Anatoly V Lozhkin

Biographic Data

ID10759667
NAMEAnatoly V Lozhkin
GIVEN NAMESAnatoly V
FAMILY NAMELozhkin
SIGNATURELOZHKIN A V
AFFILIATIONSNorth East Interdisciplinary Science Research Institute N.A. Shilo, Far East Branch Russian Academy of Sciences, Russia
VERIFIEDNo
TOTAL WORKS15
TOTAL CITATIONS23
WORKS AS AUTHOR15
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1993
LATEST PUBLICATION YEAR2026
H-INDEX2

  • Middle and Late-Holocene coastal environments of far Southeastern Russia as inferred from palynological and diatom data

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEThe Holocene2026References: 25

    Existing discontinuous palynological records from coastal and river valley exposures, with varying quality of radiocarbon control, suggested that the regional Holocene climate in southern areas of the Russian Far East was characterized by as many as 10 fluctuations in temperature and/or precipitation. In this study, palynological data from Zerkalnoye Lake, located on the western coast of the Sea of Japan, indicate a gradual decline in temperature…

  • The Enmynveem mammoth and vegetation changes in arctic Chukotka during the Late Quaternary

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research2024

    Mining operations in the Enmynveem valley, northeastern Siberia, exposed a well-preserved right hind leg of Mammuthus primigenius (woolly mammoth), dated to ca. 37,500 cal yr BP. The leg had a fracture that crosscut the midsections of the tibia and fibula. Additional skeletal and soft tissue remains, including two mummified adults (Berezovka, ca. 47,200 cal yr BP; Bolshoi Lyakhovsky, ca. 37,000 cal yr BP), document the presence of mammoths in int…

  • The role of lake basin history on palynological records from the Upper Kolyma region (northeastern Siberia)

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research2023

    Paleoecological and modern studies at Priyatnoye Lake, which is located within an intermontane depression in the interior of northeastern Siberia, indicate a similar paleovegetation record as has been documented for nearby mountain valleys, but a history of basin stability and instability that is uncharacteristic of the valley lakes. Analyses of a 385-cm-long core from the western basin of Priyatnoye Lake shows that sediment accumulation began in…

  • Another perspective on the age and origin of the Berelyokh mammoth site

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research2019

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  • Another perspective on the age and origin of the Berelyokh mammoth site (northeast Siberia)

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research2018

    The Berelyokh site includes an exceptional bone horizon consisting of 8431 remains of Mammuthus primigenius. Previous investigations, spanning ~40 years, concluded that the deaths and bone concentration were caused by spring flooding, possibly related to wetter Bølling climates. We review work from these studies with emphasis on under-reported palynological data to provide more detail on paleoenvironmental reconstructions and an alternative inter…

  • Preliminary paleoenvironmental analysis of permafrost deposits at Batagaika megaslump, Yana Uplands, northeast Siberia

    Open AccessJulian B Murton, Mary E Edwards et al.ARTICLEQuaternary Research2017

    A megaslump at Batagaika, in northern Yakutia, exposes a remarkable stratigraphic sequence of permafrost deposits ~50–80 m thick. To determine their potential for answering key questions about Quaternary environmental and climatic change in northeast Siberia, we carried out a reconnaissance study of their cryostratigraphy and paleoecology, supported by four rangefinder 14 C ages. The sequence includes two ice complexes separated by a unit of fine…

  • Western Beringia (Northeast Asia)

    Open AccessSergey B Slobodin, Patricia M Anderson et al.CHAPTERHuman Colonization of the Arctic…2017

  • Biome changes and their inferred climatic drivers in northern and eastern continental Asia at selected times since 40 cal ka bp

    Open AccessFang Tian, Xianyong Cao et al.ARTICLEVegetation History and…2017Cited by: 3References: 5

