{"refrec":{"BRefID":209263,"RR":"<b>Fedotov, A. P.; Chebykin, E.P.; Yu Semenov, M.; Vorobyova, S.S. ; Yu Osipov, E.; Golobokova, L.P.; Pogodaeva, T.V.; Zheleznyakova, T.O.; Grachev, M.A.; Tomurhuu, D.; Oyunchimeg, Ts.; Narantsetseg, Ts.; Tomurtogoo, O.; Dolgikh, P.T.; Arsenyuk, M.I.; De Batist, M.</b> (2004). Changes in the volume and salinity of Lake Khubsugul (Mongolia) in response to global climate changes in the upper Pleistocene and the Holocene. <i>Palaeogeogr. Palaeoclimatol. Palaeoecol. 209(1-4)</i>: 245-257. <a href=\"http://dx.doi.org/10.1016/j.palaeo.2003.12.022\" target=\"_blank\">dx.doi.org/10.1016/j.palaeo.2003.12.022</a>","BEntID":201248,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Palaeogeogr. Palaeoclimatol. Palaeoecol. 209(1-4)</i>: 245-257. <a href=\"https://dx.doi.org/10.1016/j.palaeo.2003.12.022\" target=\"_blank\">https://dx.doi.org/10.1016/j.palaeo.2003.12.022</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Fedotov, A. P.; Chebykin, E.P.; Yu Semenov, M.; Vorobyova, S.S. ; Yu Osipov, E.; Golobokova, L.P.; Pogodaeva, T.V.; Zheleznyakova, T.O.; Grachev, M.A.; Tomurhuu, D.; Oyunchimeg, Ts.; Narantsetseg, Ts.; Tomurtogoo, O.; Dolgikh, P.T.; Arsenyuk, M.I.; De Batist, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Fedotov, A. P. <i>et al.</i>","Englishabstract":"Two gravity cores (1.1 and 2.2 m long) of deep-water bottom sediments from Lake Khubsugul (Mongolia) were studied. The Holocene, biogenic silica and organic matter-rich part of the first core was subjected to AMS radiocarbon dating which placed the date of dramatic increase of pelagic diatoms (40 cm below sediment surface) at a calendar age of 11.5 cal ky BP. ICP-MS analysis of weak nitric acid extracts revealed that the upper Pleistocene, compared to the Holocene samples, were enriched in Ca, C<sub>inorg</sub>, Sr, Mg and depleted of U, W, Sb, V and some other elements. Transition to the Holocene resulted in an increase of total diatoms from 0 to 10<sup>8</sup> g<sup>-1</sup>, of BiSi from 1% to 20%, of organic matter from <1% to >6%. The Bølling–Allerød–Younger Dryas–Holocene abrupt climate oscillations manifested themselves in oscillations of geochemical proxies. A remarkable oscillation also occurred at 22 cm (ca. 5.5 ky BP). The Pleistocene section of the second, longer core was enriched in carbonate CO<sub>2</sub> (up to 10%) and water-extractable SO<sub>4</sub><sup>2-</sup> (up to 300 times greater than that in Holocene pore waters). All this evidence is in an accord with the earlier finding of drowned paleo-deltas at ca. 170 m below the modern lake surface of the lake [Dokl. Akad. Nauk 382 (2002) 261] and suggests that, due to low (ca. 110 mm) regional precipitation at the end of the Pleistocene, Lake Khubsugul was only 100 m deep, and that its volume was ca. 10 times less than today.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Changes in the volume and salinity of Lake Khubsugul (Mongolia) in response to global climate changes in the upper Pleistocene and the Holocene","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Paleoclimate; Lake Khubsugul level change; LGM; Holocene; Mongolia","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2018-05-17","DateCreate":"2011-11-04","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000222544100016","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.palaeo.2003.12.022"},"refs":null,"anarec":{"AnaID":209263,"PubliDate":2004,"Pagination":"245-257","XtraPublOfAnaID":null,"ISBN":null,"Volume":"209","Issue":"1-4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43483,"SerRR":"Palaeogeography, Palaeoclimatology, Palaeoecology. 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