Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Deglaciation history of Lake Ladoga (northwestern Russia) based on varved sediments. / Gromig, Raphael; Wagner, Bernd; Wennrich, Volker; Fedorov, Grigory; Savelieva, Larisa; Lebas, Elodie; Krastel, Sebastian; Brill, Dominik; Andreev, Andrei; Subetto, Dmitry; Melles, Martin.
в: Boreas, Том 48, № 2, 01.04.2019, стр. 330-348.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Deglaciation history of Lake Ladoga (northwestern Russia) based on varved sediments
AU - Gromig, Raphael
AU - Wagner, Bernd
AU - Wennrich, Volker
AU - Fedorov, Grigory
AU - Savelieva, Larisa
AU - Lebas, Elodie
AU - Krastel, Sebastian
AU - Brill, Dominik
AU - Andreev, Andrei
AU - Subetto, Dmitry
AU - Melles, Martin
PY - 2019/4/1
Y1 - 2019/4/1
N2 - Lake Ladoga in northwestern Russia is Europe's largest lake. The postglacial history of the Ladoga basin is for the first time documented continuously with high temporal resolution in the upper 13.3m of a sediment core (Co1309) from the northwestern part of the lake. We applied a multiproxy approach including radiographic imaging, (bio-)geochemical and granulometric analyses. Age control was established combining radiocarbon dating with varve chronology, the latter anchored to a correlated radiocarbon age from a lake close by. The age-depth model reveals the onset of glacial varve sedimentation at 13910 +/- 140cal. a BP, when Lake Ladoga was part of the Baltic Ice Lake. Linear extrapolation of published retreat rates of the Scandinavian Ice Sheet provides a formation age of the Luga moraine close to Lake Ladoga's southern shore of 14.5-15.9cal. ka BP, older than previously assumed. Varve sedimentation covers the BOlling/AllerOd interstadial, the Younger Dryas stadial and the Early Holocene. Varve-thickness variations, conjoined with grain-size and geochemical variations, inform about the relative position of the Scandinavian Ice Sheet and the climate during the deglaciation phase. The upper limit of the varved succession marks the change from glaciolacustrine to normal lacustrine sedimentation and post-dates the drainage of the Baltic Ice Lake as well as the formation of the Salpausselka II moraine north of Lake Ladoga, by c.250years. The Holocene sediment record is divided into three periods in the following order: (i) a lower transition zone between the Holocene boundary and c.9.5cal. ka BP, characterized by mostly massive sediments with low organic content, (ii) a phase with increased organic content from c.9.5 to 4.5cal. ka BP corresponding to the Holocene Thermal Maximum, and (iii) a phase with relatively stable sedimentation in a lacustrine environment from c.4.5cal. ka BP until present.
AB - Lake Ladoga in northwestern Russia is Europe's largest lake. The postglacial history of the Ladoga basin is for the first time documented continuously with high temporal resolution in the upper 13.3m of a sediment core (Co1309) from the northwestern part of the lake. We applied a multiproxy approach including radiographic imaging, (bio-)geochemical and granulometric analyses. Age control was established combining radiocarbon dating with varve chronology, the latter anchored to a correlated radiocarbon age from a lake close by. The age-depth model reveals the onset of glacial varve sedimentation at 13910 +/- 140cal. a BP, when Lake Ladoga was part of the Baltic Ice Lake. Linear extrapolation of published retreat rates of the Scandinavian Ice Sheet provides a formation age of the Luga moraine close to Lake Ladoga's southern shore of 14.5-15.9cal. ka BP, older than previously assumed. Varve sedimentation covers the BOlling/AllerOd interstadial, the Younger Dryas stadial and the Early Holocene. Varve-thickness variations, conjoined with grain-size and geochemical variations, inform about the relative position of the Scandinavian Ice Sheet and the climate during the deglaciation phase. The upper limit of the varved succession marks the change from glaciolacustrine to normal lacustrine sedimentation and post-dates the drainage of the Baltic Ice Lake as well as the formation of the Salpausselka II moraine north of Lake Ladoga, by c.250years. The Holocene sediment record is divided into three periods in the following order: (i) a lower transition zone between the Holocene boundary and c.9.5cal. ka BP, characterized by mostly massive sediments with low organic content, (ii) a phase with increased organic content from c.9.5 to 4.5cal. ka BP corresponding to the Holocene Thermal Maximum, and (iii) a phase with relatively stable sedimentation in a lacustrine environment from c.4.5cal. ka BP until present.
KW - SCANDINAVIAN ICE-SHEET
KW - LAST GLACIAL MAXIMUM
KW - TEMPERATURE RECONSTRUCTION
KW - SOUTHEASTERN SECTOR
KW - HOLOCENE CLIMATE
KW - OXYGEN-ISOTOPE
KW - BALTIC SEA
KW - AGE
KW - RECORDS
KW - SINGLE
UR - http://www.scopus.com/inward/record.url?scp=85061476103&partnerID=8YFLogxK
U2 - 10.1111/bor.12379
DO - 10.1111/bor.12379
M3 - Article
AN - SCOPUS:85061476103
VL - 48
SP - 330
EP - 348
JO - Boreas
JF - Boreas
SN - 0300-9483
IS - 2
ER -
ID: 39117649