Groos-Uffenorde, Helga

[["dc.bibliographiccitation.firstpage","3"],["dc.bibliographiccitation.journal","Palaeogeography, Palaeoclimatology, Palaeoecology"],["dc.bibliographiccitation.lastpage","22"],["dc.bibliographiccitation.volume","419"],["dc.contributor.author","Danielopol, Dan L."],["dc.contributor.author","Baltanás, Angel"],["dc.contributor.author","Carbonel, Pierre"],["dc.contributor.author","Colin, Jean-Paul"],["dc.contributor.author","Crasquin, Sylvie"],["dc.contributor.author","Decrouy, Laurent"],["dc.contributor.author","De Deckker, Patrick"],["dc.contributor.author","Gliozzi, Elsa"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Horne, David J."],["dc.contributor.author","Iepure, Sanda"],["dc.contributor.author","Keyser, Dietmar"],["dc.contributor.author","Kornicker, Louis S."],["dc.contributor.author","Lord, Alan"],["dc.contributor.author","Martens, Koen"],["dc.contributor.author","Matzke-Karasz, Renate"],["dc.contributor.author","Giles Miller, C."],["dc.contributor.author","Oertli, Henri J."],["dc.contributor.author","Pugliese, Nevio"],["dc.contributor.author","Russo, Antonio"],["dc.contributor.author","Sames, Benjamin"],["dc.contributor.author","Schön, Isa"],["dc.contributor.author","Siveter, David J."],["dc.contributor.author","Smith, Alison"],["dc.contributor.author","Viehberg, Finn A."],["dc.contributor.author","Wouters, Karel"],["dc.contributor.author","Yassini, Iradj"],["dc.date.accessioned","2018-08-17T12:34:08Z"],["dc.date.available","2018-08-17T12:34:08Z"],["dc.date.issued","2015"],["dc.description.abstract","he 1st International Symposium on Ostracoda (ISO) was held in Naples (1963). The philosophy behind this symposium and the logical outcome of what is now known as the International Research Group on Ostracoda (IRGO) are here reviewed, namely ostracodology over the last 50 years is sociologically analysed. Three different and important historic moments for the scientific achievements of this domain are recognised. The first one, between about 1963 and 1983, is related to applied research for the oil industry as well as to the great interest in the better description of the marine environment by both zoologists and palaeontologists. Another important aspect during this period was the work by researchers dealing with Palaeozoic ostracods, who had their own discussion group, IRGPO. Gradually, the merger of this latter group with those dealing with post-Palaeozoic ostracods at various meetings improved the communication between the two groups of specialists. A second period was approximately delineated between 1983 and 2003. During this time-slice, more emphasis was addressed to environmental research with topics such as the study of global events and long-term climate change. Ostracodologists profited also from the research “politics” within national and international programmes. Large international research teams emerged using new research methods. During the third period (2003–2013), communication and collaborative research reached a global dimension. Amongst the topics of research we cite the reconstruction of palaeoclimate using transfer functions, the building of large datasets of ostracod distributions for regional and intercontinental studies, and the implementation of actions that should lead to taxonomic harmonisation. Projects within which molecular biological techniques are routinely used, combined with sophisticated morphological information, expanded now in their importance. The documentation of the ostracod description improved through new techniques to visualise morphological details, which stimulated also communication between ostracodologists. Efforts of making available ostracod information through newsletters and electronic media are evoked."],["dc.identifier.doi","10.1016/j.palaeo.2014.08.016"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15393"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.relation.eissn","0031-0182"],["dc.title","From Naples 1963 to Rome 2013 — A brief