"],["dc.title.subtitle","The Specialised Information Service for Solid Earth Geosciences (FID GEO):"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","171"],["dc.bibliographiccitation.journal","Review of Palaeobotany and Palynology"],["dc.bibliographiccitation.lastpage","178"],["dc.bibliographiccitation.volume","221"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Kvitkina, Anna"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.date.accessioned","2018-11-07T09:51:12Z"],["dc.date.available","2018-11-07T09:51:12Z"],["dc.date.issued","2015"],["dc.description.abstract","Several laboratory experiments and field observations demonstrate that saprotrophic and ectomycorrhizal fungi effectively use pollen cytoplasm and suggest pollen produced by wind-pollinated trees as a crucial nutrient source for fungi and their plant hosts in nutrient-limited environments. However, the role of such interactions is still underestimated or neglected in ecology and paleoecology. Here, we consider pollen attacked by fungi in palynological records from Holocene raised peat bogs as a nutrient source for ecosystems in the past. The attacks occurred through the pollen germination areas by a variety of saprotrophic, ericoid mycorrhizal, ectomycorrhizal or dark septate endophyte fungi. Large amounts of attacked pollen in phases rich in Calluna vulgaris highlight the importance of Ericaceae shrubs, hosting ericoid mycorrhizal fungi and forming hotspots of decomposition in nutrient-deficit bogs. Applying estimations of pollen rain from literature, and based on own observed pollen infection rates we estimate the annual release of nitrogen, phosphate and potassium from pollen, and highlight their significance in pushing the ecosystem nutrient cycle in early spring time, when several species release their pollen. We highlight the significant role of anthropogenic changes in pollen deposition for pre-industrial bogs and hypothesize about the consequences of the pollen-based interrelation between wind-pollinated plants and their mycorrhizal fungi in paleoecology and evolution. (C) 2015 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.revpalbo.2015.07.001"],["dc.identifier.isi","000361777900016"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/35867"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1879-0615"],["dc.relation.issn","0034-6667"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Pollen as nutrient source in Holocene ombrotrophic bogs"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","19"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Interdisciplinaria Archaeologica"],["dc.bibliographiccitation.lastpage","29"],["dc.bibliographiccitation.volume","6"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Metzler, Alf"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.date.accessioned","2019-07-10T08:12:04Z"],["dc.date.available","2019-07-10T08:12:04Z"],["dc.date.issued","2015"],["dc.description.abstract","Tree rings provide not only a precise dating tool, but also contain information on environmental change. The well replicated tree ring record of northwest Germany therefore provides environmental implications with immanent, absolute and precise dating from 6703 BC to 931 AD. This offers the opportunity to investigate the environmental context of archaeological finds, if they, too, are dated by dendrochronology. We investigated 13 peat-preserved trackways from the Northwest-German lowland between 4629 BC (Neolithic) and 502 AD (Migration Period) for contemporaneousness with water table rise in the landscape. Such environmental change is well reflected in the clearly notable die-off phases of trees preserved in the mires. As an environmental proxy, the parameter “tree die-off rate a-30” is introduced: The annual number of tree die-off events is divided by the number of live trees 30 years previously. Overall, the majority of trackway constructions were found to be contemporaneous to mire water table rise and mire expansion. Possibly, a period of water table rise was a motivation for trackway construction."],["dc.identifier.doi","10.24916/iansa.2015.1.2"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14522"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60854"],["dc.identifier.url","http://iansa.eu/papers/IANSA-2015-01-achterberg.html"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.relation.doi","10.24916/iansa.2015.1.2"],["dc.relation.issn","2336-1220"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.rights","CC BY 4.0"],["dc.rights.access","openAccess"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.subject","wooden trackways; dendrochronology; mire; environmental change; Holocene climate; Neolithic"],["dc.subject.ddc","570"],["dc.title","Contemporaneousness of Trackway Construction and Environmental Change: a Dendrochronological Study in Northwest-German Mires"],["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"]]

[["dc.bibliographiccitation.firstpage","5"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Studia Quaternaria"],["dc.bibliographiccitation.lastpage","18"],["dc.bibliographiccitation.volume","32"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Schlütz, Frank"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.date.accessioned","2019-07-09T11:43:25Z"],["dc.date.available","2019-07-09T11:43:25Z"],["dc.date.issued","2015"],["dc.description.abstract","In order to reconstruct regional vegetation changes and local conditions during the fen-bog transition in the Borsteler Moor (north western Germany), a sediment core covering the period between 7.1 and 4.5 cal kyrs BP was palynologically investigated. The pollen diagram demonstrates the dominance of oak forests and a gradual replacement of trees by raised bog vegetation with the wetter conditions in the Late Atlantic. At ~ 6 cal kyrs BP, the non-pollen palynomorphs (NPP) demonstrate the succession from mesotrophic conditions, clearly indicated by a number of fungal spore types, to oligotrophic conditions, indicated by Sphagnum spores, Bryophytomyces sphagni, and testate amoebae Amphitrema, Assulina and Arcella, etc. Four relatively dry phases during the transition from fen to bog are clearly indicated by the dominance of Calluna and associated fungi as well as by the in crease of microcharcoal. Several new NPP types are described and known NPP types are identified. All NPP are dis cussed in the context of their palaeoecological indicator