Radiocarbon ages from the organic plant material from the ice wedge surrounding deposits in the Chara Basin, northern Transbaikalia, Russia

Radiocarbon ages from the organic plant material from the ice wedge surrounding deposits in the 6-8 m Chara River terrace in 1985 and 1988 sampling years.Samples of organic material for radiocarbon age determination have been selected in several parts of 8-m terrace. 14C ages have been obtained in R...

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Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Vasil'chuk, Alla Constantinovna, Stanilovskaya, Julia V
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2020
Subjects:
Holocene
ice wedge
Northern Transbaikalia
Southern permafrost areas
Stable isotopes
Event label
Latitude of event
Longitude of event
Comment of event
Sample ID
DEPTH, sediment/rock
Material
Laboratory code/label
AGE
Age, error
Calendar age, maximum/old
Calendar age, minimum/young
Age, 14C
Age, 14C calibrated, IntCal13 Reimer et al., 2013
Reimer
Ice
permafrost
wedge*
Online Access:https://dx.doi.org/10.1594/pangaea.915926
https://doi.pangaea.de/10.1594/PANGAEA.915926
Description
Summary:Radiocarbon ages from the organic plant material from the ice wedge surrounding deposits in the 6-8 m Chara River terrace in 1985 and 1988 sampling years.Samples of organic material for radiocarbon age determination have been selected in several parts of 8-m terrace. 14C ages have been obtained in Radiocarbon Laboratory of GIN RAS (L.D.Sulerzhitsky) and in Radiocarbon Laboratory of the Institute of Geology of Estonia (R.A.Rayamyae). The obtained conventional 14C ages were calibrated using the IntCal13 calibration curve after Reimer et al. (2013, doi:10.2458/azu_js_rc.55.16947).

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