Pint, Anna

[["dc.bibliographiccitation.firstpage","167"],["dc.bibliographiccitation.journal","Quaternary Science Reviews"],["dc.bibliographiccitation.lastpage","187"],["dc.bibliographiccitation.volume","149"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Seeliger, Martin"],["dc.contributor.author","Feuser, Stefan"],["dc.contributor.author","Novenko, Elena"],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Pint, Anna"],["dc.contributor.author","Pirson, Felix"],["dc.contributor.author","Brueckner, Helmut"],["dc.date.accessioned","2018-11-07T10:08:09Z"],["dc.date.available","2018-11-07T10:08:09Z"],["dc.date.issued","2016"],["dc.description.abstract","Elaia, the harbour city for ancient Pergamon (western Turkey), was investigated using geoarchaeological methods. The rise and fall of Elaia were closely linked to the flourishing period of Pergamon, which ruled wide parts of today's western Turkey in Hellenistic times. In the framework of this research, the palynological analysis of a 9 m sediment core, Ela-70, retrieved from the enclosed harbour of the city, was carried out to reconstruct the vegetation and environmental history of the wider Gulf of Elaia region. An age-depth model, based on 11 calibrated radiocarbon ages, starting from 7.5 ka BP, provides the basis for the high resolution study of sediments from the Hellenistic period, as well as before and after. The lower part of the pollen diagram is characterised by high percentages of deciduous oaks and pines, suggesting the dominance of open forests close to the coring site. The change from oak forests to a cultural landscape, with olive, pistachio, walnut, and grape, started around 850 BC, reaching a maximum ca. 250 BC, and continuing to ca. AD 800. This period is characterised by increase of fire activity, soil erosion intensity, and pastoral farming. Such long-lasting intensive land use likely led to the climax ecosystem turnover from open deciduous oak forests to pine stands, while salt marshes developed around the coring site. The discovery of the dinoflagellate cysts of Peridinium ponticum, a Black Sea endemic species, in the harbour of Elaia evidences maritime trade between the Aegean Sea and the Black Sea; its first occurrence coincides with the time of the Mithridatic Wars (1st century BC). In conclusion, palynological data, in addition to historical and archaeological records, provide a deeper insight into human environmental interactions, as derived from the geoarchaeological archive of the harbour of Elaia. (C) 2016 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.quascirev.2016.07.014"],["dc.identifier.isi","000383825400011"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/39415"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0277-3791"],["dc.title","The harbour of Elaia: A palynological archive for human environmental interactions during the last 7500 years"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Geoarchaeology"],["dc.contributor.author","May, Simon M."],["dc.contributor.author","Norpoth, Maike"],["dc.contributor.author","Pint, Anna"],["dc.contributor.author","Shumilovskikh, Lyudmila"],["dc.contributor.author","Raith, Kira"],["dc.contributor.author","Brill, Dominik"],["dc.contributor.author","Rixhon, Gilles"],["dc.contributor.author","Moret, Pierre"],["dc.contributor.author","Jiménez‐Vialás, Helena"],["dc.contributor.author","Grau‐Mira, Ignasi"],["dc.contributor.author","García‐Jiménez, Iván"],["dc.contributor.author","Marzoli, Dirce"],["dc.contributor.author","León‐Martín, César"],["dc.contributor.author","Reicherter, Klaus"],["dc.contributor.author","Brückner, Helmut"],["dc.date.accessioned","2021-04-14T08:29:25Z"],["dc.date.available","2021-04-14T08:29:25Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1002/gea.21846"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/82897"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1520-6548"],["dc.relation.issn","0883-6353"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Mid‐ to late Holocene environmental changes and human‐environment interactions in the surroundings of La Silla del Papa, SW Spain"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","71"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Journal of Quaternary Science"],["dc.bibliographiccitation.lastpage","85"],["dc.bibliographiccitation.volume","37"],["dc.contributor.affiliation","Bungenstock, Friederike; 2Lower Saxony Institute for Historical Coastal Research\r\nWilhelmshaven Germany"],["dc.contributor.affiliation","Haynert, Kristin; 3Marine Research Department\r\nSenckenberg am Meer\r\nWilhelmshaven Germany"],["dc.contributor.affiliation","Pint, Anna; 1\r\nInstitute of Geography, University of Cologne\r\nKöln Germany"],["dc.contributor.affiliation","Schlütz, Frank; 2Lower Saxony Institute for Historical Coastal Research\r\nWilhelmshaven Germany"],["dc.contributor.affiliation","Frenzel, Peter; 5\r\nInstitute of Geosciences, Friedrich Schiller University Jena\r\nJena Germany"],["dc.contributor.affiliation","Wehrmann, Achim; 3Marine Research Department\r\nSenckenberg am Meer\r\nWilhelmshaven Germany"],["dc.contributor.affiliation","Brückner, Helmut; 1\r\nInstitute of Geography, University of Cologne\r\nKöln Germany"],["dc.contributor.affiliation","Engel, Max; 6\r\nInstitute of Geography, Heidelberg University\r\nHeidelberg Germany"],["dc.contributor.author","Scheder, Juliane"],["dc.contributor.author","Bungenstock, Friederike"],["dc.contributor.author","Haynert, Kristin"],["dc.contributor.author","Pint, Anna"],["dc.contributor.author","Schlütz, Frank"],["dc.contributor.author","Frenzel, Peter"],["dc.contributor.author","Wehrmann, Achim"],["dc.contributor.author","Brückner, Helmut"],["dc.contributor.author","Engel, Max"],["dc.date.accessioned","2021-12-01T09:23:22Z"],["dc.date.available","2021-12-01T09:23:22Z"],["dc.date.issued","2021"],["dc.date.updated","2022-03-21T11:02:49Z"],["dc.description.abstract","ABSTRACT In light of global warming and rising relative sea level (RSL), detailed reconstructions of RSL histories and their controlling processes are essential in order to manage coastal‐protection challenges. This study contributes to unravelling Holocene RSL change on the East Frisian North Sea coast in high resolution and with a new approach for the German Bight. For the first time, a transfer function (vertical error: 29.7 cm ≙ ~11% of the mean tidal range) for RSL change based on a combined training set of benthic foraminifers and ostracods from the back‐barrier tidal basin of Spiekeroog is applied to the Holocene record of the back‐barrier tidal basin of Norderney. The resulting RSL curve for the Norderney tidal basin is corrected for decompaction and shows a deceleration in RSL rise between 6000 and 5000 cal bp. The smallest possible error envelope (~1 m) results from the good suitability of salt‐marsh layers between 5000 and 4000 cal bp. The RSL curve provides an approach towards the closure of the common data gap of peat‐based curves for the southern North Sea related to a lack of basal peats in the youngest age range, and verifies regional differences in glacial isostatic adjustment."],["dc.description.sponsorship","Volkswagen Foundation http://dx.doi.org/10.13039/501100001663"],["dc.description.sponsorship","Niedersächsisches Ministerium für Wissenschaft und Kultur http://dx.doi.org/10.13039/501100010570"],["dc.identifier.doi","10.1002/jqs.3380"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/94632"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-478"],["dc.relation.eissn","1099-1417"],["dc.relation.issn","0267-8179"],["dc.rights","This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made."],["dc.rights.uri","http://creativecommons.org/licenses/by-nc-nd/4.0/"],["dc.title","Insights into Holocene relative sea‐level changes in the southern North Sea using an improved microfauna‐based transfer function"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]