Schmidt, Alexander R.

[["dc.bibliographiccitation.firstpage","203"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Earth and Planetary Science Letters"],["dc.bibliographiccitation.lastpage","213"],["dc.bibliographiccitation.volume","273"],["dc.contributor.author","Schmidt, Alexander"],["dc.contributor.author","Weyer, Stefan"],["dc.contributor.author","Mezger, Klaus"],["dc.contributor.author","Scherer, Erik E."],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Brey, Gerhard P."],["dc.date.accessioned","2018-11-07T11:11:59Z"],["dc.date.available","2018-11-07T11:11:59Z"],["dc.date.issued","2008"],["dc.description.abstract","The Qinling-Dabie-Sulu orogenic belt in eastern China is one of the largest ultrahigh-pressure (UHP) terranes worldwide. Mineral Sm-Nd- and zircon U-Pb dating has been widely used to reveal the metamorphic history of this collisional orogen. However, the exact timing of the UHP metamorphic event(s) remains controversial and ages ranging from 245 Ma to 220 Ma have been suggested. We present high precision garnet-cpx Lu-Hf ages for six eclogites from the Dabie and Sulu areas. All ages fall in a narrow range between 219.6 and 224.4 Ma. Five samples define a mean age of 223.0 +/- 0.9 Ma and one sample yields a slightly younger age of 219.6 +/- 1.4 Ma. This very tight age range is particularly remarkable considering the large regional distribution of sample localities (on the order of 100 km at the time of UHP metamorphism) and the wide variety of garnet and eclogite chemical compositions represented. Two samples yield Sm-Nd ages that are indistinguishable from their Lu-Hf ages, albeit with larger uncertainties. The identical ages of eclogites from both the Dabie and the Sulu region emphasize their close genetic relationship and similar metamorphic histories. The Lu-Hf results appear to date a punctuated event of garnet growth. Alternatively, the Lu-Hf garnet ages may represent the onset of rapid, contemporaneous uplift and subsequent cooling. However, trace element zoning of Lu and Hf is still preserved in garnet porphyroblasts, even in those with a homogeneous major element distribution. Thus, complete reequilibration of the Lu-Hf system during peak-temperature conditions probably did not occur. The garnet forming event can be placed toward the final stage of the UHP metamorphism, in agreement with some published U-Pb zircon ages. A possible trigger for this short-lived and widespread mineral growth episode may have been a fluid that became available at that stage of the metamorphic history. Although HREE-depleted patterns of older zircon grains may indicate the presence of an older generation of garnet, complete eclogitisation may have been inhibited during the major part of the prograde P-T path due to dry conditions during most of the UHP metamorphism. The uniform Lu-Hf (and Sm-Nd) ages of all investigated Dabie and Sulu eclogites suggest that garnet growth and thus possibly fluid availability were limited to a short time interval over a remarkably large regional scale. (C) 2008 Elsevier B.V. All rights reserved."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft (DFG) [WE 2850-2/1]"],["dc.identifier.doi","10.1016/j.epsl.2008.06.036"],["dc.identifier.isi","000259729000020"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11244"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53559"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","1385-013X"],["dc.relation.issn","0012-821X"],["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","Rapid eclogitisation of the Dabie-Sulu UHP terrane: Constraints from Lu-Hf garnet geochronology"],["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"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific Reports"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Rikkinen, Jouko"],["dc.contributor.author","Grimaldi, David A."],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2020-12-10T18:11:11Z"],["dc.date.available","2020-12-10T18:11:11Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1038/s41598-019-55622-9"],["dc.identifier.eissn","2045-2322"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/17051"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73914"],["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","Morphological stasis in the first myxomycete from the Mesozoic, and the likely role of cryptobiosis"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","14615"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific reports"],["dc.bibliographiccitation.volume","7"],["dc.contributor.author","Regalado, Ledis"],["dc.contributor.author","Schmidt, Alexander R."],["dc.contributor.author","Appelhans, Marc S."],["dc.contributor.author","Ilsemann, Bork"],["dc.contributor.author","Schneider, Harald"],["dc.contributor.author","Krings, Michael"],["dc.contributor.author","Heinrichs, Jochen"],["dc.date.accessioned","2019-07-09T11:44:40Z"],["dc.date.available","2019-07-09T11:44:40Z"],["dc.date.issued","2017-11-06"],["dc.description.abstract","The monospecific fern genus Cystodium (Cystodiaceae; Polypodiales) occurs exclusively in the tropical forests of the Malay Archipelago, the Admiralty Islands, the Louisiade Archipelago, and the Solomon Islands. Divergence time estimates suggest that the genus originated in the Mesozoic; however, fossil evidence to validate this suggestion has been lacking. Amber from Myanmar (Burmese amber) is an important source