U-Th chronology results of Siberian and Mongolian speleothems, data used as the basis of a scientific paper. (NERC Grant NE/G013829/1)

The data presented in the Table 1 are U-Th chronology results of Siberian and Mongolian speleothems. This data is a basis for a scientific paper of Vaks, A. et al. (2013) "Speleothems Reveal 500,000-Year History of Siberian Permafrost." Science 340 (6129): 183-186. The table shows the ages of 111 layers of 36 speleothems taken from the six caves of Siberia and Mongolia. Vadose speleothems grow in caves of unsaturated zone when atmospheric water infiltrates into the caves from the surface. Therefore these speleothems cannot grow in permafrost, as well as in dry desert conditions. Therefore in Siberia the periods of speleothem growth show intervals during which the Siberian permafrost thawed and became discontinuous or absent. In Mongolian Gobi Desert the speleothem deposition periods show when the desert was both humid than present and warm enough to enable water infiltration into the caves. The data presented in tables 2 and 3 are OxCal-4.1 modeling results of the Table 1 chronology data for the Holocene (Table 2) and Marine Isotopic Stage (MIS) 5.5 (Table 3). The tables show exact durations of Holocene and MIS-5.5 permafrost thawing periods in Botovskaya and Okhotnichya Caves.
 
Citation proposal
. U-Th chronology results of Siberian and Mongolian speleothems, data used as the basis of a scientific paper. (NERC Grant NE/G013829/1). https://metadata.bgs.ac.uk/geonetwork/srv/api/records/36697b8a-5f1f-2ec7-e054-002128a47908

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Date ( Creation )
2016-06-22
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http://data.bgs.ac.uk/id/dataHolding/13606940

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GEMET - INSPIRE themes
  • Geology
Keywords
  • NERC_DDC
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The copyright of materials derived from the British Geological Survey's work is vested in the Natural Environment Research Council [NERC]. No part of this work may be reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright holder, via the BGS Intellectual Property Rights Manager. Use by customers of information provided by the BGS, is at the customer's own risk. In view of the disparate sources of information at BGS's disposal, including such material donated to BGS, that BGS accepts in good faith as being accurate, the Natural Environment Research Council (NERC) gives no warranty, expressed or implied, as to the quality or accuracy of the information supplied, or to the information's suitability for any use. NERC/BGS accepts no liability whatever in respect of loss, damage, injury or other occurence however caused.
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Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]"
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  • Geoscientific information
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Supplemental Information
The locations of the caves are as follows: 1) Lenskaya Ledyanaya Cave - 60°22'15.60""N-116°56'47.30""E 2) Botovskaya Cave - 55°18'56.83""N-105°19'28.58""E 3) Okhotnichya Cave - 52°07'40.56""N-105°29'10.76""E 4) Shar-Khana Cave - 45°35'23.1""N-108°19'18.8""E 5) Gurvan Ze’erd Cave - 42°30'15.7""N-107°27'00.1""E 6) Lovon Chombo Cave - 42°35'18.4""N-107°49'32.0""E"

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http://www.bgs.ac.uk/services/ngdc/accessions/index.html#item59589  
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2011
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See the referenced specification
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Date ( Publication )
2010-12-08
Explanation
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
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false
Statement
Lineage information may be available in the paper, Speleothems Reveal 500,000-Year History of Siberian Permafrost. https://dx.doi.org/10.1126/science.1228729

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dataset Dataset
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2021-04-22
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