review of how the International Research Group on Ostracoda (IRGO) developed as a social communication system"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","PalZ"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Schindler, Eberhard"],["dc.contributor.author","Becker, R. Thomas"],["dc.contributor.author","Dojen, Claudia"],["dc.contributor.author","Brocke, Rainer"],["dc.contributor.author","Jansen, Ulrich"],["dc.date.accessioned","2022-07-01T07:35:38Z"],["dc.date.available","2022-07-01T07:35:38Z"],["dc.date.issued","2022"],["dc.description.abstract","Abstract A new rich and diversified ostracode fauna from the Torkoz area (section Hassi Mouf South, Moroccan Anti-Atlas) is described and the ostracode distribution near the Early/Middle Devonian boundary is discussed. This ostracode fauna of a single limestone bed yields 32 taxa and is compared with the less-diversified ostracode fauna from an adjacent parallel section Hassi Mouf South as well as with a published conodont-bearing sample from section Torkoz. All three ostracode faunas are closely related, and therefore, the same latest Emsian age is postulated. Palynomorphs (acritarchs and prasinophytes) from section Torkoz support this late Early Devonian age and the scarce brachiopod fauna of the equivalent level from section Hassi Mouf South suggests a stratigraphical position very close to the Emsian/Eifelian boundary, probably latest Emsian. Zygobeyrichia subcylindrica from a thin marly bed embedded in shales, slightly below the ostracode-rich sample from section Hassi Mouf South, and the conodonts of the patulus Zone from section Torkoz, favours the position of the Early/Middle Devonian boundary within the Yeraifia Formation and not in or on top of the Rich 4 Sandstone in the SW Dra Valley area as hitherto published. The latest Early Devonian ostracode faunas from the Torkoz area belong to the shallow-water Eifelian Ecotype of G. Becker. The new genus Karlingrella for Euglyphella ? granulosa Blumenstengel, 1962 and the new species Quasillites ( Beckjennites ) gebeckeri are erected."],["dc.identifier.doi","10.1007/s12542-022-00603-z"],["dc.identifier.pii","603"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/112223"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-581"],["dc.relation.eissn","1867-6812"],["dc.relation.issn","0031-0220"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Late Early Devonian ostracodes from the Torkoz area (SW Morocco) and the Emsian/Eifelian boundary"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","613"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Palaeobiodiversity and Palaeoenvironments"],["dc.bibliographiccitation.lastpage","613"],["dc.bibliographiccitation.volume","98"],["dc.contributor.author","Nazik, Atike"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Olempska, Ewa"],["dc.contributor.author","Namık Yalçın, M."],["dc.contributor.author","Wilde, Volker"],["dc.contributor.author","Schindler, Eberhard"],["dc.contributor.author","Königshof, Peter"],["dc.contributor.author","Zor, Emine Şeker"],["dc.contributor.author","Wehrmann, Achim"],["dc.date.accessioned","2020-12-10T14:14:34Z"],["dc.date.available","2020-12-10T14:14:34Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1007/s12549-018-0364-x"],["dc.identifier.eissn","1867-1608"],["dc.identifier.issn","1867-1594"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/71390"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.iserratumof","/handle/2/71389"],["dc.title","Correction to: Late Silurian and Devonian ostracods of the Istanbul Zone (Western Pontides) and the Taurides: palaeogeographical implications"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","erratum_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","333"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Geobios"],["dc.bibliographiccitation.lastpage","348"],["dc.bibliographiccitation.volume","24"],["dc.contributor.author","Robardet, Michel"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Gandl, Josef"],["dc.contributor.author","Racheboeuf, Patrick