of new information on the diversity of vascular cryptogams in the Cretaceous. This paper describes the fossil taxon Cystodium sorbifolioides nov. sp. based on a fragment of a fertile leaf preserved in Burmese amber that represents the first fossil evidence of the family Cystodiaceae. Cystodium sorbifolioides is used to obtain a minimum age estimate for the Cystodiaceae and the closely related, monogeneric Lonchitidaceae and Lindsaeaceae. The fossil strengthens the hypothesis that the forest ecosystems of Malesia and Melanesia represent refugia for many tropical plant lineages that originated in the Cretaceous."],["dc.identifier.doi","10.1038/s41598-017-14985-7"],["dc.identifier.pmid","29097728"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14857"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/59062"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","2045-2322"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.subject.ddc","550"],["dc.title","A fossil species of the enigmatic early polypod fern genus Cystodium (Cystodiaceae) in Cretaceous amber from Myanmar."],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","e0129526"],["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","PLoS ONE"],["dc.bibliographiccitation.lastpage","12"],["dc.bibliographiccitation.volume","10"],["dc.contributor.author","Kaasalainen, Ulla"],["dc.contributor.author","Heinrichs, Jochen"],["dc.contributor.author","Krings, Michael"],["dc.contributor.author","Myllys, Leena"],["dc.contributor.author","Grabenhorst, Heinrich"],["dc.contributor.author","Rikkinen, Jouko"],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2018-11-07T09:55:56Z"],["dc.date.available","2018-11-07T09:55:56Z"],["dc.date.issued","2015"],["dc.description.abstract","One of the most important issues in molecular dating studies concerns the incorporation of reliable fossil taxa into the phylogenies reconstructed from DNA sequence variation in extant taxa. Lichens are symbiotic associations between fungi and algae and/or cyanobacteria. Several lichen fossils have been used as minimum age constraints in recent studies concerning the diversification of the Ascomycota. Recent evolutionary studies of Lecanoromycetes, an almost exclusively lichen-forming class in the Ascomycota, have utilized the Eocene amber inclusion Alectoria succinic as a minimum age constraint. However, a re-investigation of the type material revealed that this inclusion in fact represents poorly preserved plant remains, most probably of a root. Consequently, this fossil cannot be used as evidence of the presence of the genus Alectoria (Parmeliaceae, Lecanorales) or any other lichens in the Paleogene. However, newly discovered inclusions from Paleogene Baltic and Bitterfeld amber verify that alectorioid morphologies in lichens were in existence by the Paleogene. The new fossils represent either a lineage within the alectorioid group or belong to the genus Oropogon."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2015"],["dc.identifier.doi","10.1371/journal.pone.0129526"],["dc.identifier.isi","000355955300138"],["dc.identifier.pmid","26053106"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11959"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/36860"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.notes.submitter","Najko"],["dc.relation.issn","1932-6203"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Alectorioid Morphologies in Paleogene Lichens: New Evidence and Re-Evaluation of the Fossil Alectoria succini Magdefrau"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","5974"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific Reports"],["dc.bibliographiccitation.volume","4"],["dc.contributor.author","Feldberg, Kathrin"],["dc.contributor.author","Schneider, Harald"],["dc.contributor.author","Stadler, Tanja"],["dc.contributor.author","Schäfer-Verwimp, Alfons"],["dc.contributor.author","Schmidt, Alexander R."],["dc.contributor.author","Heinrichs, Jochen"],["dc.date.accessioned","2018-08-14T10:43:04Z"],["dc.date.available","2018-08-14T10:43:04Z"],["dc.date.issued","2014"],["dc.description.abstract","Recent studies have provided evidence for pulses in the diversification of angiosperms, ferns, gymnosperms, and mosses as well as various groups of animals during the Cretaceous revolution of terrestrial ecosystems. However, evidence for such pulses has not been reported so far for liverworts. Here we provide new insight into liverwort evolution by integrating a comprehensive molecular dataset with a set of 20 fossil age constraints. We found evidence for a relative constant diversification rate of generalistic liverworts (Jungermanniales) since the Palaeozoic, whereas epiphytic liverworts (Porellales) show a sudden increase of lineage accumulation in the Cretaceous. This difference is likely caused by the pronounced response of Porellales to the ecological opportunities provided by humid, megathermal forests, which were increasingly available as a result of the rise of the angiosperms."],["dc.identifier.doi","10.1038/srep05974"],["dc.identifier.pmid","25099137"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11920"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15274"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Epiphytic leafy liverworts diversified in angiosperm-dominated forests"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","10360"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific