Shumilovskikh, Lyudmila S.

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.journal","Marine Micropaleontology"],["dc.bibliographiccitation.lastpage","152"],["dc.bibliographiccitation.volume","134"],["dc.contributor.author","Mudie, Peta J."],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Mertens, Kenneth N."],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Leroy, Suzanne A.G."],["dc.date.accessioned","2020-12-10T15:20:19Z"],["dc.date.available","2020-12-10T15:20:19Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1016/j.marmicro.2017.05.004"],["dc.identifier.issn","0377-8398"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72623"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Atlas of modern dinoflagellate cyst distributions in the Black Sea Corridor: from Aegean to Aral Seas, including Marmara, Black, Azov and Caspian Seas"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","309"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Fungal Ecology"],["dc.bibliographiccitation.lastpage","315"],["dc.bibliographiccitation.volume","6"],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.date.accessioned","2018-11-07T09:22:09Z"],["dc.date.available","2018-11-07T09:22:09Z"],["dc.date.issued","2013"],["dc.description.abstract","This study links the spores of the recent ascomycete genus Potamomyces with the fossil form-taxa Mediaverrunites. Spores of the only known representative of Potamomyces, P. armatisporus, were found in recent material from Nepal together with a previously unknown spore type described here for the first time as Potamomyces nepalensis-type. Potamomyces is thus not a monotypic genus. The rarely isolated type species P. armatisporus is known as a lignicolous freshwater ascomycete from tropical rivers. Our findings indicate that the genus also lives in damp conditions in terrestrial habitats, and is recently distributed also in subtropical regions. Based on the fossil findings of Mediaverrunites, the genus Potamomyces evolved at least 25 million yr ago at the onset of younger Tertiary. Potamomyces is an excellent example of the potential of interdisciplinary fungal research, combining insights from fungal evolution, taxonomy, ancient and recent distribution and ecology. (c) 2013 Elsevier Ltd and The British Mycological Society. All rights reserved."],["dc.description.sponsorship","German Research Foundation (DFG) [Be 2116/7-1]"],["dc.identifier.doi","10.1016/j.funeco.2013.03.007"],["dc.identifier.isi","000321404600008"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/29274"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1754-5048"],["dc.title","On the relation of Potamomyces armatisporus to the fossil form-type Mediaverrunites and its taxonomical and ecological implications"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"],["local.message.claim","2021-09-10T11:52:35.258+0000|||rp31364|||submit_approve|||dc_contributor_author|||None"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.journal","Palynology"],["dc.bibliographiccitation.lastpage","9"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Abdulmanova, Irina F."],["dc.contributor.author","Efimik, Elena G."],["dc.date.accessioned","2021-04-14T08:25:36Z"],["dc.date.available","2021-04-14T08:25:36Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1080/01916122.2020.1776780"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/81683"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1558-9188"],["dc.relation.issn","0191-6122"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Does season matter for moss surface sample collection? A case study from Kungur forest-steppe, pre-Urals, Russia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Shumilovskikh, Elena S."],["dc.contributor.author","Schlütz, Frank"],["dc.contributor.author","van Geel, Bas"],["dc.date.accessioned","2022-11-01T10:17:35Z"],["dc.date.available","2022-11-01T10:17:35Z"],["dc.date.issued","2022"],["dc.identifier.doi","10.1007/s00334-022-00889-8"],["dc.identifier.pii","889"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/116850"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-605"],["dc.relation.eissn","1617-6278"],["dc.relation.iserratumof","/handle/2/90163"],["dc.relation.issn","0939-6314"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.title","Correction: NPP-ID: Non-Pollen Palynomorph Image Database as a research and educational platform"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","erratum_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Earth Surface Processes and Landforms"],["dc.contributor.author","Nottebaum, Veit"],["dc.contributor.author","Stauch, Georg"],["dc.contributor.author","Wal, Jorien. L. N."],["dc.contributor.author","Zander, Anja"],["dc.contributor.author","Schlütz, Frank"],["dc.contributor.author","Shumilovskikh, Lyudmila"],["dc.contributor.author","Reicherter, Klaus"],["dc.contributor.author","Batkhishig, Ochirbat"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.date.accessioned","2021-12-01T09:23:21Z"],["dc.date.available","2021-12-01T09:23:21Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1002/esp.5247"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/94629"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-478"],["dc.relation.eissn","1096-9837"],["dc.relation.issn","0197-9337"],["dc.title","Late Quaternary landscape evolution and paleoenvironmental implications from multiple geomorphic dryland systems, Orog Nuur Basin, Mongolia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","41"],["dc.bibliographiccitation.journal","Quaternary Science Reviews"],["dc.bibliographiccitation.lastpage","53"],["dc.bibliographiccitation.volume","135"],["dc.contributor.author","Wegwerth, Antje"],["dc.contributor.author","Kaiser, Jerome"],["dc.contributor.author","Dellwig, Olaf"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Nowaczyk, Norbert R."],["dc.contributor.author","Arz, Helge W."],["dc.date.accessioned","2018-11-07T10:17:35Z"],["dc.date.available","2018-11-07T10:17:35Z"],["dc.date.issued","2016"],["dc.description.abstract","The Marine Isotope Stage (MIS) 3 stands out due to its abrupt changes from cold and dry stadials to warm and humid interstadials, the so-called Dansgaard-Oeschger cycles that also affected temperature and rainfall in the Black Sea region. This study is based on a gravity core from the southeastern (SE) Black Sea that covers the last glacial lake stage from 64 to 20 ka BP. By using the composition of major and trace elements in the sediments, terrestrial plant-derived n-alkane flux, and Sr/Ca from benthic ostracods, we reconstruct the variability of riverine and aeolian input, salinity, and productivity in the SE Black Sea region in response to the Northern Hemisphere climate oscillations. During colder and drier stadials, the aeolian input increased relative to the riverine discharge, potentially due to southward shifted and/or stronger westerly winds and due to changes in the vegetation cover. An evaporation exceeding freshwater supply by rainfall and