Data set on sedimentology, palaeoecology and chronology of Middle to Late Pleistocene deposits on the Taimyr Peninsula, Arctic Russia
Möller, Per LU
; Benediktsson, Ivar Örn
; ANJAR, JOHANNA
LU
; Bennike, Ole
; Bernhardson, Martin
LU
; Funder, Svend
; Håkansson, Lena
; Lemdahl, Geoffrey
; Licciardi, Joseph
and Murray, Andrew S.
, et al.
(2019)
In Data in Brief
25.
- Abstract
- This Data in Brief paper contains data (including images) from Quaternary sedimentary successions investigated along the Bol’shaya Balakhnya River and the Luktakh–Upper Taimyra–Logata river system on southern Taimyr Peninsula, NW Siberia (Russia). Marine foraminifera and mollusc fauna composition, extracted from sediment samples, is presented. The chronology (time of deposition) of the sediment successions is reconstructed from three dating methods; (i) radiocarbon dating of organic detritus (from lacustrine/fluvial sediment) and molluscs (marine sediment) as finite ages (usually <42 000 years) or as non-finite ages (>42 000–48 000 years) on samples/sediments beyond the radiocarbon dating limit; (ii) Electron Spin Resonance (ESR)... (More)
- This Data in Brief paper contains data (including images) from Quaternary sedimentary successions investigated along the Bol’shaya Balakhnya River and the Luktakh–Upper Taimyra–Logata river system on southern Taimyr Peninsula, NW Siberia (Russia). Marine foraminifera and mollusc fauna composition, extracted from sediment samples, is presented. The chronology (time of deposition) of the sediment successions is reconstructed from three dating methods; (i) radiocarbon dating of organic detritus (from lacustrine/fluvial sediment) and molluscs (marine sediment) as finite ages (usually <42 000 years) or as non-finite ages (>42 000–48 000 years) on samples/sediments beyond the radiocarbon dating limit; (ii) Electron Spin Resonance (ESR) dating on marine molluscs (up to ages >400 000 years); (iii) Optically Stimulated Luminescence (OSL) dating, usually effective up to 100-150 0000 years. Terrestrial Cosmogenic Nuclide (TCN) exposure dating has been applied to boulders resting on top of moraine ridges (Ice Marginal Zones). See [1] (doi.org/10.1016/j.earscirev.2019.04.004) for interpretation and discussion of all data. (Less)
- Abstract (Swedish)
- This Data in Brief paper contains data (including images) from Quaternary sedimentary successions investigated along the Bol’shaya Balakhnya River and the Luktakh–Upper Taimyra–Logata river system on southern Taimyr Peninsula, NW Siberia (Russia). Marine foraminifera and mollusc fauna composition, extracted from sediment samples, is presented. The chronology (time of deposition) of the sediment successions is reconstructed from three dating methods; (i) radiocarbon dating of organic detritus (from lacustrine/fluvial sediment) and molluscs (marine sediment) as finite ages (usually <42 000 years) or as non-finite ages (>42 000–48 000 years) on samples/sediments beyond the radiocarbon dating limit; (ii) Electron Spin Resonance (ESR)... (More)
- This Data in Brief paper contains data (including images) from Quaternary sedimentary successions investigated along the Bol’shaya Balakhnya River and the Luktakh–Upper Taimyra–Logata river system on southern Taimyr Peninsula, NW Siberia (Russia). Marine foraminifera and mollusc fauna composition, extracted from sediment samples, is presented. The chronology (time of deposition) of the sediment successions is reconstructed from three dating methods; (i) radiocarbon dating of organic detritus (from lacustrine/fluvial sediment) and molluscs (marine sediment) as finite ages (usually <42 000 years) or as non-finite ages (>42 000–48 000 years) on samples/sediments beyond the radiocarbon dating limit; (ii) Electron Spin Resonance (ESR) dating on marine molluscs (up to ages >400 000 years); (iii) Optically Stimulated Luminescence (OSL) dating, usually effective up to 100-150 0000 years. Terrestrial Cosmogenic Nuclide (TCN) exposure dating has been applied to boulders resting on top of moraine ridges (Ice Marginal Zones). See Möller et al. (in press) for further interpretation and discussion. (Less)
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/f8cb3669-4600-4ef0-976c-6a3125efa624
- author
- Möller, Per
LU
; Benediktsson, Ivar Örn
; ANJAR, JOHANNA
LU
; Bennike, Ole
; Bernhardson, Martin
LU
; Funder, Svend
; Håkansson, Lena
; Lemdahl, Geoffrey
; Licciardi, Joseph
and Murray, Andrew S.