Reports"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Kaasalainen, Ulla"],["dc.contributor.author","Kukwa, Martin"],["dc.contributor.author","Rikkinen, Jouko"],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2019-07-22T10:02:45Z"],["dc.date.available","2019-07-22T10:02:45Z"],["dc.date.issued","2019"],["dc.description.abstract","Lichens, symbiotic consortia of lichen-forming fungi and their photosynthetic partners have long had an extremely poor fossil record. However, recently over 150 new lichens were identified from European Paleogene amber and here we analyse crustose lichens from the new material. Three fossil lichens belong to the extant genus Ochrolechia (Ochrolechiaceae, Lecanoromycetes) and one fossil has conidiomata similar to those produced by modern fungi of the order Arthoniales (Arthoniomycetes). Intriguingly, two fossil Ochrolechia specimens host lichenicolous fungi of the genus Lichenostigma (Lichenostigmatales, Arthoniomycetes). This confirms that both Ochrolechia and Lichenostigma already diversified in the Paleogene and demonstrates that also the specific association between the fungi had evolved by then. The new fossils provide a minimum age constraint for both genera at 34 million years (uppermost Eocene)."],["dc.identifier.doi","10.1038/s41598-019-46692-w"],["dc.identifier.pmid","31316089"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16287"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61781"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.eissn","2045-2322"],["dc.relation.issn","2045-2322"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Crustose lichens with lichenicolous fungi from Paleogene amber"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","900586"],["dc.bibliographiccitation.journal","Frontiers in Earth Science"],["dc.bibliographiccitation.volume","10"],["dc.contributor.affiliation","Roghi, Guido; \n1\nInstitute of Geosciences and Earth Resources (IGG-CNR), Padova, Italy"],["dc.contributor.affiliation","Gianolla, Piero; \n2\nDepartment of Physics and Earth Sciences, University of Ferrara, Ferrara, Italy"],["dc.contributor.affiliation","Kustatscher, Evelyn; \n3\nMuseum of Nature South Tyrol, Bolzano, Italy"],["dc.contributor.affiliation","Schmidt, Alexander R.; \n6\nDepartment of Geobiology, University of Göttingen, Göttingen, Germany"],["dc.contributor.affiliation","Seyfullah, Leyla J.; \n7\nDepartment of Palaeontology, University of Vienna, Vienna, Austria"],["dc.contributor.author","Roghi, Guido"],["dc.contributor.author","Gianolla, Piero"],["dc.contributor.author","Kustatscher, Evelyn"],["dc.contributor.author","Schmidt, Alexander R."],["dc.contributor.author","Seyfullah, Leyla J."],["dc.date.accessioned","2022-07-25T10:17:41Z"],["dc.date.available","2022-07-25T10:17:41Z"],["dc.date.issued","2022-07-11"],["dc.date.updated","2022-07-25T09:11:10Z"],["dc.description.abstract","The Carnian Pluvial Episode (CPE) has been recognized as a time of plant radiations and originations, likely related to observed swift changes from xerophytic to more hygrophytic floras. This suggests that the increasing humidity causally resulting from LIP volcanism was the trigger for these changes in the terrestrial realm. Understanding the cause and effects of the CPE on the plant realm, requires study of well-preserved floras that are precisely aligned with the CPE. We therefore focus on the best age-constrained section within the CPE for the terrestrial to marginal marine environment to understand the floristic composition at the early CPE. This is found in the Dolomites, Italy, and is remarkable for the preservation of the oldest fossiliferous amber found in the rock record. An integrated study of palynomorphs and macro-remains related to the conifer families of the fossil resin bearing level brings together the floral components from this section. This observed mixture of different taxa of extinct and modern conifer families underlines firmly the effects of the LIP-induced CPE on the evolution and radiation of conifers."],["dc.identifier.doi","10.3389/feart.2022.900586"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/112533"],["dc.language.iso","en"],["dc.relation.eissn","2296-6463"],["dc.rights","CC BY 4.0"],["dc.rights.uri","http://creativecommons.org/licenses/by/4.0/"],["dc.title","An Exceptionally Preserved Terrestrial Record of LIP Effects on Plants in the Carnian (Upper Triassic) Amber-Bearing Section of the Dolomites, Italy"],["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","e1067"],["dc.bibliographiccitation.journal","Paleontology and Evolutionary Science section"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","Seyfullah, Leyla J."],["dc.contributor.author","Sadowski, Eva-Maria"],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2018-08-14T10:51:54Z"],["dc.date.available","2018-08-14T10:51:54Z"],["dc.date.issued","2015"],["dc.description.abstract","Some higher plants, both angiosperms and gymnosperms, can produce resins and some of these resins can polymerize and fossilize to form ambers. Various physical and chemical techniques have been used to identify and profile different plant resins and have then been applied to fossilized resins (ambers), to try to detect their parent plant affinities and understand the process of polymerization, with varying levels of success. Here we focus on resins produced from today's most resinous conifer