R."],["dc.date.accessioned","2019-07-19T09:47:14Z"],["dc.date.available","2019-07-19T09:47:14Z"],["dc.date.issued","1991"],["dc.description.abstract","Les Trilobites et Ostracodes provenant de trois unités paléozoïques de la Zone d’Ossa-Morena (Sud de l’Espagne) apportent des précisions sur la stratigraphie du Dévonien inférieur (Praguien-Emsien inférieur) de cette région. La répartition géographique de ces fossiles confirme les affinités (au niveau spécifique) existant entre les faunes benthiques du Sud de l’Europe et du Nord de l’Afrique; en outre elle illustre l’uniformisation des faunes entre les régions nord-gondwaniennes et celles qui constituent la bordure sud du Continent des Vieux Grès Rouges. Les moules externes et internes des Ostracodes sont décrits. Ils montrent des relations avec les faunes néritiques de même âge en Europe; Cornikloedenina? meridiana nov. sp. se distingue par un lobe adductorial épineux. Des Ostracodes présentent l’ornementation en empreinte digitale caractéristique des Entomozoacea et deux groupes d’épines, l’un antéro-médian, l’autre antéro-ventral, ont été trouvés pour la première fois; ils sont décrits comme Morenozoe racheboeufi nov. gen., nov. sp. et leur position systématique est discutée."],["dc.description.abstract","Trilobites and Ostracodes from three paleozoic units of the Ossa-Morena Zone (southern Spain) bring complementary precisions about the stratigraphy of the Lower Devonian (Pragian-Lower Emsian) in this region. The geographic distribution of these fossils corroborates the affinities (at the species level) between south-central-European and north African benthic faunas; moreover it illustrates the faunal uniformization between north-gondwanan regions and the southern border of the Old Red Continent. The external and internal moulds of ostracodes are described. They show some relationship with beyrichiacean faunas of the same age in Europe, nevertheless Cornikloedenina? meridiana nov. sp. is differing both in lobation and ornamentation. The first fingerprint ostracode with a group of anterior and anteroventral spines is described as Morenozoe racheboeufi nov. gen., nov. sp. including a discussion of the relation to Entomozoacea and Thaumatocypridacea."],["dc.description.abstract","Aus drei paläozoischen Einheiten der südspanischen Ossa-Morena-Zone werden Trilobiten und Ostracoden bekannt gemacht, die Beziehungen zu benthonischen Faunen Mittel-Europas und Nord-Afrikas aufzeigen und damit die Gemeinsamkeiten der Faunen zwischen Nord -Gondwana und Süd-Rand des Qld-Red-Kontinents im Unter-Devon (Prag-und Unter-Ems-Stufe) bestätigen. Die Abdrücke und Steinkerne der Ostracoden gehören zum größten Teil zu den Beyrichiacea. Ein Teil von ihnen zeigt bisher unbekannte Ornamentierung und Lobierung und gibt Anlaß zur Abgrenzung von Cornikloedenina? meridiana nov. sp. Nur in einer Probe fanden sich wenige Exemplare einer Art, die außer der “fingerprint”-Skulptur erstmals auch 2 Gruppen deutlicher Randstacheln vorn und anteroventral zeigt. Da sie damit von allen bisher bekannten Arten abweicht, wird sie als Morenozoe racheboeufi nov. gen., nov. sp. beschrieben und werden die Beziehungen zu Entomozoacea und Thaumatocypridacea aufgezeigt."],["dc.identifier.doi","10.1016/S0016-6995(09)90013-4"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61771"],["dc.language.iso","fr"],["dc.relation.issn","0016-6995"],["dc.title","Trilobites et Ostracodes du Dévonien inférieur de la zone d’Ossa-Morena (Espagne)"],["dc.title.alternative","Lower Devonian Trilobites and Ostracodes from the Ossa-Morena zone (Spain)"],["dc.title.alternative","Unterdevonischen Trilobiten und Ostracoden aus dem Ossa-Morena-zone (Spanien)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","115"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Newsletters on