The geochemical paradox of ice‐complex sediments in north Siberia
Abstract Icy silty deposits in northern Siberia, here termed ‘ice‐complex sediments’ (ICS), have a higher salinization than other continental deposits of Neogene‐Pleistocene age. Data for salinity (%) and the ratio of Ca ion content to Cl ion content for samples from the Yana‐Indigirskaya and Kolyms...
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crwiley:10.1002/ppp.3430060405 2024-06-02T08:08:01+00:00 The geochemical paradox of ice‐complex sediments in north Siberia Konishchev, V. N. Plakht, I. R. 1995 http://dx.doi.org/10.1002/ppp.3430060405 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060405 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060405 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 6, issue 4, page 337-343 ISSN 1045-6740 1099-1530 journal-article 1995 crwiley https://doi.org/10.1002/ppp.3430060405 2024-05-03T10:40:02Z Abstract Icy silty deposits in northern Siberia, here termed ‘ice‐complex sediments’ (ICS), have a higher salinization than other continental deposits of Neogene‐Pleistocene age. Data for salinity (%) and the ratio of Ca ion content to Cl ion content for samples from the Yana‐Indigirskaya and Kolymskaya lowlands indicate that the salinization of Pleistocene permafrost is lowest, that icy silts have salinities between 0.1% and 1.0%, and that recent floodplain, coastal and alas deposits have salinities greater than 1%. These differences are thought to reflect the phase change in gas‐liquid inclusions in crystals and rocks when they break and their contents (solutions) are released during freezing. This process is termed cryocryptogenesis. It is concluded that ICS deposits were formed under less humid and colder conditions than exist today in northern Yakutia, but more humid than central Yakutia. Article in Journal/Newspaper Ice permafrost Permafrost and Periglacial Processes Yakutia Siberia Wiley Online Library Kolymskaya ENVELOPE(158.702,158.702,68.729,68.729) Permafrost and Periglacial Processes 6 4 337 343 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Icy silty deposits in northern Siberia, here termed ‘ice‐complex sediments’ (ICS), have a higher salinization than other continental deposits of Neogene‐Pleistocene age. Data for salinity (%) and the ratio of Ca ion content to Cl ion content for samples from the Yana‐Indigirskaya and Kolymskaya lowlands indicate that the salinization of Pleistocene permafrost is lowest, that icy silts have salinities between 0.1% and 1.0%, and that recent floodplain, coastal and alas deposits have salinities greater than 1%. These differences are thought to reflect the phase change in gas‐liquid inclusions in crystals and rocks when they break and their contents (solutions) are released during freezing. This process is termed cryocryptogenesis. It is concluded that ICS deposits were formed under less humid and colder conditions than exist today in northern Yakutia, but more humid than central Yakutia. |
format |
Article in Journal/Newspaper |
author |
Konishchev, V. N. Plakht, I. R. |
spellingShingle |
Konishchev, V. N. Plakht, I. R. The geochemical paradox of ice‐complex sediments in north Siberia |
author_facet |
Konishchev, V. N. Plakht, I. R. |
author_sort |
Konishchev, V. N. |
title |
The geochemical paradox of ice‐complex sediments in north Siberia |
title_short |
The geochemical paradox of ice‐complex sediments in north Siberia |
title_full |
The geochemical paradox of ice‐complex sediments in north Siberia |
title_fullStr |
The geochemical paradox of ice‐complex sediments in north Siberia |
title_full_unstemmed |
The geochemical paradox of ice‐complex sediments in north Siberia |
title_sort |
geochemical paradox of ice‐complex sediments in north siberia |
publisher |
Wiley |
publishDate |
1995 |
url |
http://dx.doi.org/10.1002/ppp.3430060405 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430060405 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430060405 |
long_lat |
ENVELOPE(158.702,158.702,68.729,68.729) |
geographic |
Kolymskaya |
geographic_facet |
Kolymskaya |
genre |
Ice permafrost Permafrost and Periglacial Processes Yakutia Siberia |
genre_facet |
Ice permafrost Permafrost and Periglacial Processes Yakutia Siberia |
op_source |
Permafrost and Periglacial Processes volume 6, issue 4, page 337-343 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430060405 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
6 |
container_issue |
4 |
container_start_page |
337 |
op_container_end_page |
343 |
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