  • Late glacial and holocene landscapes of central Beringia

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research2011

    New palynological and sedimentological data from St. Lawrence Island present a rare view into late-glacial and Holocene environments of the central Bering Land Bridge. The late glaciation was a time of dynamic landscape changes in south-central Beringia, with active thermokarst processes, including the formation and drainage of thaw lakes. The presence of such a wet, unstable substrate, if widespread, probably would have had an adverse impact on …

  • Paleoclimatic implications of glacial and postglacial refugia for Pinus pumila in western Beringia

    Open AccessPatricia M Anderson, Anatoly Lozhkin et al.ARTICLEQuaternary Research2010

    Palynological results from Julietta Lake currently provide the most direct evidence to support the existence of a glacial refugium for Pinus pumila in mountains of southwestern Beringia. Both percentages and accumulation rates indicate the evergreen shrub survived until at least ∼ 19,000 14 C yr BP in the Upper Kolyma region. Percentage data suggest numbers dwindled into the late glaciation, whereas pollen accumulation rates point towards a more …

  • Effects of sample mass and macrofossil type on radiocarbon dating of arctic and boreal lake sediments

    Open AccessW Wyatt Oswald, Patricia M Anderson et al.ARTICLEThe Holocene2005Cited by: 20References: 10

    Dating lake sediments by accelerator mass spectrometry (AMS) 14C analysis of terrestrial plant macrofossils overcomes one of the main problems associated with dating bulk sediment samples, i.e., the presence of old organic matter. Even so, many AMS dates from arctic and boreal sites appear to misrepresent the age of the sediment. To understand the nature of these apparent dating anomalies better, we conducted a series of 14C dating experiments us…

  • Implications of a 24,000-Yr Palynological Record for a Younger Dryas Cooling and for Boreal Forest Development in Northeastern Siberia

    Open AccessPatricia M Anderson, Anatoly Lozhkin et al.ARTICLEQuaternary Research2002

    A sediment core from Smorodinovoye Lake (SML), northeastern Siberia (area to the east of the Verkhoyansk Range) spanning the last 24,000 14 C yr indicates that vegetational and climatic changes in the upper Indigirka basin resemble those in eastern Siberia (Lena basin and westward). For example, maximum postglacial summer temperatures at SML probably occurred 6000–4000 14 C yr B.P., an age more in accordance with eastern than northeastern records…

  • A lacustrine pollen record from near altitudinal forest limit, Upper Kolyma Region, northeastern Siberia

    Open AccessPatricia M Anderson, Anatoly Lozhkin et al.ARTICLEThe Holocene1997References: 1

    A sediment core that spans the last c. 15 000 yr BP was raised from Elgennya Lake (62°05'N 149°00'E, 1040 m) which is located near the altitudinal forest limit in the western Annachag Mountains of the Upper Kolyma region, northeastern Siberia. Palynological data indicate the presence of a relatively unpro ductive herb-Salix tundra during full-glacial times. Although Betula shrubs first appeared in this upland valley at c. 12 100 yr BP, they proba…

  • The Last Interglaciation in Northeast Siberia

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research1995

    Alluvial, fluvial, and organic deposits of the last interglaciation are exposed along numerous river terraces in northeast Siberia. Although chronological control is often poor, the paleobotanical data suggest range extensions of up to 1000 km for the primary tree species. These data also indicate that boreal communities of the last interglaciation were similar to modern ones in composition, but their distributions were displaced significantly to…

  • Late Quaternary Lacustrine Pollen Records from Southwestern Beringia

    Open AccessAnatoly Lozhkin, Anatoly V Lozhkin et al.ARTICLEQuaternary Research1993

    Sediment cores from three lakes in the Upper Kolyma region, northeast Russia, provide the first well-dated continuous record of late Quaternary vegetation change from far southwestern Beringia. The oldest pollen zone, tentatively assigned to the Karginsk (mid-Wisconsinan) Interstade, indicates an Artemisia shrub tundra with Pinus pumila , Betula , and Alnus at mid- to low elevations. With the onset of the Sartan (late Wisconsinan) Stade, Pinus di…