Shumilovskikh, Lyudmila S.

[["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","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","177"],["dc.bibliographiccitation.journal","Palaeogeography Palaeoclimatology Palaeoecology"],["dc.bibliographiccitation.lastpage","193"],["dc.bibliographiccitation.volume","337"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Tarasov, Pavel E."],["dc.contributor.author","Arz, Helge W."],["dc.contributor.author","Fleitmann, Dominik"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Nowaczyk, Norbert"],["dc.contributor.author","Plessen, Birgit"],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:09:14Z"],["dc.date.available","2018-11-07T09:09:14Z"],["dc.date.issued","2012"],["dc.description.abstract","Sediments from the Black Sea, a region historically dominated by forests and steppe landscapes, are a valuable source of detailed information on the changes in regional terrestrial and aquatic environments at decadal to millennial scales. Here we present multi-proxy environmental records (pollen, dinoflagellate cysts, Ca, Ti and oxygen isotope data) from the uppermost 305 cm of the core 22-GC3 (42 degrees 13.53'N, 36 degrees 29.55'E) collected from a water depth of 838 m in the southern part of the Black Sea in 2007. The records span the last similar to 18 kyr (all ages are given in cal kyr BP). The pollen data reveal the dominance of the Artemisia-steppe in the region, suggesting rather dry/cold environments similar to 18-14.5 kyr BP. Warming/humidity increase during melt-water pulses (similar to 16.1-14.5 kyr BP), indicated by delta O-18 records from the 22-GC3 core sediment and from the Sofular Cave stalagmite, is expressed in more negative delta C-13 values from the Sofular Cave, usually interpreted as the spreading of C3 plants. The records representing the interstadial complex (similar to 14.5-12.9 kyr BP) show an increase in temperature and moisture, indicated by forest development, increased primary productivity and reduced surface run-off, whereas the switch from primary terrigenous to primary authigenic Ca origin occurs similar to 500 yr later. The Younger Dryas cooling is clearly demonstrated by more negative delta C-13 values from the Sofular Cave and a reduction of pines. The early Holocene (11.7-8.5 kyr BP) interval reveals relatively dry conditions compared to the mostly moist and warm middle Holocene (8.5-5 kyr BP), which is characterized by the establishment of the species-rich warm mixed and temperate deciduous forests in the low elevation belt, temperate deciduous beech-hornbeam forests in the middle and cool conifer forest in upper mountain belt. The border between the early and middle Holocene in the vegetation records coincides with the opening of the Mediterranean corridor at similar to 8.3 kyr BP, as indicated by a marked change in the dinocyst assemblages and in the sediment lithology. Changes in the pollen assemblages indicate a reduction in forest cover after similar to 5 kyr BP, which was likely caused by increased anthropogenic pressure on the regional vegetation. (C) 2012 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.palaeo.2012.04.015"],["dc.identifier.isi","000306032100015"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/26212"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1872-616X"],["dc.relation.issn","0031-0182"],["dc.title","Vegetation and environmental dynamics in the southern Black Sea region since 18 kyr BP derived from the marine core 22-GC3"],["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","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.firstpage","171"],["dc.bibliographiccitation.journal","Review of Palaeobotany and Palynology"],["dc.bibliographiccitation.lastpage","178"],["dc.bibliographiccitation.volume","221"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Achterberg, Inke"],["dc.contributor.author","Kvitkina, Anna"],["dc.contributor.author","Bauerochse, Andreas"],["dc.contributor.author","Leuschner, Hanns Hubert"],["dc.date.accessioned","2018-11-07T09:51:12Z"],["dc.date.available","2018-11-07T09:51:12Z"],["dc.date.issued","2015"],["dc.description.abstract","Several laboratory experiments and field observations demonstrate that saprotrophic and ectomycorrhizal fungi effectively use pollen cytoplasm and suggest pollen produced by wind-pollinated trees as a crucial nutrient source for fungi and their plant hosts in nutrient-limited environments. However, the role of such interactions is still underestimated or neglected in ecology and paleoecology. Here, we consider pollen attacked by fungi in palynological records from Holocene raised peat bogs as a nutrient source for ecosystems in the past. The attacks occurred through the pollen germination areas by a variety of saprotrophic, ericoid