Shumilovskikh, Lyudmila S.

[["dc.bibliographiccitation.firstpage","939"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","CLIMATE OF THE PAST"],["dc.bibliographiccitation.lastpage","954"],["dc.bibliographiccitation.volume","10"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Fleitmann, Dominik"],["dc.contributor.author","Nowaczyk, N. R."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Wegwerth, Antje"],["dc.contributor.author","Arz, Helge W."],["dc.date.accessioned","2018-11-07T09:46:01Z"],["dc.date.available","2018-11-07T09:46:01Z"],["dc.date.issued","2014"],["dc.description.abstract","High-resolution pollen and dinoflagellate cyst records from sediment core M72/5-25-GC1 were used to reconstruct vegetation dynamics in northern Anatolia and surface conditions of the Black Sea between 64 and 20 ka BP. During this period, the dominance of Artemisia in the pollen record indicates a steppe landscape and arid climate conditions. However, the concomitant presence of temperate arboreal pollen suggests the existence of glacial refugia in northern Anatolia. Long-term glacial vegetation dynamics reveal two major arid phases similar to 64-55 and 40-32 ka BP, and two major humid phases similar to 54-45 and 28-20 ka BP, correlating with higher and lower summer insolation, respectively. Dansgaard-Oeschger (D-O) cycles are clearly indicated by the 25-GC1 pollen record. Greenland interstadials are characterized by a marked increase in temperate tree pollen, indicating a spread of forests due to warm/wet conditions in northern Anatolia, whereas Greenland stadials reveal cold and arid conditions as indicated by spread of xerophytic biomes. There is evidence for a phase lag of similar to 500 to 1500 yr between initial warming and forest expansion, possibly due to successive changes in atmospheric circulation in the North Atlantic sector. The dominance of Pyxidinopsis psilata and Spiniferites cruciformis in the dinocyst record indicates brackish Black Sea conditions during the entire glacial period. The decrease of marine indicators (marine dinocysts, acritarchs) at similar to 54 ka BP and increase of freshwater algae (Pediastrum, Botryococcus) from 32 to 25 ka BP reveals freshening of the Black Sea surface water. This freshening is possibly related to humid phases in the region, to connection between Caspian Sea and Black Sea, to seasonal freshening by floating ice, and/or to closer position of river mouths due to low sea level. In the southern Black Sea, Greenland interstadials are clearly indicated by high dinocyst concentrations and calcium carbonate content, as a result of an increase in primary productivity. Heinrich events show a similar impact on the environment in the northern Anatolia/Black Sea region as Greenland stadials."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2013"],["dc.identifier.doi","10.5194/cp-10-939-2014"],["dc.identifier.isi","000338761600002"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/10124"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/34767"],["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","Orbital- and millennial-scale environmental changes between 64 and 20 ka BP recorded in Black Sea sediments"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["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","349"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Quaternary Research"],["dc.bibliographiccitation.lastpage","360"],["dc.bibliographiccitation.volume","80"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Arz, Helge W."],["dc.contributor.author","Wegwerth, Antje"],["dc.contributor.author","Fleitmann, Dominik"],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Nowaczyk, Norbert"],["dc.contributor.author","Tarasov, Pavel E."],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:17:57Z"],["dc.date.available","2018-11-07T09:17:57Z"],["dc.date.issued","2013"],["dc.description.abstract","This multiproxy study on SE Black Sea sediments provides the first detailed reconstruction of vegetation and environmental history of Northern Anatolia between 134 and 119 ka. Here, the glacial-interglacial transition is characterized by several short-lived alternating cold and warm events preceding a meltwater pulse (similar to 130.4-131.7 ka). The latter is reconstructed as a cold arid period correlated to Heinrich event 11. The initial warming is evidenced at similar to 130.4 ka by increased primary productivity in the Black Sea, disappearance of ice-rafted detritus, and spreading of oaks in Anatolia. A Younger Dryas-type event is not identifiable. The Eemian vegetation succession corresponds to the main climatic phases in Europe: i) the Quercus-Juniperus phase (128.7-126.4 ka) indicates a dry continental climate; ii) the Ostrya-Corylus-Quercus-Carpinus phase (126.4-122.9 ka) suggests warm summers, mild winters, and high year-round precipitation; iii) the Fagus-Caipinus phase (122.9-119.5 ka) indicates cooling and high precipitation; and iv) increasing Pinus at similar to 121 ka marks the onset of cooler/drier conditions. Generally, pollen reconstructions suggest altitudinal/latitudinal migrations of vegetation belts in Northern Anatolia during the Eemian caused by increased transport of moisture. The evidence for the wide distribution of Fagus around the Black Sea contrasts with the European records and is likely related to climatic and genetic factors. (C) 2013 University of Washington. Published by Elsevier Inc All rights reserved."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft (DFG) [BE 2116/20-1, SPP 1266]"],["dc.identifier.doi","10.1016/j.yqres.2013.07.005"],["dc.identifier.isi","000327285500001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/28294"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1096-0287"],["dc.relation.issn","0033-5894"],["dc.title","Vegetation and environmental changes in Northern Anatolia between 134 and 119 ka recorded in Black Sea sediments"],["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","146"],["dc.bibliographiccitation.journal","Marine Micropaleontology"],["dc.bibliographiccitation.lastpage","160"],["dc.bibliographiccitation.volume","101"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Marret, Fabienne"],["dc.contributor.author","Fleitmann, Dominik"],["dc.contributor.author","Arz, Helge W."],["dc.contributor.author","Nowaczyk, Norbert"],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2018-11-07T09:24:53Z"],["dc.date.available","2018-11-07T09:24:53Z"],["dc.date.issued","2013"],["dc.description.abstract","In