family, the Araucariaceae, which are thought to be the parent plants of some of the Southern Hemisphere's fossil resin deposits. Fourier transform infrared (FTIR) spectra of the resins of closely related Araucariaceae species were examined to test whether they could be distinguished at genus and species level and whether the results could then be used to infer the parent plant of a New Zealand amber. The resin FTIR spectra are distinguishable from each other, and the three Araucaria species sampled produced similar FTIR spectra, to which Wollemia resin is most similar. Interspecific variability of the FTIR spectra is greatest in the three Agathis species tested. The New Zealand amber sample is similar in key shared features with the resin samples, but it does differ from the extant resin samples in key distinguishing features, nonetheless it is most similar to the resin of Agathis australis in this dataset. However on comparison with previously published FTIR spectra of similar aged amber and older (Eocene) resinites both found in coals from New Zealand and fresh Agathis australis resin, our amber has some features that imply a relatively immature resin, which was not expected from an amber of the Miocene age."],["dc.identifier.doi","10.7717/peerj.1067"],["dc.identifier.pmid","26157631"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/13603"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15275"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.relation.eissn","2167-8359"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Species-level determination of closely related araucarian resins using FTIR spectroscopy and its implications for the provenance of New Zealand amber"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","e0156301"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","PLoS ONE"],["dc.bibliographiccitation.volume","11"],["dc.contributor.author","Heinrichs, Jochen"],["dc.contributor.author","Scheben, Armin"],["dc.contributor.author","Bechteler, Julia"],["dc.contributor.author","Lee, Gaik Ee"],["dc.contributor.author","Schafer-Verwimp, Alfons"],["dc.contributor.author","Hedenas, Lars"],["dc.contributor.author","Singh, Hukam"],["dc.contributor.author","Pócs, Tamás"],["dc.contributor.author","Nascimbene, Paul C."],["dc.contributor.author","Peralta, Denilson Fernandes"],["dc.contributor.author","Renner, Matthew A. M."],["dc.contributor.author","Schmidt, Alexander R."],["dc.date.accessioned","2018-11-07T10:14:04Z"],["dc.date.available","2018-11-07T10:14:04Z"],["dc.date.issued","2016"],["dc.description.abstract","Cambay amber originates from the warmest period of the Eocene, which is also well known for the appearance of early angiosperm-dominated megathermal forests. The humid climate of these forests may have triggered the evolution of epiphytic lineages of bryophytes; however, early Eocene fossils of bryophytes are rare. Here, we present evidence for lejeuneoid liverworts and pleurocarpous mosses in Cambay amber. The preserved morphology of the moss fossil is inconclusive for a detailed taxonomic treatment. The liverwort fossil is, however, distinctive; its zig-zagged stems, suberect complicate-bilobed leaves, large leaf lobules, and small, deeply bifid underleaves suggest a member of Lejeuneaceae subtribe Lejeuneinae (Harpalejeunea, Lejeunea, Microlejeunea). We tested alternative classification possibilities by conducting divergence time estimates based on DNA sequence variation of Lejeuneinae using the age of the fossil for corresponding age constraints. Consideration of the fossil as a stem group member of Microlejeunea or Lejeunea resulted in an Eocene to Late Cretaceous age of the Lejeuneinae crown group. This reconstruction is in good accordance with published divergence time estimates generated without the newly presented fossil evidence. Balancing available evidence, we describe the liverwort fossil as the extinct species Microlejeunea nyiahae, representing the oldest crown group fossil of Lejeuneaceae."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2016"],["dc.identifier.doi","10.1371/journal.pone.0156301"],["dc.identifier.isi","000377146100026"],["dc.identifier.pmid","27244582"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/13335"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/40554"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.notes.submitter","Najko"],["dc.relation.issn","1932-6203"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Crown Group Lejeuneaceae and Pleurocarpous Mosses in Early Eocene (Ypresian) Indian Amber"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","589"],["dc.bibliographiccitation.journal","European Journal of Taxonomy"],["dc.contributor.author","Ramage, Thibault"],["dc.contributor.author","Jouault, Corentin"],["dc.contributor.author","Schmidt, Alexander R."],["dc.contributor.author","Seyfullah, Leyla J."],["dc.contributor.author","Perrichot, Vincent"],["dc.date.accessioned","2020-12-10T18:48:02Z"],["dc.date.available","2020-12-10T18:48:02Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.5852/ejt.2019.589"],["dc.identifier.eissn","2118-9773"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/17177"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/78990"],["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","Two new ant species (Formicidae: Dorylinae, Ponerinae) from New Caledonia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]