mycorrhizal, ectomycorrhizal or dark septate endophyte fungi. Large amounts of attacked pollen in phases rich in Calluna vulgaris highlight the importance of Ericaceae shrubs, hosting ericoid mycorrhizal fungi and forming hotspots of decomposition in nutrient-deficit bogs. Applying estimations of pollen rain from literature, and based on own observed pollen infection rates we estimate the annual release of nitrogen, phosphate and potassium from pollen, and highlight their significance in pushing the ecosystem nutrient cycle in early spring time, when several species release their pollen. We highlight the significant role of anthropogenic changes in pollen deposition for pre-industrial bogs and hypothesize about the consequences of the pollen-based interrelation between wind-pollinated plants and their mycorrhizal fungi in paleoecology and evolution. (C) 2015 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.revpalbo.2015.07.001"],["dc.identifier.isi","000361777900016"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/35867"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1879-0615"],["dc.relation.issn","0034-6667"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Pollen as nutrient source in Holocene ombrotrophic bogs"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Palaeogeography Palaeoclimatology Palaeoecology"],["dc.bibliographiccitation.volume","393"],["dc.contributor.author","Shumilovskikh, L. S."],["dc.contributor.author","Tarasov, Pavel E."],["dc.contributor.author","Arz, Helge W."],["dc.contributor.author","Fleitmann, Dominik"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Nowaczyk, Norbert"],["dc.contributor.author","Plessen, Birgit"],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:46:39Z"],["dc.date.available","2018-11-07T09:46:39Z"],["dc.date.issued","2014"],["dc.format.extent","159"],["dc.identifier.doi","10.1016/j.palaeo.2013.11.016"],["dc.identifier.isi","000331024900013"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/34924"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1872-616X"],["dc.relation.issn","0031-0182"],["dc.title","Vegetation and environmental dynamics in the southern Black Sea region since 18 kyr BP derived from the marine core 22-GC3 (vol 337, pg 177, 2012)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","21"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","CLIMATE OF THE PAST"],["dc.bibliographiccitation.lastpage","39"],["dc.bibliographiccitation.volume","10"],["dc.contributor.author","Wang, Y."],["dc.contributor.author","Herzschuh, Ulrike"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Mischke, Steffen"],["dc.contributor.author","Birks, H. John B."],["dc.contributor.author","Wischnewski, J."],["dc.contributor.author","Bohner, J."],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.contributor.author","Diekmann, B."],["dc.contributor.author","Wuennemann, B."],["dc.contributor.author","Zhang, C."],["dc.date.accessioned","2018-11-07T09:46:18Z"],["dc.date.available","2018-11-07T09:46:18Z"],["dc.date.issued","2014"],["dc.description.abstract","Pollen records from large lakes have been used for quantitative palaeoclimate reconstruction, but the influences that lake size (as a result of species-specific variations in pollen dispersal patterns that smaller pollen grains are more easily transported to lake centre) and taphonomy have on these climatic signals have not previously been systematically investigated. We introduce the concept of pollen source area to pollen-based climate calibration using the north-eastern Tibetan Plateau as our study area. We present a pollen data set collected from large lakes in the arid to semi-arid region of central Asia. The influences that lake size and the inferred pollen source areas have on pollen compositions have been investigated through comparisons with pollen assemblages in neighbouring lakes of various sizes. Modern pollen samples collected from different parts of Lake Donggi Cona (in the north-eastern part of the Tibetan Plateau) reveal variations in pollen assemblages within this large lake, which are interpreted in terms of the species-specific dispersal and depositional patterns for different types of pollen, and in terms of fluvial input components. We have estimated the pollen source area for each lake individually and used this information to infer modern climate data with which to then develop a modern calibration data set, using both the multivariate regression tree (MRT) and weighted-averaging partial least squares (WA-PLS) approaches. Fossil pollen data from Lake Donggi Cona have been used to reconstruct the climate history of the north-eastern part of the Tibetan Plateau since the Last Glacial Maximum (LGM). The meanannual precipitation was quantitatively reconstructed using WA-PLS: extremely