order to compare the sea-surface conditions in the Black Sea during the Holocene and Eemian, sapropelic parts of marine core 22-GC3 (42 degrees 13.53'N/36 degrees 29.55'E, 838 m water depth) were studied for organic-walled dinoflagellate cyst content. The record shows a change from freshwater/brackish assemblages (Pyxidinopsis psilata, Spiniferites cruciformis, and Caspidinium rugosum) to more marine assemblages (Lingulodinium machaerophorum and Spiniferites ramosus complex) during each interglacial, due to the inflow of saline Mediterranean water. The lacustrine-marine transitions in 22-GC3 occurred at similar to 8.3 cal kyr BP during the early Holocene and similar to 128 kyr BP during the early Eemian, slightly later compared to the onset of interglacial conditions on the adjacent land. Dinoflagellate cyst assemblages reveal higher sea-surface salinity (similar to 28-30) (e.g. Spiniferites pachydermus, Bitectatodinium tepikiense, and Spiniferites mirabilis) around similar to 126.5-121 kyr BP in comparison to the Holocene (similar to 15-20) as well as relatively high sea-surface temperature (e.g. Tuberculodinium vancampoae, S. pachydermus, and S. mirabilis) especially at similar to 127.6-125.3 kyr BP. Establishment of high sea-surface salinity during the Eemian correlates very well with reconstructed relatively high global sea-level and is explained as a combined effect of increased Mediterranean supply and high temperatures at the beginning of the last interglacial. The observed changes in the dinocyst record highlight the importance of nutrients for the composition of the Eemian and Holocene dinocyst assemblages. (C) 2013 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.marmicro.2013.02.001"],["dc.identifier.isi","000321536700012"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/29937"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1872-6186"],["dc.relation.issn","0377-8398"],["dc.title","Eemian and Holocene sea-surface conditions in the southern Black Sea: Organic-walled dinoflagellate cyst record from 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","1016"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","The Holocene"],["dc.bibliographiccitation.lastpage","1028"],["dc.bibliographiccitation.volume","30"],["dc.contributor.author","Unkelbach, Julia"],["dc.contributor.author","Kashima, Kaoru"],["dc.contributor.author","Punsalpaamuu, Gaadan"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Behling, Hermann"],["dc.date.accessioned","2020-12-10T18:38:28Z"],["dc.date.available","2020-12-10T18:38:28Z"],["dc.date.issued","2020"],["dc.description.abstract","The ‘Altai Tavan Bogd’ National Park in the north-western part of the Mongolian Altai, Central Asia, is located in a forest-steppe ecosystem. It occurs under the influence of extreme continental and montane climate and is sensitive to natural and anthropogenic impacts. High-resolution (\\u0026lt;20 years per sample) multi-proxy data of pollen, non-pollen palynomorphs (NPPs), macro-charcoal, diatoms, and XRF scanning from radiocarbon-dated lacustrine sediments reveal various environmental changes and the impact of different settlement periods for the late-Holocene. From 1350 to 820 cal. yr BP (AD 600–1130), the distribution of grass steppe indicates a climate similar to present-day conditions. Rapid improvements of climatic conditions (e.g. increased rainfall events) possibly favored a recovery of forest-steppe encouraging nomadic movements into alpine areas. In the period from 820 to 400 cal. yr BP (AD 1130–1550), the decline of forested areas suggests an increasingly drier and possibly colder climate. Some political shifts during the Mongol Empire (744–582 cal. yr BP; AD 1206–1368) favored variations in nomadic grazing habits. After 400 cal. yr BP (AD 1550), moisture and temperature increased slightly, and from ca. 40 cal. yr BP (AD 1910) to present, annual temperature continued to increase more markedly favoring an additional water availability due to permafrost degradation. Diatom data suggest several intervals of increased water availability in all periods which might have caused erosion due to heavier rainfall events or increased snow melt. Immediately after most of these high-water intervals, NPP data reveal periods of increased grazing activities in the area."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft \t https://doi.org/10.13039/501100001659"],["dc.identifier.doi","10.1177/0959683620908662"],["dc.identifier.eissn","1477-0911"],["dc.identifier.issn","0959-6836"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/77330"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation.eissn","1477-0911"],["dc.relation.issn","0959-6836"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.title","Decadal high-resolution multi-proxy analysis to reconstruct natural and human-induced environmental changes over the last 1350 cal. yr BP in the Altai Tavan Bogd National Park, western Mongolia"],["dc.type","journal_article"],["dc.type.internalPublication","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","591"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Vegetation History and Archaeobotany"],["dc.bibliographiccitation.lastpage","606"],["dc.bibliographiccitation.volume","28"],["dc.contributor.author","Setyaningsih, Christina A."],["dc.contributor.author","Behling, Hermann"],["dc.contributor.author","Saad, Asmadi"],["dc.contributor.author","Shumilovskikh, Lyudmila S."],["dc.contributor.author","Sabiham, Supiandi"],["dc.contributor.author","Biagioni, Siria"],["dc.date.accessioned","2020-12-10T14:10:14Z"],["dc.date.available","2020-12-10T14:10:14Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1007/s00334-019-00716-7"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/70688"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.relation","SFB 990: Ökologische und sozioökonomische Funktionen tropischer Tieflandregenwald-Transformationssysteme (Sumatra, Indonesien)"],["dc.relation","SFB 990 | A | A01: Langzeitliche Vegetationsveränderungen, Pflanzenphänologie und Pflanzen-Bestäuber-Interaktionen in Regenwald und Regenwaldtransformationen in Zentral-Sumatra"],["dc.relation.orgunit","Abteilung Palynologie und Klimadynamik"],["dc.subject.gro","sfb990_journalarticles"],["dc.title","First palaeoecological evidence of buffalo husbandry and rice cultivation in the Kerinci Seblat National Park in Sumatra, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]