Stratigraphy"],["dc.bibliographiccitation.lastpage","147"],["dc.bibliographiccitation.volume","2"],["dc.contributor.author","Carls, Peter"],["dc.contributor.author","Gandl, Josef"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Jahnke, Hans"],["dc.contributor.author","Walliser, Otto H."],["dc.date.accessioned","2019-07-19T09:54:39Z"],["dc.date.available","2019-07-19T09:54:39Z"],["dc.date.issued","1972"],["dc.description.abstract","Die Untersuchung der Vergesellschaftung rheinischer und hercyischer Faunen in Aragón ergab: (1) Die Grenze Zlichov-Kalk / Daleje-Schiefer (= Grenze Nowakia barrandei/ N. cancellata), bisher allgemein der Grenze Ems- / Eifel-Stufe gleichgesetzt, liegt wesentlich tiefer. Sie entspricht etwa der Grenze Unter- /Ober-Ems-Stufe. Die Zlichov-Stufe gehört also ganz in die Unter-Ems-Stufe. (2) Die N. barrandei-/N. cancellata-Grenze liegt innerhalb der Zone des Spathognathodus steinhornensis und nahe dem Übergang von Polygnathus linguiformis foveolatus zu P. linguiformis linguiformis. (3) Gyroceratites laevis kommt zusammen mit Sp. steinhornensis und N. cancellata vor. Die Grenze Gyroceratites laevis/ G. gracilis liegt innerhalb der Zone der N. cancellata. (4) Der Choteč-Kalk wird dem Günteröder Kalk plus Zwischenschichten am E-Rand des Rheinischen Schiefergebirges etwa gleichgestellt. Seine Basis lieg wesentlich tiefer als bisher allgemein angenommen."],["dc.description.abstract","Rhenish and hercynic faunas associating and alternating in the Devonian of Aragón reveal new correlations: (1) The boundary Zlichov Limestones/Daleje Shales in Bohemia (= boundary Nowakia barrandei / N. cancellata), commonly identified with the Emsian /Eifelian stage boundary, is much older: cose to the Lower/Upper Emsian boundary. The entire Zlichovian is part of the late Lower Emsian. (2) The boundary N. barrandei /N. cancellata lies within the zone of Spathognathodus steinhornensis and close to the transition of Polygnathus linguiformis foveolatus to P. l. linguiformis. (3) Gyroceratites laevis occurs together with Sp. steinhornensis and N. cancellata. The boundary G. laevis/G. gracilis is within the zone of N. cancellata. (4) The Choteč Limestone of Bohemia is correlated closely with Günterod Limestone plus Zwischenschichten in Germany. Its base is considerably older than previously supposed."],["dc.description.abstract","Faunas rhenanas y hercínicas se asocian e intercambian en el Devónico de Aragón y facilitan nuevas correlaciones: (1) El límite Calizas de Zlichov / Pizarras de Daleje en Bohemia (= límite Nowakia barrandei / N. cancellata) que se identificaba con el límite de los pisos Emsiense y Eifeliense, corresponde aproximadamente al límite Emsiense Inferior /Superior. Todo el Zlichoviense pertenece al Emsiense Inferior. (2) El limite N. barrandei / N. cancellata está dentro de la biozona de Spathognathodus steinhornensis y próximo a la transición de Polygnathus linguiformis foveolatus a P. l. linguiformis. (3) Gyroceratites laevis se asocia a Sp. steinhornensis y N. cancellata. El límite G. laevis /G. gracilis está dentro de la biozona de N. cancellata. (4) La Caliza de Choteč en Bohemia, que se databa como Eifeliense superior, se relaciona con la serie de Caliza de Günterod y Zwischenschichten en Alemania. Su base es bastante inferior a lo supuesto hasta ahora."],["dc.identifier.doi","10.1127/nos/2/1972/115"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61772"],["dc.language.iso","de"],["dc.relation.issn","0078-0421"],["dc.title","Neue Daten zur Grenze Unter-/ Mittel-Devon"],["dc.title.alternative","New data about the Lower-/Middle Devonian boundary"],["dc.title.subtitle","Neue Daten zur Grenze Unter-/ Mittel-Devon"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","201"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","TURKISH JOURNAL OF EARTH SCIENCES"],["dc.bibliographiccitation.lastpage","226"],["dc.bibliographiccitation.volume","25"],["dc.contributor.author","Nazik, Atike"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.date.accessioned","2018-08-17T12:15:13Z"],["dc.date.available","2018-08-17T12:15:13Z"],["dc.date.issued","2016"],["dc.description.abstract","Recently