dry conditions are found to have dominated the LGM, with annual precipitation of around 100 mm, which is only 32% of present-day precipitation. A gradually increasing trend in moisture conditions during the Late Glacial is terminated by an abrupt reversion to a dry phase that lasts for about 1000 yr and coincides with \"Heinrich event 1\" in the North Atlantic region. Subsequent periods corresponding to the Bolling/Allerod interstadial, with annual precipitation (P-ann) of about 350 mm, and the Younger Dryas event (about 270 mm P-ann) are followed by moist conditions in the early Holocene, with annual precipitation of up to 400 mm. A drier trend after 9 cal. ka BP is followed by a second wet phase in the middle Holocene, lasting until 4.5 cal. ka BP. Relatively steady conditions with only slight fluctuations then dominate the late Holocene, resulting in the present climatic conditions. The climate changes since the LGM have been primarily driven by deglaciation and fluctuations in the intensity of the Asian summer monsoon that resulted from changes in the Northern Hemisphere summer solar insolation, as well as from changes in the North Atlantic climate through variations in the circulation patterns and intensity of the westerlies."],["dc.identifier.doi","10.5194/cp-10-21-2014"],["dc.identifier.isi","000333837600002"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11680"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/34842"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1814-9332"],["dc.relation.issn","1814-9324"],["dc.rights","CC BY 3.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/3.0"],["dc.title","Open Access Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum - extending the concept of pollen source area to pollen-based climate reconstructions from large lakes"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","31"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","CATENA"],["dc.bibliographiccitation.lastpage","44"],["dc.bibliographiccitation.volume","87"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.contributor.author","Hilgers, Alexandra"],["dc.contributor.author","Fries, Susanne"],["dc.contributor.author","Huelle, Daniela"],["dc.contributor.author","Schluetz, Frank"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Felauer, Thomas"],["dc.contributor.author","Protze, Jens"],["dc.date.accessioned","2018-11-07T08:51:36Z"],["dc.date.available","2018-11-07T08:51:36Z"],["dc.date.issued","2011"],["dc.description.abstract","Mantles of silt- and sand-size particles, paleosols and fluvial deposits preserve valuable information on Holocene environmental change. These archives were used to reconstruct the landscape history in the upper Orkhon Valley close to the former capitals of the Uighurs (Kharbalgasin Tuur) and the Mongolian Empire (Karakorum) near the recent town of Kharkhorin, Central Mongolia. A holistic approach involving the use of high spatial resolution geomorphological mapping, sedimentological and geochemical analysis, palynology, and geochronology shows several phases of landscape activity and stability in the region. This includes phases of fluvial erosion, aeolian sedimentation, and soil formation. By using luminescence and radiocarbon dating, phases of landscape change, indicated by soil formation, occurred mainly at around 6.5-6 ka. Pollen data and a weakly humic horizon at around 1.0 ka probably indicate enhanced moisture supply in the region and a reduction of human activity between the time of the reigns of the Uighurs (8th-9th century AD) and the Mongols (1220-1388 AD). Since 3 ka, especially within the last two millennia of Historical Time (300 B.C.-present), a more intensified human occupation in the Upper Orkhon Valley occurred in this region. This included a more densely grazing of cattle to supply the growing population demands of the Uighurs and Mongols. This overgrazing caused an increase in erosion and the formation and deepening of fluvial gullies. together with soil deflation and subsequent deposition of aeolian sediments. Human activity, in addition to climate, has been dominant in driving landscape evolution of this region since the late Holocene. (C) 2011 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.catena.2011.05.005"],["dc.identifier.isi","000293105300004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/21973"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0341-8162"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Holocene geomorphological processes and soil development as indicator for environmental change around Karakorum, Upper Orkhon Valley (Central Mongolia)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"],["local.message.claim","2021-09-10T11:50:43.773+0000|||rp31364|||submit_approve|||dc_contributor_author|||None"]]