, et al. (More)
- Möller, Per
LU
; Benediktsson, Ivar Örn
; ANJAR, JOHANNA
LU
; Bennike, Ole
; Bernhardson, Martin
LU
; Funder, Svend
; Håkansson, Lena
; Lemdahl, Geoffrey
; Licciardi, Joseph
; Murray, Andrew S.
and Seidenkrantz, Marit-Solveig
(Less)
- organization
- publishing date
- 2019-07-09
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- Glacial sedimentology, Glacial history, Kara Sea Ice Sheet, OSL dating, ESR dating, TCN dating
- in
- Data in Brief
- volume
- 25
- article number
- 104267
- publisher
- Elsevier
- external identifiers
-
- scopus:85069853250
- pmid:31388521
- ISSN
- 2352-3409
- DOI
- 10.1016/j.dib.2019.104267
- project
- Taymyr revisited - a quest for former Eurasian Ice Sheets margins and megafauna extinction during the last glacial cycles
- language
- English
- LU publication?
- yes
- id
- f8cb3669-4600-4ef0-976c-6a3125efa624
- date added to LUP
- 2019-04-08 14:32:13
- date last changed
- 2022-04-25 22:19:32
@article{f8cb3669-4600-4ef0-976c-6a3125efa624,
abstract = {{This Data in Brief paper contains data (including images) from Quaternary sedimentary successions investigated along the Bol’shaya Balakhnya River and the Luktakh–Upper Taimyra–Logata river system on southern Taimyr Peninsula, NW Siberia (Russia). Marine foraminifera and mollusc fauna composition, extracted from sediment samples, is presented. The chronology (time of deposition) of the sediment successions is reconstructed from three dating methods; (i) radiocarbon dating of organic detritus (from lacustrine/fluvial sediment) and molluscs (marine sediment) as finite ages (usually <42 000 years) or as non-finite ages (>42 000–48 000 years) on samples/sediments beyond the radiocarbon dating limit; (ii) Electron Spin Resonance (ESR) dating on marine molluscs (up to ages >400 000 years); (iii) Optically Stimulated Luminescence (OSL) dating, usually effective up to 100-150 0000 years. Terrestrial Cosmogenic Nuclide (TCN) exposure dating has been applied to boulders resting on top of moraine ridges (Ice Marginal Zones). See [1] (doi.org/10.1016/j.earscirev.2019.04.004) for interpretation and discussion of all data.}},
author = {{Möller, Per and Benediktsson, Ivar Örn and ANJAR, JOHANNA and Bennike, Ole and Bernhardson, Martin and Funder, Svend and Håkansson, Lena and Lemdahl, Geoffrey and Licciardi, Joseph and Murray, Andrew S. and Seidenkrantz, Marit-Solveig}},
issn = {{2352-3409}},
keywords = {{Glacial sedimentology; Glacial history; Kara Sea Ice Sheet; OSL dating; ESR dating; TCN dating}},
language = {{eng}},
month = {{07}},
publisher = {{Elsevier}},
series = {{Data in Brief}},
title = {{Data set on sedimentology, palaeoecology and chronology of Middle to Late Pleistocene deposits on the Taimyr Peninsula, Arctic Russia}},
url = {{http://dx.doi.org/10.1016/j.dib.2019.104267}},
doi = {{10.1016/j.dib.2019.104267}},
volume = {{25}},
year = {{2019}},
}