rivers possibly caused higher salinity and a lower lake level. The environmental status during MIS 4 and 2 is very much comparable with the stadial conditions during MIS 3. During warmer and more humid interstadials, lower salinity and presumably positive lake level changes most likely resulted from increased precipitation and river discharge. This likely increased primary productivity through an augmented nutrient supply. Lowest average salinities are suggested for the middle part of MIS 3 in response to enhanced meltwater from the disintegrating Fennoscandian Ice Sheet and/or by generally more humid conditions. (C) 2016 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.quascirev.2016.01.016"],["dc.identifier.isi","000372376200003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/41258"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0277-3791"],["dc.title","Northern hemisphere climate control on the environmental dynamics in the glacial Black Sea \"Lake\""],["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.firstpage","47"],["dc.bibliographiccitation.journal","Review of Palaeobotany and Palynology"],["dc.bibliographiccitation.lastpage","54"],["dc.bibliographiccitation.volume","239"],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.date.accessioned","2018-11-07T10:25:24Z"],["dc.date.available","2018-11-07T10:25:24Z"],["dc.date.issued","2017"],["dc.description.abstract","The type HdV-368 (van Geel et al., 1981) or the Podospora-type (van Geel et al., 2001) is a common representative of non-pollen palynomorphs (NPP) with high palaeoecological potential. Here we present a revision of the type on the basis of a survey of the mycological literature and incubation of related dung fungi. The characteristic truncated base of the type HdV-368 is shared by the ascospores of at least 31 species of the genus Podospora, including one species that probably belongs to the nearly related genus Schizothecium. We arrange these species in morphological spore taxa, which are named after representative species, and provide an identification key to the new types and groups including descriptions of ecology and distribution of each species. The former type of HdV-368 falls into the newly erected Podospora decipiens-type, which covers the spores of the coprophilous species P. decipiens and P. perplexens and partly of P. pleiospora and P. prethopodalis. A short discussion of the spores of coprophilous fungi as palaeoecological indicators for animal diversity, population density, vegetation, climate, local conditions, and transport events is also given. The key's application can provide detailed insights into past environmental and biodiversity changes. (C) 2017 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.revpalbo.2016.12.005"],["dc.identifier.isi","000400533700004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/42853"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.relation.issn","1879-0615"],["dc.relation.issn","0034-6667"],["dc.title","Non-pollen palynomorphs notes: 1. Type HdV-368 (Podospora-type), descriptions of associated species, and the first key to related spore types"],["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.firstpage","231"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","244"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Eckstein, Jan"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.contributor.author","Giesecke, Thomas"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Bauerochse, Andreas"],["dc.date.accessioned","2018-11-07T08:45:27Z"],["dc.date.available","2018-11-07T08:45:27Z"],["dc.date.issued","2010"],["dc.description.abstract","Excellently preserved subfossil pine and oak tree remains from the bottom layer of raised bog peat were dendroecologically investigated at Venner Moor (northwest Germany). Tree-ring analyses were combined with observations of stem and root morphology, preservation state, mineral soil relief, peat stratigraphy and pollen analysis to reconstruct in great detail environmental changes leading to the start of the raised bog formation. Hydrology was identified as the main determinant influencing tree growth and population dynamics at Venner Moor, as documented by different growth patterns and dying-off dates in relation to the mineral soil elevation. The woodland phase has been dendrochronological dated to the period from 2421-2077 BC (4371-4027 cal BP). In this period, a general change from more or less open landscape with dominating heath to wet pine forest and eventually to open raised bog occurred at the site. Comparisons with pine population dynamics at the nearby Voerdener Moor and with the independent Lower Saxony log yak Chronology (LSBOC) indicate that the reconstructed ecological changes at Venner Moor are mainly triggered by climate variations, in particular wet shifts on the decadal timescale. This example shows the value of subfossil pine layers from northwest German bogs as a high resolution proxy archive of Holocene humidity fluctuations."],["dc.description.sponsorship","German Research Foundation [LE 1805/2-1]"],["dc.identifier.doi","10.1177/0959683609350397"],["dc.identifier.isi","000274900800008"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/13085"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/20445"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0959-6836"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Dendroecological investigations at Venner Moor (northwest Germany) document climate-driven woodland dynamics and mire development in the period 2450-2050 BC"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","416"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Journal of Vegetation Science"],["dc.bibliographiccitation.lastpage","426"],["dc.bibliographiccitation.volume","29"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Novenko, Elena"],["dc.contributor.author","Giesecke, Thomas"],["dc.date.accessioned","2020-12-10T18:29:06Z"],["dc.date.available","2020-12-10T18:29:06Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1111/jvs.12585"],["dc.identifier.issn","1100-9233"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76529"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Long-term dynamics of the East European forest-steppe ecotone"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.journal","Quaternary International"],["dc.bibliographiccitation.lastpage","4"],["dc.bibliographiccitation.volume","516"],["dc.contributor.author","Novenko, Elena"],["dc.contributor.author","Tarasov, Pavel E."],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.date.accessioned","2020-12-10T15:20:59Z"],["dc.date.available","2020-12-10T15:20:59Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.quaint.2019.06.004"],["dc.identifier.issn","1040-6182"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72879"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Climate change and human-environment interaction from Neolithic to historical times"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]