Abstract This study focused on the luminescence dating of sediments from Lake El'gygytgyn, a meteorite impact crater 100 km north of the Arctic Circle in northeast Siberia, formed 3.58 Ma ago. The sediment is principally eolian deposited in to a lake with nearly permanently ice. The fine-graine...

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Main Authors: S L Forman, Ae J Pierson, Ae J Gó Mez, J Brigham-Grette, N R Nowaczyk, M Melles, Steven L Forman, A E James, Pierson Ae, Jeaneth Gó, Julie Ae, Brigham-Grette, Norbert R Nowaczyk Ae, Martin Ae, Melles
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7189
http://www.geo.umass.edu/lake_e/publications/Forman2007.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1051.7189 2023-05-15T15:01:55+02:00 S L Forman Ae J Pierson Ae J Gó Mez J Brigham-Grette N R Nowaczyk M Melles Steven L Forman A E James Pierson Ae Jeaneth Gó Julie Ae Brigham-Grette Norbert R Nowaczyk Ae Martin Ae Melles The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7189 http://www.geo.umass.edu/lake_e/publications/Forman2007.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7189 http://www.geo.umass.edu/lake_e/publications/Forman2007.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geo.umass.edu/lake_e/publications/Forman2007.pdf text 2007 ftciteseerx 2020-04-12T00:15:00Z Abstract This study focused on the luminescence dating of sediments from Lake El'gygytgyn, a meteorite impact crater 100 km north of the Arctic Circle in northeast Siberia, formed 3.58 Ma ago. The sediment is principally eolian deposited in to a lake with nearly permanently ice. The fine-grained polymineral and quartz extracts taken from nine distinct levels from the upper 12.3 m of sediment core PG1351 were dated by infrared stimulated (IRSL) and green stimulated luminescence (GSL) using multiple aliquot additive dose procedures. The veracity of these ages is evaluated by comparing to an age model for the core derived from magnetic excursions and from correlation of variations of the magnetic susceptibility record to similar magnitude variations in d 18 O in the Greenland Ice core record. The IRSL ages from the upper 9 m of core correspond well with the independent age control for the past ca. 200 ka. However, sediments deeper in the core at 12.3 m with an inferred age of ca. 250 ka age yield a saturated IRSL response and therefore a non-finite OSL age. The youngest sediment dated from 0.70 m depth yielded the IRSL age of ca. 11.5 ka, older than the corresponding age of 9.3-8.8 ka, indicating a discrepancy in dating the youngest sediments in the upper 1 m of core. This study confirms the utility of IRSL by the multiple aliquot additive dose method to date sediments < 200 ka old from eastern Siberia. Keywords Luminescence dating AE Arctic lake AE Geochronology AE Siberia Introduction A prerequisite to forward paleoenvironmental interpretations of lacustrine systems is the determination of an absolute chronology for individual This is the sixth in a series of eleven papers published in this special issue dedicated to initial studies of El'gygytgyn Crater Lake and its catchment in NE Russia. Julie Brigham-Grette, Martin Melles, Pavel Minyuk were guest editors of this special issue. Text Arctic Greenland Greenland ice core ice core Magnetic susceptibility Siberia Unknown Arctic Arctic Lake ENVELOPE(-130.826,-130.826,57.231,57.231) Brigham ENVELOPE(162.300,162.300,-77.117,-77.117) Crater Lake ENVELOPE(-60.667,-60.667,-62.983,-62.983) Greenland
institution Open Polar
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description Abstract This study focused on the luminescence dating of sediments from Lake El'gygytgyn, a meteorite impact crater 100 km north of the Arctic Circle in northeast Siberia, formed 3.58 Ma ago. The sediment is principally eolian deposited in to a lake with nearly permanently ice. The fine-grained polymineral and quartz extracts taken from nine distinct levels from the upper 12.3 m of sediment core PG1351 were dated by infrared stimulated (IRSL) and green stimulated luminescence (GSL) using multiple aliquot additive dose procedures. The veracity of these ages is evaluated by comparing to an age model for the core derived from magnetic excursions and from correlation of variations of the magnetic susceptibility record to similar magnitude variations in d 18 O in the Greenland Ice core record. The IRSL ages from the upper 9 m of core correspond well with the independent age control for the past ca. 200 ka. However, sediments deeper in the core at 12.3 m with an inferred age of ca. 250 ka age yield a saturated IRSL response and therefore a non-finite OSL age. The youngest sediment dated from 0.70 m depth yielded the IRSL age of ca. 11.5 ka, older than the corresponding age of 9.3-8.8 ka, indicating a discrepancy in dating the youngest sediments in the upper 1 m of core. This study confirms the utility of IRSL by the multiple aliquot additive dose method to date sediments < 200 ka old from eastern Siberia. Keywords Luminescence dating AE Arctic lake AE Geochronology AE Siberia Introduction A prerequisite to forward paleoenvironmental interpretations of lacustrine systems is the determination of an absolute chronology for individual This is the sixth in a series of eleven papers published in this special issue dedicated to initial studies of El'gygytgyn Crater Lake and its catchment in NE Russia. Julie Brigham-Grette, Martin Melles, Pavel Minyuk were guest editors of this special issue.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author S L Forman
Ae J Pierson
Ae J Gó Mez
J Brigham-Grette
N R Nowaczyk
M Melles
Steven L Forman
A E James
Pierson Ae
Jeaneth Gó
Julie Ae
Brigham-Grette
Norbert R Nowaczyk Ae
Martin Ae
Melles
spellingShingle S L Forman
Ae J Pierson
Ae J Gó Mez
J Brigham-Grette
N R Nowaczyk
M Melles
Steven L Forman
A E James
Pierson Ae
Jeaneth Gó
Julie Ae
Brigham-Grette
Norbert R Nowaczyk Ae
Martin Ae
Melles
author_facet S L Forman
Ae J Pierson
Ae J Gó Mez
J Brigham-Grette
N R Nowaczyk
M Melles
Steven L Forman
A E James
Pierson Ae
Jeaneth Gó
Julie Ae
Brigham-Grette
Norbert R Nowaczyk Ae
Martin Ae
Melles
author_sort S L Forman
publishDate 2007
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1051.7189
http://www.geo.umass.edu/lake_e/publications/Forman2007.pdf
long_lat ENVELOPE(-130.826,-130.826,57.231,57.231)
ENVELOPE(162.300,162.300,-77.117,-77.117)
ENVELOPE(-60.667,-60.667,-62.983,-62.983)
geographic Arctic
Arctic Lake
Brigham
Crater Lake
Greenland
geographic_facet Arctic
Arctic Lake
Brigham
Crater Lake
Greenland
genre Arctic
Greenland
Greenland ice core
ice core
Magnetic susceptibility
Siberia
genre_facet Arctic
Greenland
Greenland ice core
ice core
Magnetic susceptibility
Siberia
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http://www.geo.umass.edu/lake_e/publications/Forman2007.pdf
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