Seyfullah, Leyla J.

[["dc.bibliographiccitation.firstpage","365"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Papers in Palaeontology"],["dc.bibliographiccitation.lastpage","389"],["dc.bibliographiccitation.volume","5"],["dc.contributor.author","Kettunen, Elina"],["dc.contributor.author","Sadowski, Eva-Maria"],["dc.contributor.author","Seyfullah, Leyla J."],["dc.contributor.author","Dörfelt, Heinrich"],["dc.contributor.author","Rikkinen, Jouko"],["dc.contributor.author","Schmidt, Alexander R."],["dc.contributor.editor","Lomax, Barry"],["dc.date.accessioned","2020-12-10T14:07:15Z"],["dc.date.available","2020-12-10T14:07:15Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1002/spp2.1238"],["dc.identifier.issn","2056-2802"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/70155"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Caspary's fungi from Baltic amber: historic specimens and new evidence"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","386"],["dc.bibliographiccitation.journal","Molecular Phylogenetics and Evolution"],["dc.bibliographiccitation.lastpage","398"],["dc.bibliographiccitation.volume","78"],["dc.contributor.author","Beimforde, Christina"],["dc.contributor.author","Feldberg, Kathrin"],["dc.contributor.author","Nylinder, Stephan"],["dc.contributor.author","Rikkinen, Jouko"],["dc.contributor.author","Tuovila, Hanna"],["dc.contributor.author","Dörfelt, Heinrich"],["dc.contributor.author","Gube, Matthias"],["dc.contributor.author","Jackson, Daniel J."],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Seyfullah, Leyla J."],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2018-11-07T09:35:47Z"],["dc.date.available","2018-11-07T09:35:47Z"],["dc.date.issued","2014"],["dc.description.abstract","The phylum Ascomycota is by far the largest group in the fungal kingdom. Ecologically important mutualistic associations such as mycorrhizae and lichens have evolved in this group, which are regarded as key innovations that supported the evolution of land plants. Only a few attempts have been made to date the origin of Ascomycota lineages by using molecular clock methods, which is primarily due to the lack of satisfactory fossil calibration data. For this reason we have evaluated all of the oldest available ascomycete fossils from amber (Albian to Miocene) and chert (Devonian and Maastrichtian). The fossils represent five major ascomycete classes (Coniocybomycetes, Dothideomycetes, Eurotiomycetes, Laboulbeniomycetes, and Lecanoromycetes). We have assembled a multi-gene data set (18SrDNA, 28SrDNA, RPB1 and RPB2) from a total of 145 taxa representing most groups of the Ascomycota and utilized fossil calibration points solely from within the ascomycetes to estimate divergence times of Ascomycota lineages with a Bayesian approach. Our results suggest an initial diversification of the Pezizomycotina in the Ordovician, followed by repeated splits of lineages throughout the Phanerozoic, and indicate that this continuous diversification was unaffected by mass extinctions. We suggest that the ecological diversity within each lineage ensured that at least some taxa of each group were able to survive global crises and rapidly recovered. (C) 2014 The Authors. Published by Elsevier Inc."],["dc.description.sponsorship","German Excellence Initiative"],["dc.identifier.doi","10.1016/j.ympev.2014.04.024"],["dc.identifier.isi","000342480400034"],["dc.identifier.pmid","24792086"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11370"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/32467"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.notes.submitter","Najko"],["dc.relation.issn","1095-9513"],["dc.relation.issn","1055-7903"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY-NC-ND 3.0"],["dc.rights.uri","http://creativecommons.org/licenses/by-nc-nd/3.0/"],["dc.title","Estimating the Phanerozoic history of the Ascomycota lineages: Combining fossil and molecular data"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","53"],["dc.bibliographiccitation.journal","Review of Palaeobotany and Palynology"],["dc.bibliographiccitation.lastpage","64"],["dc.bibliographiccitation.volume","200"],["dc.contributor.author","Schmidt, Alexander R."],["dc.contributor.author","Beimforde, Christina"],["dc.contributor.author","Seyfullah, Leyla J."],["dc.contributor.author","Wege, Sarah-Elena"],["dc.contributor.author","Dörfelt, Heinrich"],["dc.contributor.author","Girard, Vincent"],["dc.contributor.author","Grabenhorst, Heinrich"],["dc.contributor.author","Gube, Matthias"],["dc.contributor.author","Heinrichs, Jochen"],["dc.contributor.author","Nel, André"],["dc.contributor.author","Nel, Patricia"],["dc.contributor.author","Perrichot, Vincent"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Rikkinen, Jouko"],["dc.date.accessioned","2018-08-14T13:50:06Z"],["dc.date.available","2018-08-14T13:50:06Z"],["dc.date.issued","2014"],["dc.description.abstract","Sooty moulds are saprophytic ascomycetes with brown hyphae, often forming extensive subicula on living plant surfaces. These fungi grow on plant exudates and honeydew secreted by sap sucking insects and are ubiquitous in many humid terrestrial ecosystems. Here, we review previously published specimens of sooty moulds and provide new fossil evidence that traces the fossil record of these fungi for about 100 million years, from the early Miocene (17 million years) to the Early Cretaceous (Albian, about 100 to 113 million years). Investigation of Mesozoic and Cenozoic ambers from different parts of the world revealed sooty moulds from eight northern hemisphere amber deposits. Fragments of superficial subicula composed of smooth brown moniliform hyphae with tapering distal ends identical to those produced by extant species in the family Metacapnodiaceae (Capnodiales) are recorded since the Albian. The fossil fungi originate from tropical to temperate coastal forests where they grew on leaves and bark of different conifer and angiosperm trees. This indicates that capnodialean sooty moulds have occupied their specialized niche since at least from when early angiosperms appeared in the fossil record."],["dc.identifier.doi","10.1016/j.revpalbo.2013.07.002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15286"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.relation.eissn","0034-6667"],["dc.title","Amber fossils of sooty moulds"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","85"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Fossil Record"],["dc.bibliographiccitation.lastpage","89"],["dc.bibliographiccitation.volume","15"],["dc.contributor.author","Kiecksee, Anna Philie"],["dc.contributor.author","Seyfullah, Leyla J."],["dc.contributor.author","Dörfelt, Heinrich"],["dc.contributor.author","Heinrichs, Jochen"],["dc.contributor.author","Süß, Herbert"],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2018-11-07T09:07:47Z"],["dc.date.available","2018-11-07T09:07:47Z"],["dc.date.issued","2012"],["dc.description.abstract","Agaricomycetes are major components of extant terrestrial ecosystems; however, their fruiting bodies are exceedingly rare as fossils. Reinvestigation of a peculiar fossil from Late Triassic sediments of southern Germany interpreted as a bracket fungus revealed that this fossil in fact represents a wood abnormality, resulting from injury to the cambium and subsequent callus growth in a Baieroxylon -like ginkgoalean wood. As a result, the fossil record of the Agaricomycetes does not yet pre-date the Early Cretaceous, suggesting a late diversification of basidiomycetes possessing large fruiting bodies. ((c) 2012 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim)"],["dc.identifier.doi","10.1002/mmng.201200006"],["dc.identifier.isi","000307107700004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25882"],["dc.language.iso","en"],["dc.notes.status","final"],["dc.notes.submitter","Najko"],["dc.relation.issn","1435-1943"],["dc.title","Pre-Cretaceous Agaricomycetes yet to be discovered: Reinvestigation of a putative Triassic bracket fungus from southern Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]