values."],["dc.identifier.doi","10.1515/squa-2015-0001"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14523"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58884"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","2300-0384"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject.ddc","570"],["dc.title","Non-Pollen Palynomorphs from Mid-Holocene Peat of the Raised Bog Borsteler Moor (Lower Saxony, Germany)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","85"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Climate of the Past"],["dc.bibliographiccitation.lastpage","100"],["dc.bibliographiccitation.volume","14"],["dc.contributor.author","Achterberg, Inke Elisabeth Maike"],["dc.contributor.author","Eckstein, Jan"],["dc.contributor.author","Birkholz, Bernhard"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.date.accessioned","2018-06-19T13:34:06Z"],["dc.date.available","2018-06-19T13:34:06Z"],["dc.date.issued","2018"],["dc.description.abstract","The investigated northwest German mire site at \"Totes Moor\" is densely covered with subfossil pine stumps (Pinus sylvestris L.) from the fen–bog transition. This facilitates the spatio-temporal reconstruction of mire development, which is based on 212 in situ tree stumps in the case study presented here. Six dendrochronologically dated site chronologies together cover 2345 years between 6703 and 3403 BC. The gaps in between are 6 to 550 years long. Additionally, a floating chronology of 309 years, containing 30 trees, was radiocarbon-dated to the beginning of the 7th millennium cal BC. Peat-stratigraphical survey was carried out additionally, and elevations a.s.l. were determined at several locations. Tree dying-off phases, which indicate water level rise at the site, mostly in context of the local fen–bog transition, are evident for ca. 6600–6450, ca. 6350–5750, ca. 5300–4900, ca. 4700–4550, ca. 3900–3850, ca. 3700–3600, ca. 3500–3450 and ca. 3400 BC. The spatial distribution of the dated in situ trees illustrates the phase-wise expansion of raised bog over fen peat at the site. The documented bog expansion pulses likely correspond to climatic wet sifts."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2018"],["dc.identifier.doi","10.5194/cp-14-85-2018"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/15189"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15121"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.rights","CC BY 3.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/3.0"],["dc.title","Dendrochronologically dated pine stumps document phase-wise bog expansion at a northwest German site between ca. 6700 and ca. 3400 BC"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","643"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.lastpage","650"],["dc.bibliographiccitation.volumetitle","2200 BC – Ein Klimasturz als Ursache für den Zerfall der Alten Welt? 2200 BC – A climatic breakdown as a cause for the collapse of the old world?"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.contributor.editor","Meller, Harald"],["dc.contributor.editor","Arz, Helge Wolfgang"],["dc.contributor.editor","Jung, Reinhard"],["dc.contributor.editor","Risch, Roberto"],["dc.date.accessioned","2022-01-28T08:33:09Z"],["dc.date.available","2022-01-28T08:33:09Z"],["dc.date.issued","2015"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/98711"],["dc.language.iso","en"],["dc.publisher","Landesamt für Denkmalpflege und Archäologie Sachsen-Anhalt – Landesmuseum für Vorgeschichte Halle (Saale)"],["dc.relation.conference","7. Mitteldeutscher Archäologentag"],["dc.relation.eventend","2014-10-26"],["dc.relation.eventlocation","Halle (Saale)"],["dc.relation.eventstart","2014-10-23"],["dc.relation.isbn","978-3-944507-29-3"],["dc.relation.ispartof","2200 BC – Ein Klimasturz als Ursache für den Zerfall der Alten Welt? 2200 BC – A climatic breakdown as a cause for the collapse of the old world?"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Evidence for climate change between 2200 BC and 2160 BC derived from subfossil bog and riverine trees from Germany"],["dc.type","conference_paper"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","9"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Gesellschaft für Geowissenschaften"],["dc.bibliographiccitation.lastpage","19"],["dc.bibliographiccitation.volume","168"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Frechen, Manfred"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Eckstein, Jan"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.date.accessioned","2018-11-07T10:26:50Z"],["dc.date.available","2018-11-07T10:26:50Z"],["dc.date.issued","2017"],["dc.description.abstract","To date, the tree-ring chronology of peat-preserved pines from Northwest Germany (Fig. 1) spans from 6703 BC to 1166 BC, but still contains two gaps. It was dated with the help of the previously constructed bog-oak chronology of Northwest Germany, the older part of which in turn has been dated using the pine chronology (Fig. 2), now covering from 6628 to 6178 BC additional to the previous span of 6069 BC to 931 AD. Compared to the oaks, chronology construction required large numbers of samples of the short-lived pine trees, many of which remained undated or dated relatively only. The dendrochronological process, which at times delivered a multitude of floating chronology fragments, was complemented by a number of radiocarbon dates. Preceding and following the calendar-dated pine chronology, there are radiocarbon dated floating chronologies. This pine record partly dates back to the beginning of the 9th millennium BC and documents environmental conditions during the early Holocene. It also shows the potential of the chronology to be extended further into the past. The Northwest German pine chronology has since been the base for dating i.a. archaeological finds, such as Neolithic wooden bog trackways. Moreover, the peat-preserved pines have proved to be valuable in palaeoenvironmental research, as they grew at sites where they were sensitive to hydrological changes. Particularly the climate-related advances of raised bog are well reflected in the material."],["dc.description.sponsorship","German Research Foundation DFG [LE 1805/1-2, FR877/16-1, HA4438/1]"],["dc.identifier.doi","10.1127/zdgg/2016/0042"],["dc.identifier.isi","000397029000003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/43126"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.relation.issn","1860-1804"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","The Gottingen tree-ring chronologies of peat-preserved oaks and pines from Northwest Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]