found materials of large beyrichiacean ostracodes from the Early Devonian of the Darlık, Korucuköy, and Kabalakdere sections in NW Anatolia stimulated the restudy of ostracode collections from the İstanbul area, including the Toula collection (GBA Vienna) and Endriss collection (previously in GPI Marburg and currently in SMF Frankfurt), and their biostratigraphical and palaeogeographical significance. The species Gibba kayseri, Gibba schmidti, Zygobeyrichia roemeri, Zygobeyrichia subcylindrica, and Zygobeyrichia onusta are documented and beyrichiid gen. et sp. indet. is described. There are great similarities with ostracode faunas from Early Devonian shallow-water sediments of Europe and North Africa (in Germany from the Rhenish Schiefergebirge to Thuringia, northern France, Spain, Poland, Bohemia, Podolia, Moravia, and North-West Africa). Therefore, this distribution questions the presence of a deeper and wider Rheic Ocean, which would be difficult for shallow-water benthic organisms to cross."],["dc.identifier.doi","10.3906/yer-1505-18"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15391"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.relation.eissn","1300-0985"],["dc.relation.eissn","1303-619X"],["dc.title","Notes on beyrichiacean ostracodes from the Early Devonian of NW Turkey andtheir palaeobiogeographical relations"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","275"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Lethaia"],["dc.bibliographiccitation.lastpage","275"],["dc.bibliographiccitation.volume","13"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.date.accessioned","2019-07-19T09:56:56Z"],["dc.date.available","2019-07-19T09:56:56Z"],["dc.date.issued","1980"],["dc.identifier.doi","10.1111/j.1502-3931.1980.tb00642.x"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61773"],["dc.language.iso","de"],["dc.relation.issn","0024-1164"],["dc.relation.issn","1502-3931"],["dc.title","International Research Group on Palaeozoic Ostracoda"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","101"],["dc.bibliographiccitation.lastpage","112"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Schindler, Eberhard"],["dc.date.accessioned","2019-07-19T09:43:29Z"],["dc.date.available","2019-07-19T09:43:29Z"],["dc.date.issued","2011"],["dc.identifier.doi","10.1007/978-94-009-1838-2_7"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61770"],["dc.language.iso","en"],["dc.publisher","Springer"],["dc.relation.isbn","978-94-010-7320-2"],["dc.relation.isbn","978-94-009-1838-2"],["dc.relation.ispartof","Ostracoda and Global Events"],["dc.title","The effect of global events on entomozoacean Ostracoda"],["dc.type","book_chapter"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","593"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Palaeobiodiversity and Palaeoenvironments"],["dc.bibliographiccitation.lastpage","612"],["dc.bibliographiccitation.volume","98"],["dc.contributor.author","Nazik, Atike"],["dc.contributor.author","Groos-Uffenorde, Helga"],["dc.contributor.author","Olempska, Ewa"],["dc.contributor.author","Yalçın, M. Namık"],["dc.contributor.author","Wilde, Volker"],["dc.contributor.author","Schindler, Eberhard"],["dc.contributor.author","Königshof, Peter"],["dc.contributor.author","Zor, Emine Şeker"],["dc.contributor.author","Wehrmann, Achim"],["dc.date.accessioned","2020-12-10T14:14:33Z"],["dc.date.available","2020-12-10T14:14:33Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1007/s12549-018-0340-5"],["dc.identifier.eissn","1867-1608"],["dc.identifier.issn","1867-1594"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/71389"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.haserratum","/handle/2/71390"],["dc.title","Late Silurian and Devonian ostracods of the Istanbul Zone (Western Pontides) and the Taurides: palaeogeographical implications"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]